Sample records for administration climate prediction

  1. Climate Prediction Center - Atlantic Hurricane Outlook

    Science.gov Websites

    Weather Service NWS logo - Click to go to the NWS home page Climate Prediction Center Home Site Map News ; Seasonal Climate Summary Archive The 2018 Atlantic hurricane season outlook is an official product of the National Oceanic and Atmospheric Administration (NOAA) Climate Prediction Center (CPC). The outlook is

  2. Climate Prediction Center - Expert Assessments: East Pacific Hurricane

    Science.gov Websites

    influence seasonal eastern Pacific hurricane activity, along with climate model forecasts. The outlook also National Weather Service NWS logo - Click to go to the NWS home page Climate Prediction Center Site Map Administration (NOAA) Climate Prediction Center (CPC), and is produced in collaboration with scientists from the

  3. ADMINISTRATIVE CLIMATE.

    ERIC Educational Resources Information Center

    BRUCE, ROBERT L.; CARTER, G.L., JR.

    IN THE COOPERATIVE EXTENSION SERVICE, STYLES OF LEADERSHIP PROFOUNDLY AFFECT THE QUALITY OF THE SERVICE RENDERED. ACCORDINGLY, MAJOR INFLUENCES ON ADMINISTRATIVE CLIMATE AND EMPLOYEE PRODUCTIVITY ARE EXAMINED IN ESSAYS ON (1) SOURCES OF JOB SATISFACTION AND DISSATISFACTION, (2) MOTIVATIONAL THEORIES BASED ON JOB-RELATED SATISFACTIONS AND NEEDS,…

  4. Administrative, Faculty, and Staff Perceptions of Organizational Climate and Commitment in Christian Higher Education

    ERIC Educational Resources Information Center

    Thomas, John Charles

    2008-01-01

    Findings of 957 surveyed employees from four evangelical higher education institutions found a negative correlation for climate and commitment and staff members. Administrators were found to have a more favorable view of their institutional climate than staff. Employee age, tenure, and classification had predictive value for organizational…

  5. Climate Prediction Center

    Science.gov Websites

    Climate Stratosphere Pacific Islands International Desks Climate.gov Climate Test Bed (CTB) JAWF USAID FEWS-NET NWS / NCEP Aviation Weather Center Climate Prediction Center Environmental Modeling Center non-operational server hosts the redesigned web pages developed, thus far, as part of the Climate

  6. Climate Prediction - NOAA's National Weather Service

    Science.gov Websites

    Statistical Models... MOS Prod GFS-LAMP Prod Climate Past Weather Predictions Weather Safety Weather Radio National Weather Service on FaceBook NWS on Facebook NWS Director Home > Climate > Predictions Climate Prediction Long range forecasts across the U.S. Climate Prediction Web Sites Climate Prediction

  7. Drought Predictability and Prediction in a Changing Climate: Assessing Current Predictive Knowledge and Capabilities, User Requirements and Research Priorities

    NASA Technical Reports Server (NTRS)

    Schubert, Siegfried

    2011-01-01

    Drought is fundamentally the result of an extended period of reduced precipitation lasting anywhere from a few weeks to decades and even longer. As such, addressing drought predictability and prediction in a changing climate requires foremost that we make progress on the ability to predict precipitation anomalies on subseasonal and longer time scales. From the perspective of the users of drought forecasts and information, drought is however most directly viewed through its impacts (e.g., on soil moisture, streamflow, crop yields). As such, the question of the predictability of drought must extend to those quantities as well. In order to make progress on these issues, the WCRP drought information group (DIG), with the support of WCRP, the Catalan Institute of Climate Sciences, the La Caixa Foundation, the National Aeronautics and Space Administration, the National Oceanic and Atmospheric Administration, and the National Science Foundation, has organized a workshop to focus on: 1. User requirements for drought prediction information on sub-seasonal to centennial time scales 2. Current understanding of the mechanisms and predictability of drought on sub-seasonal to centennial time scales 3. Current drought prediction/projection capabilities on sub-seasonal to centennial time scales 4. Advancing regional drought prediction capabilities for variables and scales most relevant to user needs on sub-seasonal to centennial time scales. This introductory talk provides an overview of these goals, and outlines the occurrence and mechanisms of drought world-wide.

  8. Climate Prediction Center - Outlooks

    Science.gov Websites

    Weather Service NWS logo - Click to go to the NWS home page Climate Prediction Center Home Site Map News Web resources and services. HOME > Outreach > Publications > Climate Diagnostics Bulletin Climate Diagnostics Bulletin - Tropics Climate Diagnostics Bulletin - Forecast Climate Diagnostics

  9. Climate Prediction Center - Outlooks

    Science.gov Websites

    Weather Service NWS logo - Click to go to the NWS home page Climate Prediction Center Home Site Map News Web resources and services. Climate Diagnostics Bulletin Climate Diagnostics Bulletin - Home Climate Diagnostics Bulletin - Tropics Climate Diagnostics Bulletin - Extratropics About the Forecast Forum ENSO

  10. Climate Prediction Center - The ENSO Cycle

    Science.gov Websites

    Weather Service NWS logo - Click to go to the NWS home page Climate Prediction Center Home Site Map News Web resources and services. HOME > El Niño/La Niña > The ENSO Cycle ENSO Cycle Banner Climate for Weather and Climate Prediction Climate Prediction Center 5830 University Research Court College

  11. On climate prediction: how much can we expect from climate memory?

    NASA Astrophysics Data System (ADS)

    Yuan, Naiming; Huang, Yan; Duan, Jianping; Zhu, Congwen; Xoplaki, Elena; Luterbacher, Jürg

    2018-03-01

    Slowing variability in climate system is an important source of climate predictability. However, it is still challenging for current dynamical models to fully capture the variability as well as its impacts on future climate. In this study, instead of simulating the internal multi-scale oscillations in dynamical models, we discussed the effects of internal variability in terms of climate memory. By decomposing climate state x(t) at a certain time point t into memory part M(t) and non-memory part ɛ (t) , climate memory effects from the past 30 years on climate prediction are quantified. For variables with strong climate memory, high variance (over 20% ) in x(t) is explained by the memory part M(t), and the effects of climate memory are non-negligible for most climate variables, but the precipitation. Regarding of multi-steps climate prediction, a power law decay of the explained variance was found, indicating long-lasting climate memory effects. The explained variances by climate memory can remain to be higher than 10% for more than 10 time steps. Accordingly, past climate conditions can affect both short (monthly) and long-term (interannual, decadal, or even multidecadal) climate predictions. With the memory part M(t) precisely calculated from Fractional Integral Statistical Model, one only needs to focus on the non-memory part ɛ (t) , which is an important quantity that determines climate predictive skills.

  12. Decadal climate prediction (project GCEP).

    PubMed

    Haines, Keith; Hermanson, Leon; Liu, Chunlei; Putt, Debbie; Sutton, Rowan; Iwi, Alan; Smith, Doug

    2009-03-13

    Decadal prediction uses climate models forced by changing greenhouse gases, as in the International Panel for Climate Change, but unlike longer range predictions they also require initialization with observations of the current climate. In particular, the upper-ocean heat content and circulation have a critical influence. Decadal prediction is still in its infancy and there is an urgent need to understand the important processes that determine predictability on these timescales. We have taken the first Hadley Centre Decadal Prediction System (DePreSys) and implemented it on several NERC institute compute clusters in order to study a wider range of initial condition impacts on decadal forecasting, eventually including the state of the land and cryosphere. The eScience methods are used to manage submission and output from the many ensemble model runs required to assess predictive skill. Early results suggest initial condition skill may extend for several years, even over land areas, but this depends sensitively on the definition used to measure skill, and alternatives are presented. The Grid for Coupled Ensemble Prediction (GCEP) system will allow the UK academic community to contribute to international experiments being planned to explore decadal climate predictability.

  13. Concordance Between Administrator and Clinician Ratings of Organizational Culture and Climate.

    PubMed

    Beidas, Rinad S; Williams, Nathaniel J; Green, Philip D; Aarons, Gregory A; Becker-Haimes, Emily M; Evans, Arthur C; Rubin, Ronnie; Adams, Danielle R; Marcus, Steven C

    2018-01-01

    Organizational culture and climate are important determinants of behavioral health service delivery for youth. The Organizational Social Context measure is a well validated assessment of organizational culture and climate that has been developed and extensively used in public sector behavioral health service settings. The degree of concordance between administrators and clinicians in their reports of organizational culture and climate may have implications for research design, inferences, and organizational intervention. However, the extent to which administrators' and clinicians' reports demonstrate concordance is just beginning to garner attention in public behavioral health settings in the United States. We investigated the concordance between 73 administrators (i.e., supervisors, clinical directors, and executive directors) and 247 clinicians in 28 child-serving programs in a public behavioral health system. Findings suggest that administrators, compared to clinicians, reported more positive cultures and climates. Organizational size moderated this relationship such that administrators in small programs (<466 youth clients served annually) provided more congruent reports of culture and climate in contrast to administrators in large programs (≥466 youth clients served annually) who reported more positive cultures and climates than clinicians. We propose a research agenda that examines the effect of concordance between administrators and clinicians on organizational outcomes in public behavioral health service settings.

  14. Development of a Climate Prediction Market

    NASA Astrophysics Data System (ADS)

    Roulston, M. S.

    2017-12-01

    Winton, a global investment firm, is planning to establish a prediction market for climate. This prediction market will allow participants to place bets on global climate up to several decades in the future. Winton is pursuing this endeavour as part of its philanthropy that funds scientific research and the communication of scientific ideas. The Winton Climate Prediction Market will be based in the U.K. It will be structured as an online gambling site subject to the regulation of the Gambling Commission. Unlike existing betting sites, the Climate Prediction Market will be subsidized: a central market maker will inject money into the market. This is in contrast to traditional bookmakers or betting exchanges who set odds in their favour or charge commissions to make a profit. The philosophy of a subsidized prediction market is that the party seeking information should fund the market, rather than the participants who provide the information. The initial market will allow bets to be placed on the atmospheric concentration of carbon dioxide and the global mean temperature anomaly. It will thus produce implied forecasts of carbon dioxide concentration as well as global temperatures. If the initial market is successful, additional markets could be added which target other climate variables, such as regional temperatures or sea-level rise. These markets could be sponsored by organizations that are interested in predictions of the specific climate variables. An online platform for the Climate Prediction Market has been developed and has been tested internally at Winton.

  15. Do We Need Better Climate Predictions to Adapt to a Changing Climate? (Invited)

    NASA Astrophysics Data System (ADS)

    Dessai, S.; Hulme, M.; Lempert, R.; Pielke, R., Jr.

    2009-12-01

    Based on a series of international scientific assessments, climate change has been presented to society as a major problem that needs urgently to be tackled. The science that underpins these assessments has been pre-dominantly from the realm of the natural sciences and central to this framing have been ‘projections’ of future climate change (and its impacts on environment and society) under various greenhouse gas emissions scenarios and using a variety of climate model predictions with embedded assumptions. Central to much of the discussion surrounding adaptation to climate change is the claim - explicit or implicit - that decision makers need accurate and increasingly precise assessments of future impacts of climate change in order to adapt successfully. If true, this claim places a high premium on accurate and precise climate predictions at a range of geographical and temporal scales; such predictions therefore become indispensable, and indeed a prerequisite for, effective adaptation decision-making. But is effective adaptation tied to the ability of the scientific enterprise to predict future climate with accuracy and precision? If so, this may impose a serious and intractable limit on adaptation. This paper proceeds in three sections. It first gathers evidence of claims that climate prediction is necessary for adaptation decision-making. This evidence is drawn from peer-reviewed literature and from published science funding strategies and government policy in a number of different countries. The second part discusses the challenges of climate prediction and why science will consistently be unable to provide accurate and precise predictions of future climate relevant for adaptation (usually at the local/regional level). Section three discusses whether these limits to future foresight represent a limit to adaptation, arguing that effective adaptation need not be limited by a general inability to predict future climate. Given the deep uncertainties involved in

  16. Climate Prediction Center - Outlooks: CFS Forecast of Seasonal Climate

    Science.gov Websites

    National Weather Service NWS logo - Click to go to the NWS home page Climate Prediction Center Home Site government Web resources and services. CFS Seasonal Climate Forecasts CFS Forecast of Seasonal Climate discontinued after October 2012. This page displays seasonal climate anomalies from the NCEP coupled forecast

  17. Climate Prediction Center - Outlooks: Current UV Index Forecast Map

    Science.gov Websites

    Weather Service NWS logo - Click to go to the NWS home page Climate Prediction Center Home Site Map News Service NOAA Center for Weather and Climate Prediction Climate Prediction Center 5830 University Research Court College Park, Maryland 20740 Page Author: Climate Prediction Center Internet Team Disclaimer

  18. Detecting failure of climate predictions

    USGS Publications Warehouse

    Runge, Michael C.; Stroeve, Julienne C.; Barrett, Andrew P.; McDonald-Madden, Eve

    2016-01-01

    The practical consequences of climate change challenge society to formulate responses that are more suited to achieving long-term objectives, even if those responses have to be made in the face of uncertainty1, 2. Such a decision-analytic focus uses the products of climate science as probabilistic predictions about the effects of management policies3. Here we present methods to detect when climate predictions are failing to capture the system dynamics. For a single model, we measure goodness of fit based on the empirical distribution function, and define failure when the distribution of observed values significantly diverges from the modelled distribution. For a set of models, the same statistic can be used to provide relative weights for the individual models, and we define failure when there is no linear weighting of the ensemble models that produces a satisfactory match to the observations. Early detection of failure of a set of predictions is important for improving model predictions and the decisions based on them. We show that these methods would have detected a range shift in northern pintail 20 years before it was actually discovered, and are increasingly giving more weight to those climate models that forecast a September ice-free Arctic by 2055.

  19. Are abrupt climate changes predictable?

    NASA Astrophysics Data System (ADS)

    Ditlevsen, Peter

    2013-04-01

    It is taken for granted that the limited predictability in the initial value problem, the weather prediction, and the predictability of the statistics are two distinct problems. Lorenz (1975) dubbed this predictability of the first and the second kind respectively. Predictability of the first kind in a chaotic dynamical system is limited due to the well-known critical dependence on initial conditions. Predictability of the second kind is possible in an ergodic system, where either the dynamics is known and the phase space attractor can be characterized by simulation or the system can be observed for such long times that the statistics can be obtained from temporal averaging, assuming that the attractor does not change in time. For the climate system the distinction between predictability of the first and the second kind is fuzzy. This difficulty in distinction between predictability of the first and of the second kind is related to the lack of scale separation between fast and slow components of the climate system. The non-linear nature of the problem furthermore opens the possibility of multiple attractors, or multiple quasi-steady states. As the ice-core records show, the climate has been jumping between different quasi-stationary climates, stadials and interstadials through the Dansgaard-Oechger events. Such a jump happens very fast when a critical tipping point has been reached. The question is: Can such a tipping point be predicted? This is a new kind of predictability: the third kind. If the tipping point is reached through a bifurcation, where the stability of the system is governed by some control parameter, changing in a predictable way to a critical value, the tipping is predictable. If the sudden jump occurs because internal chaotic fluctuations, noise, push the system across a barrier, the tipping is as unpredictable as the triggering noise. In order to hint at an answer to this question, a careful analysis of the high temporal resolution NGRIP isotope

  20. Climate Prediction Center - Monitoring & Data: Seasonal ENSO Impacts on

    Science.gov Websites

    page National Weather Service NWS logo - Click to go to the NWS home page Climate Prediction Center , state and local government Web resources and services. HOME > Monitoring and Data > U.S. Climate and Climate Prediction Climate Prediction Center 5830 University Research Court College Park, Maryland

  1. Climate Prediction Center - Expert Assessments Index

    Science.gov Websites

    Weather Service NWS logo - Click to go to the NWS home page Climate Prediction Center Home Site Map News Web resources and services. HOME > Monitoring and Data > Global Climate Data & Maps > ; Global Regional Climate Maps Regional Climate Maps Banner The Monthly regional analyses products are

  2. Assessing effects of variation in global climate data sets on spatial predictions from climate envelope models

    USGS Publications Warehouse

    Romañach, Stephanie; Watling, James I.; Fletcher, Robert J.; Speroterra, Carolina; Bucklin, David N.; Brandt, Laura A.; Pearlstine, Leonard G.; Escribano, Yesenia; Mazzotti, Frank J.

    2014-01-01

    Climate change poses new challenges for natural resource managers. Predictive modeling of species–environment relationships using climate envelope models can enhance our understanding of climate change effects on biodiversity, assist in assessment of invasion risk by exotic organisms, and inform life-history understanding of individual species. While increasing interest has focused on the role of uncertainty in future conditions on model predictions, models also may be sensitive to the initial conditions on which they are trained. Although climate envelope models are usually trained using data on contemporary climate, we lack systematic comparisons of model performance and predictions across alternative climate data sets available for model training. Here, we seek to fill that gap by comparing variability in predictions between two contemporary climate data sets to variability in spatial predictions among three alternative projections of future climate. Overall, correlations between monthly temperature and precipitation variables were very high for both contemporary and future data. Model performance varied across algorithms, but not between two alternative contemporary climate data sets. Spatial predictions varied more among alternative general-circulation models describing future climate conditions than between contemporary climate data sets. However, we did find that climate envelope models with low Cohen's kappa scores made more discrepant spatial predictions between climate data sets for the contemporary period than did models with high Cohen's kappa scores. We suggest conservation planners evaluate multiple performance metrics and be aware of the importance of differences in initial conditions for spatial predictions from climate envelope models.

  3. Using simple chaotic models to interpret climate under climate change: Implications for probabilistic climate prediction

    NASA Astrophysics Data System (ADS)

    Daron, Joseph

    2010-05-01

    Exploring the reliability of model based projections is an important pre-cursor to evaluating their societal relevance. In order to better inform decisions concerning adaptation (and mitigation) to climate change, we must investigate whether or not our models are capable of replicating the dynamic nature of the climate system. Whilst uncertainty is inherent within climate prediction, establishing and communicating what is plausible as opposed to what is likely is the first step to ensuring that climate sensitive systems are robust to climate change. Climate prediction centers are moving towards probabilistic projections of climate change at regional and local scales (Murphy et al., 2009). It is therefore important to understand what a probabilistic forecast means for a chaotic nonlinear dynamic system that is subject to changing forcings. It is in this context that we present the results of experiments using simple models that can be considered analogous to the more complex climate system, namely the Lorenz 1963 and Lorenz 1984 models (Lorenz, 1963; Lorenz, 1984). Whilst the search for a low-dimensional climate attractor remains illusive (Fraedrich, 1986; Sahay and Sreenivasan, 1996) the characterization of the climate system in such terms can be useful for conceptual and computational simplicity. Recognising that a change in climate is manifest in a change in the distribution of a particular climate variable (Stainforth et al., 2007), we first establish the equilibrium distributions of the Lorenz systems for certain parameter settings. Allowing the parameters to vary in time, we investigate the dependency of such distributions to initial conditions and discuss the implications for climate prediction. We argue that the role of chaos and nonlinear dynamic behaviour ought to have more prominence in the discussion of the forecasting capabilities in climate prediction. References: Fraedrich, K. Estimating the dimensions of weather and climate attractors. J. Atmos. Sci

  4. Enhancing seasonal climate prediction capacity for the Pacific countries

    NASA Astrophysics Data System (ADS)

    Kuleshov, Y.; Jones, D.; Hendon, H.; Charles, A.; Cottrill, A.; Lim, E.-P.; Langford, S.; de Wit, R.; Shelton, K.

    2012-04-01

    Seasonal and inter-annual climate variability is a major factor in determining the vulnerability of many Pacific Island Countries to climate change and there is need to improve weekly to seasonal range climate prediction capabilities beyond what is currently available from statistical models. In the seasonal climate prediction project under the Australian Government's Pacific Adaptation Strategy Assistance Program (PASAP), we describe a comprehensive project to strengthen the climate prediction capacities in National Meteorological Services in 14 Pacific Island Countries and East Timor. The intent is particularly to reduce the vulnerability of current services to a changing climate, and improve the overall level of information available assist with managing climate variability. Statistical models cannot account for aspects of climate variability and change that are not represented in the historical record. In contrast, dynamical physics-based models implicitly include the effects of a changing climate whatever its character or cause and can predict outcomes not seen previously. The transition from a statistical to a dynamical prediction system provides more valuable and applicable climate information to a wide range of climate sensitive sectors throughout the countries of the Pacific region. In this project, we have developed seasonal climate outlooks which are based upon the current dynamical model POAMA (Predictive Ocean-Atmosphere Model for Australia) seasonal forecast system. At present, meteorological services of the Pacific Island Countries largely employ statistical models for seasonal outlooks. Outcomes of the PASAP project enhanced capabilities of the Pacific Island Countries in seasonal prediction providing National Meteorological Services with an additional tool to analyse meteorological variables such as sea surface temperatures, air temperature, pressure and rainfall using POAMA outputs and prepare more accurate seasonal climate outlooks.

  5. Decadal climate predictions improved by ocean ensemble dispersion filtering

    NASA Astrophysics Data System (ADS)

    Kadow, C.; Illing, S.; Kröner, I.; Ulbrich, U.; Cubasch, U.

