Sample records for key decadal change

  1. Decadal-scale changes in benthic foraminiferal assemblages off Key Largo, Florida

    USGS Publications Warehouse

    Cockey, E.; Hallock, P.; Lidz, B.H.

    1996-01-01

    Assemblages of foraminiferal tests in sediments sampled off Key Largo, Florida, in 1982, 1991, and 1992 were significantly different from assemblages sampled along the same traverses in 1959-1961. Larger, algal symbiont-bearing taxa, primarily Soritidae, comprised 50-80% of the specimens in samples collected in 1959-1961, whereas Miliolidae and Rotaliidae comprised 65-90% of the specimens collected in 1991 and 1992. Test abundance in 1992 samples ranged from 1.0 ?? 102/g to 8.1 ?? 104/g; tests were least abundant in coarse, well-sorted sediments. The lack of test-density data for the 1959-1961 samples prevented assessment of whether densities of smaller foraminifera have increased, symbiotic foraminifera have decreased, or both. Between 1982 and 1992, densities of smaller foraminifera appear to have increased. Although the causes of these changes in foraminiferal assemblages are not known, possible factors include nutrient loading inshore, winnowing and transport of tests by storm activity, and disease. The shift in dominance from long-lived, algal symbiont-bearing taxa in 1959-1961 to small, fast-growing, heterotrophic taxa in 1992 is consistent with predictions of community response to gradually increasing nutrient flux into south Florida's coastal waters. This study indicates that published accounts of foraminiferal assemblages from sediments collected 30 or more years ago can be valuable resources in efforts to determine if biotic changes have occurred in coastal ecosystems. This study also indicates that family-level identifications may be sufficient to detect decadal-scale changes in foraminiferal assemblages in reef-tract sediments.

  2. Inter-decadal change in potential predictability of the East Asian summer monsoon

    NASA Astrophysics Data System (ADS)

    Li, Jiao; Ding, Ruiqiang; Wu, Zhiwei; Zhong, Quanjia; Li, Baosheng; Li, Jianping

    2018-05-01

    The significant inter-decadal change in potential predictability of the East Asian summer monsoon (EASM) has been investigated using the signal-to-noise ratio method. The relatively low potential predictability appears from the early 1950s through the late 1970s and during the early 2000s, whereas the potential predictability is relatively high from the early 1980s through the late 1990s. The inter-decadal change in potential predictability of the EASM can be attributed mainly to variations in the external signal of the EASM. The latter is mostly caused by the El Niño-Southern Oscillation (ENSO) inter-decadal variability. As a major external signal of the EASM, the ENSO inter-decadal variability experiences phase transitions from negative to positive phases in the late 1970s, and to negative phases in the late 1990s. Additionally, ENSO is generally strong (weak) during a positive (negative) phase of the ENSO inter-decadal variability. The strong ENSO is expected to have a greater influence on the EASM, and vice versa. As a result, the potential predictability of the EASM tends to be high (low) during a positive (negative) phase of the ENSO inter-decadal variability. Furthermore, a suite of Pacific Pacemaker experiments suggests that the ENSO inter-decadal variability may be a key pacemaker of the inter-decadal change in potential predictability of the EASM.

  3. Hotspots and key periods of Greenland climate change during the past six decades

    NASA Astrophysics Data System (ADS)

    Abermann, J.; Hansen, B. U.; Lund, M.; Wacker, S.; Karami, M.; Cappelen, J.

    2016-12-01

    We investigate spatial gradients of air temperature and pressure and their trends in Greenland and compare these considering varying time window lengths since 1958. Both latitudinal temperature and pressure gradients are strongest during winter. An overall temperature increase of up to 0.15°C yr-1 has been observed for 1996-2014. The strongest warming happened during February at the West Coast (up to 0.6°C/yr), weaker but significant warming occurred during summer months (up to 0.3°C/yr) both in West and in East Greenland. Pressure trends are mainly negative if at all, but largely not significant. We discuss the relevance of these findings in an upscaling context of an extensive ecosystem monitoring program that was established in 1996 in Northeast Greenland (Zackenberg, www.g-e-m.dk). Improving the understanding of the interaction between the individual components of the ecosystem is its core idea, climate being the main driver. A series of studies highlights trends and variability for biotic and abiotic parameters for this period on a point scale. In order to expand trend assessments to a Greenland-wide scale, local climate trends in Zackenberg have to be put into a larger spatio-temporal context. We find that temperature trends in Northeast Greenland and the area around Zackenberg follow the general pattern but are smaller than the average in Greenland. Compared with other time windows in the past 6 decades, the study period 1996 - 2014 marks an above average warming trend; peak warming however occurred half a decade earlier. We therefore conclude that temperature-driven ecosystem changes observed in Zackenberg mark a lower boundary for environmental changes in Greenland.

  4. Geodetic mass balance of key glaciers across High Mountain Asia: a multi-decadal survey

    NASA Astrophysics Data System (ADS)

    Maurer, J. M.; Schaefer, J. M.; Rupper, S.; Corley, A. D.

    2016-12-01

    Glaciers in High Mountain Asia (HMA) supply seasonal meltwater for large populations, yet field observations are scarce and glacier sensitivities are poorly understood. In order to link complex atmospheric driving factors with heterogeneous glacier responses, detailed remote sensing observations of past changes in ice volume are needed. Here we compile a spatially and temporally extensive satellite-based remote sensing record to quantify multi-decadal geodetic mass balance of large mountain glaciers across key regions in HMA, including the Pamir, Himachal Pradesh, Uttarakhand, Nepal, Sikkim, and Bhutan regions. By utilizing declassified spy satellite imagery from the 1970's, ASTER scenes spanning 2000-present, and the ALOS global digital surface model, a methodologically homogenous assessment of regional and individual glacier responses to climate change over several decades is obtained. Although gaps due to low radiometric contrast result in significant uncertainties, the consistent approach across the HMA provides a useful comparison of relative geodetic changes between climatically diverse regions. Various patterns of ice loss are observed, including dynamic retreat of clean-ice glaciers and downwasting of debris-covered glaciers. In particular, we highlight the pronounced thinning and retreat of glaciers undergoing calving into proglacial lakes, which has important implications regarding ongoing and future ice loss of HMA glaciers.

  5. CLARREO Cornerstone of the Earth Observing System: Measuring Decadal Change Through Accurate Emitted Infrared and Reflected Solar Spectra and Radio Occultation

    NASA Technical Reports Server (NTRS)

    Sandford, Stephen P.

    2010-01-01

    The Climate Absolute Radiance and Refractivity Observatory (CLARREO) is one of four Tier 1 missions recommended by the recent NRC Decadal Survey report on Earth Science and Applications from Space (NRC, 2007). The CLARREO mission addresses the need to provide accurate, broadly acknowledged climate records that are used to enable validated long-term climate projections that become the foundation for informed decisions on mitigation and adaptation policies that address the effects of climate change on society. The CLARREO mission accomplishes this critical objective through rigorous SI traceable decadal change observations that are sensitive to many of the key uncertainties in climate radiative forcings, responses, and feedbacks that in turn drive uncertainty in current climate model projections. These same uncertainties also lead to uncertainty in attribution of climate change to anthropogenic forcing. For the first time CLARREO will make highly accurate, global, SI-traceable decadal change observations sensitive to the most critical, but least understood, climate forcings, responses, and feedbacks. The CLARREO breakthrough is to achieve the required levels of accuracy and traceability to SI standards for a set of observations sensitive to a wide range of key decadal change variables. The required accuracy levels are determined so that climate trend signals can be detected against a background of naturally occurring variability. Climate system natural variability therefore determines what level of accuracy is overkill, and what level is critical to obtain. In this sense, the CLARREO mission requirements are considered optimal from a science value perspective. The accuracy for decadal change traceability to SI standards includes uncertainties associated with instrument calibration, satellite orbit sampling, and analysis methods. Unlike most space missions, the CLARREO requirements are driven not by the instantaneous accuracy of the measurements, but by accuracy in

  6. Decadal changes in north-American tundra plant communities

    NASA Astrophysics Data System (ADS)

    Villarreal, S.; Johnson, D. R.; Webber, P.; Ebert-May, D.; Hollister, R. D.; Tweedie, C. E.

    2013-12-01

    Improving our understanding of how tundra vegetation responds to environmental change over decadal time scales is important. Tundra plants and ecosystems are well-recognized for their susceptibility to be impacted by climate warming; changes in land-atmosphere carbon, water, and energy balance in tundra landscapes have the potential to impact regional to global-scale climate, and relatively few studies examining change in tundra landscapes have spanned decadal time scales. The majority of our understanding of tundra vegetation responses to environmental change has been derived from studies along environmental gradients, experimental manipulations, and modeling. This study synthesizes the rescue and resampling of historic vegetation study sites established during the 1960's and 1970's at three arctic tundra locations (Baffin Island, Canada, Barrow, Alaska, and Atqasuk, Alaska), and one alpine tundra location (Niwot Ridge, Colorado). We conducted a meta-analysis to examine decadal changes in plant community composition, species richness, species evenness, and species diversity at all locations and for three broad soil moisture classes (dry, moist, wet). For all sites, except Baffin Island, change over the last decade was compared with long term change to determine if rates of change have altered over time. Change in plant community composition was most dramatic at Barrow and Baffin Island (P < 0.05), while less change was detected at Niwot Ridge (P < 0.10), and Atqasuk. Plant communities also changed for all soil moisture classes. The rate of change at Barrow and in moist soil classes appears to have quickened over the last decade. Rates of early plant successional change at Baffin Island appear to have quickened relative to rates documented in the mid 1960's. There were no changes in species richness at any of the locations, but there appears to be acceleration in the loss of species richness for dry and moist tundra. Species evenness increased at Atqasuk and in dry

  7. Decadal Changes in Global Ocean Chlorophyll

    NASA Technical Reports Server (NTRS)

    Gregg, Watson W.; Conkright, Margarita E.; Koblinsky, Chester J. (Technical Monitor)

    2001-01-01

    The global ocean chlorophyll archive produced by the Coastal Zone Color Scanner (CZCS) was revised using compatible algorithms with the Sea-viewing Wide Field-of-view Sensor (SeaWIFS), and both were blended with in situ data. This methodology permitted a quantitative comparison of decadal changes in global ocean chlorophyll from the CZCS (1979-1986) and SeaWiFS (Sep. 1997-Dec. 2000) records. Global seasonal means of ocean chlorophyll decreased over the two observational segments, by 8% in winter to 16% in autumn. Chlorophyll in the high latitudes was responsible for most of the decadal change. Conversely, chlorophyll concentrations in the low latitudes increased. The differences and similarities of the two data records provide evidence of how the Earth's climate may be changing and how ocean biota respond. Furthermore, the results have implications for the ocean carbon cycle.

  8. Collaborative Research: Improving Decadal Prediction of Arctic Climate Variability and Change Using a Regional Arctic

    DOE Office of Scientific and Technical Information (OSTI.GOV)

    Gutowski, William J.

    This project developed and applied a regional Arctic System model for enhanced decadal predictions. It built on successful research by four of the current PIs with support from the DOE Climate Change Prediction Program, which has resulted in the development of a fully coupled Regional Arctic Climate 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 climate 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 climate through polar amplification. However, a system-level understanding of critical arctic processes and feedbacks needs further development. Rapid climate 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 climate and to improve seasonal to decadal predictions. To do this the project has focused on variability and long-term change of energy and freshwater flows through the arctic climate system. The three foci of this research are

  9. The last decades and matrimonial changes.

    PubMed

    Trost, J

    1992-01-01

    This paper focuses on changes in fertility, marriage patterns, cohabitation, divorce, and separation in Western European countries over the past few decades. Major trends discussed include the decline in fertility and marriage rates and the increase in nonmarital cohabitation, divorce, and separation.

  10. A decade of changes in radiation protection.

    PubMed

    Moulder, J E

    1992-04-01

    Although radiation protection standards have changed remarkably little over the past decade, there have been changes in our understanding of radiation hazards that may affect the practice of radiation medicine over the next decade. With recognition of indoor radon exposure has come a new focus for public health concerns, because it is now clear that radon rather than medical exposure is the largest controllable source of radiation exposure to the general public. Continued follow-up of irradiated populations has led to an increase in our estimate of the cancer risk for high-dose exposures; this increased risk estimate is, in turn, leading to decreases in radiation exposure limits. Although our concern about the carcinogenic risk for radiation exposure has increased, our concern about genetic consequences has decreased, because no genetic effects have yet been observed in the offspring of atomic bomb survivors. Studies of atomic bomb survivors have also led to a change in the focus of concern over prenatal radiation exposure; the principle risk now appears to be mental retardation rather than childhood cancer.

  11. Decadal changes in South Pacific sea surface temperatures and the relationship to the Pacific decadal oscillation and upper ocean heat content

    NASA Astrophysics Data System (ADS)

    Linsley, Braddock K.; Wu, Henry C.; Dassié, Emilie P.; Schrag, Daniel P.

    2015-04-01

    Decadal changes in Pacific sea surface temperatures (SSTs) and upper ocean heat content (OHC) remain poorly understood. We present an annual average composite coral Sr/Ca-derived SST time series extending back to 1791 from Fiji, Tonga, and Rarotonga (FTR) in the Pacific Decadal Oscillation (PDO) sensitive region of the southwest Pacific. Decadal SST maxima between 1805 and 1830 Common Era (C.E.) indicate unexplained elevated SSTs near the end of the Little Ice Age. The mean period of decadal SST variability in this region has a period near 25 years. Decades of warmer (cooler) FTR SST co-occur with PDO negative (positive) phases since at least ~1930 C.E. and positively correlate with South Pacific OHC (0-700 m). FTR SST is also inversely correlated with decadal changes in equatorial Pacific SST as measured by coral Sr/Ca. Collectively, these results support the fluctuating trade wind-shallow meridional overturning cell mechanism for decadal modulation of Pacific SSTs and OHC.

  12. Pesticides in groundwater of the United States: decadal-scale changes, 1993-2011

    USGS Publications Warehouse

    Toccalino, Patricia L.; Gilliom, Robert J.; Lindsey, Bruce D.; Rupert, Michael G.

    2014-01-01

    The national occurrence of 83 pesticide compounds in groundwater of the United States and decadal-scale changes in concentrations for 35 compounds were assessed for the 20-year period from 1993–2011. Samples were collected from 1271 wells in 58 nationally distributed well networks. Networks consisted of shallow (mostly monitoring) wells in agricultural and urban land-use areas and deeper (mostly domestic and public supply) wells in major aquifers in mixed land-use areas. Wells were sampled once during 1993–2001 and once during 2002–2011. Pesticides were frequently detected (53% of all samples), but concentrations seldom exceeded human-health benchmarks (1.8% of all samples). The five most frequently detected pesticide compounds—atrazine, deethylatrazine, simazine, metolachlor, and prometon—each had statistically significant (p < 0.1) changes in concentrations between decades in one or more categories of well networks nationally aggregated by land use. For agricultural networks, concentrations of atrazine, metolachlor, and prometon decreased from the first decade to the second decade. For urban networks, deethylatrazine concentrations increased and prometon concentrations decreased. For major aquifers, concentrations of deethylatrazine and simazine increased. The directions of concentration changes for individual well networks generally were consistent with changes determined from nationally aggregated data. Altogether, 36 of the 58 individual well networks had statistically significant changes in concentrations of one or more pesticides between decades, with the majority of changes attributed to the five most frequently detected pesticide compounds. The magnitudes of median decadal-scale concentration changes were small—ranging from −0.09 to 0.03 µg/L—and were 35- to 230,000-fold less than human-health benchmarks.

  13. Juvenile recruitment in loggerhead sea turtles linked to decadal changes in ocean circulation.

    PubMed

    Ascani, François; Van Houtan, Kyle S; Di Lorenzo, Emanuele; Polovina, Jeffrey J; Jones, T Todd

    2016-11-01

    Given the threats of climate change, understanding the relationship of climate with long-term population dynamics is critical for wildlife conservation. Previous studies have linked decadal climate oscillations to indices of juvenile recruitment in loggerhead sea turtles (Caretta caretta), but without a clear understanding of mechanisms. Here, we explore the underlying processes that may explain these relationships. Using the eddy-resolving Ocean General Circulation Model for the Earth Simulator, we generate hatch-year trajectories for loggerhead turtles emanating from Japan over six decades (1950-2010). We find that the proximity of the high-velocity Kuroshio Current to the primary nesting areas in southern Japan is remarkably stable and that hatchling dispersal to oceanic habitats itself does not vary on decadal timescales. However, we observe a shift in latitudes of trajectories, consistent with the Pacific Decadal Oscillation (PDO). In a negative PDO phase, the Kuroshio Extension Current (KEC) is strong and acts as a physical barrier to the northward transport of neonates. As a result, hatch-year trajectories remain mostly below 35°N in the warm, unproductive region south of the Transition Zone Chlorophyll Front (TZCF). During a positive PDO phase, however, the KEC weakens facilitating the neonates to swim north of the TZCF into cooler and more productive waters. As a result, annual cohorts from negative PDO years may face a lack of resources, whereas cohorts from positive PDO years may find sufficient resources during their pivotal first year. These model outputs indicate that the ocean circulation dynamics, combined with navigational swimming behavior, may be a key factor in the observed decadal variability of sea turtle populations. © 2016 John Wiley & Sons Ltd.

  14. Searching for forcing signatures in decadal patterns of shoreline change

    NASA Astrophysics Data System (ADS)

    Burningham, H.; French, J.

    2016-12-01

    Analysis of shoreline position at spatial scales of the order 10 - 100 km and at a multi-decadal time-scale has the potential to reveal regional coherence (or lack of) in the primary controls on shoreline tendencies and trends. Such information is extremely valuable for the evaluation of climate forcing on coastal behaviour. Segmenting a coast into discrete behaviour units based on these types of analyses is often subjective, however, and in the context of pervasive human interventions and alongshore variability in ocean climate, determining the most important controls on shoreline dynamics can be challenging. Multivariate analyses provide one means to resolve common behaviours across shoreline position datasets, thereby underpinning a more objective evaluation of possible coupling between shorelines at different scales. In an analysis of the Suffolk coast (eastern England) we explore the use of multivariate statistics to understand and classify mesoscale coastal behaviour. Suffolk comprises a relatively linear shoreline that shifts from east-facing in the north to southeast-facing in the south. Although primarily formed of a beach foreshore backed by cliffs or shingle barrier, the shoreline is punctuated at 3 locations by narrow tidal inlets with offset entrances that imply a persistent north to south sediment transport direction. Tidal regime decreases south to north from mesotidal (3.6m STR) to microtidal (1.9m STR), and the bimodal wave climate (northeast and southwest modes) presents complex local-scale variability in nearshore conditions. Shorelines exhibit a range of decadal behaviours from rapid erosion (up to 4m/yr) to quasi-stability that cannot be directly explained by the spatial organisation of contemporary landforms or coastal defences. A multivariate statistical approach to shoreline change analysis helps to define the key modes of change and determine the most likely forcing factors.

  15. The Asian battery market—a decade of change

    NASA Astrophysics Data System (ADS)

    Eckfeld, S.; Manders, J. E.; Stevenson, M. W.

    The Asian battery industry will undergo significant change over the next decade as it adapts to the enormous economic and technological pressures of our rapidly changing world. Europe and North America in recent years have seen significant rationalisation in battery manufacturing capacity and ownership for a variety of reasons. Into the future, Asia will be no exception, but the rate and magnitude of change may conceivably be greater than that already experienced elsewhere. Rationalisation in battery manufacturing plants will occur as a result of the establishment of super plants to manufacture batteries in order to improve the economies of scale and to facilitate the heavy investment in new capital and equipment that will be required to supply the newer technology battery types. The impact of 42 V automotive systems and valve-regulated lead-acid (VRLA) batteries will be influential on this scenario. It is expected that China, Japan, South Korea, and Thailand will feature heavily in the future Asian battery scene at the expense of some established countries and producers. The current state of the battery industry in Asia, factors driving change in Asia, and the likely implications for those companies that are currently manufacturing batteries in Asia or considering a future role in Asia within the coming decade are examined in this paper.

  16. SUDEP revisited - a decade on: have circumstances changed?

    PubMed

    Beran, Roy G

    2015-04-01

    A paper, published a decade ago, endorsed doctors' right to avoid discussing Sudden Unexpected Death in Epilepsy (SUDEP). It did not negate discussion, advocating same where appropriate. This paper investigates the current situation to identify any changes. The tort of negligence includes a duty to discuss "material risks" and adhere to accepted practice. Within the last decade, "material risks" for SUDEP have not altered significantly and international practice discusses SUDEP with those patients who seek advice or in whom such discussion is designed to improve patient compliance. Doctors are unlikely to be found negligent for not discussing SUDEP, acknowledging a push encouraging same, despite it being contrary to routine practice in the US, Italy, UK and elsewhere. Doctors should continue to practice the "art of medicine", discuss SUDEP when warranted and with patients seeking such advice. They must warn about risks, such as bathing alone, avoiding accident and injuries and possibly SUDEP in non-compliant patients and also consider the impact of such discussion. With no 'material' changes in the last decade, doctors must recognise when to discuss SUDEP, with which patients and in what context, accepting it may have a negative psychosocial impact on family dynamics unless discussed in a culturally competent fashion, to avoid causing additional stress for families where accepting the diagnosis of epilepsy may already prove difficult. Having formed a therapeutic relationship with the patient, discussion of SUDEP should be considered within that context, acknowledging the "art of medicine" and the implications of such discussion, similar to the situation a decade ago. Copyright © 2015 British Epilepsy Association. Published by Elsevier Ltd. All rights reserved.

  17. Vegetation Change in Interior Alaska Over the Last Four Decades

    NASA Astrophysics Data System (ADS)

    Huhman, H.; Dewitz, J.; Cristobal, J.; Prakash, A.

    2017-12-01

    The Arctic has become a generally warmer place over the past decades leading to earlier snowmelt, permafrost degradation and changing plant communities. One area in particular, vegetation change, is responding relatively rapidly to climate change, impacting the surrounding environment with changes to forest fire regime, forest type, forest resiliency, habitat availability for subsistence flora and fauna, hydrology, among others. To quantify changes in vegetation in the interior Alaska boreal forest over the last four decades, this study uses the National Land Cover Database (NLCD) decision-tree based classification methods, using both C5 and ERDAS Imagine software, to classify Landsat Surface Reflectance Images into the following NLCD-consistent vegetation classes: planted, herbaceous, shrubland, and forest (deciduous, evergreen and mixed). The results of this process are a total of four vegetation cover maps, that are freely accessible to the public, one for each decade in the 1980's, 1990's, 2000's, and a current map for 2017. These maps focus on Fairbanks, Alaska and the surrounding area covering approximately 36,140 square miles. The maps are validated with over 4,000 ground truth points collected through organizations such as the Landfire Project and the Long Term Ecological Research Network, as well as vegetation and soil spectra collected from the study area concurrent with the Landsat satellite over-passes with a Spectral Evolution PSR+ 3500 spectro-radiometer (0.35 - 2.5 μm). We anticipate these maps to be viewed by a wide user-community and may aid in preparing the residents of Alaska for changes in their subsistence food sources and will contribute to the scientific community in understanding the variety of changes that can occur in response to changing vegetation.

  18. Missing pieces of the puzzle: understanding decadal variability of Sahel Rainfall

    NASA Astrophysics Data System (ADS)

    Vellinga, Michael; Roberts, Malcolm; Vidale, Pier-Luigi; Mizielinski, Matthew; Demory, Marie-Estelle; Schiemann, Reinhard; Strachan, Jane; Bain, Caroline

    2015-04-01

    The instrumental record shows that substantial decadal fluctuations affected Sahel rainfall from the West African monsoon throughout the 20th century. Climate models generally underestimate the magnitude of decadal Sahel rainfall changes compared to observations. This shows that the processes that control low-frequency Sahel rainfall change are misrepresented in most CMIP5-era climate models. Reliable climate information of future low-frequency rainfall changes thus remains elusive. Here we identify key processes that control the magnitude of the decadal rainfall recovery in the Sahel since the mid-1980s. We show its sensitivity to model resolution and physics in a suite of experiments with global HadGEM3 model configurations at resolutions between 130-25 km. The decadal rainfall trend increases with resolution and at 60-25 km falls within the observed range. Higher resolution models have stronger increases of moisture supply and of African Easterly wave activity. Easterly waves control the occurrence of strong organised rainfall events which carry most of the decadal trend. Weak rainfall events occur too frequently at all resolutions and at low resolution contribute substantially to the decadal trend. All of this behaviour is seen across CMIP5, including future scenarios. Additional simulations with a global 12km version of HadGEM3 show that treating convection explicitly dramatically improves the properties of Sahel rainfall systems. We conclude that interaction between convective scale and global scale processes is key to decadal rainfall changes in the Sahel. This work is distributed under the Creative Commons Attribution 3.0 Unported License together with an author copyright. This license does not conflict with the regulations of the Crown Copyright.Crown Copyright

  19. Interbasin effects of the Indian Ocean on Pacific decadal climate change

    NASA Astrophysics Data System (ADS)

    Mochizuki, Takashi; Kimoto, Masahide; Watanabe, Masahiro; Chikamoto, Yoshimitsu; Ishii, Masayoshi

    2016-07-01

    We demonstrate the significant impact of the Indian Ocean on the Pacific climate on decadal timescales by comparing two sets of data assimilation experiments (pacemaker experiments) conducted over recent decades. For the Indian Ocean of an atmosphere-ocean coupled global climate model, we assimilate ocean temperature and salinity anomalies defined as deviations from climatology or as anomalies with the area-averaged changes for the Indian Ocean subtracted. When decadal sea surface temperature (SST) trends are observed to be strong over the Indian Ocean, the equatorial thermocline uniformly deepens, and the model simulates the eastward tendencies of surface wind aloft. Surface winds strongly converge around the maritime continent, and the associated strengthening of the Walker circulation suppresses an increasing trend in the equatorial Pacific SST through ocean thermocline shoaling, similar to common changes associated with seasonal Indian Ocean warming.

  20. Changes in atmospheric aerosol loading retrieved from space based measurements during the past decade

    NASA Astrophysics Data System (ADS)

    Yoon, J.; Burrows, J. P.; Vountas, M.; von Hoyningen-Huene, W.; Chang, D. Y.; Richter, A.; Hilboll, A.

    2013-10-01

    Atmospheric aerosol, generated from natural and anthropogenic sources, plays a key role in regulating visibility, air quality, and acid deposition. It is directly linked to and impacts on human health. It also reflects and absorbs incoming solar radiation and thereby influences the climate change. The cooling by aerosols is now recognized to have partly masked the atmospheric warming from fossil fuel combustion emissions. The role and potential management of short-lived climate pollutants such as aerosol are currently a topic of much scientific and public debate. Our limited knowledge of atmospheric aerosol and its influence on the Earth's radiation balance has a significant impact on the accuracy and error of current predictions of the future global climate change. In the past decades, environmental legislation in industrialized countries has begun to limit the release of anthropogenic pollutants. In contrast, in Asia as a result of the recent rapid economic development, emissions from industry and traffic have increased dramatically. In this study, the temporal changes/trends of atmospheric aerosols, derived from the satellite instruments MODIS (on board Terra and Aqua), MISR (Terra), and SeaWiFS (OrbView-2) during the past decade, are investigated. Whilst the aerosol optical thickness, AOT, over Western Europe decreases (i.e. by up to about -40% from 2003 to 2008) and parts of North America, a statistically significant increase (about +34% in the same period) over East China is observed and attributed to both the increase in industrial output and the Asian desert dust.

  1. Atlantic-induced pan-tropical climate change over the past three decades

    NASA Astrophysics Data System (ADS)

    Li, Xichen; Xie, Shang-Ping; Gille, Sarah T.; Yoo, Changhyun

    2016-03-01

    During the past three decades, tropical sea surface temperature (SST) has shown dipole-like trends, with warming over the tropical Atlantic and Indo-western Pacific but cooling over the eastern Pacific. Competing hypotheses relate this cooling, identified as a driver of the global warming hiatus, to the warming trends in either the Atlantic or Indian Ocean. However, the mechanisms, the relative importance and the interactions between these teleconnections remain unclear. Using a state-of-the-art climate model, we show that the Atlantic plays a key role in initiating the tropical-wide teleconnection, and the Atlantic-induced anomalies contribute ~55-75% of the tropical SST and circulation changes during the satellite era. The Atlantic warming drives easterly wind anomalies over the Indo-western Pacific as Kelvin waves and westerly anomalies over the eastern Pacific as Rossby waves. The wind changes induce an Indo-western Pacific warming through the wind-evaporation-SST effect, and this warming intensifies the La Niña-type response in the tropical Pacific by enhancing the easterly trade winds and through the Bjerknes ocean dynamical processes. The teleconnection develops into a tropical-wide SST dipole pattern. This mechanism, supported by observations and a hierarchy of climate models, reveals that the tropical ocean basins are more tightly connected than previously thought.

  2. Four Decades of Change in Geographical Education in Finland

    ERIC Educational Resources Information Center

    Kaivola, Taina; Rikkinen, Hannele

    2007-01-01

    Geography teaching has been under constant change over the last decades. Innovations from research in geography and higher education have diffused in school practices in various ways. International trends have been applied to national contexts in co-operation among academics, administrators and school teachers depending on policies and educational…

  3. Decadal changes in tundra land cover on Yamal Peninsula, Northwest Siberia

    NASA Astrophysics Data System (ADS)

    Forbes, B. C.; Kumpula, T.; Macias-Fauria, M.

    2017-12-01

    The Yamal-Nenets Okrug in Russia has experienced significant changes in land use and climate in recent decades. Average year-round air temperatures have increased ca. 2°C since the 1970's, with much - but not all - of the warming taking place in winter. In association with ongoing summer warming, the annual growth of erect deciduous shrubs has been accelerating while growing season seasonality has diminished, characterized by shifts in the spatial patterns of key phenological parameters. We prepared LANDSAT-derived land cover classifications for 1988 and 2014 using change detection analysis, supported by extensive ground truthing bolstered with data from Very High-Resolution (VHR) imagery (e.g. Quickbird-2, Worldview-2/3). Research was conducted within summer reindeer pastures utilized by the Yarsalinksi sovhoz, whose animals are collectively owned, as well as many privately-owned herds. The area represents bioclimatic Subzone D of the Circumpolar Arctic Vegetation Map and covers about 8500 km2. This is a key subzone for several reasons: (1) it includes Bovanenkovo, the first and largest gas deposit on Yamal to be developed; (2) it is a zone of extremely active periglacial processes (e.g. active layer detachment slides, lake drainage and recent methane-mediated craters); and (3) it is characterized by steadily increasing growth of tall willow shrubs (Salix spp.), which comprise an important source of fodder by reindeer migrating through the area in summer. These results are unique as our dataset: (1) covers sizable inland regions lying entirely within the Russian tundra zone; (2) derives from extensive ground truthing; and (3) treats all plant taxonomic groups (vascular, bryophytes, lichens) at the plot scale. Here we present the first such classifications, based on LANDSAT images from 1988 and 2014. We identify 16 classes ranging from bare ground and drained lakes, anthropogenic disturbances, through several wetland types, to various dwarf and erect tundra shrub

  4. Decadal-timescale changes of the Atlantic overturning circulation and climate in a coupled climate model with a hybrid-coordinate ocean component

    NASA Astrophysics Data System (ADS)

    Persechino, A.; Marsh, R.; Sinha, B.; Megann, A. P.; Blaker, A. T.; New, A. L.

    2012-08-01

    A wide range of statistical tools is used to investigate the decadal variability of the Atlantic Meridional Overturning Circulation (AMOC) and associated key variables in a climate model (CHIME, Coupled Hadley-Isopycnic Model Experiment), which features a novel ocean component. CHIME is as similar as possible to the 3rd Hadley Centre Coupled Model (HadCM3) with the important exception that its ocean component is based on a hybrid vertical coordinate. Power spectral analysis reveals enhanced AMOC variability for periods in the range 15-30 years. Strong AMOC conditions are associated with: (1) a Sea Surface Temperature (SST) anomaly pattern reminiscent of the Atlantic Multi-decadal Oscillation (AMO) response, but associated with variations in a northern tropical-subtropical gradient; (2) a Surface Air Temperature anomaly pattern closely linked to SST; (3) a positive North Atlantic Oscillation (NAO)-like pattern; (4) a northward shift of the Intertropical Convergence Zone. The primary mode of AMOC variability is associated with decadal changes in the Labrador Sea and the Greenland Iceland Norwegian (GIN) Seas, in both cases linked to the tropical activity about 15 years earlier. These decadal changes are controlled by the low-frequency NAO that may be associated with a rapid atmospheric teleconnection from the tropics to the extratropics. Poleward advection of salinity anomalies in the mixed layer also leads to AMOC changes that are linked to processes in the Labrador Sea. A secondary mode of AMOC variability is associated with interannual changes in the Labrador and GIN Seas, through the impact of the NAO on local surface density.

  5. Seismic rate changes associated with seasonal, annual, and decadal changes in the cryosphere

    NASA Astrophysics Data System (ADS)

    Sauber, J. M.; Luthcke, S. B.; Hall, D. K.

    2012-12-01

    Near the Bering Glacier Global Fiducial Program (GFP) in southern Alaska large cryospheric fluctuations occur in a region of upper crustal faulting and folding associated with collision and accretion of the Yakutat terrane. In this study we report constraints on seasonal, annual and decadal cryospheric changes estimated over the last decade from field, aircraft and satellite measurements and we evaluate the influence of cryospheric changes on the background seismic rate. Multi-year images from the Bering Glacier GFP are available since mid-2003 to constrain changes in extent of the Bering Glacier and to discern feature changes in the glacial surface. Starting around the same time, satellite gravimetric measurements from the Gravity Recovery and Climate experiment (GRACE) commenced. Large spatial-scale mass change calculated from the GRACE mascon solution of Luthcke et al. [2012] indicate a general trend of annual ice mass loss for southern Alaska but with large, variable seasonal mass fluctuations. Since 2007 the station position of a continuous GPS site near Cape Yakataga (Alaska EarthScope PBO site, AB35) has been available as well. In addition to changes in the geodetic position due to tectonic motion, this GPS station shows large seasonal excursions in the detrended vertical and horizontal position components consistent with snow loading in the fall and winter and melt onset/mass decrease in the spring/summer. To better understand the timing of processes responsible for the onset of cryospheric mass loss documented in the GRACE data, we examined changes in the snow cover extent and the onset of melt in the spring. We calculated the elastic displacements of the solid Earth and theoretical earthquake failure criteria associated with these annual and seasonal ice and snow changes. Additionally, we compared the seismic rate (M>1.8) from a reference background time period against other time periods with variable ice or tectonic change characteristics to test the

  6. Decadal Changes in Global Ocean Annual Primary Production

    NASA Technical Reports Server (NTRS)

    Gregg, Watson; Conkright, Margarita E.; Behrenfeld, Michael J.; Ginoux, Paul; Casey, Nancy W.; Koblinsky, Chester J. (Technical Monitor)

    2002-01-01

    The Sea-viewing Wide Field-of-View Sensor (SeaWiFS) has produced the first multi-year time series of global ocean chlorophyll observations since the demise of the Coastal Zone Color Scanner (CZCS) in 1986. Global observations from 1997-present from SeaWiFS combined with observations from 1979-1986 from the CZCS should in principle provide an opportunity to observe decadal changes in global ocean annual primary production, since chlorophyll is the primary driver for estimates of primary production. However, incompatibilities between algorithms have so far precluded quantitative analysis. We have developed and applied compatible processing methods for the CZCS, using modern advances in atmospheric correction and consistent bio-optical algorithms to advance the CZCS archive to comparable quality with SeaWiFS. We applied blending methodologies, where in situ data observations are incorporated into the CZCS and SeaWiFS data records, to provide improvement of the residuals. These re-analyzed, blended data records provide maximum compatibility and permit, for the first time, a quantitative analysis of the changes in global ocean primary production in the early-to-mid 1980's and the present, using synoptic satellite observations. An intercomparison of the global and regional primary production from these blended satellite observations is important to understand global climate change and the effects on ocean biota. Photosynthesis by chlorophyll-containing phytoplankton is responsible for biotic uptake of carbon in the oceans and potentially ultimately from the atmosphere. Global ocean annual primary decreased from the CZCS record to SeaWiFS, by nearly 6% from the early 1980s to the present. Annual primary production in the high latitudes was responsible for most of the decadal change. Conversely, primary production in the low latitudes generally increased, with the exception of the tropical Pacific. The differences and similarities of the two data records provide evidence

  7. Demographic Changes and Literacy Development in a Decade. Working Paper Series.

    ERIC Educational Resources Information Center

    Reder, Stephen; Edmonston, Barry

    Anticipated demographic changes in the United States adult population in the decade between the National Adult Literacy Survey (NALS) of 1992 and the National Assessment of Adult Literacy (NAAL), which is scheduled for 2002, were reviewed. Next, the implications of those changes for the NALS and NAAL were analyzed. The analysis focused on births,…

  8. Three decades of Martian surface changes

    USGS Publications Warehouse

    Geissler, P.E.

    2005-01-01

    The surface of Mars has changed dramatically during the three decades spanned by spacecraft exploration. Comparisons of Mars Global Surveyor images with Viking and Mariner 9 pictures suggest that more than one third of Mars' surface area has brightened or darkened by at least 10%. Such albedo changes could produce significant effects on solar heating and the global circulation of winds across the planet. All of the major changes took place in areas of moderate to high thermal inertia and rock abundance, consistent with burial of rocky surfaces by thin dust layers deposited during dust storms and subsequent exposure of the rocky surfaces by aeolian erosion. Several distinct mechanisms contribute to aeolian erosion on Mars. Prevailing winds dominate erosion at low latitudes, producing diffuse albedo boundaries and elongated wind streaks generally oriented in the direction of southern summer winds. Dust devils darken the mid to high latitudes from 45 to 70 degrees during the summer seasons, forming irregular albedo patterns consisting of dark linear tracks. Dust storms produce regional albedo variations with distinct but irregular margins. Dark sand duties in southern high latitudes appear to be associated with regional darkening that displays diffuse albedo boundaries. No surface changes were observed to repeat regularly on an annual basis, but many of the changes took place in areas that alternate episodically between high- and low-albedo states as thin mantles of dust are deposited and later stripped off. Hence the face of Mars remains recognizable after a century of telescopic observations, in spite of the enormous extent of alteration that has taken place during the era of spacecraft exploration.

  9. Decadal-scale changes of nitrate in ground water of the United States, 1988-2004

    USGS Publications Warehouse

    Rupert, Michael G.

    2008-01-01

    This study evaluated decadal-scale changes of nitrate concentrations in groundwater samples collected by the USGS National Water-Quality Assessment Program from 495 wells in 24 well networks across the USA in predominantly agricultural areas. Each well network was sampled once during 1988-1995 and resampled once during 2000-2004. Statistical tests of decadal-scale changes of nitrate concentrations in water from all 495 wells combined indicate there is a significant increase in nitrate concentrations in the data set as a whole. Eight out of the 24 well networks, or about 33%, had significant changes of nitrate concentrations. Of the eight well networks with significant decadal-scale changes of nitrate, all except one, the Willamette Valley of Oregon, had increasing nitrate concentrations. Median nitrate concentrations of three of those eight well networks increased above the USEPA maximum contaminant level of 10 mg L-1. Nitrate in water from wells with reduced conditions had significantly smaller decadal-scale changes in nitrate concentrations than oxidized and mixed waters. A subset of wells had data on ground water recharge date; nitrate concentrations increased in response to the increase of N fertilizer use since about 1950. Determining ground water recharge dates is an important component of a ground water trends investigation because recharge dates provide a link between changes in ground water quality and changes in land-use practices. Copyright ?? 2008 by the American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America. All rights reserved.

  10. Collaborative Proposal: Improving Decadal Prediction of Arctic Climate Variability and Change Using a Regional Arctic System Model (RASM)

    DOE Office of Scientific and Technical Information (OSTI.GOV)

    Maslowski, Wieslaw

    This project aims to develop, apply and evaluate a regional Arctic System model (RASM) for enhanced decadal predictions. Its overarching goal is to advance understanding of the past and present states of arctic climate and to facilitate improvements in seasonal to decadal predictions. In particular, it will focus on variability and long-term change of energy and freshwater flows through the arctic climate system. The project will also address modes of natural climate variability as well as extreme and rapid climate change in a region of the Earth that is: (i) a key indicator of the state of global climate 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 climate 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 climate modeling and predictions.« less

  11. Seismic Rate Changes Associated with Seasonal, Annual, and Decadal Changes in the Cryosphere

    NASA Technical Reports Server (NTRS)

    Sauber-Rosenberg, Jeanne

    2012-01-01

    Near the Bering Glacier Global Fiducial site in southern Alaska large cryospheric fluctuations occur in a region of upper crustal faulting and folding associated with collision and accretion of the Yakutat terrane. In this study we report constraints on seasonal, annual and decadal cryospheric changes estimated over the last decade from field, aircraft and satellite measurements, and we evaluate the influence of cryospheric changes on the background seismic rate. Multi-year images from the Bering Glacier global fiducial site are available since mid-2003 to constrain changes in extent of the Bering Glacier and to discern feature changes in the glacial surface. Starting around the same time, satellite gravimetric measurements from the Gravity Recovery and Climate experiment (GRACE) commenced. Large spatial-scale mass change calculated from the GRACE 1deg x 1deg mascon solution of Luthcke et al. [2012] indicate a general trend of annual ice mass loss for southern Alaska but with large, variable seasonal mass fluctuations. Since 2007, the station position of a continuous GPS site near Cape Yakataga (Alaska EarthScope PBO site, AB35) has been available as well. In addition to changes in the geodetic position due to tectonic motion, this GPS station shows large seasonal excursions in the detrended vertical and horizontal position components consistent with snow loading in the fall and winter and melt onset/mass decrease in the spring/summer. To better understand the timing of processes responsible for the onset of cryospheric mass loss documented in the GRACE data, we examined changes in the snow cover extent and the onset of melt in the spring. We calculated the surface displacements of the solid Earth and theoretical earthquake failure criteria associated with these annual and seasonal ice and snow changes using layered elastic half-space. Additionally, we compared the seismic rate (M>1.8) from a reference background time period against other time periods with variable

  12. Changes in breeding phenology of eastern Ontario frogs over four decades.

    PubMed

    Klaus, Samantha P; Lougheed, Stephen C

    2013-04-01

    Global climate change has been implicated in phenological shifts for a variety of taxa. Amphibian species in particular are sensitive to changes in their environment due to their biphasic life history and restricted reproductive requirements. Previous research has shown that not all temperate amphibian species respond similarly to the same suite of climatic or environmental cues, nor are individual species necessarily uniform in their responses across their range. We examined both the timing of spring emergence and calling phenology of eight anuran species in southeastern Ontario, Canada, using an approximately 40-year dataset of historical records of amphibian activity. Rana pipiens was the only species out of eight considered to emerge significantly earlier, by an estimated 22 days over four decades. Both R. pipiens and Bufo americanus have advanced initiation of calling over a four-decade span significantly earlier by an estimated 37.2 and 19.2 days, respectively. Rana sylvatica showed a trend toward earlier emergence by 19 days, whereas we did not detect changes in emergence phenology for the remaining five species. This significant shift in breeding behavior for two species correlates to significant regional increases in spring temperatures of an estimated 2.7-2.8°C overall over four decades. Our study suggests that local temperature increases have affected the timing of emergence and the onset of calling activity in some Ontario anuran species. Global decline or range shifts ultimately may be related to changes in reproductive behavior and timing mediated by shifting climate.

  13. 34 CFR 75.517 - Changes in key staff members.

    Code of Federal Regulations, 2010 CFR

    2010-07-01

    ... 34 Education 1 2010-07-01 2010-07-01 false Changes in key staff members. 75.517 Section 75.517... by a Grantee? Project Staff § 75.517 Changes in key staff members. A grantee shall comply with 34 CFR 74.25(c)(2) concerning replacement or lesser involvement of any key project staff, whether or not the...

  14. 34 CFR 75.517 - Changes in key staff members.

    Code of Federal Regulations, 2014 CFR

    2014-07-01

    ... 34 Education 1 2014-07-01 2014-07-01 false Changes in key staff members. 75.517 Section 75.517... by a Grantee? Project Staff § 75.517 Changes in key staff members. A grantee shall comply with 34 CFR 74.25(c)(2) concerning replacement or lesser involvement of any key project staff, whether or not the...

  15. 34 CFR 75.517 - Changes in key staff members.

    Code of Federal Regulations, 2013 CFR

    2013-07-01

    ... 34 Education 1 2013-07-01 2013-07-01 false Changes in key staff members. 75.517 Section 75.517... by a Grantee? Project Staff § 75.517 Changes in key staff members. A grantee shall comply with 34 CFR 74.25(c)(2) concerning replacement or lesser involvement of any key project staff, whether or not the...

  16. 34 CFR 75.517 - Changes in key staff members.

    Code of Federal Regulations, 2011 CFR

    2011-07-01

    ... 34 Education 1 2011-07-01 2011-07-01 false Changes in key staff members. 75.517 Section 75.517... by a Grantee? Project Staff § 75.517 Changes in key staff members. A grantee shall comply with 34 CFR 74.25(c)(2) concerning replacement or lesser involvement of any key project staff, whether or not the...

  17. 34 CFR 75.517 - Changes in key staff members.

    Code of Federal Regulations, 2012 CFR

    2012-07-01

    ... 34 Education 1 2012-07-01 2012-07-01 false Changes in key staff members. 75.517 Section 75.517... by a Grantee? Project Staff § 75.517 Changes in key staff members. A grantee shall comply with 34 CFR 74.25(c)(2) concerning replacement or lesser involvement of any key project staff, whether or not the...

  18. Key enablers to facilitate healthy behavior change: workshop summary.

    PubMed

    Teyhen, Deydre S; Aldag, Matt; Centola, Damon; Edinborough, Elton; Ghannadian, Jason D; Haught, Andrea; Jackson, Theresa; Kinn, Julie; Kunkler, Kevin J; Levine, Betty; Martindale, Valerie E; Neal, David; Snyder, Leslie B; Styn, Mindi A; Thorndike, Frances; Trabosh, Valerie; Parramore, David J

    2014-05-01

    The increases in preventable chronic diseases and the rising costs of health care are unsustainable. The US Army Surgeon General's vision to transition from a health care system to a system of health requires the identification of key health enablers to facilitate the adoption of healthy behaviors. In support of this vision, the US Army Telemedicine and Advanced Technology Research Center hosted a workshop in April 2013 titled "Incentives to Create and Sustain Change for Health." Members of government and academia participated to identify key health enablers that could ultimately be leveraged by technology. The key health enablers discussed included (1) public health messaging, (2) changing health habits and the environmental influence on health, (3) goal setting and tracking, (4) the role of incentives in behavior-change intervention, and (5) the role of peer and social networks on change. This report summarizes leading evidence and the group consensus on evidence-based practices with respect to the key enablers in creating healthy behavior change.

  19. Pacific Decadal Variability and Central Pacific Warming El Niño in a Changing Climate

    DOE Office of Scientific and Technical Information (OSTI.GOV)

    Di Lorenzo, Emanuele

    This research aimed at understanding the dynamics controlling decadal variability in the Pacific Ocean and its interactions with global-scale climate change. The first goal was to assess how the dynamics and statistics of the El Niño Southern Oscillation and the modes of Pacific decadal variability are represented in global climate models used in the IPCC. The second goal was to quantify how decadal dynamics are projected to change under continued greenhouse forcing, and determine their significance in the context of paleo-proxy reconstruction of long-term climate.

  20. Decadal changes in channel morphology of a freely meandering river—Powder River, Montana, 1975–2016

    USGS Publications Warehouse

    Moody, John A.; Meade, Robert H.

    2018-03-19

    Few studies exist on the long-term geomorphic effects of floods. However, the U.S. Geological Survey (USGS) was able to begin such a study after a 50-year recurrence interval flood in 1978 because 20 channel cross sections along a 100-kilometer reach of river were established in 1975 and 1977 as part of a study for a proposed dam on Powder River in southeastern Montana. These cross-section measurements (data for each channel cross section are available at the USGS ScienceBase website) have been repeated about 30 times during four decades (1975–2016) and provide a unique dataset for understanding long-term changes in channel morphology caused by an extreme flood and a spectrum of annual floods.Changes in channel morphology of a 100-kilometer reach of Powder River are documented in a series of narratives for each channel cross section that include a time series of photographs as a record of these changes. The primary change during the first decade (1975–85) was the rapid vertical growth of a new inset flood plain within the flood-widened channel. Changes during the second decade (1985–95) were characterized by slower growth of the flood plain, and the effects of ice-jam floods typical of a northward-flowing river. Changes during the third decade (1995–2005) showed little vertical growth of the inset flood plain, which had reached a height that limited overbank deposition. And changes during the final decade (2005–16) covered in this report showed that, because the new inset flood plain had reached a limiting height, the effects of the large annual flood of 2008 (largest flood since 1978) were relatively small compared to smaller floods in previous decades. Throughout these four decades, the riparian vegetation, which interacts with the river, has undergone a gradual but substantial change that may have lasting effects on the channel morphology.

  1. Multi-Decadal Change of Atmospheric Aerosols and Their Effect on Surface Radiation

    NASA Technical Reports Server (NTRS)

    Chin, Mian; Diehl, Thomas; Tan, Qian; Wild, Martin; Qian, Yun; Yu, Hongbin; Bian, Huisheng; Wang, Weiguo

    2012-01-01

    We present an investigation on multi-decadal changes of atmospheric aerosols and their effects on surface radiation using a global chemistry transport model along with the near-term to long-term data records. We focus on a 28-year time period of satellite era from 1980 to 2007, during which a suite of aerosol data from satellite observations and ground-based remote sensing and in-situ measurements have become available. We analyze the long-term global and regional aerosol optical depth and concentration trends and their relationship to the changes of emissions" and assess the role aerosols play in the multi-decadal change of solar radiation reaching the surface (known as "dimming" or "brightening") at different regions of the world, including the major anthropogenic source regions (North America, Europe, Asia) that have been experiencing considerable changes of emissions, dust and biomass burning regions that have large interannual variabilities, downwind regions that are directly affected by the changes in the source area, and remote regions that are considered to representing "background" conditions.

  2. Disabled Children and Their Families: A Decade of Policy Change

    ERIC Educational Resources Information Center

    Read, Janet; Blackburn, Clare; Spencer, Nick

    2012-01-01

    Focusing mainly on the United Kingdom, this article reviews a decade of national and international policy and legal changes in relation to disabled children and their families. It discusses attempts to transform the ways that disabled children are perceived and the rights accorded to them. The UN Convention on the Rights of Disabled Persons,…

  3. Newborn survival in Bangladesh: a decade of change and future implications.

    PubMed

    Rubayet, Sayed; Shahidullah, Mohammad; Hossain, Altaf; Corbett, Erica; Moran, Allisyn C; Mannan, Imteaz; Matin, Ziaul; Wall, Stephen N; Pfitzer, Anne; Mannan, Ishtiaq; Syed, Uzma

    2012-07-01

    Remarkable progress over the last decade has put Bangladesh on track for Millennium Development Goal (MDG) 4 for child survival and achieved a 40% decline in maternal mortality. However, since neonatal deaths make up 57% of under-five mortality in the country, increased scale up and equity in programmes for neonatal survival are critical to sustain progress. We examined change for newborn survival from 2000 to 2010 considering mortality, coverage and funding indicators, as well as contextual factors. The national neonatal mortality rate has undergone an annual decline of 4.0% since 2000, reflecting greater progress than both the regional and global averages, but the mortality reduction for children 1-59 months was double this rate, at 8.6%. Examining policy and programme change, and national and donor funding for health, we identified various factors which contributed to an environment favourable to newborn survival. Locally-generated evidence combined with re-packaged global evidence, notably The Lancet Neonatal Series, has played a role, although pathways between research and policies and programme change are often complex. Several high-profile champions have had major influence. Attention for community initiatives and considerable donor funding also appear to have contributed. There have been some increases in coverage of key interventions, such as skilled attendance at birth and postnatal care, however these are low and reach less than one-third of families. Major reductions in total fertility, some change in gross national income and other contextual factors are likely to also have had an influence in mortality reduction. However, other factors such as socio-economic and geographic inequalities, frequent changes in government and pluralistic implementation structures have provided challenges. As coverage of health services increases, a notable gap remains in quality of facility-based care. Future gains for newborn survival in Bangladesh rest upon increased

  4. Decadal changes in the Canary Current Upwelling Ecosystem

    NASA Astrophysics Data System (ADS)

    Santos, A. M.; Luis, J. M.; Relvas-Almeida, P.

    2013-12-01

    The Canary Current Upwelling System (CCUS) covers the latitudinal range 12-43 degrees N and has some singularities in relation to the other three major Eastern Boundary Upwelling Systems (EBUS), namely a major interruption in the continuity of the system at the Strait of Gibraltar and it is the only one with a sardine species from a different genus (Sardina vs Sardinops). Long-term trends in ocean temperature and coastal upwelling were investigated using the AVHRR Pathfinder SST (sea surface temperature) Version 5.1 dataset, in situ SST from the International Comprehensive Ocean-Atmosphere Data Set (ICOADS), and upwelling indices from the Pacific Fisheries Environmental Laboratory (PFEL). The analysis is applied to the eastern boundary of the North Atlantic, from 10 to 45 degrees N extending until 30 degrees W, focusing mainly in the CCUS because the strong dynamic link between the atmosphere and the ocean makes upwelling regions highly sensitive to global change and ideal to monitor and investigate its effects. The detail in SST variability results in a large extent from the fine analysis and the numerical processing carefully designed to avoid trend bias in the climatological studies. The obtained fields of SST trends show a generalized warming of the entire region. However, alternate patches of significantly different warming rates are observed, ranging from large scale down to mesoscale. Known coastal upwelling features are seen to warm at a lower rate than corresponding offshore waters, pointing to an intensification of the upwelling in the last decades. Wind data are used to attempt to explain the variability of some upwelling structures. Our results evidence the main role that mesoscale processes play in the modulation of the spatial and temporal variability of SST, namely at the decadal scale. This result prevents any global conclusion about the intensification of the upwelling at the scale of the entire CCUS. The bulk of the sardine population is located

  5. NAS Decadal Review Town Hall

    NASA Astrophysics Data System (ADS)

    The National Academies of Sciences, Engineering and Medicine is seeking community input for a study on the future of materials research (MR). Frontiers of Materials Research: A Decadal Survey will look at defining the frontiers of materials research ranging from traditional materials science and engineering to condensed matter physics. Please join members of the study committee for a town hall to discuss future directions for materials research in the United States in the context of worldwide efforts. In particular, input on the following topics will be of great value: progress, achievements, and principal changes in the R&D landscape over the past decade; identification of key MR areas that have major scientific gaps or offer promising investment opportunities from 2020-2030; and the challenges that MR may face over the next decade and how those challenges might be addressed. This study was requested by the Department of Energy and the National Science Foundation. The National Academies will issue a report in 2018 that will offer guidance to federal agencies that support materials research, science policymakers, and researchers in materials research and other adjoining fields. Learn more about the study at http://nas.edu/materials.

  6. Anthropogenic Climate Change in Asia: Key Challenges

    NASA Astrophysics Data System (ADS)

    Ramaswamy, V.

    2009-12-01

    The energy, agricultural, and water sectors in Asia, a vast continent that comprises more than half of the world's population, are crucially vulnerable to shifts in climate. The acceleration of economic development in Asia over the past few decades, the dependence of its huge agricultural economy on rainfall, and its growing energy demands have thrust climate change and its impacts squarely into important sectors of the Asian society. Further, it is likely that there has been significant anthropogenic warming over the past 50 years averaged over the Asian continent (Intergovernmental Panel on Climate Change (IPCC) [2007]; see Figure 1a). Asian megacities are already witnessing stresses in food, water, transportation, health, and air quality. The situation could become even worse with projected changes in temperature and rainfall in the 21st century, coupled with the likelihood that climate change will exacerbate extremes.

  7. Interannual variation, decadal trend, and future change in ozone outflow from East Asia

    NASA Astrophysics Data System (ADS)

    Zhu, Jia; Liao, Hong; Mao, Yuhao; Yang, Yang; Jiang, Hui

    2017-03-01

    We examine the past and future changes in the O3 outflow from East Asia using a global 3-D chemical transport model, GEOS-Chem. The simulations of Asian O3 outflow for 1986-2006 are driven by the assimilated GEOS-4 meteorological fields, and those for 2000-2050 are driven by the meteorological fields archived by the NASA Goddard Institute for Space Studies (GISS) general circulation model (GCM) 3 under the IPCC SRES A1B scenario. The evaluation of the model results against measurements shows that the GEOS-Chem model captures the seasonal cycles and interannual variations of tropospheric O3 concentrations fairly well with high correlation coefficients of 0.82-0.93 at four ground-based sites and 0.55-0.88 at two ozonesonde sites where observations are available. The increasing trends in surface-layer O3 concentrations in East Asia over the past 2 decades are captured by the model, although the modeled O3 trends have low biases. Sensitivity studies are conducted to examine the respective impacts of meteorological parameters and emissions on the variations in the outflow flux of O3. When both meteorological parameters and anthropogenic emissions varied from 1986-2006, the simulated Asian O3 outflow fluxes exhibited a statistically insignificant decadal trend; however, they showed large interannual variations (IAVs) with seasonal values of 4-9 % for the absolute percent departure from the mean (APDM) and an annual APDM value of 3.3 %. The sensitivity simulations indicated that the large IAVs in O3 outflow fluxes were mainly caused by variations in the meteorological conditions. The variations in meteorological parameters drove the IAVs in O3 outflow fluxes by altering the O3 concentrations over East Asia and by altering the zonal winds; the latter was identified to be the key factor, since the O3 outflow was highly correlated with zonal winds from 1986-2006. The simulations of the 2000-2050 changes show that the annual outflow flux of O3 will increase by 2.0, 7.9, and

  8. Mechanisms underlying recent decadal changes in subpolar North Atlantic Ocean heat content

    NASA Astrophysics Data System (ADS)

    Piecuch, Christopher G.; Ponte, Rui M.; Little, Christopher M.; Buckley, Martha W.; Fukumori, Ichiro

    2017-09-01

    The subpolar North Atlantic (SPNA) is subject to strong decadal variability, with implications for surface climate and its predictability. In 2004-2005, SPNA decadal upper ocean and sea-surface temperature trends reversed from warming during 1994-2004 to cooling over 2005-2015. This recent decadal trend reversal in SPNA ocean heat content (OHC) is studied using a physically consistent, observationally constrained global ocean state estimate covering 1992-2015. The estimate's physical consistency facilitates quantitative causal attribution of ocean variations. Closed heat budget diagnostics reveal that the SPNA OHC trend reversal is the result of heat advection by midlatitude ocean circulation. Kinematic decompositions reveal that changes in the deep and intermediate vertical overturning circulation cannot account for the trend reversal, but rather ocean heat transports by horizontal gyre circulations render the primary contributions. The shift in horizontal gyre advection reflects anomalous circulation acting on the mean temperature gradients. Maximum covariance analysis (MCA) reveals strong covariation between the anomalous horizontal gyre circulation and variations in the local wind stress curl, suggestive of a Sverdrup response. Results have implications for decadal predictability.

  9. Systematic review: has disease outcome in Crohn's disease changed during the last four decades?

    PubMed

    Wolters, F L; Russel, M G V M; Stockbrügger, R W

    2004-09-01

    Disease outcome in Crohn's disease might have changed during the last four decades. Disease outcome measurement in Crohn's disease has methodological difficulties because of patient selection and lack of proper definition of diagnostic and outcome measurement criteria. To assess possible changes in disease outcome in Crohn's disease during the last four decades. A systematic literature search was performed using the MEDLINE search engine and major international conference libraries. Articles and abstracts were selected according to stringent inclusion criteria. Forty articles and nine abstracts complied with the inclusion criteria. Seven studies with a median follow-up time between 11.1 and 17 years showed standard mortality ratios in Crohn's disease ranging between 2.16 and 0.72 with a tendency of decline during the last four decades. One study with 11.4 years mean follow-up time showed a statistically significant increased relative risk for colorectal cancer that was not confirmed by three others. Sixteen publications applied in the disease recurrence category. Probability of first resective surgery ranged between 38 and 96% during the first 15 years after diagnosis. The overall recurrence and surgical recurrence rates after first resective surgery ranged between 50 and 60, and 28 and 45% respectively during the following 15 years without an apparent time trend. This structured literature review provides no hard evidence for change in disease outcome in Crohn's disease during the last four decades. Copyright 2004 Blackwell Publishing Ltd

  10. Decadal changes in potassium, calcium, and magnesium in a deciduous forest soil.

    Treesearch

    D.W. Johnson; D.E. Todd; Carl C. Trettin; P.J. Mulholland

    2009-01-01

    Decadal changes in soil exchangeable K+, Ca2+, and Mg2+ concentrations and contents from 1972 to 2004 in eight intensively monitored plots on Walker Branch Watershed were compared with estimates of increments or decrements in vegetation and detritus. The results from these eight plots...

  11. A Decade of Field Changing Atmospheric Aerosol Research ...

    EPA Pesticide Factsheets

    Conference: Gordon Research Conference in Atmospheric Chemistry, July 28 – August 2, 2013, VermontPresentation Type: PosterTitle: An Analysis of EPA’s STAR Program and a Decade of Field Changing Research in Atmospheric AerosolsAuthors: Kristina M. Wagstrom1,2, Sherri W. Hunt31Chemical and Biomolecular Engineering, University of Connecticut, Storrs, CT2AAAS Science and Technology Policy Fellow hosted by U.S. Environmental Protection Agency, National Center for Environmental Research3U.S. Environmental Protection Agency, National Center for Environmental ResearchA number of studies in the past decade have transformed the way we think about atmospheric aerosols. The advances include, but are not limited to, source apportionment of organics using aerosol mass spectrometer data, the volatility basis set approach, quantifying isoprene oxidation, and understanding the role of aqueous oxidation of organics on SOA formation. A series of grants funded by EPA just under ten years ago supported many of these advances. These projects make up the body of work awarded under two solicitations released by the EPA’s Science to Achieve Results (STAR) program: “Measurement, Modeling, and Analysis Methods for Airborne Carbonaceous Fine Particulate Matter” (2003) and “Source Apportionment of Particulate Matter” (2004). Our goal is to present the impact of the STAR solicitations and to show how they have pushed the field forward and led to new questions.In particular

  12. Large-Scale Atmospheric Teleconnection Patterns Associated with the Interannual Variability of Heatwaves in East Asia and Its Decadal Changes

    NASA Astrophysics Data System (ADS)

    Choi, N.; Lee, M. I.; Lim, Y. K.; Kim, K. M.