    2017-06-01

    Decadal predictions by Earth system models aim to capture the state and phase of the climate several years in advance. Atmosphere-ocean interaction plays an important role for such climate forecasts. While short-term weather forecasts represent an initial value problem and long-term climate projections represent a boundary condition problem, the decadal climate prediction falls in-between these two time scales. In recent years, more precise initialization techniques of coupled Earth system models and increased ensemble sizes have improved decadal predictions. However, climate models in general start losing the initialized signal and its predictive skill from one forecast year to the next. Here we show that the climate prediction skill of an Earth system model can be improved by a shift of the ocean state toward the ensemble mean of its individual members at seasonal intervals. We found that this procedure, called ensemble dispersion filter, results in more accurate results than the standard decadal prediction. Global mean and regional temperature, precipitation, and winter cyclone predictions show an increased skill up to 5 years ahead. Furthermore, the novel technique outperforms predictions with larger ensembles and higher resolution. Our results demonstrate how decadal climate predictions benefit from ocean ensemble dispersion filtering toward the ensemble mean.Plain Language SummaryDecadal <span class="hlt">predictions</span> aim to <span class="hlt">predict</span> the <span class="hlt">climate</span> several years in advance. Atmosphere-ocean interaction plays an important role for such <span class="hlt">climate</span> forecasts. The ocean memory due to its heat capacity holds big potential skill. In recent years, more precise initialization techniques of coupled Earth system models (incl. atmosphere and ocean) have improved decadal <span class="hlt">predictions</span>. Ensembles are another important aspect. Applying slightly perturbed <span class="hlt">predictions</span> to trigger the famous butterfly effect results in an ensemble. Instead of evaluating one</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFM.A23G0302K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFM.A23G0302K"><span>Data-driven <span class="hlt">Climate</span> Modeling and <span class="hlt">Prediction</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Kondrashov, D. A.; Chekroun, M.</p> <p>2016-12-01</p> <p>Global <span class="hlt">climate</span> models aim to simulate a broad range of spatio-temporal scales of <span class="hlt">climate</span> variability with state vector having many millions of degrees of freedom. On the other hand, while detailed weather <span class="hlt">prediction</span> out to a few days requires high numerical resolution, it is fairly clear that a major fraction of large-scale <span class="hlt">climate</span> variability can be <span class="hlt">predicted</span> in a much lower-dimensional phase space. Low-dimensional models can simulate and <span class="hlt">predict</span> this fraction of <span class="hlt">climate</span> variability, provided they are able to account for linear and nonlinear interactions between the modes representing large scales of <span class="hlt">climate</span> dynamics, as well as their interactions with a much larger number of modes representing fast and small scales. This presentation will highlight several new applications by Multilayered Stochastic Modeling (MSM) [Kondrashov, Chekroun and Ghil, 2015] framework that has abundantly proven its efficiency in the modeling and real-time forecasting of various <span class="hlt">climate</span> phenomena. MSM is a data-driven inverse modeling technique that aims to obtain a low-order nonlinear system of prognostic equations driven by stochastic forcing, and estimates both the dynamical operator and the properties of the driving noise from multivariate time series of observations or a high-end model's simulation. MSM leads to a system of stochastic differential equations (SDEs) involving hidden (auxiliary) variables of fast-small scales ranked by layers, which interact with the macroscopic (observed) variables of large-slow scales to model the dynamics of the latter, and thus convey memory effects. New MSM <span class="hlt">climate</span> applications focus on development of computationally efficient low-order models by using data-adaptive decomposition methods that convey memory effects by time-embedding techniques, such as Multichannel Singular Spectrum Analysis (M-SSA) [Ghil et al. 2002] and recently developed Data-Adaptive Harmonic (DAH) decomposition method [Chekroun and Kondrashov, 2016]. In particular, new results</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/8985005','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/8985005"><span><span class="hlt">Predictability</span> of North Atlantic Multidecadal <span class="hlt">Climate</span> Variability</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Griffies; Bryan</p> <p>1997-01-10</p> <p>Atmospheric weather systems become unpredictable beyond a few weeks, but <span class="hlt">climate</span> variations can be <span class="hlt">predictable</span> over much longer periods because of the coupling of the ocean and atmosphere. With the use of a global coupled ocean-atmosphere model, it is shown that the North Atlantic may have <span class="hlt">climatic</span> <span class="hlt">predictability</span> on the order of a decade or longer. These results suggest that variations of the dominant multidecadal sea surface temperature patterns in the North Atlantic, which have been associated with changes in <span class="hlt">climate</span> over Eurasia, can be <span class="hlt">predicted</span> if an adequate and sustainable system for monitoring the Atlantic Ocean exists.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.cpc.ncep.noaa.gov/products/predictions/30day','SCIGOVWS'); return false;" href="http://www.cpc.ncep.noaa.gov/products/predictions/30day"><span><span class="hlt">Climate</span> <span class="hlt">Prediction</span> Center - monthly Outlook</span></a></p> <p><a target="_blank" href="http://www.science.gov/aboutsearch.html">Science.gov Websites</a></p> <p></p> <p></p> <p>Weather Service NWS logo - Click to go to the NWS home page <em><span class="hlt">Climate</span></em> <span class="hlt">Prediction</span> Center Site Map News Outlooks monthly <em><span class="hlt">Climate</span></em> Outlooks Banner OFFICIAL Forecasts June 2018 [UPDATED MONTHLY FORECASTS SERVICE <em>CHANGE</em> NOTICE] [EXPERIMENTAL TWO-CLASS SEASONAL FORECASTS] Text-Format Discussions Monthly Long Lead 30</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.cpc.ncep.noaa.gov/products/monitoring_and_data','SCIGOVWS'); return false;" href="http://www.cpc.ncep.noaa.gov/products/monitoring_and_data"><span><span class="hlt">Climate</span> <span class="hlt">Prediction</span> Center - Monitoring and Data</span></a></p> <p><a target="_blank" href="http://www.science.gov/aboutsearch.html">Science.gov Websites</a></p> <p></p> <p></p> <p>Weather Service NWS logo - Click to go to the NWS home page <em><span class="hlt">Climate</span></em> <span class="hlt">Prediction</span> Center Home Site Map News monthly data, time series, and maps for various <em><span class="hlt">climate</span></em> parameters, such as precipitation, temperature Oscillations (ENSO) and other <em><span class="hlt">climate</span></em> patterns such as the North Atlantic and Pacific Decadal Oscillations, and</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017Chaos..27l6902K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017Chaos..27l6902K"><span>Ocean eddies and <span class="hlt">climate</span> <span class="hlt">predictability</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Kirtman, Ben P.; Perlin, Natalie; Siqueira, Leo</p> <p>2017-12-01</p> <p>A suite of coupled <span class="hlt">climate</span> model simulations and experiments are used to examine how resolved mesoscale ocean features affect aspects of <span class="hlt">climate</span> variability, air-sea interactions, and <span class="hlt">predictability</span>. In combination with control simulations, experiments with the interactive ensemble coupling strategy are used to further amplify the role of the oceanic mesoscale field and the associated air-sea feedbacks and <span class="hlt">predictability</span>. The basic intent of the interactive ensemble coupling strategy is to reduce the atmospheric noise at the air-sea interface, allowing an assessment of how noise affects the variability, and in this case, it is also used to diagnose <span class="hlt">predictability</span> from the perspective of signal-to-noise ratios. The <span class="hlt">climate</span> variability is assessed from the perspective of sea surface temperature (SST) variance ratios, and it is shown that, unsurprisingly, mesoscale variability significantly increases SST variance. Perhaps surprising is the fact that the presence of mesoscale ocean features even further enhances the SST variance in the interactive ensemble simulation beyond what would be expected from simple linear arguments. Changes in the air-sea coupling between simulations are assessed using pointwise convective rainfall-SST and convective rainfall-SST tendency correlations and again emphasize how the oceanic mesoscale alters the local association between convective rainfall and SST. Understanding the possible relationships between the SST-forced signal and the weather noise is critically important in <span class="hlt">climate</span> <span class="hlt">predictability</span>. We use the interactive ensemble simulations to diagnose this relationship, and we find that the presence of mesoscale ocean features significantly enhances this link particularly in ocean eddy rich regions. Finally, we use signal-to-noise ratios to show that the ocean mesoscale activity increases model estimated <span class="hlt">predictability</span> in terms of convective precipitation and atmospheric upper tropospheric circulation.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29289056','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29289056"><span>Ocean eddies and <span class="hlt">climate</span> <span class="hlt">predictability</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Kirtman, Ben P; Perlin, Natalie; Siqueira, Leo</p> <p>2017-12-01</p> <p>A suite of coupled <span class="hlt">climate</span> model simulations and experiments are used to examine how resolved mesoscale ocean features affect aspects of <span class="hlt">climate</span> variability, air-sea interactions, and <span class="hlt">predictability</span>. In combination with control simulations, experiments with the interactive ensemble coupling strategy are used to further amplify the role of the oceanic mesoscale field and the associated air-sea feedbacks and <span class="hlt">predictability</span>. The basic intent of the interactive ensemble coupling strategy is to reduce the atmospheric noise at the air-sea interface, allowing an assessment of how noise affects the variability, and in this case, it is also used to diagnose <span class="hlt">predictability</span> from the perspective of signal-to-noise ratios. The <span class="hlt">climate</span> variability is assessed from the perspective of sea surface temperature (SST) variance ratios, and it is shown that, unsurprisingly, mesoscale variability significantly increases SST variance. Perhaps surprising is the fact that the presence of mesoscale ocean features even further enhances the SST variance in the interactive ensemble simulation beyond what would be expected from simple linear arguments. Changes in the air-sea coupling between simulations are assessed using pointwise convective rainfall-SST and convective rainfall-SST tendency correlations and again emphasize how the oceanic mesoscale alters the local association between convective rainfall and SST. Understanding the possible relationships between the SST-forced signal and the weather noise is critically important in <span class="hlt">climate</span> <span class="hlt">predictability</span>. We use the interactive ensemble simulations to diagnose this relationship, and we find that the presence of mesoscale ocean features significantly enhances this link particularly in ocean eddy rich regions. Finally, we use signal-to-noise ratios to show that the ocean mesoscale activity increases model estimated <span class="hlt">predictability</span> in terms of convective precipitation and atmospheric upper tropospheric circulation.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.cpc.ncep.noaa.gov/products/MD_index.shtml','SCIGOVWS'); return false;" href="http://www.cpc.ncep.noaa.gov/products/MD_index.shtml"><span><span class="hlt">Climate</span> <span class="hlt">Prediction</span> Center - Monitoring and Data Index</span></a></p> <p><a target="_blank" href="http://www.science.gov/aboutsearch.html">Science.gov Websites</a></p> <p></p> <p></p> <p>Weather Service NWS logo - Click to go to the NWS home page <em><span class="hlt">Climate</span></em> <span class="hlt">Prediction</span> Center Home Site Map News ; Atmospheric Monitoring and Data Monitoring Weather & <em><span class="hlt">Climate</span></em> in Realtime <em><span class="hlt">Climate</span></em> Diagnostics Bulletin Preliminary <em><span class="hlt">Climate</span></em> Diagnostics Bulletin Figures Monthly Atmospheric & Sea Surface Temperature Indices</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.cpc.ncep.noaa.gov/products/GODAS/background.shtml','SCIGOVWS'); return false;" href="http://www.cpc.ncep.noaa.gov/products/GODAS/background.shtml"><span><span class="hlt">Climate</span> <span class="hlt">Prediction</span> Center - NCEP Global Ocean Data Assimilation System:</span></a></p> <p><a target="_blank" href="http://www.science.gov/aboutsearch.html">Science.gov Websites</a></p> <p></p> <p></p> <p>home page National Weather Service NWS logo - Click to go to the NWS home page <em><span class="hlt">Climate</span></em> <span class="hlt">Prediction</span> Monthly in NetCDF Other formats Links NOAA Ocean <em><span class="hlt">Climate</span></em> Observation Program (OCO) <em><span class="hlt">Climate</span></em> Test Bed About <span class="hlt">Prediction</span> (NCEP) are a valuable community asset for monitoring different aspects of ocean <em><span class="hlt">climate</span></em></p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://wwwpaztcn.wr.usgs.gov/julio_pdf/Pau_etal_2011.pdf','USGSPUBS'); return false;" href="http://wwwpaztcn.wr.usgs.gov/julio_pdf/Pau_etal_2011.pdf"><span><span class="hlt">Predicting</span> phenology by integrating ecology, evolution and <span class="hlt">climate</span> science</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Pau, Stephanie; Wolkovich, Elizabeth M.; Cook, Benjamin I.; Davies, T. Jonathan; Kraft, Nathan J.B.; Bolmgren, Kjell; Betancourt, Julio L.; Cleland, Elsa E.</p> <p>2011-01-01</p> <p>Forecasting how species and ecosystems will respond to <span class="hlt">climate</span> change has been a major aim of ecology in recent years. Much of this research has focused on phenology — the timing of life-history events. Phenology has well-demonstrated links to <span class="hlt">climate</span>, from genetic to landscape scales; yet our ability to explain and <span class="hlt">predict</span> variation in phenology across species, habitats and time remains poor. Here, we outline how merging approaches from ecology, <span class="hlt">climate</span> science and evolutionary biology can advance research on phenological responses to <span class="hlt">climate</span> variability. Using insight into seasonal and interannual <span class="hlt">climate</span> variability combined with niche theory and community phylogenetics, we develop a <span class="hlt">predictive</span> approach for species' reponses to changing <span class="hlt">climate</span>. Our approach <span class="hlt">predicts</span> that species occupying higher latitudes or the early growing season should be most sensitive to <span class="hlt">climate</span> and have the most phylogenetically conserved phenologies. We further <span class="hlt">predict</span> that temperate species will respond to <span class="hlt">climate</span> change by shifting in time, while tropical species will respond by shifting space, or by evolving. Although we focus here on plant phenology, our approach is broadly applicable to ecological research of plant responses to <span class="hlt">climate</span> variability.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3270390','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3270390"><span>Uncertainty in weather and <span class="hlt">climate</span> <span class="hlt">prediction</span></span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Slingo, Julia; Palmer, Tim</p> <p>2011-01-01</p> <p>Following Lorenz's seminal work on chaos theory in the 1960s, probabilistic approaches to <span class="hlt">prediction</span> have come to dominate the science of weather and <span class="hlt">climate</span> forecasting. This paper gives a perspective on Lorenz's work and how it has influenced the ways in which we seek to represent uncertainty in forecasts on all lead times from hours to decades. It looks at how model uncertainty has been represented in probabilistic <span class="hlt">prediction</span> systems and considers the challenges posed by a changing <span class="hlt">climate</span>. Finally, the paper considers how the uncertainty in projections of <span class="hlt">climate</span> change can be addressed to deliver more reliable and confident assessments that support decision-making on adaptation and mitigation. PMID:22042896</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFM.A24D..02Y','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFM.A24D..02Y"><span>Decadal <span class="hlt">climate</span> <span class="hlt">prediction</span> in the large ensemble limit</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Yeager, S. G.; Rosenbloom, N. A.; Strand, G.; Lindsay, K. T.; Danabasoglu, G.; Karspeck, A. R.; Bates, S. C.; Meehl, G. A.</p> <p>2017-12-01</p> <p>In order to quantify the benefits of initialization for <span class="hlt">climate</span> <span class="hlt">prediction</span> on decadal timescales, two parallel sets of historical simulations are required: one "initialized" ensemble that incorporates observations of past <span class="hlt">climate</span> states and one "uninitialized" ensemble whose internal <span class="hlt">climate</span> variations evolve freely and without synchronicity. In the large ensemble limit, ensemble averaging isolates potentially <span class="hlt">predictable</span> forced and internal variance components in the "initialized" set, but only the forced variance remains after averaging the "uninitialized" set. The ensemble size needed to achieve this variance decomposition, and to robustly distinguish initialized from uninitialized decadal <span class="hlt">predictions</span>, remains poorly constrained. We examine a large ensemble (LE) of initialized decadal <span class="hlt">prediction</span> (DP) experiments carried out using the Community Earth System Model (CESM). This 40-member CESM-DP-LE set of experiments represents the "initialized" complement to the CESM large ensemble of 20th century runs (CESM-LE) documented in Kay et al. (2015). Both simulation sets share the same model configuration, historical radiative forcings, and large ensemble sizes. The twin experiments afford an unprecedented opportunity to explore the sensitivity of DP skill assessment, and in particular the skill enhancement associated with initialization, to ensemble size. This talk will highlight the benefits of a large ensemble size for initialized <span class="hlt">predictions</span> of seasonal <span class="hlt">climate</span> over land in the Atlantic sector as well as <span class="hlt">predictions</span> of shifts in the likelihood of <span class="hlt">climate</span> extremes that have large societal impact.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFM.A11F0078A','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFM.A11F0078A"><span>A new paradigm for <span class="hlt">predicting</span> zonal-mean <span class="hlt">climate</span> and <span class="hlt">climate</span> change</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Armour, K.; Roe, G.; Donohoe, A.; Siler, N.; Markle, B. R.; Liu, X.; Feldl, N.; Battisti, D. S.; Frierson, D. M.</p> <p>2016-12-01</p> <p>How will the pole-to-equator temperature gradient, or large-scale patterns of precipitation, change under global warming? Answering such questions typically involves numerical simulations with comprehensive general circulation models (GCMs) that represent the complexities of <span class="hlt">climate</span> forcing, radiative feedbacks, and atmosphere and ocean dynamics. Yet, our understanding of these <span class="hlt">predictions</span> hinges on our ability to explain them through the lens of simple models and physical theories. Here we present evidence that zonal-mean <span class="hlt">climate</span>, and its changes, can be understood in terms of a moist energy balance model that represents atmospheric heat transport as a simple diffusion of latent and sensible heat (as a down-gradient transport of moist static energy, with a diffusivity coefficient that is nearly constant with latitude). We show that the theoretical underpinnings of this model derive from the principle of maximum entropy production; that its <span class="hlt">predictions</span> are empirically supported by atmospheric reanalyses; and that it successfully <span class="hlt">predicts</span> the behavior of a hierarchy of <span class="hlt">climate</span> models - from a gray radiation aquaplanet moist GCM, to comprehensive GCMs participating in CMIP5. As an example of the power of this paradigm, we show that, given only patterns of local radiative feedbacks and <span class="hlt">climate</span> forcing, the moist energy balance model accurately <span class="hlt">predicts</span> the evolution of zonal-mean temperature and atmospheric heat transport as simulated by the CMIP5 ensemble. These results suggest that, despite all of its dynamical complexity, the atmosphere essentially responds to energy imbalances by simply diffusing latent and sensible heat down-gradient; this principle appears to explain zonal-mean <span class="hlt">climate</span> and its changes under global warming.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19860004397','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19860004397"><span>Understanding <span class="hlt">climate</span>: A strategy for <span class="hlt">climate</span> modeling and <span class="hlt">predictability</span> research, 1985-1995</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Thiele, O. (Editor); Schiffer, R. A. (Editor)</p> <p>1985-01-01</p> <p>The emphasis of the NASA strategy for <span class="hlt">climate</span> modeling and <span class="hlt">predictability</span> research is on the utilization of space technology to understand the processes which control the Earth's <span class="hlt">climate</span> system and it's sensitivity to natural and man-induced changes and to assess the possibilities for <span class="hlt">climate</span> <span class="hlt">prediction</span> on time scales of from about two weeks to several decades. Because the <span class="hlt">climate</span> is a complex multi-phenomena system, which interacts on a wide range of space and time scales, the diversity of scientific problems addressed requires a hierarchy of models along with the application of modern empirical and statistical techniques which exploit the extensive current and potential future global data sets afforded by space observations. Observing system simulation experiments, exploiting these models and data, will also provide the foundation for the future <span class="hlt">climate</span> space observing system, e.g., Earth observing system (EOS), 1985; Tropical Rainfall Measuring Mission (TRMM) North, et al. NASA, 1984.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFMNH51A0114T','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFMNH51A0114T"><span>Can We Envision a Bettor's Guide to <span class="hlt">Climate</span> <span class="hlt">Prediction</span> Markets?</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Trexler, M.</p> <p>2017-12-01</p> <p>It's one thing to set up a <span class="hlt">climate</span> <span class="hlt">prediction</span> market, it's another to find enough informed traders to make the market work. <span class="hlt">Climate</span> bets could range widely, from purely scientific or atmospheric metrics, to bets that involve the interplay of science, policy, economic, and behavioral outcomes. For a topic as complex and politicized as <span class="hlt">climate</span> change, a Bettor's Guide to <span class="hlt">Climate</span> <span class="hlt">Predictions</span> could substantially expand and diversify the pool of individuals trading in the market, increasing both its liquidity and decision-support value. The <span class="hlt">Climate</span> Web is an on-line and publically accessible Beta version of such a Bettor's Guide, implementing the knowledge management adage: "if only we knew what we know." The <span class="hlt">Climate</span> Web not only curates the key literature, news coverage, and websites relating to more than 100 <span class="hlt">climate</span> topics, from extreme event exceedance curves to <span class="hlt">climate</span> economics to <span class="hlt">climate</span> risk scenarios, it extracts and links together thousands of ideas and graphics across all of those topics. The <span class="hlt">Climate</span> Web integrates the many disciplinary silos that characterize today's often dysfunctional <span class="hlt">climate</span> policy conversations, allowing rapid cross-silo exploration and understanding. As a Bettor's Guide it would allow <span class="hlt">prediction</span> market traders to better research and understand their potential bets, and to quickly survey key thinking and uncertainties relating to those bets. The availability of such a Bettor's Guide to <span class="hlt">Climate</span> <span class="hlt">Predictions</span> should make traders willing to place more bets than they otherwise would, and should facilitate higher quality betting. The presentation will introduce the knowledge management dimensions and challenges of <span class="hlt">climate</span> <span class="hlt">prediction</span> markets, and introduce the <span class="hlt">Climate</span> Web as one solution to those challenges.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://eric.ed.gov/?q=probability+AND+statistical+AND+inference&pg=6&id=EJ992914','ERIC'); return false;" href="https://eric.ed.gov/?q=probability+AND+statistical+AND+inference&pg=6&id=EJ992914"><span><span class="hlt">Administrative</span> <span class="hlt">Climate</span> and Novices' Intent to Remain Teaching</span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Pogodzinski, Ben; Youngs, Peter; Frank, Kenneth A.; Belman, Dale</p> <p>2012-01-01</p> <p>Using survey data from novice teachers at the elementary and middle school level across 11 districts, multilevel logistic regressions were estimated to examine the association between novices' perceptions of the <span class="hlt">administrative</span> <span class="hlt">climate</span> and their desire to remain teaching within their schools. We find that the probability that a novice teacher…</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_1");'>1</a></li> <li class="active"><span>2</span></li> <li><a href="#" onclick='return showDiv("page_3");'>3</a></li> <li><a href="#" onclick='return showDiv("page_4");'>4</a></li> <li><a href="#" onclick='return showDiv("page_5");'>5</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_2 --> <div id="page_3" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_1");'>1</a></li> <li><a href="#" onclick='return showDiv("page_2");'>2</a></li> <li class="active"><span>3</span></li> <li><a href="#" onclick='return showDiv("page_4");'>4</a></li> <li><a href="#" onclick='return showDiv("page_5");'>5</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="41"> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2012-12-13/pdf/2012-30152.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2012-12-13/pdf/2012-30152.pdf"><span>77 FR 74174 - National Oceanic and Atmospheric <span class="hlt">Administration</span> (NOAA) National <span class="hlt">Climate</span> Assessment and...</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2012-12-13</p> <p>... DEPARTMENT OF COMMERCE National Oceanic and Atmospheric <span class="hlt">Administration</span> (NOAA) National <span class="hlt">Climate</span>... NOAA National <span class="hlt">Climate</span> Assessment and Development Advisory Committee (NCADAC). Time and Date: The..., DC 20006. The public will not be able to dial into the call. Please check the National <span class="hlt">Climate</span>...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5481837','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5481837"><span>Skillful <span class="hlt">prediction</span> of northern <span class="hlt">climate</span> provided by the ocean</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Årthun, Marius; Eldevik, Tor; Viste, Ellen; Drange, Helge; Furevik, Tore; Johnson, Helen L.; Keenlyside, Noel S.</p> <p>2017-01-01</p> <p>It is commonly understood that a potential for skillful <span class="hlt">climate</span> <span class="hlt">prediction</span> resides in the ocean. It nevertheless remains unresolved to what extent variable ocean heat is imprinted on the atmosphere to realize its <span class="hlt">predictive</span> potential over land. Here we assess from observations whether anomalous heat in the Gulf Stream's northern extension provides <span class="hlt">predictability</span> of northwestern European and Arctic <span class="hlt">climate</span>. We show that variations in ocean temperature in the high latitude North Atlantic and Nordic Seas are reflected in the <span class="hlt">climate</span> of northwestern Europe and in winter Arctic sea ice extent. Statistical regression models show that a significant part of northern <span class="hlt">climate</span> variability thus can be skillfully <span class="hlt">predicted</span> up to a decade in advance based on the state of the ocean. Particularly, we <span class="hlt">predict</span> that Norwegian air temperature will decrease over the coming years, although staying above the long-term (1981–2010) average. Winter Arctic sea ice extent will remain low but with a general increase towards 2020. PMID:28631732</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017NatCo...815875A','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017NatCo...815875A"><span>Skillful <span class="hlt">prediction</span> of northern <span class="hlt">climate</span> provided by the ocean</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Årthun, Marius; Eldevik, Tor; Viste, Ellen; Drange, Helge; Furevik, Tore; Johnson, Helen L.; Keenlyside, Noel S.</p> <p>2017-06-01</p> <p>It is commonly understood that a potential for skillful <span class="hlt">climate</span> <span class="hlt">prediction</span> resides in the ocean. It nevertheless remains unresolved to what extent variable ocean heat is imprinted on the atmosphere to realize its <span class="hlt">predictive</span> potential over land. Here we assess from observations whether anomalous heat in the Gulf Stream's northern extension provides <span class="hlt">predictability</span> of northwestern European and Arctic <span class="hlt">climate</span>. We show that variations in ocean temperature in the high latitude North Atlantic and Nordic Seas are reflected in the <span class="hlt">climate</span> of northwestern Europe and in winter Arctic sea ice extent. Statistical regression models show that a significant part of northern <span class="hlt">climate</span> variability thus can be skillfully <span class="hlt">predicted</span> up to a decade in advance based on the state of the ocean. Particularly, we <span class="hlt">predict</span> that Norwegian air temperature will decrease over the coming years, although staying above the long-term (1981-2010) average. Winter Arctic sea ice extent will remain low but with a general increase towards 2020.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.cpc.noaa.gov/products/analysis_monitoring/ensostuff/ensofaq.shtml','SCIGOVWS'); return false;" href="http://www.cpc.noaa.gov/products/analysis_monitoring/ensostuff/ensofaq.shtml"><span><span class="hlt">Climate</span> <span class="hlt">Prediction</span> Center - ENSO FAQ</span></a></p> <p><a target="_blank" href="http://www.science.gov/aboutsearch.html">Science.gov Websites</a></p> <p></p> <p></p> <p>Weather Service NWS logo - Click to go to the NWS home page <em><span class="hlt">Climate</span></em> <span class="hlt">Prediction</span> Center Home Site Map News Additional Links General Questions about El Niño and La Niña What is <em><span class="hlt">climate</span></em> variability? What are El Niño . Impacts How do El Niño and La Niña <em>influence</em> the U.S. Winter weather patterns? How do El Niño and La</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/27543682','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/27543682"><span>Genetically informed ecological niche models improve <span class="hlt">climate</span> change <span class="hlt">predictions</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Ikeda, Dana H; Max, Tamara L; Allan, Gerard J; Lau, Matthew K; Shuster, Stephen M; Whitham, Thomas G</p> <p>2017-01-01</p> <p>We examined the hypothesis that ecological niche models (ENMs) more accurately <span class="hlt">predict</span> species distributions when they incorporate information on population genetic structure, and concomitantly, local adaptation. Local adaptation is common in species that span a range of environmental gradients (e.g., soils and <span class="hlt">climate</span>). Moreover, common garden studies have demonstrated a covariance between neutral markers and functional traits associated with a species' ability to adapt to environmental change. We therefore <span class="hlt">predicted</span> that genetically distinct populations would respond differently to <span class="hlt">climate</span> change, resulting in <span class="hlt">predicted</span> distributions with little overlap. To test whether genetic information improves our ability to <span class="hlt">predict</span> a species' niche space, we created genetically informed ecological niche models (gENMs) using Populus fremontii (Salicaceae), a widespread tree species in which prior common garden experiments demonstrate strong evidence for local adaptation. Four major findings emerged: (i) gENMs <span class="hlt">predicted</span> population occurrences with up to 12-fold greater accuracy than models without genetic information; (ii) tests of niche similarity revealed that three ecotypes, identified on the basis of neutral genetic markers and locally adapted populations, are associated with differences in <span class="hlt">climate</span>; (iii) our forecasts indicate that ongoing <span class="hlt">climate</span> change will likely shift these ecotypes further apart in geographic space, resulting in greater niche divergence; (iv) ecotypes that currently exhibit the largest geographic distribution and niche breadth appear to be buffered the most from <span class="hlt">climate</span> change. As diverse agents of selection shape genetic variability and structure within species, we argue that gENMs will lead to more accurate <span class="hlt">predictions</span> of species distributions under <span class="hlt">climate</span> change. © 2016 John Wiley & Sons Ltd.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.cpc.ncep.noaa.gov/products/precip/CWlink/ghazards/index.php','SCIGOVWS'); return false;" href="http://www.cpc.ncep.noaa.gov/products/precip/CWlink/ghazards/index.php"><span><span class="hlt">Climate</span> <span class="hlt">Prediction</span> Center - Global Tropical Hazards Assessment</span></a></p> <p><a target="_blank" href="http://www.science.gov/aboutsearch.html">Science.gov Websites</a></p> <p></p> <p></p> <p>Skip Navigation Links www.nws.noaa.gov NOAA logo - Click to go to <em>the</em> NOAA home page National Weather Service NWS logo - Click to go to <em>the</em> NWS home page <span class="hlt">Climate</span> <span class="hlt">Prediction</span> Center Home Site Map News Organization Search Go Search <em>the</em> CPC Go <span class="hlt">Climate</span> Outlooks <span class="hlt">Climate</span> & Weather Link El Niño/La Niña MJO</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFM.A21F2211K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFM.A21F2211K"><span>Can decadal <span class="hlt">climate</span> <span class="hlt">predictions</span> be improved by ocean ensemble dispersion filtering?</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Kadow, C.; Illing, S.; Kröner, I.; Ulbrich, U.; Cubasch, U.</p> <p>2017-12-01</p> <p>Decadal <span class="hlt">predictions</span> by Earth system models aim to capture the state and phase of the <span class="hlt">climate</span> several years inadvance. Atmosphere-ocean interaction plays an important role for such <span class="hlt">climate</span> forecasts. While short-termweather forecasts represent an initial value problem and long-term <span class="hlt">climate</span> projections represent a boundarycondition problem, the decadal <span class="hlt">climate</span> <span class="hlt">prediction</span> falls in-between these two time scales. The ocean memorydue to its heat capacity holds big potential skill on the decadal scale. In recent years, more precise initializationtechniques of coupled Earth system models (incl. atmosphere and ocean) have improved decadal <span class="hlt">predictions</span>.Ensembles are another important aspect. Applying slightly perturbed <span class="hlt">predictions</span> results in an ensemble. Insteadof using and evaluating one <span class="hlt">prediction</span>, but the whole ensemble or its ensemble average, improves a predictionsystem. However, <span class="hlt">climate</span> models in general start losing the initialized signal and its <span class="hlt">predictive</span> skill from oneforecast year to the next. Here we show that the <span class="hlt">climate</span> <span class="hlt">prediction</span> skill of an Earth system model can be improvedby a shift of the ocean state toward the ensemble mean of its individual members at seasonal intervals. Wefound that this procedure, called ensemble dispersion filter, results in more accurate results than the standarddecadal <span class="hlt">prediction</span>. Global mean and regional temperature, precipitation, and winter cyclone <span class="hlt">predictions</span> showan increased skill up to 5 years ahead. Furthermore, the novel technique outperforms <span class="hlt">predictions</span> with largerensembles and higher resolution. Our results demonstrate how decadal <span class="hlt">climate</span> <span class="hlt">predictions</span> benefit from oceanensemble dispersion filtering toward the ensemble mean. This study is part of MiKlip (fona-miklip.de) - a major project on decadal <span class="hlt">climate</span> <span class="hlt">prediction</span> in Germany.We focus on the Max-Planck-Institute Earth System Model using the low-resolution version (MPI-ESM-LR) andMiKlip's basic initialization strategy as in 2017 published decadal <span class="hlt">climate</span> forecast: http</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/pages/biblio/1395319-decadal-climate-prediction-project-dcpp-contribution-cmip6','SCIGOV-DOEP'); return false;" href="https://www.osti.gov/pages/biblio/1395319-decadal-climate-prediction-project-dcpp-contribution-cmip6"><span>The Decadal <span class="hlt">Climate</span> <span class="hlt">Prediction</span> Project (DCPP) contribution to CMIP6</span></a></p> <p><a target="_blank" href="http://www.osti.gov/pages">DOE PAGES</a></p> <p>Boer, George J.; Smith, Douglas M.; Cassou, Christophe; ...</p> <p>2016-01-01</p> <p>The Decadal <span class="hlt">Climate</span> <span class="hlt">Prediction</span> Project (DCPP) is a coordinated multi-model investigation into decadal <span class="hlt">climate</span> <span class="hlt">prediction</span>, <span class="hlt">predictability</span>, and variability. The DCPP makes use of past experience in simulating and <span class="hlt">predicting</span> decadal variability and forced <span class="hlt">climate</span> change gained from the fifth Coupled Model Intercomparison Project (CMIP5) and elsewhere. It builds on recent improvements in models, in the reanalysis of <span class="hlt">climate</span> data, in methods of initialization and ensemble generation, and in data treatment and analysis to propose an extended comprehensive decadal <span class="hlt">prediction</span> investigation as a contribution to CMIP6 (Eyring et al., 2016) and to the WCRP Grand Challenge on Near Term <span class="hlt">Climate</span> Predictionmore » (Kushnir et al., 2016). The DCPP consists of three components. Component A comprises the production and analysis of an extensive archive of retrospective forecasts to be used to assess and understand historical decadal <span class="hlt">prediction</span> skill, as a basis for improvements in all aspects of end-to-end decadal <span class="hlt">prediction</span>, and as a basis for forecasting on annual to decadal timescales. Component B undertakes ongoing production, analysis and dissemination of experimental quasi-real-time multi-model forecasts as a basis for potential operational forecast production. Component C involves the organization and coordination of case studies of particular <span class="hlt">climate</span> shifts and variations, both natural and naturally forced (e.g. the “hiatus”, volcanoes), including the study of the mechanisms that determine these behaviours. Furthermore, groups are invited to participate in as many or as few of the components of the DCPP, each of which are separately prioritized, as are of interest to them.The Decadal <span class="hlt">Climate</span> <span class="hlt">Prediction</span> Project addresses a range of scientific issues involving the ability of the <span class="hlt">climate</span> system to be <span class="hlt">predicted</span> on annual to decadal timescales, the skill that is currently and potentially available, the mechanisms involved in long timescale variability, and the production</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://files.eric.ed.gov/fulltext/ED282462.pdf','ERIC'); return false;" href="http://files.eric.ed.gov/fulltext/ED282462.pdf"><span>The Campus <span class="hlt">Climate</span> Revisited: Chilly for Women Faculty, <span class="hlt">Administrators</span>, and Graduate Students.</span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Sandler, Bernice R.; Hall, Roberta M.</p> <p></p> <p>The professional <span class="hlt">climate</span> often experienced by women faculty and <span class="hlt">administrators</span> is reported, along with some consideration to the experiences of graduate and professional students. Attention is focused on subtle ways in which women are treated differently and common behaviors that create a chilly professional <span class="hlt">climate</span>. The information was obtained…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4410635','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4410635"><span>Skilful multi-year <span class="hlt">predictions</span> of tropical trans-basin <span class="hlt">climate</span> variability</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Chikamoto, Yoshimitsu; Timmermann, Axel; Luo, Jing-Jia; Mochizuki, Takashi; Kimoto, Masahide; Watanabe, Masahiro; Ishii, Masayoshi; Xie, Shang-Ping; Jin, Fei-Fei</p> <p>2015-01-01</p> <p>Tropical Pacific sea surface temperature anomalies influence the atmospheric circulation, impacting <span class="hlt">climate</span> far beyond the tropics. The <span class="hlt">predictability</span> of the corresponding atmospheric signals is typically limited to less than 1 year lead time. Here we present observational and modelling evidence for multi-year <span class="hlt">predictability</span> of coherent trans-basin <span class="hlt">climate</span> variations that are characterized by a zonal seesaw in tropical sea surface temperature and sea-level pressure between the Pacific and the other two ocean basins. State-of-the-art <span class="hlt">climate</span> model forecasts initialized from a realistic ocean state show that the low-frequency trans-basin <span class="hlt">climate</span> variability, which explains part of the El Niño Southern Oscillation flavours, can be <span class="hlt">predicted</span> up to 3 years ahead, thus exceeding the <span class="hlt">predictive</span> skill of current tropical <span class="hlt">climate</span> forecasts for natural variability. This low-frequency variability emerges from the synchronization of ocean anomalies in all basins via global reorganizations of the atmospheric Walker Circulation. PMID:25897996</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/25897996','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/25897996"><span>Skilful multi-year <span class="hlt">predictions</span> of tropical trans-basin <span class="hlt">climate</span> variability.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Chikamoto, Yoshimitsu; Timmermann, Axel; Luo, Jing-Jia; Mochizuki, Takashi; Kimoto, Masahide; Watanabe, Masahiro; Ishii, Masayoshi; Xie, Shang-Ping; Jin, Fei-Fei</p> <p>2015-04-21</p> <p>Tropical Pacific sea surface temperature anomalies influence the atmospheric circulation, impacting <span class="hlt">climate</span> far beyond the tropics. The <span class="hlt">predictability</span> of the corresponding atmospheric signals is typically limited to less than 1 year lead time. Here we present observational and modelling evidence for multi-year <span class="hlt">predictability</span> of coherent trans-basin <span class="hlt">climate</span> variations that are characterized by a zonal seesaw in tropical sea surface temperature and sea-level pressure between the Pacific and the other two ocean basins. State-of-the-art <span class="hlt">climate</span> model forecasts initialized from a realistic ocean state show that the low-frequency trans-basin <span class="hlt">climate</span> variability, which explains part of the El Niño Southern Oscillation flavours, can be <span class="hlt">predicted</span> up to 3 years ahead, thus exceeding the <span class="hlt">predictive</span> skill of current tropical <span class="hlt">climate</span> forecasts for natural variability. This low-frequency variability emerges from the synchronization of ocean anomalies in all basins via global reorganizations of the atmospheric Walker Circulation.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/biblio/21028314-origins-computer-weather-prediction-climate-modeling','SCIGOV-STC'); return false;" href="https://www.osti.gov/biblio/21028314-origins-computer-weather-prediction-climate-modeling"><span>The origins of computer weather <span class="hlt">prediction</span> and <span class="hlt">climate</span> modeling</span></a></p> <p><a target="_blank" href="http://www.osti.gov/search">DOE Office of Scientific and Technical Information (OSTI.GOV)</a></p> <p>Lynch, Peter</p> <p>2008-03-20</p> <p>Numerical simulation of an ever-increasing range of geophysical phenomena is adding enormously to our understanding of complex processes in the Earth system. The consequences for mankind of ongoing <span class="hlt">climate</span> change will be far-reaching. Earth System Models are capable of replicating <span class="hlt">climate</span> regimes of past millennia and are the best means we have of <span class="hlt">predicting</span> the future of our <span class="hlt">climate</span>. The basic ideas of numerical forecasting and <span class="hlt">climate</span> modeling were developed about a century ago, long before the first electronic computer was constructed. There were several major practical obstacles to be overcome before numerical <span class="hlt">prediction</span> could be put into practice. Amore » fuller understanding of atmospheric dynamics allowed the development of simplified systems of equations; regular radiosonde observations of the free atmosphere and, later, satellite data, provided the initial conditions; stable finite difference schemes were developed; and powerful electronic computers provided a practical means of carrying out the prodigious calculations required to <span class="hlt">predict</span> the changes in the weather. Progress in weather forecasting and in <span class="hlt">climate</span> modeling over the past 50 years has been dramatic. In this presentation, we will trace the history of computer forecasting through the ENIAC integrations to the present day. The useful range of deterministic <span class="hlt">prediction</span> is increasing by about one day each decade, and our understanding of <span class="hlt">climate</span> change is growing rapidly as Earth System Models of ever-increasing sophistication are developed.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2008JCoPh.227.3431L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2008JCoPh.227.3431L"><span>The origins of computer weather <span class="hlt">prediction</span> and <span class="hlt">climate</span> modeling</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Lynch, Peter</p> <p>2008-03-01</p> <p>Numerical simulation of an ever-increasing range of geophysical phenomena is adding enormously to our understanding of complex processes in the Earth system. The consequences for mankind of ongoing <span class="hlt">climate</span> change will be far-reaching. Earth System Models are capable of replicating <span class="hlt">climate</span> regimes of past millennia and are the best means we have of <span class="hlt">predicting</span> the future of our <span class="hlt">climate</span>. The basic ideas of numerical forecasting and <span class="hlt">climate</span> modeling were developed about a century ago, long before the first electronic computer was constructed. There were several major practical obstacles to be overcome before numerical <span class="hlt">prediction</span> could be put into practice. A fuller understanding of atmospheric dynamics allowed the development of simplified systems of equations; regular radiosonde observations of the free atmosphere and, later, satellite data, provided the initial conditions; stable finite difference schemes were developed; and powerful electronic computers provided a practical means of carrying out the prodigious calculations required to <span class="hlt">predict</span> the changes in the weather. Progress in weather forecasting and in <span class="hlt">climate</span> modeling over the past 50 years has been dramatic. In this presentation, we will trace the history of computer forecasting through the ENIAC integrations to the present day. The useful range of deterministic <span class="hlt">prediction</span> is increasing by about one day each decade, and our understanding of <span class="hlt">climate</span> change is growing rapidly as Earth System Models of ever-increasing sophistication are developed.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/biblio/931346-developing-models-predictive-climate-science','SCIGOV-STC'); return false;" href="https://www.osti.gov/biblio/931346-developing-models-predictive-climate-science"><span>Developing Models for <span class="hlt">Predictive</span> <span class="hlt">Climate</span> Science</span></a></p> <p><a target="_blank" href="http://www.osti.gov/search">DOE Office of Scientific and Technical Information (OSTI.GOV)</a></p> <p>Drake, John B; Jones, Philip W</p> <p>2007-01-01</p> <p>The Community <span class="hlt">Climate</span> System Model results from a multi-agency collaboration designed to construct cutting-edge <span class="hlt">climate</span> science simulation models for a broad research community. <span class="hlt">Predictive</span> <span class="hlt">climate</span> simulations are currently being prepared for the petascale computers of the near future. Modeling capabilities are continuously being improved in order to provide better answers to critical questions about Earth's <span class="hlt">climate</span>. <span class="hlt">Climate</span> change and its implications are front page news in today's world. Could global warming be responsible for the July 2006 heat waves in Europe and the United States? Should more resources be devoted to preparing for an increase in the frequency of strongmore » tropical storms and hurricanes like Katrina? Will coastal cities be flooded due to a rise in sea level? The National <span class="hlt">Climatic</span> Data Center (NCDC), which archives all weather data for the nation, reports that global surface temperatures have increased over the last century, and that the rate of increase is three times greater since 1976. Will temperatures continue to climb at this rate, will they decline again, or will the rate of increase become even steeper? To address such a flurry of questions, scientists must adopt a systematic approach and develop a <span class="hlt">predictive</span> framework. With responsibility for advising on energy and technology strategies, the DOE is dedicated to advancing <span class="hlt">climate</span> research in order to elucidate the causes of <span class="hlt">climate</span> change, including the role of carbon loading from fossil fuel use. Thus, <span class="hlt">climate</span> science--which by nature involves advanced computing technology and methods--has been the focus of a number of DOE's SciDAC research projects. Dr. John Drake (ORNL) and Dr. Philip Jones (LANL) served as principal investigators on the SciDAC project, 'Collaborative Design and Development of the Community <span class="hlt">Climate</span> System Model for Terascale Computers.' The Community <span class="hlt">Climate</span> System Model (CCSM) is a fully-coupled global system that provides state-of-the-art computer simulations of</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.fs.usda.gov/treesearch/pubs/24235','TREESEARCH'); return false;" href="https://www.fs.usda.gov/treesearch/pubs/24235"><span><span class="hlt">Predicting</span> extinctions as a result of <span class="hlt">climate</span> change</span></a></p> <p><a target="_blank" href="http://www.fs.usda.gov/treesearch/">Treesearch</a></p> <p>Mark W. Schwartz; Louis R. Iverson; Anantha M. Prasad; Stephen N. Matthews; Raymond J. O' Connor; Raymond J. O' Connor</p> <p>2006-01-01</p> <p>Widespread extinction is a <span class="hlt">predicted</span> ecological consequence of global warming. Extinction risk under <span class="hlt">climate</span> change scenarios is a function of distribution breadth. Focusing on trees and birds of the eastern United States, we used joint <span class="hlt">climate</span> and environment models to examine fit and <span class="hlt">climate</span> change vulnerability as a function of distribution breadth. We found that...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/18023636','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/18023636"><span>The <span class="hlt">predictive</span> validity of safety <span class="hlt">climate</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Johnson, Stephen E</p> <p>2007-01-01</p> <p>Safety professionals have increasingly turned their attention to social science for insight into the causation of industrial accidents. One social construct, safety <span class="hlt">climate</span>, has been examined by several researchers [Cooper, M. D., & Phillips, R. A. (2004). Exploratory analysis of the safety <span class="hlt">climate</span> and safety behavior relationship. Journal of Safety Research, 35(5), 497-512; Gillen, M., Baltz, D., Gassel, M., Kirsch, L., & Vacarro, D. (2002). Perceived safety <span class="hlt">climate</span>, job Demands, and coworker support among union and nonunion injured construction workers. Journal of Safety Research, 33(1), 33-51; Neal, A., & Griffin, M. A. (2002). Safety <span class="hlt">climate</span> and safety behaviour. Australian Journal of Management, 27, 66-76; Zohar, D. (2000). A group-level model of safety <span class="hlt">climate</span>: Testing the effect of group <span class="hlt">climate</span> on microaccidents in manufacturing jobs. Journal of Applied Psychology, 85(4), 587-596; Zohar, D., & Luria, G. (2005). A multilevel model of safety <span class="hlt">climate</span>: Cross-level relationships between organization and group-level <span class="hlt">climates</span>. Journal of Applied Psychology, 90(4), 616-628] who have documented its importance as a factor explaining the variation of safety-related outcomes (e.g., behavior, accidents). Researchers have developed instruments for measuring safety <span class="hlt">climate</span> and have established some degree of psychometric reliability and validity. The problem, however, is that <span class="hlt">predictive</span> validity has not been firmly established, which reduces the credibility of safety <span class="hlt">climate</span> as a meaningful social construct. The research described in this article addresses this problem and provides additional support for safety <span class="hlt">climate</span> as a viable construct and as a <span class="hlt">predictive</span> indicator of safety-related outcomes. This study used 292 employees at three locations of a heavy manufacturing organization to complete the 16 item Zohar Safety <span class="hlt">Climate</span> Questionnaire (ZSCQ) [Zohar, D., & Luria, G. (2005). A multilevel model of safety <span class="hlt">climate</span>: Cross-level relationships between organization and group</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2005IJCli..25.1265W','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2005IJCli..25.1265W"><span>A compound reconstructed <span class="hlt">prediction</span> model for nonstationary <span class="hlt">climate</span> processes</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Wang, Geli; Yang, Peicai</p> <p>2005-07-01</p> <p>Based on the idea of <span class="hlt">climate</span> hierarchy and the theory of state space reconstruction, a local approximation <span class="hlt">prediction</span> model with the compound structure is built for <span class="hlt">predicting</span> some nonstationary <span class="hlt">climate</span> process. By means of this model and the data sets consisting of north Indian Ocean sea-surface temperature, Asian zonal circulation index and monthly mean precipitation anomaly from 37 observation stations in the Inner Mongolia area of China (IMC), a regional <span class="hlt">prediction</span> experiment for the winter precipitation of IMC is also carried out. When using the same sign ratio R between the <span class="hlt">prediction</span> field and the actual field to measure the <span class="hlt">prediction</span> accuracy, an averaged R of 63% given by 10 <span class="hlt">predictions</span> samples is reached.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20120001914','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20120001914"><span>Receivers Gather Data for <span class="hlt">Climate</span>, Weather <span class="hlt">Prediction</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p></p> <p>2012-01-01</p> <p>Signals from global positioning system (GPS) satellites are now being used for more than just location and navigation information. By looking at the radio waves from GPS satellites, a technology developed at NASA s Jet Propulsion Laboratory (JPL) not only precisely calculates its position, but can also use a technique known as radio occultation to help scientists study the Earth s atmosphere and gravity field to improve weather forecasts, monitor <span class="hlt">climate</span> change, and enhance space weather research. The University Corporation for Atmospheric Research (UCAR), a nonprofit group of universities in Boulder, Colorado, compares radio occultation to the appearance of a pencil when viewed though a glass of water. The water molecules change the path of visible light waves so that the pencil appears bent, just like molecules in the air bend GPS radio signals as they pass through (or are occulted by) the atmosphere. Through measurements of the amount of bending in the signals, scientists can construct detailed images of the ionosphere (the energetic upper part of the atmosphere) and also gather information about atmospheric density, pressure, temperature, and moisture. Once collected, this data can be input into weather forecasting and <span class="hlt">climate</span> models for weather <span class="hlt">prediction</span> and <span class="hlt">climate</span> studies. Traditionally, such information is obtained through the use of weather balloons. In 1998, JPL started developing a new class of GPS space science receivers, called Black Jack, that could take precise measurements of how GPS signals are distorted or delayed along their way to the receiver. By 2006, the first demonstration of a GPS radio occultation constellation was launched through a collaboration among Taiwan s National Science Council and National Space Organization, the U.S. National Science Foundation, NASA, the National Oceanic and Atmospheric <span class="hlt">Administration</span> (NOAA), and other Federal entities. Called the Constellation Observing System for Meteorology, Ionosphere, and <span class="hlt">Climate</span> (COSMIC</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/27128312','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/27128312"><span><span class="hlt">Predicting</span> Dengue Fever Outbreaks in French Guiana Using <span class="hlt">Climate</span> Indicators.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Adde, Antoine; Roucou, Pascal; Mangeas, Morgan; Ardillon, Vanessa; Desenclos, Jean-Claude; Rousset, Dominique; Girod, Romain; Briolant, Sébastien; Quenel, Philippe; Flamand, Claude</p> <p>2016-04-01</p> <p>Dengue fever epidemic dynamics are driven by complex interactions between hosts, vectors and viruses. Associations between <span class="hlt">climate</span> and dengue have been studied around the world, but the results have shown that the impact of the <span class="hlt">climate</span> can vary widely from one study site to another. In French Guiana, <span class="hlt">climate</span>-based models are not available to assist in developing an early warning system. This study aims to evaluate the potential of using oceanic and atmospheric conditions to help <span class="hlt">predict</span> dengue fever outbreaks in French Guiana. Lagged correlations and composite analyses were performed to identify the <span class="hlt">climatic</span> conditions that characterized a typical epidemic year and to define the best indices for <span class="hlt">predicting</span> dengue fever outbreaks during the period 1991-2013. A logistic regression was then performed to build a forecast model. We demonstrate that a model based on summer Equatorial Pacific Ocean sea surface temperatures and Azores High sea-level pressure had <span class="hlt">predictive</span> value and was able to <span class="hlt">predict</span> 80% of the outbreaks while incorrectly <span class="hlt">predicting</span> only 15% of the non-epidemic years. <span class="hlt">Predictions</span> for 2014-2015 were consistent with the observed non-epidemic conditions, and an outbreak in early 2016 was <span class="hlt">predicted</span>. These findings indicate that outbreak resurgence can be modeled using a simple combination of <span class="hlt">climate</span> indicators. This might be useful for anticipating public health actions to mitigate the effects of major outbreaks, particularly in areas where resources are limited and medical infrastructures are generally insufficient.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFM.A12A..02L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFM.A12A..02L"><span>Towards a unified Global Weather-<span class="hlt">Climate</span> <span class="hlt">Prediction</span> System</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Lin, S. J.</p> <p>2016-12-01</p> <p>The Geophysical Fluid Dynamics Laboratory has been developing a unified regional-global modeling system with variable resolution capabilities that can be used for severe weather <span class="hlt">predictions</span> and kilometer scale regional <span class="hlt">climate</span> simulations within a unified global modeling system. The foundation of this flexible modeling system is the nonhydrostatic Finite-Volume Dynamical Core on the Cubed-Sphere (FV3). A unique aspect of FV3 is that it is "vertically Lagrangian" (Lin 2004), essentially reducing the equation sets to two dimensions, and is the single most important reason why FV3 outperforms other non-hydrostatic cores. Owning to its accuracy, adaptability, and computational efficiency, the FV3 has been selected as the "engine" for NOAA's Next Generation Global <span class="hlt">Prediction</span> System (NGGPS). We have built into the modeling system a stretched grid, a two-way regional-global nested grid, and an optimal combination of the stretched and two-way nests capability, making kilometer-scale regional simulations within a global modeling system feasible. Our main scientific goal is to enable simulations of high impact weather phenomena (such as tornadoes, thunderstorms, category-5 hurricanes) within an IPCC-class <span class="hlt">climate</span> modeling system previously regarded as impossible. In this presentation I will demonstrate that, with the FV3, it is computationally feasible to simulate not only super-cell thunderstorms, but also the subsequent genesis of tornado-like vortices using a global model that was originally designed for <span class="hlt">climate</span> simulations. The development and tuning strategy between traditional weather and <span class="hlt">climate</span> models are fundamentally different due to different metrics. We were able to adapt and use traditional "<span class="hlt">climate</span>" metrics or standards, such as angular momentum conservation, energy conservation, and flux balance at top of the atmosphere, and gain insight into problems of traditional weather <span class="hlt">prediction</span> model for medium-range weather <span class="hlt">prediction</span>, and vice versa. Therefore, the</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_1");'>1</a></li> <li><a href="#" onclick='return showDiv("page_2");'>2</a></li> <li class="active"><span>3</span></li> <li><a href="#" onclick='return showDiv("page_4");'>4</a></li> <li><a href="#" onclick='return showDiv("page_5");'>5</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_3 --> <div id="page_4" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_2");'>2</a></li> <li><a href="#" onclick='return showDiv("page_3");'>3</a></li> <li class="active"><span>4</span></li> <li><a href="#" onclick='return showDiv("page_5");'>5</a></li> <li><a href="#" onclick='return showDiv("page_6");'>6</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="61"> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/26661387','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/26661387"><span>The interactive roles of mastery <span class="hlt">climate</span> and performance <span class="hlt">climate</span> in <span class="hlt">predicting</span> intrinsic motivation.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Buch, R; Nerstad, C G L; Säfvenbom, R</p> <p>2017-02-01</p> <p>This study examined the interplay between perceived mastery and performance <span class="hlt">climates</span> in <span class="hlt">predicting</span> increased intrinsic motivation. The results of a two-wave longitudinal study comprising of 141 individuals from three military academies revealed a positive relationship between a perceived mastery <span class="hlt">climate</span> and increased intrinsic motivation only for individuals who perceived a low performance <span class="hlt">climate</span>. This finding suggests a positive relationship between a perceived mastery <span class="hlt">climate</span> and increased intrinsic motivation only when combined with low perceptions of a performance <span class="hlt">climate</span>. Hence, introducing a performance <span class="hlt">climate</span> in addition to a mastery <span class="hlt">climate</span> can be an undermining motivational strategy, as it attenuates the positive relationship between a mastery <span class="hlt">climate</span> and increased intrinsic motivation. Implications for future research and practice are discussed. © 2015 John Wiley & Sons A/S. Published by John Wiley & Sons Ltd.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015E%26ES...23a2016H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015E%26ES...23a2016H"><span>Regional Design Approach in Designing <span class="hlt">Climatic</span> Responsive <span class="hlt">Administrative</span> Building in the 21st Century</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Haja Bava Mohidin, Hazrina Binti; Ismail, Alice Sabrina</p> <p>2015-01-01</p> <p>The objective of this paper is to explicate on the study of modern <span class="hlt">administrative</span> building in Malaysia which portrays regional design approach that conforms to the local context and <span class="hlt">climate</span> by reviewing two case studies; Perdana Putra (1999) and former Prime Minister's Office (1967). This paper is significant because the country's stature and political statement was symbolized by <span class="hlt">administrative</span> building as a national icon. In other words, it is also viewed as a cultural object that is closely tied to a particular social context and nation historical moment. <span class="hlt">Administrative</span> building, therefore, may exhibit various meanings. This paper uses structuralism paradigm and semiotic principles as a methodological approach. This paper is of importance for practicing architects and society in the future as it offers new knowledge and understanding in identifying the suitable <span class="hlt">climatic</span> consideration that may reflect regionalist design approach in modern <span class="hlt">administrative</span> building. These elements then may be adopted in designing public buildings in the future with regional values that are important for expressing national culture to symbolize the identity of place and society as well as responsive to <span class="hlt">climate</span> change.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/biblio/1408807-us-climate-variability-predictability-project','SCIGOV-STC'); return false;" href="https://www.osti.gov/biblio/1408807-us-climate-variability-predictability-project"><span>US <span class="hlt">Climate</span> Variability and <span class="hlt">Predictability</span> Project</span></a></p> <p><a target="_blank" href="http://www.osti.gov/search">DOE Office of Scientific and Technical Information (OSTI.GOV)</a></p> <p>Patterson, Mike</p> <p></p> <p>The US CLIVAR Project Office administers the US CLIVAR Program with its mission to advance understanding and <span class="hlt">prediction</span> of <span class="hlt">climate</span> variability and change across timescales with an emphasis on the role of the ocean and its interaction with other elements of the Earth system. The Project Office promotes and facilitates scientific collaboration within the US and international <span class="hlt">climate</span> and Earth science communities, addressing priority topics from subseasonal to centennial <span class="hlt">climate</span> variability and change; the global energy imbalance; the ocean’s role in <span class="hlt">climate</span>, water, and carbon cycles; <span class="hlt">climate</span> and weather extremes; and polar <span class="hlt">climate</span> changes. This project provides essential one-year supportmore » of the Project Office, enabling the participation of US scientists in the meetings of the US CLIVAR bodies that guide scientific planning and implementation, including the scientific steering committee that establishes program goals and evaluates progress of activities to address them, the science team of funded investigators studying the ocean overturning circulation in the Atlantic, and two working groups tackling the priority research topics of Arctic change influence on midlatitude <span class="hlt">climate</span> and weather extremes and the decadal-scale widening of the tropical belt.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016EGUGA..18.4525B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016EGUGA..18.4525B"><span>Toward seamless weather-<span class="hlt">climate</span> and environmental <span class="hlt">prediction</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Brunet, Gilbert</p> <p>2016-04-01</p> <p>Over the last decade or so, <span class="hlt">predicting</span> the weather, <span class="hlt">climate</span> and atmospheric composition has emerged as one of the most important areas of scientific endeavor. This is partly because the remarkable increase in skill of current weather forecasts has made society more and more dependent on them day to day for a whole range of decision making. And it is partly because <span class="hlt">climate</span> change is now widely accepted and the realization is growing rapidly that it will affect every person in the world profoundly, either directly or indirectly. One of the important endeavors of our societies is to remain at the cutting-edge of modelling and <span class="hlt">predicting</span> the evolution of the fully coupled environmental system: atmosphere (weather and composition), oceans, land surface (physical and biological), and cryosphere. This effort will provide an increasingly accurate and reliable service across all the socio-economic sectors that are vulnerable to the effects of adverse weather and <span class="hlt">climatic</span> conditions, whether now or in the future. This emerging challenge was at the center of the World Weather Open Science Conference (Montreal, 2014).The outcomes of the conference are described in the World Meteorological Organization (WMO) book: Seamless <span class="hlt">Prediction</span> of the Earth System: from Minutes to Months, (G. Brunet, S. Jones, P. Ruti Eds., WMO-No. 1156, 2015). It is freely available on line at the WMO website. We will discuss some of the outcomes of the conference for the WMO World Weather Research Programme (WWRP) and Global Atmospheric Watch (GAW) long term goals and provide examples of seamless modelling and <span class="hlt">prediction</span> across a range of timescales at convective and sub-kilometer scales for regional coupled forecasting applications at Environment and <span class="hlt">Climate</span> Change Canada (ECCC).</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015AGUFM.A11N0269L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015AGUFM.A11N0269L"><span>The <span class="hlt">Climate</span> Variability & <span class="hlt">Predictability</span> (CVP) Program at NOAA - Recent Program Advancements</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Lucas, S. E.; Todd, J. F.</p> <p>2015-12-01</p> <p>The <span class="hlt">Climate</span> Variability & <span class="hlt">Predictability</span> (CVP) Program supports research aimed at providing process-level understanding of the <span class="hlt">climate</span> system through observation, modeling, analysis, and field studies. This vital knowledge is needed to improve <span class="hlt">climate</span> models and <span class="hlt">predictions</span> so that scientists can better anticipate the impacts of future <span class="hlt">climate</span> variability and change. To achieve its mission, the CVP Program supports research carried out at NOAA and other federal laboratories, NOAA Cooperative Institutes, and academic institutions. The Program also coordinates its sponsored projects with major national and international scientific bodies including the World <span class="hlt">Climate</span> Research Programme (WCRP), the International and U.S. <span class="hlt">Climate</span> Variability and <span class="hlt">Predictability</span> (CLIVAR/US CLIVAR) Program, and the U.S. Global Change Research Program (USGCRP). The CVP program sits within NOAA's <span class="hlt">Climate</span> Program Office (http://cpo.noaa.gov/CVP). The CVP Program currently supports multiple projects in areas that are aimed at improved representation of physical processes in global models. Some of the topics that are currently funded include: i) Improved Understanding of Intraseasonal Tropical Variability - DYNAMO field campaign and post -field projects, and the new <span class="hlt">climate</span> model improvement teams focused on MJO processes; ii) <span class="hlt">Climate</span> Process Teams (CPTs, co-funded with NSF) with projects focused on Cloud macrophysical parameterization and its application to aerosol indirect effects, and Internal-Wave Driven Mixing in Global Ocean Models; iii) Improved Understanding of Tropical Pacific Processes, Biases, and Climatology; iv) Understanding Arctic Sea Ice Mechanism and <span class="hlt">Predictability</span>;v) AMOC Mechanisms and Decadal <span class="hlt">Predictability</span> Recent results from CVP-funded projects will be summarized. Additional information can be found at http://cpo.noaa.gov/CVP.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3145734','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3145734"><span>Recent ecological responses to <span class="hlt">climate</span> change support <span class="hlt">predictions</span> of high extinction risk</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Maclean, Ilya M. D.; Wilson, Robert J.</p> <p>2011-01-01</p> <p><span class="hlt">Predicted</span> effects of <span class="hlt">climate</span> change include high extinction risk for many species, but confidence in these <span class="hlt">predictions</span> is undermined by a perceived lack of empirical support. Many studies have now documented ecological responses to recent <span class="hlt">climate</span> change, providing the opportunity to test whether the magnitude and nature of recent responses match <span class="hlt">predictions</span>. Here, we perform a global and multitaxon metaanalysis to show that empirical evidence for the realized effects of <span class="hlt">climate</span> change supports <span class="hlt">predictions</span> of future extinction risk. We use International Union for Conservation of Nature (IUCN) Red List criteria as a common scale to estimate extinction risks from a wide range of <span class="hlt">climate</span> impacts, ecological responses, and methods of analysis, and we compare <span class="hlt">predictions</span> with observations. Mean extinction probability across studies making <span class="hlt">predictions</span> of the future effects of <span class="hlt">climate</span> change was 7% by 2100 compared with 15% based on observed responses. After taking account of possible bias in the type of <span class="hlt">climate</span> change impact analyzed and the parts of the world and taxa studied, there was less discrepancy between the two approaches: <span class="hlt">predictions</span> suggested a mean extinction probability of 10% across taxa and regions, whereas empirical evidence gave a mean probability of 14%. As well as mean overall extinction probability, observations also supported <span class="hlt">predictions</span> in terms of variability in extinction risk and the relative risk associated with broad taxonomic groups and geographic regions. These results suggest that <span class="hlt">predictions</span> are robust to methodological assumptions and provide strong empirical support for the assertion that anthropogenic <span class="hlt">climate</span> change is now a major threat to global biodiversity. PMID:21746924</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/21746924','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/21746924"><span>Recent ecological responses to <span class="hlt">climate</span> change support <span class="hlt">predictions</span> of high extinction risk.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Maclean, Ilya M D; Wilson, Robert J</p> <p>2011-07-26</p> <p><span class="hlt">Predicted</span> effects of <span class="hlt">climate</span> change include high extinction risk for many species, but confidence in these <span class="hlt">predictions</span> is undermined by a perceived lack of empirical support. Many studies have now documented ecological responses to recent <span class="hlt">climate</span> change, providing the opportunity to test whether the magnitude and nature of recent responses match <span class="hlt">predictions</span>. Here, we perform a global and multitaxon metaanalysis to show that empirical evidence for the realized effects of <span class="hlt">climate</span> change supports <span class="hlt">predictions</span> of future extinction risk. We use International Union for Conservation of Nature (IUCN) Red List criteria as a common scale to estimate extinction risks from a wide range of <span class="hlt">climate</span> impacts, ecological responses, and methods of analysis, and we compare <span class="hlt">predictions</span> with observations. Mean extinction probability across studies making <span class="hlt">predictions</span> of the future effects of <span class="hlt">climate</span> change was 7% by 2100 compared with 15% based on observed responses. After taking account of possible bias in the type of <span class="hlt">climate</span> change impact analyzed and the parts of the world and taxa studied, there was less discrepancy between the two approaches: <span class="hlt">predictions</span> suggested a mean extinction probability of 10% across taxa and regions, whereas empirical evidence gave a mean probability of 14%. As well as mean overall extinction probability, observations also supported <span class="hlt">predictions</span> in terms of variability in extinction risk and the relative risk associated with broad taxonomic groups and geographic regions. These results suggest that <span class="hlt">predictions</span> are robust to methodological assumptions and provide strong empirical support for the assertion that anthropogenic <span class="hlt">climate</span> change is now a major threat to global biodiversity.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2010EGUGA..1212960M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2010EGUGA..1212960M"><span>Initializing decadal <span class="hlt">climate</span> <span class="hlt">predictions</span> over the North Atlantic region</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Matei, Daniela Mihaela; Pohlmann, Holger; Jungclaus, Johann; Müller, Wolfgang; Haak, Helmuth; Marotzke, Jochem</p> <p>2010-05-01</p> <p>Decadal <span class="hlt">climate</span> <span class="hlt">prediction</span> aims to <span class="hlt">predict</span> the internally-generated decadal <span class="hlt">climate</span> variability in addition to externally-forced <span class="hlt">climate</span> change signal. In order to achieve this it is necessary to start the <span class="hlt">predictions</span> from the current <span class="hlt">climate</span> state. In this study we investigate the forecast skill of the North Atlantic decadal <span class="hlt">climate</span> <span class="hlt">predictions</span> using two different ocean initialization strategies. First we apply an assimilation of ocean synthesis data provided by the GECCO project (Köhl and Stammer, 2008) as initial conditions for the coupled model ECHAM5/MPI-OM. Hindcast experiments are then performed over the period 1952-2001. An alternative approach is one in which the subsurface ocean temperature and salinity are diagnosed from an ensemble of ocean model runs forced by the NCEP-NCAR atmospheric reanalyzes for the period 1948-2007, then nudge into the coupled model to produce initial conditions for the hindcast experiments. An anomaly coupling scheme is used in both approaches to avoid the hindcast drift and the associated initial shock. Differences between the two assimilation approaches are discussed by comparing them with the observational data in key regions and processes. We asses the skill of the initialized decadal hindcast experiments against the <span class="hlt">prediction</span> skill of the non-initialized hindcasts simulation. We obtain an overview of the regions with the highest <span class="hlt">predictability</span> from the regional distribution of the anomaly correlation coefficients and RMSE for the SAT. For the first year the hindcast skill is increased over almost all ocean regions in the NCEP-forced approach. This increase in the hindcast skill for the 1 year lead time is somewhat reduced in the GECCO approach. At lead time 5yr and 10yr, the skill enhancement is still found over the North Atlantic and North Pacific regions. We also consider the potential <span class="hlt">predictability</span> of the Atlantic Meridional Overturning Circulation (AMOC) and Nordic Seas Overflow by comparing the <span class="hlt">predicted</span> values to</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/servlets/purl/1422909','SCIGOV-STC'); return false;" href="https://www.osti.gov/servlets/purl/1422909"><span><span class="hlt">Climate</span> Modeling and Causal Identification for Sea Ice <span class="hlt">Predictability</span></span></a></p> <p><a target="_blank" href="http://www.osti.gov/search">DOE Office of Scientific and Technical Information (OSTI.GOV)</a></p> <p>Hunke, Elizabeth Clare; Urrego Blanco, Jorge Rolando; Urban, Nathan Mark</p> <p></p> <p>This project aims to better understand causes of ongoing changes in the Arctic <span class="hlt">climate</span> system, particularly as decreasing sea ice trends have been observed in recent decades and are expected to continue in the future. As part of the Sea Ice <span class="hlt">Prediction</span> Network, a multi-agency effort to improve sea ice <span class="hlt">prediction</span> products on seasonal-to-interannual time scales, our team is studying sensitivity of sea ice to a collection of physical process and feedback mechanism in the coupled <span class="hlt">climate</span> system. During 2017 we completed a set of <span class="hlt">climate</span> model simulations using the fully coupled ACME-HiLAT model. The simulations consisted of experiments inmore » which cloud, sea ice, and air-ocean turbulent exchange parameters previously identified as important for driving output uncertainty in <span class="hlt">climate</span> models were perturbed to account for parameter uncertainty in simulated <span class="hlt">climate</span> variables. We conducted a sensitivity study to these parameters, which built upon a previous study we made for standalone simulations (Urrego-Blanco et al., 2016, 2017). Using the results from the ensemble of coupled simulations, we are examining robust relationships between <span class="hlt">climate</span> variables that emerge across the experiments. We are also using causal discovery techniques to identify interaction pathways among <span class="hlt">climate</span> variables which can help identify physical mechanisms and provide guidance in <span class="hlt">predictability</span> studies. This work further builds on and leverages the large ensemble of standalone sea ice simulations produced in our previous w14_seaice project.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/21304515','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/21304515"><span><span class="hlt">Predicting</span> <span class="hlt">climate</span> change impacts on polar bear litter size.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Molnár, Péter K; Derocher, Andrew E; Klanjscek, Tin; Lewis, Mark A</p> <p>2011-02-08</p> <p><span class="hlt">Predicting</span> the ecological impacts of <span class="hlt">climate</span> warming is critical for species conservation. Incorporating future warming into population models, however, is challenging because reproduction and survival cannot be measured for yet unobserved environmental conditions. In this study, we use mechanistic energy budget models and data obtainable under current conditions to <span class="hlt">predict</span> polar bear litter size under future conditions. In western Hudson Bay, we <span class="hlt">predict</span> <span class="hlt">climate</span> warming-induced litter size declines that jeopardize population viability: ∼28% of pregnant females failed to reproduce for energetic reasons during the early 1990s, but 40-73% could fail if spring sea ice break-up occurs 1 month earlier than during the 1990s, and 55-100% if break-up occurs 2 months earlier. Simultaneously, mean litter size would decrease by 22-67% and 44-100%, respectively. The expected timeline for these declines varies with <span class="hlt">climate</span>-model-specific sea ice <span class="hlt">predictions</span>. Similar litter size declines may occur in over one-third of the global polar bear population.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016ClDy...46.1459R','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016ClDy...46.1459R"><span>A new framework for <span class="hlt">climate</span> sensitivity and <span class="hlt">prediction</span>: a modelling perspective</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Ragone, Francesco; Lucarini, Valerio; Lunkeit, Frank</p> <p>2016-03-01</p> <p>The sensitivity of <span class="hlt">climate</span> models to increasing CO2 concentration and the <span class="hlt">climate</span> response at decadal time-scales are still major factors of uncertainty for the assessment of the long and short term effects of anthropogenic <span class="hlt">climate</span> change. While the relative slow progress on these issues is partly due to the inherent inaccuracies of numerical <span class="hlt">climate</span> models, this also hints at the need for stronger theoretical foundations to the problem of studying <span class="hlt">climate</span> sensitivity and performing <span class="hlt">climate</span> change <span class="hlt">predictions</span> with numerical models. Here we demonstrate that it is possible to use Ruelle's response theory to <span class="hlt">predict</span> the impact of an arbitrary CO2 forcing scenario on the global surface temperature of a general circulation model. Response theory puts the concept of <span class="hlt">climate</span> sensitivity on firm theoretical grounds, and addresses rigorously the problem of <span class="hlt">predictability</span> at different time-scales. Conceptually, these results show that performing <span class="hlt">climate</span> change experiments with general circulation models is a well defined problem from a physical and mathematical point of view. Practically, these results show that considering one single CO2 forcing scenario is enough to construct operators able to <span class="hlt">predict</span> the response of <span class="hlt">climatic</span> observables to any other CO2 forcing scenario, without the need to perform additional numerical simulations. We also introduce a general relationship between <span class="hlt">climate</span> sensitivity and <span class="hlt">climate</span> response at different time scales, thus providing an explicit definition of the inertia of the system at different time scales. This technique allows also for studying systematically, for a large variety of forcing scenarios, the time horizon at which the <span class="hlt">climate</span> change signal (in an ensemble sense) becomes statistically significant. While what we report here refers to the linear response, the general theory allows for treating nonlinear effects as well. These results pave the way for redesigning and interpreting <span class="hlt">climate</span> change experiments from a radically new</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/28382671','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/28382671"><span>Relationships Among Student, Staff, and <span class="hlt">Administrative</span> Measures of School <span class="hlt">Climate</span> and Student Health and Academic Outcomes.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Gase, Lauren N; Gomez, Louis M; Kuo, Tony; Glenn, Beth A; Inkelas, Moira; Ponce, Ninez A</p> <p>2017-05-01</p> <p>School <span class="hlt">climate</span> is an integral part of a comprehensive approach to improving the well-being of students; however, little is known about the relationships between its different domains and measures. We examined the relationships between student, staff, and <span class="hlt">administrative</span> measures of school <span class="hlt">climate</span> to understand the extent to which they were related to each other and student outcomes. The sample included 33,572 secondary school students from 121 schools in Los Angeles County during the 2014-2015 academic year. A multilevel regression model was constructed to examine the association between the domains and measures of school <span class="hlt">climate</span> and 5 outcomes of student well-being: depressive symptoms or suicidal ideation, tobacco use, alcohol use, marijuana use, and grades. Student, staff, and <span class="hlt">administrative</span> measures of school <span class="hlt">climate</span> were weakly correlated. Strong associations were found between student outcomes and student reports of engagement and safety, while school staff reports and <span class="hlt">administrative</span> measures of school <span class="hlt">climate</span> showed limited associations with student outcomes. As schools seek to measure and implement interventions aimed at improving school <span class="hlt">climate</span>, consideration should be given to grounding these efforts in a multidimensional conceptualization of <span class="hlt">climate</span> that values student perspectives and includes elements of both engagement and safety. © 2017, American School Health Association.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5876042','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5876042"><span>Relationships between Student, Staff, and <span class="hlt">Administrative</span> Measures of School <span class="hlt">Climate</span> and Student Health and Academic Outcomes</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Gase, Lauren Nichol; Gomez, Louis M.; Kuo, Tony; Glenn, Beth A.; Inkelas, Moira; Ponce, Ninez A.</p> <p>2018-01-01</p> <p>BACKGROUND School <span class="hlt">climate</span> is an integral part of a comprehensive approach to improving the wellbeing of students; however, little is known about the relationships between its different domains and measures. This study examined the relationships between student, staff, and <span class="hlt">administrative</span> measures of school <span class="hlt">climate</span> in order to understand the extent to which they were related to each other and student outcomes. METHODS The sample included 33,572 secondary school students from 121 schools in Los Angeles County during the 2014–2015 academic year. A multilevel regression model was constructed to examine the association between the domains and measures of school <span class="hlt">climate</span> and five outcomes of student wellbeing: depressive symptoms or suicidal ideation, tobacco use, alcohol use, marijuana use, and grades. RESULTS Student, staff, and <span class="hlt">administrative</span> measures of school <span class="hlt">climate</span> were weakly correlated. Strong associations were found between student outcomes and student reports of engagement and safety, while school staff reports and <span class="hlt">administrative</span> measures of school <span class="hlt">climate</span> showed limited associations with student outcomes. CONCLUSIONS As schools seek to measure and implement interventions aimed at improving school <span class="hlt">climate</span>, consideration should be given to grounding these efforts in a multi-dimensional conceptualization of <span class="hlt">climate</span> that values student perspectives and includes elements of both engagement and safety. PMID:28382671</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFMGC34A..08E','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFMGC34A..08E"><span>A Signal to Noise Paradox in <span class="hlt">Climate</span> <span class="hlt">Predictions</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Eade, R.; Scaife, A. A.; Smith, D.; Dunstone, N. J.; MacLachlan, C.; Hermanson, L.; Ruth, C.</p> <p>2017-12-01</p> <p>Recent advances in <span class="hlt">climate</span> modelling have resulted in the achievement of skilful long-range <span class="hlt">prediction</span>, particular that associated with the winter circulation over the north Atlantic (e.g. Scaife et al 2014, Stockdale et al 2015, Dunstone et al 2016) including impacts over Europe and North America, and further afield. However, while highly significant and potentially useful skill exists, the signal-to-noise ratio of the ensemble mean to total variability in these ensemble <span class="hlt">predictions</span> is anomalously small (Scaife et al 2014) and the correlation between the ensemble mean and historical observations exceeds the proportion of <span class="hlt">predictable</span> variance in the ensemble (Eade et al 2014). This means the real world is more <span class="hlt">predictable</span> than our <span class="hlt">climate</span> models. Here we discuss a series of hypothesis tests that have been carried out to assess issues with model mechanisms compared to the observed world, and present the latest findings in our attempt to determine the cause of the anomalously weak <span class="hlt">predicted</span> signals in our seasonal-to-decadal hindcasts.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70187296','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70187296"><span><span class="hlt">Predicted</span> changes in <span class="hlt">climatic</span> niche and <span class="hlt">climate</span> refugia of conservation priority salamander species in the northeastern United States</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Sutton, William B.; Barrett, Kyle; Moody, Allison T.; Loftin, Cynthia S.; deMaynadier, Phillip G.; Nanjappa, Priya</p> <p>2015-01-01</p> <p>Global <span class="hlt">climate</span> change represents one of the most extensive and pervasive threats to wildlife populations. Amphibians, specifically salamanders, are particularly susceptible to the effects of changing <span class="hlt">climates</span> due to their restrictive physiological requirements and low vagility; however, little is known about which landscapes and species are vulnerable to <span class="hlt">climate</span> change. Our study objectives included, (1) evaluating species-specific <span class="hlt">predictions</span> (based on 2050 <span class="hlt">climate</span> projections) and vulnerabilities to <span class="hlt">climate</span> change and (2) using collective species responses to identify areas of <span class="hlt">climate</span> refugia for conservation priority salamanders in the northeastern United States. All evaluated salamander species were projected to lose a portion of their <span class="hlt">climatic</span> niche. Averaged projected losses ranged from 3%–100% for individual species, with the Cow Knob Salamander (Plethodon punctatus), Cheat Mountain Salamander (Plethodon nettingi), Shenandoah Mountain Salamander (Plethodon virginia), Mabee’s Salamander (Ambystoma mabeei), and Streamside Salamander (Ambystoma barbouri) <span class="hlt">predicted</span> to lose at least 97% of their landscape-scale <span class="hlt">climatic</span> niche. The Western Allegheny Plateau was <span class="hlt">predicted</span> to lose the greatest salamander <span class="hlt">climate</span> refugia richness (i.e., number of species with a <span class="hlt">climatically</span>-suitable niche in a landscape patch), whereas the Central Appalachians provided refugia for the greatest number of species during current and projected <span class="hlt">climate</span> scenarios. Our results can be used to identify species and landscapes that are likely to be further affected by <span class="hlt">climate</span> change and potentially resilient habitats that will provide consistent <span class="hlt">climatic</span> conditions in the face of environmental change.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014GeoRL..41.1035T','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014GeoRL..41.1035T"><span>Seasonal to interannual Arctic sea ice <span class="hlt">predictability</span> in current global <span class="hlt">climate</span> models</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Tietsche, S.; Day, J. J.; Guemas, V.; Hurlin, W. J.; Keeley, S. P. E.; Matei, D.; Msadek, R.; Collins, M.; Hawkins, E.</p> <p>2014-02-01</p> <p>We establish the first intermodel comparison of seasonal to interannual <span class="hlt">predictability</span> of present-day Arctic <span class="hlt">climate</span> by performing coordinated sets of idealized ensemble <span class="hlt">predictions</span> with four state-of-the-art global <span class="hlt">climate</span> models. For Arctic sea ice extent and volume, there is potential <span class="hlt">predictive</span> skill for lead times of up to 3 years, and potential <span class="hlt">prediction</span> errors have similar growth rates and magnitudes across the models. Spatial patterns of potential <span class="hlt">prediction</span> errors differ substantially between the models, but some features are robust. Sea ice concentration errors are largest in the marginal ice zone, and in winter they are almost zero away from the ice edge. Sea ice thickness errors are amplified along the coasts of the Arctic Ocean, an effect that is dominated by sea ice advection. These results give an upper bound on the ability of current global <span class="hlt">climate</span> models to <span class="hlt">predict</span> important aspects of Arctic <span class="hlt">climate</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/18451859','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/18451859"><span>Advancing decadal-scale <span class="hlt">climate</span> <span class="hlt">prediction</span> in the North Atlantic sector.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Keenlyside, N S; Latif, M; Jungclaus, J; Kornblueh, L; Roeckner, E</p> <p>2008-05-01</p> <p>The <span class="hlt">climate</span> of the North Atlantic region exhibits fluctuations on decadal timescales that have large societal consequences. Prominent examples include hurricane activity in the Atlantic, and surface-temperature and rainfall variations over North America, Europe and northern Africa. Although these multidecadal variations are potentially <span class="hlt">predictable</span> if the current state of the ocean is known, the lack of subsurface ocean observations that constrain this state has been a limiting factor for realizing the full skill potential of such <span class="hlt">predictions</span>. Here we apply a simple approach-that uses only sea surface temperature (SST) observations-to partly overcome this difficulty and perform retrospective decadal <span class="hlt">predictions</span> with a <span class="hlt">climate</span> model. Skill is improved significantly relative to <span class="hlt">predictions</span> made with incomplete knowledge of the ocean state, particularly in the North Atlantic and tropical Pacific oceans. Thus these results point towards the possibility of routine decadal <span class="hlt">climate</span> <span class="hlt">predictions</span>. Using this method, and by considering both internal natural <span class="hlt">climate</span> variations and projected future anthropogenic forcing, we make the following forecast: over the next decade, the current Atlantic meridional overturning circulation will weaken to its long-term mean; moreover, North Atlantic SST and European and North American surface temperatures will cool slightly, whereas tropical Pacific SST will remain almost unchanged. Our results suggest that global surface temperature may not increase over the next decade, as natural <span class="hlt">climate</span> variations in the North Atlantic and tropical Pacific temporarily offset the projected anthropogenic warming.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3105343','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3105343"><span><span class="hlt">Predicting</span> <span class="hlt">climate</span> change impacts on polar bear litter size</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Molnár, Péter K.; Derocher, Andrew E.; Klanjscek, Tin; Lewis, Mark A.</p> <p>2011-01-01</p> <p><span class="hlt">Predicting</span> the ecological impacts of <span class="hlt">climate</span> warming is critical for species conservation. Incorporating future warming into population models, however, is challenging because reproduction and survival cannot be measured for yet unobserved environmental conditions. In this study, we use mechanistic energy budget models and data obtainable under current conditions to <span class="hlt">predict</span> polar bear litter size under future conditions. In western Hudson Bay, we <span class="hlt">predict</span> <span class="hlt">climate</span> warming-induced litter size declines that jeopardize population viability: ∼28% of pregnant females failed to reproduce for energetic reasons during the early 1990s, but 40–73% could fail if spring sea ice break-up occurs 1 month earlier than during the 1990s, and 55–100% if break-up occurs 2 months earlier. Simultaneously, mean litter size would decrease by 22–67% and 44–100%, respectively. The expected timeline for these declines varies with <span class="hlt">climate</span>-model-specific sea ice <span class="hlt">predictions</span>. Similar litter size declines may occur in over one-third of the global polar bear population. PMID:21304515</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017ClDy...48.1841V','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017ClDy...48.1841V"><span>Decadal <span class="hlt">climate</span> <span class="hlt">prediction</span> with a refined anomaly initialisation approach</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Volpi, Danila; Guemas, Virginie; Doblas-Reyes, Francisco J.; Hawkins, Ed; Nichols, Nancy K.</p> <p>2017-03-01</p> <p>In decadal <span class="hlt">prediction</span>, the objective is to exploit both the sources of <span class="hlt">predictability</span> from the external radiative forcings and from the internal variability to provide the best possible <span class="hlt">climate</span> information for the next decade. <span class="hlt">Predicting</span> the <span class="hlt">climate</span> system internal variability relies on initialising the <span class="hlt">climate</span> model from observational estimates. We present a refined method of anomaly initialisation (AI) applied to the ocean and sea ice components of the global <span class="hlt">climate</span> forecast model EC-Earth, with the following key innovations: (1) the use of a weight applied to the observed anomalies, in order to avoid the risk of introducing anomalies recorded in the observed <span class="hlt">climate</span>, whose amplitude does not fit in the range of the internal variability generated by the model; (2) the AI of the ocean density, instead of calculating it from the anomaly initialised state of temperature and salinity. An experiment initialised with this refined AI method has been compared with a full field and standard AI experiment. Results show that the use of such refinements enhances the surface temperature skill over part of the North and South Atlantic, part of the South Pacific and the Mediterranean Sea for the first forecast year. However, part of such improvement is lost in the following forecast years. For the tropical Pacific surface temperature, the full field initialised experiment performs the best. The <span class="hlt">prediction</span> of the Arctic sea-ice volume is improved by the refined AI method for the first three forecast years and the skill of the Atlantic multidecadal oscillation is significantly increased compared to a non-initialised forecast, along the whole forecast time.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29170567','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29170567"><span><span class="hlt">Predicting</span> ecological responses in a changing ocean: the effects of future <span class="hlt">climate</span> uncertainty.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Freer, Jennifer J; Partridge, Julian C; Tarling, Geraint A; Collins, Martin A; Genner, Martin J</p> <p>2018-01-01</p> <p><span class="hlt">Predicting</span> how species will respond to <span class="hlt">climate</span> change is a growing field in marine ecology, yet knowledge of how to incorporate the uncertainty from future <span class="hlt">climate</span> data into these <span class="hlt">predictions</span> remains a significant challenge. To help overcome it, this review separates <span class="hlt">climate</span> uncertainty into its three components (scenario uncertainty, model uncertainty, and internal model variability) and identifies four criteria that constitute a thorough interpretation of an ecological response to <span class="hlt">climate</span> change in relation to these parts (awareness, access, incorporation, communication). Through a literature review, the extent to which the marine ecology community has addressed these criteria in their <span class="hlt">predictions</span> was assessed. Despite a high awareness of <span class="hlt">climate</span> uncertainty, articles favoured the most severe emission scenario, and only a subset of <span class="hlt">climate</span> models were used as input into ecological analyses. In the case of sea surface temperature, these models can have projections unrepresentative against a larger ensemble mean. Moreover, 91% of studies failed to incorporate the internal variability of a <span class="hlt">climate</span> model into results. We explored the influence that the choice of emission scenario, <span class="hlt">climate</span> model, and model realisation can have when <span class="hlt">predicting</span> the future distribution of the pelagic fish, Electrona antarctica . Future distributions were highly influenced by the choice of <span class="hlt">climate</span> model, and in some cases, internal variability was important in determining the direction and severity of the distribution change. Increased clarity and availability of processed <span class="hlt">climate</span> data would facilitate more comprehensive explorations of <span class="hlt">climate</span> uncertainty, and increase in the quality and standard of marine <span class="hlt">prediction</span> studies.</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_2");'>2</a></li> <li><a href="#" onclick='return showDiv("page_3");'>3</a></li> <li class="active"><span>4</span></li> <li><a href="#" onclick='return showDiv("page_5");'>5</a></li> <li><a href="#" onclick='return showDiv("page_6");'>6</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_4 --> <div id="page_5" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_3");'>3</a></li> <li><a href="#" onclick='return showDiv("page_4");'>4</a></li> <li class="active"><span>5</span></li> <li><a href="#" onclick='return showDiv("page_6");'>6</a></li> <li><a href="#" onclick='return showDiv("page_7");'>7</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="81"> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/20349837','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/20349837"><span>Integrating environmental and genetic effects to <span class="hlt">predict</span> responses of tree populations to <span class="hlt">climate</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Wang, Tongli; O'Neill, Gregory A; Aitken, Sally N</p> <p>2010-01-01</p> <p><span class="hlt">Climate</span> is a major environmental factor affecting the phenotype of trees and is also a critical agent of natural selection that has molded among-population genetic variation. Population response functions describe the environmental effect of planting site <span class="hlt">climates</span> on the performance of a single population, whereas transfer functions describe among-population genetic variation molded by natural selection for <span class="hlt">climate</span>. Although these approaches are widely used to <span class="hlt">predict</span> the responses of trees to <span class="hlt">climate</span> change, both have limitations. We present a novel approach that integrates both genetic and environmental effects into a single "universal response function" (URF) to better <span class="hlt">predict</span> the influence of <span class="hlt">climate</span> on phenotypes. Using a large lodgepole pine (Pinus contorta Dougl. ex Loud.) field transplant experiment composed of 140 populations planted on 62 sites to demonstrate the methodology, we show that the URF makes full use of data from provenance trials to: (1) improve <span class="hlt">predictions</span> of <span class="hlt">climate</span> change impacts on phenotypes; (2) reduce the size and cost of future provenance trials without compromising <span class="hlt">predictive</span> power; (3) more fully exploit existing, less comprehensive provenance tests; (4) quantify and compare environmental and genetic effects of <span class="hlt">climate</span> on population performance; and (5) <span class="hlt">predict</span> the performance of any population growing in any <span class="hlt">climate</span>. Finally, we discuss how the last attribute allows the URF to be used as a mechanistic model to <span class="hlt">predict</span> population and species ranges for the future and to guide assisted migration of seed for reforestation, restoration, or afforestation and genetic conservation in a changing <span class="hlt">climate</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFM.A33J0415R','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFM.A33J0415R"><span>Improving Seasonal <span class="hlt">Climate</span> <span class="hlt">Predictability</span> in the Colorado River Basin for Enhanced Decision Support</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Rajagopal, S.; Mahmoud, M. I.</p> <p>2016-12-01</p> <p>The water resource management community is increasingly seeking skillful seasonal <span class="hlt">climate</span> forecasts with long lead times. But <span class="hlt">predicting</span> wet or dry <span class="hlt">climate</span> with sufficient lead time (3 months) for a season (especially winter) in the Colorado River Basin (CRB) is a challenging problem. The typical approach taken to <span class="hlt">predicting</span> winter <span class="hlt">climate</span> is based on using <span class="hlt">climate</span> indices and <span class="hlt">climate</span> models to <span class="hlt">predict</span> precipitation or streamflow in the Colorado River Basin. In addition to this approach; which may have a long lead time, water supply forecasts are also generated based on current observations by the Colorado River Forecast Center. Recently, the effects of coupled atmospheric-ocean phenomena such as ENSO over North America, and atmospheric circulation patterns at the 500 mb pressure level, which make the CRB wet or dry, have been studied separately. In the current work we test whether combining <span class="hlt">climate</span> indices and circulation patterns improve <span class="hlt">predictability</span> in the CRB. To accomplish this, the atmospheric circulation data from the Earth System Research Laboratory (ESRL) and <span class="hlt">climate</span> indices data from the <span class="hlt">Climate</span> <span class="hlt">Prediction</span> Center were combined using logical functions. To quantify the skill in <span class="hlt">prediction</span>, statistics such as the hit ratio and false alarm ratio were computed. The results from using a combination of <span class="hlt">climate</span> indices and atmospheric circulation patterns suggest that there is an improvement in the <span class="hlt">prediction</span> skill with hit ratios higher than 0.8, as compared to using either predictor individually (which typically produced a hit ratio of 0.6). Based on this result, there is value in using this hybrid approach when compared to a black box statistical model, as the <span class="hlt">climate</span> index is an analog to the moisture availability and the right atmospheric circulation pattern helps in transporting that moisture to the Basin.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29745027','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29745027"><span>Ecological genomics <span class="hlt">predicts</span> <span class="hlt">climate</span> vulnerability in an endangered southwestern songbird.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Ruegg, Kristen; Bay, Rachael A; Anderson, Eric C; Saracco, James F; Harrigan, Ryan J; Whitfield, Mary; Paxton, Eben H; Smith, Thomas B</p> <p>2018-05-09</p> <p>Few regions have been more severely impacted by <span class="hlt">climate</span> change in the USA than the Desert Southwest. Here, we use ecological genomics to assess the potential for adaptation to rising global temperatures in a widespread songbird, the willow flycatcher (Empidonax traillii), and find the endangered desert southwestern subspecies (E. t. extimus) most vulnerable to future <span class="hlt">climate</span> change. Highly significant correlations between present abundance and estimates of genomic vulnerability - the mismatch between current and <span class="hlt">predicted</span> future genotype-environment relationships - indicate small, fragmented populations of the southwestern willow flycatcher will have to adapt most to keep pace with <span class="hlt">climate</span> change. Links between <span class="hlt">climate</span>-associated genotypes and genes important to thermal tolerance in birds provide a potential mechanism for adaptation to temperature extremes. Our results demonstrate that the incorporation of genotype-environment relationships into landscape-scale models of <span class="hlt">climate</span> vulnerability can facilitate more precise <span class="hlt">predictions</span> of <span class="hlt">climate</span> impacts and help guide conservation in threatened and endangered groups. © 2018 John Wiley & Sons Ltd/CNRS.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014IJBm...58.1119D','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014IJBm...58.1119D"><span>Challenges in <span class="hlt">predicting</span> <span class="hlt">climate</span> change impacts on pome fruit phenology</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Darbyshire, Rebecca; Webb, Leanne; Goodwin, Ian; Barlow, E. W. R.</p> <p>2014-08-01</p> <p><span class="hlt">Climate</span> projection data were applied to two commonly used pome fruit flowering models to investigate potential differences in <span class="hlt">predicted</span> full bloom timing. The two methods, fixed thermal time and sequential chill-growth, produced different results for seven apple and pear varieties at two Australian locations. The fixed thermal time model <span class="hlt">predicted</span> incremental advancement of full bloom, while results were mixed from the sequential chill-growth model. To further investigate how the sequential chill-growth model reacts under <span class="hlt">climate</span> perturbed conditions, four simulations were created to represent a wider range of species physiological requirements. These were applied to five Australian locations covering varied <span class="hlt">climates</span>. Lengthening of the chill period and contraction of the growth period was common to most results. The relative dominance of the chill or growth component tended to <span class="hlt">predict</span> whether full bloom advanced, remained similar or was delayed with <span class="hlt">climate</span> warming. The simplistic structure of the fixed thermal time model and the exclusion of winter chill conditions in this method indicate it is unlikely to be suitable for projection analyses. The sequential chill-growth model includes greater complexity; however, reservations in using this model for impact analyses remain. The results demonstrate that appropriate representation of physiological processes is essential to adequately <span class="hlt">predict</span> changes to full bloom under <span class="hlt">climate</span> perturbed conditions with greater model development needed.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014AGUFM.H23F0938Y','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014AGUFM.H23F0938Y"><span><span class="hlt">Predicted</span> impacts of <span class="hlt">climate</span> change on malaria transmission in West Africa</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Yamana, T. K.; Eltahir, E. A. B.</p> <p>2014-12-01</p> <p>Increases in temperature and changes in precipitation due to <span class="hlt">climate</span> change are expected to alter the spatial distribution of malaria transmission. This is especially true in West Africa, where malaria prevalence follows the current north-south gradients in temperature and precipitation. We assess the skill of GCMs at simulating past and present <span class="hlt">climate</span> in West Africa in order to select the most credible <span class="hlt">climate</span> <span class="hlt">predictions</span> for the periods 2030-2060 and 2070-2100. We then use the Hydrology, Entomology and Malaria Transmission Simulator (HYDREMATS), a mechanistic model of malaria transmission, to translate the <span class="hlt">predicted</span> changes in <span class="hlt">climate</span> into <span class="hlt">predicted</span> changes availability of mosquito breeding sites, mosquito populations, and malaria prevalence. We investigate the role of acquired immunity in determining a population's response to changes in exposure to the malaria parasite.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013EOSTr..94Q..63S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013EOSTr..94Q..63S"><span>New Congressional <span class="hlt">Climate</span> Change Task Force Calls on President to Use <span class="hlt">Administrative</span> Authority</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Showstack, Randy</p> <p>2013-02-01</p> <p>Spurred by U.S. congressional inaction on <span class="hlt">climate</span> change and by President Barack Obama's comments on the topic in his 21 January inaugural address, several Democratic members of Congress announced at a Capitol Hill briefing the formation of a bicameral task force on <span class="hlt">climate</span> change. In addition, they have called on the president to use his <span class="hlt">administrative</span> authority to deal with the issue.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20140010438','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20140010438"><span><span class="hlt">Prediction</span> of Seasonal <span class="hlt">Climate</span>-induced Variations in Global Food Production</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Iizumi, Toshichika; Sakuma, Hirofumi; Yokozawa, Masayuki; Luo, Jing-Jia; Challinor, Andrew J.; Brown, Molly E.; Sakurai, Gen; Yamagata, Toshio</p> <p>2013-01-01</p> <p>Consumers, including the poor in many countries, are increasingly dependent on food imports and are therefore exposed to variations in yields, production, and export prices in the major food-producing regions of the world. National governments and commercial entities are paying increased attention to the cropping forecasts of major food-exporting countries as well as to their own domestic food production. Given the increased volatility of food markets and the rising incidence of <span class="hlt">climatic</span> extremes affecting food production, food price spikes may increase in prevalence in future years. Here we present a global assessment of the reliability of crop failure hindcasts for major crops at two lead times derived by linking ensemble seasonal <span class="hlt">climatic</span> forecasts with statistical crop models. We assessed the reliability of hindcasts (i.e., retrospective forecasts for the past) of crop yield loss relative to the previous year for two lead times. Pre-season yield <span class="hlt">predictions</span> employ <span class="hlt">climatic</span> forecasts and have lead times of approximately 3 to 5 months for providing information regarding variations in yields for the coming cropping season. Within-season yield <span class="hlt">predictions</span> use <span class="hlt">climatic</span> forecasts with lead times of 1 to 3 months. Pre-season <span class="hlt">predictions</span> can be of value to national governments and commercial concerns, complemented by subsequent updates from within-season <span class="hlt">predictions</span>. The latter incorporate information on the most recent <span class="hlt">climatic</span> data for the upcoming period of reproductive growth. In addition to such <span class="hlt">predictions</span>, hindcasts using observations from satellites were performed to demonstrate the upper limit of the reliability of crop forecasting.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/24892737','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/24892737"><span>Phylogeny <span class="hlt">predicts</span> future habitat shifts due to <span class="hlt">climate</span> change.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Kuntner, Matjaž; Năpăruş, Magdalena; Li, Daiqin; Coddington, Jonathan A</p> <p>2014-01-01</p> <p>Taxa may respond differently to <span class="hlt">climatic</span> changes, depending on phylogenetic or ecological effects, but studies that discern among these alternatives are scarce. Here, we use two species pairs from globally distributed spider clades, each pair representing two lifestyles (generalist, specialist) to test the relative importance of phylogeny versus ecology in <span class="hlt">predicted</span> responses to <span class="hlt">climate</span> change. We used a recent phylogenetic hypothesis for nephilid spiders to select four species from two genera (Nephilingis and Nephilengys) that match the above criteria, are fully allopatric but combined occupy all subtropical-tropical regions. Based on their records, we modeled each species niche spaces and <span class="hlt">predicted</span> their ecological shifts 20, 40, 60, and 80 years into the future using customized GIS tools and projected <span class="hlt">climatic</span> changes. Phylogeny better <span class="hlt">predicts</span> the species current ecological preferences than do lifestyles. By 2080 all species face dramatic reductions in suitable habitat (54.8-77.1%) and adapt by moving towards higher altitudes and latitudes, although at different tempos. Phylogeny and life style explain simulated habitat shifts in altitude, but phylogeny is the sole best predictor of latitudinal shifts. Models incorporating phylogenetic relatedness are an important additional tool to <span class="hlt">predict</span> accurately biotic responses to global change.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/19244094','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/19244094"><span>Relationship of hospital organizational culture to patient safety <span class="hlt">climate</span> in the Veterans Health <span class="hlt">Administration</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Hartmann, Christine W; Meterko, Mark; Rosen, Amy K; Shibei Zhao; Shokeen, Priti; Singer, Sara; Gaba, David M</p> <p>2009-06-01</p> <p>Improving safety <span class="hlt">climate</span> could enhance patient safety, yet little evidence exists regarding the relationship between hospital characteristics and safety <span class="hlt">climate</span>. This study assessed the relationship between hospitals' organizational culture and safety <span class="hlt">climate</span> in Veterans Health <span class="hlt">Administration</span> (VA) hospitals nationally. Data were collected from a sample of employees in a stratified random sample of 30 VA hospitals over a 6-month period (response rate = 50%; n = 4,625). The Patient Safety <span class="hlt">Climate</span> in Healthcare Organizations (PSCHO) and the Zammuto and Krakower surveys were used to measure safety <span class="hlt">climate</span> and organizational culture, respectively. Higher levels of safety <span class="hlt">climate</span> were significantly associated with higher levels of group and entrepreneurial cultures, while lower levels of safety <span class="hlt">climate</span> were associated with higher levels of hierarchical culture. Hospitals could use these results to design specific interventions aimed at improving safety <span class="hlt">climate</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4182597','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4182597"><span><span class="hlt">Predicting</span> Vulnerabilities of North American Shorebirds to <span class="hlt">Climate</span> Change</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Galbraith, Hector; DesRochers, David W.; Brown, Stephen; Reed, J. Michael</p> <p>2014-01-01</p> <p>Despite an increase in conservation efforts for shorebirds, there are widespread declines of many species of North American shorebirds. We wanted to know whether these declines would be exacerbated by <span class="hlt">climate</span> change, and whether relatively secure species might become at–risk species. Virtually all of the shorebird species breeding in the USA and Canada are migratory, which means <span class="hlt">climate</span> change could affect extinction risk via changes on the breeding, wintering, and/or migratory refueling grounds, and that ecological synchronicities could be disrupted at multiple sites. To <span class="hlt">predict</span> the effects of <span class="hlt">climate</span> change on shorebird extinction risks, we created a categorical risk model complementary to that used by Partners–in–Flight and the U.S. Shorebird Conservation Plan. The model is based on anticipated changes in breeding, migration, and wintering habitat, degree of dependence on ecological synchronicities, migration distance, and degree of specialization on breeding, migration, or wintering habitat. We evaluated 49 species, and for 3 species we evaluated 2 distinct populations each, and found that 47 (90%) taxa are <span class="hlt">predicted</span> to experience an increase in risk of extinction. No species was reclassified into a lower–risk category, although 6 species had at least one risk factor decrease in association with <span class="hlt">climate</span> change. The number of species that changed risk categories in our assessment is sensitive to how much of an effect of <span class="hlt">climate</span> change is required to cause the shift, but even at its least sensitive, 20 species were at the highest risk category for extinction. Based on our results it appears that shorebirds are likely to be highly vulnerable to <span class="hlt">climate</span> change. Finally, we discuss both how our approach can be integrated with existing risk assessments and potential future directions for <span class="hlt">predicting</span> change in extinction risk due to <span class="hlt">climate</span> change. PMID:25268907</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/25268907','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/25268907"><span><span class="hlt">Predicting</span> vulnerabilities of North American shorebirds to <span class="hlt">climate</span> change.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Galbraith, Hector; DesRochers, David W; Brown, Stephen; Reed, J Michael</p> <p>2014-01-01</p> <p>Despite an increase in conservation efforts for shorebirds, there are widespread declines of many species of North American shorebirds. We wanted to know whether these declines would be exacerbated by <span class="hlt">climate</span> change, and whether relatively secure species might become at-risk species. Virtually all of the shorebird species breeding in the USA and Canada are migratory, which means <span class="hlt">climate</span> change could affect extinction risk via changes on the breeding, wintering, and/or migratory refueling grounds, and that ecological synchronicities could be disrupted at multiple sites. To <span class="hlt">predict</span> the effects of <span class="hlt">climate</span> change on shorebird extinction risks, we created a categorical risk model complementary to that used by Partners-in-Flight and the U.S. Shorebird Conservation Plan. The model is based on anticipated changes in breeding, migration, and wintering habitat, degree of dependence on ecological synchronicities, migration distance, and degree of specialization on breeding, migration, or wintering habitat. We evaluated 49 species, and for 3 species we evaluated 2 distinct populations each, and found that 47 (90%) taxa are <span class="hlt">predicted</span> to experience an increase in risk of extinction. No species was reclassified into a lower-risk category, although 6 species had at least one risk factor decrease in association with <span class="hlt">climate</span> change. The number of species that changed risk categories in our assessment is sensitive to how much of an effect of <span class="hlt">climate</span> change is required to cause the shift, but even at its least sensitive, 20 species were at the highest risk category for extinction. Based on our results it appears that shorebirds are likely to be highly vulnerable to <span class="hlt">climate</span> change. Finally, we discuss both how our approach can be integrated with existing risk assessments and potential future directions for <span class="hlt">predicting</span> change in extinction risk due to <span class="hlt">climate</span> change.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFM.A23G0296L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFM.A23G0296L"><span>The <span class="hlt">Climate</span> Variability & <span class="hlt">Predictability</span> (CVP) Program at NOAA - Recent Program Advancements in Understanding AMOC</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Lucas, S. E.</p> <p>2016-12-01</p> <p>The <span class="hlt">Climate</span> Variability & <span class="hlt">Predictability</span> (CVP) Program supports research aimed at providing process-level understanding of the <span class="hlt">climate</span> system through observation, modeling, analysis, and field studies. This vital knowledge is needed to improve <span class="hlt">climate</span> models and <span class="hlt">predictions</span> so that scientists can better anticipate the impacts of future <span class="hlt">climate</span> variability and change. To achieve its mission, the CVP Program supports research carried out at NOAA and other federal laboratories, NOAA Cooperative Institutes, and academic institutions. The Program also coordinates its sponsored projects with major national and international scientific bodies including the World <span class="hlt">Climate</span> Research Programme (WCRP), the International and U.S. <span class="hlt">Climate</span> Variability and <span class="hlt">Predictability</span> (CLIVAR/US CLIVAR) Program, and the U.S. Global Change Research Program (USGCRP). The CVP program sits within NOAA's <span class="hlt">Climate</span> Program Office (http://cpo.noaa.gov/CVP). This poster will present the recently funded CVP projects on improving the understanding Atlantic Meridional Overturning Circulation (AMOC), its impact on decadal <span class="hlt">predictability</span>, and its relationship with the overall <span class="hlt">climate</span> system.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2009EOSTr..90..343G','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2009EOSTr..90..343G"><span>The Urgent Need for Improved <span class="hlt">Climate</span> Models and <span class="hlt">Predictions</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Goddard, Lisa; Baethgen, Walter; Kirtman, Ben; Meehl, Gerald</p> <p>2009-09-01</p> <p>An investment over the next 10 years of the order of US$2 billion for developing improved <span class="hlt">climate</span> models was recommended in a report (http://wcrp.wmo.int/documents/WCRP_WorldModellingSummit_Jan2009.pdf) from the May 2008 World Modelling Summit for <span class="hlt">Climate</span> <span class="hlt">Prediction</span>, held in Reading, United Kingdom, and presented by the World <span class="hlt">Climate</span> Research Programme. The report indicated that “<span class="hlt">climate</span> models will, as in the past, play an important, and perhaps central, role in guiding the trillion dollar decisions that the peoples, governments and industries of the world will be making to cope with the consequences of changing <span class="hlt">climate</span>.” If trillions of dollars are going to be invested in making decisions related to <span class="hlt">climate</span> impacts, an investment of $2 billion, which is less than 0.1% of that amount, to provide better <span class="hlt">climate</span> information seems prudent. One example of investment in adaptation is the World Bank's <span class="hlt">Climate</span> Investment Fund, which has drawn contributions of more than $6 billion for work on clean technologies and adaptation efforts in nine pilot countries and two pilot regions. This is just the beginning of expenditures on adaptation efforts by the World Bank and other mechanisms, focusing on only a small fraction of the nations of the world and primarily aimed at anticipated anthropogenic <span class="hlt">climate</span> change. Moreover, decisions are being made now, all around the world—by individuals, companies, and governments—that affect people and their livelihoods today, not just 50 or more years in the future. <span class="hlt">Climate</span> risk management, whether related to projects of the scope of the World Bank's or to the planning and decisions of municipalities, will be best guided by meaningful <span class="hlt">climate</span> information derived from observations of the past and model <span class="hlt">predictions</span> of the future.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014AGUFM.H31H0729O','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014AGUFM.H31H0729O"><span>An Empirical Approach to <span class="hlt">Predicting</span> Effects of <span class="hlt">Climate</span> Change on Stream Water Chemistry</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Olson, J. R.; Hawkins, C. P.</p> <p>2014-12-01</p> <p><span class="hlt">Climate</span> change may affect stream solute concentrations by three mechanisms: dilution associated with increased precipitation, evaporative concentration associated with increased temperature, and changes in solute inputs associated with changes in <span class="hlt">climate</span>-driven weathering. We developed empirical models <span class="hlt">predicting</span> base-flow water chemistry from watershed geology, soils, and <span class="hlt">climate</span> for 1975 individual stream sites across the conterminous USA. We then <span class="hlt">predicted</span> future solute concentrations (2065 and 2099) by applying down-scaled global <span class="hlt">climate</span> model <span class="hlt">predictions</span> to these models. The electrical conductivity model (EC, model R2 = 0.78) <span class="hlt">predicted</span> mean increases in EC of 19 μS/cm by 2065 and 40 μS/cm by 2099. However <span class="hlt">predicted</span> responses for individual streams ranged from a 43% decrease to a 4x increase. Streams with the greatest <span class="hlt">predicted</span> decreases occurred in the southern Rocky Mountains and Mid-West, whereas southern California and Sierra Nevada streams showed the greatest increases. Generally, streams in dry areas underlain by non-calcareous rocks were <span class="hlt">predicted</span> to be the most vulnerable to increases in EC associated with <span class="hlt">climate</span> change. <span class="hlt">Predicted</span> changes in other water chemistry parameters (e.g., Acid Neutralization Capacity (ANC), SO4, and Ca) were similar to EC, although the magnitude of ANC and SO4 change was greater. <span class="hlt">Predicted</span> changes in ANC and SO4 are in general agreement with those changes already observed in seven locations with long term records.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018ClDy..tmp.2335P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018ClDy..tmp.2335P"><span>An effective drift correction for dynamical downscaling of decadal global <span class="hlt">climate</span> <span class="hlt">predictions</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Paeth, Heiko; Li, Jingmin; Pollinger, Felix; Müller, Wolfgang A.; Pohlmann, Holger; Feldmann, Hendrik; Panitz, Hans-Jürgen</p> <p>2018-04-01</p> <p>Initialized decadal <span class="hlt">climate</span> <span class="hlt">predictions</span> with coupled <span class="hlt">climate</span> models are often marked by substantial <span class="hlt">climate</span> drifts that emanate from a mismatch between the climatology of the coupled model system and the data set used for initialization. While such drifts may be easily removed from the <span class="hlt">prediction</span> system when analyzing individual variables, a major problem prevails for multivariate issues and, especially, when the output of the global <span class="hlt">prediction</span> system shall be used for dynamical downscaling. In this study, we present a statistical approach to remove <span class="hlt">climate</span> drifts in a multivariate context and demonstrate the effect of this drift correction on regional <span class="hlt">climate</span> model simulations over the Euro-Atlantic sector. The statistical approach is based on an empirical orthogonal function (EOF) analysis adapted to a very large data matrix. The <span class="hlt">climate</span> drift emerges as a dramatic cooling trend in North Atlantic sea surface temperatures (SSTs) and is captured by the leading EOF of the multivariate output from the global <span class="hlt">prediction</span> system, accounting for 7.7% of total variability. The SST cooling pattern also imposes drifts in various atmospheric variables and levels. The removal of the first EOF effectuates the drift correction while retaining other components of intra-annual, inter-annual and decadal variability. In the regional <span class="hlt">climate</span> model, the multivariate drift correction of the input data removes the cooling trends in most western European land regions and systematically reduces the discrepancy between the output of the regional <span class="hlt">climate</span> model and observational data. In contrast, removing the drift only in the SST field from the global model has hardly any positive effect on the regional <span class="hlt">climate</span> model.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/26173081','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/26173081"><span>A Novel Modelling Approach for <span class="hlt">Predicting</span> Forest Growth and Yield under <span class="hlt">Climate</span> Change.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Ashraf, M Irfan; Meng, Fan-Rui; Bourque, Charles P-A; MacLean, David A</p> <p>2015-01-01</p> <p>Global <span class="hlt">climate</span> is changing due to increasing anthropogenic emissions of greenhouse gases. Forest managers need growth and yield models that can be used to <span class="hlt">predict</span> future forest dynamics during the transition period of present-day forests under a changing <span class="hlt">climatic</span> regime. In this study, we developed a forest growth and yield model that can be used to <span class="hlt">predict</span> individual-tree growth under current and projected future <span class="hlt">climatic</span> conditions. The model was constructed by integrating historical tree growth records with <span class="hlt">predictions</span> from an ecological process-based model using neural networks. The new model <span class="hlt">predicts</span> basal area (BA) and volume growth for individual trees in pure or mixed species forests. For model development, tree-growth data under current <span class="hlt">climatic</span> conditions were obtained using over 3000 permanent sample plots from the Province of Nova Scotia, Canada. Data to reflect tree growth under a changing <span class="hlt">climatic</span> regime were projected with JABOWA-3 (an ecological process-based model). Model validation with designated data produced model efficiencies of 0.82 and 0.89 in <span class="hlt">predicting</span> individual-tree BA and volume growth. Model efficiency is a relative index of model performance, where 1 indicates an ideal fit, while values lower than zero means the <span class="hlt">predictions</span> are no better than the average of the observations. Overall mean <span class="hlt">prediction</span> error (BIAS) of basal area and volume growth <span class="hlt">predictions</span> was nominal (i.e., for BA: -0.0177 cm(2) 5-year(-1) and volume: 0.0008 m(3) 5-year(-1)). Model variability described by root mean squared error (RMSE) in basal area <span class="hlt">prediction</span> was 40.53 cm(2) 5-year(-1) and 0.0393 m(3) 5-year(-1) in volume <span class="hlt">prediction</span>. The new modelling approach has potential to reduce uncertainties in growth and yield <span class="hlt">predictions</span> under different <span class="hlt">climate</span> change scenarios. This novel approach provides an avenue for forest managers to generate required information for the management of forests in transitional periods of <span class="hlt">climate</span> change. Artificial intelligence technology</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4501821','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4501821"><span>A Novel Modelling Approach for <span class="hlt">Predicting</span> Forest Growth and Yield under <span class="hlt">Climate</span> Change</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Ashraf, M. Irfan; Meng, Fan-Rui; Bourque, Charles P.-A.; MacLean, David A.</p> <p>2015-01-01</p> <p>Global <span class="hlt">climate</span> is changing due to increasing anthropogenic emissions of greenhouse gases. Forest managers need growth and yield models that can be used to <span class="hlt">predict</span> future forest dynamics during the transition period of present-day forests under a changing <span class="hlt">climatic</span> regime. In this study, we developed a forest growth and yield model that can be used to <span class="hlt">predict</span> individual-tree growth under current and projected future <span class="hlt">climatic</span> conditions. The model was constructed by integrating historical tree growth records with <span class="hlt">predictions</span> from an ecological process-based model using neural networks. The new model <span class="hlt">predicts</span> basal area (BA) and volume growth for individual trees in pure or mixed species forests. For model development, tree-growth data under current <span class="hlt">climatic</span> conditions were obtained using over 3000 permanent sample plots from the Province of Nova Scotia, Canada. Data to reflect tree growth under a changing <span class="hlt">climatic</span> regime were projected with JABOWA-3 (an ecological process-based model). Model validation with designated data produced model efficiencies of 0.82 and 0.89 in <span class="hlt">predicting</span> individual-tree BA and volume growth. Model efficiency is a relative index of model performance, where 1 indicates an ideal fit, while values lower than zero means the <span class="hlt">predictions</span> are no better than the average of the observations. Overall mean <span class="hlt">prediction</span> error (BIAS) of basal area and volume growth <span class="hlt">predictions</span> was nominal (i.e., for BA: -0.0177 cm2 5-year-1 and volume: 0.0008 m3 5-year-1). Model variability described by root mean squared error (RMSE) in basal area <span class="hlt">prediction</span> was 40.53 cm2 5-year-1 and 0.0393 m3 5-year-1 in volume <span class="hlt">prediction</span>. The new modelling approach has potential to reduce uncertainties in growth and yield <span class="hlt">predictions</span> under different <span class="hlt">climate</span> change scenarios. This novel approach provides an avenue for forest managers to generate required information for the management of forests in transitional periods of <span class="hlt">climate</span> change. Artificial intelligence technology has substantial</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://rosap.ntl.bts.gov/view/dot/17353','DOTNTL'); return false;" href="https://rosap.ntl.bts.gov/view/dot/17353"><span><span class="hlt">Administration</span> proposals on <span class="hlt">climate</span> change and energy independence : hearings before the Committee on Transportation and Infrastructure</span></a></p> <p><a target="_blank" href="http://ntlsearch.bts.gov/tris/index.do">DOT National Transportation Integrated Search</a></p> <p></p> <p>2007-05-01</p> <p>This memorandum briefly summarizes <span class="hlt">climate</span> change and its potential impacts. It then focuses in more detail on <span class="hlt">administration</span> proposals and policies regarding <span class="hlt">climate</span> change and energy independence. It will also look at legislative branch proposals a...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/25051868','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/25051868"><span>Values and uncertainties in <span class="hlt">climate</span> <span class="hlt">prediction</span>, revisited.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Parker, Wendy</p> <p>2014-06-01</p> <p>Philosophers continue to debate both the actual and the ideal roles of values in science. Recently, Eric Winsberg has offered a novel, model-based challenge to those who argue that the internal workings of science can and should be kept free from the influence of social values. He contends that model-based assignments of probability to hypotheses about future <span class="hlt">climate</span> change are unavoidably influenced by social values. I raise two objections to Winsberg's argument, neither of which can wholly undermine its conclusion but each of which suggests that his argument exaggerates the influence of social values on estimates of uncertainty in <span class="hlt">climate</span> <span class="hlt">prediction</span>. I then show how a more traditional challenge to the value-free ideal seems tailor-made for the <span class="hlt">climate</span> context.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29358696','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29358696"><span>Land-surface initialisation improves seasonal <span class="hlt">climate</span> <span class="hlt">prediction</span> skill for maize yield forecast.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Ceglar, Andrej; Toreti, Andrea; Prodhomme, Chloe; Zampieri, Matteo; Turco, Marco; Doblas-Reyes, Francisco J</p> <p>2018-01-22</p> <p>Seasonal crop yield forecasting represents an important source of information to maintain market stability, minimise socio-economic impacts of crop losses and guarantee humanitarian food assistance, while it fosters the use of <span class="hlt">climate</span> information favouring adaptation strategies. As <span class="hlt">climate</span> variability and extremes have significant influence on agricultural production, the early <span class="hlt">prediction</span> of severe weather events and unfavourable conditions can contribute to the mitigation of adverse effects. Seasonal <span class="hlt">climate</span> forecasts provide additional value for agricultural applications in several regions of the world. However, they currently play a very limited role in supporting agricultural decisions in Europe, mainly due to the poor skill of relevant surface variables. Here we show how a combined stress index (CSI), considering both drought and heat stress in summer, can <span class="hlt">predict</span> maize yield in Europe and how land-surface initialised seasonal <span class="hlt">climate</span> forecasts can be used to <span class="hlt">predict</span> it. The CSI explains on average nearly 53% of the inter-annual maize yield variability under observed <span class="hlt">climate</span> conditions and shows how concurrent heat stress and drought events have influenced recent yield anomalies. Seasonal <span class="hlt">climate</span> forecast initialised with realistic land-surface achieves better (and marginally useful) skill in <span class="hlt">predicting</span> the CSI than with climatological land-surface initialisation in south-eastern Europe, part of central Europe, France and Italy.</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_3");'>3</a></li> <li><a href="#" onclick='return showDiv("page_4");'>4</a></li> <li class="active"><span>5</span></li> <li><a href="#" onclick='return showDiv("page_6");'>6</a></li> <li><a href="#" onclick='return showDiv("page_7");'>7</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_5 --> <div id="page_6" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_4");'>4</a></li> <li><a href="#" onclick='return showDiv("page_5");'>5</a></li> <li class="active"><span>6</span></li> <li><a href="#" onclick='return showDiv("page_7");'>7</a></li> <li><a href="#" onclick='return showDiv("page_8");'>8</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="101"> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013NatCC...3..904I','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013NatCC...3..904I"><span><span class="hlt">Prediction</span> of seasonal <span class="hlt">climate</span>-induced variations in global food production</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Iizumi, Toshichika; Sakuma, Hirofumi; Yokozawa, Masayuki; Luo, Jing-Jia; Challinor, Andrew J.; Brown, Molly E.; Sakurai, Gen; Yamagata, Toshio</p> <p>2013-10-01</p> <p>Consumers, including the poor in many countries, are increasingly dependent on food imports and are thus exposed to variations in yields, production and export prices in the major food-producing regions of the world. National governments and commercial entities are therefore paying increased attention to the cropping forecasts of important food-exporting countries as well as to their own domestic food production. Given the increased volatility of food markets and the rising incidence of <span class="hlt">climatic</span> extremes affecting food production, food price spikes may increase in prevalence in future years. Here we present a global assessment of the reliability of crop failure hindcasts for major crops at two lead times derived by linking ensemble seasonal <span class="hlt">climatic</span> forecasts with statistical crop models. We found that moderate-to-marked yield loss over a substantial percentage (26-33%) of the harvested area of these crops is reliably <span class="hlt">predictable</span> if <span class="hlt">climatic</span> forecasts are near perfect. However, only rice and wheat production are reliably <span class="hlt">predictable</span> at three months before the harvest using within-season hindcasts. The reliabilities of estimates varied substantially by crop--rice and wheat yields were the most <span class="hlt">predictable</span>, followed by soybean and maize. The reasons for variation in the reliability of the estimates included the differences in crop sensitivity to the <span class="hlt">climate</span> and the technology used by the crop-producing regions. Our findings reveal that the use of seasonal <span class="hlt">climatic</span> forecasts to <span class="hlt">predict</span> crop failures will be useful for monitoring global food production and will encourage the adaptation of food systems toclimatic extremes.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20080007122','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20080007122"><span><span class="hlt">Climate</span>-Induced Boreal Forest Change: <span class="hlt">Predictions</span> versus Current Observations</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Soja, Amber J.; Tchebakova, Nadezda M.; French, Nancy H. F.; Flannigan, Michael D.; Shugart, Herman H.; Stocks, Brian J.; Sukhinin, Anatoly I.; Parfenova, E. I.; Chapin, F. Stuart, III; Stackhouse, Paul W., Jr.</p> <p>2007-01-01</p> <p>For about three decades, there have been many <span class="hlt">predictions</span> of the potential ecological response in boreal regions to the currently warmer conditions. In essence, a widespread, naturally occurring experiment has been conducted over time. In this paper, we describe previously modeled <span class="hlt">predictions</span> of ecological change in boreal Alaska, Canada and Russia, and then we investigate potential evidence of current <span class="hlt">climate</span>-induced change. For instance, ecological models have suggested that warming will induce the northern and upslope migration of the treeline and an alteration in the current mosaic structure of boreal forests. We present evidence of the migration of keystone ecosystems in the upland and lowland treeline of mountainous regions across southern Siberia. Ecological models have also <span class="hlt">predicted</span> a moisture-stress-related dieback in white spruce trees in Alaska, and current investigations show that as temperatures increase, white spruce tree growth is declining. Additionally, it was suggested that increases in infestation and wildfire disturbance would be catalysts that precipitate the alteration of the current mosaic forest composition. In Siberia, five of the last seven years have resulted in extreme fire seasons, and extreme fire years have also been more frequent in both Alaska and Canada. In addition, Alaska has experienced extreme and geographically expansive multi-year outbreaks of the spruce beetle, which had been previously limited by the cold, moist environment. We suggest that there is substantial evidence throughout the circumboreal region to conclude that the biosphere within the boreal terrestrial environment has already responded to the transient effects of <span class="hlt">climate</span> change. Additionally, temperature increases and warming-induced change are progressing faster than had been <span class="hlt">predicted</span> in some regions, suggesting a potential non-linear rapid response to changes in <span class="hlt">climate</span>, as opposed to the <span class="hlt">predicted</span> slow linear response to <span class="hlt">climate</span> change.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19790012404','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19790012404"><span>Third National Aeronautics and Space <span class="hlt">Administration</span> Weather and <span class="hlt">climate</span> program science review</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Kreins, E. R. (Editor)</p> <p>1977-01-01</p> <p>Research results of developing experimental and prototype operational systems, sensors, and space facilities for monitoring, and understanding the atmosphere are reported. Major aspects include: (1) detection, monitoring, and <span class="hlt">prediction</span> of severe storms; (2) improvement of global forecasting; and (3) monitoring and <span class="hlt">prediction</span> of <span class="hlt">climate</span> change.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2005IJCli..25.1881C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2005IJCli..25.1881C"><span>Weather and seasonal <span class="hlt">climate</span> <span class="hlt">prediction</span> for South America using a multi-model superensemble</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Chaves, Rosane R.; Ross, Robert S.; Krishnamurti, T. N.</p> <p>2005-11-01</p> <p>This work examines the feasibility of weather and seasonal <span class="hlt">climate</span> <span class="hlt">predictions</span> for South America using the multi-model synthetic superensemble approach for <span class="hlt">climate</span>, and the multi-model conventional superensemble approach for numerical weather <span class="hlt">prediction</span>, both developed at Florida State University (FSU). The effect on seasonal <span class="hlt">climate</span> forecasts of the number of models used in the synthetic superensemble is investigated. It is shown that the synthetic superensemble approach for <span class="hlt">climate</span> and the conventional superensemble approach for numerical weather <span class="hlt">prediction</span> can reduce the errors over South America in seasonal <span class="hlt">climate</span> <span class="hlt">prediction</span> and numerical weather <span class="hlt">prediction</span>.For <span class="hlt">climate</span> <span class="hlt">prediction</span>, a suite of 13 models is used. The forecast lead-time is 1 month for the <span class="hlt">climate</span> forecasts, which consist of precipitation and surface temperature forecasts. The multi-model ensemble is comprised of four versions of the FSU-Coupled Ocean-Atmosphere Model, seven models from the Development of a European Multi-model Ensemble System for Seasonal to Interannual <span class="hlt">Prediction</span> (DEMETER), a version of the Community <span class="hlt">Climate</span> Model (CCM3), and a version of the <span class="hlt">predictive</span> Ocean Atmosphere Model for Australia (POAMA). The results show that conditions over South America are appropriately simulated by the Florida State University Synthetic Superensemble (FSUSSE) in comparison to observations and that the skill of this approach increases with the use of additional models in the ensemble. When compared to observations, the forecasts are generally better than those from both a single <span class="hlt">climate</span> model and the multi-model ensemble mean, for the variables tested in this study.For numerical weather <span class="hlt">prediction</span>, the conventional Florida State University Superensemble (FSUSE) is used to <span class="hlt">predict</span> the mass and motion fields over South America. <span class="hlt">Predictions</span> of mean sea level pressure, 500 hPa geopotential height, and 850 hPa wind are made with a multi-model superensemble comprised of six global models for the period</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4192637','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4192637"><span>Extracting <span class="hlt">climate</span> memory using Fractional Integrated Statistical Model: A new perspective on <span class="hlt">climate</span> <span class="hlt">prediction</span></span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Yuan, Naiming; Fu, Zuntao; Liu, Shida</p> <p>2014-01-01</p> <p>Long term memory (LTM) in <span class="hlt">climate</span> variability is studied by means of fractional integral techniques. By using a recently developed model, Fractional Integral Statistical Model (FISM), we in this report proposed a new method, with which one can estimate the long-lasting influences of historical <span class="hlt">climate</span> states on the present time quantitatively, and further extract the influence as <span class="hlt">climate</span> memory signals. To show the usability of this method, two examples, the Northern Hemisphere monthly Temperature Anomalies (NHTA) and the Pacific Decadal Oscillation index (PDO), are analyzed in this study. We find the <span class="hlt">climate</span> memory signals indeed can be extracted and the whole variations can be further decomposed into two parts: the cumulative <span class="hlt">climate</span> memory (CCM) and the weather-scale excitation (WSE). The stronger LTM is, the larger proportion the <span class="hlt">climate</span> memory signals will account for in the whole variations. With the <span class="hlt">climate</span> memory signals extracted, one can at least determine on what basis the considered time series will continue to change. Therefore, this report provides a new perspective on <span class="hlt">climate</span> <span class="hlt">prediction</span>. PMID:25300777</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014AGUFMGC52B..06T','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014AGUFMGC52B..06T"><span>Seasonal <span class="hlt">Prediction</span> of Hydro-<span class="hlt">Climatic</span> Extremes in the Greater Horn of Africa Under Evolving <span class="hlt">Climate</span> Conditions to Support Adaptation Strategies</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Tadesse, T.; Zaitchik, B. F.; Habib, S.; Funk, C. C.; Senay, G. B.; Dinku, T.; Policelli, F. S.; Block, P.; Baigorria, G. A.; Beyene, S.; Wardlow, B.; Hayes, M. J.</p> <p>2014-12-01</p> <p>The development of effective strategies to adapt to changes in the character of droughts and floods in Africa will rely on improved seasonal <span class="hlt">prediction</span> systems that are robust to an evolving <span class="hlt">climate</span> baseline and can be integrated into disaster preparedness and response. Many efforts have been made to build models to improve seasonal forecasts in the Greater Horn of Africa region (GHA) using satellite and <span class="hlt">climate</span> data, but these efforts and models must be improved and translated into future conditions under evolving <span class="hlt">climate</span> conditions. This has considerable social significance, but is challenged by the nature of <span class="hlt">climate</span> <span class="hlt">predictability</span> and the adaptability of coupled natural and human systems facing exposure to <span class="hlt">climate</span> extremes. To address these issues, work is in progress under a project funded by NASA. The objectives of the project include: 1) Characterize and explain large-scale drivers in the ocean-atmosphere-land system associated with years of extreme flood or drought in the GHA. 2) Evaluate the performance of state-of-the-art seasonal forecast methods for <span class="hlt">prediction</span> of decision-relevant metrics of hydrologic extremes. 3) Apply seasonal forecast systems to <span class="hlt">prediction</span> of socially relevant impacts on crops, flood risk, and economic outcomes, and assess the value of these <span class="hlt">predictions</span> to decision makers. 4) Evaluate the robustness of seasonal <span class="hlt">prediction</span> systems to evolving <span class="hlt">climate</span> conditions. The National Drought Mitigation Center (University of Nebraska-Lincoln, USA) is leading this project in collaboration with the USGS, Johns Hopkins University, University of Wisconsin-Madison, the International Research Institute for <span class="hlt">Climate</span> and Society, NASA, and GHA local experts. The project is also designed to have active engagement of end users in various sectors, university researchers, and extension agents in GHA through workshops and/or webinars. This project is expected improve and implement new and existing <span class="hlt">climate</span>- and remote sensing-based agricultural</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4878477','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4878477"><span><span class="hlt">Predicting</span> the evolutionary dynamics of seasonal adaptation to novel <span class="hlt">climates</span> in Arabidopsis thaliana</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Fournier-Level, Alexandre; Perry, Emily O.; Wang, Jonathan A.; Braun, Peter T.; Migneault, Andrew; Cooper, Martha D.; Metcalf, C. Jessica E.; Schmitt, Johanna</p> <p>2016-01-01</p> <p><span class="hlt">Predicting</span> whether and how populations will adapt to rapid <span class="hlt">climate</span> change is a critical goal for evolutionary biology. To examine the genetic basis of fitness and <span class="hlt">predict</span> adaptive evolution in novel <span class="hlt">climates</span> with seasonal variation, we grew a diverse panel of the annual plant Arabidopsis thaliana (multiparent advanced generation intercross lines) in controlled conditions simulating four <span class="hlt">climates</span>: a present-day reference <span class="hlt">climate</span>, an increased-temperature <span class="hlt">climate</span>, a winter-warming only <span class="hlt">climate</span>, and a poleward-migration <span class="hlt">climate</span> with increased photoperiod amplitude. In each <span class="hlt">climate</span>, four successive seasonal cohorts experienced dynamic daily temperature and photoperiod variation over a year. We measured 12 traits and developed a genomic <span class="hlt">prediction</span> model for fitness evolution in each seasonal environment. This model was used to simulate evolutionary trajectories of the base population over 50 y in each <span class="hlt">climate</span>, as well as 100-y scenarios of gradual <span class="hlt">climate</span> change following adaptation to a reference <span class="hlt">climate</span>. Patterns of plastic and evolutionary fitness response varied across seasons and <span class="hlt">climates</span>. The increased-temperature <span class="hlt">climate</span> promoted genetic divergence of subpopulations across seasons, whereas in the winter-warming and poleward-migration <span class="hlt">climates</span>, seasonal genetic differentiation was reduced. In silico “resurrection experiments” showed limited evolutionary rescue compared with the plastic response of fitness to seasonal <span class="hlt">climate</span> change. The genetic basis of adaptation and, consequently, the dynamics of evolutionary change differed qualitatively among scenarios. Populations with fewer founding genotypes and populations with genetic diversity reduced by prior selection adapted less well to novel conditions, demonstrating that adaptation to rapid <span class="hlt">climate</span> change requires the maintenance of sufficient standing variation. PMID:27140640</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/27140640','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/27140640"><span><span class="hlt">Predicting</span> the evolutionary dynamics of seasonal adaptation to novel <span class="hlt">climates</span> in Arabidopsis thaliana.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Fournier-Level, Alexandre; Perry, Emily O; Wang, Jonathan A; Braun, Peter T; Migneault, Andrew; Cooper, Martha D; Metcalf, C Jessica E; Schmitt, Johanna</p> <p>2016-05-17</p> <p><span class="hlt">Predicting</span> whether and how populations will adapt to rapid <span class="hlt">climate</span> change is a critical goal for evolutionary biology. To examine the genetic basis of fitness and <span class="hlt">predict</span> adaptive evolution in novel <span class="hlt">climates</span> with seasonal variation, we grew a diverse panel of the annual plant Arabidopsis thaliana (multiparent advanced generation intercross lines) in controlled conditions simulating four <span class="hlt">climates</span>: a present-day reference <span class="hlt">climate</span>, an increased-temperature <span class="hlt">climate</span>, a winter-warming only <span class="hlt">climate</span>, and a poleward-migration <span class="hlt">climate</span> with increased photoperiod amplitude. In each <span class="hlt">climate</span>, four successive seasonal cohorts experienced dynamic daily temperature and photoperiod variation over a year. We measured 12 traits and developed a genomic <span class="hlt">prediction</span> model for fitness evolution in each seasonal environment. This model was used to simulate evolutionary trajectories of the base population over 50 y in each <span class="hlt">climate</span>, as well as 100-y scenarios of gradual <span class="hlt">climate</span> change following adaptation to a reference <span class="hlt">climate</span>. Patterns of plastic and evolutionary fitness response varied across seasons and <span class="hlt">climates</span>. The increased-temperature <span class="hlt">climate</span> promoted genetic divergence of subpopulations across seasons, whereas in the winter-warming and poleward-migration <span class="hlt">climates</span>, seasonal genetic differentiation was reduced. In silico "resurrection experiments" showed limited evolutionary rescue compared with the plastic response of fitness to seasonal <span class="hlt">climate</span> change. The genetic basis of adaptation and, consequently, the dynamics of evolutionary change differed qualitatively among scenarios. Populations with fewer founding genotypes and populations with genetic diversity reduced by prior selection adapted less well to novel conditions, demonstrating that adaptation to rapid <span class="hlt">climate</span> change requires the maintenance of sufficient standing variation.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://files.eric.ed.gov/fulltext/EJ1103516.pdf','ERIC'); return false;" href="http://files.eric.ed.gov/fulltext/EJ1103516.pdf"><span>The Relationship between Organizational <span class="hlt">Climate</span> and the Organizational Silence of <span class="hlt">Administrative</span> Staff in Education Department</span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Pozveh, Asghar Zamani; Karimi, Fariba</p> <p>2016-01-01</p> <p>The aim of the present study was to determine the relationship between organizational <span class="hlt">climate</span> and the organizational silence of <span class="hlt">administrative</span> staff in Education Department in Isfahan. The research method was descriptive and correlational-type method. The study population was <span class="hlt">administrative</span> staff of Education Department in Isfahan during the…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/27195983','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/27195983"><span>Improved <span class="hlt">Predictions</span> of the Geographic Distribution of Invasive Plants Using <span class="hlt">Climatic</span> Niche Models.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Ramírez-Albores, Jorge E; Bustamante, Ramiro O; Badano, Ernesto I</p> <p>2016-01-01</p> <p><span class="hlt">Climatic</span> niche models for invasive plants are usually constructed with occurrence records taken from literature and collections. Because these data neither discriminate among life-cycle stages of plants (adult or juvenile) nor the origin of individuals (naturally established or man-planted), the resulting models may mispredict the distribution ranges of these species. We propose that more accurate <span class="hlt">predictions</span> could be obtained by modelling <span class="hlt">climatic</span> niches with data of naturally established individuals, particularly with occurrence records of juvenile plants because this would restrict the <span class="hlt">predictions</span> of models to those sites where <span class="hlt">climatic</span> conditions allow the recruitment of the species. To test this proposal, we focused on the Peruvian peppertree (Schinus molle), a South American species that has largely invaded Mexico. Three <span class="hlt">climatic</span> niche models were constructed for this species using high-resolution dataset gathered in the field. The first model included all occurrence records, irrespective of the life-cycle stage or origin of peppertrees (generalized niche model). The second model only included occurrence records of naturally established mature individuals (adult niche model), while the third model was constructed with occurrence records of naturally established juvenile plants (regeneration niche model). When models were compared, the generalized <span class="hlt">climatic</span> niche model <span class="hlt">predicted</span> the presence of peppertrees in sites located farther beyond the <span class="hlt">climatic</span> thresholds that naturally established individuals can tolerate, suggesting that human activities influence the distribution of this invasive species. The adult and regeneration <span class="hlt">climatic</span> niche models concurred in their <span class="hlt">predictions</span> about the distribution of peppertrees, suggesting that naturally established adult trees only occur in sites where <span class="hlt">climatic</span> conditions allow the recruitment of juvenile stages. These results support the proposal that <span class="hlt">climatic</span> niches of invasive plants should be modelled with data of</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4873032','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4873032"><span>Improved <span class="hlt">Predictions</span> of the Geographic Distribution of Invasive Plants Using <span class="hlt">Climatic</span> Niche Models</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Ramírez-Albores, Jorge E.; Bustamante, Ramiro O.</p> <p>2016-01-01</p> <p><span class="hlt">Climatic</span> niche models for invasive plants are usually constructed with occurrence records taken from literature and collections. Because these data neither discriminate among life-cycle stages of plants (adult or juvenile) nor the origin of individuals (naturally established or man-planted), the resulting models may mispredict the distribution ranges of these species. We propose that more accurate <span class="hlt">predictions</span> could be obtained by modelling <span class="hlt">climatic</span> niches with data of naturally established individuals, particularly with occurrence records of juvenile plants because this would restrict the <span class="hlt">predictions</span> of models to those sites where <span class="hlt">climatic</span> conditions allow the recruitment of the species. To test this proposal, we focused on the Peruvian peppertree (Schinus molle), a South American species that has largely invaded Mexico. Three <span class="hlt">climatic</span> niche models were constructed for this species using high-resolution dataset gathered in the field. The first model included all occurrence records, irrespective of the life-cycle stage or origin of peppertrees (generalized niche model). The second model only included occurrence records of naturally established mature individuals (adult niche model), while the third model was constructed with occurrence records of naturally established juvenile plants (regeneration niche model). When models were compared, the generalized <span class="hlt">climatic</span> niche model <span class="hlt">predicted</span> the presence of peppertrees in sites located farther beyond the <span class="hlt">climatic</span> thresholds that naturally established individuals can tolerate, suggesting that human activities influence the distribution of this invasive species. The adult and regeneration <span class="hlt">climatic</span> niche models concurred in their <span class="hlt">predictions</span> about the distribution of peppertrees, suggesting that naturally established adult trees only occur in sites where <span class="hlt">climatic</span> conditions allow the recruitment of juvenile stages. These results support the proposal that <span class="hlt">climatic</span> niches of invasive plants should be modelled with data of</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4494270','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4494270"><span>Livestock Helminths in a Changing <span class="hlt">Climate</span>: Approaches and Restrictions to Meaningful <span class="hlt">Predictions</span></span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Fox, Naomi J.; Marion, Glenn; Davidson, Ross S.; White, Piran C. L.; Hutchings, Michael R.</p> <p>2012-01-01</p> <p>Simple Summary Parasitic helminths represent one of the most pervasive challenges to livestock, and their intensity and distribution will be influenced by <span class="hlt">climate</span> change. There is a need for long-term <span class="hlt">predictions</span> to identify potential risks and highlight opportunities for control. We explore the approaches to modelling future helminth risk to livestock under <span class="hlt">climate</span> change. One of the limitations to model creation is the lack of purpose driven data collection. We also conclude that models need to include a broad view of the livestock system to generate meaningful <span class="hlt">predictions</span>. Abstract <span class="hlt">Climate</span> change is a driving force for livestock parasite risk. This is especially true for helminths including the nematodes Haemonchus contortus, Teladorsagia circumcincta, Nematodirus battus, and the trematode Fasciola hepatica, since survival and development of free-living stages is chiefly affected by temperature and moisture. The paucity of long term <span class="hlt">predictions</span> of helminth risk under <span class="hlt">climate</span> change has driven us to explore optimal modelling approaches and identify current bottlenecks to generating meaningful <span class="hlt">predictions</span>. We classify approaches as correlative or mechanistic, exploring their strengths and limitations. <span class="hlt">Climate</span> is one aspect of a complex system and, at the farm level, husbandry has a dominant influence on helminth transmission. Continuing environmental change will necessitate the adoption of mitigation and adaptation strategies in husbandry. Long term <span class="hlt">predictive</span> models need to have the architecture to incorporate these changes. Ultimately, an optimal modelling approach is likely to combine mechanistic processes and physiological thresholds with correlative bioclimatic modelling, incorporating changes in livestock husbandry and disease control. Irrespective of approach, the principal limitation to parasite <span class="hlt">predictions</span> is the availability of active surveillance data and empirical data on physiological responses to <span class="hlt">climate</span> variables. By combining improved empirical</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/23330960','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/23330960"><span><span class="hlt">Predicting</span> responses to <span class="hlt">climate</span> change requires all life-history stages.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Zeigler, Sara</p> <p>2013-01-01</p> <p>In Focus: Radchuk, V., Turlure, C. & Schtickzelle, N. (2013) Each life stage matters: the importance of assessing response to <span class="hlt">climate</span> change over the complete life cycle in butterflies. Journal of Animal Ecology, 82, 275-285. Population-level responses to <span class="hlt">climate</span> change depend on many factors, including unexpected interactions among life history attributes; however, few studies examine <span class="hlt">climate</span> change impacts over complete life cycles of focal species. Radchuk, Turlure & Schtickzelle () used experimental and modelling approaches to <span class="hlt">predict</span> population dynamics for the bog fritillary butterfly under warming scenarios. Although they found that warming improved fertility and survival of all stages with one exception, populations were <span class="hlt">predicted</span> to decline because overwintering larvae, whose survival declined with warming, were disproportionately important contributors to population growth. This underscores the importance of considering all life history stages in analyses of <span class="hlt">climate</span> change's effects on population dynamics. © 2012 The Authors. Journal of Animal Ecology © 2012 British Ecological Society.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.dtic.mil/docs/citations/ADA626666','DTIC-ST'); return false;" href="http://www.dtic.mil/docs/citations/ADA626666"><span>Toward Seamless Weather-<span class="hlt">Climate</span> <span class="hlt">Prediction</span> with a Global Cloud Resolving Model</span></a></p> <p><a target="_blank" href="http://www.dtic.mil/">DTIC Science & Technology</a></p> <p></p> <p>2016-01-14</p> <p>distribution is unlimited. TOWARD SEAMLESS WEATHER- <span class="hlt">CLIMATE</span> <span class="hlt">PREDICTION</span> WITH A GLOBAL CLOUD RESOLVING MODEL PI: Tim Li IPRC/SOEST, University of Hawaii at...Project Final Report 3. DATES COVERED (From - To) 1 May 2012 - 30 September 2015 4. TITLE AND SUBTITLE TOWARD SEAMLESS WEATHER- <span class="hlt">CLIMATE</span> <span class="hlt">PREDICTION</span> WITH...A GLOBAL CLOUD RESOLVING MODEL 5a. CONTRACT NUMBER 5b. GRANT NUMBER N000141210450 5c. PROGRAM ELEMENT NUMBER ONR Marine Meteorology Program 6</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/25607371','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/25607371"><span><span class="hlt">Predicting</span> <span class="hlt">climate</span>-driven regime shifts versus rebound potential in coral reefs.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Graham, Nicholas A J; Jennings, Simon; MacNeil, M Aaron; Mouillot, David; Wilson, Shaun K</p> <p>2015-02-05</p> <p><span class="hlt">Climate</span>-induced coral bleaching is among the greatest current threats to coral reefs, causing widespread loss of live coral cover. Conditions under which reefs bounce back from bleaching events or shift from coral to algal dominance are unknown, making it difficult to <span class="hlt">predict</span> and plan for differing reef responses under <span class="hlt">climate</span> change. Here we document and <span class="hlt">predict</span> long-term reef responses to a major <span class="hlt">climate</span>-induced coral bleaching event that caused unprecedented region-wide mortality of Indo-Pacific corals. Following loss of >90% live coral cover, 12 of 21 reefs recovered towards pre-disturbance live coral states, while nine reefs underwent regime shifts to fleshy macroalgae. Functional diversity of associated reef fish communities shifted substantially following bleaching, returning towards pre-disturbance structure on recovering reefs, while becoming progressively altered on regime shifting reefs. We identified threshold values for a range of factors that accurately <span class="hlt">predicted</span> ecosystem response to the bleaching event. Recovery was favoured when reefs were structurally complex and in deeper water, when density of juvenile corals and herbivorous fishes was relatively high and when nutrient loads were low. Whether reefs were inside no-take marine reserves had no bearing on ecosystem trajectory. Although conditions governing regime shift or recovery dynamics were diverse, pre-disturbance quantification of simple factors such as structural complexity and water depth accurately <span class="hlt">predicted</span> ecosystem trajectories. These findings foreshadow the likely divergent but <span class="hlt">predictable</span> outcomes for reef ecosystems in response to <span class="hlt">climate</span> change, thus guiding improved management and adaptation.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2010ems..confE..22B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2010ems..confE..22B"><span>The National Oceanic and Atmospheric <span class="hlt">Administration</span> (NOAA) <span class="hlt">Climate</span> Services Portal: A New Centralized Resource for Distributed <span class="hlt">Climate</span> Information</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Burroughs, J.; Baldwin, R.; Herring, D.; Lott, N.; Boyd, J.; Handel, S.; Niepold, F.; Shea, E.</p> <p>2010-09-01</p> <p>With the rapid rise in the development of Web technologies and <span class="hlt">climate</span> services across NOAA, there has been an increasing need for greater collaboration regarding NOAA's online <span class="hlt">climate</span> services. The drivers include the need to enhance NOAA's Web presence in response to customer requirements, emerging needs for improved decision-making capabilities across all sectors of society facing impacts from <span class="hlt">climate</span> variability and change, and the importance of leveraging <span class="hlt">climate</span> data and services to support research and public education. To address these needs, NOAA (during fiscal year 2009) embarked upon an ambitious program to develop a NOAA <span class="hlt">Climate</span> Services Portal (NCS Portal). Four NOAA offices are leading the effort: 1) the NOAA <span class="hlt">Climate</span> Program Office (CPO), 2) the National Ocean Service's Coastal Services Center (CSC), 3) the National Weather Service's <span class="hlt">Climate</span> <span class="hlt">Prediction</span> Center (CPC), and 4) the National Environmental Satellite, Data, and Information Service's (NESDIS) National <span class="hlt">Climatic</span> Data Center (NCDC). Other offices and programs are also contributing in many ways to the effort. A prototype NCS Portal is being placed online for public access in January 2010, http://www.<span class="hlt">climate</span>.gov. This website only scratches the surface of the many <span class="hlt">climate</span> services across NOAA, but this effort, via direct user engagement, will gradually expand the scope and breadth of the NCS Portal to greatly enhance the accessibility and usefulness of NOAA's <span class="hlt">climate</span> data and services.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://cfpub.epa.gov/si/si_public_record_report.cfm?dirEntryId=277755&keyword=geology&actType=&TIMSType=+&TIMSSubTypeID=&DEID=&epaNumber=&ntisID=&archiveStatus=Both&ombCat=Any&dateBeginCreated=&dateEndCreated=&dateBeginPublishedPresented=&dateEndPublishedPresented=&dateBeginUpdated=&dateEndUpdated=&dateBeginCompleted=&dateEndCompleted=&personID=&role=Any&journalID=&publisherID=&sortBy=revisionDate&count=50','EPA-EIMS'); return false;" href="https://cfpub.epa.gov/si/si_public_record_report.cfm?dirEntryId=277755&keyword=geology&actType=&TIMSType=+&TIMSSubTypeID=&DEID=&epaNumber=&ntisID=&archiveStatus=Both&ombCat=Any&dateBeginCreated=&dateEndCreated=&dateBeginPublishedPresented=&dateEndPublishedPresented=&dateBeginUpdated=&dateEndUpdated=&dateBeginCompleted=&dateEndCompleted=&personID=&role=Any&journalID=&publisherID=&sortBy=revisionDate&count=50"><span>How does spatial variability of <span class="hlt">climate</span> affect catchment streamflow <span class="hlt">predictions</span>?</span></a></p> <p><a target="_blank" href="http://oaspub.epa.gov/eims/query.page">EPA Science Inventory</a></p> <p></p> <p></p> <p>Spatial variability of <span class="hlt">climate</span> can negatively affect catchment streamflow <span class="hlt">predictions</span> if it is not explicitly accounted for in hydrologic models. In this paper, we examine the changes in streamflow <span class="hlt">predictability</span> when a hydrologic model is run with spatially variable (distribute...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015AGUFMPA23B2191G','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015AGUFMPA23B2191G"><span><span class="hlt">Prediction</span> Markets and Beliefs about <span class="hlt">Climate</span>: Results from Agent-Based Simulations</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Gilligan, J. M.; John, N. J.; van der Linden, M.</p> <p>2015-12-01</p> <p><span class="hlt">Climate</span> scientists have long been frustrated by persistent doubts a large portion of the public expresses toward the scientific consensus about anthropogenic global warming. The political and ideological polarization of this doubt led Vandenbergh, Raimi, and Gilligan [1] to propose that <span class="hlt">prediction</span> markets for <span class="hlt">climate</span> change might influence the opinions of those who mistrust the scientific community but do trust the power of markets.We have developed an agent-based simulation of a <span class="hlt">climate</span> <span class="hlt">prediction</span> market in which traders buy and sell future contracts that will pay off at some future year with a value that depends on the global average temperature at that time. The traders form a heterogeneous population with different ideological positions, different beliefs about anthropogenic global warming, and different degrees of risk aversion. We also vary characteristics of the market, including the topology of social networks among the traders, the number of traders, and the completeness of the market. Traders adjust their beliefs about <span class="hlt">climate</span> according to the gains and losses they and other traders in their social network experience. This model <span class="hlt">predicts</span> that if global temperature is predominantly driven by greenhouse gas concentrations, <span class="hlt">prediction</span> markets will cause traders' beliefs to converge toward correctly accepting anthropogenic warming as real. This convergence is largely independent of the structure of the market and the characteristics of the population of traders. However, it may take considerable time for beliefs to converge. Conversely, if temperature does not depend on greenhouse gases, the model <span class="hlt">predicts</span> that traders' beliefs will not converge. We will discuss the policy-relevance of these results and more generally, the use of agent-based market simulations for policy analysis regarding <span class="hlt">climate</span> change, seasonal agricultural weather forecasts, and other applications.[1] MP Vandenbergh, KT Raimi, & JM Gilligan. UCLA Law Rev. 61, 1962 (2014).</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.ars.usda.gov/research/publications/publication/?seqNo115=337444','TEKTRAN'); return false;" href="http://www.ars.usda.gov/research/publications/publication/?seqNo115=337444"><span><span class="hlt">Prediction</span> technologies for assessment of <span class="hlt">climate</span> change impacts</span></a></p> <p><a target="_blank" href="https://www.ars.usda.gov/research/publications/find-a-publication/">USDA-ARS?s Scientific Manuscript database</a></p> <p></p> <p></p> <p>Temperatures, precipitation, and weather patterns are changing, in response to increasing carbon dioxide in the atmosphere. With these relatively rapid changes, existing soil erosion <span class="hlt">prediction</span> technologies that rely upon <span class="hlt">climate</span> stationarity are potentially becoming less reliable. This is especiall...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://eric.ed.gov/?q=school+AND+climate&pg=3&id=EJ1136399','ERIC'); return false;" href="https://eric.ed.gov/?q=school+AND+climate&pg=3&id=EJ1136399"><span>Relationships among Student, Staff, and <span class="hlt">Administrative</span> Measures of School <span class="hlt">Climate</span> and Student Health and Academic Outcomes</span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Gase, Lauren N.; Gomez, Louis M.; Kuo, Tony; Glenn, Beth A.; Inkelas, Moira; Ponce, Ninez A.</p> <p>2017-01-01</p> <p>Background: School <span class="hlt">climate</span> is an integral part of a comprehensive approach to improving the well-being of students; however, little is known about the relationships between its different domains and measures. We examined the relationships between student, staff, and <span class="hlt">administrative</span> measures of school <span class="hlt">climate</span> to understand the extent to which they…</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_4");'>4</a></li> <li><a href="#" onclick='return showDiv("page_5");'>5</a></li> <li class="active"><span>6</span></li> <li><a href="#" onclick='return showDiv("page_7");'>7</a></li> <li><a href="#" onclick='return showDiv("page_8");'>8</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_6 --> <div id="page_7" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_5");'>5</a></li> <li><a href="#" onclick='return showDiv("page_6");'>6</a></li> <li class="active"><span>7</span></li> <li><a href="#" onclick='return showDiv("page_8");'>8</a></li> <li><a href="#" onclick='return showDiv("page_9");'>9</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="121"> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/20513712','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/20513712"><span>Woody plants and the <span class="hlt">prediction</span> of <span class="hlt">climate</span>-change impacts on bird diversity.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Kissling, W D; Field, R; Korntheuer, H; Heyder, U; Böhning-Gaese, K</p> <p>2010-07-12</p> <p>Current methods of assessing <span class="hlt">climate</span>-induced shifts of species distributions rarely account for species interactions and usually ignore potential differences in response times of interacting taxa to <span class="hlt">climate</span> change. Here, we used species-richness data from 1005 breeding bird and 1417 woody plant species in Kenya and employed model-averaged coefficients from regression models and median <span class="hlt">climatic</span> forecasts assembled across 15 <span class="hlt">climate</span>-change scenarios to <span class="hlt">predict</span> bird species richness under <span class="hlt">climate</span> change. Forecasts assuming an instantaneous response of woody plants and birds to <span class="hlt">climate</span> change suggested increases in future bird species richness across most of Kenya whereas forecasts assuming strongly lagged woody plant responses to <span class="hlt">climate</span> change indicated a reversed trend, i.e. reduced bird species richness. Uncertainties in <span class="hlt">predictions</span> of future bird species richness were geographically structured, mainly owing to uncertainties in projected precipitation changes. We conclude that assessments of future species responses to <span class="hlt">climate</span> change are very sensitive to current uncertainties in regional <span class="hlt">climate</span>-change projections, and to the inclusion or not of time-lagged interacting taxa. We expect even stronger effects for more specialized plant-animal associations. Given the slow response time of woody plant distributions to <span class="hlt">climate</span> change, current estimates of future biodiversity of many animal taxa may be both biased and too optimistic.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/26496438','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/26496438"><span>Potential Distribution <span class="hlt">Predicted</span> for Rhynchophorus ferrugineus in China under Different <span class="hlt">Climate</span> Warming Scenarios.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Ge, Xuezhen; He, Shanyong; Wang, Tao; Yan, Wei; Zong, Shixiang</p> <p>2015-01-01</p> <p>As the primary pest of palm trees, Rhynchophorus ferrugineus (Olivier) (Coleoptera: Curculionidae) has caused serious harm to palms since it first invaded China. The present study used CLIMEX 1.1 to <span class="hlt">predict</span> the potential distribution of R. ferrugineus in China according to both current <span class="hlt">climate</span> data (1981-2010) and future <span class="hlt">climate</span> warming estimates based on simulated <span class="hlt">climate</span> data for the 2020s (2011-2040) provided by the Tyndall Center for <span class="hlt">Climate</span> Change Research (TYN SC 2.0). Additionally, the Ecoclimatic Index (EI) values calculated for different <span class="hlt">climatic</span> conditions (current and future, as simulated by the B2 scenario) were compared. Areas with a suitable <span class="hlt">climate</span> for R. ferrugineus distribution were located primarily in central China according to the current <span class="hlt">climate</span> data, with the northern boundary of the distribution reaching to 40.1°N and including Tibet, north Sichuan, central Shaanxi, south Shanxi, and east Hebei. There was little difference in the potential distribution <span class="hlt">predicted</span> by the four emission scenarios according to future <span class="hlt">climate</span> warming estimates. The primary <span class="hlt">prediction</span> under future <span class="hlt">climate</span> warming models was that, compared with the current <span class="hlt">climate</span> model, the number of highly favorable habitats would increase significantly and expand into northern China, whereas the number of both favorable and marginally favorable habitats would decrease. Contrast analysis of EI values suggested that <span class="hlt">climate</span> change and the density of site distribution were the main effectors of the changes in EI values. These results will help to improve control measures, prevent the spread of this pest, and revise the targeted quarantine areas.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4619733','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4619733"><span>Potential Distribution <span class="hlt">Predicted</span> for Rhynchophorus ferrugineus in China under Different <span class="hlt">Climate</span> Warming Scenarios</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Ge, Xuezhen; He, Shanyong; Wang, Tao; Yan, Wei; Zong, Shixiang</p> <p>2015-01-01</p> <p>As the primary pest of palm trees, Rhynchophorus ferrugineus (Olivier) (Coleoptera: Curculionidae) has caused serious harm to palms since it first invaded China. The present study used CLIMEX 1.1 to <span class="hlt">predict</span> the potential distribution of R. ferrugineus in China according to both current <span class="hlt">climate</span> data (1981–2010) and future <span class="hlt">climate</span> warming estimates based on simulated <span class="hlt">climate</span> data for the 2020s (2011–2040) provided by the Tyndall Center for <span class="hlt">Climate</span> Change Research (TYN SC 2.0). Additionally, the Ecoclimatic Index (EI) values calculated for different <span class="hlt">climatic</span> conditions (current and future, as simulated by the B2 scenario) were compared. Areas with a suitable <span class="hlt">climate</span> for R. ferrugineus distribution were located primarily in central China according to the current <span class="hlt">climate</span> data, with the northern boundary of the distribution reaching to 40.1°N and including Tibet, north Sichuan, central Shaanxi, south Shanxi, and east Hebei. There was little difference in the potential distribution <span class="hlt">predicted</span> by the four emission scenarios according to future <span class="hlt">climate</span> warming estimates. The primary <span class="hlt">prediction</span> under future <span class="hlt">climate</span> warming models was that, compared with the current <span class="hlt">climate</span> model, the number of highly favorable habitats would increase significantly and expand into northern China, whereas the number of both favorable and marginally favorable habitats would decrease. Contrast analysis of EI values suggested that <span class="hlt">climate</span> change and the density of site distribution were the main effectors of the changes in EI values. These results will help to improve control measures, prevent the spread of this pest, and revise the targeted quarantine areas. PMID:26496438</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5703285','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5703285"><span><span class="hlt">Climate</span> extremes and <span class="hlt">predicted</span> warming threaten Mediterranean Holocene firs forests refugia</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Camarero, J. Julio; Carrer, Marco; Gutiérrez, Emilia; Alla, Arben Q.; Andreu-Hayles, Laia; Hevia, Andrea; Koutavas, Athanasios; Martínez-Sancho, Elisabet; Nola, Paola; Papadopoulos, Andreas; Pasho, Edmond; Toromani, Ervin</p> <p>2017-01-01</p> <p>Warmer and drier <span class="hlt">climatic</span> conditions are projected for the 21st century; however, the role played by extreme <span class="hlt">climatic</span> events on forest vulnerability is still little understood. For example, more severe droughts and heat waves could threaten quaternary relict tree refugia such as Circum-Mediterranean fir forests (CMFF). Using tree-ring data and a process-based model, we characterized the major <span class="hlt">climate</span> constraints of recent (1950–2010) CMFF growth to project their vulnerability to 21st-century <span class="hlt">climate</span>. Simulations <span class="hlt">predict</span> a 30% growth reduction in some fir species with the 2050s business-as-usual emission scenario, whereas growth would increase in moist refugia due to a longer and warmer growing season. Fir populations currently subjected to warm and dry conditions will be the most vulnerable in the late 21st century when <span class="hlt">climatic</span> conditions will be analogous to the most severe dry/heat spells causing dieback in the late 20th century. Quantification of growth trends based on <span class="hlt">climate</span> scenarios could allow defining vulnerability thresholds in tree populations. The presented <span class="hlt">predictions</span> call for conservation strategies to safeguard relict tree populations and anticipate how many refugia could be threatened by 21st-century dry spells. PMID:29109266</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29109266','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29109266"><span><span class="hlt">Climate</span> extremes and <span class="hlt">predicted</span> warming threaten Mediterranean Holocene firs forests refugia.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Sánchez-Salguero, Raúl; Camarero, J Julio; Carrer, Marco; Gutiérrez, Emilia; Alla, Arben Q; Andreu-Hayles, Laia; Hevia, Andrea; Koutavas, Athanasios; Martínez-Sancho, Elisabet; Nola, Paola; Papadopoulos, Andreas; Pasho, Edmond; Toromani, Ervin; Carreira, José A; Linares, Juan C</p> <p>2017-11-21</p> <p>Warmer and drier <span class="hlt">climatic</span> conditions are projected for the 21st century; however, the role played by extreme <span class="hlt">climatic</span> events on forest vulnerability is still little understood. For example, more severe droughts and heat waves could threaten quaternary relict tree refugia such as Circum-Mediterranean fir forests (CMFF). Using tree-ring data and a process-based model, we characterized the major <span class="hlt">climate</span> constraints of recent (1950-2010) CMFF growth to project their vulnerability to 21st-century <span class="hlt">climate</span>. Simulations <span class="hlt">predict</span> a 30% growth reduction in some fir species with the 2050s business-as-usual emission scenario, whereas growth would increase in moist refugia due to a longer and warmer growing season. Fir populations currently subjected to warm and dry conditions will be the most vulnerable in the late 21st century when <span class="hlt">climatic</span> conditions will be analogous to the most severe dry/heat spells causing dieback in the late 20th century. Quantification of growth trends based on <span class="hlt">climate</span> scenarios could allow defining vulnerability thresholds in tree populations. The presented <span class="hlt">predictions</span> call for conservation strategies to safeguard relict tree populations and anticipate how many refugia could be threatened by 21st-century dry spells.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/biblio/1027816-complex-networks-unified-framework-descriptive-analysis-predictive-modeling-climate','SCIGOV-STC'); return false;" href="https://www.osti.gov/biblio/1027816-complex-networks-unified-framework-descriptive-analysis-predictive-modeling-climate"><span>Complex networks as a unified framework for descriptive analysis and <span class="hlt">predictive</span> modeling in <span class="hlt">climate</span></span></a></p> <p><a target="_blank" href="http://www.osti.gov/search">DOE Office of Scientific and Technical Information (OSTI.GOV)</a></p> <p>Steinhaeuser, Karsten J K; Chawla, Nitesh; Ganguly, Auroop R</p> <p></p> <p>The analysis of <span class="hlt">climate</span> data has relied heavily on hypothesis-driven statistical methods, while projections of future <span class="hlt">climate</span> are based primarily on physics-based computational models. However, in recent years a wealth of new datasets has become available. Therefore, we take a more data-centric approach and propose a unified framework for studying <span class="hlt">climate</span>, with an aim towards characterizing observed phenomena as well as discovering new knowledge in the <span class="hlt">climate</span> domain. Specifically, we posit that complex networks are well-suited for both descriptive analysis and <span class="hlt">predictive</span> modeling tasks. We show that the structural properties of <span class="hlt">climate</span> networks have useful interpretation within the domain. Further,more » we extract clusters from these networks and demonstrate their <span class="hlt">predictive</span> power as <span class="hlt">climate</span> indices. Our experimental results establish that the network clusters are statistically significantly better predictors than clusters derived using a more traditional clustering approach. Using complex networks as data representation thus enables the unique opportunity for descriptive and <span class="hlt">predictive</span> modeling to inform each other.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFMGC13A1188R','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFMGC13A1188R"><span>Establishing a Real-Money <span class="hlt">Prediction</span> Market for <span class="hlt">Climate</span> on Decadal Horizons</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Roulston, M. S.; Hand, D. J.; Harding, D. W.</p> <p>2016-12-01</p> <p>A plan to establish a not-for-profit <span class="hlt">prediction</span> market that will allow participants to bet on the value of selected <span class="hlt">climate</span> variables decades into the future will be presented. It is hoped that this market will provide an objective measure of the consensus view on <span class="hlt">climate</span> change, including information concerning the uncertainty of <span class="hlt">climate</span> projections. The proposed design of the market and the definition of the <span class="hlt">climate</span> variables underlying the contracts will be discussed, as well as relevant regulatory and legal issues.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://cfpub.epa.gov/si/si_public_record_report.cfm?dirEntryId=188451&Lab=NRMRL&keyword=fossils&actType=&TIMSType=+&TIMSSubTypeID=&DEID=&epaNumber=&ntisID=&archiveStatus=Both&ombCat=Any&dateBeginCreated=&dateEndCreated=&dateBeginPublishedPresented=&dateEndPublishedPresented=&dateBeginUpdated=&dateEndUpdated=&dateBeginCompleted=&dateEndCompleted=&personID=&role=Any&journalID=&publisherID=&sortBy=revisionDate&count=50','EPA-EIMS'); return false;" href="https://cfpub.epa.gov/si/si_public_record_report.cfm?dirEntryId=188451&Lab=NRMRL&keyword=fossils&actType=&TIMSType=+&TIMSSubTypeID=&DEID=&epaNumber=&ntisID=&archiveStatus=Both&ombCat=Any&dateBeginCreated=&dateEndCreated=&dateBeginPublishedPresented=&dateEndPublishedPresented=&dateBeginUpdated=&dateEndUpdated=&dateBeginCompleted=&dateEndCompleted=&personID=&role=Any&journalID=&publisherID=&sortBy=revisionDate&count=50"><span>Timing and <span class="hlt">Prediction</span> of <span class="hlt">Climate</span> Change and Hydrological Impacts: Periodicity in Natural Variations</span></a></p> <p><a target="_blank" href="http://oaspub.epa.gov/eims/query.page">EPA Science Inventory</a></p> <p></p> <p></p> <p>Hydrological impacts from <span class="hlt">climate</span> change are of principal interest to water resource policy-makers and practicing engineers, and <span class="hlt">predictive</span> <span class="hlt">climatic</span> models have been extensively investigated to quantify the impacts. In palaeoclmatic investigations, <span class="hlt">climate</span> proxy evidence has une...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=20080032874&hterms=tropospheric+ozone&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D60%26Ntt%3Dtropospheric%2Bozone','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=20080032874&hterms=tropospheric+ozone&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D60%26Ntt%3Dtropospheric%2Bozone"><span>Role of <span class="hlt">Climate</span> Change in Global <span class="hlt">Predictions</span> of Future Tropospheric Ozone and Aerosols</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Liao, Hong; Chen, Wei-Ting; Seinfeld, John H.</p> <p>2006-01-01</p> <p>A unified tropospheric chemistry-aerosol model within the Goddard Institute for Space Studies general circulation model II is applied to simulate an equilibrium CO2-forced <span class="hlt">climate</span> in the year 2100 to examine the effects of <span class="hlt">climate</span> change on global distributions of tropospheric ozone and sulfate, nitrate, ammonium, black carbon, primary organic carbon, secondary organic carbon, sea salt, and mineral dust aerosols. The year 2100 CO2 concentration as well as the anthropogenic emissions of ozone precursors and aerosols/aerosol precursors are based on the Intergovernmental Panel on <span class="hlt">Climate</span> Change Special Report on Emissions Scenarios (SRES) A2. Year 2100 global O3 and aerosol burdens <span class="hlt">predicted</span> with changes in both <span class="hlt">climate</span> and emissions are generally 5-20% lower than those simulated with changes in emissions alone; as exceptions, the nitrate burden is 38% lower, and the secondary organic aerosol burden is 17% higher. Although the CO2-driven <span class="hlt">climate</span> change alone is <span class="hlt">predicted</span> to reduce the global O3 concentrations over or near populated and biomass burning areas because of slower transport, enhanced biogenic hydrocarbon emissions, decomposition of peroxyacetyl nitrate at higher temperatures, and the increase of O3 production by increased water vapor at high NOx levels. The warmer <span class="hlt">climate</span> influences aerosol burdens by increasing aerosol wet deposition, altering <span class="hlt">climate</span>-sensitive emissions, and shifting aerosol thermodynamic equilibrium. <span class="hlt">Climate</span> change affects the estimates of the year 2100 direct radiative forcing as a result of the <span class="hlt">climate</span>-induced changes in burdens and different climatological conditions; with full gas-aerosol coupling and accounting for ozone and direct radiative forcings by the O2, sulfate, nitrate, black carbon, and organic carbon are <span class="hlt">predicted</span> to be +0.93, -0.72, -1.0, +1.26, and -0.56 W m(exp -2), respectively, using present-day <span class="hlt">climate</span> and year 2100 emissions, while they are <span class="hlt">predicted</span> to be +0.76, -0.72, 0.74, +0.97, and -0.58 W m(exp -2</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5433747','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5433747"><span>Life history trade-off moderates model <span class="hlt">predictions</span> of diversity loss from <span class="hlt">climate</span> change</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p></p> <p>2017-01-01</p> <p><span class="hlt">Climate</span> change can trigger species range shifts, local extinctions and changes in diversity. Species interactions and dispersal capacity are important mediators of community responses to <span class="hlt">climate</span> change. The interaction between multispecies competition and variation in dispersal capacity has recently been shown to exacerbate the effects of <span class="hlt">climate</span> change on diversity and to increase <span class="hlt">predictions</span> of extinction risk dramatically. Dispersal capacity, however, is part of a species’ overall ecological strategy and are likely to trade off with other aspects of its life history that influence population growth and persistence. In plants, a well-known example is the trade-off between seed mass and seed number. The presence of such a trade-off might buffer the diversity loss <span class="hlt">predicted</span> by models with random but neutral (i.e. not impacting fitness otherwise) differences in dispersal capacity. Using a trait-based metacommunity model along a warming <span class="hlt">climatic</span> gradient the effect of three different dispersal scenarios on model <span class="hlt">predictions</span> of diversity change were compared. Adding random variation in species dispersal capacity caused extinctions by the introduction of strong fitness differences due an inherent property of the dispersal kernel. Simulations including a fitness-equalising trade-off based on empirical relationships between seed mass (here affecting dispersal distance, establishment probability, and seedling biomass) and seed number (fecundity) maintained higher initial species diversity and <span class="hlt">predicted</span> lower extinction risk and diversity loss during <span class="hlt">climate</span> change than simulations with variable dispersal capacity. Large seeded species persisted during <span class="hlt">climate</span> change, but developed lags behind their <span class="hlt">climate</span> niche that may cause extinction debts. Small seeded species were more extinction-prone during <span class="hlt">climate</span> change but tracked their niches through dispersal and colonisation, despite competitive resistance from residents. Life history trade-offs involved in coexistence</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/28520770','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/28520770"><span>Life history trade-off moderates model <span class="hlt">predictions</span> of diversity loss from <span class="hlt">climate</span> change.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Moor, Helen</p> <p>2017-01-01</p> <p><span class="hlt">Climate</span> change can trigger species range shifts, local extinctions and changes in diversity. Species interactions and dispersal capacity are important mediators of community responses to <span class="hlt">climate</span> change. The interaction between multispecies competition and variation in dispersal capacity has recently been shown to exacerbate the effects of <span class="hlt">climate</span> change on diversity and to increase <span class="hlt">predictions</span> of extinction risk dramatically. Dispersal capacity, however, is part of a species' overall ecological strategy and are likely to trade off with other aspects of its life history that influence population growth and persistence. In plants, a well-known example is the trade-off between seed mass and seed number. The presence of such a trade-off might buffer the diversity loss <span class="hlt">predicted</span> by models with random but neutral (i.e. not impacting fitness otherwise) differences in dispersal capacity. Using a trait-based metacommunity model along a warming <span class="hlt">climatic</span> gradient the effect of three different dispersal scenarios on model <span class="hlt">predictions</span> of diversity change were compared. Adding random variation in species dispersal capacity caused extinctions by the introduction of strong fitness differences due an inherent property of the dispersal kernel. Simulations including a fitness-equalising trade-off based on empirical relationships between seed mass (here affecting dispersal distance, establishment probability, and seedling biomass) and seed number (fecundity) maintained higher initial species diversity and <span class="hlt">predicted</span> lower extinction risk and diversity loss during <span class="hlt">climate</span> change than simulations with variable dispersal capacity. Large seeded species persisted during <span class="hlt">climate</span> change, but developed lags behind their <span class="hlt">climate</span> niche that may cause extinction debts. Small seeded species were more extinction-prone during <span class="hlt">climate</span> change but tracked their niches through dispersal and colonisation, despite competitive resistance from residents. Life history trade-offs involved in coexistence</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/28324174','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/28324174"><span>Combining <span class="hlt">climatic</span> and soil properties better <span class="hlt">predicts</span> covers of Brazilian biomes.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Arruda, Daniel M; Fernandes-Filho, Elpídio I; Solar, Ricardo R C; Schaefer, Carlos E G R</p> <p>2017-04-01</p> <p>Several techniques have been used to model the area covered by biomes or species. However, most models allow little freedom of choice of response variables and are conditioned to the use of <span class="hlt">climate</span> predictors. This major restriction of the models has generated distributions of low accuracy or inconsistent with the actual cover. Our objective was to characterize the environmental space of the most representative biomes of Brazil and <span class="hlt">predict</span> their cover, using <span class="hlt">climate</span> and soil-related predictors. As sample units, we used 500 cells of 100 km 2 for ten biomes, derived from the official vegetation map of Brazil (IBGE 2004). With a total of 38 (<span class="hlt">climatic</span> and soil-related) predictors, an a priori model was run with the random forest classifier. Each biome was calibrated with 75% of the samples. The final model was based on four <span class="hlt">climate</span> and six soil-related predictors, the most important variables for the a priori model, without collinearity. The model reached a kappa value of 0.82, generating a highly consistent <span class="hlt">prediction</span> with the actual cover of the country. We showed here that the richness of biomes should not be underestimated, and that in spite of the complex relationship, highly accurate modeling based on <span class="hlt">climatic</span> and soil-related predictors is possible. These predictors are complementary, for covering different parts of the multidimensional niche. Thus, a single biome can cover a wide range of <span class="hlt">climatic</span> space, versus a narrow range of soil types, so that its <span class="hlt">prediction</span> is best adjusted by soil-related variables, or vice versa.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017SciNa.104...32A','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017SciNa.104...32A"><span>Combining <span class="hlt">climatic</span> and soil properties better <span class="hlt">predicts</span> covers of Brazilian biomes</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Arruda, Daniel M.; Fernandes-Filho, Elpídio I.; Solar, Ricardo R. C.; Schaefer, Carlos E. G. R.</p> <p>2017-04-01</p> <p>Several techniques have been used to model the area covered by biomes or species. However, most models allow little freedom of choice of response variables and are conditioned to the use of <span class="hlt">climate</span> predictors. This major restriction of the models has generated distributions of low accuracy or inconsistent with the actual cover. Our objective was to characterize the environmental space of the most representative biomes of Brazil and <span class="hlt">predict</span> their cover, using <span class="hlt">climate</span> and soil-related predictors. As sample units, we used 500 cells of 100 km2 for ten biomes, derived from the official vegetation map of Brazil (IBGE 2004). With a total of 38 (<span class="hlt">climatic</span> and soil-related) predictors, an a priori model was run with the random forest classifier. Each biome was calibrated with 75% of the samples. The final model was based on four <span class="hlt">climate</span> and six soil-related predictors, the most important variables for the a priori model, without collinearity. The model reached a kappa value of 0.82, generating a highly consistent <span class="hlt">prediction</span> with the actual cover of the country. We showed here that the richness of biomes should not be underestimated, and that in spite of the complex relationship, highly accurate modeling based on <span class="hlt">climatic</span> and soil-related predictors is possible. These predictors are complementary, for covering different parts of the multidimensional niche. Thus, a single biome can cover a wide range of <span class="hlt">climatic</span> space, versus a narrow range of soil types, so that its <span class="hlt">prediction</span> is best adjusted by soil-related variables, or vice versa.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://cfpub.epa.gov/si/si_public_record_report.cfm?dirEntryId=131193&keyword=extinction&actType=&TIMSType=+&TIMSSubTypeID=&DEID=&epaNumber=&ntisID=&archiveStatus=Both&ombCat=Any&dateBeginCreated=&dateEndCreated=&dateBeginPublishedPresented=&dateEndPublishedPresented=&dateBeginUpdated=&dateEndUpdated=&dateBeginCompleted=&dateEndCompleted=&personID=&role=Any&journalID=&publisherID=&sortBy=revisionDate&count=50','EPA-EIMS'); return false;" href="https://cfpub.epa.gov/si/si_public_record_report.cfm?dirEntryId=131193&keyword=extinction&actType=&TIMSType=+&TIMSSubTypeID=&DEID=&epaNumber=&ntisID=&archiveStatus=Both&ombCat=Any&dateBeginCreated=&dateEndCreated=&dateBeginPublishedPresented=&dateEndPublishedPresented=&dateBeginUpdated=&dateEndUpdated=&dateBeginCompleted=&dateEndCompleted=&personID=&role=Any&journalID=&publisherID=&sortBy=revisionDate&count=50"><span><span class="hlt">PREDICTING</span> <span class="hlt">CLIMATE</span>-INDUCED RANGE SHIFTS: MODEL DIFFERENCES AND MODEL RELIABILITY</span></a></p> <p><a target="_blank" href="http://oaspub.epa.gov/eims/query.page">EPA Science Inventory</a></p> <p></p> <p></p> <p><span class="hlt">Predicted</span> changes in the global <span class="hlt">climate</span> are likely to cause large shifts in the geographic ranges of many plant and animal species. To date, <span class="hlt">predictions</span> of future range shifts have relied on a variety of modeling approaches with different levels of model accuracy. Using a common ...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFMGC53G..07L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFMGC53G..07L"><span>Using decadal <span class="hlt">climate</span> <span class="hlt">prediction</span> to characterize and manage changing drought and flood risks in Colorado</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Lazrus, H.; Done, J.; Morss, R. E.</p> <p>2017-12-01</p> <p>A new branch of <span class="hlt">climate</span> science, known as decadal <span class="hlt">prediction</span>, seeks to <span class="hlt">predict</span> the time-varying trajectory of <span class="hlt">climate</span> over the next 3-30 years and not just the longer-term trends. Decadal <span class="hlt">predictions</span> bring <span class="hlt">climate</span> information into the time horizon of decision makers, particularly those tasked with managing water resources and floods whose master planning is often on the timescale of decades. Information from decadal <span class="hlt">predictions</span> may help alleviate some aspects of vulnerability by helping to inform decisions that reduce drought and flood exposure and increase adaptive capacities including preparedness, response, and recovery. This presentation will highlight an interdisciplinary project - involving atmospheric and social scientists - on the development of decadal <span class="hlt">climate</span> information and its use in decision making. The presentation will explore the skill and utility of decadal drought and flood <span class="hlt">prediction</span> along Colorado's Front Range, an area experiencing rapid population growth and uncertain <span class="hlt">climate</span> variability and <span class="hlt">climate</span> change impacts. Innovative statistical and dynamical atmospheric modeling techniques explore the extent to which Colorado precipitation can be <span class="hlt">predicted</span> on decadal scales using remote Pacific Ocean surface temperature patterns. Concurrently, stakeholder interviews with flood managers in Colorado are being used to explore the potential utility of decadal <span class="hlt">climate</span> information. Combining the modeling results with results from the stakeholder interviews shows that while there is still significant uncertainty surrounding precipitation on decadal time scales, relevant and well communicated decadal information has potential to be useful for drought and flood management.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFM.H11C1184L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFM.H11C1184L"><span>Beyond <span class="hlt">Prediction</span>: the Many Ways in which <span class="hlt">Climate</span> Science can Inform Adaptation Decisions</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Lempert, R. J.</p> <p>2017-12-01</p> <p><span class="hlt">Climate</span> science provides an increasingly rich understanding of current and future <span class="hlt">climate</span>, but this understanding is often not fully incorporated into <span class="hlt">climate</span> adaptation decisions. In particular, the provision of <span class="hlt">climate</span> information is still trapped in a narrow <span class="hlt">prediction</span>-based framework, which envisions a sequential process that begins with model-based forecasts of future <span class="hlt">climate</span> and decision makers then acting on those forecasts. Among its challenges, this framework can discourage action when <span class="hlt">climate</span> <span class="hlt">predictions</span> are deemed too uncertain, encourage overconfidence when <span class="hlt">climate</span> scientists and decision makers fail to focus on decision-relevant but poorly understood extreme events, and offers a too-narrow communication path among <span class="hlt">climate</span> scientists and decision makers. This talk will describe how robust decision approaches, organized around the idea of stress testing proposed adaptation decisions over a wide range of futures, can enable a richer flow information among <span class="hlt">climate</span> scientists and decision makers. The talk illustrates these themes with two examples: 1) conservation management that explores the tradeoffs among alternative <span class="hlt">climate</span> information products with different combinations of ensemble size and spatial resolution and 2) water quality implementation planning that focuses on the handling of extremes.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.noaa.gov/climate','SCIGOVWS'); return false;" href="http://www.noaa.gov/climate"><span><span class="hlt">Climate</span> | National Oceanic and Atmospheric <span class="hlt">Administration</span></span></a></p> <p><a target="_blank" href="http://www.science.gov/aboutsearch.html">Science.gov Websites</a></p> <p></p> <p></p> <p>to help people understand and prepare for <em><span class="hlt">climate</span></em> variability and <em>change</em>. <em><span class="hlt">Climate</span></em>. NOAA From to help people understand and prepare for <em><span class="hlt">climate</span></em> variability and <em>change</em>. LATEST FEATURES // Ocean Jump to Content Enter Search Terms Weather <em><span class="hlt">Climate</span></em> Oceans & Coasts Fisheries Satellites</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/26486780','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/26486780"><span>Livestock Helminths in a Changing <span class="hlt">Climate</span>: Approaches and Restrictions to Meaningful <span class="hlt">Predictions</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Fox, Naomi J; Marion, Glenn; Davidson, Ross S; White, Piran C L; Hutchings, Michael R</p> <p>2012-03-06</p> <p><span class="hlt">Climate</span> change is a driving force for livestock parasite risk. This is especially true for helminths including the nematodes Haemonchus contortus, Teladorsagia circumcincta, Nematodirus battus, and the trematode Fasciola hepatica, since survival and development of free-living stages is chiefly affected by temperature and moisture. The paucity of long term <span class="hlt">predictions</span> of helminth risk under <span class="hlt">climate</span> change has driven us to explore optimal modelling approaches and identify current bottlenecks to generating meaningful <span class="hlt">predictions</span>. We classify approaches as correlative or mechanistic, exploring their strengths and limitations. <span class="hlt">Climate</span> is one aspect of a complex system and, at the farm level, husbandry has a dominant influence on helminth transmission. Continuing environmental change will necessitate the adoption of mitigation and adaptation strategies in husbandry. Long term <span class="hlt">predictive</span> models need to have the architecture to incorporate these changes. Ultimately, an optimal modelling approach is likely to combine mechanistic processes and physiological thresholds with correlative bioclimatic modelling, incorporating changes in livestock husbandry and disease control. Irrespective of approach, the principal limitation to parasite <span class="hlt">predictions</span> is the availability of active surveillance data and empirical data on physiological responses to <span class="hlt">climate</span> variables. By combining improved empirical data and refined models with a broad view of the livestock system, robust projections of helminth risk can be developed.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://files.eric.ed.gov/fulltext/EJ1134498.pdf','ERIC'); return false;" href="http://files.eric.ed.gov/fulltext/EJ1134498.pdf"><span>Effects of the Leadership Roles of <span class="hlt">Administrators</span> Who Work at Special Education Schools upon Organizational <span class="hlt">Climate</span></span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Üstün, Ahmet</p> <p>2017-01-01</p> <p>This research aims to determine the effects of the leadership roles of <span class="hlt">administrators</span> who work at special education schools upon organizational <span class="hlt">climate</span>. This research has been conducted using the case study technique, which is a kind of qualitative research approach. The study group of this research consists of four <span class="hlt">administrators</span> including three…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/biblio/1408807-us-climate-variability-predictability-clivar-project-final-report','SCIGOV-STC'); return false;" href="https://www.osti.gov/biblio/1408807-us-climate-variability-predictability-clivar-project-final-report"><span>US <span class="hlt">Climate</span> Variability and <span class="hlt">Predictability</span> (CLIVAR) Project- Final Report</span></a></p> <p><a target="_blank" href="http://www.osti.gov/search">DOE Office of Scientific and Technical Information (OSTI.GOV)</a></p> <p>Patterson, Mike</p> <p></p> <p>The US CLIVAR Project Office administers the US CLIVAR Program with its mission to advance understanding and <span class="hlt">prediction</span> of <span class="hlt">climate</span> variability and change across timescales with an emphasis on the role of the ocean and its interaction with other elements of the Earth system. The Project Office promotes and facilitates scientific collaboration within the US and international <span class="hlt">climate</span> and Earth science communities, addressing priority topics from subseasonal to centennial <span class="hlt">climate</span> variability and change; the global energy imbalance; the ocean’s role in <span class="hlt">climate</span>, water, and carbon cycles; <span class="hlt">climate</span> and weather extremes; and polar <span class="hlt">climate</span> changes. This project provides essential one-year supportmore » of the Project Office, enabling the participation of US scientists in the meetings of the US CLIVAR bodies that guide scientific planning and implementation, including the scientific steering committee that establishes program goals and evaluates progress of activities to address them, the science team of funded investigators studying the ocean overturning circulation in the Atlantic, and two working groups tackling the priority research topics of Arctic change influence on midlatitude <span class="hlt">climate</span> and weather extremes and the decadal-scale widening of the tropical belt.« less</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_5");'>5</a></li> <li><a href="#" onclick='return showDiv("page_6");'>6</a></li> <li class="active"><span>7</span></li> <li><a href="#" onclick='return showDiv("page_8");'>8</a></li> <li><a href="#" onclick='return showDiv("page_9");'>9</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_7 --> <div id="page_8" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_6");'>6</a></li> <li><a href="#" onclick='return showDiv("page_7");'>7</a></li> <li class="active"><span>8</span></li> <li><a href="#" onclick='return showDiv("page_9");'>9</a></li> <li><a href="#" onclick='return showDiv("page_10");'>10</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="141"> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015ClDy...44.2723B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015ClDy...44.2723B"><span>The <span class="hlt">prediction</span> of surface temperature in the new seasonal <span class="hlt">prediction</span> system based on the MPI-ESM coupled <span class="hlt">climate</span> model</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Baehr, J.; Fröhlich, K.; Botzet, M.; Domeisen, D. I. V.; Kornblueh, L.; Notz, D.; Piontek, R.; Pohlmann, H.; Tietsche, S.; Müller, W. A.</p> <p>2015-05-01</p> <p>A seasonal forecast system is presented, based on the global coupled <span class="hlt">climate</span> model MPI-ESM as used for CMIP5 simulations. We describe the initialisation of the system and analyse its <span class="hlt">predictive</span> skill for surface temperature. The presented system is initialised in the atmospheric, oceanic, and sea ice component of the model from reanalysis/observations with full field nudging in all three components. For the initialisation of the ensemble, bred vectors with a vertically varying norm are implemented in the ocean component to generate initial perturbations. In a set of ensemble hindcast simulations, starting each May and November between 1982 and 2010, we analyse the <span class="hlt">predictive</span> skill. Bias-corrected ensemble forecasts for each start date reproduce the observed surface temperature anomalies at 2-4 months lead time, particularly in the tropics. Niño3.4 sea surface temperature anomalies show a small root-mean-square error and <span class="hlt">predictive</span> skill up to 6 months. Away from the tropics, <span class="hlt">predictive</span> skill is mostly limited to the ocean, and to regions which are strongly influenced by ENSO teleconnections. In summary, the presented seasonal <span class="hlt">prediction</span> system based on a coupled <span class="hlt">climate</span> model shows <span class="hlt">predictive</span> skill for surface temperature at seasonal time scales comparable to other seasonal <span class="hlt">prediction</span> systems using different underlying models and initialisation strategies. As the same model underlying our seasonal <span class="hlt">prediction</span> system—with a different initialisation—is presently also used for decadal <span class="hlt">predictions</span>, this is an important step towards seamless seasonal-to-decadal <span class="hlt">climate</span> <span class="hlt">predictions</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70119412','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70119412"><span>Space can substitute for time in <span class="hlt">predicting</span> <span class="hlt">climate</span>-change effects on biodiversity</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Blois, Jessica L.; Williams, John W.; Fitzpatrick, Matthew C.; Jackson, Stephen T.; Ferrier, Simon</p> <p>2013-01-01</p> <p>“Space-for-time” substitution is widely used in biodiversity modeling to infer past or future trajectories of ecological systems from contemporary spatial patterns. However, the foundational assumption—that drivers of spatial gradients of species composition also drive temporal changes in diversity—rarely is tested. Here, we empirically test the space-for-time assumption by constructing orthogonal datasets of compositional turnover of plant taxa and <span class="hlt">climatic</span> dissimilarity through time and across space from Late Quaternary pollen records in eastern North America, then modeling <span class="hlt">climate</span>-driven compositional turnover. <span class="hlt">Predictions</span> relying on space-for-time substitution were ∼72% as accurate as “time-for-time” <span class="hlt">predictions</span>. However, space-for-time substitution performed poorly during the Holocene when temporal variation in <span class="hlt">climate</span> was small relative to spatial variation and required subsampling to match the extent of spatial and temporal <span class="hlt">climatic</span> gradients. Despite this caution, our results generally support the judicious use of space-for-time substitution in modeling community responses to <span class="hlt">climate</span> change.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/23690569','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/23690569"><span>Space can substitute for time in <span class="hlt">predicting</span> <span class="hlt">climate</span>-change effects on biodiversity.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Blois, Jessica L; Williams, John W; Fitzpatrick, Matthew C; Jackson, Stephen T; Ferrier, Simon</p> <p>2013-06-04</p> <p>"Space-for-time" substitution is widely used in biodiversity modeling to infer past or future trajectories of ecological systems from contemporary spatial patterns. However, the foundational assumption--that drivers of spatial gradients of species composition also drive temporal changes in diversity--rarely is tested. Here, we empirically test the space-for-time assumption by constructing orthogonal datasets of compositional turnover of plant taxa and <span class="hlt">climatic</span> dissimilarity through time and across space from Late Quaternary pollen records in eastern North America, then modeling <span class="hlt">climate</span>-driven compositional turnover. <span class="hlt">Predictions</span> relying on space-for-time substitution were ∼72% as accurate as "time-for-time" <span class="hlt">predictions</span>. However, space-for-time substitution performed poorly during the Holocene when temporal variation in <span class="hlt">climate</span> was small relative to spatial variation and required subsampling to match the extent of spatial and temporal <span class="hlt">climatic</span> gradients. Despite this caution, our results generally support the judicious use of space-for-time substitution in modeling community responses to <span class="hlt">climate</span> change.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/23350033','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/23350033"><span><span class="hlt">Predictions</span> of avian Plasmodium expansion under <span class="hlt">climate</span> change.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Loiseau, Claire; Harrigan, Ryan J; Bichet, Coraline; Julliard, Romain; Garnier, Stéphane; Lendvai, Adám Z; Chastel, Olivier; Sorci, Gabriele</p> <p>2013-01-01</p> <p>Vector-borne diseases are particularly responsive to changing environmental conditions. Diurnal temperature variation has been identified as a particularly important factor for the development of malaria parasites within vectors. Here, we conducted a survey across France, screening populations of the house sparrow (Passer domesticus) for malaria (Plasmodium relictum). We investigated whether variation in remotely-sensed environmental variables accounted for the spatial variation observed in prevalence and parasitemia. While prevalence was highly correlated to diurnal temperature range and other measures of temperature variation, environmental conditions could not <span class="hlt">predict</span> spatial variation in parasitemia. Based on our empirical data, we mapped malaria distribution under <span class="hlt">climate</span> change scenarios and <span class="hlt">predicted</span> that Plasmodium occurrence will spread to regions in northern France, and that prevalence levels are likely to increase in locations where transmission already occurs. Our findings, based on remote sensing tools coupled with empirical data suggest that <span class="hlt">climatic</span> change will significantly alter transmission of malaria parasites.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70034288','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70034288"><span><span class="hlt">Climatic</span> extremes improve <span class="hlt">predictions</span> of spatial patterns of tree species</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Zimmermann, N.E.; Yoccoz, N.G.; Edwards, T.C.; Meier, E.S.; Thuiller, W.; Guisan, Antoine; Schmatz, D.R.; Pearman, P.B.</p> <p>2009-01-01</p> <p>Understanding niche evolution, dynamics, and the response of species to <span class="hlt">climate</span> change requires knowledge of the determinants of the environmental niche and species range limits. Mean values of <span class="hlt">climatic</span> variables are often used in such analyses. In contrast, the increasing frequency of <span class="hlt">climate</span> extremes suggests the importance of understanding their additional influence on range limits. Here, we assess how measures representing <span class="hlt">climate</span> extremes (i.e., interannual variability in <span class="hlt">climate</span> parameters) explain and <span class="hlt">predict</span> spatial patterns of 11 tree species in Switzerland. We find clear, although comparably small, improvement (+20% in adjusted D2, +8% and +3% in cross-validated True Skill Statistic and area under the receiver operating characteristics curve values) in models that use measures of extremes in addition to means. The primary effect of including information on <span class="hlt">climate</span> extremes is a correction of local overprediction and underprediction. Our results demonstrate that measures of <span class="hlt">climate</span> extremes are important for understanding the <span class="hlt">climatic</span> limits of tree species and assessing species niche characteristics. The inclusion of <span class="hlt">climate</span> variability likely will improve models of species range limits under future conditions, where changes in mean <span class="hlt">climate</span> and increased variability are expected.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2010EGUGA..1213972P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2010EGUGA..1213972P"><span>Nudging atmosphere and ocean reanalyses for seasonal <span class="hlt">climate</span> <span class="hlt">predictions</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Piontek, Robert; Baehr, Johanna; Kornblueh, Luis; Müller, Wolfgang Alexander; Haak, Helmuth; Botzet, Michael; Matei, Daniela</p> <p>2010-05-01</p> <p>Seasonal <span class="hlt">climate</span> forecasts based on state-of-the-art <span class="hlt">climate</span> models have been developed recently. Here, we critically discuss the obstacles encountered in the setup of the ECHAM6/MPIOM global coupled <span class="hlt">climate</span> model to perform <span class="hlt">climate</span> <span class="hlt">predictions</span> on seasonal to decadal time scales. We particularly focus on the initialization procedure, especially on the implementation of the nudging scheme, in which different reanalysis products are used in the atmosphere (e.g.ERA40), and the ocean (e.g., GECCO). Nudging in the atmosphere appears to be sensitive to the following choices: limiting the spectral range of nudging, whether or not temperature is nudged, the strength of the nudging coefficient for surface pressure, and the height at which the planetary boundary layer is excluded from nudging. We find that including nudging in both the atmosphere and the ocean gives improved results over nudging only the ocean or the atmosphere. For the implementation of the nudging in the atmosphere, we find the most significant improvements in the solution when either the planetary boundary layer is excluded, or if nudging of temperature is omitted. There are significant improvements in the solution when resolution is increased in both the atmosphere and in the ocean. Our tests form the basis for the <span class="hlt">prediction</span> system introduced in the abstract of Müller et al., where hindcasts are analysed as well.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/21249228','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/21249228"><span><span class="hlt">Predicting</span> impacts of <span class="hlt">climate</span> change on Fasciola hepatica risk.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Fox, Naomi J; White, Piran C L; McClean, Colin J; Marion, Glenn; Evans, Andy; Hutchings, Michael R</p> <p>2011-01-10</p> <p>Fasciola hepatica (liver fluke) is a physically and economically devastating parasitic trematode whose rise in recent years has been attributed to <span class="hlt">climate</span> change. <span class="hlt">Climate</span> has an impact on the free-living stages of the parasite and its intermediate host Lymnaea truncatula, with the interactions between rainfall and temperature having the greatest influence on transmission efficacy. There have been a number of short term <span class="hlt">climate</span> driven forecasts developed to <span class="hlt">predict</span> the following season's infection risk, with the Ollerenshaw index being the most widely used. Through the synthesis of a modified Ollerenshaw index with the UKCP09 fine scale <span class="hlt">climate</span> projection data we have developed long term seasonal risk forecasts up to 2070 at a 25 km square resolution. Additionally UKCIP gridded datasets at 5 km square resolution from 1970-2006 were used to highlight the <span class="hlt">climate</span>-driven increase to date. The maps show unprecedented levels of future fasciolosis risk in parts of the UK, with risk of serious epidemics in Wales by 2050. The seasonal risk maps demonstrate the possible change in the timing of disease outbreaks due to increased risk from overwintering larvae. Despite an overall long term increase in all regions of the UK, spatio-temporal variation in risk levels is expected. Infection risk will reduce in some areas and fluctuate greatly in others with a <span class="hlt">predicted</span> decrease in summer infection for parts of the UK due to restricted water availability. This forecast is the first approximation of the potential impacts of <span class="hlt">climate</span> change on fasciolosis risk in the UK. It can be used as a basis for indicating where active disease surveillance should be targeted and where the development of improved mitigation or adaptation measures is likely to bring the greatest benefits.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014EGUGA..1612973C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014EGUGA..1612973C"><span>Can phenological models <span class="hlt">predict</span> tree phenology accurately under <span class="hlt">climate</span> change conditions?</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Chuine, Isabelle; Bonhomme, Marc; Legave, Jean Michel; García de Cortázar-Atauri, Inaki; Charrier, Guillaume; Lacointe, André; Améglio, Thierry</p> <p>2014-05-01</p> <p>The onset of the growing season of trees has been globally earlier by 2.3 days/decade during the last 50 years because of global warming and this trend is <span class="hlt">predicted</span> to continue according to <span class="hlt">climate</span> forecast. The effect of temperature on plant phenology is however not linear because temperature has a dual effect on bud development. On one hand, low temperatures are necessary to break bud dormancy, and on the other hand higher temperatures are necessary to promote bud cells growth afterwards. Increasing phenological changes in temperate woody species have strong impacts on forest trees distribution and productivity, as well as crops cultivation areas. Accurate <span class="hlt">predictions</span> of trees phenology are therefore a prerequisite to understand and foresee the impacts of <span class="hlt">climate</span> change on forests and agrosystems. Different process-based models have been developed in the last two decades to <span class="hlt">predict</span> the date of budburst or flowering of woody species. They are two main families: (1) one-phase models which consider only the ecodormancy phase and make the assumption that endodormancy is always broken before adequate <span class="hlt">climatic</span> conditions for cell growth occur; and (2) two-phase models which consider both the endodormancy and ecodormancy phases and <span class="hlt">predict</span> a date of dormancy break which varies from year to year. So far, one-phase models have been able to <span class="hlt">predict</span> accurately tree bud break and flowering under historical <span class="hlt">climate</span>. However, because they do not consider what happens prior to ecodormancy, and especially the possible negative effect of winter temperature warming on dormancy break, it seems unlikely that they can provide accurate <span class="hlt">predictions</span> in future <span class="hlt">climate</span> conditions. It is indeed well known that a lack of low temperature results in abnormal pattern of bud break and development in temperate fruit trees. An accurate modelling of the dormancy break date has thus become a major issue in phenology modelling. Two-phases phenological models <span class="hlt">predict</span> that global warming should delay</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016JGRD..12112125W','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016JGRD..12112125W"><span>Land-atmosphere coupling and <span class="hlt">climate</span> <span class="hlt">prediction</span> over the U.S. Southern Great Plains</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Williams, Ian N.; Lu, Yaqiong; Kueppers, Lara M.; Riley, William J.; Biraud, Sebastien C.; Bagley, Justin E.; Torn, Margaret S.</p> <p>2016-10-01</p> <p>Biases in land-atmosphere coupling in <span class="hlt">climate</span> models can contribute to <span class="hlt">climate</span> <span class="hlt">prediction</span> biases, but land models are rarely evaluated in the context of this coupling. We tested land-atmosphere coupling and explored effects of land surface parameterizations on <span class="hlt">climate</span> <span class="hlt">prediction</span> in a single-column version of the National Center for Atmospheric Research Community Earth System Model (CESM1.2.2) and an off-line Community Land Model (CLM4.5). The correlation between leaf area index (LAI) and surface evaporative fraction (ratio of latent to total turbulent heat flux) was substantially underpredicted compared to observations in the U.S. Southern Great Plains, while the correlation between soil moisture and evaporative fraction was overpredicted by CLM4.5. To estimate the impacts of these errors on <span class="hlt">climate</span> <span class="hlt">prediction</span>, we modified CLM4.5 by prescribing observed LAI, increasing soil resistance to evaporation, increasing minimum stomatal conductance, and increasing leaf reflectance. The modifications improved the <span class="hlt">predicted</span> soil moisture-evaporative fraction (EF) and LAI-EF correlations in off-line CLM4.5 and reduced the root-mean-square error in summer 2 m air temperature and precipitation in the coupled model. The modifications had the largest effect on <span class="hlt">prediction</span> during a drought in summer 2006, when a warm bias in daytime 2 m air temperature was reduced from +6°C to a smaller cold bias of -1.3°C, and a corresponding dry bias in precipitation was reduced from -111 mm to -23 mm. The role of vegetation in droughts and heat waves is underpredicted in CESM1.2.2, and improvements in land surface models can improve <span class="hlt">prediction</span> of <span class="hlt">climate</span> extremes.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3962238','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3962238"><span>Can the biomass-ratio hypothesis <span class="hlt">predict</span> mixed-species litter decomposition along a <span class="hlt">climatic</span> gradient?</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Tardif, Antoine; Shipley, Bill; Bloor, Juliette M. G.; Soussana, Jean-François</p> <p>2014-01-01</p> <p>Background and Aims The biomass-ratio hypothesis states that ecosystem properties are driven by the characteristics of dominant species in the community. In this study, the hypothesis was operationalized as community-weighted means (CWMs) of monoculture values and tested for <span class="hlt">predicting</span> the decomposition of multispecies litter mixtures along an abiotic gradient in the field. Methods Decomposition rates (mg g−1 d−1) of litter from four herb species were measured using litter-bed experiments with the same soil at three sites in central France along a correlated <span class="hlt">climatic</span> gradient of temperature and precipitation. All possible combinations from one to four species mixtures were tested over 28 weeks of incubation. Observed mixture decomposition rates were compared with those <span class="hlt">predicted</span> by the biomass-ratio hypothesis. Variability of the <span class="hlt">prediction</span> errors was compared with the species richness of the mixtures, across sites, and within sites over time. Key Results Both positive and negative <span class="hlt">prediction</span> errors occurred. Despite this, the biomass-ratio hypothesis was true as an average claim for all sites (r = 0·91) and for each site separately, except for the <span class="hlt">climatically</span> intermediate site, which showed mainly synergistic deviations. Variability decreased with increasing species richness and in less favourable <span class="hlt">climatic</span> conditions for decomposition. Conclusions Community-weighted mean values provided good <span class="hlt">predictions</span> of mixed-species litter decomposition, converging to the <span class="hlt">predicted</span> values with increasing species richness and in <span class="hlt">climates</span> less favourable to decomposition. Under a context of <span class="hlt">climate</span> change, abiotic variability would be important to take into account when <span class="hlt">predicting</span> ecosystem processes. PMID:24482152</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017ClDy...49.2365O','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017ClDy...49.2365O"><span><span class="hlt">Climate</span> <span class="hlt">predictability</span> and <span class="hlt">prediction</span> skill on seasonal time scales over South America from CHFP models</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Osman, Marisol; Vera, C. S.</p> <p>2017-10-01</p> <p>This work presents an assessment of the <span class="hlt">predictability</span> and skill of <span class="hlt">climate</span> anomalies over South America. The study was made considering a multi-model ensemble of seasonal forecasts for surface air temperature, precipitation and regional circulation, from coupled global circulation models included in the <span class="hlt">Climate</span> Historical Forecast Project. <span class="hlt">Predictability</span> was evaluated through the estimation of the signal-to-total variance ratio while <span class="hlt">prediction</span> skill was assessed computing anomaly correlation coefficients. Both indicators present over the continent higher values at the tropics than at the extratropics for both, surface air temperature and precipitation. Moreover, <span class="hlt">predictability</span> and <span class="hlt">prediction</span> skill for temperature are slightly higher in DJF than in JJA while for precipitation they exhibit similar levels in both seasons. The largest values of <span class="hlt">predictability</span> and skill for both variables and seasons are found over northwestern South America while modest but still significant values for extratropical precipitation at southeastern South America and the extratropical Andes. The <span class="hlt">predictability</span> levels in ENSO years of both variables are slightly higher, although with the same spatial distribution, than that obtained considering all years. Nevertheless, <span class="hlt">predictability</span> at the tropics for both variables and seasons diminishes in both warm and cold ENSO years respect to that in all years. The latter can be attributed to changes in signal rather than in the noise. <span class="hlt">Predictability</span> and <span class="hlt">prediction</span> skill for low-level winds and upper-level zonal winds over South America was also assessed. Maximum levels of <span class="hlt">predictability</span> for low-level winds were found were maximum mean values are observed, i.e. the regions associated with the equatorial trade winds, the midlatitudes westerlies and the South American Low-Level Jet. <span class="hlt">Predictability</span> maxima for upper-level zonal winds locate where the subtropical jet peaks. Seasonal changes in wind <span class="hlt">predictability</span> are observed that seem to be related to</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=20090026582&hterms=imbalance&qs=N%3D0%26Ntk%3DAll%26Ntx%3Dmode%2Bmatchall%26Ntt%3Dimbalance','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=20090026582&hterms=imbalance&qs=N%3D0%26Ntk%3DAll%26Ntx%3Dmode%2Bmatchall%26Ntt%3Dimbalance"><span>Monitoring Top-of-Atmosphere Radiative Energy Imbalance for <span class="hlt">Climate</span> <span class="hlt">Prediction</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Lin, Bing; Chambers, Lin H.; Stackhouse, Paul W., Jr.; Minnis, Patrick</p> <p>2009-01-01</p> <p>Large <span class="hlt">climate</span> feedback uncertainties limit the <span class="hlt">prediction</span> accuracy of the Earth s future <span class="hlt">climate</span> with an increased CO2 atmosphere. One potential to reduce the feedback uncertainties using satellite observations of top-of-atmosphere (TOA) radiative energy imbalance is explored. Instead of solving the initial condition problem in previous energy balance analysis, current study focuses on the boundary condition problem with further considerations on <span class="hlt">climate</span> system memory and deep ocean heat transport, which is more applicable for the <span class="hlt">climate</span>. Along with surface temperature measurements of the present <span class="hlt">climate</span>, the <span class="hlt">climate</span> feedbacks are obtained based on the constraints of the TOA radiation imbalance. Comparing to the feedback factor of 3.3 W/sq m/K of the neutral <span class="hlt">climate</span> system, the estimated feedback factor for the current <span class="hlt">climate</span> system ranges from -1.3 to -1.0 W/sq m/K with an uncertainty of +/-0.26 W/sq m/K. That is, a positive <span class="hlt">climate</span> feedback is found because of the measured TOA net radiative heating (0.85 W/sq m) to the <span class="hlt">climate</span> system. The uncertainty is caused by the uncertainties in the <span class="hlt">climate</span> memory length. The estimated time constant of the <span class="hlt">climate</span> is large (70 to approx. 120 years), implying that the <span class="hlt">climate</span> is not in an equilibrium state under the increasing CO2 forcing in the last century.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://cfpub.epa.gov/si/si_public_record_report.cfm?dirEntryId=141569&keyword=extinction&actType=&TIMSType=+&TIMSSubTypeID=&DEID=&epaNumber=&ntisID=&archiveStatus=Both&ombCat=Any&dateBeginCreated=&dateEndCreated=&dateBeginPublishedPresented=&dateEndPublishedPresented=&dateBeginUpdated=&dateEndUpdated=&dateBeginCompleted=&dateEndCompleted=&personID=&role=Any&journalID=&publisherID=&sortBy=revisionDate&count=50','EPA-EIMS'); return false;" href="https://cfpub.epa.gov/si/si_public_record_report.cfm?dirEntryId=141569&keyword=extinction&actType=&TIMSType=+&TIMSSubTypeID=&DEID=&epaNumber=&ntisID=&archiveStatus=Both&ombCat=Any&dateBeginCreated=&dateEndCreated=&dateBeginPublishedPresented=&dateEndPublishedPresented=&dateBeginUpdated=&dateEndUpdated=&dateBeginCompleted=&dateEndCompleted=&personID=&role=Any&journalID=&publisherID=&sortBy=revisionDate&count=50"><span><span class="hlt">PREDICTING</span> <span class="hlt">CLIMATE</span>-INDUCED RANGE SHIFTS FOR MAMMALS: HOW GOOD ARE THE MODELS?</span></a></p> <p><a target="_blank" href="http://oaspub.epa.gov/eims/query.page">EPA Science Inventory</a></p> <p></p> <p></p> <p>In order to manage wildlife and conserve biodiversity, it is critical that we understand the potential impacts of <span class="hlt">climate</span> change on species distributions. Several different approaches to <span class="hlt">predicting</span> <span class="hlt">climate</span>-induced geographic range shifts have been proposed to address this proble...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/28221708','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/28221708"><span>Improved management of small pelagic fisheries through seasonal <span class="hlt">climate</span> <span class="hlt">prediction</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Tommasi, Désirée; Stock, Charles A; Pegion, Kathleen; Vecchi, Gabriel A; Methot, Richard D; Alexander, Michael A; Checkley, David M</p> <p>2017-03-01</p> <p>Populations of small pelagic fish are strongly influenced by <span class="hlt">climate</span>. The inability of managers to anticipate environment-driven fluctuations in stock productivity or distribution can lead to overfishing and stock collapses, inflexible management regulations inducing shifts in the functional response to human predators, lost opportunities to harvest populations, bankruptcies in the fishing industry, and loss of resilience in the human food supply. Recent advances in dynamical global <span class="hlt">climate</span> <span class="hlt">prediction</span> systems allow for sea surface temperature (SST) anomaly <span class="hlt">predictions</span> at a seasonal scale over many shelf ecosystems. Here we assess the utility of SST <span class="hlt">predictions</span> at this "fishery relevant" scale to inform management, using Pacific sardine as a case study. The value of SST anomaly <span class="hlt">predictions</span> to management was quantified under four harvest guidelines (HGs) differing in their level of integration of SST data and <span class="hlt">predictions</span>. The HG that incorporated stock biomass forecasts informed by skillful SST <span class="hlt">predictions</span> led to increases in stock biomass and yield, and reductions in the probability of yield and biomass falling below socioeconomic or ecologically acceptable levels. However, to mitigate the risk of collapse in the event of an erroneous forecast, it was important to combine such forecast-informed harvest controls with additional harvest restrictions at low biomass. © 2016 by the Ecological Society of America.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017EGUGA..19.4289K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017EGUGA..19.4289K"><span><span class="hlt">Climate</span> change and <span class="hlt">predicting</span> soil loss from rainfall</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Kinnell, Peter</p> <p>2017-04-01</p> <p>Conceptually, rainfall has a certain capacity to cause soil loss from an eroding area while soil surfaces have a certain resistance to being eroded by rainfall. The terms "rainfall erosivity' and "soil erodibility" are frequently used to encapsulate the concept and in the Revised Universal Soil Loss Equation (RUSLE), the most widely used soil loss <span class="hlt">prediction</span> equation in the world, average annual values of the R "erosivity" factor and the K "erodibility" factor provide a basis for accounting for variation in rainfall erosion associated with geographic variations of <span class="hlt">climate</span> and soils. In many applications of RUSLE, R and K are considered to be independent but in reality they are not. In RUSLE2, provision has been made to take account of the fact that K values determined using soil physical factors have to be adjusted for variations in <span class="hlt">climate</span> because runoff is not directly included as a factor in determining R. Also, the USLE event erosivity index EI30 is better related to accounting for event sediment concentration than event soil loss. While the USLE-M, a modification of the USLE which includes runoff as a factor in determining the event erosivity index provides better estimates of event soil loss when event runoff is known, runoff <span class="hlt">prediction</span> provides a challenge to modelling event soil loss as <span class="hlt">climate</span> changes</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29302012','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29302012"><span>Genomic signals of selection <span class="hlt">predict</span> <span class="hlt">climate</span>-driven population declines in a migratory bird.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Bay, Rachael A; Harrigan, Ryan J; Underwood, Vinh Le; Gibbs, H Lisle; Smith, Thomas B; Ruegg, Kristen</p> <p>2018-01-05</p> <p>The ongoing loss of biodiversity caused by rapid <span class="hlt">climatic</span> shifts requires accurate models for <span class="hlt">predicting</span> species' responses. Despite evidence that evolutionary adaptation could mitigate <span class="hlt">climate</span> change impacts, evolution is rarely integrated into <span class="hlt">predictive</span> models. Integrating population genomics and environmental data, we identified genomic variation associated with <span class="hlt">climate</span> across the breeding range of the migratory songbird, yellow warbler ( Setophaga petechia ). Populations requiring the greatest shifts in allele frequencies to keep pace with future <span class="hlt">climate</span> change have experienced the largest population declines, suggesting that failure to adapt may have already negatively affected populations. Broadly, our study suggests that the integration of genomic adaptation can increase the accuracy of future species distribution models and ultimately guide more effective mitigation efforts. Copyright © 2018, American Association for the Advancement of Science.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015AGUFM.H12B..02A','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015AGUFM.H12B..02A"><span>Darcy's law <span class="hlt">predicts</span> widespread forest mortalityunder <span class="hlt">climate</span> warming</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Allen, C. D.; McDowell, N. G.</p> <p>2015-12-01</p> <p>Drought and heat-induced tree mortality is accelerating in many forest biomes as a consequence of a warming <span class="hlt">climate</span>, resulting in a threat to global forests unlike any in recorded history. Forests store the majority of terrestrial carbon, thus their loss may have significant and sustained impacts on the global carbon cycle. We used a hydraulic corollary to Darcy's law, a core principle of vascular plant physiology, to <span class="hlt">predict</span> characteristics of plants that will survive and die during drought under warmer future <span class="hlt">climates</span>. Plants that are tall with isohydric stomatal regulation, low hydraulic conductance, and high leaf area are most likely to die from future drought stress. Thus, tall trees of old-growth forests are at the greatest risk of loss, which has ominous implications for terrestrial carbon storage. This application of Darcy's law indicates today's forests generally should be replaced by shorter and more xeric plants, owing to future warmer droughts and associated wildfires and pest attacks. The Darcy's corollary also provides a simple, robust framework for informing forest management interventions needed to promote the survival of current forests. There are assumptions and omissions in this theoretical <span class="hlt">prediction</span>, as well as new evidence supporting its <span class="hlt">predictions</span>, both of which I will review. Given the robustness of Darcy's law for <span class="hlt">predictions</span> of vascular plant function, we conclude with high certainty that today's forests are going to be subject to continued increases in mortality rates that will result in substantial reorganization of their structure and carbon storage.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/28078972','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/28078972"><span>The <span class="hlt">predictive</span> state: Science, territory and the future of the Indian <span class="hlt">climate</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Mahony, Martin</p> <p>2014-02-01</p> <p>Acts of scientific calculation have long been considered central to the formation of the modern nation state, yet the transnational spaces of knowledge generation and political action associated with <span class="hlt">climate</span> change seem to challenge territorial modes of political order. This article explores the changing geographies of <span class="hlt">climate</span> <span class="hlt">prediction</span> through a study of the ways in which <span class="hlt">climate</span> change is rendered knowable at the national scale in India. The recent controversy surrounding an erroneous <span class="hlt">prediction</span> of melting Himalayan glaciers by the Intergovernmental Panel on <span class="hlt">Climate</span> Change provides a window onto the complex and, at times, antagonistic relationship between the Panel and Indian political and scientific communities. The Indian reaction to the error, made public in 2009, drew upon a national history of contestation around <span class="hlt">climate</span> change science and corresponded with the establishment of a scientific assessment network, the Indian Network for <span class="hlt">Climate</span> Change Assessment, which has given the state a new platform on which to bring together knowledge about the future <span class="hlt">climate</span>. I argue that the Indian Network for <span class="hlt">Climate</span> Change Assessment is indicative of the growing use of regional <span class="hlt">climate</span> models within longer traditions of national territorial knowledge-making, allowing a rescaling of <span class="hlt">climate</span> change according to local norms and practices of linking scientific knowledge to political action. I illustrate the complex co-production of the epistemic and the normative in <span class="hlt">climate</span> politics, but also seek to show how co-productionist understandings of science and politics can function as strategic resources in the ongoing negotiation of social order. In this case, scientific rationalities and modes of environmental governance contribute to the contested epistemic construction of territory and the evolving spatiality of the modern nation state under a changing <span class="hlt">climate</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014NatCC...4..625B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014NatCC...4..625B"><span><span class="hlt">Climate</span> fails to <span class="hlt">predict</span> wood decomposition at regional scales</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Bradford, Mark A.; Warren, Robert J., II; Baldrian, Petr; Crowther, Thomas W.; Maynard, Daniel S.; Oldfield, Emily E.; Wieder, William R.; Wood, Stephen A.; King, Joshua R.</p> <p>2014-07-01</p> <p>Decomposition of organic matter strongly influences ecosystem carbon storage. In Earth-system models, <span class="hlt">climate</span> is a predominant control on the decomposition rates of organic matter. This assumption is based on the mean response of decomposition to <span class="hlt">climate</span>, yet there is a growing appreciation in other areas of global change science that projections based on mean responses can be irrelevant and misleading. We test whether <span class="hlt">climate</span> controls on the decomposition rate of dead wood--a carbon stock estimated to represent 73 +/- 6 Pg carbon globally--are sensitive to the spatial scale from which they are inferred. We show that the common assumption that <span class="hlt">climate</span> is a predominant control on decomposition is supported only when local-scale variation is aggregated into mean values. Disaggregated data instead reveal that local-scale factors explain 73% of the variation in wood decomposition, and <span class="hlt">climate</span> only 28%. Further, the temperature sensitivity of decomposition estimated from local versus mean analyses is 1.3-times greater. Fundamental issues with mean correlations were highlighted decades ago, yet mean <span class="hlt">climate</span>-decomposition relationships are used to generate simulations that inform management and adaptation under environmental change. Our results suggest that to <span class="hlt">predict</span> accurately how decomposition will respond to <span class="hlt">climate</span> change, models must account for local-scale factors that control regional dynamics.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/24119205','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/24119205"><span><span class="hlt">Predicting</span> evolutionary responses to <span class="hlt">climate</span> change in the sea.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Munday, Philip L; Warner, Robert R; Monro, Keyne; Pandolfi, John M; Marshall, Dustin J</p> <p>2013-12-01</p> <p>An increasing number of short-term experimental studies show significant effects of projected ocean warming and ocean acidification on the performance on marine organisms. Yet, it remains unclear if we can reliably <span class="hlt">predict</span> the impact of <span class="hlt">climate</span> change on marine populations and ecosystems, because we lack sufficient understanding of the capacity for marine organisms to adapt to rapid <span class="hlt">climate</span> change. In this review, we emphasise why an evolutionary perspective is crucial to understanding <span class="hlt">climate</span> change impacts in the sea and examine the approaches that may be useful for addressing this challenge. We first consider what the geological record and present-day analogues of future <span class="hlt">climate</span> conditions can tell us about the potential for adaptation to <span class="hlt">climate</span> change. We also examine evidence that phenotypic plasticity may assist marine species to persist in a rapidly changing <span class="hlt">climate</span>. We then outline the various experimental approaches that can be used to estimate evolutionary potential, focusing on molecular tools, quantitative genetics, and experimental evolution, and we describe the benefits of combining different approaches to gain a deeper understanding of evolutionary potential. Our goal is to provide a platform for future research addressing the evolutionary potential for marine organisms to cope with <span class="hlt">climate</span> change. © 2013 John Wiley & Sons Ltd/CNRS.</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_6");'>6</a></li> <li><a href="#" onclick='return showDiv("page_7");'>7</a></li> <li class="active"><span>8</span></li> <li><a href="#" onclick='return showDiv("page_9");'>9</a></li> <li><a href="#" onclick='return showDiv("page_10");'>10</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_8 --> <div id="page_9" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_7");'>7</a></li> <li><a href="#" onclick='return showDiv("page_8");'>8</a></li> <li class="active"><span>9</span></li> <li><a href="#" onclick='return showDiv("page_10");'>10</a></li> <li><a href="#" onclick='return showDiv("page_11");'>11</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="161"> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.fs.usda.gov/treesearch/pubs/27219','TREESEARCH'); return false;" href="https://www.fs.usda.gov/treesearch/pubs/27219"><span><span class="hlt">Predicting</span> <span class="hlt">climate</span>-induced range shifts: model differences and model reliability.</span></a></p> <p><a target="_blank" href="http://www.fs.usda.gov/treesearch/">Treesearch</a></p> <p>Joshua J. Lawler; Denis White; Ronald P. Neilson; Andrew R. Blaustein</p> <p>2006-01-01</p> <p><span class="hlt">Predicted</span> changes in the global <span class="hlt">climate</span> are likely to cause large shifts in the geographic ranges of many plant and animal species. To date, <span class="hlt">predictions</span> of future range shifts have relied on a variety of modeling approaches with different levels of model accuracy. Using a common data set, we investigated the potential implications of alternative modeling approaches for...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2011AGUFMGC13A0942W','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2011AGUFMGC13A0942W"><span><span class="hlt">Predicting</span> the Impacts of <span class="hlt">Climate</span> Change on Central American Agriculture</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Winter, J. M.; Ruane, A. C.; Rosenzweig, C.</p> <p>2011-12-01</p> <p>Agriculture is a vital component of Central America's economy. Poor crop yields and harvest reliability can produce food insecurity, malnutrition, and conflict. Regional <span class="hlt">climate</span> models (RCMs) and agricultural models have the potential to greatly enhance the efficiency of Central American agriculture and water resources management under both current and future <span class="hlt">climates</span>. A series of numerical experiments was conducted using Regional <span class="hlt">Climate</span> Model Version 3 (RegCM3) and the Weather Research and Forecasting Model (WRF) to evaluate the ability of RCMs to reproduce the current <span class="hlt">climate</span> of Central America and assess changes in temperature and precipitation under multiple future <span class="hlt">climate</span> scenarios. Control simulations were thoroughly compared to a variety of observational datasets, including local weather station data, gridded meteorological data, and high-resolution satellite-based precipitation products. Future <span class="hlt">climate</span> simulations were analyzed for both mean shifts in <span class="hlt">climate</span> and changes in <span class="hlt">climate</span> variability, including extreme events (droughts, heat waves, floods). To explore the impacts of changing <span class="hlt">climate</span> on maize, bean, and rice yields in Central America, RCM output was used to force the Decision Support System for Agrotechnology Transfer Model (DSSAT). These results were synthesized to create <span class="hlt">climate</span> change impacts <span class="hlt">predictions</span> for Central American agriculture that explicitly account for evolving distributions of precipitation and temperature extremes.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018WRR....54..916L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018WRR....54..916L"><span>Attribution of Large-Scale <span class="hlt">Climate</span> Patterns to Seasonal Peak-Flow and Prospects for <span class="hlt">Prediction</span> Globally</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Lee, Donghoon; Ward, Philip; Block, Paul</p> <p>2018-02-01</p> <p>Flood-related fatalities and impacts on society surpass those from all other natural disasters globally. While the inclusion of large-scale <span class="hlt">climate</span> drivers in streamflow (or high-flow) <span class="hlt">prediction</span> has been widely studied, an explicit link to global-scale long-lead <span class="hlt">prediction</span> is lacking, which can lead to an improved understanding of potential flood propensity. Here we attribute seasonal peak-flow to large-scale <span class="hlt">climate</span> patterns, including the El Niño Southern Oscillation (ENSO), Pacific Decadal Oscillation (PDO), North Atlantic Oscillation (NAO), and Atlantic Multidecadal Oscillation (AMO), using streamflow station observations and simulations from PCR-GLOBWB, a global-scale hydrologic model. Statistically significantly correlated <span class="hlt">climate</span> patterns and streamflow autocorrelation are subsequently applied as predictors to build a global-scale season-ahead <span class="hlt">prediction</span> model, with <span class="hlt">prediction</span> performance evaluated by the mean squared error skill score (MSESS) and the categorical Gerrity skill score (GSS). Globally, fair-to-good <span class="hlt">prediction</span> skill (20% ≤ MSESS and 0.2 ≤ GSS) is evident for a number of locations (28% of stations and 29% of land area), most notably in data-poor regions (e.g., West and Central Africa). The persistence of such relevant <span class="hlt">climate</span> patterns can improve understanding of the propensity for floods at the seasonal scale. The <span class="hlt">prediction</span> approach developed here lays the groundwork for further improving local-scale seasonal peak-flow <span class="hlt">prediction</span> by identifying relevant global-scale <span class="hlt">climate</span> patterns. This is especially attractive for regions with limited observations and or little capacity to develop flood early warning systems.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://files.eric.ed.gov/fulltext/ED410897.pdf','ERIC'); return false;" href="http://files.eric.ed.gov/fulltext/ED410897.pdf"><span><span class="hlt">Administrative</span> Satisfaction and the Regulatory <span class="hlt">Climate</span> at Public Institutions. AIR 1997 Annual Forum Paper.</span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Volkwein, James Fredericks; Malik, Shaukat M.; Napierski-Prancl, Michelle</p> <p></p> <p>This study examined the effects of state regulation of financial, personnel, and academic resources on the <span class="hlt">administrative</span> flexibility granted to universities, and tested the hypothesis that state regulatory <span class="hlt">climate</span> influences levels of managerial satisfaction. Data were gathered through two surveys. The first covered management flexibility and…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018GeoRL..45.4273A','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018GeoRL..45.4273A"><span>Machine Learning <span class="hlt">Predictions</span> of a Multiresolution <span class="hlt">Climate</span> Model Ensemble</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Anderson, Gemma J.; Lucas, Donald D.</p> <p>2018-05-01</p> <p>Statistical models of high-resolution <span class="hlt">climate</span> models are useful for many purposes, including sensitivity and uncertainty analyses, but building them can be computationally prohibitive. We generated a unique multiresolution perturbed parameter ensemble of a global <span class="hlt">climate</span> model. We use a novel application of a machine learning technique known as random forests to train a statistical model on the ensemble to make high-resolution model <span class="hlt">predictions</span> of two important quantities: global mean top-of-atmosphere energy flux and precipitation. The random forests leverage cheaper low-resolution simulations, greatly reducing the number of high-resolution simulations required to train the statistical model. We demonstrate that high-resolution <span class="hlt">predictions</span> of these quantities can be obtained by training on an ensemble that includes only a small number of high-resolution simulations. We also find that global annually averaged precipitation is more sensitive to resolution changes than to any of the model parameters considered.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2006AGUFM.B51C0332I','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2006AGUFM.B51C0332I"><span>National Scale <span class="hlt">Prediction</span> of Soil Carbon Sequestration under Scenarios of <span class="hlt">Climate</span> Change</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Izaurralde, R. C.; Thomson, A. M.; Potter, S. R.; Atwood, J. D.; Williams, J. R.</p> <p>2006-12-01</p> <p>Carbon sequestration in agricultural soils is gaining momentum as a tool to mitigate the rate of increase of atmospheric CO2. Researchers from the Pacific Northwest National Laboratory, Texas A&M University, and USDA-NRCS used the EPIC model to develop national-scale <span class="hlt">predictions</span> of soil carbon sequestration with adoption of no till (NT) under scenarios of <span class="hlt">climate</span> change. In its current form, the EPIC model simulates soil C changes resulting from heterotrophic respiration and wind / water erosion. Representative modeling units were created to capture the <span class="hlt">climate</span>, soil, and management variability at the 8-digit hydrologic unit (USGS classification) watershed scale. The soils selected represented at least 70% of the variability within each watershed. This resulted in 7,540 representative modeling units for 1,412 watersheds. Each watershed was assigned a major crop system: corn, soybean, spring wheat, winter wheat, cotton, hay, alfalfa, corn-soybean rotation or wheat-fallow rotation based on information from the National Resource Inventory. Each representative farm was simulated with conventional tillage and no tillage, and with and without irrigation. <span class="hlt">Climate</span> change scenarios for two future periods (2015-2045 and 2045-2075) were selected from GCM model runs using the IPCC SRES scenarios of A2 and B2 from the UK Hadley Center (HadCM3) and US DOE PCM (PCM) models. Changes in mean and standard deviation of monthly temperature and precipitation were extracted from gridded files and applied to baseline <span class="hlt">climate</span> (1960-1990) for each of the 1,412 modeled watersheds. Modeled crop yields were validated against historical USDA NASS county yields (1960-1990). The HadCM3 model <span class="hlt">predicted</span> the most severe changes in <span class="hlt">climate</span> parameters. Overall, there would be little difference between the A2 and B2 scenarios. Carbon offsets were calculated as the difference in soil C change between conventional and no till. Overall, C offsets during the first 30-y period (513 Tg C) are <span class="hlt">predicted</span> to</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=20100014787&hterms=ocean+climate+changes&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D30%26Ntt%3Docean%2Bclimate%2Bchanges','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=20100014787&hterms=ocean+climate+changes&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D30%26Ntt%3Docean%2Bclimate%2Bchanges"><span>The Impact of Ocean Observations in Seasonal <span class="hlt">Climate</span> <span class="hlt">Prediction</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Rienecker, Michele; Keppenne, Christian; Kovach, Robin; Marshak, Jelena</p> <p>2010-01-01</p> <p>The ocean provides the most significant memory for the <span class="hlt">climate</span> system. Hence, a critical element in <span class="hlt">climate</span> forecasting with coupled models is the initialization of the ocean with states from an ocean data assimilation system. Remotely-sensed ocean surface fields (e.g., sea surface topography, SST, winds) are now available for extensive periods and have been used to constrain ocean models to provide a record of <span class="hlt">climate</span> variations. Since the ocean is virtually opaque to electromagnetic radiation, the assimilation of these satellite data is essential to extracting the maximum information content. More recently, the Argo drifters have provided unprecedented sampling of the subsurface temperature and salinity. Although the duration of this observation set has been too short to provide solid statistical evidence of its impact, there are indications that Argo improves the forecast skill of coupled systems. This presentation will address the impact these different observations have had on seasonal <span class="hlt">climate</span> <span class="hlt">predictions</span> with the GMAO's coupled model.