    2017-12-01

    Heatwave is an extreme hot weather event which accompanies fatal damage to human health. The heatwave has a strong relationship with the large-scale atmospheric teleconnection patterns. In this study, we examine the spatial pattern of heatwave in East Asia by using the EOF analysis and the relationship between heatwave frequency and large-scale atmospheric teleconnection patterns. We also separate the time scale of heatwave frequency as the time scale longer than a decade and the interannual time scale. The long-term variation of heatwave frequency in East Asia shows a linkage with the sea surface temperature (SST) variability over the North Atlantic with a decadal time scale (a.k.a. the Atlantic Multidecadal Oscillation; AMO). On the other hands, the interannual variation of heatwave frequency is linked with the two dominant spatial patterns associated with the large-scale teleconnection patterns mimicking the Scandinavian teleconnection (SCAND-like) pattern and the circumglobal teleconnection (CGT-like) pattern, respectively. It is highlighted that the interannual variation of heatwave frequency in East Asia shows a remarkable change after mid-1990s. While the heatwave frequency was mainly associated with the CGT-like pattern before mid-1990s, the SCAND-like pattern becomes the most dominant one after mid-1990s, making the CGT-like pattern as the second. This study implies that the large-scale atmospheric teleconnection patterns play a key role in developing heatwave events in East Asia. This study further discusses possible mechanisms for the decadal change in the linkage between heatwave frequency and the large-scale teleconnection patterns in East Asia such as early melting of snow cover and/or weakening of East Asian jet stream due to global warming.

  13. Older Adults' Attitudes Toward Cohabitation: Two Decades of Change.

    PubMed

    Brown, Susan L; Wright, Matthew R

    2016-07-01

    Our study tracks cohort change in the attitudes of adults aged 50 and older toward cohabitation from 1994 to 2012. We used data from the 1994, 2002, and 2012 waves of the General Social Survey to examine the roles of cohort replacement and intracohort change in the trend toward favorable cohabitation attitudes and to examine sociodemographic variation in patterns of support for cohabitation. Support for cohabitation accelerated over time with nearly half (46%) of older adults reporting favorable attitudes toward cohabitation in 2012 versus just 20% in 1994. This shift in older adults' attitudes largely reflected cohort replacement rather than intracohort change. Some of the factors associated with later life cohabitation experience were linked to supportive attitudes. Cohort succession is fueling the growing acceptance of cohabitation among older adults and coincides with the rapid growth in later life cohabitation that has occurred in recent decades. © The Author 2015. Published by Oxford University Press on behalf of The Gerontological Society of America. All rights reserved. For permissions, please e-mail: journals.permissions@oup.com.

  14. Progressive Bidirectional Age-Related Changes in Default Mode Network Effective Connectivity across Six Decades

    PubMed Central

    Li, Karl; Laird, Angela R.; Price, Larry R.; McKay, D. Reese; Blangero, John; Glahn, David C.; Fox, Peter T.

    2016-01-01

    The default mode network (DMN) is a set of regions that is tonically engaged during the resting state and exhibits task-related deactivation that is readily reproducible across a wide range of paradigms and modalities. The DMN has been implicated in numerous disorders of cognition and, in particular, in disorders exhibiting age-related cognitive decline. Despite these observations, investigations of the DMN in normal aging are scant. Here, we used blood oxygen level dependent (BOLD) functional magnetic resonance imaging (fMRI) acquired during rest to investigate age-related changes in functional connectivity of the DMN in 120 healthy normal volunteers comprising six, 20-subject, decade cohorts (from 20–29 to 70–79). Structural equation modeling (SEM) was used to assess age-related changes in inter-regional connectivity within the DMN. SEM was applied both using a previously published, meta-analytically derived, node-and-edge model, and using exploratory modeling searching for connections that optimized model fit improvement. Although the two models were highly similar (only 3 of 13 paths differed), the sample demonstrated significantly better fit with the exploratory model. For this reason, the exploratory model was used to assess age-related changes across the decade cohorts. Progressive, highly significant changes in path weights were found in 8 (of 13) paths: four rising, and four falling (most changes were significant by the third or fourth decade). In all cases, rising paths and falling paths projected in pairs onto the same nodes, suggesting compensatory increases associated with age-related decreases. This study demonstrates that age-related changes in DMN physiology (inter-regional connectivity) are bidirectional, progressive, of early onset and part of normal aging. PMID:27378909

  15. Progressive Bidirectional Age-Related Changes in Default Mode Network Effective Connectivity across Six Decades.

    PubMed

    Li, Karl; Laird, Angela R; Price, Larry R; McKay, D Reese; Blangero, John; Glahn, David C; Fox, Peter T

    2016-01-01

    The default mode network (DMN) is a set of regions that is tonically engaged during the resting state and exhibits task-related deactivation that is readily reproducible across a wide range of paradigms and modalities. The DMN has been implicated in numerous disorders of cognition and, in particular, in disorders exhibiting age-related cognitive decline. Despite these observations, investigations of the DMN in normal aging are scant. Here, we used blood oxygen level dependent (BOLD) functional magnetic resonance imaging (fMRI) acquired during rest to investigate age-related changes in functional connectivity of the DMN in 120 healthy normal volunteers comprising six, 20-subject, decade cohorts (from 20-29 to 70-79). Structural equation modeling (SEM) was used to assess age-related changes in inter-regional connectivity within the DMN. SEM was applied both using a previously published, meta-analytically derived, node-and-edge model, and using exploratory modeling searching for connections that optimized model fit improvement. Although the two models were highly similar (only 3 of 13 paths differed), the sample demonstrated significantly better fit with the exploratory model. For this reason, the exploratory model was used to assess age-related changes across the decade cohorts. Progressive, highly significant changes in path weights were found in 8 (of 13) paths: four rising, and four falling (most changes were significant by the third or fourth decade). In all cases, rising paths and falling paths projected in pairs onto the same nodes, suggesting compensatory increases associated with age-related decreases. This study demonstrates that age-related changes in DMN physiology (inter-regional connectivity) are bidirectional, progressive, of early onset and part of normal aging.

  16. Decadal change of the south Atlantic ocean Angola-Benguela frontal zone since 1980

    NASA Astrophysics Data System (ADS)

    Vizy, Edward K.; Cook, Kerry H.; Sun, Xiaoming

    2018-01-01

    High-resolution simulations with a regional atmospheric model coupled to an intermediate-level mixed layer ocean model along with multiple atmospheric and oceanic reanalyses are analyzed to understand how and why the Angola-Benguela frontal Zone (ABFZ) has changed since 1980. A southward shift of 0.05°-0.55° latitude decade-1 in the annual mean ABFZ position accompanied by an intensification of + 0.05 to + 0.13 K/100-km decade-1 has occurred as ocean mixed layer temperatures have warmed (cooled) equatorward (poleward) of the front over the 1980-2014 period. These changes are captured in a 35-year model integration. The oceanic warming north of the ABFZ is associated with a weakening of vertical entrainment, reduced cooling associated with vertical diffusion, and a deepening of the mixed layer along the Angola coast. These changes coincide with a steady weakening of the onshore atmospheric flow as the zonal pressure gradient between the eastern equatorial Atlantic and the Congo Basin weakens. Oceanic cooling poleward of the ABFZ is primarily due to enhanced advection of cooler water from the south and east, increased cooling by vertical diffusion, and shoaling of the mixed layer depth. In the atmosphere, these changes are related to an intensification and poleward shift of the South Atlantic sub-tropical anticyclone as surface winds, hence the westward mixed layer ocean currents, intensify in the Benguela upwelling region along the Namibian coast. With a few caveats, these findings demonstrate that air/sea interactions play a prominent role in influencing the observed decadal variability of the ABFZ over the southeastern Atlantic since 1980.

  17. Meridional Modes and Increasing Pacific Decadal Variability Under Anthropogenic Forcing

    NASA Astrophysics Data System (ADS)

    Liguori, Giovanni; Di Lorenzo, Emanuele

    2018-01-01

    Pacific decadal variability has strong impacts on the statistics of weather, atmosphere extremes, droughts, hurricanes, marine heatwaves, and marine ecosystems. Sea surface temperature (SST) observations show that the variance of the El Niño-like decadal variability has increased by 30% (1920-2015) with a stronger coupling between the major Pacific climate modes. Although we cannot attribute these trends to global climate change, the examination of 30 members of the Community Earth System Model Large Ensemble (LENS) forced with the RCP8.5 radiative forcing scenario (1920-2100) suggests that significant anthropogenic trends in Pacific decadal variance will emerge by 2020 in response to a more energetic North Pacific Meridional Mode (PMM)—a well-known El Niño precursor. The PMM is a key mechanism for energizing and coupling tropical and extratropical decadal variability. In the LENS, the increase in PMM variance is consistent with an intensification of the winds-evaporation-SST thermodynamic feedback that results from a warmer mean climate.

  18. Changes in Lithuanian Pre-School and Pre-Primary Education Quality over the Last Decade

    ERIC Educational Resources Information Center

    Monkeviciene, Ona; Stankeviciene, Kristina

    2011-01-01

    Over the last decade, the changes in Lithuanian pre-school and pre-primary education have been predetermined by changes in paradigms of children's education and strategic education documents that provided for guidelines of high quality children's (self-)education, an increasing attention of society to the quality of children's education, training…

  19. The Future We Want: Key Issues on Sustainable Development in Higher Education after Rio and the UN Decade of Education for Sustainable Development

    ERIC Educational Resources Information Center

    Leal Filho, Walter; Manolas, Evangelos; Pace, Paul

    2015-01-01

    Purpose: This paper aims to provide a description of the achievements of the United Nations (UN) Decade of Education for Sustainable Development (2005-2014) with a focus on higher education, and it describes some of the key issues which will guide sustainable development in the coming years. Design/methodology/approach: The paper initially…

  20. Decadal land cover change dynamics in Bhutan.

    PubMed

    Gilani, Hammad; Shrestha, Him Lal; Murthy, M S R; Phuntso, Phuntso; Pradhan, Sudip; Bajracharya, Birendra; Shrestha, Basanta

    2015-01-15

    Land cover (LC) is one of the most important and easily detectable indicators of change in ecosystem services and livelihood support systems. This paper describes the decadal dynamics in LC changes at national and sub-national level in Bhutan derived by applying object-based image analysis (OBIA) techniques to 1990, 2000, and 2010 Landsat (30 m spatial resolution) data. Ten LC classes were defined in order to give a harmonized legend land cover classification system (LCCS). An accuracy of 83% was achieved for LC-2010 as determined from spot analysis using very high resolution satellite data from Google Earth Pro and limited field verification. At the national level, overall forest increased from 25,558 to 26,732 km(2) between 1990 and 2010, equivalent to an average annual growth rate of 59 km(2)/year (0.22%). There was an overall reduction in grassland, shrubland, and barren area, but the observations were highly dependent on time of acquisition of the satellite data and climatic conditions. The greatest change from non-forest to forest (277 km(2)) was in Bumthang district, followed by Wangdue Phodrang and Trashigang, with the least (1 km(2)) in Tsirang. Forest and scrub forest covers close to 75% of the land area of Bhutan, and just over half of the total area (51%) has some form of conservation status. This study indicates that numerous applications and analyses can be carried out to support improved land cover and land use (LCLU) management. It will be possible to replicate this study in the future as comparable new satellite data is scheduled to become available. Copyright © 2014 Elsevier Ltd. All rights reserved.

  1. Large decadal-scale changes in uranium and bicarbonate in groundwater of the irrigated western U.S

    USGS Publications Warehouse

    Burow, Karen R.; Belitz, Kenneth; Dubrovsky, Neil M.; Jurgens, Bryant C.

    2017-01-01

    Samples collected about one decade apart from 1105 wells from across the U.S. were compiled to assess whether uranium concentrations in the arid climate are linked to changing bicarbonate concentrations in the irrigated western U.S. Uranium concentrations in groundwater were high in the arid climate in the western U.S, where uranium sources are abundant. Sixty-four wells (6%) were above the U.S. EPA MCL of 30 μg/L; all but one are in the arid west. Concentrations were low to non-detectable in the humid climate. Large uranium and bicarbonate increases (differences are greater than the uncertainty in concentrations) occur in 109 wells between decade 1 and decade 2. Similarly, large uranium and bicarbonate decreases occur in 76 wells between the two decades. Significantly more wells are concordant (uranium and bicarbonate are both going the same direction) than discordant (uranium and bicarbonate are going opposite directions) (p < 0.001; Chi-square test). The largest percent difference in uranium concentrations occur in wells where uranium is increasing and bicarbonate is also increasing. These large differences occur mostly in the arid climate. Results are consistent with the hypothesis that changing uranium concentrations are linked to changes in bicarbonate in irrigated areas of the western U.S.

  2. Interannual and Decadal Changes in Salinity in the Oceanic Subtropical Gyres

    NASA Astrophysics Data System (ADS)

    Bulusu, Subrahmanyam

    2017-04-01

    There is evidence that the global water cycle has been undergoing an intensification over several decades as a response to increasing atmospheric temperatures, particularly in regions with skewed evaporation - precipitation (E-P) patterns such as the oceanic subtropical gyres. Moreover, observational data (rain gauges, etc.) are quite sparse over such areas due to the inaccessibility of open ocean regions. In this work, a comparison of observational and model simulations are conducted to highlight the potential applications of satellite derived salinity from NASA Aquarius Salinity mission, NASA Soil Moisture and Ocean Salinity (SMOS), and ESA's Soil Moisture Active Passive (SMAP). We explored spatial and temporal salinity changes (and trends) in surface and subsurface in the oceanic subtropical gyres using Argo floats salinity data, Simple Ocean Data Assimilation (SODA) reanalysis, Estimating the Circulations & Climate of the Ocean GECCO (German ECCO) model simulations, and Hybrid Coordinate Ocean Model (HYCOM). Our results based on SODA reanalysis reveals that a positive rising trend in sea surface salinity in the subtropical gyres emphasizing evidence for decadal intensification in the surface forcing in these regions. Zonal drift in the location of the salinity maximum of the south Pacific, north Atlantic, and south Indian regions implies a change in the mean near-surface currents responsible for advecting high salinity waters into the region. Also we found out that an overall salinity increase within the mixed layer, and a subsurface salinity decrease at depths greater than 200m in the global subtropical gyres over 61 years. We determine that freshwater fluxes at the air-sea interface are the primary drivers of the sea surface salinity (SSS) signature over these open ocean regions by quantifying the advective contribution within the surface layer. This was demonstrated through a mixed layer salinity budget in each subtropical gyre based on the vertically

  3. Experiencing limits of acceptable change: some thoughts after a decade of implementation

    Treesearch

    Stephen F. McCool; David N. Cole

    1997-01-01

    Wilderness managers and researchers have experienced implementation of the Limits of Acceptable Change planning system for over a decade. In a sense, implementation of LAC has been a broad scale experiment in planning, with the hypothesis being that LAC processes are more effective approaches to deal with questions of recreation management in protected areas than the...

  4. Using decadal climate prediction to characterize and manage changing drought and flood risks in Colorado

    NASA Astrophysics Data System (ADS)

    Lazrus, H.; Done, J.; Morss, R. E.

    2017-12-01

    A new branch of climate science, known as decadal prediction, seeks to predict the time-varying trajectory of climate over the next 3-30 years and not just the longer-term trends. Decadal predictions bring climate 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 predictions 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 climate information and its use in decision making. The presentation will explore the skill and utility of decadal drought and flood prediction along Colorado's Front Range, an area experiencing rapid population growth and uncertain climate variability and climate change impacts. Innovative statistical and dynamical atmospheric modeling techniques explore the extent to which Colorado precipitation can be predicted 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 climate 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.

  5. New Zealand: long-term care in a decade of change.

    PubMed

    Ashton, T

    2000-01-01

    Long-term care in New Zealand incorporates a mix of public and private funding and provision. After a decade of structural change, the purchasing of almost all publicly funded health and social care is now the responsibility of one central agency. Services for older persons are poorly integrated, and there are problems of access to and quality of some services. Efforts are being made to address these problems. The challenge now is to ensure that this groundwork is not lost amid the turmoil of yet another round of restructuring by an enthusiastic, newly elected government.

  6. Inter-Annual and Decadal Changes in Tropospheric and Stratospheric Ozone

    NASA Technical Reports Server (NTRS)

    Ziemke, Jr. R.; Chandra, S.

    2011-01-01

    Ozone data beginning October 2004 from the Aura Ozone Monitoring Instrument (OMI) and Aura Microwave Limb Sounder (MLS) are used to evaluate the accuracy of the Cloud slicing technique in effort to develop long data records of tropospheric and stratospheric ozone and studying their long-term changes. Using this technique, we have produced a 32-year (1979-2010) long record of tropospheric and stratospheric ozone from the combined Total Ozone Mapping Spectrometer (Toms) and OMI. The analyses of these time series suggest that the quasi-biennial oscillation (QBO) is the dominant source of inter-annual changes of 30-40 Dobson Units (DU). Tropospheric ozone also indicates a QBO signal in the peak to peak changes varying from 2 to 7 DU. Decadal changes in global stratospheric ozone indicate a turnaround in ozone loss around mid 1990's with most of these changes occurring in the Northern Hemisphere from the subtropics to high latitudes. The trend results are generally consistent with the prediction of chemistry climate models which include the reduction of ozone destroying substances beginning in the late 1980's mandated by the Montreal Protocol.

  7. A decade in diabetes specialist services, 2000 to 2011, in England: the views of consultant diabetologists and diabetes specialist nurses amidst persistent healthcare delivery change.

    PubMed

    Gosden, C A; Barnard, K; Williams, D R R; Tinati, T; Turner, B; Holt, R I G

    2015-12-01

    To assess the impact of continual major National Health Service reorganization on commissioning, organizational and delivery arrangements for secondary care diabetes services. To explore how consultant diabetologists and diabetes specialist nurses perceive the issues facing diabetes specialist services in 2011 and how these have changed in the preceding decade. We used a longitudinal case study approach that combined quantitative and qualitative methods. Five locations in England were purposively selected to represent the wider diabetes specialist community, and seven semi-structured interviews were conducted. Interviews were recorded, transcribed verbatim and analysed using Framework analysis. Findings were compared with and contrasted to results from national quantitative surveys of diabetes specialist services undertaken in 2000 and 2006. Clinicians viewed positively the expertise and commitment of multidisciplinary teams and their ability to adapt to new situations. Negative perceptions persisted throughout the decade, relating to the continual change that threatens to dismantle relationships and services which had taken many years to establish. Lack of resources, inadequate manpower planning and poor access to psychological support for people with diabetes remained constant themes from 2000 to 2011. A willingness to innovate and work differently to improve services was identified; however, clinicians must be supported through organizational changes to ensure people with diabetes receive high-quality care. The disruptive nature of organizational change was a recurrent theme throughout the decade. Periods of stability must exist within commissioning to allow relationships, which are key to integration, to be maintained and permit service improvements to develop. © 2015 The Authors. Diabetic Medicine © 2015 Diabetes UK.

  8. Breastfeeding: what changed after a decade?1.

    PubMed

    Toryiama, Áurea Tamami Minagawa; Fujimori, Elizabeth; Palombo, Claudia Nery Teixeira; Duarte, Luciane Simões; Borges, Ana Luiza Vilela; Chofakian, Christiane Borges do Nascimento

    2017-10-30

    to analyze the changes in prevalence, median duration and correlates of breastfeeding in a small city in São Paulo state, Brazil. analysis of two cross-sectional studies, conducted at intervals of one decade, with 261 and 302 children younger than two years, respectively. We used Kaplan-Meier survival analysis for calculation of the median duration of breastfeeding, and Cox regression for correlates analysis, with significance level of 5%. an increase of 33.4% in the prevalence of exclusive breastfeeding and 20.9% in breastfeeding was identified. Regarding the latter, the median duration increased from 7.2 to 12 months. In the most recent study, the median duration was lower in first-born children who used pacifiers, and it was not associated with breastfeeding incentive actions. advances in the prevalence and duration of breastfeeding were observed during the 10 year-period, however, pacifier use still remains associated to a shorter median duration of breastfeeding. Our findings contribute to highlighting the need for intensification of nursing actions in the promotion of breastfeeding, and discouragement regarding the use of pacifiers.

  9. Simulated decadal modes of the NH atmospheric circulation arising from intra-decadal variability, external forcing and slow-decadal climate processes

    NASA Astrophysics Data System (ADS)

    Lou, Jiale; Zheng, Xiaogu; Frederiksen, Carsten S.; Liu, Haibo; Grainger, Simon; Ying, Kairan

    2017-04-01

    A decadal variance decomposition method is applied to the Northern Hemisphere (NH) 500-hPa geopotential height (GPH) and the sea level pressure (SLP) taken from the last millennium (850-1850 AD) experiment with the coupled climate model CCSM4, to estimate the contribution of the intra-decadal variability to the inter-decadal variability. By removing the intra-decadal variability from the total inter-decadal variability, the residual variability is more likely to be associated with slowly varying external forcings and slow-decadal climate processes, and therefore is referred to as slow-decadal variability. The results show that the (multi-)decadal changes of the NH 500-hPa GPH are primarily dominated by slow-decadal variability, whereas the NH SLP field is primarily dominated by the intra-decadal variability. At both pressure levels, the leading intra-decadal modes each have features related to the El Niño-southern oscillation, the intra-decadal variability of the Pacific decadal oscillation (PDO) and the Arctic oscillation (AO); while the leading slow-decadal modes are associated with external radiative forcing (mostly with volcanic aerosol loadings), the Atlantic multi-decadal oscillation and the slow-decadal variability of AO and PDO. Moreover, the radiative forcing has much weaker effect to the SLP than that to the 500-hPa GPH.

  10. A decade of changes in brain volume and cognition.

    PubMed

    Aljondi, Rowa; Szoeke, Cassandra; Steward, Chris; Yates, Paul; Desmond, Patricia

    2018-05-09

    Brain atrophy can occur several decades prior to onset of cognitive impairments. However, few longitudinal studies have examined the relationship between brain volume changes and cognition over a long follow-up period in healthy elderly women. In the present study we investigate the relationship between whole brain and hippocampal atrophy rates and longitudinal changes in cognition, including verbal episodic memory and executive function, in older women. We also examine whether baseline brain volume predicts subsequent changes in cognitive performance over a 10-year period. A total of 60 individuals from the population-based Women's Healthy Ageing Project with a mean age at baseline of 59 years underwent 3T MRI. Of these, 40 women completed follow-up cognitive assessments, 23 of whom had follow-up MRI scans. Linear regression analysis was used to examine the relationship between brain atrophy and changes in verbal episodic memory and executive function over a 10-year period. The results show that baseline measurements of frontal and temporal grey matter volumes predict changes in verbal episodic memory performance, whereas hippocampal volume at baseline is associated with changes in executive function performance over a 10-year period of follow-ups. In addition, higher whole brain and hippocampal atrophy rates are correlated with a decline in verbal episodic memory. These findings indicate that in addition to atrophy rate, smaller regional grey matter volumes even 10 years prior is associated with increased rates of cognitive decline. This study suggests useful neuroimaging biomarkers for the prediction of cognitive decline in healthy elderly women.

  11. Role of internal variability in recent decadal to multidecadal tropical Pacific climate changes

    NASA Astrophysics Data System (ADS)