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014NatCC...4..217P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014NatCC...4..217P"><span>Life history and spatial traits <span class="hlt">predict</span> extinction risk due to <span class="hlt">climate</span> change</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Pearson, Richard G.; Stanton, Jessica C.; Shoemaker, Kevin T.; Aiello-Lammens, Matthew E.; Ersts, Peter J.; Horning, Ned; Fordham, Damien A.; Raxworthy, Christopher J.; Ryu, Hae Yeong; McNees, Jason; Akçakaya, H. Reşit</p> <p>2014-03-01</p> <p>There is an urgent need to develop effective vulnerability assessments for evaluating the conservation status of species in a changing <span class="hlt">climate</span>. Several new assessment approaches have been proposed for evaluating the vulnerability of species to <span class="hlt">climate</span> change based on the expectation that established assessments such as the IUCN Red List need revising or superseding in light of the threat that <span class="hlt">climate</span> change brings. However, although previous studies have identified ecological and life history attributes that characterize declining species or those listed as threatened, no study so far has undertaken a quantitative analysis of the attributes that cause species to be at high risk of extinction specifically due to <span class="hlt">climate</span> change. We developed a simulation approach based on generic life history types to show here that extinction risk due to <span class="hlt">climate</span> change can be <span class="hlt">predicted</span> using a mixture of spatial and demographic variables that can be measured in the present day without the need for complex forecasting models. Most of the variables we found to be important for <span class="hlt">predicting</span> extinction risk, including occupied area and population size, are already used in species conservation assessments, indicating that present systems may be better able to identify species vulnerable to <span class="hlt">climate</span> change than previously thought. Therefore, although <span class="hlt">climate</span> change brings many new conservation challenges, we find that it may not be fundamentally different from other threats in terms of assessing extinction risks.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2011AGUFMGC11A0885B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2011AGUFMGC11A0885B"><span>Using <span class="hlt">Prediction</span> Markets to Generate Probability Density Functions for <span class="hlt">Climate</span> Change Risk Assessment</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Boslough, M.</p> <p>2011-12-01</p> <p><span class="hlt">Climate</span>-related uncertainty is traditionally presented as an error bar, but it is becoming increasingly common to express it in terms of a probability density function (PDF). PDFs are a necessary component of probabilistic risk assessments, for which simple "best estimate" values are insufficient. Many groups have generated PDFs for <span class="hlt">climate</span> sensitivity using a variety of methods. These PDFs are broadly consistent, but vary significantly in their details. One axiom of the verification and validation community is, "codes don't make <span class="hlt">predictions</span>, people make <span class="hlt">predictions</span>." This is a statement of the fact that subject domain experts generate results using assumptions within a range of epistemic uncertainty and interpret them according to their expert opinion. Different experts with different methods will arrive at different PDFs. For effective decision support, a single consensus PDF would be useful. We suggest that market methods can be used to aggregate an ensemble of opinions into a single distribution that expresses the consensus. <span class="hlt">Prediction</span> markets have been shown to be highly successful at forecasting the outcome of events ranging from elections to box office returns. In <span class="hlt">prediction</span> markets, traders can take a position on whether some future event will or will not occur. These positions are expressed as contracts that are traded in a double-action market that aggregates price, which can be interpreted as a consensus probability that the event will take place. Since <span class="hlt">climate</span> sensitivity cannot directly be measured, it cannot be <span class="hlt">predicted</span>. However, the changes in global mean surface temperature are a direct consequence of <span class="hlt">climate</span> sensitivity, changes in forcing, and internal variability. Viable <span class="hlt">prediction</span> markets require an undisputed event outcome on a specific date. <span class="hlt">Climate</span>-related markets exist on Intrade.com, an online trading exchange. One such contract is titled "Global Temperature Anomaly for Dec 2011 to be greater than 0.65 Degrees C." Settlement is based</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/24677422','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/24677422"><span>Cetacean range and <span class="hlt">climate</span> in the eastern North Atlantic: future <span class="hlt">predictions</span> and implications for conservation.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Lambert, Emily; Pierce, Graham J; Hall, Karen; Brereton, Tom; Dunn, Timothy E; Wall, Dave; Jepson, Paul D; Deaville, Rob; MacLeod, Colin D</p> <p>2014-06-01</p> <p>There is increasing evidence that the distributions of a large number of species are shifting with global <span class="hlt">climate</span> change as they track changing surface temperatures that define their thermal niche. Modelling efforts to <span class="hlt">predict</span> species distributions under future <span class="hlt">climates</span> have increased with concern about the overall impact of these distribution shifts on species ecology, and especially where barriers to dispersal exist. Here we apply a bio-<span class="hlt">climatic</span> envelope modelling technique to investigate the impacts of <span class="hlt">climate</span> change on the geographic range of ten cetacean species in the eastern North Atlantic and to assess how such modelling can be used to inform conservation and management. The modelling process integrates elements of a species' habitat and thermal niche, and employs "hindcasting" of historical distribution changes in order to verify the accuracy of the modelled relationship between temperature and species range. If this ability is not verified, there is a risk that inappropriate or inaccurate models will be used to make future <span class="hlt">predictions</span> of species distributions. Of the ten species investigated, we found that while the models for nine could successfully explain current spatial distribution, only four had a good ability to <span class="hlt">predict</span> distribution changes over time in response to changes in water temperature. Applied to future <span class="hlt">climate</span> scenarios, the four species-specific models with good <span class="hlt">predictive</span> abilities indicated range expansion in one species and range contraction in three others, including the potential loss of up to 80% of suitable white-beaked dolphin habitat. Model <span class="hlt">predictions</span> allow identification of affected areas and the likely time-scales over which impacts will occur. Thus, this work provides important information on both our ability to <span class="hlt">predict</span> how individual species will respond to future <span class="hlt">climate</span> change and the applicability of <span class="hlt">predictive</span> distribution models as a tool to help construct viable conservation and management strategies. © 2014 John</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2006ClDy...26..285K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2006ClDy...26..285K"><span>Examination of multi-model ensemble seasonal <span class="hlt">prediction</span> methods using a simple <span class="hlt">climate</span> system</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Kang, In-Sik; Yoo, Jin Ho</p> <p>2006-02-01</p> <p>A simple <span class="hlt">climate</span> model was designed as a proxy for the real <span class="hlt">climate</span> system, and a number of <span class="hlt">prediction</span> models were generated by slightly perturbing the physical parameters of the simple model. A set of long (240 years) historical hindcast <span class="hlt">predictions</span> were performed with various <span class="hlt">prediction</span> models, which are used to examine various issues of multi-model ensemble seasonal <span class="hlt">prediction</span>, such as the best ways of blending multi-models and the selection of models. Based on these results, we suggest a feasible way of maximizing the benefit of using multi models in seasonal <span class="hlt">prediction</span>. In particular, three types of multi-model ensemble <span class="hlt">prediction</span> systems, i.e., the simple composite, superensemble, and the composite after statistically correcting individual <span class="hlt">predictions</span> (corrected composite), are examined and compared to each other. The superensemble has more of an overfitting problem than the others, especially for the case of small training samples and/or weak external forcing, and the corrected composite produces the best <span class="hlt">prediction</span> skill among the multi-model systems.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29375800','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29375800"><span>Shifts in frog size and phenology: Testing <span class="hlt">predictions</span> of <span class="hlt">climate</span> change on a widespread anuran using data from prior to rapid <span class="hlt">climate</span> warming.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Sheridan, Jennifer A; Caruso, Nicholas M; Apodaca, Joseph J; Rissler, Leslie J</p> <p>2018-01-01</p> <p>Changes in body size and breeding phenology have been identified as two major ecological consequences of <span class="hlt">climate</span> change, yet it remains unclear whether <span class="hlt">climate</span> acts directly or indirectly on these variables. To better understand the relationship between <span class="hlt">climate</span> and ecological changes, it is necessary to determine environmental predictors of both size and phenology using data from prior to the onset of rapid <span class="hlt">climate</span> warming, and then to examine spatially explicit changes in <span class="hlt">climate</span>, size, and phenology, not just general spatial and temporal trends. We used 100 years of natural history collection data for the wood frog, Lithobates sylvaticus with a range >9 million km 2 , and spatially explicit environmental data to determine the best predictors of size and phenology prior to rapid <span class="hlt">climate</span> warming (1901-1960). We then tested how closely size and phenology changes <span class="hlt">predicted</span> by those environmental variables reflected actual changes from 1961 to 2000. Size, phenology, and <span class="hlt">climate</span> all changed as expected (smaller, earlier, and warmer, respectively) at broad spatial scales across the entire study range. However, while spatially explicit changes in <span class="hlt">climate</span> variables accurately <span class="hlt">predicted</span> changes in phenology, they did not accurately <span class="hlt">predict</span> size changes during recent <span class="hlt">climate</span> change (1961-2000), contrary to expectations from numerous recent studies. Our results suggest that changes in <span class="hlt">climate</span> are directly linked to observed phenological shifts. However, the mechanisms driving observed body size changes are yet to be determined, given the less straightforward relationship between size and <span class="hlt">climate</span> factors examined in this study. We recommend that caution be used in "space-for-time" studies where measures of a species' traits at lower latitudes or elevations are considered representative of those under future projected <span class="hlt">climate</span> conditions. Future studies should aim to determine mechanisms driving trends in phenology and body size, as well as the impact of <span class="hlt">climate</span> on population</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://cfpub.epa.gov/si/si_public_record_report.cfm?dirEntryId=244851&keyword=analysis+AND+climatic&actType=&TIMSType=+&TIMSSubTypeID=&DEID=&epaNumber=&ntisID=&archiveStatus=Both&ombCat=Any&dateBeginCreated=&dateEndCreated=&dateBeginPublishedPresented=&dateEndPublishedPresented=&dateBeginUpdated=&dateEndUpdated=&dateBeginCompleted=&dateEndCompleted=&personID=&role=Any&journalID=&publisherID=&sortBy=revisionDate&count=50','EPA-EIMS'); return false;" href="https://cfpub.epa.gov/si/si_public_record_report.cfm?dirEntryId=244851&keyword=analysis+AND+climatic&actType=&TIMSType=+&TIMSSubTypeID=&DEID=&epaNumber=&ntisID=&archiveStatus=Both&ombCat=Any&dateBeginCreated=&dateEndCreated=&dateBeginPublishedPresented=&dateEndPublishedPresented=&dateBeginUpdated=&dateEndUpdated=&dateBeginCompleted=&dateEndCompleted=&personID=&role=Any&journalID=&publisherID=&sortBy=revisionDate&count=50"><span>A linear regression model for <span class="hlt">predicting</span> PNW estuarine temperatures in a changing <span class="hlt">climate</span></span></a></p> <p><a target="_blank" href="http://oaspub.epa.gov/eims/query.page">EPA Science Inventory</a></p> <p></p> <p></p> <p>Pacific Northwest coastal regions, estuaries, and associated ecosystems are vulnerable to the potential effects of <span class="hlt">climate</span> change, especially to changes in nearshore water temperature. While <span class="hlt">predictive</span> <span class="hlt">climate</span> models simulate future air temperatures, no such projections exist for...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/servlets/purl/1030607','SCIGOV-STC'); return false;" href="https://www.osti.gov/servlets/purl/1030607"><span>Towards the <span class="hlt">Prediction</span> of Decadal to Centennial <span class="hlt">Climate</span> Processes in the Coupled Earth System Model</span></a></p> <p><a target="_blank" href="http://www.osti.gov/search">DOE Office of Scientific and Technical Information (OSTI.GOV)</a></p> <p>Liu, Zhengyu; Kutzbach, J.; Jacob, R.</p> <p>2011-12-05</p> <p>In this proposal, we have made major advances in the understanding of decadal and long term <span class="hlt">climate</span> variability. (a) We performed a systematic study of multidecadal <span class="hlt">climate</span> variability in FOAM-LPJ and CCSM-T31, and are starting exploring decadal variability in the IPCC AR4 models. (b) We develop several novel methods for the assessment of <span class="hlt">climate</span> feedbacks in the observation. (c) We also developed a new initialization scheme DAI (Dynamical Analogue Initialization) for ensemble decadal <span class="hlt">prediction</span>. (d) We also studied <span class="hlt">climate</span>-vegetation feedback in the observation and models. (e) Finally, we started a pilot program using Ensemble Kalman Filter in CGCM for decadalmore » <span class="hlt">climate</span> <span class="hlt">prediction</span>.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013AGUFM.A31F0167L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013AGUFM.A31F0167L"><span>The <span class="hlt">Climate</span> Variability & <span class="hlt">Predictability</span> (CVP) Program at NOAA - DYNAMO Recent Project Advancements</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Lucas, S. E.; Todd, J. F.; Higgins, W.</p> <p>2013-12-01</p> <p>The <span class="hlt">Climate</span> Variability & <span class="hlt">Predictability</span> (CVP) Program supports research aimed at providing process-level understanding of the <span class="hlt">climate</span> system through observation, modeling, analysis, and field studies. This vital knowledge is needed to improve <span class="hlt">climate</span> models and <span class="hlt">predictions</span> so that scientists can better anticipate the impacts of future <span class="hlt">climate</span> variability and change. To achieve its mission, the CVP Program supports research carried out at NOAA and other federal laboratories, NOAA Cooperative Institutes, and academic institutions. The Program also coordinates its sponsored projects with major national and international scientific bodies including the World <span class="hlt">Climate</span> Research Programme (WCRP), the International Geosphere-Biosphere Programme (IGBP), and the U.S. Global Change Research Program (USGCRP). The CVP program sits within the Earth System Science (ESS) Division at NOAA's <span class="hlt">Climate</span> Program Office. Dynamics of the Madden-Julian Oscillation (DYNAMO): The Indian Ocean is one of Earth's most sensitive regions because the interactions between ocean and atmosphere there have a discernable effect on global <span class="hlt">climate</span> patterns. The tropical weather that brews in that region can move eastward along the equator and reverberate around the globe, shaping weather and <span class="hlt">climate</span> in far-off places. The vehicle for this variability is a phenomenon called the Madden-Julian Oscillation, or MJO. The MJO, which originates over the Indian Ocean roughly every 30 to 90 days, is known to influence the Asian and Australian monsoons. It can also enhance hurricane activity in the northeast Pacific and Gulf of Mexico, trigger torrential rainfall along the west coast of North America, and affect the onset of El Niño. CVP-funded scientists participated in the DYNAMO field campaign in 2011-12. Results from this international campaign are expected to improve researcher's insights into this influential phenomenon. A better understanding of the processes governing MJO is an essential step toward</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013AGUFM.A11G0132Y','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013AGUFM.A11G0132Y"><span><span class="hlt">Prediction</span> of meningococcal meningitis epidemics in western Africa by using <span class="hlt">climate</span> information</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>YAKA, D. P.; Sultan, B.; Tarbangdo, F.; Thiaw, W. M.</p> <p>2013-12-01</p> <p>The variations of certain <span class="hlt">climatic</span> parameters and the degradation of ecosystems, can affect human's health by influencing the transmission, the spatiotemporal repartition and the intensity of infectious diseases. It is mainly the case of meningococcal meningitis (MCM) whose epidemics occur particularly in Sahelo-Soudanian <span class="hlt">climatic</span> area of Western Africa under quite particular <span class="hlt">climatic</span> conditions. Meningococcal Meningitis (MCM) is a contagious infection disease due to the bacteria Neisseria meningitis. MCM epidemics occur worldwide but the highest incidence is observed in the "meningitis belt" of sub-Saharan Africa, stretching from Senegal to Ethiopia. In spite of standards, strategies of prevention and control of MCS epidemic from World Health Organization (WHO) and States, African Sahelo-Soudanian countries remain frequently afflicted by disastrous epidemics. In fact, each year, during the dry season (February-April), 25 to 250 thousands of cases are observed. Children under 15 are particularly affected. Among favourable conditions for the resurgence and dispersion of the disease, <span class="hlt">climatic</span> conditions may be important inducing seasonal fluctuations in disease incidence and contributing to explain the spatial pattern of the disease roughly circumscribed to the ecological Sahelo-Sudanian band. In this study, we tried to analyse the relationships between <span class="hlt">climatic</span> factors, ecosystems degradation and MCM for a better understanding of MCM epidemic dynamic and their <span class="hlt">prediction</span>. We have shown that MCM epidemics, whether at the regional, national or local level, occur in a specific period of the year, mainly from January to May characterised by a dry, hot and sandy weather. We have identified both in situ (meteorological synoptic stations) and satellitales <span class="hlt">climatic</span> variables (NCEP reanalysis dataset) whose seasonal variability is dominating in MCM seasonal transmission. Statistical analysis have measured the links between seasonal variation of certain <span class="hlt">climatic</span> parameters</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/28474676','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/28474676"><span>A dynamic eco-evolutionary model <span class="hlt">predicts</span> slow response of alpine plants to <span class="hlt">climate</span> warming.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Cotto, Olivier; Wessely, Johannes; Georges, Damien; Klonner, Günther; Schmid, Max; Dullinger, Stefan; Thuiller, Wilfried; Guillaume, Frédéric</p> <p>2017-05-05</p> <p>Withstanding extinction while facing rapid <span class="hlt">climate</span> change depends on a species' ability to track its ecological niche or to evolve a new one. Current methods that <span class="hlt">predict</span> <span class="hlt">climate</span>-driven species' range shifts use ecological modelling without eco-evolutionary dynamics. Here we present an eco-evolutionary forecasting framework that combines niche modelling with individual-based demographic and genetic simulations. Applying our approach to four endemic perennial plant species of the Austrian Alps, we show that accounting for eco-evolutionary dynamics when <span class="hlt">predicting</span> species' responses to <span class="hlt">climate</span> change is crucial. Perennial species persist in unsuitable habitats longer than <span class="hlt">predicted</span> by niche modelling, causing delayed range losses; however, their evolutionary responses are constrained because long-lived adults produce increasingly maladapted offspring. Decreasing population size due to maladaptation occurs faster than the contraction of the species range, especially for the most abundant species. Monitoring of species' local abundance rather than their range may likely better inform on species' extinction risks under <span class="hlt">climate</span> change.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2011PhDT.........5F','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2011PhDT.........5F"><span>New Methods for Estimating Seasonal Potential <span class="hlt">Climate</span> <span class="hlt">Predictability</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Feng, Xia</p> <p></p> <p>This study develops two new statistical approaches to assess the seasonal potential <span class="hlt">predictability</span> of the observed <span class="hlt">climate</span> variables. One is the univariate analysis of covariance (ANOCOVA) model, a combination of autoregressive (AR) model and analysis of variance (ANOVA). It has the advantage of taking into account the uncertainty of the estimated parameter due to sampling errors in statistical test, which is often neglected in AR based methods, and accounting for daily autocorrelation that is not considered in traditional ANOVA. In the ANOCOVA model, the seasonal signals arising from external forcing are determined to be identical or not to assess any interannual variability that may exist is potentially <span class="hlt">predictable</span>. The bootstrap is an attractive alternative method that requires no hypothesis model and is available no matter how mathematically complicated the parameter estimator. This method builds up the empirical distribution of the interannual variance from the resamplings drawn with replacement from the given sample, in which the only <span class="hlt">predictability</span> in seasonal means arises from the weather noise. These two methods are applied to temperature and water cycle components including precipitation and evaporation, to measure the extent to which the interannual variance of seasonal means exceeds the unpredictable weather noise compared with the previous methods, including Leith-Shukla-Gutzler (LSG), Madden, and Katz. The potential <span class="hlt">predictability</span> of temperature from ANOCOVA model, bootstrap, LSG and Madden exhibits a pronounced tropical-extratropical contrast with much larger <span class="hlt">predictability</span> in the tropics dominated by El Nino/Southern Oscillation (ENSO) than in higher latitudes where strong internal variability lowers <span class="hlt">predictability</span>. Bootstrap tends to display highest <span class="hlt">predictability</span> of the four methods, ANOCOVA lies in the middle, while LSG and Madden appear to generate lower <span class="hlt">predictability</span>. Seasonal precipitation from ANOCOVA, bootstrap, and Katz, resembling that</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2008AGUFMPA13C1350H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2008AGUFMPA13C1350H"><span>The Nested Regional <span class="hlt">Climate</span> Model: An Approach Toward <span class="hlt">Prediction</span> Across Scales</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Hurrell, J. W.; Holland, G. J.; Large, W. G.</p> <p>2008-12-01</p> <p>The reality of global <span class="hlt">climate</span> change has become accepted and society is rapidly moving to questions of consequences on space and time scales that are relevant to proper planning and development of adaptation strategies. There are a number of urgent challenges for the scientific community related to improved and more detailed <span class="hlt">predictions</span> of regional <span class="hlt">climate</span> change on decadal time scales. Two important examples are potential impacts of <span class="hlt">climate</span> change on North Atlantic hurricane activity and on water resources over the intermountain West. The latter is dominated by complex topography, so that accurate simulations of regional <span class="hlt">climate</span> variability and change require much finer spatial resolution than is provided with state-of-the-art <span class="hlt">climate</span> models. <span class="hlt">Climate</span> models also do not explicitly resolve tropical cyclones, even though these storms have dramatic societal impacts and play an important role in regulating <span class="hlt">climate</span>. Moreover, the debate over the impact of global warming on tropical cyclones has at times been acrimonious, and the lack of hard evidence has left open opportunities for misinterpretation and justification of pre-existing beliefs. These and similar topics are being assessed at NCAR, in partnership with university colleagues, through the development of a Nested Regional <span class="hlt">Climate</span> Model (NRCM). This is an ambitious effort to combine a state of the science mesoscale weather model (WRF), a high resolution regional ocean modeling system (ROMS), and a <span class="hlt">climate</span> model (CCSM) to better simulate the complex, multi-scale interactions intrinsic to atmospheric and oceanic fluid motions that are limiting our ability to <span class="hlt">predict</span> likely future changes in regional weather statistics and <span class="hlt">climate</span>. The NRCM effort is attracting a large base of earth system scientists together with societal groups as diverse as the Western Governor's Association and the offshore oil industry. All of these groups require <span class="hlt">climate</span> data on scales of a few kilometers (or less), so that the NRCM program is</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5683072','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5683072"><span><span class="hlt">Predicting</span> Sexual Assault Perpetration in the US Army Using <span class="hlt">Administrative</span> Data</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Rosellini, Anthony J.; Monahan, John; Street, Amy E.; Petukhova, Maria V.; Sampson, Nancy A.; Benedek, David M.; Bliese, Paul; Stein, Murray B.; Ursano, Robert J.; Kessler, Ronald C.</p> <p>2017-01-01</p> <p>Introduction The Department of Defense uses a universal prevention framework for sexual assault prevention, with each branch implementing their own branch-wide programs. Intensive interventions exist, but would be cost-effective only if targeted at high-risk personnel. This study developed actuarial models to identify male U.S. Army soldiers at high risk of <span class="hlt">administratively</span>-recorded sexual assault perpetration. Methods This study investigated <span class="hlt">administratively</span>-recorded sexual assault perpetration among the 821,807 male Army soldiers serving 2004–2009. Other temporally prior <span class="hlt">administrative</span> data were used as predictors. Penalized discrete-time (person-month) survival analysis (conducted in 2016) was used to select the smallest possible number of stable predictors to maximize number of sexual assaults among the 5% of soldiers with highest <span class="hlt">predicted</span> risk of perpetration (top-ventile concentration of risk [COR]). Separate models were developed for assaults against non-family and intra-family adults and minors. Results 4,640 male soldiers were found to be perpetrators against non-family adults, 1,384 against non-family minors, 380 against intra-family adults, and 335 against intra-family minors. Top-ventile COR was 16.2–20.2% <span class="hlt">predicting</span> perpetration against non-family adults and minors and 34.2–65.1% against intra-family adults and minors. Final predictors consisted largely of measures of prior crime involvement and the presence-treatment of mental disorders. Conclusions <span class="hlt">Administrative</span> data can be used to develop actuarial models that identify a high proportion of sexual assault perpetrators. If a system is developed to routinely consolidate <span class="hlt">administrative</span> predictors, <span class="hlt">predictions</span> could be generated periodically to identify those in need of preventive intervention. Whether this would be cost-effective, though, would depend on intervention costs, effectiveness, and competing risks. PMID:28818420</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_7");'>7</a></li> <li><a href="#" onclick='return showDiv("page_8");'>8</a></li> <li class="active"><span>9</span></li> <li><a href="#" onclick='return showDiv("page_10");'>10</a></li> <li><a href="#" onclick='return showDiv("page_11");'>11</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_9 --> <div id="page_10" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_8");'>8</a></li> <li><a href="#" onclick='return showDiv("page_9");'>9</a></li> <li class="active"><span>10</span></li> <li><a href="#" onclick='return showDiv("page_11");'>11</a></li> <li><a href="#" onclick='return showDiv("page_12");'>12</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="181"> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29685183','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29685183"><span>Landscape genomic <span class="hlt">prediction</span> for restoration of a Eucalyptus foundation species under <span class="hlt">climate</span> change.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Supple, Megan Ann; Bragg, Jason G; Broadhurst, Linda M; Nicotra, Adrienne B; Byrne, Margaret; Andrew, Rose L; Widdup, Abigail; Aitken, Nicola C; Borevitz, Justin O</p> <p>2018-04-24</p> <p>As species face rapid environmental change, we can build resilient populations through restoration projects that incorporate <span class="hlt">predicted</span> future <span class="hlt">climates</span> into seed sourcing decisions. Eucalyptus melliodora is a foundation species of a critically endangered community in Australia that is a target for restoration. We examined genomic and phenotypic variation to make empirical based recommendations for seed sourcing. We examined isolation by distance and isolation by environment, determining high levels of gene flow extending for 500 km and correlations with <span class="hlt">climate</span> and soil variables. Growth experiments revealed extensive phenotypic variation both within and among sampling sites, but no site-specific differentiation in phenotypic plasticity. Model <span class="hlt">predictions</span> suggest that seed can be sourced broadly across the landscape, providing ample diversity for adaptation to environmental change. Application of our landscape genomic model to E. melliodora restoration projects can identify genomic variation suitable for <span class="hlt">predicted</span> future <span class="hlt">climates</span>, thereby increasing the long term probability of successful restoration. © 2018, Supple et al.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.fs.usda.gov/treesearch/pubs/33373','TREESEARCH'); return false;" href="https://www.fs.usda.gov/treesearch/pubs/33373"><span><span class="hlt">Predicting</span> forest attributes from <span class="hlt">climate</span> data using a recursive partitioning and regression tree algorithm</span></a></p> <p><a target="_blank" href="http://www.fs.usda.gov/treesearch/">Treesearch</a></p> <p>Greg C. Liknes; Christopher W. Woodall; Charles H. Perry</p> <p>2009-01-01</p> <p><span class="hlt">Climate</span> information frequently is included in geospatial modeling efforts to improve the <span class="hlt">predictive</span> capability of other data sources. The selection of an appropriate <span class="hlt">climate</span> data source requires consideration given the number of choices available. With regard to <span class="hlt">climate</span> data, there are a variety of parameters (e.g., temperature, humidity, precipitation), time intervals...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/28804989','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/28804989"><span>Improving <span class="hlt">predictions</span> of tropical forest response to <span class="hlt">climate</span> change through integration of field studies and ecosystem modeling.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Feng, Xiaohui; Uriarte, María; González, Grizelle; Reed, Sasha; Thompson, Jill; Zimmerman, Jess K; Murphy, Lora</p> <p>2018-01-01</p> <p>Tropical forests play a critical role in carbon and water cycles at a global scale. Rapid <span class="hlt">climate</span> change is anticipated in tropical regions over the coming decades and, under a warmer and drier <span class="hlt">climate</span>, tropical forests are likely to be net sources of carbon rather than sinks. However, our understanding of tropical forest response and feedback to <span class="hlt">climate</span> change is very limited. Efforts to model <span class="hlt">climate</span> change impacts on carbon fluxes in tropical forests have not reached a consensus. Here, we use the Ecosystem Demography model (ED2) to <span class="hlt">predict</span> carbon fluxes of a Puerto Rican tropical forest under realistic <span class="hlt">climate</span> change scenarios. We parameterized ED2 with species-specific tree physiological data using the <span class="hlt">Predictive</span> Ecosystem Analyzer workflow and projected the fate of this ecosystem under five future <span class="hlt">climate</span> scenarios. The model successfully captured interannual variability in the dynamics of this tropical forest. Model <span class="hlt">predictions</span> closely followed observed values across a wide range of metrics including aboveground biomass, tree diameter growth, tree size class distributions, and leaf area index. Under a future warming and drying <span class="hlt">climate</span> scenario, the model <span class="hlt">predicted</span> reductions in carbon storage and tree growth, together with large shifts in forest community composition and structure. Such rapid changes in <span class="hlt">climate</span> led the forest to transition from a sink to a source of carbon. Growth respiration and root allocation parameters were responsible for the highest fraction of <span class="hlt">predictive</span> uncertainty in modeled biomass, highlighting the need to target these processes in future data collection. Our study is the first effort to rely on Bayesian model calibration and synthesis to elucidate the key physiological parameters that drive uncertainty in tropical forests responses to <span class="hlt">climatic</span> change. We propose a new path forward for model-data synthesis that can substantially reduce uncertainty in our ability to model tropical forest responses to future <span class="hlt">climate</span>. © 2017 John</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70190745','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70190745"><span>Improving <span class="hlt">predictions</span> of tropical forest response to <span class="hlt">climate</span> change through integration of field studies and ecosystem modeling</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Feng, Xiaohui; Uriarte, María; González, Grizelle; Reed, Sasha C.; Thompson, Jill; Zimmerman, Jess K.; Murphy, Lora</p> <p>2018-01-01</p> <p>Tropical forests play a critical role in carbon and water cycles at a global scale. Rapid <span class="hlt">climate</span> change is anticipated in tropical regions over the coming decades and, under a warmer and drier <span class="hlt">climate</span>, tropical forests are likely to be net sources of carbon rather than sinks. However, our understanding of tropical forest response and feedback to <span class="hlt">climate</span> change is very limited. Efforts to model <span class="hlt">climate</span> change impacts on carbon fluxes in tropical forests have not reached a consensus. Here we use the Ecosystem Demography model (ED2) to <span class="hlt">predict</span> carbon fluxes of a Puerto Rican tropical forest under realistic <span class="hlt">climate</span> change scenarios. We parameterized ED2 with species-specific tree physiological data using the <span class="hlt">Predictive</span> Ecosystem Analyzer workflow and projected the fate of this ecosystem under five future <span class="hlt">climate</span> scenarios. The model successfully captured inter-annual variability in the dynamics of this tropical forest. Model <span class="hlt">predictions</span> closely followed observed values across a wide range of metrics including above-ground biomass, tree diameter growth, tree size class distributions, and leaf area index. Under a future warming and drying <span class="hlt">climate</span> scenario, the model <span class="hlt">predicted</span> reductions in carbon storage and tree growth, together with large shifts in forest community composition and structure. Such rapid changes in <span class="hlt">climate</span> led the forest to transition from a sink to a source of carbon. Growth respiration and root allocation parameters were responsible for the highest fraction of <span class="hlt">predictive</span> uncertainty in modeled biomass, highlighting the need to target these processes in future data collection. Our study is the first effort to rely on Bayesian model calibration and synthesis to elucidate the key physiological parameters that drive uncertainty in tropical forests responses to <span class="hlt">climatic</span> change. We propose a new path forward for model-data synthesis that can substantially reduce uncertainty in our ability to model tropical forest responses to future <span class="hlt">climate</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29420265','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29420265"><span><span class="hlt">Climate</span>, ecosystems, and planetary futures: The challenge to <span class="hlt">predict</span> life in Earth system models.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Bonan, Gordon B; Doney, Scott C</p> <p>2018-02-02</p> <p>Many global change stresses on terrestrial and marine ecosystems affect not only ecosystem services that are essential to humankind, but also the trajectory of future <span class="hlt">climate</span> by altering energy and mass exchanges with the atmosphere. Earth system models, which simulate terrestrial and marine ecosystems and biogeochemical cycles, offer a common framework for ecological research related to <span class="hlt">climate</span> processes; analyses of vulnerability, impacts, and adaptation; and <span class="hlt">climate</span> change mitigation. They provide an opportunity to move beyond physical descriptors of atmospheric and oceanic states to societally relevant quantities such as wildfire risk, habitat loss, water availability, and crop, fishery, and timber yields. To achieve this, the science of <span class="hlt">climate</span> <span class="hlt">prediction</span> must be extended to a more multifaceted Earth system <span class="hlt">prediction</span> that includes the biosphere and its resources. Copyright © 2018, American Association for the Advancement of Science.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2008AGUFM.B52A..07D','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2008AGUFM.B52A..07D"><span><span class="hlt">Predicting</span> effects of <span class="hlt">climate</span> change on the composition and function of soil microbial communities</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Dubinsky, E.; Brodie, E.; Myint, C.; Ackerly, D.; van Nostrand, J.; Bird, J.; Zhou, J.; Andersen, G.; Firestone, M.</p> <p>2008-12-01</p> <p>Complex soil microbial communities regulate critical ecosystem processes that will be altered by <span class="hlt">climate</span> change. A critical step towards <span class="hlt">predicting</span> the impacts of <span class="hlt">climate</span> change on terrestrial ecosystems is to determine the primary controllers of soil microbial community composition and function, and subsequently evaluate <span class="hlt">climate</span> change scenarios that alter these controllers. We surveyed complex soil bacterial and archaeal communities across a range of <span class="hlt">climatic</span> and edaphic conditions to identify critical controllers of soil microbial community composition in the field and then tested the resulting <span class="hlt">predictions</span> using a 2-year manipulation of precipitation and temperature using mesocosms of California annual grasslands. Community DNA extracted from field soils sampled from six different ecosystems was assayed for bacterial and archaeal communities using high-density phylogenetic microarrays as well as functional gene arrays. Correlations among the relative abundances of thousands of microbial taxa and edaphic factors such as soil moisture and nutrient content provided a basis for <span class="hlt">predicting</span> community responses to changing soil conditions. Communities of soil bacteria and archaea were strongly structured by single environmental predictors, particularly variables related to soil water. Bacteria in the Actinomycetales and Bacilli consistently demonstrated a strong negative response to increasing soil moisture, while taxa in a greater variety of lineages responded positively to increasing soil moisture. In the <span class="hlt">climate</span> change experiment, overall bacterial community structure was impacted significantly by total precipitation but not by plant species. Changes in soil moisture due to decreased rainfall resulted in significant and <span class="hlt">predictable</span> alterations in community structure. Over 70% of the bacterial taxa in common with the cross-ecosystem study responded as <span class="hlt">predicted</span> to altered precipitation, with the most conserved response from Actinobacteria. The functional consequences</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29867150','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29867150"><span>Role of subsurface ocean in decadal <span class="hlt">climate</span> <span class="hlt">predictability</span> over the South Atlantic.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Morioka, Yushi; Doi, Takeshi; Storto, Andrea; Masina, Simona; Behera, Swadhin K</p> <p>2018-06-04</p> <p>Decadal <span class="hlt">climate</span> <span class="hlt">predictability</span> in the South Atlantic is explored by performing reforecast experiments using a coupled general circulation model with two initialization schemes; one is assimilated with observed sea surface temperature (SST) only, and the other is additionally assimilated with observed subsurface ocean temperature and salinity. The South Atlantic is known to undergo decadal variability exhibiting a meridional dipole of SST anomalies through variations in the subtropical high and ocean heat transport. Decadal reforecast experiments in which only the model SST is initialized with the observation do not <span class="hlt">predict</span> well the observed decadal SST variability in the South Atlantic, while the other experiments in which the model SST and subsurface ocean are initialized with the observation skillfully <span class="hlt">predict</span> the observed decadal SST variability, particularly in the Southeast Atlantic. In-depth analysis of upper-ocean heat content reveals that a significant improvement of zonal heat transport in the Southeast Atlantic leads to skillful <span class="hlt">prediction</span> of decadal SST variability there. These results demonstrate potential roles of subsurface ocean assimilation in the skillful <span class="hlt">prediction</span> of decadal <span class="hlt">climate</span> variability over the South Atlantic.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29696859','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29696859"><span>[Potential distribution of Panax ginseng and its <span class="hlt">predicted</span> responses to <span class="hlt">climate</span> change.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Zhao, Ze Fang; Wei, Hai Yan; Guo, Yan Long; Gu, Wei</p> <p>2016-11-18</p> <p>This study utilized Panax ginseng as the research object. Based on BioMod2 platform, with species presence data and 22 <span class="hlt">climatic</span> variables, the potential geographic distribution of P. ginseng under the current conditions in northeast China was simulated with ten species distribution model. And then with the receiver-operating characteristic curve (ROC) as weights, we build an ensemble model, which integrated the results of 10 models, using the ensemble model, the future distributions of P. ginseng were also projected for the periods 2050s and 2070s under the <span class="hlt">climate</span> change scenarios of RCP 8.5, RCP 6, RCP 4.5 and RCP 2.6 emission scenarios described in the Special Report on Emissions Scenarios (SRES) of IPCC (Intergovernmental Panel on <span class="hlt">Climate</span> Change). The results showed that for the entire region of study area, under the present <span class="hlt">climatic</span> conditions, 10.4% of the areas were identified as suitable habitats, which were mainly located in northeast Changbai Mountains area and the southeastern region of the Xiaoxing'an Mountains. The model simulations indicated that the suitable habitats would have a relatively significant change under the different <span class="hlt">climate</span> change scenarios, and generally the range of suitable habitats would be a certain degree of decrease. Meanwhile, the goodness-of-fit, <span class="hlt">predicted</span> ranges, and weights of explanatory variables was various for each model. And according to the goodness-of-fit, Maxent had the highest model performance, and GAM, RF and ANN were followed, while SRE had the lowest <span class="hlt">prediction</span> accuracy. In this study we established an ensemble model, which could improve the accuracy of the existing species distribution models, and optimization of species distribution <span class="hlt">prediction</span> results.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFMGC41A1000H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFMGC41A1000H"><span>Macroweather <span class="hlt">Predictions</span> and <span class="hlt">Climate</span> Projections using Scaling and Historical Observations</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Hébert, R.; Lovejoy, S.; Del Rio Amador, L.</p> <p>2017-12-01</p> <p>There are two fundamental time scales that are pertinent to decadal forecasts and multidecadal projections. The first is the lifetime of planetary scale structures, about 10 days (equal to the deterministic <span class="hlt">predictability</span> limit), and the second is - in the anthropocene - the scale at which the forced anthropogenic variability exceeds the internal variability (around 16 - 18 years). These two time scales define three regimes of variability: weather, macroweather and <span class="hlt">climate</span> that are respectively characterized by increasing, decreasing and then increasing varibility with scale.We discuss how macroweather temperature variability can be skilfully <span class="hlt">predicted</span> to its theoretical stochastic <span class="hlt">predictability</span> limits by exploiting its long-range memory with the Stochastic Seasonal and Interannual <span class="hlt">Prediction</span> System (StocSIPS). At multi-decadal timescales, the temperature response to forcing is approximately linear and this can be exploited to make projections with a Green's function, or <span class="hlt">Climate</span> Response Function (CRF). To make the problem tractable, we exploit the temporal scaling symmetry and restrict our attention to global mean forcing and temperature response using a scaling CRF characterized by the scaling exponent H and an inner scale of linearity τ. An aerosol linear scaling factor α and a non-linear volcanic damping exponent ν were introduced to account for the large uncertainty in these forcings. We estimate the model and forcing parameters by Bayesian inference using historical data and these allow us to analytically calculate a median (and likely 66% range) for the transient <span class="hlt">climate</span> response, and for the equilibrium <span class="hlt">climate</span> sensitivity: 1.6K ([1.5,1.8]K) and 2.4K ([1.9,3.4]K) respectively. Aerosol forcing typically has large uncertainty and we find a modern (2005) forcing very likely range (90%) of [-1.0, -0.3] Wm-2 with median at -0.7 Wm-2. Projecting to 2100, we find that to keep the warming below 1.5 K, future emissions must undergo cuts similar to Representative</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/23892370','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/23892370"><span>Using physiology to <span class="hlt">predict</span> the responses of ants to <span class="hlt">climatic</span> warming.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Diamond, Sarah E; Penick, Clint A; Pelini, Shannon L; Ellison, Aaron M; Gotelli, Nicholas J; Sanders, Nathan J; Dunn, Robert R</p> <p>2013-12-01</p> <p>Physiological intolerance of high temperatures places limits on organismal responses to the temperature increases associated with global <span class="hlt">climatic</span> change. Because ants are geographically widespread, ecologically diverse, and thermophilic, they are an ideal system for exploring the extent to which physiological tolerance can <span class="hlt">predict</span> responses to environmental change. Here, we expand on simple models that use thermal tolerance to <span class="hlt">predict</span> the responses of ants to <span class="hlt">climatic</span> warming. We investigated the degree to which changes in the abundance of ants under warming reflect reductions in the thermal niche space for their foraging. In an eastern deciduous forest system in the United States with approximately 40 ant species, we found that for some species, the loss of thermal niche space for foraging was related to decreases in abundance with increasing experimental <span class="hlt">climatic</span> warming. However, many ant species exhibited no loss of thermal niche space. For one well-studied species, Temnothorax curvispinosus, we examined both survival of workers and growth of colonies (a correlate of reproductive output) as functions of temperature in the laboratory, and found that the range of thermal tolerances for colony growth was much narrower than for survival of workers. We evaluated these functions in the context of experimental <span class="hlt">climatic</span> warming and found that the difference in the responses of these two attributes to temperature generates differences in the means and especially the variances of expected fitness under warming. The expected mean growth of colonies was optimized at intermediate levels of warming (2-4°C above ambient); yet, the expected variance monotonically increased with warming. In contrast, the expected mean and variance of the survival of workers decreased when warming exceeded 4°C above ambient. Together, these results for T. curvispinosus emphasize the importance of measuring reproduction (colony growth) in the context of <span class="hlt">climatic</span> change: indeed, our examination</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70192652','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70192652"><span>Optimal population <span class="hlt">prediction</span> of sandhill crane recruitment based on <span class="hlt">climate</span>-mediated habitat limitations</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Gerber, Brian D.; Kendall, William L.; Hooten, Mevin B.; Dubovsky, James A.; Drewien, Roderick C.</p> <p>2015-01-01</p> <p><span class="hlt">Prediction</span> is fundamental to scientific enquiry and application; however, ecologists tend to favour explanatory modelling. We discuss a <span class="hlt">predictive</span> modelling framework to evaluate ecological hypotheses and to explore novel/unobserved environmental scenarios to assist conservation and management decision-makers. We apply this framework to develop an optimal <span class="hlt">predictive</span> model for juvenile (<1 year old) sandhill crane Grus canadensis recruitment of the Rocky Mountain Population (RMP). We consider spatial <span class="hlt">climate</span> predictors motivated by hypotheses of how drought across multiple time-scales and spring/summer weather affects recruitment.Our <span class="hlt">predictive</span> modelling framework focuses on developing a single model that includes all relevant predictor variables, regardless of collinearity. This model is then optimized for <span class="hlt">prediction</span> by controlling model complexity using a data-driven approach that marginalizes or removes irrelevant predictors from the model. Specifically, we highlight two approaches of statistical regularization, Bayesian least absolute shrinkage and selection operator (LASSO) and ridge regression.Our optimal <span class="hlt">predictive</span> Bayesian LASSO and ridge regression models were similar and on average 37% superior in <span class="hlt">predictive</span> accuracy to an explanatory modelling approach. Our <span class="hlt">predictive</span> models confirmed a priori hypotheses that drought and cold summers negatively affect juvenile recruitment in the RMP. The effects of long-term drought can be alleviated by short-term wet spring–summer months; however, the alleviation of long-term drought has a much greater positive effect on juvenile recruitment. The number of freezing days and snowpack during the summer months can also negatively affect recruitment, while spring snowpack has a positive effect.Breeding habitat, mediated through <span class="hlt">climate</span>, is a limiting factor on population growth of sandhill cranes in the RMP, which could become more limiting with a changing <span class="hlt">climate</span> (i.e. increased drought). These effects are likely not</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/25504863','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/25504863"><span>Microbial models with data-driven parameters <span class="hlt">predict</span> stronger soil carbon responses to <span class="hlt">climate</span> change.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Hararuk, Oleksandra; Smith, Matthew J; Luo, Yiqi</p> <p>2015-06-01</p> <p>Long-term carbon (C) cycle feedbacks to <span class="hlt">climate</span> depend on the future dynamics of soil organic carbon (SOC). Current models show low <span class="hlt">predictive</span> accuracy at simulating contemporary SOC pools, which can be improved through parameter estimation. However, major uncertainty remains in global soil responses to <span class="hlt">climate</span> change, particularly uncertainty in how the activity of soil microbial communities will respond. To date, the role of microbes in SOC dynamics has been implicitly described by decay rate constants in most conventional global carbon cycle models. Explicitly including microbial biomass dynamics into C cycle model formulations has shown potential to improve model <span class="hlt">predictive</span> performance when assessed against global SOC databases. This study aimed to data-constrained parameters of two soil microbial models, evaluate the improvements in performance of those calibrated models in <span class="hlt">predicting</span> contemporary carbon stocks, and compare the SOC responses to <span class="hlt">climate</span> change and their uncertainties between microbial and conventional models. Microbial models with calibrated parameters explained 51% of variability in the observed total SOC, whereas a calibrated conventional model explained 41%. The microbial models, when forced with <span class="hlt">climate</span> and soil carbon input <span class="hlt">predictions</span> from the 5th Coupled Model Intercomparison Project (CMIP5), produced stronger soil C responses to 95 years of <span class="hlt">climate</span> change than any of the 11 CMIP5 models. The calibrated microbial models <span class="hlt">predicted</span> between 8% (2-pool model) and 11% (4-pool model) soil C losses compared with CMIP5 model projections which ranged from a 7% loss to a 22.6% gain. Lastly, we observed unrealistic oscillatory SOC dynamics in the 2-pool microbial model. The 4-pool model also produced oscillations, but they were less prominent and could be avoided, depending on the parameter values. © 2014 John Wiley & Sons Ltd.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFMIN31B0077A','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFMIN31B0077A"><span><span class="hlt">Predicting</span> Seagrass Occurrence in a Changing <span class="hlt">Climate</span> Using Random Forests</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Aydin, O.; Butler, K. A.</p> <p>2017-12-01</p> <p>Seagrasses are marine plants that can quickly sequester vast amounts of carbon (up to 100 times more and 12 times faster than tropical forests). In this work, we present an integrated GIS and machine learning approach to build a data-driven model of seagrass presence-absence. We outline a random forest approach that avoids the prevalence bias in many ecological presence-absence models. One of our goals is to <span class="hlt">predict</span> global seagrass occurrence from a spatially limited training sample. In addition, we conduct a sensitivity study which investigates the vulnerability of seagrass to changing <span class="hlt">climate</span> conditions. We integrate multiple data sources including fine-scale seagrass data from MarineCadastre.gov and the recently available globally extensive publicly available Ecological Marine Units (EMU) dataset. These data are used to train a model for seagrass occurrence along the U.S. coast. In situ oceans data are interpolated using Empirical Bayesian Kriging (EBK) to produce globally extensive <span class="hlt">prediction</span> variables. A neural network is used to estimate probable future values of <span class="hlt">prediction</span> variables such as ocean temperature to assess the impact of a warming <span class="hlt">climate</span> on seagrass occurrence. The proposed workflow can be generalized to many presence-absence models.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/23429000','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/23429000"><span>Derivation and validation of in-hospital mortality <span class="hlt">prediction</span> models in ischaemic stroke patients using <span class="hlt">administrative</span> data.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Lee, Jason; Morishima, Toshitaka; Kunisawa, Susumu; Sasaki, Noriko; Otsubo, Tetsuya; Ikai, Hiroshi; Imanaka, Yuichi</p> <p>2013-01-01</p> <p>Stroke and other cerebrovascular diseases are a major cause of death and disability. <span class="hlt">Predicting</span> in-hospital mortality in ischaemic stroke patients can help to identify high-risk patients and guide treatment approaches. Chart reviews provide important clinical information for mortality <span class="hlt">prediction</span>, but are laborious and limiting in sample sizes. <span class="hlt">Administrative</span> data allow for large-scale multi-institutional analyses but lack the necessary clinical information for outcome research. However, <span class="hlt">administrative</span> claims data in Japan has seen the recent inclusion of patient consciousness and disability information, which may allow more accurate mortality <span class="hlt">prediction</span> using <span class="hlt">administrative</span> data alone. The aim of this study was to derive and validate models to <span class="hlt">predict</span> in-hospital mortality in patients admitted for ischaemic stroke using <span class="hlt">administrative</span> data. The sample consisted of 21,445 patients from 176 Japanese hospitals, who were randomly divided into derivation and validation subgroups. Multivariable logistic regression models were developed using 7- and 30-day and overall in-hospital mortality as dependent variables. Independent variables included patient age, sex, comorbidities upon admission, Japan Coma Scale (JCS) score, Barthel Index score, modified Rankin Scale (mRS) score, and admissions after hours and on weekends/public holidays. Models were developed in the derivation subgroup, and coefficients from these models were applied to the validation subgroup. <span class="hlt">Predictive</span> ability was analysed using C-statistics; calibration was evaluated with Hosmer-Lemeshow χ(2) tests. All three models showed <span class="hlt">predictive</span> abilities similar or surpassing that of chart review-based models. The C-statistics were highest in the 7-day in-hospital mortality <span class="hlt">prediction</span> model, at 0.906 and 0.901 in the derivation and validation subgroups, respectively. For the 30-day in-hospital mortality <span class="hlt">prediction</span> models, the C-statistics for the derivation and validation subgroups were 0.893 and 0</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2009AGUFM.H33D0903C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2009AGUFM.H33D0903C"><span>A blueprint for using <span class="hlt">climate</span> change <span class="hlt">predictions</span> in an eco-hydrological study</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Caporali, E.; Fatichi, S.; Ivanov, V. Y.</p> <p>2009-12-01</p> <p>There is a growing interest to extend <span class="hlt">climate</span> change <span class="hlt">predictions</span> to smaller, catchment-size scales and identify their implications on hydrological and ecological processes. Small scale processes are, in fact, expected to mediate <span class="hlt">climate</span> changes, producing local effects and feedbacks that can interact with the principal consequences of the change. This is particularly applicable, when a complex interaction, such as the inter-relationship between the hydrological cycle and vegetation dynamics, is considered. This study presents a blueprint methodology for studying <span class="hlt">climate</span> change impacts, as inferred from <span class="hlt">climate</span> models, on eco-hydrological dynamics at the catchment scale. <span class="hlt">Climate</span> conditions, present or future, are imposed through input hydrometeorological variables for hydrological and eco-hydrological models. These variables are simulated with an hourly weather generator as an outcome of a stochastic downscaling technique. The generator is parameterized to reproduce the <span class="hlt">climate</span> of southwestern Arizona for present (1961-2000) and future (2081-2100) conditions. The methodology provides the capability to generate ensemble realizations for the future that take into account the heterogeneous nature of <span class="hlt">climate</span> <span class="hlt">predictions</span> from different models. The generated time series of meteorological variables for the two scenarios corresponding to the current and mean expected future serve as input to a coupled hydrological and vegetation dynamics model, “Tethys-Chloris”. The hydrological model reproduces essential components of the land-surface hydrological cycle, solving the mass and energy budget equations. The vegetation model parsimoniously parameterizes essential plant life-cycle processes, including photosynthesis, phenology, carbon allocation, and tissue turnover. The results for the two mean scenarios are compared and discussed in terms of changes in the hydrological balance components, energy fluxes, and indices of vegetation productivity The need to account for</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017ThApC.tmp..166H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017ThApC.tmp..166H"><span><span class="hlt">Prediction</span> of <span class="hlt">climate</span> change in Brunei Darussalam using statistical downscaling model</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Hasan, Dk. Siti Nurul Ain binti Pg. Ali; Ratnayake, Uditha; Shams, Shahriar; Nayan, Zuliana Binti Hj; Rahman, Ena Kartina Abdul</p> <p>2017-06-01</p> <p><span class="hlt">Climate</span> is changing and evidence suggests that the impact of <span class="hlt">climate</span> change would influence our everyday lives, including agriculture, built environment, energy management, food security and water resources. Brunei Darussalam located within the heart of Borneo will be affected both in terms of precipitation and temperature. Therefore, it is crucial to comprehend and assess how important <span class="hlt">climate</span> indicators like temperature and precipitation are expected to vary in the future in order to minimise its impact. This study assesses the application of a statistical downscaling model (SDSM) for downscaling General Circulation Model (GCM) results for maximum and minimum temperatures along with precipitation in Brunei Darussalam. It investigates future <span class="hlt">climate</span> changes based on numerous scenarios using Hadley Centre Coupled Model, version 3 (HadCM3), Canadian Earth System Model (CanESM2) and third-generation Coupled Global <span class="hlt">Climate</span> Model (CGCM3) outputs. The SDSM outputs were improved with the implementation of bias correction and also using a monthly sub-model instead of an annual sub-model. The outcomes of this assessment show that monthly sub-model performed better than the annual sub-model. This study indicates a satisfactory applicability for generation of maximum temperatures, minimum temperatures and precipitation for future periods of 2017-2046 and 2047-2076. All considered models and the scenarios were consistent in <span class="hlt">predicting</span> increasing trend of maximum temperature, increasing trend of minimum temperature and decreasing trend of precipitations. Maximum overall trend of Tmax was also observed for CanESM2 with Representative Concentration Pathways (RCP) 8.5 scenario. The increasing trend is 0.014 °C per year. Accordingly, by 2076, the highest <span class="hlt">prediction</span> of average maximum temperatures is that it will increase by 1.4 °C. The same model <span class="hlt">predicts</span> an increasing trend of Tmin of 0.004 °C per year, while the highest trend is seen under CGCM3-A2 scenario which is 0.009 </p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/28448303','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/28448303"><span><span class="hlt">Predictability</span> of Interruptions During Medication <span class="hlt">Administration</span> With Related Behavioral Management Strategies.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Johnson, Maree; Weidemann, Gabrielle; Adams, Rebecca; Manias, Elizabeth; Levett-Jones, Tracy; Aguilar, Vicki; Everett, Bronwyn</p> <p></p> <p>The aim of this qualitative study was to examine the nature of interruptions during medication <span class="hlt">administration</span>. Focus groups were conducted with medical/surgical nurses (n = 15), critical care nurses (n = 13), and nurse managers/educators/specialists (n = 6). Most interruptions (78%) were <span class="hlt">predictable</span>. Nurse-adopted strategies included blocking, engaging, mediating, multitasking, and preventing. Educational content was developed that relates behavioral strategies to respond to <span class="hlt">predictable</span> and unpredictable interruptions.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFM.H33K1721W','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFM.H33K1721W"><span>Land-atmosphere coupling and <span class="hlt">climate</span> <span class="hlt">prediction</span> over the U.S. Southern Great Plains</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Williams, I. N.; Lu, Y.; Kueppers, L. M.; Riley, W. J.; Biraud, S.; Bagley, J. E.; Torn, M. S.</p> <p>2016-12-01</p> <p>Biases in land-atmosphere coupling in <span class="hlt">climate</span> models can contribute to <span class="hlt">climate</span> <span class="hlt">prediction</span> biases, but land models are rarely evaluated in the context of this coupling. We tested land-atmosphere coupling and explored effects of land surface parameterizations on <span class="hlt">climate</span> <span class="hlt">prediction</span> in a single-column version of the NCAR Community Earth System Model (CESM1.2.2) and an offline Community Land Model (CLM4.5). The correlation between leaf area index (LAI) and surface evaporative fraction (ratio of latent to total turbulent heat flux) was substantially underpredicted compared to observations in the U.S. Southern Great Plains, while the correlation between soil moisture and evaporative fraction was overpredicted by CLM4.5. These correlations were improved by prescribing observed LAI, increasing soil resistance to evaporation, increasing minimum stomatal conductance, and increasing leaf reflectance. The modifications reduced the root mean squared error (RMSE) in daytime 2 m air temperature from 3.6 C to 2 C in summer (JJA), and reduced RMSE in total JJA precipitation from 133 to 84 mm. The modifications had the largest effect on <span class="hlt">prediction</span> of summer drought in 2006, when a warm bias in daytime 2 m air temperature was reduced from +6 C to a smaller cold bias of -1.3 C, and a corresponding dry bias in total JJA precipitation was reduced from -111 mm to -23 mm. Thus, the role of vegetation in droughts and heat waves is likely underpredicted in CESM1.2.2, and improvements in land surface models can improve <span class="hlt">prediction</span> of <span class="hlt">climate</span> extremes.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017JHyd..551..300H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017JHyd..551..300H"><span>Toward a categorical drought <span class="hlt">prediction</span> system based on U.S. Drought Monitor (USDM) and <span class="hlt">climate</span> forecast</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Hao, Zengchao; Xia, Youlong; Luo, Lifeng; Singh, Vijay P.; Ouyang, Wei; Hao, Fanghua</p> <p>2017-08-01</p> <p>Disastrous impacts of recent drought events around the world have led to extensive efforts in drought monitoring and <span class="hlt">prediction</span>. Various drought information systems have been developed with different indicators to provide early drought warning. The <span class="hlt">climate</span> forecast from North American Multimodel Ensemble (NMME) has been among the most salient progress in <span class="hlt">climate</span> <span class="hlt">prediction</span> and its application for drought <span class="hlt">prediction</span> has been considerably growing. Since its development in 1999, the U.S. Drought Monitor (USDM) has played a critical role in drought monitoring with different drought categories to characterize drought severity, which has been employed to aid decision making by a wealth of users such as natural resource managers and authorities. Due to wide applications of USDM, the development of drought <span class="hlt">prediction</span> with USDM drought categories would greatly aid decision making. This study presented a categorical drought <span class="hlt">prediction</span> system for <span class="hlt">predicting</span> USDM drought categories in the U.S., based on the initial conditions from USDM and seasonal <span class="hlt">climate</span> forecasts from NMME. Results of USDM drought categories <span class="hlt">predictions</span> in the U.S. demonstrate the potential of the <span class="hlt">prediction</span> system, which is expected to contribute to operational early drought warning in the U.S.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2009AGUFMNG13A1084G','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2009AGUFMNG13A1084G"><span>Knowledge discovery and nonlinear modeling can complement <span class="hlt">climate</span> model simulations for <span class="hlt">predictive</span> insights about <span class="hlt">climate</span> extremes and their impacts</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Ganguly, A. R.; Steinbach, M.; Kumar, V.</p> <p>2009-12-01</p> <p>The IPCC AR4 not only provided conclusive evidence about anticipated global warming at century scales, but also indicated with a high level of certainty that the warming is caused by anthropogenic emissions. However, an outstanding knowledge-gap is to develop credible projections of <span class="hlt">climate</span> extremes and their impacts. <span class="hlt">Climate</span> extremes are defined in this context as extreme weather and hydrological events, as well as changes in regional hydro-meteorological patterns, especially at decadal scales. While temperature extremes from <span class="hlt">climate</span> models have relatively better skills, hydrological variables and their extremes have significant shortcomings. Credible projections about tropical storms, sea level rise, coastal storm surge, land glacier melts, and landslides remain elusive. The next generation of <span class="hlt">climate</span> models is expected to have higher precision. However, their ability to provide more accurate projections of <span class="hlt">climate</span> extremes remains to be tested. Projections of observed trends into the future may not be reliable in non-stationary environments like <span class="hlt">climate</span> change, even though functional relationships derived from physics may hold. On the other hand, assessments of <span class="hlt">climate</span> change impacts which are useful for stakeholders and policy makers depend critically on regional and decadal scale projections of <span class="hlt">climate</span> extremes. Thus, <span class="hlt">climate</span> impacts scientists often need to develop qualitative inferences about the not so-well <span class="hlt">predicted</span> <span class="hlt">climate</span> extremes based on insights from observations (e.g., increased hurricane intensity) or conceptual understanding (e.g., relation of wildfires to regional warming or drying and hurricanes to SST). However, neither conceptual understanding nor observed trends may be reliable when extrapolating in a non-stationary environment. These urgent societal priorities offer fertile grounds for nonlinear modeling and knowledge discovery approaches. Thus, qualitative inferences on <span class="hlt">climate</span> extremes and impacts may be transformed into quantitative</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_8");'>8</a></li> <li><a href="#" onclick='return showDiv("page_9");'>9</a></li> <li class="active"><span>10</span></li> <li><a href="#" onclick='return showDiv("page_11");'>11</a></li> <li><a href="#" onclick='return showDiv("page_12");'>12</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_10 --> <div id="page_11" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_9");'>9</a></li> <li><a href="#" onclick='return showDiv("page_10");'>10</a></li> <li class="active"><span>11</span></li> <li><a href="#" onclick='return showDiv("page_12");'>12</a></li> <li><a href="#" onclick='return showDiv("page_13");'>13</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="201"> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/28223487','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/28223487"><span>Selenium deficiency risk <span class="hlt">predicted</span> to increase under future <span class="hlt">climate</span> change.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Jones, Gerrad D; Droz, Boris; Greve, Peter; Gottschalk, Pia; Poffet, Deyan; McGrath, Steve P; Seneviratne, Sonia I; Smith, Pete; Winkel, Lenny H E</p> <p>2017-03-14</p> <p>Deficiencies of micronutrients, including essential trace elements, affect up to 3 billion people worldwide. The dietary availability of trace elements is determined largely by their soil concentrations. Until now, the mechanisms governing soil concentrations have been evaluated in small-scale studies, which identify soil physicochemical properties as governing variables. However, global concentrations of trace elements and the factors controlling their distributions are virtually unknown. We used 33,241 soil data points to model recent (1980-1999) global distributions of Selenium (Se), an essential trace element that is required for humans. Worldwide, up to one in seven people have been estimated to have low dietary Se intake. Contrary to small-scale studies, soil Se concentrations were dominated by <span class="hlt">climate</span>-soil interactions. Using moderate <span class="hlt">climate</span>-change scenarios for 2080-2099, we <span class="hlt">predicted</span> that changes in <span class="hlt">climate</span> and soil organic carbon content will lead to overall decreased soil Se concentrations, particularly in agricultural areas; these decreases could increase the prevalence of Se deficiency. The importance of <span class="hlt">climate</span>-soil interactions to Se distributions suggests that other trace elements with similar retention mechanisms will be similarly affected by <span class="hlt">climate</span> change.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFMIN33B0115M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFMIN33B0115M"><span><span class="hlt">Predictability</span> of Extreme <span class="hlt">Climate</span> Events via a Complex Network Approach</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Muhkin, D.; Kurths, J.</p> <p>2017-12-01</p> <p>We analyse <span class="hlt">climate</span> dynamics from a complex network approach. This leads to an inverse problem: Is there a backbone-like structure underlying the <span class="hlt">climate</span> system? For this we propose a method to reconstruct and analyze a complex network from data generated by a spatio-temporal dynamical system. This approach enables us to uncover relations to global circulation patterns in oceans and atmosphere. This concept is then applied to Monsoon data; in particular, we develop a general framework to <span class="hlt">predict</span> extreme events by combining a non-linear synchronization technique with complex networks. Applying this method, we uncover a new mechanism of extreme floods in the eastern Central Andes which could be used for operational forecasts. Moreover, we analyze the Indian Summer Monsoon (ISM) and identify two regions of high importance. By estimating an underlying critical point, this leads to an improved <span class="hlt">prediction</span> of the onset of the ISM; this scheme was successful in 2016 and 2017.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://eric.ed.gov/?q=ex+AND+post+AND+facto+AND+studies&pg=6&id=ED566447','ERIC'); return false;" href="https://eric.ed.gov/?q=ex+AND+post+AND+facto+AND+studies&pg=6&id=ED566447"><span>The Effects of Teacher Perceptions of <span class="hlt">Administrative</span> Support, School <span class="hlt">Climate</span>, and Academic Success in Urban Schools</span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Robinson, Lakishia N.</p> <p>2015-01-01</p> <p>Teacher turnover refers to major changes in teachers' assignments from one school year to the next. Past research has given an overview of several factors of teacher turnover. These factors include the school environment, teacher collaborative efforts, <span class="hlt">administrative</span> support, school <span class="hlt">climate</span>, location, salary, classroom management, academic…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.cpc.ncep.noaa.gov/products/predictions/short_range/cold/wc_610.php','SCIGOVWS'); return false;" href="http://www.cpc.ncep.noaa.gov/products/predictions/short_range/cold/wc_610.php"><span><span class="hlt">Climate</span> <span class="hlt">Prediction</span> Center - 6-10 Day Wind Chill Outlook</span></a></p> <p><a target="_blank" href="http://www.science.gov/aboutsearch.html">Science.gov Websites</a></p> <p></p> <p></p> <p>8-14 Day Obsrv'd About Us Our Mission Who We Are Contact Us CPC Information CPC <em>Web</em> Team 6-10 & official <em>Web</em> portal to all federal, state, and local government <em>Web</em> resources and services. 6-10 Day Lowest Park, Maryland 20740 <span class="hlt">Climate</span> <span class="hlt">Prediction</span> Center <em>Web</em> Team Page last modified: August 30, 2012 Disclaimer</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017EGUGA..1914860C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017EGUGA..1914860C"><span>Seasonal-to-decadal <span class="hlt">predictability</span> in the Nordic Seas and Arctic with the Norwegian <span class="hlt">Climate</span> <span class="hlt">Prediction</span> Model</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Counillon, Francois; Kimmritz, Madlen; Keenlyside, Noel; Wang, Yiguo; Bethke, Ingo</p> <p>2017-04-01</p> <p>The Norwegian <span class="hlt">Climate</span> <span class="hlt">Prediction</span> Model combines the Norwegian Earth System Model and the Ensemble Kalman Filter data assimilation method. The <span class="hlt">prediction</span> skills of different versions of the system (with 30 members) are tested in the Nordic Seas and the Arctic region. Comparing the hindcasts branched from a SST-only assimilation run with a free ensemble run of 30 members, we are able to dissociate the <span class="hlt">predictability</span> rooted in the external forcing from the <span class="hlt">predictability</span> harvest from SST derived initial conditions. The latter adds <span class="hlt">predictability</span> in the North Atlantic subpolar gyre and the Nordic Seas regions and overall there is very little degradation or forecast drift. Combined assimilation of SST and T-S profiles further improves the <span class="hlt">prediction</span> skill in the Nordic Seas and into the Arctic. These lead to multi-year <span class="hlt">predictability</span> in the high-latitudes. Ongoing developments of strongly coupled assimilation (ocean and sea ice) of ice concentration in idealized twin experiment will be shown, as way to further enhance <span class="hlt">prediction</span> skill in the Arctic.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFMNH53E..03M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFMNH53E..03M"><span>Towards a Unified Framework in Hydroclimate Extremes <span class="hlt">Prediction</span> in Changing <span class="hlt">Climate</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Moradkhani, H.; Yan, H.; Zarekarizi, M.; Bracken, C.</p> <p>2016-12-01</p> <p>Spatio-temporal analysis and <span class="hlt">prediction</span> of hydroclimate extremes are of paramount importance in disaster mitigation and emergency management. The IPCC special report on managing the risks of extreme events and disasters emphasizes that the global warming would change the frequency, severity, and spatial pattern of extremes. In addition to <span class="hlt">climate</span> change, land use and land cover changes also influence the extreme characteristics at regional scale. Therefore, natural variability and anthropogenic changes to the hydroclimate system result in nonstationarity in hydroclimate variables. In this presentation recent advancements in developing and using Bayesian approaches to account for non-stationarity in hydroclimate extremes are discussed. Also, implications of these approaches in flood frequency analysis, treatment of spatial dependence, the impact of large-scale <span class="hlt">climate</span> variability, the selection of cause-effect covariates, with quantification of model errors in extreme <span class="hlt">prediction</span> is explained. Within this framework, the applicability and usefulness of the ensemble data assimilation for extreme flood <span class="hlt">predictions</span> is also introduced. Finally, a practical and easy to use approach for better communication with decision-makers and emergency managers is presented.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFMGC23A1209H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFMGC23A1209H"><span>Toward Evaluating the <span class="hlt">Predictability</span> of Arctic-related <span class="hlt">Climate</span> Variations: Initial Results from ArCS Project Theme 5</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Hasumi, H.</p> <p>2016-12-01</p> <p>We present initial results from the theme 5 of the project ArCS, which is a national flagship project for Arctic research in Japan. The goal of theme 5 is to evaluate the <span class="hlt">predictability</span> of Arctic-related <span class="hlt">climate</span> variations, wherein we aim to: (1) establish the scientific basis of <span class="hlt">climate</span> <span class="hlt">predictability</span>; and (2) develop a method for <span class="hlt">predicting</span>/projecting medium- and long-term <span class="hlt">climate</span> variations. Variability in the Arctic environment remotely influences middle and low latitudes. Since some of the processes specific to the Arctic environment function as a long memory of the state of the <span class="hlt">climate</span>, understanding of the process of remote connections would lead to higher-precision and longer-term <span class="hlt">prediction</span> of global <span class="hlt">climate</span> variations. Conventional <span class="hlt">climate</span> models have large uncertainty in the Arctic region. By making Arctic processes in <span class="hlt">climate</span> models more sophisticated, we aim to clarify the role of multi-sphere interaction in the Arctic environment. In this regard, our newly developed high resolution ice-ocean model has revealed the relationship between the oceanic heat transport into the Arctic Ocean and the synoptic scale atmospheric variability. We also aim to reveal the mechanism of remote connections by conducting <span class="hlt">climate</span> simulations and analyzing various types of <span class="hlt">climate</span> datasets. Our atmospheric model experiments under possible future situations of Arctic sea ice cover indicate that reduction of sea ice qualitatively alters the basic mechanism of remote connection. Also, our analyses of <span class="hlt">climate</span> data have identified the cause of recent more frequent heat waves at Eurasian mid-to-high latitudes and clarified the dynamical process which forms the West Pacific pattern, a dominant mode of the atmospheric anomalous circulation in the West Pacific region which also exhibits a significant signal in the Arctic stratosphere.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2011AGUFMNG44A..03G','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2011AGUFMNG44A..03G"><span>Computational data sciences for assessment and <span class="hlt">prediction</span> of <span class="hlt">climate</span> extremes</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Ganguly, A. R.</p> <p>2011-12-01</p> <p><span class="hlt">Climate</span> extremes may be defined inclusively as severe weather events or large shifts in global or regional weather patterns which may be caused or exacerbated by natural <span class="hlt">climate</span> variability or <span class="hlt">climate</span> change. This area of research arguably represents one of the largest knowledge-gaps in <span class="hlt">climate</span> science which is relevant for informing resource managers and policy makers. While physics-based <span class="hlt">climate</span> models are essential in view of non-stationary and nonlinear dynamical processes, their current pace of uncertainty reduction may not be adequate for urgent stakeholder needs. The structure of the models may in some cases preclude reduction of uncertainty for critical processes at scales or for the extremes of interest. On the other hand, methods based on complex networks, extreme value statistics, machine learning, and space-time data mining, have demonstrated significant promise to improve scientific understanding and generate enhanced <span class="hlt">predictions</span>. When combined with conceptual process understanding at multiple spatiotemporal scales and designed to handle massive data, interdisciplinary data science methods and algorithms may complement or supplement physics-based models. Specific examples from the prior literature and our ongoing work suggests how data-guided improvements may be possible, for example, in the context of ocean meteorology, <span class="hlt">climate</span> oscillators, teleconnections, and atmospheric process understanding, which in turn can improve projections of regional <span class="hlt">climate</span>, precipitation extremes and tropical cyclones in an useful and interpretable fashion. A community-wide effort is motivated to develop and adapt computational data science tools for translating <span class="hlt">climate</span> model simulations to information relevant for adaptation and policy, as well as for improving our scientific understanding of <span class="hlt">climate</span> extremes from both observed and model-simulated data.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.cpc.ncep.noaa.gov/products/outreach/CDPW41/CDPW41.php','SCIGOVWS'); return false;" href="http://www.cpc.ncep.noaa.gov/products/outreach/CDPW41/CDPW41.php"><span><span class="hlt">Climate</span> <span class="hlt">Prediction</span> Center - Outreach: 41st Annual <span class="hlt">Climate</span> Diagnostics &</span></a></p> <p><a target="_blank" href="http://www.science.gov/aboutsearch.html">Science.gov Websites</a></p> <p></p> <p></p> <p>the University of Maine <em><span class="hlt">Climate</span></em> <em>Change</em> Institute and School of Earth and <em><span class="hlt">Climate</span></em> Sciences and is co (drought, heat waves, severe weather, tropical cyclones) in the framework of <em><span class="hlt">climate</span></em> variability and <em>change</em> and including the use of paleoclimate data. Arctic <em><span class="hlt">climate</span></em> variability and <em>change</em>, and linkages to</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.fs.usda.gov/treesearch/pubs/33179','TREESEARCH'); return false;" href="https://www.fs.usda.gov/treesearch/pubs/33179"><span>Approaches to <span class="hlt">predicting</span> potential impacts of <span class="hlt">climate</span> change on forest disease: an example with Armillaria root disease</span></a></p> <p><a target="_blank" href="http://www.fs.usda.gov/treesearch/">Treesearch</a></p> <p>Ned B. Klopfenstein; Mee-Sook Kim; John W. Hanna; Bryce A. Richardson; John E. Lundquist</p> <p>2009-01-01</p> <p><span class="hlt">Predicting</span> <span class="hlt">climate</span> change influences on forest diseases will foster forest management practices that minimize adverse impacts of diseases. Precise locations of accurately identified pathogens and hosts must be documented and spatially referenced to determine which <span class="hlt">climatic</span> factors influence species distribution. With this information, bioclimatic models can <span class="hlt">predict</span> the...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/19537550','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/19537550"><span>Comparing niche- and process-based models to reduce <span class="hlt">prediction</span> uncertainty in species range shifts under <span class="hlt">climate</span> change.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Morin, Xavier; Thuiller, Wilfried</p> <p>2009-05-01</p> <p>Obtaining reliable <span class="hlt">predictions</span> of species range shifts under <span class="hlt">climate</span> change is a crucial challenge for ecologists and stakeholders. At the continental scale, niche-based models have been widely used in the last 10 years to <span class="hlt">predict</span> the potential impacts of <span class="hlt">climate</span> change on species distributions all over the world, although these models do not include any mechanistic relationships. In contrast, species-specific, process-based <span class="hlt">predictions</span> remain scarce at the continental scale. This is regrettable because to secure relevant and accurate <span class="hlt">predictions</span> it is always desirable to compare <span class="hlt">predictions</span> derived from different kinds of models applied independently to the same set of species and using the same raw data. Here we compare <span class="hlt">predictions</span> of range shifts under <span class="hlt">climate</span> change scenarios for 2100 derived from niche-based models with those of a process-based model for 15 North American boreal and temperate tree species. A general pattern emerged from our comparisons: niche-based models tend to <span class="hlt">predict</span> a stronger level of extinction and a greater proportion of colonization than the process-based model. This result likely arises because niche-based models do not take phenotypic plasticity and local adaptation into account. Nevertheless, as the two kinds of models rely on different assumptions, their complementarity is revealed by common findings. Both modeling approaches highlight a major potential limitation on species tracking their <span class="hlt">climatic</span> niche because of migration constraints and identify similar zones where species extirpation is likely. Such convergent <span class="hlt">predictions</span> from models built on very different principles provide a useful way to offset uncertainties at the continental scale. This study shows that the use in concert of both approaches with their own caveats and advantages is crucial to obtain more robust results and that comparisons among models are needed in the near future to gain accuracy regarding <span class="hlt">predictions</span> of range shifts under <span class="hlt">climate</span> change.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/25808951','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/25808951"><span>Optimal population <span class="hlt">prediction</span> of sandhill crane recruitment based on <span class="hlt">climate</span>-mediated habitat limitations.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Gerber, Brian D; Kendall, William L; Hooten, Mevin B; Dubovsky, James A; Drewien, Roderick C</p> <p>2015-09-01</p> <p>1. <span class="hlt">Prediction</span> is fundamental to scientific enquiry and application; however, ecologists tend to favour explanatory modelling. We discuss a <span class="hlt">predictive</span> modelling framework to evaluate ecological hypotheses and to explore novel/unobserved environmental scenarios to assist conservation and management decision-makers. We apply this framework to develop an optimal <span class="hlt">predictive</span> model for juvenile (<1 year old) sandhill crane Grus canadensis recruitment of the Rocky Mountain Population (RMP). We consider spatial <span class="hlt">climate</span> predictors motivated by hypotheses of how drought across multiple time-scales and spring/summer weather affects recruitment. 2. Our <span class="hlt">predictive</span> modelling framework focuses on developing a single model that includes all relevant predictor variables, regardless of collinearity. This model is then optimized for <span class="hlt">prediction</span> by controlling model complexity using a data-driven approach that marginalizes or removes irrelevant predictors from the model. Specifically, we highlight two approaches of statistical regularization, Bayesian least absolute shrinkage and selection operator (LASSO) and ridge regression. 3. Our optimal <span class="hlt">predictive</span> Bayesian LASSO and ridge regression models were similar and on average 37% superior in <span class="hlt">predictive</span> accuracy to an explanatory modelling approach. Our <span class="hlt">predictive</span> models confirmed a priori hypotheses that drought and cold summers negatively affect juvenile recruitment in the RMP. The effects of long-term drought can be alleviated by short-term wet spring-summer months; however, the alleviation of long-term drought has a much greater positive effect on juvenile recruitment. The number of freezing days and snowpack during the summer months can also negatively affect recruitment, while spring snowpack has a positive effect. 4. Breeding habitat, mediated through <span class="hlt">climate</span>, is a limiting factor on population growth of sandhill cranes in the RMP, which could become more limiting with a changing <span class="hlt">climate</span> (i.e. increased drought). These effects are</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFMGC13G0838B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFMGC13G0838B"><span>Dynamic response of airborne infections to <span class="hlt">climate</span> change: <span class="hlt">predictions</span> for varicella</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Baker, R.; Mahmud, A. S.; Metcalf, C. J. E.</p> <p>2017-12-01</p> <p>Characterizing how <span class="hlt">climate</span> change will alter the burden of infectious diseases has clear applications for public health policy. Despite our uniquely detailed understanding of the transmission process for directly transmitted infections, the impact of <span class="hlt">climate</span> variables on these infections remains understudied. We develop a novel methodology for estimating the causal relationship between <span class="hlt">climate</span> and directly transmitted infections, which combines an epidemiological model of disease transmission with panel regression techniques. Our method allows us to move beyond correlational approaches to studying the link between <span class="hlt">climate</span> and infectious diseases. Further, we can generate semi-mechanistic projections of incidence across <span class="hlt">climate</span> scenarios. We illustrate our approach using 30 years of reported cases of varicella, a common airborne childhood infection, across 32 states in Mexico. We find significantly increased varicella transmission in drier conditions. We use this to map potential changes in the magnitude and variability of varicella incidence in Mexico as a result of projected changes in future <span class="hlt">climate</span> conditions. Our results indicate that the <span class="hlt">predicted</span> decrease in humidity in Mexico towards the end of the century will increase incidence of varicella, all else equal, and that these changes in incidence will be non-uniform across the year.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2009AGUFMGC34A..04W','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2009AGUFMGC34A..04W"><span>Uncertainty and Risk in the <span class="hlt">Predictions</span> of Global <span class="hlt">Climate</span> Models. (Invited)</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Winsberg, E.</p> <p>2009-12-01</p> <p>There has been a great deal of emphasis, in recent years, on developing methods for assigning probabilities, in the form of quantitative margins of uncertainty (QMUs) to the <span class="hlt">predictions</span> of global <span class="hlt">climate</span> models. In this paper, I will argue that a large part of the motivation for this activity has been misplaced. Rather than explicit QMUs, <span class="hlt">climate</span> scientists ought to focus on risk mitigation: offering policy advice about what courses of action need to be taken in order to reduce the risk of negative outcomes to acceptable levels. The advantages of QMUs are clear. QMUs can be an extremely effective tool for dividing our intellectual labor into the epistemic and the normative. If scientists can manage to objectively assign probabilities to various outcomes given certain choices of action, then they can effectively leave decisions about the relative social value of these outcomes out of the work they do as experts. In this way, it is commonly thought, scientists can keep ethical questions—like questions about the relative value of environmental stability vs. the availability of fossil fuels for economic development—separate from the purely scientific questions about the workings of the <span class="hlt">climate</span> system. It is this line of thinking, or so I argue, that has motivated the large quantity of intellectual labor that has recently been devoted, by both <span class="hlt">climate</span> scientists and statisticians, to attaching QMUs to the <span class="hlt">predictions</span> of global <span class="hlt">climate</span> models. Such an approach, and the attendant division of labor that it affords between those who discover the facts and those who decide what we should value, has obvious advantages. Scientists, after all, are not elected leaders, and they lack the political legitimacy to make decisions on behalf of the public about what is socially valuable. Elected leaders, on the other hand, rarely have the expertise they would need to accurately forecast, for themselves, what the likely outcomes of their policy choices would be. Since it would be</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014EGUGA..1612907S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014EGUGA..1612907S"><span>On the use and potential use of seasonal to decadal <span class="hlt">climate</span> <span class="hlt">predictions</span> for decision-making in Europe</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Soares, Marta Bruno; Dessai, Suraje</p> <p>2014-05-01</p> <p>The need for <span class="hlt">climate</span> information to help inform decision-making in sectors susceptible to <span class="hlt">climate</span> events and impacts is widely recognised. In Europe, developments in the science and models underpinning the study of <span class="hlt">climate</span> variability and change have led to an increased interest in seasonal to decadal <span class="hlt">climate</span> <span class="hlt">predictions</span> (S2DCP). While seasonal <span class="hlt">climate</span> forecasts are now routinely produced operationally by a number of centres around the world, decadal <span class="hlt">climate</span> <span class="hlt">predictions</span> are still in its infancy restricted to the realm of research. Contrary to other regions of the world, where the use of these types of forecasts, particularly at seasonal timescales, has been pursued in recent years due to higher levels of <span class="hlt">predictability</span>, little is known about the uptake and <span class="hlt">climate</span> information needs of end-users regarding S2DCP in Europe. To fill this gap we conducted in-depth interviews with experts and decision-makers across a range of European sectors, a workshop with European <span class="hlt">climate</span> services providers, and a systematic literature review on the use of S2DCP in Europe. This study is part of the EUropean Provision Of Regional Impact Assessment on a Seasonal-to-decadal timescale (EUPORIAS) project which aims to develop semi-operational prototypes of impact <span class="hlt">prediction</span> systems in Europe on seasonal to decadal timescales. We found that the emerging landscape of users and potential users of S2DCP in Europe is complex and heterogeneous. Differences in S2DCP information needs across and within organisations and sectors are largely underpinned by factors such as the institutional and regulatory context of the organisations, the plethora of activities and decision-making processes involved, the level of expertise and capacity of the users, and the availability of resources within the organisations. In addition, although the use of S2DCP across Europe is still fairly limited, particular sectors such as agriculture, health, energy, water, (re)insurance, and transport are taking the lead on</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016EGUGA..1815826M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016EGUGA..1815826M"><span>Evaluating Antarctic sea ice <span class="hlt">predictability</span> at seasonal to interannual timescales in global <span class="hlt">climate</span> models</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Marchi, Sylvain; Fichefet, Thierry; Goosse, Hugues; Zunz, Violette; Tietsche, Steffen; Day, Jonny; Hawkins, Ed</p> <p>2016-04-01</p> <p>Unlike the rapid sea ice losses reported in the Arctic, satellite observations show an overall increase in Antarctic sea ice extent over recent decades. Although many processes have already been suggested to explain this positive trend, it remains the subject of current investigations. Understanding the evolution of the Antarctic sea ice turns out to be more complicated than for the Arctic for two reasons: the lack of observations and the well-known biases of <span class="hlt">climate</span> models in the Southern Ocean. Irrespective of those issues, another one is to determine whether the positive trend in sea ice extent would have been <span class="hlt">predictable</span> if adequate observations and models were available some decades ago. This study of Antarctic sea ice <span class="hlt">predictability</span> is carried out using 6 global <span class="hlt">climate</span> models (HadGEM1.2, MPI-ESM-LR, GFDL CM3, EC-Earth V2, MIROC 5.2 and ECHAM 6-FESOM) which are all part of the APPOSITE project. These models are used to perform hindcast simulations in a perfect model approach. The <span class="hlt">predictive</span> skill is estimated thanks to the PPP (Potential Prognostic <span class="hlt">Predictability</span>) and the ACC (Anomaly Correlation Coefficient). The former is a measure of the uncertainty of the ensemble while the latter assesses the accuracy of the <span class="hlt">prediction</span>. These two indicators are applied to different variables related to sea ice, in particular the total sea ice extent and the ice edge location. This first model intercomparison study about sea ice <span class="hlt">predictability</span> in the Southern Ocean aims at giving a general overview of Antarctic sea ice <span class="hlt">predictability</span> in current global <span class="hlt">climate</span> models.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29341358','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29341358"><span>Thermal and hydrologic responses to <span class="hlt">climate</span> change <span class="hlt">predict</span> marked alterations in boreal stream invertebrate assemblages.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Mustonen, Kaisa-Riikka; Mykrä, Heikki; Marttila, Hannu; Sarremejane, Romain; Veijalainen, Noora; Sippel, Kalle; Muotka, Timo; Hawkins, Charles P</p> <p>2018-06-01</p> <p>Air temperature at the northernmost latitudes is <span class="hlt">predicted</span> to increase steeply and precipitation to become more variable by the end of the 21st century, resulting in altered thermal and hydrological regimes. We applied five <span class="hlt">climate</span> scenarios to <span class="hlt">predict</span> the future (2070-2100) benthic macroinvertebrate assemblages at 239 near-pristine sites across Finland (ca. 1200 km latitudinal span). We used a multitaxon distribution model with air temperature and modeled daily flow as predictors. As expected, projected air temperature increased the most in northernmost Finland. <span class="hlt">Predicted</span> taxonomic richness also increased the most in northern Finland, congruent with the <span class="hlt">predicted</span> northwards shift of many species' distributions. Compositional changes were <span class="hlt">predicted</span> to be high even without changes in richness, suggesting that species replacement may be the main mechanism causing <span class="hlt">climate</span>-induced changes in macroinvertebrate assemblages. Northern streams were <span class="hlt">predicted</span> to lose much of the seasonality of their flow regimes, causing potentially marked changes in stream benthic assemblages. Sites with the highest loss of seasonality were <span class="hlt">predicted</span> to support future assemblages that deviate most in compositional similarity from the present-day assemblages. Macroinvertebrate assemblages were also <span class="hlt">predicted</span> to change more in headwaters than in larger streams, as headwaters were particularly sensitive to changes in flow patterns. Our results emphasize the importance of focusing protection and mitigation on headwater streams with high-flow seasonality because of their vulnerability to <span class="hlt">climate</span> change. © 2018 John Wiley & Sons Ltd.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017E%26ES...58a2054N','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017E%26ES...58a2054N"><span><span class="hlt">Predictive</span> Modeling of Rice Yellow Stem Borer Population Dynamics under <span class="hlt">Climate</span> Change Scenarios in Indramayu</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Nurhayati, E.; Koesmaryono, Y.; Impron</p> <p>2017-03-01</p> <p>Rice Yellow Stem Borer (YSB) is one of the major insect pests in rice plants that has high attack intensity in rice production center areas, especially in West Java. This pest is consider as holometabola insects that causes rice damage in the vegetative phase (deadheart) as well as generative phase (whitehead). <span class="hlt">Climatic</span> factor is one of the environmental factors influence the pattern of dynamics population. The purpose of this study was to develop a <span class="hlt">predictive</span> modeling of YSB pest dynamics population under <span class="hlt">climate</span> change scenarios (2016-2035 period) using Dymex Model in Indramayu area, West Java. YSB modeling required two main components, namely <span class="hlt">climate</span> parameters and YSB development lower threshold of temperature (To) to describe YSB life cycle in every phase. Calibration and validation test of models showed the coefficient of determination (R2) between the <span class="hlt">predicted</span> results and observations of the study area were 0.74 and 0.88 respectively, which was able to illustrate the development, mortality, transfer of individuals from one stage to the next life also fecundity and YSB reproduction. On baseline <span class="hlt">climate</span> condition, there was a tendency of population abundance peak (outbreak) occured when a change of rainfall intensity in the rainy season transition to dry season or the opposite conditions was happen. In both of application of <span class="hlt">climate</span> change scenarios, the model outputs were generated well and able to <span class="hlt">predict</span> the pattern of YSB population dynamics with a the increasing trend of specific population numbers, generation numbers per season and also shifting pattern of populations abundance peak in the future <span class="hlt">climatic</span> conditions. These results can be adopted as a tool to <span class="hlt">predict</span> outbreak and to give early warning to control YSB pest more effectively.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFM.B31G0556F','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFM.B31G0556F"><span>Improving <span class="hlt">predictions</span> of carbon fluxes in the tropics undre <span class="hlt">climatic</span> changes using ED2</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Feng, X.; Uriarte, M.</p> <p>2016-12-01</p> <p>Tropical forests play a critical role in the exchange of carbon between land and atmosphere, highlighting the urgency of understanding the effects of <span class="hlt">climate</span> change on these ecosystems. The most optimistic <span class="hlt">predictions</span> of <span class="hlt">climate</span> models indicate that global mean temperatures will increase by up to 2 0C with some tropical regions experiencing extreme heat. Drought and heat-induced tree mortality will accelerate the release of carbon to the atmosphere creating a positive feedback that greatly exacerbates global warming. Thus, under a warmer and drier <span class="hlt">climate</span>, tropical forests may become net sources, rather than sinks, of carbon. Earth system models have not reached a consensus on the magnitude and direction of <span class="hlt">climate</span> change impacts on tropical forests, calling into question the reliability of their <span class="hlt">predictions</span>. Thus, there is an immediate need to improve the representation of tropical forests in earth system models to make robust <span class="hlt">predictions</span>. The goal of our study is to quantify the responses of tropical forests to <span class="hlt">climate</span> variability and improve the <span class="hlt">predictive</span> capacity of terrestrial ecosystem models. We have collected species-specific physiological and functional trait data from 144 tree species in a Puerto Rican rainforest to parameterize the Ecosystem Demography model (ED2). The large amount of data generated by this research will lead to better validation and lowering the uncertainty in future model <span class="hlt">predictions</span>. To best represent the forest landscape in ED2, all the trees have been assigned to three plant functional types (PFTs): early, mid, and late successional species. Trait data for each PFT were synthesized in a Bayesian meta-analytical model and posterior distributions of traits were used to parameterize the ED2 model. Model <span class="hlt">predictions</span> show that biomass production of late successional PFT (118.89 ton/ha) was consistently higher than mid (71.33 ton/ha) and early (13.21 ton/ha) PFTs. However, mid successional PFT had the highest contributions to NPP for the</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018E%26PSL.481..171W','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018E%26PSL.481..171W"><span>North Atlantic <span class="hlt">climate</span> model bias influence on multiyear <span class="hlt">predictability</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Wu, Y.; Park, T.; Park, W.; Latif, M.</p> <p>2018-01-01</p> <p>The influences of North Atlantic biases on multiyear <span class="hlt">predictability</span> of unforced surface air temperature (SAT) variability are examined in the Kiel <span class="hlt">Climate</span> Model (KCM). By employing a freshwater flux correction over the North Atlantic to the model, which strongly alleviates both North Atlantic sea surface salinity (SSS) and sea surface temperature (SST) biases, the freshwater flux-corrected integration depicts significantly enhanced multiyear SAT <span class="hlt">predictability</span> in the North Atlantic sector in comparison to the uncorrected one. The enhanced SAT <span class="hlt">predictability</span> in the corrected integration is due to a stronger and more variable Atlantic Meridional Overturning Circulation (AMOC) and its enhanced influence on North Atlantic SST. Results obtained from preindustrial control integrations of models participating in the Coupled Model Intercomparison Project Phase 5 (CMIP5) support the findings obtained from the KCM: models with large North Atlantic biases tend to have a weak AMOC influence on SAT and exhibit a smaller SAT <span class="hlt">predictability</span> over the North Atlantic sector.</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_9");'>9</a></li> <li><a href="#" onclick='return showDiv("page_10");'>10</a></li> <li class="active"><span>11</span></li> <li><a href="#" onclick='return showDiv("page_12");'>12</a></li> <li><a href="#" onclick='return showDiv("page_13");'>13</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_11 --> <div id="page_12" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_10");'>10</a></li> <li><a href="#" onclick='return showDiv("page_11");'>11</a></li> <li class="active"><span>12</span></li> <li><a href="#" onclick='return showDiv("page_13");'>13</a></li> <li><a href="#" onclick='return showDiv("page_14");'>14</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="221"> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFM.A52E..04L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFM.A52E..04L"><span>Improved Decadal <span class="hlt">Climate</span> <span class="hlt">Prediction</span> in the North Atlantic using EnOI-Assimilated Initial Condition</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Li, Q.; Xin, X.; Wei, M.; Zhou, W.</p> <p>2017-12-01</p> <p>Decadal <span class="hlt">prediction</span> experiments of Beijing <span class="hlt">Climate</span> Center <span class="hlt">climate</span> system model version 1.1(BCC-CSM1.1) participated in Coupled Model Intercomparison Project Phase 5 (CMIP5) had poor skill in extratropics of the North Atlantic, the initialization of which was done by relaxing modeled ocean temperature to the Simple Ocean Data Assimilation (SODA) reanalysis data. This study aims to improve the <span class="hlt">prediction</span> skill of this model by using the assimilation technique in the initialization. New ocean data are firstly generated by assimilating the sea surface temperature (SST) of the Hadley Centre Sea Ice and Sea Surface Temperature (HadISST) dataset to the ocean model of BCC-CSM1.1 via Ensemble Optimum Interpolation (EnOI). Then a suite of decadal re-forecasts launched annually over the period 1961-2005 is carried out with simulated ocean temperature restored to the assimilated ocean data. Comparisons between the re-forecasts and previous CMIP5 forecasts show that the re-forecasts are more skillful in mid-to-high latitude SST of the North Atlantic. Improved <span class="hlt">prediction</span> skill is also found for the Atlantic multi-decadal Oscillation (AMO), which is consistent with the better skill of Atlantic meridional overturning circulation (AMOC) <span class="hlt">predicted</span> by the re-forecasts. We conclude that the EnOI assimilation generates better ocean data than the SODA reanalysis for initializing decadal <span class="hlt">climate</span> <span class="hlt">prediction</span> of BCC-CSM1.1 model.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2004JCli...17.2667M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2004JCli...17.2667M"><span><span class="hlt">Climate</span> <span class="hlt">Prediction</span> for Brazil's Nordeste: Performance of Empirical and Numerical Modeling Methods.</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Moura, Antonio Divino; Hastenrath, Stefan</p> <p>2004-07-01</p> <p>Comparisons of performance of <span class="hlt">climate</span> forecast methods require consistency in the predictand and a long common reference period. For Brazil's Nordeste, empirical methods developed at the University of Wisconsin use preseason (October January) rainfall and January indices of the fields of meridional wind component and sea surface temperature (SST) in the tropical Atlantic and the equatorial Pacific as input to stepwise multiple regression and neural networking. These are used to <span class="hlt">predict</span> the March June rainfall at a network of 27 stations. An experiment at the International Research Institute for <span class="hlt">Climate</span> <span class="hlt">Prediction</span>, Columbia University, with a numerical model (ECHAM4.5) used global SST information through February to <span class="hlt">predict</span> the March June rainfall at three grid points in the Nordeste. The predictands for the empirical and numerical model forecasts are correlated at +0.96, and the period common to the independent portion of record of the empirical <span class="hlt">prediction</span> and the numerical modeling is 1968 99. Over this period, <span class="hlt">predicted</span> versus observed rainfall are evaluated in terms of correlation, root-mean-square error, absolute error, and bias. Performance is high for both approaches. Numerical modeling produces a correlation of +0.68, moderate errors, and strong negative bias. For the empirical methods, errors and bias are small, and correlations of +0.73 and +0.82 are reached between <span class="hlt">predicted</span> and observed rainfall.<HR ALIGN="center" WIDTH="30%"></p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012AGUFMGC43E1072B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012AGUFMGC43E1072B"><span><span class="hlt">Prediction</span>-Market-Based Quantification of <span class="hlt">Climate</span> Change Consensus and Uncertainty</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Boslough, M.</p> <p>2012-12-01</p> <p>Intrade is an online trading exchange that includes <span class="hlt">climate</span> <span class="hlt">prediction</span> markets. One such family of contracts can be described as "Global temperature anomaly for 2012 to be greater than x °C or more," where the figure x ranges in increments of .05 from .30 to 1.10 (relative to the 1951-1980 base period), based on data published by NASA GISS. Each market will settle at 10.00 if the published global temperature anomaly for 2012 is equal to or greater than x, and will otherwise settle at 0.00. Similar contracts will be available for 2013. Global warming hypotheses can be cast as probabilistic <span class="hlt">predictions</span> for future temperatures. The first modern such <span class="hlt">climate</span> <span class="hlt">prediction</span> is that of Broecker (1975), whose temperatures are easily separable from his CO2 growth scenario—which he overestimated—by interpolating his table of temperature as a function of CO2 concentration and projecting the current trend into the near future. For the current concentration of 395 ppm, Broecker's equilibrium temperature anomaly <span class="hlt">prediction</span> relative to pre-industrial is 1.05 °C, or about 0.75 °C relative to the GISS base period. His neglect of lag in response to the changes in radiative forcing was partially compensated by his low sensitivity of 2.4 °C, leading to a slight overestimate. Simple linear extrapolation of the current trend since 1975 yields an estimate of .65 ± .09 °C (net warming of .95 °C) for anthropogenic global warming with a normal distribution of random natural variability. To evaluate an extreme case, we can estimate the <span class="hlt">prediction</span> Broecker would have made if he had used the Lindzen & Choi (2009) <span class="hlt">climate</span> sensitivity of 0.5 °C. The net post-industrial warming by 2012 would have been 0.21 °C, for an expected change of -0.09 from the GISS base period. This is the temperature to which the Earth would be expected to revert if the observed warming since the 19th century was merely due to random natural variability that coincidentally mimicked Broecker's anthropogenic</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://files.eric.ed.gov/fulltext/ED441907.pdf','ERIC'); return false;" href="http://files.eric.ed.gov/fulltext/ED441907.pdf"><span>Falling Off Track: How Teacher-Student Relationships <span class="hlt">Predict</span> Early High School Failure Rates.</span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Miller, Shazia Rafiullah</p> <p></p> <p>This paper examines the relationship between the <span class="hlt">climate</span> of teacher-student relations within a school and individual student's likelihood of freshman year success. Using <span class="hlt">administrative</span> data from the Chicago Public Schools and survey data, researchers used hierarchical linear modeling to determine whether teacher-student <span class="hlt">climate</span> <span class="hlt">predicts</span> students'…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/27516864','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/27516864"><span><span class="hlt">Predicting</span> the distributions of predator (snow leopard) and prey (blue sheep) under <span class="hlt">climate</span> change in the Himalaya.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Aryal, Achyut; Shrestha, Uttam Babu; Ji, Weihong; Ale, Som B; Shrestha, Sujata; Ingty, Tenzing; Maraseni, Tek; Cockfield, Geoff; Raubenheimer, David</p> <p>2016-06-01</p> <p>Future <span class="hlt">climate</span> change is likely to affect distributions of species, disrupt biotic interactions, and cause spatial incongruity of predator-prey habitats. Understanding the impacts of future <span class="hlt">climate</span> change on species distribution will help in the formulation of conservation policies to reduce the risks of future biodiversity losses. Using a species distribution modeling approach by MaxEnt, we modeled current and future distributions of snow leopard (Panthera uncia) and its common prey, blue sheep (Pseudois nayaur), and observed the changes in niche overlap in the Nepal Himalaya. Annual mean temperature is the major <span class="hlt">climatic</span> factor responsible for the snow leopard and blue sheep distributions in the energy-deficient environments of high altitudes. Currently, about 15.32% and 15.93% area of the Nepal Himalaya are suitable for snow leopard and blue sheep habitats, respectively. The bioclimatic models show that the current suitable habitats of both snow leopard and blue sheep will be reduced under future <span class="hlt">climate</span> change. The <span class="hlt">predicted</span> suitable habitat of the snow leopard is decreased when blue sheep habitats is incorporated in the model. Our <span class="hlt">climate</span>-only model shows that only 11.64% (17,190 km(2)) area of Nepal is suitable for the snow leopard under current <span class="hlt">climate</span> and the suitable habitat reduces to 5,435 km(2) (reduced by 24.02%) after incorporating the <span class="hlt">predicted</span> distribution of blue sheep. The <span class="hlt">predicted</span> distribution of snow leopard reduces by 14.57% in 2030 and by 21.57% in 2050 when the <span class="hlt">predicted</span> distribution of blue sheep is included as compared to 1.98% reduction in 2030 and 3.80% reduction in 2050 based on the <span class="hlt">climate</span>-only model. It is <span class="hlt">predicted</span> that future <span class="hlt">climate</span> may alter the predator-prey spatial interaction inducing a lower degree of overlap and a higher degree of mismatch between snow leopard and blue sheep niches. This suggests increased energetic costs of finding preferred prey for snow leopards - a species already facing energetic constraints due to the</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/servlets/purl/1330744','SCIGOV-STC'); return false;" href="https://www.osti.gov/servlets/purl/1330744"><span>Collaborative Proposal: Improving Decadal <span class="hlt">Prediction</span> of Arctic <span class="hlt">Climate</span> Variability and Change Using a Regional Arctic System Model (RASM)</span></a></p> <p><a target="_blank" href="http://www.osti.gov/search">DOE Office of Scientific and Technical Information (OSTI.GOV)</a></p> <p>Maslowski, Wieslaw</p> <p></p> <p>This project aims to develop, apply and evaluate a regional Arctic System model (RASM) for enhanced decadal <span class="hlt">predictions</span>. Its overarching goal is to advance understanding of the past and present states of arctic <span class="hlt">climate</span> and to facilitate improvements in seasonal to decadal <span class="hlt">predictions</span>. In particular, it will focus on variability and long-term change of energy and freshwater flows through the arctic <span class="hlt">climate</span> system. The project will also address modes of natural <span class="hlt">climate</span> variability as well as extreme and rapid <span class="hlt">climate</span> change in a region of the Earth that is: (i) a key indicator of the state of global <span class="hlt">climate</span> throughmore » polar amplification and (ii) which is undergoing environmental transitions not seen in instrumental records. RASM will readily allow the addition of other earth system components, such as ecosystem or biochemistry models, thus allowing it to facilitate studies of <span class="hlt">climate</span> impacts (e.g., droughts and fires) and of ecosystem adaptations to these impacts. As such, RASM is expected to become a foundation for more complete Arctic System models and part of a model hierarchy important for improving <span class="hlt">climate</span> modeling and <span class="hlt">predictions</span>.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017EGUGA..19.7130S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017EGUGA..19.7130S"><span>Visualization of uncertainties and forecast skill in user-tailored seasonal <span class="hlt">climate</span> <span class="hlt">predictions</span> for agriculture</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Sedlmeier, Katrin; Gubler, Stefanie; Spierig, Christoph; Flubacher, Moritz; Maurer, Felix; Quevedo, Karim; Escajadillo, Yury; Avalos, Griña; Liniger, Mark A.; Schwierz, Cornelia</p> <p>2017-04-01</p> <p>Seasonal <span class="hlt">climate</span> forecast products potentially have a high value for users of different sectors. During the first phase (2012-2015) of the project CLIMANDES (a pilot project of the Global Framework for <span class="hlt">Climate</span> Services led by WMO [http://www.wmo.int/gfcs/climandes]), a demand study conducted with Peruvian farmers indicated a large interest in seasonal <span class="hlt">climate</span> information for agriculture. The study further showed that the required information should by precise, timely, and understandable. In addition to the actual forecast, two complex measures are essential to understand seasonal <span class="hlt">climate</span> <span class="hlt">predictions</span> and their limitations correctly: forecast uncertainty and forecast skill. The former can be sampled by using an ensemble of <span class="hlt">climate</span> simulations, the latter derived by comparing forecasts of past time periods to observations. Including uncertainty and skill information in an understandable way for end-users (who are often not technically educated) poses a great challenge. However, neglecting this information would lead to a false sense of determinism which could prove fatal to the credibility of <span class="hlt">climate</span> information. Within the second phase (2016-2018) of the project CLIMANDES, one goal is to develop a prototype of a user-tailored seasonal forecast for the agricultural sector in Peru. In this local context, the basic education level of the rural farming community presents a major challenge for the communication of seasonal <span class="hlt">climate</span> <span class="hlt">predictions</span>. This contribution proposes different graphical presentations of <span class="hlt">climate</span> forecasts along with possible approaches to visualize and communicate the associated skill and uncertainties, considering end users with varying levels of technical knowledge.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/28325893','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/28325893"><span>A robust empirical seasonal <span class="hlt">prediction</span> of winter NAO and surface <span class="hlt">climate</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Wang, L; Ting, M; Kushner, P J</p> <p>2017-03-21</p> <p>A key determinant of winter weather and <span class="hlt">climate</span> in Europe and North America is the North Atlantic Oscillation (NAO), the dominant mode of atmospheric variability in the Atlantic domain. Skilful seasonal forecasting of the surface <span class="hlt">climate</span> in both Europe and North America is reflected largely in how accurately models can <span class="hlt">predict</span> the NAO. Most dynamical models, however, have limited skill in seasonal forecasts of the winter NAO. A new empirical model is proposed for the seasonal forecast of the winter NAO that exhibits higher skill than current dynamical models. The empirical model provides robust and skilful <span class="hlt">prediction</span> of the December-January-February (DJF) mean NAO index using a multiple linear regression (MLR) technique with autumn conditions of sea-ice concentration, stratospheric circulation, and sea-surface temperature. The <span class="hlt">predictability</span> is, for the most part, derived from the relatively long persistence of sea ice in the autumn. The lower stratospheric circulation and sea-surface temperature appear to play more indirect roles through a series of feedbacks among systems driving NAO evolution. This MLR model also provides skilful seasonal outlooks of winter surface temperature and precipitation over many regions of Eurasia and eastern North America.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.fs.usda.gov/treesearch/pubs/40075','TREESEARCH'); return false;" href="https://www.fs.usda.gov/treesearch/pubs/40075"><span>Approaches to <span class="hlt">predicting</span> potential impacts of <span class="hlt">climate</span> change on forest disease: An example with Armillaria root disease</span></a></p> <p><a target="_blank" href="http://www.fs.usda.gov/treesearch/">Treesearch</a></p> <p>Ned B. Klopfenstein; Mee-Sook Kim; John W. Hanna; Bryce A. Richardson; John E. Lundquist</p> <p>2011-01-01</p> <p><span class="hlt">Climate</span> change will likely have dramatic impacts on forest health because many forest trees could become maladapted to <span class="hlt">climate</span>. Furthermore, <span class="hlt">climate</span> change will have additional impacts on forest health through changes in the distribution and severity of forest disease. Methods are needed to <span class="hlt">predict</span> the influence of <span class="hlt">climate</span> change on forest disease so that appropriate...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.noaanews.noaa.gov/stories2012/20121015_ncwcp.html','SCIGOVWS'); return false;" href="http://www.noaanews.noaa.gov/stories2012/20121015_ncwcp.html"><span>NOAA's world-class weather and <span class="hlt">climate</span> <span class="hlt">prediction</span> center opens at</span></a></p> <p><a target="_blank" href="http://www.science.gov/aboutsearch.html">Science.gov Websites</a></p> <p></p> <p></p> <p>StumbleUpon Digg More Destinations NOAA's <em>world</em>-class weather and <span class="hlt">climate</span> <span class="hlt">prediction</span> center opens at currents and large-scale rain and snow storms. Billions of earth observations from around the <em>world</em> flow operations. Investing in this center is an investment in our human capital, serving as a <em>world</em> class facility</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29374176','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29374176"><span>Decadal <span class="hlt">climate</span> <span class="hlt">predictability</span> in the southern Indian Ocean captured by SINTEX-F using a simple SST-nudging scheme.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Morioka, Yushi; Doi, Takeshi; Behera, Swadhin K</p> <p>2018-01-26</p> <p>Decadal <span class="hlt">climate</span> variability in the southern Indian Ocean has great influences on southern African <span class="hlt">climate</span> through modulation of atmospheric circulation. Although many efforts have been made to understanding physical mechanisms, <span class="hlt">predictability</span> of the decadal <span class="hlt">climate</span> variability, in particular, the internally generated variability independent from external atmospheric forcing, remains poorly understood. This study investigates <span class="hlt">predictability</span> of the decadal <span class="hlt">climate</span> variability in the southern Indian Ocean using a coupled general circulation model, called SINTEX-F. The ensemble members of the decadal reforecast experiments were initialized with a simple sea surface temperature (SST) nudging scheme. The observed positive and negative peaks during late 1990s and late 2000s are well reproduced in the reforecast experiments initiated from 1994 and 1999, respectively. The experiments initiated from 1994 successfully capture warm SST and high sea level pressure anomalies propagating from the South Atlantic to the southern Indian Ocean. Also, the other experiments initiated from 1999 skillfully <span class="hlt">predict</span> phase change from a positive to negative peak. These results suggest that the SST-nudging initialization has the essence to capture the <span class="hlt">predictability</span> of the internally generated decadal <span class="hlt">climate</span> variability in the southern Indian Ocean.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012HESS...16.2531R','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012HESS...16.2531R"><span>Applying simple water-energy balance frameworks to <span class="hlt">predict</span> the <span class="hlt">climate</span> sensitivity of streamflow over the continental United States</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Renner, M.; Bernhofer, C.</p> <p>2012-08-01</p> <p>The <span class="hlt">prediction</span> of <span class="hlt">climate</span> effects on terrestrial ecosystems and water resources is one of the major research questions in hydrology. Conceptual water-energy balance models can be used to gain a first order estimate of how long-term average streamflow is changing with a change in water and energy supply. A common framework for investigation of this question is based on the Budyko hypothesis, which links hydrological response to aridity. Recently, Renner et al. (2012) introduced the <span class="hlt">climate</span> change impact hypothesis (CCUW), which is based on the assumption that the total efficiency of the catchment ecosystem to use the available water and energy for actual evapotranspiration remains constant even under <span class="hlt">climate</span> changes. Here, we confront the <span class="hlt">climate</span> sensitivity approaches (the Budyko approach of Roderick and Farquhar, 2011, and the CCUW) with data of more than 400 basins distributed over the continental United States. We first estimate the sensitivity of streamflow to changes in precipitation using long-term average data of the period 1949 to 2003. This provides a hydro-<span class="hlt">climatic</span> status of the respective basins as well as their expected proportional effect to changes in <span class="hlt">climate</span>. Next, we test the ability of both approaches to <span class="hlt">predict</span> <span class="hlt">climate</span> impacts on streamflow by splitting the data into two periods. We (i) analyse the long-term average changes in hydro-climatology and (ii) derive a statistical classification of potential <span class="hlt">climate</span> and basin change impacts based on the significance of observed changes in runoff, precipitation and potential evapotranspiration. Then we (iii) use the different <span class="hlt">climate</span> sensitivity methods to <span class="hlt">predict</span> the change in streamflow given the observed changes in water and energy supply and (iv) evaluate the <span class="hlt">predictions</span> by (v) using the statistical classification scheme and (vi) a conceptual approach to separate the impacts of changes in <span class="hlt">climate</span> from basin characteristics change on streamflow. This allows us to evaluate the observed changes in</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4724863','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4724863"><span>A Severe Sepsis Mortality <span class="hlt">Prediction</span> Model and Score for Use with <span class="hlt">Administrative</span> Data</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Ford, Dee W.; Goodwin, Andrew J.; Simpson, Annie N.; Johnson, Emily; Nadig, Nandita; Simpson, Kit N.</p> <p>2016-01-01</p> <p>Objective <span class="hlt">Administrative</span> data is used for research, quality improvement, and health policy in severe sepsis. However, there is not a sepsis-specific tool applicable to <span class="hlt">administrative</span> data with which to adjust for illness severity. Our objective was to develop, internally validate, and externally validate a severe sepsis mortality <span class="hlt">prediction</span> model and associated mortality <span class="hlt">prediction</span> score. Design Retrospective cohort study using 2012 <span class="hlt">administrative</span> data from five US states. Three cohorts of patients with severe sepsis were created: 1) ICD-9-CM codes for severe sepsis/septic shock, 2) ‘Martin’ approach, and 3) ‘Angus’ approach. The model was developed and internally validated in ICD-9-CM cohort and externally validated in other cohorts. Integer point values for each predictor variable were generated to create a sepsis severity score. Setting Acute care, non-federal hospitals in NY, MD, FL, MI, and WA Subjects Patients in one of three severe sepsis cohorts: 1) explicitly coded (n=108,448), 2) Martin cohort (n=139,094), and 3) Angus cohort (n=523,637) Interventions None Measurements and Main Results Maximum likelihood estimation logistic regression to develop a <span class="hlt">predictive</span> model for in-hospital mortality. Model calibration and discrimination assessed via Hosmer-Lemeshow goodness-of-fit (GOF) and C-statistics respectively. Primary cohort subset into risk deciles and observed versus <span class="hlt">predicted</span> mortality plotted. GOF demonstrated p>0.05 for each cohort demonstrating sound calibration. C-statistic ranged from low of 0.709 (sepsis severity score) to high of 0.838 (Angus cohort) suggesting good to excellent model discrimination. Comparison of observed versus expected mortality was robust although accuracy decreased in highest risk decile. Conclusions Our sepsis severity model and score is a tool that provides reliable risk adjustment for <span class="hlt">administrative</span> data. PMID:26496452</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017GeoRL..4412208L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017GeoRL..4412208L"><span>Mitigating the Impacts of <span class="hlt">Climate</span> Nonstationarity on Seasonal Streamflow <span class="hlt">Predictability</span> in the U.S. Southwest</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Lehner, Flavio; Wood, Andrew W.; Llewellyn, Dagmar; Blatchford, Douglas B.; Goodbody, Angus G.; Pappenberger, Florian</p> <p>2017-12-01</p> <p>Seasonal streamflow <span class="hlt">predictions</span> provide a critical management tool for water managers in the American Southwest. In recent decades, persistent <span class="hlt">prediction</span> errors for spring and summer runoff volumes have been observed in a number of watersheds in the American Southwest. While mostly driven by decadal precipitation trends, these errors also relate to the influence of increasing temperature on streamflow in these basins. Here we show that incorporating seasonal temperature forecasts from operational global <span class="hlt">climate</span> <span class="hlt">prediction</span> models into streamflow forecasting models adds <span class="hlt">prediction</span> skill for watersheds in the headwaters of the Colorado and Rio Grande River basins. Current dynamical seasonal temperature forecasts now show sufficient skill to reduce streamflow forecast errors in snowmelt-driven regions. Such <span class="hlt">predictions</span> can increase the resilience of streamflow forecasting and water management systems in the face of continuing warming as well as decadal-scale temperature variability and thus help to mitigate the impacts of <span class="hlt">climate</span> nonstationarity on streamflow <span class="hlt">predictability</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFM.U21B..01B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFM.U21B..01B"><span>Importance of Anthropogenic Aerosols for <span class="hlt">Climate</span> <span class="hlt">Prediction</span>: a Study on East Asian Sulfate Aerosols</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Bartlett, R. E.; Bollasina, M. A.</p> <p>2017-12-01</p> <p><span class="hlt">Climate</span> <span class="hlt">prediction</span> is vital to ensure that we are able to adapt to our changing <span class="hlt">climate</span>. Understandably, the main focus for such <span class="hlt">prediction</span> is greenhouse gas forcing, as this will be the main anthropogenic driver of long-term global <span class="hlt">climate</span> change; however, other forcings could still be important. Atmospheric aerosols represent one such forcing, especially in regions with high present-day aerosol loading such as Asia; yet, uncertainty in their future emissions are under-sampled by commonly used <span class="hlt">climate</span> forcing projections, such as the Representative Concentration Pathways (RCPs). Globally, anthropogenic aerosols exert a net cooling, but their effects show large variation at regional scales. Studies have shown that aerosols impact locally upon temperature, precipitation and hydroclimate, and also upon larger scale atmospheric circulation (for example, the Asian monsoon) with implications for <span class="hlt">climate</span> remote from aerosol sources. We investigate how future <span class="hlt">climate</span> could evolve differently given the same greenhouse gas forcing pathway but differing aerosol emissions. Specifically, we use <span class="hlt">climate</span> modelling experiments (using HadGEM2-ES) of two scenarios based upon RCP2.6 greenhouse gas forcing but with large differences in sulfur dioxide emissions over East Asia. Results show that increased sulfate aerosols (associated with increased sulfur dioxide) lead to large regional cooling through aerosol-radiation and aerosol-cloud interactions. Focussing on dynamical mechanisms, we explore the consequences of this cooling for the Asian summer and winter monsoons. In addition to local temperature and precipitation changes, we find significant changes to large scale atmospheric circulation. Wave-like responses to upper-level atmospheric changes propagate across the northern hemisphere with far-reaching effects on surface <span class="hlt">climate</span>, for example, cooling over Europe. Within the tropics, we find alterations to zonal circulation (notably, shifts in the Pacific Walker cell) and monsoon</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20140011845','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20140011845"><span>Reducing Uncertainty in Chemistry <span class="hlt">Climate</span> Model <span class="hlt">Predictions</span> of Stratospheric Ozone</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Douglass, A. R.; Strahan, S. E.; Oman, L. D.; Stolarski, R. S.</p> <p>2014-01-01</p> <p>Chemistry <span class="hlt">climate</span> models (CCMs) are used to <span class="hlt">predict</span> the future evolution of stratospheric ozone as ozone-depleting substances decrease and greenhouse gases increase, cooling the stratosphere. CCM <span class="hlt">predictions</span> exhibit many common features, but also a broad range of values for quantities such as year of ozone-return-to-1980 and global ozone level at the end of the 21st century. Multiple linear regression is applied to each of 14 CCMs to separate ozone response to chlorine change from that due to <span class="hlt">climate</span> change. We show that the sensitivity of lower atmosphere ozone to chlorine change deltaO3/deltaCly is a near linear function of partitioning of total inorganic chlorine (Cly) into its reservoirs; both Cly and its partitioning are controlled by lower atmospheric transport. CCMs with realistic transport agree with observations for chlorine reservoirs and produce similar ozone responses to chlorine change. After 2035 differences in response to chlorine contribute little to the spread in CCM results as the anthropogenic contribution to Cly becomes unimportant. Differences among upper stratospheric ozone increases due to temperature decreases are explained by differences in ozone sensitivity to temperature change deltaO3/deltaT due to different contributions from various ozone loss processes, each with their own temperature dependence. In the lower atmosphere, tropical ozone decreases caused by a <span class="hlt">predicted</span> speed-up in the Brewer-Dobson circulation may or may not be balanced by middle and high latitude increases, contributing most to the spread in late 21st century <span class="hlt">predictions</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFMGC13D0804C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFMGC13D0804C"><span>Ensembles-based <span class="hlt">predictions</span> of <span class="hlt">climate</span> change impacts on bioclimatic zones in Northeast Asia</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Choi, Y.; Jeon, S. W.; Lim, C. H.; Ryu, J.</p> <p>2017-12-01</p> <p>Biodiversity is rapidly declining globally and efforts are needed to mitigate this continually increasing loss of species. Clustering of areas with similar habitats can be used to prioritize protected areas and distribute resources for the conservation of species, selection of representative sample areas for research, and evaluation of impacts due to environmental changes. In this study, Northeast Asia (NEA) was classified into 14 bioclimatic zones using statistical techniques, which are correlation analysis and principal component analysis (PCA), and the iterative self-organizing data analysis technique algorithm (ISODATA). Based on these bioclimatic classification, we <span class="hlt">predicted</span> shift of bioclimatic zones due to <span class="hlt">climate</span> change. The input variables include the current <span class="hlt">climatic</span> data (1960-1990) and the future <span class="hlt">climatic</span> data of the HadGEM2-AO model (RCP 4.5(2050, 2070) and 8.5(2050, 2070)) provided by WorldClim. Using these data, multi-modeling methods including maximum likelihood classification, random forest, and species distribution modelling have been used to project the impact of <span class="hlt">climate</span> change on the spatial distribution of bioclimatic zones within NEA. The results of various models were compared and analyzed by overlapping each result. As the result, significant changes in bioclimatic conditions can be expected throughout the NEA by 2050s and 2070s. The overall zones moved upward and some zones were <span class="hlt">predicted</span> to disappear. This analysis provides the basis for understanding potential impacts of <span class="hlt">climate</span> change on biodiversity and ecosystem. Also, this could be used more effectively to support decision making on <span class="hlt">climate</span> change adaptation.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFM.H13G1480L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFM.H13G1480L"><span><span class="hlt">Predicting</span> Nitrate Transport under Future <span class="hlt">Climate</span> Scenarios beneath the Nebraska Management Systems Evaluation Area (MSEA) site</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Li, Y.; Akbariyeh, S.; Gomez Peña, C. A.; Bartlet-Hunt, S.</p> <p>2017-12-01</p> <p>Understanding the impacts of future <span class="hlt">climate</span> change on soil hydrological processes and solute transport is crucial to develop appropriate strategies to minimize adverse impacts of agricultural activities on groundwater quality. The goal of this work is to evaluate the direct effects of <span class="hlt">climate</span> change on the fate and transport of nitrate beneath a center-pivot irrigated corn field in Nebraska Management Systems Evaluation Area (MSEA) site. Future groundwater recharge rate and actual evapotranspiration rate were <span class="hlt">predicted</span> based on an inverse modeling approach using <span class="hlt">climate</span> data generated by Weather Research and Forecasting (WRF) model under the RCP 8.5 scenario, which was downscaled from global CCSM4 model to a resolution of 24 by 24 km2. A groundwater flow model was first calibrated based on historical groundwater table measurement and was then applied to <span class="hlt">predict</span> future groundwater table in the period 2057-2060. Finally, <span class="hlt">predicted</span> future groundwater recharge rate, actual evapotranspiration rate, and groundwater level, together with future precipitation data from WRF, were used in a three-dimensional (3D) model, which was validated based on rich historic data set collected from 1993-1996, to <span class="hlt">predict</span> nitrate concentration in soil and groundwater from the year 2057 to 2060. Future groundwater recharge was found to be decreasing in the study area compared to average groundwater recharge data from the literature. Correspondingly, groundwater elevation was <span class="hlt">predicted</span> to decrease (1 to 2 ft) over the five years of simulation. <span class="hlt">Predicted</span> higher transpiration data from <span class="hlt">climate</span> model resulted in lower infiltration of nitrate concentration in subsurface within the root zone.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFM.H13G1480L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFM.H13G1480L"><span><span class="hlt">Predicting</span> Nitrate Transport under Future <span class="hlt">Climate</span> Scenarios beneath the Nebraska Management Systems Evaluation Area (MSEA) site</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Li, Y.; Akbariyeh, S.; Gomez Peña, C. A.; Bartlet-Hunt, S.</p> <p>2016-12-01</p> <p>Understanding the impacts of future <span class="hlt">climate</span> change on soil hydrological processes and solute transport is crucial to develop appropriate strategies to minimize adverse impacts of agricultural activities on groundwater quality. The goal of this work is to evaluate the direct effects of <span class="hlt">climate</span> change on the fate and transport of nitrate beneath a center-pivot irrigated corn field in Nebraska Management Systems Evaluation Area (MSEA) site. Future groundwater recharge rate and actual evapotranspiration rate were <span class="hlt">predicted</span> based on an inverse modeling approach using <span class="hlt">climate</span> data generated by Weather Research and Forecasting (WRF) model under the RCP 8.5 scenario, which was downscaled from global CCSM4 model to a resolution of 24 by 24 km2. A groundwater flow model was first calibrated based on historical groundwater table measurement and was then applied to <span class="hlt">predict</span> future groundwater table in the period 2057-2060. Finally, <span class="hlt">predicted</span> future groundwater recharge rate, actual evapotranspiration rate, and groundwater level, together with future precipitation data from WRF, were used in a three-dimensional (3D) model, which was validated based on rich historic data set collected from 1993-1996, to <span class="hlt">predict</span> nitrate concentration in soil and groundwater from the year 2057 to 2060. Future groundwater recharge was found to be decreasing in the study area compared to average groundwater recharge data from the literature. Correspondingly, groundwater elevation was <span class="hlt">predicted</span> to decrease (1 to 2 ft) over the five years of simulation. <span class="hlt">Predicted</span> higher transpiration data from <span class="hlt">climate</span> model resulted in lower infiltration of nitrate concentration in subsurface within the root zone.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/2254526','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/2254526"><span>Nurse practitioners: leadership behaviors and organizational <span class="hlt">climate</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Jones, L C; Guberski, T D; Soeken, K L</p> <p>1990-01-01</p> <p>The purpose of this article is to examine the relationships of individual nurse practitioners' perceptions of the leadership <span class="hlt">climate</span> in their organizations and self-reported formal and informal leadership behaviors. The nine <span class="hlt">climate</span> dimensions (Structure, Responsibility, Reward, Perceived Support of Risk Taking, Warmth, Support, Standard Setting, Conflict, and Identity) identified by Litwin and Stringer in 1968 were used to <span class="hlt">predict</span> five leadership dimensions (Meeting Organizational Needs, Managing Resources, Leadership Competence, Task Accomplishment, and Communications). Demographic variables of age, educational level, and percent of time spent performing <span class="hlt">administrative</span> functions were forced as a first step in each multiple regression analysis and used to explain a significant amount of variance in all but one analysis. All leadership dimensions were <span class="hlt">predicted</span> by at least one organizational <span class="hlt">climate</span> dimension: (1) Meeting Organizational Needs by Risk and Reward; (2) Managing Resources by Risk and Structure; (3) Leadership Competence by Risk and Standards; (4) Task Accomplishment by Structure, Risk, and Standards; and (5) Communication by Rewards.</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_10");'>10</a></li> <li><a href="#" onclick='return showDiv("page_11");'>11</a></li> <li class="active"><span>12</span></li> <li><a href="#" onclick='return showDiv("page_13");'>13</a></li> <li><a href="#" onclick='return showDiv("page_14");'>14</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_12 --> <div id="page_13" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_11");'>11</a></li> <li><a href="#" onclick='return showDiv("page_12");'>12</a></li> <li class="active"><span>13</span></li> <li><a href="#" onclick='return showDiv("page_14");'>14</a></li> <li><a href="#" onclick='return showDiv("page_15");'>15</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="241"> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3631642','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3631642"><span><span class="hlt">Predicting</span> <span class="hlt">climate</span> effects on Pacific sardine</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Deyle, Ethan R.; Fogarty, Michael; Hsieh, Chih-hao; Kaufman, Les; MacCall, Alec D.; Munch, Stephan B.; Perretti, Charles T.; Ye, Hao; Sugihara, George</p> <p>2013-01-01</p> <p>For many marine species and habitats, <span class="hlt">climate</span> change and overfishing present a double threat. To manage marine resources effectively, it is necessary to adapt management to changes in the physical environment. Simple relationships between environmental conditions and fish abundance have long been used in both fisheries and fishery management. In many cases, however, physical, biological, and human variables feed back on each other. For these systems, associations between variables can change as the system evolves in time. This can obscure relationships between population dynamics and environmental variability, undermining our ability to forecast changes in populations tied to physical processes. Here we present a methodology for identifying physical forcing variables based on nonlinear forecasting and show how the method provides a <span class="hlt">predictive</span> understanding of the influence of physical forcing on Pacific sardine. PMID:23536299</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=20160000368&hterms=analysis+climatic&qs=N%3D0%26Ntk%3DAll%26Ntx%3Dmode%2Bmatchall%26Ntt%3Danalysis%2Bclimatic','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=20160000368&hterms=analysis+climatic&qs=N%3D0%26Ntk%3DAll%26Ntx%3Dmode%2Bmatchall%26Ntt%3Danalysis%2Bclimatic"><span>Uncertainties in <span class="hlt">Predicting</span> Rice Yield by Current Crop Models Under a Wide Range of <span class="hlt">Climatic</span> Conditions</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Li, Tao; Hasegawa, Toshihiro; Yin, Xinyou; Zhu, Yan; Boote, Kenneth; Adam, Myriam; Bregaglio, Simone; Buis, Samuel; Confalonieri, Roberto; Fumoto, Tamon; <a style="text-decoration: none; " href="javascript:void(0); " onClick="displayelement('author_20160000368'); toggleEditAbsImage('author_20160000368_show'); toggleEditAbsImage('author_20160000368_hide'); "> <img style="display:inline; width:12px; height:12px; " src="images/arrow-up.gif" width="12" height="12" border="0" alt="hide" id="author_20160000368_show"> <img style="width:12px; height:12px; display:none; " src="images/arrow-down.gif" width="12" height="12" border="0" alt="hide" id="author_20160000368_hide"></p> <p>2014-01-01</p> <p><span class="hlt">Predicting</span> rice (Oryza sativa) productivity under future <span class="hlt">climates</span> is important for global food security. Ecophysiological crop models in combination with <span class="hlt">climate</span> model outputs are commonly used in yield <span class="hlt">prediction</span>, but uncertainties associated with crop models remain largely unquantified. We evaluated 13 rice models against multi-year experimental yield data at four sites with diverse <span class="hlt">climatic</span> conditions in Asia and examined whether different modeling approaches on major physiological processes attribute to the uncertainties of <span class="hlt">prediction</span> to field measured yields and to the uncertainties of sensitivity to changes in temperature and CO2 concentration [CO2]. We also examined whether a use of an ensemble of crop models can reduce the uncertainties. Individual models did not consistently reproduce both experimental and regional yields well, and uncertainty was larger at the warmest and coolest sites. The variation in yield projections was larger among crop models than variation resulting from 16 global <span class="hlt">climate</span> model-based scenarios. However, the mean of <span class="hlt">predictions</span> of all crop models reproduced experimental data, with an uncertainty of less than 10 percent of measured yields. Using an ensemble of eight models calibrated only for phenology or five models calibrated in detail resulted in the uncertainty equivalent to that of the measured yield in well-controlled agronomic field experiments. Sensitivity analysis indicates the necessity to improve the accuracy in <span class="hlt">predicting</span> both biomass and harvest index in response to increasing [CO2] and temperature.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012EGUGA..1413219L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012EGUGA..1413219L"><span>Do GCM's <span class="hlt">predict</span> the <span class="hlt">climate</span>.... Or the low frequency weather?</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Lovejoy, S.; Schertzer, D.; Varon, D.</p> <p>2012-04-01</p> <p> control runs (i.e. without <span class="hlt">climate</span> forcing) of GCM based <span class="hlt">climate</span> forecasting systems including those of the Institut Pierre Simon Laplace (Paris) and the Earth Forecasting System (Hamburg). In order for these systems to go beyond simply <span class="hlt">predicting</span> low frequency weather i.e. in order for them to <span class="hlt">predict</span> the <span class="hlt">climate</span>, they need appropriate <span class="hlt">climate</span> forcings and/ or new internal mechanisms of variability. Using statistical scaling techniques we examine the scale dependence of fluctuations from forced and unforced GCM outputs, including from the ECHO-G and EFS simulations in the Millenium <span class="hlt">climate</span> reconstruction project and compare this with data, multiproxies and paleo data. Our general conclusion is that the models systematically underestimate the multidecadal, multicentennial scale variability.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/28952248','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/28952248"><span>[<span class="hlt">Predictions</span> of potential geographical distribution of Alhagi sparsifolia under <span class="hlt">climate</span> change].</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Yang, Xia; Zheng, Jiang-Hua; Mu, Chen; Lin, Jun</p> <p>2017-02-01</p> <p>Specific information on geographic distribution of a species is important for its conservation. This study was conducted to determine the potential geographic distribution of Alhagi sparsifolia, which is a plant used in traditional Uighur medicine, and <span class="hlt">predict</span> how <span class="hlt">climate</span> change would affect its geographic range. The potential geographic distribution of A. sparsifolia under the current conditions in China was simulated with MaxEnt software based on species presence data at 42 locations and 19 <span class="hlt">climatic</span> variables. The future distributions of A. sparsifolia were also projected in 2050 and 2070 under the <span class="hlt">climate</span> change scenarios of RCP2.6 and RCP8.5 described in 5th Assessment Report of the Intergovernmental Panel on <span class="hlt">Climate</span> Change (IPCC).The result showed that mean temperature of the coldest quarter, annual mean temperature, precipitation of the coldest quarter, annual precipitation, precipitation of the wettest month, mean temperature of the wettest quarter and the temperature annual range were the seven <span class="hlt">climatic</span> factors influencing the geographic distribution of A. sparsifolia under current <span class="hlt">climate</span>, the suitable habitats are mainly located in the Xinjiang, in the middle and north of Gansu, in the west of Neimeng, in the north of Nei Monggol. From 2050 to 2070, the model simulations indicated that the suitable habitats of A. sparsifolia would decrease under the <span class="hlt">climate</span> change scenarios of RCP2.6 and scenarios of RCP8.5 on the whole. Copyright© by the Chinese Pharmaceutical Association.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/27500587','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/27500587"><span>Mechanistic variables can enhance <span class="hlt">predictive</span> models of endotherm distributions: the American pika under current, past, and future <span class="hlt">climates</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Mathewson, Paul D; Moyer-Horner, Lucas; Beever, Erik A; Briscoe, Natalie J; Kearney, Michael; Yahn, Jeremiah M; Porter, Warren P</p> <p>2017-03-01</p> <p>How <span class="hlt">climate</span> constrains species' distributions through time and space is an important question in the context of conservation planning for <span class="hlt">climate</span> change. Despite increasing awareness of the need to incorporate mechanism into species distribution models (SDMs), mechanistic modeling of endotherm distributions remains limited in this literature. Using the American pika (Ochotona princeps) as an example, we present a framework whereby mechanism can be incorporated into endotherm SDMs. Pika distribution has repeatedly been found to be constrained by warm temperatures, so we used Niche Mapper, a mechanistic heat-balance model, to convert macroclimate data to pika-specific surface activity time in summer across the western United States. We then explored the difference between using a macroclimate predictor (summer temperature) and using a mechanistic predictor (<span class="hlt">predicted</span> surface activity time) in SDMs. Both approaches accurately <span class="hlt">predicted</span> pika presences in current and past <span class="hlt">climate</span> regimes. However, the activity models <span class="hlt">predicted</span> 8-19% less habitat loss in response to annual temperature increases of ~3-5 °C <span class="hlt">predicted</span> in the region by 2070, suggesting that pikas may be able to buffer some <span class="hlt">climate</span> change effects through behavioral thermoregulation that can be captured by mechanistic modeling. Incorporating mechanism added value to the modeling by providing increased confidence in areas where different modeling approaches agreed and providing a range of outcomes in areas of disagreement. It also provided a more proximate variable relating animal distribution to <span class="hlt">climate</span>, allowing investigations into how unique habitat characteristics and intraspecific phenotypic variation may allow pikas to exist in areas outside those <span class="hlt">predicted</span> by generic SDMs. Only a small number of easily obtainable data are required to parameterize this mechanistic model for any endotherm, and its use can improve SDM <span class="hlt">predictions</span> by explicitly modeling a widely applicable direct physiological effect</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70176315','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70176315"><span>Mechanistic variables can enhance <span class="hlt">predictive</span> models of endotherm distributions: The American pika under current, past, and future <span class="hlt">climates</span></span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Mathewson, Paul; Moyer-Horner, Lucas; Beever, Erik; Briscoe, Natalie; Kearney, Michael T.; Yahn, Jeremiah; Porter, Warren P.</p> <p>2017-01-01</p> <p>How <span class="hlt">climate</span> constrains species’ distributions through time and space is an important question in the context of conservation planning for <span class="hlt">climate</span> change. Despite increasing awareness of the need to incorporate mechanism into species distribution models (SDMs), mechanistic modeling of endotherm distributions remains limited in this literature. Using the American pika (Ochotona princeps) as an example, we present a framework whereby mechanism can be incorporated into endotherm SDMs. Pika distribution has repeatedly been found to be constrained by warm temperatures, so we used Niche Mapper, a mechanistic heat-balance model, to convert macroclimate data to pika-specific surface activity time in summer across the western United States. We then explored the difference between using a macroclimate predictor (summer temperature) and using a mechanistic predictor (<span class="hlt">predicted</span> surface activity time) in SDMs. Both approaches accurately <span class="hlt">predicted</span> pika presences in current and past <span class="hlt">climate</span> regimes. However, the activity models <span class="hlt">predicted</span> 8–19% less habitat loss in response to annual temperature increases of ~3–5 °C <span class="hlt">predicted</span> in the region by 2070, suggesting that pikas may be able to buffer some <span class="hlt">climate</span> change effects through behavioral thermoregulation that can be captured by mechanistic modeling. Incorporating mechanism added value to the modeling by providing increased confidence in areas where different modeling approaches agreed and providing a range of outcomes in areas of disagreement. It also provided a more proximate variable relating animal distribution to <span class="hlt">climate</span>, allowing investigations into how unique habitat characteristics and intraspecific phenotypic variation may allow pikas to exist in areas outside those <span class="hlt">predicted</span> by generic SDMs. Only a small number of easily obtainable data are required to parameterize this mechanistic model for any endotherm, and its use can improve SDM <span class="hlt">predictions</span> by explicitly modeling a widely applicable direct physiological effect</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2008AGUSMGC43A..13H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2008AGUSMGC43A..13H"><span>Short Term Weather Forecasting and Long Term <span class="hlt">Climate</span> <span class="hlt">Predictions</span> in Mesoamerica</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Hardin, D. M.; Daniel, I.; Mecikalski, J.; Graves, S.</p> <p>2008-05-01</p> <p>The SERVIR project utilizes several <span class="hlt">predictive</span> models to support regional monitoring and decision support in Mesoamerica. Short term forecasts ranging from a few hours to several days produce more than 30 data products that are used daily by decision makers, as well as news organizations in the region. The forecast products can be visualized in both two and three dimensional viewers such as Google Maps and Google Earth. Other viewers developed specifically for the Mesoamerican region by the University of Alabama in Huntsville and the Institute for the Application of Geospatial Technologies in Auburn New York can also be employed. In collaboration with the NASA Short Term <span class="hlt">Prediction</span> Research and Transition (SpoRT) Center SERVIR utilizes the Weather Research and Forecast (WRF) model to produce short-term (24 hr) regional weather forecasts twice a day. Temperature, precipitation, wind, and other variables are forecast in 10km and 30km grids over the Mesoamerica region. Using the PSU/NCAR Mesoscale Model, known as MM5, SERVIR produces 48 hour- forecasts of soil temperature, two meter surface temperature, three hour accumulated precipitation, winds at different heights, and other variables. These are forecast hourly in 9km grids. Working in collaboration with the Atmospheric Science Department of the University of Alabama in Huntsville produces a suite of short-term (0-6 hour) weather <span class="hlt">prediction</span> products are generated. These "convective initiation" products <span class="hlt">predict</span> the onset of thunderstorm rainfall and lightning within a 1-hour timeframe. Models are also employed for long term <span class="hlt">predictions</span>. The SERVIR project, under USAID funding, has developed comprehensive regional <span class="hlt">climate</span> change scenarios of Mesoamerica for future years: 2010, 2015, 2025, 2050, and 2099. These scenarios were created using the Pennsylvania State University/National Center for Atmospheric Research (MM5) model and processed on the Oak Ridge National Laboratory Cheetah supercomputer. The goal of these</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/21078096','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/21078096"><span><span class="hlt">Predicted</span> effects of <span class="hlt">climate</span> warming on the distribution of 50 stream fishes in Wisconsin, USA.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Lyons, J; Stewart, J S; Mitro, M</p> <p>2010-11-01</p> <p>Summer air and stream water temperatures are expected to rise in the state of Wisconsin, U.S.A., over the next 50 years. To assess potential <span class="hlt">climate</span> warming effects on stream fishes, <span class="hlt">predictive</span> models were developed for 50 common fish species using classification-tree analysis of 69 environmental variables in a geographic information system. Model accuracy was 56·0-93·5% in validation tests. Models were applied to all 86 898 km of stream in the state under four different <span class="hlt">climate</span> scenarios: current conditions, limited <span class="hlt">climate</span> warming (summer air temperatures increase 1° C and water 0·8° C), moderate warming (air 3° C and water 2·4° C) and major warming (air 5° C and water 4° C). With <span class="hlt">climate</span> warming, 23 fishes were <span class="hlt">predicted</span> to decline in distribution (three to extirpation under the major warming scenario), 23 to increase and four to have no change. Overall, declining species lost substantially more stream length than increasing species gained. All three cold-water and 16 cool-water fishes and four of 31 warm-water fishes were <span class="hlt">predicted</span> to decline, four warm-water fishes to remain the same and 23 warm-water fishes to increase in distribution. Species changes were <span class="hlt">predicted</span> to be most dramatic in small streams in northern Wisconsin that currently have cold to cool summer water temperatures and are dominated by cold-water and cool-water fishes, and least in larger and warmer streams and rivers in southern Wisconsin that are currently dominated by warm-water fishes. Results of this study suggest that even small increases in summer air and water temperatures owing to <span class="hlt">climate</span> warming will have major effects on the distribution of stream fishes in Wisconsin. © 2010 The Authors. Journal of Fish Biology © 2010 The Fisheries Society of the British Isles.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70048367','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70048367"><span><span class="hlt">Climate</span> downscaling effects on <span class="hlt">predictive</span> ecological models: a case study for threatened and endangered vertebrates in the southeastern United States</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Bucklin, David N.; Watling, James I.; Speroterra, Carolina; Brandt, Laura A.; Mazzotti, Frank J.; Romañach, Stephanie S.</p> <p>2013-01-01</p> <p>High-resolution (downscaled) projections of future <span class="hlt">climate</span> conditions are critical inputs to a wide variety of ecological and socioeconomic models and are created using numerous different approaches. Here, we conduct a sensitivity analysis of spatial <span class="hlt">predictions</span> from <span class="hlt">climate</span> envelope models for threatened and endangered vertebrates in the southeastern United States to determine whether two different downscaling approaches (with and without the use of a regional <span class="hlt">climate</span> model) affect <span class="hlt">climate</span> envelope model <span class="hlt">predictions</span> when all other sources of variation are held constant. We found that <span class="hlt">prediction</span> maps differed spatially between downscaling approaches and that the variation attributable to downscaling technique was comparable to variation between maps generated using different general circulation models (GCMs). Precipitation variables tended to show greater discrepancies between downscaling techniques than temperature variables, and for one GCM, there was evidence that more poorly resolved precipitation variables contributed relatively more to model uncertainty than more well-resolved variables. Our work suggests that ecological modelers requiring high-resolution <span class="hlt">climate</span> projections should carefully consider the type of downscaling applied to the <span class="hlt">climate</span> projections prior to their use in <span class="hlt">predictive</span> ecological modeling. The uncertainty associated with alternative downscaling methods may rival that of other, more widely appreciated sources of variation, such as the general circulation model or emissions scenario with which future <span class="hlt">climate</span> projections are created.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.fs.usda.gov/treesearch/pubs/54546','TREESEARCH'); return false;" href="https://www.fs.usda.gov/treesearch/pubs/54546"><span>Dynamic-landscape metapopulation models <span class="hlt">predict</span> complex response of wildlife populations to <span class="hlt">climate</span> and landscape change</span></a></p> <p><a target="_blank" href="http://www.fs.usda.gov/treesearch/">Treesearch</a></p> <p>Thomas W. Bonnot; Frank R. Thompson; Joshua J. Millspaugh</p> <p>2017-01-01</p> <p>The increasing need to <span class="hlt">predict</span> how <span class="hlt">climate</span> change will impact wildlife species has exposed limitations in how well current approaches model important biological processes at scales at which those processes interact with <span class="hlt">climate</span>. We used a comprehensive approach that combined recent advances in landscape and population modeling into dynamic-landscape metapopulation...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/servlets/purl/1415029','SCIGOV-STC'); return false;" href="https://www.osti.gov/servlets/purl/1415029"><span>Collaborative Research: Improving Decadal <span class="hlt">Prediction</span> of Arctic <span class="hlt">Climate</span> Variability and Change Using a Regional Arctic</span></a></p> <p><a target="_blank" href="http://www.osti.gov/search">DOE Office of Scientific and Technical Information (OSTI.GOV)</a></p> <p>Gutowski, William J.</p> <p></p> <p>This project developed and applied a regional Arctic System model for enhanced decadal <span class="hlt">predictions</span>. It built on successful research by four of the current PIs with support from the DOE <span class="hlt">Climate</span> Change <span class="hlt">Prediction</span> Program, which has resulted in the development of a fully coupled Regional Arctic <span class="hlt">Climate</span> Model (RACM) consisting of atmosphere, land-hydrology, ocean and sea ice components. An expanded RACM, a Regional Arctic System Model (RASM), has been set up to include ice sheets, ice caps, mountain glaciers, and dynamic vegetation to allow investigation of coupled physical processes responsible for decadal-scale <span class="hlt">climate</span> change and variability in the Arctic. RASMmore » can have high spatial resolution (~4-20 times higher than currently practical in global models) to advance modeling of critical processes and determine the need for their explicit representation in Global Earth System Models (GESMs). The pan-Arctic region is a key indicator of the state of global <span class="hlt">climate</span> through polar amplification. However, a system-level understanding of critical arctic processes and feedbacks needs further development. Rapid <span class="hlt">climate</span> change has occurred in a number of Arctic System components during the past few decades, including retreat of the perennial sea ice cover, increased surface melting of the Greenland ice sheet, acceleration and thinning of outlet glaciers, reduced snow cover, thawing permafrost, and shifts in vegetation. Such changes could have significant ramifications for global sea level, the ocean thermohaline circulation and heat budget, ecosystems, native communities, natural resource exploration, and commercial transportation. The overarching goal of the RASM project has been to advance understanding of past and present states of arctic <span class="hlt">climate</span> and to improve seasonal to decadal <span class="hlt">predictions</span>. To do this the project has focused on variability and long-term change of energy and freshwater flows through the arctic <span class="hlt">climate</span> system. The three foci of this research are</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFMGC44A..07S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFMGC44A..07S"><span><span class="hlt">Predicting</span> summer residential electricity demand across the U.S.A using <span class="hlt">climate</span> information</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Sun, X.; Wang, S.; Lall, U.</p> <p>2017-12-01</p> <p>We developed a Bayesian Hierarchical model to <span class="hlt">predict</span> monthly residential per capita electricity consumption at the state level across the USA using <span class="hlt">climate</span> information. The summer period was selected since cooling requirements may be directly associated with electricity use, while for winter a mix of energy sources may be used to meet heating needs. Historical monthly electricity consumption data from 1990 to 2013 were used to build a <span class="hlt">predictive</span> model with a set of corresponding <span class="hlt">climate</span> and non-<span class="hlt">climate</span> covariates. A clustering analysis was performed first to identify groups of states that had similar temporal patterns for the cooling degree days of each state. Then, a partial pooling model was applied to each cluster to assess the sensitivity of monthly per capita residential electricity demand to each predictor (including cooling-degree-days, gross domestic product (GDP) per capita, per capita electricity demand of previous month and previous year, and the residential electricity price). The sensitivity of residential electricity to cooling-degree-days has an identifiable geographic distribution with higher values in northeastern United States.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015HESS...19.2821T','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015HESS...19.2821T"><span>Including the dynamic relationship between <span class="hlt">climatic</span> variables and leaf area index in a hydrological model to improve streamflow <span class="hlt">prediction</span> under a changing <span class="hlt">climate</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Tesemma, Z. K.; Wei, Y.; Peel, M. C.; Western, A. W.</p> <p>2015-06-01</p> <p>Anthropogenic <span class="hlt">climate</span> change is projected to enrich the atmosphere with carbon dioxide, change vegetation dynamics and influence the availability of water at the catchment scale. This study combines a nonlinear model for estimating changes in leaf area index (LAI) due to <span class="hlt">climatic</span> fluctuations with the variable infiltration capacity (VIC) hydrological model to improve catchment streamflow <span class="hlt">prediction</span> under a changing <span class="hlt">climate</span>. The combined model was applied to 13 gauged sub-catchments with different land cover types (crop, pasture and tree) in the Goulburn-Broken catchment, Australia, for the "Millennium Drought" (1997-2009) relative to the period 1983-1995, and for two future periods (2021-2050 and 2071-2100) and two emission scenarios (Representative Concentration Pathway (RCP) 4.5 and RCP8.5) which were compared with the baseline historical period of 1981-2010. This region was projected to be warmer and mostly drier in the future as <span class="hlt">predicted</span> by 38 Coupled Model Intercomparison Project Phase 5 (CMIP5) runs from 15 global <span class="hlt">climate</span> models (GCMs) and for two emission scenarios. The results showed that during the Millennium Drought there was about a 29.7-66.3 % reduction in mean annual runoff due to reduced precipitation and increased temperature. When drought-induced changes in LAI were included, smaller reductions in mean annual runoff of between 29.3 and 61.4 % were <span class="hlt">predicted</span>. The proportional increase in runoff due to modeling LAI was 1.3-10.2 % relative to not including LAI. For projected <span class="hlt">climate</span> change under the RCP4.5 emission scenario, ignoring the LAI response to changing <span class="hlt">climate</span> could lead to a further reduction in mean annual runoff of between 2.3 and 27.7 % in the near-term (2021-2050) and 2.3 to 23.1 % later in the century (2071-2100) relative to modeling the dynamic response of LAI to precipitation and temperature changes. Similar results (near-term 2.5-25.9 % and end of century 2.6-24.2 %) were found for <span class="hlt">climate</span> change under the RCP8.5 emission scenario</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFM.A31H2288D','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFM.A31H2288D"><span>Probabilistic empirical <span class="hlt">prediction</span> of seasonal <span class="hlt">climate</span>: evaluation and potential applications</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Dieppois, B.; Eden, J.; van Oldenborgh, G. J.</p> <p>2017-12-01</p> <p>Preparing for episodes with risks of anomalous weather a month to a year ahead is an important challenge for governments, non-governmental organisations, and private companies and is dependent on the availability of reliable forecasts. The majority of operational seasonal forecasts are made using process-based dynamical models, which are complex, computationally challenging and prone to biases. Empirical forecast approaches built on statistical models to represent physical processes offer an alternative to dynamical systems and can provide either a benchmark for comparison or independent supplementary forecasts. Here, we present a new evaluation of an established empirical system used to <span class="hlt">predict</span> seasonal <span class="hlt">climate</span> across the globe. Forecasts for surface air temperature, precipitation and sea level pressure are produced by the KNMI Probabilistic Empirical <span class="hlt">Prediction</span> (K-PREP) system every month and disseminated via the KNMI <span class="hlt">Climate</span> Explorer (climexp.knmi.nl). K-PREP is based on multiple linear regression and built on physical principles to the fullest extent with <span class="hlt">predictive</span> information taken from the global CO2-equivalent concentration, large-scale modes of variability in the <span class="hlt">climate</span> system and regional-scale information. K-PREP seasonal forecasts for the period 1981-2016 will be compared with corresponding dynamically generated forecasts produced by operational forecast systems. While there are many regions of the world where empirical forecast skill is extremely limited, several areas are identified where K-PREP offers comparable skill to dynamical systems. We discuss two key points in the future development and application of the K-PREP system: (a) the potential for K-PREP to provide a more useful basis for reference forecasts than those based on persistence or climatology, and (b) the added value of including K-PREP forecast information in multi-model forecast products, at least for known regions of good skill. We also discuss the potential development of</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015NatCC...5..669M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015NatCC...5..669M"><span>Darcy's law <span class="hlt">predicts</span> widespread forest mortality under <span class="hlt">climate</span> warming</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>McDowell, Nathan G.; Allen, Craig D.</p> <p>2015-07-01</p> <p>Drought and heat-induced tree mortality is accelerating in many forest biomes as a consequence of a warming <span class="hlt">climate</span>, resulting in a threat to global forests unlike any in recorded history. Forests store the majority of terrestrial carbon, thus their loss may have significant and sustained impacts on the global carbon cycle. We use a hydraulic corollary to Darcy’s law, a core principle of vascular plant physiology, to <span class="hlt">predict</span> characteristics of plants that will survive and die during drought under warmer future <span class="hlt">climates</span>. Plants that are tall with isohydric stomatal regulation, low hydraulic conductance, and high leaf area are most likely to die from future drought stress. Thus, tall trees of old-growth forests are at the greatest risk of loss, which has ominous implications for terrestrial carbon storage. This application of Darcy’s law indicates today’s forests generally should be replaced by shorter and more xeric plants, owing to future warmer droughts and associated wildfires and pest attacks. The Darcy’s corollary also provides a simple, robust framework for informing forest management interventions needed to promote the survival of current forests. Given the robustness of Darcy’s law for <span class="hlt">predictions</span> of vascular plant function, we conclude with high certainty that today’s forests are going to be subject to continued increases in mortality rates that will result in substantial reorganization of their structure and carbon storage.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014EGUGA..16.3977F','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014EGUGA..16.3977F"><span><span class="hlt">Predicting</span> Low Flow Conditions from <span class="hlt">Climatic</span> Indices - Indicator-Based Modeling for <span class="hlt">Climate</span> Change Impact Assessment</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Fangmann, Anne; Haberlandt, Uwe</p> <p>2014-05-01</p> <p>In the face of <span class="hlt">climate</span> change, the assessment of future hydrological regimes has become indispensable in the field of water resources management. Investigation of potential change is vital for proper planning, especially with regard to hydrological extremes. Commonly, projection of future streamflow is done applying process-based hydrological models, using <span class="hlt">climate</span> model data as input, whose complex model structures generally require excessive amounts of time and effort for set-up and computation. This study aims at identifying practical alternatives to the employment of sophisticated models by considering simpler, yet sufficiently accurate methods for modeling rainfall-runoff relations with regard to hydrological extremes. The focus is thereby put on the <span class="hlt">prediction</span> of low flow periods, which are, in contrast to flood events, characterized by extended durations and spatial dimensions. The models to be established in this study base on indicators, which characterize both meteorological and hydrological conditions within dry periods. This approach makes direct use of the coupling between atmospheric driving forces and streamflow response with the underlying presumption that low-precipitation and high-evaporation periods result in diminished flow, implying that relationships exist between the properties of both meteorological and hydrological events (duration, volume, severity etc.). Eventually, optimal combinations of meteorological indicators are sought that are suitable to <span class="hlt">predict</span> various low flow characteristics with satisfactory accuracy. Two approaches for model specification are tested: a) multiple linear regression, and b) Fuzzy logic. The data used for this study are daily time series of mean discharge obtained from 294 gauges with variable record length situated in the federal state of Lower Saxony, Germany, as well as interpolated <span class="hlt">climate</span> variables available for a period from 1951 to 2011. After extraction of a variety of indicators from the available</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013AcO....49...23K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013AcO....49...23K"><span><span class="hlt">Predicting</span> impacts of <span class="hlt">climate</span> change on medicinal asclepiads of Pakistan using Maxent modeling</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Khanum, Rizwana; Mumtaz, A. S.; Kumar, Sunil</p> <p>2013-05-01</p> <p>Maximum entropy (Maxent) modeling was used to <span class="hlt">predict</span> the potential <span class="hlt">climatic</span> niches of three medicinally important Asclepiad species: Pentatropis spiralis, Tylophora hirsuta, and Vincetoxicum arnottianum. All three species are members of the Asclepiad plant family, yet they differ in ecological requirements, biogeographic importance, and conservation value. Occurrence data were collected from herbarium specimens held in major herbaria of Pakistan and two years (2010 and 2011) of field surveys. The Maxent model performed better than random for the three species with an average test AUC value of 0.74 for P. spiralis, 0.84 for V. arnottianum, and 0.59 for T. hirsuta. Under the future <span class="hlt">climate</span> change scenario, the Maxent model <span class="hlt">predicted</span> habitat gains for P. spiralis in southern Punjab and Balochistan, and loss of habitat in south-eastern Sindh. Vincetoxicum arnottianum as well as T. hirsuta would gain habitat in upper Peaks of northern parts of Pakistan. T. hirsuta is <span class="hlt">predicted</span> to lose most of the habitats in northern Punjab and in parches from lower peaks of Galliat, Zhob, Qalat etc. The <span class="hlt">predictive</span> modeling approach presented here may be applied to other rare Asclepiad species, especially those under constant extinction threat.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70048115','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70048115"><span>Modeling responses of large-river fish populations to global <span class="hlt">climate</span> change through downscaling and incorporation of <span class="hlt">predictive</span> uncertainty</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Wildhaber, Mark L.; Wikle, Christopher K.; Anderson, Christopher J.; Franz, Kristie J.; Moran, Edward H.; Dey, Rima; Mader, Helmut; Kraml, Julia</p> <p>2012-01-01</p> <p><span class="hlt">Climate</span> change operates over a broad range of spatial and temporal scales. Understanding its effects on ecosystems requires multi-scale models. For understanding effects on fish populations of riverine ecosystems, <span class="hlt">climate</span> <span class="hlt">predicted</span> by coarse-resolution Global <span class="hlt">Climate</span> Models must be downscaled to Regional <span class="hlt">Climate</span> Models to watersheds to river hydrology to population response. An additional challenge is quantifying sources of uncertainty given the highly nonlinear nature of interactions between <span class="hlt">climate</span> variables and community level processes. We present a modeling approach for understanding and accomodating uncertainty by applying multi-scale <span class="hlt">climate</span> models and a hierarchical Bayesian modeling framework to Midwest fish population dynamics and by linking models for system components together by formal rules of probability. The proposed hierarchical modeling approach will account for sources of uncertainty in forecasts of community or population response. The goal is to evaluate the potential distributional changes in an ecological system, given distributional changes implied by a series of linked <span class="hlt">climate</span> and system models under various emissions/use scenarios. This understanding will aid evaluation of management options for coping with global <span class="hlt">climate</span> change. In our initial analyses, we found that <span class="hlt">predicted</span> pallid sturgeon population responses were dependent on the <span class="hlt">climate</span> scenario considered.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4150295','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4150295"><span>A perspective on sustained marine observations for <span class="hlt">climate</span> modelling and <span class="hlt">prediction</span></span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Dunstone, Nick J.</p> <p>2014-01-01</p> <p>Here, I examine some of the many varied ways in which sustained global ocean observations are used in numerical modelling activities. In particular, I focus on the use of ocean observations to initialize <span class="hlt">predictions</span> in ocean and <span class="hlt">climate</span> models. Examples are also shown of how models can be used to assess the impact of both current ocean observations and to simulate that of potential new ocean observing platforms. The ocean has never been better observed than it is today and similarly ocean models have never been as capable at representing the real ocean as they are now. However, there remain important unanswered questions that can likely only be addressed via future improvements in ocean observations. In particular, ocean observing systems need to respond to the needs of the burgeoning field of near-term <span class="hlt">climate</span> <span class="hlt">predictions</span>. Although new ocean observing platforms promise exciting new discoveries, there is a delicate balance to be made between their funding and that of the current ocean observing system. Here, I identify the need to secure long-term funding for ocean observing platforms as they mature, from a mainly research exercise to an operational system for sustained observation over <span class="hlt">climate</span> change time scales. At the same time, considerable progress continues to be made via ship-based observing campaigns and I highlight some that are dedicated to addressing uncertainties in key ocean model parametrizations. The use of ocean observations to understand the prominent long time scale changes observed in the North Atlantic is another focus of this paper. The exciting first decade of monitoring of the Atlantic meridional overturning circulation by the RAPID-MOCHA array is highlighted. The use of ocean and <span class="hlt">climate</span> models as tools to further probe the drivers of variability seen in such time series is another exciting development. I also discuss the need for a concerted combined effort from <span class="hlt">climate</span> models and ocean observations in order to understand the current slow</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/25157195','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/25157195"><span>A perspective on sustained marine observations for <span class="hlt">climate</span> modelling and <span class="hlt">prediction</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Dunstone, Nick J</p> <p>2014-09-28</p> <p>Here, I examine some of the many varied ways in which sustained global ocean observations are used in numerical modelling activities. In particular, I focus on the use of ocean observations to initialize <span class="hlt">predictions</span> in ocean and <span class="hlt">climate</span> models. Examples are also shown of how models can be used to assess the impact of both current ocean observations and to simulate that of potential new ocean observing platforms. The ocean has never been better observed than it is today and similarly ocean models have never been as capable at representing the real ocean as they are now. However, there remain important unanswered questions that can likely only be addressed via future improvements in ocean observations. In particular, ocean observing systems need to respond to the needs of the burgeoning field of near-term <span class="hlt">climate</span> <span class="hlt">predictions</span>. Although new ocean observing platforms promise exciting new discoveries, there is a delicate balance to be made between their funding and that of the current ocean observing system. Here, I identify the need to secure long-term funding for ocean observing platforms as they mature, from a mainly research exercise to an operational system for sustained observation over <span class="hlt">climate</span> change time scales. At the same time, considerable progress continues to be made via ship-based observing campaigns and I highlight some that are dedicated to addressing uncertainties in key ocean model parametrizations. The use of ocean observations to understand the prominent long time scale changes observed in the North Atlantic is another focus of this paper. The exciting first decade of monitoring of the Atlantic meridional overturning circulation by the RAPID-MOCHA array is highlighted. The use of ocean and <span class="hlt">climate</span> models as tools to further probe the drivers of variability seen in such time series is another exciting development. I also discuss the need for a concerted combined effort from <span class="hlt">climate</span> models and ocean observations in order to understand the current slow</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_11");'>11</a></li> <li><a href="#" onclick='return showDiv("page_12");'>12</a></li> <li class="active"><span>13</span></li> <li><a href="#" onclick='return showDiv("page_14");'>14</a></li> <li><a href="#" onclick='return showDiv("page_15");'>15</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_13 --> <div id="page_14" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_12");'>12</a></li> <li><a href="#" onclick='return showDiv("page_13");'>13</a></li> <li class="active"><span>14</span></li> <li><a href="#" onclick='return showDiv("page_15");'>15</a></li> <li><a href="#" onclick='return showDiv("page_16");'>16</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="261"> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFMGC24A..08T','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFMGC24A..08T"><span><span class="hlt">Predicting</span> <span class="hlt">Climate</span>-sensitive Infectious Diseases: Development of a Federal Science Plan and the Path Forward</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Trtanj, J.; Balbus, J. M.; Brown, C.; Shimamoto, M. M.</p> <p>2017-12-01</p> <p>The transmission and spread of infectious diseases, especially vector-borne diseases, water-borne diseases and zoonosis, are influenced by short and long-term <span class="hlt">climate</span> factors, in conjunction with numerous other drivers. Public health interventions, including vaccination, vector control programs, and outreach campaigns could be made more effective if the geographic range and timing of increased disease risk could be more accurately targeted, and high risk areas and populations identified. While some progress has been made in <span class="hlt">predictive</span> modeling for transmission of these diseases using <span class="hlt">climate</span> and weather data as inputs, they often still start after the first case appears, the skill of those models remains limited, and their use by public health officials infrequent. And further, <span class="hlt">predictions</span> with lead times of weeks, months or seasons are even rarer, yet the value of acting early holds the potential to save more lives, reduce cost and enhance both economic and national security. Information on high-risk populations and areas for infectious diseases is also potentially useful for the federal defense and intelligence communities as well. The US Global Change Research Program, through its Interagency Group on <span class="hlt">Climate</span> Change and Human Health (CCHHG), has put together a science plan that pulls together federal scientists and programs working on <span class="hlt">predictive</span> modeling of <span class="hlt">climate</span>-sensitive diseases, and draws on academic and other partners. Through a series of webinars and an in-person workshop, the CCHHG has convened key federal and academic stakeholders to assess the current state of science and develop an integrated science plan to identify data and observation systems needs as well as a targeted research agenda for enhancing <span class="hlt">predictive</span> modeling. This presentation will summarize the findings from this effort and engage AGU members on plans and next steps to improve <span class="hlt">predictive</span> modeling for infectious diseases.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://eric.ed.gov/?q=zero+AND+one&pg=4&id=EJ875294','ERIC'); return false;" href="https://eric.ed.gov/?q=zero+AND+one&pg=4&id=EJ875294"><span>Schoolwide Social-Behavioral <span class="hlt">Climate</span>, Student Problem Behavior, and Related <span class="hlt">Administrative</span> Decisions: Empirical Patterns from 1,510 Schools Nationwide</span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Spaulding, Scott A.; Irvin, Larry K.; Horner, Robert H.; May, Seth L.; Emeldi, Monica; Tobin, Tary J.; Sugai, George</p> <p>2010-01-01</p> <p>Office discipline referral (ODR) data provide useful information about problem behavior and consequence patterns, social-behavioral <span class="hlt">climates</span>, and effects of social-behavioral interventions in schools. The authors report patterns of ODRs and subsequent <span class="hlt">administrative</span> decisions from 1,510 schools nationwide that used the School-Wide Information…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29098819','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29098819"><span>[<span class="hlt">Prediction</span> of the potential distribution of Tibetan medicinal Lycium ruthenicum in context of <span class="hlt">climate</span> change].</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Lin, Li; Jin, Ling; Wang, Zhen-Heng; Cui, Zhi-Jia; Ma, Yi</p> <p>2017-07-01</p> <p>To <span class="hlt">predict</span> the suitable distribution patterns of Lycium ruthenicum in the present and future under the background of <span class="hlt">climate</span> change, and provide reference for the resources sustainable utilization and GAP standardized planting. The software of Maxent and ArcGis was used to <span class="hlt">predict</span> the potential suitable regions and grades of L. ruthenicum in China based on the 149 distribution information, <span class="hlt">climate</span> data of contemporary (1950-2000) and future (20-80 decade of 21 century), and considering of three greenhouse gaseous emission scenario. The results showed that:the suitable distribution regions of L. ruthenicum are mainly concentrated in Xinjiang, Qinghai, Gansu, Neimenggu, and Ningxia province in present. In addition, Shaanxi, Shanxi and Xizang are also distribution regions.The suitable distribution area of L. ruthenicum is 284.506 949×104 km2, accounted for 29.6% of the land area of China.The relatively stable area of the suitable regions accounted for 25.2% of the total suitable region area.Under the background of <span class="hlt">climate</span> change, compared with contemporary, the total area of suitable region is reducing and moderately suitable area is increasing at different degree at the 20, 30, 40, 50, 60, 70, 80 decade of 21 century. <span class="hlt">Climate</span> change both can change the total area of suitable regions and habitat suitability of L. ruthenicum. It could provide a strategic guidance for protection, development and utilization of L. ruthenicum though the <span class="hlt">prediction</span> of potential suitable regions distribution of L. ruthenicum based on the mainly factor of <span class="hlt">climate</span> change. Copyright© by the Chinese Pharmaceutical Association.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29479693','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29479693"><span>Revisiting concepts of thermal physiology: <span class="hlt">Predicting</span> responses of mammals to <span class="hlt">climate</span> change.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Mitchell, Duncan; Snelling, Edward P; Hetem, Robyn S; Maloney, Shane K; Strauss, Willem Maartin; Fuller, Andrea</p> <p>2018-02-26</p> <p>The accuracy of <span class="hlt">predictive</span> models (also known as mechanistic or causal models) of animal responses to <span class="hlt">climate</span> change depends on properly incorporating the principles of heat transfer and thermoregulation into those models. Regrettably, proper incorporation of these principles is not always evident. We have revisited the relevant principles of thermal physiology and analysed how they have been applied in <span class="hlt">predictive</span> models of large mammals, which are particularly vulnerable, to <span class="hlt">climate</span> change. We considered dry heat exchange, evaporative heat transfer, the thermoneutral zone and homeothermy, and we examined the roles of size and shape in the thermal physiology of large mammals. We report on the following misconceptions in influential <span class="hlt">predictive</span> models: underestimation of the role of radiant heat transfer, misassignment of the role and misunderstanding of the sustainability of evaporative cooling, misinterpretation of the thermoneutral zone as a zone of thermal tolerance or as a zone of sustainable energetics, confusion of upper critical temperature and critical thermal maximum, overestimation of the metabolic energy cost of evaporative cooling, failure to appreciate that the current advantages of size and shape will become disadvantageous as <span class="hlt">climate</span> change advances, misassumptions about skin temperature and, lastly, misconceptions about the relationship between body core temperature and its variability with body mass in large mammals. Not all misconceptions invalidate the models, but we believe that preventing inappropriate assumptions from propagating will improve model accuracy, especially as models progress beyond their current typically static format to include genetic and epigenetic adaptation that can result in phenotypic plasticity. © 2018 The Authors. Journal of Animal Ecology © 2018 British Ecological Society.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2011AGUFMNG51A1652L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2011AGUFMNG51A1652L"><span>Do GCM's <span class="hlt">Predict</span> the <span class="hlt">Climate</span>.... Or the Low Frequency Weather?</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Lovejoy, S.; Varon, D.; Schertzer, D. J.</p> <p>2011-12-01</p> <p> <span class="hlt">predicting</span> this low frequency weather so as to <span class="hlt">predict</span> the <span class="hlt">climate</span>, they need appropriate <span class="hlt">climate</span> forcings and/ or new internal mechanisms of variability. We examine this using wavelet analyses of forced and unforced GCM outputs, including the ECHO-G simulation used in the Millenium project. For example, we find that <span class="hlt">climate</span> scenarios with large CO2 increases do give rise to a <span class="hlt">climate</span> regime but that Hc>1 i.e. much larger than that of natural variability which for temperatures has Hc≈0.4. In comparison, the (largely volcanic) forcing of the ECHO-G Millenium simulation is fairly realistic (Hc≈0.4), although it is not clear that this mechanism can explain the even lower frequency variability found in the paleotemperature series, nor is it clear that this is compatible with low frequency solar or orbital forcings.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/27859101','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/27859101"><span>Can trait patterns along gradients <span class="hlt">predict</span> plant community responses to <span class="hlt">climate</span> change?</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Guittar, John; Goldberg, Deborah; Klanderud, Kari; Telford, Richard J; Vandvik, Vigdis</p> <p>2016-10-01</p> <p>Plant functional traits vary consistently along <span class="hlt">climate</span> gradients and are therefore potential predictors of plant community response to <span class="hlt">climate</span> change. We test this space-for-time assumption by combining a spatial gradient study with whole-community turf transplantation along temperature and precipitation gradients in a network of 12 grassland sites in Southern Norway. Using data on eight traits for 169 species and annual vegetation censuses of 235 turfs over 5 yr, we quantify trait-based responses to <span class="hlt">climate</span> change by comparing observed community dynamics in transplanted turfs to field-parameterized null model simulations. Three traits related to species architecture (maximum height, number of dormant meristems, and ramet-ramet connection persistence) varied consistently along spatial temperature gradients and also correlated to changes in species abundances in turfs transplanted to warmer <span class="hlt">climates</span>. Two traits associated with resource acquisition strategy (SLA, leaf area) increased along spatial temperature gradients but did not correlate to changes in species abundances following warming. No traits correlated consistently with precipitation. Our study supports the hypothesis that spatial associations between plant traits and broad-scale <span class="hlt">climate</span> variables can be <span class="hlt">predictive</span> of community response to <span class="hlt">climate</span> change, but it also suggests that not all traits with clear patterns along <span class="hlt">climate</span> gradients will necessarily influence community response to an equal degree. © 2016 by the Ecological Society of America.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3651425','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3651425"><span>Origin of seasonal <span class="hlt">predictability</span> for summer <span class="hlt">climate</span> over the Northwestern Pacific</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Kosaka, Yu; Xie, Shang-Ping; Lau, Ngar-Cheung; Vecchi, Gabriel A.</p> <p>2013-01-01</p> <p>Summer <span class="hlt">climate</span> in the Northwestern Pacific (NWP) displays large year-to-year variability, affecting densely populated Southeast and East Asia by impacting precipitation, temperature, and tropical cyclones. The Pacific–Japan (PJ) teleconnection pattern provides a crucial link of high <span class="hlt">predictability</span> from the tropics to East Asia. Using coupled <span class="hlt">climate</span> model experiments, we show that the PJ pattern is the atmospheric manifestation of an air–sea coupled mode spanning the Indo-NWP warm pool. The PJ pattern forces the Indian Ocean (IO) via a westward propagating atmospheric Rossby wave. In response, IO sea surface temperature feeds back and reinforces the PJ pattern via a tropospheric Kelvin wave. Ocean coupling increases both the amplitude and temporal persistence of the PJ pattern. Cross-correlation of ocean–atmospheric anomalies confirms the coupled nature of this PJIO mode. The ocean–atmosphere feedback explains why the last echoes of El Niño–Southern Oscillation are found in the IO-NWP in the form of the PJIO mode. We demonstrate that the PJIO mode is indeed highly <span class="hlt">predictable</span>; a characteristic that can enable benefits to society. PMID:23610388</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29136659','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29136659"><span><span class="hlt">Predicting</span> the distributions of Egypt's medicinal plants and their potential shifts under future <span class="hlt">climate</span> change.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Kaky, Emad; Gilbert, Francis</p> <p>2017-01-01</p> <p><span class="hlt">Climate</span> change is one of the most difficult of challenges to conserving biodiversity, especially for countries with few data on the distributions of their taxa. Species distribution modelling is a modern approach to the assessment of the potential effects of <span class="hlt">climate</span> change on biodiversity, with the great advantage of being robust to small amounts of data. Taking advantage of a recently validated dataset, we use the medicinal plants of Egypt to identify hotspots of diversity now and in the future by <span class="hlt">predicting</span> the effect of <span class="hlt">climate</span> change on the pattern of species richness using species distribution modelling. Then we assess how Egypt's current Protected Area network is likely to perform in protecting plants under <span class="hlt">climate</span> change. The patterns of species richness show that in most cases the A2a 'business as usual' scenario was more harmful than the B2a 'moderate mitigation' scenario. <span class="hlt">Predicted</span> species richness inside Protected Areas was higher than outside under all scenarios, indicating that Egypt's PAs are well placed to help conserve medicinal plants.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013WRR....49.6671P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013WRR....49.6671P"><span>The value of model averaging and dynamical <span class="hlt">climate</span> model <span class="hlt">predictions</span> for improving statistical seasonal streamflow forecasts over Australia</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Pokhrel, Prafulla; Wang, Q. J.; Robertson, David E.</p> <p>2013-10-01</p> <p>Seasonal streamflow forecasts are valuable for planning and allocation of water resources. In Australia, the Bureau of Meteorology employs a statistical method to forecast seasonal streamflows. The method uses predictors that are related to catchment wetness at the start of a forecast period and to <span class="hlt">climate</span> during the forecast period. For the latter, a predictor is selected among a number of lagged <span class="hlt">climate</span> indices as candidates to give the "best" model in terms of model performance in cross validation. This study investigates two strategies for further improvement in seasonal streamflow forecasts. The first is to combine, through Bayesian model averaging, multiple candidate models with different lagged <span class="hlt">climate</span> indices as predictors, to take advantage of different <span class="hlt">predictive</span> strengths of the multiple models. The second strategy is to introduce additional candidate models, using rainfall and sea surface temperature <span class="hlt">predictions</span> from a global <span class="hlt">climate</span> model as predictors. This is to take advantage of the direct simulations of various dynamic processes. The results show that combining forecasts from multiple statistical models generally yields more skillful forecasts than using only the best model and appears to moderate the worst forecast errors. The use of rainfall <span class="hlt">predictions</span> from the dynamical <span class="hlt">climate</span> model marginally improves the streamflow forecasts when viewed over all the study catchments and seasons, but the use of sea surface temperature <span class="hlt">predictions</span> provide little additional benefit.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFM.A51E0119Y','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFM.A51E0119Y"><span>Summer precipitation <span class="hlt">prediction</span> in the source region of the Yellow River using <span class="hlt">climate</span> indices</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Yuan, F.</p> <p>2016-12-01</p> <p>The source region of the Yellow River contributes about 35% of the total water yield in the Yellow River basin playing an important role in meeting downstream water resources requirements. The summer precipitation from June to September in the source region of the Yellow River accounts for about 70% of the annual total, and its decrease would cause further water shortage problems. Consequently, the objectives of this study are to improve the understanding of the linkages between the precipitation in the source region of the Yellow River and global teleconnection patterns, and to <span class="hlt">predict</span> the summer precipitation based on revealed teleconnections. Spatial variability of precipitation was investigated based on three homogeneous sub-regions. Principal component analysis and singular value decomposition were used to find significant relations between the precipitation in the source region of the Yellow River and global teleconnection patterns using <span class="hlt">climate</span> indices. A back-propagation neural network was developed to <span class="hlt">predict</span> the summer precipitation using significantly correlated <span class="hlt">climate</span> indices. It was found that precipitation in the study area is positively related to North Atlantic Oscillation, West Pacific Pattern and El Nino Southern Oscillation, and inversely related to Polar Eurasian pattern. Summer precipitation was overall well <span class="hlt">predicted</span> using these significantly correlated <span class="hlt">climate</span> indices, and the Pearson correlation coefficient between <span class="hlt">predicted</span> and observed summer precipitation was in general larger than 0.6. The results are useful for integrated water resources management in the Yellow River basin.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=19990063645&hterms=climate+change+evidence&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D60%26Ntt%3Dclimate%2Bchange%2Bevidence','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=19990063645&hterms=climate+change+evidence&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D60%26Ntt%3Dclimate%2Bchange%2Bevidence"><span>NASA's Earth Observing System: The Transition from <span class="hlt">Climate</span> Monitoring to <span class="hlt">Climate</span> Change <span class="hlt">Prediction</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>King, Michael D.; Herring, David D.</p> <p>1998-01-01</p> <p>Earth's 4.5 billion year history is a study in change. Natural geological forces have been rearranging the surface features and <span class="hlt">climatic</span> conditions of our planet since its beginning. There is scientific evidence that some of these natural changes have not only led to mass extinctions of species (e.g., dinosaurs), but have also severely impacted human civilizations. For instance, there is evidence that a relatively sudden <span class="hlt">climate</span> change caused a 300-year drought that contributed to the downfall of Akkadia, one of the most powerful empires in the Middle-East region around 2200 BC. More recently, the "little ice age" from 1200-1400 AD forced the Vikings to abandon Greenland when temperatures there dropped by about 1.5 C, rendering it too difficult to grow enough crops to sustain the population. Today, there is compelling scientific evidence that human activities have attained the magnitude of a geological force and are speeding up the rate of global change. For example, carbon dioxide levels have risen 30 percent since the industrial revolution and about 40 percent of the world's land surface has been transformed by humans. We don't understand the cause-and-effect relationships among Earth's land, ocean, and atmosphere well enough to <span class="hlt">predict</span> what, if any, impacts these rapid changes will have on future <span class="hlt">climate</span> conditions. We need to make many measurements all over the world, over a long period of time, in order to assemble the information needed to construct accurate computer models that will enable us to forecast <span class="hlt">climate</span> change. In 1988, the Earth System Sciences Committee, sponsored by NASA, issued a report calling for an integrated, long-term strategy for measuring the vital signs of Earth's <span class="hlt">climate</span> system. The report urged that the measurements must all be intimately coupled with focused process studies, they must facilitate development of Earth system models, and they must be stored in an information system that ensures open access to consistent, long-term data</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.fs.usda.gov/treesearch/pubs/56130','TREESEARCH'); return false;" href="https://www.fs.usda.gov/treesearch/pubs/56130"><span>Towards a <span class="hlt">predictive</span> understanding of belowground process responses to <span class="hlt">climate</span> change: have we moved any closer?</span></a></p> <p><a target="_blank" href="http://www.fs.usda.gov/treesearch/">Treesearch</a></p> <p>Elise Pendall; Lindsey Rustad; Josh Schimel</p> <p>2008-01-01</p> <p>Belowground processes, including root production and exudation, microbial activity and community dynamics, and biogeochemical cycling interact to help regulate <span class="hlt">climate</span> change. Feedbacks associated with these processes, such as warming-enhanced decomposition rates, give rise to major uncertainties in <span class="hlt">predictions</span> of future <span class="hlt">climate</span>. Uncertainties associated with these...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2009EGUGA..1112225S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2009EGUGA..1112225S"><span><span class="hlt">Prediction</span> of future <span class="hlt">climate</span> change for the Blue Nile, using a nested Regional <span class="hlt">Climate</span> Model</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Soliman, E.; Jeuland, M.</p> <p>2009-04-01</p> <p>Although the Nile River Basin is rich in natural resources, it faces many challenges. Rainfall is highly variable across the region, on both seasonal and inter-annual scales. This variability makes the region vulnerable to droughts and floods. Many development projects involving Nile waters are currently underway, or being studied. These projects will lead to land-use patterns changes and water distribution and availability. It is thus important to assess the effects of a) these projects and b) evolving water resource management and policies, on regional hydrological processes. This paper seeks to establish a basis for evaluation of such impacts within the Blue Nile River sub-basin, using the RegCM3 Regional <span class="hlt">Climate</span> Model to simulate interactions between the land surface and <span class="hlt">climatic</span> processes. We first present results from application of this RCM model nested with downscaled outputs obtained from the ECHAM5/MPI-OM1 transient simulations for the 20th Century. We then investigate changes associated with mid-21st century emissions forcing of the SRES A1B scenario. The results obtained from the <span class="hlt">climate</span> model are then fed as inputs to the Nile Forecast System (NFS), a hydrologic distributed rainfall runoff model of the Nile Basin, The interaction between <span class="hlt">climatic</span> and hydrological processes on the land surface has been fully coupled. Rainfall patterns and evaporation rates have been generated using RegCM3, and the resulting runoff and Blue Nile streamflow patterns have been simulated using the NFS. This paper compares the results obtained from the RegCM3 <span class="hlt">climate</span> model with observational datasets for precipitation and temperature from the <span class="hlt">Climate</span> Research Unit (UK) and the NASA Goddard Space Flight Center GPCP (USA) for 1985-2000. The validity of the streamflow <span class="hlt">predictions</span> from the NFS is assessed using historical gauge records. Finally, we present results from modeling of the A1B emissions scenario of the IPCC for the years 2034-2055. Our results indicate that future</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/28844791','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/28844791"><span><span class="hlt">Climates</span> Past, Present, and Yet-to-Come Shape <span class="hlt">Climate</span> Change Vulnerabilities.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Nadeau, Christopher P; Urban, Mark C; Bridle, Jon R</p> <p>2017-10-01</p> <p><span class="hlt">Climate</span> change is altering life at multiple scales, from genes to ecosystems. <span class="hlt">Predicting</span> the vulnerability of populations to <span class="hlt">climate</span> change is crucial to mitigate negative impacts. We suggest that regional patterns of spatial and temporal <span class="hlt">climatic</span> variation scaled to the traits of an organism can <span class="hlt">predict</span> where and why populations are most vulnerable to <span class="hlt">climate</span> change. Specifically, historical <span class="hlt">climatic</span> variation affects the sensitivity and response capacity of populations to <span class="hlt">climate</span> change by shaping traits and the genetic variation in those traits. Present and future <span class="hlt">climatic</span> variation can affect both <span class="hlt">climate</span> change exposure and population responses. We provide seven <span class="hlt">predictions</span> for how <span class="hlt">climatic</span> variation might affect the vulnerability of populations to <span class="hlt">climate</span> change and suggest key directions for future research. Copyright © 2017 Elsevier Ltd. All rights reserved.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5903596','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5903596"><span>Understanding the dynamics in distribution of invasive alien plant species under <span class="hlt">predicted</span> <span class="hlt">climate</span> change in Western Himalaya</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Chitale, Vishwas; Rijal, Srijana Joshi; Bisht, Neha; Shrestha, Bharat Babu</p> <p>2018-01-01</p> <p>Invasive alien plant species (IAPS) can pose severe threats to biodiversity and stability of native ecosystems, therefore, <span class="hlt">predicting</span> the distribution of the IAPS plays a crucial role in effective planning and management of ecosystems. In the present study, we use Maximum Entropy (MaxEnt) modelling approach to <span class="hlt">predict</span> the potential of distribution of eleven IAPS under future <span class="hlt">climatic</span> conditions under RCP 2.6 and RCP 8.5 in part of Kailash sacred landscape region in Western Himalaya. Based on the model <span class="hlt">predictions</span>, distribution of most of these invasive plants is expected to expand under future <span class="hlt">climatic</span> scenarios, which might pose a serious threat to the native ecosystems through competition for resources in the study area. Native scrublands and subtropical needle-leaved forests will be the most affected ecosystems by the expansion of these IAPS. The present study is first of its kind in the Kailash Sacred Landscape in the field of invasive plants and the <span class="hlt">predictions</span> of potential distribution under future <span class="hlt">climatic</span> conditions from our study could help decision makers in planning and managing these forest ecosystems effectively. PMID:29664961</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29664961','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29664961"><span>Understanding the dynamics in distribution of invasive alien plant species under <span class="hlt">predicted</span> <span class="hlt">climate</span> change in Western Himalaya.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Thapa, Sunil; Chitale, Vishwas; Rijal, Srijana Joshi; Bisht, Neha; Shrestha, Bharat Babu</p> <p>2018-01-01</p> <p>Invasive alien plant species (IAPS) can pose severe threats to biodiversity and stability of native ecosystems, therefore, <span class="hlt">predicting</span> the distribution of the IAPS plays a crucial role in effective planning and management of ecosystems. In the present study, we use Maximum Entropy (MaxEnt) modelling approach to <span class="hlt">predict</span> the potential of distribution of eleven IAPS under future <span class="hlt">climatic</span> conditions under RCP 2.6 and RCP 8.5 in part of Kailash sacred landscape region in Western Himalaya. Based on the model <span class="hlt">predictions</span>, distribution of most of these invasive plants is expected to expand under future <span class="hlt">climatic</span> scenarios, which might pose a serious threat to the native ecosystems through competition for resources in the study area. Native scrublands and subtropical needle-leaved forests will be the most affected ecosystems by the expansion of these IAPS. The present study is first of its kind in the Kailash Sacred Landscape in the field of invasive plants and the <span class="hlt">predictions</span> of potential distribution under future <span class="hlt">climatic</span> conditions from our study could help decision makers in planning and managing these forest ecosystems effectively.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/17587061','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/17587061"><span><span class="hlt">Predicting</span> body temperature and activity of adult Polyommatus icarus using neural network models under current and projected <span class="hlt">climate</span> scenarios.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Howe, P D; Bryant, S R; Shreeve, T G</p> <p>2007-10-01</p> <p>We use field observations in two geographic regions within the British Isles and regression and neural network models to examine the relationship between microhabitat use, thoracic temperatures and activity in a widespread lycaenid butterfly, Polyommatus icarus. We also make <span class="hlt">predictions</span> for future activity under <span class="hlt">climate</span> change scenarios. Individuals from a univoltine northern population initiated flight with significantly lower thoracic temperatures than individuals from a bivoltine southern population. Activity is dependent on body temperature and neural network models of body temperature are better at <span class="hlt">predicting</span> body temperature than generalized linear models. Neural network models of activity with a sole input of <span class="hlt">predicted</span> body temperature (using weather and microclimate variables) are good predictors of observed activity and were better predictors than generalized linear models. By modelling activity under <span class="hlt">climate</span> change scenarios for 2080 we <span class="hlt">predict</span> differences in activity in relation to both regional differences of <span class="hlt">climate</span> change and differing body temperature requirements for activity in different populations. Under average conditions for low-emission scenarios there will be little change in the activity of individuals from central-southern Britain and a reduction in northwest Scotland from 2003 activity levels. Under high-emission scenarios, flight-dependent activity in northwest Scotland will increase the greatest, despite smaller <span class="hlt">predicted</span> increases in temperature and decreases in cloud cover. We suggest that neural network models are an effective way of <span class="hlt">predicting</span> future activity in changing <span class="hlt">climates</span> for microhabitat-specialist butterflies and that regional differences in the thermoregulatory response of populations will have profound effects on how they respond to <span class="hlt">climate</span> change.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017ThApC.tmp..152W','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017ThApC.tmp..152W"><span>Evaluation of global <span class="hlt">climate</span> model on performances of precipitation simulation and <span class="hlt">prediction</span> in the Huaihe River basin</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Wu, Yenan; Zhong, Ping-an; Xu, Bin; Zhu, Feilin; Fu, Jisi</p> <p>2017-06-01</p> <p>Using <span class="hlt">climate</span> models with high performance to <span class="hlt">predict</span> the future <span class="hlt">climate</span> changes can increase the reliability of results. In this paper, six kinds of global <span class="hlt">climate</span> models that selected from the Coupled Model Intercomparison Project Phase 5 (CMIP5) under Representative Concentration Path (RCP) 4.5 scenarios were compared to the measured data during baseline period (1960-2000) and evaluate the simulation performance on precipitation. Since the results of single <span class="hlt">climate</span> models are often biased and highly uncertain, we examine the back propagation (BP) neural network and arithmetic mean method in assembling the precipitation of multi models. The delta method was used to calibrate the result of single model and multimodel ensembles by arithmetic mean method (MME-AM) during the validation period (2001-2010) and the <span class="hlt">predicting</span> period (2011-2100). We then use the single models and multimodel ensembles to <span class="hlt">predict</span> the future precipitation process and spatial distribution. The result shows that BNU-ESM model has the highest simulation effect among all the single models. The multimodel assembled by BP neural network (MME-BP) has a good simulation performance on the annual average precipitation process and the deterministic coefficient during the validation period is 0.814. The simulation capability on spatial distribution of precipitation is: calibrated MME-AM > MME-BP > calibrated BNU-ESM. The future precipitation <span class="hlt">predicted</span> by all models tends to increase as the time period increases. The order of average increase amplitude of each season is: winter > spring > summer > autumn. These findings can provide useful information for decision makers to make <span class="hlt">climate</span>-related disaster mitigation plans.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/26027583','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/26027583"><span>Spatial Models for <span class="hlt">Prediction</span> and Early Warning of Aedes aegypti Proliferation from Data on <span class="hlt">Climate</span> Change and Variability in Cuba.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Ortiz, Paulo L; Rivero, Alina; Linares, Yzenia; Pérez, Alina; Vázquez, Juan R</p> <p>2015-04-01</p> <p><span class="hlt">Climate</span> variability, the primary expression of <span class="hlt">climate</span> change, is one of the most important environmental problems affecting human health, particularly vector-borne diseases. Despite research efforts worldwide, there are few studies addressing the use of information on <span class="hlt">climate</span> variability for prevention and early warning of vector-borne infectious diseases. Show the utility of <span class="hlt">climate</span> information for vector surveillance by developing spatial models using an entomological indicator and information on <span class="hlt">predicted</span> <span class="hlt">climate</span> variability in Cuba to provide early warning of danger of increased risk of dengue transmission. An ecological study was carried out using retrospective and prospective analyses of time series combined with spatial statistics. Several entomological and <span class="hlt">climatic</span> indicators were considered using complex Bultó indices -1 and -2. Moran's I spatial autocorrelation coefficient specified for a matrix of neighbors with a radius of 20 km, was used to identify the spatial structure. Spatial structure simulation was based on simultaneous autoregressive and conditional autoregressive models; agreement between <span class="hlt">predicted</span> and observed values for number of Aedes aegypti foci was determined by the concordance index Di and skill factor Bi. Spatial and temporal distributions of populations of Aedes aegypti were obtained. Models for describing, simulating and <span class="hlt">predicting</span> spatial patterns of Aedes aegypti populations associated with <span class="hlt">climate</span> variability patterns were put forward. The ranges of <span class="hlt">climate</span> variability affecting Aedes aegypti populations were identified. Forecast maps were generated for the municipal level. Using the Bultó indices of <span class="hlt">climate</span> variability, it is possible to construct spatial models for <span class="hlt">predicting</span> increased Aedes aegypti populations in Cuba. At 20 x 20 km resolution, the models are able to provide warning of potential changes in vector populations in rainy and dry seasons and by month, thus demonstrating the usefulness of <span class="hlt">climate</span> information for</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2008PhDT.......140S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2008PhDT.......140S"><span>Understanding and <span class="hlt">predicting</span> <span class="hlt">climate</span> variations in the Middle East for sustainable water resource management and development</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Samuels, Rana</p> <p></p> <p>Water issues are a source of tension between Israelis and Palestinians. In the and region of the Middle East, water supply is not just scarce but also uncertain: It is not uncommon for annual rainfall to be as little as 60% or as much as 125% of the multiannual average. This combination of scarcity and uncertainty exacerbates the already strained economy and the already tensed political situation. The uncertainty could be alleviated if it were possible to better forecast water availability. Such forecasting is key not only for water planning and management, but also for economic policy and for political decision making. Water forecasts at multiple time scales are necessary for crop choice, aquifer operation and investments in desalination infrastructure. The unequivocal warming of the <span class="hlt">climate</span> system adds another level of uncertainty as global and regional water cycles change. This makes the <span class="hlt">prediction</span> of water availability an even greater challenge. Understanding the impact of <span class="hlt">climate</span> change on precipitation can provide the information necessary for appropriate risk assessment and water planning. Unfortunately, current global circulation models (GCMs) are only able to <span class="hlt">predict</span> long term <span class="hlt">climatic</span> evolution at large scales but not local rainfall. The statistics of local precipitation are traditionally <span class="hlt">predicted</span> using historical rainfall data. Obviously these data cannot anticipate changes that result from <span class="hlt">climate</span> change. It is therefore clear that integration of the global information about <span class="hlt">climate</span> evolution and local historical data is needed to provide the much needed <span class="hlt">predictions</span> of regional water availability. Currently, there is no theoretical or computational framework that enables such integration for this region. In this dissertation both a conceptual framework and a computational platform for such integration are introduced. In particular, suite of models that link forecasts of <span class="hlt">climatic</span> evolution under different CO2 emissions scenarios to observed rainfall</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_12");'>12</a></li> <li><a href="#" onclick='return showDiv("page_13");'>13</a></li> <li class="active"><span>14</span></li> <li><a href="#" onclick='return showDiv("page_15");'>15</a></li> <li><a href="#" onclick='return showDiv("page_16");'>16</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_14 --> <div id="page_15" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_13");'>13</a></li> <li><a href="#" onclick='return showDiv("page_14");'>14</a></li> <li class="active"><span>15</span></li> <li><a href="#" onclick='return showDiv("page_16");'>16</a></li> <li><a href="#" onclick='return showDiv("page_17");'>17</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="281"> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70147933','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70147933"><span>The <span class="hlt">predicted</span> influence of <span class="hlt">climate</span> change on lesser prairie-chicken reproductive parameters</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Grisham, Blake A.; Boal, Clint W.; Haukos, David A.; Davis, D.; Boydston, Kathy K.; Dixon, Charles; Heck, Willard R.</p> <p>2013-01-01</p> <p>The Southern High Plains is anticipated to experience significant changes in temperature and precipitation due to <span class="hlt">climate</span> change. These changes may influence the lesser prairie-chicken (Tympanuchus pallidicinctus) in positive or negative ways. We assessed the potential changes in clutch size, incubation start date, and nest survival for lesser prairie-chickens for the years 2050 and 2080 based on modeled <span class="hlt">predictions</span> of <span class="hlt">climate</span> change and reproductive data for lesser prairie-chickens from 2001-2011 on the Southern High Plains of Texas and New Mexico. We developed 9 a priori models to assess the relationship between reproductive parameters and biologically relevant weather conditions. We selected weather variable(s) with the most model support and then obtained future <span class="hlt">predicted</span> values from climatewizard.org. We conducted 1,000 simulations using each reproductive parameter's linear equation obtained from regression calculations, and the future <span class="hlt">predicted</span> value for each weather variable to <span class="hlt">predict</span> future reproductive parameter values for lesser prairie-chickens. There was a high degree of model uncertainty for each reproductive value. Winter temperature had the greatest effect size for all three parameters, suggesting a negative relationship between above-average winter temperature and reproductive output. The above-average winter temperatures are correlated to La Nina events, which negatively affect lesser prairie-chickens through resulting drought conditions. By 2050 and 2080, nest survival was <span class="hlt">predicted</span> to be below levels considered viable for population persistence; however, our assessment did not consider annual survival of adults, chick survival, or the positive benefit of habitat management and conservation, which may ultimately offset the potentially negative effect of drought on nest survival.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015AGUFM.A11F0100L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015AGUFM.A11F0100L"><span>GFDL's unified regional-global weather-<span class="hlt">climate</span> modeling system with variable resolution capability for severe weather <span class="hlt">predictions</span> and regional <span class="hlt">climate</span> simulations</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Lin, S. J.</p> <p>2015-12-01</p> <p>The NOAA/Geophysical Fluid Dynamics Laboratory has been developing a unified regional-global modeling system with variable resolution capabilities that can be used for severe weather <span class="hlt">predictions</span> (e.g., tornado outbreak events and cat-5 hurricanes) and ultra-high-resolution (1-km) regional <span class="hlt">climate</span> simulations within a consistent global modeling framework. The fundation of this flexible regional-global modeling system is the non-hydrostatic extension of the vertically Lagrangian dynamical core (Lin 2004, Monthly Weather Review) known in the community as FV3 (finite-volume on the cubed-sphere). Because of its flexability and computational efficiency, the FV3 is one of the final candidates of NOAA's Next Generation Global <span class="hlt">Prediction</span> System (NGGPS). We have built into the modeling system a stretched (single) grid capability, a two-way (regional-global) multiple nested grid capability, and the combination of the stretched and two-way nests, so as to make convection-resolving regional <span class="hlt">climate</span> simulation within a consistent global modeling system feasible using today's High Performance Computing System. One of our main scientific goals is to enable simulations of high impact weather phenomena (such as tornadoes, thunderstorms, category-5 hurricanes) within an IPCC-class <span class="hlt">climate</span> modeling system previously regarded as impossible. In this presentation I will demonstrate that it is computationally feasible to simulate not only super-cell thunderstorms, but also the subsequent genesis of tornadoes using a global model that was originally designed for century long <span class="hlt">climate</span> simulations. As a unified weather-<span class="hlt">climate</span> modeling system, we evaluated the performance of the model with horizontal resolution ranging from 1 km to as low as 200 km. In particular, for downscaling studies, we have developed various tests to ensure that the large-scale circulation within the global varaible resolution system is well simulated while at the same time the small-scale can be accurately captured</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/25785866','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/25785866"><span><span class="hlt">Climate</span>-based models for pulsed resources improve <span class="hlt">predictability</span> of consumer population dynamics: outbreaks of house mice in forest ecosystems.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Holland, E Penelope; James, Alex; Ruscoe, Wendy A; Pech, Roger P; Byrom, Andrea E</p> <p>2015-01-01</p> <p>Accurate <span class="hlt">predictions</span> of the timing and magnitude of consumer responses to episodic seeding events (masts) are important for understanding ecosystem dynamics and for managing outbreaks of invasive species generated by masts. While models relating consumer populations to resource fluctuations have been developed successfully for a range of natural and modified ecosystems, a critical gap that needs addressing is better <span class="hlt">prediction</span> of resource pulses. A recent model used change in summer temperature from one year to the next (ΔT) for <span class="hlt">predicting</span> masts for forest and grassland plants in New Zealand. We extend this <span class="hlt">climate</span>-based method in the framework of a model for consumer-resource dynamics to <span class="hlt">predict</span> invasive house mouse (Mus musculus) outbreaks in forest ecosystems. Compared with previous mast models based on absolute temperature, the ΔT method for <span class="hlt">predicting</span> masts resulted in an improved model for mouse population dynamics. There was also a threshold effect of ΔT on the likelihood of an outbreak occurring. The improved <span class="hlt">climate</span>-based method for <span class="hlt">predicting</span> resource pulses and consumer responses provides a straightforward rule of thumb for determining, with one year's advance warning, whether management intervention might be required in invaded ecosystems. The approach could be applied to consumer-resource systems worldwide where <span class="hlt">climatic</span> variables are used to model the size and duration of resource pulses, and may have particular relevance for ecosystems where global change scenarios <span class="hlt">predict</span> increased variability in <span class="hlt">climatic</span> events.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012AGUFM.H43A1308F','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012AGUFM.H43A1308F"><span>Potential Seasonal <span class="hlt">Predictability</span> of Water Cycle in Observations and Reanalysis</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Feng, X.; Houser, P.</p> <p>2012-12-01</p> <p>Identification of <span class="hlt">predictability</span> of water cycle variability is crucial for <span class="hlt">climate</span> <span class="hlt">prediction</span>, water resources availability, ecosystem management and hazard mitigation. An analysis that can assess the potential skill in seasonal <span class="hlt">prediction</span> was proposed by the authors, named as analysis of covariance (ANOCOVA). This method tests whether interannual variability of seasonal means exceeds that due to weather noise under the null hypothesis that seasonal means are identical every year. It has the advantage of taking into account autocorrelation structure in the daily time series but also accounting for the uncertainty of the estimated parameters in the significance test. During the past several years, multiple reanalysis datasets have become available for studying <span class="hlt">climate</span> variability and understanding <span class="hlt">climate</span> system. We are motivated to compare the potential <span class="hlt">predictability</span> of water cycle variation from different reanalysis datasets against observations using the newly proposed ANOCOVA method. The selected eight reanalyses include the National Centers for Environmental <span class="hlt">Prediction</span>-National Center for Atmospheric Research (NCEP/NCAR) 40-year Reanalysis Project (NNRP), the National Centers for Environmental <span class="hlt">Prediction</span>-Department of Energy (NCEP/DOE) Reanalysis Project (NDRP), the European Centre for Medium-Range Weather Forecasts (ECMWF) 40-year Reanalysis, The Japan Meteorological Agency 25-year Reanalysis Project (JRA25), the ECMWF) Interim Reanalysis (ERAINT), the NCEP <span class="hlt">Climate</span> Forecast System Reanalysis (CFSR), the National Aeronautics and Space <span class="hlt">Administration</span> (NASA) Modern-Era Retrospective Analysis for Research and Applications (MERRA), and the National Oceanic and Atmospheric <span class="hlt">Administration</span>-Cooperative Institute for Research in Environmental Sciences (NOAA/CIRES) 20th Century Reanalysis Version 2 (20CR). For key water cycle components, precipitation and evaporation, all reanalyses consistently show high fraction of <span class="hlt">predictable</span> variance in the tropics, low</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5358348','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5358348"><span>Selenium deficiency risk <span class="hlt">predicted</span> to increase under future <span class="hlt">climate</span> change</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Jones, Gerrad D.; Droz, Boris; Greve, Peter; Gottschalk, Pia; Poffet, Deyan; McGrath, Steve P.; Seneviratne, Sonia I.; Smith, Pete; Winkel, Lenny H. E.</p> <p>2017-01-01</p> <p>Deficiencies of micronutrients, including essential trace elements, affect up to 3 billion people worldwide. The dietary availability of trace elements is determined largely by their soil concentrations. Until now, the mechanisms governing soil concentrations have been evaluated in small-scale studies, which identify soil physicochemical properties as governing variables. However, global concentrations of trace elements and the factors controlling their distributions are virtually unknown. We used 33,241 soil data points to model recent (1980–1999) global distributions of Selenium (Se), an essential trace element that is required for humans. Worldwide, up to one in seven people have been estimated to have low dietary Se intake. Contrary to small-scale studies, soil Se concentrations were dominated by climate–soil interactions. Using moderate <span class="hlt">climate</span>-change scenarios for 2080–2099, we <span class="hlt">predicted</span> that changes in <span class="hlt">climate</span> and soil organic carbon content will lead to overall decreased soil Se concentrations, particularly in agricultural areas; these decreases could increase the prevalence of Se deficiency. The importance of climate–soil interactions to Se distributions suggests that other trace elements with similar retention mechanisms will be similarly affected by <span class="hlt">climate</span> change. PMID:28223487</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://eric.ed.gov/?q=descriptive+AND+correlation&pg=6&id=EJ1063609','ERIC'); return false;" href="https://eric.ed.gov/?q=descriptive+AND+correlation&pg=6&id=EJ1063609"><span><span class="hlt">Predicting</span> Satisfaction in Physical Education from Motivational <span class="hlt">Climate</span> and Self-Determined Motivation</span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Baena-Extremera, Antonio; Gómez-López, Manuel; Granero-Gallegos, Antonio; Ortiz-Camacho, Maria del Mar</p> <p>2015-01-01</p> <p>The purpose of this research study was to determine to what extent the motivational <span class="hlt">climate</span> perceived by students in Physical Education (PE) classes <span class="hlt">predicts</span> self-determined motivation, and satisfaction with physical education classes. Questionnaires were administered to 758 high school students aged 13-18 years. We used the Spanish versions of…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3306657','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3306657"><span><span class="hlt">Predicting</span> the effect of <span class="hlt">climate</span> change on African trypanosomiasis: integrating epidemiology with parasite and vector biology</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Moore, Sean; Shrestha, Sourya; Tomlinson, Kyle W.; Vuong, Holly</p> <p>2012-01-01</p> <p><span class="hlt">Climate</span> warming over the next century is expected to have a large impact on the interactions between pathogens and their animal and human hosts. Vector-borne diseases are particularly sensitive to warming because temperature changes can alter vector development rates, shift their geographical distribution and alter transmission dynamics. For this reason, African trypanosomiasis (sleeping sickness), a vector-borne disease of humans and animals, was recently identified as one of the 12 infectious diseases likely to spread owing to <span class="hlt">climate</span> change. We combine a variety of direct effects of temperature on vector ecology, vector biology and vector–parasite interactions via a disease transmission model and extrapolate the potential compounding effects of projected warming on the epidemiology of African trypanosomiasis. The model <span class="hlt">predicts</span> that epidemics can occur when mean temperatures are between 20.7°C and 26.1°C. Our model does not <span class="hlt">predict</span> a large-range expansion, but rather a large shift of up to 60 per cent in the geographical extent of the range. The model also <span class="hlt">predicts</span> that 46–77 million additional people may be at risk of exposure by 2090. Future research could expand our analysis to include other environmental factors that influence tsetse populations and disease transmission such as humidity, as well as changes to human, livestock and wildlife distributions. The modelling approach presented here provides a framework for using the <span class="hlt">climate</span>-sensitive aspects of vector and pathogen biology to <span class="hlt">predict</span> changes in disease prevalence and risk owing to <span class="hlt">climate</span> change. PMID:22072451</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70048483','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70048483"><span>Validating <span class="hlt">predictions</span> from <span class="hlt">climate</span> envelope models</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Watling, J.; Bucklin, D.; Speroterra, C.; Brandt, L.; Cabal, C.; Romañach, Stephanie S.; Mazzotti, Frank J.</p> <p>2013-01-01</p> <p><span class="hlt">Climate</span> envelope models are a potentially important conservation tool, but their ability to accurately forecast species’ distributional shifts using independent survey data has not been fully evaluated. We created <span class="hlt">climate</span> envelope models for 12 species of North American breeding birds previously shown to have experienced poleward range shifts. For each species, we evaluated three different approaches to <span class="hlt">climate</span> envelope modeling that differed in the way they treated <span class="hlt">climate</span>-induced range expansion and contraction, using random forests and maximum entropy modeling algorithms. All models were calibrated using occurrence data from 1967–1971 (t1) and evaluated using occurrence data from 1998–2002 (t2). Model sensitivity (the ability to correctly classify species presences) was greater using the maximum entropy algorithm than the random forest algorithm. Although sensitivity did not differ significantly among approaches, for many species, sensitivity was maximized using a hybrid approach that assumed range expansion, but not contraction, in t2. Species for which the hybrid approach resulted in the greatest improvement in sensitivity have been reported from more land cover types than species for which there was little difference in sensitivity between hybrid and dynamic approaches, suggesting that habitat generalists may be buffered somewhat against <span class="hlt">climate</span>-induced range contractions. Specificity (the ability to correctly classify species absences) was maximized using the random forest algorithm and was lowest using the hybrid approach. Overall, our results suggest cautious optimism for the use of <span class="hlt">climate</span> envelope models to forecast range shifts, but also underscore the importance of considering non-<span class="hlt">climate</span> drivers of species range limits. The use of alternative <span class="hlt">climate</span> envelope models that make different assumptions about range expansion and contraction is a new and potentially useful way to help inform our understanding of <span class="hlt">climate</span> change effects on species.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4214750','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4214750"><span><span class="hlt">Climate</span> Change Simulations <span class="hlt">Predict</span> Altered Biotic Response in a Thermally Heterogeneous Stream System</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Westhoff, Jacob T.; Paukert, Craig P.</p> <p>2014-01-01</p> <p><span class="hlt">Climate</span> change is <span class="hlt">predicted</span> to increase water temperatures in many lotic systems, but little is known about how changes in air temperature affect lotic systems heavily influenced by groundwater. Our objectives were to document spatial variation in temperature for spring-fed Ozark streams in Southern Missouri USA, create a spatially explicit model of mean daily water temperature, and use downscaled <span class="hlt">climate</span> models to <span class="hlt">predict</span> the number of days meeting suitable stream temperature for three aquatic species of concern to conservation and management. Longitudinal temperature transects and stationary temperature loggers were used in the Current and Jacks Fork Rivers during 2012 to determine spatial and temporal variability of water temperature. Groundwater spring influence affected river water temperatures in both winter and summer, but springs that contributed less than 5% of the main stem discharge did not affect river temperatures beyond a few hundred meters downstream. A multiple regression model using variables related to season, mean daily air temperature, and a spatial influence factor (metric to account for groundwater influence) was a strong predictor of mean daily water temperature (r2 = 0.98; RMSE = 0.82). Data from two downscaled <span class="hlt">climate</span> simulations under the A2 emissions scenario were used to <span class="hlt">predict</span> daily water temperatures for time steps of 1995, 2040, 2060, and 2080. By 2080, peak numbers of optimal growth temperature days for smallmouth bass are expected to shift to areas with more spring influence, largemouth bass are expected to experience more optimal growth days (21 – 317% increase) regardless of spring influence, and Ozark hellbenders may experience a reduction in the number of optimal growth days in areas with the highest spring influence. Our results provide a framework for assessing fine-scale (10 s m) thermal heterogeneity and <span class="hlt">predict</span> shifts in thermal conditions at the watershed and reach scale. PMID:25356982</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2010EGUGA..12.3854B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2010EGUGA..12.3854B"><span>An <span class="hlt">prediction</span> and explanation of '<span class="hlt">climatic</span> swing</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Barkin, Yury</p> <p>2010-05-01</p> <p>Introduction. In works of the author [1, 2] the mechanism has been offered and the scenario of formation of congelations and warming of the Earth and their inversion and asymmetric displays in opposite hemispheres has been described. These planetary thermal processes are connected with gravitational forced oscillations of the core-mantle system of the Earth, controlling and directing submission of heat in the top layers of the mantle and on a surface of the Earth. It is shown, that action of this mechanism should observed in various time scales. In particular significant changes of a <span class="hlt">climate</span> should occur to the thousand-year periods, with the periods in tens and hundred thousand years. Thus excitation of system the core-mantle is caused by planetary secular orbital perturbations and by perturbations of the Earth rotation which as is known are characterized by significant amplitudes. But also in a short time scale the <span class="hlt">climate</span> variations with the interannual and decade periods also should be observed, how dynamic consequences of the swing of the core-mantle system of the Earth with the same periods [3]. The fundamental phenomenon of secular polar drift of the core relatively to the viscous-elastic and changeable mantle [4] in last years has obtained convincing confirmations various geosciences. Reliable an attribute of influence of oscillations of the core on a variation of natural processes is their property of inversion when, for example, activity of process accrues in northern hemisphere and decreases in a southern hemisphere. Such contrast secular changes in northern and southern (N/S) hemispheres have been <span class="hlt">predicted</span> on the base of geodynamic model [1] and revealed according to observations: from gravimetry measurements of a gravity [5]; in determination of a secular trend of a sea level, as global, and in northern and southern hemispheres [6, 7]; in redistribution of air masses [6, 8]; in geodetic measurements of changes of average radiuses of northern and</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013AGUFMGC12C..02S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013AGUFMGC12C..02S"><span>Tracking Expected Improvements of Decadal <span class="hlt">Prediction</span> in <span class="hlt">Climate</span> Services</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Suckling, E.; Thompson, E.; Smith, L. A.</p> <p>2013-12-01</p> <p>Physics-based simulation models are ultimately expected to provide the best available (decision-relevant) probabilistic <span class="hlt">climate</span> <span class="hlt">predictions</span>, as they can capture the dynamics of the Earth System across a range of situations, situations for which observations for the construction of empirical models are scant if not nonexistent. This fact in itself provides neither evidence that <span class="hlt">predictions</span> from today's Earth Systems Models will outperform today's empirical models, nor a guide to the space and time scales on which today's model <span class="hlt">predictions</span> are adequate for a given purpose. Empirical (data-based) models are employed to make probability forecasts on decadal timescales. The skill of these forecasts is contrasted with that of state-of-the-art <span class="hlt">climate</span> models, and the challenges faced by each approach are discussed. The focus is on providing decision-relevant probability forecasts for decision support. An empirical model, known as Dynamic Climatology is shown to be competitive with CMIP5 <span class="hlt">climate</span> models on decadal scale probability forecasts. Contrasting the skill of simulation models not only with each other but also with empirical models can reveal the space and time scales on which a generation of simulation models exploits their physical basis effectively. It can also quantify their ability to add information in the formation of operational forecasts. Difficulties (i) of information contamination (ii) of the interpretation of probabilistic skill and (iii) of artificial skill complicate each modelling approach, and are discussed. "Physics free" empirical models provide fixed, quantitative benchmarks for the evaluation of ever more complex <span class="hlt">climate</span> models, that is not available from (inter)comparisons restricted to only complex models. At present, empirical models can also provide a background term for blending in the formation of probability forecasts from ensembles of simulation models. In weather forecasting this role is filled by the climatological distribution, and</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3551960','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3551960"><span><span class="hlt">Predicting</span> the Impact of <span class="hlt">Climate</span> Change on Threatened Species in UK Waters</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Jones, Miranda C.; Dye, Stephen R.; Fernandes, Jose A.; Frölicher, Thomas L.; Pinnegar, John K.; Warren, Rachel; Cheung, William W. L.</p> <p>2013-01-01</p> <p>Global <span class="hlt">climate</span> change is affecting the distribution of marine species and is thought to represent a threat to biodiversity. Previous studies project expansion of species range for some species and local extinction elsewhere under <span class="hlt">climate</span> change. Such range shifts raise concern for species whose long-term persistence is already threatened by other human disturbances such as fishing. However, few studies have attempted to assess the effects of future <span class="hlt">climate</span> change on threatened vertebrate marine species using a multi-model approach. There has also been a recent surge of interest in <span class="hlt">climate</span> change impacts on protected areas. This study applies three species distribution models and two sets of <span class="hlt">climate</span> model projections to explore the potential impacts of <span class="hlt">climate</span> change on marine species by 2050. A set of species in the North Sea, including seven threatened and ten major commercial species were used as a case study. Changes in habitat suitability in selected candidate protected areas around the UK under future <span class="hlt">climatic</span> scenarios were assessed for these species. Moreover, change in the degree of overlap between commercial and threatened species ranges was calculated as a proxy of the potential threat posed by overfishing through bycatch. The ensemble projections suggest northward shifts in species at an average rate of 27 km per decade, resulting in small average changes in range overlap between threatened and commercially exploited species. Furthermore, the adverse consequences of <span class="hlt">climate</span> change on the habitat suitability of protected areas were projected to be small. Although the models show large variation in the <span class="hlt">predicted</span> consequences of <span class="hlt">climate</span> change, the multi-model approach helps identify the potential risk of increased exposure to human stressors of critically endangered species such as common skate (Dipturus batis) and angelshark (Squatina squatina). PMID:23349829</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/23349829','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/23349829"><span><span class="hlt">Predicting</span> the impact of <span class="hlt">climate</span> change on threatened species in UK waters.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Jones, Miranda C; Dye, Stephen R; Fernandes, Jose A; Frölicher, Thomas L; Pinnegar, John K; Warren, Rachel; Cheung, William W L</p> <p>2013-01-01</p> <p>Global <span class="hlt">climate</span> change is affecting the distribution of marine species and is thought to represent a threat to biodiversity. Previous studies project expansion of species range for some species and local extinction elsewhere under <span class="hlt">climate</span> change. Such range shifts raise concern for species whose long-term persistence is already threatened by other human disturbances such as fishing. However, few studies have attempted to assess the effects of future <span class="hlt">climate</span> change on threatened vertebrate marine species using a multi-model approach. There has also been a recent surge of interest in <span class="hlt">climate</span> change impacts on protected areas. This study applies three species distribution models and two sets of <span class="hlt">climate</span> model projections to explore the potential impacts of <span class="hlt">climate</span> change on marine species by 2050. A set of species in the North Sea, including seven threatened and ten major commercial species were used as a case study. Changes in habitat suitability in selected candidate protected areas around the UK under future <span class="hlt">climatic</span> scenarios were assessed for these species. Moreover, change in the degree of overlap between commercial and threatened species ranges was calculated as a proxy of the potential threat posed by overfishing through bycatch. The ensemble projections suggest northward shifts in species at an average rate of 27 km per decade, resulting in small average changes in range overlap between threatened and commercially exploited species. Furthermore, the adverse consequences of <span class="hlt">climate</span> change on the habitat suitability of protected areas were projected to be small. Although the models show large variation in the <span class="hlt">predicted</span> consequences of <span class="hlt">climate</span> change, the multi-model approach helps identify the potential risk of increased exposure to human stressors of critically endangered species such as common skate (Dipturus batis) and angelshark (Squatina squatina).</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29851600','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29851600"><span><span class="hlt">Climate</span> services for health: <span class="hlt">predicting</span> the evolution of the 2016 dengue season in Machala, Ecuador.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Lowe, Rachel; Stewart-Ibarra, Anna M; Petrova, Desislava; García-Díez, Markel; Borbor-Cordova, Mercy J; Mejía, Raúl; Regato, Mary; Rodó, Xavier</p> <p>2017-07-01</p> <p>El Niño and its effect on local meteorological conditions potentially influences interannual variability in dengue transmission in southern coastal Ecuador. El Oro province is a key dengue surveillance site, due to the high burden of dengue, seasonal transmission, co-circulation of all four dengue serotypes, and the recent introduction of chikungunya and Zika. In this study, we used <span class="hlt">climate</span> forecasts to <span class="hlt">predict</span> the evolution of the 2016 dengue season in the city of Machala, following one of the strongest El Niño events on record. We incorporated precipitation, minimum temperature, and Niño3·4 index forecasts in a Bayesian hierarchical mixed model to <span class="hlt">predict</span> dengue incidence. The model was initiated on Jan 1, 2016, producing monthly dengue forecasts until November, 2016. We accounted for misreporting of dengue due to the introduction of chikungunya in 2015, by using active surveillance data to correct reported dengue case data from passive surveillance records. We then evaluated the forecast retrospectively with available epidemiological information. The <span class="hlt">predictions</span> correctly forecast an early peak in dengue incidence in March, 2016, with a 90% chance of exceeding the mean dengue incidence for the previous 5 years. Accounting for the proportion of chikungunya cases that had been incorrectly recorded as dengue in 2015 improved the <span class="hlt">prediction</span> of the magnitude of dengue incidence in 2016. This dengue <span class="hlt">prediction</span> framework, which uses seasonal <span class="hlt">climate</span> and El Niño forecasts, allows a <span class="hlt">prediction</span> to be made at the start of the year for the entire dengue season. Combining active surveillance data with routine dengue reports improved not only model fit and performance, but also the accuracy of benchmark estimates based on historical seasonal averages. This study advances the state-of-the-art of <span class="hlt">climate</span> services for the health sector, by showing the potential value of incorporating <span class="hlt">climate</span> information in the public health decision-making process in Ecuador. European Union</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFMGC51A1120O','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFMGC51A1120O"><span>Application of a GCM Ensemble Seasonal <span class="hlt">Climate</span> Forecasts to Crop Yield <span class="hlt">Prediction</span> in East Africa</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Ogutu, G.; Franssen, W.; Supit, I.; Hutjes, R. W. A.</p> <p>2016-12-01</p> <p>We evaluated the potential use of ECMWF System-4 seasonal <span class="hlt">climate</span> forecasts (S4) for impacts analysis over East Africa. Using the 15 member, 7 months ensemble forecasts initiated every month for 1981-2010, we tested precipitation (tp), air temperature (tas) and surface shortwave radiation (rsds) forecast skill against the WATCH forcing Data ERA-Interim (WFDEI) re-analysis and other data. We used these forecasts as input in the WOFOST crop model to <span class="hlt">predict</span> maize yields. Forecast skill is assessed using anomaly correlation (ACC), Ranked Probability Skill Score (RPSS) and the Relative Operating Curve Skill Score (ROCSS) for MAM, JJA and OND growing seasons. <span class="hlt">Predicted</span> maize yields (S4-yields) are verified against historical observed FAO and nationally reported (NAT) yield statistics, and yields from the same crop model forced by WFDEI (WFDEI-yields). <span class="hlt">Predictability</span> of the <span class="hlt">climate</span> forecasts vary with season, location and lead-time. The OND tp forecasts show skill over a larger area up to three months lead-time compared to MAM and JJA. Upper- and lower-tercile tp forecasts are 20-80% better than climatology. Good tas forecast skill is apparent with three months lead-time. The rsds is less skillful than tp and tas in all seasons when verified against WFDEI but higher against others. S4-forecasts captures ENSO related anomalous years with region dependent skill. Anomalous ENSO influence is also seen in simulated yields. Focussing on the main sowing dates in the northern (July), equatorial (March-April) and southern (December) regions, WFDEI-yields are lower than FAO and NAT but anomalies are comparable. Yield anomalies are <span class="hlt">predictable</span> 3-months before sowing in most of the regions. Differences in interannual variability in the range of ±40% may be related to sensitivity of WOFOST to drought stress while the ACCs are largely positive ranging from 0.3 to 0.6. Above and below-normal yields are <span class="hlt">predictable</span> with 2-months lead time. We evidenced a potential use of seasonal</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.cpc.ncep.noaa.gov/products/predictions/610day/fxus06.html','SCIGOVWS'); return false;" href="http://www.cpc.ncep.noaa.gov/products/predictions/610day/fxus06.html"><span><span class="hlt">Climate</span> <span class="hlt">Prediction</span> Center - 6-10 and 8-14 Day Prognostic Discussions</span></a></p> <p><a target="_blank" href="http://www.science.gov/aboutsearch.html">Science.gov Websites</a></p> <p></p> <p></p> <p>About Us Our Mission Who We Are Contact Us CPC <em>Information</em> CPC Web Team 6-10 Day outlooks are issued DISCUSSIONS FOR 6 TO 10 AND 8 TO 14 DAY OUTLOOKS NWS <span class="hlt">CLIMATE</span> <span class="hlt">PREDICTION</span> CENTER <em>COLLEGE</em> PARK MD 300 PM EDT SAT CONSISTENCY ISSUES. IN THESE CASES, FORECASTS ARE MANUALLY DRAWN BUT <em>A</em> FULL DISCUSSION IS NOT ISSUED. THE</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2006CliPD...2..979L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2006CliPD...2..979L"><span><span class="hlt">Predicting</span> Pleistocene <span class="hlt">climate</span> from vegetation</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Loehle, C.</p> <p>2006-10-01</p> <p><span class="hlt">Climates</span> at the Last Glacial Maximum have been inferred from fossil pollen assemblages, but these inferred <span class="hlt">climates</span> are colder than those produced by <span class="hlt">climate</span> simulations. Biogeographic evidence also argues against these inferred cold <span class="hlt">climates</span>. The recolonization of glaciated zones in eastern North America following the last ice age produced distinct biogeographic patterns. It has been assumed that a wide zone south of the ice was tundra or boreal parkland (Boreal-Parkland Zone or BPZ), which would have been recolonized from southern refugia as the ice melted, but the patterns in this zone differ from those in the glaciated zone, which creates a major biogeographic anomaly. In the glacial zone, there are few endemics but in the BPZ there are many across multiple taxa. In the glacial zone, there are the expected gradients of genetic diversity with distance from the ice-free zone, but no evidence of this is found in the BPZ. Many races and related species exist in the BPZ which would have merged or hybridized if confined to the same refugia. Evidence for distinct southern refugia for most temperate species is lacking. Extinctions of temperate flora were rare. The interpretation of spruce as a boreal <span class="hlt">climate</span> indicator may be mistaken over much of the region if the spruce was actually an extinct temperate species. All of these anomalies call into question the concept that <span class="hlt">climates</span> in the zone south of the ice were very cold or that temperate species had to migrate far to the south. Similar anomalies exist in Europe and on tropical mountains. An alternate hypothesis is that low CO2 levels gave an advantage to pine and spruce, which are the dominant trees in the BPZ, and to herbaceous species over trees, which also fits the observed pattern. Most temperate species could have survived across their current ranges at lower abundance by retreating to moist microsites. These would be microrefugia not easily detected by pollen records, especially if most species became rare</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFM.A41M..07A','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFM.A41M..07A"><span>Multi-scale enhancement of <span class="hlt">climate</span> <span class="hlt">prediction</span> over land by improving the model sensitivity to vegetation variability</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Alessandri, A.; Catalano, F.; De Felice, M.; Hurk, B. V. D.; Doblas-Reyes, F. J.; Boussetta, S.; Balsamo, G.; Miller, P. A.</p> <p>2017-12-01</p> <p>Here we demonstrate, for the first time, that the implementation of a realistic representation of vegetation in Earth System Models (ESMs) can significantly improve <span class="hlt">climate</span> simulation and <span class="hlt">prediction</span> across multiple time-scales. The effective sub-grid vegetation fractional coverage vary seasonally and at interannual time-scales in response to leaf-canopy growth, phenology and senescence. Therefore it affects biophysical parameters such as the surface resistance to evapotranspiration, albedo, roughness lenght, and soil field capacity. To adequately represent this effect in the EC-Earth ESM, we included an exponential dependence of the vegetation cover on the Leaf Area Index.By comparing two sets of simulations performed with and without the new variable fractional-coverage parameterization, spanning from centennial (20th Century) simulations and retrospective <span class="hlt">predictions</span> to the decadal (5-years), seasonal (2-4 months) and weather (4 days) time-scales, we show for the first time a significant multi-scale enhancement of vegetation impacts in <span class="hlt">climate</span> simulation and <span class="hlt">prediction</span> over land. Particularly large effects at multiple time scales are shown over boreal winter middle-to-high latitudes over Canada, West US, Eastern Europe, Russia and eastern Siberia due to the implemented time-varying shadowing effect by tree-vegetation on snow surfaces. Over Northern Hemisphere boreal forest regions the improved representation of vegetation-cover consistently correct the winter warm biases, improves the <span class="hlt">climate</span> change sensitivity, the decadal potential <span class="hlt">predictability</span> as well as the skill of forecasts at seasonal and weather time-scales. Significant improvements of the <span class="hlt">prediction</span> of 2m temperature and rainfall are also shown over transitional land surface hot spots. Both the potential <span class="hlt">predictability</span> at decadal time-scale and seasonal-forecasts skill are enhanced over Sahel, North American Great Plains, Nordeste Brazil and South East Asia, mainly related to improved performance in</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014AGUFM.A13G3268M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014AGUFM.A13G3268M"><span>Decadal <span class="hlt">prediction</span> of European soil moisture from 1961 to 2010 using a regional <span class="hlt">climate</span> model</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Mieruch-Schnuelle, S.; Schädler, G.; Feldmann, H.