    Bordbar, Mohammad Hadi; Martin, Thomas; Latif, Mojib; Park, Wonsun

    2017-05-01

    While the Earth's surface has considerably warmed over the past two decades, the tropical Pacific has featured a cooling of sea surface temperatures in its eastern and central parts, which went along with an unprecedented strengthening of the equatorial trade winds, the surface component of the Pacific Walker Circulation (PWC). Previous studies show that this decadal trend in the trade winds is generally beyond the range of decadal trends simulated by climate models when forced by historical radiative forcing. There is still a debate on the origin of and the potential role that internal variability may have played in the recent decadal surface wind trend. Using a number of long control (unforced) integrations of global climate models and several observational data sets, we address the question as to whether the recent decadal to multidecadal trends are robustly classified as an unusual event or the persistent response to external forcing. The observed trends in the tropical Pacific surface climate are still within the range of the long-term internal variability spanned by the models but represent an extreme realization of this variability. Thus, the recent observed decadal trends in the tropical Pacific, though highly unusual, could be of natural origin. We note that the long-term trends in the selected PWC indices exhibit a large observational uncertainty, even hindering definitive statements about the sign of the trends.Plain Language SummaryWhile the Earth's surface has considerably warmed over the past two <span class="hlt">decades</span>, the tropical Pacific has featured a cooling of sea surface temperatures in its eastern and central parts, which went along with an unprecedented strengthening of the equatorial trade winds. Here we show that climate models simulate a high level of internal variability, so that the recent <span class="hlt">changes</span> in the tropical Pacific could still be due to natural processes.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.fs.usda.gov/treesearch/pubs/53054','TREESEARCH'); return false;" href="https://www.fs.usda.gov/treesearch/pubs/53054"><span><span class="hlt">Decadal</span> <span class="hlt">change</span> of forest biomass carbon stocks and tree demography in the Delaware River Basin</span></a></p> <p><a target="_blank" href="http://www.fs.usda.gov/treesearch/">Treesearch</a></p> <p>Bing Xu; Yude Pan; Alain F. Plante; Arthur Johnson; Jason Cole; Richard Birdsey</p> <p>2016-01-01</p> <p>Quantifying forest biomass carbon (C) stock <span class="hlt">change</span> is important for understanding forest dynamics and their feedbacks with climate <span class="hlt">change</span>. Forests in the northeastern U.S. have been a net carbon sink in recent <span class="hlt">decades</span>, but C accumulation in some northern hardwood forests has been halted due to the impact of emerging stresses such as invasive pests, land use <span class="hlt">change</span> and...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2011AGUFM.H42G..02S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2011AGUFM.H42G..02S"><span>Examining the last few <span class="hlt">decades</span> of global hydroclimate for evidence of anthropogenic <span class="hlt">change</span> amidst natural variability</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Seager, R.; Naik, N.; Ting, M.; Kushnir, Y.; Kelley, C. P.</p> <p>2011-12-01</p> <p>Climate models robustly predict that the deep tropics and mid-latitude-to-subpolar regions will moisten, and the subtropical dry zones both dry and expand, as a consequence of global warming driven by rising greenhouse gases. The models also predict that this transition to a more extreme climatological mean global hydroclimate should already be underway. Given the importance of these predictions it is an imperative that the climate science community assess whether there is evidence within the observational record that they are correct. This task is made difficult by the tremendous natural variability of the hydrological cycle on seasonal to multidecadal timescales. Here we will use instrumental observations, reanalyses, sea surface temperature forced atmosphere models and coupled model simulations, and a variety of methodologies, to attempt to separate global radiatively-forced hydroclimate <span class="hlt">change</span> from ongoing natural variability. The results will be applied to explain trends and recent events in <span class="hlt">key</span> regions such as Mexico, the United States and the Mediterranean. It is concluded that the signal of anthropogenic <span class="hlt">change</span> is small compared to the amplitude of natural variability but that it is a discernible contributor. Globally the evidence reveals that radiatively-forced hydroclimate <span class="hlt">change</span> is occurring with an amplitude and spatial pattern largely consistent with the predictions by IPCC AR4 models of hydroclimate <span class="hlt">change</span> to date. However it will also be shown that the radiatively-forced component does not in and of itself provide a useful prediction of near term hydroclimate <span class="hlt">change</span> because for many regions the amplitude of natural <span class="hlt">decadal</span> variability is as large or larger. Useful predictions need to account for how natural variability may evolve as well as forced <span class="hlt">change</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017EGUGA..19.6747L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017EGUGA..19.6747L"><span>Effect of climate variability and <span class="hlt">change</span> on winter haze over eastern China in recent <span class="hlt">decades</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Liao, Hong; Yang, Yang</p> <p>2017-04-01</p> <p>In recent years, eastern China has frequently experienced persistent and severe winter haze pollution episodes with high aerosol concentrations, which have affected half of the 1.3 billion people in China. In this work, the increases in wintertime aerosol concentrations and severe haze events in eastern China over 1985-2015 were quantified by using observed atmospheric visibility from the National Climatic Data Center Global Summary of Day database, observed PM2.5 concentrations from the network of China National Environmental Monitoring Centre (CNEMC), and simulated PM2.5 concentrations from the Goddard Earth-Observing System (GEOS) chemical transport model (GEOS-Chem). Observed winter haze days (defined as days with atmospheric visibility less than 10 km and relative humidity less than 80%) averaged over eastern China (105-122.5°E, 20-45°N) increased from 21 days in 1980 to 42 days in 2014. Observed severe haze days (defined as days with PM2.5 >150 μg m-3) occurred mainly over Northern China. Considering variations in both anthropogenic emissions and meteorological parameters, the GEOS-Chem model simulated an increasing trend in wintertime surface-layer PM2.5 concentrations of 10.5 (±6.2) μg m-3 <span class="hlt">decade</span>-1 over eastern China in the past <span class="hlt">decades</span>. Sensitivity studies showed that <span class="hlt">changes</span> in anthropogenic emissions and in climate contributed 87% and 17% to this increasing trend, respectively. Wintertime severe haze events over eastern China showed large interannual variations, driven by climate variability. Process analyses were performed to identify the <span class="hlt">key</span> meteorological parameters that determined the interannual variations of wintertime severe haze events.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5706605','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5706605"><span>Breastfeeding: what <span class="hlt">changed</span> after a <span class="hlt">decade</span>? 1</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Toryiama, Áurea Tamami Minagawa; Fujimori, Elizabeth; Palombo, Claudia Nery Teixeira; Duarte, Luciane Simões; Borges, Ana Luiza Vilela; Chofakian, Christiane Borges do Nascimento</p> <p>2017-01-01</p> <p>ABSTRACT Objective: to analyze the <span class="hlt">changes</span> in prevalence, median duration and correlates of breastfeeding in a small city in São Paulo state, Brazil. Method: analysis of two cross-sectional studies, conducted at intervals of one <span class="hlt">decade</span>, with 261 and 302 children younger than two years, respectively. We used Kaplan-Meier survival analysis for calculation of the median duration of breastfeeding, and Cox regression for correlates analysis, with significance level of 5%. Results: an increase of 33.4% in the prevalence of exclusive breastfeeding and 20.9% in breastfeeding was identified. Regarding the latter, the median duration increased from 7.2 to 12 months. In the most recent study, the median duration was lower in first-born children who used pacifiers, and it was not associated with breastfeeding incentive actions. Conclusions: advances in the prevalence and duration of breastfeeding were observed during the 10 year-period, however, pacifier use still remains associated to a shorter median duration of breastfeeding. Our findings contribute to highlighting the need for intensification of nursing actions in the promotion of breastfeeding, and discouragement regarding the use of pacifiers. PMID:29091126</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.fs.usda.gov/treesearch/pubs/40977','TREESEARCH'); return false;" href="https://www.fs.usda.gov/treesearch/pubs/40977"><span><span class="hlt">Changes</span> in early-successional hardwood forest area in four bird conservation regions across four <span class="hlt">decades</span></span></a></p> <p><a target="_blank" href="http://www.fs.usda.gov/treesearch/">Treesearch</a></p> <p>Sonja N. Oswalt; Kathleen E. Franzreb; David A. Buehler</p> <p>2012-01-01</p> <p>Early successional hardwood forests constitute important breeding habitat for many migratory songbirds. Declines in populations of these species suggest <span class="hlt">changes</span> in habitat availability either on the species’ wintering grounds or on their early successional breeding grounds. We used Forest Inventory and Analysis data from 11 states across four <span class="hlt">decades</span> to examine <span class="hlt">changes</span>...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://cfpub.epa.gov/si/si_public_record_report.cfm?dirEntryId=311024&keyword=physical+AND+chemistry&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=311024&keyword=physical+AND+chemistry&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 <span class="hlt">Decade</span> of Field <span class="hlt">Changing</span> Atmospheric Aerosol Research: Outcomes of EPA’s STAR Program</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>Conference: Gordon Research Conference in Atmospheric Chemistry, July 28 – August 2, 2013, VermontPresentation Type: PosterTitle: An Analysis of EPA’s STAR Program and a <span class="hlt">Decade</span> of Field <span class="hlt">Changing</span> Research in Atmospheric AerosolsAuthors: Kristina M. Wagstrom1,2, Sherri ...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015AGUFM.B21M..08I','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015AGUFM.B21M..08I"><span><span class="hlt">Changes</span> in terrestrial CO2 budget in Siberia in the past three <span class="hlt">decades</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Ichii, K.; Kondo, M.; Ueyama, M.; Ito, A.; Kobayashi, H.; Maksyutov, S. S.; Maki, T.; Nakamura, T.; Niwa, Y.; Patra, P. K.; Saeki, T.; Sato, H.; Sasai, T.; Saigusa, N.; Tian, H.; Yanagi, Y.; Zhang, B.</p> <p>2015-12-01</p> <p>Siberia is one of the regions where significant warming is proceeding, and the warming might cause <span class="hlt">changes</span> in terrestrial carbon cycle. We analyzed interannual and <span class="hlt">decadal</span> <span class="hlt">changes</span> in terrestrial CO2 fluxes in the regions using multiple data sets, such as empirically estimated carbon fluxes based on multiple eddy-covariance sites (empirical upscaling; Support Vector Regression with AsiaFlux data), satellite-based vegetation index data, multiple terrestrial carbon cycle models from Asia-MIP (e.g. BEAMS, Biome-BGC, SEIB-DGVM, and VISIT), and atmospheric inverse models (e.g. ACTM, JMA, NICAM-TM) for the past 3 <span class="hlt">decades</span> (1980s, 1990s, and 2000s). First, we checked the consistency in interannual variation of net carbon exchange between empirical upscaling and Asia-MIP model for 2001-2011 period, and found these two estimations show overall consistent interannual variation. Second, we analyzed net carbon exchange form Asia-MIP models and atmospheric inversions for the past three <span class="hlt">decades</span>, and found persistent increases in terrestrial CO2 sink from two estimates. Magnitudes of estimated terrestrial CO2 sinks are also consistent (e.g. Asia-MIP: 0.2 PgC yr-1 in 1980s and 0.3 PgC yr-1 in 2000s and Inversions: 0.2 PgC yr-1 in 1980s and 0.5 PgC/yr in 2000s). We further analyzed the cause of persistent increases in CO2 uptake in the region using Asia-MIP model outputs, and climate <span class="hlt">changes</span> (both warming and increases in water availability) and CO2 fertilization plays almost equivalent roles in sink increases. In addition, both gross primary productivity (GPP) and ecosystem respiration (RE) were increased, but increase in GPP was larger than that in RE.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://eric.ed.gov/?q=water+AND+politics&pg=2&id=EJ970873','ERIC'); return false;" href="https://eric.ed.gov/?q=water+AND+politics&pg=2&id=EJ970873"><span>Thirty Years of Education in China: Between <span class="hlt">Change</span> and No <span class="hlt">Change</span>--A Comparative Analysis of Four <span class="hlt">Key</span> Documents on Education Policy</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>Wenbin, Hu</p> <p>2012-01-01</p> <p>This article reviews the education reform and development footprints in China by analyzing four <span class="hlt">key</span> education policy documents in the past three <span class="hlt">decades</span>. The conclusion is that the reform and development of China's educational establishment have provided excellent support for the operations of China's political and economic systems. The reality is…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/26486804','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/26486804"><span>Continent-scale global <span class="hlt">change</span> attribution in European birds - combining annual and <span class="hlt">decadal</span> time scales.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Jørgensen, Peter Søgaard; Böhning-Gaese, Katrin; Thorup, Kasper; Tøttrup, Anders P; Chylarecki, Przemysław; Jiguet, Frédéric; Lehikoinen, Aleksi; Noble, David G; Reif, Jiri; Schmid, Hans; van Turnhout, Chris; Burfield, Ian J; Foppen, Ruud; Voříšek, Petr; van Strien, Arco; Gregory, Richard D; Rahbek, Carsten</p> <p>2016-02-01</p> <p>Species attributes are commonly used to infer impacts of environmental <span class="hlt">change</span> on multiyear species trends, e.g. <span class="hlt">decadal</span> <span class="hlt">changes</span> in population size. However, by themselves attributes are of limited value in global <span class="hlt">change</span> attribution since they do not measure the <span class="hlt">changing</span> environment. A broader foundation for attributing species responses to global <span class="hlt">change</span> may be achieved by complementing an attributes-based approach by one estimating the relationship between repeated measures of organismal and environmental <span class="hlt">changes</span> over short time scales. To assess the benefit of this multiscale perspective, we investigate the recent impact of multiple environmental <span class="hlt">changes</span> on European farmland birds, here focusing on climate <span class="hlt">change</span> and land use <span class="hlt">change</span>. We analyze more than 800 time series from 18 countries spanning the past two <span class="hlt">decades</span>. Analysis of long-term population growth rates documents simultaneous responses that can be attributed to both climate <span class="hlt">change</span> and land-use <span class="hlt">change</span>, including long-term increases in populations of hot-dwelling species and declines in long-distance migrants and farmland specialists. In contrast, analysis of annual growth rates yield novel insights into the potential mechanisms driving long-term climate induced <span class="hlt">change</span>. In particular, we find that birds are affected by winter, spring, and summer conditions depending on the distinct breeding phenology that corresponds to their migratory strategy. Birds in general benefit from higher temperatures or higher primary productivity early on or in the peak of the breeding season with the largest effect sizes observed in cooler parts of species' climatic ranges. Our results document the potential of combining time scales and integrating both species attributes and environmental variables for global <span class="hlt">change</span> attribution. We suggest such an approach will be of general use when high-resolution time series are available in large-scale biodiversity surveys. © 2015 John Wiley & Sons Ltd.</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('http://adsabs.harvard.edu/abs/2017EGUGA..1915977C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017EGUGA..1915977C"><span>Multi-<span class="hlt">decadal</span> frontal <span class="hlt">change</span> rates of tidewater glaciers in the Canadian Arctic Archipelago</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Cook, Alison; Copland, Luke; Stokes, Chris; Bentley, Mike</p> <p>2017-04-01</p> <p>Recent studies of post-2000 observational data have shown variability in the dynamic ice discharge of tidewater glaciers throughout the Canadian Arctic Archipelago (CAA). Expanding this to all tidewater glaciers in the region on a <span class="hlt">decadal</span> time scale using earlier records can help identify when glacier retreat began, and determine longer-term temporal trends in mass balance. Our study shows that over 94% of 300 tidewater glaciers in the CAA (from southern Baffin Island to Ellesmere Island, excluding those on the northern coast) have retreated since the earliest observational records (aerial photographs acquired in 1958-1960). Mean overall length <span class="hlt">change</span> rate of the 211 glaciers in the Queen Elizabeth Islands (QEI) is -9.3 ma-1 (± 1.38 SE), and of the 89 glaciers on Baffin and Bylot Islands (BBI) is -7.1 ma-1 (± 0.72 SE). Mean frontal widths of tidewater glaciers in the QEI are greater than those on islands to the south, resulting in greater mean area loss from this region. Each glacier has 6 frontal positions digitised from a range of image sources at approximately <span class="hlt">decadal</span> intervals. Length <span class="hlt">change</span> rates have been calculated across each time interval for each glacier, based on area <span class="hlt">changes</span> divided by glacier frontal width. Results indicate a similar temporal pattern throughout the region, whereby glaciers show minimal <span class="hlt">change</span> in early years with retreat rates slowly increasing, followed by acceleration in retreat rates since the late 1990s. Mean <span class="hlt">change</span> rates in the QEI and BBI in the 1960s were -6.92 ma-1 and -0.51 ma-1 respectively, increasing to -28.96 ma-1 and -24.84 ma-1 since 2010. The same trend (at differing magnitudes) has been observed within each latitudinal degree band, and for glaciers of differing frontal widths. Further observations of glacier <span class="hlt">changes</span> and links to climate <span class="hlt">change</span> are revealed on the poster.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017NatCC...7..200K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017NatCC...7..200K"><span>Regional dry-season climate <span class="hlt">changes</span> due to three <span class="hlt">decades</span> of Amazonian deforestation</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Khanna, Jaya; Medvigy, David; Fueglistaler, Stephan; Walko, Robert</p> <p>2017-02-01</p> <p>More than 20% of the Amazon rainforest has been cleared in the past three <span class="hlt">decades</span>, triggering important hydroclimatic <span class="hlt">changes</span>. Small-scale (a few kilometres) deforestation in the 1980s has caused thermally triggered atmospheric circulations that increase regional cloudiness and precipitation frequency. However, these circulations are predicted to diminish as deforestation increases. Here we use multi-<span class="hlt">decadal</span> satellite records and numerical model simulations to show a regime shift in the regional hydroclimate accompanying increasing deforestation in Rondônia, Brazil. Compared with the 1980s, present-day deforested areas in downwind western Rondônia are found to be wetter than upwind eastern deforested areas during the local dry season. The resultant precipitation <span class="hlt">change</span> in the two regions is approximately +/-25% of the deforested area mean. Meso-resolution simulations robustly reproduce this transition when forced with increasing deforestation alone, showing that large-scale climate variability plays a negligible role. Furthermore, deforestation-induced surface roughness reduction is found to play an essential role in the present-day dry-season hydroclimate. Our study illustrates the strong scale sensitivity of the climatic response to Amazonian deforestation and suggests that deforestation is sufficiently advanced to have caused a shift from a thermally to a dynamically driven hydroclimatic regime.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4628714','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4628714"><span>Over-the-Counter Hearing Aids: A Lost <span class="hlt">Decade</span> for <span class="hlt">Change</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>Chan, Zoe Yee Ting; McPherson, Bradley</p> <p>2015-01-01</p> <p>Background. Hearing aids sold directly to consumers in retail stores or through the internet, without individual prescription by audiological professionals, are termed over-the-counter (OTC) devices. This study aimed to determine whether there was any <span class="hlt">change</span> in the electroacoustic characteristics of OTC devices compared to research carried out a <span class="hlt">decade</span> earlier. The previous results indicated that most OTC devices were low-frequency-emphasis devices and were unsuitable for elderly people with presbycusis, who were likely to be the major consumers of these products. Methods. Ten OTC devices were selected and their electroacoustic performance was measured. Appropriate clients for the OTC devices were derived, using four linear prescription formulae, and OTC suitability for elderly persons with presbycusis was investigated. Results. OTC electroacoustic characteristics were similar to those in the earlier study. Most OTC devices were not acoustically appropriate for potential consumers with presbycusis. Although several of the devices could match prescriptive targets for individuals with presbycusis, their poor electroacoustic performance—including ineffective volume control function, high equivalent input noise, and irregular frequency response—may override their potential benefit. Conclusion. The low-cost OTC devices were generally not suitable for the main consumers of these products, and there has been little improvement in the appropriateness of these devices over the past <span class="hlt">decade</span>. PMID:26557701</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017Geomo.281....1P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017Geomo.281....1P"><span><span class="hlt">Decadal</span> <span class="hlt">changes</span> in North Atlantic atmospheric circulation patterns recorded by sand spits since 1800 CE</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Poirier, Clément; Tessier, Bernadette; Chaumillon, Éric; Bertin, Xavier; Fruergaard, Mikkel; Mouazé, Dominique; Noël, Suzanne; Weill, Pierre; Wöppelmann, Guy</p> <p>2017-03-01</p> <p>Present-day coastal barriers represent around 15% of the world's oceanic shorelines, and play an important role as early warning indicators of environmental <span class="hlt">change</span>. Among them, wave-dominated barriers are dynamic landforms that tend to migrate landward in response to storms and sea-level <span class="hlt">change</span>. High rates of sediment supply can locally offset the global retrogradation trend, providing valuable records of past environmental <span class="hlt">change</span> occurring on transgressive coasts. However, geochronological control limits the temporal resolution of such records to millennial or centennial timescales, and the <span class="hlt">decadal</span> or even faster response of wave-built barriers to historical climate <span class="hlt">changes</span> is therefore poorly understood. In this study, we show that shoreline dynamics of sand spits reconstructed from old cartographic documents has been synchronous on both margins of the North Atlantic Ocean since about 1800 CE. Spit growth accelerated drastically during three periods lasting about 15 years, characterised by positive North Atlantic Oscillation (NAO) and negative East Atlantic-West Russia (EA-WR) atmospheric circulation patterns. These <span class="hlt">changes</span> are in phase with periods of increased volcanic activity. We use a high-resolution wave hindcast (1948-2014 CE) in a reference area to confirm the association between NAO and EA-WR as a proxy for offshore and nearshore wave height and for associated longshore sediment transport (LST) involved in spit growth. A 24-month lagged correlation between sediment transport and volcanic aerosol optical thickness (concentration of ashes in the atmosphere) is observed, suggesting that spit shoreline dynamics at the <span class="hlt">decadal</span> timescale is partially forced by external climate drivers via cascading effects on atmospheric circulation patterns and wave climate. Our results imply that NAO variability alone is not sufficient to understand the evolution of wave-built coastal environments. The associated sediment record can be used to reconstruct multi-<span class="hlt">decadal</span></p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4522805','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4522805"><span>Climate <span class="hlt">change</span> and <span class="hlt">decadal</span> shifts in the phenology of larval fishes in the California Current ecosystem</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Asch, Rebecca G.</p> <p>2015-01-01</p> <p>Climate <span class="hlt">change</span> has prompted an earlier arrival of spring in numerous ecosystems. It is uncertain whether such <span class="hlt">changes</span> are occurring in Eastern Boundary Current Upwelling ecosystems, because these regions are subject to natural <span class="hlt">decadal</span> climate variability, and regional climate models predict seasonal delays in upwelling. To answer this question, the phenology of 43 species of larval fishes was investigated between 1951 and 2008 off southern California. Ordination of the fish community showed earlier phenological progression in more recent years. Thirty-nine percent of seasonal peaks in larval abundance occurred earlier in the year, whereas 18% were delayed. The species whose phenology became earlier were characterized by an offshore, pelagic distribution, whereas species with delayed phenology were more likely to reside in coastal, demersal habitats. Phenological <span class="hlt">changes</span> were more closely associated with a trend toward earlier warming of surface waters rather than <span class="hlt">decadal</span> climate cycles, such as the Pacific <span class="hlt">Decadal</span> Oscillation and North Pacific Gyre Oscillation. Species with long-term advances and delays in phenology reacted similarly to warming at the interannual time scale as demonstrated by responses to the El Niño Southern Oscillation. The trend toward earlier spawning was correlated with <span class="hlt">changes</span> in sea surface temperature (SST) and mesozooplankton displacement volume, but not coastal upwelling. SST and upwelling were correlated with delays in fish phenology. For species with 20th century advances in phenology, future projections indicate that current trends will continue unabated. The fate of species with delayed phenology is less clear due to differences between Intergovernmental Panel on Climate <span class="hlt">Change</span> models in projected upwelling trends. PMID:26159416</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://files.eric.ed.gov/fulltext/ED040096.pdf','ERIC'); return false;" href="http://files.eric.ed.gov/fulltext/ED040096.pdf"><span>Tradition and <span class="hlt">Change</span> in the Social Studies: Some Observations on a <span class="hlt">Decade</span> of Reform.</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>Lunstrum, John P.</p> <p></p> <p>Trends in social studies education in the 1960's which appeared significant and which may well affect the developments of the next <span class="hlt">decade</span> include: (1) curriculum evangelism--the zealous, uncritical pursuit of fashionable educational ideas--and the institutionalization of innovative <span class="hlt">changes</span>, (2) restraints on intellectual freedom by the radical…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://eric.ed.gov/?q=COMPARATIVE+AND+LAW&pg=3&id=EJ1053789','ERIC'); return false;" href="https://eric.ed.gov/?q=COMPARATIVE+AND+LAW&pg=3&id=EJ1053789"><span>Reflections on a <span class="hlt">Decade</span> of <span class="hlt">Changes</span> in Homeschooling and the Homeschooled into Higher Education</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>Gloeckner, Gene W.; Jones, Paul</p> <p>2013-01-01</p> <p>This article reviews selected research on successes of homeschooled students over the past <span class="hlt">decade</span>. The article raises several methods issues, especially related to sampling issues and recent <span class="hlt">changes</span> in some state laws. In addition the article reviews research collected from college admission's officers' on their perceptions and attitudes relate to…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFMOS31B2016S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFMOS31B2016S"><span>Identifying <span class="hlt">Decadal</span> to Multi-<span class="hlt">decadal</span> Variability in the Pacific by Empirical Mode Decomposition</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Sommers, L. A.; Hamlington, B.; Cheon, S. H.</p> <p>2016-12-01</p> <p>Large scale climate variability in the Pacific Ocean like that associated with ENSO and the Pacific <span class="hlt">Decadal</span> Oscillation (PDO) has been shown to have a significant impact on climate and sea level across a range of timescales. The <span class="hlt">changes</span> related to these climate signals have worldwide impacts on fisheries, weather, and precipitation patterns among others. Understanding these inter-annual to multi-<span class="hlt">decadal</span> oscillations is imperative to longer term climate forecasts and understanding how climate will behave, and its effect on <span class="hlt">changes</span> in sea level. With a 110-year reconstruction of sea level, we examine <span class="hlt">decadal</span> to multi-<span class="hlt">decadal</span> variability seen in the sea level fluctuations in the Pacific Ocean. Using empirical mode decomposition (EMD), we break down regional sea level into a series of intrinsic mode functions (IMFs) and attempt attribution of these IMFs to specific climate modes of variability. In particular, and not unexpectedly, we identify IMFs associated with the PDO, finding correlations between the PDO Index and IMFs in the Pacific Ocean upwards of 0.6-0.8 over the 110-year reconstructed record. Perhaps more significantly, we also find evidence of a longer multi-<span class="hlt">decadal</span> signal ( 50-60 years) in the higher order IMFs. This lower frequency variability has been suggested in previous literature as influencing GMSL, but here we find a regional pattern associated with this multi-<span class="hlt">decadal</span> signal. By identifying and separating these periodic climate signals, we can gain a better understanding of how the sea level variability associated with these modes can impact sea level on short timescales and serve to exacerbate the effects of long-term sea level <span class="hlt">change</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013EGUGA..15.8353C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013EGUGA..15.8353C"><span>Winter precipitation <span class="hlt">change</span> in South China in recent <span class="hlt">decades</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Cai, Jingning</p> <p>2013-04-01</p> <p>Precipitation <span class="hlt">change</span> is one of important climate researches in China, but winter precipitation variation in South China has not been studied so frequently. In China, it is rainy when hot; so summer precipitation is usually one focus in research, esp. in South China. However, winter precipitation and its <span class="hlt">change</span> influence people profoundly in South China, also. The most recent example is what happened over South China in winter 2008. In this winter, millions of people suffered from the unusual cold and snowy winter. It led to huge loss in economy and traffic as well. Roads closed and railway stations were jammed and crowded with people; many planes were grounded for heavy snow and bad weather. Transmission lines faulted in the mountains. The ommunication signals were affected. Everyday food supply including vegetables and meats had to be delayed or interrupted. In some city even water supply was interrupted. And garbage in the city was piled up. Just in this winter the snow depth and coverage area in many places in South China broke or equaled the historical records. In fact, it isn't the only one unusual winter precipitation event in South China. Since 1950s, several freezing and snowy winters struck the South in China. In this research, winter precipitation <span class="hlt">change</span> in recent years in South China has been discussed based on the precipitation observations. The associated large scale atmospheric circulation <span class="hlt">change</span> is also analyzed. It is found that snowy winter in South China hardly comes in most periods of 2000s, but in recent <span class="hlt">decades</span> this heavy snow in winter has appeared several times as observations shows. This phenomenon could be related to the large scale atmospheric circulation <span class="hlt">change</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015AGUFM.H53G1731Z','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015AGUFM.H53G1731Z"><span>Bottom Topographic <span class="hlt">Changes</span> of Poyang Lake During Past <span class="hlt">Decade</span> Using Multi-temporal Satellite Images</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Zhang, S.</p> <p>2015-12-01</p> <p>Poyang Lake, as a well-known international wetland in the Ramsar Convention List, is the largest freshwater lake in China. It plays crucial ecological role in flood storage and biological diversity. Poyang Lake is facing increasingly serious water crises, including seasonal dry-up, decreased wetland area, and water resource shortage, all of which are closely related to progressive bottom topographic <span class="hlt">changes</span> over recent years. Time-series of bottom topography would contribute to our understanding of the lake's evolution during the past several <span class="hlt">decades</span>. However, commonly used methods for mapping bottom topography fail to frequently update quality bathymetric data for Poyang Lake restricted by weather and accessibility. These deficiencies have limited our ability to characterize the bottom topographic <span class="hlt">changes</span> and understanding lake erosion or deposition trend. To fill the gap, we construct a <span class="hlt">decadal</span> bottom topography of Poyang Lake with a total of 146 time series medium resolution satellite images based on the Waterline Method. It was found that Poyang Lake has eroded with a rate of -14.4 cm/ yr from 2000 to 2010. The erosion trend was attributed to the impacts of human activities, especially the operation of the Three Gorge Dams, sand excavation, and the implementation of water conservancy project. A <span class="hlt">decadal</span> quantitative understanding bottom topography of Poyang Lake might provide a foundation to model the lake evolutionary processes and assist both researchers and local policymakers in ecological management, wetland protection and lake navigation safety.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013AGUFM.H53J..06L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013AGUFM.H53J..06L"><span>Projecting Global <span class="hlt">Decadal</span> <span class="hlt">Change</span> in Water Supply for Strategic Planning: Window Size Sensitivity in CMIP5 GCMs</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Luck, M.; Landis, M.; Gassert, F.; Luo, T.; Reig, P.</p> <p>2013-12-01</p> <p>Climate adaptation and strategic planning by states, corporations, and long-term investors require reliable information on the range of possible climatic <span class="hlt">changes</span>. However, most decision makers are incapable of planning over the century-scale time horizons for which global climate models (GCMs) are developed. Even the most forward-looking actors rarely consider scenarios more than several <span class="hlt">decades</span> into the future. The mismatch in model design and practical demands poses a challenge in extracting useful information on the <span class="hlt">decadal</span> scale from global climate <span class="hlt">change</span> models. Here, we explore options and limitations in generating <span class="hlt">decadal</span> water supply <span class="hlt">change</span> projections, as evaluated for the World Resources Institute's Aqueduct project's estimates of future <span class="hlt">change</span> in water stress. Our approach uses an ensemble of six CMIP5 GCMs, selected to represent a broad lineage of models that best reproduce the mean and standard deviation of recent streamflow records in 18 large river basins, bias corrected to GLDAS-2.0 runoff. We examine sensitivity of point estimates of climate normal supply and water supply variability (interannual and seasonal) at the years 2020, 2030, and 2040, with a focus on using temporal windows of different lengths (11-, 21-, and 31-years) to generate the point estimates. With the aim of creating practical information for non-expert audiences, we will discuss the persistent question of 'how can we balance uncertainty and usability in designing scientific data products?'</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70111438','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70111438"><span>Improving understanding of near-term barrier island evolution through multi-<span class="hlt">decadal</span> assessment of morphologic <span class="hlt">change</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>Lentz, Erika E.; Hapke, Cheryl J.; Stockdon, Hilary F.; Hehre, Rachel E.</p> <p>2013-01-01</p> <p>Observed morphodynamic <span class="hlt">changes</span> over multiple <span class="hlt">decades</span> were coupled with storm-driven run-up characteristics at Fire Island, New York, to explore the influence of wave processes relative to the impacts of other coastal <span class="hlt">change</span> drivers on the near-term evolution of the barrier island. Historical topography was generated from digital stereo-photogrammetry and compared with more recent lidar surveys to quantify near-term (<span class="hlt">decadal</span>) morphodynamic <span class="hlt">changes</span> to the beach and primary dune system between the years 1969, 1999, and 2009. Notably increased profile volumes were observed along the entirety of the island in 1999, and likely provide the eolian source for the steady dune crest progradation observed over the relatively quiescent <span class="hlt">decade</span> that followed. Persistent patterns of erosion and accretion over 10-, 30-, and 40-year intervals are attributable to variations in island morphology, human activity, and variations in offshore bathymetry and island orientation that influence the wave energy reaching the coast. Areas of documented long-term historical inlet formation and extensive bayside marsh development show substantial landward translation of the dune–beach profile over the near-term period of this study. Correlations among areas predicted to overwash, observed elevation <span class="hlt">changes</span> of the dune crestline, and observed instances of overwash in undeveloped segments of the barrier island verify that overwash locations can be accurately predicted in undeveloped segments of coast. In fact, an assessment of 2012 aerial imagery collected after Hurricane Sandy confirms that overwash occurred at the majority of near-term locations persistently predicted to overwash. In addition to the storm wave climate, factors related to variations within the geologic framework which in turn influence island orientation, offshore slope, and sediment supply impact island behavior on near-term timescales.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29904134','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29904134"><span>Hydroclimatic <span class="hlt">changes</span> of Lake Bosten in Northwest China during the last <span class="hlt">decades</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Yao, Junqiang; Chen, Yaning; Zhao, Yong; Yu, Xiaojing</p> <p>2018-06-14</p> <p>Bosten Lake, the largest inland freshwater lake in China, has experienced drastic <span class="hlt">change</span> over the past five <span class="hlt">decades</span>. Based on the lake water balance model and climate elasticity method, we identify annual <span class="hlt">changes</span> in the lake's water components during 1961-2016 and investigate its water balance. We find a complex pattern in the lake's water: a decrease (1961-1987), a rapid increase (1988-2002), a drastic decrease (2003-2012), and a recent drastic increase (2013-2016). We also estimated the lake's water balance, finding that the drastic <span class="hlt">changes</span> are caused by a climate-driven regime shift coupled with human disturbance. The <span class="hlt">changes</span> in the lake accelerated after 1987, which may have been driven by regional climate wetting. During 2003 to 2012, implementation of the ecological water conveyance project (EWCP) significantly increased the lake's outflow, while a decreased precipitation led to an increased drought frequency. The glacier retreating trend accelerated by warming, and caused large variations in the observed lake's <span class="hlt">changes</span> in recent years. Furthermore, wastewater emissions may give rise to water degradation, human activity is completely <span class="hlt">changing</span> the natural water cycle system in the Bosten Lake. Indeed, the future of Bosten Lake is largely dependent on mankind.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/25104833','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/25104833"><span>Suicide rates in children aged 10-14 years worldwide: <span class="hlt">changes</span> in the past two <span class="hlt">decades</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Kõlves, Kairi; De Leo, Diego</p> <p>2014-10-01</p> <p>Limited research is focused on suicides in children aged below 15 years. To analyse worldwide suicide rates in children aged 10-14 years in two <span class="hlt">decades</span>: 1990-1999 and 2000-2009. Suicide data for 81 countries or territories were retrieved from the World Health Organization Mortality Database, and population data from the World Bank data-set. In the past two <span class="hlt">decades</span> the suicide rate per 100 000 in boys aged 10-14 years in 81 countries has shown a minor decline (from 1.61 to 1.52) whereas in girls it has shown a slight increase (from 0.85 to 0.94). Although the average rate has not <span class="hlt">changed</span> significantly, rates have decreased in Europe and increased in South America. The suicide rates remain critical for boys in some former USSR republics. The <span class="hlt">changes</span> may be related to economic recession and its impact on children from diverse cultural backgrounds, but may also be due to improvements in mortality registration in South America. Royal College of Psychiatrists.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFMOS43C..03S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFMOS43C..03S"><span>The impact of multi-<span class="hlt">decadal</span> sub-surface circulation <span class="hlt">changes</span> on sea surface chlorophyll patterns in the tropical Pacific</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Schollaert Uz, S.; Busalacchi, A. J.; Smith, T. M.; Evans, M. N.; Brown, C.; Hackert, E. C.; Wang, X.</p> <p>2016-12-01</p> <p>The tropical Pacific is a region of strong forcing where physical oceanography primarily controls biological variability over the seasonal to interannual time scales observed since dedicated ocean color satellite remote sensing began in 1997. To quantify how multi-<span class="hlt">decadal</span>, climate-scale <span class="hlt">changes</span> impact marine biological dynamics, we used the correlation with sea-surface temperature and height to reconstruct a 50-year time series of surface chlorophyll concentrations. The reconstruction demonstrates greatest skill away from the coast and within 10o of the equator where chlorophyll variance is greatest and primarily associated with El Niño Southern Oscillation (ENSO) dynamics and secondarily associated with <span class="hlt">decadal</span> variability. We observe significant basin-wide differences between east and central Pacific events when the El Niño events are strong: chlorophyll increases with La Niña and decreases with El Niño, with larger declines east of 180o for remotely-forced east Pacific events and west of 180o for locally-forced central Pacific events. Chlorophyll variations also reflect the physical dynamics of Pacific <span class="hlt">decadal</span> variability with small but significant differences between cool and warm eras: consistent with advection variability west of 180o and likely driven by subsurface <span class="hlt">changes</span> in the nutricline depth between 110-140oW. Comparisons with output from a fully-coupled biogeochemical model support the hypothesis that this anomalous region is controlled by lower frequency <span class="hlt">changes</span> in subsurface circulation patterns that transport nutrients to the surface. Basin-wide chlorophyll distributions exhibiting spatial heterogeneity in response to multi-<span class="hlt">decadal</span> climate forcing imply similar long-term <span class="hlt">changes</span> in phytoplankton productivity, with implications for the marine food web and the ocean's role as a carbon sink.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/19087944','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/19087944"><span><span class="hlt">Decadal</span> climate prediction (project GCEP).</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Haines, Keith; Hermanson, Leon; Liu, Chunlei; Putt, Debbie; Sutton, Rowan; Iwi, Alan; Smith, Doug</p> <p>2009-03-13</p> <p><span class="hlt">Decadal</span> prediction uses climate models forced by <span class="hlt">changing</span> greenhouse gases, as in the International Panel for Climate <span class="hlt">Change</span>, 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. <span class="hlt">Decadal</span> 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 <span class="hlt">Decadal</span> Prediction System (DePreSys) and implemented it on several NERC institute compute clusters in order to study a wider range of initial condition impacts on <span class="hlt">decadal</span> 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 <span class="hlt">decadal</span> climate predictability.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2010APS..MAR.S1091H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2010APS..MAR.S1091H"><span>Giant-Magnetoresistance(GMR) Siegel <span class="hlt">KEY</span> FIRST Experimental Discovery <span class="hlt">Decade</span>-Earlier PRE-``Fert"-``Gruenberg" in Nuc"el"ar ``Super"alloys: Science?;``SEANCE!!!; Ethics?; SHMETHICS!!!</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Hoffman, R.; Siegel, E.</p> <p>2010-03-01</p> <p>(So MIScalled) ``Fert"-``Grunberg"[PRL(1988;1989)] GMR 2007 physics Nobel/Wolf/Japan-Prizes VS. <span class="hlt">decade</span>-earlier(1973-1977) <span class="hlt">KEY</span> FIRST Siegel at:Westin"kl"ouse/PSEG/IAEA/ABB[google:``Martin Ebner"(94-04) in financial media]/Vattenfall/Wallenbergs/nuc"el"ar-DoE Labs[at flickr.com, search on ``Giant- Magnotoresistance''; find: Intl.Conf.Mag.Alloys & Oxides(ICMAO), Haifa(Aug./1977); J.Mag.Mag.Mtls,(JMMM)7,312(1978)``unavailable: not yet scanned''/modified(last R(H) GMR Figs(7;8) deleted!!!) on JMMM/Reed-Elsevier website until 7/29/08 conveniently one- half-year after last (Nobel)award(12/2007); conveniently effectively deleted!!!; google: ``If Leaks Could Kill''; many APS/MRS Mtgs(1970s)<<<1988/1989] <span class="hlt">decade</span>-earlier GMR: (1978)<<< (1988); 1988-1978 =10 years = one full decadeprecedence!!!] first experimental discovery in (so MIScalled) ``super''alloys [182/82, Hastelloy-X, 600, 690(!!!), Stainless-Steels: ANY/ALL!!!] generic endemic Wigner's[JAP,17,857(1946)]- disease/Ostwald-ripening/spinodal-decomposition/overageing- embrittlement/ thermo-mechanical-INstability!</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=20110015504&hterms=browning&qs=N%3D0%26Ntk%3DAll%26Ntx%3Dmode%2Bmatchall%26Ntt%3Dbrowning','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=20110015504&hterms=browning&qs=N%3D0%26Ntk%3DAll%26Ntx%3Dmode%2Bmatchall%26Ntt%3Dbrowning"><span>Browning in Desert Boundaries in Asia in Recent <span class="hlt">Decades</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Jeong, Su-Jong; Ho, Chang-Hoi; Brown, Molly E.; Kug, Jong-Seong; Piao, Shilong</p> <p>2011-01-01</p> <p>In this study, the <span class="hlt">changes</span> in desert boundaries in Asia (Gobi, Karakum, Lut, Taklimakan, and Thar deserts) during the growing season (April October) in the years 1982 2008 were investigated by analyzing the normalized difference vegetation index (NDVI), precipitation, and temperature. In the desert boundary regions, the domain mean NDVI values increased by 7.2% per <span class="hlt">decade</span> in 1982 1998 but decreased by 6.8% per <span class="hlt">decade</span> thereafter. Accordingly, the bare soil areas (or nonvegetated areas) of the inside of the desert boundaries contracted by 9.8% per <span class="hlt">decade</span> in the 1990s and expanded by 8.7% per <span class="hlt">decade</span> in the 2000s. It is noted that the five deserts experience nearly simultaneous NDVI <span class="hlt">changes</span> although they cover a very diverse area of Asia. In contrast, <span class="hlt">changes</span> in temperature and precipitation in the deserts show rather diverse results. In desert boundaries located along 40 N (Gobi, Taklimakan, and Karakum), the <span class="hlt">decadal</span> <span class="hlt">changes</span> in vegetation greenness were mainly related to regional climate during the entire analysis period. Precipitation increased in the 1990s, providing favorable conditions for vegetation growth (i.e., greening), but precipitation reduced (19 mm per <span class="hlt">decade</span>) and warming intensified (0.7 C per <span class="hlt">decade</span>) in the 2000s, causing less moisture to be available for vegetation growth (i.e., browning). In desert boundaries below 40 N (Lut and Thar), although an increase in precipitation (8 mm per <span class="hlt">decade</span>) led to greening in the 1990s, local <span class="hlt">changes</span> in precipitation and temperature did not necessarily cause browning in the 2000s. Observed multidecadal <span class="hlt">changes</span> in vegetation greenness in the present study suggest that under significant global and/or regional warming, <span class="hlt">changes</span> in moisture availability for vegetation growth in desert boundaries are an important factor when understanding <span class="hlt">decadal</span> <span class="hlt">changes</span> in areas vulnerable to desertification over Asia.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018ClDy..tmp...54T','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018ClDy..tmp...54T"><span>Forced <span class="hlt">decadal</span> <span class="hlt">changes</span> in the East Asian summer monsoon: the roles of greenhouse gases and anthropogenic aerosols</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Tian, Fangxing; Dong, Buwen; Robson, Jon; Sutton, Rowan</p> <p>2018-02-01</p> <p>Since the mid-1990s precipitation trends over eastern China display a dipole pattern, characterized by positive anomalies in the south and negative anomalies in the north, named as the Southern-Flood-Northern-Drought (SFND) pattern. This work investigates the drivers of <span class="hlt">decadal</span> <span class="hlt">changes</span> of the East Asian summer monsoon (EASM), and the dynamical mechanisms involved, by using a coupled climate model (specifically an atmospheric general circulation model coupled to an ocean mixed layer model) forced by <span class="hlt">changes</span> in (1) anthropogenic greenhouse gases (GHG), (2) anthropogenic aerosol (AA) and (3) the combined effects of both GHG and AA (All Forcing) between two periods across the mid-1990s. The model experiment forced by <span class="hlt">changes</span> in All Forcing shows a dipole pattern of response in precipitation over China that is similar to the observed SFND pattern across the mid-1990s, which suggests that anthropogenic forcing <span class="hlt">changes</span> played an important role in the observed <span class="hlt">decadal</span> <span class="hlt">changes</span>. Furthermore, the experiments with separate forcings indicate that GHG and AA forcing dominate different parts of the SFND pattern. In particular, <span class="hlt">changes</span> in GHG increase precipitation over southern China, whilst <span class="hlt">changes</span> in AA dominate in the drought conditions over northern China. Increases in GHG cause increased moisture transport convergence over eastern China, which leads to increased precipitation. The AA forcing <span class="hlt">changes</span> weaken the EASM, which lead to divergent wind anomalies over northern China and reduced precipitation.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/26169046','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/26169046"><span>A <span class="hlt">Decade</span> of <span class="hlt">Change</span>: Training and Career Paths of Cardiothoracic Surgery Residents 2003 to 2014.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Stephens, Elizabeth H; Odell, David; Stein, William; LaPar, Damien J; DeNino, Walter F; Aftab, Muhammad; Berfield, Kathleen; Eilers, Amanda L; Groth, Shawn; Lazar, John F; Robich, Michael P; Shah, Asad A; Smith, Danielle A; Stock, Cameron; Tchantchaleishvili, Vakhtang; Mery, Carlos M; Turek, Joseph W; Salazar, Jorge; Nguyen, Tom C</p> <p>2015-10-01</p> <p>During the past <span class="hlt">decade</span>, cardiothoracic surgery (CTS) education has undergone tremendous <span class="hlt">change</span> with the advent of new technologies and the implementation of integrated programs, to name a few. The goal of this study was to assess how residents' career paths, training, and perceptions <span class="hlt">changed</span> during this period. The 2006 to 2014 surveys accompanying the Thoracic Surgery Residents Association/Thoracic Surgery Directors' Association in-training examination taken by CTS residents were analyzed, along with a 2003 survey of graduating CTS residents. Of 2,563 residents surveyed, 2,434 (95%) responded. During the <span class="hlt">decade</span>, fewer residents were interested in mixed adult cardiac/thoracic practice (20% in 2014 vs 52% in 2003, p = 0.004), more planned on additional training (10% in 2003 vs 41% to 47% from 2011 to 2014), and the frequent use of simulation increased from 1% in 2009 to 24% in 2012 (p < 0.001). More residents recommended CTS to potential trainees (79% in 2014 vs 65% in 2010, p = 0.007). Job offers increased from a low of 12% in 2008 with three or more offers to 34% in 2014. Debt increased from 0% with more than $200,000 in 2003 to 40% in 2013 (p < 0.001). Compared with residents in traditional programs, more integrated residents in 2014 were interested in adult cardiac surgery (53% vs 31%) and congenital surgery (22% vs 7%), fewer were interested in general thoracic surgery (5% vs 31%, p < 0.001), and more planned on additional training (66% vs 36%, p < 0.001). With the evolution in CTS over the last <span class="hlt">decade</span>, residents' training and career paths have <span class="hlt">changed</span> substantially, with increased specialization and simulation accompanied by increased resident satisfaction and an improved job market. Copyright © 2015 The Society of Thoracic Surgeons. Published by Elsevier Inc. All rights reserved.</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/2017E3SWC..2104023K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017E3SWC..2104023K"><span><span class="hlt">Key</span> Trends in Institutional <span class="hlt">Changes</span> Under Sustainable Development</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Karpova, Olga; Pevneva, Inna; Dymova, Irina; Kostina, Tatiana; Li, Sergey</p> <p>2017-11-01</p> <p>The article is devoted to the consideration of the essential problems of accounting institution formation under the sustainable development of the country and the region. The research is based on the <span class="hlt">key</span> research the field of the intuition economics and considers the trends of institutional <span class="hlt">changes</span> including incremental, evolutionary and revolutionary. Approaches to the analysis of institutions are presented as well. The first approach states that economic efficiency is guaranteed by newly emerging institutions. The second approach involves certain internal and external incentives for <span class="hlt">changing</span> institutions. Whereas the third approach insists on considering institutional <span class="hlt">changes</span> to be the relation of individual economic entities to institutional innovations in terms of the net benefit from their implementation. The conclusion draws the leading role of the state in the process of the emergence and further development of newly created institutions focusing on the fact that not every <span class="hlt">change</span> leads to greater efficiency. Thus it is crucial to consider the previous background of institutions development at implementing <span class="hlt">changes</span> in accounting and control.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018GeoRL..45..354Z','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018GeoRL..45..354Z"><span>Dominant Role of Atlantic Multidecadal Oscillation in the Recent <span class="hlt">Decadal</span> <span class="hlt">Changes</span> in Western North Pacific Tropical Cyclone Activity</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Zhang, Wei; Vecchi, Gabriel A.; Murakami, Hiroyuki; Villarini, Gabriele; Delworth, Thomas L.; Yang, Xiaosong; Jia, Liwei</p> <p>2018-01-01</p> <p>Over the 1997-2014 period, the mean frequency of western North Pacific (WNP) tropical cyclones (TCs) was markedly lower ( 18%) than the period 1980-1996. Here we show that these <span class="hlt">changes</span> were driven by an intensification of the vertical wind shear in the southeastern/eastern WNP tied to the <span class="hlt">changes</span> in the Walker circulation, which arose primarily in response to the enhanced sea surface temperature (SST) warming in the North Atlantic, while the SST anomalies associated with the negative phase of the Pacific <span class="hlt">Decadal</span> Oscillation in the tropical Pacific and the anthropogenic forcing play only secondary roles. These results are based on observations and experiments using the Geophysical Fluid Dynamics Laboratory Forecast-oriented Low-ocean Resolution Coupled Climate Model coupled climate model. The present study suggests a crucial role of the North Atlantic SST in causing <span class="hlt">decadal</span> <span class="hlt">changes</span> to WNP TC frequency.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4832269','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4832269"><span>Brain volumetric <span class="hlt">changes</span> and cognitive ageing during the eighth <span class="hlt">decade</span> of life</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Dickie, David Alexander; Cox, Simon R.; Valdes Hernandez, Maria del C.; Corley, Janie; Royle, Natalie A.; Pattie, Alison; Aribisala, Benjamin S.; Redmond, Paul; Muñoz Maniega, Susana; Taylor, Adele M.; Sibbett, Ruth; Gow, Alan J.; Starr, John M.; Bastin, Mark E.; Wardlaw, Joanna M.; Deary, Ian J.</p> <p>2015-01-01</p> <p>Abstract Later‐life <span class="hlt">changes</span> in brain tissue volumes—decreases in the volume of healthy grey and white matter and increases in the volume of white matter hyperintensities (WMH)—are strong candidates to explain some of the variation in ageing‐related cognitive decline. We assessed fluid intelligence, memory, processing speed, and brain volumes (from structural MRI) at mean age 73 years, and at mean age 76 in a narrow‐age sample of older individuals (n = 657 with brain volumetric data at the initial wave, n = 465 at follow‐up). We used latent variable modeling to extract error‐free cognitive levels and slopes. Initial levels of cognitive ability were predictive of subsequent brain tissue volume <span class="hlt">changes</span>. Initial brain volumes were not predictive of subsequent cognitive <span class="hlt">changes</span>. Brain volume <span class="hlt">changes</span>, especially increases in WMH, were associated with declines in each of the cognitive abilities. All statistically significant results were modest in size (absolute r‐values ranged from 0.114 to 0.334). These results build a comprehensive picture of macrostructural brain volume <span class="hlt">changes</span> and declines in important cognitive faculties during the eighth <span class="hlt">decade</span> of life. Hum Brain Mapp 36:4910–4925, 2015. © 2015 The Authors. Human Brain Mapping Published by Wiley Periodicals, Inc PMID:26769551</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20160012763','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20160012763"><span>Contribution of Phenological and Physiological Variations on Northern Vegetation Productivity <span class="hlt">Changes</span> over Last Three <span class="hlt">Decades</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Ganguly, Sangram</p> <p>2015-01-01</p> <p>Plant phenology and maximum photosynthetic state determine spatiotemporal variability of gross primary productivity (GPP) of vegetation. Recent warming induced impacts accelerate shifts of phenology and physiological status over Northern vegetated land. Thus, understanding and quantifying these <span class="hlt">changes</span> are very important. Here, we investigate 1) how vegetation phenology and physiological status (maximum photosynthesis) are evolved over last three <span class="hlt">decades</span> and 2) how such components (phenology and physiological status) contribute on inter-annual variation of the GPP during the last three <span class="hlt">decades</span>. We utilized both long-term remotely sensed (GIMMS (Global Inventory Modeling and Mapping Studies), NDVI3g (Normalized Difference Vegetation Index 3rd generation) and MODIS (Moderate Resolution Imaging Spectroradiometer)) to extract larger scale phenology metrics (growing season start, end and duration); and productivity (i.e., growing season integrated vegetation index, GSIVI) to answer these questions. For evaluation purpose, we also introduced field-measured phenology and productivity datasets (e.g., FLUXNET) and possible remotely-sensed and modeled metrics at continental and regional scales. From this investigation, we found that onset of the growing season has advanced by 1.61 days per <span class="hlt">decade</span> and the growing season end has delayed by 0.67 days per <span class="hlt">decade</span> over the circumpolar region. This asymmetric extension of growing season results in a longer growing-season trend (2.96 days per <span class="hlt">decade</span>) and widespread increasing vegetation-productivity trend (2.96 GSIVI per <span class="hlt">decade</span>) over Northern land. However, the regionally-diverged phenology shift and maximum photosynthetic state contribute differently characterized productivity, inter-annual variability and trend. We quantified that about 50 percent, 13 percent and 6.5 percent of Northern land's inter-annual variability are dominantly controlled by the onset of the growing season, the end of the growing season and the maximum</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017JIEIB..98..353B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017JIEIB..98..353B"><span>A New Three Dimensional Based <span class="hlt">Key</span> Generation Technique in AVK</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Banerjee, Subhasish; Dutta, Manash Pratim; Bhunia, Chandan Tilak</p> <p>2017-08-01</p> <p>In modern era, ensuring high order security becomes one and only objective of computer networks. From the last few <span class="hlt">decades</span>, many researchers have given their contributions to achieve the secrecy over the communication channel. In achieving perfect security, Shannon had done the pioneer work on perfect secret theorem and illustrated that secrecy of the shared information can be maintained if the <span class="hlt">key</span> becomes variable in nature instead of static one. In this regard, a <span class="hlt">key</span> generation technique has been proposed where the <span class="hlt">key</span> can be <span class="hlt">changed</span> every time whenever a new block of data needs to be exchanged. In our scheme, the <span class="hlt">keys</span> not only vary in bit sequences but also in size. The experimental study is also included in this article to prove the correctness and effectiveness of our proposed technique.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=20040075030&hterms=TOM&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D20%26Ntt%3DTOM','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=20040075030&hterms=TOM&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D20%26Ntt%3DTOM"><span>Evaluation of a Multi-<span class="hlt">Decadal</span> Simulation of Stratospheric Ozone by Comparison with Total Ozone Mapping Spectrometer (TOMS) Observations</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Douglass, Anne R.; Stolarski, Richard S.; Steenrod, Steven; Pawson, Steven</p> <p>2003-01-01</p> <p>One <span class="hlt">key</span> application of atmospheric chemistry and transport models is prediction of the response of ozone and other constituents to various natural and anthropogenic perturbations. These include <span class="hlt">changes</span> in composition, such as the previous rise and recent decline in emission of man-made chlorofluorcarbons, <span class="hlt">changes</span> in aerosol loading due to volcanic eruption, and <span class="hlt">changes</span> in solar forcing. Comparisons of hindcast model results for the past few <span class="hlt">decades</span> with observations are a <span class="hlt">key</span> element of model evaluation and provide a sense of the reliability of model predictions. The 25 year data set from Total Ozone Mapping Spectrometers is a cornerstone of such model evaluation. Here we report evaluation of three-dimensional multi-<span class="hlt">decadal</span> simulation of stratospheric composition. Meteorological fields for this off-line calculation are taken from a 50 year simulation of a general circulation model. Model fields are compared with observations from TOMS and also with observations from the Stratospheric Aerosol and Gas Experiment (SAGE), Microwave Limb Sounder (MLS), Cryogenic Limb Array Etalon Spectrometer (CLAES), and the Halogen Occultation Experiment (HALOE). This overall evaluation will emphasize the spatial, seasonal, and interannual variability of the simulation compared with observed atmospheric variability.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29425479','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29425479"><span>Differential Risk of Hypertension Among Lean and Nonlean Rural Subjects in Relation to <span class="hlt">Decadal</span> <span class="hlt">Changes</span> in Anthropometry.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Deshpande-Joshi, Sayali S; Rao, Shobha</p> <p>2018-02-09</p> <p>Assessing risk of hypertension in relation to <span class="hlt">decadal</span> <span class="hlt">changes</span> in anthropometry among cohort of young rural Indian men. Subjects (n = 140) were measured in 2005 and 2015 for blood pressure, body mass index (BMI), body fat (BF), waist circumference (WC), waist-to-hip ratio (WHR), and additionally for visceral fat (VF) at follow-up. <span class="hlt">Decadal</span> <span class="hlt">changes</span> showed significant (p < 0.001) increase in mean anthropometric measures and in prevalence of overall obesity (BMI ≥25 kg/m 2 ) from 3.6% to 37.1%; adiposity (BF ≥25%) from 5.1% to 40.9%; and central obesity (WHR ≥0.9) from 0.7% to 24.3%. Prevalence of hypertension increased (20.7% to 27.1%) but was not statistically significant. VF correlated significantly (p < 0.001) with <span class="hlt">decadal</span> <span class="hlt">changes</span> (Δ) in BMI, BF, WC, and WHR, and the correlations were stronger (r = 0.90, 0.78, 0.84, and 0.56, respectively) for lean (baseline BMI < median) subjects than nonlean (baseline BMI ≥median) subjects (r = 0.68, 0.40, 0.61, and 0.43, respectively). Risk of hypertension was significant (odds ratio [OR] = 11.0, 95% confidence interval [CI]: 2.8-42.8) for subjects with higher ΔBMI (≥4.7 kg/m 2 ) compared with those with lower ΔBMI (<4.7 kg/m 2 ) among lean but was not significant among nonlean subjects. This was also true for <span class="hlt">change</span> in other adiposity indicators, indicating greater vulnerability of lean subjects. Further, among lean subjects, ORs reduced considerably after adjusting for VF, whereas among nonlean subjects ORs continued to remain nonsignificant but showing independent significance for VF. For similar level of <span class="hlt">change</span> in adiposity indicators, lean subjects were at greater risk of hypertension than nonlean subjects, probably due to higher VF deposition.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/27799419','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/27799419"><span>HIV decline associated with <span class="hlt">changes</span> in risk behaviours among young <span class="hlt">key</span> populations in Nepal: analysis of population-based HIV prevalence surveys between 2001 and 2012.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Deuba, Keshab; Ekström, Anna Mia; Tomson, Göran; Shrestha, Rachana; Marrone, Gaetano</p> <p>2017-08-01</p> <p>We assessed <span class="hlt">changes</span> in HIV prevalence and risk behaviours among young <span class="hlt">key</span> populations in Nepal. A total of 7505 participants (aged 16-24 years) from <span class="hlt">key</span> populations who were at increased risk of HIV infection (2767 people who inject drugs (PWID); 852 men who have sex with men/transgender (MSM/TG); 2851 female sex workers (FSW) and 1035 male labour migrants) were recruited randomly over a 12-year period, 2001-2012. Local epidemic zones of Nepal (Kathmandu valley, Pokhara valley, Terai Highway and West to Far West hills) were analysed separately. We found a very strong and consistent decline in HIV prevalence over the past <span class="hlt">decade</span> in different epidemic zones among PWID and MSM/TG in Kathmandu, the capital city, most likely due to a parallel increase in safe needle and syringe use and increased condom use. A decrease in HIV prevalence in 22 Terai highway districts, sharing an open border with India, was also consistent with increased condom use among FSW. Among male labour migrants, HIV prevalence was low throughout the period in the West to Far West hilly regions. Condom use by migrant workers involved with FSW abroad increased while their condom use with Nepalese FSW declined. Other risk determinants such as mean age at starting first injection, injection frequency, place of commercial sex solicitation, their mean age when leaving to work abroad did not <span class="hlt">change</span> consistently across epidemic zones among the young <span class="hlt">key</span> populations under study. In Nepal, the decline in HIV prevalence over the past <span class="hlt">decade</span> was remarkably significant and consistent with an increase in condom use and safer use of clean needles and syringes. However, diverging trends in risk behaviours across local epidemic zones of Nepal suggest a varying degree of implementation of national HIV prevention policies. This calls for continued preventive efforts as well as surveillance to sustain the observed downward trend.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/15358969','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/15358969"><span>Two <span class="hlt">decades</span> of organizational <span class="hlt">change</span> in health care: what have we learned?</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Bazzoli, Gloria J; Dynan, Linda; Burns, Lawton R; Yap, Clarence</p> <p>2004-09-01</p> <p>The 1980s and 1990s witnessed a substantial wave of organizational restructuring among hospitals and physicians, as health providers rethought their organizational roles given perceived market imperatives. Mergers, acquisitions, internal restructuring, and new interorganizational relationships occurred at a record pace. Matching this was a large wave of study and discourse among health services researchers, industry experts, and consultants to understand the causes and consequences of organizational <span class="hlt">change</span>. In many cases, this literature provides mixed signals about what was accomplished through these organizational efforts. The purpose of this review is to synthesize this diverse literature. This review examines studies of horizontal consolidation and integration of hospitals, horizontal consolidation and integration of physician organizations, and integration and relationship development between physicians and hospitals. In all, around 100 studies were examined to assess what was learned through two <span class="hlt">decades</span> of research on organizational <span class="hlt">change</span> in health care.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2009AGUFM.A31H..01V','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2009AGUFM.A31H..01V"><span>Reconstruction of regional climate and climate <span class="hlt">change</span> in past <span class="hlt">decades</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>von Storch, H.; Feser, F.; Weisse, R.; Zahn, M.</p> <p>2009-12-01</p> <p>Regional climate models, which are constrained by large scale information (spectral nudging) provided by re-analyses, allow for the construction of a mostly homogeneous description of regional weather statistics since about 1950. The potential of this approach has been demonstrated for Northern Europe. That data set, named CoastDat, does not only contain hourly data on atmospheric variables, in particular wind, but also on marine weather, i.e., short term water level, current and sea state variations. Another example is the multi-<span class="hlt">decadal</span> variability of Polar Lows in the subarctic waters. The utility of such data sets is broad, from risk assessments related to coastal wind and wave conditions, assessment of determining the causes for regional climate <span class="hlt">change</span>, a-posteriori analysis of the efficiency of environmental legislation (example: lead). In the paper, the methodology is outlined, examples are provided and the utility of the product discussed.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013AGUFMGC11D1028L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013AGUFMGC11D1028L"><span>The Parana paradox: can a model explain the <span class="hlt">decadal</span> impacts of climate variability and land-cover <span class="hlt">change</span>?</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Lee, E.; Moorcroft, P. R.; Livino, A.; Briscoe, J.</p> <p>2013-12-01</p> <p>Since the 1970s, despite a decrease in rainfall, flow in the Parana river has increased. This paradox is explored using the Ecosystem Demography (ED) model. If there were no <span class="hlt">change</span> in land cover, the modeled runoff decreased from the 1970s to the 2000s by 11.8% (with 1970 land cover) or 18.8% (with 2008 land cover). When the model is run holding climate constant, the <span class="hlt">decadal</span> average of the modeled runoff increased by 24.4% (with the 1970s climate) or by 33.6% (with 2000s climate). When the model is run allowing both the actual climate and land-cover <span class="hlt">changes</span>, the model gives an increase in the <span class="hlt">decadal</span> average of runoff by 8.5%. This agrees well with 10.5% increase in the actual stream flow as measured at Itaipu. There are three main conclusions from this work. First, the ED model is able to explain a major, paradoxical, reality in the Parana basin. Second, it is necessary to take into account both climate and land use <span class="hlt">changes</span> when exploring past or future <span class="hlt">changes</span> in river flows. Third, the ED model, now coupled with a regional climate model (i.e., EDBRAMS), is a sound basis for exploring likely <span class="hlt">changes</span> in river flows in major South American rivers.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014ClDy...43.1357H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014ClDy...43.1357H"><span>Intensification of <span class="hlt">decadal</span> and multi-<span class="hlt">decadal</span> sea level variability in the western tropical Pacific during recent <span class="hlt">decades</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Han, Weiqing; Meehl, Gerald A.; Hu, Aixue; Alexander, Michael A.; Yamagata, Toshio; Yuan, Dongliang; Ishii, Masayoshi; Pegion, Philip; Zheng, Jian; Hamlington, Benjamin D.; Quan, Xiao-Wei; Leben, Robert R.</p> <p>2014-09-01</p> <p>Previous studies have linked the rapid sea level rise (SLR) in the western tropical Pacific (WTP) since the early 1990s to the Pacific <span class="hlt">decadal</span> climate modes, notably the Pacific <span class="hlt">Decadal</span> Oscillation in the north Pacific or Interdecadal Pacific Oscillation (IPO) considering its basin wide signature. Here, the authors investigate the <span class="hlt">changing</span> patterns of <span class="hlt">decadal</span> (10-20 years) and multidecadal (>20 years) sea level variability (global mean SLR removed) in the Pacific associated with the IPO, by analyzing satellite and in situ observations, together with reconstructed and reanalysis products, and performing ocean and atmosphere model experiments. Robust intensification is detected for both <span class="hlt">decadal</span> and multidecadal sea level variability in the WTP since the early 1990s. The IPO intensity, however, did not increase and thus cannot explain the faster SLR. The observed, accelerated WTP SLR results from the combined effects of Indian Ocean and WTP warming and central-eastern tropical Pacific cooling associated with the IPO cold transition. The warm Indian Ocean acts in concert with the warm WTP and cold central-eastern tropical Pacific to drive intensified easterlies and negative Ekman pumping velocity in western-central tropical Pacific, thereby enhancing the western tropical Pacific SLR. On <span class="hlt">decadal</span> timescales, the intensified sea level variability since the late 1980s or early 1990s results from the "out of phase" relationship of sea surface temperature anomalies between the Indian and central-eastern tropical Pacific since 1985, which produces "in phase" effects on the WTP sea level variability.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/22692413','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/22692413"><span>Newborn survival in Uganda: a <span class="hlt">decade</span> of <span class="hlt">change</span> and future implications.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Mbonye, Anthony K; Sentongo, Miriam; Mukasa, Gelasius K; Byaruhanga, Romano; Sentumbwe-Mugisa, Olive; Waiswa, Peter; Naamala Sengendo, Hanifah; Aliganyira, Patrick; Nakakeeto, Margaret; Lawn, Joy E; Kerber, Kate</p> <p>2012-07-01</p> <p>Each year in Uganda 141 000 children die before reaching their fifth birthday; 26% of these children die in their first month of life. In a setting of persistently high fertility rates, a crisis in human resources for health and a recent history of civil unrest, Uganda has prioritized Millennium Development Goals 4 and 5 for child and maternal survival. As part of a multi-country analysis we examined <span class="hlt">change</span> for newborn survival over the past <span class="hlt">decade</span> through mortality and health system coverage indicators as well as national and donor funding for health, and policy and programme <span class="hlt">change</span>. Between 2000 and 2010 Uganda's neonatal mortality rate reduced by 2.2% per year, which is greater than the regional average rate of decline but slower than national reductions in maternal mortality and under-five mortality after the neonatal period. While existing population-based data are insufficient to measure national <span class="hlt">changes</span> in coverage and quality of services, national attention for maternal and child health has been clear and authorized from the highest levels. Attention and policy <span class="hlt">change</span> for newborn health is comparatively recent. This recognized gap has led to a specific focus on newborn health through a national Newborn Steering Committee, which has been given a mandate from the Ministry of Health to advise on newborn survival issues since 2006. This multi-disciplinary and inter-agency network of stakeholders has been able to preside over a number of important policy <span class="hlt">changes</span> at the level of facility care, education and training, community-based service delivery through Village Health Teams and <span class="hlt">changes</span> to essential drugs and commodities. The committee's comprehensive reach has enabled rapid policy <span class="hlt">change</span> and increased attention to newborn survival in a relatively short space of time. Translating this favourable policy environment into district-level implementation and high quality services is now the priority.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014cosp...40E3732Y','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014cosp...40E3732Y"><span>A Nominal Balloon Instrument Payload to Address Questions from the Planetary <span class="hlt">Decadal</span> Survey</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Young, Eliot; Kremic, Tibor; Dankanich, John</p> <p></p> <p>The Planetary Science <span class="hlt">Decadal</span> Survey (entitled "Visions and Voyages for Planetary Science in the <span class="hlt">Decade</span> 2013 - 2022", available online at https://solarsystem.nasa.gov/2013<span class="hlt">decadal</span>/) serves as a roadmap for activities to be pursued by the Planetary Science Division of NASA's Science Mission Directorate. This document outlines roughly 200 <span class="hlt">key</span> research areas and questions in chapters covering different parts of the solar system (e.g., Mars, Small Bodies, etc.). We have reviewed the <span class="hlt">Decadal</span> Survey to assess whether any of the <span class="hlt">key</span> questions can be addressed by high altitude balloon-borne payloads. Although some questions can only be answered by in situ experiments, we found that approximately one quarter of the <span class="hlt">key</span> questions were well suited to balloon payloads. In many of those cases, balloons were competitive or superior to other existing facilities, including HST, SOFIA or Keck telescopes. We will present specific telescope and instrument bench designs that are capable of addressing <span class="hlt">key</span> questions in the <span class="hlt">Decadal</span> Survey. The instrument bench takes advantage of two of the main benefits of high-altitude observations: diffraction-limited imaging in visible and UV wavelengths and unobstructed spectroscopy in near-IR (1 - 5 microns) wavelengths. Our optical prescription produces diffraction-limited PSFs in both visible and IR beams. We will discuss pointing and thermal stability, two of the main challenges facing a balloon-borne telescope.