</p> <p>2014-12-01</p> <p>The German national research program on decadal <span class="hlt">climate</span> <span class="hlt">prediction</span>(MiKlip) aims at the development of an operational decadal predictionsystem. To explore the potential of decadal <span class="hlt">predictions</span> a hindcastensemble from 1961 to 2010 has been generated by the MPI-ESM, the newEarth system model of the Max Planck Institute for Meteorology. Toimprove the decadal <span class="hlt">predictions</span> on higher spatial resolutions wedownscaled the MPI-ESM simulations by the regional model COSMO-CLM(CCLM) for Europe. In this study we will characterize and validatethe <span class="hlt">predictability</span> of extreme states of soil moisture in Europesimulated by the MPI-ESM and the value added by the CCLM. The wateramount stored in the soil is a crucial component of the <span class="hlt">climate</span> systemand especially important for agriculture, and has an influence onevaporation, groundwater and runoff. Thus, skillful <span class="hlt">prediction</span> of soilmoisture in the order of years up to a decade could be used tomitigate risk and benefit society. Since soil moisture observationsare rare and validation of model output is difficult, we will ratherinvestigate the effective drought index (EDI), which can be retrievedsolely from precipitation data. Therefore we show that the EDI is agood estimator of the soil water content.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3708951','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3708951"><span>The <span class="hlt">Predicted</span> Influence of <span class="hlt">Climate</span> Change on Lesser Prairie-Chicken Reproductive Parameters</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Grisham, Blake A.; Boal, Clint W.; Haukos, David A.; Davis, Dawn M.; Boydston, Kathy K.; Dixon, Charles; Heck, Willard R.</p> <p>2013-01-01</p> <p>The Southern High Plains is anticipated to experience significant changes in temperature and precipitation due to <span class="hlt">climate</span> change. These changes may influence the lesser prairie-chicken (Tympanuchus pallidicinctus) in positive or negative ways. We assessed the potential changes in clutch size, incubation start date, and nest survival for lesser prairie-chickens for the years 2050 and 2080 based on modeled <span class="hlt">predictions</span> of <span class="hlt">climate</span> change and reproductive data for lesser prairie-chickens from 2001–2011 on the Southern High Plains of Texas and New Mexico. We developed 9 a priori models to assess the relationship between reproductive parameters and biologically relevant weather conditions. We selected weather variable(s) with the most model support and then obtained future <span class="hlt">predicted</span> values from climatewizard.org. We conducted 1,000 simulations using each reproductive parameter’s linear equation obtained from regression calculations, and the future <span class="hlt">predicted</span> value for each weather variable to <span class="hlt">predict</span> future reproductive parameter values for lesser prairie-chickens. There was a high degree of model uncertainty for each reproductive value. Winter temperature had the greatest effect size for all three parameters, suggesting a negative relationship between above-average winter temperature and reproductive output. The above-average winter temperatures are correlated to La Niña events, which negatively affect lesser prairie-chickens through resulting drought conditions. By 2050 and 2080, nest survival was <span class="hlt">predicted</span> to be below levels considered viable for population persistence; however, our assessment did not consider annual survival of adults, chick survival, or the positive benefit of habitat management and conservation, which may ultimately offset the potentially negative effect of drought on nest survival. PMID:23874549</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_13");'>13</a></li> <li><a href="#" onclick='return showDiv("page_14");'>14</a></li> <li class="active"><span>15</span></li> <li><a href="#" onclick='return showDiv("page_16");'>16</a></li> <li><a href="#" onclick='return showDiv("page_17");'>17</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_15 --> <div id="page_16" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_14");'>14</a></li> <li><a href="#" onclick='return showDiv("page_15");'>15</a></li> <li class="active"><span>16</span></li> <li><a href="#" onclick='return showDiv("page_17");'>17</a></li> <li><a href="#" onclick='return showDiv("page_18");'>18</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="301"> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/23874549','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/23874549"><span>The <span class="hlt">predicted</span> influence of <span class="hlt">climate</span> change on lesser prairie-chicken reproductive parameters.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Grisham, Blake A; Boal, Clint W; Haukos, David A; Davis, Dawn M; Boydston, Kathy K; Dixon, Charles; Heck, Willard R</p> <p>2013-01-01</p> <p>The Southern High Plains is anticipated to experience significant changes in temperature and precipitation due to <span class="hlt">climate</span> change. These changes may influence the lesser prairie-chicken (Tympanuchus pallidicinctus) in positive or negative ways. We assessed the potential changes in clutch size, incubation start date, and nest survival for lesser prairie-chickens for the years 2050 and 2080 based on modeled <span class="hlt">predictions</span> of <span class="hlt">climate</span> change and reproductive data for lesser prairie-chickens from 2001-2011 on the Southern High Plains of Texas and New Mexico. We developed 9 a priori models to assess the relationship between reproductive parameters and biologically relevant weather conditions. We selected weather variable(s) with the most model support and then obtained future <span class="hlt">predicted</span> values from climatewizard.org. We conducted 1,000 simulations using each reproductive parameter's linear equation obtained from regression calculations, and the future <span class="hlt">predicted</span> value for each weather variable to <span class="hlt">predict</span> future reproductive parameter values for lesser prairie-chickens. There was a high degree of model uncertainty for each reproductive value. Winter temperature had the greatest effect size for all three parameters, suggesting a negative relationship between above-average winter temperature and reproductive output. The above-average winter temperatures are correlated to La Niña events, which negatively affect lesser prairie-chickens through resulting drought conditions. By 2050 and 2080, nest survival was <span class="hlt">predicted</span> to be below levels considered viable for population persistence; however, our assessment did not consider annual survival of adults, chick survival, or the positive benefit of habitat management and conservation, which may ultimately offset the potentially negative effect of drought on nest survival.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2010AGUFM.H51A0874B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2010AGUFM.H51A0874B"><span>Optimal selection of MULTI-model downscaled ensembles for interannual and seasonal <span class="hlt">climate</span> <span class="hlt">prediction</span> in the eastern seaboard of Thailand</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Bejranonda, W.; Koch, M.</p> <p>2010-12-01</p> <p>Because of the imminent threat of the water resources of the eastern seaboard of Thailand, a <span class="hlt">climate</span> impact study has been carried out there. To that avail, a hydrological watershed model is being used to simulate the future water availability in the wake of possible <span class="hlt">climate</span> change in the region. The hydrological model is forced by <span class="hlt">predictions</span> from global <span class="hlt">climate</span> models (GCMs) that are to be downscaled in an appropriate manner. The challenge at that stage of the <span class="hlt">climate</span> impact analysis lies then the in the choice of the best GCM and the (statistical) downscaling method. In this study the selection of coarse grid resolution output of the GCMs, transferring information to the fine grid of local <span class="hlt">climate</span>-hydrology is achieved by cross-correlation and multiple linear regression using meteorological data in the eastern seaboard of Thailand observed between 1970-1999. The grids of 20 atmosphere/ocean global <span class="hlt">climate</span> models (AOGCM), covering latitude 12.5-15.0 N and longitude 100.0-102.5 E were examined using the <span class="hlt">Climate</span>-Change Scenario Generator (SCENGEN). With that tool the model efficiency of the <span class="hlt">prediction</span> of daily precipitation and mean temperature was calculated by comparing the 1980-1999 ECMWF reanalysis <span class="hlt">predictions</span> with the observed data during that time period. The root means square errors of the <span class="hlt">predictions</span> were considered and ranked to select the top 5 models, namely, BCCR-BCM2.0, GISS-ER, ECHO-G, ECHAM5/MPI-OM and PCM. The daily time-series of 338 predictors in 9 runs of the 5 selected models were gathered from the CMIP3 multi-model database. Monthly time-serial cross-correlations between the <span class="hlt">climate</span> predictors and the meteorological measurements from 25 rainfall, 4 minimum and maximum temperature, 4 humidity and 2 solar radiation stations in the study area were then computed and ranked. Using the ranked predictors, a multiple-linear regression model (downscaling transfer model) to forecast the local <span class="hlt">climate</span> was set up. To improve the <span class="hlt">prediction</span> power of this</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29615005','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29615005"><span>Improving risk <span class="hlt">prediction</span> accuracy for new soldiers in the U.S. Army by adding self-report survey data to <span class="hlt">administrative</span> data.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Bernecker, Samantha L; Rosellini, Anthony J; Nock, Matthew K; Chiu, Wai Tat; Gutierrez, Peter M; Hwang, Irving; Joiner, Thomas E; Naifeh, James A; Sampson, Nancy A; Zaslavsky, Alan M; Stein, Murray B; Ursano, Robert J; Kessler, Ronald C</p> <p>2018-04-03</p> <p>High rates of mental disorders, suicidality, and interpersonal violence early in the military career have raised interest in implementing preventive interventions with high-risk new enlistees. The Army Study to Assess Risk and Resilience in Servicemembers (STARRS) developed risk-targeting systems for these outcomes based on machine learning methods using <span class="hlt">administrative</span> data predictors. However, <span class="hlt">administrative</span> data omit many risk factors, raising the question whether risk targeting could be improved by adding self-report survey data to <span class="hlt">prediction</span> models. If so, the Army may gain from routinely administering surveys that assess additional risk factors. The STARRS New Soldier Survey was administered to 21,790 Regular Army soldiers who agreed to have survey data linked to <span class="hlt">administrative</span> records. As reported previously, machine learning models using <span class="hlt">administrative</span> data as predictors found that small proportions of high-risk soldiers accounted for high proportions of negative outcomes. Other machine learning models using self-report survey data as predictors were developed previously for three of these outcomes: major physical violence and sexual violence perpetration among men and sexual violence victimization among women. Here we examined the extent to which this survey information increases <span class="hlt">prediction</span> accuracy, over models based solely on <span class="hlt">administrative</span> data, for those three outcomes. We used discrete-time survival analysis to estimate a series of models <span class="hlt">predicting</span> first occurrence, assessing how model fit improved and concentration of risk increased when adding the <span class="hlt">predicted</span> risk score based on survey data to the <span class="hlt">predicted</span> risk score based on <span class="hlt">administrative</span> data. The addition of survey data improved <span class="hlt">prediction</span> significantly for all outcomes. In the most extreme case, the percentage of reported sexual violence victimization among the 5% of female soldiers with highest <span class="hlt">predicted</span> risk increased from 17.5% using only <span class="hlt">administrative</span> predictors to 29.4% adding survey</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012EGUGA..14...79K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012EGUGA..14...79K"><span><span class="hlt">Climate</span> extremes in the Pacific: improving seasonal <span class="hlt">prediction</span> of tropical cyclones and extreme ocean temperatures to improve resilience</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Kuleshov, Y.; Jones, D.; Spillman, C. M.</p> <p>2012-04-01</p> <p><span class="hlt">Climate</span> change and <span class="hlt">climate</span> extremes have a major impact on Australia and Pacific Island countries. Of particular concern are tropical cyclones and extreme ocean temperatures, the first being the most destructive events for terrestrial systems, while the latter has the potential to devastate ocean ecosystems through coral bleaching. As a practical response to <span class="hlt">climate</span> change, under the Pacific-Australia <span class="hlt">Climate</span> Change Science and Adaptation Planning program (PACCSAP), we are developing enhanced web-based information tools for providing seasonal forecasts for <span class="hlt">climatic</span> extremes in the Western Pacific. Tropical cyclones are the most destructive weather systems that impact on coastal areas. Interannual variability in the intensity and distribution of tropical cyclones is large, and presently greater than any trends that are ascribable to <span class="hlt">climate</span> change. In the warming environment, <span class="hlt">predicting</span> tropical cyclone occurrence based on historical relationships, with predictors such as sea surface temperatures (SSTs) now frequently lying outside of the range of past variability meaning that it is not possible to find historical analogues for the seasonal conditions often faced by Pacific countries. Elevated SSTs are the primary trigger for mass coral bleaching events, which can lead to widespread damage and mortality on reef systems. Degraded coral reefs present many problems, including long-term loss of tourism and potential loss or degradation of fisheries. The monitoring and <span class="hlt">prediction</span> of thermal stress events enables the support of a range of adaptive and management activities that could improve reef resilience to extreme conditions. Using the <span class="hlt">climate</span> model POAMA (<span class="hlt">Predictive</span> Ocean-Atmosphere Model for Australia), we aim to improve accuracy of seasonal forecasts of tropical cyclone activity and extreme SSTs for the regions of Western Pacific. Improved knowledge of extreme <span class="hlt">climatic</span> events, with the assistance of tailored forecast tools, will help enhance the resilience and</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70148592','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70148592"><span>Darcy’s law <span class="hlt">predicts</span> widespread forest mortality under <span class="hlt">climate</span> warming</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>McDowell, Nate G.; Allen, Craig D.</p> <p>2015-01-01</p> <p>Drought and heat-induced tree mortality is accelerating in many forest biomes as a consequence of a warming <span class="hlt">climate</span>, resulting in a threat to global forests unlike any in recorded history. Forests store the majority of terrestrial carbon, thus their loss may have significant and sustained impacts on the global carbon cycle. We use a hydraulic corollary to Darcy’s law, a core principle of vascular plant physiology, to <span class="hlt">predict</span> characteristics of plants that will survive and die during drought under warmer future <span class="hlt">climates</span>. Plants that are tall with isohydric stomatal regulation, low hydraulic conductance, and high leaf area are most likely to die from future drought stress. Thus, tall trees of old-growth forests are at the greatest risk of loss, which has ominous implications for terrestrial carbon storage. This application of Darcy’s law indicates today’s forests generally should be replaced by shorter and more xeric plants, owing to future warmer droughts and associated wildfires and pest attacks. The Darcy’s corollary also provides a simple, robust framework for informing forest management interventions needed to promote the survival of current forests. Given the robustness of Darcy’s law for <span class="hlt">predictions</span> of vascular plant function, we conclude with high certainty that today’s forests are going to be subject to continued increases in mortality rates that will result in substantial reorganization of their structure and carbon storage.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFMGC33D1099S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFMGC33D1099S"><span>Development of <span class="hlt">predictive</span> weather scenarios for early <span class="hlt">prediction</span> of rice yield in South Korea</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Shin, Y.; Cho, J.; Jung, I.</p> <p>2017-12-01</p> <p>International grain prices are becoming unstable due to frequent occurrence of abnormal weather phenomena caused by <span class="hlt">climate</span> change. Early <span class="hlt">prediction</span> of grain yield using weather forecast data is important for stabilization of international grain prices. The APEC <span class="hlt">Climate</span> Center (APCC) is providing seasonal forecast data based on monthly <span class="hlt">climate</span> <span class="hlt">prediction</span> models for global seasonal forecasting services. The 3-month and 6-month seasonal forecast data using the multi-model ensemble (MME) technique are provided in their own website, ADSS (APCC Data Service System, http://adss.apcc21.org/). The spatial resolution of seasonal forecast data for each individual model is 2.5°×2.5°(about 250km) and the time scale is created as monthly. In this study, we developed customized weather forecast scenarios that are combined seasonal forecast data and observational data apply to early rice yield <span class="hlt">prediction</span> model. Statistical downscale method was applied to produce meteorological input data of crop model because field scale crop model (ORYZA2000) requires daily weather data. In order to determine whether the forecasting data is suitable for the crop model, we produced spatio-temporal downscaled weather scenarios and evaluated the <span class="hlt">predictability</span> by comparison with observed weather data at 57 ASOS stations in South Korea. The customized weather forecast scenarios can be applied to various application fields not only early rice yield <span class="hlt">prediction</span>. Acknowledgement This work was carried out with the support of "Cooperative Research Program for Agriculture Science and Technology Development (Project No: PJ012855022017)" Rural Development <span class="hlt">Administration</span>, Republic of Korea.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/23364210','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/23364210"><span>The combination of work organizational <span class="hlt">climate</span> and individual work commitment <span class="hlt">predicts</span> return to work in women but not in men.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Holmgren, Kristina; Ekbladh, Elin; Hensing, Gunnel; Dellve, Lotta</p> <p>2013-02-01</p> <p>To analyze if the combination of organizational <span class="hlt">climate</span> and work commitment can <span class="hlt">predict</span> return to work (RTW). This prospective Swedish study was based on 2285 participants, 19 to 64 years old, consecutively selected from the employed population, newly sick-listed for more than 14 days. Data were collected in 2008 through postal questionnaire and from register data. Among women, the combination of good organizational <span class="hlt">climate</span> and fair work commitment <span class="hlt">predicted</span> an early RTW with an adjusted relative risk of 2.05 (1.32 to 3.18). Among men, none of the adjusted variables or combinations of variables was found significantly to <span class="hlt">predict</span> RTW. This study demonstrated the importance of integrative effects of organizational <span class="hlt">climate</span> and individual work commitment on RTW among women. These factors did not <span class="hlt">predict</span> RTW in men. More research is needed to understand the RTW process among men.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://eric.ed.gov/?q=strategies+AND+learning&pg=2&id=EJ1099886','ERIC'); return false;" href="https://eric.ed.gov/?q=strategies+AND+learning&pg=2&id=EJ1099886"><span><span class="hlt">Predicting</span> High School Student Use of Learning Strategies: The Role of Preferred Learning Styles and Classroom <span class="hlt">Climate</span></span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Cheema, Jehanzeb; Kitsantas, Anastasia</p> <p>2016-01-01</p> <p>This study investigated the <span class="hlt">predictiveness</span> of preferred learning styles (competitive and cooperative) and classroom <span class="hlt">climate</span> (teacher support and disciplinary <span class="hlt">climate</span>) on learning strategy use in mathematics. The student survey part of the Programme for International Student Assessment 2003 comprising of 4633 US observations was used in a weighted…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/servlets/purl/889817','SCIGOV-STC'); return false;" href="https://www.osti.gov/servlets/purl/889817"><span><span class="hlt">Predicting</span> Coupled Ocean-Atmosphere Modes with a <span class="hlt">Climate</span> Modeling Hierarchy -- Final Report</span></a></p> <p><a target="_blank" href="http://www.osti.gov/search">DOE Office of Scientific and Technical Information (OSTI.GOV)</a></p> <p>Michael Ghil, UCLA; Andrew W. Robertson, IRI, Columbia Univ.; Sergey Kravtsov, U. of Wisconsin, Milwaukee</p> <p></p> <p>The goal of the project was to determine midlatitude <span class="hlt">climate</span> <span class="hlt">predictability</span> associated with tropical-extratropical interactions on interannual-to-interdecadal time scales. Our strategy was to develop and test a hierarchy of <span class="hlt">climate</span> models, bringing together large GCM-based <span class="hlt">climate</span> models with simple fluid-dynamical coupled ocean-ice-atmosphere models, through the use of advanced probabilistic network (PN) models. PN models were used to develop a new diagnostic methodology for analyzing coupled ocean-atmosphere interactions in large <span class="hlt">climate</span> simulations made with the NCAR Parallel <span class="hlt">Climate</span> Model (PCM), and to make these tools user-friendly and available to other researchers. We focused on interactions between the tropics and extratropics throughmore » atmospheric teleconnections (the Hadley cell, Rossby waves and nonlinear circulation regimes) over both the North Atlantic and North Pacific, and the ocean’s thermohaline circulation (THC) in the Atlantic. We tested the hypothesis that variations in the strength of the THC alter sea surface temperatures in the tropical Atlantic, and that the latter influence the atmosphere in high latitudes through an atmospheric teleconnection, feeding back onto the THC. The PN model framework was used to mediate between the understanding gained with simplified primitive equations models and multi-century simulations made with the PCM. The project team is interdisciplinary and built on an existing synergy between atmospheric and ocean scientists at UCLA, computer scientists at UCI, and <span class="hlt">climate</span> researchers at the IRI.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017EGUGA..1915934V','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017EGUGA..1915934V"><span>Evaluation of a new CNRM-CM6 model version for seasonal <span class="hlt">climate</span> <span class="hlt">predictions</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Volpi, Danila; Ardilouze, Constantin; Batté, Lauriane; Dorel, Laurant; Guérémy, Jean-François; Déqué, Michel</p> <p>2017-04-01</p> <p>This work presents the quality assessment of a new version of the Météo-France coupled <span class="hlt">climate</span> <span class="hlt">prediction</span> system, which has been developed in the EU COPERNICUS <span class="hlt">Climate</span> Change Services framework to carry out seasonal forecast. The system is based on the CNRM-CM6 model, with Arpege-Surfex 6.2.2 as atmosphere/land component and Nemo 3.2 as ocean component, which has directly embedded the sea-ice component Gelato 6.0. In order to have a robust diagnostic, the experiment is composed by 60 ensemble members generated with stochastic dynamic perturbations. The experiment has been performed over a 37-year re-forecast period from 1979 to 2015, with two start dates per year, respectively in May 1st and November 1st. The evaluation of the <span class="hlt">predictive</span> skill of the model is shown under two perspectives: on the one hand, the ability of the model to faithfully respond to positive or negative ENSO, NAO and QBO events, independently of the <span class="hlt">predictability</span> of these events. Such assessment is carried out through a composite analysis, and shows that the model succeeds in reproducing the main patterns for 2-meter temperature, precipitation and geopotential height at 500 hPa during the winter season. On the other hand, the model <span class="hlt">predictive</span> skill of the same events (positive and negative ENSO, NAO and QBO) is evaluated.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012EGUGA..14.2064C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012EGUGA..14.2064C"><span>Simulating infectious disease risk based on <span class="hlt">climatic</span> drivers: from numerical weather <span class="hlt">prediction</span> to long term <span class="hlt">climate</span> change scenario</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Caminade, C.; Ndione, J. A.; Diallo, M.; MacLeod, D.; Faye, O.; Ba, Y.; Dia, I.; Medlock, J. M.; Leach, S.; McIntyre, K. M.; Baylis, M.; Morse, A. P.</p> <p>2012-04-01</p> <p><span class="hlt">Climate</span> variability is an important component in determining the incidence of a number of diseases with significant health and socioeconomic impacts. In particular, vector born diseases are the most likely to be affected by <span class="hlt">climate</span>; directly via the development rates and survival of both the pathogen and the vector, and indirectly through changes in the surrounding environmental conditions. Disease risk models of various complexities using different streams of <span class="hlt">climate</span> forecasts as inputs have been developed within the QWeCI EU and ENHanCE ERA-NET project frameworks. This work will present two application examples, one for Africa and one for Europe. First, we focus on Rift Valley fever over sub-Saharan Africa, a zoonosis that affects domestic animals and humans by causing an acute fever. We show that the Rift Valley fever outbreak that occurred in late 2010 in the northern Sahelian region of Mauritania might have been anticipated ten days in advance using the GFS numerical weather <span class="hlt">prediction</span> system. Then, an ensemble of regional <span class="hlt">climate</span> projections is employed to model the <span class="hlt">climatic</span> suitability of the Asian tiger mosquito for the future over Europe. The Asian tiger mosquito is an invasive species originally from Asia which is able to transmit West Nile and Chikungunya Fever among others. This species has spread worldwide during the last decades, mainly through the shipments of goods from Asia. Different disease models are employed and inter-compared to achieve such a task. Results show that the <span class="hlt">climatic</span> conditions over southern England, central Western Europe and the Balkans might become more suitable for the mosquito (including the proviso that the mosquito has already been introduced) to establish itself in the future.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70037586','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70037586"><span><span class="hlt">Predicted</span> effects of <span class="hlt">climate</span> warming on the distribution of 50 stream fishes in Wisconsin, U.S.A.</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Lyons, J.; Stewart, J.S.; Mitro, M.</p> <p>2010-01-01</p> <p>Summer air and stream water temperatures are expected to rise in the state of Wisconsin, U.S.A., over the next 50 years. To assess potential <span class="hlt">climate</span> warming effects on stream fishes, <span class="hlt">predictive</span> models were developed for 50 common fish species using classification-tree analysis of 69 environmental variables in a geographic information system. Model accuracy was 56.0-93.5% in validation tests. Models were applied to all 86 898 km of stream in the state under four different <span class="hlt">climate</span> scenarios: current conditions, limited <span class="hlt">climate</span> warming (summer air temperatures increase 1?? C and water 0.8?? C), moderate warming (air 3?? C and water 2.4?? C) and major warming (air 5?? C and water 4?? C). With <span class="hlt">climate</span> warming, 23 fishes were <span class="hlt">predicted</span> to decline in distribution (three to extirpation under the major warming scenario), 23 to increase and four to have no change. Overall, declining species lost substantially more stream length than increasing species gained. All three cold-water and 16 cool-water fishes and four of 31 warm-water fishes were <span class="hlt">predicted</span> to decline, four warm-water fishes to remain the same and 23 warm-water fishes to increase in distribution. Species changes were <span class="hlt">predicted</span> to be most dramatic in small streams in northern Wisconsin that currently have cold to cool summer water temperatures and are dominated by cold-water and cool-water fishes, and least in larger and warmer streams and rivers in southern Wisconsin that are currently dominated by warm-water fishes. Results of this study suggest that even small increases in summer air and water temperatures owing to <span class="hlt">climate</span> warming will have major effects on the distribution of stream fishes in Wisconsin. ?? 2010 The Authors. Journal of Fish Biology ?? 2010 The Fisheries Society of the British Isles.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://onlinelibrary.wiley.com/doi/10.1111/j.1095-8649.2010.02763.x/full','USGSPUBS'); return false;" href="http://onlinelibrary.wiley.com/doi/10.1111/j.1095-8649.2010.02763.x/full"><span><span class="hlt">Predicted</span> effects of <span class="hlt">climate</span> warming on the distribution of 50 stream fishes in Wisconsin, U.S.A.</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Stewart, Jana S.; Lyons, John D.; Matt Mitro,</p> <p>2010-01-01</p> <p>Summer air and stream water temperatures are expected to rise in the state of Wisconsin, U.S.A., over the next 50 years. To assess potential <span class="hlt">climate</span> warming effects on stream fishes, <span class="hlt">predictive</span> models were developed for 50 common fish species using classification-tree analysis of 69 environmental variables in a geographic information system. Model accuracy was 56·0–93·5% in validation tests. Models were applied to all 86 898 km of stream in the state under four different <span class="hlt">climate</span> scenarios: current conditions, limited <span class="hlt">climate</span> warming (summer air temperatures increase 1° C and water 0·8° C), moderate warming (air 3° C and water 2·4° C) and major warming (air 5° C and water 4° C). With <span class="hlt">climate</span> warming, 23 fishes were <span class="hlt">predicted</span> to decline in distribution (three to extirpation under the major warming scenario), 23 to increase and four to have no change. Overall, declining species lost substantially more stream length than increasing species gained. All three cold-water and 16 cool-water fishes and four of 31 warm-water fishes were <span class="hlt">predicted</span> to decline, four warm-water fishes to remain the same and 23 warm-water fishes to increase in distribution. Species changes were <span class="hlt">predicted</span> to be most dramatic in small streams in northern Wisconsin that currently have cold to cool summer water temperatures and are dominated by cold-water and cool-water fishes, and least in larger and warmer streams and rivers in southern Wisconsin that are currently dominated by warm-water fishes. Results of this study suggest that even small increases in summer air and water temperatures owing to <span class="hlt">climate</span> warming will have major effects on the distribution of stream fishes in Wisconsin.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29876079','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29876079"><span>Age and area <span class="hlt">predict</span> patterns of species richness in pumice rafts contingent on oceanic <span class="hlt">climatic</span> zone encountered.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Velasquez, Eleanor; Bryan, Scott E; Ekins, Merrick; Cook, Alex G; Hurrey, Lucy; Firn, Jennifer</p> <p>2018-05-01</p> <p>The theory of island biogeography <span class="hlt">predicts</span> that area and age explain species richness patterns (or alpha diversity) in insular habitats. Using a unique natural phenomenon, pumice rafting, we measured the influence of area, age, and oceanic <span class="hlt">climate</span> on patterns of species richness. Pumice rafts are formed simultaneously when submarine volcanoes erupt, the pumice clasts breakup irregularly, forming irregularly shaped pumice stones which while floating through the ocean are colonized by marine biota. We analyze two eruption events and more than 5,000 pumice clasts collected from 29 sites and three <span class="hlt">climatic</span> zones. Overall, the older and larger pumice clasts held more species. Pumice clasts arriving in tropical and subtropical <span class="hlt">climates</span> showed this same trend, where in temperate locations species richness (alpha diversity) increased with area but decreased with age. Beta diversity analysis of the communities forming on pumice clasts that arrived in different <span class="hlt">climatic</span> zones showed that tropical and subtropical clasts transported similar communities, while species composition on temperate clasts differed significantly from both tropical and subtropical arrivals. Using these thousands of insular habitats, we find strong evidence that area and age but also <span class="hlt">climatic</span> conditions <span class="hlt">predict</span> the fundamental dynamics of species richness colonizing pumice clasts.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19900010409','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19900010409"><span>Regional <span class="hlt">climate</span> change <span class="hlt">predictions</span> from the Goddard Institute for Space Studies high resolution GCM</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Crane, Robert G.; Hewitson, Bruce</p> <p>1990-01-01</p> <p>Model simulations of global <span class="hlt">climate</span> change are seen as an essential component of any program aimed at understanding human impact on the global environment. A major weakness of current general circulation models (GCMs), however, is their inability to <span class="hlt">predict</span> reliably the regional consequences of a global scale change, and it is these regional scale <span class="hlt">predictions</span> that are necessary for studies of human/environmental response. This research is directed toward the development of a methodology for the validation of the synoptic scale climatology of GCMs. This is developed with regard to the Goddard Institute for Space Studies (GISS) GCM Model 2, with the specific objective of using the synoptic circulation form a doubles CO2 simulation to estimate regional <span class="hlt">climate</span> change over North America, south of Hudson Bay. This progress report is specifically concerned with validating the synoptic climatology of the GISS GCM, and developing the transfer function to derive grid-point temperatures from the synoptic circulation. Principal Components Analysis is used to characterize the primary modes of the spatial and temporal variability in the observed and simulated <span class="hlt">climate</span>, and the model validation is based on correlations between component loadings, and power spectral analysis of the component scores. The results show that the high resolution GISS model does an excellent job of simulating the synoptic circulation over the U.S., and that grid-point temperatures can be <span class="hlt">predicted</span> with reasonable accuracy from the circulation patterns.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFMGC51A1131K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFMGC51A1131K"><span>High resolution crop growth simulation for identification of potential adaptation strategies under <span class="hlt">climate</span> change</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Kim, K. S.; Yoo, B. H.</p> <p>2016-12-01</p> <p>Impact assessment of <span class="hlt">climate</span> change on crop production would facilitate planning of adaptation strategies. Because socio-environmental conditions would differ by local areas, it would be advantageous to assess potential adaptation measures at a specific area. The objectives of this study was to develop a crop growth simulation system at a very high spatial resolution, e.g., 30 m, and to assess different adaptation options including shift of planting date and use of different cultivars. The Decision Support System for Agrotechnology Transfer (DSSAT) model was used to <span class="hlt">predict</span> yields of soybean and maize in Korea. Gridded data for <span class="hlt">climate</span> and soil were used to prepare input data for the DSSAT model. Weather input data were prepared at the resolution of 30 m using bilinear interpolation from gridded <span class="hlt">climate</span> scenario data. Those <span class="hlt">climate</span> data were obtained from Korean Meteorology <span class="hlt">Administration</span>. Spatial resolution of temperature and precipitation was 1 km whereas that of solar radiation was 12.5 km. Soil series data at the 30 m resolution were obtained from the soil database operated by Rural Development <span class="hlt">Administration</span>, Korea. The SOL file, which is a soil input file for the DSSAT model was prepared using physical and chemical properties of a given soil series, which were available from the soil database. Crop yields were <span class="hlt">predicted</span> by potential adaptation options based on planting date and cultivar. For example, 10 planting dates and three cultivars were used to identify ideal management options for <span class="hlt">climate</span> change adaptation. In <span class="hlt">prediction</span> of maize yield, combination of 20 planting dates and two cultivars was used as management options. <span class="hlt">Predicted</span> crop yields differed by site even within a relatively small region. For example, the maximum of average yields for 2001-2010 seasons differed by sites In a county of which areas is 520 km2 (Fig. 1). There was also spatial variation in the ideal management option in the region (Fig. 2). These results suggested that local</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29867087','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29867087"><span>Model structures amplify uncertainty in <span class="hlt">predicted</span> soil carbon responses to <span class="hlt">climate</span> change.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Shi, Zheng; Crowell, Sean; Luo, Yiqi; Moore, Berrien</p> <p>2018-06-04</p> <p>Large model uncertainty in projected future soil carbon (C) dynamics has been well documented. However, our understanding of the sources of this uncertainty is limited. Here we quantify the uncertainties arising from model parameters, structures and their interactions, and how those uncertainties propagate through different models to projections of future soil carbon stocks. Both the vertically resolved model and the microbial explicit model project much greater uncertainties to <span class="hlt">climate</span> change than the conventional soil C model, with both positive and negative C-<span class="hlt">climate</span> feedbacks, whereas the conventional model consistently <span class="hlt">predicts</span> positive soil C-<span class="hlt">climate</span> feedback. Our findings suggest that diverse model structures are necessary to increase confidence in soil C projection. However, the larger uncertainty in the complex models also suggests that we need to strike a balance between model complexity and the need to include diverse model structures in order to forecast soil C dynamics with high confidence and low uncertainty.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2011HESSD...810825R','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2011HESSD...810825R"><span>Applying a simple water-energy balance framework to <span class="hlt">predict</span> the <span class="hlt">climate</span> sensitivity of streamflow over the continental United States</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Renner, M.; Bernhofer, C.</p> <p>2011-12-01</p> <p>The <span class="hlt">prediction</span> of <span class="hlt">climate</span> effects on terrestrial ecosystems and water resources is one of the major research questions in hydrology. Conceptual water-energy balance models can be used to gain a first order estimate of how long-term average streamflow is changing with a change in water and energy supply. A common framework for investigation of this question is based on the Budyko hypothesis, which links hydrological response to aridity. Recently, Renner et al. (2011) introduced the CCUW hypothesis, which is based on the assumption that the total efficiency of the catchment ecosystem to use the available water and energy for actual evapotranspiration remains constant even under <span class="hlt">climate</span> changes. Here, we confront the <span class="hlt">climate</span> sensitivity approaches (including several versions of Budyko's approach and the CCUW) with data of more than 400 basins distributed over the continental United States. We first map an estimate of the sensitivity of streamflow to changes in precipitation using long-term average data of the period 1949-2003. This provides a hydro-<span class="hlt">climatic</span> status of the respective basins as well as their expected proportional effect on changes in <span class="hlt">climate</span>. Next, by splitting the data in two periods, we (i) analyse the long-term average changes in hydro-climatolgy, we (ii) use the different <span class="hlt">climate</span> sensitivity methods to <span class="hlt">predict</span> the change in streamflow given the observed changes in water and energy supply and (iii) we apply a quantitative approach to separate the impacts of changes in the long-term average <span class="hlt">climate</span> from basin characteristics change on streamflow. This allows us to evaluate the observed changes in streamflow as well as to evaluate the impact of basin changes on the validity of <span class="hlt">climate</span> sensitivity approaches. The apparent increase of streamflow in the majority of basins in the US is dominated by a <span class="hlt">climate</span> trend towards increased humidity. It is further evident that impacts of changes in basin characteristics appear in parallel with <span class="hlt">climate</span> changes. There</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.aphis.usda.gov/wildlife_damage/nwrc/symposia/invasive_symposium/content/Rodda138_145_MVIS.pdf','USGSPUBS'); return false;" href="https://www.aphis.usda.gov/wildlife_damage/nwrc/symposia/invasive_symposium/content/Rodda138_145_MVIS.pdf"><span><span class="hlt">Climate</span> matching as a tool for <span class="hlt">predicting</span> potential North American spread of Brown Treesnakes</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Rodda, Gordon H.; Reed, Robert N.; Jarnevich, Catherine S.; Witmer, G.W.; Pitt, W. C.; Fagerstone, K.A.</p> <p>2007-01-01</p> <p><span class="hlt">Climate</span> matching identifies extralimital destinations that could be colonized by a potential invasive species on the basis of similarity to <span class="hlt">climates</span> found in the species’ native range. <span class="hlt">Climate</span> is a proxy for the factors that determine whether a population will reproduce enough to offset mortality. Previous <span class="hlt">climate</span> matching models (e.g., Genetic Algorithm for Rule-set <span class="hlt">Prediction</span> [GARP]) for brown treesnakes (Boiga irregularis) were unsatisfactory, perhaps because the models failed to allow different combinations of <span class="hlt">climate</span> attributes to influence a species’ range limits in different parts of the range. Therefore, we explored the <span class="hlt">climate</span> space described by bivariate parameters of native range temperature and rainfall, allowing up to two months of aestivation in the warmer portions of the range, or four months of hibernation in temperate climes. We found colonization area to be minimally sensitive to assumptions regarding hibernation temperature thresholds. Although brown treesnakes appear to be limited by dry weather in the interior of Australia, aridity rarely limits potential distribution in most of the world. Potential colonization area in North America is limited primarily by cold. <span class="hlt">Climatically</span> suitable portions of the United States (US) mainland include the Central Valley of California, mesic patches in the Southwest, and the southeastern coastal plain from Texas to Virginia.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/26747843','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/26747843"><span><span class="hlt">Predicting</span> the genetic consequences of future <span class="hlt">climate</span> change: The power of coupling spatial demography, the coalescent, and historical landscape changes.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Brown, Jason L; Weber, Jennifer J; Alvarado-Serrano, Diego F; Hickerson, Michael J; Franks, Steven J; Carnaval, Ana C</p> <p>2016-01-01</p> <p><span class="hlt">Climate</span> change is a widely accepted threat to biodiversity. Species distribution models (SDMs) are used to forecast whether and how species distributions may track these changes. Yet, SDMs generally fail to account for genetic and demographic processes, limiting population-level inferences. We still do not understand how <span class="hlt">predicted</span> environmental shifts will impact the spatial distribution of genetic diversity within taxa. We propose a novel method that <span class="hlt">predicts</span> spatially explicit genetic and demographic landscapes of populations under future <span class="hlt">climatic</span> conditions. We use carefully parameterized SDMs as estimates of the spatial distribution of suitable habitats and landscape dispersal permeability under present-day, past, and future conditions. We use empirical genetic data and approximate Bayesian computation to estimate unknown demographic parameters. Finally, we employ these parameters to simulate realistic and complex models of responses to future environmental shifts. We contrast parameterized models under current and future landscapes to quantify the expected magnitude of change. We implement this framework on neutral genetic data available from Penstemon deustus. Our results <span class="hlt">predict</span> that future <span class="hlt">climate</span> change will result in geographically widespread declines in genetic diversity in this species. The extent of reduction will heavily depend on the continuity of population networks and deme sizes. To our knowledge, this is the first study to provide spatially explicit <span class="hlt">predictions</span> of within-species genetic diversity using <span class="hlt">climatic</span>, demographic, and genetic data. Our approach accounts for <span class="hlt">climatic</span>, geographic, and biological complexity. This framework is promising for understanding evolutionary consequences of <span class="hlt">climate</span> change, and guiding conservation planning. © 2016 Botanical Society of America.</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_14");'>14</a></li> <li><a href="#" onclick='return showDiv("page_15");'>15</a></li> <li class="active"><span>16</span></li> <li><a href="#" onclick='return showDiv("page_17");'>17</a></li> <li><a href="#" onclick='return showDiv("page_18");'>18</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_16 --> <div id="page_17" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_15");'>15</a></li> <li><a href="#" onclick='return showDiv("page_16");'>16</a></li> <li class="active"><span>17</span></li> <li><a href="#" onclick='return showDiv("page_18");'>18</a></li> <li><a href="#" onclick='return showDiv("page_19");'>19</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="321"> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013EGUGA..1514247S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013EGUGA..1514247S"><span>Towards a Seamless Framework for Drought Analysis and <span class="hlt">Prediction</span> from Seasonal to <span class="hlt">Climate</span> Change Time Scales (Plinius Medal Lecture)</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Sheffield, Justin</p> <p>2013-04-01</p> <p>Droughts arguably cause the most impacts of all natural hazards in terms of the number of people affected and the long-term economic costs and ecosystem stresses. Recent droughts worldwide have caused humanitarian and economic problems such as food insecurity across the Horn of Africa, agricultural economic losses across the central US and loss of livelihoods in rural western India. The prospect of future increases in drought severity and duration driven by projected changes in precipitation patterns and increasing temperatures is worrisome. Some evidence for <span class="hlt">climate</span> change impacts on drought is already being seen for some regions, such as the Mediterranean and east Africa. Mitigation of the impacts of drought requires advance warning of developing conditions and enactment of drought plans to reduce vulnerability. A key element of this is a drought early warning system that at its heart is the capability to monitor evolving hydrological conditions and water resources storage, and provide reliable and robust <span class="hlt">predictions</span> out to several months, as well as the capacity to act on this information. At longer time scales, planning and policy-making need to consider the potential impacts of <span class="hlt">climate</span> change and its impact on drought risk, and do this within the context of natural <span class="hlt">climate</span> variability, which is likely to dominate any <span class="hlt">climate</span> change signal over the next few decades. There are several challenges that need to be met to advance our capability to provide both early warning at seasonal time scales and risk assessment under <span class="hlt">climate</span> change, regionally and globally. Advancing our understanding of drought <span class="hlt">predictability</span> and risk requires knowledge of drought at all time scales. This includes understanding of past drought occurrence, from the paleoclimate record to the recent past, and understanding of drought mechanisms, from initiation, through persistence to recovery and translation of this understanding to <span class="hlt">predictive</span> models. Current approaches to monitoring and</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3520996','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3520996"><span><span class="hlt">Predicting</span> the Distribution of Commercially Important Invertebrate Stocks under Future <span class="hlt">Climate</span></span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Russell, Bayden D.; Connell, Sean D.; Mellin, Camille; Brook, Barry W.; Burnell, Owen W.; Fordham, Damien A.</p> <p>2012-01-01</p> <p>The future management of commercially exploited species is challenging because techniques used to <span class="hlt">predict</span> the future distribution of stocks under <span class="hlt">climate</span> change are currently inadequate. We projected the future distribution and abundance of two commercially harvested abalone species (blacklip abalone, Haliotis rubra and greenlip abalone, H. laevigata) inhabiting coastal South Australia, using multiple species distribution models (SDM) and for decadal time slices through to 2100. Projections are based on two contrasting global greenhouse gas emissions scenarios. The SDMs identified August (winter) Sea Surface Temperature (SST) as the best descriptor of abundance and forecast that warming of winter temperatures under both scenarios may be beneficial to both species by allowing increased abundance and expansion into previously uninhabited coasts. This range expansion is unlikely to be realised, however, as projected warming of March SST is projected to exceed temperatures which cause up to 10-fold increases in juvenile mortality. By linking fine-resolution forecasts of sea surface temperature under different <span class="hlt">climate</span> change scenarios to SDMs and physiological experiments, we provide a practical first approximation of the potential impact of <span class="hlt">climate</span>-induced change on two species of marine invertebrates in the same fishery. PMID:23251326</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/biblio/57432-workshop-satellite-situ-observations-climate-prediction','SCIGOV-STC'); return false;" href="https://www.osti.gov/biblio/57432-workshop-satellite-situ-observations-climate-prediction"><span>Workshop on Satellite and In situ Observations for <span class="hlt">Climate</span> <span class="hlt">Prediction</span></span></a></p> <p><a target="_blank" href="http://www.osti.gov/search">DOE Office of Scientific and Technical Information (OSTI.GOV)</a></p> <p>Acker, J.G.; Busalacchi, A.</p> <p>1995-02-01</p> <p>Participants in this workshop, which convened in Venice, Italy, 6-8 May 1993, met to consider the current state of <span class="hlt">climate</span> monitoring programs and instrumentation for the purpose of climatological <span class="hlt">prediction</span> on short-term (seasonal to interannual) timescales. Data quality and coverage requirements for definition of oceanographic heat and momentum fluxes, scales of inter- and intra-annual variability, and land-ocean-atmosphere exchange processes were examined. Advantages and disadvantages of earth-based and spaceborne monitoring systems were considered, as were the structures for future monitoring networks, research programs, and modeling studies.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=19950045311&hterms=climate+exchange&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D30%26Ntt%3Dclimate%2Bexchange','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=19950045311&hterms=climate+exchange&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D30%26Ntt%3Dclimate%2Bexchange"><span>Workshop on Satellite and In situ Observations for <span class="hlt">Climate</span> <span class="hlt">Prediction</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Acker, James G.; Busalacchi, Antonio</p> <p>1995-01-01</p> <p>Participants in this workshop, which convened in Venice, Italy, 6-8 May 1993, met to consider the current state of <span class="hlt">climate</span> monitoring programs and instrumentation for the purpose of climatological <span class="hlt">prediction</span> on short-term (seasonal to interannual) timescales. Data quality and coverage requirements for definition of oceanographic heat and momentum fluxes, scales of inter- and intra-annual variability, and land-ocean-atmosphere exchange processes were examined. Advantages and disadvantages of earth-based and spaceborne monitoring systems were considered, as were the structures for future monitoring networks, research programs, and modeling studies.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/28395705','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/28395705"><span>Validation of Nurse Practitioner Primary Care Organizational <span class="hlt">Climate</span> Questionnaire: A New Tool to Study Nurse Practitioner Practice Settings.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Poghosyan, Lusine; Chaplin, William F; Shaffer, Jonathan A</p> <p>2017-04-01</p> <p>Favorable organizational <span class="hlt">climate</span> in primary care settings is necessary to expand the nurse practitioner (NP) workforce and promote their practice. Only one NP-specific tool, the Nurse Practitioner Primary Care Organizational <span class="hlt">Climate</span> Questionnaire (NP-PCOCQ), measures NP organizational <span class="hlt">climate</span>. We confirmed NP-PCOCQ's factor structure and established its <span class="hlt">predictive</span> validity. A crosssectional survey design was used to collect data from 314 NPs in Massachusetts in 2012. Confirmatory factor analysis and regression models were used. The 4-factor model characterized NP-PCOCQ. The NP-PCOCQ score <span class="hlt">predicted</span> job satisfaction (beta = .36; p < .001) and intent to leave job (odds ratio = .28; p = .011). NP-PCOCQ can be used by researchers to produce new evidence and by <span class="hlt">administrators</span> to assess organizational <span class="hlt">climate</span> in their clinics. Further testing of NP-PCOCQ is needed.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFM.A41P..07R','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFM.A41P..07R"><span>Atmospheric Rivers in Europe: impacts, <span class="hlt">predictability</span>, and future <span class="hlt">climate</span> scenarios</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Ramos, A. M.; Tome, R.; Sousa, P. M.; Liberato, M. L. R.; Lavers, D.; Trigo, R. M.</p> <p>2017-12-01</p> <p>In recent years a strong relationship has been found between Atmospheric Rivers (ARs) and extreme precipitation and floods across western Europe, with some regions having 8 of their top 10 annual maxima precipitation events related to ARs. In the particular case of the Iberian Peninsula, the association between ARs and extreme precipitation days in the western river basins is noteworthy, while for the eastern and southern basins the impact of ARs is reduced. An automated ARs detection algorithm is used for the North Atlantic Ocean Basin, allowing the identification of major ARs affecting western European coasts in the present <span class="hlt">climate</span> and under different <span class="hlt">climate</span> change scenarios. We have used both reanalyzes and six General Circulation models under three <span class="hlt">climate</span> scenarios (the control simulation, the RCP4.5 and RCP8.5 scenarios). The western coast of Europe was divided into five domains, namely the Iberian Peninsula, France, UK, Southern Scandinavia and the Netherlands, and Northern Scandinavia. It was found that there is an increase in the vertically integrated horizontal water transport which led to an increase in the AR frequency, a result more visible in the high emission scenarios (RCP8.5) for the 2074-2099 period. Since ARs are associated with high impact weather, it is important to study their <span class="hlt">predictability</span>. This assessment was performed with the ECMWF ensemble forecasts up to 10 days for winters 2013/14, 2014/15 and 2015/16 for events that made landfall in the Iberian Peninsula. We show the model's potential added value to detect upcoming ARs events, which is particularly useful to <span class="hlt">predict</span> potential hydrometeorological extremes. AcknowledgementsThis work was supported by the project FORLAND - Hydrogeomorphologic risk in Portugal: driving forces and application for land use planning [PTDC / ATPGEO / 1660/2014] funded by the Portuguese Foundation for Science and Technology (FCT), Portugal. A. M. Ramos was also supported by a FCT postdoctoral grant (FCT</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014JARS....8.3572N','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014JARS....8.3572N"><span>Fine-spatial scale <span class="hlt">predictions</span> of understory species using <span class="hlt">climate</span>- and LiDAR-derived terrain and canopy metrics</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Nijland, Wiebe; Nielsen, Scott E.; Coops, Nicholas C.; Wulder, Michael A.; Stenhouse, Gordon B.</p> <p>2014-01-01</p> <p>Food and habitat resources are critical components of wildlife management and conservation efforts. The grizzly bear (Ursus arctos) has diverse diets and habitat requirements particularly for understory plant species, which are impacted by human developments and forest management activities. We use light detection and ranging (LiDAR) data to <span class="hlt">predict</span> the occurrence of 14 understory plant species relevant to bear forage and compare our <span class="hlt">predictions</span> with more conventional <span class="hlt">climate</span>- and land cover-based models. We use boosted regression trees to model each of the 14 understory species across 4435 km2 using occurrence (presence-absence) data from 1941 field plots. Three sets of models were fitted: <span class="hlt">climate</span> only, <span class="hlt">climate</span> and basic land and forest covers from Landsat 30-m imagery, and a <span class="hlt">climate</span>- and LiDAR-derived model describing both the terrain and forest canopy. Resulting model accuracies varied widely among species. Overall, 8 of 14 species models were improved by including the LiDAR-derived variables. For <span class="hlt">climate</span>-only models, mean annual precipitation and frost-free periods were the most important variables. With inclusion of LiDAR-derived attributes, depth-to-water table, terrain-intercepted annual radiation, and elevation were most often selected. This suggests that fine-scale terrain conditions affect the distribution of the studied species more than canopy conditions.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFM.P33C2896C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFM.P33C2896C"><span>Formation of Valley Networks in a Cold and Icy Early Mars <span class="hlt">Climate</span>: <span class="hlt">Predictions</span> for Erosion Rates and Channel Morphology</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Cassanelli, J.</p> <p>2017-12-01</p> <p>Mars is host to a diverse array of valley networks, systems of linear-to-sinuous depressions which are widely distributed across the surface and which exhibit branching patterns similar to the dendritic drainage patterns of terrestrial fluvial systems. Characteristics of the valley networks are indicative of an origin by fluvial activity, providing among the most compelling evidence for the past presence of flowing liquid water on the surface of Mars. Stratigraphic and crater age dating techniques suggest that the formation of the valley networks occurred predominantly during the early geologic history of Mars ( 3.7 Ga). However, whether the valley networks formed predominantly by rainfall in a relatively warm and wet early Mars <span class="hlt">climate</span>, or by snowmelt and episodic rainfall in an ambient cold and icy <span class="hlt">climate</span>, remains disputed. Understanding the formative environment of the valley networks will help distinguish between these warm and cold end-member early Mars <span class="hlt">climate</span> models. Here we test a conceptual model for channel incision and evolution under cold and icy conditions with a substrate characterized by the presence of an ice-free dry active layer and subjacent ice-cemented regolith, similar to that found in the Antarctic McMurdo Dry Valleys. We implement numerical thermal models, quantitative erosion and transport estimates, and morphometric analyses in order to outline <span class="hlt">predictions</span> for (1) the precise nature and structure of the substrate, (2) fluvial erosion/incision rates, and (3) channel morphology. Model <span class="hlt">predictions</span> are compared against morphologic and morphometric observational data to evaluate consistency with the assumed cold <span class="hlt">climate</span> scenario. In the cold <span class="hlt">climate</span> scenario, the substrate is <span class="hlt">predicted</span> to be characterized by a kilometers-thick globally-continuous cryosphere below a 50-100 meter thick desiccated ice-free zone. Initial results suggest that, with the <span class="hlt">predicted</span> substrate structure, fluvial channel erosion and morphology in a cold early Mars</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29239569','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29239569"><span><span class="hlt">Climate</span> impact on malaria in northern Burkina Faso.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Tourre, Yves M; Vignolles, Cécile; Viel, Christian; Mounier, Flore</p> <p>2017-11-27</p> <p>The Paluclim project managed by the French Centre National d'Etudes Spatiales (CNES) found that total rainfall for a 3-month period is a confounding factor for the density of malaria vectors in the region of Nouna in the Sahel <span class="hlt">administrative</span> territory of northern Burkina Faso. Following the models introduced in 1999 by Craig et al. and in 2003 by Tanser et al., a <span class="hlt">climate</span> impact model for malaria risk (using different <span class="hlt">climate</span> indices) was created. Several <span class="hlt">predictions</span> of this risk at different temporal scales (i.e. seasonal, inter-annual and low-frequency) were assessed using this <span class="hlt">climate</span> model. The main result of this investigation was the discovery of a significant link between malaria risk and low-frequency rainfall variability related to the Atlantic Multi-decadal Oscillation (AMO). This result is critical for the health information systems in this region. Knowledge of the AMO phases would help local authorities to organise preparedness and prevention of malaria, which is of particular importance in the <span class="hlt">climate</span> change context.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012EGUGA..14..585Y','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012EGUGA..14..585Y"><span>A <span class="hlt">climate</span>-based spatiotemporal <span class="hlt">prediction</span> for dengue fever epidemics: a case study in southern Taiwan</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Yu, H.-L.; Yang, S.-J.; Lin, Y.-C.</p> <p>2012-04-01</p> <p>Dengue Fever (DF) has been identified by the World Health organization (WHO) as one of the most serious vector-borne infectious diseases in tropical and sub-tropical areas. DF has been one of the most important epidemics in Taiwan which occur annually especially in southern Taiwan during summer and autumn. Most DF studies have focused mainly on temporal DF patterns and its close association with <span class="hlt">climatic</span> covariates, whereas few studies have investigated the spatial DF patterns (spatial dependence and clustering) and composite space-time effects of the DF epidemics. The present study proposes a spatio-temporal DF <span class="hlt">prediction</span> approach based on stochastic Bayesian Maximum Entropy (BME) analysis. Core and site-specific knowledge bases are considered, including <span class="hlt">climate</span> and health datasets under conditions of uncertainty, space-time dependence functions, and a Poisson regression model of <span class="hlt">climatic</span> variables contributing to DF occurrences in southern Taiwan during 2007, when the highest number of DF cases was recorded in the history of Taiwan epidemics (over 2000). The obtained results show that the DF outbreaks in the study area are highly influenced by <span class="hlt">climatic</span> conditions. Furthermore, the analysis can provide the required "one-week-ahead" outbreak warnings based on spatio-temporal <span class="hlt">predictions</span> of DF distributions. Therefore, the proposed analysis can provide the Taiwan Disease Control Agency with a valuable tool to timely identify, control, and even efficiently prevent DF spreading across space-time.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018TCry...12.1137K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018TCry...12.1137K"><span>Canadian snow and sea ice: assessment of snow, sea ice, and related <span class="hlt">climate</span> processes in Canada's Earth system model and <span class="hlt">climate-prediction</span> system</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Kushner, Paul J.; Mudryk, Lawrence R.; Merryfield, William; Ambadan, Jaison T.; Berg, Aaron; Bichet, Adéline; Brown, Ross; Derksen, Chris; Déry, Stephen J.; Dirkson, Arlan; Flato, Greg; Fletcher, Christopher G.; Fyfe, John C.; Gillett, Nathan; Haas, Christian; Howell, Stephen; Laliberté, Frédéric; McCusker, Kelly; Sigmond, Michael; Sospedra-Alfonso, Reinel; Tandon, Neil F.; Thackeray, Chad; Tremblay, Bruno; Zwiers, Francis W.</p> <p>2018-04-01</p> <p>The Canadian Sea Ice and Snow Evolution (CanSISE) Network is a <span class="hlt">climate</span> research network focused on developing and applying state-of-the-art observational data to advance dynamical <span class="hlt">prediction</span>, projections, and understanding of seasonal snow cover and sea ice in Canada and the circumpolar Arctic. This study presents an assessment from the CanSISE Network of the ability of the second-generation Canadian Earth System Model (CanESM2) and the Canadian Seasonal to Interannual <span class="hlt">Prediction</span> System (CanSIPS) to simulate and <span class="hlt">predict</span> snow and sea ice from seasonal to multi-decadal timescales, with a focus on the Canadian sector. To account for observational uncertainty, model structural uncertainty, and internal <span class="hlt">climate</span> variability, the analysis uses multi-source observations, multiple Earth system models (ESMs) in Phase 5 of the Coupled Model Intercomparison Project (CMIP5), and large initial-condition ensembles of CanESM2 and other models. It is found that the ability of the CanESM2 simulation to capture snow-related <span class="hlt">climate</span> parameters, such as cold-region surface temperature and precipitation, lies within the range of currently available international models. Accounting for the considerable disagreement among satellite-era observational datasets on the distribution of snow water equivalent, CanESM2 has too much springtime snow mass over Canada, reflecting a broader northern hemispheric positive bias. Biases in seasonal snow cover extent are generally less pronounced. CanESM2 also exhibits retreat of springtime snow generally greater than observational estimates, after accounting for observational uncertainty and internal variability. Sea ice is biased low in the Canadian Arctic, which makes it difficult to assess the realism of long-term sea ice trends there. The strengths and weaknesses of the modelling system need to be understood as a practical tradeoff: the Canadian models are relatively inexpensive computationally because of their moderate resolution, thus enabling their</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5019498','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5019498"><span>Impacts of <span class="hlt">Climate</span> Change on Native Landcover: Seeking Future <span class="hlt">Climatic</span> Refuges</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Mangabeira Albernaz, Ana Luisa</p> <p>2016-01-01</p> <p><span class="hlt">Climate</span> change is a driver for diverse impacts on global biodiversity. We investigated its impacts on native landcover distribution in South America, seeking to <span class="hlt">predict</span> its effect as a new force driving habitat loss and population isolation. Moreover, we mapped potential future <span class="hlt">climatic</span> refuges, which are likely to be key areas for biodiversity conservation under <span class="hlt">climate</span> change scenarios. <span class="hlt">Climatically</span> similar native landcovers were aggregated using a decision tree, generating a reclassified landcover map, from which 25% of the map’s coverage was randomly selected to fuel distribution models. We selected the best geographical distribution models among twelve techniques, validating the <span class="hlt">predicted</span> distribution for current <span class="hlt">climate</span> with the landcover map and used the best technique to <span class="hlt">predict</span> the future distribution. All landcover categories showed changes in area and displacement of the latitudinal/longitudinal centroid. Closed vegetation was the only landcover type <span class="hlt">predicted</span> to expand its distributional range. The range contractions <span class="hlt">predicted</span> for other categories were intense, even suggesting extirpation of the sparse vegetation category. The landcover refuges under future <span class="hlt">climate</span> change represent a small proportion of the South American area and they are disproportionately represented and unevenly distributed, predominantly occupying five of 26 South American countries. The <span class="hlt">predicted</span> changes, regardless of their direction and intensity, can put biodiversity at risk because they are expected to occur in the near future in terms of the temporal scales of ecological and evolutionary processes. Recognition of the threat of <span class="hlt">climate</span> change allows more efficient conservation actions. PMID:27618445</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/27618445','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/27618445"><span>Impacts of <span class="hlt">Climate</span> Change on Native Landcover: Seeking Future <span class="hlt">Climatic</span> Refuges.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Zanin, Marina; Mangabeira Albernaz, Ana Luisa</p> <p>2016-01-01</p> <p><span class="hlt">Climate</span> change is a driver for diverse impacts on global biodiversity. We investigated its impacts on native landcover distribution in South America, seeking to <span class="hlt">predict</span> its effect as a new force driving habitat loss and population isolation. Moreover, we mapped potential future <span class="hlt">climatic</span> refuges, which are likely to be key areas for biodiversity conservation under <span class="hlt">climate</span> change scenarios. <span class="hlt">Climatically</span> similar native landcovers were aggregated using a decision tree, generating a reclassified landcover map, from which 25% of the map's coverage was randomly selected to fuel distribution models. We selected the best geographical distribution models among twelve techniques, validating the <span class="hlt">predicted</span> distribution for current <span class="hlt">climate</span> with the landcover map and used the best technique to <span class="hlt">predict</span> the future distribution. All landcover categories showed changes in area and displacement of the latitudinal/longitudinal centroid. Closed vegetation was the only landcover type <span class="hlt">predicted</span> to expand its distributional range. The range contractions <span class="hlt">predicted</span> for other categories were intense, even suggesting extirpation of the sparse vegetation category. The landcover refuges under future <span class="hlt">climate</span> change represent a small proportion of the South American area and they are disproportionately represented and unevenly distributed, predominantly occupying five of 26 South American countries. The <span class="hlt">predicted</span> changes, regardless of their direction and intensity, can put biodiversity at risk because they are expected to occur in the near future in terms of the temporal scales of ecological and evolutionary processes. Recognition of the threat of <span class="hlt">climate</span> change allows more efficient conservation actions.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017JHyd..554..635Z','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017JHyd..554..635Z"><span>Hydrological responses to <span class="hlt">climatic</span> changes in the Yellow River basin, China: <span class="hlt">Climatic</span> elasticity and streamflow <span class="hlt">prediction</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Zhang, Qiang; Liu, Jianyu; Singh, Vijay P.; Shi, Peijun; Sun, Peng</p> <p>2017-11-01</p> <p><span class="hlt">Prediction</span> of streamflow of the Yellow River basin was done using downscaled precipitation and temperature based on outputs of 12 GCMs under RCP2.6 and RCP8.5 scenarios. Streamflow changes of 37 tributaries of the Yellow River basin during 2070-2099 were <span class="hlt">predicted</span> related to different GCMs and <span class="hlt">climatic</span> scenarios using Budyko framework. The results indicated that: (1) When compared to precipitation and temperature during 1960-1979, increasing precipitation and temperature are dominant during 2070-2099. Particularly, under RCP8.5, increase of 10% and 30% can be detected for precipitation and temperature respectively; (2) Precipitation changes have larger fractional contribution to streamflow changes than temperature changes, being the major driver for spatial and temporal patterns of water resources across the Yellow River basin; (3) 2070-2099 period will witness increased streamflow depth and decreased streamflow can be found mainly in the semi-humid regions and headwater regions of the Yellow River basin, which can be attributed to more significant increase of temperature than precipitation in these regions; (4) Distinctly different picture of streamflow changes can be observed with consideration of different outputs of GCMs which can be attributed to different outputs of GCMs under different scenarios. Even so, under RCP2.6 and RCP8.5 scenarios, 36.8% and 71.1% of the tributaries of the Yellow River basin are dominated by increasing streamflow. The results of this study are of theoretical and practical merits in terms of management of water resources and also irrigated agriculture under influences of changing <span class="hlt">climate</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/biblio/947036-predicting-future-threats-long-term-survival-gila-trout-using-high-resolution-simulation-climate-change','SCIGOV-STC'); return false;" href="https://www.osti.gov/biblio/947036-predicting-future-threats-long-term-survival-gila-trout-using-high-resolution-simulation-climate-change"><span><span class="hlt">Predicting</span> future threats to the long-term survival of Gila Trout using a high-resolution simulation of <span class="hlt">climate</span> change</span></a></p> <p><a target="_blank" href="http://www.osti.gov/search">DOE Office of Scientific and Technical Information (OSTI.GOV)</a></p> <p>Kennedy, Thomas L.; Gutzler, David S.; Leung, Lai R.</p> <p>2008-11-20</p> <p>Regional <span class="hlt">climates</span> are a major factor in determining the distribution of many species. Anthropogenic inputs of greenhouse gases into the atmosphere have been <span class="hlt">predicted</span> to cause rapid <span class="hlt">climatic</span> changes in the next 50-100 years. Species such as the Gila Trout (Onchorhynchus gilae) that have small ranges, limited dispersal capabilities, and narrow physiological tolerances will become increasingly susceptible to extinction as their <span class="hlt">climate</span> envelope changes. This study uses a regional <span class="hlt">climate</span> change simulation (Leung et al. 2004) to determine changes in the <span class="hlt">climate</span> envelope for Gila Trout, which is sensitive to maximum temperature, associated with a plausible scenario for greenhouse gasmore » increases. The model <span class="hlt">predicts</span> approximately a 2° C increase in temperature and a doubling by the mid 21st Century in the annual number of days during which temperature exceeds 37°C, and a 25% increase in the number of days above 32°C, across the current geographical range of Gila Trout. At the same time summer rainfall decreases by more than 20%. These <span class="hlt">climate</span> changes would reduce their available habitat by decreasing the size of their <span class="hlt">climate</span> envelope. Warmer temperatures coupled with a decrease in summer precipitation would also tend to increase the intensity and frequency of forest fires that are a major threat to their survival. The <span class="hlt">climate</span> envelope approach utilized here could be used to assess <span class="hlt">climate</span> change threats to other rare species with limited ranges and dispersal capabilities.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/20416059','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/20416059"><span><span class="hlt">Predicting</span> and mapping malaria under <span class="hlt">climate</span> change scenarios: the potential redistribution of malaria vectors in Africa.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Tonnang, Henri E Z; Kangalawe, Richard Y M; Yanda, Pius Z</p> <p>2010-04-23</p> <p>Malaria is rampant in Africa and causes untold mortality and morbidity. Vector-borne diseases are <span class="hlt">climate</span> sensitive and this has raised considerable concern over the implications of <span class="hlt">climate</span> change on future disease risk. The problem of malaria vectors (Anopheles mosquitoes) shifting from their traditional locations to invade new zones is an important concern. The vision of this study was to exploit the sets of information previously generated by entomologists, e.g. on geographical range of vectors and malaria distribution, to build models that will enable <span class="hlt">prediction</span> and mapping the potential redistribution of Anopheles mosquitoes in Africa. The development of the modelling tool was carried out through calibration of CLIMEX parameters. The model helped estimate the potential geographical distribution and seasonal abundance of the species in relation to <span class="hlt">climatic</span> factors. These included temperature, rainfall and relative humidity, which characterized the living environment for Anopheles mosquitoes. The same parameters were used in determining the ecoclimatic index (EI). The EI values were exported to a GIS package for special analysis and proper mapping of the potential future distribution of Anopheles gambiae and Anophles arabiensis within the African continent under three <span class="hlt">climate</span> change scenarios. These results have shown that shifts in these species boundaries southward and eastward of Africa may occur rather than jumps into quite different <span class="hlt">climatic</span> environments. In the absence of adequate control, these <span class="hlt">predictions</span> are crucial in understanding the possible future geographical range of the vectors and the disease, which could facilitate planning for various adaptation options. Thus, the outputs from this study will be helpful at various levels of decision making, for example, in setting up of an early warning and sustainable strategies for <span class="hlt">climate</span> change and <span class="hlt">climate</span> change adaptation for malaria vectors control programmes in Africa.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://files.eric.ed.gov/fulltext/EJ1143138.pdf','ERIC'); return false;" href="http://files.eric.ed.gov/fulltext/EJ1143138.pdf"><span>Moving toward Collective Impact in <span class="hlt">Climate</span> Change Literacy: The <span class="hlt">Climate</span> Literacy and Energy Awareness Network (CLEAN)</span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Ledley, Tamara Shapiro; Gold, Anne U.; Niepold, Frank; McCaffrey, Mark</p> <p>2014-01-01</p> <p>In recent years, various <span class="hlt">climate</span> change education efforts have been launched, including federally (National Oceanic and Atmospheric <span class="hlt">Administration</span>, National Aeronautics and Space <span class="hlt">Administration</span>, National Science Foundation, etc.) and privately funded projects. In addition, <span class="hlt">climate</span> literacy and energy literacy frameworks have been developed and…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/21210799','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/21210799"><span>The relationship between organizational <span class="hlt">climate</span> and quality of chronic disease management.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Benzer, Justin K; Young, Gary; Stolzmann, Kelly; Osatuke, Katerine; Meterko, Mark; Caso, Allison; White, Bert; Mohr, David C</p> <p>2011-06-01</p> <p>To test the utility of a two-dimensional model of organizational <span class="hlt">climate</span> for explaining variation in diabetes care between primary care clinics. Secondary data were obtained from 223 primary care clinics in the Department of Veterans Affairs health care system. Organizational <span class="hlt">climate</span> was defined using the dimensions of task and relational <span class="hlt">climate</span>. The association between primary care organizational <span class="hlt">climate</span> and diabetes processes and intermediate outcomes were estimated for 4,539 patients in a cross-sectional study. All data were collected from <span class="hlt">administrative</span> datasets. The <span class="hlt">climate</span> data were drawn from the 2007 VA All Employee Survey, and the outcomes data were collected as part of the VA External Peer Review Program. <span class="hlt">Climate</span> data were aggregated to the facility level of analysis and merged with patient-level data. Relational <span class="hlt">climate</span> was related to an increased likelihood of diabetes care process adherence, with significant but small effects for adherence to intermediate outcomes. Task <span class="hlt">climate</span> was generally not shown to be related to adherence. The role of relational <span class="hlt">climate</span> in <span class="hlt">predicting</span> the quality of chronic care was supported. Future research should examine the mediators and moderators of relational <span class="hlt">climate</span> and further investigate task <span class="hlt">climate</span>. © Health Research and Educational Trust.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/27564574','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/27564574"><span><span class="hlt">Predicting</span> athletes' functional and dysfunctional emotions: The role of the motivational <span class="hlt">climate</span> and motivation regulations.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Ruiz, Montse C; Haapanen, Saara; Tolvanen, Asko; Robazza, Claudio; Duda, Joan L</p> <p>2017-08-01</p> <p>This study examined the relationships between perceptions of the motivational <span class="hlt">climate</span>, motivation regulations, and the intensity and functionality levels of athletes' pleasant and unpleasant emotional states. Specifically, we examined the hypothesised mediational role of motivation regulations in the <span class="hlt">climate</span>-emotion relationship. We also tested a sequence in which emotions were assumed to be <span class="hlt">predicted</span> by the motivational <span class="hlt">climate</span> dimensions and then served as antecedents to variability in motivation regulations. Participants (N = 494) completed a multi-section questionnaire assessing targeted variables. Structural equation modelling (SEM) revealed that a perceived task-involving <span class="hlt">climate</span> was a positive predictor of autonomous motivation and of the impact of functional anger, and a negative predictor of the intensity of anxiety and dysfunctional anger. Autonomous motivation was a partial mediator of perceptions of a task-involving <span class="hlt">climate</span> and the impact of functional anger. An ego-involving <span class="hlt">climate</span> was a positive predictor of controlled motivation, and of the intensity and impact of functional anger and the intensity of dysfunctional anger. Controlled motivation partially mediated the relationship between an ego-involving <span class="hlt">climate</span> and the intensity of dysfunctional anger. Good fit to the data also emerged for the motivational <span class="hlt">climate</span>, emotional states, and motivation regulations sequence. Findings provide support for the consideration of hedonic tone and functionality distinctions in the assessment of athletes' emotional states.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/1997TellA..49..513S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/1997TellA..49..513S"><span>Correlation of spatial <span class="hlt">climate</span>/weather maps and the advantages of using the Mahalanobis metric in <span class="hlt">predictions</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Stephenson, D. B.</p> <p>1997-10-01</p> <p>The skill in <span class="hlt">predicting</span> spatially varying weather/<span class="hlt">climate</span> maps depends on the definition of the measure of similarity between the maps. Under the justifiable approximation that the anomaly maps are distributed multinormally, it is shown analytically that the choice of weighting metric, used in defining the anomaly correlation between spatial maps, can change the resulting probability distribution of the correlation coefficient. The estimate of the numbers of degrees of freedom based on the variance of the correlation distribution can vary from unity up to the number of grid points depending on the choice of weighting metric. The (pseudo-) inverse of the sample covariance matrix acts as a special choice for the metric in that it gives a correlation distribution which has minimal kurtosis and maximum dimension. Minimal kurtosis suggests that the average <span class="hlt">predictive</span> skill might be improved due to the rarer occurrence of troublesome outlier patterns far from the mean state. Maximum dimension has a disadvantage for analogue <span class="hlt">prediction</span> schemes in that it gives the minimum number of analogue states. This metric also has an advantage in that it allows one to powerfully test the null hypothesis of multinormality by examining the second and third moments of the correlation coefficient which were introduced by Mardia as invariant measures of multivariate kurtosis and skewness. For these reasons, it is suggested that this metric could be usefully employed in the <span class="hlt">prediction</span> of weather/<span class="hlt">climate</span> and in fingerprinting anthropogenic <span class="hlt">climate</span> change. The ideas are illustrated using the bivariate example of the observed monthly mean sea-level pressures at Darwin and Tahitifrom 1866 1995.</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_15");'>15</a></li> <li><a href="#" onclick='return showDiv("page_16");'>16</a></li> <li class="active"><span>17</span></li> <li><a href="#" onclick='return showDiv("page_18");'>18</a></li> <li><a href="#" onclick='return showDiv("page_19");'>19</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_17 --> <div id="page_18" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_16");'>16</a></li> <li><a href="#" onclick='return showDiv("page_17");'>17</a></li> <li class="active"><span>18</span></li> <li><a href="#" onclick='return showDiv("page_19");'>19</a></li> <li><a href="#" onclick='return showDiv("page_20");'>20</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="341"> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUOSME11A..05L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUOSME11A..05L"><span>Integrating <span class="hlt">Climate</span> Science, Marine Ecology, and Fisheries Economics to <span class="hlt">Predict</span> the Effects of <span class="hlt">Climate</span> Change on New England lobster Fisheries</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Le Bris, A.; Pershing, A. J.; Holland, D. S.; Mills, K.; Sun, C. H. J.</p> <p>2016-02-01</p> <p>The Gulf of Maine and the northwest Atlantic shelf have experienced one of the fastest warming rates of the global ocean over the past decade, and concerns are growing about the long-term sustainability of the fishing industries in the region. The lucrative American lobster fishery occurs over a steep temperature gradient, providing a unique opportunity to evaluate the consequences of <span class="hlt">climate</span> change and variability on marine socio-ecological systems. This study aims at developing an integrated <span class="hlt">climate</span>, population dynamics, and fishery economics model to <span class="hlt">predict</span> consequences of <span class="hlt">climate</span> change on the American lobster fishery. In this talk, we first describe a mechanistic model that combines life-history theory and a size-spectrum approach to simulate the dynamics of the population. Results show that as temperature increases, early growth rate and predation on small individuals increases, while size-at-maturity, maximum length and predation on large individuals decreases, resulting in a lower recruitment in the southern New-England and higher recruitment in the northern Gulf of Maine. Second, we present an integrated fishery and economic module that links temperature to landings and price through its influence on catchability and abundance. Preliminary results show that temperature is positively correlated with landings and negatively correlated with price in the Gulf of Maine. Finally, we discuss how model simulations under various fishing effort, market and <span class="hlt">climate</span> scenarios can be used to identify adaptation opportunities to improve the resilience of the fishery to <span class="hlt">climate</span> change.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018HESS...22..287M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018HESS...22..287M"><span>Regression-based season-ahead drought <span class="hlt">prediction</span> for southern Peru conditioned on large-scale <span class="hlt">climate</span> variables</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Mortensen, Eric; Wu, Shu; Notaro, Michael; Vavrus, Stephen; Montgomery, Rob; De Piérola, José; Sánchez, Carlos; Block, Paul</p> <p>2018-01-01</p> <p>Located at a complex topographic, <span class="hlt">climatic</span>, and hydrologic crossroads, southern Peru is a semiarid region that exhibits high spatiotemporal variability in precipitation. The economic viability of the region hinges on this water, yet southern Peru is prone to water scarcity caused by seasonal meteorological drought. Meteorological droughts in this region are often triggered during El Niño episodes; however, other large-scale <span class="hlt">climate</span> mechanisms also play a noteworthy role in controlling the region's hydrologic cycle. An extensive season-ahead precipitation <span class="hlt">prediction</span> model is developed to help bolster the existing capacity of stakeholders to plan for and mitigate deleterious impacts of drought. In addition to existing <span class="hlt">climate</span> indices, large-scale <span class="hlt">climatic</span> variables, such as sea surface temperature, are investigated to identify potential drought predictors. A principal component regression framework is applied to 11 potential predictors to produce an ensemble forecast of regional January-March precipitation totals. Model hindcasts of 51 years, compared to climatology and another model conditioned solely on an El Niño-Southern Oscillation index, achieve notable skill and perform better for several metrics, including ranked probability skill score and a hit-miss statistic. The information provided by the developed model and ancillary modeling efforts, such as extending the lead time of and spatially disaggregating precipitation <span class="hlt">predictions</span> to the local level as well as forecasting the number of wet-dry days per rainy season, may further assist regional stakeholders and policymakers in preparing for drought.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFM.C11C0918M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFM.C11C0918M"><span>Toward Process-resolving Synthesis and <span class="hlt">Prediction</span> of Arctic <span class="hlt">Climate</span> Change Using the Regional Arctic System Model</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Maslowski, W.</p> <p>2017-12-01</p> <p>The Regional Arctic System Model (RASM) has been developed to better understand the operation of Arctic System at process scale and to improve <span class="hlt">prediction</span> of its change at a spectrum of time scales. RASM is a pan-Arctic, fully coupled ice-ocean-atmosphere-land model with marine biogeochemistry extension to the ocean and sea ice models. The main goal of our research is to advance a system-level understanding of critical processes and feedbacks in the Arctic and their links with the Earth System. The secondary, an equally important objective, is to identify model needs for new or additional observations to better understand such processes and to help constrain models. Finally, RASM has been used to produce sea ice forecasts for September 2016 and 2017, in contribution to the Sea Ice Outlook of the Sea Ice <span class="hlt">Prediction</span> Network. Future RASM forecasts, are likely to include increased resolution for model components and ecosystem <span class="hlt">predictions</span>. Such research is in direct support of the US environmental assessment and <span class="hlt">prediction</span> needs, including those of the U.S. Navy, Department of Defense, and the recent IARPC Arctic Research Plan 2017-2021. In addition to an overview of RASM technical details, selected model results are presented from a hierarchy of <span class="hlt">climate</span> models together with available observations in the region to better understand potential oceanic contributions to polar amplification. RASM simulations are analyzed to evaluate model skill in representing seasonal climatology as well as interannual and multi-decadal <span class="hlt">climate</span> variability and <span class="hlt">predictions</span>. Selected physical processes and resulting feedbacks are discussed to emphasize the need for fully coupled <span class="hlt">climate</span> model simulations, high model resolution and sensitivity of simulated sea ice states to scale dependent model parameterizations controlling ice dynamics, thermodynamics and coupling with the atmosphere and ocean.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=19990064064&hterms=Change+climate&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D30%26Ntt%3DChange%2Bclimate','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=19990064064&hterms=Change+climate&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D30%26Ntt%3DChange%2Bclimate"><span><span class="hlt">Predicting</span> Decade-to-Century <span class="hlt">Climate</span> Change: Prospects for Improving Models</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Somerville, Richard C. J.</p> <p>1999-01-01</p> <p>Recent research has led to a greatly increased understanding of the uncertainties in today's <span class="hlt">climate</span> models. In attempting to <span class="hlt">predict</span> the <span class="hlt">climate</span> of the 21st century, we must confront not only computer limitations on the affordable resolution of global models, but also a lack of physical realism in attempting to model key processes. Until we are able to incorporate adequate treatments of critical elements of the entire biogeophysical <span class="hlt">climate</span> system, our models will remain subject to these uncertainties, and our scenarios of future <span class="hlt">climate</span> change, both anthropogenic and natural, will not fully meet the requirements of either policymakers or the public. The areas of most-needed model improvements are thought to include air-sea exchanges, land surface processes, ice and snow physics, hydrologic cycle elements, and especially the role of aerosols and cloud-radiation interactions. Of these areas, cloud-radiation interactions are known to be responsible for much of the inter-model differences in sensitivity to greenhouse gases. Recently, we have diagnostically evaluated several current and proposed model cloud-radiation treatments against extensive field observations. Satellite remote sensing provides an indispensable component of the observational resources. Cloud-radiation parameterizations display a strong sensitivity to vertical resolution, and we find that vertical resolutions typically used in global models are far from convergence. We also find that newly developed advanced parameterization schemes with explicit cloud water budgets and interactive cloud radiative properties are potentially capable of matching observational data closely. However, it is difficult to evaluate the realism of model-produced fields of cloud extinction, cloud emittance, cloud liquid water content and effective cloud droplet radius until high-quality measurements of these quantities become more widely available. Thus, further progress will require a combination of theoretical and modeling</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013EGUGA..15.1085K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013EGUGA..15.1085K"><span>Pacific-Australia <span class="hlt">Climate</span> Change Science and Adaptation Planning program: supporting <span class="hlt">climate</span> science and enhancing <span class="hlt">climate</span> services in Pacific Island Countries</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Kuleshov, Yuriy; Jones, David; Hendon, Harry; Charles, Andrew; Shelton, Kay; de Wit, Roald; Cottrill, Andrew; Nakaegawa, Toshiyuki; Atalifo, Terry; Prakash, Bipendra; Seuseu, Sunny; Kaniaha, Salesa</p> <p>2013-04-01</p> <p>Over the past few years, significant progress in developing <span class="hlt">climate</span> science for the Pacific has been achieved through a number of research projects undertaken under the Australian government International <span class="hlt">Climate</span> Change Adaptation Initiative (ICCAI). <span class="hlt">Climate</span> change has major impact on Pacific Island Countries and advancement in understanding past, present and futures <span class="hlt">climate</span> in the region is vital for island nation to develop adaptation strategies to their rapidly changing environment. This new science is now supporting new services for a wide range of stakeholders in the Pacific through the National Meteorological Agencies of the region. Seasonal <span class="hlt">climate</span> <span class="hlt">prediction</span> is particularly important for planning in agriculture, tourism and other weather-sensitive industries, with operational services provided by all National Meteorological Services in the region. The interaction between <span class="hlt">climate</span> variability and <span class="hlt">climate</span> change, for example during droughts or very warm seasons, means that much of the early impacts of <span class="hlt">climate</span> change are being felt through seasonal variability. A means to reduce these impacts is to improve forecasts to support decision making. Historically, seasonal <span class="hlt">climate</span> <span class="hlt">prediction</span> has been developed based on statistical past relationship. Statistical methods relate meteorological variables (e.g. temperature and rainfall) to indices which describe large-scale environment (e.g. ENSO indices) using historical data. However, with observed <span class="hlt">climate</span> change, statistical approaches based on historical data are getting less accurate and less reliable. Recognising the value of seasonal forecasts, we have used outputs of a dynamical model POAMA (<span class="hlt">Predictive</span> Ocean Atmosphere Model for Australia), to develop web-based information tools (http://poama.bom.gov.au/experimental/pasap/index.shtml) which are now used by <span class="hlt">climate</span> services in 15 partner countries in the Pacific for preparing seasonal <span class="hlt">climate</span> outlooks. Initial comparison conducted during 2012 has shown that the</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=1569571','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=1569571"><span>Integrating seasonal <span class="hlt">climate</span> <span class="hlt">prediction</span> and agricultural models for insights into agricultural practice</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Hansen, James W</p> <p>2005-01-01</p> <p>Interest in integrating crop simulation models with dynamic seasonal <span class="hlt">climate</span> forecast models is expanding in response to a perceived opportunity to add value to seasonal <span class="hlt">climate</span> forecasts for agriculture. Integrated modelling may help to address some obstacles to effective agricultural use of <span class="hlt">climate</span> information. First, modelling can address the mismatch between farmers' needs and available operational forecasts. Probabilistic crop yield forecasts are directly relevant to farmers' livelihood decisions and, at a different scale, to early warning and market applications. Second, credible ex ante evidence of livelihood benefits, using integrated climate–crop–economic modelling in a value-of-information framework, may assist in the challenge of obtaining institutional, financial and political support; and inform targeting for greatest benefit. Third, integrated modelling can reduce the risk and learning time associated with adaptation and adoption, and related uncertainty on the part of advisors and advocates. It can provide insights to advisors, and enhance site-specific interpretation of recommendations when driven by spatial data. Model-based ‘discussion support systems’ contribute to learning and farmer–researcher dialogue. Integrated climate–crop modelling may play a genuine, but limited role in efforts to support <span class="hlt">climate</span> risk management in agriculture, but only if they are used appropriately, with understanding of their capabilities and limitations, and with cautious evaluation of model <span class="hlt">predictions</span> and of the insights that arises from model-based decision analysis. PMID:16433092</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016EGUGA..18..483K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016EGUGA..18..483K"><span>Evaluation of GCMs in the context of regional <span class="hlt">predictive</span> <span class="hlt">climate</span> impact studies.</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Kokorev, Vasily; Anisimov, Oleg</p> <p>2016-04-01</p> <p>Significant improvements in the structure, complexity, and general performance of earth system models (ESMs) have been made in the recent decade. Despite these efforts, the range of uncertainty in <span class="hlt">predicting</span> regional <span class="hlt">climate</span> impacts remains large. The problem is two-fold. Firstly, there is an intrinsic conflict between the local and regional scales of <span class="hlt">climate</span> impacts and adaptation strategies, on one hand, and larger scales, at which ESMs demonstrate better performance, on the other. Secondly, there is a growing understanding that majority of the impacts involve thresholds, and are thus driven by extreme <span class="hlt">climate</span> events, whereas accent in <span class="hlt">climate</span> projections is conventionally made on gradual changes in means. In this study we assess the uncertainty in projecting extreme <span class="hlt">climatic</span> events within a region-specific and process-oriented context by examining the skills and ranking of ESMs. We developed a synthetic regionalization of Northern Eurasia that accounts for the spatial features of modern <span class="hlt">climatic</span> changes and major environmental and socio-economical impacts. Elements of such fragmentation could be considered as natural focus regions that bridge the gap between the spatial scales adopted in <span class="hlt">climate</span>-impacts studies and patterns of <span class="hlt">climate</span> change simulated by ESMs. In each focus region we selected several target meteorological variables that govern the key regional impacts, and examined the ability of the models to replicate their seasonal and annual means and trends by testing them against observations. We performed a similar evaluation with regard to extremes and statistics of the target variables. And lastly, we used the results of these analyses to select sets of models that demonstrate the best performance at selected focus regions with regard to selected sets of target meteorological parameters. Ultimately, we ranked the models according to their skills, identified top-end models that "better than average" reproduce the behavior of <span class="hlt">climatic</span> parameters, and</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AcO....71...31K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AcO....71...31K"><span><span class="hlt">Predicting</span> impacts of <span class="hlt">climate</span> change on habitat connectivity of Kalopanax septemlobus in South Korea</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Kang, Wanmo; Minor, Emily S.; Lee, Dowon; Park, Chan-Ryul</p> <p>2016-02-01</p> <p>Understanding the drivers of habitat distribution patterns and assessing habitat connectivity are crucial for conservation in the face of <span class="hlt">climate</span> change. In this study, we examined a sparsely distributed tree species, Kalopanax septemlobus (Araliaceae), which has been heavily disturbed by human use in temperate forests of South Korea. We used maximum entropy distribution modeling (MaxEnt) to identify the <span class="hlt">climatic</span> and topographic factors driving the distribution of the species. Then, we constructed habitat models under current and projected <span class="hlt">climate</span> conditions for the year 2050 and evaluated changes in the extent and connectivity of the K. septemlobus habitat. Annual mean temperature and terrain slope were the two most important predictors of species distribution. Our models <span class="hlt">predicted</span> the range shift of K. septemlobus toward higher elevations under medium-low and high emissions scenarios for 2050, with dramatic reductions in suitable habitat (51% and 85%, respectively). In addition, connectivity analysis indicated that <span class="hlt">climate</span> change is expected to reduce future levels of habitat connectivity. Even under the Representative Construction Pathway (RCP) 4.5 medium-low warming scenario, the projected <span class="hlt">climate</span> conditions will decrease habitat connectivity by 78%. Overall, suitable habitats for K. septemlobus populations will likely become more isolated depending on the severity of global warming. The approach presented here can be used to efficiently assess species and habitat vulnerability to <span class="hlt">climate</span> change.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFMGC23J..06R','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFMGC23J..06R"><span>Mechanistic Lake Modeling to Understand and <span class="hlt">Predict</span> Heterogeneous Responses to <span class="hlt">Climate</span> Warming</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Read, J. S.; Winslow, L. A.; Rose, K. C.; Hansen, G. J.</p> <p>2016-12-01</p> <p>Substantial warming has been documented for of hundreds globally distributed lakes, with likely impacts on ecosystem processes. Despite a clear pattern of widespread warming, thermal responses of individual lakes to <span class="hlt">climate</span> change are often heterogeneous, with the warming rates of neighboring lakes varying across depths and among seasons. We aggregated temperature observations and parameterized mechanistic models for 9,000 lakes in the U.S. states of Minnesota, Wisconsin, and Michigan to examine broad-scale lake warming trends and among-lake diversity. Daily lake temperature profiles and ice-cover dynamics were simulated using the General Lake Model for the contemporary period (1979-2015) using drivers from the North American Land Data Assimilation System (NLDAS-2) and for contemporary and future periods (1980-2100) using downscaled data from six global circulation models driven by the Representative <span class="hlt">Climate</span> Pathway 8.5 scenario. For the contemporary period, modeled vs observed summer mean surface temperatures had a root mean squared error of 0.98°C with modeled warming trends similar to observed trends. Future simulations under the extreme 8.5 scenario <span class="hlt">predicted</span> a median lake summer surface warming rate of 0.57°C/decade until mid-century, with slower rates in the later half of the 21st century (0.35°C/decade). Modeling scenarios and analysis of field data suggest that the lake-specific properties of size, water clarity, and depth are strong controls on the sensitivity of lakes to <span class="hlt">climate</span> change. For example, a simulated 1% annual decline in water clarity was sufficient to override the effects of <span class="hlt">climate</span> warming on whole lake water temperatures in some - but not all - study lakes. Understanding heterogeneous lake responses to <span class="hlt">climate</span> variability can help identify lake-specific features that influence resilience to <span class="hlt">climate</span> change.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/24015532','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/24015532"><span>[Effects of sampling plot number on tree species distribution <span class="hlt">prediction</span> under <span class="hlt">climate</span> change].</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Liang, Yu; He, Hong-Shi; Wu, Zhi-Wei; Li, Xiao-Na; Luo, Xu</p> <p>2013-05-01</p> <p>Based on the neutral landscapes under different degrees of landscape fragmentation, this paper studied the effects of sampling plot number on the <span class="hlt">prediction</span> of tree species distribution at landscape scale under <span class="hlt">climate</span> change. The tree species distribution was <span class="hlt">predicted</span> by the coupled modeling approach which linked an ecosystem process model with a forest landscape model, and three contingent scenarios and one reference scenario of sampling plot numbers were assumed. The differences between the three scenarios and the reference scenario under different degrees of landscape fragmentation were tested. The results indicated that the effects of sampling plot number on the <span class="hlt">prediction</span> of tree species distribution depended on the tree species life history attributes. For the generalist species, the <span class="hlt">prediction</span> of their distribution at landscape scale needed more plots. Except for the extreme specialist, landscape fragmentation degree also affected the effects of sampling plot number on the <span class="hlt">prediction</span>. With the increase of simulation period, the effects of sampling plot number on the <span class="hlt">prediction</span> of tree species distribution at landscape scale could be changed. For generalist species, more plots are needed for the long-term simulation.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016EGUGA..1817143S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016EGUGA..1817143S"><span>Detailed <span class="hlt">predictions</span> of <span class="hlt">climate</span> induced changes in the thermal and flow regimes in mountain streams of the Iberian Peninsula</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Santiago, José M.; Muñoz-Mas, Rafael; García de Jalón, Diego; Solana, Joaquín; Alonso, Carlos; Martínez-Capel, Francisco; Ribalaygua, Jaime; Pórtoles, Javier; Monjo, Robert</p> <p>2016-04-01</p> <p>Streamflow and temperature regimes are well-known to influence on the availability of suitable physical habitat for instream biological communities. General Circulation Models (GCMs) have <span class="hlt">predicted</span> significant changes in timing and geographic distribution of precipitation and atmospheric temperature for the ongoing century. However, differences in these <span class="hlt">predictions</span> may arise when focusing on different spatial and temporal scales. Therefore, to perform substantiated mitigation and management actions detailed scales are necessary to adequately forecast the consequent thermal and flow regimes. Regional <span class="hlt">predictions</span> are relatively abundant but detailed ones, both spatially and temporally, are still scarce. The present study aimed at <span class="hlt">predicting</span> the effects of <span class="hlt">climate</span> change on the thermal and flow regime in the Iberian Peninsula, refining the resolution of previous studies. For this purpose, the study encompassed 28 sites at eight different mountain rivers and streams in the central part of the Iberian Peninsula (Spain). The daily flow was modelled using different daily, monthly and quarterly lags of the historical precipitation and temperature time series. These precipitation-runoff models were developed by means of M5 model trees. On the other hand water temperature was modelled at similar time scale by means of nonlinear regression from dedicated site-specific data. The developed models were used to simulate the temperature and flow regime under two Representative Concentration Pathway (RCPs) <span class="hlt">climate</span> change scenarios (RCP 4.5 and RCP 8.5) until the end of the present century by considering nine different GCMs, which were pertinently downscaled. The precipitation-runoff models achieved high accuracy (NSE>0.7), especially in regards of the low flows of the historical series. Results concomitantly forecasted flow reductions between 7 and 17 % (RCP4.5) and between 8 and 49% (RCP8.5) of the annual average in the most cases, being variable the magnitude and timing at each</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.cpc.ncep.noaa.gov/products/analysis_monitoring/lanina/usdivtp/writeup.shtml','SCIGOVWS'); return false;" href="http://www.cpc.ncep.noaa.gov/products/analysis_monitoring/lanina/usdivtp/writeup.shtml"><span><span class="hlt">Climate</span> <span class="hlt">Prediction</span> Center - Monitoring & Data: La Niña Seasonal Maps and</span></a></p> <p><a target="_blank" href="http://www.science.gov/aboutsearch.html">Science.gov Websites</a></p> <p></p> <p></p> <p>Statistics</A> Skip Navigation Links www.nws.noaa.gov NOAA logo - Click to go to <em>the</em> NOAA home page National Weather Service NWS logo - Click to go to <em>the</em> NWS home page <span class="hlt">Climate</span> <span class="hlt">Prediction</span> Center Home Site Map News Organization Search Go Search <em>the</em> CPC Go About Us Our Mission Who We Are Contact Us</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018InAgr..32..203P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018InAgr..32..203P"><span>Integrated model for <span class="hlt">predicting</span> rice yield with <span class="hlt">climate</span> change</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Park, Jin-Ki; Das, Amrita; Park, Jong-Hwa</p> <p>2018-04-01</p> <p>Rice is the chief agricultural product and one of the primary food source. For this reason, it is of pivotal importance for worldwide economy and development. Therefore, in a decision-support-system both for the farmers and in the planning and management of the country's economy, forecasting yield is vital. However, crop yield, which is a dependent of the soil-bio-atmospheric system, is difficult to represent in statistical language. This paper describes a novel approach for <span class="hlt">predicting</span> rice yield using artificial neural network, spatial interpolation, remote sensing and GIS methods. Herein, the variation in the yield is attributed to <span class="hlt">climatic</span> parameters and crop health, and the normalized difference vegetation index from MODIS is used as an indicator of plant health and growth. Due importance was given to scaling up the input parameters using spatial interpolation and GIS and minimising the sources of error in every step of the modelling. The low percentage error (2.91) and high correlation (0.76) signifies the robust performance of the proposed model. This simple but effective approach is then used to estimate the influence of <span class="hlt">climate</span> change on South Korean rice production. As proposed in the RCP8.5 scenario, an upswing in temperature may increase the rice yield throughout South Korea.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/24884398','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/24884398"><span>Stroke survivors over-estimate their medication self-<span class="hlt">administration</span> (MSA) ability, <span class="hlt">predicting</span> memory loss.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Barrett, A M; Galletta, Elizabeth E; Zhang, Jun; Masmela, Jenny R; Adler, Uri S</p> <p>2014-01-01</p> <p>Medication self-<span class="hlt">administration</span> (MSA) may be cognitively challenging after stroke, but guidelines are currently lacking for identifying high-functioning stroke survivors who may have difficulty with this task. Complicating this matter, stroke survivors may not be aware of their cognitive problems (cognitive anosognosia) and may over-estimate their MSA competence. The authors wished to evaluate medication self-<span class="hlt">administration</span> and MSA self-awareness in 24 consecutive acute stroke survivors undergoing inpatient rehabilitation, to determine if they would over-estimate their medication self-<span class="hlt">administration</span> and if this <span class="hlt">predicted</span> memory disorder. Stroke survivors were tested on the Hopkins Medication Schedule and also their memory, naming mood and dexterity were evaluated, comparing their performance to 17 matched controls. The anosognosia ratio indicated MSA over-estimation in stroke survivors compared with controls--no other over-estimation errors were noted relative to controls. A strong correlation was observed between over-estimation of MSA ability and verbal memory deficit, suggesting that formally assessing MSA and MSA self-awareness may help detect cognitive deficits. Assessing medication self-<span class="hlt">administration</span> and MSA self-awareness may be useful in rehabilitation and successful community-return after stroke.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFM.A23F2435L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFM.A23F2435L"><span>The <span class="hlt">Climate</span> Variability & <span class="hlt">Predictability</span> (CVP) Program at NOAA - Observing and Understanding Processes Affecting the Propagation of Intraseasonal Oscillations in the Maritime Continent Region</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Lucas, S. E.</p> <p>2017-12-01</p> <p>The <span class="hlt">Climate</span> Variability & <span class="hlt">Predictability</span> (CVP) Program supports research aimed at providing process-level understanding of the <span class="hlt">climate</span> system through observation, modeling, analysis, and field studies. This vital knowledge is needed to improve <span class="hlt">climate</span> models and <span class="hlt">predictions</span> so that scientists can better anticipate the impacts of future <span class="hlt">climate</span> variability and change. To achieve its mission, the CVP Program supports research carried out at NOAA and other federal laboratories, NOAA Cooperative Institutes, and academic institutions. The Program also coordinates its sponsored projects with major national and international scientific bodies including the World <span class="hlt">Climate</span> Research Programme (WCRP), the International and U.S. <span class="hlt">Climate</span> Variability and <span class="hlt">Predictability</span> (CLIVAR/US CLIVAR) Program, and the U.S. Global Change Research Program (USGCRP). The CVP program sits within NOAA's <span class="hlt">Climate</span> Program Office (http://cpo.noaa.gov/CVP). In 2017, the CVP Program had a call for proposals focused on observing and understanding processes affecting the propagation of intraseasonal oscillations in the Maritime Continent region. This poster will present the recently funded CVP projects, the expected scientific outcomes, the geographic areas of their work in the Maritime Continent region, and the collaborations with the Office of Naval Research, Indonesian Agency for Meteorology, Climatology and Geophysics (BMKG), Japan Agency for Marine-Earth Science and Technology (JAMSTEC) and other partners.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012AGUFM.B33E0566R','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012AGUFM.B33E0566R"><span>Joint Applications Pilot of the National <span class="hlt">Climate</span> <span class="hlt">Predictions</span> and Projections Platform and the North Central <span class="hlt">Climate</span> Science Center: Delivering <span class="hlt">climate</span> projections on regional scales to support adaptation planning</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Ray, A. J.; Ojima, D. S.; Morisette, J. T.</p> <p>2012-12-01</p> <p>The DOI North Central <span class="hlt">Climate</span> Science Center (NC CSC) and the NOAA/NCAR National <span class="hlt">Climate</span> <span class="hlt">Predictions</span> and Projections (NCPP) Platform and have initiated a joint pilot study to collaboratively explore the "best available <span class="hlt">climate</span> information" to support key land management questions and how to provide this information. NCPP's mission is to support state of the art approaches to develop and deliver comprehensive regional <span class="hlt">climate</span> information and facilitate its use in decision making and adaptation planning. This presentation will describe the evolving joint pilot as a tangible, real-world demonstration of linkages between <span class="hlt">climate</span> science, ecosystem science and resource management. Our joint pilot is developing a deliberate, ongoing interaction to prototype how NCPP will work with CSCs to develop and deliver needed <span class="hlt">climate</span> information products, including translational information to support <span class="hlt">climate</span> data understanding and use. This pilot also will build capacity in the North Central CSC by working with NCPP to use <span class="hlt">climate</span> information used as input to ecological modeling. We will discuss lessons to date on developing and delivering needed <span class="hlt">climate</span> information products based on this strategic partnership. Four projects have been funded to collaborate to incorporate <span class="hlt">climate</span> information as part of an ecological modeling project, which in turn will address key DOI stakeholder priorities in the region: Riparian Corridors: Projecting <span class="hlt">climate</span> change effects on cottonwood and willow seed dispersal phenology, flood timing, and seedling recruitment in western riparian forests. Sage Grouse & Habitats: Integrating <span class="hlt">climate</span> and biological data into land management decision models to assess species and habitat vulnerability Grasslands & Forests: Projecting future effects of land management, natural disturbance, and CO2 on woody encroachment in the Northern Great Plains The value of <span class="hlt">climate</span> information: Supporting management decisions in the Plains and Prairie Potholes LCC. NCCSC's role in</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/22269559','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/22269559"><span>Psychosocial safety <span class="hlt">climate</span> moderates the job demand-resource interaction in <span class="hlt">predicting</span> workgroup distress.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Dollard, Maureen F; Tuckey, Michelle R; Dormann, Christian</p> <p>2012-03-01</p> <p>Psychosocial safety <span class="hlt">climate</span> (PSC) arises from workplace policies, practices, and procedures for the protection of worker psychological health and safety that are largely driven by management. Many work stress theories are based on the fundamental interaction hypothesis - that a high level of job demands (D) will lead to psychological distress and that this relationship will be offset when there are high job resources (R). However we proposed that this interaction really depends on the organizational context; in particular high levels of psychosocial safety <span class="hlt">climate</span> will enable the safe utilization of resources to reduce demands. The study sample consisted of police constables from 23 police units (stations) with longitudinal survey responses at two time points separated by 14 months (Time 1, N=319, Time 2, N=139). We used hierarchical linear modeling to assess the effect of the proposed three-way interaction term (PSC×D×R) on change in workgroup distress variance over time. Specifically we confirmed the interaction between emotional demands and emotional resources (assessed at the individual level), in the context of unit psychosocial safety <span class="hlt">climate</span> (aggregated individual data). As <span class="hlt">predicted</span>, high emotional resources moderated the positive relationship between emotional demands and change in workgroup distress but only when there were high levels of unit psychosocial safety <span class="hlt">climate</span>. Results were confirmed using a split-sample analysis. Results support psychosocial safety <span class="hlt">climate</span> as a property of the organization and a target for higher order controls for reducing work stress. The 'right' <span class="hlt">climate</span> enables resources to do their job. Copyright © 2011 Elsevier Ltd. All rights reserved.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://cfpub.epa.gov/si/si_public_record_report.cfm?dirEntryId=331152&Lab=NHEERL&keyword=sea&actType=&TIMSType=+&TIMSSubTypeID=&DEID=&epaNumber=&ntisID=&archiveStatus=Both&ombCat=Any&dateBeginCreated=&dateEndCreated=&dateBeginPublishedPresented=&dateEndPublishedPresented=&dateBeginUpdated=&dateEndUpdated=&dateBeginCompleted=&dateEndCompleted=&personID=&role=Any&journalID=&publisherID=&sortBy=revisionDate&count=50','EPA-EIMS'); return false;" href="https://cfpub.epa.gov/si/si_public_record_report.cfm?dirEntryId=331152&Lab=NHEERL&keyword=sea&actType=&TIMSType=+&TIMSSubTypeID=&DEID=&epaNumber=&ntisID=&archiveStatus=Both&ombCat=Any&dateBeginCreated=&dateEndCreated=&dateBeginPublishedPresented=&dateEndPublishedPresented=&dateBeginUpdated=&dateEndUpdated=&dateBeginCompleted=&dateEndCompleted=&personID=&role=Any&journalID=&publisherID=&sortBy=revisionDate&count=50"><span>The Icarus challenge - <span class="hlt">Predicting</span> vulnerability to <span class="hlt">climate</span> change using an algorithm-based species' trait approach</span></a></p> <p><a target="_blank" href="http://oaspub.epa.gov/eims/query.page">EPA Science Inventory</a></p> <p></p> <p></p> <p>The Icarus challenge - <span class="hlt">Predicting</span> vulnerability to <span class="hlt">climate</span> change using an algorithm-based species’ trait approachHenry Lee II, Christina Folger, Deborah A. Reusser, Patrick Clinton, and Rene Graham1 U.S. EPA, Western Ecology Division, Newport, OR USA E-mail: lee.henry@ep...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFM.A14C..05M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFM.A14C..05M"><span>Ocean-Atmosphere Coupling Processes Affecting <span class="hlt">Predictability</span> in the <span class="hlt">Climate</span> System</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Miller, A. J.; Subramanian, A. C.; Seo, H.; Eliashiv, J. D.</p> <p>2017-12-01</p> <p><span class="hlt">Predictions</span> of the ocean and atmosphere are often sensitive to coupling at the air-sea interface in ways that depend on the temporal and spatial scales of the target fields. We will discuss several aspects of these types of coupled interactions including oceanic and atmospheric forecast applications. For oceanic mesoscale eddies, the coupling can influence the energetics of the oceanic flow itself. For Madden-Julian Oscillation onset, the coupling timestep should resolve the diurnal cycle to properly raise time-mean SST and latent heat flux prior to deep convection. For Atmospheric River events, the evolving SST field can alter the trajectory and intensity of precipitation anomalies along the California coast. Improvements in <span class="hlt">predictions</span> will also rely on identifying and alleviating sources of biases in the <span class="hlt">climate</span> states of the coupled system. Surprisingly, forecast skill can also be improved by enhancing stochastic variability in the atmospheric component of coupled models as found in a multiscale ensemble modeling approach.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5430113','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5430113"><span>The Odds of Success: <span class="hlt">Predicting</span> Registered Health Information <span class="hlt">Administrator</span> Exam Success</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Dolezel, Diane; McLeod, Alexander</p> <p>2017-01-01</p> <p>The purpose of this study was to craft a <span class="hlt">predictive</span> model to examine the relationship between grades in specific academic courses, overall grade point average (GPA), on-campus versus online course delivery, and success in passing the Registered Health Information <span class="hlt">Administrator</span> (RHIA) exam on the first attempt. Because student success in passing the exam on the first attempt is assessed as part of the accreditation process, this study is important to health information management (HIM) programs. Furthermore, passing the exam greatly expands the graduate's job possibilities because the demand for credentialed graduates far exceeds the supply of credentialed graduates. Binary logistic regression was utilized to explore the relationships between the predictor variables and success in passing the RHIA exam on the first attempt. Results indicate that the student's cumulative GPA, specific HIM course grades, and course delivery method were <span class="hlt">predictive</span> of success. PMID:28566994</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_16");'>16</a></li> <li><a href="#" onclick='return showDiv("page_17");'>17</a></li> <li class="active"><span>18</span></li> <li><a href="#" onclick='return showDiv("page_19");'>19</a></li> <li><a href="#" onclick='return showDiv("page_20");'>20</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_18 --> <div id="page_19" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_17");'>17</a></li> <li><a href="#" onclick='return showDiv("page_18");'>18</a></li> <li class="active"><span>19</span></li> <li><a href="#" onclick='return showDiv("page_20");'>20</a></li> <li><a href="#" onclick='return showDiv("page_21");'>21</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="361"> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3729955','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3729955"><span>Pathogen-Host Associations and <span class="hlt">Predicted</span> Range Shifts of Human Monkeypox in Response to <span class="hlt">Climate</span> Change in Central Africa</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Thomassen, Henri A.; Fuller, Trevon; Asefi-Najafabady, Salvi; Shiplacoff, Julia A. G.; Mulembakani, Prime M.; Blumberg, Seth; Johnston, Sara C.; Kisalu, Neville K.; Kinkela, Timothée L.; Fair, Joseph N.; Wolfe, Nathan D.; Shongo, Robert L.; LeBreton, Matthew; Meyer, Hermann; Wright, Linda L.; Muyembe, Jean-Jacques; Buermann, Wolfgang; Okitolonda, Emile; Hensley, Lisa E.; Lloyd-Smith, James O.; Smith, Thomas B.; Rimoin, Anne W.</p> <p>2013-01-01</p> <p><span class="hlt">Climate</span> change is <span class="hlt">predicted</span> to result in changes in the geographic ranges and local prevalence of infectious diseases, either through direct effects on the pathogen, or indirectly through range shifts in vector and reservoir species. To better understand the occurrence of monkeypox virus (MPXV), an emerging Orthopoxvirus in humans, under contemporary and future <span class="hlt">climate</span> conditions, we used ecological niche modeling techniques in conjunction with <span class="hlt">climate</span> and remote-sensing variables. We first created spatially explicit probability distributions of its candidate reservoir species in Africa's Congo Basin. Reservoir species distributions were subsequently used to model current and projected future distributions of human monkeypox (MPX). Results indicate that forest clearing and <span class="hlt">climate</span> are significant driving factors of the transmission of MPX from wildlife to humans under current <span class="hlt">climate</span> conditions. Models under contemporary <span class="hlt">climate</span> conditions performed well, as indicated by high values for the area under the receiver operator curve (AUC), and tests on spatially randomly and non-randomly omitted test data. Future projections were made on IPCC 4th Assessment <span class="hlt">climate</span> change scenarios for 2050 and 2080, ranging from more conservative to more aggressive, and representing the potential variation within which range shifts can be expected to occur. Future projections showed range shifts into regions where MPX has not been recorded previously. Increased suitability for MPX was <span class="hlt">predicted</span> in eastern Democratic Republic of Congo. Models developed here are useful for identifying areas where environmental conditions may become more suitable for human MPX; targeting candidate reservoir species for future screening efforts; and prioritizing regions for future MPX surveillance efforts. PMID:23935820</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015ClDy...44..559H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015ClDy...44..559H"><span><span class="hlt">Climate</span> drift of AMOC, North Atlantic salinity and arctic sea ice in CFSv2 decadal <span class="hlt">predictions</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Huang, Bohua; Zhu, Jieshun; Marx, Lawrence; Wu, Xingren; Kumar, Arun; Hu, Zeng-Zhen; Balmaseda, Magdalena A.; Zhang, Shaoqing; Lu, Jian; Schneider, Edwin K.; Kinter, James L., III</p> <p>2015-01-01</p> <p>There are potential advantages to extending operational seasonal forecast models to <span class="hlt">predict</span> decadal variability but major efforts are required to assess the model fidelity for this task. In this study, we examine the North Atlantic <span class="hlt">climate</span> simulated by the NCEP <span class="hlt">Climate</span> Forecast System, version 2 (CFSv2), using a set of ensemble decadal hindcasts and several 30-year simulations initialized from realistic ocean-atmosphere states. It is found that a substantial <span class="hlt">climate</span> drift occurs in the first few years of the CFSv2 hindcasts, which represents a major systematic bias and may seriously affect the model's fidelity for decadal <span class="hlt">prediction</span>. In particular, it is noted that a major reduction of the upper ocean salinity in the northern North Atlantic weakens the Atlantic meridional overturning circulation (AMOC) significantly. This freshening is likely caused by the excessive freshwater transport from the Arctic Ocean and weakened subtropical water transport by the North Atlantic Current. A potential source of the excessive freshwater is the quick melting of sea ice, which also causes unrealistically thin ice cover in the Arctic Ocean. Our sensitivity experiments with adjusted sea ice albedo parameters produce a sustainable ice cover with realistic thickness distribution. It also leads to a moderate increase of the AMOC strength. This study suggests that a realistic freshwater balance, including a proper sea ice feedback, is crucial for simulating the North Atlantic <span class="hlt">climate</span> and its variability.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2011AGUFMGC43B0900C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2011AGUFMGC43B0900C"><span>Evaluating the uncertainty of <span class="hlt">predicting</span> future <span class="hlt">climate</span> time series at the hourly time scale</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Caporali, E.; Fatichi, S.; Ivanov, V. Y.</p> <p>2011-12-01</p> <p>A stochastic downscaling methodology is developed to generate hourly, point-scale time series for several meteorological variables, such as precipitation, cloud cover, shortwave radiation, air temperature, relative humidity, wind speed, and atmospheric pressure. The methodology uses multi-model General Circulation Model (GCM) realizations and an hourly weather generator, AWE-GEN. Probabilistic descriptions of factors of change (a measure of <span class="hlt">climate</span> change with respect to historic conditions) are computed for several <span class="hlt">climate</span> statistics and different aggregation times using a Bayesian approach that weights the individual GCM contributions. The Monte Carlo method is applied to sample the factors of change from their respective distributions thereby permitting the generation of time series in an ensemble fashion, which reflects the uncertainty of <span class="hlt">climate</span> projections of future as well as the uncertainty of the downscaling procedure. Applications of the methodology and probabilistic expressions of certainty in reproducing future <span class="hlt">climates</span> for the periods, 2000 - 2009, 2046 - 2065 and 2081 - 2100, using the 1962 - 1992 period as the baseline, are discussed for the location of Firenze (Italy). The <span class="hlt">climate</span> <span class="hlt">predictions</span> for the period of 2000 - 2009 are tested against observations permitting to assess the reliability and uncertainties of the methodology in reproducing statistics of meteorological variables at different time scales.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/24788252','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/24788252"><span>The effect of organizational <span class="hlt">climate</span> on patient-centered medical home implementation.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Reddy, Ashok; Shea, Judy A; Canamucio, Anne; Werner, Rachel M</p> <p>2015-01-01</p> <p>Organizational <span class="hlt">climate</span> is a key determinant of successful adoption of innovations; however, its relation to medical home implementation is unknown. This study examined the association between primary care providers' (PCPs') perception of organization <span class="hlt">climate</span> and medical home implementation in the Veterans Health <span class="hlt">Administration</span>. Multivariate regression was used to test the hypothesis that organizational <span class="hlt">climate</span> <span class="hlt">predicts</span> medical home implementation. This analysis of 191 PCPs found that higher scores in 2 domains of organizational <span class="hlt">climate</span> (communication and cooperation, and orientation to quality improvement) were associated with a statistically significantly higher percentage (from 7 to 10 percentage points) of PCPs implementing structural changes to support the medical home model. In addition, some aspects of a better organizational <span class="hlt">climate</span> were associated with improved organizational processes of care, including a higher percentage of patients contacted within 2 days of hospital discharge (by 2 to 3 percentage points) and appointments made within 3 days of a patient request (by 2 percentage points). © The Author(s) 2014.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://cfpub.epa.gov/si/si_public_record_report.cfm?dirEntryId=234506&keyword=Mathematical+AND+modeling&actType=&TIMSType=+&TIMSSubTypeID=&DEID=&epaNumber=&ntisID=&archiveStatus=Both&ombCat=Any&dateBeginCreated=&dateEndCreated=&dateBeginPublishedPresented=&dateEndPublishedPresented=&dateBeginUpdated=&dateEndUpdated=&dateBeginCompleted=&dateEndCompleted=&personID=&role=Any&journalID=&publisherID=&sortBy=revisionDate&count=50','EPA-EIMS'); return false;" href="https://cfpub.epa.gov/si/si_public_record_report.cfm?dirEntryId=234506&keyword=Mathematical+AND+modeling&actType=&TIMSType=+&TIMSSubTypeID=&DEID=&epaNumber=&ntisID=&archiveStatus=Both&ombCat=Any&dateBeginCreated=&dateEndCreated=&dateBeginPublishedPresented=&dateEndPublishedPresented=&dateBeginUpdated=&dateEndUpdated=&dateBeginCompleted=&dateEndCompleted=&personID=&role=Any&journalID=&publisherID=&sortBy=revisionDate&count=50"><span><span class="hlt">Predicting</span> Plausible Impacts of Sets of <span class="hlt">Climate</span> and Land Use Change Scenarios on Water Resources</span></a></p> <p><a target="_blank" href="http://oaspub.epa.gov/eims/query.page">EPA Science Inventory</a></p> <p></p> <p></p> <p>Global changes in <span class="hlt">climate</span> and land use can alTect the quantity and quality of water resources. Hence, we need a methodology to <span class="hlt">predict</span> these ramifications. Using the Little Miami River (LMR) watershed as a case study, this paper describes a spatial analytical approach integrating...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013AGUFM.H21F1117P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013AGUFM.H21F1117P"><span><span class="hlt">Predicting</span> the Affects of <span class="hlt">Climate</span> Change on Evapotranspiration and Agricultural Productivity of Semi-arid Basins</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Peri, L.; Tyler, S. W.; Zheng, C.; Pohll, G. M.; Yao, Y.</p> <p>2013-12-01</p> <p>Many arid and semi-arid regions around the world are experiencing water shortages that have become increasingly problematic. Since the late 1800s, upstream diversions in Nevada's Walker River have delivered irrigation supply to the surrounding agricultural fields resulting in a dramatic water level decline of the terminal Walker Lake. Salinity has also increased because the only outflow from the lake is evaporation from the lake surface. The Heihe River basin of northwestern China, a similar semi-arid catchment, is also facing losses from evaporation of terminal locations, agricultural diversions and evapotranspiration (ET) of crops. Irrigated agriculture is now experiencing increased competition for use of diminishing water resources while a demand for ecological conservation continues to grow. It is important to understand how the existing agriculture in these regions will respond as <span class="hlt">climate</span> changes. <span class="hlt">Predicting</span> the affects of <span class="hlt">climate</span> change on groundwater flow, surface water flow, ET and agricultural productivity of the Walker and Heihe River basins is essential for future conservation of water resources. ET estimates from remote sensing techniques can provide estimates of crop water consumption. By determining similarities of both hydrologic cycles, critical components missing in both systems can be determined and <span class="hlt">predictions</span> of impacts of <span class="hlt">climate</span> change and human management strategies can be assessed.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5432165','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5432165"><span>Continental divide: <span class="hlt">Predicting</span> <span class="hlt">climate</span>-mediated fragmentation and biodiversity loss in the boreal forest</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Murray, Dennis L.; Peers, Michael J. L.; Majchrzak, Yasmine N.; Wehtje, Morgan; Ferreira, Catarina; Pickles, Rob S. A.; Row, Jeffrey R.; Thornton, Daniel H.</p> <p>2017-01-01</p> <p><span class="hlt">Climate</span> change threatens natural landscapes through shifting distribution and abundance of species and attendant change in the structure and function of ecosystems. However, it remains unclear how <span class="hlt">climate</span>-mediated variation in species’ environmental niche space may lead to large-scale fragmentation of species distributions, altered meta-population dynamics and gene flow, and disrupted ecosystem integrity. Such change may be especially relevant when species distributions are restricted either spatially or to a narrow environmental niche, or when environments are rapidly changing. Here, we use range-wide environmental niche models to posit that <span class="hlt">climate</span>-mediated range fragmentation aggravates the direct effects of <span class="hlt">climate</span> change on species in the boreal forest of North America. We show that <span class="hlt">climate</span> change will directly alter environmental niche suitability for boreal-obligate species of trees, birds and mammals (n = 12), with most species ranges becoming smaller and shifting northward through time. Importantly, species distributions will become increasingly fragmented, as characterized by smaller mean size and greater isolation of environmentally-suitable landscape patches. This loss is especially pronounced along the Ontario-Québec border, where the boreal forest is narrowest and roughly 78% of suitable niche space could disappear by 2080. Despite the diversity of taxa surveyed, patterns of range fragmentation are remarkably consistent, with our models <span class="hlt">predicting</span> that spruce grouse (Dendragapus canadensis), boreal chickadee (Poecile hudsonicus), moose (Alces americanus) and caribou (Rangifer tarandus) could have entirely disjunct east-west population segments in North America. These findings reveal potentially dire consequences of <span class="hlt">climate</span> change on population continuity and species diversity in the boreal forest, highlighting the need to better understand: 1) extent and primary drivers of anticipated <span class="hlt">climate</span>-mediated range loss and fragmentation; 2) diversity of</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/28505173','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/28505173"><span>Continental divide: <span class="hlt">Predicting</span> <span class="hlt">climate</span>-mediated fragmentation and biodiversity loss in the boreal forest.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Murray, Dennis L; Peers, Michael J L; Majchrzak, Yasmine N; Wehtje, Morgan; Ferreira, Catarina; Pickles, Rob S A; Row, Jeffrey R; Thornton, Daniel H</p> <p>2017-01-01</p> <p><span class="hlt">Climate</span> change threatens natural landscapes through shifting distribution and abundance of species and attendant change in the structure and function of ecosystems. However, it remains unclear how <span class="hlt">climate</span>-mediated variation in species' environmental niche space may lead to large-scale fragmentation of species distributions, altered meta-population dynamics and gene flow, and disrupted ecosystem integrity. Such change may be especially relevant when species distributions are restricted either spatially or to a narrow environmental niche, or when environments are rapidly changing. Here, we use range-wide environmental niche models to posit that <span class="hlt">climate</span>-mediated range fragmentation aggravates the direct effects of <span class="hlt">climate</span> change on species in the boreal forest of North America. We show that <span class="hlt">climate</span> change will directly alter environmental niche suitability for boreal-obligate species of trees, birds and mammals (n = 12), with most species ranges becoming smaller and shifting northward through time. Importantly, species distributions will become increasingly fragmented, as characterized by smaller mean size and greater isolation of environmentally-suitable landscape patches. This loss is especially pronounced along the Ontario-Québec border, where the boreal forest is narrowest and roughly 78% of suitable niche space could disappear by 2080. Despite the diversity of taxa surveyed, patterns of range fragmentation are remarkably consistent, with our models <span class="hlt">predicting</span> that spruce grouse (Dendragapus canadensis), boreal chickadee (Poecile hudsonicus), moose (Alces americanus) and caribou (Rangifer tarandus) could have entirely disjunct east-west population segments in North America. These findings reveal potentially dire consequences of <span class="hlt">climate</span> change on population continuity and species diversity in the boreal forest, highlighting the need to better understand: 1) extent and primary drivers of anticipated <span class="hlt">climate</span>-mediated range loss and fragmentation; 2) diversity of</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29651147','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29651147"><span>Response to <span class="hlt">climate</span> change of montane herbaceous plants in the genus Rhodiola <span class="hlt">predicted</span> by ecological niche modelling.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>You, Jianling; Qin, Xiaoping; Ranjitkar, Sailesh; Lougheed, Stephen C; Wang, Mingcheng; Zhou, Wen; Ouyang, Dongxin; Zhou, Yin; Xu, Jianchu; Zhang, Wenju; Wang, Yuguo; Yang, Ji; Song, Zhiping</p> <p>2018-04-12</p> <p><span class="hlt">Climate</span> change profoundly influences species distributions. These effects are evident in poleward latitudinal range shifts for many taxa, and upward altitudinal range shifts for alpine species, that resulted from increased annual global temperatures since the Last Glacial Maximum (LGM, ca. 22,000 BP). For the latter, the ultimate consequence of upward shifts may be extinction as species in the highest alpine ecosystems can migrate no further, a phenomenon often characterized as "nowhere to go". To <span class="hlt">predict</span> responses to <span class="hlt">climate</span> change of the alpine plants on the Qinghai-Tibetan Plateau (QTP), we used ecological niche modelling (ENM) to estimate the range shifts of 14 Rhodiola species, beginning with the Last Interglacial (ca. 120,000-140,000 BP) through to 2050. Distributions of Rhodiola species appear to be shaped by temperature-related variables. The southeastern QTP, and especially the Hengduan Mountains, were the origin and center of distribution for Rhodiola, and also served as refugia during the LGM. Under future <span class="hlt">climate</span> scenario in 2050, Rhodiola species might have to migrate upward and northward, but many species would expand their ranges contra the <span class="hlt">prediction</span> of the "nowhere to go" hypothesis, caused by the appearance of additional potential habitat concomitant with the reduction of permafrost with <span class="hlt">climate</span> warming.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/24446429','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/24446429"><span><span class="hlt">Predicting</span> plant invasions under <span class="hlt">climate</span> change: are species distribution models validated by field trials?</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Sheppard, Christine S; Burns, Bruce R; Stanley, Margaret C</p> <p>2014-09-01</p> <p><span class="hlt">Climate</span> change may facilitate alien species invasion into new areas, particularly for species from warm native ranges introduced into areas currently marginal for temperature. Although conclusions from modelling approaches and experimental studies are generally similar, combining the two approaches has rarely occurred. The aim of this study was to validate species distribution models by conducting field trials in sites of differing suitability as <span class="hlt">predicted</span> by the models, thus increasing confidence in their ability to assess invasion risk. Three recently naturalized alien plants in New Zealand were used as study species (Archontophoenix cunninghamiana, Psidium guajava and Schefflera actinophylla): they originate from warm native ranges, are woody bird-dispersed species and of concern as potential weeds. Seedlings were grown in six sites across the country, differing both in <span class="hlt">climate</span> and suitability (as <span class="hlt">predicted</span> by the species distribution models). Seedling growth and survival were recorded over two summers and one or two winter seasons, and temperature and precipitation were monitored hourly at each site. Additionally, alien seedling performances were compared to those of closely related native species (Rhopalostylis sapida, Lophomyrtus bullata and Schefflera digitata). Furthermore, half of the seedlings were sprayed with pesticide, to investigate whether enemy release may influence performance. The results showed large differences in growth and survival of the alien species among the six sites. In the more suitable sites, performance was frequently higher compared to the native species. Leaf damage from invertebrate herbivory was low for both alien and native seedlings, with little evidence that the alien species should have an advantage over the native species because of enemy release. Correlations between performance in the field and <span class="hlt">predicted</span> suitability of species distribution models were generally high. The projected increase in minimum temperature and reduced</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/25856241','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/25856241"><span><span class="hlt">Predicting</span> plant diversity patterns in Madagascar: understanding the effects of <span class="hlt">climate</span> and land cover change in a biodiversity hotspot.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Brown, Kerry A; Parks, Katherine E; Bethell, Colin A; Johnson, Steig E; Mulligan, Mark</p> <p>2015-01-01</p> <p><span class="hlt">Climate</span> and land cover change are driving a major reorganization of terrestrial biotic communities in tropical ecosystems. In an effort to understand how biodiversity patterns in the tropics will respond to individual and combined effects of these two drivers of environmental change, we use species distribution models (SDMs) calibrated for recent <span class="hlt">climate</span> and land cover variables and projected to future scenarios to <span class="hlt">predict</span> changes in diversity patterns in Madagascar. We collected occurrence records for 828 plant genera and 2186 plant species. We developed three scenarios, (i.e., <span class="hlt">climate</span> only, land cover only and combined <span class="hlt">climate</span>-land cover) based on recent and future <span class="hlt">climate</span> and land cover variables. We used this modelling framework to investigate how the impacts of changes to <span class="hlt">climate</span> and land cover influenced biodiversity across ecoregions and elevation bands. There were large-scale <span class="hlt">climate</span>- and land cover-driven changes in plant biodiversity across Madagascar, including both losses and gains in diversity. The sharpest declines in biodiversity were projected for the eastern escarpment and high elevation ecosystems. Sharp declines in diversity were driven by the combined <span class="hlt">climate</span>-land cover scenarios; however, there were subtle, region-specific differences in model outputs for each scenario, where certain regions experienced relatively higher species loss under <span class="hlt">climate</span> or land cover only models. We strongly caution that <span class="hlt">predicted</span> future gains in plant diversity will depend on the development and maintenance of dispersal pathways that connect current and future suitable habitats. The forecast for Madagascar's plant diversity in the face of future environmental change is worrying: regional diversity will continue to decrease in response to the combined effects of <span class="hlt">climate</span> and land cover change, with habitats such as ericoid thickets and eastern lowland and sub-humid forests particularly vulnerable into the future.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4391717','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4391717"><span><span class="hlt">Predicting</span> Plant Diversity Patterns in Madagascar: Understanding the Effects of <span class="hlt">Climate</span> and Land Cover Change in a Biodiversity Hotspot</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Brown, Kerry A.; Parks, Katherine E.; Bethell, Colin A.; Johnson, Steig E.; Mulligan, Mark</p> <p>2015-01-01</p> <p><span class="hlt">Climate</span> and land cover change are driving a major reorganization of terrestrial biotic communities in tropical ecosystems. In an effort to understand how biodiversity patterns in the tropics will respond to individual and combined effects of these two drivers of environmental change, we use species distribution models (SDMs) calibrated for recent <span class="hlt">climate</span> and land cover variables and projected to future scenarios to <span class="hlt">predict</span> changes in diversity patterns in Madagascar. We collected occurrence records for 828 plant genera and 2186 plant species. We developed three scenarios, (i.e., <span class="hlt">climate</span> only, land cover only and combined <span class="hlt">climate</span>-land cover) based on recent and future <span class="hlt">climate</span> and land cover variables. We used this modelling framework to investigate how the impacts of changes to <span class="hlt">climate</span> and land cover influenced biodiversity across ecoregions and elevation bands. There were large-scale <span class="hlt">climate</span>- and land cover-driven changes in plant biodiversity across Madagascar, including both losses and gains in diversity. The sharpest declines in biodiversity were projected for the eastern escarpment and high elevation ecosystems. Sharp declines in diversity were driven by the combined <span class="hlt">climate</span>-land cover scenarios; however, there were subtle, region-specific differences in model outputs for each scenario, where certain regions experienced relatively higher species loss under <span class="hlt">climate</span> or land cover only models. We strongly caution that <span class="hlt">predicted</span> future gains in plant diversity will depend on the development and maintenance of dispersal pathways that connect current and future suitable habitats. The forecast for Madagascar’s plant diversity in the face of future environmental change is worrying: regional diversity will continue to decrease in response to the combined effects of <span class="hlt">climate</span> and land cover change, with habitats such as ericoid thickets and eastern lowland and sub-humid forests particularly vulnerable into the future. PMID:25856241</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.cpc.ncep.noaa.gov/data','SCIGOVWS'); return false;" href="http://www.cpc.ncep.noaa.gov/data"><span><span class="hlt">Climate</span> <span class="hlt">Prediction</span> Center - Monitoring & Data Index</span></a></p> <p><a target="_blank" href="http://www.science.gov/aboutsearch.html">Science.gov Websites</a></p> <p></p> <p></p> <p>Data North American Monsoon Experiment United States <span class="hlt">Climate</span> Data & Graphics ENSO <em>Impacts</em> on the United States Previous ENSO Events El Niño <em>Impacts</em> on United States <span class="hlt">Climate</span> El Niño <em>Impacts</em> State by State La Niña <em>Impacts</em> by Region El Niño's Influence on United States Precipitation Amounts El Niño</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016EGUGA..18.5251A','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016EGUGA..18.5251A"><span>Multi-scale enhancement of <span class="hlt">climate</span> <span class="hlt">prediction</span> over land by increasing the model sensitivity to vegetation variability in EC-Earth</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Alessandri, Andrea; Catalano, Franco; De Felice, Matteo; Van Den Hurk, Bart; Doblas Reyes, Francisco; Boussetta, Souhail; Balsamo, Gianpaolo; Miller, Paul</p> <p>2016-04-01</p> <p>The EC-Earth earth system model has been recently developed to include the dynamics of vegetation. In its original formulation, vegetation variability is simply operated by the Leaf Area Index (LAI), which affects <span class="hlt">climate</span> basically by changing the vegetation physiological resistance to evapotranspiration. This coupling has been found to have only a weak effect on the surface <span class="hlt">climate</span> modeled by EC-Earth. In reality, the effective sub-grid vegetation fractional coverage will vary seasonally and at interannual time-scales in response to leaf-canopy growth, phenology and senescence. Therefore it affects biophysical parameters such as the albedo, surface roughness and soil field capacity. To adequately represent this effect in EC-Earth, we included an exponential dependence of the vegetation cover on the LAI. By comparing two sets of simulations performed with and without the new variable fractional-coverage parameterization, spanning retrospective <span class="hlt">predictions</span> at the decadal (5-years), seasonal and sub-seasonal time-scales, we show for the first time a significant multi-scale enhancement of vegetation impacts in <span class="hlt">climate</span> simulation and <span class="hlt">prediction</span> over land. Particularly large effects at multiple time scales are shown over boreal winter middle-to-high latitudes over Canada, West US, Eastern Europe, Russia and eastern Siberia due to the implemented time-varying shadowing effect by tree-vegetation on snow surfaces. Over Northern Hemisphere boreal forest regions the improved representation of vegetation cover tends to correct the winter warm biases, improves the <span class="hlt">climate</span> change sensitivity, the decadal potential <span class="hlt">predictability</span> as well as the skill of forecasts at seasonal and sub-seasonal time-scales. Significant improvements of the <span class="hlt">prediction</span> of 2m temperature and rainfall are also shown over transitional land surface hot spots. Both the potential <span class="hlt">predictability</span> at decadal time-scale and seasonal-forecasts skill are enhanced over Sahel, North American Great Plains, Nordeste</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017JPhCS.887a2023Q','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017JPhCS.887a2023Q"><span>The <span class="hlt">prediction</span> of the impact of <span class="hlt">climatic</span> factors on short-term electric power load based on the big data of smart city</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Qiu, Yunfei; Li, Xizhong; Zheng, Wei; Hu, Qinghe; Wei, Zhanmeng; Yue, Yaqin</p> <p>2017-08-01</p> <p>The <span class="hlt">climate</span> changes have great impact on the residents’ electricity consumption, so the study on the impact of <span class="hlt">climatic</span> factors on electric power load is of significance. In this paper, the effects of the data of temperature, rainfall and wind of smart city on short-term power load is studied to <span class="hlt">predict</span> power load. The authors studied the relation between power load and daily temperature, rainfall and wind in the 31 days of January of one year. In the research, the authors used the Matlab neural network toolbox to establish the combinational forecasting model. The authors trained the original input data continuously to get the internal rules inside the data and used the rules to <span class="hlt">predict</span> the daily power load in the next January. The <span class="hlt">prediction</span> method relies on the accuracy of weather forecasting. If the weather forecasting is different from the actual weather, we need to correct the <span class="hlt">climatic</span> factors to ensure accurate <span class="hlt">prediction</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/servlets/purl/1225814','SCIGOV-STC'); return false;" href="https://www.osti.gov/servlets/purl/1225814"><span>Characterization of the Dynamics of <span class="hlt">Climate</span> Systems and Identification of Missing Mechanisms Impacting the Long Term <span class="hlt">Predictive</span> Capabilities of Global <span class="hlt">Climate</span> Models Utilizing Dynamical Systems Approaches to the Analysis of Observed and Modeled <span class="hlt">Climate</span></span></a></p> <p><a target="_blank" href="http://www.osti.gov/search">DOE Office of Scientific and Technical Information (OSTI.GOV)</a></p> <p>Bhatt, Uma S.; Wackerbauer, Renate; Polyakov, Igor V.</p> <p></p> <p>The goal of this research was to apply fractional and non-linear analysis techniques in order to develop a more complete characterization of <span class="hlt">climate</span> change and variability for the oceanic, sea ice and atmospheric components of the Earth System. This research applied two measures of dynamical characteristics of time series, the R/S method of calculating the Hurst exponent and Renyi entropy, to observational and modeled <span class="hlt">climate</span> data in order to evaluate how well <span class="hlt">climate</span> models capture the long-term dynamics evident in observations. Fractional diffusion analysis was applied to ARGO ocean buoy data to quantify ocean transport. Self organized maps were appliedmore » to North Pacific sea level pressure and analyzed in ways to improve seasonal <span class="hlt">predictability</span> for Alaska fire weather. This body of research shows that these methods can be used to evaluate <span class="hlt">climate</span> models and shed light on <span class="hlt">climate</span> mechanisms (i.e., understanding why something happens). With further research, these methods show promise for improving seasonal to longer time scale forecasts of <span class="hlt">climate</span>.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3492365','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3492365"><span>The Impact of <span class="hlt">Climate</span> Change on Indigenous Arabica Coffee (Coffea arabica): <span class="hlt">Predicting</span> Future Trends and Identifying Priorities</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Gole, Tadesse Woldemariam; Baena, Susana</p> <p>2012-01-01</p> <p>Precise modelling of the influence of <span class="hlt">climate</span> change on Arabica coffee is limited; there are no data available for indigenous populations of this species. In this study we model the present and future <span class="hlt">predicted</span> distribution of indigenous Arabica, and identify priorities in order to facilitate appropriate decision making for conservation, monitoring and future research. Using distribution data we perform bioclimatic modelling and examine future distribution with the HadCM3 <span class="hlt">climate</span> model for three emission scenarios (A1B, A2A, B2A) over three time intervals (2020, 2050, 2080). The models show a profoundly negative influence on indigenous Arabica. In a locality analysis the most favourable outcome is a c. 65% reduction in the number of pre-existing bioclimatically suitable localities, and at worst an almost 100% reduction, by 2080. In an area analysis the most favourable outcome is a 38% reduction in suitable bioclimatic space, and the least favourable a c. 90% reduction, by 2080. Based on known occurrences and ecological tolerances of Arabica, bioclimatic unsuitability would place populations in peril, leading to severe stress and a high risk of extinction. This study establishes a fundamental baseline for assessing the consequences of <span class="hlt">climate</span> change on wild populations of Arabica coffee. Specifically, it: (1) identifies and categorizes localities and areas that are <span class="hlt">predicted</span> to be under threat from <span class="hlt">climate</span> change now and in the short- to medium-term (2020–2050), representing assessment priorities for ex situ conservation; (2) identifies ‘core localities’ that could have the potential to withstand <span class="hlt">climate</span> change until at least 2080, and therefore serve as long-term in situ storehouses for coffee genetic resources; (3) provides the location and characterization of target locations (populations) for on-the-ground monitoring of <span class="hlt">climate</span> change influence. Arabica coffee is confimed as a <span class="hlt">climate</span> sensitivite species, supporting data and inference that existing</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3097397','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3097397"><span>The Relationship between Organizational <span class="hlt">Climate</span> and Quality of Chronic Disease Management</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Benzer, Justin K; Young, Gary; Stolzmann, Kelly; Osatuke, Katerine; Meterko, Mark; Caso, Allison; White, Bert; Mohr, David C</p> <p>2011-01-01</p> <p>Objective To test the utility of a two-dimensional model of organizational <span class="hlt">climate</span> for explaining variation in diabetes care between primary care clinics. Data Sources/Study Setting Secondary data were obtained from 223 primary care clinics in the Department of Veterans Affairs health care system. Study Design Organizational <span class="hlt">climate</span> was defined using the dimensions of task and relational <span class="hlt">climate</span>. The association between primary care organizational <span class="hlt">climate</span> and diabetes processes and intermediate outcomes were estimated for 4,539 patients in a cross-sectional study. Data Collection/Extraction Methods All data were collected from <span class="hlt">administrative</span> datasets. The <span class="hlt">climate</span> data were drawn from the 2007 VA All Employee Survey, and the outcomes data were collected as part of the VA External Peer Review Program. <span class="hlt">Climate</span> data were aggregated to the facility level of analysis and merged with patient-level data. Principal Findings Relational <span class="hlt">climate</span> was related to an increased likelihood of diabetes care process adherence, with significant but small effects for adherence to intermediate outcomes. Task <span class="hlt">climate</span> was generally not shown to be related to adherence. Conclusions The role of relational <span class="hlt">climate</span> in <span class="hlt">predicting</span> the quality of chronic care was supported. Future research should examine the mediators and moderators of relational <span class="hlt">climate</span> and further investigate task <span class="hlt">climate</span>. PMID:21210799</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/22384205','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/22384205"><span>A comparison of <span class="hlt">administrative</span> and physiologic <span class="hlt">predictive</span> models in determining risk adjusted mortality rates in critically ill patients.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Enfield, Kyle B; Schafer, Katherine; Zlupko, Mike; Herasevich, Vitaly; Novicoff, Wendy M; Gajic, Ognjen; Hoke, Tracey R; Truwit, Jonathon D</p> <p>2012-01-01</p> <p>Hospitals are increasingly compared based on clinical outcomes adjusted for severity of illness. Multiple methods exist to adjust for differences between patients. The challenge for consumers of this information, both the public and healthcare providers, is interpreting differences in risk adjustment models particularly when models differ in their use of <span class="hlt">administrative</span> and physiologic data. We set to examine how <span class="hlt">administrative</span> and physiologic models compare to each when applied to critically ill patients. We prospectively abstracted variables for a physiologic and <span class="hlt">administrative</span> model of mortality from two intensive care units in the United States. <span class="hlt">Predicted</span> mortality was compared through the Pearsons Product coefficient and Bland-Altman analysis. A subgroup of patients admitted directly from the emergency department was analyzed to remove potential confounding changes in condition prior to ICU admission. We included 556 patients from two academic medical centers in this analysis. The <span class="hlt">administrative</span> model and physiologic models <span class="hlt">predicted</span> mortalities for the combined cohort were 15.3% (95% CI 13.7%, 16.8%) and 24.6% (95% CI 22.7%, 26.5%) (t-test p-value<0.001). The r(2) for these models was 0.297. The Bland-Atlman plot suggests that at low <span class="hlt">predicted</span> mortality there was good agreement; however, as mortality increased the models diverged. Similar results were found when analyzing a subgroup of patients admitted directly from the emergency department. When comparing the two hospitals, there was a statistical difference when using the <span class="hlt">administrative</span> model but not the physiologic model. Unexplained mortality, defined as those patients who died who had a <span class="hlt">predicted</span> mortality less than 10%, was a rare event by either model. In conclusion, while it has been shown that <span class="hlt">administrative</span> models provide estimates of mortality that are similar to physiologic models in non-critically ill patients with pneumonia, our results suggest this finding can not be applied globally to</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFM.H23H1769K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFM.H23H1769K"><span><span class="hlt">Predicting</span> Plant-Accessible Water in the Critical Zone: Mountain Ecosystems in a Mediterranean <span class="hlt">Climate</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Klos, P. Z.; Goulden, M.; Riebe, C. S.; Tague, C.; O'Geen, A. T.; Flinchum, B. A.; Safeeq, M.; Conklin, M. H.; Hart, S. C.; Asefaw Berhe, A.; Hartsough, P. C.; Holbrook, S.; Bales, R. C.</p> <p>2017-12-01</p> <p>Enhanced understanding of subsurface water storage, and the below-ground architecture and processes that create it, will advance our ability to <span class="hlt">predict</span> how the impacts of <span class="hlt">climate</span> change - including drought, forest mortality, wildland fire, and strained water security - will take form in the decades to come. Previous research has examined the importance of plant-accessible water in soil, but in upland landscapes within Mediterranean <span class="hlt">climates</span> the soil is often only the upper extent of subsurface water storage. We draw insights from both this previous research and a case study of the Southern Sierra Critical Zone Observatory to: define attributes of subsurface storage, review observed patterns in its distribution, highlight nested methods for its estimation across scales, and showcase the fundamental processes controlling its formation. We observe that forest ecosystems at our sites subsist on lasting plant-accessible stores of subsurface water during the summer dry period and during multi-year droughts. This indicates that trees in these forest ecosystems are rooted deeply in the weathered, highly porous saprolite, which reaches up to 10-20 m beneath the surface. This confirms the importance of large volumes of subsurface water in supporting ecosystem resistance to <span class="hlt">climate</span> and landscape change across a range of spatiotemporal scales. This research enhances the ability to <span class="hlt">predict</span> the extent of deep subsurface storage across landscapes; aiding in the advancement of both critical zone science and the management of natural resources emanating from similar mountain ecosystems worldwide.</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_17");'>17</a></li> <li><a href="#" onclick='return showDiv("page_18");'>18</a></li> <li class="active"><span>19</span></li> <li><a href="#" onclick='return showDiv("page_20");'>20</a></li> <li><a href="#" onclick='return showDiv("page_21");'>21</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_19 --> <div id="page_20" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_18");'>18</a></li> <li><a href="#" onclick='return showDiv("page_19");'>19</a></li> <li class="active"><span>20</span></li> <li><a href="#" onclick='return showDiv("page_21");'>21</a></li> <li><a href="#" onclick='return showDiv("page_22");'>22</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="381"> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/25631995','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/25631995"><span><span class="hlt">Climate</span> variability slows evolutionary responses of Colias butterflies to recent <span class="hlt">climate</span> change.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Kingsolver, Joel G; Buckley, Lauren B</p> <p>2015-03-07</p> <p>How does recent <span class="hlt">climate</span> warming and <span class="hlt">climate</span> variability alter fitness, phenotypic selection and evolution in natural populations? We combine biophysical, demographic and evolutionary models with recent <span class="hlt">climate</span> data to address this question for the subalpine and alpine butterfly, Colias meadii, in the southern Rocky Mountains. We focus on <span class="hlt">predicting</span> patterns of selection and evolution for a key thermoregulatory trait, melanin (solar absorptivity) on the posterior ventral hindwings, which affects patterns of body temperature, flight activity, adult and egg survival, and reproductive success in Colias. Both mean annual summer temperatures and thermal variability within summers have increased during the past 60 years at subalpine and alpine sites. At the subalpine site, <span class="hlt">predicted</span> directional selection on wing absorptivity has shifted from generally positive (favouring increased wing melanin) to generally negative during the past 60 years, but there is substantial variation among years in the <span class="hlt">predicted</span> magnitude and direction of selection and the optimal absorptivity. The <span class="hlt">predicted</span> magnitude of directional selection at the alpine site declined during the past 60 years and varies substantially among years, but selection has generally been positive at this site. <span class="hlt">Predicted</span> evolutionary responses to mean <span class="hlt">climate</span> warming at the subalpine site since 1980 is small, because of the variability in selection and asymmetry of the fitness function. At both sites, the <span class="hlt">predicted</span> effects of adaptive evolution on mean population fitness are much smaller than the fluctuations in mean fitness due to <span class="hlt">climate</span> variability among years. Our analyses suggest that variation in <span class="hlt">climate</span> within and among years may strongly limit evolutionary responses of ectotherms to mean <span class="hlt">climate</span> warming in these habitats. © 2015 The Author(s) Published by the Royal Society. All rights reserved.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2009AGUFM.B21C..02S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2009AGUFM.B21C..02S"><span>Optimality Based Dynamic Plant Allocation Model: <span class="hlt">Predicting</span> Acclimation Response to <span class="hlt">Climate</span> Change</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Srinivasan, V.; Drewry, D.; Kumar, P.; Sivapalan, M.</p> <p>2009-12-01</p> <p>Allocation of assimilated carbon to different plant parts determines the future plant status and is important to <span class="hlt">predict</span> long term (months to years) vegetated land surface fluxes. Plants have the ability to modify their allometry and exhibit plasticity by varying the relative proportions of the structural biomass contained in each of its tissue. The ability of plants to be plastic provides them with the potential to acclimate to changing environmental conditions in order to enhance their probability of survival. Allometry based allocation models and other empirical allocation models do not account for plant plasticity cause by acclimation due to environmental changes. In the absence of a detailed understanding of the various biophysical processes involved in plant growth and development an optimality approach is adopted here to <span class="hlt">predict</span> carbon allocation in plants. Existing optimality based models of plant growth are either static or involve considerable empiricism. In this work, we adopt an optimality based approach (coupled with limitations on plant plasticity) to <span class="hlt">predict</span> the dynamic allocation of assimilated carbon to different plant parts. We explore the applicability of this approach using several optimization variables such as net primary productivity, net transpiration, realized growth rate, total end of growing season reproductive biomass etc. We use this approach to <span class="hlt">predict</span> the dynamic nature of plant acclimation in its allocation of carbon to different plant parts under current and future <span class="hlt">climate</span> scenarios. This approach is designed as a growth sub-model in the multi-layer canopy plant model (MLCPM) and is used to obtain land surface fluxes and plant properties over the growing season. The framework of this model is such that it retains the generality and can be applied to different types of ecosystems. We test this approach using the data from free air carbon dioxide enrichment (FACE) experiments using soybean crop at the Soy-FACE research site. Our</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017ClDy..tmp..897G','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017ClDy..tmp..897G"><span>The impacts of oceanic deep temperature perturbations in the North Atlantic on decadal <span class="hlt">climate</span> variability and <span class="hlt">predictability</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Germe, Agathe; Sévellec, Florian; Mignot, Juliette; Fedorov, Alexey; Nguyen, Sébastien; Swingedouw, Didier</p> <p>2017-12-01</p> <p>Decadal <span class="hlt">climate</span> <span class="hlt">predictability</span> in the North Atlantic is largely related to ocean low frequency variability, whose sensitivity to initial conditions is not very well understood. Recently, three-dimensional oceanic temperature anomalies optimally perturbing the North Atlantic Mean Temperature (NAMT) have been computed via an optimization procedure using a linear adjoint to a realistic ocean general circulation model. The spatial pattern of the identified perturbations, localized in the North Atlantic, has the largest magnitude between 1000 and 4000 m depth. In the present study, the impacts of these perturbations on NAMT, on the Atlantic meridional overturning circulation (AMOC), and on <span class="hlt">climate</span> in general are investigated in a global coupled model that uses the same ocean model as was used to compute the three-dimensional optimal perturbations. In the coupled model, these perturbations induce AMOC and NAMT anomalies peaking after 5 and 10 years, respectively, generally consistent with the ocean-only linear <span class="hlt">predictions</span>. To further understand their impact, their magnitude was varied in a broad range. For initial perturbations with a magnitude comparable to the internal variability of the coupled model, the model response exhibits a strong signature in sea surface temperature and precipitation over North America and the Sahel region. The existence and impacts of these ocean perturbations have important implications for decadal <span class="hlt">prediction</span>: they can be seen either as a source of <span class="hlt">predictability</span> or uncertainty, depending on whether the current observing system can detect them or not. In fact, comparing the magnitude of the imposed perturbations with the uncertainty of available ocean observations such as Argo data or ocean state estimates suggests that only the largest perturbations used in this study could be detectable. This highlights the importance for decadal <span class="hlt">climate</span> <span class="hlt">prediction</span> of accurate ocean density initialisation in the North Atlantic at intermediate and greater</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/26436603','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/26436603"><span><span class="hlt">Predicting</span> non-familial major physical violent crime perpetration in the US Army from <span class="hlt">administrative</span> data.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Rosellini, A J; Monahan, J; Street, A E; Heeringa, S G; Hill, E D; Petukhova, M; Reis, B Y; Sampson, N A; Bliese, P; Schoenbaum, M; Stein, M B; Ursano, R J; Kessler, R C</p> <p>2016-01-01</p> <p>Although interventions exist to reduce violent crime, optimal implementation requires accurate targeting. We report the results of an attempt to develop an actuarial model using machine learning methods to <span class="hlt">predict</span> future violent crimes among US Army soldiers. A consolidated <span class="hlt">administrative</span> database for all 975 057 soldiers in the US Army in 2004-2009 was created in the Army Study to Assess Risk and Resilience in Servicemembers (Army STARRS). Of these soldiers, 5771 committed a first founded major physical violent crime (murder-manslaughter, kidnapping, aggravated arson, aggravated assault, robbery) over that time period. Temporally prior <span class="hlt">administrative</span> records measuring socio-demographic, Army career, criminal justice, medical/pharmacy, and contextual variables were used to build an actuarial model for these crimes separately among men and women using machine learning methods (cross-validated stepwise regression, random forests, penalized regressions). The model was then validated in an independent 2011-2013 sample. Key predictors were indicators of disadvantaged social/socioeconomic status, early career stage, prior crime, and mental disorder treatment. Area under the receiver-operating characteristic curve was 0.80-0.82 in 2004-2009 and 0.77 in the 2011-2013 validation sample. Of all <span class="hlt">administratively</span> recorded crimes, 36.2-33.1% (male-female) were committed by the 5% of soldiers having the highest <span class="hlt">predicted</span> risk in 2004-2009 and an even higher proportion (50.5%) in the 2011-2013 validation sample. Although these results suggest that the models could be used to target soldiers at high risk of violent crime perpetration for preventive interventions, final implementation decisions would require further validation and weighing of <span class="hlt">predicted</span> effectiveness against intervention costs and competing risks.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2007AGUFM.C21B0444W','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2007AGUFM.C21B0444W"><span><span class="hlt">Predicting</span> Soil Frost and its Response to <span class="hlt">Climate</span> Change in Northeastern U.S. Forests</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Wicklein, H. F.; Ollinger, S. V.; Campbell, J.; Frolking, S.</p> <p>2007-12-01</p> <p>Depth and duration of seasonal snow cover has important effects on temperate forest ecosystems. In the northeastern U.S., recent <span class="hlt">predictions</span> are that <span class="hlt">climate</span> warming over the coming century will cause an increase in soil freezing as soils lose the insulation of continuous wintertime snow cover. These studies have also linked soil freezing to elevated nitrate export from soils and streams. In the present study, we used a physically based energy and water exchange model, SHAW (Simultaneous Heat and Water), to <span class="hlt">predict</span> soil frost and snowpack dynamics at three forested sites in New England: Hubbard Brook (NH), Harvard Forest (MA), and Howland Forest (ME). Results indicate an inverse relationship across all three sites between the depth and duration of the snowpack and soil frost. Simulations were conducted for all three sites with historical weather data for the past 20-40 years, and for future projections (2000-2100) using two different IPCC <span class="hlt">climate</span> scenarios (A1fi and BI) derived from statistically downscaled GCM simulations. Under both scenarios and at all three sites, SHAW <span class="hlt">predicted</span> that both the amount of soil frost and the number of extreme soil freezing events will decrease during the 2000-2100 period. In addition, there was no relationship between <span class="hlt">predicted</span> soil frost, 1966-2000, and observed stream nitrate concentration at Hubbard Brook. These results run counter to existing theories regarding both the impacts of soil frost and the changes that are expected to occur into the future. There was, however, a positive correlation between <span class="hlt">predicted</span> soil frost and growing season CO2 uptake at Harvard Forest over the 1992-2002 period. This suggests that soil freezing does play an important role in forest biogeochemistry, albeit a different role than that which has been discussed in the literature.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017EGUGA..19.8858P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017EGUGA..19.8858P"><span>Nonlinear Synergistic Emergence and <span class="hlt">Predictability</span> in Complex Systems: Theory and Hydro-<span class="hlt">Climatic</span> Applications</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Perdigão, Rui A. P.; Hall, Julia; Pires, Carlos A. L.; Blöschl, Günter</p> <p>2017-04-01</p> <p>Classical and stochastic dynamical system theories assume structural coherence and dynamic recurrence with invariants of motion that are not necessarily so. These are grounded on the unproven assumption of universality in the dynamic laws derived from statistical kinematic evaluation of non-representative empirical records. As a consequence, the associated formulations revolve around a restrictive set of configurations and intermittencies e.g. in an ergodic setting, beyond which any <span class="hlt">predictability</span> is essentially elusive. Moreover, dynamical systems are fundamentally framed around dynamic codependence among intervening processes, i.e. entail essentially redundant interactions such as couplings and feedbacks. That precludes synergistic cooperation among processes that, whilst independent from each other, jointly produce emerging dynamic behaviour not present in any of the intervening parties. In order to overcome these fundamental limitations, we introduce a broad class of non-recursive dynamical systems that formulate dynamic emergence of unprecedented states in a fundamental synergistic manner, with fundamental principles in mind. The overall theory enables innovations to be <span class="hlt">predicted</span> from the internal system dynamics before any a priori information is provided about the associated dynamical properties. The theory is then illustrated to anticipate, from non-emergent records, the spatiotemporal emergence of multiscale hyper chaotic regimes, critical transitions and structural coevolutionary changes in synthetic and real-world complex systems. Example applications are provided within the hydro-<span class="hlt">climatic</span> context, formulating and dynamically forecasting evolving hydro-<span class="hlt">climatic</span> distributions, including the emergence of extreme precipitation and flooding in a structurally changing hydro-<span class="hlt">climate</span> system. Validation is then conducted with a posteriori verification of the simulated dynamics against observational records. Agreement between simulations and observations is</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/24986530','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/24986530"><span>Robust model <span class="hlt">predictive</span> control for optimal continuous drug <span class="hlt">administration</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Sopasakis, Pantelis; Patrinos, Panagiotis; Sarimveis, Haralambos</p> <p>2014-10-01</p> <p>In this paper the model <span class="hlt">predictive</span> control (MPC) technology is used for tackling the optimal drug <span class="hlt">administration</span> problem. The important advantage of MPC compared to other control technologies is that it explicitly takes into account the constraints of the system. In particular, for drug treatments of living organisms, MPC can guarantee satisfaction of the minimum toxic concentration (MTC) constraints. A whole-body physiologically-based pharmacokinetic (PBPK) model serves as the dynamic <span class="hlt">prediction</span> model of the system after it is formulated as a discrete-time state-space model. Only plasma measurements are assumed to be measured on-line. The rest of the states (drug concentrations in other organs and tissues) are estimated in real time by designing an artificial observer. The complete system (observer and MPC controller) is able to drive the drug concentration to the desired levels at the organs of interest, while satisfying the imposed constraints, even in the presence of modelling errors, disturbances and noise. A case study on a PBPK model with 7 compartments, constraints on 5 tissues and a variable drug concentration set-point illustrates the efficiency of the methodology in drug dosing control applications. The proposed methodology is also tested in an uncertain setting and proves successful in presence of modelling errors and inaccurate measurements. Copyright © 2014 Elsevier Ireland Ltd. All rights reserved.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/20098495','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/20098495"><span><span class="hlt">Climate</span> change and risk of leishmaniasis in north america: <span class="hlt">predictions</span> from ecological niche models of vector and reservoir species.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>González, Camila; Wang, Ophelia; Strutz, Stavana E; González-Salazar, Constantino; Sánchez-Cordero, Víctor; Sarkar, Sahotra</p> <p>2010-01-19</p> <p><span class="hlt">Climate</span> change is increasingly being implicated in species' range shifts throughout the world, including those of important vector and reservoir species for infectious diseases. In North America (México, United States, and Canada), leishmaniasis is a vector-borne disease that is autochthonous in México and Texas and has begun to expand its range northward. Further expansion to the north may be facilitated by <span class="hlt">climate</span> change as more habitat becomes suitable for vector and reservoir species for leishmaniasis. The analysis began with the construction of ecological niche models using a maximum entropy algorithm for the distribution of two sand fly vector species (Lutzomyia anthophora and L. diabolica), three confirmed rodent reservoir species (Neotoma albigula, N. floridana, and N. micropus), and one potential rodent reservoir species (N. mexicana) for leishmaniasis in northern México and the United States. As input, these models used species' occurrence records with topographic and <span class="hlt">climatic</span> parameters as explanatory variables. Models were tested for their ability to <span class="hlt">predict</span> correctly both a specified fraction of occurrence points set aside for this purpose and occurrence points from an independently derived data set. These models were refined to obtain <span class="hlt">predicted</span> species' geographical distributions under increasingly strict assumptions about the ability of a species to disperse to suitable habitat and to persist in it, as modulated by its ecological suitability. Models successful at <span class="hlt">predictions</span> were fitted to the extreme A2 and relatively conservative B2 projected <span class="hlt">climate</span> scenarios for 2020, 2050, and 2080 using publicly available interpolated <span class="hlt">climate</span> data from the Third Intergovernmental Panel on <span class="hlt">Climate</span> Change Assessment Report. Further analyses included estimation of the projected human population that could potentially be exposed to leishmaniasis in 2020, 2050, and 2080 under the A2 and B2 scenarios. All confirmed vector and reservoir species will see an</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://files.eric.ed.gov/fulltext/EJ1099787.pdf','ERIC'); return false;" href="http://files.eric.ed.gov/fulltext/EJ1099787.pdf"><span>The <span class="hlt">Prediction</span> Power of Servant and Ethical Leadership Behaviours of <span class="hlt">Administrators</span> on Teachers' Job Satisfaction</span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Güngör, Semra Kiranli</p> <p>2016-01-01</p> <p>The purpose of this study is to identify servant leadership and ethical leadership behaviors of <span class="hlt">administrators</span> and the <span class="hlt">prediction</span> power of these behaviors on teachers' job satisfaction according to the views of schoolteachers. This research, figured in accordance with the quantitative research processes. The target population of the research has…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018ERL....13f4030F','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018ERL....13f4030F"><span>A universal model for <span class="hlt">predicting</span> human migration under <span class="hlt">climate</span> change: examining future sea level rise in Bangladesh</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Frankel Davis, Kyle; Bhattachan, Abinash; D’Odorico, Paolo; Suweis, Samir</p> <p>2018-06-01</p> <p><span class="hlt">Climate</span> change is expected to impact the habitability of many places around the world in significant and unprecedented ways in the coming decades. While previous studies have provided estimates of populations potentially exposed to various <span class="hlt">climate</span> impacts, little work has been done to assess the number of people that may actually be displaced or where they will choose to go. Here we modify a diffusion-based model of human mobility in combination with population, geographic, and <span class="hlt">climatic</span> data to estimate the sources, destinations, and flux of potential migrants as driven by sea level rise (SLR) in Bangladesh in the years 2050 and 2100. Using only maps of population and elevation, we <span class="hlt">predict</span> that 0.9 million people (by year 2050) to 2.1 million people (by year 2100) could be displaced by direct inundation and that almost all of this movement will occur locally within the southern half of the country. We also find that destination locations should anticipate substantial additional demands on jobs (594 000), housing (197 000), and food (783 × 109 calories) by mid-century as a result of those displaced by SLR. By linking the sources of migrants displaced by SLR with their likely destinations, we demonstrate an effective approach for <span class="hlt">predicting</span> <span class="hlt">climate</span>-driven migrant flows, especially in data-limited settings.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/28584173','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/28584173"><span>Spatial, seasonal and <span class="hlt">climatic</span> <span class="hlt">predictive</span> models of Rift Valley fever disease across Africa.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Redding, David W; Tiedt, Sonia; Lo Iacono, Gianni; Bett, Bernard; Jones, Kate E</p> <p>2017-07-19</p> <p>Understanding the emergence and subsequent spread of human infectious diseases is a critical global challenge, especially for high-impact zoonotic and vector-borne diseases. Global <span class="hlt">climate</span> and land-use change are likely to alter host and vector distributions, but understanding the impact of these changes on the burden of infectious diseases is difficult. Here, we use a Bayesian spatial model to investigate environmental drivers of one of the most important diseases in Africa, Rift Valley fever (RVF). The model uses a hierarchical approach to determine how environmental drivers vary both spatially and seasonally, and incorporates the effects of key <span class="hlt">climatic</span> oscillations, to produce a continental risk map of RVF in livestock (as a proxy for human RVF risk). We find RVF risk has a distinct seasonal spatial pattern influenced by <span class="hlt">climatic</span> variation, with the majority of cases occurring in South Africa and Kenya in the first half of an El Niño year. Irrigation, rainfall and human population density were the main drivers of RVF cases, independent of seasonal, <span class="hlt">climatic</span> or spatial variation. By accounting more subtly for the patterns in RVF data, we better determine the importance of underlying environmental drivers, and also make space- and time-sensitive <span class="hlt">predictions</span> to better direct future surveillance resources.This article is part of the themed issue 'One Health for a changing world: zoonoses, ecosystems and human well-being'. © 2017 The Authors.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5468690','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5468690"><span>Spatial, seasonal and <span class="hlt">climatic</span> <span class="hlt">predictive</span> models of Rift Valley fever disease across Africa</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p></p> <p>2017-01-01</p> <p>Understanding the emergence and subsequent spread of human infectious diseases is a critical global challenge, especially for high-impact zoonotic and vector-borne diseases. Global <span class="hlt">climate</span> and land-use change are likely to alter host and vector distributions, but understanding the impact of these changes on the burden of infectious diseases is difficult. Here, we use a Bayesian spatial model to investigate environmental drivers of one of the most important diseases in Africa, Rift Valley fever (RVF). The model uses a hierarchical approach to determine how environmental drivers vary both spatially and seasonally, and incorporates the effects of key <span class="hlt">climatic</span> oscillations, to produce a continental risk map of RVF in livestock (as a proxy for human RVF risk). We find RVF risk has a distinct seasonal spatial pattern influenced by <span class="hlt">climatic</span> variation, with the majority of cases occurring in South Africa and Kenya in the first half of an El Niño year. Irrigation, rainfall and human population density were the main drivers of RVF cases, independent of seasonal, <span class="hlt">climatic</span> or spatial variation. By accounting more subtly for the patterns in RVF data, we better determine the importance of underlying environmental drivers, and also make space- and time-sensitive <span class="hlt">predictions</span> to better direct future surveillance resources. This article is part of the themed issue ‘One Health for a changing world: zoonoses, ecosystems and human well-being’. PMID:28584173</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3831435','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3831435"><span>Functional traits <span class="hlt">predict</span> relationship between plant abundance dynamic and long-term <span class="hlt">climate</span> warming</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Soudzilovskaia, Nadejda A.; Elumeeva, Tatiana G.; Onipchenko, Vladimir G.; Shidakov, Islam I.; Salpagarova, Fatima S.; Khubiev, Anzor B.; Tekeev, Dzhamal K.; Cornelissen, Johannes H. C.</p> <p>2013-01-01</p> <p><span class="hlt">Predicting</span> <span class="hlt">climate</span> change impact on ecosystem structure and services is one of the most important challenges in ecology. Until now, plant species response to <span class="hlt">climate</span> change has been described at the level of fixed plant functional types, an approach limited by its inflexibility as there is much interspecific functional variation within plant functional types. Considering a plant species as a set of functional traits greatly increases our possibilities for analysis of ecosystem functioning and carbon and nutrient fluxes associated therewith. Moreover, recently assembled large-scale databases hold comprehensive per-species data on plant functional traits, allowing a detailed functional description of many plant communities on Earth. Here, we show that plant functional traits can be used as predictors of vegetation response to <span class="hlt">climate</span> warming, accounting in our test ecosystem (the species-rich alpine belt of Caucasus mountains, Russia) for 59% of variability in the per-species abundance relation to temperature. In this mountain belt, traits that promote conservative leaf water economy (higher leaf mass per area, thicker leaves) and large investments in belowground reserves to support next year’s shoot buds (root carbon content) were the best predictors of the species increase in abundance along with temperature increase. This finding demonstrates that plant functional traits constitute a highly useful concept for forecasting changes in plant communities, and their associated ecosystem services, in response to <span class="hlt">climate</span> change. PMID:24145400</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014FrES....8..457L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014FrES....8..457L"><span>Regional <span class="hlt">climate</span> model downscaling may improve the <span class="hlt">prediction</span> of alien plant species distributions</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Liu, Shuyan; Liang, Xin-Zhong; Gao, Wei; Stohlgren, Thomas J.</p> <p>2014-12-01</p> <p>Distributions of invasive species are commonly <span class="hlt">predicted</span> with species distribution models that build upon the statistical relationships between observed species presence data and <span class="hlt">climate</span> data. We used field observations, <span class="hlt">climate</span> station data, and Maximum Entropy species distribution models for 13 invasive plant species in the United States, and then compared the models with inputs from a General Circulation Model (hereafter GCM-based models) and a downscaled Regional <span class="hlt">Climate</span> Model (hereafter, RCM-based models).We also compared species distributions based on either GCM-based or RCM-based models for the present (1990-1999) to the future (2046-2055). RCM-based species distribution models replicated observed distributions remarkably better than GCM-based models for all invasive species under the current <span class="hlt">climate</span>. This was shown for the presence locations of the species, and by using four common statistical metrics to compare modeled distributions. For two widespread invasive taxa ( Bromus tectorum or cheatgrass, and Tamarix spp. or tamarisk), GCM-based models failed miserably to reproduce observed species distributions. In contrast, RCM-based species distribution models closely matched observations. Future species distributions may be significantly affected by using GCM-based inputs. Because invasive plants species often show high resilience and low rates of local extinction, RCM-based species distribution models may perform better than GCM-based species distribution models for planning containment programs for invasive species.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://eric.ed.gov/?q=survey&pg=6&id=EJ1074448','ERIC'); return false;" href="https://eric.ed.gov/?q=survey&pg=6&id=EJ1074448"><span>A Safer Place? LGBT Educators, School <span class="hlt">Climate</span>, and Implications for <span class="hlt">Administrators</span></span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Wright, Tiffany E.; Smith, Nancy J.</p> <p>2015-01-01</p> <p>Over an 8-year span, two survey studies were conducted to analyze LGBT -teachers' perceptions of their school <span class="hlt">climate</span> and the impact of school leaders on that <span class="hlt">climate</span>. This article presents nonparametric, descriptive, and qualitative results of the National Survey of Educators' Perceptions of School <span class="hlt">Climate</span> 2011 compared with survey results from…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5035090','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5035090"><span><span class="hlt">Predicting</span> the Potential Distribution of Polygala tenuifolia Willd. under <span class="hlt">Climate</span> Change in China</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Li, Lin; Zhao, Yao; Pei, Lin; Zhao, Jiancheng</p> <p>2016-01-01</p> <p>Global warming has created opportunities and challenges for the survival and development of species. Determining how <span class="hlt">climate</span> change may impact multiple ecosystem levels and lead to various species adaptations is necessary for both biodiversity conservation and sustainable biological resource utilization. In this study, we employed Maxent to <span class="hlt">predict</span> changes in the habitat range and altitude of Polygala tenuifolia Willd. under current and future <span class="hlt">climate</span> scenarios in China. Four representative concentration pathways (RCP2.6, RCP4.5, RCP6.0, and RCP8.5) were modeled for two time periods (2050 and 2070). The model inputs included 732 presence points and nine sets of environmental variables under the current conditions and the four RCPs in 2050 and 2070. The area under the receiver-operating characteristic (ROC) curve (AUC) was used to evaluate model performance. All of the AUCs were greater than 0.80, thereby placing these models in the “very good” category. Using a jackknife analysis, the precipitation in the warmest quarter, annual mean temperature, and altitude were found to be the top three variables that affect the range of P. tenuifolia. Additionally, we found that the <span class="hlt">predicted</span> highly suitable habitat was in reasonable agreement with its actual distribution. Furthermore, the highly suitable habitat area was slowly reduced over time. PMID:27661983</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/28747719','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/28747719"><span>Multi-year <span class="hlt">predictability</span> of <span class="hlt">climate</span>, drought, and wildfire in southwestern North America.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Chikamoto, Yoshimitsu; Timmermann, Axel; Widlansky, Matthew J; Balmaseda, Magdalena A; Stott, Lowell</p> <p>2017-07-26</p> <p>Past severe droughts over North America have led to massive water shortages and increases in wildfire frequency. Triggering sources for multi-year droughts in this region include randomly occurring atmospheric blocking patterns, ocean impacts on atmospheric circulation, and <span class="hlt">climate</span>'s response to anthropogenic radiative forcings. A combination of these sources translates into a difficulty to <span class="hlt">predict</span> the onset and length of such droughts on multi-year timescales. Here we present results from a new multi-year dynamical <span class="hlt">prediction</span> system that exhibits a high degree of skill in forecasting wildfire probabilities and drought for 10-23 and 10-45 months lead time, which extends far beyond the current seasonal <span class="hlt">prediction</span> activities for southwestern North America. Using a state-of-the-art earth system model along with 3-dimensional ocean data assimilation and by prescribing the external radiative forcings, this system simulates the observed low-frequency variability of precipitation, soil water, and wildfire probabilities in close agreement with observational records and reanalysis data. The underlying source of multi-year <span class="hlt">predictability</span> can be traced back to variations of the Atlantic/Pacific sea surface temperature gradient, external radiative forcings, and the low-pass filtering characteristics of soils.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/25703827','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/25703827"><span>Modelling the influence of <span class="hlt">predicted</span> future <span class="hlt">climate</span> change on the risk of wind damage within New Zealand's planted forests.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Moore, John R; Watt, Michael S</p> <p>2015-08-01</p> <p>Wind is the major abiotic disturbance in New Zealand's planted forests, but little is known about how the risk of wind damage may be affected by future <span class="hlt">climate</span> change. We linked a mechanistic wind damage model (ForestGALES) to an empirical growth model for radiata pine (Pinus radiata D. Don) and a process-based growth model (cenw) to <span class="hlt">predict</span> the risk of wind damage under different future emissions scenarios and assumptions about the future wind <span class="hlt">climate</span>. The cenw model was used to estimate site productivity for constant CO2 concentration at 1990 values and for assumed increases in CO2 concentration from current values to those expected during 2040 and 2090 under the B1 (low), A1B (mid-range) and A2 (high) emission scenarios. Stand development was modelled for different levels of site productivity, contrasting silvicultural regimes and sites across New Zealand. The risk of wind damage was <span class="hlt">predicted</span> for each regime and emission scenario combination using the ForestGALES model. The sensitivity to changes in the intensity of the future wind <span class="hlt">climate</span> was also examined. Results showed that increased tree growth rates under the different emissions scenarios had the greatest impact on the risk of wind damage. The increase in risk was greatest for stands growing at high stand density under the A2 emissions scenario with increased CO2 concentration. The increased productivity under this scenario resulted in increased tree height, without a corresponding increase in diameter, leading to more slender trees that were <span class="hlt">predicted</span> to be at greater risk from wind damage. The risk of wind damage was further increased by the modest increases in the extreme wind <span class="hlt">climate</span> that are <span class="hlt">predicted</span> to occur. These results have implications for the development of silvicultural regimes that are resilient to <span class="hlt">climate</span> change and also indicate that future productivity gains may be offset by greater losses from disturbances. © 2015 John Wiley & Sons Ltd.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015GMDD....8.8809D','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015GMDD....8.8809D"><span>The Arctic <span class="hlt">Predictability</span> and <span class="hlt">Prediction</span> on Seasonal-to-Interannual TimEscales (APPOSITE) data set</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Day, J. J.; Tietsche, S.; Collins, M.; Goessling, H. F.; Guemas, V.; Guillory, A.; Hurlin, W. J.; Ishii, M.; Keeley, S. P. E.; Matei, D.; Msadek, R.; Sigmond, M.; Tatebe, H.; Hawkins, E.</p> <p>2015-10-01</p> <p>Recent decades have seen significant developments in seasonal-to-interannual timescale <span class="hlt">climate</span> <span class="hlt">prediction</span> capabilities. However, until recently the potential of such systems to <span class="hlt">predict</span> Arctic <span class="hlt">climate</span> had not been assessed. This paper describes a multi-model <span class="hlt">predictability</span> experiment which was run as part of the Arctic <span class="hlt">Predictability</span> and <span class="hlt">Prediction</span> On Seasonal to Inter-annual Timescales (APPOSITE) project. The main goal of APPOSITE was to quantify the timescales on which Arctic <span class="hlt">climate</span> is <span class="hlt">predictable</span>. In order to achieve this, a coordinated set of idealised initial-value <span class="hlt">predictability</span> experiments, with seven general circulation models, was conducted. This was the first model intercomparison project designed to quantify the <span class="hlt">predictability</span> of Arctic <span class="hlt">climate</span> on seasonal to inter-annual timescales. Here we present a description of the archived data set (which is available at the British Atmospheric Data Centre) and an update of the project's results. Although designed to address Arctic <span class="hlt">predictability</span>, this data set could also be used to assess the <span class="hlt">predictability</span> of other regions and modes of <span class="hlt">climate</span> variability on these timescales, such as the El Niño Southern Oscillation.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70195385','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70195385"><span>Range position and <span class="hlt">climate</span> sensitivity: The structure of among-population demographic responses to <span class="hlt">climatic</span> variation</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Amburgey, Staci M.; Miller, David A. W.; Grant, Evan H. Campbell; Rittenhouse, Tracy A. G.; Benard, Michael F.; Richardson, Jonathan L.; Urban, Mark C.; Hughson, Ward; Brand, Adrianne B,; Davis, Christopher J.; Hardin, Carmen R.; Paton, Peter W. C.; Raithel, Christopher J.; Relyea, Rick A.; Scott, A. Floyd; Skelly, David K.; Skidds, Dennis E.; Smith, Charles K.; Werner, Earl E.</p> <p>2018-01-01</p> <p>Species’ distributions will respond to <span class="hlt">climate</span> change based on the relationship between local demographic processes and <span class="hlt">climate</span> and how this relationship varies based on range position. A rarely tested demographic <span class="hlt">prediction</span> is that populations at the extremes of a species’ <span class="hlt">climate</span> envelope (e.g., populations in areas with the highest mean annual temperature) will be most sensitive to local shifts in <span class="hlt">climate</span> (i.e., warming). We tested this <span class="hlt">prediction</span> using a dynamic species distribution model linking demographic rates to variation in temperature and precipitation for wood frogs (Lithobates sylvaticus) in North America. Using long-term monitoring data from 746 populations in 27 study areas, we determined how <span class="hlt">climatic</span> variation affected population growth rates and how these relationships varied with respect to long-term <span class="hlt">climate</span>. Some models supported the <span class="hlt">predicted</span> pattern, with negative effects of extreme summer temperatures in hotter areas and positive effects on recruitment for summer water availability in drier areas. We also found evidence of interacting temperature and precipitation influencing population size, such as extreme heat having less of a negative effect in wetter areas. Other results were contrary to <span class="hlt">predictions</span>, such as positive effects of summer water availability in wetter parts of the range and positive responses to winter warming especially in milder areas. In general, we found wood frogs were more sensitive to changes in temperature or temperature interacting with precipitation than to changes in precipitation alone. Our results suggest that sensitivity to changes in <span class="hlt">climate</span> cannot be <span class="hlt">predicted</span> simply by knowing locations within the species’ <span class="hlt">climate</span> envelope. Many <span class="hlt">climate</span> processes did not affect population growth rates in the <span class="hlt">predicted</span> direction based on range position. Processes such as species-interactions, local adaptation, and interactions with the physical landscape likely affect the responses we observed. Our work highlights the</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_18");'>18</a></li> <li><a href="#" onclick='return showDiv("page_19");'>19</a></li> <li class="active"><span>20</span></li> <li><a href="#" onclick='return showDiv("page_21");'>21</a></li> <li><a href="#" onclick='return showDiv("page_22");'>22</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_20 --> <div id="page_21" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_19");'>19</a></li> <li><a href="#" onclick='return showDiv("page_20");'>20</a></li> <li class="active"><span>21</span></li> <li><a href="#" onclick='return showDiv("page_22");'>22</a></li> <li><a href="#" onclick='return showDiv("page_23");'>23</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="401"> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015EGUGA..17.5479P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015EGUGA..17.5479P"><span>Effects of lateral boundary condition resolution and update frequency on regional <span class="hlt">climate</span> model <span class="hlt">predictions</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Pankatz, Klaus; Kerkweg, Astrid</p> <p>2015-04-01</p> <p>The work presented is part of the joint project "DecReg" ("Regional decadal <span class="hlt">predictability</span>") which is in turn part of the project "MiKlip" ("Decadal <span class="hlt">predictions</span>"), an effort funded by the German Federal Ministry of Education and Research to improve decadal <span class="hlt">predictions</span> on a global and regional scale. In MiKlip, one big question is if regional <span class="hlt">climate</span> modeling shows "added value", i.e. to evaluate, if regional <span class="hlt">climate</span> models (RCM) produce better results than the driving models. However, the scope of this study is to look more closely at the setup specific details of regional <span class="hlt">climate</span> modeling. As regional models only simulate a small domain, they have to inherit information about the state of the atmosphere at their lateral boundaries from external data sets. There are many unresolved questions concerning the setup of lateral boundary conditions (LBC). External data sets come from global models or from global reanalysis data-sets. A temporal resolution of six hours is common for this kind of data. This is mainly due to the fact, that storage space is a limiting factor, especially for <span class="hlt">climate</span> simulations. However, theoretically, the coupling frequency could be as high as the time step of the driving model. Meanwhile, it is unclear if a more frequent update of the LBCs has a significant effect on the <span class="hlt">climate</span> in the domain of the RCM. The first study examines how the RCM reacts to a higher update frequency. The study is based on a 30 year time slice experiment for three update frequencies of the LBC, namely six hours, one hour and six minutes. The evaluation of means, standard deviations and statistics of the <span class="hlt">climate</span> in the regional domain shows only small deviations, some statistically significant though, of 2m temperature, sea level pressure and precipitation. The second part of the first study assesses parameters linked to cyclone activity, which is affected by the LBC update frequency. Differences in track density and strength are found when comparing the simulations</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFMGC13A1192G','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFMGC13A1192G"><span>Betting and Belief: Modeling the Impact of <span class="hlt">Prediction</span> Markets on Public Attribution of <span class="hlt">Climate</span> Change</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Gilligan, J. M.; Nay, J. J.; van der Linden, M.</p> <p>2016-12-01</p> <p>Despite overwhelming scientific evidence and an almost complete consensus among scientists, a large fraction of the American public is not convinced that global warming is anthropogenic. This doubt correlates strongly with political, ideological, and cultural orientation. [1] It has been proposed that people who do not trust <span class="hlt">climate</span> scientists tend to trust markets, so <span class="hlt">prediction</span> markets might be able to influence their beliefs about the causes of <span class="hlt">climate</span> change. [2] We present results from an agent-based simulation of a <span class="hlt">prediction</span> market in which traders invest based on their beliefs about what drives global temperature change (here, either CO2 concentration or total solar irradiance (TSI), which is a popular hypothesis among many who doubt the dominant role of CO2). At each time step, traders use historical and observed temperatures and projected future forcings (CO2 or TSI) to update Bayesian posterior probability distributions for future temperatures, conditional on their belief about what drives <span class="hlt">climate</span> change. Traders then bet on future temperatures by trading in <span class="hlt">climate</span> futures. Trading proceeds by a continuous double auction. Traders are randomly assigned initial beliefs about <span class="hlt">climate</span> change, and they have some probability of changing their beliefs to match those of the most successful traders in their social network. We simulate two alternate realities in which the global temperature is controlled either by CO2 or by TSI, with stochastic noise. In both cases traders' beliefs converge, with a large majority reaching agreement on the actual cause of <span class="hlt">climate</span> change. This convergence is robust, but the speed with which consensus emerges depends on characteristics of the traders' psychology and the structure of the market. Our model can serve as a test-bed for studying how beliefs might evolve under different market structures and different modes of decision-making and belief-change. We will report progress on studying alternate models of belief-change. This</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2011-10-20/pdf/2011-27113.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2011-10-20/pdf/2011-27113.pdf"><span>76 FR 65183 - National Oceanic and Atmospheric <span class="hlt">Administration</span></span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2011-10-20</p> <p>... DEPARTMENT OF COMMERCE National Oceanic and Atmospheric <span class="hlt">Administration</span> National <span class="hlt">Climate</span> Assessment... Oceanic and Atmospheric <span class="hlt">Administration</span> (NOAA), Department of Commerce (DOC). ACTION: Notice of open..., National Oceanic and Atmospheric <span class="hlt">Administration</span>. [FR Doc. 2011-27113 Filed 10-19-11; 8:45 am] BILLING CODE...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFMNH33A1909R','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFMNH33A1909R"><span><span class="hlt">Predicting</span> Impacts of Lightning Strikes on Aviation under a Changing <span class="hlt">Climate</span> Using Regression Kriging</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Rakas, J.; Ding, C.; Murthi, A.; Lukovic, J.; Bajat, B.</p> <p>2016-12-01</p> <p>Lightning is a serious hazard that can cause significant impacts on human infrastructure. In the aviation industry, lightning strikes cause damage and outages to air traffic control equipment and facilities at airports that result in major disruptions in commercial air travel, compounding delays during storm events that lead to losses in the millions of dollars. To date poor attention has been given to how lightning might change with the increase of greenhouse gases and temperature. Under some <span class="hlt">climate</span> change scenarios, the increase in the occurrence and severity of storms in the future with potential for increases in lightning activity has been studied. Recent findings suggest that lighting rates will increase 12 percent per every degree Celsius rise in global temperatures. That will results to a 50 percent increase by the end of the century. Accurate <span class="hlt">prediction</span> of the intensity and frequency of lightning strikes is therefore required by the air traffic management and control sector in order to develop more robust adaptation and mitigation strategies under the threat of global <span class="hlt">climate</span> change and increasing lightning rates. In this work, we use the regression kriging method to <span class="hlt">predict</span> lightning strikes over several regions over the contiguous United Sates using two meteorological variables- namely convective available potential energy (CAPE) and total precipitation rate. These two variables are used as a measure of storm convection, since strong convections are related to more lightning. Specifically, CAPE multiplied by precipitation is used as a proxy for lightning strikes owing to a strong linear relationship between the two. These two meteorological variables are obtained from a subset of models used in phase 5 of the coupled model inter-comparison experiment pertaining to the "high emissions" <span class="hlt">climate</span> change scenario corresponding to the representative concentration pathway (RCP) 8.5. Precipitation observations from the National Weather Cooperative Network (COOP</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/24223272','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/24223272"><span><span class="hlt">Climate</span> change, species distribution models, and physiological performance metrics: <span class="hlt">predicting</span> when biogeographic models are likely to fail.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Woodin, Sarah A; Hilbish, Thomas J; Helmuth, Brian; Jones, Sierra J; Wethey, David S</p> <p>2013-09-01</p> <p>Modeling the biogeographic consequences of <span class="hlt">climate</span> change requires confidence in model <span class="hlt">predictions</span> under novel conditions. However, models often fail when extended to new locales, and such instances have been used as evidence of a change in physiological tolerance, that is, a fundamental niche shift. We explore an alternative explanation and propose a method for <span class="hlt">predicting</span> the likelihood of failure based on physiological performance curves and environmental variance in the original and new environments. We define the transient event margin (TEM) as the gap between energetic performance failure, defined as CTmax, and the upper lethal limit, defined as LTmax. If TEM is large relative to environmental fluctuations, models will likely fail in new locales. If TEM is small relative to environmental fluctuations, models are likely to be robust for new locales, even when mechanism is unknown. Using temperature, we <span class="hlt">predict</span> when biogeographic models are likely to fail and illustrate this with a case study. We suggest that failure is <span class="hlt">predictable</span> from an understanding of how <span class="hlt">climate</span> drives nonlethal physiological responses, but for many species such data have not been collected. Successful biogeographic forecasting thus depends on understanding when the mechanisms limiting distribution of a species will differ among geographic regions, or at different times, resulting in realized niche shifts. TEM allows <span class="hlt">prediction</span> of the likelihood of such model failure.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012AGUFMGC41B0961F','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012AGUFMGC41B0961F"><span>Dynamic <span class="hlt">Predictions</span> of Crop Yield and Irrigation in Sub-Saharan Africa Due to <span class="hlt">Climate</span> Change Impacts</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Foster-Wittig, T.</p> <p>2012-12-01</p> <p>The highest damages from <span class="hlt">climate</span> change are <span class="hlt">predicted</span> to be in the agricultural sector in sub-Saharan Africa. Agriculture is <span class="hlt">predicted</span> to be especially vulnerable in this region because of its current state of high temperature and low precipitation and because it is usually rain-fed or relies on relatively basic technologies which therefore limit its ability to sustain in increased poor <span class="hlt">climatic</span> conditions [1]. The goal of this research is to quantify the vulnerability of this ecosystem by projecting future changes in agriculture due to IPCC <span class="hlt">predicted</span> <span class="hlt">climate</span> change impacts on precipitation and temperature. This research will provide a better understanding of the relationship between precipitation and rain-fed agriculture in savannas. In order to quantify the effects of <span class="hlt">climate</span> change on agriculture, the impacts of <span class="hlt">climate</span> change are modeled through the use of a land surface vegetation dynamics model previously developed combined with a crop model [2,4]. In this project, it will be used to model yield for point cropland locations within sub-Saharan Africa between Kenya and Botswana with a range of annual rainfall. With this model, future projections are developed for what can be anticipated for the crop yield based on two precipitation <span class="hlt">climate</span> change scenarios; (1) decreased depth and (2) decreased frequency as well as temperature change scenarios; (3) only temperature increased, (4) temperature increase dand decreased precipitation depth, and (5) temperature increased and decreased precipitation frequency. Therefore, this will allow conclusions to be drawn about how mean precipitation and a changing <span class="hlt">climate</span> effect food security in sub-Saharan Africa. As an additional analysis, irrigation is added to the model as it is thought to be the solution to protect food security by maximizing on the potential of food production. In water-limited areas such as Sub-Saharan Africa, it is important to consider water efficient irrigation techniques such as demand-based micro</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/26110279','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/26110279"><span>Association of <span class="hlt">Climatic</span> Variability, Vector Population and Malarial Disease in District of Visakhapatnam, India: A Modeling and <span class="hlt">Prediction</span> Analysis.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Srimath-Tirumula-Peddinti, Ravi Chandra Pavan Kumar; Neelapu, Nageswara Rao Reddy; Sidagam, Naresh</p> <p>2015-01-01</p> <p>Malarial incidence, severity, dynamics and distribution of malaria are strongly determined by <span class="hlt">climatic</span> factors, i.e., temperature, precipitation, and relative humidity. The objectives of the current study were to analyse and model the relationships among <span class="hlt">climate</span>, vector and malaria disease in district of Visakhapatnam, India to understand malaria transmission mechanism (MTM). Epidemiological, vector and <span class="hlt">climate</span> data were analysed for the years 2005 to 2011 in Visakhapatnam to understand the magnitude, trends and seasonal patterns of the malarial disease. Statistical software MINITAB ver. 14 was used for performing correlation, linear and multiple regression analysis. Perennial malaria disease incidence and mosquito population was observed in the district of Visakhapatnam with peaks in seasons. All the <span class="hlt">climatic</span> variables have a significant influence on disease incidence as well as on mosquito populations. Correlation coefficient analysis, seasonal index and seasonal analysis demonstrated significant relationships among <span class="hlt">climatic</span> factors, mosquito population and malaria disease incidence in the district of Visakhapatnam, India. Multiple regression and ARIMA (I) models are best suited models for modeling and <span class="hlt">prediction</span> of disease incidences and mosquito population. <span class="hlt">Predicted</span> values of average temperature, mosquito population and malarial cases increased along with the year. Developed MTM algorithm observed a major MTM cycle following the June to August rains and occurring between June to September and minor MTM cycles following March to April rains and occurring between March to April in the district of Visakhapatnam. Fluctuations in <span class="hlt">climatic</span> factors favored an increase in mosquito populations and thereby increasing the number of malarial cases. Rainfall, temperatures (20°C to 33°C) and humidity (66% to 81%) maintained a warmer, wetter <span class="hlt">climate</span> for mosquito growth, parasite development and malaria transmission. Changes in <span class="hlt">climatic</span> factors influence malaria directly by</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4482491','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4482491"><span>Association of <span class="hlt">Climatic</span> Variability, Vector Population and Malarial Disease in District of Visakhapatnam, India: A Modeling and <span class="hlt">Prediction</span> Analysis</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Srimath-Tirumula-Peddinti, Ravi Chandra Pavan Kumar; Neelapu, Nageswara Rao Reddy; Sidagam, Naresh</p> <p>2015-01-01</p> <p>Background Malarial incidence, severity, dynamics and distribution of malaria are strongly determined by <span class="hlt">climatic</span> factors, i.e., temperature, precipitation, and relative humidity. The objectives of the current study were to analyse and model the relationships among <span class="hlt">climate</span>, vector and malaria disease in district of Visakhapatnam, India to understand malaria transmission mechanism (MTM). Methodology Epidemiological, vector and <span class="hlt">climate</span> data were analysed for the years 2005 to 2011 in Visakhapatnam to understand the magnitude, trends and seasonal patterns of the malarial disease. Statistical software MINITAB ver. 14 was used for performing correlation, linear and multiple regression analysis. Results/Findings Perennial malaria disease incidence and mosquito population was observed in the district of Visakhapatnam with peaks in seasons. All the <span class="hlt">climatic</span> variables have a significant influence on disease incidence as well as on mosquito populations. Correlation coefficient analysis, seasonal index and seasonal analysis demonstrated significant relationships among <span class="hlt">climatic</span> factors, mosquito population and malaria disease incidence in the district of Visakhapatnam, India. Multiple regression and ARIMA (I) models are best suited models for modeling and <span class="hlt">prediction</span> of disease incidences and mosquito population. <span class="hlt">Predicted</span> values of average temperature, mosquito population and malarial cases increased along with the year. Developed MTM algorithm observed a major MTM cycle following the June to August rains and occurring between June to September and minor MTM cycles following March to April rains and occurring between March to April in the district of Visakhapatnam. Fluctuations in <span class="hlt">climatic</span> factors favored an increase in mosquito populations and thereby increasing the number of malarial cases. Rainfall, temperatures (20°C to 33°C) and humidity (66% to 81%) maintained a warmer, wetter <span class="hlt">climate</span> for mosquito growth, parasite development and malaria transmission. Conclusions</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017EGUGA..19.2086O','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017EGUGA..19.2086O"><span>Development of the virtual research environment for analysis, evaluation and <span class="hlt">prediction</span> of global <span class="hlt">climate</span> change impacts on the regional environment</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Okladnikov, Igor; Gordov, Evgeny; Titov, Alexander; Fazliev, Alexander</p> <p>2017-04-01</p> <p>Description and the first results of the Russian Science Foundation project "Virtual computational information environment for analysis, evaluation and <span class="hlt">prediction</span> of the impacts of global <span class="hlt">climate</span> change on the environment and <span class="hlt">climate</span> of a selected region" is presented. The project is aimed at development of an Internet-accessible computation and information environment providing unskilled in numerical modelling and software design specialists, decision-makers and stakeholders with reliable and easy-used tools for in-depth statistical analysis of <span class="hlt">climatic</span> characteristics, and instruments for detailed analysis, assessment and <span class="hlt">prediction</span> of impacts of global <span class="hlt">climate</span> change on the environment and <span class="hlt">climate</span> of the targeted region. In the framework of the project, approaches of "cloud" processing and analysis of large geospatial datasets will be developed on the technical platform of the Russian leading institution involved in research of <span class="hlt">climate</span> change and its consequences. Anticipated results will create a pathway for development and deployment of thematic international virtual research laboratory focused on interdisciplinary environmental studies. VRE under development will comprise best features and functionality of earlier developed information and computing system <span class="hlt">CLIMATE</span> (http://<span class="hlt">climate</span>.scert.ru/), which is widely used in Northern Eurasia environment studies. The Project includes several major directions of research listed below. 1. Preparation of geo-referenced data sets, describing the dynamics of the current and possible future <span class="hlt">climate</span> and environmental changes in detail. 2. Improvement of methods of analysis of <span class="hlt">climate</span> change. 3. Enhancing the functionality of the VRE prototype in order to create a convenient and reliable tool for the study of regional social, economic and political consequences of <span class="hlt">climate</span> change. 4. Using the output of the first three tasks, compilation of the VRE prototype, its validation, preparation of applicable detailed description of</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2007EOSTr..88..111G','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2007EOSTr..88..111G"><span>Reconstruction of Past Mediterranean <span class="hlt">Climate</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>García-Herrera, Ricardo; Luterbacher, Jürg; Lionello, Piero; Gonzáles-Rouco, Fidel; Ribera, Pedro; Rodó, Xavier; Kull, Christoph; Zerefos, Christos</p> <p>2007-02-01</p> <p>First MEDCLIVAR Workshop on Reconstruction of Past Mediterranean <span class="hlt">Climate</span>; Pablo de Olavide University, Carmona, Spain, 8-11 November 2006; Mediterranean <span class="hlt">Climate</span> Variability and <span class="hlt">Predictability</span> (MEDCLIVAR; http://www.medclivar.eu) is a program that coordinates and promotes research on different aspects of Mediterranean <span class="hlt">climate</span>. The main MEDCLIVAR goals include the reconstruction of past <span class="hlt">climate</span>, describing patterns and mechanisms characterizing <span class="hlt">climate</span> space-time variability, extremes at different time and space scales, coupled <span class="hlt">climate</span> model/empirical reconstruction comparisons, seasonal forecasting, and the identification of the forcings responsible for the observed changes. The program has been endorsed by CLIVAR (<span class="hlt">Climate</span> Variability and <span class="hlt">Predictability</span> project) and is funded by the European Science Foundation.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5876960','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5876960"><span><span class="hlt">Predicting</span> Circulatory Diseases from Psychosocial Safety <span class="hlt">Climate</span>: A Prospective Cohort Study from Australia</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Becher, Harry; Dollard, Maureen F.; Smith, Peter</p> <p>2018-01-01</p> <p>Circulatory diseases (CDs) (including myocardial infarction, angina, stroke or hypertension) are among the leading causes of death in the world. In this paper, we explore for the first time the impact of a specific aspect of organizational <span class="hlt">climate</span>, Psychosocial Safety <span class="hlt">Climate</span> (PSC), on CDs. We used two waves of interview data from Australia, with an average lag of 5 years (excluding baseline CDs, final n = 1223). Logistic regression was conducted to estimate the prospective associations between PSC at baseline on incident CDs at follow-up. It was found that participants in low PSC environments were 59% more likely to develop new CD than those in high PSC environments. Logistic regression showed that high PSC at baseline <span class="hlt">predicts</span> lower CD risk at follow-up (OR = 0.98, 95% CI 0.96–1.00) and this risk remained unchanged even after additional adjustment for known job design risk factors (effort reward imbalance and job strain). These results suggest that PSC is an independent risk factor for CDs in Australia. Beyond job design this study implicates organizational <span class="hlt">climate</span> and prevailing management values regarding worker psychological health as the genesis of CDs. PMID:29495533</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017CoPhC.220..188D','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017CoPhC.220..188D"><span>Atlas : A library for numerical weather <span class="hlt">prediction</span> and <span class="hlt">climate</span> modelling</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Deconinck, Willem; Bauer, Peter; Diamantakis, Michail; Hamrud, Mats; Kühnlein, Christian; Maciel, Pedro; Mengaldo, Gianmarco; Quintino, Tiago; Raoult, Baudouin; Smolarkiewicz, Piotr K.; Wedi, Nils P.</p> <p>2017-11-01</p> <p>The algorithms underlying numerical weather <span class="hlt">prediction</span> (NWP) and <span class="hlt">climate</span> models that have been developed in the past few decades face an increasing challenge caused by the paradigm shift imposed by hardware vendors towards more energy-efficient devices. In order to provide a sustainable path to exascale High Performance Computing (HPC), applications become increasingly restricted by energy consumption. As a result, the emerging diverse and complex hardware solutions have a large impact on the programming models traditionally used in NWP software, triggering a rethink of design choices for future massively parallel software frameworks. In this paper, we present Atlas, a new software library that is currently being developed at the European Centre for Medium-Range Weather Forecasts (ECMWF), with the scope of handling data structures required for NWP applications in a flexible and massively parallel way. Atlas provides a versatile framework for the future development of efficient NWP and <span class="hlt">climate</span> applications on emerging HPC architectures. The applications range from full Earth system models, to specific tools required for post-processing weather forecast products. The Atlas library thus constitutes a step towards affordable exascale high-performance simulations by providing the necessary abstractions that facilitate the application in heterogeneous HPC environments by promoting the co-design of NWP algorithms with the underlying hardware.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29396527','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29396527"><span><span class="hlt">Climate</span> Based <span class="hlt">Predictability</span> of Oil Palm Tree Yield in Malaysia.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Oettli, Pascal; Behera, Swadhin K; Yamagata, Toshio</p> <p>2018-02-02</p> <p>The influence of local conditions and remote <span class="hlt">climate</span> modes on the interannual variability of oil palm fresh fruit bunches (FFB) total yields in Malaysia and two major regions (Peninsular Malaysia and Sabah/Sarawak) is explored. On a country scale, the state of sea-surface temperatures (SST) in the tropical Pacific Ocean during the previous boreal winter is found to influence the regional <span class="hlt">climate</span>. When El Niño occurs in the Pacific Ocean, rainfall in Malaysia reduces but air temperature increases, generating a high level of water stress for palm trees. As a result, the yearly production of FFB becomes lower than that of a normal year since the water stress during the boreal spring has an important impact on the total annual yields of FFB. Conversely, La Niña sets favorable conditions for palm trees to produce more FFB by reducing chances of water stress risk. The region of the Leeuwin current also seems to play a secondary role through the Ningaloo Niño/ Niña in the interannual variability of FFB yields. Based on these findings, a linear model is constructed and its ability to reproduce the interannual signal is assessed. This model has shown some skills in <span class="hlt">predicting</span> the total FFB yield.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016ThApC.126..437N','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016ThApC.126..437N"><span>Performance evaluation of NCEP <span class="hlt">climate</span> forecast system for the <span class="hlt">prediction</span> of winter temperatures over India</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Nageswararao, M. M.; Mohanty, U. C.; Kiran Prasad, S.; Osuri, Krishna K.; Ramakrishna, S. S. V. S.</p> <p>2016-11-01</p> <p>The surface air temperature during the winter season (December-February) in India adversely affects agriculture as well as day-to-day life. Therefore, the accurate <span class="hlt">prediction</span> of winter temperature in extended range is of utmost importance. The National Center for Environmental <span class="hlt">Prediction</span> (NCEP) has been providing <span class="hlt">climatic</span> variables from the fully coupled global <span class="hlt">climate</span> model, known as <span class="hlt">Climate</span> Forecast System version 1 (CFSv1) on monthly to seasonal scale since 2004, and it has been upgraded to CFSv2 subsequently in 2011. In the present study, the performance of CFSv1 and CFSv2 in simulating the winter 2 m maximum, minimum, and mean temperatures ( T max, T min, and T mean, respectively) over India is evaluated with respect to India Meteorological Department (IMD) 1° × 1° observations. The hindcast data obtained from both versions of CFS from 1982 to 2009 (27 years) with November initial conditions (lead-1) are used. The analyses of winter ( T max, T min, and T mean) temperatures revealed that CFSv1 and CFSv2 are able to replicate the patterns of observed climatology, interannual variability, and coefficient of variation with a slight negative bias. Of the two, CFSv2 is appreciable in capturing increasing trends of winter temperatures like observed. The T max, T min, and T mean correlations from CFSv2 is significantly high (0.35, 0.53, and 0.51, respectively), while CFSv1 correlations are less (0.29, 0.15, and 0.12) and insignificant. This performance of CFSv2 may be due to the better estimation of surface heat budget terms and realistic CO2 concentration, which were absent in CFSv1. CFSv2 proved to have a high probability of detection in <span class="hlt">predicting</span> different categories (below, near, and above normal) for winter T min, which are required for crop yield and public utility services, over north India.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016EGUGA..1814413E','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016EGUGA..1814413E"><span>An empirical system for probabilistic seasonal <span class="hlt">climate</span> <span class="hlt">prediction</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Eden, Jonathan; van Oldenborgh, Geert Jan; Hawkins, Ed; Suckling, Emma</p> <p>2016-04-01</p> <p>Preparing for episodes with risks of anomalous weather a month to a year ahead is an important challenge for governments, non-governmental organisations, and private companies and is dependent on the availability of reliable forecasts. The majority of operational seasonal forecasts are made using process-based dynamical models, which are complex, computationally challenging and prone to biases. Empirical forecast approaches built on statistical models to represent physical processes offer an alternative to dynamical systems and can provide either a benchmark for comparison or independent supplementary forecasts. Here, we present a simple empirical system based on multiple linear regression for producing probabilistic forecasts of seasonal surface air temperature and precipitation across the globe. The global CO2-equivalent concentration is taken as the primary predictor; subsequent predictors, including large-scale modes of variability in the <span class="hlt">climate</span> system and local-scale information, are selected on the basis of their physical relationship with the predictand. The focus given to the <span class="hlt">climate</span> change signal as a source of skill and the probabilistic nature of the forecasts produced constitute a novel approach to global empirical <span class="hlt">prediction</span>. Hindcasts for the period 1961-2013 are validated against observations using deterministic (correlation of seasonal means) and probabilistic (continuous rank probability skill scores) metrics. Good skill is found in many regions, particularly for surface air temperature and most notably in much of Europe during the spring and summer seasons. For precipitation, skill is generally limited to regions with known El Niño-Southern Oscillation (ENSO) teleconnections. The system is used in a quasi-operational framework to generate empirical seasonal forecasts on a monthly basis.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20150014242','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20150014242"><span>Uncertainty in Model <span class="hlt">Predictions</span> of Vibrio Vulnificus Response to <span class="hlt">Climate</span> Variability and Change: A Chesapeake Bay Case Study</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Urquhart, Erin A.; Zaitchik, Benjamin F.; Waugh, Darryn W.; Guikema, Seth D.; Del Castillo, Carlos E.</p> <p>2014-01-01</p> <p>The effect that <span class="hlt">climate</span> change and variability will have on waterborne bacteria is a topic of increasing concern for coastal ecosystems, including the Chesapeake Bay. Surface water temperature trends in the Bay indicate a warming pattern of roughly 0.3-0.4 C per decade over the past 30 years. It is unclear what impact future warming will have on pathogens currently found in the Bay, including Vibrio spp. Using historical environmental data, combined with three different statistical models of Vibrio vulnificus probability, we explore the relationship between environmental change and <span class="hlt">predicted</span> Vibrio vulnificus presence in the upper Chesapeake Bay. We find that the <span class="hlt">predicted</span> response of V. vulnificus probability to high temperatures in the Bay differs systematically between models of differing structure. As existing publicly available datasets are inadequate to determine which model structure is most appropriate, the impact of <span class="hlt">climatic</span> change on the probability of V. vulnificus presence in the Chesapeake Bay remains uncertain. This result points to the challenge of characterizing <span class="hlt">climate</span> sensitivity of ecological systems in which data are sparse and only statistical models of ecological sensitivity exist.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFM.A23G0307A','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFM.A23G0307A"><span>Multi-scale enhancement of <span class="hlt">climate</span> <span class="hlt">prediction</span> over land by increasing the model sensitivity to vegetation variability in EC-Earth</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Alessandri, A.; Catalano, F.; De Felice, M.; van den Hurk, B.; Doblas-Reyes, F. J.; Boussetta, S.; Balsamo, G.; Miller, P. A.</p> <p>2016-12-01</p> <p>The European consortium earth system model (EC-Earth; http://www.ec-earth.org) has been recently developed to include the dynamics of vegetation. In its original formulation, vegetation variability is simply operated by the Leaf Area Index (LAI), which affects <span class="hlt">climate</span> basically by changing the vegetation physiological resistance to evapotranspiration. This coupling has been found to have only a weak effect on the surface <span class="hlt">climate</span> modeled by EC-Earth. In reality, the effective sub-grid vegetation fractional coverage will vary seasonally and at interannual time-scales in response to leaf-canopy growth, phenology and senescence. Therefore it affects biophysical parameters such as the albedo, surface roughness and soil field capacity. To adequately represent this effect in EC-Earth, we included an exponential dependence of the vegetation cover on the LAI. By comparing two sets of simulations performed with and without the new variable fractional-coverage parameterization, spanning from centennial (20th Century) simulations and retrospective <span class="hlt">predictions</span> to the decadal (5-years), seasonal and weather time-scales, we show for the first time a significant multi-scale enhancement of vegetation impacts in <span class="hlt">climate</span> simulation and <span class="hlt">prediction</span> over land. Particularly large effects at multiple time scales are shown over boreal winter middle-to-high latitudes over Canada, West US, Eastern Europe, Russia and eastern Siberia due to the implemented time-varying shadowing effect by tree-vegetation on snow surfaces. Over Northern Hemisphere boreal forest regions the improved representation of vegetation cover tends to correct the winter warm biases, improves the <span class="hlt">climate</span> change sensitivity, the decadal potential <span class="hlt">predictability</span> as well as the skill of forecasts at seasonal and weather time-scales. Significant improvements of the <span class="hlt">prediction</span> of 2m temperature and rainfall are also shown over transitional land surface hot spots. Both the potential <span class="hlt">predictability</span> at decadal time-scale and</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017ClDy...49.1215A','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017ClDy...49.1215A"><span>Multi-scale enhancement of <span class="hlt">climate</span> <span class="hlt">prediction</span> over land by increasing the model sensitivity to vegetation variability in EC-Earth</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Alessandri, Andrea; Catalano, Franco; De Felice, Matteo; Van Den Hurk, Bart; Doblas Reyes, Francisco; Boussetta, Souhail; Balsamo, Gianpaolo; Miller, Paul A.</p> <p>2017-08-01</p> <p>The EC-Earth earth system model has been recently developed to include the dynamics of vegetation. In its original formulation, vegetation variability is simply operated by the Leaf Area Index (LAI), which affects <span class="hlt">climate</span> basically by changing the vegetation physiological resistance to evapotranspiration. This coupling has been found to have only a weak effect on the surface <span class="hlt">climate</span> modeled by EC-Earth. In reality, the effective sub-grid vegetation fractional coverage will vary seasonally and at interannual time-scales in response to leaf-canopy growth, phenology and senescence. Therefore it affects biophysical parameters such as the albedo, surface roughness and soil field capacity. To adequately represent this effect in EC-Earth, we included an exponential dependence of the vegetation cover on the LAI. By comparing two sets of simulations performed with and without the new variable fractional-coverage parameterization, spanning from centennial (twentieth century) simulations and retrospective <span class="hlt">predictions</span> to the decadal (5-years), seasonal and weather time-scales, we show for the first time a significant multi-scale enhancement of vegetation impacts in <span class="hlt">climate</span> simulation and <span class="hlt">prediction</span> over land. Particularly large effects at multiple time scales are shown over boreal winter middle-to-high latitudes over Canada, West US, Eastern Europe, Russia and eastern Siberia due to the implemented time-varying shadowing effect by tree-vegetation on snow surfaces. Over Northern Hemisphere boreal forest regions the improved representation of vegetation cover tends to correct the winter warm biases, improves the <span class="hlt">climate</span> change sensitivity, the decadal potential <span class="hlt">predictability</span> as well as the skill of forecasts at seasonal and weather time-scales. Significant improvements of the <span class="hlt">prediction</span> of 2 m temperature and rainfall are also shown over transitional land surface hot spots. Both the potential <span class="hlt">predictability</span> at decadal time-scale and seasonal-forecasts skill are enhanced over</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017EGUGA..19.9248A','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017EGUGA..19.9248A"><span>Multi-scale enhancement of <span class="hlt">climate</span> <span class="hlt">prediction</span> over land by increasing the model sensitivity to vegetation variability in EC-Earth</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Alessandri, Andrea; Catalano, Franco; De Felice, Matteo; Van Den Hurk, Bart; Doblas Reyes, Francisco; Boussetta, Souhail; Balsamo, Gianpaolo; Miller, Paul A.</p> <p>2017-04-01</p> <p>The EC-Earth earth system model has been recently developed to include the dynamics of vegetation. In its original formulation, vegetation variability is simply operated by the Leaf Area Index (LAI), which affects <span class="hlt">climate</span> basically by changing the vegetation physiological resistance to evapotranspiration. This coupling has been found to have only a weak effect on the surface <span class="hlt">climate</span> modeled by EC-Earth. In reality, the effective sub-grid vegetation fractional coverage will vary seasonally and at interannual time-scales in response to leaf-canopy growth, phenology and senescence. Therefore it affects biophysical parameters such as the albedo, surface roughness and soil field capacity. To adequately represent this effect in EC-Earth, we included an exponential dependence of the vegetation cover on the LAI. By comparing two sets of simulations performed with and without the new variable fractional-coverage parameterization, spanning from centennial (20th Century) simulations and retrospective <span class="hlt">predictions</span> to the decadal (5-years), seasonal and weather time-scales, we show for the first time a significant multi-scale enhancement of vegetation impacts in <span class="hlt">climate</span> simulation and <span class="hlt">prediction</span> over land. Particularly large effects at multiple time scales are shown over boreal winter middle-to-high latitudes over Canada, West US, Eastern Europe, Russia and eastern Siberia due to the implemented time-varying shadowing effect by tree-vegetation on snow surfaces. Over Northern Hemisphere boreal forest regions the improved representation of vegetation cover tends to correct the winter warm biases, improves the <span class="hlt">climate</span> change sensitivity, the decadal potential <span class="hlt">predictability</span> as well as the skill of forecasts at seasonal and weather time-scales. Significant improvements of the <span class="hlt">prediction</span> of 2m temperature and rainfall are also shown over transitional land surface hot spots. Both the potential <span class="hlt">predictability</span> at decadal time-scale and seasonal-forecasts skill are enhanced over Sahel</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5731736','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5731736"><span>Direct and indirect <span class="hlt">climate</span> controls <span class="hlt">predict</span> heterogeneous early-mid 21st century wildfire burned area across western and boreal North America</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Falk, Donald A.; Westerling, Anthony L.; Swetnam, Thomas W.</p> <p>2017-01-01</p> <p><span class="hlt">Predicting</span> wildfire under future conditions is complicated by complex interrelated drivers operating across large spatial scales. Annual area burned (AAB) is a useful index of global wildfire activity. Current and antecedent seasonal <span class="hlt">climatic</span> conditions, and the timing of snowpack melt, have been suggested as important drivers of AAB. As <span class="hlt">climate</span> warms, seasonal <span class="hlt">climate</span> and snowpack co-vary in intricate ways, influencing fire at continental and sub-continental scales. We used independent records of seasonal <span class="hlt">climate</span> and snow cover duration (last date of permanent snowpack, LDPS) and cell-based Structural Equation Models (SEM) to separate direct (<span class="hlt">climatic</span>) and indirect (snow cover) effects on relative changes in AAB under future <span class="hlt">climatic</span> scenarios across western and boreal North America. To isolate seasonal <span class="hlt">climate</span> variables with the greatest effect on AAB, we ran multiple regression models of log-transformed AAB on seasonal <span class="hlt">climate</span> variables and LDPS. We used the results of multiple regressions to project future AAB using GCM ensemble <span class="hlt">climate</span> variables and LDPS, and validated model <span class="hlt">predictions</span> with recent AAB trends. Direct influences of spring and winter temperatures on AAB are larger and more widespread than the indirect effect mediated by changes in LDPS in most areas. Despite significant warming trends and reductions in snow cover duration, projected responses of AAB to early-mid 21st century are heterogeneous across the continent. Changes in AAB range from strongly increasing (one order of magnitude increases in AAB) to moderately decreasing (more than halving of baseline AAB). Annual wildfire area burned in coming decades is likely to be highly geographically heterogeneous, reflecting interacting regional and seasonal <span class="hlt">climate</span> drivers of fire occurrence and spread. PMID:29244839</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_19");'>19</a></li> <li><a href="#" onclick='return showDiv("page_20");'>20</a></li> <li class="active"><span>21</span></li> <li><a href="#" onclick='return showDiv("page_22");'>22</a></li> <li><a href="#" onclick='return showDiv("page_23");'>23</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_21 --> <div id="page_22" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_20");'>20</a></li> <li><a href="#" onclick='return showDiv("page_21");'>21</a></li> <li class="active"><span>22</span></li> <li><a href="#" onclick='return showDiv("page_23");'>23</a></li> <li><a href="#" onclick='return showDiv("page_24");'>24</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="421"> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29244839','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29244839"><span>Direct and indirect <span class="hlt">climate</span> controls <span class="hlt">predict</span> heterogeneous early-mid 21st century wildfire burned area across western and boreal North America.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Kitzberger, Thomas; Falk, Donald A; Westerling, Anthony L; Swetnam, Thomas W</p> <p>2017-01-01</p> <p><span class="hlt">Predicting</span> wildfire under future conditions is complicated by complex interrelated drivers operating across large spatial scales. Annual area burned (AAB) is a useful index of global wildfire activity. Current and antecedent seasonal <span class="hlt">climatic</span> conditions, and the timing of snowpack melt, have been suggested as important drivers of AAB. As <span class="hlt">climate</span> warms, seasonal <span class="hlt">climate</span> and snowpack co-vary in intricate ways, influencing fire at continental and sub-continental scales. We used independent records of seasonal <span class="hlt">climate</span> and snow cover duration (last date of permanent snowpack, LDPS) and cell-based Structural Equation Models (SEM) to separate direct (<span class="hlt">climatic</span>) and indirect (snow cover) effects on relative changes in AAB under future <span class="hlt">climatic</span> scenarios across western and boreal North America. To isolate seasonal <span class="hlt">climate</span> variables with the greatest effect on AAB, we ran multiple regression models of log-transformed AAB on seasonal <span class="hlt">climate</span> variables and LDPS. We used the results of multiple regressions to project future AAB using GCM ensemble <span class="hlt">climate</span> variables and LDPS, and validated model <span class="hlt">predictions</span> with recent AAB trends. Direct influences of spring and winter temperatures on AAB are larger and more widespread than the indirect effect mediated by changes in LDPS in most areas. Despite significant warming trends and reductions in snow cover duration, projected responses of AAB to early-mid 21st century are heterogeneous across the continent. Changes in AAB range from strongly increasing (one order of magnitude increases in AAB) to moderately decreasing (more than halving of baseline AAB). Annual wildfire area burned in coming decades is likely to be highly geographically heterogeneous, reflecting interacting regional and seasonal <span class="hlt">climate</span> drivers of fire occurrence and spread.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/26489417','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/26489417"><span>Dynamically downscaling <span class="hlt">predictions</span> for deciduous tree leaf emergence in California under current and future <span class="hlt">climate</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Medvigy, David; Kim, Seung Hee; Kim, Jinwon; Kafatos, Menas C</p> <p>2016-07-01</p> <p>Models that <span class="hlt">predict</span> the timing of deciduous tree leaf emergence are typically very sensitive to temperature. However, many temperature data products, including those from <span class="hlt">climate</span> models, have been developed at a very coarse spatial resolution. Such coarse-resolution temperature products can lead to highly biased <span class="hlt">predictions</span> of leaf emergence. This study investigates how dynamical downscaling of <span class="hlt">climate</span> models impacts simulations of deciduous tree leaf emergence in California. Models for leaf emergence are forced with temperatures simulated by a general circulation model (GCM) at ~200-km resolution for 1981-2000 and 2031-2050 conditions. GCM simulations are then dynamically downscaled to 32- and 8-km resolution, and leaf emergence is again simulated. For 1981-2000, the regional average leaf emergence date is 30.8 days earlier in 32-km simulations than in ~200-km simulations. Differences between the 32 and 8 km simulations are small and mostly local. The impact of downscaling from 200 to 8 km is ~15 % smaller in 2031-2050 than in 1981-2000, indicating that the impacts of downscaling are unlikely to be stationary.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://cfpub.epa.gov/si/si_public_record_report.cfm?dirEntryId=225085&Lab=NHEERL&keyword=example+AND+comparative+AND+research&actType=&TIMSType=+&TIMSSubTypeID=&DEID=&epaNumber=&ntisID=&archiveStatus=Both&ombCat=Any&dateBeginCreated=&dateEndCreated=&dateBeginPublishedPresented=&dateEndPublishedPresented=&dateBeginUpdated=&dateEndUpdated=&dateBeginCompleted=&dateEndCompleted=&personID=&role=Any&journalID=&publisherID=&sortBy=revisionDate&count=50','EPA-EIMS'); return false;" href="https://cfpub.epa.gov/si/si_public_record_report.cfm?dirEntryId=225085&Lab=NHEERL&keyword=example+AND+comparative+AND+research&actType=&TIMSType=+&TIMSSubTypeID=&DEID=&epaNumber=&ntisID=&archiveStatus=Both&ombCat=Any&dateBeginCreated=&dateEndCreated=&dateBeginPublishedPresented=&dateEndPublishedPresented=&dateBeginUpdated=&dateEndUpdated=&dateBeginCompleted=&dateEndCompleted=&personID=&role=Any&journalID=&publisherID=&sortBy=revisionDate&count=50"><span>Using biogeographic distributions and natural history to <span class="hlt">predict</span> marine/estuarine species at risk to <span class="hlt">climate</span> change</span></a></p> <p><a target="_blank" href="http://oaspub.epa.gov/eims/query.page">EPA Science Inventory</a></p> <p></p> <p></p> <p>Effects of <span class="hlt">climate</span> change on marine and estuarine species will vary with attributes of the species and the spatial patterns of environmental change at the habitat and global scales. To better <span class="hlt">predict</span> which species are at greatest risk, we are developing a knowledge base of specie...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016EGUGA..18.6707H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016EGUGA..18.6707H"><span>The Arctic <span class="hlt">Predictability</span> and <span class="hlt">Prediction</span> on Seasonal-to-Interannual TimEscales (APPOSITE) project: a summary</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Hawkins, Ed; Day, Jonny; Tietsche, Steffen</p> <p>2016-04-01</p> <p>Recent years have seen significant developments in seasonal-to-interannual timescale <span class="hlt">climate</span> <span class="hlt">prediction</span> capabilities. However, until recently the potential of such systems to <span class="hlt">predict</span> Arctic <span class="hlt">climate</span> had not been assessed. We describe a multi-model <span class="hlt">predictability</span> experiment which was run as part of the Arctic <span class="hlt">Predictability</span> and <span class="hlt">Prediction</span> On Seasonal to Inter-annual TimEscales (APPOSITE) project. The main goal of APPOSITE was to quantify the timescales on which Arctic <span class="hlt">climate</span> is <span class="hlt">predictable</span>. In order to achieve this, a coordinated set of idealised initial-value <span class="hlt">predictability</span> experiments, with seven general circulation models, was conducted. This was the first model intercomparison project designed to quantify the <span class="hlt">predictability</span> of Arctic <span class="hlt">climate</span> on seasonal to inter-annual timescales. Here we provide a summary and update of the project's results which include: (1) quantifying the <span class="hlt">predictability</span> of Arctic <span class="hlt">climate</span>, especially sea ice; (2) the state-dependence of this <span class="hlt">predictability</span>, finding that extreme years are potentially more <span class="hlt">predictable</span> than neutral years; (3) analysing a spring '<span class="hlt">predictability</span> barrier' to skillful forecasts; (4) initial sea ice thickness information provides much of the skill for summer forecasts; (5) quantifying the sources of error growth and uncertainty in Arctic <span class="hlt">predictions</span>. The dataset is now publicly available.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFMGC23A1220I','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFMGC23A1220I"><span>Statistical <span class="hlt">prediction</span> of September Arctic Sea Ice minimum based on stable teleconnections with global <span class="hlt">climate</span> and oceanic patterns</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Ionita, M.; Grosfeld, K.; Scholz, P.; Lohmann, G.</p> <p>2016-12-01</p> <p>Sea ice in both Polar Regions is an important indicator for the expression of global <span class="hlt">climate</span> change and its polar amplification. Consequently, a broad information interest exists on sea ice, its coverage, variability and long term change. Knowledge on sea ice requires high quality data on ice extent, thickness and its dynamics. However, its <span class="hlt">predictability</span> depends on various <span class="hlt">climate</span> parameters and conditions. In order to provide insights into the potential development of a monthly/seasonal signal, we developed a robust statistical model based on ocean heat content, sea surface temperature and atmospheric variables to calculate an estimate of the September minimum sea ice extent for every year. Although previous statistical attempts at monthly/seasonal forecasts of September sea ice minimum show a relatively reduced skill, here it is shown that more than 97% (r = 0.98) of the September sea ice extent can <span class="hlt">predicted</span> three months in advance by using previous months conditions via a multiple linear regression model based on global sea surface temperature (SST), mean sea level pressure (SLP), air temperature at 850hPa (TT850), surface winds and sea ice extent persistence. The statistical model is based on the identification of regions with stable teleconnections between the predictors (climatological parameters) and the predictand (here sea ice extent). The results based on our statistical model contribute to the sea ice <span class="hlt">prediction</span> network for the sea ice outlook report (https://www.arcus.org/sipn) and could provide a tool for identifying relevant regions and <span class="hlt">climate</span> parameters that are important for the sea ice development in the Arctic and for detecting sensitive and critical regions in global coupled <span class="hlt">climate</span> models with focus on sea ice formation.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=2799657','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=2799657"><span><span class="hlt">Climate</span> Change and Risk of Leishmaniasis in North America: <span class="hlt">Predictions</span> from Ecological Niche Models of Vector and Reservoir Species</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>González, Camila; Wang, Ophelia; Strutz, Stavana E.; González-Salazar, Constantino; Sánchez-Cordero, Víctor; Sarkar, Sahotra</p> <p>2010-01-01</p> <p>Background <span class="hlt">Climate</span> change is increasingly being implicated in species' range shifts throughout the world, including those of important vector and reservoir species for infectious diseases. In North America (México, United States, and Canada), leishmaniasis is a vector-borne disease that is autochthonous in México and Texas and has begun to expand its range northward. Further expansion to the north may be facilitated by <span class="hlt">climate</span> change as more habitat becomes suitable for vector and reservoir species for leishmaniasis. Methods and Findings The analysis began with the construction of ecological niche models using a maximum entropy algorithm for the distribution of two sand fly vector species (Lutzomyia anthophora and L. diabolica), three confirmed rodent reservoir species (Neotoma albigula, N. floridana, and N. micropus), and one potential rodent reservoir species (N. mexicana) for leishmaniasis in northern México and the United States. As input, these models used species' occurrence records with topographic and <span class="hlt">climatic</span> parameters as explanatory variables. Models were tested for their ability to <span class="hlt">predict</span> correctly both a specified fraction of occurrence points set aside for this purpose and occurrence points from an independently derived data set. These models were refined to obtain <span class="hlt">predicted</span> species' geographical distributions under increasingly strict assumptions about the ability of a species to disperse to suitable habitat and to persist in it, as modulated by its ecological suitability. Models successful at <span class="hlt">predictions</span> were fitted to the extreme A2 and relatively conservative B2 projected <span class="hlt">climate</span> scenarios for 2020, 2050, and 2080 using publicly available interpolated <span class="hlt">climate</span> data from the Third Intergovernmental Panel on <span class="hlt">Climate</span> Change Assessment Report. Further analyses included estimation of the projected human population that could potentially be exposed to leishmaniasis in 2020, 2050, and 2080 under the A2 and B2 scenarios. All confirmed vector and</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2008AGUFMGC21A0709I','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2008AGUFMGC21A0709I"><span>Decadal Recruitment and Mortality of Ponderosa pine <span class="hlt">Predicted</span> for the 21st Century Under five Downscaled <span class="hlt">Climate</span> Change Scenarios</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Ironside, K. E.; Cole, K. L.; Eischeid, J. K.; Garfin, G. M.; Shaw, J. D.; Cobb, N. S.</p> <p>2008-12-01</p> <p>Ponderosa pine (Pinus ponderosa var. scopulorum) is the dominant conifer in higher elevation regions of the southwestern United States. Because this species is so prominent, southwestern montane ecosystems will be significantly altered if this species is strongly affected by future <span class="hlt">climate</span> changes. These changes could be highly challenging for land management agencies. In order to model the consequences of future <span class="hlt">climates</span>, 20th Century recruitment events and mortality for ponderosa pine were characterized using measures of seasonal water balance (precipitation - potential evapotranspiration). These relationships, assuming they will remain unchanged, were then used to <span class="hlt">predict</span> 21st Century changes in ponderosa pine occurrence in the southwest. Twenty-one AR4 IPCC General Circulation Model (GCM) A1B simulation results were ranked on their ability to simulate the later 20th Century (1950-2000 AD) precipitation seasonality, spatial patterns, and quantity in the western United States. Among the top ranked GCMs, five were selected for downscaling to a 4 km grid that represented a range in <span class="hlt">predictions</span> in terms of changes in water balance. <span class="hlt">Predicted</span> decadal changes in southwestern ponderosa pine for the 21st Century for these five <span class="hlt">climate</span> change scenarios were calculated using a multiple quadratic logistic regression model. Similar models of other western tree species (Pinus edulis, Yucca brevifolia) <span class="hlt">predicted</span> severe contractions, especially in the southern half of their ranges. However, the results for Ponderosa pine suggested future expansions throughout its range to both higher and lower elevations, as well as very significant expansions northward.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29331243','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29331243"><span>Tolerance and potential for adaptation of a Baltic Sea rockweed under <span class="hlt">predicted</span> <span class="hlt">climate</span> change conditions.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Rugiu, Luca; Manninen, Iita; Rothäusler, Eva; Jormalainen, Veijo</p> <p>2018-03-01</p> <p><span class="hlt">Climate</span> change is threating species' persistence worldwide. To <span class="hlt">predict</span> species responses to <span class="hlt">climate</span> change we need information not just on their environmental tolerance but also on its adaptive potential. We tested how the foundation species of rocky littoral habitats, Fucus vesiculosus, responds to combined hyposalinity and warming projected to the Baltic Sea by 2070-2099. We quantified responses of replicated populations originating from the entrance, central, and marginal Baltic regions. Using replicated individuals, we tested for the presence of within-population tolerance variation. Future conditions hampered growth and survival of the central and marginal populations whereas the entrance populations fared well. Further, both the among- and within-population variation in responses to <span class="hlt">climate</span> change indicated existence of genetic variation in tolerance. Such standing genetic variation provides the raw material necessary for adaptation to a changing environment, which may eventually ensure the persistence of the species in the inner Baltic Sea. Copyright © 2017 Elsevier Ltd. All rights reserved.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012EPJWC..2501077P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012EPJWC..2501077P"><span>Calibration of the heat balance model for <span class="hlt">prediction</span> of car <span class="hlt">climate</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Pokorný, Jan; Fišer, Jan; Jícha, Miroslav</p> <p>2012-04-01</p> <p>In the paper, the authors refer to development a heat balance model to <span class="hlt">predict</span> car <span class="hlt">climate</span> and power heat load. Model is developed in Modelica language using Dymola as interpreter. It is a dynamical system, which describes a heat exchange between car cabin and ambient. Inside a car cabin, there is considered heat exchange between air zone, interior and air-conditioning system. It is considered 1D heat transfer with a heat accumulation and a relative movement Sun respect to the car cabin, whilst car is moving. Measurements of the real operating conditions of gave us data for model calibration. The model was calibrated for Škoda Felicia parking-summer scenarios.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/27893496','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/27893496"><span>Do Leadership Style, Unit <span class="hlt">Climate</span>, and Safety <span class="hlt">Climate</span> Contribute to Safe Medication Practices?