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/28858417','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/28858417"><span><span class="hlt">Changes</span> of tooth color in middle and old age: A longitudinal study over a <span class="hlt">decade</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Hassel, Alexander J; Johanning, Marvin; Grill, Sabine; Schröder, Johannes; Wahl, Hans-Werner; Corcodel, Nicoleta; Klotz, Anna-Luisa; Rammelsberg, Peter; Zenthöfer, Andreas</p> <p>2017-11-12</p> <p>To evaluate <span class="hlt">changes</span> in tooth color for 2 age cohorts (younger cohort, YC: 1950-1952; older cohort, OC: 1930-1932) over a mean observation period of 8 years. Sixty-one participants with 106 upper central incisors were subjected to baseline and follow-up examinations (YC: n = 46/OC: n = 15). International Commission on Illumination color coordinates of 1 or 2 unrestored test teeth for each participant were recorded by use of a spectrophotometer (VITA Easyshade 1) during both measurement times. <span class="hlt">Changes</span> of color coordinates during the study period were evaluated by use of generalized linear mixed models with the variable "participant" as random effect. ΔE ab and E 2000 color differences were calculated between baseline and follow-up. Significant <span class="hlt">changes</span> in color coordinates were observed, with the exception of lightness in OC. The direction of the <span class="hlt">changes</span> depended on the cohort. A decrease of lightness (value) was observed in YC (ΔL = 4.0; P < .001) whereas in OC chroma increased (ΔC = -3.3; P < .001). For both groups, a significant shift to more reddish tooth colors was observed. In almost all cases, color differences between baseline and follow-up exceeded the 50:50 acceptability thresholds for color differences (ΔE = 2.7) in both YC (≈90%) and OC (≈80%). For both quinquagenarians and septuagenarians, clinically relevant <span class="hlt">changes</span> in tooth color were observed after a <span class="hlt">decade</span>; these could affect the long-term success of prosthetic restorations in terms of a satisfactory color match between natural teeth and dental prostheses. In contrast with the findings of cross-sectional studies, the <span class="hlt">changes</span> were partially age-group-specific. Tooth color can <span class="hlt">change</span> over a <span class="hlt">decade</span>. When fixed dental prostheses are planned, one should consider that <span class="hlt">changes</span> of tooth color could lead to mismatch between a restoration and adjacent teeth during the period in clinical service. © 2017 Wiley Periodicals, Inc.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017HESS...21.3041B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017HESS...21.3041B"><span>Water-food-energy nexus with <span class="hlt">changing</span> agricultural scenarios in India during recent <span class="hlt">decades</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Barik, Beas; Ghosh, Subimal; Saheer Sahana, A.; Pathak, Amey; Sekhar, Muddu</p> <p>2017-06-01</p> <p>Meeting the growing water and food demands in a densely populated country like India is a major challenge. It requires an extensive investigation into the <span class="hlt">changing</span> patterns of the checks and balances behind the maintenance of food security at the expense of depleting groundwater, along with high energy consumption. Here we present a comprehensive set of analyses which assess the present status of the water-food-energy nexus in India, along with its <span class="hlt">changing</span> pattern, in the last few <span class="hlt">decades</span>. We find that with the growth of population and consequent increase in the food demands, the food production has also increased, and this has been made possible with the intensification of irrigation. However, during the recent <span class="hlt">decade</span> (after 1996), the increase in food production has not been sufficient to meet its growing demands, precipitating a decline in the per-capita food availability. We also find a statistically significant declining trend of groundwater storage in India during the last <span class="hlt">decade</span>, as derived from the Gravity Recovery and Climate Experiment (GRACE) satellite datasets. Regional studies reveal contrasting trends between northern and western-central India. North-western India and the middle Ganga basin show a decrease in the groundwater storage as opposed to an increasing storage over western-central India. Comparison with well data reveals that the highest consistency of GRACE-derived storage data with available well measurements is in the middle Ganga basin. After analysing the data for the last 2 <span class="hlt">decades</span>, we further showcase that, after a drought, the groundwater storage drops but is unable to recover to its original condition even after good monsoon years. The groundwater storage reveals a very strong negative correlation with the electricity consumption for agricultural usage, which may also be considered as a proxy for groundwater pumped for irrigation in a region. The electricity usage for agricultural purposes has an increasing trend and, interestingly</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFM.H33N..02C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFM.H33N..02C"><span>Modeling urbanized watershed flood response <span class="hlt">changes</span> with distributed hydrological model: <span class="hlt">key</span> hydrological processes, parameterization and case studies</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Chen, Y.</p> <p>2017-12-01</p> <p>Urbanization is the world development trend for the past century, and the developing countries have been experiencing much rapider urbanization in the past <span class="hlt">decades</span>. Urbanization brings many benefits to human beings, but also causes negative impacts, such as increasing flood risk. Impact of urbanization on flood response has long been observed, but quantitatively studying this effect still faces great challenges. For example, setting up an appropriate hydrological model representing the <span class="hlt">changed</span> flood responses and determining accurate model parameters are very difficult in the urbanized or urbanizing watershed. In the Pearl River Delta area, rapidest urbanization has been observed in China for the past <span class="hlt">decades</span>, and dozens of highly urbanized watersheds have been appeared. In this study, a physically based distributed watershed hydrological model, the Liuxihe model is employed and revised to simulate the hydrological processes of the highly urbanized watershed flood in the Pearl River Delta area. A virtual soil type is then defined in the terrain properties dataset, and its runoff production and routing algorithms are added to the Liuxihe model. Based on a parameter sensitive analysis, the <span class="hlt">key</span> hydrological processes of a highly urbanized watershed is proposed, that provides insight into the hydrological processes and for parameter optimization. Based on the above analysis, the model is set up in the Songmushan watershed where there is hydrological data observation. A model parameter optimization and updating strategy is proposed based on the remotely sensed LUC types, which optimizes model parameters with PSO algorithm and updates them based on the <span class="hlt">changed</span> LUC types. The model parameters in Songmushan watershed are regionalized at the Pearl River Delta area watersheds based on the LUC types of the other watersheds. A dozen watersheds in the highly urbanized area of Dongguan City in the Pearl River Delta area were studied for the flood response <span class="hlt">changes</span> due to</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/28138548','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/28138548"><span>Accelerated freshening of Antarctic Bottom Water over the last <span class="hlt">decade</span> in the Southern Indian Ocean.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Menezes, Viviane V; Macdonald, Alison M; Schatzman, Courtney</p> <p>2017-01-01</p> <p>Southern Ocean abyssal waters, in contact with the atmosphere at their formation sites around Antarctica, not only bring signals of a <span class="hlt">changing</span> climate with them as they move around the globe but also contribute to that <span class="hlt">change</span> through heat uptake and sea level rise. A repeat hydrographic line in the Indian sector of the Southern Ocean, occupied three times in the last two <span class="hlt">decades</span> (1994, 2007, and, most recently, 2016), reveals that Antarctic Bottom Water (AABW) continues to become fresher (0.004 ± 0.001 kg/g <span class="hlt">decade</span> -1 ), warmer (0.06° ± 0.01°C <span class="hlt">decade</span> -1 ), and less dense (0.011 ± 0.002 kg/m 3 <span class="hlt">decade</span> -1 ). The most recent observations in the Australian-Antarctic Basin show a particularly striking acceleration in AABW freshening between 2007 and 2016 (0.008 ± 0.001 kg/g <span class="hlt">decade</span> -1 ) compared to the 0.002 ± 0.001 kg/g <span class="hlt">decade</span> -1 seen between 1994 and 2007. Freshening is, in part, responsible for an overall shift of the mean temperature-salinity curve toward lower densities. The marked freshening may be linked to an abrupt iceberg-glacier collision and calving event that occurred in 2010 on the George V/Adélie Land Coast, the main source region of bottom waters for the Australian-Antarctic Basin. Because AABW is a <span class="hlt">key</span> component of the global overturning circulation, the persistent decrease in bottom water density and the associated increase in steric height that result from continued warming and freshening have important consequences beyond the Southern Indian Ocean.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015AGUFM.A41R..06C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015AGUFM.A41R..06C"><span><span class="hlt">Decadal</span> <span class="hlt">changes</span> in aerosol absorption across Brazil resulting from <span class="hlt">changes</span> in biomass burning practices</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Coe, H.; Morgan, W.; Darbyshire, E.; Allan, J. D.; Flynn, M.; Liu, D.; Langridge, J.; Johnson, B. T.; Haywood, J. M.; Longo, K.; Artaxo, P.; Highwood, E.; Mollard, J.</p> <p>2015-12-01</p> <p>Open biomass burning makes a substantial contribution to the global budget of black carbon, yet models significantly underestimate absorption aerosol optical depth compared to observations by approximately a factor of two over South America. These large differences need to be addressed. Recent work has shown that the number of deforestation fires has decreased across Amazonia over the last <span class="hlt">decade</span>, giving rise to a decrease in the abundance of biomass burning aerosol across the region. At the same time there has been an increase in the frequency of agricultural burning across regions that have previously been deforested, as well as increased burning in the east of Brazil in the Cerrado regions. We sampled both of these types of open burning extensively during a recent aircraft experiment. Significant concentrations of organic carbon as well as black carbon were observed, with this ratio providing the main control on the single scattering albedo (SSA).Deforestation fires and wild forest fires are prevalent across the south west of the Amazon Basin, where smouldering burning dominates. In the east of Brazil, agricultural burning proceeds via a much more efficient form of combustion and as a result, black carbon is a much larger fraction of the aerosol mass and SSAs are much lower than in the west. We have analysed MISR data across the region to show that whilst aerosol optical depths have decreased during the dry season over the last <span class="hlt">decade</span>, with greater rates of reduction occurring over the south western margins of Amazonia, absorption aerosol optical depths have significantly increased over the Cerrado and remained constant over south western Amazonia. This has led to a decline in SSA across the whole of the region with greater reductions occurring over the eastern states. This finding is consistent with our aircraft measurements. We will discuss the implications of these <span class="hlt">changes</span> for air quality and climate across the region.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFMPA11D..08W','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFMPA11D..08W"><span>Economic Value of Narrowing the Uncertainty in Climate Sensitivity: <span class="hlt">Decadal</span> <span class="hlt">Change</span> in Shortwave Cloud Radiative Forcing and Low Cloud Feedback</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Wielicki, B. A.; Cooke, R. M.; Golub, A. A.; Mlynczak, M. G.; Young, D. F.; Baize, R. R.</p> <p>2016-12-01</p> <p>Several previous studies have been published on the economic value of narrowing the uncertainty in climate sensitivity (Cooke et al. 2015, Cooke et al. 2016, Hope, 2015). All three of these studies estimated roughly 10 Trillion U.S. dollars for the Net Present Value and Real Option Value at a discount rate of 3%. This discount rate is the nominal discount rate used in the U.S. Social Cost of Carbon Memo (2010). The Cooke et al studies approached this problem by examining advances in accuracy of global temperature measurements, while the Hope 2015 study did not address the type of observations required. While temperature <span class="hlt">change</span> is related to climate sensitivity, large uncertainties of a factor of 3 in current anthropogenic radiative forcing (IPCC, 2013) would need to be solved for advanced <span class="hlt">decadal</span> temperature <span class="hlt">change</span> observations to assist the challenge of narrowing climate sensitivity. The present study takes a new approach by extending the Cooke et al. 2015,2016 papers to replace observations of temperature <span class="hlt">change</span> to observations of <span class="hlt">decadal</span> <span class="hlt">change</span> in the effects of <span class="hlt">changing</span> clouds on the Earths radiative energy balance, a measurement known as Cloud Radiative Forcing, or Cloud Radiative Effect. <span class="hlt">Decadal</span> <span class="hlt">change</span> in this observation is direclty related to the largest uncertainty in climate sensitivity which is cloud feedback from <span class="hlt">changing</span> amount of low clouds, primarily low clouds over the world's oceans. As a result, <span class="hlt">decadal</span> <span class="hlt">changes</span> in shortwave cloud radiative forcing are more directly related to cloud feedback uncertainty which is the dominant uncertainty in climate sensitivity. This paper will show results for the new approach, and allow an examination of the sensitivity of economic value results to different observations used as a constraint on uncertainty in climate sensitivity. The analysis suggests roughly a doubling of economic value to 20 Trillion Net Present Value or Real Option Value at 3% discount rate. The higher economic value results from two <span class="hlt">changes</span>: a</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('http://adsabs.harvard.edu/abs/2018ThApC.tmp...64Z','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018ThApC.tmp...64Z"><span>Inter-<span class="hlt">decadal</span> <span class="hlt">change</span> of the lagged inter-annual relationship between local sea surface temperature and tropical cyclone activity over the western North Pacific</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Zhao, Haikun; Wu, Liguang; Raga, G. B.</p> <p>2018-02-01</p> <p>This study documents the inter-<span class="hlt">decadal</span> <span class="hlt">change</span> of the lagged inter-annual relationship between the TC frequency (TCF) and the local sea surface temperature (SST) in the western North Pacific (WNP) during 1979-2014. An abrupt shift of the lagged relationship between them is observed to occur in 1998. Before the shift (1979-1997), a moderately positive correlation (0.35) between previous-year local SST and TCF is found, while a significantly negative correlation (- 0.71) is found since the shift (1998-2014). The inter-<span class="hlt">decadal</span> <span class="hlt">change</span> of the lagged relationship between TCF and local SST over the WNP is also accompanied by an inter-<span class="hlt">decadal</span> <span class="hlt">change</span> in the lagged inter-annual relationship between large-scale factors affecting TCs and local SST over the WNP. During 1998-2014, the previous-year local SST shows a significant negative correlation with the mid-level moisture and a significant positive correlation with the vertical wind shear over the main development region of WNP TC genesis. Almost opposite relationships are seen during 1979-1997, with a smaller magnitude of the correlation coefficients. These <span class="hlt">changes</span> are consistent with the <span class="hlt">changes</span> of the lagged inter-annual relationship between upper- and lower-level winds and local SST over the WNP. Analyses further suggests that the inter-<span class="hlt">decadal</span> shift of the lagged inter-annual relationship between WNP TCF and local SST may be closely linked to the inter-<span class="hlt">decadal</span> <span class="hlt">change</span> of inter-annual SST transition over the tropical central-eastern Pacific associated with the climate regime shift in the late 1990s. Details on the underlying physical process need further investigation using observations and simulations.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://eric.ed.gov/?q=Pehkonen+AND+Erkki&pg=2&id=EJ610669','ERIC'); return false;" href="https://eric.ed.gov/?q=Pehkonen+AND+Erkki&pg=2&id=EJ610669"><span>Teachers' Professional Development: What Are the <span class="hlt">Key</span> <span class="hlt">Change</span> Factors for Mathematics Teachers?</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>Pehkonen, Erkki; Torner, Gunter</p> <p>1999-01-01</p> <p>Surveyed and interviewed 13 experienced German middle school mathematics teachers to examine <span class="hlt">key</span> factors causing discontinuity in their professional development. Results included 49 statements about <span class="hlt">change</span> that fell into four categories. Researchers extracted three <span class="hlt">change</span> factors not reported in earlier literature: experiences and observations…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/28428539','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/28428539"><span>Separating <span class="hlt">decadal</span> global water cycle variability from sea level rise.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Hamlington, B D; Reager, J T; Lo, M-H; Karnauskas, K B; Leben, R R</p> <p>2017-04-20</p> <p>Under a warming climate, amplification of the water cycle and <span class="hlt">changes</span> in precipitation patterns over land are expected to occur, subsequently impacting the terrestrial water balance. On global scales, such <span class="hlt">changes</span> in terrestrial water storage (TWS) will be reflected in the water contained in the ocean and can manifest as global sea level variations. Naturally occurring climate-driven TWS variability can temporarily obscure the long-term trend in sea level rise, in addition to modulating the impacts of sea level rise through natural periodic undulation in regional and global sea level. The internal variability of the global water cycle, therefore, confounds both the detection and attribution of sea level rise. Here, we use a suite of observations to quantify and map the contribution of TWS variability to sea level variability on <span class="hlt">decadal</span> timescales. In particular, we find that <span class="hlt">decadal</span> sea level variability centered in the Pacific Ocean is closely tied to low frequency variability of TWS in <span class="hlt">key</span> areas across the globe. The unambiguous identification and clean separation of this component of variability is the missing step in uncovering the anthropogenic trend in sea level and understanding the potential for low-frequency modulation of future TWS impacts including flooding and drought.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/27313946','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/27313946"><span><span class="hlt">Change</span> in Practice over Four <span class="hlt">Decades</span> in the Management of Graves' Disease in Scotland.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Smith, D M; Dutta, S; Ahmed, F; Thaha, M A</p> <p>2016-01-01</p> <p>There is continuing debate on the optimal treatment for Grave's thyrotoxicosis with a resultant variation in clinical practice. The present study aimed to ascertain <span class="hlt">changes</span> in practice in the treatment of Grave's thyrotoxicosis in Tayside, Scotland, over the past four <span class="hlt">decades</span>. Methods. The "Scottish automated follow-up register" (SAFUR) was queried to identify all patients treated for Grave's thyrotoxicosis from 1968 to 2007 inclusive. Patients were divided into 4 groups (Groups A to D) according to the <span class="hlt">decades</span>. Demographic profile, treatment modalities, radioactive iodine (RAI) dose, and recurrence rates were studied and outcomes were compared by χ (2) test and ANOVA using SPSS v15.0. A p value of < 0.05 was considered significant. Results. Altogether, 3737 patients were diagnosed with Grave's thyrotoxicosis over the 4 <span class="hlt">decades</span>. Use of RAI has increased from 43.1% in Group A to 68% in Group D (p < 0.001). The dose of RAI has increased (p < 0.001) and there has been a reduction in recurrence rate with higher dose of RAI. Surgical intervention rates decreased from 55.3% to 12.3% (p < 0.001) over time. Conclusions. Analysis of a large dataset of patients with Grave's thyrotoxicosis suggests increasing use of RAI as the preferred first line of treatment. Furthermore, using a single higher dose of RAI and adoption of total thyroidectomy have decreased recurrence rates.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4904117','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4904117"><span><span class="hlt">Change</span> in Practice over Four <span class="hlt">Decades</span> in the Management of Graves' Disease in Scotland</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Smith, D. M.; Dutta, S.; Ahmed, F.; Thaha, M. A.</p> <p>2016-01-01</p> <p>There is continuing debate on the optimal treatment for Grave's thyrotoxicosis with a resultant variation in clinical practice. The present study aimed to ascertain <span class="hlt">changes</span> in practice in the treatment of Grave's thyrotoxicosis in Tayside, Scotland, over the past four <span class="hlt">decades</span>. Methods. The “Scottish automated follow-up register” (SAFUR) was queried to identify all patients treated for Grave's thyrotoxicosis from 1968 to 2007 inclusive. Patients were divided into 4 groups (Groups A to D) according to the <span class="hlt">decades</span>. Demographic profile, treatment modalities, radioactive iodine (RAI) dose, and recurrence rates were studied and outcomes were compared by χ 2 test and ANOVA using SPSS v15.0. A p value of < 0.05 was considered significant. Results. Altogether, 3737 patients were diagnosed with Grave's thyrotoxicosis over the 4 <span class="hlt">decades</span>. Use of RAI has increased from 43.1% in Group A to 68% in Group D (p < 0.001). The dose of RAI has increased (p < 0.001) and there has been a reduction in recurrence rate with higher dose of RAI. Surgical intervention rates decreased from 55.3% to 12.3% (p < 0.001) over time. Conclusions. Analysis of a large dataset of patients with Grave's thyrotoxicosis suggests increasing use of RAI as the preferred first line of treatment. Furthermore, using a single higher dose of RAI and adoption of total thyroidectomy have decreased recurrence rates. PMID:27313946</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/20853187','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/20853187"><span>NDVI indicated characteristics of vegetation cover <span class="hlt">change</span> in China's metropolises over the last three <span class="hlt">decades</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Sun, Jinyu; Wang, Xuhui; Chen, Anping; Ma, Yuecun; Cui, Mengdi; Piao, Shilong</p> <p>2011-08-01</p> <p>How urban vegetation was influenced by three <span class="hlt">decades</span> of intensive urbanization in China is of great interest but rarely studied. In this paper, we used satellite derived Normalized Difference Vegetation Index (NDVI) and socioeconomic data to evaluate effects of urbanization on vegetation cover in China's 117 metropolises over the last three <span class="hlt">decades</span>. Our results suggest that current urbanization has caused deterioration of urban vegetation across most cities in China, particularly in East China. At the national scale, average urban area NDVI (NDVI(u)) significantly decreased during the last three <span class="hlt">decades</span> (P < 0.01), and two distinct periods with different trends can be identified, 1982-1990 and 1990-2006. NDVI(u) did not show statistically significant trend before 1990 but decrease remarkably after 1990 (P < 0.01). Different regions also showed difference in the timing of NDVI(u) turning point. The year when NDVI(u) started to decline significantly for Central China and East China was 1987 and 1990, respectively, while NDVI(u) in West China remained relatively constant until 1998. NDVI(u) <span class="hlt">changes</span> in the Yangtze River Delta and the Pearl River Delta, two regions which has been undergoing the most rapid urbanization in China, also show different characteristics. The Pearl River Delta experienced a rapid decline in NDVI(u) from the early 1980s to the mid-1990s; while in the Yangtze River Delta, NDVI(u) did not decline significantly until the early 1990s. Such different patterns of NDVI(u) <span class="hlt">changes</span> are closely linked with policy-oriented difference in urbanization dynamics of these regions, which highlights the importance of implementing a sustainable urban development policy.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3689001','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3689001"><span><span class="hlt">Decadal</span> <span class="hlt">Changes</span> in the World's Coastal Latitudinal Temperature Gradients</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Baumann, Hannes; Doherty, Owen</p> <p>2013-01-01</p> <p>Most of the world's living marine resources inhabit coastal environments, where average thermal conditions <span class="hlt">change</span> predictably with latitude. These coastal latitudinal temperature gradients (CLTG) coincide with important ecological clines,e.g., in marine species diversity or adaptive genetic variations, but how tightly thermal and ecological gradients are linked remains unclear. A first step is to consistently characterize the world's CLTGs. We extracted coastal cells from a global 1°×1° dataset of weekly sea surface temperatures (SST, 1982–2012) to quantify spatial and temporal variability of the world's 11 major CLTGs. Gradient strength, i.e., the slope of the linear mean-SST/latitude relationship, varied 3-fold between the steepest (North-American Atlantic and Asian Pacific gradients: −0.91°C and −0.68°C lat−1, respectively) and weakest CLTGs (African Indian Ocean and the South- and North-American Pacific gradients: −0.28, −0.29, −0.32°C lat−1, respectively). Analyzing CLTG strength by year revealed that seven gradients have weakened by 3–10% over the past three <span class="hlt">decades</span> due to increased warming at high compared to low latitudes. Almost the entire South-American Pacific gradient (6–47°S), however, has considerably cooled over the study period (−0.3 to −1.7°C, 31 years), and the substantial weakening of the North-American Atlantic gradient (−10%) was due to warming at high latitudes (42–60°N, +0.8 to +1.6°C,31 years) and significant mid-latitude cooling (Florida to Cape Hatteras 26–35°N, −0.5 to −2.2°C, 31 years). Average SST trends rarely resulted from uniform shifts throughout the year; instead individual seasonal warming or cooling patterns elicited the observed <span class="hlt">changes</span> in annual means. This is consistent with our finding of increased seasonality (i.e., summer-winter SST amplitude) in three quarters of all coastal cells (331 of 433). Our study highlights the regionally variable footprint of global climate <span class="hlt">change</span></p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFMGC32B..01P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFMGC32B..01P"><span>Inability of CMIP5 Climate Models to Simulate Recent Multi-<span class="hlt">decadal</span> Climate <span class="hlt">Change</span> in the Tropical Pacific.</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Power, S.; Delage, F.; Kociuba, G.; Wang, G.; Smith, I.</p> <p>2017-12-01</p> <p>Observed 15-year surface temperature trends beginning 1998 or later have attracted a great deal of interest because of an apparent slowdown in the rate of global warming, and contrasts between climate model simulations and observations of such trends. Many studies have addressed the statistical significance of these relatively short trends, whether they indicate a possible bias in models and the implications for global warming generally. Here we analyse historical and projected <span class="hlt">changes</span> in 38 CMIP5 climate models. All of the models simulate multi-<span class="hlt">decadal</span> warming in the Pacific over the past half-century that exceeds observed values. This stark difference cannot be fully explained by observed, internal multi-<span class="hlt">decadal</span> climate variability, even if allowance is made for an apparent tendency for models to underestimate internal multi-<span class="hlt">decadal</span> variability in the Pacific. We also show that CMIP5 models are not able to simulate the magnitude of the strengthening of the Walker Circulation over the past thirty years. Some of the reasons for these major shortcomings in the ability of models to simulate multi-<span class="hlt">decadal</span> variability in the Pacific, and the impact these findings have on our confidence in global 21st century projections, will be discussed.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/28332928','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/28332928"><span>Attitudinal <span class="hlt">Changes</span> Toward Homosexuality During the Past Two <span class="hlt">Decades</span> (1994-2014) in Korea.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Youn, Gahyun</p> <p>2018-01-01</p> <p>This study was conducted to examine recent Korean perspectives on homosexuality by comparing attitudes toward mental illness, crime, friendship, and civil rights related to homosexual people in 1994, 1999, 2004, 2009, and 2014. The respondents were 3,299 Korean men and women between 18 and 59 years of age, and the data were collected across 5 years. The major findings were that there has been greater acceptance of homosexuality and civil rights for homosexuals during the past two <span class="hlt">decades</span>, but the <span class="hlt">changes</span> have been slow; Korean homosexuals remain subjects of social stigma and discrimination primarily due to increased Christian activism.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29787903','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29787903"><span>Flood risk (d)evolution: Disentangling <span class="hlt">key</span> drivers of flood risk <span class="hlt">change</span> with a retro-model experiment.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Zischg, Andreas Paul; Hofer, Patrick; Mosimann, Markus; Röthlisberger, Veronika; Ramirez, Jorge A; Keiler, Margreth; Weingartner, Rolf</p> <p>2018-05-19</p> <p>Flood risks are dynamically <span class="hlt">changing</span> over time. Over <span class="hlt">decades</span> and centuries, the main drivers for flood risk <span class="hlt">change</span> are influenced either by perturbations or slow alterations in the natural environment or, more importantly, by socio-economic development and human interventions. However, <span class="hlt">changes</span> in the natural and human environment are intertwined. Thus, the analysis of the main drivers for flood risk <span class="hlt">changes</span> requires a disentangling of the individual risk components. Here, we present a method for isolating the individual effects of selected drivers of <span class="hlt">change</span> and selected flood risk management options based on a model experiment. In contrast to purely synthetic model experiments, we built our analyses upon a retro-model consisting of several spatio-temporal stages of river morphology and settlement structure. The main advantage of this approach is that the overall long-term dynamics are known and do not have to be assumed. We used this model setup to analyse the temporal evolution of the flood risk, for an ex-post evaluation of the <span class="hlt">key</span> drivers of <span class="hlt">change</span>, and for analysing possible alternative pathways for flood risk evolution under different governance settings. We showed that in the study region the construction of lateral levees and the consecutive river incision are the main drivers for decreasing flood risks over the last century. A rebound effect in flood risk can be observed following an increase in settlements since the 1960s. This effect is not as relevant as the river engineering measures, but it will become increasingly relevant in the future with continued socio-economic growth. The presented approach could provide a methodological framework for studying pathways for future flood risk evolvement and for the formulation of narratives for adapting governmental flood risk strategies to the spatio-temporal dynamics in the built environment. Copyright © 2018 Elsevier B.V. All rights reserved.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5694658','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5694658"><span>The <span class="hlt">Changing</span> Role of Health Care Professionals in Nursing Homes: A Systematic Literature Review of a <span class="hlt">Decade</span> of <span class="hlt">Change</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>van Stenis, Arend R.; van Wingerden, Jessica; Kolkhuis Tanke, Isolde</p> <p>2017-01-01</p> <p>Although the role of health care professionals is known to have <span class="hlt">changed</span> over the last years, few formal efforts have been made to examine this <span class="hlt">change</span> through means of a scientific review. Therefore, the goal of this paper was to investigate the <span class="hlt">changing</span> role of health care professionals in nursing homes, as well as the conditions that make this <span class="hlt">change</span> possible. A systematic review of health care literature published in the last <span class="hlt">decade</span> (2007–2017) was utilized to address these goals. Our findings suggest that although health care in nursing homes is shifting from task-oriented care to relation-oriented care (e.g., through an increased focus on patient dignity), various obstacles (e.g., negative self-image, work pressure, and a lack of developmental opportunities), needs (e.g., shared values, personal development, personal empowerment, team development, and demonstrating expertise), and competences (e.g., communication skills, attentiveness, negotiation skills, flexibility, teamwork, expertise, and coaching and leadership skills) still need to be addressed in order to successfully facilitate this <span class="hlt">change</span>. As such, this paper provides various implications for health care research, health care institutions, practitioners, HR professionals and managers, and occupational health research. PMID:29184529</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://coastaldynamics2017.dk/proceedings.html','USGSPUBS'); return false;" href="http://coastaldynamics2017.dk/proceedings.html"><span>Climate <span class="hlt">change</span>-driven cliff and beach evolution at <span class="hlt">decadal</span> to centennial time scales</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Erikson, Li; O'Neill, Andrea; Barnard, Patrick; Vitousek, Sean; Limber, Patrick</p> <p>2017-01-01</p> <p>Here we develop a computationally efficient method that evolves cross-shore profiles of sand beaches with or without cliffs along natural and urban coastal environments and across expansive geographic areas at <span class="hlt">decadal</span> to centennial time-scales driven by 21st century climate <span class="hlt">change</span> projections. The model requires projected sea level rise rates, extrema of nearshore wave conditions, bluff recession and shoreline <span class="hlt">change</span> rates, and cross-shore profiles representing present-day conditions. The model is applied to the ~470-km long coast of the Southern California Bight, USA, using recently available projected nearshore waves and bluff recession and shoreline <span class="hlt">change</span> rates. The results indicate that eroded cliff material, from unarmored cliffs, contribute 11% to 26% to the total sediment budget. Historical beach nourishment rates will need to increase by more than 30% for a 0.25 m sea level rise (~2044) and by at least 75% by the year 2100 for a 1 m sea level rise, if evolution of the shoreline is to keep pace with rising sea levels.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/26851614','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/26851614"><span>For Better or Worse? <span class="hlt">Change</span> in Service Use by Children Investigated by Child Welfare Over a <span class="hlt">Decade</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Stein, Ruth E K; Hurlburt, Michael S; Heneghan, Amy M; Zhang, Jinjin; Kerker, Bonnie; Landsverk, John; Horwitz, Sarah McCue</p> <p>2016-04-01</p> <p>Children, particularly minority children, referred to child welfare because of suspected maltreatment are vulnerable and need many services. We sought to assess whether service use has improved over the past <span class="hlt">decade</span> and whether racial-ethnic disparities in service use have decreased. We used 2 national data sets (the National Survey of Child and Adolescent Well-Being [NSCAW] I and II) collected a <span class="hlt">decade</span> apart to assess <span class="hlt">changes</span> over time in health, education, mental health (MH), and dental services and overall service use. In NSCAW II more children were young, had lower Child Behavior Checklist (CBCL) scores, and were Hispanic. We found significant increases in dental services, a decrease in special education services, and a decrease in MH services on the bivariate level (all P < .01). A large proportion of the <span class="hlt">change</span> in MH services occurred in school settings, but the pattern continued when examining only those services delivered outside of school. The greatest decrease occurred for children with CBCL scores <64. However, in multivariate analyses, older children, white non-Hispanic children, and children placed out of the home were significantly more likely to receive MH services. Rates of MH services controlling for CBCL scores showed no improvement over the <span class="hlt">decade</span>, nor was there a decrease in racial and ethnic disparities. These data showed no <span class="hlt">change</span> in MH services over time for children referred for child welfare evaluation, but improvement in dental services was noted. Racial and ethnic disparities persist. Decrease in MH services occurred predominantly among children whose MH symptoms were below the clinical range. Copyright © 2016 Academic Pediatric Association. Published by Elsevier Inc. All rights reserved.</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 <span class="hlt">Decadal</span> Climate 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 <span class="hlt">decadal</span> climate variability in the models is essential for the quality of <span class="hlt">decadal</span> climate predictions. Therefore, the understanding of those processes leading to <span class="hlt">decadal</span> climate variability needs to be improved. Several of these processes are already included in climate 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 - <span class="hlt">Decadal</span> Climate Predictions" (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 climate response to aerosol perturbations caused by volcanic eruptions and the stratospheric <span class="hlt">decadal</span> variability due to solar forcing, climate <span class="hlt">change</span> and ozone recovery. To account for the interaction between <span class="hlt">changing</span> ozone concentrations and climate a computationally efficient ozone chemistry module is developed and implemented in the MiKlip prediction 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 predictability 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://adsabs.harvard.edu/abs/1994ClDy....9..303T','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/1994ClDy....9..303T"><span><span class="hlt">Decadal</span> atmosphere-ocean variations in the Pacific</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Trenberth, Kevin E.; Hurrell, James W.</p> <p>1994-03-01</p> <p>Considerable evidence has emerged of a substantial <span class="hlt">decade</span>-long <span class="hlt">change</span> in the north Pacific atmosphere and ocean lasting from about 1976 to 1988. Observed significant <span class="hlt">changes</span> in the atmospheric circulation throughout the troposphere revealed a deeper and eastward shifted Aleutian low pressure system in the winter half year which advected warmer and moister air along the west coast of North America and into Alaska and colder air over the north Pacific. Consequently, there were increases in temperatures and sea surface temperatures (SSTs) along the west coast of North America and Alaska but decreases in SSTs over the central north Pacific, as well as <span class="hlt">changes</span> in coastal rainfall and streamflow, and decreases in sea ice in the Bering Sea. Associated <span class="hlt">changes</span> occurred in the surface wind stress, and, by inference, in the Sverdrup transport in the north Pacific Ocean. <span class="hlt">Changes</span> in the monthly mean flow were accompanied by a southward shift in the storm tracks and associated synoptic eddy activity and in the surface ocean sensible and latent heat fluxes. In addition to the <span class="hlt">changes</span> in the physical environment, the deeper Aleutian low increased the nutrient supply as seen through increases in total chlorophyll in the water column, phytoplankton and zooplankton. These <span class="hlt">changes</span>, along with the altered ocean currents and temperatures, <span class="hlt">changed</span> the migration patterns and increased the stock of many fish species. A north Pacific (NP) index is defined to measure the <span class="hlt">decadal</span> variations, and the temporal variability of the index is explored on daily, annual, interannual and <span class="hlt">decadal</span> time scales. The dominant atmosphere-ocean relation in the north Pacific is one where atmospheric <span class="hlt">changes</span> lead SSTs by one to two months. However, strong ties are revealed with events in the tropical Pacific, with <span class="hlt">changes</span> in tropical Pacific SSTs leading SSTs in the north Pacific by three months. <span class="hlt">Changes</span> in the storm tracks in the north Pacific help to reinforce and maintain the anomalous circulation in the</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://eric.ed.gov/?q=friend+AND+parent&pg=6&id=EJ929083','ERIC'); return false;" href="https://eric.ed.gov/?q=friend+AND+parent&pg=6&id=EJ929083"><span>Coping with Relationship Stressors: A <span class="hlt">Decade</span> Review</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>Seiffge-Krenke, Inge</p> <p>2011-01-01</p> <p>This review identifies <span class="hlt">key</span> issues in research on adolescent coping with stress with parents, friends, and romantic partners during the past <span class="hlt">decade</span>. An analysis of 78 studies revealed findings on relationship stressors and the potential links between the use of different coping styles for different relationship types. Research has confirmed…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://jnah.cnah.org/','USGSPUBS'); return false;" href="http://jnah.cnah.org/"><span><span class="hlt">Decadal</span> <span class="hlt">changes</span> in phenology of peak abundance patterns of woodland pond salamanders in northern Wisconsin</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Donner, Deahn M.; Ribic, Christine; Beck, Albert J.; Higgins, Dale; Eklund, Dan; Reinecke, Susan</p> <p>2015-01-01</p> <p>Woodland ponds are important landscape features that help sustain populations of amphibians that require this aquatic habitat for successful reproduction. Species abundance patterns often reflect site-specific differences in hydrology, physical characteristics, and surrounding vegetation. Large-scale processes such as <span class="hlt">changing</span> land cover and environmental conditions are other potential drivers influencing amphibian populations in the Upper Midwest, but little information exists on the combined effects of these factors. We used Blue-spotted (Ambystoma laterale Hallowell) and Spotted Salamander (A. maculatum Shaw) monitoring data collected at the same woodland ponds thirteen years apart to determine if <span class="hlt">changing</span> environmental conditions and vegetation cover in surrounding landscapes influenced salamander movement phenology and abundance. Four woodland ponds in northern Wisconsin were sampled for salamanders in April 1992-1994 and 2005-2007. While Blue-spotted Salamanders were more abundant than Spotted Salamanders in all ponds, there was no <span class="hlt">change</span> in the numbers of either species over the years. However, peak numbers of Blue-spotted Salamanders occurred 11.7 days earlier (range: 9-14 days) in the 2000s compared to the 1990s; Spotted Salamanders occurred 9.5 days earlier (range: 3 - 13 days). Air and water temperatures (April 13- 24) increased, on average, 4.8°C and 3.7°C, respectively, between the <span class="hlt">decades</span> regardless of pond. There were no discernible <span class="hlt">changes</span> in canopy openness in surrounding forests between <span class="hlt">decades</span> that would have warmed the water sooner (i.e., more light penetration). Our finding that salamander breeding phenology can vary by roughly 10 days in Wisconsin contributes to growing evidence that amphibian populations have responded to <span class="hlt">changing</span> climate conditions by shifting life-cycle events. Managers can use this information to adjust monitoring programs and forest management activities in the surrounding landscape to avoid vulnerable amphibian</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70176120','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70176120"><span><span class="hlt">Key</span> ecological responses to nitrogen are altered by climate <span class="hlt">change</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>Greaver, T.L.; Clark, C.M.; Compton, J.E.; Vallano, D.; Talhelm, A. F.; Weaver, C.P.; Band, L.E.; Baron, Jill S.; Davidson, E.A.; Tague, C.L.; Felker-Quinn, E.; Lynch, J.A.; Herrick, J.D.; Liu, L.; Goodale, C.L.; Novak, K. J.; Haeuber, R. A.</p> <p>2016-01-01</p> <p>Climate <span class="hlt">change</span> and anthropogenic nitrogen deposition are both important ecological threats. Evaluating their cumulative effects provides a more holistic view of ecosystem vulnerability to human activities, which would better inform policy decisions aimed to protect the sustainability of ecosystems. Our knowledge of the cumulative effects of these stressors is growing, but we lack an integrated understanding. In this Review, we describe how climate <span class="hlt">change</span> alters <span class="hlt">key</span> processes in terrestrial and freshwater ecosystems related to nitrogen cycling and availability, and the response of ecosystems to nitrogen addition in terms of carbon cycling, acidification and biodiversity.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016NatCC...6..836G','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016NatCC...6..836G"><span><span class="hlt">Key</span> ecological responses to nitrogen are altered by climate <span class="hlt">change</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Greaver, T. L.; Clark, C. M.; Compton, J. E.; Vallano, D.; Talhelm, A. F.; Weaver, C. P.; Band, L. E.; Baron, J. S.; Davidson, E. A.; Tague, C. L.; Felker-Quinn, E.; Lynch, J. A.; Herrick, J. D.; Liu, L.; Goodale, C. L.; Novak, K. J.; Haeuber, R. A.</p> <p>2016-09-01</p> <p>Climate <span class="hlt">change</span> and anthropogenic nitrogen deposition are both important ecological threats. Evaluating their cumulative effects provides a more holistic view of ecosystem vulnerability to human activities, which would better inform policy decisions aimed to protect the sustainability of ecosystems. Our knowledge of the cumulative effects of these stressors is growing, but we lack an integrated understanding. In this Review, we describe how climate <span class="hlt">change</span> alters <span class="hlt">key</span> processes in terrestrial and freshwater ecosystems related to nitrogen cycling and availability, and the response of ecosystems to nitrogen addition in terms of carbon cycling, acidification and biodiversity.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016EGUGA..18..107W','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016EGUGA..18..107W"><span>Mapping <span class="hlt">decadal</span> land cover <span class="hlt">changes</span> in the woodlands of north eastern Namibia using the Landsat satellite archive (1975-2014)</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Wingate, Vladimir; Phinn, Stuart; Kuhn, Nikolaus</p> <p>2016-04-01</p> <p>Woodland savannahs provide essential ecosystem functions and services to communities. On the African continent, they are widely utilized and converted to intensive land uses. This study investigates the land cover <span class="hlt">changes</span> over 108,038 km2 in NE Namibia using multi-sensor Landsat imagery, at <span class="hlt">decadal</span> intervals from 1975 to 2014, with a post-classification <span class="hlt">change</span> detection method and supervised Regression Tree classifiers. We discuss likely impacts of land tenure and reforms over the past four <span class="hlt">decades</span> on <span class="hlt">changes</span> in land use and land cover. These included losses, gains and exchanges between predominant land cover classes. Exchanges comprised logical conversions between woodland and agricultural classes, implying woodland clearing for arable farming, cropland abandonment and vegetation succession. The dominant <span class="hlt">change</span> was a reduction in the area of the woodland class due to the expansion of the agricultural class, specifically, small-scale cereal and pastoral production. Woodland area decreased from 90% of the study area in 1975 to 83% in 2014, while cleared land increased from 9% to 14%. We found that the main land cover <span class="hlt">changes</span> are conversion from woodland to agricultural and urban land uses, driven by urban expansion and woodland clearing for subsistence-based agriculture and pastoralism.</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('https://eric.ed.gov/?q=private+AND+sector+AND+public+AND+sector+AND+differences&pg=7&id=ED524540','ERIC'); return false;" href="https://eric.ed.gov/?q=private+AND+sector+AND+public+AND+sector+AND+differences&pg=7&id=ED524540"><span>Vital Collaboratives, Alliances, and Partnerships: A Search for <span class="hlt">Key</span> Elements of an Effective Public-Private Partnership</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>Young, Charles Keith</p> <p>2010-01-01</p> <p>Owing to the significant structural <span class="hlt">changes</span> that have occurred in the global marketplace over the past 2 <span class="hlt">decades</span>, a corresponding increase of public-private partnerships have been established among the business sector, local governments, and public community colleges. This qualitative project sought to identify and substantiate <span class="hlt">key</span> elements that…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://eric.ed.gov/?q=increase+AND+productivity&pg=6&id=EJ863153','ERIC'); return false;" href="https://eric.ed.gov/?q=increase+AND+productivity&pg=6&id=EJ863153"><span>The <span class="hlt">Change</span> in Publication Rates at Undergraduate Institutions during the Last Three <span class="hlt">Decades</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>Leber, Phyllis A.; Williams, Benjamin R.; Yoder, Claude H.</p> <p>2009-01-01</p> <p>Publication rates for chemistry faculty at 55 predominantly undergraduate institutions were ascertained from the number of publications and presentations produced over the past three <span class="hlt">decades</span>. Comparison of the publications for the last <span class="hlt">decade</span> with those reported for the earlier <span class="hlt">decades</span> showed that the majority of institutions surveyed have…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012AGUFM.A21E0116R','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012AGUFM.A21E0116R"><span>Observing <span class="hlt">Decadal</span> Trends in Atmospheric Feedbacks and Climate <span class="hlt">Change</span> with Zeus and CLARREO</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Revercomb, H. E.; Best, F. A.; Knuteson, R. O.; Tobin, D. C.; Taylor, J. K.; Gero, P.; Adler, D. P.; Pettersen, C.; Mulligan, M.; Tobin, D. C.</p> <p>2012-12-01</p> <p>New technologies for observing <span class="hlt">decadal</span> trends in atmospheric feedbacks and climate <span class="hlt">change</span> from space have been recently demonstrated via a NASA Instrument Incubator Program (IIP) project of our group and the Anderson Group of Harvard University. Using these new technologies, a mission named Zeus has been proposed to the first NASA Earth Venture Instruments opportunity (EVI-1). Zeus would provide a low cost mechanism to initiate a new era in high spectral resolution IR climate Benchmark and Intercalibration observations, the basis for which has been established by definition of the CLARREO mission in the 2007 NRC "<span class="hlt">Decadal</span> Survey" and by the Science Definition Team established by NASA LaRC to further the full blown CLARREO mission. Zeus EVI is a low-cost, low-risk, and high-value EVI mission that will deploy an Absolute Radiance Interferometer (ARI) instrument to measure absolute spectrally resolved infrared radiance over much of the Earth-emitted spectrum with ultra-high accuracy (<0.1 K 3-sigma brightness temperature). Zeus makes use of broad spectral coverage (3.7-50 microns) and high spectral resolution (<1 cm-1) to provide benchmark products for climate trending with much higher information content than traditional spectrally-integrated measurements. While ARI requirements for accuracy and spectral properties are demanding, the overall instrument is relatively simple and low-cost because of the limited requirements on spatial sampling (25-100 km nadir-only footprints spaced at < 250 km) and on noise performance (climate products are created by combining many samples). The orbit chosen for Zeus must provide coverage immune to time-of-day sampling errors. Because of its relatively high rate of precession, an attractive baseline option for Zeus EVI is the 51.6 degrees inclination orbit of the International Space Station (ISS). For Zeus deployment on the ISS, higher latitude climate benchmark information will be obtained from operational sounders intercalibrated by</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://eric.ed.gov/?q=changing+AND+beliefs&pg=7&id=EJ722555','ERIC'); return false;" href="https://eric.ed.gov/?q=changing+AND+beliefs&pg=7&id=EJ722555"><span>Six <span class="hlt">Key</span> Factors for <span class="hlt">Changing</span> Preservice Teachers' Attitudes/Beliefs about Diversity</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>Garmon, M. Arthur</p> <p>2005-01-01</p> <p>In this article the author postulates there are six <span class="hlt">key</span> factors associated with <span class="hlt">changing</span> preservice teachers' attitudes toward and beliefs about diversity-their dispositions, which include openness, self-awarenesss/self-reflectiveness, and commitment to social justice; and their experiences, which include intercultural, educational, and support…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017EGUGA..19.4171A','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017EGUGA..19.4171A"><span>Effect of environmental <span class="hlt">change</span> on the morphology of tidally influenced deltas over multi-<span class="hlt">decadal</span> timescale</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Angamuthu, Balaji; Darby, Stephen; Nicholls, Robert</p> <p>2017-04-01</p> <p>An understanding of the geomorphological processes affecting deltas is essential to improve our understanding of the risks that deltas face, especially as human impacts are likely to intensify in the future. Unfortunately, there is limited reliable data on river deltas, meaning that the task of demonstrating the links between morphodynamic and environmental <span class="hlt">change</span> is challenging. This presentation aims to answer the questions of how delta morphology evolves over multi-<span class="hlt">decadal</span> timescales under multiple drivers, focussing on tidally-influenced deltas, as some of these, such as the Ganges-Brahmaputra-Meghna (GBM) delta are heavily populated. A series of idealised model simulations over 102 years were used to explore the influence of three <span class="hlt">key</span> drivers on delta morphodynamics, both individually and together: (i) varying combinations of water and sediment discharges from the upstream catchment, (ii) varying rates of relative sea-level rise (RSLR), and (iii) selected human interventions within the delta, such as polders, cross-dams and <span class="hlt">changing</span> land cover. Model simulations revealed that delta progradation rates are more sensitive to variations in water discharge than variations in fluvial sediment supply. Unlike mere aggradation during RSLR, the delta front experienced aggradational progradation due to tides. As expected, the area of the simulated sub-aerial delta increases with increasing sediment discharge, but decreases with increasing water discharge. But, human modifications are important. For example, the sub-aerial delta shrinks with increasing RSLR, but it does not when the sub-aerial delta is polderised, provided the polders are restricted from erosion. However, the polders are vulnerable to flooding as they lose relative elevation and can make the delta building process unsustainable. Cross-dams built to steer zones of land accretion within the delta accomplish their local goal, but may not result in net land gain at the scale of the delta. Applying these</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018TCry...12..477L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018TCry...12..477L"><span><span class="hlt">Decadal</span> <span class="hlt">changes</span> of surface elevation over permafrost area estimated using reflected GPS signals</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Liu, Lin; Larson, Kristine M.</p> <p>2018-02-01</p> <p>Conventional benchmark-based survey and Global Positioning System (GPS) have been used to measure surface elevation <span class="hlt">changes</span> over permafrost areas, usually once or a few times a year. Here we use reflected GPS signals to measure temporal <span class="hlt">changes</span> of ground surface elevation due to dynamics of the active layer and near-surface permafrost. Applying the GPS interferometric reflectometry technique to the multipath signal-to-noise ratio data collected by a continuously operating GPS receiver mounted deep in permafrost in Barrow, Alaska, we can retrieve the vertical distance between the antenna and reflecting surface. Using this unique kind of observables, we obtain daily <span class="hlt">changes</span> of surface elevation during July and August from 2004 to 2015. Our results show distinct temporal variations at three timescales: regular thaw settlement within each summer, strong interannual variability that is characterized by a sub-<span class="hlt">decadal</span> subsidence trend followed by a brief uplift trend, and a secular subsidence trend of 0.26 ± 0.02 cm year-1 during 2004 and 2015. This method provides a new way to fully utilize data from continuously operating GPS sites in cold regions for studying dynamics of the frozen ground consistently and sustainably over a long time.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/26477304','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/26477304"><span>The <span class="hlt">changing</span> model of big pharma: impact of <span class="hlt">key</span> trends.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Gautam, Ajay; Pan, Xiaogang</p> <p>2016-03-01</p> <p>Recent years have seen exciting breakthroughs in biomedical sciences that are producing truly novel therapeutics for unmet patient needs. However, the pharmaceutical industry is also facing significant barriers in the form of pricing and reimbursement, continued patent expirations and challenging market dynamics. In this article, we have analyzed data from the 1995-2015 period, on <span class="hlt">key</span> aspects such as revenue distribution, research units, portfolio mix and emerging markets to identify four <span class="hlt">key</span> trends that help to understand the <span class="hlt">change</span> in strategic focus, realignment of R&D footprint, the shift from primary care toward specialty drugs and biologics and the growth of emerging markets as major revenue drivers for big pharma. Copyright © 2015 The Authors. Published by Elsevier Ltd.. All rights reserved.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/22692419','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/22692419"><span>Newborn survival in Malawi: a <span class="hlt">decade</span> of <span class="hlt">change</span> and future implications.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Zimba, Evelyn; Kinney, Mary V; Kachale, Fannie; Waltensperger, Karen Z; Blencowe, Hannah; Colbourn, Tim; George, Joby; Mwansambo, Charles; Joshua, Martias; Chanza, Harriet; Nyasulu, Dorothy; Mlava, Grace; Gamache, Nathalie; Kazembe, Abigail; Lawn, Joy E</p> <p>2012-07-01</p> <p>Malawi is one of two low-income sub-Saharan African countries on track to meet the Millennium Development Goal (MDG 4) for child survival despite high fertility and HIV and low health worker density. With neonatal deaths becoming an increasing proportion of under-five deaths, addressing newborn survival is critical for achieving MDG 4. We examine <span class="hlt">change</span> for newborn survival in the <span class="hlt">decade</span> 2000-10, analysing mortality and coverage indicators whilst considering other contextual factors. We assess national and donor funding, as well as policy and programme <span class="hlt">change</span> for newborn survival using standard analyses and tools being applied as part of a multi-country analysis. Compared with the 1990s, progress towards MDG 4 and 5 accelerated considerably from 2000 to 2010. Malawi's neonatal mortality rate (NMR) reduced slower than annual reductions in mortality for children 1-59 months and maternal mortality (NMR reduced 3.5% annually). Yet, the NMR reduced at greater pace than the regional and global averages. A significant increase in facility births and other health system <span class="hlt">changes</span>, including increased human resources, likely contributed to this decline. High level attention for maternal health and associated comprehensive policy <span class="hlt">change</span> has provided a platform for a small group of technical and programme experts to link in high impact interventions for newborn survival. The initial entry point for newborn care in Malawi was mainly through facility initiatives, such as Kangaroo Mother Care. This transitioned to an integrated and comprehensive approach at community and facility level through the Community-Based Maternal and Newborn Care package, now being implemented in 17 of 28 districts. Addressing quality gaps, especially for care at birth in facilities, and including newborn interventions in child health programmes, will be critical to the future agenda of newborn survival in Malawi.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70033972','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70033972"><span><span class="hlt">Decadal</span>-timescale estuarine geomorphic <span class="hlt">change</span> under future scenarios of climate and sediment supply</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Ganju, N.K.; Schoellhamer, D.H.</p> <p>2010-01-01</p> <p>Future estuarine geomorphic <span class="hlt">change</span>, in response to climate <span class="hlt">change</span>, sea-level rise, and watershed sediment supply, may govern ecological function, navigation, and water quality. We estimated geomorphic <span class="hlt">changes</span> in Suisun Bay, CA, under four scenarios using a tidal-timescale hydrodynamic/sediment transport model. Computational expense and data needs were reduced using the morphological hydrograph concept and the morphological acceleration factor. The four scenarios included (1) present-day conditions; (2) sea-level rise and freshwater flow <span class="hlt">changes</span> of 2030; (3) sea-level rise and decreased watershed sediment supply of 2030; and (4) sea-level rise, freshwater flow <span class="hlt">changes</span>, and decreased watershed sediment supply of 2030. Sea-level rise increased water levels thereby reducing wave-induced bottom shear stress and sediment redistribution during the wind-wave season. Decreased watershed sediment supply reduced net deposition within the estuary, while minor <span class="hlt">changes</span> in freshwater flow timing and magnitude induced the smallest overall effect. In all future scenarios, net deposition in the entire estuary and in the shallowest areas did not keep pace with sea-level rise, suggesting that intertidal and wetland areas may struggle to maintain elevation. Tidal-timescale simulations using future conditions were also used to infer <span class="hlt">changes</span> in optical depth: though sea-level rise acts to decrease mean light irradiance, decreased suspended-sediment concentrations increase irradiance, yielding small <span class="hlt">changes</span> in optical depth. The modeling results also assisted with the development of a dimensionless estuarine geomorphic number representing the ratio of potential sediment import forces to sediment export forces; we found the number to be linearly related to relative geomorphic <span class="hlt">change</span> in Suisun Bay. The methods implemented here are widely applicable to evaluating future scenarios of estuarine <span class="hlt">change</span> over <span class="hlt">decadal</span> timescales. ?? The Author(s) 2009.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70028201','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70028201"><span>Spatial use by wintering greater white-fronted geese relative to a <span class="hlt">decade</span> of habitat <span class="hlt">change</span> in California's Central Valley</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Ackerman, Joshua T.; Takekawa, John Y.; Orthmeyer, D.L.; Fleskes, J.P.; Yee, J.L.; Kruse, K.L.</p> <p>2006-01-01</p> <p>We investigated the effect of recent habitat <span class="hlt">changes</span> in California's Central Valley on wintering Pacific greater white-fronted geese (Anser albifrons frontalis) by comparing roost-to-feed distances, distributions, population range sizes, and habitat use during 1987-1990 and 1998-2000. These habitat <span class="hlt">changes</span> included wetland restoration and agricultural land enhancement due to the 1990 implementation of the Central Valley Joint Venture, increased land area used for rice (Oryza sativa) production, and the practice of flooding, rather than burning, rice straw residues for decomposition because of burning restrictions enacted in 1991. Using radiotelemetry, we tracked 192 female geese and recorded 4,516 locations. Geese traveled shorter distances between roosting and feeding sites during 1998-2000 (24.2 ?? 2.2 km) than during 1987-1990 (32.5 ?? 3.4 km); distance traveled tended to decline throughout winter during both <span class="hlt">decades</span> and varied among watershed basins. Population range size was smaller during 1998-2000 (3,367 km2) than during 1987-1990 (5,145 km2), despite a 2.2-fold increase in the size of the Pacific Flyway population of white-fronted geese during the same time period. The population range size also tended to increase throughout winter during both <span class="hlt">decades</span>. Feeding and roosting distributions of geese also differed between <span class="hlt">decades</span>; geese shifted into basins that had the greatest increases in the amount of area in rice production (i.e., American Basin) and out of other basins (i.e., Delta Basin). The use of rice habitat for roosting (1987-1990: 40%, 1998-2000: 54%) and feeding (1987-1990: 57%, 1998-2000: 72%) increased between <span class="hlt">decades</span>, whereas use of wetlands declined for roosting (1987-1990: 36%, 1998-2000: 31%) and feeding (1987-1990: 22%, 1998-2000: 12%). Within postharvested rice habitats, geese roosted and fed primarily in burned rice fields during 1987-1990 (roost: 43%, feed: 34%), whereas they used flooded rice fields during 1998-2000 (roost: 78%, feed: 64</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=20150008935&hterms=coming&qs=N%3D0%26Ntk%3DAll%26Ntx%3Dmode%2Bmatchall%26Ntt%3Dcoming','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=20150008935&hterms=coming&qs=N%3D0%26Ntk%3DAll%26Ntx%3Dmode%2Bmatchall%26Ntt%3Dcoming"><span>Relay Telecommunications for the Coming <span class="hlt">Decade</span> of Mars Exploration</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Edwards, C.; DePaula, R.</p> <p>2010-01-01</p> <p>Over the past <span class="hlt">decade</span>, an evolving network of relay-equipped orbiters has advanced our capabilities for Mars exploration. NASA's Mars Global Surveyor, 2001 Mars Odyssey, and Mars Reconnaissance Orbiter (MRO), as well as ESA's Mars Express Orbiter, have provided telecommunications relay services to the 2003 Mars Exploration Rovers, Spirit and Opportunity, and to the 2007 Phoenix Lander. Based on these successes, a roadmap for continued Mars relay services is in place for the coming <span class="hlt">decade</span>. MRO and Odyssey will provide <span class="hlt">key</span> relay support to the 2011 Mars Science Laboratory (MSL) mission, including capture of critical event telemetry during entry, descent, and landing, as well as support for command and telemetry during surface operations, utilizing new capabilities of the Electra relay payload on MRO and the Electra-Lite payload on MSL to allow significant increase in data return relative to earlier missions. Over the remainder of the <span class="hlt">decade</span> a number of additional orbiter and lander missions are planned, representing new orbital relay service providers and new landed relay users. In this paper we will outline this Mars relay roadmap, quantifying relay performance over time, illustrating planned support scenarios, and identifying <span class="hlt">key</span> challenges and technology infusion opportunities.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFM.B13E0674B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFM.B13E0674B"><span>Uncertainties in detecting <span class="hlt">decadal</span> <span class="hlt">change</span> in extractable soil elements in Northern Forests</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Bartlett, O.; Bailey, S. W.; Ducey, M. J.</p> <p>2016-12-01</p> <p>Northern Forest ecosystems have been or are being impacted by land use <span class="hlt">change</span>, forest harvesting, acid deposition, atmospheric CO2 enrichment, and climate <span class="hlt">change</span>. Each of these has the potential to modify soil forming processes, and the resulting chemical stocks. Horizontal and vertical variations in concentrations complicate determination of temporal <span class="hlt">change</span>. This study evaluates sample design, sample size, and differences among observers as sources of uncertainty when quantifying soil temporal <span class="hlt">change</span> over regional scales. Forty permanent, northern hardwood, monitoring plots were established on the White Mountain National Forest in central New Hampshire and western Maine. Soil pits were characterized and sampled by genetic horizon at plot center in 2001 and resampled again in 2014 two-meters on contour from the original sampling location. Each soil horizon was characterized by depth, color, texture, structure, consistency, boundaries, coarse fragments, and roots from the forest floor to the upper C horizon, the relatively unaltered glacial till parent material. Laboratory analyses included pH in 0.01 M CaCl2 solution and extractable Ca, Mg, Na, K, Al, Mn, and P in 1 M NH4OAc solution buffered at pH 4.8. Significant elemental differences were identified by genetic horizon from paired t-tests (p ≤ 0.05) indicate temporal <span class="hlt">change</span> across the study region. Power analysis, 0.9 power (α = 0.05), revealed sampling size was appropriate within this region to detect concentration <span class="hlt">change</span> by genetic horizon using a stratified sample design based on topographic metrics. There were no significant differences between observers' descriptions of physical properties. As physical properties would not be expected to <span class="hlt">change</span> over a <span class="hlt">decade</span>, this suggests spatial variation in physical properties between the pairs of sampling pits did not detract from our ability to detect temporal <span class="hlt">change</span>. These results suggest that resampling efforts within a site, repeated across a region, to quantify</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013DSRII..96...19P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013DSRII..96...19P"><span>Status and <span class="hlt">changing</span> patterns on coral reefs in Thailand during the last two <span class="hlt">decades</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Phongsuwan, Niphon; Chankong, Anchalee; Yamarunpatthana, Chaimongkol; Chansang, Hansa; Boonprakob, Ronnawon; Petchkumnerd, Padorn; Thongtham, Nalinee; Paokantha, Sathika; Chanmethakul, Thanongsak; Panchaiyapoom, Paitoon; Bundit, On-Anong</p> <p>2013-11-01</p> <p>A long-term survey on monitoring coral reef status using the Manta-tow technique has been carried out over approximately two <span class="hlt">decades</span> in Thailand. This paper presents results of the survey from three off-shore areas (north, central and south) in the Andaman Sea (since 1988) and from the two near-shore areas and one off-shore area in the Gulf of Thailand (GoT, since 1995). The results revealed variations in the <span class="hlt">change</span> of live coral cover over time between different locations. Natural and direct/indirect man-made disturbances have influenced these <span class="hlt">changes</span>. Until early 2010, reefs in the Andaman Sea were in better condition than those in the Gulf of Thailand. The coral bleaching in mid-2010, however, greatly impacted many reefs both seas. The northern off-shore area in the Andaman Sea showed the most damage, while reefs in the lower west of the Gulf of Thailand were least affected. Long-term monitoring of <span class="hlt">changes</span> on reefs subjected to different environmental factors and human pressures is essential for the understanding and prediction of reef recovery in the face of climate <span class="hlt">change</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://eric.ed.gov/?q=marketing+AND+research&pg=2&id=EJ948755','ERIC'); return false;" href="https://eric.ed.gov/?q=marketing+AND+research&pg=2&id=EJ948755"><span>A <span class="hlt">Decade</span> of Scholarship in Marketing Education</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>Abernethy, Avery M.; Padgett, Daniel</p> <p>2011-01-01</p> <p>The teaching environment in business schools has <span class="hlt">changed</span> dramatically over the last <span class="hlt">decade</span>. But the last comprehensive review of the scholarship of teaching was conducted more than a <span class="hlt">decade</span> ago. Where and from whom do the best practices for teaching originate today? To answer this question, the authors examine marketing education scholarship…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/24814028','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/24814028"><span><span class="hlt">Changes</span> in clinical presentation and staging of lung cancer over two <span class="hlt">decades</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Leiro-Fernández, Virginia; Mouronte-Roibás, Cecilia; Ramos-Hernández, Cristina; Botana-Rial, Maribel; González-Piñeiro, Ana; García-Rodríguez, Esmeralda; Represas-Represas, Cristina; Fernández-Villar, Alberto</p> <p>2014-10-01</p> <p>Important clinical and epidemiological <span class="hlt">changes</span> have been observed in lung cancer (LC) in our healthcare area compared to the previous <span class="hlt">decade</span>. In the last 10 years, specific LC care circuits have been implemented and the active search for cases has been stepped up. The aim of this study was to analyze the progress of these <span class="hlt">changes</span> over the last 20 years. This is a retrospective study comparing clinical and epidemiological <span class="hlt">changes</span> between 2 historical cohorts of LC patients (1992-1994 [group 1, 164 patients] and 2004-2006 [group 2, 250 patients]) and a current group from the period 2011-2012 (group 3, 209 patients) Two hundred and nine (209) LC patients were included in group 3 (2011-2012 period). After comparing groups 3 and 2, a non-significant rise in smoking was observed in women (59% vs 41%, p=.25), while the prevalence of adenocarcinoma was unchanged (45% vs 44%, p=.9). The main <span class="hlt">changes</span> observed were the increase in cases with previous malignancies (23% vs 16%, p=.04), the rise in patients with no associated LC symptoms (33% vs 16%, p<.001), and an increased number of localized NSCLC (non-small cell LC) diagnoses (42% vs 24% in series 2, p<.001 and 14.2% in series 1, p<.001). The number of LC patients diagnosed in localized stages has increased significantly. Furthermore, the number of patients with no symptoms associated with LC and with a history of previous malignancy were significantly increased. Copyright © 2013 SEPAR. Published by Elsevier Espana. All rights reserved.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016EGUGA..18.4811H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016EGUGA..18.4811H"><span>Abrupt <span class="hlt">decadal</span>-to-centennial hydroclimate <span class="hlt">changes</span> in the Mediterranean region since the mid-Holocene</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Hu, Hsun-Ming; Shen, Chuan-Chou; Jiang, Xiuyang; Wang, Yongjin; Mii, Horng-Sheng; Michel, Véronique</p> <p>2016-04-01</p> <p>A series of severe drought events in the Mediterranean region over the past two <span class="hlt">decades</span> has posed a threat on both human society and biosystem. Holocene hydrological dynamics can offer valuable clues for understanding future climate and making proper adaption strategy. Here, we present a <span class="hlt">decadal</span>-resolved stalagmite record documenting various hydroclimatic fluctuations in the north central Mediterranean region since the middle Holocene. The stalagmite δ18O sequence shows dramatic instability, characterized by abrupt shifts between dry and wet conditions <50 years. The timing of regional culture demises, such as the Hittite Kingdom, Mycenaean Greece, Akkadian Empire, Egyptian Old Kingdom, and Uruk, occurred during the drought events, suggesting an important role of climate impact on human civilization. The unstable hydroclimate evolution is related to transferred North Atlantic Oscillation states. Rate of rapid transfer of precipitation patterns, which can be pin-pointed by our good chronology, improves the prediction to future climate <span class="hlt">changes</span> in North Atlantic region. We also found that a strong correlation between this stalagmite δ18O and sea surface temperatures especially in Pacific Ocean. This agreement suggests a distant interregional climate teleconnection.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012GBioC..26.3001F','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012GBioC..26.3001F"><span><span class="hlt">Decadal</span> <span class="hlt">changes</span> in the aragonite and calcite saturation state of the Pacific Ocean</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Feely, Richard A.; Sabine, Christopher L.; Byrne, Robert H.; Millero, Frank J.; Dickson, Andrew G.; Wanninkhof, Rik; Murata, Akihiko; Miller, Lisa A.; Greeley, Dana</p> <p>2012-09-01</p> <p>Based on measurements from the WOCE/JGOFS global CO2 survey, the CLIVAR/CO2 Repeat Hydrography Program and the Canadian Line P survey, we have observed an average decrease of 0.34% yr-1 in the saturation state of surface seawater in the Pacific Ocean with respect to aragonite and calcite. The upward migrations of the aragonite and calcite saturation horizons, averaging about 1 to 2 m yr-1, are the direct result of the uptake of anthropogenic CO2 by the oceans and regional <span class="hlt">changes</span> in circulation and biogeochemical processes. The shoaling of the saturation horizon is regionally variable, with more rapid shoaling in the South Pacific where there is a larger uptake of anthropogenic CO2. In some locations, particularly in the North Pacific Subtropical Gyre and in the California Current, the <span class="hlt">decadal</span> <span class="hlt">changes</span> in circulation can be the dominant factor in controlling the migration of the saturation horizon. If CO2 emissions continue as projected over the rest of this century, the resulting <span class="hlt">changes</span> in the marine carbonate system would mean that many coral reef systems in the Pacific would no longer be able to sustain a sufficiently high rate of calcification to maintain the viability of these ecosystems as a whole, and these <span class="hlt">changes</span> perhaps could seriously impact the thousands of marine species that depend on them for survival.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://files.eric.ed.gov/fulltext/ED101230.pdf','ERIC'); return false;" href="http://files.eric.ed.gov/fulltext/ED101230.pdf"><span>A <span class="hlt">Decade</span> of <span class="hlt">Change</span> in Employer Attitudes Toward Epilepsy.</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>Hartlage, Lawrence C.</p> <p></p> <p>The attitudes of parents and peers toward handicaps, particularly epilepsy, play an important part in determining how debilitating the handicap may actually be. This project compared attitudes of employers toward epilepsy in the early 1960's with their attitudes in the current <span class="hlt">decade</span>. As a control for possible generalized shifts in employer…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://eric.ed.gov/?q=Contraceptives+AND+adolescence&pg=5&id=EJ492556','ERIC'); return false;" href="https://eric.ed.gov/?q=Contraceptives+AND+adolescence&pg=5&id=EJ492556"><span>Adolescent Contraceptive Use and Communication: <span class="hlt">Changes</span> over a <span class="hlt">Decade</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>Poppen, Paul J.</p> <p>1994-01-01</p> <p>Compared sexual experiences of 186 college students in 1979 to those of 215 college students in 1989. Found that self-reported condom use increased over <span class="hlt">decade</span>. Percentage of respondents using any method of contraception and percentage who discussed contraception with partner increased from first to current partner but did not increase between…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://eric.ed.gov/?q=APA&pg=2&id=EJ1156406','ERIC'); return false;" href="https://eric.ed.gov/?q=APA&pg=2&id=EJ1156406"><span>Race, Ethnicity, and Gender of Faculty Members in APA- and CACREP-Accredited Programs: <span class="hlt">Changes</span> over Five <span class="hlt">Decades</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>Baggerly, Jennifer; Tan, Tony Xing; Pichotta, David; Warner, Aisha</p> <p>2017-01-01</p> <p>This study examined <span class="hlt">changes</span> in race, ethnicity, and gender of faculty members in APA- and CACREP-accredited counseling programs over 5 <span class="hlt">decades</span> based on the year of their degree. Of those faculty members working in accredited programs who graduated in the 1960s/1970s, 26.7% were female, 5.6% were racially diverse, and 1.7% were Latina/o. Of those…</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://eric.ed.gov/?q=lodges&pg=5&id=ED227243','ERIC'); return false;" href="https://eric.ed.gov/?q=lodges&pg=5&id=ED227243"><span>The <span class="hlt">Changing</span> Face of FE. Personal Perspectives on the <span class="hlt">Changes</span> That Have Taken Place in Further Education over the Last <span class="hlt">Decade</span>. An Occasional 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>Parkes, David, Ed.</p> <p></p> <p>In this occasional paper, seven persons--a further education (FE) officer, two principals, the head of a specialist youth training unit, a plumbing teacher, a head of division of alternative education, and a Further Education Staff College (Coombe Lodge) tutor--give their views of the <span class="hlt">changes</span> in further education in England during the past <span class="hlt">decade</span>.…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/28427433','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/28427433"><span>Prevalence of subclinical mastitis in Finnish dairy cows: <span class="hlt">changes</span> during recent <span class="hlt">decades</span> and impact of cow and herd factors.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Hiitiö, Heidi; Vakkamäki, Johanna; Simojoki, Heli; Autio, Tiina; Junnila, Jouni; Pelkonen, Sinikka; Pyörälä, Satu</p> <p>2017-04-20</p> <p>The dairy industry has undergone substantial structural <span class="hlt">changes</span> as intensive farming has developed during recent <span class="hlt">decades</span>. Mastitis continues to be the most common production disease of dairy cows. Nationwide surveys of mastitis prevalence are useful in monitoring udder health of dairy herds and to study the impact of structural <span class="hlt">changes</span> on the dairy industry. This survey on bovine subclinical mastitis was the first based on cow composite milk somatic cell count (SCC) data from the Finnish national health monitoring and milk recording database. A cow with composite milk SCC ≥200,000 cells/ml in at least one of the four test milkings during the year was considered to have subclinical mastitis and a cow with composite milk SCC ≥200,000 cells/ml in three or in all four test milkings during the year to have chronic subclinical mastitis. The aim of the study was to determine the prevalence of subclinical mastitis and chronic subclinical mastitis in Finland in 1991, 2001 and 2010 and to investigate cow and herd factors associated with elevated SCC. Prevalence of subclinical mastitis in Finland decreased over recent <span class="hlt">decades</span> from 22.3% (1991) and 20.1% (2001) to 19.0% (2010). Prevalence of chronic subclinical mastitis was 20.4% in 1991, 15.5% in 2001 and 16.1% in 2010. The most significant cow and herd factors associated with subclinical mastitis or high milk SCC were increasing parity, Holstein breed, free-stalls with an automatic milking system and organic production. Milk SCC were highest from July to September. Main factors associated with chronic mastitis were increasing parity and Holstein breed. Prevalence of subclinical mastitis in Finland decreased over recent <span class="hlt">decades</span>, the greatest <span class="hlt">change</span> taking place during the first <span class="hlt">decade</span> of the study. Prevalence of chronic subclinical mastitis significantly decreased from 1991. The most significant factors associated with both types of mastitis were increasing parity and Holstein breed, and for subclinical mastitis also</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20160001319','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20160001319"><span>Watching the Blue Planet from Space over Recent <span class="hlt">Decades</span>: What's up for Science and Society?</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Lindstrom, Eric J.</p> <p>2015-01-01</p> <p>Since the first photographs of “Earth Rise” taken by the Apollo astronauts in the 1960s galvanized the environmental movement, imaging of our planet from low Earth orbit has grown more sophisticated and diverse. Satellite and astronaut observations and imagery of the <span class="hlt">changing</span> ocean still have the power to galvanize oceanographers and society. So what are some of the <span class="hlt">key</span> ideas for oceanography and society that come out of out recent <span class="hlt">decades</span> of ocean observation from space? Satellite oceanography has made fundamental contributions to our understanding and estimation of <span class="hlt">changing</span> sea level, winds and storminess over the oceans, primary productivity of the seas, the role of the ocean in the water cycle, and the <span class="hlt">changes</span> in the ocean known as ocean acidification. Some of these phenomena interact in complex ways and Mother Nature hides the future well. However, some things are clear. Sea level rise has been monitored from space for more than 20 years and now we have a more nuanced understanding of regional variation in sea level rise and the contributions of ocean thermal expansion and the melting of glaciers and ice sheets. Wind vectors at the ocean surface have been measured for more than 2 <span class="hlt">decades</span> and provide evidence for shifts in wind patterns that help, for example, explain some of the regional variations in sea level rise. Chlorophyll-a has been estimated in a multi-<span class="hlt">decadal</span> record of observations and is being used to describe the shifts and trends in ocean primary productivity. Sea surface temperature estimation from space has records going back to the 1970s and provides critical information for the interaction of the ocean with the atmosphere. Sea surface salinity has been measured from space only within the last <span class="hlt">decade</span> and provides a novel new view of regional, seasonal, and inter-annual <span class="hlt">changes</span> in the ocean related to precipitation, river run-off, and eddy transport. Potential <span class="hlt">changes</span> in the Earth’s water cycle have a huge societal impact.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/11697254','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/11697254"><span>Understanding human impact on the Baltic ecosystem: <span class="hlt">changing</span> views in recent <span class="hlt">decades</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Elmgren, R</p> <p>2001-08-01</p> <p>Grave environmental problems, including contamination of biota by organochlorines and heavy metals, and increasing deep-water oxygen deficiency, were discovered in the Baltic Sea in the late 1960s. Toxic pollutants, including the newly discovered PCB, were initially seen as the main threat to the Baltic ecosystem, and the impaired reproduction found in Baltic seals and white-tailed eagles implied a threat also to human fish eaters. Countermeasures gradually gave results, and today the struggle to limit toxic pollution of the Baltic is an international environmental success story. Calculations showed that Baltic deep-water oxygen consumption must have increased, and that the Baltic nutrient load had grown about fourfold for nitrogen and 8 times for phosphorus. Evidence of increased organic production at all trophic levels in the ecosystem gradually accumulated. Phosphorus was first thought to limit Baltic primary production, but measurements soon showed that nitrogen is generally limiting in the open Baltic proper, except for nitrogen-fixing cyanobacteria. Today, the debate is concerned with whether phosphorus, by limiting nitrogen-fixers, can control open-sea ecosystem production, even where phytoplankton is clearly nitrogen limited. The Baltic lesson teaches us that our views of newly discovered environmental problems undergo repeated <span class="hlt">changes</span>, and that it may take <span class="hlt">decades</span> for scientists to agree on their causes. Once society decides on countermeasures, it may take <span class="hlt">decades</span> for them to become effective, and for nature to recover. Thus, environmental management decisions can hardly wait for scientific certainty. We should therefore view environmental management decisions as experiments, to be monitored, learned from, and then modified as needed.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015EPSC...10..916B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015EPSC...10..916B"><span>The International Lunar <span class="hlt">Decade</span> Declaration</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Beldavs, V.; Foing, B.; Bland, D.; Crisafulli, J.</p> <p>2015-10-01</p> <p>The International Lunar <span class="hlt">Decade</span> Declaration was discussed at the conference held November 9-13, 2014 in Hawaii "The Next Giant Leap: Leveraging Lunar Assets for Sustainable Pathways to Space" - http://2014giantleap.aerospacehawaii.info/ and accepted by a core group that forms the International Lunar <span class="hlt">Decade</span> Working Group (ILDWG) that is seeking to make the proposed global event and <span class="hlt">decade</span> long process a reality. The Declaration will be updated from time to time by members of the ILDWreflecting new knowledge and fresh perspectives that bear on building a global consortium with a mission to progress from lunar exploration to the transformation of the Moon into a wealth gene rating platform for the expansion of humankind into the solar system. When <span class="hlt">key</span> organizations have endorsed the idea and joined the effort the text of the Declaration will be considered final. An earlier International Lunar <span class="hlt">Decade</span> proposal was issued at the 8th ICEUM Conference in 2006 in Beijing together with 13 specific initiatives for lunar exploration[1,2,3]. These initiatives have been largely implemented with coordination among the different space agencies involved provided by the International Lunar Exploration Working Group[2,3]. The Second International Lunar <span class="hlt">Decade</span> from 2015 reflects current trends towards increasing involvement of commercial firms in space, particularly seeking opportunities beyond low Earth orbit. The central vision of the International Lunar <span class="hlt">Decade</span> is to build the foundations for a sustainable space economy through international collaboration concurrently addressing Lunar exploration and building a shared knowledge base;Policy development that enables collabo rative research and development leading to lunar mining and industrial and commercial development;Infrastructure on the Moon and in cislunar space (communications, transport, energy systems, way-stations, other) that reduces costs, lowers risks and speeds up the time to profitable operations;Enabling technologies</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013AGUFM.C11C..05F','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013AGUFM.C11C..05F"><span>A <span class="hlt">Decade</span> of Arctic Sea Ice Thickness <span class="hlt">Change</span> from Airborne and Satellite Altimetry (Invited)</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Farrell, S. L.; Richter-Menge, J.; Kurtz, N. T.; McAdoo, D. C.; Newman, T.; Zwally, H.; Ruth, J.</p> <p>2013-12-01</p> <p>Altimeters on both airborne and satellite platforms provide direct measurements of sea ice freeboard from which sea ice thickness may be calculated. Satellite altimetry observations of Arctic sea ice from ICESat and CryoSat-2 indicate a significant decline in ice thickness, and volume, over the last <span class="hlt">decade</span>. During this time the ice pack has experienced a rapid <span class="hlt">change</span> in its composition, transitioning from predominantly thick, multi-year ice to thinner, increasingly seasonal ice. We will discuss the regional trends in ice thickness derived from ICESat and IceBridge altimetry between 2003 and 2013, contrasting observations of the multi-year ice pack with seasonal ice zones. ICESat ceased operation in 2009, and the final, reprocessed data set became available recently. We extend our analysis to April 2013 using data from the IceBridge airborne mission, which commenced operations in 2009. We describe our current efforts to more accurately convert from freeboard to ice thickness, with a modified methodology that corrects for range errors, instrument biases, and includes an enhanced treatment of snow depth, with respect to ice type. With the planned launch by NASA of ICESat-2 in 2016 we can expect continuity of the sea ice thickness time series through the end of this <span class="hlt">decade</span>. Data from the ICESat-2 mission, together with ongoing observations from CryoSat-2, will allow us to understand both the <span class="hlt">decadal</span> trends and inter-annual variability in the Arctic sea ice thickness record. We briefly present the status of planned ICESat-2 sea ice data products, and demonstrate the utility of micro-pulse, photon-counting laser altimetry over sea ice.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/11743485','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/11743485"><span>An analysis of 6 <span class="hlt">decades</span> of hygiene-related advertising: 1940-2000.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Aiello, A E; Larson, E L</p> <p>2001-12-01</p> <p>To describe and analyze trends in hygiene-related advertisements and examine potential social and regulatory <span class="hlt">changes</span> that might be associated with these trends. From 1940 to 2000, advertisements in January issues of 2 widely read magazines were analyzed every fifth year, and 2 additional magazines only available from 1960 to 2000 were also analyzed every fifth year. In a content analysis, the total number of advertisements were determined and specific advertisements were grouped into categories (personal hygiene, dishwashing, laundry, and house cleaning) and further examined for the presence of 4 <span class="hlt">key</span> claims (aesthetics, health effects, time-saving, and microbial effects). From 1940 to 2000 for all magazines combined, 10.4% of the advertisements were devoted to hygiene products. After 1960 there were significantly fewer hygiene advertisements as compared with 1940 to 1955, and there was a significant increase after 1980 (P <.00001). Throughout all 6 <span class="hlt">decades</span>, most advertisements related to personal hygiene. There were no significant differences over time in the proportion of advertisements that made claims related to health, microbial effects, or aesthetics, but significantly more advertisements before 1960 made time-savings claims (P =.009). This content analysis reflects a cyclical attention in consumer advertising to personal and home hygiene products during the past 6 <span class="hlt">decades</span>, with a waning of interest in the <span class="hlt">decades</span> from 1960 to 1980 and an apparent resurgence of advertisements from 1985 to 2000. The potential contributions of federal regulatory bodies and societal <span class="hlt">changes</span> (e.g., new marketing strategies and options, product development, new and re-emerging infectious diseases, increasing concern about antimicrobial resistance, and increasing recognition that infectious diseases are unlikely to be eradicated) to these marketing trends are discussed.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20150000354','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20150000354"><span><span class="hlt">Changes</span> in Global Tropospheric OH Expected as a Result of Climate <span class="hlt">Change</span> Over the Last Several <span class="hlt">Decades</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Nicely, Julie M.; Salawitch, Ross J.; Canty, Timothy P.; Douglass, Anne R.; Duncan, Bryan N.; Lang, C.; Liang, Qing; Oman, Luke D.; Rodriguez, Jose M.; Stolarksi, Richard; <a style="text-decoration: none; " href="javascript:void(0); " onClick="displayelement('author_20150000354'); toggleEditAbsImage('author_20150000354_show'); toggleEditAbsImage('author_20150000354_hide'); "> <img style="display:inline; width:12px; height:12px; " src="images/arrow-up.gif" width="12" height="12" border="0" alt="hide" id="author_20150000354_show"> <img style="width:12px; height:12px; display:none; " src="images/arrow-down.gif" width="12" height="12" border="0" alt="hide" id="author_20150000354_hide"></p> <p>2014-01-01</p> <p>The oxidizing capacity of the troposphere is controlled primarily by the abundance of hydroxyl radical (OH). The global mean concentration of OH, [OH]_GLOBAL, inferred from measurements of methyl chloroform, has remained relatively constant during the past several <span class="hlt">decades</span>, despite rising levels of CH4 that should have led to a steady decline. Here we examine other factors that may have affected [OH]_GLOBAL, such as the <span class="hlt">changing</span> overhead burden of stratospheric O3 using observations from OMI, TOMS and SBUV; rising tropospheric H2O using observations from AIRS and reanalysis fields from MERRA; and widening of the climatological tropics using widening rate estimates from the literature and global OH fields from the GEOS Chemistry-Climate Model. Our analysis suggests these factors may have contributed a positive trend to [OH]_GLOBAL large enough to counter the decrease due to CH4.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/28501963','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/28501963"><span>Salinity-driven <span class="hlt">decadal</span> <span class="hlt">changes</span> in phytoplankton community in the NW Arabian Gulf of Kuwait.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Al-Said, Turki; Al-Ghunaim, Aws; Subba Rao, D V; Al-Yamani, Faiza; Al-Rifaie, Kholood; Al-Baz, Ali</p> <p>2017-06-01</p> <p>Evaluation of hydrological data obtained between 2000 and 2013 from a time series station in Kuwait Bay (station K6) and an offshore southern location (station 18) off Kuwait showed drastic increase in salinity by 6 units. We tested the hypothesis that increased salinity impacted phytoplankton community characteristics in these semiarid waters. The Arabian Gulf receives seasonal freshwater discharge in the north via Shatt Al-Arab estuary with a peak during March-July. A north to south gradient in the proportion of the freshwater exists between station A in the vicinity of Shatt Al-Arab estuary and station 18 in the southern offshore area. At station A, the proportion of freshwater was the highest (25.6-42.5%) in 1997 but decreased to 0.8-4.6% by 2012-2013. The prevailing hyperhaline conditions off Kuwait are attributed to decrease in the river flow. Phytoplankton data showed a decrease in the number of constituent taxa in the last one <span class="hlt">decade</span> from 353 to 159 in the Kuwait Bay and from 164 to 156 in the offshore area. A shift in their biomass was caused by a decrease in diatom species from 243 to 92 in the coastal waters and from 108 to 83 in the offshore areas with a concomitant increase of smaller algae. Mutivariate agglomerative hierarchical cluster analysis, non-metric multi-dimensional scaling, and one-way analysis of similarity analyses on phytoplankton data at different taxonomic levels confirmed significant <span class="hlt">changes</span> in their community organization on a <span class="hlt">decadal</span> scale. These evidences support our hypothesis that the salinity-related environmental <span class="hlt">changes</span> have resulted in a coincidental decrease in species diversity and significant <span class="hlt">changes</span> in phytoplankton community between the years 2000-2002 and 2012-2013, off Kuwait. This in turn would affect the pelagic trophodynamics as evident from a drastic decrease in the catch landings of Tenulosa ilisha (Suboor), Carangoides sp. (Hamam), Otolithes ruber (Nowaiby), Parastromateus niger (Halwaya), and Epinephelus</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/23897562','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/23897562"><span>Development of <span class="hlt">key</span> indicators to quantify the health impacts of climate <span class="hlt">change</span> on Canadians.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Cheng, June J; Berry, Peter</p> <p>2013-10-01</p> <p>This study aimed at developing a list of <span class="hlt">key</span> human health indicators for quantifying the health impacts of climate <span class="hlt">change</span> in Canada. A literature review was conducted in OVID Medline to identify health morbidity and mortality indicators currently used to quantify climate <span class="hlt">change</span> impacts. Public health frameworks and other studies of climate <span class="hlt">change</span> indicators were reviewed to identify criteria with which to evaluate the list of proposed <span class="hlt">key</span> indicators and a rating scale was developed. Total scores for each indicator were calculated based on the rating scale. A total of 77 health indicators were identified from the literature. After evaluation using the chosen criteria, 8 indicators were identified as the best for use. They include excess daily all-cause mortality due to heat, premature deaths due to air pollution (ozone and particulate matter 2.5), preventable deaths from climate <span class="hlt">change</span>, disability-adjusted life years lost from climate <span class="hlt">change</span>, daily all-cause mortality, daily non-accidental mortality, West Nile Disease incidence, and Lyme borreliosis incidence. There is need for further data and research related to health effect quantification in the area of climate <span class="hlt">change</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017EGUGA..19.8467R','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017EGUGA..19.8467R"><span>North Atlantic sub-<span class="hlt">decadal</span> variability in climate models</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Reintges, Annika; Martin, Thomas; Latif, Mojib; Park, Wonsun</p> <p>2017-04-01</p> <p>The North Atlantic Oscillation (NAO) is the dominant variability mode for the winter climate of the North Atlantic sector. During a positive (negative) NAO phase, the sea level pressure (SLP) difference between the subtropical Azores high and the subpolar Icelandic low is anomalously strong (weak). This affects, for example, temperature, precipitation, wind, and surface heat flux over the North Atlantic, and over large parts of Europe. In observations we find enhanced sub-<span class="hlt">decadal</span> variability of the NAO index that goes along with a dipolar sea surface temperature (SST) pattern. The corresponding SLP and SST patterns are reproduced in a control experiment of the Kiel Climate Model (KCM). Large-scale air-sea interaction is suggested to be essential for the North Atlantic sub-<span class="hlt">decadal</span> variability in the KCM. The Atlantic Meridional Overturning Circulation (AMOC) plays a <span class="hlt">key</span> role, setting the timescale of the variability by providing a delayed negative feedback to the NAO. The interplay of the NAO and the AMOC on the sub-<span class="hlt">decadal</span> timescale is further investigated in the CMIP5 model ensemble. For example, the average CMIP5 model AMOC pattern associated with sub-<span class="hlt">decadal</span> variability is characterized by a deep-reaching dipolar structure, similar to the KCM's sub-<span class="hlt">decadal</span> AMOC variability pattern. The results suggest that dynamical air-sea interactions are crucial to generate enhanced sub-<span class="hlt">decadal</span> variability in the North Atlantic climate.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2011AGUFM.B43B0294D','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2011AGUFM.B43B0294D"><span>Simulating Residential Demand in Singapore through Five <span class="hlt">Decades</span> of Demographic <span class="hlt">Change</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Davis, N. R.; Fernández, J.</p> <p>2011-12-01</p> <p>Singapore's rapid and well-documented development over the last half-century provides an ideal case for studying urban metabolism. Extensive data [1, 2] facilitate the modeling of historical dynamics of population and resource consumption. This paper presents an agent-based population model that simulates <span class="hlt">key</span> demographic factors - number, size, and relative income of households - through fifty years of development in Singapore. This is the first step in a broader study linking demographic factors to residential demand for urban land, materials, water, and energy. Previous studies of the resource demands of housing stock have accounted for demographics by modifying the important population driver with a single, aggregated "lifestyle" term [3, 4]. However, demographic <span class="hlt">changes</span> that result from development can influence the nature of the residential sector, and warrant a closer look. Increasing levels of education and affluence coupled with decreasing birth rates have yielded an aging population and <span class="hlt">changing</span> family structures in Singapore [5]. These factors all contribute to an increasingly resource-intense residential sector. Singaporeans' elevated per capita income and life expectancy have created demand for larger household area, which means a growing percentage of available land must be dedicated to residential use [6]. While the majority of Singapore's housing is public - a strategy designed to maximize land use efficiency - residents are increasingly seeking private alternatives [7]. In the private sector, lower density housing puts even greater pressure on the finite supply of undeveloped land. Agent-based modeling is used to study the selected aspects of demography. The population is disaggregated into historical time-series distributions of age, family size, education, and income. We propose a simplified methodology correlating average education level with birth rate, and income to categorize households and establish housing unit demand. Aggregated lifestyle</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/25323549','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/25323549"><span>Combined effects of the Pacific <span class="hlt">Decadal</span> Oscillation and El Niño-Southern Oscillation on global land dry-wet <span class="hlt">changes</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, Shanshan; Huang, Jianping; He, Yongli; Guan, Yuping</p> <p>2014-10-17</p> <p>The effects of natural variability, especially El Niño-Southern Oscillation (ENSO) effects, have been the focus of several recent studies on the <span class="hlt">change</span> of drought patterns with climate <span class="hlt">change</span>. The interannual relationship between ENSO and the global climate is not stationary and can be modulated by the Pacific <span class="hlt">Decadal</span> Oscillation (PDO). However, the global land distribution of the dry-wet <span class="hlt">changes</span> associated with the combination of ENSO and the PDO remains unclear. In the present study, this is investigated using a revised Palmer Drought Severity Index dataset (sc_PDSI_pm). We find that the effect of ENSO on dry-wet <span class="hlt">changes</span> varies with the PDO phase. When in phase with the PDO, ENSO-induced dry-wet <span class="hlt">changes</span> are magnified with respect to the canonical pattern. When out of phase, these dry-wet variations weaken or even disappear. This remarkable contrast in ENSO's influence between the two phases of the PDO highlights exciting new avenues for obtaining improved global climate predictions. In recent <span class="hlt">decades</span>, the PDO has turned negative with more La Niña events, implying more rain and flooding over land. La Niña-induced wet areas become wetter and the dry areas become drier and smaller due to the effects of the cold PDO phase.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29314468','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29314468"><span>A mineralogical record of ocean <span class="hlt">change</span>: <span class="hlt">Decadal</span> and centennial patterns in the California mussel.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>McCoy, Sophie J; Kamenos, Nicholas A; Chung, Peter; Wootton, Timothy J; Pfister, Catherine A</p> <p>2018-06-01</p> <p>Ocean acidification, a product of increasing atmospheric carbon dioxide, may already have affected calcified organisms in the coastal zone, such as bivalves and other shellfish. Understanding species' responses to climate <span class="hlt">change</span> requires the context of long-term dynamics. This can be particularly difficult given the longevity of many important species in contrast with the relatively rapid onset of environmental <span class="hlt">changes</span>. Here, we present a unique archival dataset of mussel shells from a locale with recent environmental monitoring and historical climate reconstructions. We compare shell structure and composition in modern mussels, mussels from the 1970s, and mussel shells dating back to 1000-2420 years BP. Shell mineralogy has <span class="hlt">changed</span> dramatically over the past 15 years, despite evidence for consistent mineral structure in the California mussel, Mytilus californianus, over the prior 2500 years. We present evidence for increased disorder in the calcium carbonate shells of mussels and greater variability between individuals. These <span class="hlt">changes</span> in the last <span class="hlt">decade</span> contrast markedly from a background of consistent shell mineralogy for centuries. Our results use an archival record of natural specimens to provide centennial-scale context for altered minerology and variability in shell features as a response to acidification stress and illustrate the utility of long-term studies and archival records in global <span class="hlt">change</span> ecology. Increased variability between individuals is an emerging pattern in climate <span class="hlt">change</span> responses, which may equally expose the vulnerability of organisms and the potential of populations for resilience. © 2017 John Wiley & Sons Ltd.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2009DPS....41.1632T','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2009DPS....41.1632T"><span>Rings Research in the Next <span class="hlt">Decade</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Tiscareno, Matthew S.; Albers, N.; Brahic, A.; Brooks, S. M.; Burns, J. A.; Chavez, C.; Colwell, J. E.; Cuzzi, J. N.; de Pater, I.; Dones, L.; Durisen, R. H.; Filacchione, G.; Giuliatti Winter, S. M.; Gordon, M. K.; Graps, A.; Hamilton, D. P.; Hedman, M. M.; Horanyi, M.; Kempf, S.; Krueger, H.; Lewis, M. C.; Lissauer, J. J.; Murray, C. D.; Nicholson, P. D.; Olkin, C. B.; Pappalardo, R. T.; Salo, H.; Schmidt, J.; Showalter, M. R.; Spahn, F.; Spilker, L. J.; Srama, R.; Sremcevic, M.; Stewart, G. R.; Yanamandra-Fisher, P.</p> <p>2009-12-01</p> <p>The study of planetary ring systems is a <span class="hlt">key</span> component of planetary science for several reasons: 1) The evolution and current states of planets and their satellites are affected in many ways by rings, while 2) conversely, properties of planets and moons and other solar system populations are revealed by their effects on rings; 3) highly structured and apparently delicate ring systems may be bellwethers, constraining various theories of the origin and evolution of their entire planetary system; and finally, 4) planetary rings provide an easily observable analogue to other astrophysical disk systems, enabling real "ground truth” results applicable to disks much more remote in space and/or time, including proto-planetary disks, circum-stellar disks, and even galaxies. Significant advances have been made in rings science in the past <span class="hlt">decade</span>. The highest-priority rings research recommendations of the last Planetary Science <span class="hlt">Decadal</span> Survey were to operate and extend the Cassini orbiter mission at Saturn; this has been done with tremendous success, accounting for much of the progress made on <span class="hlt">key</span> science questions, as we will describe. Important progress in understanding the rings of Saturn and other planets has also come from Earth-based observational and theoretical work, again as prioritized by the last <span class="hlt">Decadal</span> Survey. However, much important work remains to be done. At Saturn, the Cassini Solstice Mission must be brought to a successful completion. Priority should also be placed on sending spacecraft to Neptune and/or Uranus, now unvisited for more than 20 years. At Jupiter and Pluto, opportunities afforded by visiting spacecraft capable of studying rings should be exploited. On Earth, the need for continued research and analysis remains strong, including in-depth analysis of rings data already obtained, numerical and theoretical modeling work, laboratory analysis of materials and processes analogous to those found in the outer solar system, and continued Earth</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/22692418','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/22692418"><span>Newborn survival in Pakistan: a <span class="hlt">decade</span> of <span class="hlt">change</span> and future implications.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Khan, Amanullah; Kinney, Mary V; Hazir, Tabish; Hafeez, Assad; Wall, Stephen N; Ali, Nabeela; Lawn, Joy E; Badar, Asma; Khan, Ali Asghar; Uzma, Qudsia; Bhutta, Zulfiqar A</p> <p>2012-07-01</p> <p>Pakistan has the world's third highest national number of newborn deaths (194 000 in 2010). Major national challenges over the past <span class="hlt">decade</span> have affected health and development including several large humanitarian disasters, destabilizing political insurgency, high levels of poverty and an often hard-to-reach predominately rural population with diverse practices. As part of a multi-country analysis, we examined <span class="hlt">changes</span> for newborn survival between 2000 and 2010 in terms of mortality, coverage and health system indicators as well as national and donor funding. Neonatal mortality declined by only 0.9% per annum between 2000 and 2010; less than the global average (2.1%) and less than national maternal and child mortality declines. Coverage of newborn care interventions increased marginally, with wide socio-economic variations. There was little focus on newborn health until 2000 when considerable policy <span class="hlt">change</span> occurred, including integration of newborn care into existing community-based maternal and child packages delivered by the Lady Health Worker Programme and national behaviour <span class="hlt">change</span> communications strategies and programmes. The National Maternal, Newborn and Child Health Programme catalyzed newborn services at both facility and community levels. Civil society and academics have linked with government and several research studies have been highly influential. Since 2005, donor funding mentioning the term 'newborn' has increased more for Pakistan than for other countries. The country faces ongoing challenges in reducing neonatal mortality, and in much of Pakistan, societal norms discourage care-seeking and many women are unable to access care for themselves or their children. The policy advances and existing delivery platforms offer the potential to substantially accelerate progress in reducing neonatal deaths. The recent decision to dismantle the national Ministry of Health and devolve responsibility for health sector management to the provincial level presents</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFM.A41H0147L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFM.A41H0147L"><span>Space-based observatories providing <span class="hlt">key</span> data for climate <span class="hlt">change</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>Lecomte, J.; Juillet, J. J.</p> <p>2016-12-01</p> <p>The Sentinel-1 & 3 mission are part of the Copernicus program, previously known as GMES (Global Monitoring for Environment and Security), whose overall objective is to support Europe's goals regarding sustainable development and global governance of the environment by providing timely and quality data, information, services and knowledge. This European Earth Observation program is led by the European Commission and the space infrastructure is developed under the European Space Agency leadership. Many services will be developed through the Copernicus program among different thematic areas. The climate <span class="hlt">change</span> is one of this thematic area and the Sentinel-1 & 3 satellites will provide <span class="hlt">key</span> space-based observations in this area. The Sentinel-1 mission is based on a constellation of 2 identical satellites each one embarking C-SAR Instrument and provides capability for continuous radar mapping of the Earth with enhanced revisit frequency, coverage, timeliness and reliability for operational services and applications requiring long time series. In particular, Sentinel 1 provides all-weather, day-and-night estimates of soil moisture, wind speed and direction, sea ice, continental ice sheets and glaciers. The Sentinel-3 mission will mainly be devoted to the provision of Ocean observation data in routine, long term (20 years of operations) and continuous fashion with a consistent quality and a very high level of availability. Among these data, very accurate surface temperatures and topography measurements will be provided and will constitute <span class="hlt">key</span> indicators, once ingested in climate <span class="hlt">change</span> models, for identifying climate drivers and expected climate impacts. The paper will briefly recall the satellite architectures, their main characteristics and performance. The inflight performance and <span class="hlt">key</span> features of their images or data of the 3 satellites namely Sentinel 1A, 1B and 3A will be reviewed to demonstrate the quality and high scientific potential of the data as well as their</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018ACP....18.2341L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018ACP....18.2341L"><span><span class="hlt">Decadal</span> <span class="hlt">changes</span> in summertime reactive oxidized nitrogen and surface ozone over the Southeast 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>Li, Jingyi; Mao, Jingqiu; Fiore, Arlene M.; Cohen, Ronald C.; Crounse, John D.; Teng, Alex P.; Wennberg, Paul O.; Lee, Ben H.; Lopez-Hilfiker, Felipe D.; Thornton, Joel A.; Peischl, Jeff; Pollack, Ilana B.; Ryerson, Thomas B.; Veres, Patrick; Roberts, James M.; Neuman, J. Andrew; Nowak, John B.; Wolfe, Glenn M.; Hanisco, Thomas F.; Fried, Alan; Singh, Hanwant B.; Dibb, Jack; Paulot, Fabien; Horowitz, Larry W.</p> <p>2018-02-01</p> <p>Widespread efforts to abate ozone (O3) smog have significantly reduced emissions of nitrogen oxides (NOx) over the past 2 <span class="hlt">decades</span> in the Southeast US, a place heavily influenced by both anthropogenic and biogenic emissions. How reactive nitrogen speciation responds to the reduction in NOx emissions in this region remains to be elucidated. Here we exploit aircraft measurements from ICARTT (July-August 2004), SENEX (June-July 2013), and SEAC4RS (August-September 2013) and long-term ground measurement networks alongside a global chemistry-climate model to examine <span class="hlt">decadal</span> <span class="hlt">changes</span> in summertime reactive oxidized nitrogen (RON) and ozone over the Southeast US. We show that our model can reproduce the mean vertical profiles of major RON species and the total (NOy) in both 2004 and 2013. Among the major RON species, nitric acid (HNO3) is dominant (˜ 42-45 %), followed by NOx (31 %), total peroxy nitrates (ΣPNs; 14 %), and total alkyl nitrates (ΣANs; 9-12 %) on a regional scale. We find that most RON species, including NOx, ΣPNs, and HNO3, decline proportionally with decreasing NOx emissions in this region, leading to a similar decline in NOy. This linear response might be in part due to the nearly constant summertime supply of biogenic VOC emissions in this region. Our model captures the observed relative <span class="hlt">change</span> in RON and surface ozone from 2004 to 2013. Model sensitivity tests indicate that further reductions of NOx emissions will lead to a continued decline in surface ozone and less frequent high-ozone events.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://eric.ed.gov/?q=EDUCATION+AND+TICS&pg=2&id=EJ944785','ERIC'); return false;" href="https://eric.ed.gov/?q=EDUCATION+AND+TICS&pg=2&id=EJ944785"><span>Tourette Syndrome and Tic Disorders: A <span class="hlt">Decade</span> of Progress</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>Swain, James E.; Scahill, Lawrence; Lombroso, Paul J.; King, Robert A.; Leckman, James F.</p> <p>2007-01-01</p> <p>Objective: This is a review of progress made in the understanding of Tourette syndrome (TS) during the past <span class="hlt">decade</span> including models of pathogenesis, state-of-the-art assessment techniques, and treatment. Method: Computerized literature searches were conducted under the <span class="hlt">key</span> words "Tourette syndrome," "Tourette disorder," and "tics." Only references…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/27441550','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/27441550"><span>Patterns of Distribution and Spatial Indicators of Ecosystem <span class="hlt">Change</span> Based on <span class="hlt">Key</span> Species in the Southern Benguela.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Watermeyer, Katherine E; Hutchings, Laurence; Jarre, Astrid; Shannon, Lynne J</p> <p>2016-01-01</p> <p>Several commercially and ecologically important species in the southern Benguela have undergone southward and eastward shifts in their distributions over previous <span class="hlt">decades</span>, most notably the small pelagic fish sardine Sardinops sagax and anchovy Engraulis encrasicolus. Understanding these <span class="hlt">changes</span> and their implications is essential in implementing an ecosystem approach to fisheries in the southern Benguela and attempting to appreciate the potential impacts of future environmental <span class="hlt">change</span>. To investigate possible impacts of these shifts at an ecosystem level, distribution maps for before (1985-1991), during (1997-2000) and after (2003-2008) the shift in small pelagic fish were constructed for 14 <span class="hlt">key</span> species from catch and survey data, and used to calculate spatial indicators including proportion east and west of Cape Agulhas, relative overlap in biomass and area, index of diversity, connectivity. Potential interactions on the south and west coasts were also compared. For several species (redeye; chub mackerel; kingklip; chokka squid; yellowtail), previously unidentified increases in the proportion of biomass east of Cape Agulhas were shown to have occurred over the same period as that of small pelagic fish, although none to the same degree. On average, overlap with small pelagic fish increased over time and overall system connectivity was lowest in the intermediate period, possibly indicating a system under transition. Connectivity declined over time on the west coast while increasing on the east coast. Distributions of other species have <span class="hlt">changed</span> over time, with the region east of Cape Agulhas becoming increasingly important in terms of potential trophic interaction. Variations in distribution of biomass and structural complexity affect the trophic structure and hence functioning of the system, and implications should be considered when attempting to identify the possible ecosystem impacts of current and future system-level <span class="hlt">change</span>.</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('http://adsabs.harvard.edu/abs/2012QSRv...35...82H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012QSRv...35...82H"><span>Holocene <span class="hlt">key</span> coral species in the Northwest Pacific: indicators of reef formation and reef ecosystem responses to global climate <span class="hlt">change</span> and anthropogenic stresses in the near future</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Hongo, Chuki</p> <p>2012-03-01</p> <p>The geological record of <span class="hlt">key</span> coral species that contribute to reef formation and maintenance of reef ecosystems is important for understanding the ecosystem response to global-scale climate <span class="hlt">change</span> and anthropogenic stresses in the near future. Future responses can be predicted from accumulated data on Holocene reef species identified in drillcore and from data on raised reef terraces. The present study analyzes a dataset based on 27 drillcores, raised reef terraces, and 134 radiocarbon and U-Th ages from reefs of the Northwest Pacific, with the aim of examining the role of <span class="hlt">key</span> coral species in reef growth and maintenance for reef ecosystem during Holocene sea-level <span class="hlt">change</span>. The results indicate a latitudinal <span class="hlt">change</span> in <span class="hlt">key</span> coral species: arborescent Acropora (Acropora intermedia and Acropora muricata) was the dominant reef builder at reef crests in the tropics, whereas Porites (Porites australiensis, Porites lutea, and Porites lobata) was the dominant contributor to reef growth in the subtropics between 10,000 and 7000 cal. years BP (when the rate of sea-level rise was 10 m/ka). Acropora digitifera, Acropora hyacinthus, Acropora robusta/A. abrotanoides, Isopora palifera, Favia stelligera, and Goniastrea retiformis from the corymbose and tabular Acropora facies were the main <span class="hlt">key</span> coral species at reef crests between 7000 and 5000 cal. years BP (when the rate of sea-level rise was 5 m/ka) and during the following period of stable sea-level. Massive Porites (P. australiensis, P. lutea, and P. lobata) contributed to reef growth in shallow lagoons during the period of stable sea level. <span class="hlt">Key</span> coral species from the corymbose and tabular Acropora facies have the potential to build reefs and maintain ecosystems in the near future under a global sea-level rise of 2-6 m/ka, as do <span class="hlt">key</span> coral species from the arborescent Acropora facies and massive Porites facies, which show vigorous growth and are tolerant to relatively deep-water, low-energy environments. However, these species</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012GeoRL..3921705A','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012GeoRL..3921705A"><span>The amplitude of <span class="hlt">decadal</span> to multidecadal variability in precipitation simulated by state-of-the-art climate models</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Ault, T. R.; Cole, J. E.; St. George, S.</p> <p>2012-11-01</p> <p>We assess the magnitude of <span class="hlt">decadal</span> to multidecadal (D2M) variability in Climate Model Intercomparison Project 5 (CMIP5) simulations that will be used to understand, and plan for, climate <span class="hlt">change</span> as part of the Intergovernmental Panel on Climate <span class="hlt">Change</span>'s 5th Assessment Report. Model performance on D2M timescales is evaluated using metrics designed to characterize the relative and absolute magnitude of variability at these frequencies. In observational data, we find that between 10% and 35% of the total variance occurs on D2M timescales. Regions characterized by the high end of this range include Africa, Australia, western North America, and the Amazon region of South America. In these areas D2M fluctuations are especially prominent and linked to prolonged drought. D2M fluctuations account for considerably less of the total variance (between 5% and 15%) in the CMIP5 archive of historical (1850-2005) simulations. The discrepancy between observation and model based estimates of D2M prominence reflects two features of the CMIP5 archive. First, interannual components of variability are generally too energetic. Second, <span class="hlt">decadal</span> components are too weak in several <span class="hlt">key</span> regions. Our findings imply that projections of the future lack sufficient <span class="hlt">decadal</span> variability, presenting a limited view of prolonged drought and pluvial risk.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013AGUFM.C33A0696S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013AGUFM.C33A0696S"><span>Long-term trends and <span class="hlt">changes</span> of soil temperature of recent <span class="hlt">decade</span> in the permafrost zone of Russia</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Sherstiukov, A.</p> <p>2013-12-01</p> <p>The northern regions of Russia have rich natural resources (oil, gas). In recent years in these areas are increasingly built engineering structure for oil and gas production and their transportation. Current global warming has a great influence on soil condition in the permafrost zone. This can lead to negative effects on buildings and infrastructure which are built on frozen soils. <span class="hlt">Changes</span> of the soil state in area of permafrost demand serious studying. Next steps have been done for research of this problem: Part 1. a) The daily data set of soil temperature under natural surface at depths up to 320 cm at the Russian meteorological stations has been prepared. The earliest year of data set is 1963, the current version is ending in 2011 (660 stations of Russia). Quality control of original data was performed in creating this data set. b) The data set of computed depth of soil seasonal thawing at the Russian meteorological stations till 2011 has been prepared (107 stations with yearly depth of thawing). Part 2. <span class="hlt">Changes</span> of soils' condition for the last five <span class="hlt">decades</span> have been researched based on the prepared data sets. The <span class="hlt">change</span> of mean annual soil temperature at depths has been researched and soil warming in the vast area for 1963 - 2010 has been shown, the great trends (0,2 ÷ 0,4°C /10 years) increase at 320 cm have been found in Western and Eastern Siberia, and the greatest trends (0,4 ÷ 0,5°C/10 years) are found in their south part. This creates favorable conditions for increase of seasonal thawing depth in a permafrost zone, especially in its south part. The map of average depth of soil seasonal thawing for the same period (1963-2010) was made. It showed that the greatest depths of thawing 300-400 cm were observed near the border of permafrost and the smallest depths 50-250 cm predominate in the area of continuous permafrost. Part 3. Global warming of climate was slowed down from the beginning of the XXI century as it is known from publications. Additional</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/biblio/944109-decadal-changes-potassium-calcium-magnesium-deciduous-forest-soil','SCIGOV-STC'); return false;" href="https://www.osti.gov/biblio/944109-decadal-changes-potassium-calcium-magnesium-deciduous-forest-soil"><span><span class="hlt">Decadal</span> <span class="hlt">changes</span> in potassium, calcium, and magnesium in a deciduous forest soil</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>Mulholland, Patrick J; Johnson, Dale W.; Todd Jr, Donald E</p> <p>2008-01-01</p> <p><span class="hlt">Decadal</span> <span class="hlt">changes</span> in soil exchangeable K{sup +}, Ca{sup 2+}, and Mg{sup 2+} concentrations and contents from 1972 to 2004 in eight intensively monitored plots on Walker Branch Watershed were compared with estimates of increments or decrements in vegetation and detritus. The results from these eight plots compared favorably with those from a more extensive set from 24 soil sampling plots sampled in 1972 and 2004. Increases in exchangeable K{sup +} were noted between 1972 and 1982, but few <span class="hlt">changes</span> were noted between 1982 and 2004 despite significant increments in vegetation and detritus and significant potential losses by leaching. Total Kmore » contents of soils in the 0- to 60-cm sampling depth were very large and a slight amount of weathering could have replenished the K{sup +} lost from exchanges sites. With one notable exception, exchangeable Ca{sup 2+} and Mg{sup 2+} concentrations and contents decreased continuously during the sampling period. Decreases in exchangeable Ca{sup 2+} could be attributed mostly to increments in biomass and detritus, whereas decreases in exchangeable Mg{sup 2+} could not and were attributed to leaching. The major exception to these patterns was in the case of exchangeable Ca{sup 2+}, where significant increases were noted in one plot and attributed to Ca release from the decomposition of Ca-rich coarse woody debris from oak (Quercus spp.) mortality. With minor exceptions, soils and <span class="hlt">changes</span> in soils among the eight intensively sampled core plots were similar to those in a more extensive set of plots distributed across the watershed. This study shows that averaging among plots can mask significant and important spatial patterns in soil <span class="hlt">change</span> that must be taken into account in assessing long-term trends.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://cfpub.epa.gov/si/si_public_record_report.cfm?dirEntryId=235715&keyword=sandra&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=235715&keyword=sandra&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">Decadal</span> <span class="hlt">Changes</span> In Benthic Community Measures In New York Harbor</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>Monitoring in New York Harbor, NY, as part of the Regional Environmental Monitoring and Assessment Program has spanned a <span class="hlt">decade</span>, and includes habitat and water quality measures and sediment contaminant levels from four sub-basins (Upper NY Harbor, Lower NY Harbor, Newark Bay, and...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4902101','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4902101"><span>Hospitalization due to drug use did not <span class="hlt">change</span> after a <span class="hlt">decade</span> of the Psychiatric Reform</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Balbinot, Alexandre Dido; Horta, Rogério Lessa; da Costa, Juvenal Soares Dias; Araújo, Renata Brasil; Poletto, Simone; Teixeira, Marina Bressaneli</p> <p>2016-01-01</p> <p>ABSTRACT OBJECTIVE To investigate whether the psychiatric hospitalization rates due to use of psychoactive substances and average time of hospitalization suffered any <span class="hlt">changes</span> after the first <span class="hlt">decade</span> of effective implementation of the psychiatric reform in Brazil. METHODS This article examines the evolution of hospitalizations due to disorders arising from the use of alcohol or other substances in the state of Santa Catarina, Southern Brazil, from 2000 to 2012. This is an ecological, time-series study, which uses data from admissions obtained by the Informatics Service of the Brazilian Unified Health System. Hospitalization rates by 100,000 inhabitants and average time of occupancy of beds were estimated. Coefficients of variation of these rates were estimated by Poisson Regression. RESULTS The total and male hospitalization rates did not vary (p = 0.056 and p = 0.244, respectively). We observed an increase of 3.0% for the female sex (p = 0.049). We did not observe any significant variation for occupancy time of beds. CONCLUSIONS The deployment of services triggered by the Brazilian psychiatric reform was not accompanied by a reduction of hospitalization rates or mean occupancy time of hospitalized patients during this first <span class="hlt">decade</span> of implementation of the reform. PMID:27253902</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/servlets/purl/1167250','SCIGOV-STC'); return false;" href="https://www.osti.gov/servlets/purl/1167250"><span>A Generalized Stability Analysis of the AMOC in Earth System Models: Implication for <span class="hlt">Decadal</span> Variability and Abrupt Climate <span class="hlt">Change</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>Fedorov, Alexey V.</p> <p>2015-01-14</p> <p>The central goal of this research project was to understand the mechanisms of <span class="hlt">decadal</span> and multi-<span class="hlt">decadal</span> variability of the Atlantic Meridional Overturning Circulation (AMOC) as related to climate variability and abrupt climate <span class="hlt">change</span> within a hierarchy of climate models ranging from realistic ocean models to comprehensive Earth system models. Generalized Stability Analysis, a method that quantifies the transient and asymptotic growth of perturbations in the system, is one of the main approaches used throughout this project. The topics we have explored range from physical mechanisms that control AMOC variability to the factors that determine AMOC predictability in the Earth systemmore » models, to the stability and variability of the AMOC in past climates.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015EPSC...10..917B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015EPSC...10..917B"><span>Strategy for the International Lunar <span class="hlt">Decade</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Beldavs, V.; Dunlop, D.; Foing, B.</p> <p>2015-10-01</p> <p>LD is a global event and process for international collaboration in space initiated by the International Lunar Exploration Working Group (ILEWG), the National Space Society and the National Science Centre FOTONIKA-LV of the University of Latvia. ILD is planned for launch in 2017, the 60th anniversary of the International Geophysical Year that marked the dawn of the space age with the launch of Sputnik. ILD is envisioned as a <span class="hlt">decade</span> long process of international collaboration with lunar exploration concurrent with development of policies, <span class="hlt">key</span> enabling technologies and infrastructures on the Moon and in cislunar space leading towards an eventual goal of industrial development of the Moon and economic activity beyond Earth orbit[1]. This second International Lunar <span class="hlt">Decade</span> will build on the foundations of the ILD first proposed in by the Planetary Society in 2006 at International Conference on Exploration and Utilisation of the Moon (ICEUM), was endorsed by ICEUM participants[3], and then by ILEWG, COSPAR and other organizations. Starting in 2007, the work plan included a series of recommendations for lunar exploration missions coordinated through the ILEWG agencies and COSPAR. Advances in technology such as CubeSats and 3D printing and fundamental <span class="hlt">changes</span> in mind-set marked by initiatives such as the Google Lunar-X prize and asteroid mining ventures have made industrial development of the Moon a thinkable proposition. The ILD to be launched in 2017 is intended to set the stage for the Moon to become a wealth generating platform for human expansion into the solar system.ILD is being organized to engage existing organizations involved in space collaboration such as COSPAR, COPUOS, ISECG, technical and scientific organizations and others that address space policy, space law, space security, governance and related concerns. Additional organizations will be involved that deal with structures, ecosystems, financing, economic development and health and life support and</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2001DPS....33.1420G','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2001DPS....33.1420G"><span><span class="hlt">Decadal</span> Survey: Planetary Rings Panel</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Gordon, M. K.; Cuzzi, J. N.; Lissauer, J. J.; Poulet, F.; Brahic, A.; Charnoz, S.; Ferrari, C.; Burns, J. A.; Nicholson, P. D.; Durisen, R. H.; Rappaport, N. J.; Spilker, L. J.; Yanamandra-Fisher, P.; Bosh, A. S.; Olkin, C.; Larson, S. M.; Graps, A. L.; Krueger, H.; Black, G. J.; Festou, M.; Karjalainen, R.; Salo, H. J.; Murray, C. D.; Showalter, M. R.; Dones, L.; Levison, H. F.; Namouni, F.; Araki, S.; Lewis, M. C.; Brooks, S.; Colwell, J. E.; Esposito, L. W.; Horanyi, M.; Stewart, G. R.; Krivov, A.; Schmidt, J.; Spahn, F.; Hamilton, D. P.; Giuliatti-Winter, S.; French, R. G.</p> <p>2001-11-01</p> <p>The National Research Council's Committee on Planetary and Lunar Exploration(COMPLEX) met earlier this year to begin the organization of a major activity, "A New Strategy for Solar System Exploration." Several members of the planetary rings community formed an ad hoc panel to discuss the current state and future prospects for the study of planetary rings. In this paper we summarize fundamental questions of ring science, list the <span class="hlt">key</span> science questions expected to occupy the planetary rings community for the <span class="hlt">decade</span> 2003-2013, outline the initiatives, missions, and other supporting activities needed to address those questions, and recommend priorities.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/26686070','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/26686070"><span>Four <span class="hlt">decades</span> of land-cover, land-use and hydroclimatology <span class="hlt">changes</span> in the Itacaiúnas River watershed, southeastern Amazon.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Souza-Filho, Pedro Walfir M; de Souza, Everaldo B; Silva Júnior, Renato O; Nascimento, Wilson R; Versiani de Mendonça, Breno R; Guimarães, José Tasso F; Dall'Agnol, Roberto; Siqueira, José Oswaldo</p> <p>2016-02-01</p> <p>Long-term human-induced impacts have significantly <span class="hlt">changed</span> the Amazonian landscape. The most dramatic land cover and land use (LCLU) <span class="hlt">changes</span> began in the early 1970s with the establishment of the Trans-Amazon Highway and large government projects associated with the expansion of agricultural settlement and cattle ranching, which cleared significant tropical forest cover in the areas of new and accelerated human development. Taking the <span class="hlt">changes</span> in the LCLU over the past four <span class="hlt">decades</span> as a basis, this study aims to determine the consequences of land cover (forest and savanna) and land use (pasturelands, mining and urban) <span class="hlt">changes</span> on the hydroclimatology of the Itacaiúnas River watershed area of the located in the southeastern Amazon region. We analyzed a multi-<span class="hlt">decadal</span> Landsat dataset from 1973, 1984, 1994, 2004 and 2013 and a 40-yr time series of water discharge from the Itacaiúnas River, as well as air temperature and relative humidity data over this drainage area for the same period. We employed standard Landsat image processing techniques in conjunction with a geographic object-based image analysis and multi-resolution classification approach. With the goal of detecting possible long-term trends, non-parametric Mann-Kendall test was applied, based on a Sen slope estimator on a 40-yr annual PREC, TMED and RH time series, considering the spatial average of the entire watershed. In the 1970s, the region was entirely covered by forest (99%) and savanna (∼0.3%). Four <span class="hlt">decades</span> later, only ∼48% of the tropical forest remains, while pasturelands occupy approximately 50% of the watershed area. Moreover, in protected areas, nearly 97% of the tropical forest remains conserved, while the forest cover of non-protected areas is quite fragmented and, consequently, unevenly distributed, covering an area of only 30%. Based on observational data analysis, there is evidence that the conversion of forest cover to extensive and homogeneous pasturelands was accompanied by systematic</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2010AGUFMNH21C1409P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2010AGUFMNH21C1409P"><span>Is there a societal need for <span class="hlt">decadal</span> local sea level forecasting?</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Plag, H.</p> <p>2010-12-01</p> <p> deglaciation, rapid LSL <span class="hlt">changes</span> altered coast lines within <span class="hlt">decades</span>. But large-scale built environment was absent and the much smaller number of human beings could easily adopt to shifting coast lines. Today, with wide-spread built environment and crucial, potentially polluting infrastructure in coastal zones, rapid <span class="hlt">changes</span> in coast lines and increased inundation risks during storm surges would be economically and environmentally devastating. In the absence of actionable century-scale GSL and LSL predictions, and in the face of low-probability but extremely high-risk rapid LSL events, there is a growing societal need for forecasts of LSL <span class="hlt">changes</span> on <span class="hlt">decadal</span> time scales. To a certain extent, a <span class="hlt">decadal</span> sea level forecasting service would be comparable to the ongoing sky-watch for near-Earth objects, which aims to provide early detection of the low-probability/high-risk event of a large object approaching Earth. <span class="hlt">Key</span> elements of a <span class="hlt">decadal</span> LSL forecasting service would be a Global Cryosphere Watch (GCW) and models capable of assimilating GCW and other observations as a basis for reliable decadel LSL forecasts. Such a service could facilitate mitigation and adaptation where and when necessary. Setting up such a service now would enable the assessment of its predictive capabilities.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFM.H42H..04B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFM.H42H..04B"><span>Hydrologic impacts of land cover variability and <span class="hlt">change</span> at seasonal to <span class="hlt">decadal</span> time scales over North America, 1992-2016</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Bohn, T. J.; Vivoni, E. R.</p> <p>2017-12-01</p> <p>Land cover variability and <span class="hlt">change</span> have been shown to influence the terrestrial hydrologic cycle by altering the partitioning of moisture and energy fluxes. However, the magnitude and directionality of the relationship between land cover and surface hydrology has been shown to vary substantially across regions. Here, we provide an assessment of the impacts of land cover <span class="hlt">change</span> on hydrologic processes at seasonal (vegetation phenology) to <span class="hlt">decadal</span> scales (land cover conversion) in the United States and Mexico. To this end, we combine time series of remotely-sensed land surface characteristics with land cover maps for different <span class="hlt">decades</span> as input to the Variable Infiltration Capacity hydrologic model. Land surface characteristics (leaf area index, surface albedo, and canopy fraction derived from normalized difference vegetation index) were obtained from the Moderate Resolution Imaging Spectrometer (MODIS) at 8-day intervals over the period 2000-2016. Land cover maps representing conditions in 1992, 2001, and 2011 were derived by homogenizing the National Land Cover Database over the US and the INEGI Series I through V maps over Mexico. An additional map covering all of North America was derived from the most frequent land cover class observed in each pixel of the MODIS MOD12Q1 product during 2001-2013. Land surface characteristics were summarized over land cover fractions at 1/16 degree (6 km) resolution. For each land cover map, hydrologic simulations were conducted that covered the period 1980-2013, using the best-available, hourly meteorological forcings at a similar spatial resolution. Based on these simulations, we present a comparison of the contributions of land cover <span class="hlt">change</span> and climate variability at seasonal to <span class="hlt">decadal</span> scales on the hydrologic and energy budgets, identifying the dominant components through time and space. This work also offers a valuable dataset on land cover variability and its hydrologic response for continental-scale assessments and modeling.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://eric.ed.gov/?q=IT+AND+Governance+AND+business&pg=2&id=EJ1054760','ERIC'); return false;" href="https://eric.ed.gov/?q=IT+AND+Governance+AND+business&pg=2&id=EJ1054760"><span>The UN <span class="hlt">Decade</span> of Education for Sustainable Development: Business as Usual in the End</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>Huckle, John; Wals, Arjen E. J.</p> <p>2015-01-01</p> <p>An analysis of the literature supporting the UN <span class="hlt">Decade</span> of Education for Sustainable Development and a sample of its <span class="hlt">key</span> products suggests that it failed to acknowledge or challenge neoliberalism as a hegemonic force blocking transitions towards genuine sustainability. The authors argue that the rationale for the <span class="hlt">Decade</span> was idealistic and that…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012AGUFMGC43G..08R','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012AGUFMGC43G..08R"><span>Climate <span class="hlt">Change</span> and Water Working Group - User Needs to Manage Hydrclimatic Risk from Days to <span class="hlt">Decades</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Raff, D. A.; Brekke, L. D.; Werner, K.; Wood, A.; White, K. D.</p> <p>2012-12-01</p> <p>The Federal Climate <span class="hlt">Change</span> Water Working Group (CCAWWG) provides engineering and scientific collaborations in support of water management. CCAWWG objectives include building working relationships across federal science and water management agencies, provide a forum to share expertise and leverage resources, develop education and training forums, to work with water managers to understand scientific needs and to foster collaborative efforts across the Federal and non-Federal water management and science communities to address those needs. Identifying and addressing water management needs has been categorized across two major time scales: days to a <span class="hlt">decade</span> and multi-<span class="hlt">decadal</span>, respectively. These two time periods are termed "Short-Term" and "Long-Term" in terms of the types of water management decisions they support where Short-Term roughly correlates to water management operations and Long-Term roughly correlates to planning activities. This presentation will focus on portraying the identified water management user needs across these two time periods. User Needs for Long-Term planning were identified in the 2011 Reclamation and USACE "Addressing Climate <span class="hlt">Change</span> in Long-Term Water Resources Planning and Management: User Needs for Improving Tools and Information." User needs for Long-Term planning are identified across eight major categories: Summarize Relevant Literature, Obtain Climate <span class="hlt">Change</span> Information, Make Decisions About How to Use the Climate <span class="hlt">Change</span> Information, Assess Natural Systems Response, Assess Socioeconomic and Institutional Response, Assess System Risks and Evaluate Alternatives, Assess and Characterize Uncertainties, and Communicating Results and Uncertainties to Decisionmakers. User Needs for Short-Term operations are focused on needs relative to available or desired monitoring and forecast products from the hydroclimatic community. These needs are presenting in the 2012 USACE, Reclamation, and NOAA - NWS "Short-Term Water Management Decisions: User</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014AGUFM.H12D..05R','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014AGUFM.H12D..05R"><span>Long-Term Soil Experiments: A <span class="hlt">Key</span> to Managing Earth's Rapidly <span class="hlt">Changing</span> Critical Zones</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Richter, D., Jr.</p> <p>2014-12-01</p> <p>In a few <span class="hlt">decades</span>, managers of Earth's Critical Zones (biota, humans, land, and water) will be challenged to double food and fiber production and diminish adverse effects of management on the wider environment. To meet these challenges, an array of scientific approaches is being used to increase understanding of Critical Zone functioning and evolution, and one amongst these approaches needs to be long-term soil field studies to move us beyond black boxing the belowground Critical Zone, i.e., to further understanding of processes driving <span class="hlt">changes</span> in the soil environment. Long-term soil experiments (LTSEs) provide direct observations of soil <span class="hlt">change</span> and functioning across time scales of <span class="hlt">decades</span>, data critical for biological, biogeochemical, and environmental assessments of sustainability; for predictions of soil fertility, productivity, and soil-environment interactions; and for developing models at a wide range of temporal and spatial scales. Unfortunately, LTSEs globally are not in a good state, and they take years to mature, are vulnerable to loss, and even today remain to be fully inventoried. Of the 250 LTSEs in a web-based network, results demonstrate that soils and belowground Critical Zones are highly dynamic and responsive to human management. The objective of this study is to review the contemporary state of LTSEs and consider how they contribute to three open questions: (1) can soils sustain a doubling of food production in the coming <span class="hlt">decades</span> without further impinging on the wider environment, (2) how do soils interact with the global C cycle, and (3) how can soil management establish greater control over nutrient cycling. While LTSEs produce significant data and perspectives for all three questions, there is on-going need and opportunity for reviews of the long-term soil-research base, for establishment of an efficiently run network of LTSEs aimed at sustainability and improving management control over C and nutrient cycling, and for research teams that</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://files.eric.ed.gov/fulltext/ED468169.pdf','ERIC'); return false;" href="http://files.eric.ed.gov/fulltext/ED468169.pdf"><span>Alberta's Post-Secondary Education System: Developing the Blueprint for <span class="hlt">Change</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>Alberta Learning, Edmonton.</p> <p></p> <p>This paper was prepared as a step in the consultation process to develop a Blueprint for <span class="hlt">Change</span> that will take postsecondary education in Alberta through the next <span class="hlt">decade</span>. The Blueprint will identify <span class="hlt">key</span> strategies to shape future directions and identify priorities for <span class="hlt">change</span>. This document reflects feedback from stakeholders to a previous…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29629563','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29629563"><span><span class="hlt">Changes</span> in Collegiate Ice Hockey Player Anthropometrics and Aerobic Fitness Over Three <span class="hlt">Decades</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Triplett, Ashley N; Ebbing, Amy C; Green, Matthew R; Connolly, Christopher P; Carrier, David P; Pivarnik, James M</p> <p>2018-04-09</p> <p>Over the past several <span class="hlt">decades</span>, an increased emphasis on fitness training has emerged among collegiate ice hockey teams, with the objective to improve on-ice performance. However, it is unknown if this increase in training has translated over time to <span class="hlt">changes</span> in anthropometric and fitness profiles of collegiate ice hockey players. The purposes of this study were to describe anthropometric (height, weight, BMI, %fat) and aerobic fitness (VO<sub>2peak</sub>) characteristics of collegiate ice hockey players over 36 years, and to evaluate whether these characteristics differ between player positions. Anthropometric and physiologic data were obtained through preseason fitness testing of players (N=279) from a NCAA Division I men's ice hockey team from the years of 1980 through 2015. <span class="hlt">Changes</span> over time in the anthropometric and physiologic variables were evaluated via regression analysis using linear and polynomial models and differences between player position were compared via ANOVA (p<0.05). Regression analysis revealed a cubic model best predicted <span class="hlt">changes</span> in mean height (R<sup>2</sup>=0.65), weight (R<sup>2</sup>=0.77), and BMI (R<sup>2</sup>=0.57), while a quadratic model best fit <span class="hlt">change</span> in %fat by year (R<sup>2</sup>=0.30). Little <span class="hlt">change</span> was observed over time in the anthropometric characteristics. Defensemen were significantly taller than forwards (184.7±12.1 vs. 181.3±5.9cm)(p=0.007) and forwards had a higher relative VO<sub>2peak</sub> compared to defensemen (58.7±4.7 vs. 57.2±4.4ml/kg/min)(p=0.032). No significant differences were observed in %fat or weight by position. While average player heights and weights fluctuated over time, increased emphasis on fitness training did not affect athletes' relative aerobic fitness. Differences in height and aerobic fitness levels were observed between player position.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.fs.usda.gov/treesearch/pubs/54297','TREESEARCH'); return false;" href="https://www.fs.usda.gov/treesearch/pubs/54297"><span><span class="hlt">Decadal</span>-scale <span class="hlt">changes</span> in forest soil carbon and nitrogen storage are influenced by organic matter removal during timber harvest</span></a></p> <p><a target="_blank" href="http://www.fs.usda.gov/treesearch/">Treesearch</a></p> <p>Ryan M. Mushinski; Thomas W. Boutton; D. Andrew Scott</p> <p>2017-01-01</p> <p>This study investigates whether different intensities of organic matter removal associated with timber harvest influence <span class="hlt">decadal</span>-scale storage of soil organic carbon (SOC) and total nitrogen (TN) in the top 1 m of mineral soil 18 years postharvest in a Pinus taeda L. forest in the Gulf Coastal Plain. We quantified forest harvest-related <span class="hlt">changes</span> in...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70186672','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70186672"><span>Observations and 3D hydrodynamics-based modeling of <span class="hlt">decadal</span>-scale shoreline <span class="hlt">change</span> along the Outer Banks, North Carolina</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Safak, Ilgar; List, Jeffrey; Warner, John C.; Kumar, Nirnimesh</p> <p>2017-01-01</p> <p>Long-term <span class="hlt">decadal</span>-scale shoreline <span class="hlt">change</span> is an important parameter for quantifying the stability of coastal systems. The <span class="hlt">decadal</span>-scale coastal <span class="hlt">change</span> is controlled by processes that occur on short time scales (such as storms) and long-term processes (such as prevailing waves). The ability to predict <span class="hlt">decadal</span>-scale shoreline <span class="hlt">change</span> is not well established and the fundamental physical processes controlling this <span class="hlt">change</span> are not well understood. Here we investigate the processes that create large-scale long-term shoreline <span class="hlt">change</span> along the Outer Banks of North Carolina, an uninterrupted 60 km stretch of coastline, using both observations and a numerical modeling approach. Shoreline positions for a 24-yr period were derived from aerial photographs of the Outer Banks. Analysis of the shoreline position data showed that, although variable, the shoreline eroded an average of 1.5 m/yr throughout this period. The modeling approach uses a three-dimensional hydrodynamics-based numerical model coupled to a spectral wave model and simulates the full 24-yr time period on a spatial grid running on a short (second scale) time-step to compute the sediment transport patterns. The observations and the model results show similar magnitudes (O(105 m3/yr)) and patterns of alongshore sediment fluxes. Both the observed and the modeled alongshore sediment transport rates have more rapid <span class="hlt">changes</span> at the north of our section due to continuously curving coastline, and possible effects of alongshore variations in shelf bathymetry. The southern section with a relatively uniform orientation, on the other hand, has less rapid transport rate <span class="hlt">changes</span>. Alongshore gradients of the modeled sediment fluxes are translated into shoreline <span class="hlt">change</span> rates that have agreement in some locations but vary in others. Differences between observations and model results are potentially influenced by geologic framework processes not included in the model. Both the observations and the model results show higher rates of</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://eric.ed.gov/?q=benchmarking&pg=6&id=EJ1055931','ERIC'); return false;" href="https://eric.ed.gov/?q=benchmarking&pg=6&id=EJ1055931"><span>Learning Outcomes as a <span class="hlt">Key</span> Concept in Policy Documents throughout Policy <span class="hlt">Changes</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>Prøitz, Tine Sophie</p> <p>2015-01-01</p> <p>Learning outcomes can be considered to be a <span class="hlt">key</span> concept in a <span class="hlt">changing</span> education policy landscape, enhancing aspects such as benchmarking and competition. Issues relating to concepts of performance have a long history of debate within the field of education. Today, the concept of learning outcomes has become central in education policy development,…</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('http://adsabs.harvard.edu/abs/2007JSR....58..220K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2007JSR....58..220K"><span>Multi-<span class="hlt">decadal</span> <span class="hlt">changes</span> in the megabenthos of the Bay of Fundy: The effects of fishing</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Kenchington, Ellen L.; Kenchington, Trevor J.; Henry, Lea-Anne; Fuller, Susanna; Gonzalez, Patricia</p> <p>2007-10-01</p> <p>Analysis of presence / absence records from two comparable megabenthic surveys of scallop grounds in the Bay of Fundy, Canada, in 1966-67 and 1997 showed profound <span class="hlt">change</span> over three <span class="hlt">decades</span>. There were no indications that any species were lost and the average number of taxa per station remained steady. However, spatial heterogeneities in the community were reduced and species composition <span class="hlt">changed</span> significantly. Some taxa widespread in 1966-67 declined while others expanded, with frequencies of occurrence of individual taxa <span class="hlt">changing</span> by up to 71%. The whelks Buccinum undatum and Colus spp., the bivalves Astarte spp. and Cyclocardia borealis, the toad crabs Hyas spp., the sea urchin Strongylocentrotus droebachiensis and the brittle stars (Ophiurida) showed particular increases. Corresponding declines were seen in the boring sponges Cliona spp., the horse mussel Modiolus modiolus, the scallop Chlamys islandica, the fan worm Pseudopotamilla reniformis and the stalked tunicate Boltenia ovifera. Replacement of attached, fragile, epifaunal, filter-feeding taxa by a combination of motile scavengers, motile filter-feeders and robust, burrowing filter-feeders suggests that the primary cause of the temporal <span class="hlt">change</span> was physical impacts by fishing gear, even though trawling and scallop dragging in the area were neither intense nor new developments. Secondary causes of <span class="hlt">change</span> may have included other ecosystem effects of fishing (supply of discards and bait), a mass mortality of scallops and a range expansion of a bryozoan ( Flustra foliacea).</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://eric.ed.gov/?q=carnegie&id=EJ1113154','ERIC'); return false;" href="https://eric.ed.gov/?q=carnegie&id=EJ1113154"><span>Investigating MBA Degrees Earned by Women: A <span class="hlt">Decade</span> of <span class="hlt">Change</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>McConnell, Cheryl; Rush, Douglas; Gartland, Myles</p> <p>2016-01-01</p> <p>The authors examined master of business administration (MBA) degrees earned by women at U.S. higher education institutions at three specific years spanning a <span class="hlt">decade</span>: 2003, 2008, and 2013 to determine whether there was a significant difference in the percentage of MBA degrees earned by women based on the independent variables of institutional type,…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3857279','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3857279"><span>Infective Endocarditis Epidemiology Over Five <span class="hlt">Decades</span>: A Systematic Review</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Slipczuk, Leandro; Codolosa, J. Nicolas; Davila, Carlos D.; Romero-Corral, Abel; Yun, Jeong; Pressman, Gregg S.; Figueredo, Vincent M.</p> <p>2013-01-01</p> <p>Aims To Assess <span class="hlt">changes</span> in infective endocarditis (IE) epidemiology over the last 5 <span class="hlt">decades</span>. Methods and Results We searched the published literature using PubMed, MEDLINE, and EMBASE from inception until December 2011. Data From Einstein Medical Center, Philadelphia, PA were also included. Criteria for inclusion in this systematic review included studies with reported IE microbiology, IE definition, description of population studied, and time frame. Two authors independently extracted data and assessed manuscript quality. One hundred sixty studies (27,083 patients) met inclusion criteria. Among hospital-based studies (n=142; 23,606 patients) staphylococcal IE percentage increased over time, with coagulase-negative staphylococcus (CNS) increasing over each of the last 5 <span class="hlt">decades</span> (p<0.001) and Staphylococcus aureus (SA) in the last <span class="hlt">decade</span> (21% to 30%; p<0.05). Streptococcus viridans (SV) and culture negative (CN) IE frequency decreased over time (p<0.001), while enterococcal IE increased in the last <span class="hlt">decade</span> (p<0.01). Patient age and male predominance increased over time as well. In subgroup analysis, SA frequency increased in North America, but not the rest of the world. This was due, in part, to an increase in intravenous drug abuse IE in North America (p<0.001). Among population-based studies (n=18; 3,477 patients) no significant <span class="hlt">changes</span> were found. Conclusion Important <span class="hlt">changes</span> occurred in IE epidemiology over the last half-century, especially in the last <span class="hlt">decade</span>. Staphylococcal and enterococcal IE percentage increased while SV and CN IE decreased. Moreover, mean age at diagnosis increased together with male:female ratio. These <span class="hlt">changes</span> should be considered at the time of decision-making in treatment of and prophylaxis for IE. PMID:24349331</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70020587','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70020587"><span><span class="hlt">Decadal</span> variability of precipitation over Western North America</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Cayan, D.R.; Dettinger, M.D.; Diaz, Henry F.; Graham, N.E.