</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Farag, Amany; Tullai-McGuinness, Susan; Anthony, Mary K; Burant, Christopher</p> <p>2017-01-01</p> <p>This study aims at: examining if leadership style and unit <span class="hlt">climate</span> <span class="hlt">predict</span> safety <span class="hlt">climate</span>; and testing the direct, indirect, and total effect of leadership style, unit <span class="hlt">climate</span>, and safety <span class="hlt">climate</span> on nurses' safe medication practices. The Institute of Medicine and nursing scholars propose that safety <span class="hlt">climate</span> is a prerequisite to safety practices. However, there is limited empirical evidence about factors contributing to the development of safety <span class="hlt">climate</span> and about the association with nurses' safe medication practices. This cross-sectional study used survey data from 246 RNs working in a Magnet® hospital. Leadership style and unit <span class="hlt">climate</span> <span class="hlt">predicted</span> 20% to 50% of variance on all safety <span class="hlt">climate</span> dimensions. Model testing revealed the indirect impact of leadership style and unit <span class="hlt">climate</span> on nurses' safe medication practices. Our hypothesized model explained small amount of the variance on nurses' safe medication practices. This finding suggests that nurses' safe medication practices are influenced by multiple contextual and personal factors that should be further examined.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/20375046','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/20375046"><span>Non-<span class="hlt">climatic</span> thermal adaptation: implications for species' responses to <span class="hlt">climate</span> warming.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Marshall, David J; McQuaid, Christopher D; Williams, Gray A</p> <p>2010-10-23</p> <p>There is considerable interest in understanding how ectothermic animals may physiologically and behaviourally buffer the effects of <span class="hlt">climate</span> warming. Much less consideration is being given to how organisms might adapt to non-<span class="hlt">climatic</span> heat sources in ways that could confound <span class="hlt">predictions</span> for responses of species and communities to <span class="hlt">climate</span> warming. Although adaptation to non-<span class="hlt">climatic</span> heat sources (solar and geothermal) seems likely in some marine species, <span class="hlt">climate</span> warming <span class="hlt">predictions</span> for marine ectotherms are largely based on adaptation to <span class="hlt">climatically</span> relevant heat sources (air or surface sea water temperature). Here, we show that non-<span class="hlt">climatic</span> solar heating underlies thermal resistance adaptation in a rocky-eulittoral-fringe snail. Comparisons of the maximum temperatures of the air, the snail's body and the rock substratum with solar irradiance and physiological performance show that the highest body temperature is primarily controlled by solar heating and re-radiation, and that the snail's upper lethal temperature exceeds the highest <span class="hlt">climatically</span> relevant regional air temperature by approximately 22°C. Non-<span class="hlt">climatic</span> thermal adaptation probably features widely among marine and terrestrial ectotherms and because it could enable species to tolerate <span class="hlt">climatic</span> rises in air temperature, it deserves more consideration in general and for inclusion into <span class="hlt">climate</span> warming models.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20140012054','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20140012054"><span>Advancing Drought Understanding, Monitoring and <span class="hlt">Prediction</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Mariotti, Annarita; Schubert, Siegfried D.; Mo, Kingtse; Peters-Lidard, Christa; Wood, Andy; Pulwarty, Roger; Huang, Jin; Barrie, Dan</p> <p>2013-01-01</p> <p>, focused and coordinated research efforts are needed, drawing from excellence across the broad drought research community. To meet this challenge, National Oceanic and Atmospheric <span class="hlt">Administration</span> (NOAA)'s Drought Task Force was established in October 2011 with the ambitious goal of achieving significant new advances in the ability to understand, monitor, and <span class="hlt">predict</span> drought over North America. The Task Force (duration of October 2011-September 2014) is an initiative of NOAA's <span class="hlt">Climate</span> Program Office Modeling, Analysis, <span class="hlt">Predictions</span>, and Projections (MAPP) program in partnership with NIDIS. It brings together over 30 leading MAPP-funded drought scientists from multiple academic and federal institutions [involves scientists from NOAA's research laboratories and centers, the National Aeronautics and Space <span class="hlt">Administration</span> (NASA), U.S. Department of Agriculture, National Center for Atmospheric Research (NCAR), and many universities] in a concerted research effort that builds on individual MAPP research projects. These projects span the wide spectrum of drought research needed to make fundamental advances, from those aimed at the basic understanding of drought mechanisms to those aimed at testing new drought monitoring and <span class="hlt">prediction</span> tools for operational and service purposes (as part of NCEP's <span class="hlt">Climate</span> Test Bed). The Drought Task Force provides focus and coordination to MAPP drought research activities and also facilitates synergies with other national and international drought research efforts, including those by the GDIS.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.fs.usda.gov/treesearch/pubs/37074','TREESEARCH'); return false;" href="https://www.fs.usda.gov/treesearch/pubs/37074"><span>Survey of Armillaria spp. in the Oregon East Cascades: Baseline data for <span class="hlt">predicting</span> <span class="hlt">climatic</span> influences on Armillaria root disease</span></a></p> <p><a target="_blank" href="http://www.fs.usda.gov/treesearch/">Treesearch</a></p> <p>J. W. Hanna; A. L. Smith; H. M. Maffei; M.-S. Kim; N. B. Klopfenstein</p> <p>2008-01-01</p> <p>Root disease pathogens, such as Armillaria solidipes Peck (recently recognized older name for A. ostoyae), will likely have increasing impacts to forest ecosystems as trees undergo stress due to <span class="hlt">climate</span> change. Before we can <span class="hlt">predict</span> future impacts of root disease pathogens, we must first develop an ability to <span class="hlt">predict</span> current distributions of the pathogens (and their...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5111361','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5111361"><span><span class="hlt">Predicting</span> non-familial major physical violent crime perpetration in the U.S. Army from <span class="hlt">administrative</span> data</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Rosellini, Anthony J.; Monahan, John; Street, Amy E.; Heeringa, Steven G.; Hill, Eric D.; Petukhova, Maria; Reis, Ben Y.; Sampson, Nancy A.; Bliese, Paul; Schoenbaum, Michael; Stein, Murray B.; Ursano, Robert; Kessler, Ronald C.</p> <p>2016-01-01</p> <p>BACKGROUND Although interventions exist to reduce violent crime, optimal implementation requires accurate targeting. We report the results of an attempt to develop an actuarial model using machine learning methods to <span class="hlt">predict</span> future violent crimes among U.S. Army soldiers. METHODS A consolidated <span class="hlt">administrative</span> database for all 975,057 soldiers in the U.S. Army in 2004-2009 was created in the Army Study to Assess Risk and Resilience in Servicemembers (Army STARRS). 5,771 of these soldiers committed a first founded major physical violent crime (murder-manslaughter, kidnapping, aggravated arson, aggravated assault, robbery) over that time period. Temporally prior <span class="hlt">administrative</span> records measuring socio-demographic, Army career, criminal justice, medical/pharmacy, and contextual variables were used to build an actuarial model for these crimes separately among men and women using machine learning methods (cross-validated stepwise regression; random forests; penalized regressions). The model was then validated in an independent 2011-2013 sample. RESULTS Key predictors were indicators of disadvantaged social/socio-economic status, early career stage, prior crime, and mental disorder treatment. Area under the receiver operating characteristic curve was .80-.82 in 2004-2009 and .77 in a 2011-2013 validation sample. 36.2-33.1% (male-female) of all <span class="hlt">administratively</span>-recorded crimes were committed by the 5% of soldiers having highest <span class="hlt">predicted</span> risk in 2004-2009 and an even higher proportion (50.5%) in the 2011-2013 validation sample. CONCLUSIONS Although these results suggest that the models could be used to target soldiers at high risk of violent crime perpetration for preventive interventions, final implementation decisions would require further validation and weighing of <span class="hlt">predicted</span> effectiveness against intervention costs and competing risks. PMID:26436603</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017QSRv..155...50M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017QSRv..155...50M"><span>Ice core and <span class="hlt">climate</span> reanalysis analogs to <span class="hlt">predict</span> Antarctic and Southern Hemisphere <span class="hlt">climate</span> changes</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Mayewski, P. A.; Carleton, A. M.; Birkel, S. D.; Dixon, D.; Kurbatov, A. V.; Korotkikh, E.; McConnell, J.; Curran, M.; Cole-Dai, J.; Jiang, S.; Plummer, C.; Vance, T.; Maasch, K. A.; Sneed, S. B.; Handley, M.</p> <p>2017-01-01</p> <p>A primary goal of the SCAR (Scientific Committee for Antarctic Research) initiated AntClim21 (Antarctic <span class="hlt">Climate</span> in the 21st Century) Scientific Research Programme is to develop analogs for understanding past, present and future <span class="hlt">climates</span> for the Antarctic and Southern Hemisphere. In this contribution to AntClim21 we provide a framework for achieving this goal that includes: a description of basic <span class="hlt">climate</span> parameters; comparison of existing <span class="hlt">climate</span> reanalyses; and ice core sodium records as proxies for the frequencies of marine air mass intrusion spanning the past ∼2000 years. The resulting analog examples include: natural variability, a continuation of the current trend in Antarctic and Southern Ocean <span class="hlt">climate</span> characterized by some regions of warming and some cooling at the surface of the Southern Ocean, Antarctic ozone healing, a generally warming <span class="hlt">climate</span> and separate increases in the meridional and zonal winds. We emphasize changes in atmospheric circulation because the atmosphere rapidly transports heat, moisture, momentum, and pollutants, throughout the middle to high latitudes. In addition, atmospheric circulation interacts with temporal variations (synoptic to monthly scales, inter-annual, decadal, etc.) of sea ice extent and concentration. We also investigate associations between Antarctic atmospheric circulation features, notably the Amundsen Sea Low (ASL), and primary <span class="hlt">climate</span> teleconnections including the SAM (Southern Annular Mode), ENSO (El Nîno Southern Oscillation), the Pacific Decadal Oscillation (PDO), the AMO (Atlantic Multidecadal Oscillation), and solar irradiance variations.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20110015782','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20110015782"><span><span class="hlt">Climate</span> Change Impacts and Responses: Societal Indicators for the National <span class="hlt">Climate</span> Assessment</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Kenney, Melissa A.; Chen, Robert S.; Maldonado, Julie; Quattrochi, Dale</p> <p>2011-01-01</p> <p>The <span class="hlt">Climate</span> Change Impacts and Responses: Societal Indicators for the National <span class="hlt">Climate</span> Assessment workshop, sponsored by the National Aeronautics and Space <span class="hlt">Administration</span> (NASA) for the National <span class="hlt">Climate</span> Assessment (NCA), was held on April 28-29, 2011 at The Madison Hotel in Washington, DC. A group of 56 experts (see list in Appendix B) convened to share their experiences. Participants brought to bear a wide range of disciplinary expertise in the social and natural sciences, sector experience, and knowledge about developing and implementing indicators for a range of purposes. Participants included representatives from federal and state government, non-governmental organizations, tribes, universities, and communities. The purpose of the workshop was to assist the NCA in developing a strategic framework for <span class="hlt">climate</span>-related physical, ecological, and socioeconomic indicators that can be easily communicated with the U.S. population and that will support monitoring, assessment, <span class="hlt">prediction</span>, evaluation, and decision-making. The NCA indicators are envisioned as a relatively small number of policy-relevant integrated indicators designed to provide a consistent, objective, and transparent overview of major variations in <span class="hlt">climate</span> impacts, vulnerabilities, adaptation, and mitigation activities across sectors, regions, and timeframes. The workshop participants were asked to provide input on a number of topics, including: (1) categories of societal indicators for the NCA; (2) alternative approaches to constructing indicators and the better approaches for NCA to consider; (3) specific requirements and criteria for implementing the indicators; and (4) sources of data for and creators of such indicators. Socioeconomic indicators could include demographic, cultural, behavioral, economic, public health, and policy components relevant to impacts, vulnerabilities, and adaptation to <span class="hlt">climate</span> change as well as both proactive and reactive responses to <span class="hlt">climate</span> change. Participants provided</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012AGUFMGC43D1061F','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012AGUFMGC43D1061F"><span>The Dependencies of Ecosystem Pattern, Structure, and Dynamics on <span class="hlt">Climate</span>, <span class="hlt">Climate</span> Variability, and <span class="hlt">Climate</span> Change</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Flanagan, S.; Hurtt, G. C.; Fisk, J. P.; Rourke, O.</p> <p>2012-12-01</p> <p>A robust understanding of the sensitivity of the pattern, structure, and dynamics of ecosystems to <span class="hlt">climate</span>, <span class="hlt">climate</span> variability, and <span class="hlt">climate</span> change is needed to <span class="hlt">predict</span> ecosystem responses to current and projected <span class="hlt">climate</span> change. We present results of a study designed to first quantify the sensitivity of ecosystems to <span class="hlt">climate</span> through the use of <span class="hlt">climate</span> and ecosystem data, and then use the results to test the sensitivity of the <span class="hlt">climate</span> data in a state-of the art ecosystem model. A database of available ecosystem characteristics such as mean canopy height, above ground biomass, and basal area was constructed from sources like the National Biomass and Carbon Dataset (NBCD). The ecosystem characteristics were then paired by latitude and longitude with the corresponding <span class="hlt">climate</span> characteristics temperature, precipitation, photosynthetically active radiation (PAR) and dew point that were retrieved from the North American Regional Reanalysis (NARR). The average yearly and seasonal means of the <span class="hlt">climate</span> data, and their associated maximum and minimum values, over the 1979-2010 time frame provided by NARR were constructed and paired with the ecosystem data. The compiled results provide natural patterns of vegetation structure and distribution with regard to <span class="hlt">climate</span> data. An advanced ecosystem model, the Ecosystem Demography model (ED), was then modified to allow yearly alterations to its mechanistic <span class="hlt">climate</span> lookup table and used to <span class="hlt">predict</span> the sensitivities of ecosystem pattern, structure, and dynamics to <span class="hlt">climate</span> data. The combined ecosystem structure and <span class="hlt">climate</span> data results were compared to ED's output to check the validity of the model. After verification, <span class="hlt">climate</span> change scenarios such as those used in the last IPCC were run and future forest structure changes due to <span class="hlt">climate</span> sensitivities were identified. The results of this study can be used to both quantify and test key relationships for next generation models. The sensitivity of ecosystem characteristics to <span class="hlt">climate</span> data</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4211457','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4211457"><span>Non-<span class="hlt">climatic</span> constraints on upper elevational plant range expansion under <span class="hlt">climate</span> change</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Brown, Carissa D.; Vellend, Mark</p> <p>2014-01-01</p> <p>We are limited in our ability to <span class="hlt">predict</span> <span class="hlt">climate</span>-change-induced range shifts by our inadequate understanding of how non-<span class="hlt">climatic</span> factors contribute to determining range limits along putatively <span class="hlt">climatic</span> gradients. Here, we present a unique combination of observations and experiments demonstrating that seed predation and soil properties strongly limit regeneration beyond the upper elevational range limit of sugar maple, a tree species of major economic importance. Most strikingly, regeneration beyond the range limit occurred almost exclusively when seeds were experimentally protected from predators. Regeneration from seed was depressed on soil from beyond the range edge when this soil was transplanted to sites within the range, with indirect evidence suggesting that fungal pathogens play a role. Non-<span class="hlt">climatic</span> factors are clearly in need of careful attention when attempting to <span class="hlt">predict</span> the biotic consequences of <span class="hlt">climate</span> change. At minimum, we can expect non-<span class="hlt">climatic</span> factors to create substantial time lags between the creation of more favourable <span class="hlt">climatic</span> conditions and range expansion. PMID:25253462</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/28395353','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/28395353"><span><span class="hlt">Predicting</span> Directly Measured Trunk and Upper Arm Postures in Paper Mill Work From <span class="hlt">Administrative</span> Data, Workers' Ratings and Posture Observations.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Heiden, Marina; Garza, Jennifer; Trask, Catherine; Mathiassen, Svend Erik</p> <p>2017-03-01</p> <p>A cost-efficient approach for assessing working postures could be to build statistical models for <span class="hlt">predicting</span> results of direct measurements from cheaper data, and apply these models to samples in which only the latter data are available. The present study aimed to build and assess the performance of statistical models <span class="hlt">predicting</span> inclinometer-assessed trunk and arm posture among paper mill workers. Separate models were built using <span class="hlt">administrative</span> data, workers' ratings of their exposure, and observations of the work from video recordings as predictors. Trunk and upper arm postures were measured using inclinometry on 28 paper mill workers during three work shifts each. Simultaneously, the workers were video filmed, and their postures were assessed by observation of the videos afterwards. Workers' ratings of exposure, and <span class="hlt">administrative</span> data on staff and production during the shifts were also collected. Linear mixed models were fitted for <span class="hlt">predicting</span> inclinometer-assessed exposure variables (median trunk and upper arm angle, proportion of time with neutral trunk and upper arm posture, and frequency of periods in neutral trunk and upper arm inclination) from <span class="hlt">administrative</span> data, workers' ratings, and observations, respectively. Performance was evaluated in terms of Akaike information criterion, proportion of variance explained (R2), and standard error (SE) of the model estimate. For models performing well, validity was assessed by bootstrap resampling. Models based on <span class="hlt">administrative</span> data performed poorly (R2 ≤ 15%) and would not be useful for assessing posture in this population. Models using workers' ratings of exposure performed slightly better (8% ≤ R2 ≤ 27% for trunk posture; 14% ≤ R2 ≤ 36% for arm posture). The best model was obtained when using observational data for <span class="hlt">predicting</span> frequency of periods with neutral arm inclination. It explained 56% of the variance in the postural exposure, and its SE was 5.6. Bootstrap validation of this model showed similar</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/26608411','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/26608411"><span>Future <span class="hlt">climate</span> change is <span class="hlt">predicted</span> to shift long-term persistence zones in the cold-temperate kelp Laminaria hyperborea.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Assis, Jorge; Lucas, Ana Vaz; Bárbara, Ignacio; Serrão, Ester Álvares</p> <p>2016-02-01</p> <p>Global <span class="hlt">climate</span> change is shifting species distributions worldwide. At rear edges (warmer, low latitude range margins), the consequences of small variations in environmental conditions can be magnified, producing large negative effects on species ranges. A major outcome of shifts in distributions that only recently received attention is the potential to reduce the levels of intra-specific diversity and consequently the global evolutionary and adaptive capacity of species to face novel disturbances. This is particularly important for low dispersal marine species, such as kelps, that generally retain high and unique genetic diversity at rear ranges resulting from long-term persistence, while ranges shifts during <span class="hlt">climatic</span> glacial/interglacial cycles. Using ecological niche modelling, we (1) infer the major environmental forces shaping the distribution of a cold-temperate kelp, Laminaria hyperborea (Gunnerus) Foslie, and we (2) <span class="hlt">predict</span> the effect of past <span class="hlt">climate</span> changes in shaping regions of long-term persistence (i.e., <span class="hlt">climatic</span> refugia), where this species might hypothetically harbour higher genetic diversity given the absence of bottlenecks and local extinctions over the long term. We further (3) assessed the consequences of future <span class="hlt">climate</span> for the fate of L. hyperborea using different scenarios of greenhouse gas emissions (RCP 2.6 and RCP 8.5). Results show NW Iberia, SW Ireland and W English Channel, Faroe Islands and S Iceland, as regions where L. hyperborea may have persisted during past <span class="hlt">climate</span> extremes until present day. All <span class="hlt">predictions</span> for the future showed expansions to northern territories coupled with the significant loss of suitable habitats at low latitude range margins, where long-term persistence was inferred (e.g., NW Iberia). This pattern was particularly evident in the most agressive scenario of <span class="hlt">climate</span> change (RCP 8.5), likely driving major biodiversity loss, changes in ecosystem functioning and the impoverishment of the global gene pool of L</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_20");'>20</a></li> <li><a href="#" onclick='return showDiv("page_21");'>21</a></li> <li class="active"><span>22</span></li> <li><a href="#" onclick='return showDiv("page_23");'>23</a></li> <li><a href="#" onclick='return showDiv("page_24");'>24</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_22 --> <div id="page_23" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_21");'>21</a></li> <li><a href="#" onclick='return showDiv("page_22");'>22</a></li> <li class="active"><span>23</span></li> <li><a href="#" onclick='return showDiv("page_24");'>24</a></li> <li><a href="#" onclick='return showDiv("page_25");'>25</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="441"> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/28223483','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/28223483"><span>Seasonal <span class="hlt">prediction</span> of US summertime ozone using statistical analysis of large scale <span class="hlt">climate</span> patterns.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Shen, Lu; Mickley, Loretta J</p> <p>2017-03-07</p> <p>We develop a statistical model to <span class="hlt">predict</span> June-July-August (JJA) daily maximum 8-h average (MDA8) ozone concentrations in the eastern United States based on large-scale <span class="hlt">climate</span> patterns during the previous spring. We find that anomalously high JJA ozone in the East is correlated with these springtime patterns: warm tropical Atlantic and cold northeast Pacific sea surface temperatures (SSTs), as well as positive sea level pressure (SLP) anomalies over Hawaii and negative SLP anomalies over the Atlantic and North America. We then develop a linear regression model to <span class="hlt">predict</span> JJA MDA8 ozone from 1980 to 2013, using the identified SST and SLP patterns from the previous spring. The model explains ∼45% of the variability in JJA MDA8 ozone concentrations and ∼30% variability in the number of JJA ozone episodes (>70 ppbv) when averaged over the eastern United States. This seasonal <span class="hlt">predictability</span> results from large-scale ocean-atmosphere interactions. Warm tropical Atlantic SSTs can trigger diabatic heating in the atmosphere and influence the extratropical <span class="hlt">climate</span> through stationary wave propagation, leading to greater subsidence, less precipitation, and higher temperatures in the East, which increases surface ozone concentrations there. Cooler SSTs in the northeast Pacific are also associated with more summertime heatwaves and high ozone in the East. On average, models participating in the Atmospheric Model Intercomparison Project fail to capture the influence of this ocean-atmosphere interaction on temperatures in the eastern United States, implying that such models would have difficulty simulating the interannual variability of surface ozone in this region.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5347621','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5347621"><span>Seasonal <span class="hlt">prediction</span> of US summertime ozone using statistical analysis of large scale <span class="hlt">climate</span> patterns</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Mickley, Loretta J.</p> <p>2017-01-01</p> <p>We develop a statistical model to <span class="hlt">predict</span> June–July–August (JJA) daily maximum 8-h average (MDA8) ozone concentrations in the eastern United States based on large-scale <span class="hlt">climate</span> patterns during the previous spring. We find that anomalously high JJA ozone in the East is correlated with these springtime patterns: warm tropical Atlantic and cold northeast Pacific sea surface temperatures (SSTs), as well as positive sea level pressure (SLP) anomalies over Hawaii and negative SLP anomalies over the Atlantic and North America. We then develop a linear regression model to <span class="hlt">predict</span> JJA MDA8 ozone from 1980 to 2013, using the identified SST and SLP patterns from the previous spring. The model explains ∼45% of the variability in JJA MDA8 ozone concentrations and ∼30% variability in the number of JJA ozone episodes (>70 ppbv) when averaged over the eastern United States. This seasonal <span class="hlt">predictability</span> results from large-scale ocean–atmosphere interactions. Warm tropical Atlantic SSTs can trigger diabatic heating in the atmosphere and influence the extratropical <span class="hlt">climate</span> through stationary wave propagation, leading to greater subsidence, less precipitation, and higher temperatures in the East, which increases surface ozone concentrations there. Cooler SSTs in the northeast Pacific are also associated with more summertime heatwaves and high ozone in the East. On average, models participating in the Atmospheric Model Intercomparison Project fail to capture the influence of this ocean–atmosphere interaction on temperatures in the eastern United States, implying that such models would have difficulty simulating the interannual variability of surface ozone in this region. PMID:28223483</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/21078097','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/21078097"><span>Cod Gadus morhua and <span class="hlt">climate</span> change: processes, productivity and <span class="hlt">prediction</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Brander, K M</p> <p>2010-11-01</p> <p>Environmental factors act on individual fishes directly and indirectly. The direct effects on rates and behaviour can be studied experimentally and in the field, particularly with the advent of ever smarter tags for tracking fishes and their environment. Indirect effects due to changes in food, predators, parasites and diseases are much more difficult to estimate and <span class="hlt">predict</span>. <span class="hlt">Climate</span> can affect all life-history stages through direct and indirect processes and although the consequences in terms of growth, survival and reproductive output can be monitored, it is often difficult to determine the causes. Investigation of cod Gadus morhua populations across the whole North Atlantic Ocean has shown large-scale patterns of change in productivity due to lower individual growth and condition, caused by large-scale <span class="hlt">climate</span> forcing. If a population is being heavily exploited then a drop in productivity can push it into decline unless the level of fishing is reduced: the idea of a stable carrying capacity is a dangerous myth. Overexploitation can be avoided by keeping fishing mortality low and by monitoring and responding rapidly to changes in productivity. There are signs that this lesson has been learned and that G. morhua will continue to be a mainstay of the human diet. © 2010 The Author. Journal of Fish Biology © 2010 The Fisheries Society of the British Isles.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.cpc.ncep.noaa.gov/products/monitoring_and_data/pacific.shtml','SCIGOVWS'); return false;" href="http://www.cpc.ncep.noaa.gov/products/monitoring_and_data/pacific.shtml"><span>CPC - Monitoring & Data: Pacific Island <span class="hlt">Climate</span> Data</span></a></p> <p><a target="_blank" href="http://www.science.gov/aboutsearch.html">Science.gov Websites</a></p> <p></p> <p></p> <p>Weather Service NWS logo - Click to go to the NWS home page <em><span class="hlt">Climate</span></em> <span class="hlt">Prediction</span> Center Home Site Map News Web resources and services. HOME > Monitoring and Data > Pacific Islands <em><span class="hlt">Climate</span></em> Data & Maps island stations. NOAA/ National Weather Service NOAA Center for Weather and <em><span class="hlt">Climate</span></em> <span class="hlt">Prediction</span> <em><span class="hlt">Climate</span></em></p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.cpc.ncep.noaa.gov/products/analysis_monitoring/regional_monitoring/usa.shtml','SCIGOVWS'); return false;" href="http://www.cpc.ncep.noaa.gov/products/analysis_monitoring/regional_monitoring/usa.shtml"><span><span class="hlt">Climate</span> <span class="hlt">Prediction</span> Center - Monitoring and Data - Regional <span class="hlt">Climate</span> Maps:</span></a></p> <p><a target="_blank" href="http://www.science.gov/aboutsearch.html">Science.gov Websites</a></p> <p></p> <p></p> <p>; Precipitation & <em>Temperature</em> > Regional <span class="hlt">Climate</span> Maps: USA Menu Weekly 1-Month 3-Month 12-Month Weekly Total Precipitation Average <em>Temperature</em> Extreme Maximum <em>Temperature</em> Extreme Minimum <em>Temperature</em> Departure of Average <em>Temperature</em> from Normal Extreme Apparent <em>Temperature</em> Minimum Wind Chill <em>Temperature</em></p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013AGUFM.B41A0379J','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013AGUFM.B41A0379J"><span>From field to region yield <span class="hlt">predictions</span> in response to pedo-<span class="hlt">climatic</span> variations in Eastern Canada</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>JÉGO, G.; Pattey, E.; Liu, J.</p> <p>2013-12-01</p> <p>The increase in global population coupled with new pressures to produce energy and bioproducts from agricultural land requires an increase in crop productivity. However, the influence of <span class="hlt">climate</span> and soil variations on crop production and environmental performance is not fully understood and accounted for to define more sustainable and economical management strategies. Regional crop modeling can be a great tool for understanding the impact of <span class="hlt">climate</span> variations on crop production, for planning grain handling and for assessing the impact of agriculture on the environment, but it is often limited by the availability of input data. The STICS ("Simulateur mulTIdisciplinaire pour les Cultures Standard") crop model, developed by INRA (France) is a functional crop model which has a built-in module to optimize several input parameters by minimizing the difference between calculated and measured output variables, such as Leaf Area Index (LAI). STICS crop model was adapted to the short growing season of the Mixedwood Plains Ecozone using field experiments results, to <span class="hlt">predict</span> biomass and yield of soybean, spring wheat and corn. To minimize the numbers of inference required for regional applications, 'generic' cultivars rather than specific ones have been calibrated in STICS. After the calibration of several model parameters, the root mean square error (RMSE) of yield and biomass <span class="hlt">predictions</span> ranged from 10% to 30% for the three crops. A bit more scattering was obtained for LAI (20%<RMSE<38%). Results indicated so far that one cultivar was enough to describe soybean and spring wheat, while at least two cultivars were required for corn. Flux datasets were also instrumental to select the evapotranspiration function that performed the best in STICS and to make a preliminary verification of the sensitivity of the biomass <span class="hlt">prediction</span> to <span class="hlt">climate</span> variations. Using RS data to re-initialize input parameters that are not readily available (e.g. seeding date) is considered an effective way</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.ncep.noaa.gov','SCIGOVWS'); return false;" href="http://www.ncep.noaa.gov"><span>National Centers for Environmental <span class="hlt">Prediction</span> (NCEP)</span></a></p> <p><a target="_blank" href="http://www.science.gov/aboutsearch.html">Science.gov Websites</a></p> <p></p> <p></p> <p>Tropical Marine Fire Weather Forecast Maps Unified Surface Analysis <em><span class="hlt">Climate</span></em> <em><span class="hlt">Climate</span></em> <span class="hlt">Prediction</span> <em><span class="hlt">Climate</span></em> forecasts of hazardous flight conditions at all levels within domestic and international air space. <em><span class="hlt">Climate</span></em> <span class="hlt">Prediction</span> Center monitors and forecasts short-term <em><span class="hlt">climate</span></em> fluctuations and provides information on the</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016EGUGA..18.7413P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016EGUGA..18.7413P"><span>Processes Understanding of Decadal <span class="hlt">Climate</span> Variability</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Prömmel, Kerstin; Cubasch, Ulrich</p> <p>2016-04-01</p> <p>The realistic representation of decadal <span class="hlt">climate</span> variability in the models is essential for the quality of decadal <span class="hlt">climate</span> <span class="hlt">predictions</span>. Therefore, the understanding of those processes leading to decadal <span class="hlt">climate</span> variability needs to be improved. Several of these processes are already included in <span class="hlt">climate</span> models but their importance has not yet completely been clarified. The simulation of other processes requires sometimes a higher resolution of the model or an extension by additional subsystems. This is addressed within one module of the German research program "MiKlip II - Decadal <span class="hlt">Climate</span> <span class="hlt">Predictions</span>" (http://www.fona-miklip.de/en/) with a focus on the following processes. Stratospheric processes and their impact on the troposphere are analysed regarding the <span class="hlt">climate</span> response to aerosol perturbations caused by volcanic eruptions and the stratospheric decadal variability due to solar forcing, <span class="hlt">climate</span> change and ozone recovery. To account for the interaction between changing ozone concentrations and <span class="hlt">climate</span> a computationally efficient ozone chemistry module is developed and implemented in the MiKlip <span class="hlt">prediction</span> system. The ocean variability and air-sea interaction are analysed with a special focus on the reduction of the North Atlantic cold bias. In addition, the <span class="hlt">predictability</span> of the oceanic carbon uptake with a special emphasis on the underlying mechanism is investigated. This addresses a combination of physical, biological and chemical processes.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.cpc.ncep.noaa.gov/products/predictions/30day/fxus07.html','SCIGOVWS'); return false;" href="http://www.cpc.ncep.noaa.gov/products/predictions/30day/fxus07.html"><span><span class="hlt">Climate</span> <span class="hlt">Prediction</span> Center - Seasonal Outlook</span></a></p> <p><a target="_blank" href="http://www.science.gov/aboutsearch.html">Science.gov Websites</a></p> <p></p> <p></p> <p>SEASONAL <span class="hlt">CLIMATE</span> VARIABILITY, INCLUDING ENSO, <em>SOIL</em> MOISTURE, AND VARIOUS STATE-OF-THE-ART DYNAMICAL MODEL ACROSS PARTS OF THE EAST-CENTRAL CONUS CENTERED ON THE MISSISSIPPI RIVER. THIS IS DUE TO VERY HIGH <em>SOIL</em> TRENDS, NEGATIVE <em>SOIL</em> MOISTURE ANOMALIES, LAGGED ENSO REGRESSIONS, AND DYNAMICAL MODEL GUIDANCE ARE ALL</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3566174','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3566174"><span><span class="hlt">Climate</span>-Driven Range Extension of Amphistegina (Protista, Foraminiferida): Models of Current and <span class="hlt">Predicted</span> Future Ranges</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Langer, Martin R.; Weinmann, Anna E.; Lötters, Stefan; Bernhard, Joan M.; Rödder, Dennis</p> <p>2013-01-01</p> <p>Species-range expansions are a <span class="hlt">predicted</span> and realized consequence of global <span class="hlt">climate</span> change. <span class="hlt">Climate</span> warming and the poleward widening of the tropical belt have induced range shifts in a variety of marine and terrestrial species. Range expansions may have broad implications on native biota and ecosystem functioning as shifting species may perturb recipient communities. Larger symbiont-bearing foraminifera constitute ubiquitous and prominent components of shallow water ecosystems, and range shifts of these important protists are likely to trigger changes in ecosystem functioning. We have used historical and newly acquired occurrence records to compute current range shifts of Amphistegina spp., a larger symbiont-bearing foraminifera, along the eastern coastline of Africa and compare them to analogous range shifts currently observed in the Mediterranean Sea. The study provides new evidence that amphisteginid foraminifera are rapidly progressing southwestward, closely approaching Port Edward (South Africa) at 31°S. To project future species distributions, we applied a species distribution model (SDM) based on ecological niche constraints of current distribution ranges. Our model indicates that further warming is likely to cause a continued range extension, and <span class="hlt">predicts</span> dispersal along nearly the entire southeastern coast of Africa. The average rates of amphisteginid range shift were computed between 8 and 2.7 km year−1, and are projected to lead to a total southward range expansion of 267 km, or 2.4° latitude, in the year 2100. Our results corroborate findings from the fossil record that some larger symbiont-bearing foraminifera cope well with rising water temperatures and are beneficiaries of global <span class="hlt">climate</span> change. PMID:23405081</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/23405081','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/23405081"><span><span class="hlt">Climate</span>-driven range extension of Amphistegina (protista, foraminiferida): models of current and <span class="hlt">predicted</span> future ranges.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Langer, Martin R; Weinmann, Anna E; Lötters, Stefan; Bernhard, Joan M; Rödder, Dennis</p> <p>2013-01-01</p> <p>Species-range expansions are a <span class="hlt">predicted</span> and realized consequence of global <span class="hlt">climate</span> change. <span class="hlt">Climate</span> warming and the poleward widening of the tropical belt have induced range shifts in a variety of marine and terrestrial species. Range expansions may have broad implications on native biota and ecosystem functioning as shifting species may perturb recipient communities. Larger symbiont-bearing foraminifera constitute ubiquitous and prominent components of shallow water ecosystems, and range shifts of these important protists are likely to trigger changes in ecosystem functioning. We have used historical and newly acquired occurrence records to compute current range shifts of Amphistegina spp., a larger symbiont-bearing foraminifera, along the eastern coastline of Africa and compare them to analogous range shifts currently observed in the Mediterranean Sea. The study provides new evidence that amphisteginid foraminifera are rapidly progressing southwestward, closely approaching Port Edward (South Africa) at 31°S. To project future species distributions, we applied a species distribution model (SDM) based on ecological niche constraints of current distribution ranges. Our model indicates that further warming is likely to cause a continued range extension, and <span class="hlt">predicts</span> dispersal along nearly the entire southeastern coast of Africa. The average rates of amphisteginid range shift were computed between 8 and 2.7 km year(-1), and are projected to lead to a total southward range expansion of 267 km, or 2.4° latitude, in the year 2100. Our results corroborate findings from the fossil record that some larger symbiont-bearing foraminifera cope well with rising water temperatures and are beneficiaries of global <span class="hlt">climate</span> change.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20170004542','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20170004542"><span>The Future of Planetary <span class="hlt">Climate</span> Modeling and Weather <span class="hlt">Prediction</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Del Genio, A. D.; Domagal-Goldman, S. D.; Kiang, N. Y.; Kopparapu, R. K.; Schmidt, G. A.; Sohl, L. E.</p> <p>2017-01-01</p> <p>Modeling of planetary <span class="hlt">climate</span> and weather has followed the development of tools for studying Earth, with lags of a few years. Early Earth <span class="hlt">climate</span> studies were performed with 1-dimensionalradiative-convective models, which were soon fol-lowed by similar models for the <span class="hlt">climates</span> of Mars and Venus and eventually by similar models for exoplan-ets. 3-dimensional general circulation models (GCMs) became common in Earth science soon after and within several years were applied to the meteorology of Mars, but it was several decades before a GCM was used to simulate extrasolar planets. Recent trends in Earth weather and and <span class="hlt">climate</span> modeling serve as a useful guide to how modeling of Solar System and exoplanet weather and <span class="hlt">climate</span> will evolve in the coming decade.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4427447','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4427447"><span>Morbidity Rate <span class="hlt">Prediction</span> of Dengue Hemorrhagic Fever (DHF) Using the Support Vector Machine and the Aedes aegypti Infection Rate in Similar <span class="hlt">Climates</span> and Geographical Areas</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Kesorn, Kraisak; Ongruk, Phatsavee; Chompoosri, Jakkrawarn; Phumee, Atchara; Thavara, Usavadee; Tawatsin, Apiwat; Siriyasatien, Padet</p> <p>2015-01-01</p> <p>Background In the past few decades, several researchers have proposed highly accurate <span class="hlt">prediction</span> models that have typically relied on <span class="hlt">climate</span> parameters. However, <span class="hlt">climate</span> factors can be unreliable and can lower the effectiveness of <span class="hlt">prediction</span> when they are applied in locations where <span class="hlt">climate</span> factors do not differ significantly. The purpose of this study was to improve a dengue surveillance system in areas with similar <span class="hlt">climate</span> by exploiting the infection rate in the Aedes aegypti mosquito and using the support vector machine (SVM) technique for forecasting the dengue morbidity rate. Methods and Findings Areas with high incidence of dengue outbreaks in central Thailand were studied. The proposed framework consisted of the following three major parts: 1) data integration, 2) model construction, and 3) model evaluation. We discovered that the Ae. aegypti female and larvae mosquito infection rates were significantly positively associated with the morbidity rate. Thus, the increasing infection rate of female mosquitoes and larvae led to a higher number of dengue cases, and the <span class="hlt">prediction</span> performance increased when those predictors were integrated into a <span class="hlt">predictive</span> model. In this research, we applied the SVM with the radial basis function (RBF) kernel to forecast the high morbidity rate and take precautions to prevent the development of pervasive dengue epidemics. The experimental results showed that the introduced parameters significantly increased the <span class="hlt">prediction</span> accuracy to 88.37% when used on the test set data, and these parameters led to the highest performance compared to state-of-the-art forecasting models. Conclusions The infection rates of the Ae. aegypti female mosquitoes and larvae improved the morbidity rate forecasting efficiency better than the <span class="hlt">climate</span> parameters used in classical frameworks. We demonstrated that the SVM-R-based model has high generalization performance and obtained the highest <span class="hlt">prediction</span> performance compared to classical models as measured by</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.cpc.ncep.noaa.gov/products/predictions//multi_season/13_seasonal_outlooks/color/churchill.php','SCIGOVWS'); return false;" href="http://www.cpc.ncep.noaa.gov/products/predictions//multi_season/13_seasonal_outlooks/color/churchill.php"><span><span class="hlt">Climate</span> <span class="hlt">Prediction</span> Center - Seasonal Color Maps</span></a></p> <p><a target="_blank" href="http://www.science.gov/aboutsearch.html">Science.gov Websites</a></p> <p></p> <p></p> <p>HOME > Outlook Maps > Monthly to Seasonal Outlooks > Seasonal Outlooks > <em>Color</em> Monthly & ; Seasonal Outlooks Monthly & Seasonal <span class="hlt">Climate</span> Outlooks Banner Issued: 17 May 2018 [EXPERIMENTAL <em>TWO</em></p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018RSPTA.37670305M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018RSPTA.37670305M"><span><span class="hlt">Climate</span> risk index for Italy</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Mysiak, Jaroslav; Torresan, Silvia; Bosello, Francesco; Mistry, Malcolm; Amadio, Mattia; Marzi, Sepehr; Furlan, Elisa; Sperotto, Anna</p> <p>2018-06-01</p> <p>We describe a <span class="hlt">climate</span> risk index that has been developed to inform national <span class="hlt">climate</span> adaptation planning in Italy and that is further elaborated in this paper. The index supports national authorities in designing adaptation policies and plans, guides the initial problem formulation phase, and identifies <span class="hlt">administrative</span> areas with higher propensity to being adversely affected by <span class="hlt">climate</span> change. The index combines (i) <span class="hlt">climate</span> change-amplified hazards; (ii) high-resolution indicators of exposure of chosen economic, social, natural and built- or manufactured capital (MC) assets and (iii) vulnerability, which comprises both present sensitivity to <span class="hlt">climate</span>-induced hazards and adaptive capacity. We use standardized anomalies of selected extreme <span class="hlt">climate</span> indices derived from high-resolution regional <span class="hlt">climate</span> model simulations of the EURO-CORDEX initiative as proxies of <span class="hlt">climate</span> change-altered weather and <span class="hlt">climate</span>-related hazards. The exposure and sensitivity assessment is based on indicators of manufactured, natural, social and economic capital assets exposed to and adversely affected by <span class="hlt">climate</span>-related hazards. The MC refers to material goods or fixed assets which support the production process (e.g. industrial machines and buildings); Natural Capital comprises natural resources and processes (renewable and non-renewable) producing goods and services for well-being; Social Capital (SC) addressed factors at the individual (people's health, knowledge, skills) and collective (institutional) level (e.g. families, communities, organizations and schools); and Economic Capital (EC) includes owned and traded goods and services. The results of the <span class="hlt">climate</span> risk analysis are used to rank the subnational <span class="hlt">administrative</span> and statistical units according to the <span class="hlt">climate</span> risk challenges, and possibly for financial resource allocation for <span class="hlt">climate</span> adaptation. This article is part of the theme issue `Advances in risk assessment for <span class="hlt">climate</span> change adaptation policy'.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/23363925','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/23363925"><span>[<span class="hlt">Prediction</span> of heat-related mortality impacts under <span class="hlt">climate</span> change scenarios in Shanghai].</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Guo, Ya-fei; Li, Tian-tian; Cheng, Yan-li; Ge, Tan-xi; Chen, Chen; Liu, Fan</p> <p>2012-11-01</p> <p>To project the future impacts of <span class="hlt">climate</span> change on heat-related mortality in shanghai. The statistical downscaling techniques were applied to simulate the daily mean temperatures of Shanghai in the middle and farther future under the changing <span class="hlt">climate</span>. Based on the published exposure-reaction relationship of temperature and mortality in Shanghai, we projected the heat-related mortality in the middle and farther future under the circumstance of high speed increase of carbon e mission (A2) and low speed increase of carbon emission (B2). The data of 1961 to 1990 was used to establish the model, and the data of 1991 - 2001 was used to testify the model, and then the daily mean temperature from 2030 to 2059 and from 2070 to 2099 were simulated and the heat-related mortality was projected. The data resources were from U.S. National <span class="hlt">Climatic</span> Data Center (NCDC), U.S. National Centers for Environmental <span class="hlt">Prediction</span> Reanalysis Data in SDSM Website and UK Hadley Centre Coupled Model Data in SDSM Website. The explained variance and the standard error of the established model was separately 98.1% and 1.24°C. The R(2) value of the simulated trend line equaled to 0.978 in Shanghai, as testified by the model. Therefore, the temperature <span class="hlt">prediction</span> model simulated daily mean temperatures well. Under A2 scenario, the daily mean temperature in 2030 - 2059 and 2070 - 2099 were projected to be 17.9°C and 20.4°C, respectively, increasing by 1.1°C and 3.6°C when compared to baseline period (16.8°C). Under B2 scenario, the daily mean temperature in 2030 - 2059 and 2070 - 2099 were projected to be 17.8°C and 19.1°C, respectively, increasing by 1.0°C and 2.3°C when compared to baseline period (16.8°C). Under A2 scenario, annual average heat-related mortality were projected to be 516 cases and 1191 cases in 2030 - 2059 and 2070 - 2099, respectively, increasing 53.6% and 254.5% when compared with baseline period (336 cases). Under B2 scenario, annual average heat-related mortality were</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29120515','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29120515"><span>The effects of crew resource management on teamwork and safety <span class="hlt">climate</span> at Veterans Health <span class="hlt">Administration</span> facilities.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Schwartz, Miriam E; Welsh, Deborah E; Paull, Douglas E; Knowles, Regina S; DeLeeuw, Lori D; Hemphill, Robin R; Essen, Keith E; Sculli, Gary L</p> <p>2017-11-09</p> <p>Communication failure is a significant source of adverse events in health care and a leading root cause of sentinel events reported to the Joint Commission. The Veterans Health <span class="hlt">Administration</span> National Center for Patient Safety established Clinical Team Training (CTT) as a comprehensive program to enhance patient safety and to improve communication and teamwork among health care professionals. CTT is based on techniques used in aviation's Crew Resource Management (CRM) training. The aviation industry has reached a significant safety record in large part related to the culture change generated by CRM and sustained by its recurrent implementation. This article focuses on the improvement of communication, teamwork, and patient safety by utilizing a standardized, CRM-based, interprofessional, immersive training in diverse clinical areas. The Teamwork and Safety <span class="hlt">Climate</span> Questionnaire was used to evaluate safety <span class="hlt">climate</span> before and after CTT. The scores for all of the 27 questions on the questionnaire showed an increase from baseline to 12 months, and 11 of those increases were statistically significant. A recurrent training is recommended to maintain the positive outcomes. CTT enhances patient safety and reduces risk of patient harm by improving teamwork and facilitating clear, concise, specific and timely communication among health care professionals. © 2017 American Society for Healthcare Risk Management of the American Hospital Association.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20130014807','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20130014807"><span>Assessment of the APCC Coupled MME Suite in <span class="hlt">Predicting</span> the Distinctive <span class="hlt">Climate</span> Impacts of Two Flavors of ENSO during Boreal Winter</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Jeong, Hye-In; Lee, Doo Young; Karumuri, Ashok; Ahn, Joong-Bae; Lee, June-Yi; Luo, Jing-Jia; Schemm, Jae-Kyung E.; Hendon, Harry H.; Braganza, Karl; Ham, Yoo-Geun</p> <p>2012-01-01</p> <p>Forecast skill of the APEC <span class="hlt">Climate</span> Center (APCC) Multi-Model Ensemble (MME) seasonal forecast system in <span class="hlt">predicting</span> two main types of El Nino-Southern Oscillation (ENSO), namely canonical (or cold tongue) and Modoki ENSO, and their regional <span class="hlt">climate</span> impacts is assessed for boreal winter. The APCC MME is constructed by simple composite of ensemble forecasts from five independent coupled ocean-atmosphere <span class="hlt">climate</span> models. Based on a hindcast set targeting boreal winter <span class="hlt">prediction</span> for the period 19822004, we show that the MME can <span class="hlt">predict</span> and discern the important differences in the patterns of tropical Pacific sea surface temperature anomaly between the canonical and Modoki ENSO one and four month ahead. Importantly, the four month lead MME beats the persistent forecast. The MME reasonably <span class="hlt">predicts</span> the distinct impacts of the canonical ENSO, including the strong winter monsoon rainfall over East Asia, the below normal rainfall and above normal temperature over Australia, the anomalously wet conditions across the south and cold conditions over the whole area of USA, and the anomalously dry conditions over South America. However, there are some limitations in capturing its regional impacts, especially, over Australasia and tropical South America at a lead time of one and four months. Nonetheless, forecast skills for rainfall and temperature over East Asia and North America during ENSO Modoki are comparable to or slightly higher than those during canonical ENSO events.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/17015341','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/17015341"><span>Sexual selection <span class="hlt">predicts</span> advancement of avian spring migration in response to <span class="hlt">climate</span> change.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Spottiswoode, Claire N; Tøttrup, Anders P; Coppack, Timothy</p> <p>2006-12-22</p> <p>Global warming has led to earlier spring arrival of migratory birds, but the extent of this advancement varies greatly among species, and it remains uncertain to what degree these changes are phenotypically plastic responses or microevolutionary adaptations to changing environmental conditions. We suggest that sexual selection could help to understand this variation, since early spring arrival of males is favoured by female choice. <span class="hlt">Climate</span> change could weaken the strength of natural selection opposing sexual selection for early migration, which would <span class="hlt">predict</span> greatest advancement in species with stronger female choice. We test this hypothesis comparatively by investigating the degree of long-term change in spring passage at two ringing stations in northern Europe in relation to a synthetic estimate of the strength of female choice, composed of degree of extra-pair paternity, relative testes size and degree of sexually dichromatic plumage colouration. We found that species with a stronger index of sexual selection have indeed advanced their date of spring passage to a greater extent. This relationship was stronger for the changes in the median passage date of the whole population than for changes in the timing of first-arriving individuals, suggesting that selection has not only acted on protandrous males. These results suggest that sexual selection may have an impact on the responses of organisms to <span class="hlt">climate</span> change, and knowledge of a species' mating system might help to inform attempts at <span class="hlt">predicting</span> these.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012AGUFMGC43E1073L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012AGUFMGC43E1073L"><span>Good Models Gone Bad: Quantifying and <span class="hlt">Predicting</span> Parameter-Induced <span class="hlt">Climate</span> Model Simulation Failures</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Lucas, D. D.; Klein, R.; Tannahill, J.; Brandon, S.; Covey, C. C.; Domyancic, D.; Ivanova, D. P.</p> <p>2012-12-01</p> <p>Simulations using IPCC-class <span class="hlt">climate</span> models are subject to fail or crash for a variety of reasons. Statistical analysis of the failures can yield useful insights to better understand and improve the models. During the course of uncertainty quantification (UQ) ensemble simulations to assess the effects of ocean model parameter uncertainties on <span class="hlt">climate</span> simulations, we experienced a series of simulation failures of the Parallel Ocean Program (POP2). About 8.5% of our POP2 runs failed for numerical reasons at certain combinations of parameter values. We apply support vector machine (SVM) classification from the fields of pattern recognition and machine learning to quantify and <span class="hlt">predict</span> the probability of failure as a function of the values of 18 POP2 parameters. The SVM classifiers readily <span class="hlt">predict</span> POP2 failures in an independent validation ensemble, and are subsequently used to determine the causes of the failures via a global sensitivity analysis. Four parameters related to ocean mixing and viscosity are identified as the major sources of POP2 failures. Our method can be used to improve the robustness of complex scientific models to parameter perturbations and to better steer UQ ensembles. This work was performed under the auspices of the U.S. Department of Energy by Lawrence Livermore National Laboratory under Contract DE-AC52-07NA27344 and was funded by the Uncertainty Quantification Strategic Initiative Laboratory Directed Research and Development Project at LLNL under project tracking code 10-SI-013 (UCRL LLNL-ABS-569112).</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_21");'>21</a></li> <li><a href="#" onclick='return showDiv("page_22");'>22</a></li> <li class="active"><span>23</span></li> <li><a href="#" onclick='return showDiv("page_24");'>24</a></li> <li><a href="#" onclick='return showDiv("page_25");'>25</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_23 --> <div id="page_24" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_21");'>21</a></li> <li><a href="#" onclick='return showDiv("page_22");'>22</a></li> <li><a href="#" onclick='return showDiv("page_23");'>23</a></li> <li class="active"><span>24</span></li> <li><a href="#" onclick='return showDiv("page_25");'>25</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="461"> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/27667778','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/27667778"><span>Can we <span class="hlt">predict</span> ectotherm responses to <span class="hlt">climate</span> change using thermal performance curves and body temperatures?</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Sinclair, Brent J; Marshall, Katie E; Sewell, Mary A; Levesque, Danielle L; Willett, Christopher S; Slotsbo, Stine; Dong, Yunwei; Harley, Christopher D G; Marshall, David J; Helmuth, Brian S; Huey, Raymond B</p> <p>2016-11-01</p> <p>Thermal performance curves (TPCs), which quantify how an ectotherm's body temperature (T b ) affects its performance or fitness, are often used in an attempt to <span class="hlt">predict</span> organismal responses to <span class="hlt">climate</span> change. Here, we examine the key - but often biologically unreasonable - assumptions underlying this approach; for example, that physiology and thermal regimes are invariant over ontogeny, space and time, and also that TPCs are independent of previously experienced T b. We show how a critical consideration of these assumptions can lead to biologically useful hypotheses and experimental designs. For example, rather than assuming that TPCs are fixed during ontogeny, one can measure TPCs for each major life stage and incorporate these into stage-specific ecological models to reveal the life stage most likely to be vulnerable to <span class="hlt">climate</span> change. Our overall goal is to explicitly examine the assumptions underlying the integration of TPCs with T b , to develop a framework within which empiricists can place their work within these limitations, and to facilitate the application of thermal physiology to understanding the biological implications of <span class="hlt">climate</span> change. © 2016 John Wiley & Sons Ltd/CNRS.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3752767','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3752767"><span><span class="hlt">Climate</span> and Non-<span class="hlt">Climate</span> Drivers of Dengue Epidemics in Southern Coastal Ecuador</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Stewart-Ibarra, Anna M.; Lowe, Rachel</p> <p>2013-01-01</p> <p>We report a statistical mixed model for assessing the importance of <span class="hlt">climate</span> and non-<span class="hlt">climate</span> drivers of interannual variability in dengue fever in southern coastal Ecuador. Local <span class="hlt">climate</span> data and Pacific sea surface temperatures (Oceanic Niño Index [ONI]) were used to <span class="hlt">predict</span> dengue standardized morbidity ratios (SMRs; 1995–2010). Unobserved confounding factors were accounted for using non-structured yearly random effects. We found that ONI, rainfall, and minimum temperature were positively associated with dengue, with more cases of dengue during El Niño events. We assessed the influence of non-<span class="hlt">climatic</span> factors on dengue SMR using a subset of data (2001–2010) and found that the percent of households with Aedes aegypti immatures was also a significant predictor. Our results indicate that monitoring the <span class="hlt">climate</span> and non-<span class="hlt">climate</span> drivers identified in this study could provide some <span class="hlt">predictive</span> lead for forecasting dengue epidemics, showing the potential to develop a dengue early-warning system in this region. PMID:23478584</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29478885','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29478885"><span>Combining public participatory surveillance and occupancy modelling to <span class="hlt">predict</span> the distributional response of Ixodes scapularis to <span class="hlt">climate</span> change.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Lieske, David J; Lloyd, Vett K</p> <p>2018-03-01</p> <p>Ixodes scapularis, a known vector of Borrelia burgdorferi sensu stricto (Bbss), is undergoing range expansion in many parts of Canada. The province of New Brunswick, which borders jurisdictions with established populations of I. scapularis, constitutes a range expansion zone for this species. To better understand the current and potential future distribution of this tick under <span class="hlt">climate</span> change projections, this study applied occupancy modelling to distributional records of adult ticks that successfully overwintered, obtained through passive surveillance. This study indicates that I. scapularis occurs throughout the southern-most portion of the province, in close proximity to coastlines and major waterways. Milder winter conditions, as indicated by the number of degree days <0 °C, was determined to be a strong predictor of tick occurrence, as was, to a lesser degree, rising levels of annual precipitation, leading to a final model with a <span class="hlt">predictive</span> accuracy of 0.845 (range: 0.828-0.893). Both RCP 4.5 and RCP 8.5 <span class="hlt">climate</span> projections <span class="hlt">predict</span> that a significant proportion of the province (roughly a quarter to a third) will be highly suitable for I. scapularis by the 2080s. Comparison with cases of canine infection show good spatial agreement with baseline model <span class="hlt">predictions</span>, but the presence of canine Borrelia infections beyond the <span class="hlt">climate</span> envelope, defined by the highest probabilities of tick occurrence, suggest the presence of Bbss-carrying ticks distributed by long-range dispersal events. This research demonstrates that <span class="hlt">predictive</span> statistical modelling of multi-year surveillance information is an efficient way to identify areas where I. scapularis is most likely to occur, and can be used to guide subsequent active sampling efforts in order to better understand fine scale species distributional patterns. Copyright © 2018 The Authors. Published by Elsevier GmbH.. All rights reserved.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29396464','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29396464"><span><span class="hlt">Predicting</span> optimum crop designs using crop models and seasonal <span class="hlt">climate</span> forecasts.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Rodriguez, D; de Voil, P; Hudson, D; Brown, J N; Hayman, P; Marrou, H; Meinke, H</p> <p>2018-02-02</p> <p>Expected increases in food demand and the need to limit the incorporation of new lands into agriculture to curtail emissions, highlight the urgency to bridge productivity gaps, increase farmers profits and manage risks in dryland cropping. A way to bridge those gaps is to identify optimum combination of genetics (G), and agronomic managements (M) i.e. crop designs (GxM), for the prevailing and expected growing environment (E). Our understanding of crop stress physiology indicates that in hindsight, those optimum crop designs should be known, while the main problem is to <span class="hlt">predict</span> relevant attributes of the E, at the time of sowing, so that optimum GxM combinations could be informed. Here we test our capacity to inform that "hindsight", by linking a tested crop model (APSIM) with a skillful seasonal <span class="hlt">climate</span> forecasting system, to answer "What is the value of the skill in seasonal <span class="hlt">climate</span> forecasting, to inform crop designs?" Results showed that the GCM POAMA-2 was reliable and skillful, and that when linked with APSIM, optimum crop designs could be informed. We conclude that reliable and skillful GCMs that are easily interfaced with crop simulation models, can be used to inform optimum crop designs, increase farmers profits and reduce risks.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/23988300','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/23988300"><span><span class="hlt">Predicted</span> altitudinal shifts and reduced spatial distribution of Leishmania infantum vector species under <span class="hlt">climate</span> change scenarios in Colombia.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>González, Camila; Paz, Andrea; Ferro, Cristina</p> <p>2014-01-01</p> <p>Visceral leishmaniasis (VL) is caused by the trypanosomatid parasite Leishmania infantum (=Leishmania chagasi), and is epidemiologically relevant due to its wide geographic distribution, the number of annual cases reported and the increase in its co-infection with HIV. Two vector species have been incriminated in the Americas: Lutzomyia longipalpis and Lutzomyia evansi. In Colombia, L. longipalpis is distributed along the Magdalena River Valley while L. evansi is only found in the northern part of the Country. Regarding the epidemiology of the disease, in Colombia the incidence of VL has decreased over the last few years without any intervention being implemented. Additionally, changes in transmission cycles have been reported with urban transmission occurring in the Caribbean Coast. In Europe and North America <span class="hlt">climate</span> change seems to be driving a latitudinal shift of leishmaniasis transmission. Here, we explored the spatial distribution of the two known vector species of L. infantum in Colombia and projected its future distribution into <span class="hlt">climate</span> change scenarios to establish the expansion potential of the disease. An updated database including L. longipalpis and L. evansi collection records from Colombia was compiled. Ecological niche models were performed for each species using the Maxent software and 13 Worldclim bioclimatic coverages. Projections were made for the pessimistic CSIRO A2 scenario, which <span class="hlt">predicts</span> the higher increase in temperature due to non-emission reduction, and the optimistic Hadley B2 Scenario <span class="hlt">predicting</span> the minimum increase in temperature. The database contained 23 records for L. evansi and 39 records for L. longipalpis, distributed along the Magdalena River Valley and the Caribbean Coast, where the potential distribution areas of both species were also <span class="hlt">predicted</span> by Maxent. <span class="hlt">Climate</span> change projections showed a general overall reduction in the spatial distribution of the two vector species, promoting a shift in altitudinal distribution for L</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4027327','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4027327"><span>Generating temporal model using <span class="hlt">climate</span> variables for the <span class="hlt">prediction</span> of dengue cases in Subang Jaya, Malaysia</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Dom, Nazri Che; Hassan, A Abu; Latif, Z Abd; Ismail, Rodziah</p> <p>2013-01-01</p> <p>Objective To develop a forecasting model for the incidence of dengue cases in Subang Jaya using time series analysis. Methods The model was performed using the Autoregressive Integrated Moving Average (ARIMA) based on data collected from 2005 to 2010. The fitted model was then used to <span class="hlt">predict</span> dengue incidence for the year 2010 by extrapolating dengue patterns using three different approaches (i.e. 52, 13 and 4 weeks ahead). Finally cross correlation between dengue incidence and <span class="hlt">climate</span> variable was computed over a range of lags in order to identify significant variables to be included as external regressor. Results The result of this study revealed that the ARIMA (2,0,0) (0,0,1)52 model developed, closely described the trends of dengue incidence and confirmed the existence of dengue fever cases in Subang Jaya for the year 2005 to 2010. The <span class="hlt">prediction</span> per period of 4 weeks ahead for ARIMA (2,0,0)(0,0,1)52 was found to be best fit and consistent with the observed dengue incidence based on the training data from 2005 to 2010 (Root Mean Square Error=0.61). The <span class="hlt">predictive</span> power of ARIMA (2,0,0) (0,0,1)52 is enhanced by the inclusion of <span class="hlt">climate</span> variables as external regressor to forecast the dengue cases for the year 2010. Conclusions The ARIMA model with weekly variation is a useful tool for disease control and prevention program as it is able to effectively <span class="hlt">predict</span> the number of dengue cases in Malaysia.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3297386','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3297386"><span><span class="hlt">Predicting</span> ecosystem shifts requires new approaches that integrate the effects of <span class="hlt">climate</span> change across entire systems</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Russell, Bayden D.; Harley, Christopher D. G.; Wernberg, Thomas; Mieszkowska, Nova; Widdicombe, Stephen; Hall-Spencer, Jason M.; Connell, Sean D.</p> <p>2012-01-01</p> <p>Most studies that forecast the ecological consequences of <span class="hlt">climate</span> change target a single species and a single life stage. Depending on <span class="hlt">climatic</span> impacts on other life stages and on interacting species, however, the results from simple experiments may not translate into accurate <span class="hlt">predictions</span> of future ecological change. Research needs to move beyond simple experimental studies and environmental envelope projections for single species towards identifying where ecosystem change is likely to occur and the drivers for this change. For this to happen, we advocate research directions that (i) identify the critical species within the target ecosystem, and the life stage(s) most susceptible to changing conditions and (ii) the key interactions between these species and components of their broader ecosystem. A combined approach using macroecology, experimentally derived data and modelling that incorporates energy budgets in life cycle models may identify critical abiotic conditions that disproportionately alter important ecological processes under forecasted <span class="hlt">climates</span>. PMID:21900317</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2010GeoRL..3711809B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2010GeoRL..3711809B"><span>Northern Hemisphere <span class="hlt">climate</span> trends in reanalysis and forecast model <span class="hlt">predictions</span>: The 500 hPa annual means</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Bordi, I.; Fraedrich, K.; Sutera, A.</p> <p>2010-06-01</p> <p>The lead time dependent <span class="hlt">climates</span> of the ECMWF weather <span class="hlt">prediction</span> model, initialized with ERA-40 reanalysis, are analysed using 44 years of day-1 to day-10 forecasts of the northern hemispheric 500-hPa geopotential height fields. The study addresses the question whether short-term tendencies have an impact on long-term trends. Comparing <span class="hlt">climate</span> trends of ERA-40 with those of the forecasts, it seems that the forecast model rapidly loses the memory of initial conditions creating its own <span class="hlt">climate</span>. All forecast trends show a high degree of consistency. Comparison results suggest that: (i) Only centers characterized by an upward trend are statistical significant when increasing the lead time. (ii) In midilatitudes an upward trend larger than the one observed in the reanalysis characterizes the forecasts, while in the tropics there is a good agreement. (iii) The downward trend in reanalysis at high latitudes characterizes also the day-1 forecast which, however, increasing lead time approaches zero.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.ars.usda.gov/research/publications/publication/?seqNo115=332993','TEKTRAN'); return false;" href="http://www.ars.usda.gov/research/publications/publication/?seqNo115=332993"><span>Does an understanding of ecosystems responses to rainfall pulses improve <span class="hlt">predictions</span> of responses of drylands to <span class="hlt">climate</span> change?</span></a></p> <p><a target="_blank" href="https://www.ars.usda.gov/research/publications/find-a-publication/">USDA-ARS?s Scientific Manuscript database</a></p> <p></p> <p></p> <p>Drylands will experience more intense and frequent droughts and floods. Ten-year field experiments manipulating the amount and variability of precipitation suggest that we cannot <span class="hlt">predict</span> responses of drylands to <span class="hlt">climate</span> change based on pulse experimentation. Long-term drought experiments showed no e...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015AGUFMPA13A2193G','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015AGUFMPA13A2193G"><span>Using NMME in Region-Specific Operational Seasonal <span class="hlt">Climate</span> Forecasts</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Gronewold, A.; Bolinger, R. A.; Fry, L. M.; Kompoltowicz, K.</p> <p>2015-12-01</p> <p>The National Oceanic and Atmospheric <span class="hlt">Administration</span>'s <span class="hlt">Climate</span> <span class="hlt">Prediction</span> Center (NOAA/CPC) provides access to a suite of real-time monthly <span class="hlt">climate</span> forecasts that comprise the North American Multi-Model Ensemble (NMME) in an attempt to meet increasing demands for monthly to seasonal <span class="hlt">climate</span> <span class="hlt">prediction</span>. While the graphical map forecasts of the NMME are informative, there is a need to provide decision-makers with probabilistic forecasts specific to their region of interest. Here, we demonstrate the potential application of the NMME to address regional <span class="hlt">climate</span> projection needs by developing new forecasts of temperature and precipitation for the North American Great Lakes, the largest system of lakes on Earth. Regional opertional water budget forecasts rely on these outlooks to initiate monthly forecasts not only of the water budget, but of monthly lake water levels as well. More specifically, we present an alternative for improving existing operational protocols that currently involve a relatively time-consuming and subjective procedure based on interpreting the maps of the NMME. In addition, all forecasts are currently presented in the NMME in a probabilistic format, with equal weighting given to each member of the ensemble. In our new evolution of this product, we provide historical context for the forecasts by superimposing them (in an on-line graphical user interface) with the historical range of observations. Implementation of this new tool has already led to noticeable advantages in regional water budget forecasting, and has the potential to be transferred to other regional decision-making authorities as well.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012AGUFMIN41A1467H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012AGUFMIN41A1467H"><span>Enhancement of Local <span class="hlt">Climate</span> Analysis Tool</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Horsfall, F. M.; Timofeyeva, M. M.; Dutton, J.</p> <p>2012-12-01</p> <p>The National Oceanographic and Atmospheric <span class="hlt">Administration</span> (NOAA) National Weather Service (NWS) will enhance its Local <span class="hlt">Climate</span> Analysis Tool (LCAT) to incorporate specific capabilities to meet the needs of various users including energy, health, and other communities. LCAT is an online interactive tool that provides quick and easy access to <span class="hlt">climate</span> data and allows users to conduct analyses at the local level such as time series analysis, trend analysis, compositing, correlation and regression techniques, with others to be incorporated as needed. LCAT uses principles of Artificial Intelligence in connecting human and computer perceptions on application of data and scientific techniques in multiprocessing simultaneous users' tasks. Future development includes expanding the type of data currently imported by LCAT (historical data at stations and <span class="hlt">climate</span> divisions) to gridded reanalysis and General Circulation Model (GCM) data, which are available on global grids and thus will allow for <span class="hlt">climate</span> studies to be conducted at international locations. We will describe ongoing activities to incorporate NOAA <span class="hlt">Climate</span> Forecast System (CFS) reanalysis data (CFSR), NOAA model output data, including output from the National Multi Model Ensemble <span class="hlt">Prediction</span> System (NMME) and longer term projection models, and plans to integrate LCAT into the Earth System Grid Federation (ESGF) and its protocols for accessing model output and observational data to ensure there is no redundancy in development of tools that facilitate scientific advancements and use of <span class="hlt">climate</span> model information in applications. Validation and inter-comparison of forecast models will be included as part of the enhancement to LCAT. To ensure sustained development, we will investigate options for open sourcing LCAT development, in particular, through the University Corporation for Atmospheric Research (UCAR).</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014ClDy...42.1425M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014ClDy...42.1425M"><span>Global seasonal <span class="hlt">climate</span> <span class="hlt">predictability</span> in a two tiered forecast system: part I: boreal summer and fall seasons</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Misra, Vasubandhu; Li, H.; Wu, Z.; DiNapoli, S.</p> <p>2014-03-01</p> <p>This paper shows demonstrable improvement in the global seasonal <span class="hlt">climate</span> <span class="hlt">predictability</span> of boreal summer (at zero lead) and fall (at one season lead) seasonal mean precipitation and surface temperature from a two-tiered seasonal hindcast forced with forecasted SST relative to two other contemporary operational coupled ocean-atmosphere <span class="hlt">climate</span> models. The results from an extensive set of seasonal hindcasts are analyzed to come to this conclusion. This improvement is attributed to: (1) The multi-model bias corrected SST used to force the atmospheric model. (2) The global atmospheric model which is run at a relatively high resolution of 50 km grid resolution compared to the two other coupled ocean-atmosphere models. (3) The physics of the atmospheric model, especially that related to the convective parameterization scheme. The results of the seasonal hindcast are analyzed for both deterministic and probabilistic skill. The probabilistic skill analysis shows that significant forecast skill can be harvested from these seasonal hindcasts relative to the deterministic skill analysis. The paper concludes that the coupled ocean-atmosphere seasonal hindcasts have reached a reasonable fidelity to exploit their SST anomaly forecasts to force such relatively higher resolution two tier <span class="hlt">prediction</span> experiments to glean further boreal summer and fall seasonal <span class="hlt">prediction</span> skill.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015GMD.....8.3947E','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015GMD.....8.3947E"><span>A global empirical system for probabilistic seasonal <span class="hlt">climate</span> <span class="hlt">prediction</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Eden, J. M.; van Oldenborgh, G. J.; Hawkins, E.; Suckling, E. B.</p> <p>2015-12-01</p> <p>Preparing for episodes with risks of anomalous weather a month to a year ahead is an important challenge for governments, non-governmental organisations, and private companies and is dependent on the availability of reliable forecasts. The majority of operational seasonal forecasts are made using process-based dynamical models, which are complex, computationally challenging and prone to biases. Empirical forecast approaches built on statistical models to represent physical processes offer an alternative to dynamical systems and can provide either a benchmark for comparison or independent supplementary forecasts. Here, we present a simple empirical system based on multiple linear regression for producing probabilistic forecasts of seasonal surface air temperature and precipitation across the globe. The global CO2-equivalent concentration is taken as the primary predictor; subsequent predictors, including large-scale modes of variability in the <span class="hlt">climate</span> system and local-scale information, are selected on the basis of their physical relationship with the predictand. The focus given to the <span class="hlt">climate</span> change signal as a source of skill and the probabilistic nature of the forecasts produced constitute a novel approach to global empirical <span class="hlt">prediction</span>. Hindcasts for the period 1961-2013 are validated against observations using deterministic (correlation of seasonal means) and probabilistic (continuous rank probability skill scores) metrics. Good skill is found in many regions, particularly for surface air temperature and most notably in much of Europe during the spring and summer seasons. For precipitation, skill is generally limited to regions with known El Niño-Southern Oscillation (ENSO) teleconnections. The system is used in a quasi-operational framework to generate empirical seasonal forecasts on a monthly basis.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2007AdSpR..40..907T','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2007AdSpR..40..907T"><span>Understanding the origin of the solar cyclic activity for an improved earth <span class="hlt">climate</span> <span class="hlt">prediction</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Turck-Chièze, Sylvaine; Lambert, Pascal</p> <p></p> <p>This review is dedicated to the processes which could explain the origin of the great extrema of the solar activity. We would like to reach a more suitable estimate and <span class="hlt">prediction</span> of the temporal solar variability and its real impact on the Earth <span class="hlt">climatic</span> models. The development of this new field is stimulated by the SoHO helioseismic measurements and by some recent solar modelling improvement which aims to describe the dynamical processes from the core to the surface. We first recall assumptions on the potential different solar variabilities. Then, we introduce stellar seismology and summarize the main SOHO results which are relevant for this field. Finally we mention the dynamical processes which are presently introduced in new solar models. We believe that the knowledge of two important elements: (1) the magnetic field interplay between the radiative zone and the convective zone and (2) the role of the gravity waves, would allow to understand the origin of the grand minima and maxima observed during the last millennium. Complementary observables like acoustic and gravity modes, radius and spectral irradiance from far UV to visible in parallel to the development of 1D-2D-3D simulations will improve this field. PICARD, SDO, DynaMICCS are key projects for a <span class="hlt">prediction</span> of the next century variability. Some helioseismic indicators constitute the first necessary information to properly describe the Sun-Earth <span class="hlt">climatic</span> connection.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29712797','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29712797"><span><span class="hlt">Climate</span> risk index for Italy.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Mysiak, Jaroslav; Torresan, Silvia; Bosello, Francesco; Mistry, Malcolm; Amadio, Mattia; Marzi, Sepehr; Furlan, Elisa; Sperotto, Anna</p> <p>2018-06-13</p> <p>We describe a <span class="hlt">climate</span> risk index that has been developed to inform national <span class="hlt">climate</span> adaptation planning in Italy and that is further elaborated in this paper. The index supports national authorities in designing adaptation policies and plans, guides the initial problem formulation phase, and identifies <span class="hlt">administrative</span> areas with higher propensity to being adversely affected by <span class="hlt">climate</span> change. The index combines (i) <span class="hlt">climate</span> change-amplified hazards; (ii) high-resolution indicators of exposure of chosen economic, social, natural and built- or manufactured capital (MC) assets and (iii) vulnerability, which comprises both present sensitivity to <span class="hlt">climate</span>-induced hazards and adaptive capacity. We use standardized anomalies of selected extreme <span class="hlt">climate</span> indices derived from high-resolution regional <span class="hlt">climate</span> model simulations of the EURO-CORDEX initiative as proxies of <span class="hlt">climate</span> change-altered weather and <span class="hlt">climate</span>-related hazards. The exposure and sensitivity assessment is based on indicators of manufactured, natural, social and economic capital assets exposed to and adversely affected by <span class="hlt">climate</span>-related hazards. The MC refers to material goods or fixed assets which support the production process (e.g. industrial machines and buildings); Natural Capital comprises natural resources and processes (renewable and non-renewable) producing goods and services for well-being; Social Capital (SC) addressed factors at the individual (people's health, knowledge, skills) and collective (institutional) level (e.g. families, communities, organizations and schools); and Economic Capital (EC) includes owned and traded goods and services. The results of the <span class="hlt">climate</span> risk analysis are used to rank the subnational <span class="hlt">administrative</span> and statistical units according to the <span class="hlt">climate</span> risk challenges, and possibly for financial resource allocation for <span class="hlt">climate</span> adaptation.This article is part of the theme issue 'Advances in risk assessment for <span class="hlt">climate</span> change adaptation policy'. © 2018 The Authors.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5938637','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5938637"><span><span class="hlt">Climate</span> risk index for Italy</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Torresan, Silvia; Bosello, Francesco; Mistry, Malcolm; Amadio, Mattia; Marzi, Sepehr; Furlan, Elisa; Sperotto, Anna</p> <p>2018-01-01</p> <p>We describe a <span class="hlt">climate</span> risk index that has been developed to inform national <span class="hlt">climate</span> adaptation planning in Italy and that is further elaborated in this paper. The index supports national authorities in designing adaptation policies and plans, guides the initial problem formulation phase, and identifies <span class="hlt">administrative</span> areas with higher propensity to being adversely affected by <span class="hlt">climate</span> change. The index combines (i) <span class="hlt">climate</span> change-amplified hazards; (ii) high-resolution indicators of exposure of chosen economic, social, natural and built- or manufactured capital (MC) assets and (iii) vulnerability, which comprises both present sensitivity to <span class="hlt">climate</span>-induced hazards and adaptive capacity. We use standardized anomalies of selected extreme <span class="hlt">climate</span> indices derived from high-resolution regional <span class="hlt">climate</span> model simulations of the EURO-CORDEX initiative as proxies of <span class="hlt">climate</span> change-altered weather and <span class="hlt">climate</span>-related hazards. The exposure and sensitivity assessment is based on indicators of manufactured, natural, social and economic capital assets exposed to and adversely affected by <span class="hlt">climate</span>-related hazards. The MC refers to material goods or fixed assets which support the production process (e.g. industrial machines and buildings); Natural Capital comprises natural resources and processes (renewable and non-renewable) producing goods and services for well-being; Social Capital (SC) addressed factors at the individual (people's health, knowledge, skills) and collective (institutional) level (e.g. families, communities, organizations and schools); and Economic Capital (EC) includes owned and traded goods and services. The results of the <span class="hlt">climate</span> risk analysis are used to rank the subnational <span class="hlt">administrative</span> and statistical units according to the <span class="hlt">climate</span> risk challenges, and possibly for financial resource allocation for <span class="hlt">climate</span> adaptation. This article is part of the theme issue ‘Advances in risk assessment for <span class="hlt">climate</span> change adaptation policy’. PMID:29712797</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013AGUFM.B53E..05M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013AGUFM.B53E..05M"><span>Projected <span class="hlt">climate</span> change impacts and short term <span class="hlt">predictions</span> on staple crops in Sub-Saharan Africa</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Mereu, V.; Spano, D.; Gallo, A.; Carboni, G.</p> <p>2013-12-01</p> <p>. Multiple combinations of soils and <span class="hlt">climate</span> conditions, crop management and varieties were considered for the different Agro-Ecological Zones. The <span class="hlt">climate</span> impact was assessed using future <span class="hlt">climate</span> <span class="hlt">prediction</span>, statistically and/or dynamically downscaled, for specific areas. Direct and indirect effects of different CO2 concentrations projected for the future periods were separately explored to estimate their effects on crops. Several adaptation strategies (e.g., introduction of full irrigation, shift of the ordinary sowing/planting date, changes in the ordinary fertilization management) were also evaluated with the aim to reduce the negative impact of <span class="hlt">climate</span> change on crop production. The results of the study, analyzed at local, AEZ and country level, will be discussed.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=2981944','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=2981944"><span>Genetic and physiological bases for phenological responses to current and <span class="hlt">predicted</span> <span class="hlt">climates</span></span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Wilczek, A. M.; Burghardt, L. T.; Cobb, A. R.; Cooper, M. D.; Welch, S. M.; Schmitt, J.</p> <p>2010-01-01</p> <p>We are now reaching the stage at which specific genetic factors with known physiological effects can be tied directly and quantitatively to variation in phenology. With such a mechanistic understanding, scientists can better <span class="hlt">predict</span> phenological responses to novel seasonal <span class="hlt">climates</span>. Using the widespread model species Arabidopsis thaliana, we explore how variation in different genetic pathways can be linked to phenology and life-history variation across geographical regions and seasons. We show that the expression of phenological traits including flowering depends critically on the growth season, and we outline an integrated life-history approach to phenology in which the timing of later life-history events can be contingent on the environmental cues regulating earlier life stages. As flowering time in many plants is determined by the integration of multiple environmentally sensitive gene pathways, the novel combinations of important seasonal cues in projected future <span class="hlt">climates</span> will alter how phenology responds to variation in the flowering time gene network with important consequences for plant life history. We discuss how phenology models in other systems—both natural and agricultural—could employ a similar framework to explore the potential contribution of genetic variation to the physiological integration of cues determining phenology. PMID:20819808</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/19245378','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/19245378"><span><span class="hlt">Predicting</span> population survival under future <span class="hlt">climate</span> change: density dependence, drought and extraction in an insular bighorn sheep.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Colchero, Fernando; Medellin, Rodrigo A; Clark, James S; Lee, Raymond; Katul, Gabriel G</p> <p>2009-05-01</p> <p>1. Our understanding of the interplay between density dependence, <span class="hlt">climatic</span> perturbations, and conservation practices on the dynamics of small populations is still limited. This can result in uninformed strategies that put endangered populations at risk. Moreover, the data available for a large number of populations in such circumstances are sparse and mined with missing data. Under the current <span class="hlt">climate</span> change scenarios, it is essential to develop appropriate inferential methods that can make use of such data sets. 2. We studied a population of desert bighorn sheep introduced to Tiburon Island, Mexico in 1975 and subjected to irregular extractions for the last 10 years. The unique attributes of this population are absence of predation and disease, thereby permitting us to explore the combined effect of density dependence, environmental variability and extraction in a 'controlled setting.' Using a combination of nonlinear discrete models with long-term field data, we constructed three basic Bayesian state space models with increasing density dependence (DD), and the same three models with the addition of summer drought effects. 3. We subsequently used Monte Carlo simulations to evaluate the combined effect of drought, DD, and increasing extractions on the probability of population survival under two <span class="hlt">climate</span> change scenarios (based on the Intergovernmental Panel on <span class="hlt">Climate</span> Change <span class="hlt">predictions</span>): (i) increase in drought variability; and (ii) increase in mean drought severity. 4. The population grew from 16 individuals introduced in 1975 to close to 700 by 1993. Our results show that the population's growth was dominated by DD, with drought having a secondary but still relevant effect on its dynamics. 5. Our <span class="hlt">predictions</span> suggest that under <span class="hlt">climate</span> change scenario (i), extraction dominates the fate of the population, while for scenario (ii), an increase in mean drought affects the population's probability of survival in an equivalent magnitude as extractions. Thus, for the</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://rosap.ntl.bts.gov/view/dot/27118','DOTNTL'); return false;" href="https://rosap.ntl.bts.gov/view/dot/27118"><span><span class="hlt">Climate</span> change & extreme weather vulnerability assessment framework.</span></a></p> <p><a target="_blank" href="http://ntlsearch.bts.gov/tris/index.do">DOT National Transportation Integrated Search</a></p> <p></p> <p>2012-12-01</p> <p>The Federal Highway <span class="hlt">Administrations</span> (FHWAs) <span class="hlt">Climate</span> Change and Extreme Weather Vulnerability : Assessment Framework is a guide for transportation agencies interested in assessing their vulnerability : to <span class="hlt">climate</span> change and extreme weather event...</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_21");'>21</a></li> <li><a href="#" onclick='return showDiv("page_22");'>22</a></li> <li><a href="#" onclick='return showDiv("page_23");'>23</a></li> <li class="active"><span>24</span></li> <li><a href="#" onclick='return showDiv("page_25");'>25</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_24 --> <div id="page_25" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_21");'>21</a></li> <li><a href="#" onclick='return showDiv("page_22");'>22</a></li> <li><a href="#" onclick='return showDiv("page_23");'>23</a></li> <li><a href="#" onclick='return showDiv("page_24");'>24</a></li> <li class="active"><span>25</span></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="481"> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/24078353','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/24078353"><span>Influence and <span class="hlt">predictive</span> capacity of <span class="hlt">climate</span> anomalies on daily to decadal extremes in canopy photosynthesis.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Desai, Ankur R</p> <p>2014-02-01</p> <p>Significant advances have been made over the past decades in capabilities to simulate diurnal and seasonal variation of leaf-level and canopy-scale photosynthesis in temperate and boreal forests. However, long-term <span class="hlt">prediction</span> of future forest productivity in a changing <span class="hlt">climate</span> may be more dependent on how <span class="hlt">climate</span> and biological anomalies influence extremes in interannual to decadal variability of canopy ecosystem carbon exchanges. These exchanges can differ markedly from leaf level responses, especially owing to the prevalence of long lags in nutrient and water cycling. Until recently, multiple long-term (10+ year) high temporal frequency (daily) observations of canopy exchange were not available to reliably assess this claim. An analysis of one of the longest running North American eddy covariance flux towers reveals that single <span class="hlt">climate</span> variables do not adequately explain carbon exchange anomalies beyond the seasonal timescale. Daily to weekly lagged anomalies of photosynthesis positively autocorrelate with daily photosynthesis. This effect suggests a negative feedback in photosynthetic response to <span class="hlt">climate</span> extremes, such as anomalies in evapotranspiration and maximum temperature. Moisture stress in the prior season did inhibit photosynthesis, but mechanisms are difficult to assess. A complex interplay of integrated and lagged productivity and moisture-limiting factors indicate a critical role of seasonal thresholds that limit growing season length and peak productivity. These results lead toward a new conceptual framework for improving earth system models with long-term flux tower observations.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2009EGUGA..11.3734S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2009EGUGA..11.3734S"><span><span class="hlt">Prediction</span> of future <span class="hlt">climate</span> change for the Blue Nile, using RCM nested in GCM</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Sayed, E.; Jeuland, M.; Aty, M.</p> <p>2009-04-01</p> <p>Although the Nile River Basin is rich in natural resources, it faces many challenges. Rainfall is highly variable across the region, on both seasonal and inter-annual scales. This variability makes the region vulnerable to droughts and floods. Many development projects involving Nile waters are currently underway, or being studied. These projects will lead to land-use patterns changes and water distribution and availability. It is thus important to assess the effects of a) these projects and b) evolving water resource management and policies, on regional hydrological processes. This paper seeks to establish a basis for evaluation of such impacts within the Blue Nile River sub-basin, using the RegCM3 Regional <span class="hlt">Climate</span> Model to simulate interactions between the land surface and <span class="hlt">climatic</span> processes. We first present results from application of this RCM model nested with downscaled outputs obtained from the ECHAM5/MPI-OM1 transient simulations for the 20th Century. We then investigate changes associated with mid-21st century emissions forcing of the SRES A1B scenario. The results obtained from the <span class="hlt">climate</span> model are then fed as inputs to the Nile Forecast System (NFS), a hydrologic distributed rainfall runoff model of the Nile Basin, The interaction between <span class="hlt">climatic</span> and hydrological processes on the land surface has been fully coupled. Rainfall patterns and evaporation rates have been generated using RegCM3, and the resulting runoff and Blue Nile streamflow patterns have been simulated using the NFS. This paper compares the results obtained from the RegCM3 <span class="hlt">climate</span> model with observational datasets for precipitation and temperature from the <span class="hlt">Climate</span> Research Unit (UK) and the NASA Goddard Space Flight Center GPCP (USA) for 1985-2000. The validity of the streamflow <span class="hlt">predictions</span> from the NFS is assessed using historical gauge records. Finally, we present results from modeling of the A1B emissions scenario of the IPCC for the years 2034-2055. Our results indicate that future</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012AGUFM.B41B0277W','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012AGUFM.B41B0277W"><span><span class="hlt">Predicting</span> fire activity in the US over the next 50 years using new IPCC <span class="hlt">climate</span> projections</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Wang, D.; Morton, D. C.; Collatz, G. J.</p> <p>2012-12-01</p> <p>Fire is an integral part of the Earth system with both direct and indirect effects on terrestrial ecosystems, the atmosphere, and human societies (Bowman et al. 2009). <span class="hlt">Climate</span> conditions regulate fire activities through a variety of ways, e.g., influencing the conditions for ignition and fire spread, changing vegetation growth and decay and thus the accumulation of fuels for combustion (Arora and Boer 2005). Our recent study disclosed the burned area (BA) in US is strongly correlated with potential evaporation (PE), a measurement of <span class="hlt">climatic</span> dryness derived from National Centers for Environmental <span class="hlt">Prediction</span> (NCEP) North American Regional Reanalysis (NARR) <span class="hlt">climate</span> data (Morton et al. 2012). The correlation varies spatially and temporally. With regard to fire of peak fire seasons, Northwestern US, Great Plains and Alaska have the strongest BA/PE relationship. Using the recently released the Global Fire Emissions Database (GFED) Version 3 (van der Werf et al. 2010), we showed increasing BA in the last decade in most of NCA regions. Longer time series of Monitoring Trends in Burn Severity (MTBS) (Eidenshink et al. 2007) data showed the increasing trends occurred in all NCA regions from 1984 to 2010. This relationship between BA and PE provides us the basis to <span class="hlt">predict</span> the future fire activities in the projected <span class="hlt">climate</span> conditions. In this study, we build spatially explicit predictors using the historic PE/BA relationship. PE from 2011 to 2060 is calculated from the Coupled Model Intercomparison Project Phase 5 (CMIP5) data and the historic PE/BA relationship is then used to estimate BA. This study examines the spatial pattern and temporal dynamics of the future US fires driven by new <span class="hlt">climate</span> <span class="hlt">predictions</span> for the next 50 years. Reference: Arora, V.K., & Boer, G.J. (2005). Fire as an interactive component of dynamic vegetation models. Journal of Geophysical Research-Biogeosciences, 110 Bowman, D.M.J.S., Balch, J.K., Artaxo, P., Bond, W.J., Carlson, J.M., Cochrane, M.A., D</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/28412400','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/28412400"><span><span class="hlt">Prediction</span> of Losartan-Active Carboxylic Acid Metabolite Exposure Following Losartan <span class="hlt">Administration</span> Using Static and Physiologically Based Pharmacokinetic Models.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Nguyen, Hoa Q; Lin, Jian; Kimoto, Emi; Callegari, Ernesto; Tse, Susanna; Obach, R Scott</p> <p>2017-09-01</p> <p>The aim of this study was to evaluate a strategy based on static and dynamic physiologically based pharmacokinetic (PBPK) modeling for the <span class="hlt">prediction</span> of metabolite and parent drug area under the time-concentration curve ratio (AUC m /AUC p ) and their PK profiles in humans using in vitro data when active transport processes are involved in disposition. The strategy was applied to losartan and its pharmacologically active metabolite carboxylosartan as test compounds. Hepatobiliary transport including transport-mediated uptake, canilicular and basolateral efflux, and metabolic clearance estimates were obtained from in vitro studies using human liver microsomes and sandwich-cultured hepatocytes. Human renal clearance of carboxylosartan was estimated from dog renal clearance using allometric scaling approach. All clearance mechanisms were mechanistically incorporated in a static model to <span class="hlt">predict</span> the relative exposure of carboxylosartan versus losartan (AUC m /AUC p ). The <span class="hlt">predicted</span> AUC m /AUC p were consistent with the observed data following intravenous and oral <span class="hlt">administration</span> of losartan. Moreover, the in vitro parameters were used as initial parameters in PBPK permeability-limited disposition models to <span class="hlt">predict</span> the concentration-time profiles for both parent and its active metabolite after oral <span class="hlt">administration</span> of losartan. The PBPK model was able to recover the plasma profiles of both losartan and carboxylosartan, further substantiating the validity of this approach. Copyright © 2017 American Pharmacists Association®. Published by Elsevier Inc. All rights reserved.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016NatCC...6.1110G','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016NatCC...6.1110G"><span>Phylogenetic approaches reveal biodiversity threats under <span class="hlt">climate</span> change</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>González-Orozco, Carlos E.; Pollock, Laura J.; Thornhill, Andrew H.; Mishler, Brent D.; Knerr, Nunzio; Laffan, Shawn W.; Miller, Joseph T.; Rosauer, Dan F.; Faith, Daniel P.; Nipperess, David A.; Kujala, Heini; Linke, Simon; Butt, Nathalie; Külheim, Carsten; Crisp, Michael D.; Gruber, Bernd</p> <p>2016-12-01</p> <p><span class="hlt">Predicting</span> the consequences of <span class="hlt">climate</span> change for biodiversity is critical to conservation efforts. Extensive range losses have been <span class="hlt">predicted</span> for thousands of individual species, but less is known about how <span class="hlt">climate</span> change might impact whole clades and landscape-scale patterns of biodiversity. Here, we show that <span class="hlt">climate</span> change scenarios imply significant changes in phylogenetic diversity and phylogenetic endemism at a continental scale in Australia using the hyper-diverse clade of eucalypts. We <span class="hlt">predict</span> that within the next 60 years the vast majority of species distributions (91%) across Australia will shrink in size (on average by 51%) and shift south on the basis of projected suitable <span class="hlt">climatic</span> space. Geographic areas currently with high phylogenetic diversity and endemism are <span class="hlt">predicted</span> to change substantially in future <span class="hlt">climate</span> scenarios. Approximately 90% of the current areas with concentrations of palaeo-endemism (that is, places with old evolutionary diversity) are <span class="hlt">predicted</span> to disappear or shift their location. These findings show that <span class="hlt">climate</span> change threatens whole clades of the phylogenetic tree, and that the outlined approach can be used to forecast areas of biodiversity losses and continental-scale impacts of <span class="hlt">climate</span> change.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/23451090','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/23451090"><span><span class="hlt">Climate</span> and pH <span class="hlt">predict</span> the potential range of the invasive apple snail (Pomacea insularum) in the southeastern United States.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Byers, James E; McDowell, William G; Dodd, Shelley R; Haynie, Rebecca S; Pintor, Lauren M; Wilde, Susan B</p> <p>2013-01-01</p> <p><span class="hlt">Predicting</span> the potential range of invasive species is essential for risk assessment, monitoring, and management, and it can also inform us about a species' overall potential invasiveness. However, modeling the distribution of invasive species that have not reached their equilibrium distribution can be problematic for many <span class="hlt">predictive</span> approaches. We apply the modeling approach of maximum entropy (MaxEnt) that is effective with incomplete, presence-only datasets to <span class="hlt">predict</span> the distribution of the invasive island apple snail, Pomacea insularum. This freshwater snail is native to South America and has been spreading in the USA over the last decade from its initial introductions in Texas and Florida. It has now been documented throughout eight southeastern states. The snail's extensive consumption of aquatic vegetation and ability to accumulate and transmit algal toxins through the food web heighten concerns about its spread. Our model shows that under current <span class="hlt">climate</span> conditions the snail should remain mostly confined to the coastal plain of the southeastern USA where it is limited by minimum temperature in the coldest month and precipitation in the warmest quarter. Furthermore, low pH waters (pH <5.5) are detrimental to the snail's survival and persistence. Of particular note are low-pH blackwater swamps, especially Okefenokee Swamp in southern Georgia (with a pH below 4 in many areas), which are <span class="hlt">predicted</span> to preclude the snail's establishment even though many of these areas are well matched <span class="hlt">climatically</span>. Our results elucidate the factors that affect the regional distribution of P. insularum, while simultaneously presenting a spatial basis for the <span class="hlt">prediction</span> of its future spread. Furthermore, the model for this species exemplifies that combining <span class="hlt">climatic</span> and habitat variables is a powerful way to model distributions of invasive species.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.emc.ncep.noaa.gov/gcwmb/ppl.php','SCIGOVWS'); return false;" href="http://www.emc.ncep.noaa.gov/gcwmb/ppl.php"><span>National Centers for Environmental <span class="hlt">Prediction</span></span></a></p> <p><a target="_blank" href="http://www.science.gov/aboutsearch.html">Science.gov Websites</a></p> <p></p> <p></p> <p><em>Modeling</em> Mesoscale <em>Modeling</em> Marine <em>Modeling</em> and <em>Analysis</em> Teams <span class="hlt">Climate</span> Data Assimilation Ensembles and Post Products People GLOBAL <span class="hlt">CLIMATE</span> & WEATHER <em>MODELING</em> Personnel Jordan Alpert Email Website Dave Behringer <span class="hlt">Prediction</span> Environmental <em>Modeling</em> Center NOAA Center for Weather and <span class="hlt">Climate</span> <span class="hlt">Prediction</span> (NCWCP) 5830</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19970003259','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19970003259"><span>Modeling <span class="hlt">Climate</span> Change in the Absence of <span class="hlt">Climate</span> Change Data. Editorial Comment</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Skiles, J. W.</p> <p>1995-01-01</p> <p>Practitioners of <span class="hlt">climate</span> change <span class="hlt">prediction</span> base many of their future <span class="hlt">climate</span> scenarios on General Circulation Models (GCM's), each model with differing assumptions and parameter requirements. For representing the atmosphere, GCM's typically contain equations for calculating motion of particles, thermodynamics and radiation, and continuity of water vapor. Hydrology and heat balance are usually included for continents, and sea ice and heat balance are included for oceans. The current issue of this journal contains a paper by Van Blarcum et al. (1995) that <span class="hlt">predicts</span> runoff from nine high-latitude rivers under a doubled CO2 atmosphere. The paper is important since river flow is an indicator variable for <span class="hlt">climate</span> change. The authors show that precipitation will increase under the imposed perturbations and that owing to higher temperatures earlier in the year that cause the snow pack to melt sooner, runoff will also increase. They base their simulations on output from a GCM coupled with an interesting water routing scheme they have devised. <span class="hlt">Climate</span> change models have been linked to other models to <span class="hlt">predict</span> deforestation.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/26619186','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/26619186"><span>Ecological Niche Modelling <span class="hlt">Predicts</span> Southward Expansion of Lutzomyia (Nyssomyia) flaviscutellata (Diptera: Psychodidae: Phlebotominae), Vector of Leishmania (Leishmania) amazonensis in South America, under <span class="hlt">Climate</span> Change.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Carvalho, Bruno M; Rangel, Elizabeth F; Ready, Paul D; Vale, Mariana M</p> <p>2015-01-01</p> <p>Vector borne diseases are susceptible to <span class="hlt">climate</span> change because distributions and densities of many vectors are <span class="hlt">climate</span> driven. The Amazon region is endemic for cutaneous leishmaniasis and is <span class="hlt">predicted</span> to be severely impacted by <span class="hlt">climate</span> change. Recent records suggest that the distributions of Lutzomyia (Nyssomyia) flaviscutellata and the parasite it transmits, Leishmania (Leishmania) amazonensis, are expanding southward, possibly due to <span class="hlt">climate</span> change, and sometimes associated with new human infection cases. We define the vector's <span class="hlt">climatic</span> niche and explore future projections under <span class="hlt">climate</span> change scenarios. Vector occurrence records were compiled from the literature, museum collections and Brazilian Health Departments. Six bioclimatic variables were used as predictors in six ecological niche model algorithms (BIOCLIM, DOMAIN, MaxEnt, GARP, logistic regression and Random Forest). Projections for 2050 used 17 general circulation models in two greenhouse gas representative concentration pathways: "stabilization" and "high increase". Ensemble models and consensus maps were produced by overlapping binary <span class="hlt">predictions</span>. Final model outputs showed good performance and significance. The use of species absence data substantially improved model performance. Currently, L. flaviscutellata is widely distributed in the Amazon region, with records in the Atlantic Forest and savannah regions of Central Brazil. Future projections indicate expansion of the <span class="hlt">climatically</span> suitable area for the vector in both scenarios, towards higher latitudes and elevations. L. flaviscutellata is likely to find increasingly suitable conditions for its expansion into areas where human population size and density are much larger than they are in its current locations. If environmental conditions change as <span class="hlt">predicted</span>, the range of the vector is likely to expand to southeastern and central-southern Brazil, eastern Paraguay and further into the Amazonian areas of Bolivia, Peru, Ecuador, Colombia and Venezuela</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4664266','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4664266"><span>Ecological Niche Modelling <span class="hlt">Predicts</span> Southward Expansion of Lutzomyia (Nyssomyia) flaviscutellata (Diptera: Psychodidae: Phlebotominae), Vector of Leishmania (Leishmania) amazonensis in South America, under <span class="hlt">Climate</span> Change</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Carvalho, Bruno M.; Ready, Paul D.</p> <p>2015-01-01</p> <p>Vector borne diseases are susceptible to <span class="hlt">climate</span> change because distributions and densities of many vectors are <span class="hlt">climate</span> driven. The Amazon region is endemic for cutaneous leishmaniasis and is <span class="hlt">predicted</span> to be severely impacted by <span class="hlt">climate</span> change. Recent records suggest that the distributions of Lutzomyia (Nyssomyia) flaviscutellata and the parasite it transmits, Leishmania (Leishmania) amazonensis, are expanding southward, possibly due to <span class="hlt">climate</span> change, and sometimes associated with new human infection cases. We define the vector’s <span class="hlt">climatic</span> niche and explore future projections under <span class="hlt">climate</span> change scenarios. Vector occurrence records were compiled from the literature, museum collections and Brazilian Health Departments. Six bioclimatic variables were used as predictors in six ecological niche model algorithms (BIOCLIM, DOMAIN, MaxEnt, GARP, logistic regression and Random Forest). Projections for 2050 used 17 general circulation models in two greenhouse gas representative concentration pathways: “stabilization” and “high increase”. Ensemble models and consensus maps were produced by overlapping binary <span class="hlt">predictions</span>. Final model outputs showed good performance and significance. The use of species absence data substantially improved model performance. Currently, L. flaviscutellata is widely distributed in the Amazon region, with records in the Atlantic Forest and savannah regions of Central Brazil. Future projections indicate expansion of the <span class="hlt">climatically</span> suitable area for the vector in both scenarios, towards higher latitudes and elevations. L. flaviscutellata is likely to find increasingly suitable conditions for its expansion into areas where human population size and density are much larger than they are in its current locations. If environmental conditions change as <span class="hlt">predicted</span>, the range of the vector is likely to expand to southeastern and central-southern Brazil, eastern Paraguay and further into the Amazonian areas of Bolivia, Peru, Ecuador, Colombia and</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.fs.usda.gov/treesearch/pubs/41185','TREESEARCH'); return false;" href="https://www.fs.usda.gov/treesearch/pubs/41185"><span>Modeling and <span class="hlt">predicting</span> vegetation response of western USA grasslands, shrublands, and deserts to <span class="hlt">climate</span> change (Chapter 1)</span></a></p> <p><a target="_blank" href="http://www.fs.usda.gov/treesearch/">Treesearch</a></p> <p>Megan M. Friggens; Marcus V. Warwell; Jeanne C. Chambers; Stanley G. Kitchen</p> <p>2012-01-01</p> <p>Experimental research and species distribution modeling <span class="hlt">predict</span> large changes in the distributions of species and vegetation types in the Interior West due to <span class="hlt">climate</span> change. Species’ responses will depend not only on their physiological tolerances but also on their phenology, establishment properties, biotic interactions, and capacity to evolve and migrate. Because...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/1998EOSTr..79Q.394S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/1998EOSTr..79Q.394S"><span><span class="hlt">Climate</span> Web sites</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Showstack, Randy</p> <p></p> <p>With the growing interest in extreme <span class="hlt">climate</span> and weather events, the National Oceanic and Atmospheric <span class="hlt">Administration</span> (NOAA) has set up a one-stop Web site. It includes data on tornadoes, hurricanes, and heavy rainfall, temperature extremes, global <span class="hlt">climate</span> change, satellite images, and El Niño and La Niña. The Web address is http://www.ncdc.noaa.gov.Another good <span class="hlt">climate</span> Web site is the La Niña Home Page. Set up by the Environmental and Societal Impacts Group of the National Center for Atmospheric Research, the site includes forecasts, data sources, impacts, and Internet links.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015JHyd..526..221P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015JHyd..526..221P"><span>Drought <span class="hlt">prediction</span> till 2100 under RCP 8.5 <span class="hlt">climate</span> change scenarios for Korea</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Park, Chang-Kyun; Byun, Hi-Ryong; Deo, Ravinesh; Lee, Bo-Ra</p> <p>2015-07-01</p> <p>An important step in mitigating the negative impacts of drought requires effective methodologies for <span class="hlt">predicting</span> the future events. This study utilises the daily Effective Drought Index (EDI) to precisely and quantitatively <span class="hlt">predict</span> future drought occurrences in Korea over the period 2014-2100. The EDI is computed from precipitation data generated by the regional <span class="hlt">climate</span> model (HadGEM3-RA) under the Representative Concentration Pathway (RCP 8.5) scenario. Using this data for 678 grid points (12.5 km interval) groups of cluster regions with similar <span class="hlt">climates</span>, the G1 (Northwest), G2 (Middle), G3 (Northeast) and G4 (Southern) regions, are constructed. Drought forecasting period is categorised into the early phase (EP, 2014-2040), middle phase (MP, 2041-2070) and latter phase (LP, 2071-2100). Future drought events are quantified and ranked according to the duration and intensity. Moreover, the occurrences of drought (when, where, how severe) within the clustered regions are represented as a spatial map over Korea. Based on the grid-point averages, the most severe future drought throughout the 87-year period are expected to occur in Namwon around 2039-2041 with peak intensity (minimum EDI) -3.54 and projected duration of 580 days. The most severe drought by cluster analysis is expected to occur in the G3 region with a mean intensity of -2.85 in 2027. Within the spatial area of investigation, 6.6 years of drought periodicity and a slight decrease in the peak intensity is noted. Finally a spatial-temporal drought map is constructed for all clusters and time-periods under consideration.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014AGUFM.H23N1070B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014AGUFM.H23N1070B"><span>Drought <span class="hlt">Prediction</span> till 2100 Under RCP 8.5 <span class="hlt">Climate</span> Change Scenarios for Korea</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Byun, H. R.; Park, C. K.; Deo, R. C.</p> <p>2014-12-01</p> <p>An important step in mitigating the negative impacts of drought requires effective methodologies for <span class="hlt">predicting</span> the future events. This study utilizes the daily Effective Drought Index (EDI) to precisely and quantitatively <span class="hlt">predict</span> future drought occurrences in Korea over the period 2014-2100. The EDI is computed from precipitation data generated by the regional <span class="hlt">climate</span> model (HadGEM3-RA) under the Representative Concentration Pathway (RCP 8.5) scenario. Using this data for 678 grid points (12.5 km interval) groups of cluster regions with similar <span class="hlt">climates</span>, the G1 (Northwest), G2 (Middle), G3 (Northeast) and G4 (Southern) regions, are constructed. Drought forecasting period is categorised into the early phase (EP, 2014-2040), middle phase (MP, 2041-2070) and latter phase (LP, 2071-2100). Future drought events are quantified and ranked according to the duration and intensity. Moreover, the occurrences of drought (when, where, how severe) within the clustered regions are represented as a spatial map over Korea. Based on the grid-point averages, the most severe future drought throughout the 87-year period are expected to occur in Namwon around 2039-2041 with peak intensity (minimum EDI) -3.54 and projected duration of 580 days. The most severe drought by cluster analysis is expected to occur in the G3 region with a mean intensity of -2.85 in 2027. Within the spatial area of investigation, 6 years of drought periodicity and a slight decrease in the peak intensity is noted. Finally a spatial-temporal drought map is constructed for all clusters and time-periods under consideration.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016EGUGA..1813114W','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016EGUGA..1813114W"><span>Assimilation of temperature and salinity profile data in the Norwegian <span class="hlt">Climate</span> <span class="hlt">Prediction</span> Model</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Wang, Yiguo; Counillon, Francois; Bertino, Laurent; Bethke, Ingo; Keenlyside, Noel</p> <p>2016-04-01</p> <p>Assimilating temperature and salinity profile data is promising to constrain the ocean component of Earth system models for the purpose of seasonal-to-dedacal <span class="hlt">climate</span> <span class="hlt">predictions</span>. However, assimilating temperature and salinity profiles that are measured in standard depth coordinate (z-coordinate) into isopycnic coordinate ocean models that are discretised by water densities is challenging. Prior studies (Thacker and Esenkov, 2002; Xie and Zhu, 2010) suggested that converting observations to the model coordinate (i.e. innovations in isopycnic coordinate) performs better than interpolating model state to observation coordinate (i.e. innovations in z-coordinate). This problem is revisited here with the Norwegian <span class="hlt">Climate</span> <span class="hlt">Prediction</span> Model, which applies the ensemble Kalman filter (EnKF) into the ocean isopycnic model (MICOM) of the Norwegian Earth System Model. We perform Observing System Simulation Experiments (OSSEs) to compare two schemes (the EnKF-z and EnKF-ρ). In OSSEs, the truth is set to the EN4 objective analyses and observations are perturbations of the truth with white noises. Unlike in previous studies, it is found that EnKF-z outperforms EnKF-ρ for different observed vertical resolution, inhomogeneous sampling (e.g. upper 1000 meter observations only), or lack of salinity measurements. That is mostly because the operator converting observations into isopycnic coordinate is strongly non-linear. We also study the horizontal localisation radius at certain arbitrary grid points. Finally, we perform the EnKF-z with the chosen localisation radius in a realistic framework with NorCPM over a 5-year analysis period. The analysis is validated by different independent datasets.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.dtic.mil/docs/citations/ADA228623','DTIC-ST'); return false;" href="http://www.dtic.mil/docs/citations/ADA228623"><span>Spatial and Temporal <span class="hlt">Climate</span> Variations Influencing Medium-Range Temperature <span class="hlt">Predictions</span> Over South-Central European Russia</span></a></p> <p><a target="_blank" href="http://www.dtic.mil/">DTIC Science & Technology</a></p> <p></p> <p>1990-05-01</p> <p>forecasting using an analog approach. J. of <span class="hlt">Climate</span>. 2, 594-607. Veigas , K.W. and Ostby. F.P., 1963: Application of a moving coordinate <span class="hlt">prediction</span> model...n 0 r4~ g-- u0=) en m% en ’n fn v"~~ ~ ~ v lA V V A - - -- ~ CU c~ cc~ o ~ ~ cc 9k* . . . * . 89 B-i14 fl - n 0 00 en~0 en 0 00 r- =a T 00oo r</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014AGUFMGC32A..02M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014AGUFMGC32A..02M"><span>Disease in a more variable and unpredictable <span class="hlt">climate</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>McMahon, T. A.; Raffel, T.; Rohr, J. R.; Halstead, N.; Venesky, M.; Romansic, J.</p> <p>2014-12-01</p> <p>Global <span class="hlt">climate</span> change is shifting the dynamics of infectious diseases of humans and wildlife with potential adverse consequences for disease control. Despite this, the role of global <span class="hlt">climate</span> change in the decline of biodiversity and the emergence of infectious diseases remains controversial. <span class="hlt">Climate</span> change is expected to increase <span class="hlt">climate</span> variability in addition to increasing mean temperatures, making <span class="hlt">climate</span> less <span class="hlt">predictable</span>. However, few empirical or theoretical studies have considered the effects of <span class="hlt">climate</span> variability or <span class="hlt">predictability</span> on disease, despite it being likely that hosts and parasites will have differential responses to <span class="hlt">climatic</span> shifts. Here we present a theoretical framework for how temperature variation and its <span class="hlt">predictability</span> influence disease risk by affecting host and parasite acclimation responses. Laboratory experiments and field data on disease-associated frog declines in Latin America support this framework and provide evidence that unpredictable temperature fluctuations, on both monthly and diurnal timescales, decrease frog resistance to the pathogenic chytrid fungus Batrachochytrium dendrobatidis (Bd). Furthermore, the pattern of temperature-dependent growth of the fungus on frogs was inconsistent with the pattern of Bd growth in culture, emphasizing the importance of accounting for the host-parasite interaction when <span class="hlt">predicting</span> <span class="hlt">climate</span>-dependent disease dynamics. Consistent with our laboratory experiments, increased regional temperature variability associated with global El Niño <span class="hlt">climatic</span> events was the best predictor of widespread amphibian losses in the genus Atelopus. Thus, incorporating the effects of small-scale temporal variability in <span class="hlt">climate</span> can greatly improve our ability to <span class="hlt">predict</span> the effects of <span class="hlt">climate</span> change on disease.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29498787','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29498787"><span><span class="hlt">Climate</span> change likely to reduce orchid bee abundance even in <span class="hlt">climatic</span> suitable sites.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Faleiro, Frederico Valtuille; Nemésio, André; Loyola, Rafael</p> <p>2018-06-01</p> <p>Studies have tested whether model <span class="hlt">predictions</span> based on species' occurrence can <span class="hlt">predict</span> the spatial pattern of population abundance. The relationship between <span class="hlt">predicted</span> environmental suitability and population abundance varies in shape, strength and <span class="hlt">predictive</span> power. However, little attention has been paid to the congruence in <span class="hlt">predictions</span> of different models fed with occurrence or abundance data, in particular when comparing metrics of <span class="hlt">climate</span> change impact. Here, we used the ecological niche modeling fit with presence-absence and abundance data of orchid bees to <span class="hlt">predict</span> the effect of <span class="hlt">climate</span> change on species and assembly level distribution patterns. In addition, we assessed whether <span class="hlt">predictions</span> of presence-absence models can be used as a proxy to abundance patterns. We obtained georeferenced abundance data of orchid bees (Hymenoptera: Apidae: Euglossina) in the Brazilian Atlantic Forest. Sampling method consisted in attracting male orchid bees to baits of at least five different aromatic compounds and collecting the individuals with entomological nets or bait traps. We limited abundance data to those obtained by similar standard sampling protocol to avoid bias in abundance estimation. We used boosted regression trees to model ecological niches and project them into six <span class="hlt">climate</span> models and two Representative Concentration Pathways. We found that models based on species occurrences worked as a proxy for changes in population abundance when the output of the models were continuous; results were very different when outputs were discretized to binary <span class="hlt">predictions</span>. We found an overall trend of diminishing abundance in the future, but a clear retention of <span class="hlt">climatically</span> suitable sites too. Furthermore, geographic distance to gained <span class="hlt">climatic</span> suitable areas can be very short, although it embraces great variation. Changes in species richness and turnover would be concentrated in western and southern Atlantic Forest. Our findings offer support to the ongoing debate of suitability</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017ClDy...48.3283L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017ClDy...48.3283L"><span>MJO <span class="hlt">prediction</span> using the sub-seasonal to seasonal forecast model of Beijing <span class="hlt">Climate</span> Center</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Liu, Xiangwen; Wu, Tongwen; Yang, Song; Li, Tim; Jie, Weihua; Zhang, Li; Wang, Zaizhi; Liang, Xiaoyun; Li, Qiaoping; Cheng, Yanjie; Ren, Hongli; Fang, Yongjie; Nie, Suping</p> <p>2017-05-01</p> <p>By conducting several sets of hindcast experiments using the Beijing <span class="hlt">Climate</span> Center <span class="hlt">Climate</span> System Model, which participates in the Sub-seasonal to Seasonal (S2S) <span class="hlt">Prediction</span> Project, we systematically evaluate the model's capability in forecasting MJO and its main deficiencies. In the original S2S hindcast set, MJO forecast skill is about 16 days. Such a skill shows significant seasonal-to-interannual variations. It is found that the model-dependent MJO forecast skill is more correlated with the Indian Ocean Dipole (IOD) than with the El Niño-Southern Oscillation. The highest skill is achieved in autumn when the IOD attains its maturity. Extended skill is found when the IOD is in its positive phase. MJO forecast skill's close association with the IOD is partially due to the quickly strengthening relationship between MJO amplitude and IOD intensity as lead time increases to about 15 days, beyond which a rapid weakening of the relationship is shown. This relationship transition may cause the forecast skill to decrease quickly with lead time, and is related to the unrealistic amplitude and phase evolutions of <span class="hlt">predicted</span> MJO over or near the equatorial Indian Ocean during anomalous IOD phases, suggesting a possible influence of exaggerated IOD variability in the model. The results imply that the upper limit of intraseasonal <span class="hlt">predictability</span> is modulated by large-scale external forcing background state in the tropical Indian Ocean. Two additional sets of hindcast experiments with improved atmosphere and ocean initial conditions (referred to as S2S_IEXP1 and S2S_IEXP2, respectively) are carried out, and the results show that the overall MJO forecast skill is increased to 21-22 days. It is found that the optimization of initial sea surface temperature condition largely accounts for the increase of the overall MJO forecast skill, even though the improved initial atmosphere conditions also play a role. For the DYNAMO/CINDY field campaign period, the forecast skill increases</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016EGUGA..18.1340V','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016EGUGA..18.1340V"><span>Improving <span class="hlt">Predictions</span> and Management of Hydrological Extremes through <span class="hlt">Climate</span> Services</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>van den Hurk, Bart; Wijngaard, Janet; Pappenberger, Florian; Bouwer, Laurens; Weerts, Albrecht; Buontempo, Carlo; Doescher, Ralf; Manez, Maria; Ramos, Maria-Helena; Hananel, Cedric; Ercin, Ertug; Hunink, Johannes; Klein, Bastian; Pouget, Laurent; Ward, Philip</p> <p>2016-04-01</p> <p>The EU Roadmap on <span class="hlt">Climate</span> Services can be seen as a result of convergence between the society's call for "actionable research", and the <span class="hlt">climate</span> research community providing tailored data, information and knowledge. However, although weather and <span class="hlt">climate</span> have clearly distinct definitions, a strong link between weather and <span class="hlt">climate</span> services exists that is not explored extensively. Stakeholders being interviewed in the context of the Roadmap consider <span class="hlt">climate</span> as a far distant long term feature that is difficult to consider in present-day decision taking, which is dominated by daily experience with handling extreme events. It is argued that this experience is a rich source of inspiration to increase society's resilience to an unknown future. A newly started European research project, IMPREX, is built on the notion that "experience in managing current day weather extremes is the best learning school to anticipate consequences of future <span class="hlt">climate</span>". This paper illustrates possible ways to increase the link between information and services addressing weather and <span class="hlt">climate</span> time scales by discussing the underlying concepts of IMPREX and its expected outcome.</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_21");'>21</a></li> <li><a href="#" onclick='return showDiv("page_22");'>22</a></li> <li><a href="#" onclick='return showDiv("page_23");'>23</a></li> <li><a href="#" onclick='return showDiv("page_24");'>24</a></li> <li class="active"><span>25</span></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_25 --> <div class="footer-extlink text-muted" style="margin-bottom:1rem; text-align:center;">Some links on this page may take you to non-federal websites. 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