</p> <p>1998-01-01</p> <p><span class="hlt">Decadal</span> (>7- yr period) variations of precipitation over western North America account for 20%-50% of the variance of annual precipitation. Spatially, the <span class="hlt">decadal</span> variability is broken into several regional [O(1000 km)] components. These <span class="hlt">decadal</span> variations are contributed by fluctuations in precipitation from seasons of the year that vary from region to region and that are not necessarily concentrated in the wettest season(s) alone. The precipitation variations are linked to various <span class="hlt">decadal</span> atmospheric circulation and SST anomaly patterns where scales range from regional to global scales and that emphasize tropical or extratropical connections, depending upon which precipitation region is considered. Further, wet or dry <span class="hlt">decades</span> are associated with <span class="hlt">changes</span> in frequency of at least a few short-period circulation 'modes' such as the Pacific-North American pattern. Precipitation fluctuations over the southwestern United States and the Saskatchewan region of western Canada are associated with extensive shifts of sea level pressure and SST anomalies, suggesting that they are components of low-frequency precipitation variability from global-scale climate proceses. Consistent with the global scale of its pressure and SST connection, the Southwest <span class="hlt">decadal</span> precipitation is aligned with opposing precipitation fluctuations in northern Africa.<span class="hlt">Decadal</span> (>7-yr period) variations of precipitation over western North America account for 20%-50% of the variance of annual precipitation. Spatially, the <span class="hlt">decadal</span> variability is broken into several regional [O(1000 km)] components. These <span class="hlt">decadal</span> variations are contributed by fluctuations in precipitation from seasons of the year that vary from region to region and that are not necessarily concentrated in the wettest season(s) alone. The precipitation variations are linked to various <span class="hlt">decadal</span> atmospheric circulation and SST anomaly patterns where scales range from regional to global scales and that emphasize tropical or extratropical</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://cfpub.epa.gov/si/si_public_record_report.cfm?dirEntryId=340919&Lab=NERL&keyword=Remote+AND+sensing&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=340919&Lab=NERL&keyword=Remote+AND+sensing&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>Simulating <span class="hlt">Changes</span> in Tropospheric Composition, Aerosol Radiative Effects, and Atmospheric Deposition across the Northern Hemisphere: Contrasting Multi-<span class="hlt">Decadal</span> Trends between Asia and North America</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>Significant and contrasting <span class="hlt">changes</span> in tropospheric composition across the Northern hemisphere have occurred over the past two <span class="hlt">decades</span> as a result of <span class="hlt">changing</span> patterns of emissions of primary aerosol and gaseous precursors. During this period, SO2 and NOx emissions across the US...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4356643','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4356643"><span>Allergenic pollen season variations in the past two <span class="hlt">decades</span> under <span class="hlt">changing</span> climate in the United States</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Zhang, Yong; Bielory, Leonard; Mi, Zhongyuan; Cai, Ting; Robock, Alan; Georgopoulos, Panos</p> <p>2014-01-01</p> <p>Many diseases are linked with climate trends and variations. In particular, climate <span class="hlt">change</span> is expected to alter the spatiotemporal dynamics of allergenic airborne pollen and potentially increase occurrence of allergic airway disease. Understanding the spatiotemporal patterns of <span class="hlt">changes</span> in pollen season timing and levels is thus important in assessing climate impacts on aerobiology and allergy caused by allergenic airborne pollen. Here we describe the spatiotemporal patterns of <span class="hlt">changes</span> in the seasonal timing and levels of allergenic airborne pollen for multiple taxa in different climate regions at a continental scale. The allergenic pollen seasons of representative trees, weeds and grass during the past <span class="hlt">decade</span> (2001–2010) across the contiguous United States have been observed to start 3.0 (95% Confidence Interval (CI), 1.1–4.9) days earlier on average than in the 1990s (1994–2000). The average peak value and annual total of daily counted airborne pollen have increased by 42.4% (95% CI, 21.9%–62.9%) and 46.0% (95% CI, 21.5%–70.5%), respectively. <span class="hlt">Changes</span> of pollen season timing and airborne levels depend on latitude, and are associated with <span class="hlt">changes</span> of growing degree days, frost free days, and precipitation. These <span class="hlt">changes</span> are likely due to recent climate <span class="hlt">change</span> and particularly the enhanced warming and precipitation at higher latitudes in the contiguous United States. PMID:25266307</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018Natur.553..194P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018Natur.553..194P"><span>Fire frequency drives <span class="hlt">decadal</span> <span class="hlt">changes</span> in soil carbon and nitrogen and ecosystem productivity</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Pellegrini, Adam F. A.; Ahlström, Anders; Hobbie, Sarah E.; Reich, Peter B.; Nieradzik, Lars P.; Staver, A. Carla; Scharenbroch, Bryant C.; Jumpponen, Ari; Anderegg, William R. L.; Randerson, James T.; Jackson, Robert B.</p> <p>2018-01-01</p> <p>Fire frequency is <span class="hlt">changing</span> globally and is projected to affect the global carbon cycle and climate. However, uncertainty about how ecosystems respond to <span class="hlt">decadal</span> <span class="hlt">changes</span> in fire frequency makes it difficult to predict the effects of altered fire regimes on the carbon cycle; for instance, we do not fully understand the long-term effects of fire on soil carbon and nutrient storage, or whether fire-driven nutrient losses limit plant productivity. Here we analyse data from 48 sites in savanna grasslands, broadleaf forests and needleleaf forests spanning up to 65 years, during which time the frequency of fires was altered at each site. We find that frequently burned plots experienced a decline in surface soil carbon and nitrogen that was non-saturating through time, having 36 per cent (±13 per cent) less carbon and 38 per cent (±16 per cent) less nitrogen after 64 years than plots that were protected from fire. Fire-driven carbon and nitrogen losses were substantial in savanna grasslands and broadleaf forests, but not in temperate and boreal needleleaf forests. We also observe comparable soil carbon and nitrogen losses in an independent field dataset and in dynamic model simulations of global vegetation. The model study predicts that the long-term losses of soil nitrogen that result from more frequent burning may in turn decrease the carbon that is sequestered by net primary productivity by about 20 per cent of the total carbon that is emitted from burning biomass over the same period. Furthermore, we estimate that the effects of <span class="hlt">changes</span> in fire frequency on ecosystem carbon storage may be 30 per cent too low if they do not include multidecadal <span class="hlt">changes</span> in soil carbon, especially in drier savanna grasslands. Future <span class="hlt">changes</span> in fire frequency may shift ecosystem carbon storage by <span class="hlt">changing</span> soil carbon pools and nitrogen limitations on plant growth, altering the carbon sink capacity of frequently burning savanna grasslands and broadleaf forests.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29227988','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29227988"><span>Fire frequency drives <span class="hlt">decadal</span> <span class="hlt">changes</span> in soil carbon and nitrogen and ecosystem productivity.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Pellegrini, Adam F A; Ahlström, Anders; Hobbie, Sarah E; Reich, Peter B; Nieradzik, Lars P; Staver, A Carla; Scharenbroch, Bryant C; Jumpponen, Ari; Anderegg, William R L; Randerson, James T; Jackson, Robert B</p> <p>2018-01-11</p> <p>Fire frequency is <span class="hlt">changing</span> globally and is projected to affect the global carbon cycle and climate. However, uncertainty about how ecosystems respond to <span class="hlt">decadal</span> <span class="hlt">changes</span> in fire frequency makes it difficult to predict the effects of altered fire regimes on the carbon cycle; for instance, we do not fully understand the long-term effects of fire on soil carbon and nutrient storage, or whether fire-driven nutrient losses limit plant productivity. Here we analyse data from 48 sites in savanna grasslands, broadleaf forests and needleleaf forests spanning up to 65 years, during which time the frequency of fires was altered at each site. We find that frequently burned plots experienced a decline in surface soil carbon and nitrogen that was non-saturating through time, having 36 per cent (±13 per cent) less carbon and 38 per cent (±16 per cent) less nitrogen after 64 years than plots that were protected from fire. Fire-driven carbon and nitrogen losses were substantial in savanna grasslands and broadleaf forests, but not in temperate and boreal needleleaf forests. We also observe comparable soil carbon and nitrogen losses in an independent field dataset and in dynamic model simulations of global vegetation. The model study predicts that the long-term losses of soil nitrogen that result from more frequent burning may in turn decrease the carbon that is sequestered by net primary productivity by about 20 per cent of the total carbon that is emitted from burning biomass over the same period. Furthermore, we estimate that the effects of <span class="hlt">changes</span> in fire frequency on ecosystem carbon storage may be 30 per cent too low if they do not include multidecadal <span class="hlt">changes</span> in soil carbon, especially in drier savanna grasslands. Future <span class="hlt">changes</span> in fire frequency may shift ecosystem carbon storage by <span class="hlt">changing</span> soil carbon pools and nitrogen limitations on plant growth, altering the carbon sink capacity of frequently burning savanna grasslands and broadleaf forests.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017GeoRL..44.8557U','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017GeoRL..44.8557U"><span>Emerging European winter precipitation pattern linked to atmospheric circulation <span class="hlt">changes</span> over the North Atlantic region in recent <span class="hlt">decades</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Ummenhofer, Caroline C.; Seo, Hyodae; Kwon, Young-Oh; Parfitt, Rhys; Brands, Swen; Joyce, Terrence M.</p> <p>2017-08-01</p> <p>Dominant European winter precipitation patterns over the past century, along with their associated extratropical North Atlantic circulation <span class="hlt">changes</span>, are evaluated using cluster analysis. Contrary to the four regimes traditionally identified based on daily wintertime atmospheric circulation patterns, five distinct seasonal precipitation regimes are detected here. Recurrent precipitation patterns in each regime are linked to <span class="hlt">changes</span> in atmospheric blocking, storm track, and sea surface temperatures across the North Atlantic region. Multidecadal variability in the frequency of the precipitation patterns reveals more (fewer) winters with wet conditions in northern (southern) Europe in recent <span class="hlt">decades</span> and an emerging distinct pattern of enhanced wintertime precipitation over the northern British Isles. This pattern has become unusually common since the 1980s and is associated with <span class="hlt">changes</span> in moisture transport and more frequent atmospheric river events. The observed precipitation <span class="hlt">changes</span> post-1950 coincide with <span class="hlt">changes</span> in storm track activity over the central/eastern North Atlantic toward the northern British Isles.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/27534301','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/27534301"><span>Facilitating the Concept of Universal Design Among Design Students - <span class="hlt">Changes</span> in Teaching in the Last <span class="hlt">Decade</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Vavik, Tom</p> <p>2016-01-01</p> <p>This short paper describes and reflects on how the teaching of the concept of Universal Design (UD) has developed in the last <span class="hlt">decade</span> at the Institute of Design at the Oslo School of Architecture and Design (AHO). Four main <span class="hlt">changes</span> are described. Firstly, the curriculum has evolved from teaching guidelines and principles to focusing on design processes. Secondly, an increased emphasis is put on cognitive accessibility. Thirdly, non-stigmatizing aesthetics expressions and solutions that communicate through different senses have become more important subjects. Fourthly the teaching of UD has moved from the second to the first year curriculum.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.usgs.gov/sir/2012/5049/','USGSPUBS'); return false;" href="https://pubs.usgs.gov/sir/2012/5049/"><span>Methods for evaluating temporal groundwater quality data and results of <span class="hlt">decadal</span>-scale <span class="hlt">changes</span> in chloride, dissolved solids, and nitrate concentrations in groundwater in the United States, 1988-2010</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Lindsey, Bruce D.; Rupert, Michael G.</p> <p>2012-01-01</p> <p><span class="hlt">Decadal</span>-scale <span class="hlt">changes</span> in groundwater quality were evaluated by the U.S. Geological Survey National Water-Quality Assessment (NAWQA) Program. Samples of groundwater collected from wells during 1988-2000 - a first sampling event representing the <span class="hlt">decade</span> ending the 20th century - were compared on a pair-wise basis to samples from the same wells collected during 2001-2010 - a second sampling event representing the <span class="hlt">decade</span> beginning the 21st century. The data set consists of samples from 1,236 wells in 56 well networks, representing major aquifers and urban and agricultural land-use areas, with analytical results for chloride, dissolved solids, and nitrate. Statistical analysis was done on a network basis rather than by individual wells. Although spanning slightly more or less than a 10-year period, the two-sample comparison between the first and second sampling events is referred to as an analysis of <span class="hlt">decadal</span>-scale <span class="hlt">change</span> based on a step-trend analysis. The 22 principal aquifers represented by these 56 networks account for nearly 80 percent of the estimated withdrawals of groundwater used for drinking-water supply in the Nation. Well networks where <span class="hlt">decadal</span>-scale <span class="hlt">changes</span> in concentrations were statistically significant were identified using the Wilcoxon-Pratt signed-rank test. For the statistical analysis of chloride, dissolved solids, and nitrate concentrations at the network level, more than half revealed no statistically significant <span class="hlt">change</span> over the <span class="hlt">decadal</span> period. However, for networks that had statistically significant <span class="hlt">changes</span>, increased concentrations outnumbered decreased concentrations by a large margin. Statistically significant increases of chloride concentrations were identified for 43 percent of 56 networks. Dissolved solids concentrations increased significantly in 41 percent of the 54 networks with dissolved solids data, and nitrate concentrations increased significantly in 23 percent of 56 networks. At least one of the three - chloride, dissolved solids, or</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70158674','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70158674"><span>Many atolls may be uninhabitable within <span class="hlt">decades</span> due to climate <span class="hlt">change</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>Storlazzi, Curt; Elias, Edwin P.L.; Berkowitz, Paul</p> <p>2015-01-01</p> <p>Observations show global sea level is rising due to climate <span class="hlt">change</span>, with the highest rates in the tropical Pacific Ocean where many of the world’s low-lying atolls are located. Sea-level rise is particularly critical for low-lying carbonate reef-lined atoll islands; these islands have limited land and water available for human habitation, water and food sources, and ecosystems that are vulnerable to inundation from sea-level rise. Here we demonstrate that sea-level rise will result in larger waves and higher wave-driven water levels along atoll islands’ shorelines than at present. Numerical model results reveal waves will synergistically interact with sea-level rise, causing twice as much land forecast to be flooded for a given value of sea-level rise than currently predicted by current models that do not take wave-driven water levels into account. Atolls with islands close to the shallow reef crest are more likely to be subjected to greater wave-induced run-up and flooding due to sea-level rise than those with deeper reef crests farther from the islands’ shorelines. It appears that many atoll islands will be flooded annually, salinizing the limited freshwater resources and thus likely forcing inhabitants to abandon their islands in <span class="hlt">decades</span>, not centuries, as previously thought.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/servlets/purl/1378474','SCIGOV-STC'); return false;" href="https://www.osti.gov/servlets/purl/1378474"><span>AMOC <span class="hlt">decadal</span> variability in Earth system models: Mechanisms and climate impacts</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>Fedorov, Alexey</p> <p></p> <p>This is the final report for the project titled "AMOC <span class="hlt">decadal</span> variability in Earth system models: Mechanisms and climate impacts". The central goal of this one-year research project was to understand the mechanisms of <span class="hlt">decadal</span> and multi-<span class="hlt">decadal</span> variability of the Atlantic Meridional Overturning Circulation (AMOC) within a hierarchy of climate models ranging from realistic ocean GCMs to Earth system models. The AMOC is a <span class="hlt">key</span> element of ocean circulation responsible for oceanic transport of heat from low to high latitudes and controlling, to a large extent, climate variations in the North Atlantic. The questions of the AMOC stability, variability andmore » predictability, directly relevant to the questions of climate predictability, were at the center of the research work.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3833470','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3833470"><span>Access to Medicines in Resource-limited Settings: The End of a Golden <span class="hlt">Decade</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>Ford, Nathan; Arkinstall, James</p> <p>2012-01-01</p> <p>Strong international mobilization and political will drove a golden <span class="hlt">decade</span> for global health. <span class="hlt">Key</span> initiatives over the last <span class="hlt">decade</span> include setting of health-related Millennium Development Goals; the Commission on Macroeconomics and Health; the creation of the Global Fund to Fight AIDS, Tuberculosis and Malaria; the Doha Declaration on the TRIPS Agreement and Public Health affirming countries' rights to protect public health when implementing patent rules; and the creation of product development partnerships to address neglected areas of research and development. Significant progress was made in reducing the incidence of and morbidity and mortality from human immunodeficiency virus (HIV), tuberculosis (TB), and malaria, with a major impact made through increased access to medicines. Antiretroviral treatment for HIV was expanded to 6.6 million people, and medication prices were reduced significantly through generic competition. However, donor support has started to decline at a time when many patients still wait for treatment and the prices of needed newer medicines are on the increase due to patent protection. TB incidence has started to decrease, but progress in diagnosis and treatment of multi-drug-resistant TB has been slow due to complexity of treatment and high drug costs. Promising new TB drugs in development need to be introduced rapidly and appropriately while treatment is being expanded. The introduction of more affordable artemisinin combination therapies for malaria contributed to significantly reducing malaria incidence and mortality, but challenges remain in ensuring that the latest recommendations for treating severe malaria are implemented. Looking to the next <span class="hlt">decade</span>, there is a worrisome mismatch between additional health priorities accompanied by shifting burdens of disease that need to be addressed and dwindling political attention and financial support. Difficulties in producing and guaranteeing access to affordable medicines are expected from a</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFM.B24D..02S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFM.B24D..02S"><span><span class="hlt">Key</span> Process Uncertainties in Soil Carbon Dynamics: Comparing Multiple Model Structures and Observational Meta-analysis</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Sulman, B. N.; Moore, J.; Averill, C.; Abramoff, R. Z.; Bradford, M.; Classen, A. T.; Hartman, M. D.; Kivlin, S. N.; Luo, Y.; Mayes, M. A.; Morrison, E. W.; Riley, W. J.; Salazar, A.; Schimel, J.; Sridhar, B.; Tang, J.; Wang, G.; Wieder, W. R.</p> <p>2016-12-01</p> <p>Soil carbon (C) dynamics are crucial to understanding and predicting C cycle responses to global <span class="hlt">change</span> and soil C modeling is a <span class="hlt">key</span> tool for understanding these dynamics. While first order model structures have historically dominated this area, a recent proliferation of alternative model structures representing different assumptions about microbial activity and mineral protection is providing new opportunities to explore process uncertainties related to soil C dynamics. We conducted idealized simulations of soil C responses to warming and litter addition using models from five research groups that incorporated different sets of assumptions about processes governing soil C decomposition and stabilization. We conducted a meta-analysis of published warming and C addition experiments for comparison with simulations. Assumptions related to mineral protection and microbial dynamics drove strong differences among models. In response to C additions, some models predicted long-term C accumulation while others predicted transient increases that were counteracted by accelerating decomposition. In experimental manipulations, doubling litter addition did not <span class="hlt">change</span> soil C stocks in studies spanning as long as two <span class="hlt">decades</span>. This result agreed with simulations from models with strong microbial growth responses and limited mineral sorption capacity. In observations, warming initially drove soil C loss via increased CO2 production, but in some studies soil C rebounded and increased over <span class="hlt">decadal</span> time scales. In contrast, all models predicted sustained C losses under warming. The disagreement with experimental results could be explained by physiological or community-level acclimation, or by warming-related <span class="hlt">changes</span> in plant growth. In addition to the role of microbial activity, assumptions related to mineral sorption and protected C played a <span class="hlt">key</span> role in driving long-term model responses. In general, simulations were similar in their initial responses to perturbations but diverged over</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/20965643','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/20965643"><span>Urban ecological systems: scientific foundations and a <span class="hlt">decade</span> of progress.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Pickett, S T A; Cadenasso, M L; Grove, J M; Boone, Christopher G; Groffman, Peter M; Irwin, Elena; Kaushal, Sujay S; Marshall, Victoria; McGrath, Brian P; Nilon, C H; Pouyat, R V; Szlavecz, Katalin; Troy, Austin; Warren, Paige</p> <p>2011-03-01</p> <p>Urban ecological studies, including focus on cities, suburbs, and exurbs, while having deep roots in the early to mid 20th century, have burgeoned in the last several <span class="hlt">decades</span>. We use the state factor approach to highlight the role of important aspects of climate, substrate, organisms, relief, and time in differentiating urban from non-urban areas, and for determining heterogeneity within spatially extensive metropolitan areas. In addition to reviewing <span class="hlt">key</span> findings relevant to each state factor, we note the emergence of tentative "urban syndromes" concerning soils, streams, wildlife and plants, and homogenization of certain ecosystem functions, such as soil organic carbon dynamics. We note the utility of the ecosystem approach, the human ecosystem framework, and watersheds as integrative tools to tie information about multiple state factors together. The organismal component of urban complexes includes the social organization of the human population, and we review <span class="hlt">key</span> modes by which human populations within urban areas are differentiated, and how such differentiation affects environmentally relevant actions. Emerging syntheses in land <span class="hlt">change</span> science and ecological urban design are also summarized. The multifaceted frameworks and the growing urban knowledge base do however identify some pressing research needs. Copyright © 2010 Elsevier Ltd. All rights reserved.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017EGUGA..19.2884H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017EGUGA..19.2884H"><span><span class="hlt">Decadally</span> resolved Lateglacial radiocarbon evidence from New Zealand kauri</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Hogg, Alan; Southon, John; Turney, Chris; Palmer, Jonathan; Bronk Ramsey, Christopher; Fenwick, Pavla; Boswijk, Gretel; Büntgen, Ulf; Friedrich, Michael; Helle, Gerhard; Hughen, Konrad; Jones, Richard; Kromer, Bernd; Noronha, Alexandra; Reinig, Frederick; Reynard, Linda; Staff, Richard; Wacker, Lukas</p> <p>2017-04-01</p> <p>The Last Glacial-Interglacial Transition (LGIT; 15,000 - 11,000 cal BP) was characterised by complex spatiotemporal patterns of climate <span class="hlt">change</span>, with numerous studies requiring accurate chronological control to decipher leads from lags in global palaeoclimatic, -environmental and archaeological records. However, close scrutiny of the few available tree-ring chronologies and radiocarbon-dated sequences composing the IntCal13 radiocarbon (14C) calibration curve, indicates significant weakness in 14C calibration across <span class="hlt">key</span> periods of the LGIT. Here, we present a <span class="hlt">decadally</span>-resolved atmospheric 14C record derived from New Zealand kauri spanning Greenland Stadial 1 (GS-1; 12,900 - 11,650 cal BP). Two floating kauri 14C time series, curve-matched to IntCal13, serve as a radiocarbon backbone through GS-1. Floating Northern Hemisphere (NH) 14C datasets are matched against the new kauri data, forming a robust NH 14C time series to 14,200 cal BP. Our results show that IntCal13 is questionable from 12,200 - 11,900 cal BP and the 10,400 BP 14C plateau is approximately five <span class="hlt">decades</span> too short. By precisely aligning Southern and Northern Hemisphere tree-ring 14C records with marine 14C sequences, we document two relatively short periods of North Atlantic Meridional Overturning Circulation (AMOC) collapse during GS-1. Hence, sustained North Atlantic cooling across GS-1 was not driven by a prolonged AMOC reduction but was probably due to an equatorward migration of the Polar Front.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017ACP....1711135S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017ACP....1711135S"><span>Variability and quasi-<span class="hlt">decadal</span> <span class="hlt">changes</span> in the methane budget over the period 2000-2012</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Saunois, Marielle; Bousquet, Philippe; Poulter, Ben; Peregon, Anna; Ciais, Philippe; Canadell, Josep G.; Dlugokencky, Edward J.; Etiope, Giuseppe; Bastviken, David; Houweling, Sander; Janssens-Maenhout, Greet; Tubiello, Francesco N.; Castaldi, Simona; Jackson, Robert B.; Alexe, Mihai; Arora, Vivek K.; Beerling, David J.; Bergamaschi, Peter; Blake, Donald R.; Brailsford, Gordon; Bruhwiler, Lori; Crevoisier, Cyril; Crill, Patrick; Covey, Kristofer; Frankenberg, Christian; Gedney, Nicola; Höglund-Isaksson, Lena; Ishizawa, Misa; Ito, Akihiko; Joos, Fortunat; Kim, Heon-Sook; Kleinen, Thomas; Krummel, Paul; Lamarque, Jean-François; Langenfelds, Ray; Locatelli, Robin; Machida, Toshinobu; Maksyutov, Shamil; Melton, Joe R.; Morino, Isamu; Naik, Vaishali; O'Doherty, Simon; Parmentier, Frans-Jan W.; Patra, Prabir K.; Peng, Changhui; Peng, Shushi; Peters, Glen P.; Pison, Isabelle; Prinn, Ronald; Ramonet, Michel; Riley, William J.; Saito, Makoto; Santini, Monia; Schroeder, Ronny; Simpson, Isobel J.; Spahni, Renato; Takizawa, Atsushi; Thornton, Brett F.; Tian, Hanqin; Tohjima, Yasunori; Viovy, Nicolas; Voulgarakis, Apostolos; Weiss, Ray; Wilton, David J.; Wiltshire, Andy; Worthy, Doug; Wunch, Debra; Xu, Xiyan; Yoshida, Yukio; Zhang, Bowen; Zhang, Zhen; Zhu, Qiuan</p> <p>2017-09-01</p> <p>Following the recent Global Carbon Project (GCP) synthesis of the <span class="hlt">decadal</span> methane (CH4) budget over 2000-2012 (Saunois et al., 2016), we analyse here the same dataset with a focus on quasi-<span class="hlt">decadal</span> and inter-annual variability in CH4 emissions. The GCP dataset integrates results from top-down studies (exploiting atmospheric observations within an atmospheric inverse-modelling framework) and bottom-up models (including process-based models for estimating land surface emissions and atmospheric chemistry), inventories of anthropogenic emissions, and data-driven approaches. The annual global methane emissions from top-down studies, which by construction match the observed methane growth rate within their uncertainties, all show an increase in total methane emissions over the period 2000-2012, but this increase is not linear over the 13 years. Despite differences between individual studies, the mean emission anomaly of the top-down ensemble shows no significant trend in total methane emissions over the period 2000-2006, during the plateau of atmospheric methane mole fractions, and also over the period 2008-2012, during the renewed atmospheric methane increase. However, the top-down ensemble mean produces an emission shift between 2006 and 2008, leading to 22 [16-32] Tg CH4 yr-1 higher methane emissions over the period 2008-2012 compared to 2002-2006. This emission increase mostly originated from the tropics, with a smaller contribution from mid-latitudes and no significant <span class="hlt">change</span> from boreal regions. The regional contributions remain uncertain in top-down studies. Tropical South America and South and East Asia seem to contribute the most to the emission increase in the tropics. However, these two regions have only limited atmospheric measurements and remain therefore poorly constrained. The sectorial partitioning of this emission increase between the periods 2002-2006 and 2008-2012 differs from one atmospheric inversion study to another. However, all top-down studies</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=20180002887&hterms=methane&qs=N%3D0%26Ntk%3DAll%26Ntx%3Dmode%2Bmatchall%26Ntt%3Dmethane','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=20180002887&hterms=methane&qs=N%3D0%26Ntk%3DAll%26Ntx%3Dmode%2Bmatchall%26Ntt%3Dmethane"><span>Variability and Quasi-<span class="hlt">Decadal</span> <span class="hlt">Changes</span> in the Methane Budget over the Period 2000-2012</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Saunois, Marielle; Bousquet, Philippe; Poulter, Ben; Peregon, Anna; Ciais, Philippe; Canadell, Josep G.; Dlugokencky, Edward J.; Etiope, Giuseppe; Bastviken, David; Houweling, Sander; <a style="text-decoration: none; " href="javascript:void(0); " onClick="displayelement('author_20180002887'); toggleEditAbsImage('author_20180002887_show'); toggleEditAbsImage('author_20180002887_hide'); "> <img style="display:inline; width:12px; height:12px; " src="images/arrow-up.gif" width="12" height="12" border="0" alt="hide" id="author_20180002887_show"> <img style="width:12px; height:12px; display:none; " src="images/arrow-down.gif" width="12" height="12" border="0" alt="hide" id="author_20180002887_hide"></p> <p>2017-01-01</p> <p>Following the recent Global Carbon Project (GCP) synthesis of the <span class="hlt">decadal</span> methane (CH4) budget over 2000- 2012, we analyse here the same dataset with a focus on quasi-<span class="hlt">decadal</span> and inter-annual variability in CH4 emissions. The GCP dataset integrates results from top-down studies (exploiting atmospheric observations within an atmospheric inverse-modelling framework) and bottom-up models (including process-based models for estimating land surface emissions and atmospheric chemistry), inventories of anthropogenic emissions, and data-driven approaches. The annual global methane emissions from top-down studies, which by construction match the observed methane growth rate within their uncertainties, all show an increase in total methane emissions over the period 2000-2012, but this increase is not linear over the 13 years. Despite differences between individual studies, the mean emission anomaly of the top-down ensemble shows no significant trend in total methane emissions over the period 2000-2006, during the plateau of atmospheric methane mole fractions, and also over the period 2008-2012, during the renewed atmospheric methane increase. However, the top-down ensemble mean produces an emission shift between 2006 and 2008, leading to 22 [16-32] Tg CH4 yr(exp -1) higher methane emissions over the period 2008-2012 compared to 2002-2006. This emission increase mostly originated from the tropics, with a smaller contribution from mid-latitudes and no significant <span class="hlt">change</span> from boreal regions. The regional contributions remain uncertain in top-down studies. Tropical South America and South and East Asia seem to contribute the most to the emission increase in the tropics. However, these two regions have only limited atmospheric measurements and remain therefore poorly constrained. The sectorial partitioning of this emission increase between the periods 2002-2006 and 2008-2012 differs from one atmospheric inversion study to another. However, all top-down studies suggest smaller</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013AGUFM.H31F1268H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013AGUFM.H31F1268H"><span>Water Cycle Missions for the Next <span class="hlt">Decade</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Houser, P. R.</p> <p>2013-12-01</p> <p>The global water cycle describes the circulation of water as a vital and dynamic substance in its liquid, solid, and vapor phases as it moves through the atmosphere, oceans and land. Life in its many forms exists because of water, and modern civilization depends on learning how to live within the constraints imposed by the availability of water. The scientific challenge posed by the need to observe the global water cycle is to integrate in situ and space-borne observations to quantify the <span class="hlt">key</span> water-cycle state variables and fluxes. The vision to address that challenge is a series of Earth observation missions that will measure the states, stocks, flows, and residence times of water on regional to global scales followed by a series of coordinated missions that will address the processes, on a global scale, that underlie variability and <span class="hlt">changes</span> in water in all its three phases. The accompanying societal challenge is to foster the improved use of water data and information as a basis for enlightened management of water resources, to protect life and property from effects of extremes in the water cycle. A major <span class="hlt">change</span> in thinking about water science that goes beyond its physics to include its role in ecosystems and society is also required. Better water-cycle observations, especially on the continental and global scales, will be essential. Water-cycle predictions need to be readily available globally to reduce loss of life and property caused by water-related natural hazards. Building on the 2007 Earth Science <span class="hlt">Decadal</span> Survey, NASA's Plan for a Climate-Centric Architecture for Earth Observations and Applications from Space , and the 2012 Chapman Conference on Remote Sensing of the Terrestrial Water Cycle, a workshop was held in April 2013 to gather wisdom and determine how to prepare for the next generation of water cycle missions in support of the second Earth Science <span class="hlt">Decadal</span> Survey. This talk will present the outcomes of the workshop including the intersection between</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('https://www.ncbi.nlm.nih.gov/pubmed/28159758','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/28159758"><span>Longitudinal study of weight, energy intake and physical activity <span class="hlt">change</span> across two <span class="hlt">decades</span> in older Scottish women.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Yang, Tiffany C; Gryka, Anna A; Aucott, Lorna S; Duthie, Garry G; Macdonald, Helen M</p> <p>2017-05-01</p> <p>The perimenopausal and postmenopausal periods are times of pronounced physiological <span class="hlt">change</span> in body mass index (BMI), physical activity and energy intake. Understanding these <span class="hlt">changes</span> in middle age could contribute to formation of potential public health targets. A longitudinal cohort of 5119 perimenopausal women from the Aberdeen Prospective Osteoporosis Screening Study (APOSS) recruited between 1990 and 1994, with follow-up visits at 1997-1999 and 2009-2011. At each visit, participants were weighed, measured and completed socioeconomic and demographic questionnaires. Participants at the first visit were asked to recall body weights at 20, 30 and 40 years of age. We assessed trends in BMI, physical activity and energy intake across and within visits. Over 2 <span class="hlt">decades</span>, obesity prevalence doubled from 14% to 28% of the participants, with 69% of participants being categorised as overweight or obese. Greater than 70% of participants gained >5% of their baseline BMI with weight gain occurring across all weight categories. Energy intake and physical activity levels (PALs) did not <span class="hlt">change</span> during the 2 <span class="hlt">decades</span> after menopause (p trend=0.06 and 0.11, respectively), but, within the second visit, energy intake increased concomitantly with a decrease in physical activity across increasing quartiles of BMI (p trend <0.001 for all). Overweight and obesity increased by over 50% over the course of 20 years. Weight gain occurred across the adult life course regardless of starting weight. The marked increase in dietary intake and decrease in PALs in middle age suggest a potential critical period for intervention to curb excess weight gain. Published by the BMJ Publishing Group Limited. For permission to use (where not already granted under a licence) please go to http://www.bmj.com/company/products-services/rights-and-licensing/.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://images.nasa.gov/#/details-PIA03890.html','SCIGOVIMAGE-NASA'); return false;" href="https://images.nasa.gov/#/details-PIA03890.html"><span>Florida <span class="hlt">Keys</span></span></a></p> <p><a target="_blank" href="https://images.nasa.gov/">NASA Image and Video Library</a></p> <p></p> <p>2002-12-13</p> <p>The Florida <span class="hlt">Keys</span> are a chain of islands, islets and reefs extending from Virginia <span class="hlt">Key</span> to the Dry Tortugas for about 309 kilometers (192 miles). The <span class="hlt">keys</span> are chiefly limestone and coral formations. The larger islands of the group are <span class="hlt">Key</span> West (with its airport), <span class="hlt">Key</span> Largo, Sugarloaf <span class="hlt">Key</span>, and Boca Chica <span class="hlt">Key</span>. A causeway extends from the mainland to <span class="hlt">Key</span> West. This image was acquired on October 28, 2001, by the Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) on NASA's Terra satellite. With its 14 spectral bands from the visible to the thermal infrared wavelength region, and its high spatial resolution of 15 to 90 meters (about 50 to 300 feet), ASTER images Earth to map and monitor the <span class="hlt">changing</span> surface of our planet. http://photojournal.jpl.nasa.gov/catalog/PIA03890</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://eric.ed.gov/?q=risk+AND+management+AND+framework&pg=5&id=EJ929087','ERIC'); return false;" href="https://eric.ed.gov/?q=risk+AND+management+AND+framework&pg=5&id=EJ929087"><span>Normative Sexuality Development in Adolescence: A <span class="hlt">Decade</span> in Review, 2000-2009</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>Tolman, Deborah L.; McClelland, Sara I.</p> <p>2011-01-01</p> <p>This review details a <span class="hlt">key</span> innovation across the field of adolescent sexuality research over the last <span class="hlt">decade</span>--conceptualizing sexuality as a normative aspect of adolescent development. Anchored in a growing articulation of adolescent sexuality as having positive qualities and consequences, we provide an organizing framework for understanding…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018GeoJI.213..434M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018GeoJI.213..434M"><span>Convectively driven <span class="hlt">decadal</span> zonal accelerations in Earth's fluid core</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>More, Colin; Dumberry, Mathieu</p> <p>2018-04-01</p> <p>Azimuthal accelerations of cylindrical surfaces co-axial with the rotation axis have been inferred to exist in Earth's fluid core on the basis of magnetic field observations and <span class="hlt">changes</span> in the length-of-day. These accelerations have a typical timescale of <span class="hlt">decades</span>. However, the physical mechanism causing the accelerations is not well understood. Scaling arguments suggest that the leading order torque averaged over cylindrical surfaces should arise from the Lorentz force. <span class="hlt">Decadal</span> fluctuations in the magnetic field inside the core, driven by convective flows, could then force <span class="hlt">decadal</span> <span class="hlt">changes</span> in the Lorentz torque and generate zonal accelerations. We test this hypothesis by constructing a quasi-geostrophic model of magnetoconvection, with thermally driven flows perturbing a steady, imposed background magnetic field. We show that when the Alfvén number in our model is similar to that in Earth's fluid core, temporal fluctuations in the torque balance are dominated by the Lorentz torque, with the latter generating mean zonal accelerations. Our model reproduces both fast, free Alfvén waves and slow, forced accelerations, with ratios of relative strength and relative timescale similar to those inferred for the Earth's core. The temporal <span class="hlt">changes</span> in the magnetic field which drive the time-varying Lorentz torque are produced by the underlying convective flows, shearing and advecting the magnetic field on a timescale associated with convective eddies. Our results support the hypothesis that temporal <span class="hlt">changes</span> in the magnetic field deep inside Earth's fluid core drive the observed <span class="hlt">decadal</span> zonal accelerations of cylindrical surfaces through the Lorentz torque.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://cfpub.epa.gov/si/si_public_record_report.cfm?dirEntryId=84742&keyword=increase+AND+productivity&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=84742&keyword=increase+AND+productivity&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>MODELING THE IMPACTS OF <span class="hlt">DECADAL</span> <span class="hlt">CHANGES</span> IN RIVERINE NUTRIENT FLUXES ON COASTAL EUTROPHICATION NEAR THE MISSISSIPPI RIVER DELTA. (R827785E02)</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><p>A mathematical model was used to link <span class="hlt">decadal</span> <span class="hlt">changes</span> in the Mississippi River nutrient flux to coastal eutrophication near the Mississippi River Delta. Model simulations suggest that bottom water hypoxia intensified about 30 years ago, as a probable consequence of increased n...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013ClDy...40.1453K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013ClDy...40.1453K"><span>A further assessment of vegetation feedback on <span class="hlt">decadal</span> Sahel rainfall variability</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Kucharski, Fred; Zeng, Ning; Kalnay, Eugenia</p> <p>2013-03-01</p> <p>The effect of vegetation feedback on <span class="hlt">decadal</span>-scale Sahel rainfall variability is analyzed using an ensemble of climate model simulations in which the atmospheric general circulation model ICTPAGCM ("SPEEDY") is coupled to the dynamic vegetation model VEGAS to represent feedbacks from surface albedo <span class="hlt">change</span> and evapotranspiration, forced externally by observed sea surface temperature (SST) <span class="hlt">changes</span>. In the control experiment, where the full vegetation feedback is included, the ensemble is consistent with the observed <span class="hlt">decadal</span> rainfall variability, with a forced component 60 % of the observed variability. In a sensitivity experiment where climatological vegetation cover and albedo are prescribed from the control experiment, the ensemble of simulations is not consistent with the observations because of strongly reduced amplitude of <span class="hlt">decadal</span> rainfall variability, and the forced component drops to 35 % of the observed variability. The <span class="hlt">decadal</span> rainfall variability is driven by SST forcing, but significantly enhanced by land-surface feedbacks. Both, local evaporation and moisture flux convergence <span class="hlt">changes</span> are important for the total rainfall response. Also the internal <span class="hlt">decadal</span> variability across the ensemble members (not SST-forced) is much stronger in the control experiment compared with the one where vegetation cover and albedo are prescribed. It is further shown that this positive vegetation feedback is physically related to the albedo feedback, supporting the Charney hypothesis.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3078828','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3078828"><span>Driving a <span class="hlt">decade</span> of <span class="hlt">change</span>: HIV/AIDS, patents and access to medicines for all</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>2011-01-01</p> <p>Since 2000, access to antiretroviral drugs to treat HIV infection has dramatically increased to reach more than five million people in developing countries. Essential to this achievement was the dramatic reduction in antiretroviral prices, a result of global political mobilization that cleared the way for competitive production of generic versions of widely patented medicines. Global trade rules agreed upon in 1994 required many developing countries to begin offering patents on medicines for the first time. Government and civil society reaction to expected increases in drug prices precipitated a series of events challenging these rules, culminating in the 2001 World Trade Organization's Doha Declaration on the Agreement on Trade-Related Aspects of Intellectual Property Rights and Public Health. The Declaration affirmed that patent rules should be interpreted and implemented to protect public health and to promote access to medicines for all. Since Doha, more than 60 low- and middle-income countries have procured generic versions of patented medicines on a large scale. Despite these <span class="hlt">changes</span>, however, a "treatment timebomb" awaits. First, increasing numbers of people need access to newer antiretrovirals, but treatment costs are rising since new ARVs are likely to be more widely patented in developing countries. Second, policy space to produce or import generic versions of patented medicines is shrinking in some developing countries. Third, funding for medicines is falling far short of needs. Expanded use of the existing flexibilities in patent law and new models to address the second wave of the access to medicines crisis are required. One promising new mechanism is the UNITAID-supported Medicines Patent Pool, which seeks to facilitate access to patents to enable competitive generic medicines production and the development of improved products. Such innovative approaches are possible today due to the previous <span class="hlt">decade</span> of AIDS activism. However, the Pool is just one of</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2009EGUGA..11.3241R','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2009EGUGA..11.3241R"><span>Does mesoscale matters in <span class="hlt">decadal</span> <span class="hlt">changes</span> observed in the northern Canary upwelling system?</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Relvas, P.; Luís, J.; Santos, A. M. P.</p> <p>2009-04-01</p> <p>The Western Iberia constitutes the northern limb of the Canary Current Upwelling System, one of the four Eastern Boundary Upwelling Systems of the world ocean. The strong dynamic link between the atmosphere and the ocean makes these systems highly sensitive to global <span class="hlt">change</span>, ideal to monitor and investigate its effects. In order to investigate <span class="hlt">decadal</span> <span class="hlt">changes</span> of the mesoscale patterns in the Northern Canary upwelling system (off Western Iberia), the field of the satellite-derived sea surface temperature (SST) trends was built at the pixel scale (4x4 km) for the period 1985-2007, based on the monthly mean data from the Advanced Very High Resolution Radiometer (AVHRR) on board NOAA series satellites, provided by the NASA Physical Oceanography Distributed Active Archive Center (PO.DAAC) at the Jet Propulsion Laboratory. The time series were limited to the nighttime passes to avoid the solar heating effect and a suite of procedures were followed to guarantee that the temperature trends were not biased towards the seasonally more abundant summer data, when the sky is considerably clear. A robust linear fit was applied to each individual pixel, crossing along the time the same pixel in all the processed monthly mean AVHRR SST images from 1985 until 2007. The field of the SST trends was created upon the slopes of the linear fits applied to each pixel. Monthly mean SST time series from the one degree enhanced International Comprehensive Ocean-Atmosphere Data Set (ICOADS) and from near-shore measurements collected on a daily basis by the Portuguese Meteorological Office (IM) are also used to compare the results and extend the analysis back until 1960. A generalized warming trend is detected in the coastal waters off Western Iberia during the last <span class="hlt">decades</span>, no matter which data set we analyse. However, significant spatial differences in the warming rates are observed in the satellite-derived SST trends. Remarkably, off the southern part of the Western Iberia the known</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 <span class="hlt">decadal</span> climate predictions 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><span class="hlt">Decadal</span> climate prediction aims to predict the internally-generated <span class="hlt">decadal</span> climate variability in addition to externally-forced climate <span class="hlt">change</span> signal. In order to achieve this it is necessary to start the predictions from the current climate state. In this study we investigate the forecast skill of the North Atlantic <span class="hlt">decadal</span> climate predictions 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 <span class="hlt">key</span> regions and processes. We asses the skill of the initialized <span class="hlt">decadal</span> hindcast experiments against the prediction skill of the non-initialized hindcasts simulation. We obtain an overview of the regions with the highest predictability 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 predictability of the Atlantic Meridional Overturning Circulation (AMOC) and Nordic Seas Overflow by comparing the predicted values to</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/22353882','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/22353882"><span>Efficient <span class="hlt">key</span> pathway mining: combining networks and OMICS data.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Alcaraz, Nicolas; Friedrich, Tobias; Kötzing, Timo; Krohmer, Anton; Müller, Joachim; Pauling, Josch; Baumbach, Jan</p> <p>2012-07-01</p> <p>Systems biology has emerged over the last <span class="hlt">decade</span>. Driven by the advances in sophisticated measurement technology the research community generated huge molecular biology data sets. These comprise rather static data on the interplay of biological entities, for instance protein-protein interaction network data, as well as quite dynamic data collected for studying the behavior of individual cells or tissues in accordance with <span class="hlt">changing</span> environmental conditions, such as DNA microarrays or RNA sequencing. Here we bring the two different data types together in order to gain higher level knowledge. We introduce a significantly improved version of the <span class="hlt">Key</span>PathwayMiner software framework. Given a biological network modelled as a graph and a set of expression studies, <span class="hlt">Key</span>PathwayMiner efficiently finds and visualizes connected sub-networks where most components are expressed in most cases. It finds all maximal connected sub-networks where all nodes but k exceptions are expressed in all experimental studies but at most l exceptions. We demonstrate the power of the new approach by comparing it to similar approaches with gene expression data previously used to study Huntington's disease. In addition, we demonstrate <span class="hlt">Key</span>PathwayMiner's flexibility and applicability to non-array data by analyzing genome-scale DNA methylation profiles from colorectal tumor cancer patients. <span class="hlt">Key</span>PathwayMiner release 2 is available as a Cytoscape plugin and online at http://keypathwayminer.mpi-inf.mpg.de.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.fs.usda.gov/treesearch/pubs/37862','TREESEARCH'); return false;" href="https://www.fs.usda.gov/treesearch/pubs/37862"><span>Sensitivity of Arctic carbon in a <span class="hlt">changing</span> climate</span></a></p> <p><a target="_blank" href="http://www.fs.usda.gov/treesearch/">Treesearch</a></p> <p>A. David McGuire; Henry P. Huntington; Simon Wilson</p> <p>2009-01-01</p> <p>The Arctic has been warming rapidly in the past few <span class="hlt">decades</span>. A <span class="hlt">key</span> question is how that warming will affect the cycling of carbon (C) in the Arctic system. At present, the Arctic is a global sink for C. If that <span class="hlt">changes</span> and the Arctic becomes a carbon source, global climate warming may speed up.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFM.A41P..04D','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFM.A41P..04D"><span>Atmospheric River Characteristics under <span class="hlt">Decadal</span> Climate Variability</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Done, J.; Ge, M.</p> <p>2017-12-01</p> <p>How does <span class="hlt">decadal</span> climate variability <span class="hlt">change</span> the nature and predictability of atmospheric river events? <span class="hlt">Decadal</span> swings in atmospheric river frequency, or shifts in the proportion of precipitation falling as rain, could challenge current water resource and flood risk management practice. Physical multi-scale processes operating between Pacific sea surface temperatures (SSTs) and atmospheric rivers over the Western U.S. are explored using the global Model for Prediction Across Scales (MPAS). A 45km global mesh is refined over the Western U.S. to 12km to capture the major terrain effects on precipitation. The performance of the MPAS is first evaluated for a case study atmospheric river event over California. Atmospheric river characteristics are then compared in a pair of idealized simulations, each driven by Pacific SST patterns characteristic of opposite phases of the Interdecadal Pacific Oscillation (IPO). Given recent evidence that we have entered a positive phase of the IPO, implications for current reservoir management practice over the next <span class="hlt">decade</span> will be discussed. This work contributes to the NSF-funded project UDECIDE (Understanding Decision-Climate Interactions on <span class="hlt">Decadal</span> Scales). UDECIDE brings together practitioners, engineers, statisticians, and climate scientists to understand the role of <span class="hlt">decadal</span> climate information for water management and decisions.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFMGC33D1104M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFMGC33D1104M"><span>A <span class="hlt">Decade</span> of Annual National Land Cover Products - the Cropland Data Layer</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Mueller, R.; Johnson, D. M.; Sandborn, A.; Willis, P.; Ebinger, L.; Yang, Z.; Seffrin, R.; Boryan, C. G.; Hardin, R.</p> <p>2017-12-01</p> <p>The Cropland Data Layer (CDL) is a national land cover product produced by the US Department of Agriculture/National Agricultural Statistics Service (NASS) to assess planted crop acreage on an annual basis. The 2017 CDL product serves as the <span class="hlt">decadal</span> anniversary for the mapping of conterminous US agriculture. The CDL is a supervised land cover classification derived from medium resolution Earth observing satellites that capture crop phenology throughout the growing season, leveraging confidentially held ground reference information from the USDA Farm Service Agency (FSA) as training data. The CDL currently uses ancillary geospatial data from the US Geological Survey's National Land Cover Database (NLCD), and Imperviousness and Forest Canopy layers as well as the National Elevation Dataset as training for the non-agricultural domain. Accuracy assessments are documented and released annually with metadata publication. NASS is currently reprocessing the 2008 and 2009 CDL products to 30m resolution. They were originally processed and released at 56m based on the Resourcesat-1 AWiFS sensor. Additionally, best practices learned from processing the FSA ground reference data were applied to the historical training set, providing an enhanced classification at 30m. The release of these reprocessed products in the fall of 2017, along with the 2017 CDL annual product will be discussed and will complete a <span class="hlt">decade</span>'s worth of annual 30m products. Discussions of <span class="hlt">change</span> and trend analytics as well as partnerships with <span class="hlt">key</span> industry stakeholders will be displayed on the evolution and improvements made to this <span class="hlt">decadal</span> geospatial crop specific land cover product.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/23737998','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/23737998"><span>Top-down regulation, climate and multi-<span class="hlt">decadal</span> <span class="hlt">changes</span> in coastal zoobenthos communities in two Baltic Sea areas.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Olsson, Jens; Bergström, Lena; Gårdmark, Anna</p> <p>2013-01-01</p> <p>The structure of many marine ecosystems has <span class="hlt">changed</span> substantially during recent <span class="hlt">decades</span>, as a result of overexploitation, climate <span class="hlt">change</span> and eutrophication. Despite of the apparent ecological and economical importance of coastal areas and communities, this aspect has received relatively little attention in coastal systems. Here we assess the temporal development of zoobenthos communities in two areas on the Swedish Baltic Sea coast during 30 years, and relate their development to <span class="hlt">changes</span> in climate, eutrophication and top-down regulation from fish. Both communities show substantial structural <span class="hlt">changes</span>, with a decrease in marine polychaetes and species sensitive to increased water temperatures. Concurrently, opportunistic species tolerant to environmental perturbation have increased in abundance. Species composition show a similar temporal development in both communities and significant <span class="hlt">changes</span> in species composition occurred in both data sets in the late 1980s and early 1990s. The <span class="hlt">change</span> in species composition was associated with large scale <span class="hlt">changes</span> in climate (salinity and water temperature) and to the structure of the local fish community, whereas we found no effects of nutrient loading or ambient nutrient concentrations. Our results suggest that these coastal zoobenthos communities have gone through substantial structural <span class="hlt">changes</span> over the last 30 years, resulting in communities of different species composition with potentially different ecological functions. We hence suggest that the temporal development of coastal zoobenthos communities should be assessed in light of prevailing climatic conditions considering the potential for top-down effects exerted by local fish communities.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3663797','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3663797"><span>Top-Down Regulation, Climate and Multi-<span class="hlt">Decadal</span> <span class="hlt">Changes</span> in Coastal Zoobenthos Communities in Two Baltic Sea 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>Olsson, Jens; Bergström, Lena; Gårdmark, Anna</p> <p>2013-01-01</p> <p>The structure of many marine ecosystems has <span class="hlt">changed</span> substantially during recent <span class="hlt">decades</span>, as a result of overexploitation, climate <span class="hlt">change</span> and eutrophication. Despite of the apparent ecological and economical importance of coastal areas and communities, this aspect has received relatively little attention in coastal systems. Here we assess the temporal development of zoobenthos communities in two areas on the Swedish Baltic Sea coast during 30 years, and relate their development to <span class="hlt">changes</span> in climate, eutrophication and top-down regulation from fish. Both communities show substantial structural <span class="hlt">changes</span>, with a decrease in marine polychaetes and species sensitive to increased water temperatures. Concurrently, opportunistic species tolerant to environmental perturbation have increased in abundance. Species composition show a similar temporal development in both communities and significant <span class="hlt">changes</span> in species composition occurred in both data sets in the late 1980s and early 1990s. The <span class="hlt">change</span> in species composition was associated with large scale <span class="hlt">changes</span> in climate (salinity and water temperature) and to the structure of the local fish community, whereas we found no effects of nutrient loading or ambient nutrient concentrations. Our results suggest that these coastal zoobenthos communities have gone through substantial structural <span class="hlt">changes</span> over the last 30 years, resulting in communities of different species composition with potentially different ecological functions. We hence suggest that the temporal development of coastal zoobenthos communities should be assessed in light of prevailing climatic conditions considering the potential for top-down effects exerted by local fish communities. PMID:23737998</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2009AGUFMOS23A1170A','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2009AGUFMOS23A1170A"><span>Characterization Of Dissolved Organic Mattter In The Florida <span class="hlt">Keys</span> Ecosystem</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Adams, D. G.; Shank, G. C.</p> <p>2009-12-01</p> <p>Over the past few <span class="hlt">decades</span>, Scleractinian coral populations in the Florida <span class="hlt">Keys</span> have increasingly experienced mortality due to bleaching events as well as microbial mediated illnesses such as black band and white band disease. Such pathologies seem to be most correlated with elevated sea surface temperatures, increased UV exposures, and shifts in the microbial community living on the coral itself. Recent studies indicate that corals’ exposure to UV in the Florida <span class="hlt">Keys</span> is primarily controlled by the concentration of CDOM (Chromophoric Dissolved Organic Matter) in the water column. Further, microbial community alterations may be linked to <span class="hlt">changes</span> in concentration and chemical composition of the larger DOM (Dissolved Organic Matter) pool. Our research characterized the spatial and temporal properties of DOM in Florida Bay and along the <span class="hlt">Keys</span> ecosystems using DOC analyses, in-situ water column optical measurements, and spectral analyses including absorbance and fluorescence measurements. We analyzed DOM characteristics along transects running from the mouth of the Shark River at the southwest base of the Everglades, through Florida Bay, and along near-shore <span class="hlt">Keys</span> coastal waters. Two 12 hour time-series samplings were also performed at the Seven-Mile Bridge, the primary Florida Bay discharge channel to the lower <span class="hlt">Keys</span> region. Photo-bleaching experiments showed that the chemical characteristics of the DOM pool are altered by exposure to solar radiation. Results also show that DOC (~0.8-5.8 mg C/L) and CDOM (~0.5-16.5 absorbance coefficient at 305nm) concentrations exhibit seasonal fluctuations in our study region. EEM analyses suggest seasonal transitions between primarily marine (summer) and terrestrial (winter) sources along the <span class="hlt">Keys</span>. We are currently combining EEM-PARAFAC analysis with in-situ optical measurements to model <span class="hlt">changes</span> in the spectral properties of DOM in the water column. Additionally, we are using stable δ13C isotopic analysis to further characterize DOM</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015AGUFMIN23E..03B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015AGUFMIN23E..03B"><span>Advanced Cyberinfrastructure for Geochronology as a Collaborative Endeavor: A <span class="hlt">Decade</span> of Progress, A <span class="hlt">Decade</span> of Plans</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Bowring, J. F.; McLean, N. M.; Walker, J. D.; Gehrels, G. E.; Rubin, K. H.; Dutton, A.; Bowring, S. A.; Rioux, M. E.</p> <p>2015-12-01</p> <p>The Cyber Infrastructure Research and Development Lab for the Earth Sciences (CIRDLES.org) has worked collaboratively for the last <span class="hlt">decade</span> with geochronologists from EARTHTIME and EarthChem to build cyberinfrastructure geared to ensuring transparency and reproducibility in geoscience workflows and is engaged in refining and extending that work to serve additional geochronology domains during the next <span class="hlt">decade</span>. ET_Redux (formerly U-Pb_Redux) is a free open-source software system that provides end-to-end support for the analysis of U-Pb geochronological data. The system reduces raw mass spectrometer (TIMS and LA-ICPMS) data to U-Pb dates, allows users to interpret ages from these data, and then facilitates the seamless federation of the results from one or more labs into a community web-accessible database using standard and open techniques. This EarthChem database - GeoChron.org - depends on <span class="hlt">keyed</span> references to the System for Earth Sample Registration (SESAR) database that stores metadata about registered samples. These <span class="hlt">keys</span> are each a unique International Geo Sample Number (IGSN) assigned to a sample and to its derivatives. ET_Redux provides for interaction with this archive, allowing analysts to store, maintain, retrieve, and share their data and analytical results electronically with whomever they choose. This initiative has created an open standard for the data elements of a complete reduction and analysis of U-Pb data, and is currently working to complete the same for U-series geochronology. We have demonstrated the utility of interdisciplinary collaboration between computer scientists and geoscientists in achieving a working and useful system that provides transparency and supports reproducibility, allowing geochemists to focus on their specialties. The software engineering community also benefits by acquiring research opportunities to improve development process methodologies used in the design, implementation, and sustainability of domain-specific software.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3293817','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3293817"><span>Differential Response to Soil Salinity in Endangered <span class="hlt">Key</span> Tree Cactus: Implications for Survival in a <span class="hlt">Changing</span> Climate</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Goodman, Joie; Maschinski, Joyce; Hughes, Phillip; McAuliffe, Joe; Roncal, Julissa; Powell, Devon; Sternberg, Leonel O'reilly</p> <p>2012-01-01</p> <p>Understanding reasons for biodiversity loss is essential for developing conservation and management strategies and is becoming increasingly urgent with climate <span class="hlt">change</span>. Growing at elevations <1.4 m in the Florida <span class="hlt">Keys</span>, USA, the endangered <span class="hlt">Key</span> tree cactus (Pilosocereus robinii) experienced 84 percent loss of total stems from 1994 to 2007. The most severe losses of 99 and 88 percent stems occurred in the largest populations in the Lower <span class="hlt">Keys</span>, where nine storms with high wind velocities and storm surges, occurred during this period. In contrast, three populations had substantial stem proliferation. To evaluate possible mortality factors related to <span class="hlt">changes</span> in climate or forest structure, we examined habitat variables: soil salinity, elevation, canopy cover, and habitat structure near 16 dying or dead and 18 living plants growing in the Lower <span class="hlt">Keys</span>. Soil salinity and elevation were the preliminary factors that discriminated live and dead plants. Soil salinity was 1.5 times greater, but elevation was 12 cm higher near dead plants than near live plants. However, distribution-wide stem loss was not significantly related to salinity or elevation. Controlled salinity trials indicated that salt tolerance to levels above 40 mM NaCl was related to maternal origin. Salt sensitive plants from the Lower <span class="hlt">Keys</span> had less stem growth, lower root:shoot ratios, lower potassium: sodium ratios and lower recovery rate, but higher δ 13C than a salt tolerant lineage of unknown origin. Unraveling the genetic structure of salt tolerant and salt sensitive lineages in the Florida <span class="hlt">Keys</span> will require further genetic tests. Worldwide rare species restricted to fragmented, low-elevation island habitats, with little or no connection to higher ground will face challenges from climate <span class="hlt">change</span>-related factors. These great conservation challenges will require traditional conservation actions and possibly managed relocation that must be informed by studies such as these. PMID:22403670</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/22403670','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/22403670"><span>Differential response to soil salinity in endangered <span class="hlt">key</span> tree cactus: implications for survival in a <span class="hlt">changing</span> climate.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Goodman, Joie; Maschinski, Joyce; Hughes, Phillip; McAuliffe, Joe; Roncal, Julissa; Powell, Devon; Sternberg, Leonel O'reilly</p> <p>2012-01-01</p> <p>Understanding reasons for biodiversity loss is essential for developing conservation and management strategies and is becoming increasingly urgent with climate <span class="hlt">change</span>. Growing at elevations <1.4 m in the Florida <span class="hlt">Keys</span>, USA, the endangered <span class="hlt">Key</span> tree cactus (Pilosocereus robinii) experienced 84 percent loss of total stems from 1994 to 2007. The most severe losses of 99 and 88 percent stems occurred in the largest populations in the Lower <span class="hlt">Keys</span>, where nine storms with high wind velocities and storm surges, occurred during this period. In contrast, three populations had substantial stem proliferation. To evaluate possible mortality factors related to <span class="hlt">changes</span> in climate or forest structure, we examined habitat variables: soil salinity, elevation, canopy cover, and habitat structure near 16 dying or dead and 18 living plants growing in the Lower <span class="hlt">Keys</span>. Soil salinity and elevation were the preliminary factors that discriminated live and dead plants. Soil salinity was 1.5 times greater, but elevation was 12 cm higher near dead plants than near live plants. However, distribution-wide stem loss was not significantly related to salinity or elevation. Controlled salinity trials indicated that salt tolerance to levels above 40 mM NaCl was related to maternal origin. Salt sensitive plants from the Lower <span class="hlt">Keys</span> had less stem growth, lower root:shoot ratios, lower potassium: sodium ratios and lower recovery rate, but higher δ (13)C than a salt tolerant lineage of unknown origin. Unraveling the genetic structure of salt tolerant and salt sensitive lineages in the Florida <span class="hlt">Keys</span> will require further genetic tests. Worldwide rare species restricted to fragmented, low-elevation island habitats, with little or no connection to higher ground will face challenges from climate <span class="hlt">change</span>-related factors. These great conservation challenges will require traditional conservation actions and possibly managed relocation that must be informed by studies such as these.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/25317557','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/25317557"><span>Limited impact on <span class="hlt">decadal</span>-scale climate <span class="hlt">change</span> from increased use of natural gas.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>McJeon, Haewon; Edmonds, Jae; Bauer, Nico; Clarke, Leon; Fisher, Brian; Flannery, Brian P; Hilaire, Jérôme; Krey, Volker; Marangoni, Giacomo; Mi, Raymond; Riahi, Keywan; Rogner, Holger; Tavoni, Massimo</p> <p>2014-10-23</p> <p>The most important energy development of the past <span class="hlt">decade</span> has been the wide deployment of hydraulic fracturing technologies that enable the production of previously uneconomic shale gas resources in North America. If these advanced gas production technologies were to be deployed globally, the energy market could see a large influx of economically competitive unconventional gas resources. The climate implications of such abundant natural gas have been hotly debated. Some researchers have observed that abundant natural gas substituting for coal could reduce carbon dioxide (CO2) emissions. Others have reported that the non-CO2 greenhouse gas emissions associated with shale gas production make its lifecycle emissions higher than those of coal. Assessment of the full impact of abundant gas on climate <span class="hlt">change</span> requires an integrated approach to the global energy-economy-climate systems, but the literature has been limited in either its geographic scope or its coverage of greenhouse gases. Here we show that market-driven increases in global supplies of unconventional natural gas do not discernibly reduce the trajectory of greenhouse gas emissions or climate forcing. Our results, based on simulations from five state-of-the-art integrated assessment models of energy-economy-climate systems independently forced by an abundant gas scenario, project large additional natural gas consumption of up to +170 per cent by 2050. The impact on CO2 emissions, however, is found to be much smaller (from -2 per cent to +11 per cent), and a majority of the models reported a small increase in climate forcing (from -0.3 per cent to +7 per cent) associated with the increased use of abundant gas. Our results show that although market penetration of globally abundant gas may substantially <span class="hlt">change</span> the future energy system, it is not necessarily an effective substitute for climate <span class="hlt">change</span> mitigation policy.</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.ncbi.nlm.nih.gov/pubmed/26818465','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/26818465"><span><span class="hlt">Changing</span> clinical patterns in rheumatoid arthritis management over two <span class="hlt">decades</span>: sequential observational studies.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Mian, Aneela N; Ibrahim, Fowzia; Scott, Ian C; Bahadur, Sardar; Filkova, Maria; Pollard, Louise; Steer, Sophia; Kingsley, Gabrielle H; Scott, David L; Galloway, James</p> <p>2016-01-27</p> <p>Rheumatoid arthritis (RA) treatment paradigms have shifted over the last two <span class="hlt">decades</span>. There has been increasing emphasis on combination disease modifying anti-rheumatic drug (DMARD) therapy, newer biologic therapies have become available and there is a greater focus on achieving remission. We have evaluated the impact of treatment <span class="hlt">changes</span> on disease activity scores for 28 joints (DAS28) and disability measured by the health assessment questionnaire scores (HAQ). Four cross-sectional surveys between 1996 and 2014 in two adjacent secondary care rheumatology departments in London evaluated <span class="hlt">changes</span> in drug therapy, DAS28 and its component parts and HAQ scores (in three surveys). Descriptive statistics used means and standard deviations (SD) or medians and interquartile ranges (IQR) to summarise <span class="hlt">changes</span>. Spearman's correlations assessed relationships between assessments. 1324 patients were studied. Gender ratios, age and mean disease duration were similar across all cohorts. There were temporal increases in the use of any DMARDs (rising from 61% to 87% of patients from 1996-2014), combination DMARDs (1% to 41%) and biologic (0 to 32%). Mean DAS28 fell (5.2 to 3.7), active disease (DAS28 > 5.1) declined (50% to 18%) and DAS28 remission (DAS28 < 2.6) increased (8% to 28%). In contrast HAQ scores were unchanged (1.30 to 1.32) and correlations between DAS28 and HAQ weakened (Spearman's rho fell from 0.56 to 0.44). Treatment intensity has increased over time, disease activity has fallen and there are more remissions. However, these improvements in controlling synovitis have not resulted in comparable reductions in disability measured by HAQ. As a consequence the relationship between DAS28 and HAQ has become weaker over time. Although the reasons for this divergence between disease activity and disability are uncertain, focussing treatment entirely in suppressing synovitis may be insufficient.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/22692416','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/22692416"><span>Newborn survival in Nepal: a <span class="hlt">decade</span> of <span class="hlt">change</span> and future implications.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Pradhan, Y V; Upreti, Shyam Raj; Pratap K C, Naresh; K C, Ashish; Khadka, Neena; Syed, Uzma; Kinney, Mary V; Adhikari, Ramesh Kant; Shrestha, Parashu Ram; Thapa, Kusum; Bhandari, Amit; Grear, Kristina; Guenther, Tanya; Wall, Stephen N</p> <p>2012-07-01</p> <p>Nepal is on target to meet the Millennium Development Goals for maternal and child health despite high levels of poverty, poor infrastructure, difficult terrain and recent conflict. Each year, nearly 35,000 Nepali children die before their fifth birthday, with almost two-thirds of these deaths occurring in the first month of life, the neonatal period. As part of a multi-country analysis, we examined <span class="hlt">changes</span> for newborn survival between 2000 and 2010 in terms of mortality, coverage and health system indicators as well as national and donor funding. Over the <span class="hlt">decade</span>, Nepal's neonatal mortality rate reduced by 3.6% per year, which is faster than the regional average (2.0%) but slower than national annual progress for mortality of children aged 1-59 months (7.7%) and maternal mortality (7.5%). A dramatic reduction in the total fertility rate, improvements in female education and increasing <span class="hlt">change</span> in skilled birth attendance, as well as increased coverage of community-based child health interventions, are likely to have contributed to these mortality declines. Political commitment and support for newborn survival has been generated through strategic use of global and national data and effective partnerships using primarily a selective newborn-focused approach for advocacy and planning. Nepal was the first low-income country to have a national newborn strategy, influencing similar strategies in other countries. The Community-Based Newborn Care Package is delivered through the nationally available Female Community Health Volunteers and was piloted in 10 of 75 districts, with plans to increase to 35 districts in mid-2013. Innovation and scale up, especially of community-based packages, and public health interventions and commodities appear to move relatively rapidly in Nepal compared with some other countries. Much remains to be done to achieve high rates of effective coverage of community care, and especially to improve the quality of facility-based care given the rapid</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=20010020923&hterms=landfill&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D10%26Ntt%3Dlandfill','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=20010020923&hterms=landfill&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D10%26Ntt%3Dlandfill"><span>Contribution of <span class="hlt">Changing</span> Sources and Sinks to the Growth Rate of Atmospheric Methane Concentrations for the Last Two <span class="hlt">Decades</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Matthews, Elaine; Walter, B.; Bogner, J.; Sarma, D.; Portney, B.; Hansen, James (Technical Monitor)</p> <p>2000-01-01</p> <p>In situ measurements of atmospheric methane concentrations begun in the early 1980s show <span class="hlt">decadal</span> trends, as well as large interannual variations, in growth rate. Recent research indicates that while wetlands can explain several of the large growth anomalies for individual years, the <span class="hlt">decadal</span> trend may be the combined effect of increasing sinks, due to increases in tropospheric OH, and stabilizing sources. We discuss new 20-year histories of annual, global source strengths for all major methane sources, i.e., natural wetlands, rice cultivation, ruminant animals, landfills, fossil fuels, and biomass burning, and present estimates of the temporal pattern of the sink required to reconcile these sources and atmospheric concentrations over the time period. Analysis of the individual emission sources, together with model-derived estimates of the OH sink strength, indicates that the growth rate of atmospheric methane observed over the last 20 years can only be explained by a combination of <span class="hlt">changes</span> in source emissions and an increasing tropospheric sink.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/21975172','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/21975172"><span>Climate <span class="hlt">change</span> and tropical biodiversity: a new focus.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Brodie, Jedediah; Post, Eric; Laurance, William F</p> <p>2012-03-01</p> <p>Considerable efforts are focused on the consequences of climate <span class="hlt">change</span> for tropical rainforests. However, potentially the greatest threats to tropical biodiversity (synergistic interactions between climatic <span class="hlt">changes</span> and human land use) remain understudied. <span class="hlt">Key</span> concerns are that aridification could increase the accessibility of previously non-arable or remote lands, elevate fire impacts and exacerbate ecological effects of habitat disturbance. The growing climatic <span class="hlt">change</span> literature often fails to appreciate that, in coming <span class="hlt">decades</span>, climate-land use interactions might be at least as important as abiotic <span class="hlt">changes</span> per se for the fate of tropical biodiversity. In this review, we argue that protected area expansion along <span class="hlt">key</span> ecological gradients, regulation of human-lit fires, strategic forest-carbon financing and re-evaluations of agricultural and biofuel subsidies could ameliorate some of these synergistic threats. Copyright © 2011 Elsevier Ltd. All rights reserved.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/26220636','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/26220636"><span><span class="hlt">Changing</span> Trends in Treatment of Acute Mania: Experience of a Tertiary Centre Over a <span class="hlt">Decade</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Arıkan, Mehmet Kemal; Poyraz, Cana Aksoy; Baş, Alper; Sağlam, N Gamze Usta; Batun, Gizem Cetiner; Gültekin, Gözde; Poyraz, Burç Çağrı</p> <p>2016-06-01</p> <p>We investigated trends over a <span class="hlt">decade</span> in the prescription of lithium, antiepileptics, and antipsychotic agents at discharge for patients hospitalised for acute mania. We conducted a retrospective review of medical records for 165 inpatients with acute mania who had been hospitalised in Cerrahpaşa Faculty of Medicine, Department of Psychiatry during 2001-2002 and 2011-2012. Among 165 patients, prescription of olanzapine at discharge increased from 3 to 46 % (p < 0.001), while prescription of haloperidol decreased from 55 to 21 % (p < 0.001). Use of other atypical antipsychotics did not <span class="hlt">change</span> significantly (risperidone decreased from 14 to 11 %, p = 0.5; quetiapine increased from 10 to 16 %, p = 0.2). Use of valproate, carbamazepine, and lithium did not <span class="hlt">change</span> significantly. Use of electroconvulsive therapy in acute mania decreased by half from 27 to 13 % (p = 0.02). Typical antipsychotics alone or in combination with antiepileptics were the most common treatment regimen at discharge at 2001-2002; while 10 years later, they had been largely replaced by lithium or antiepileptics combined with second generation antipsychotics. Antipsychotic agents remained to be an important component of acute treatment of mania in our practice.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017GeoRL..4411012N','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017GeoRL..4411012N"><span>Attribution of Observed Streamflow <span class="hlt">Changes</span> in <span class="hlt">Key</span> British Columbia Drainage Basins</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Najafi, Mohammad Reza; Zwiers, Francis W.; Gillett, Nathan P.</p> <p>2017-11-01</p> <p>We study the observed decline in summer streamflow in four <span class="hlt">key</span> river basins in British Columbia (BC), Canada, using a formal detection and attribution (D&A) analysis procedure. Reconstructed and simulated streamflow is generated using the semidistributed variable infiltration capacity hydrologic model, which is driven by 1/16° gridded observations and downscaled climate model data from the Coupled Model Intercomparison Project phase 5 (CMIP5), respectively. The internal variability of the regional hydrologic components using 5100 years of streamflow was simulated using CMIP5 preindustrial control runs. Results show that the observed <span class="hlt">changes</span> in summer streamflow are inconsistent with simulations representing the responses to natural forcing factors alone, while the response to anthropogenic and natural forcing factors combined is detected in these <span class="hlt">changes</span>. A two-signal D&A analysis indicates that the effects of anthropogenic (ANT) forcing factors are discernable from natural forcing in BC, albeit with large uncertainties.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016PolSc..10..199T','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016PolSc..10..199T"><span>Relationship between the Arctic oscillation and surface air temperature in multi-<span class="hlt">decadal</span> 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>Tanaka, Hiroshi L.; Tamura, Mina</p> <p>2016-09-01</p> <p>In this study, a simple energy balance model (EBM) was integrated in time, considering a hypothetical long-term variability in ice-albedo feedback mimicking the observed multi-<span class="hlt">decadal</span> temperature variability. A natural variability was superimposed on a linear warming trend due to the increasing radiative forcing of CO2. The result demonstrates that the superposition of the natural variability and the background linear trend can offset with each other to show the warming hiatus for some period. It is also stressed that the rapid warming during 1970-2000 can be explained by the superposition of the natural variability and the background linear trend at least within the simple model. The <span class="hlt">key</span> process of the fluctuating planetary albedo in multi-<span class="hlt">decadal</span> time scale is investigated using the JRA-55 reanalysis data. It is found that the planetary albedo increased for 1958-1970, decreased for 1970-2000, and increased for 2000-2012, as expected by the simple EBM experiments. The multi-<span class="hlt">decadal</span> variability in the planetary albedo is compared with the time series of the AO mode and Barents Sea mode of surface air temperature. It is shown that the recent AO negative pattern showing warm Arctic and cold mid-latitudes is in good agreement with planetary albedo <span class="hlt">change</span> indicating negative anomaly in high latitudes and positive anomaly in mid-latitudes. Moreover, the Barents Sea mode with the warm Barents Sea and cold mid-latitudes shows long-term variability similar to planetary albedo <span class="hlt">change</span>. Although further studies are needed, the natural variabilities of both the AO mode and Barents Sea mode indicate some possible link to the planetary albedo as suggested by the simple EBM to cause the warming hiatus in recent years.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://eric.ed.gov/?q=education+AND+policy+AND+higher+AND+education&pg=7&id=EJ752132','ERIC'); return false;" href="https://eric.ed.gov/?q=education+AND+policy+AND+higher+AND+education&pg=7&id=EJ752132"><span><span class="hlt">Changing</span> Structures of the Higher Education Systems: The Increasing Complexity of Underlying Forces</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>Teichler, Ulrich</p> <p>2006-01-01</p> <p><span class="hlt">Changes</span> of the shape and the size of higher education systems have been a <span class="hlt">key</span> issue of both higher education policy and higher education research for more than four <span class="hlt">decades</span>. It is widely assumed that the expansion of student enrolment was the most powerful factor in evoking structural <span class="hlt">change</span> and has caused increasing diversification. This article…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://eric.ed.gov/?q=employment+AND+situation+AND+survey&pg=4&id=ED539386','ERIC'); return false;" href="https://eric.ed.gov/?q=employment+AND+situation+AND+survey&pg=4&id=ED539386"><span><span class="hlt">Key</span> Data on Education in Europe 2012</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>Ranguelov, Stanislav; De Coster, Isabelle; Norani, Sogol; Paolini, Giulia</p> <p>2012-01-01</p> <p><span class="hlt">Key</span> Data on Education in Europe 2012 is a Eurydice flagship publication tracing the main developments of European education systems over the last <span class="hlt">decade</span>. The report combines statistical data with qualitative information to describe the organisation, management and functioning of 37 European education systems from pre-primary to higher education.…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017MS%26E..245d2005Z','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017MS%26E..245d2005Z"><span>Through The <span class="hlt">Decades</span> - <span class="hlt">Changes</span> in Social, Economic, Legal and Planning Determinants of Residential Development across <span class="hlt">Decades</span> - Evidence from Suburban Areas in Poland</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Źróbek-Różańska, Alina; Zysk, Elżbieta; Źróbek, Ryszard</p> <p>2017-10-01</p> <p>Poland has experienced many political, legal, social and economic transformations. For the last twelve <span class="hlt">decades</span>, this country was under foreign partition, in the war, under the influence of socialist system with centrally planned economy and finally regained autonomy and rapidly introduced market economy. Each epoch had its own characteristic, that can be recognized also in the residential buildings development. Therefore, the authors focused on the social, economic, legal and planning conditionings that shaped the development of the residential buildings with the most characteristic periods: pre-II world war, 50-ties, 60-ties, 70-ties, 80-ties, 90-ties and XXI century. Some of them are visible in the still existing residential buildings, especially in the suburban villages. The most recent process that can be observed in the study area is urban sprawl. Since the beginning of the XXI century, urban population in Poland has been gradually declining, while suburban villages transform into ‘urban-like’ districts. The aim of the study was to arrange and present in the <span class="hlt">decade-by-decade</span> manner, the social, economic, legal and planning conditionings that were valid in particular periods. It was realized by correlating information on the contemporary social trends, economic conditions, legal framework and planning regulations. Presentation was enriched by the examples of the buildings developed in the accordance with the contemporary restrictions.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018EaFut...6..118Z','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018EaFut...6..118Z"><span>Impact of Climate <span class="hlt">Change</span> on Siberian High and Wintertime Air Pollution in China in Past Two <span class="hlt">Decades</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Zhao, Shuyu; Feng, Tian; Tie, Xuexi; Long, Xin; Li, Guohui; Cao, Junji; Zhou, Weijian; An, Zhisheng</p> <p>2018-02-01</p> <p>China has suffered severe air pollutions during wintertime as national industrialization and urbanization have been increasingly developed in the past <span class="hlt">decades</span>. Recent studies suggest that climate <span class="hlt">change</span> has important impacts on extreme haze events in northern China. This study uses reanalysis datasets to analyze the trend and variability of Siberian High (SiH) intensity, and its relationship with the Arctic temperature and sea ice cover (SIC) in past two <span class="hlt">decades</span>. The results show that Arctic is warming accompanied by a rapid decline of SIC, while Eurasia is cooling and SiH intensity is gradually enhancing. The statistics illustrates that the SiH has a significantly positive correlation to the temperature (R = 0.70), and a significant anticorrelation to the SIC (R = -0.69), and this is because the warming Arctic and the reducing SIC enhanced the SiH. The enhanced SiH leads to strengthened northerly winds in the North China Plain (NCP). The WRF-Chem model calculation reveals the strengthened northerly winds during the stronger SiH period in January 2016 produce a significant decrease in PM2.5 (particulate matter with aerodynamic diameter less than 2.5 µm) concentrations by 100-200 µg m-3 than that during the weaker one in January 2013. A sensitivity calculation figures out the reduction of PM2.5 concentrations due to a decrease of 50% in emissions is comparable to <span class="hlt">changes</span> from the weak SiH condition to the strong SiH condition, suggesting that extreme climate variability in the past few years could have an equivalent impact as a consequence of a large emission reduction on wintertime air pollution in the NCP.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2002EGSGA..27..643L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2002EGSGA..27..643L"><span>Spatial Organization In Europe of <span class="hlt">Decadal</span> and Interdecadal Fluctuations In Annual Rainfall</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Lucero, O. A.; Rodriguez, N. C.</p> <p></p> <p>In this research the spatial patterns of <span class="hlt">decadal</span> and bidecadal fluctuations in annual rainfall in Europe are identified. Filtering of time series of anomaly of annual rainfall is carried out using the Morlet wavelet technique. Reconstruction is achieved by sum- ming the contributions from bands of wavelet timescales; the <span class="hlt">decadal</span> band and the bidecadal band are composed of contributions from the band of (10- to 17-year] and (17- to 27- year] timescales respectively. Results indicate that 1) the spatial organi- zation of <span class="hlt">decadal</span> and bidecadal components of annual rainfall are standing wave-like organized patterns. Three standing <span class="hlt">decadal</span> fluctuations zonally aligned formed the spatial pattern from 1900 until 1931; thereafter the pattern <span class="hlt">changed</span> into a NW-SE orientation. The <span class="hlt">decadal</span> band shows an average 12-year period. 2) The spatial orga- nization of bidecadal component was composed of three standing fluctuations since 1903 to 1986. After 1987 two standing bidecadal fluctuations were located on Europe. The orientation of bidecadal fluctuations <span class="hlt">changed</span> during the period under study. Until 1913 the spatial pattern of the bidecadal component was zonally aligned. Since 1913 until 1986 the three bidecadal fluctuations composing the spatial pattern were aligned SW U NE; starting 1987 the spatial pattern is composed of two standing fluctuations zonally aligned. The bidecadal spatial pattern shows an average period of 20- to 22- year length. 3) At <span class="hlt">decadal</span> and bidecadal timescales, the first principal component of the spatial field of anomaly of annual rainfall and the NAO index are connected. The upper positive third (lower negative third) of values of first principal component are indicative of extensive area with positive (negative) anomaly of annual rainfall. 4) At <span class="hlt">decadal</span> timescale the relative phase between the first PC and the NAO index <span class="hlt">changes</span> through the period under study; these <span class="hlt">changes</span> define three regimes: 1) Dur- ing the regime covering the period 1900 (start of</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://eric.ed.gov/?q=feminist+AND+psychotherapy&pg=2&id=EJ221154','ERIC'); return false;" href="https://eric.ed.gov/?q=feminist+AND+psychotherapy&pg=2&id=EJ221154"><span>A <span class="hlt">Decade</span> of Feminist Influence on Psychotherapy.</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>Brodsky, Annette M.</p> <p>1980-01-01</p> <p>Last <span class="hlt">decade</span> has seen some major impacts of feminism on institution of psychotherapy regarding theories, treatment techniques, and assessment instruments. <span class="hlt">Changes</span> in attitudes toward women as therapists and as clients have reflected general advances of women's movement. Presented at American Psychological Association Convention, Toronto, Canada,…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015EGUGA..1711910C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015EGUGA..1711910C"><span>Observations of <span class="hlt">changes</span> in the dissolved CO2 system in the North Sea, in four summers of the 2001-2011 <span class="hlt">decade</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Clargo, Nicola; Salt, Lesley; Thomas, Helmuth; de Baar, Hein</p> <p>2015-04-01</p> <p>Since the industrial revolution, atmospheric concentrations of carbon dioxide (CO2) have risen dramatically, largely due to the combustion of fossil fuels, <span class="hlt">changes</span> in land-use patterns and the production of cement. The oceans have absorbed a large amount of this CO2, with resulting impacts on ocean chemistry. Coastal seas play a significant role in the mitigation of anthropogenic atmospheric CO2 as they contribute approximately 10-30% of global primary productivity despite accounting for only 7% of the surface area. The North Sea is a perfect natural laboratory in which to study the CO2 system as it consists of two biogeochemically distinct regions displaying both oceanic and relatively coastal behaviour. It has also been identified as a continental shelf pump with respect to CO2, transporting it to the deeper waters of the North Atlantic. Large scale forcing has been shown to have a significant impact on the CO2 system over varying time scales, often masking the effects of anthropogenic influence. Here, we present data from the North Sea spanning the 2001-2011 <span class="hlt">decade</span>. In order to investigate the dynamics of the dissolved CO2 system in this region in the face of climate <span class="hlt">change</span>, four basin-wide cruises were conducted during the summers of 2001, 2005, 2008 and 2011. The acquired Dissolved Inorganic Carbon (DIC) and alkalinity data were then used to fully resolve the carbon system in order to assess trends over the 2001-2011 <span class="hlt">decade</span>. We find significant interannual variability, but with a consistent, notable trend in decreasing pH. We found that surface alkalinity remained relatively constant over the <span class="hlt">decade</span>, whereas DIC increased, indicating that the pH decline is DIC-driven. We also found that the partial pressure of CO2 (pCO2) increased faster than concurrent atmospheric CO2 concentrations, and that the CO2 buffering capacity of the North Sea decreased over the <span class="hlt">decade</span>, with implications for future CO2 uptake.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018ClDy...50.1597H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018ClDy...50.1597H"><span><span class="hlt">Decadal</span> fluctuations in the western Pacific recorded by long precipitation records in Taiwan</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Huang, Wan-Ru; Wang, S.-Y. Simon; Guan, Biing T.</p> <p>2018-03-01</p> <p>A 110-year precipitation record in Taiwan, located at the western edge of the subtropical North Pacific, depicts a pronounced quasi-<span class="hlt">decadal</span> oscillation (QDO). The QDO in Taiwan exhibits a fluctuating relationship with the similar <span class="hlt">decadal</span> variations of sea surface temperature (SST) anomalies in the central equatorial Pacific, known as the Pacific QDO. A regime <span class="hlt">change</span> was observed around 1960, such that the <span class="hlt">decadal</span> variation of Taiwan's precipitation became more synchronized with the Pacific QDO's coupled evolutions of SST and atmospheric circulation than before, while the underlying pattern of the Pacific QOD did not <span class="hlt">change</span>. Using long-term reanalysis data and CMIP5 single-forcing experiments, the presented analysis suggests that increased SST in the subtropical western Pacific and the strengthened western extension of the North Pacific subtropical anticyclone may have collectively enhanced the relationship between the Taiwan precipitation and the Pacific QDO. This finding provides possible clues to similar regime <span class="hlt">changes</span> in quasi-<span class="hlt">decadal</span> variability observed around the western Pacific rim.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018PrOce.161..131J','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018PrOce.161..131J"><span><span class="hlt">Decadal</span> variability on the Northwest European continental shelf</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Jones, Sam; Cottier, Finlo; Inall, Mark; Griffiths, Colin</p> <p>2018-02-01</p> <p><span class="hlt">Decadal</span> scale time series of the shelf seas are important for understanding both climate and process studies. Despite numerous investigations of long-term temperature variability in the shelf seas, studies of salinity variability are few. Salt is a more conservative tracer than temperature in shallow seas, and it can reveal <span class="hlt">changes</span> in local hydrographic conditions as well as transmitted basin-scale <span class="hlt">changes</span>. Here, new inter-annual salinity time series on the northwest European shelf are developed and a 13 year high resolution salinity record from a coastal mooring in western Scotland is presented and analysed. We find strong temporal variability in coastal salinity on timescales ranging from tidal to inter-annual, with the magnitude of variability greatest during winter months. There is little seasonality and no significant <span class="hlt">decadal</span> trend in the coastal time series of salinity. We propose 4 hydrographic states to explain salinity variance in the shelf area west of Scotland based on the interaction between a baroclinic coastal current and wind-forced barotropic flow: while wind forcing is important, we find that <span class="hlt">changes</span> in the buoyancy-driven flow are more likely to influence long-term salinity observations. We calculate that during prevailing westerly wind conditions, surface waters in the Sea of the Hebrides receive a mix of 62% Atlantic origin water to 38% coastal sources. This contrasts with easterly wind conditions, during which the mix is 6% Atlantic to 94% coastal sources on average. This 'switching' between hydrographic states is expected to impact nutrient transport and therefore modify the level of primary productivity on the shelf. This strong local variability in salinity is roughly an order of magnitude greater than <span class="hlt">changes</span> in the adjacent ocean basin, and we infer from this that Scottish coastal waters are likely to be resilient to <span class="hlt">decadal</span> <span class="hlt">changes</span> in ocean climate.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/26488299','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/26488299"><span>Spatially Extensive Standardized Surveys Reveal Widespread, Multi-<span class="hlt">Decadal</span> Increase in East Antarctic Adélie Penguin Populations.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Southwell, Colin; Emmerson, Louise; McKinlay, John; Newbery, Kym; Takahashi, Akinori; Kato, Akiko; Barbraud, Christophe; DeLord, Karine; Weimerskirch, Henri</p> <p>2015-01-01</p> <p>Seabirds are considered to be useful and practical indicators of the state of marine ecosystems because they integrate across <span class="hlt">changes</span> in the lower trophic levels and the physical environment. Signals from this <span class="hlt">key</span> group of species can indicate broad scale impacts or response to environmental <span class="hlt">change</span>. Recent studies of penguin populations, the most commonly abundant Antarctic seabirds in the west Antarctic Peninsula and western Ross Sea, have demonstrated that physical <span class="hlt">changes</span> in Antarctic marine environments have profound effects on biota at high trophic levels. Large populations of the circumpolar-breeding Adélie penguin occur in East Antarctica, but direct, standardized population data across much of this vast coastline have been more limited than in other Antarctic regions. We combine extensive new population survey data, new population estimation methods, and re-interpreted historical survey data to assess <span class="hlt">decadal</span>-scale <span class="hlt">change</span> in East Antarctic Adélie penguin breeding populations. We show that, in contrast to the west Antarctic Peninsula and western Ross Sea where breeding populations have decreased or shown variable trends over the last 30 years, East Antarctic regional populations have almost doubled in abundance since the 1980's and have been increasing since the earliest counts in the 1960's. The population <span class="hlt">changes</span> are associated with five-year lagged <span class="hlt">changes</span> in the physical environment, suggesting that the <span class="hlt">changing</span> environment impacts primarily on the pre-breeding age classes. East Antarctic marine ecosystems have been subject to a number of <span class="hlt">changes</span> over the last 50 years which may have influenced Adélie penguin population growth, including <span class="hlt">decadal</span>-scale climate variation, an inferred mid-20th century sea-ice contraction, and early-to-mid 20th century exploitation of fish and whale populations.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4619065','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4619065"><span>Spatially Extensive Standardized Surveys Reveal Widespread, Multi-<span class="hlt">Decadal</span> Increase in East Antarctic Adélie Penguin Populations</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Southwell, Colin; Emmerson, Louise; McKinlay, John; Newbery, Kym; Takahashi, Akinori; Kato, Akiko; Barbraud, Christophe; DeLord, Karine; Weimerskirch, Henri</p> <p>2015-01-01</p> <p>Seabirds are considered to be useful and practical indicators of the state of marine ecosystems because they integrate across <span class="hlt">changes</span> in the lower trophic levels and the physical environment. Signals from this <span class="hlt">key</span> group of species can indicate broad scale impacts or response to environmental <span class="hlt">change</span>. Recent studies of penguin populations, the most commonly abundant Antarctic seabirds in the west Antarctic Peninsula and western Ross Sea, have demonstrated that physical <span class="hlt">changes</span> in Antarctic marine environments have profound effects on biota at high trophic levels. Large populations of the circumpolar-breeding Adélie penguin occur in East Antarctica, but direct, standardized population data across much of this vast coastline have been more limited than in other Antarctic regions. We combine extensive new population survey data, new population estimation methods, and re-interpreted historical survey data to assess <span class="hlt">decadal</span>-scale <span class="hlt">change</span> in East Antarctic Adélie penguin breeding populations. We show that, in contrast to the west Antarctic Peninsula and western Ross Sea where breeding populations have decreased or shown variable trends over the last 30 years, East Antarctic regional populations have almost doubled in abundance since the 1980’s and have been increasing since the earliest counts in the 1960’s. The population <span class="hlt">changes</span> are associated with five-year lagged <span class="hlt">changes</span> in the physical environment, suggesting that the <span class="hlt">changing</span> environment impacts primarily on the pre-breeding age classes. East Antarctic marine ecosystems have been subject to a number of <span class="hlt">changes</span> over the last 50 years which may have influenced Adélie penguin population growth, including <span class="hlt">decadal</span>-scale climate variation, an inferred mid-20th century sea-ice contraction, and early-to-mid 20th century exploitation of fish and whale populations. PMID:26488299</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/21521088','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/21521088"><span><span class="hlt">Decades</span> of transition for the US reserves: <span class="hlt">changing</span> demands on reserve identity and mental well-being.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Griffith, James</p> <p>2011-04-01</p> <p>The US strategic defence policy has undergone dramatic <span class="hlt">changes</span> in the last two <span class="hlt">decades</span>, with more recent <span class="hlt">changes</span> having placed increased demands on members of the reserve components. Rapid and often unexpected call-ups of reserves for operational missions, both domestic and international, required meeting standards for mobilization and deployment. Standards were in place but not necessarily met. Mobilizations pointed to several areas of unpreparedness; at first, obvious areas, such as members being physically unfit, inadequately trained and improperly equipped and less than competent unit leaders; and later, less obvious areas, in particular, emergent personal adjustment problems. During these mobilizations, unique consequences of stressors on individual reservists were evident, including worries about family and civilian job during deployment, adjustments to returning and reintegration, post-deployment post-traumatic stress disorder and related symptoms, and now suicide. Some have explained these findings, though lacking is a broad explanatory framework. Reserve identity is offered as a preliminary concept to interpret reservists' deployment experiences, post-deployment adjustment, and associated mental health needs, providing a basis for preventive intervention strategies.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://eric.ed.gov/?q=divorce+AND+poverty&pg=7&id=ED224557','ERIC'); return false;" href="https://eric.ed.gov/?q=divorce+AND+poverty&pg=7&id=ED224557"><span>America's Children and Their Families: <span class="hlt">Key</span> Facts.</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>Simons, Janet M.; Eng, Mary</p> <p></p> <p>For advocates, parents, educators, researchers, and speechmakers, this book brings together <span class="hlt">key</span> facts and statistical data about the American family, now and in the near future. The first section provides an overview of population and demographic trends extending through the first <span class="hlt">decade</span> of the 21st century. This overview is followed by sections…</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('https://www.ncbi.nlm.nih.gov/pubmed/24236844','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/24236844"><span>The A to Z of pharmaceutical cocrystals: a <span class="hlt">decade</span> of fast-moving new science and patents.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Almarsson, Örn; Peterson, Matthew L; Zaworotko, Michael</p> <p>2012-07-01</p> <p>From aspirin to zoledronic acid, pharmaceutical cocrystals emerged in the past <span class="hlt">decade</span> as a promising new weapon in the arsenal of drug development. Resurgence of interest in multicomponent crystal compositions has led to significant advances in the science of cocrystal design and discovery. These advances have built upon crystal engineering, which provides a deep understanding of supramolecular interactions between molecules that govern crystal packing and physicochemical properties of crystalline materials. Concomitantly, the patent landscape of pharmaceutical cocrystals developed rapidly in the last <span class="hlt">decade</span>. This review presents a broad survey of patents issued in the area of pharmaceutical cocrystals. In addition, the review contains analyses of <span class="hlt">key</span> patents in the area involving compositions and methodologies. Along the way, the main events of the past <span class="hlt">decade</span> representing a renaissance of cocrystals of pharmaceutical materials are chronicled. Future directions in the area are discussed in light of <span class="hlt">key</span> pending patent applications and recent publications of seminal interest.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012EGUGA..14..747P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012EGUGA..14..747P"><span>The trajectories and determinants of agricultural land-use <span class="hlt">change</span> over the last two <span class="hlt">decades</span> in post-Soviet European Russia</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Prishchepov, A. V.; Müller, D.; Sieber, A.; Kuemmerle, T.; Radeloff, V. C.; Hostert, P.</p> <p>2012-04-01</p> <p>The transition from state-command to market-driven economies in Russia in 1991 triggered fundamental political, economic and institutional <span class="hlt">changes</span>, which in turn drastically affected agricultural land use. Large tracks of agricultural lands became abandoned, particularly during the first <span class="hlt">decade</span> of the transition. However, it is not clear how the <span class="hlt">changing</span> socio-economic and political conditions in post-Soviet Russia <span class="hlt">changed</span> abandonment trajectories over the last two <span class="hlt">decades</span>. We analyzed agricultural land-use <span class="hlt">change</span>, both agricultural land abandonment and recultivation of once abandoned agricultural lands, with multitemporal Landsat TM/ETM+ images for 1990-2000-2009 to study Ryazan province in the forest-steppe transition zone and Rostov province in the steppe zone of European Russia. We classified agricultural land use <span class="hlt">change</span> over 1990-2000-2009 with Support Vector Machines and assessed classification accuracies with independently of training datasets collected validation data. Overall accuracies were over 80%. We summarized the rates of agricultural land use <span class="hlt">change</span>, and quantified the spatial determinants of these land use <span class="hlt">change</span> processes using logistic regressions. Results indicated that 28% of agricultural land managed in 1990 were abandoned by the year 2000 in Ryazan province. From 2000 to 2009, agricultural land abandonment increased by another half what was abandoned from 1990 to 2000 and comprised 42% of abandoned agricultural that was managed in 1990 while only 1.4% of previously abandoned agricultural land was recultivated. In other words, agricultural abandonment was a continuous and permanent land use <span class="hlt">change</span> in Ryazan province. In Rostov province, abandonment rates were substantially lower at nearly 10% of the agricultural land managed in 1990 and only minor additional abandonment from 2000 to 2009. The pattern of agricultural land abandonment in Ryazan province was largely determined by a mix of socio-economic and environmental factors (e.g. increased</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/18798456','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/18798456"><span>[Multiple pregnancies prevalence: its raise on last <span class="hlt">decade</span>].</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Herrera, Ricardo Jorge Hernández; Torres, Mauro Ochoa; Santos, Roberto Flores; Flores, Raúl Cortés; Sánchez, Gerardo Forsbasch</p> <p>2008-09-01</p> <p>Multiple pregnancies prevalence has been increasing in last <span class="hlt">decade</span>, which have also increased the requirements of neonatal intensive care units and all problems related to premature neonate or low birth weight. Prevalence rate of twin (18 to 26 in 1,000 births), and triple pregnancies (0.37 to 1.74 in 1,000 births) have raised too, perhaps due to assisted reproductive techniques. To know incidence of multiple pregnancies at Unidad Medica de Alta Especialidad no. 23, from Institute Mexicano del Seguro Social. Retrospective and descriptive study. We review the files of multiple pregnancies from 1972 to 2006 to estimate its rate and <span class="hlt">change</span> every five and ten years. We registered 9,055 twin pregnancies during the period, with a rate of 7.1 to 14.4 in 1,000 (63% of increase in the last <span class="hlt">decade</span> [12.6 in 1,000 births] compared with the previous <span class="hlt">decade</span> [7.7 in 1,000 births]; p < 0.005). Pregnancies with three or more fetuses were 202, with 191 triplets, 13 with four, three with five, and one with six products (646 newborns). Incidence of multiple pregnancies with four or more products has also increased in last <span class="hlt">decade</span>: 230 times higher than two <span class="hlt">decades</span> before. Multiple pregnancies rate has increased in last <span class="hlt">decade</span>: 63% in twin pregnancies, 217% in triplets, and 230 times more than expected in four or more products pregnancies.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/27259038','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/27259038"><span><span class="hlt">Key</span> challenges and priorities for modelling European grasslands under climate <span class="hlt">change</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Kipling, Richard P; Virkajärvi, Perttu; Breitsameter, Laura; Curnel, Yannick; De Swaef, Tom; Gustavsson, Anne-Maj; Hennart, Sylvain; Höglind, Mats; Järvenranta, Kirsi; Minet, Julien; Nendel, Claas; Persson, Tomas; Picon-Cochard, Catherine; Rolinski, Susanne; Sandars, Daniel L; Scollan, Nigel D; Sebek, Leon; Seddaiu, Giovanna; Topp, Cairistiona F E; Twardy, Stanislaw; Van Middelkoop, Jantine; Wu, Lianhai; Bellocchi, Gianni</p> <p>2016-10-01</p> <p>Grassland-based ruminant production systems are integral to sustainable food production in Europe, converting plant materials indigestible to humans into nutritious food, while providing a range of environmental and cultural benefits. Climate <span class="hlt">change</span> poses significant challenges for such systems, their productivity and the wider benefits they supply. In this context, grassland models have an important role in predicting and understanding the impacts of climate <span class="hlt">change</span> on grassland systems, and assessing the efficacy of potential adaptation and mitigation strategies. In order to identify the <span class="hlt">key</span> challenges for European grassland modelling under climate <span class="hlt">change</span>, modellers and researchers from across Europe were consulted via workshop and questionnaire. Participants identified fifteen challenges and considered the current state of modelling and priorities for future research in relation to each. A review of literature was undertaken to corroborate and enrich the information provided during the horizon scanning activities. Challenges were in four categories relating to: 1) the direct and indirect effects of climate <span class="hlt">change</span> on the sward 2) climate <span class="hlt">change</span> effects on grassland systems outputs 3) mediation of climate <span class="hlt">change</span> impacts by site, system and management and 4) cross-cutting methodological issues. While research priorities differed between challenges, an underlying theme was the need for accessible, shared inventories of models, approaches and data, as a resource for stakeholders and to stimulate new research. Developing grassland models to effectively support efforts to tackle climate <span class="hlt">change</span> impacts, while increasing productivity and enhancing ecosystem services, will require engagement with stakeholders and policy-makers, as well as modellers and experimental researchers across many disciplines. The challenges and priorities identified are intended to be a resource 1) for grassland modellers and experimental researchers, to stimulate the development of new research</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/23618022','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/23618022"><span>Coping with child hunger in Canada: have household strategies <span class="hlt">changed</span> over a <span class="hlt">decade</span>?</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>McIntyre, Lynn; Bartoo, Aaron C; Pow, Jody; Potestio, Melissa L</p> <p>2012-11-05</p> <p>To determine if household coping strategies for child hunger in Canada have <span class="hlt">changed</span> over a <span class="hlt">decade</span> (1996-2007). We applied t-tests to data derived from Cycle 2 (1996-1997; n=8165) and Cycle 7 (2006-2007; n=15,961) of the National Longitudinal Survey of Children and Youth (NLSCY) to determine <span class="hlt">changes</span> in household coping strategies for child hunger. Data were restricted to households with children aged 2-9 years, allowing for cross-sectional analysis of two independent samples. Logistic regression was employed to estimate the odds of reporting child hunger for socio-demographic characteristics and the odds of using different coping strategies. The national prevalence of child hunger fell from 1.5% in 1997 to 0.7% in 2007 (p<0.001). The determinants of child hunger (increased child age and household size, lack of home ownership, low household income, lone-parent status, family dysfunction) and hunger frequency (regular versus occasional) were similar in both NLSCY cycles. Utilization of food banks and other community resources as a method of coping with child hunger remained static despite an increase in national food banks/affiliated agencies in Canada (2,141 in 1998 to 3,540 in 2007). In contrast, there was an increased reliance on reducing household food variety, an internal coping mechanism, to manage child hunger (17.6% Cycle 2 to 35.1% Cycle 7; p=0.03). Community outreach programs between 1997 and 2007 had little impact on coping strategies utilized by households facing child hunger. Our results indicate that current initiatives fail to reach these families.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://eric.ed.gov/?q=poverty&pg=7&id=EJ888915','ERIC'); return false;" href="https://eric.ed.gov/?q=poverty&pg=7&id=EJ888915"><span>Poverty and the American Family: A <span class="hlt">Decade</span> in Review</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>Edin, Kathryn; Kissane, Rebecca Joyce</p> <p>2010-01-01</p> <p>Because of dramatic levels of economic volatility and massive <span class="hlt">changes</span> in welfare policies, scholars in this <span class="hlt">decade</span> worried anew about whether our official poverty measure, adopted in the 1960s, is adequate. Poverty's causes continued to be debated, with demographic factors often pitted against policy and maternal employment <span class="hlt">changes</span>. Some scholars…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017JHyd..553..559S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017JHyd..553..559S"><span>High resolution <span class="hlt">decadal</span> precipitation predictions over the continental United States for impacts assessment</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Salvi, Kaustubh; Villarini, Gabriele; Vecchi, Gabriel A.</p> <p>2017-10-01</p> <p>Unprecedented alterations in precipitation characteristics over the last century and especially in the last two <span class="hlt">decades</span> have posed serious socio-economic problems to society in terms of hydro-meteorological extremes, in particular flooding and droughts. The origin of these alterations has its roots in <span class="hlt">changing</span> climatic conditions; however, its threatening implications can only be dealt with through meticulous planning that is based on realistic and skillful <span class="hlt">decadal</span> precipitation predictions (DPPs). Skillful DPPs represent a very challenging prospect because of the complexities associated with precipitation predictions. Because of the limited skill and coarse spatial resolution, the DPPs provided by General Circulation Models (GCMs) fail to be directly applicable for impact assessment. Here, we focus on nine GCMs and quantify the seasonally and regionally averaged skill in DPPs over the continental United States. We address the problems pertaining to the limited skill and resolution by applying linear and kernel regression-based statistical downscaling approaches. For both the approaches, statistical relationships established over the calibration period (1961-1990) are applied to the retrospective and near future <span class="hlt">decadal</span> predictions by GCMs to obtain DPPs at ∼4 km resolution. The skill is quantified across different metrics that evaluate potential skill, biases, long-term statistical properties, and uncertainty. Both the statistical approaches show improvements with respect to the raw GCM data, particularly in terms of the long-term statistical properties and uncertainty, irrespective of lead time. The outcome of the study is monthly DPPs from nine GCMs with 4-km spatial resolution, which can be used as a <span class="hlt">key</span> input for impacts assessments.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://eric.ed.gov/?q=security+AND+stakeholder&pg=2&id=EJ1033559','ERIC'); return false;" href="https://eric.ed.gov/?q=security+AND+stakeholder&pg=2&id=EJ1033559"><span>Understanding <span class="hlt">Key</span> Stakeholder Belief Systems or Institutional Logics Related to Nontenure-Track Faculty and the <span class="hlt">Changing</span> Professoriate</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>Teachers College Record, 2014</p> <p>2014-01-01</p> <p>Background/context: Over the past 40 years, the composition of the professoriate has <span class="hlt">changed</span> substantially across all institutional types. Once predominantly tenure track, now nontenure-track faculty (NTTF) constitute more than 70% of the faculty. While these major <span class="hlt">changes</span> have occurred, we know little about <span class="hlt">key</span> stakeholders' views…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/26108747','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/26108747"><span><span class="hlt">Decadal</span> <span class="hlt">changes</span> in the land use/land cover and shoreline along the coastal districts of southern Gujarat, India.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Misra, A; Balaji, R</p> <p>2015-07-01</p> <p>The coastal zone along the districts of Surat, Navsari, and Valsad in southern Gujarat, India, is reported to be facing serious environmental challenges in the form of shoreline erosion, wetland loss, and man-made encroachments. This study assesses the <span class="hlt">decadal</span> land use/ land cover (LULC) <span class="hlt">changes</span> in these three districts for the years 1990, 2001, and 2014 using satellite datasets of Landsat TM, ETM, and OLI. The LULC <span class="hlt">changes</span> are identified by using band ratios as a pre-classification step, followed by implementation of hybrid classification (a combination of supervised and unsupervised classification). An accuracy assessment is carried out for each dataset, and the overall accuracy ranges from 90 to 95%. It is observed that the spatial extents of aquaculture, urban built-up, and barren classes have appreciated over time, whereas the coverage of mudflats has depreciated due to rapid urbanization. The <span class="hlt">changes</span> in the shoreline of these districts have also been analyzed for the same years, and significant <span class="hlt">changes</span> are found in the form of shoreline erosion. The LULC maps prepared as well as the shoreline <span class="hlt">change</span> analysis done for this study area will enable the local decision makers to adopt better land-use planning and shoreline protection measures, which will further aid in sustainable future developments in this region.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/27025270','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/27025270"><span>A <span class="hlt">decade</span> of pig genome sequencing: a window on pig domestication and evolution.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Groenen, Martien A M</p> <p>2016-03-29</p> <p>Insight into how genomes <span class="hlt">change</span> and adapt due to selection addresses <span class="hlt">key</span> questions in evolutionary biology and in domestication of animals and plants by humans. In that regard, the pig and its close relatives found in Africa and Eurasia represent an excellent group of species that enables studies of the effect of both natural and human-mediated selection on the genome. The recent completion of the draft genome sequence of a domestic pig and the development of next-generation sequencing technology during the past <span class="hlt">decade</span> have created unprecedented possibilities to address these questions in great detail. In this paper, I review recent whole-genome sequencing studies in the pig and closely-related species that provide insight into the demography, admixture and selection of these species and, in particular, how domestication and subsequent selection of Sus scrofa have shaped the genomes of these animals.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://cfpub.epa.gov/si/si_public_record_report.cfm?direntryid=336232','PESTICIDES'); return false;" href="https://cfpub.epa.gov/si/si_public_record_report.cfm?direntryid=336232"><span>Contrasting <span class="hlt">Decadal</span>-Scale <span class="hlt">Changes</span> in Elevation and ...</span></a></p> <p><a target="_blank" href="http://www.epa.gov/pesticides/search.htm">EPA Pesticide Factsheets</a></p> <p></p> <p></p> <p>Northeastern US salt marshes face multiple co-stressors, including accelerating rates of relative sea level rise (RSLR), elevated nutrient inputs, and low sediment supplies. In order to evaluate how marsh surface elevations respond to such factors, we used surface elevation tables (SETs) and surface elevation pins to measure <span class="hlt">changes</span> in marsh surface elevation in two eastern Long Island Sound salt marshes, Barn Island and Mamacoke marshes. We compare marsh elevation <span class="hlt">change</span> at these two systems with recent rates of RSLR and find evidence of differences between the two sites; Barn Island is maintaining its historic rate of elevation gain (2.3 ± 0.24 mm year−1 from 2003 to 2013) and is no longer keeping pace with RSLR, while Mamacoke shows evidence of a recent increase in rates (4.2 ± 0.52 mm year−1 from 1994 to 2014) to maintain its elevation relative to sea level. In addition to data on short-term elevation responses at these marshes, both sites have unusually long and detailed data on historic vegetation species composition extending back more than half a century. Over this study period, vegetation patterns track elevation <span class="hlt">change</span> relative to sea levels, with the Barn Island plant community shifting towards those plants that are found at lower elevations and the Mamacoke vegetation patterns showing little <span class="hlt">change</span> in plant composition. We hypothesize that the apparent contrasting trend in marsh elevation at the sites is due to differences in sediment a</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/23820665','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/23820665"><span>The impact of IT over five <span class="hlt">decades</span> - towards the Ambient organization.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Bjørn-Andersen, Niels; Raymond, Benoit</p> <p>2014-03-01</p> <p>This contribution to the Ken D. Eason special issue is an illustration of the value of socio-technical analysis applied at an organizational level. We provide a brief historical overview of socio-technical IS research and review studies investigating the impact of IT on organizational structures in the last five <span class="hlt">decades</span>, identifying a dominating (new) research theme in each <span class="hlt">decade</span>. A <span class="hlt">key</span> overall impact of IT in all <span class="hlt">decades</span> has been a dramatic decrease in transaction costs making it increasingly easier for organizations to source from external providers. A five level taxonomy of sourcing arrangement is developed together with a framework of organizational activities, and a number of significant cases are offered of how organizations are sourcing practically all types of business processes, including innovation. We argue that future IT will further accelerate the movement towards more sourcing, eventually leading to a new type of organization that we call the Ambient organization. Copyright © 2013 Elsevier Ltd and The Ergonomics Society. All rights reserved.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29703895','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29703895"><span>Limits on determining the skill of North Atlantic Ocean <span class="hlt">decadal</span> predictions.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Menary, Matthew B; Hermanson, Leon</p> <p>2018-04-27</p> <p>The northern North Atlantic is important globally both through its impact on the Atlantic Meridional Overturning Circulation (AMOC) and through widespread atmospheric teleconnections. The region has been shown to be potentially predictable a <span class="hlt">decade</span> ahead with the skill of <span class="hlt">decadal</span> predictions assessed against reanalyses of the ocean state. Here, we show that the prediction skill in this region is strongly dependent on the choice of reanalysis used for validation, and describe the causes. Multiannual skill in <span class="hlt">key</span> metrics such as Labrador Sea density and the AMOC depends on more than simply the choice of the prediction model. Instead, this skill is related to the similarity between the nature of interannual density variability in the underlying climate model and the chosen reanalysis. The climate models used in these <span class="hlt">decadal</span> predictions are also used in climate projections, which raises questions about the sensitivity of these projections to the models' innate North Atlantic density variability.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016EGUGA..18.5406C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016EGUGA..18.5406C"><span>Weakening of the relationship between the Indian Ocean Dipole and the ENSO in recent <span class="hlt">decades</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Choi, Jun-Young; Ham, Yoo-Geun; Kug, Jong-Seong</p> <p>2016-04-01</p> <p>This study reports, on the 20th century the relationship between the El Nino Southern Oscillation (ENSO) and the Indian Ocean Dipole (IOD) was weaker then late 1990s. We shows that 15-yr moving correlation between the Nino3.4 index during the December to February (DJF) and IOD index during the September to November (SON) season. At this results we divided previous <span class="hlt">decades</span> (1979 to 1998) and late <span class="hlt">decades</span> (1999 to 2014). The correlation coefficient was 0.64 in the previous <span class="hlt">decades</span> and 0.21 in the late <span class="hlt">decades</span>. Late <span class="hlt">decades</span> was suddenly weaker then previous <span class="hlt">decades</span>. Because, there is a big difference between previous <span class="hlt">decades</span> and late <span class="hlt">decades</span> in the ENSO regressed precipitation anomaly spatial distribution during the El Nino developing the MAM season. There was existed positive precipitation anomalies over the off-equatorial western Pacific. It was induced the cross-equatorial southerly flow over the eastern Indian Ocean and maritime continent. It means cross-equatorial southerly flow was <span class="hlt">key</span> point to understanding ENSO-IOD coupling system. In addition, using the climate models participated in Coupled Model Intercomparison Project phase 5 (CMIP5) supports the observational results.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=20020022509&hterms=climate+change+evidence&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D50%26Ntt%3Dclimate%2Bchange%2Bevidence','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=20020022509&hterms=climate+change+evidence&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D50%26Ntt%3Dclimate%2Bchange%2Bevidence"><span>Evidence for Large <span class="hlt">Decadal</span> Variability in the Tropical Mean Radiative Energy Budget</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Wielicki, Bruce A.; Wong, Takmeng; Allan, Richard; Slingo, Anthony; Kiehl, Jeffrey T.; Soden, Brian J.; Gordon, C. T.; Miller, Alvin J.; Yang, Shi-Keng; Randall, David R.; <a style="text-decoration: none; " href="javascript:void(0); " onClick="displayelement('author_20020022509'); toggleEditAbsImage('author_20020022509_show'); toggleEditAbsImage('author_20020022509_hide'); "> <img style="display:inline; width:12px; height:12px; " src="images/arrow-up.gif" width="12" height="12" border="0" alt="hide" id="author_20020022509_show"> <img style="width:12px; height:12px; display:none; " src="images/arrow-down.gif" width="12" height="12" border="0" alt="hide" id="author_20020022509_hide"></p> <p>2001-01-01</p> <p>It is widely assumed that variations in the radiative energy budget at large time and space scales are very small. We present new evidence from a compilation of over two <span class="hlt">decades</span> of accurate satellite data that the top-of-atmosphere (TOA) tropical radiative energy budget is much more dynamic and variable than previously thought. We demonstrate that the radiation budget <span class="hlt">changes</span> are caused by <span class="hlt">changes</span> In tropical mean cloudiness. The results of several current climate model simulations fall to predict this large observed variation In tropical energy budget. The missing variability in the models highlights the critical need to Improve cloud modeling in the tropics to support Improved prediction of tropical climate on Inter-annual and <span class="hlt">decadal</span> time scales. We believe that these data are the first rigorous demonstration of <span class="hlt">decadal</span> time scale <span class="hlt">changes</span> In the Earth's tropical cloudiness, and that they represent a new and necessary test of climate models.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018JHyd..560..461F','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018JHyd..560..461F"><span><span class="hlt">Decadal</span> <span class="hlt">changes</span> of reference crop evapotranspiration attribution: Spatial and temporal variability over China 1960-2011</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Fan, Ze-Xin; Thomas, Axel</p> <p>2018-05-01</p> <p>Atmospheric evaporative demand can be used as a measure of the hydrological cycle and the global energy balance. Its long-term variation and the role of driving climatic factors have received increasingly attention in climate <span class="hlt">change</span> studies. FAO-Penman-Monteith reference crop evapotranspiration rates were estimated for 644 meteorological stations over China for the period 1960-2011 to analyze spatial and temporal attribution variability. Attribution of climatic variables to reference crop evapotranspiration rates was not stable over the study period. While for all of China the contribution of sunshine duration remained relatively stable, the importance of relative humidity increased considerably during the last two <span class="hlt">decades</span>, particularly in winter. Spatially distributed attribution analysis shows that the position of the center of maximum contribution of sunshine duration has shifted from Southeast to Northeast China while in West China the contribution of wind speed has decreased dramatically. In contrast relative humidity has become an important factor in most parts of China. <span class="hlt">Changes</span> in the Asian Monsoon circulation may be responsible for altered patterns of cloudiness and a general decrease of wind speeds over China. The continuously low importance of temperature confirms that global warming does not necessarily lead to rising atmospheric evaporative demand.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://eric.ed.gov/?q=word+AND+2013&pg=2&id=EJ1087329','ERIC'); return false;" href="https://eric.ed.gov/?q=word+AND+2013&pg=2&id=EJ1087329"><span>Has First-Grade Core Reading Program Text Complexity <span class="hlt">Changed</span> across Six <span class="hlt">Decades</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>Fitzgerald, Jill; Elmore, Jeff; Relyea, Jackie Eunjung; Hiebert, Elfrieda H.; Stenner, A. Jackson</p> <p>2016-01-01</p> <p>The purpose of the study was to address possible text complexity shifts across the past six <span class="hlt">decades</span> for a continually best-selling first-grade core reading program. The anthologies of one publisher's seven first-grade core reading programs were examined using computer-based analytics, dating from 1962 to 2013. Variables were Overall Text…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=1724566','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=1724566"><span>Have the attitudes of Australian squash players towards protective eyewear <span class="hlt">changed</span> over the past <span class="hlt">decade</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>Eime, R; Finch, C</p> <p>2002-01-01</p> <p>Objective: To assess indicative trends in the use of protective eyewear by Australian squash players and their attitudes towards its use since 1989. Methods: Data were extracted from three Australian surveys of squash players conducted in 1989, 1995, and 2000. Responses to directly similar attitudinal questions relating to protective eyewear use from each survey were compared. The proportion of players giving each response was calculated for each survey, along with 95% confidence intervals for the differences between the 2000 survey and those from the earlier surveys. Results: Self reported use of protective eyewear ranged from 10.0% in 1989, to 8.6% in 1995, and 18.8% in 2000. However, only 8.9% of the players surveyed in 2000 actually wore appropriate standards approved/polycarbonate lens eyewear. This can be compared with 8.0% and 2.0% of players who reported wearing appropriate polycarbonate lens eyewear in the 1989 and 1995 surveys respectively. Compared with the 1995 survey, significantly more players in 2000 believed that more players should wear protective eyewear (95% confidence interval (CI) for difference 1 to 18). A significantly higher proportion of players also supported the compulsory use of protective eyewear by juniors in 2000 than in both 1989 (95% CI for difference 6 to 24) and 1995 (95% CI for difference 5 to 22). No other attitudes had significantly <span class="hlt">changed</span> over the <span class="hlt">decade</span>. Conclusion: These data suggest that self reported use of protective eyewear has probably increased over the past <span class="hlt">decade</span>. However, many players report wearing inappropriate eyewear. A transition from positive attitudes to appropriate eyewear behaviours is required before mandatory protective eyewear use can be effectively introduced. PMID:12453839</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2007AGUFMGC12A..04A','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2007AGUFMGC12A..04A"><span><span class="hlt">Changes</span> of cloudiness over tropical land during the past few <span class="hlt">decades</span> and its link to global climate <span class="hlt">change</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Arias, P.; Fu, R.; Li, W.</p> <p>2007-12-01</p> <p>Tropical forests play a <span class="hlt">key</span> role in determining the global carbon-climate feedback in the 21st century. <span class="hlt">Changes</span> in rainforest growth and mortality rates, especially in the deep and least perturbed forest areas, have been consistently observed across global tropics in recent years. Understanding the underlying causes of these <span class="hlt">changes</span>, especially their links to the global climate <span class="hlt">change</span>, is especially important in determining the future of the tropical rainforests in the 21st century. Previous studies have mostly focus on the potential influences from elevated atmospheric CO2 and increasing surface temperature. Because the rainforests in wet tropical region is often light limited, we explore whether cloudiness have <span class="hlt">changed</span>, if so, whether it is consistent with that expected from <span class="hlt">changes</span> in forest growth rate. We will report our observational analysis examining the trends in annual average shortwave (SW) downwelling radiation, total cloud cover, and cumulus cover over the tropical land regions and to link them with trends in convective available potencial energy (CAPE). ISCCP data and radiosonde records available from the Department of Atmospheric Sciences of the University of Wyoming (http://www.weather.uwyo.edu/upperair/sounding.html) are used to study the trends. The period for the trend analysis is 1984-2004 for the ISCCP data and 1980-2006 for the radiosondes. The results for the Amazon rainforest region suggest a decreasing trend in total cloud and convective cloud covers, which results in an increase in downwelling SW radiation at the surface. These <span class="hlt">changes</span> of total and convective clouds are consistent with a trend of decreasing CAPE and an elevated Level of Free Convection (LFC) height, as obtained from the radiosondes. All the above mentioned trends are statistically significant based on the Mann-Kendall test with 95% of confidence. These results consistently suggest the downward surface solar radiation has been increasing since 1984, result from a decrease</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016ClDy...47..967A','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016ClDy...47..967A"><span>Inter-<span class="hlt">decadal</span> <span class="hlt">change</span> in El Niño-Southern Oscillation examined with Bjerknes stability index analysis</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>An, Soon-Il; Bong, Hayoung</p> <p>2016-08-01</p> <p>Characteristics of El Niño-Southern Oscillation (ENSO) have <span class="hlt">changed</span> since the late 1970s as it synchronized with the Pacific <span class="hlt">Decadal</span> Oscillation (PDO). In order to investigate the primary feedback process responsible for the interdecadal <span class="hlt">change</span> in ENSO characteristics according to the PDO, using the ocean assimilation data (SODA) and the reanalysis data (NCEP/NCAR), we performed Bjerknes linear stability index (BJ index) analysis of two <span class="hlt">decadal</span> periods: one before the late 1970s (the nPDO period) and the other after the late 1970s (the pPDO period). The BJ index for the pPDO period (-0.07 year-1 for the growth rate of the eastern Pacific SST anomaly) is significantly larger than that for the nPDO period (-0.25 year-1). The larger BJ index value is primarily due to the enhanced zonal advection feedback (ZA; +0.44 year-1), thermocline feedback (TH; +0.33 year-1), and the reduced damping by the mean meridional current (MD; +0.16 year-1). The increases in ZA and TH are mainly attributed to the shoaling of the mean thermocline depth, which increased the sensitivity of the ocean dynamic fields to the wind forcing; and the reduced MD is related to the reduced mean meridional current associated with the weakened trade wind. The enhanced positive feedback is partly compensated by the enhanced thermodynamic damping including the shortwave, sensible heat flux and latent heat flux (collectively, -0.88 year-1). Interestingly, the <span class="hlt">change</span> in air-sea coupling strength from the nPDO to the pPDO period was small. Without the two extreme El Niño events (1982-1983 and 1997-1998) in the pPDO period (pPDO_noBIG), the difference in BJ index between nPDO and pPDO_noBIG periods became smaller (~0.07 year-1), indicating that the two extreme El Niño events largely contribute to the larger ENSO variability of the pPDO period, possibly due to nonlinear feedback processes. Nevertheless, qualitative similarity in each of the feedback and damping components of BJ index exists between the p</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://www.ncbi.nlm.nih.gov/pubmed/25723993','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/25723993"><span>Scaling-up HIV responses with <span class="hlt">key</span> populations in West Africa.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Wheeler, Tisha; Wolf, R Cameron; Kapesa, Laurent; Cheng Surdo, Alison; Dallabetta, Gina</p> <p>2015-03-01</p> <p>Despite <span class="hlt">decades</span> of HIV responses in pockets of West and Central Africa (WCA), the HIV response with <span class="hlt">key</span> populations remains an understudied area. Recently, there has been a proliferation of studies highlighting epidemiologic and behavioral data that challenge attitudes of complacency among donors and country governments uncomfortable in addressing <span class="hlt">key</span> populations. The articles in this series highlight new studies that provide a better understanding of the epidemiologic and structural burden facing <span class="hlt">key</span> populations in the WCA region and how to improve responses through more effective targeting. <span class="hlt">Key</span> populations face pervasive structural barriers including institutional and sexual violence and an intersection of stigma, criminalization, and marginalization as sexual minorities. Despite <span class="hlt">decades</span> of smaller interventions that have shown the importance of integrated services for <span class="hlt">key</span> populations, there remains incongruent provision of outreach or testing or family planning pointing to sustained risk. There remains an incongruent resource provision for <span class="hlt">key</span> populations where they shoulder the burden of HIV and their access to services alone could turn around HIV epidemics within the region. These proximal and distal determinants must be addressed in regional efforts, led by the community, and resourced for scale, targeting those most at risk for the acquisition and transmission of HIV. This special issue builds the knowledge base for the region focusing on interventions that remove barriers to service access including treatment uptake for those living with HIV. Better analysis and use of data for strategic planning are shown to lead to more effective targeting of prevention, care, and HIV treatment programs with <span class="hlt">key</span> populations. These articles further demonstrate the immediate need for comprehensive action to address HIV among <span class="hlt">key</span> populations throughout the WCA region.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/26301625','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/26301625"><span><span class="hlt">Decadally</span> cycling soil carbon is more sensitive to warming than faster-cycling soil carbon.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Lin, Junjie; Zhu, Biao; Cheng, Weixin</p> <p>2015-12-01</p> <p>The response of soil organic carbon (SOC) pools to globally rising surface temperature crucially determines the feedback between climate <span class="hlt">change</span> and the global carbon cycle. However, there is a lack of studies investigating the temperature sensitivity of decomposition for <span class="hlt">decadally</span> cycling SOC which is the main component of total soil carbon stock and the most relevant to global <span class="hlt">change</span>. We tackled this issue using two <span class="hlt">decadally</span> (13) C-labeled soils and a much improved measuring system in a long-term incubation experiment. Results indicated that the temperature sensitivity of decomposition for <span class="hlt">decadally</span> cycling SOC (>23 years in one soil and >55 years in the other soil) was significantly greater than that for faster-cycling SOC (<23 or 55 years) or for the entire SOC stock. Moreover, <span class="hlt">decadally</span> cycling SOC contributed substantially (35-59%) to the total CO2 loss during the 360-day incubation. Overall, these results indicate that the decomposition of <span class="hlt">decadally</span> cycling SOC is highly sensitive to temperature <span class="hlt">change</span>, which will likely make this large SOC stock vulnerable to loss by global warming in the 21st century and beyond. © 2015 John Wiley & Sons Ltd.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFMGC41A0995R','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFMGC41A0995R"><span>Impact of natural variability on the perception of climate <span class="hlt">change</span> for the upcoming <span class="hlt">decades</span>: Analysis of the CanESM2-LE and CESM-LE large ensembles</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Rondeau-Genesse, G.; Braun, M.; Chaumont, D.</p> <p>2017-12-01</p> <p>The pace of climate <span class="hlt">change</span> can have a direct impact on the efforts required to adapt. However, for relatively short time scales, this pace can be masked by natural variability (NV). In some cases, this variability might cause, for a few <span class="hlt">decades</span>, climate <span class="hlt">change</span> to exceed what would be expected from the greenhouse gas (GHG) emissions alone or, to the contrary, it might cause slowdowns or even hiatuses. This phenomenon is difficult to explore using ensembles such as CMIP5, which are composed of multiple climatological models and thus combine both NV and inter-model differences. This study analyses CanESM2-LE and CESM-LE, two state-of-the-art large ensembles (LE) comprised of multiple realizations from a single climatological model and a single GHG emission scenario. We explore the relationship between NV and climate <span class="hlt">change</span> over the next few <span class="hlt">decades</span> in Canada and the United States. Temperature indices, namely the mean annual temperature and the 3-day maximum and minimum temperatures are assessed. Results indicate that under the RCP8.5, temperatures within most of the individual large ensemble members will increase in a roughly linear manner between 2021 and 2060. Nevertheless, in some regions such as parts of Canada and Alaska, there is a 20 to 35% probability that the temperature increase will slow down between 2021 and 2040. Such a slowdown in warming temperatures would provide some leeway for adaptation projects, but this phenomenon is caused by NV alone and, as such, is only temporary. Indeed, members of the large ensembles where a slowdown of warming is found during the 2021-2040 period are two to five times more likely to experience a period of very fast warming in the following <span class="hlt">decades</span>. The opposite scenario, where the <span class="hlt">changes</span> expected by 2050 would occur early because of NV, remains fairly uncommon for the mean annual temperature. For the extreme temperature indices however, this early warming still occurs in 5 to 20% of the large ensemble members. As such</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015BGD....12.6003S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015BGD....12.6003S"><span>Inter-<span class="hlt">decadal</span> <span class="hlt">changes</span> in the intensity of the Oxygen Minimum Zone off Concepción, Chile (~ 36° S) over the last century</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Srain, B.; Pantoja, S.; Sepúlveda, J.; Lange, C. B.; Muñoz, P.; Summons, R. E.; McKay, J.; Salamanca, M.</p> <p>2015-04-01</p> <p>We reconstructed oxygenation <span class="hlt">changes</span> in the Oxygen Minimum Zone of the upwelling ecosystem off Concepción (36° S), Chile, using inorganic and organic proxies in a sediment core covering the last ca. 110 years of sedimentation in this area. Authigenic enrichments of Mo, U and Cd were observed between ca. 1935-1971 CE indicating a prolonged period of more reduced conditions in bottom waters and surface sediments. Significant positive correlations (p < 0.05; Spearman) between redox sensitive metals, algal sterols, biomarkers of anaerobic microorganisms, and archaeal glycerol dialkyl glycerol tetraether indicated a coupling among bottom water oxygen depletion, and increased primary and export production, suggesting that the period with low O2 of ca. 35 years, follows low frequency inter-<span class="hlt">decadal</span> variation of the Pacific <span class="hlt">Decadal</span> Oscillation, which may have resulted in O2 depletion over the entire continental shelf off Concepción. Taken together with the concurrent increase in sedimentary molecular indicators of anaerobic microbes allow us to suggest that the prokaryote community has been influenced by <span class="hlt">changes</span> in oxygenation of the water column.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://eric.ed.gov/?q=public+AND+administration&id=EJ1172057','ERIC'); return false;" href="https://eric.ed.gov/?q=public+AND+administration&id=EJ1172057"><span>Teaching Public Administration: <span class="hlt">Key</span> Themes 1996-2016</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>Fenwick, John</p> <p>2018-01-01</p> <p>In this article, the aim is to explore some of the <span class="hlt">key</span> themes to emerge in the journal during the past two <span class="hlt">decades</span>. Each selected theme will be reviewed in the light of issues raised in particular papers. The aim of this approach is, first, to facilitate reflection upon the contribution of the journal as its subject matter has moved from a concern…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70095755','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70095755"><span><span class="hlt">Key</span> landscape ecology metrics for assessing climate <span class="hlt">change</span> adaptation options: Rate of <span class="hlt">change</span> and patchiness of impacts</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>López-Hoffman, Laura; Breshears, David D.; Allen, Craig D.; Miller, Marc L.</p> <p>2013-01-01</p> <p>Under a <span class="hlt">changing</span> climate, devising strategies to help stakeholders adapt to alterations to ecosystems and their services is of utmost importance. In western North America, diminished snowpack and river flows are causing relatively gradual, homogeneous (system-wide) <span class="hlt">changes</span> in ecosystems and services. In addition, increased climate variability is also accelerating the incidence of abrupt and patchy disturbances such as fires, floods and droughts. This paper posits that two <span class="hlt">key</span> variables often considered in landscape ecology—the rate of <span class="hlt">change</span> and the degree of patchiness of change—can aid in developing climate <span class="hlt">change</span> adaptation strategies. We use two examples from the “borderland” region of the southwestern United States and northwestern Mexico. In piñon-juniper woodland die-offs that occurred in the southwestern United States during the 2000s, ecosystem services suddenly crashed in some parts of the system while remaining unaffected in other locations. The precise timing and location of die-offs was uncertain. On the other hand, slower, homogeneous <span class="hlt">change</span>, such as the expected declines in water supply to the Colorado River delta, will likely impact the entire ecosystem, with ecosystem services everywhere in the delta subject to alteration, and all users likely exposed. The rapidity and spatial heterogeneity of faster, patchy climate <span class="hlt">change</span> exemplified by tree die-off suggests that decision-makers and local stakeholders would be wise to operate under a Rawlsian “veil of ignorance,” and implement adaptation strategies that allow ecosystem service users to equitably share the risk of sudden loss of ecosystem services before actual ecosystem <span class="hlt">changes</span> occur. On the other hand, in the case of slower, homogeneous, system-wide impacts to ecosystem services as exemplified by the Colorado River delta, adaptation strategies can be implemented after the <span class="hlt">changes</span> begin, but will require a fundamental rethinking of how ecosystems and services are used and valued. In</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5323239','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5323239"><span>A <span class="hlt">Decade</span> of <span class="hlt">Change</span>: Measuring the Extent, Depth and Severity of Food Insecurity</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>2016-01-01</p> <p>Rates of food insecurity in the US have been rising since 2000 spiking with the onset of the Great Recession in 2008, and have remained essentially unchanged since then despite improvements in the economy. The present study employed a series of indices adapted from the poverty literature to examine the depth and severity of food insecurity across the <span class="hlt">decade</span> by race and ethnicity among low-income households with and without children. The most rapid increases in the depth and severity of food insecurity were found among low-income households without children. Non-Hispanic White households with and without children had lower prevalence rates but steeper increases in the depth and severity of food insecurity throughout the <span class="hlt">decade</span>. Non-Hispanic Black households with and without children were at the most disadvantaged among low-income populations. PMID:28239245</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70187427','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70187427"><span>Designing ecological climate <span class="hlt">change</span> impact assessments to reflect <span class="hlt">key</span> climatic drivers</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Sofaer, Helen R.; Barsugli, Joseph J.; Jarnevich, Catherine S.; Abatzoglou, John T.; Talbert, Marian; Miller, Brian W.; Morisette, Jeffrey T.</p> <p>2017-01-01</p> <p>Identifying the climatic drivers of an ecological system is a <span class="hlt">key</span> step in assessing its vulnerability to climate <span class="hlt">change</span>. The climatic dimensions to which a species or system is most sensitive – such as means or extremes – can guide methodological decisions for projections of ecological impacts and vulnerabilities. However, scientific workflows for combining climate projections with ecological models have received little explicit attention. We review Global Climate Model (GCM) performance along different dimensions of <span class="hlt">change</span> and compare frameworks for integrating GCM output into ecological models. In systems sensitive to climatological means, it is straightforward to base ecological impact assessments on mean projected <span class="hlt">changes</span> from several GCMs. Ecological systems sensitive to climatic extremes may benefit from what we term the ‘model space’ approach: a comparison of ecological projections based on simulated climate from historical and future time periods. This approach leverages the experimental framework used in climate modeling, in which historical climate simulations serve as controls for future projections. Moreover, it can capture projected <span class="hlt">changes</span> in the intensity and frequency of climatic extremes, rather than assuming that future means will determine future extremes. Given the recent emphasis on the ecological impacts of climatic extremes, the strategies we describe will be applicable across species and systems. We also highlight practical considerations for the selection of climate models and data products, emphasizing that the spatial resolution of the climate <span class="hlt">change</span> signal is generally coarser than the grid cell size of downscaled climate model output. Our review illustrates how an understanding of how climate model outputs are derived and downscaled can improve the selection and application of climatic data used in ecological modeling.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/28173628','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/28173628"><span>Designing ecological climate <span class="hlt">change</span> impact assessments to reflect <span class="hlt">key</span> climatic drivers.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Sofaer, Helen R; Barsugli, Joseph J; Jarnevich, Catherine S; Abatzoglou, John T; Talbert, Marian K; Miller, Brian W; Morisette, Jeffrey T</p> <p>2017-07-01</p> <p>Identifying the climatic drivers of an ecological system is a <span class="hlt">key</span> step in assessing its vulnerability to climate <span class="hlt">change</span>. The climatic dimensions to which a species or system is most sensitive - such as means or extremes - can guide methodological decisions for projections of ecological impacts and vulnerabilities. However, scientific workflows for combining climate projections with ecological models have received little explicit attention. We review Global Climate Model (GCM) performance along different dimensions of <span class="hlt">change</span> and compare frameworks for integrating GCM output into ecological models. In systems sensitive to climatological means, it is straightforward to base ecological impact assessments on mean projected <span class="hlt">changes</span> from several GCMs. Ecological systems sensitive to climatic extremes may benefit from what we term the 'model space' approach: a comparison of ecological projections based on simulated climate from historical and future time periods. This approach leverages the experimental framework used in climate modeling, in which historical climate simulations serve as controls for future projections. Moreover, it can capture projected <span class="hlt">changes</span> in the intensity and frequency of climatic extremes, rather than assuming that future means will determine future extremes. Given the recent emphasis on the ecological impacts of climatic extremes, the strategies we describe will be applicable across species and systems. We also highlight practical considerations for the selection of climate models and data products, emphasizing that the spatial resolution of the climate <span class="hlt">change</span> signal is generally coarser than the grid cell size of downscaled climate model output. Our review illustrates how an understanding of how climate model outputs are derived and downscaled can improve the selection and application of climatic data used in ecological modeling. © 2017 John Wiley & Sons Ltd.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012AGUFMGC13E..06G','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012AGUFMGC13E..06G"><span>Assessment of Climate <span class="hlt">Change</span> in the Southwest United States: <span class="hlt">Key</span> Findings</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Garfin, G. M.</p> <p>2012-12-01</p> <p>The Assessment of Climate <span class="hlt">Change</span> in the Southwest United States, is a technical input to the National Climate Assessment. The 121-author report summarizes knowledge about climate <span class="hlt">change</span> and its impacts across Arizona, California, Colorado, Nevada, New Mexico, and Utah. The report looks at links between climate and natural resources, vulnerabilities to climate variability and <span class="hlt">change</span> across the region and along the U.S.-Mexico border, and adaptation and mitigation choices for addressing future <span class="hlt">changes</span>. The period since 1950 has been warmer than any period of comparable length in the last 600 years. Droughts of the past 2,000 years have exceeded the most severe and sustained drought during 1901-2010. In the last <span class="hlt">decade</span>, flows in the major river basins of the Southwest have been lower than their 20th century averages; many snowmelt-fed streams in the region exhibited earlier snowmelt and earlier center of mass of annual streamflows. Climate models project continued temperature increases, with longer and hotter summer heat waves. Average precipitation is projected to decrease in the southern part of the region. Reduced streamflows are projected for the Rio Grande, Colorado, and San Joaquin rivers. More frequent and intense winter flooding is projected for the western Sierra Nevada, whereas Colorado Front Range summer flooding is projected to increase. Observed ecosystems impacts include <span class="hlt">changes</span> in phenology, widespread forest disturbance due to the confluence of drought, increased temperatures, and <span class="hlt">changes</span> to insect life cycles. Area burned by wildfire is projected to increase in most of the Southwest. Plant and animal species' distributions will be affected by climate <span class="hlt">change</span>, and studies show that observed climate <span class="hlt">changes</span> are strongly associated with observed <span class="hlt">changes</span> in species' distributions. California coastal ecosystems will be affected by a combination of ocean warming, reduced oxygen content, sea level rise and ocean acidification. When west coast sea levels are</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFMGC32B..01O','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFMGC32B..01O"><span>Increasing Megadrought Risk at the Intersection of <span class="hlt">Decadal</span> to Centennial Variability and Climate <span class="hlt">Change</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Overpeck, J. T.; Parsons, L. A.; Loope, G. R.; Ault, T.; Cole, J. E.; Otto-Bliesner, B. L.; Buckle, N.; Stevenson, S.; Fasullo, J.</p> <p>2016-12-01</p> <p>Even more than the 1930's U.S. Dust Bowl Drought, the 20th century Sahel drought stands out as the most unprecedented drought of the instrumental era, in part because it extended over multiple <span class="hlt">decades</span>. Paleoclimatic evidence makes it clear that this Sahel drought was nonetheless not really unprecedented - droughts many <span class="hlt">decades</span> long have occurred in sub-Saharan Africa regularly over the last several thousand years, and these constitute what is now increasingly referred to as "megadrought." Paleoclimatic evidence also makes it clear that all drought-prone semi-arid and arid regions of the globe, including southwestern North America, southeastern Australia, and the Mediterranean/Middle Eastern region likely experienced multiple such multidecadal megadroughts in recent pre-Anthropocene Earth history. In other regions of the globe, including parts of South Asia and Amazonia, short but devastating droughts of the last 50-150 years, were also eclipsed in recent Earth history by much more serious megadrought, although these megadroughts were shorter than the multidecadal droughts of Africa or SW North America. In the past, megadroughts have occurred for reasons that are increasingly well understood in terms of ocean-atmosphere dynamics that led to unusually persistent precipitation deficits. Many of these same dynamics are well simulated in state-of-the-art Earth System Models, and yet comparisons between simulated and observed paleohydroclimatic variability suggests the models generally underestimate the risk of megadrought. Paleohydroclimatic records in some cases overestimate drought persistence, but there appear to be other issues at play that need to be better understood and simulated: positive land-atmosphere feedbacks, overly energetic interannual (i.e., ENSO) modes of variability, and insufficient internal multidecadal to centennial coupled climate system variability. Taking these issues and the impact of anthropogenic climate <span class="hlt">change</span> into account means that the</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/26562303','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/26562303"><span><span class="hlt">Decadal</span> Trend in Agricultural Abandonment and Woodland Expansion in an Agro-Pastoral Transition Band in Northern China.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Wang, Chao; Gao, Qiong; Wang, Xian; Yu, Mei</p> <p>2015-01-01</p> <p>Land use land cover (LULC) <span class="hlt">changes</span> frequently in ecotones due to the large climate and soil gradients, and complex landscape composition and configuration. Accurate mapping of LULC <span class="hlt">changes</span> in ecotones is of great importance for assessment of ecosystem functions/services and policy-decision support. <span class="hlt">Decadal</span> or sub-<span class="hlt">decadal</span> mapping of LULC provides scenarios for modeling biogeochemical processes and their feedbacks to climate, and evaluating effectiveness of land-use policies, e.g. forest conversion. However, it remains a great challenge to produce reliable LULC maps in moderate resolution and to evaluate their uncertainties over large areas with complex landscapes. In this study we developed a robust LULC classification system using multiple classifiers based on MODIS (Moderate Resolution Imaging Spectroradiometer) data and posterior data fusion. Not only does the system create LULC maps with high statistical accuracy, but also it provides pixel-level uncertainties that are essential for subsequent analyses and applications. We applied the classification system to the Agro-pasture transition band in northern China (APTBNC) to detect the <span class="hlt">decadal</span> <span class="hlt">changes</span> in LULC during 2003-2013 and evaluated the effectiveness of the implementation of major <span class="hlt">Key</span> Forestry Programs (KFPs). In our study, the random forest (RF), support vector machine (SVM), and weighted k-nearest neighbors (WKNN) classifiers outperformed the artificial neural networks (ANN) and naive Bayes (NB) in terms of high classification accuracy and low sensitivity to training sample size. The Bayesian-average data fusion based on the results of RF, SVM, and WKNN achieved the 87.5% Kappa statistics, higher than any individual classifiers and the majority-vote integration. The pixel-level uncertainty map agreed with the traditional accuracy assessment. However, it conveys spatial variation of uncertainty. Specifically, it pinpoints the southwestern area of APTBNC has higher uncertainty than other part of the region</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFMOS23D..01H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFMOS23D..01H"><span>Multi-<span class="hlt">decadal</span> trend and space-time variability of sea level over the Indian Ocean since the 1950s: impact of <span class="hlt">decadal</span> climate modes</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Han, W.; Stammer, D.; Meehl, G. A.; Hu, A.; Sienz, F.</p> <p>2016-12-01</p> <p>Sea level varies on <span class="hlt">decadal</span> and multi-<span class="hlt">decadal</span> timescales over the Indian Ocean. The variations are not spatially uniform, and can deviate considerably from the global mean sea level rise (SLR) due to various geophysical processes. One of these processes is the <span class="hlt">change</span> of ocean circulation, which can be partly attributed to natural internal modes of climate variability. Over the Indian Ocean, the most influential climate modes on <span class="hlt">decadal</span> and multi-<span class="hlt">decadal</span> timescales are the Interdecadal Pacific Oscillation (IPO) and <span class="hlt">decadal</span> variability of the Indian Ocean dipole (IOD). Here, we first analyze observational datasets to investigate the impacts of IPO and IOD on spatial patterns of <span class="hlt">decadal</span> and interdecadal (hereafter decal) sea level variability & multi-<span class="hlt">decadal</span> trend over the Indian Ocean since the 1950s, using a new statistical approach of Bayesian Dynamical Linear regression Model (DLM). The Bayesian DLM overcomes the limitation of "time-constant (static)" regression coefficients in conventional multiple linear regression model, by allowing the coefficients to vary with time and therefore measuring "time-evolving (dynamical)" relationship between climate modes and sea level. For the multi-<span class="hlt">decadal</span> sea level trend since the 1950s, our results show that climate modes and non-climate modes (the part that cannot be explained by climate modes) have comparable contributions in magnitudes but with different spatial patterns, with each dominating different regions of the Indian Ocean. For <span class="hlt">decadal</span> variability, climate modes are the major contributors for sea level variations over most region of the tropical Indian Ocean. The relative importance of IPO and <span class="hlt">decadal</span> variability of IOD, however, varies spatially. For example, while IOD <span class="hlt">decadal</span> variability dominates IPO in the eastern equatorial basin (85E-100E, 5S-5N), IPO dominates IOD in causing sea level variations in the tropical southwest Indian Ocean (45E-65E, 12S-2S). To help decipher the possible contribution of external</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014EGUGA..1611711W','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014EGUGA..1611711W"><span>Influence of climate variability versus <span class="hlt">change</span> at multi-<span class="hlt">decadal</span> time scales on hydrological extremes</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Willems, Patrick</p> <p>2014-05-01</p> <p>Recent studies have shown that rainfall and hydrological extremes do not randomly occur in time, but are subject to multidecadal oscillations. In addition to these oscillations, there are temporal trends due to climate <span class="hlt">change</span>. Design statistics, such as intensity-duration-frequency (IDF) for extreme rainfall or flow-duration-frequency (QDF) relationships, are affected by both types of temporal <span class="hlt">changes</span> (short term and long term). This presentation discusses these <span class="hlt">changes</span>, how they influence water engineering design and decision making, and how this influence can be assessed and taken into account in practice. The multidecadal oscillations in rainfall and hydrological extremes were studied based on a technique for the identification and analysis of <span class="hlt">changes</span> in extreme quantiles. The statistical significance of the oscillations was evaluated by means of a non-parametric bootstrapping method. Oscillations in large scale atmospheric circulation were identified as the main drivers for the temporal oscillations in rainfall and hydrological extremes. They also explain why spatial phase shifts (e.g. north-south variations in Europe) exist between the oscillation highs and lows. Next to the multidecadal climate oscillations, several stations show trends during the most recent <span class="hlt">decades</span>, which may be attributed to climate <span class="hlt">change</span> as a result of anthropogenic global warming. Such attribution to anthropogenic global warming is, however, uncertain. It can be done based on simulation results with climate models, but it is shown that the climate model results are too uncertain to enable a clear attribution. Water engineering design statistics, such as extreme rainfall IDF or peak or low flow QDF statistics, obviously are influenced by these temporal variations (oscillations, trends). It is shown in the paper, based on the Brussels 10-minutes rainfall data, that rainfall design values may be about 20% biased or different when based on short rainfall series of 10 to 15 years length, and</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://files.eric.ed.gov/fulltext/EJ1138539.pdf','ERIC'); return false;" href="http://files.eric.ed.gov/fulltext/EJ1138539.pdf"><span>Investigating <span class="hlt">Changing</span> in Social Studies Textbooks of Public Review (Basic Fourth and Fifth) Based on the Emphasis on Critical Thinking Skills Facione in the Last Three <span class="hlt">Decades</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>Aghababaeian, Parinaz; Moghaddam, Shams Aldin Hashemi; Nateghi, Faezeh; Faghihi, Alireza</p> <p>2017-01-01</p> <p>This study investigated the <span class="hlt">changes</span> in public school social studies textbooks in general period of Iran (fourth and fifth grades) based on the emphasis on Facione critical thinking skills in the past three <span class="hlt">decades</span>. In this study, content analysis of qualitative and quantitative methods was used to evaluate <span class="hlt">changes</span> in textbook. For this purpose,…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://files.eric.ed.gov/fulltext/ED270116.pdf','ERIC'); return false;" href="http://files.eric.ed.gov/fulltext/ED270116.pdf"><span><span class="hlt">Key</span> Issues in the Networking Field Today. Proceedings of the Library of Congress Network Advisory Committee Meeting (Washington, DC, May 6-8, 1985). Network Planning Paper No. 12.</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>Library of Congress, Washington, DC. Network Development Office.</p> <p></p> <p>The May 1985 program session of the Library of Congress Network Advisory Committee focused on the identification of <span class="hlt">key</span> issues in the networking field. Presentations included discussions of major network developments in the last two <span class="hlt">decades</span>, the <span class="hlt">changing</span> network players, the impact of technology on networks, and library networks and the law. The…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016EaFut...4..549K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016EaFut...4..549K"><span>Solar geoengineering could substantially reduce climate risks—A research hypothesis for the next <span class="hlt">decade</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Keith, David W.; Irvine, Peter J.</p> <p>2016-11-01</p> <p>We offer a hypothesis that if solar geoengineering (SG) were deployed to offset half of the increase in global-mean temperature from the date of deployment using a technology and deployment method chosen to approximate a reduction in the solar constant then, over the 21st century, it would (a) substantially reduce the global aggregate risks of climate <span class="hlt">change</span>, (b) without making any country worse off, and (c) with the aggregate risks from side-effects being small in comparison to the reduction in climate risks. We do not set out to demonstrate this hypothesis; rather we propose it with the goal of stimulating a strategic engagement of the SG research community with policy-relevant questions. We elaborate seven sub-hypotheses on the effects of our scenario for <span class="hlt">key</span> risks of climate <span class="hlt">change</span> that could be assessed in future modeling work. As an example, we provide a defence of one of our sub-hypotheses, that our scenario of SG would reduce the risk of drought in dry regions, but also identify issues that may undermine this sub-hypothesis and how future work could resolve this question. SG cannot substitute for emissions mitigation but it may be a useful supplement. It is our hope that scientific and technical research over the next <span class="hlt">decade</span> focuses more closely on well-articulated variants of the <span class="hlt">key</span> policy-relevant question: could SG be designed and deployed in such a way that it could substantially and equitably reduce climate risks?</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/28811521','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/28811521"><span><span class="hlt">Decadal</span> trends in Red Sea maximum surface temperature.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Chaidez, V; Dreano, D; Agusti, S; Duarte, C M; Hoteit, I</p> <p>2017-08-15</p> <p>Ocean warming is a major consequence of climate <span class="hlt">change</span>, with the surface of the ocean having warmed by 0.11 °C <span class="hlt">decade</span> -1 over the last 50 years and is estimated to continue to warm by an additional 0.6 - 2.0 °C before the end of the century 1 . However, there is considerable variability in the rates experienced by different ocean regions, so understanding regional trends is important to inform on possible stresses for marine organisms, particularly in warm seas where organisms may be already operating in the high end of their thermal tolerance. Although the Red Sea is one of the warmest ecosystems on earth, its historical warming trends and thermal evolution remain largely understudied. We characterized the Red Sea's thermal regimes at the basin scale, with a focus on the spatial distribution and <span class="hlt">changes</span> over time of sea surface temperature maxima, using remotely sensed sea surface temperature data from 1982 - 2015. The overall rate of warming for the Red Sea is 0.17 ± 0.07 °C <span class="hlt">decade</span> -1 , while the northern Red Sea is warming between 0.40 and 0.45 °C <span class="hlt">decade</span> -1 , all exceeding the global rate. Our findings show that the Red Sea is fast warming, which may in the future challenge its organisms and communities.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018ACP....18.2035M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018ACP....18.2035M"><span>Predicting <span class="hlt">decadal</span> trends in cloud droplet number concentration using reanalysis and satellite data</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>McCoy, Daniel T.; Bender, Frida A.-M.; Grosvenor, Daniel P.; Mohrmann, Johannes K.; Hartmann, Dennis L.; Wood, Robert; Field, Paul R.</p> <p>2018-02-01</p> <p>Cloud droplet number concentration (CDNC) is the <span class="hlt">key</span> state variable that moderates the relationship between aerosol and the radiative forcing arising from aerosol-cloud interactions. Uncertainty related to the effect of anthropogenic aerosol on cloud properties represents the largest uncertainty in total anthropogenic radiative forcing. Here we show that regionally averaged time series of the Moderate-Resolution Imaging Spectroradiometer (MODIS) observed CDNC of low, liquid-topped clouds is well predicted by the MERRA2 reanalysis near-surface sulfate mass concentration over <span class="hlt">decadal</span> timescales. A multiple linear regression between MERRA2 reanalyses masses of sulfate (SO4), black carbon (BC), organic carbon (OC), sea salt (SS), and dust (DU) shows that CDNC across many different regimes can be reproduced by a simple power-law fit to near-surface SO4, with smaller contributions from BC, OC, SS, and DU. This confirms previous work using a less sophisticated retrieval of CDNC on monthly timescales. The analysis is supported by an examination of remotely sensed sulfur dioxide (SO2) over maritime volcanoes and the east coasts of North America and Asia, revealing that maritime CDNC responds to <span class="hlt">changes</span> in SO2 as observed by the ozone monitoring instrument (OMI). This investigation of aerosol reanalysis and top-down remote-sensing observations reveals that emission controls in Asia and North America have decreased CDNC in their maritime outflow on a <span class="hlt">decadal</span> timescale.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFM.A21G2226J','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFM.A21G2226J"><span>Quantifying the <span class="hlt">decadal</span> <span class="hlt">changes</span> of PM2.5 over New York through a combination of satellite, model and in-situ measurements</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Jin, X.; Fiore, A. M.; Curci, G.; Lyapustin, A.; Wang, Y.; Civerolo, K.; Ku, M.; van Donkelaar, A.; Martin, R.</p> <p>2017-12-01</p> <p>Ambient exposure to fine particulate matter (PM2.5) is one of the top global health concerns. Efforts have been made to regulate PM2.5 precursor emissions across the U.S.A, which are expected to mitigate the air pollution related health impacts. However, quantifying the health outcomes from emission controls requires robust estimates of PM2.5 exposures that accurately describe the spatial and temporal variability of PM2.5. Satellite remote sensing offers the potential to fill the gaps of the sparse, limited sampling of in situ measurement networks and is increasingly being used in health assessments. We provide new estimates of PM2.5 over New York State with 1 km spatial resolution that use Multi-Angle Implementation of Atmospheric Correction (MAIAC) AOD and a regional air quality model (CMAQ) to estimate the AOD-PM2.5 scaling factors. Next, we evaluate three major sources of uncertainties of satellite-derived PM2.5 data and their impacts on the derived <span class="hlt">decadal</span> <span class="hlt">changes</span>: 1) satellite retrieval of AOD, 2) optical properties of the particles, 3) relationships between the aerosol burden in the planetary boundary layer and full atmospheric column. Finally, we analyze the <span class="hlt">decadal</span> <span class="hlt">changes</span> of PM2.5 over New York State using the newly developed PM2.5 data, alongside four other PM2.5 estimates including satellite-derived PM2.5 developed by van Donkelaar et al. (2015), statistical land use regression developed by Beckerman et al. (2013), CMAQ simulations, and a Bayesian fusion of CMAQ and ground-based measurements. By evaluating the <span class="hlt">decadal</span> <span class="hlt">changes</span> of PM2.5 from multiple datasets over areas with dense (e.g. New York City area) and sparse ground-based measurements (e.g. upstate New York), we evaluate the extent to which satellite remote sensing could help better quantify the health outcomes of emission controls. References: Beckerman et al., (2013), A Hybrid Approach to Estimating National Scale Spatiotemporal Variability of PM2.5 in the Contiguous United States, Environ. Sci</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('http://adsabs.harvard.edu/abs/2016Geomo.257...75M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016Geomo.257...75M"><span>Multi-<span class="hlt">decadal</span> shoreline <span class="hlt">changes</span> on Takú Atoll, Papua New Guinea: Observational evidence of early reef island recovery after the impact of storm waves</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Mann, Thomas; Westphal, Hildegard</p> <p>2016-03-01</p> <p>Hurricanes, tropical cyclones and other high-magnitude events are important steering mechanisms in the geomorphic development of coral reef islands. Sandy reef islands located outside the storm belts are strongly sensitive to the impact of occasional high-magnitude events and show abrupt, commonly erosive geomorphic <span class="hlt">change</span> in response to such events. Based on the interpretation of remote sensing data, it is well known that the process of landform recovery might take several <span class="hlt">decades</span> or even longer. However, despite the increasing amount of scientific attention towards short- and long-term island dynamics, the lack of data and models often prevent a robust analysis of the timing and nature of recovery initiation. Here we show how natural island recovery starts immediately after the impact of a high-magnitude event. We analyze multi-temporal shoreline <span class="hlt">changes</span> on Takú Atoll, Papua New Guinea and combine our findings with a unique set of published field observations (Smithers and Hoeke, 2014). Trends of shoreline <span class="hlt">change</span> since 1943 and <span class="hlt">changes</span> in planform island area indicate a long-term accretionary mode for most islands. Apparent shoreline instability is detected for the last <span class="hlt">decade</span> of analysis, however this can be explained by the impact of storm waves in December 2008 that (temporarily?) masked the long-term trend. The transition from negative to positive rates of <span class="hlt">change</span> in the aftermath of this storm event is indicative of inherent negative feedback processes that counteract short-term <span class="hlt">changes</span> in energy input and represent the initiation of island recovery. Collectively, our results support the concept of dynamic rather than static reef islands and clearly demonstrate how short-term processes can influence interpretations of medium-term <span class="hlt">change</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/28694674','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/28694674"><span>Mechanisms of chronic pain - <span class="hlt">key</span> considerations for appropriate physical therapy management.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Courtney, Carol A; Fernández-de-Las-Peñas, César; Bond, Samantha</p> <p>2017-07-01</p> <p>In last <span class="hlt">decades</span>, knowledge of nociceptive pain mechanisms has expanded rapidly. The use of quantitative sensory testing has provided evidence that peripheral and central sensitization mechanisms play a relevant role in localized and widespread chronic pain syndromes. In fact, almost any patient suffering with a chronic pain condition will demonstrate impairments in the central nervous system. In addition, it is accepted that pain is associated with different types of trigger factors including social, physiological, and psychological. This rational has provoked a <span class="hlt">change</span> in the understanding of potential mechanisms of manual therapies, <span class="hlt">changing</span> from a biomechanical/medical viewpoint, to a neurophysiological/nociceptive viewpoint. Therefore, interventions for patients with chronic pain should be applied based on current knowledge of nociceptive mechanisms since determining potential drivers of the sensitization process is critical for effective management. The current paper reviews mechanisms of chronic pain from a clinical and neurophysiological point of view and summarizes <span class="hlt">key</span> messages for clinicians for proper management of individuals with chronic pain.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFMPP14A..06C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFMPP14A..06C"><span>Spatiotemporal Patterns of Hydrological <span class="hlt">Changes</span> During the Younger Dryas Onset from <span class="hlt">Decadally</span>-Resolved Lacustrine Biomarker Records: a W-E European Transect</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Collins, J.; Aichner, B.; Engels, S.; Lane, C.; Maas, D.; Neugebauer, I.; Ott, F.; Slowinski, M. M.; Wulf, S.; Plessen, B.; Brauer, A.; Sachse, D.</p> <p>2016-12-01</p> <p>Future projections of European hydroclimate <span class="hlt">change</span> remain uncertain, highlighting the need for an improved understanding of past abrupt European hydroclimate <span class="hlt">change</span>, particularly in terms of identifying vulnerable regions. However, most existing continental paleohydrological records are not of sufficiently high resolution and/or sufficiently well dated for the assessment of leads and lags across the European continent and with the Greenland ice cores. To better understand mechanisms and feedbacks of hydrological <span class="hlt">changes</span> during the last major abrupt climate <span class="hlt">change</span>, the Younger Dryas (YD) cold period, we measured biomarker hydrogen isotopes (δD values) from terrestrial and aquatic sources on four high-resolution lacustrine sediment profiles. The sites span a 900km W-E transect from western Germany to eastern Poland and include: Meerfelder Maar, western Germany [MFM]; Hämelsee, northern-central Germany [HÄM]; Rehwiese, eastern Germany [RW]; Trzechowskie, central Poland [TRZ]. These sediments are annually laminated and contain common tephra layers, permitting a direct comparison of each site and allowing the identification of leads and lags in the response of the hydrological cycle to YD cooling on <span class="hlt">decadal</span> timescales. We observed a decrease in biomarker δD values, likely reflecting cooling, that coincided with the onset of Greenland Stadial 1 in the NGRIP ice core at 12,846 years BP in the western European sites, with a progressive lag of several <span class="hlt">decades</span> in the more easterly sites. Furthermore, we observed that the onset of aridification at all four sites occurred later but at roughly at the same time, coinciding with the biostratigraphically-defined onset of the YD at 12,679. A decrease in the magnitude of <span class="hlt">changes</span> in biomarker δD values and aridification from W to E suggests a less strong aridification in eastern Europe. Our results suggest that hydrological <span class="hlt">changes</span> at the onset of the YD were not uniform and were strongest and most abrupt in western Europe</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/21941276','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/21941276"><span>A <span class="hlt">decade</span> of molecular cell biology: achievements and challenges.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Akhtar, Asifa; Fuchs, Elaine; Mitchison, Tim; Shaw, Reuben J; St Johnston, Daniel; Strasser, Andreas; Taylor, Susan; Walczak, Claire; Zerial, Marino</p> <p>2011-09-23</p> <p>Nature Reviews Molecular Cell Biology celebrated its 10-year anniversary during this past year with a series of specially commissioned articles. To complement this, here we have asked researchers from across the field for their insights into how molecular cell biology research has evolved during this past <span class="hlt">decade</span>, the <span class="hlt">key</span> concepts that have emerged and the most promising interfaces that have developed. Their comments highlight the broad impact that particular advances have had, some of the basic understanding that we still require, and the collaborative approaches that will be essential for driving the field forward.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/19037313','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/19037313"><span>Agulhas leakage dynamics affects <span class="hlt">decadal</span> variability in Atlantic overturning circulation.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Biastoch, A; Böning, C W; Lutjeharms, J R E</p> <p>2008-11-27</p> <p>Predicting the evolution of climate over <span class="hlt">decadal</span> timescales requires a quantitative understanding of the dynamics that govern the meridional overturning circulation (MOC). Comprehensive ocean measurement programmes aiming to monitor MOC variations have been established in the subtropical North Atlantic (RAPID, at latitude 26.5 degrees N, and MOVE, at latitude 16 degrees N) and show strong variability on intraseasonal to interannual timescales. Observational evidence of longer-term <span class="hlt">changes</span> in MOC transport remains scarce, owing to infrequent sampling of transoceanic sections over past <span class="hlt">decades</span>. Inferences based on long-term sea surface temperature records, however, supported by model simulations, suggest a variability with an amplitude of +/-1.5-3 Sv (1 Sv = 10(6) m(3) s(-1)) on <span class="hlt">decadal</span> timescales in the subtropics. Such variability has been attributed to variations of deep water formation in the sub-arctic Atlantic, particularly the renewal rate of Labrador Sea Water. Here we present results from a model simulation that suggest an additional influence on <span class="hlt">decadal</span> MOC variability having a Southern Hemisphere origin: dynamic signals originating in the Agulhas leakage region at the southern tip of Africa. These contribute a MOC signal in the tropical and subtropical North Atlantic that is of the same order of magnitude as the northern source. A complete rationalization of observed MOC <span class="hlt">changes</span> therefore also requires consideration of signals arriving from the south.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018ClDy..tmp.2381G','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018ClDy..tmp.2381G"><span><span class="hlt">Decadal</span> modulation of the relationship between intraseasonal tropical variability and ENSO</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Gushchina, Daria; Dewitte, Boris</p> <p>2018-05-01</p> <p>The El Niño Southern Oscillation (ENSO) amplitude is modulated at <span class="hlt">decadal</span> timescales, which, over the last <span class="hlt">decades</span>, has been related to the low-frequency <span class="hlt">changes</span> in the frequency of occurrence of the two types of El Niño events, that is the Eastern Pacific (EP) and Central Pacific (CP) El Niños. Meanwhile ENSO is tightly linked to the intraseasonal tropical variability (ITV) that is generally enhanced prior to El Niño development and can act as a trigger of the event. Here we revisit the ITV/ENSO relationship taking into account <span class="hlt">changes</span> in ENSO properties over the last six <span class="hlt">decades</span>. The focus is on two main components of ITV, the Madden-Julian Oscillation (MJO) and convectively coupled equatorial Rossby waves (ER). We show that the ITV/ENSO relationship exhibits a <span class="hlt">decadal</span> modulation that is not related in a straight-forward manner to the <span class="hlt">change</span> in occurrence of El Niño types and Pacific <span class="hlt">decadal</span> modes. While enhanced MJO activity associated to EP El Niño development mostly took place over the period 1985-2000, the ER activity is enhanced prior to El Niño development over the whole period with a tendency to relate more to CP El Niño than to EP El Niño. In particular the relationship between ER activity and ENSO was particularly strong for the period 2000-2015, which results in a significant positive long-term trend of the predictive value of ER activity. The statistics of the MJO and ER activity is consistent with the hypothesis that they can be considered a state-dependent noise for ENSO linked to distinct lower frequency climate modes.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015AGUFMPA23A2186G','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015AGUFMPA23A2186G"><span>A critical reflection of a <span class="hlt">decade</span> of urbanization and global environmental <span class="hlt">change</span> research and science coordination</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Griffith, C.</p> <p>2015-12-01</p> <p>The Urbanization and Global Environmental <span class="hlt">Change</span> (UGEC) Project was established in 2005 when attention to the bidirectional interactions of urbanization and GEC issues and the associated system responses was very new and the community of UGEC researchers very small. Much of the urban scholarship used specific disciplinary lenses through which to understand the city, e.g., in terms of demographics and population growth, ecology of cities or economics of cities. Over the last <span class="hlt">decade</span> new analytical lenses have revealed much more about how cities function, the underlying socio-economic and ecological processes that drive urbanization, their dynamic and teleconnected nature, and other bio-physical interactions within the Earth system. Furthermore, it is within the cities that the impacts of current and projected urbanization and environmental <span class="hlt">changes</span> are felt, but also where action is taken and where great potential for intervention of urbanization trajectories exists towards creating more livable urban futures. A former IHDP core project, now Future Earth project, UGEC is in its sunset/synthesis phase and exploring future directions. This presentation will: Give an brief overview of UGEC evolution over the course of the last <span class="hlt">decade</span> not only in terms of the science, but also the institution Present preliminary results from a critical analysis of UGEC's ten year role as a GEC research coordination project including its impact, strengths and weaknesses Make the case for greater interdisciplinarity (particularly across the physical sciences and humanities) and involvement of other stakeholders (private sector and decisionmakers) in future urbanization and environmental research, as 'urban' is a crosscutting issue that has both global to local scale implications Present work that UGEC is leading, which is to advance an urban agenda within the new Future Earth initiative as part of the recently awarded Cluster Activity 'Livable Urban Futures', as an example of research</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2007AGUSM.A51D..07W','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2007AGUSM.A51D..07W"><span><span class="hlt">Decadal</span> Variations in Surface Solar Radiation</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Wild, M.</p> <p>2007-05-01</p> <p>Satellite estimates provide some information on the amount of solar radiation absorbed by the planet back to the 1980s. The amount of solar radiation reaching the Earth surface can be traced further back in time, untill the 1960s at widespread locations and into the first half of the 20th Century at selected sites. These surface sites suggest significant <span class="hlt">decadal</span> variations in solar radiation incident at the surface, with indication for a widespread dimming from the 1960s up to the mid 1980s, and a recovery thereafter. Indications for <span class="hlt">changes</span> in surface solar radiation may also be seen in observatinal records of diurnal temperature range, which provide a better global coverage than the radiation measurrements. Trends in diurnal temperature ranges over global land surfaces show, after <span class="hlt">decades</span> of decline, a distinct tendency to level off since the mid 1980s. This provides further support for a significant shift in surface solar radiation during the 1980s. There is evidence that the <span class="hlt">changes</span> in surface solar radiation are linked to associated <span class="hlt">changes</span> in atmospheric aerosol. Variations in scattering sulfur and absorbing black carbon aerosols are in line with the variations in surface solar radiation. This suggests that at least a part of the variations in surface solar radiation should also be seen in the clear sky planetary albedo. Model simulations with a GCM which includes a sophisticated interactive treatment of aerosols and their emission histories (ECHAM5 HAM), can be used to address this issue. The model is shown to be capable of reproducing the reversal from dimming to brightening under cloud-free conditions in many parts of the world, in line with observational evidence. Associated <span class="hlt">changes</span> can also be seen in the clear sky planetary albedo, albeit of smaller magnitude.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/biblio/1275738-frontiers-decadal-climate-variability-proceedings-workshop','SCIGOV-STC'); return false;" href="https://www.osti.gov/biblio/1275738-frontiers-decadal-climate-variability-proceedings-workshop"><span>Frontiers in <span class="hlt">Decadal</span> Climate Variability: Proceedings of a Workshop</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>Purcell, Amanda</p> <p></p> <p>A number of studies indicate an apparent slowdown in the overall rise in global average surface temperature between roughly 1998 and 2014. Most models did not predict such a slowdown--a fact that stimulated a lot of new research on variability of Earth's climate system. At a September 2015 workshop, leading scientists gathered to discuss current understanding of climate variability on <span class="hlt">decadal</span> timescales (10 to 30 years) and whether and how prediction of it might be improved. Many researchers have focused their attention on the climate system itself, which is known to vary across seasons, <span class="hlt">decades</span>, and other timescales. Several naturalmore » variables produce "ups and downs" in the climate system, which are superimposed on the long-term warming trend due to human influence. Understanding <span class="hlt">decadal</span> climate variability is important not only for assessing global climate <span class="hlt">change</span> but also for improving decision making related to infrastructure, water resources, agriculture, energy, and other realms. Like the well-studied El Nino and La Nina interannual variations, <span class="hlt">decadal</span> climate variability is associated with specific regional patterns of temperature and precipitation, such as heat waves, cold spells, and droughts. Several participants shared research that assesses <span class="hlt">decadal</span> predictive capability of current models.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015AGUFM.A23K..08W','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015AGUFM.A23K..08W"><span><span class="hlt">Decadal</span> variability of surface solar radiation over China</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Wang, K.</p> <p>2015-12-01</p> <p>Observations show that national average surface solar radiation (Rs) decreased by -8.0 W m-2 per <span class="hlt">decade</span> from 1960 to 1990 and sharply increased from 1990 to 1993. However, none of the state-of-the-art climate models can reproduce such decrease/increase of Rs. This study shows that Rs observations over China have significant inhomogeneity. Before 1989, Rs was calculated as a sum of direct (Rsdir) and diffuse (Rsdif) solar radiation observations measured by pyrheliometers and shaded pyranometers separately. Due to technical limitations and irregular calibration, pyranometers before 1990 had a strong sensitivity drift problem, which introduced crucial spurious decreasing trends into Rsdif and Rs data. From 1990 to 1993, instruments and measurement methods were replaced and measuring stations were restructured in China, which resulted in an abrupt increase in the observed Rs. Rs calculated from Sunshine duration (SunDu) provide a reliable reference in assessing <span class="hlt">decadal</span> variability of Rs. SunDu derived Rs have no sensitivity drift problem because of its daily <span class="hlt">changed</span> recording material. SunDu-derived Rs averaged over China decreased by -2.9 W m-2 per <span class="hlt">decade</span> from 1961 to 1990, and had a negligible trend afterward. During the period of 1994-2012 when Rs observations were free of inhomogeneity mentioned above, the observed and SunDu-derived Rs consistently show a negligible trend, being less than 0.1 W m-2 per <span class="hlt">decade</span>. These trends can be reproduced by high-quality CMIP5 Earth System Models (ESM). This level of agreement is due to the incorporation of a near real emission inventory of atmospheric aerosols by CMIP5 ESMs. Rs from ERA-Interim has a good agreement with SunDu-derived Rs. However, ERA-interim does not allow aerosol loading to <span class="hlt">change</span> annually. ERA-Interim Rs shows an unreliable increasing trend of 1.9 W m-2 per <span class="hlt">decade</span> from 1990 to 2013 because it does not include the impact of recent increased atmospheric aerosols over China. GEWEX Rs calculated from ISCCP cloud</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/22515468','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/22515468"><span>Families in Bollywood cinema: <span class="hlt">changes</span> and context.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Deakin, Nicholas; Bhugra, Dinesh</p> <p>2012-04-01</p> <p>With increasing and rapid urbanization and population <span class="hlt">changes</span> in India, a growing number of people are migrating from rural areas to urban areas, which brings about major <span class="hlt">changes</span> in support systems. As a result, the portrayal of families has also <span class="hlt">changed</span> in Hindi cinema over the last 50 years. Recent family melodramas have focused on an idealized version of joint and extended families. In this paper we use some <span class="hlt">key</span> Hindi films of the 1960s and of the last two <span class="hlt">decades</span> to compare how films have <span class="hlt">changed</span> and how, in view of <span class="hlt">changing</span> audiences, they have created a version of the family which is far from real. Clinicians need to be aware of these <span class="hlt">changes</span> while dealing with patients and their families (the latter may have unrealistic expectations of their own family members).</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017ClDy...49.2931B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017ClDy...49.2931B"><span><span class="hlt">Changes</span> in intense tropical cyclone activity for the western North Pacific during the last <span class="hlt">decades</span> derived from a regional climate model simulation</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Barcikowska, Monika; Feser, Frauke; Zhang, Wei; Mei, Wei</p> <p>2017-11-01</p> <p>An atmospheric regional climate model (CCLM) was employed to dynamically downscale atmospheric reanalyses (NCEP/NCAR 1, ERA 40) over the western North Pacific and South East Asia. This approach is used for the first time to reconstruct a tropical cyclone climatology, which extends beyond the satellite era and serves as an alternative data set for inhomogeneous observation-derived records (Best Track Data sets). The simulated TC climatology skillfully reproduces observations of the recent <span class="hlt">decades</span> (1978-2010), including spatial patterns, frequency, lifetime, trends, variability on interannual and <span class="hlt">decadal</span> time scales and their association with the large-scale circulation patterns. These skills, facilitated here with the spectral nudging method, seem to be a prerequisite to understand the factors determining spatio-temporal variability of TC activity over the western North Pacific. Long-term trends (1948-2011 and 1959-2001) in both simulations show a strong increase of intense tropical cyclone activity. This contrasts with pronounced multidecadal variations found in observations. The discrepancy may partly originate from temporal inhomogeneities in atmospheric reanalyses and Best Track Data, which affect both the model-based and observational-based trends. An adjustment, which removes the simulated upward trend, reduces the apparent discrepancy. Ultimately, our observational and modeling analysis suggests an important contribution of multi-<span class="hlt">decadal</span> fluctuations in the TC activity during the last six <span class="hlt">decades</span>. Nevertheless, due to the uncertainties associated with the inconsistencies and quality <span class="hlt">changes</span> of those data sets, we call for special caution when reconstructing long-term TC statistics either from atmospheric reanalyses or Best Track Data.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018GBioC..32..654C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018GBioC..32..654C"><span>The eMLR(C*) Method to Determine <span class="hlt">Decadal</span> <span class="hlt">Changes</span> in the Global Ocean Storage of Anthropogenic CO2</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Clement, Dominic; Gruber, Nicolas</p> <p>2018-04-01</p> <p>The determination of the <span class="hlt">decadal</span> <span class="hlt">change</span> in anthropogenic CO2 in the global ocean from repeat hydrographic surveys represents a formidable challenge, which we address here by introducing a seamless new method. This method builds on the extended multiple linear regression (eMLR) approach to identify the anthropogenic CO2 signal, but in order to improve the robustness of this method, we fit C∗ rather than dissolved inorganic carbon and use a probabilistic method for the selection of the predictors. In order to account for the multiyear nature of the surveys, we adjust all C∗ observations of a particular observing period to a common reference year by assuming a transient steady state. We finally use the eMLR models together with global gridded climatological distributions of the predictors to map the estimated <span class="hlt">change</span> in anthropogenic CO2 to the global ocean. Testing this method with synthetic data generated from a hindcast simulation with an ocean model reveals that the method is able to reconstruct the <span class="hlt">change</span> in anthropogenic CO2 with only a small global bias (<5%). Within ocean basins, the errors can be larger, mostly driven by <span class="hlt">changes</span> in ocean circulation. Overall, we conclude from the model that the method has an accuracy of retrieving the column integrated <span class="hlt">change</span> in anthropogenic CO2 of about ±10% at the scale of whole ocean basins. We expect that this uncertainty needs to be doubled to about ±20% when the <span class="hlt">change</span> in anthropogenic CO2 is reconstructed from observations.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018EnMan..61..132Z','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018EnMan..61..132Z"><span>Temporal Dynamics of the Driving Factors of Urban Landscape <span class="hlt">Change</span> of Addis Ababa During the Past Three <span class="hlt">Decades</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Zewdie, Meskerem; Worku, Hailu; Bantider, Amare</p> <p>2018-01-01</p> <p>Mapping and quantifying urban landscape dynamics and the underlying driving factors are crucial for devising appropriate policies, especially in cities of developing countries where the <span class="hlt">change</span> is rapid. This study analyzed three <span class="hlt">decades</span> (1984-2014) of land use land cover <span class="hlt">change</span> of Addis Ababa using Landsat imagery and examined the underlying factors and their temporal dynamics through expert interview using Analytic Hierarchy Process (AHP). Classification results revealed that urban area increased by 50%, while agricultural land and forest decreased by 34 and 16%, respectively. The driving factors operated differently during the pre and post-1991 period. The year 1991 was chosen because it marked government <span class="hlt">change</span> in the country resulting in policy <span class="hlt">change</span>. Policy had the highest influence during the pre-1991 period. Land use <span class="hlt">change</span> in this period was associated with the housing sector as policies and institutional setups were permissive to this sector. Population growth and in-migration were also important factors. Economic factors played significant role in the post-1991 period. The fact that urban land has a market value, the growth of private investment, and the speculated property market were among the economic factors. Policy reforms since 2003 were also influential to the <span class="hlt">change</span>. Others such as accessibility, demography, and neighborhood factors were a response to economic factors. All the above-mentioned factors had vital role in shaping the urban pattern of the city. These findings can help planners and policymakers to better understand the dynamic relationship of urban land use and the driving factors to better manage the city.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29098363','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29098363"><span>Temporal Dynamics of the Driving Factors of Urban Landscape <span class="hlt">Change</span> of Addis Ababa During the Past Three <span class="hlt">Decades</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Zewdie, Meskerem; Worku, Hailu; Bantider, Amare</p> <p>2018-01-01</p> <p>Mapping and quantifying urban landscape dynamics and the underlying driving factors are crucial for devising appropriate policies, especially in cities of developing countries where the <span class="hlt">change</span> is rapid. This study analyzed three <span class="hlt">decades</span> (1984-2014) of land use land cover <span class="hlt">change</span> of Addis Ababa using Landsat imagery and examined the underlying factors and their temporal dynamics through expert interview using Analytic Hierarchy Process (AHP). Classification results revealed that urban area increased by 50%, while agricultural land and forest decreased by 34 and 16%, respectively. The driving factors operated differently during the pre and post-1991 period. The year 1991 was chosen because it marked government <span class="hlt">change</span> in the country resulting in policy <span class="hlt">change</span>. Policy had the highest influence during the pre-1991 period. Land use <span class="hlt">change</span> in this period was associated with the housing sector as policies and institutional setups were permissive to this sector. Population growth and in-migration were also important factors. Economic factors played significant role in the post-1991 period. The fact that urban land has a market value, the growth of private investment, and the speculated property market were among the economic factors. Policy reforms since 2003 were also influential to the <span class="hlt">change</span>. Others such as accessibility, demography, and neighborhood factors were a response to economic factors. All the above-mentioned factors had vital role in shaping the urban pattern of the city. These findings can help planners and policymakers to better understand the dynamic relationship of urban land use and the driving factors to better manage the city.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://eric.ed.gov/?q=linear+AND+induction+AND+accelerator%5b+AND+%c3%97+AND+%5d&pg=2&id=EJ991013','ERIC'); return false;" href="https://eric.ed.gov/?q=linear+AND+induction+AND+accelerator%5b+AND+%c3%97+AND+%5d&pg=2&id=EJ991013"><span><span class="hlt">Key</span> Lessons about Induction for Policy Makers and Researchers</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>Wayne, Andrew J.</p> <p>2012-01-01</p> <p>The purpose of this chapter is to digest the core chapters of this volume, which draws together some of the most sophisticated thinking on new teacher induction from the last <span class="hlt">decade</span>. This chapter attends to five <span class="hlt">key</span> understandings about induction programs, including their context, design, implementation, and outcomes. These understandings emerge…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=20170010425&hterms=records&qs=N%3D0%26Ntk%3DAll%26Ntx%3Dmode%2Bmatchall%26Ntt%3Drecords','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=20170010425&hterms=records&qs=N%3D0%26Ntk%3DAll%26Ntx%3Dmode%2Bmatchall%26Ntt%3Drecords"><span>Multi-<span class="hlt">Decadal</span> Records of Stratospheric Composition and Their Relationship to Stratospheric Circulation <span class="hlt">Change</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Douglass, Anne R.; Strahan, Susan E.; Oman, Luke D.; Stolarski, Richard S.</p> <p>2017-01-01</p> <p>Constituent evolution for 1990-2015 simulated using the Global Modeling Initiative chemistry and transport model driven by meteorological fields from the Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2) is compared with three sources of observations: ground-based column measurements of HNO3 and HCl from two stations in the Network for the Detection of Atmospheric Composition <span class="hlt">Change</span> (NDACC, 1990- ongoing), profiles of CH4 from the Halogen Occultation Experiment (HALOE) on the Upper Atmosphere Research Satellite (UARS, 1992-2005), and profiles of N2O from the Microwave Limb Sounder on the Earth Observing System satellite Aura (2005- ongoing). The differences between observed and simulated values are shown to be time dependent, with better agreement after 2000 compared with the prior <span class="hlt">decade</span>. Furthermore, the differences between observed and simulated HNO3 and HCl columns are shown to be correlated with each other, suggesting that issues with the simulated transport and mixing cause the differences during the 1990s and that these issues are less important during the later years. Because the simulated fields are related to mean age in the lower stratosphere, we use these comparisons to evaluate the time dependence of mean age. The ongoing NDACC column observations provide critical information necessary to substantiate trends in mean age obtained using fields from MERRA-2 or any other reanalysis products.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://files.eric.ed.gov/fulltext/EJ1122590.pdf','ERIC'); return false;" href="http://files.eric.ed.gov/fulltext/EJ1122590.pdf"><span>Enhancing the Capacity to Create Behavior <span class="hlt">Change</span>: Extension <span class="hlt">Key</span> Leaders' Opinions about Social Marketing and Evaluation</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>Warner, Laura A.</p> <p>2014-01-01</p> <p>Extension educators endeavor to create and measure outcomes beyond knowledge gain. The purpose of this qualitative study was to explore the role of social marketing as a method for creating behavior <span class="hlt">change</span> within the University of Florida Extension system through <span class="hlt">key</span> leader opinions. Additionally, the study sought to identify perceptions about…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018NatCC...8..493M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018NatCC...8..493M"><span>Model tropical Atlantic biases underpin diminished Pacific <span class="hlt">decadal</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>McGregor, Shayne; Stuecker, Malte F.; Kajtar, Jules B.; England, Matthew H.; Collins, Mat</p> <p>2018-06-01</p> <p>Pacific trade winds have displayed unprecedented strengthening in recent <span class="hlt">decades</span>1. This strengthening has been associated with east Pacific sea surface cooling2 and the early twenty-first-century slowdown in global surface warming2,3, amongst a host of other substantial impacts4-9. Although some climate models produce the timing of these recently observed trends10, they all fail to produce the trend magnitude2,11,12. This may in part be related to the apparent model underrepresentation of low-frequency Pacific Ocean variability and <span class="hlt">decadal</span> wind trends2,11-13 or be due to a misrepresentation of a forced response1,14-16 or a combination of both. An increasingly prominent connection between the Pacific and Atlantic basins has been identified as a <span class="hlt">key</span> driver of this strengthening of the Pacific trade winds12,17-20. Here we use targeted climate model experiments to show that combining the recent Atlantic warming trend with the typical climate model bias leads to a substantially underestimated response for the Pacific Ocean wind and surface temperature. The underestimation largely stems from a reduction and eastward shift of the atmospheric heating response to the tropical Atlantic warming trend. This result suggests that the recent Pacific trends and model <span class="hlt">decadal</span> variability may be better captured by models with improved mean-state climatologies.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015EGUGA..1710771M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015EGUGA..1710771M"><span>Climate-<span class="hlt">change</span> driven increase in high intensity rainfall events: Analysis of development in the last <span class="hlt">decades</span> and towards an extrapolation of future progression</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Müller, Eva; Pfister, Angela; Gerd, Büger; Maik, Heistermann; Bronstert, Axel</p> <p>2015-04-01</p> <p>Hydrological extreme events can be triggered by rainfall on different spatiotemporal scales: river floods are typically caused by event durations of between hours and days, while urban flash floods as well as soil erosion or contaminant transport rather result from storms events of very short duration (minutes). Still, the analysis of climate <span class="hlt">change</span> impacts on rainfall-induced extreme events is usually carried out using daily precipitation data at best. Trend analyses of extreme rainfall at sub-daily or even sub-hourly time scales are rare. In this contribution two lines of research are combined: first, we analyse sub-hourly rainfall data for several <span class="hlt">decades</span> in three European regions.Second, we investigate the scaling behaviour of heavy short-term precipitation with temperature, i.e. the dependence of high intensity rainfall on the atmospheric temperature at that particular time and location. The trend analysis of high-resolution rainfall data shows for the first time that the frequency of short and intensive storm events in the temperate lowland regions in Germany has increased by up to 0.5 events per year over the last <span class="hlt">decades</span>. I.e. this trend suggests that the occurrence of these types of storms have multiplied over only a few <span class="hlt">decades</span>. Parallel to the <span class="hlt">changes</span> in the rainfall regime, increases in the annual and seasonal average temperature and <span class="hlt">changes</span> in the occurrence of circulation patterns responsible for the generation of high-intensity storms have been found. The analysis of temporally highly resolved rainfall records from three European regions further indicates that extreme precipitation events are more intense with warmer temperatures during the rainfall event. These observations follow partly the Clausius-Clapeyron relation. Based on this relation one may derive a general rule of maximum rainfall intensity associated to the event temperature, roughly following the Clausius-Clapeyron (CC) relation. This rule might be used for scenarios of future maximum</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/2016ThApC.124..653X','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016ThApC.124..653X"><span>Impact of warming climate and cultivar <span class="hlt">change</span> on maize phenology in the last three <span class="hlt">decades</span> in North China Plain</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Xiao, Dengpan; Qi, Yongqing; Shen, Yanjun; Tao, Fulu; Moiwo, Juana P.; Liu, Jianfeng; Wang, Rede; Zhang, He; Liu, Fengshan</p> <p>2016-05-01</p> <p>As climate <span class="hlt">change</span> could significantly influence crop phenology and subsequent crop yield, adaptation is a critical mitigation process of the vulnerability of crop growth and production to climate <span class="hlt">change</span>. Thus, to ensure crop production and food security, there is the need for research on the natural (shifts in crop growth periods) and artificial (shifts in crop cultivars) modes of crop adaptation to climate <span class="hlt">change</span>. In this study, field observations in 18 stations in North China Plain (NCP) are used in combination with Agricultural Production Systems Simulator (APSIM)-Maize model to analyze the trends in summer maize phenology in relation to climate <span class="hlt">change</span> and cultivar shift in 1981-2008. Apparent warming in most of the investigated stations causes early flowering and maturity and consequently shortens reproductive growth stage. However, APSIM-Maize model run for four representative stations suggests that cultivar shift delays maturity and thereby prolongs reproductive growth (flowering to maturity) stage by 2.4-3.7 day per <span class="hlt">decade</span> (d 10a-1). The study suggests a gradual adaptation of maize production process to ongoing climate <span class="hlt">change</span> in NCP via shifts in high thermal cultivars and phenological processes. It is concluded that cultivation of maize cultivars with longer growth periods and higher thermal requirements could mitigate the negative effects of warming climate on crop production and food security in the NCP study area and beyond.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016cosp...41E.163B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016cosp...41E.163B"><span>Towards the Next International Lunar <span class="hlt">Decade</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Beldavs, Vidvuds</p> <p>2016-07-01</p> <p> infrastructure that would make lunar development feasible. Presentations, posters and papers were presented at about a dozen conferences in 2015 and the idea of ILD continued to evolve. Where initially launch was anticipated in 2017 commemorating the 60th anniversary of the IGY and the of launch of Sputnik other possibilities have been discussed including launch on July 20, 2019 commemorating the 50th anniversary of the Apollo 11 landing. Current thinking is that the ILD will span the timeframe from 2020 to 2030 aiming towards achieving breakthrough to a self-sustaining space economy beyond Earth orbit. <span class="hlt">Key</span> to this would be technologies for ISRU as well as markets for products derived from lunar resources and the policies that needed for private investment in lunar resource ventures. The international collaboration envisioned in ILD will coordinate action in lunar exploration, technology development and infrastructure construction and deployment in cislunar space and on the Moon to enable lunar operations, including manned facilities on the Moon as well as at E-M Lagrange points and facilities in Earth orbit. The ILD concept is increasingly including consideration of specific building block elements such as the proposed energy, communication and navigation lunar utility [5]. In 2016 it is anticipated that ILD will be presented at ten more conferences and that <span class="hlt">key</span> organizations will include ILD in their plans. We anticipate worldwide celebrations commemorating the launch of Sputnik and the dawn of the space age in 2017. A major goal is that ILD become a theme of the UNISPACE +50 conference in 2018. The 50th anniversary of the landing of Apollo 11 on the Moon on July 20, 2019 will mark the launch of ILD itself marking the <span class="hlt">decade</span> 2020-2030 as a paradigm shift from government-centric, budget driven deep space initiatives to a self-sustaining space economy with the expectation of significant expansion of space exploration along with profit-making space business. References: [1] http</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012AGUFMPA14A..04B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012AGUFMPA14A..04B"><span>Argumentation <span class="hlt">Key</span> to Communicating Climate <span class="hlt">Change</span> to the Public</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Bleicher, R. E.; Lambert, J. L.</p> <p>2012-12-01</p> <p>Argumentation plays an important role in how we communicate climate <span class="hlt">change</span> science to the public and is a <span class="hlt">key</span> component integrated throughout the Next Generation Science Standards. A scientific argument can be described as a disagreement between explanations with data being used to justify each position. Argumentation is social process where two or more individuals construct and critique arguments (Kuhn & Udell, 2003; Nussbaum, 1997). Sampson, Grooms, and Walker's (2011) developed a framework for understanding the components of a scientific argument. The three components start with a claim (a conjecture, conclusion, explanation, or an answer to a research question). This claim must fit the evidence (observations that show trends over time, relationships between variables or difference between groups). The evidence must be justified with reasoning (explains how the evidence supports the explanation and whey it should count as support). In a scientific argument, or debate, the controversy focuses on how data were collected, what data can or should be included, and what inferences can be made based on a set of evidence. Toulmin's model (1969) also includes rebutting or presenting an alternative explanation supported by counter evidence and reasoning of why the alternative is not the appropriate explanation for the question of the problem. The process of scientific argumentation should involve the construction and critique of scientific arguments, one that involves the consideration of alternative hypotheses (Lawson, 2003). Scientific literacy depends as much on the ability to refute and recognize poor scientific arguments as much as it does on the ability to present an effective argument based on good scientific data (Osborne, 2010). Argument is, therefore, a core feature of science. When students learn to construct a sound scientific argument, they demonstrate critical thinking and a mastery of the science being taught. To present a convincing argument in support of</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><span class="hlt">Decadal</span> Recruitment and Mortality of Ponderosa pine Predicted for the 21st Century Under five Downscaled Climate <span class="hlt">Change</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>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 climate <span class="hlt">changes</span>. These <span class="hlt">changes</span> could be highly challenging for land management agencies. In order to model the consequences of future climates, 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 predict 21st Century <span class="hlt">changes</span> 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 predictions in terms of <span class="hlt">changes</span> in water balance. Predicted <span class="hlt">decadal</span> <span class="hlt">changes</span> in southwestern ponderosa pine for the 21st Century for these five climate <span class="hlt">change</span> scenarios were calculated using a multiple quadratic logistic regression model. Similar models of other western tree species (Pinus edulis, Yucca brevifolia) predicted 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('http://adsabs.harvard.edu/abs/2017AGUFMGC33H..05L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFMGC33H..05L"><span>The summer North Atlantic Oscillation (SNAO) variability on <span class="hlt">decadal</span> to paleoclimate time scales</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Linderholm, H. W.; Folland, C. K.; Zhang, P.; Gunnarson, B. E.; Jeong, J. H.; Ren, H.</p> <p>2017-12-01</p> <p>The summer North Atlantic Oscillation (SNAO), strongly related to the latitude of the North Atlantic and European summer storm tracks, exerts a considerable influence on European summer climate variability and extremes. Here we extend the period covered by the SNAO from July and August to June, July and August (JJA). As well as marked interannual variability, the JJA SNAO has shown a large inter-<span class="hlt">decadal</span> <span class="hlt">change</span> since the 1970s. <span class="hlt">Decadally</span> averaged, there has been a <span class="hlt">change</span> from a very positive to a rather negative SNAO phase. This <span class="hlt">change</span> in SNAO phase is opposite in sign from that expected by a number of climate models under enhanced greenhouse forcing by the late twenty first century. It has led to noticeably wetter summers in North West Europe in the last <span class="hlt">decade</span>. On interannual to multidecadal timescales, SNAO variability is linked to variations in North Atlantic sea surface temperature (SST): observations and models indicate an association between the Atlantic Multi-<span class="hlt">decadal</span> Oscillation (AMO) where the cold (warm) phase of the AMO corresponds a positive (negative) phase of the SNAO. Observations also indicate a link with SST in the Gulf Stream region of the North Atlantic where, particularly on <span class="hlt">decadal</span> time scales, SST warming may favour a more positive phase of the SNAO. Influences of Arctic climate <span class="hlt">change</span> on North Atlantic and European atmospheric circulation may also exist, particularly reduced sea ice coverage, perhaps favouring the negative phase of the SNAO. A new tree-ring data based JJA SNAO reconstruction extending over the last millennium, as well as climate model output for the same period, enables us to examine the influence of North Atlantic SST and Arctic sea-ice coverage, as well as SNAO impacts on European summer climate, in a long-term, pre-industrial context.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014PhDT.........6T','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014PhDT.........6T"><span>A multi-<span class="hlt">decadal</span> remote sensing study on glacial <span class="hlt">change</span> in the North Patagonia Ice Field Chile</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Tetteh, Lucy Korlekwor</p> <p></p> <p>Glaciers in the North Patagonian Ice Fields are temperate glaciers and can be studied to understand the dynamics of climate <span class="hlt">change</span>. However, the ice field has been neglected in mass balance studies. In this study, multi <span class="hlt">decadal</span> study of glacial mass balance, glacier retreat and glacial lake expansion in the North Patagonia were studied. Landsat (TM, ETM+ and 8) and ASTER images were used. San Quintin glacier experienced the highest retreat. Demarcation of glacier lakes boundaries indicated an increase in glacial lake area an addition of 4 new glacial lakes. Nef glacier recorded the highest mass gain of 9.91 plus or minus 1.96 m.w.e.a.-1 and HPN-4 glacier recorded the highest mass loss of -8.9 plus or minus 1.96 m.w.e.a. -1. However, there is a high uncertainty in the elevation values in the DEM due to the rugged nature of the terrain and presence of the heavy snow cover.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012AcMeS..26..289C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012AcMeS..26..289C"><span><span class="hlt">Decadal</span> features of heavy rainfall events in eastern China</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Chen, Huopo; Sun, Jianqi; Fan, Ke</p> <p>2012-06-01</p> <p>Based on daily precipitation data, the spatial-temporal features of heavy rainfall events (HREs) during 1960-2009 are investigated. The results indicate that the HREs experienced strong <span class="hlt">decadal</span> variability in the past 50 years, and the <span class="hlt">decadal</span> features varied across regions. More HRE days are observed in the 1960s, 1980s, and 1990s over Northeast China (NEC); in the 1960s, 1970s, and 1990s over North China (NC); in the early 1960s, 1980s, and 2000s over the Huaihe River basin (HR); in the 1970s-1990s over the mid-lower reaches of the Yangtze River valley (YR); and in the 1970s and 1990s over South China (SC). These <span class="hlt">decadal</span> <span class="hlt">changes</span> of HRE days in eastern China are closely associated with the <span class="hlt">decadal</span> variations of water content and stratification stability of the local atmosphere. The intensity of HREs in each sub-region is also characterized by strong <span class="hlt">decadal</span> variability. The HRE intensity and frequency co-vary on the long-term trend, and show consistent variability over NEC, NC, and YR, but inconsistent variability over SC and HR. Further analysis of the relationships between the annual rainfall and HRE frequency as well as intensity indicates that the HRE frequency is the major contributor to the total rainfall variability in eastern China, while the HRE intensity shows only relative weak contribution.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://files.eric.ed.gov/fulltext/ED341756.pdf','ERIC'); return false;" href="http://files.eric.ed.gov/fulltext/ED341756.pdf"><span>The Hispanic Family: The <span class="hlt">Decade</span> of <span class="hlt">Change</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>Rios, Abdin Noboa</p> <p></p> <p>This speech covers a broad range of issues surrounding the Hispanic American family and the <span class="hlt">changes</span> it has undergone in the last 10 years. Some of the challenges that past and current society presents to minority groups are cited, and a discussion of family reviews its importance and the meaning of the concept "family" for successful identity. The…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3282063','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3282063"><span>A <span class="hlt">decade</span> of molecular cell biology: achievements and challenges</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Akhtar, Asifa; Fuchs, Elaine; Mitchison, Tim; Shaw, Reuben J.; St Johnston, Daniel; Strasser, Andreas; Taylor, Susan; Walczak, Claire; Zerial, Marino</p> <p>2012-01-01</p> <p>Nature Reviews Molecular Cell Biology celebrated its 10-year anniversary during this past year with a series of specially commissioned articles. To complement this, here we have asked researchers from across the field for their insights into how molecular cell biology research has evolved during this past <span class="hlt">decade</span>, the <span class="hlt">key</span> concepts that have emerged and the most promising interfaces that have developed. Their comments highlight the broad impact that particular advances have had, some of the basic understanding that we still require, and the collaborative approaches that will be essential for driving the field forward. PMID:21941276</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://eric.ed.gov/?q=quality+AND+improvement+AND+facilities&pg=6&id=ED560581','ERIC'); return false;" href="https://eric.ed.gov/?q=quality+AND+improvement+AND+facilities&pg=6&id=ED560581"><span>How Have Schools <span class="hlt">Changed</span> over the Past <span class="hlt">Decade</span>? PISA in Focus. No. 52</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>OECD Publishing, 2015</p> <p>2015-01-01</p> <p>It seems that everyone is talking about improving education. Indeed, over the past <span class="hlt">decade</span>, governments have invested more in education in an effort to improve the quality of primary and secondary schools. Has this investment paid off? In every PISA cycle since 2000, students and school principals were asked a series of questions relating to their…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/26515811','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/26515811"><span><span class="hlt">Changes</span> in Ocean Heat, Carbon Content, and Ventilation: A Review of the First <span class="hlt">Decade</span> of GO-SHIP Global Repeat Hydrography.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Talley, L D; Feely, R A; Sloyan, B M; Wanninkhof, R; Baringer, M O; Bullister, J L; Carlson, C A; Doney, S C; Fine, R A; Firing, E; Gruber, N; Hansell, D A; Ishii, M; Johnson, G C; Katsumata, K; Key, R M; Kramp, M; Langdon, C; Macdonald, A M; Mathis, J T; McDonagh, E L; Mecking, S; Millero, F J; Mordy, C W; Nakano, T; Sabine, C L; Smethie, W M; Swift, J H; Tanhua, T; Thurnherr, A M; Warner, M J; Zhang, J-Z</p> <p>2016-01-01</p> <p>Global ship-based programs, with highly accurate, full water column physical and biogeochemical observations repeated <span class="hlt">decadally</span> since the 1970s, provide a crucial resource for documenting ocean <span class="hlt">change</span>. The ocean, a central component of Earth's climate system, is taking up most of Earth's excess anthropogenic heat, with about 19% of this excess in the abyssal ocean beneath 2,000 m, dominated by Southern Ocean warming. The ocean also has taken up about 27% of anthropogenic carbon, resulting in acidification of the upper ocean. Increased stratification has resulted in a decline in oxygen and increase in nutrients in the Northern Hemisphere thermocline and an expansion of tropical oxygen minimum zones. Southern Hemisphere thermocline oxygen increased in the 2000s owing to stronger wind forcing and ventilation. The most recent <span class="hlt">decade</span> of global hydrography has mapped dissolved organic carbon, a large, bioactive reservoir, for the first time and quantified its contribution to export production (∼20%) and deep-ocean oxygen utilization. Ship-based measurements also show that vertical diffusivity increases from a minimum in the thermocline to a maximum within the bottom 1,500 m, shifting our physical paradigm of the ocean's overturning circulation.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/26671456','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/26671456"><span>Three <span class="hlt">decades</span> of eating disorders in Dutch primary care: decreasing incidence of bulimia nervosa but not of anorexia nervosa.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Smink, F R E; van Hoeken, D; Donker, G A; Susser, E S; Oldehinkel, A J; Hoek, H W</p> <p>2016-04-01</p> <p>Whether the incidence of eating disorders in Western, industrialized countries has <span class="hlt">changed</span> over time has been the subject of much debate. The purpose of this primary-care study was to examine <span class="hlt">changes</span> in the incidence of eating disorders in The Netherlands during the 1980s, 1990s and 2000s. A nationwide network of general practitioners (GPs), serving a representative sample (~1%) of the total Dutch population, recorded newly diagnosed patients with anorexia nervosa (AN) and bulimia nervosa (BN) in their practice during 1985-1989, 1995-1999, and 2005-2009. GPs are <span class="hlt">key</span> players in the Dutch healthcare system, as their written referral is mandatory in order to get access to specialized (mental) healthcare, covered by health insurance. Health insurance is virtually universal in The Netherlands (99% of the population). A substantial number of GPs participated in all three study periods, during which the same case identification criteria were used and the same psychiatrist was responsible for making the final diagnoses. Incidence rates were calculated and for comparison between periods, incidence rate ratios. The overall incidence rate of BN decreased significantly in the past three <span class="hlt">decades</span> (from 8.6 per 100,000 person-years in 1985-1989 to 6.1 in 1995-1999, and 3.2 in 2005-2009). The overall incidence of AN remained fairly stable during three <span class="hlt">decades</span>, i.e. 7.4 per 100,000 person-years in 1985-1989, 7.8 in 1995-1999, and 6.0 in 2005-2009. The incidence rate of BN decreased significantly over the past three <span class="hlt">decades</span>, while the overall incidence rate of AN remained stable.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/servlets/purl/1127130','SCIGOV-STC'); return false;" href="https://www.osti.gov/servlets/purl/1127130"><span>Collaborative Research: Separating Forced and Unforced <span class="hlt">Decadal</span> Predictability in Models and Observations</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>Tippett, Michael K.</p> <p>2014-04-09</p> <p>This report is a progress report of the accomplishments of the research grant “Collaborative Research: Separating Forced and Unforced <span class="hlt">Decadal</span> Predictability in Models and Observa- tions” during the period 1 May 2011- 31 August 2013. This project is a collaborative one between Columbia University and George Mason University. George Mason University will submit a final technical report at the conclusion of their no-cost extension. The purpose of the proposed research is to identify unforced predictable components on <span class="hlt">decadal</span> time scales, distinguish these components from forced predictable components, and to assess the reliability of model predictions of these components. Components ofmore » unforced <span class="hlt">decadal</span> predictability will be isolated by maximizing the Average Predictability Time (APT) in long, multimodel control runs from state-of-the-art climate models. Components with <span class="hlt">decadal</span> predictability have large APT, so maximizing APT ensures that components with <span class="hlt">decadal</span> predictability will be detected. Optimal fingerprinting techniques, as used in detection and attribution analysis, will be used to separate variations due to natural and anthropogenic forcing from those due to unforced <span class="hlt">decadal</span> predictability. This methodology will be applied to the <span class="hlt">decadal</span> hindcasts generated by the CMIP5 project to assess the reliability of model projections. The question of whether anthropogenic forcing <span class="hlt">changes</span> <span class="hlt">decadal</span> predictability, or gives rise to new forms of <span class="hlt">decadal</span> predictability, also will be investigated.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFM.B13K..08D','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFM.B13K..08D"><span>Mechanisms of microbial destabilization of soil C shifts over <span class="hlt">decades</span> of warming</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>DeAngelis, K.; Pold, G.; Chowdhury, P. R.; Schnabel, J.; Grandy, S.; Melillo, J. M.</p> <p>2017-12-01</p> <p>Microbes are major actors in regulating the earth's biogeochemical cycles, with temperature-sensitive microbial tradeoffs improving ecosystem biogeochemical models. Meanwhile, the Earth's climate is <span class="hlt">changing</span>, with <span class="hlt">decades</span> of warming undercutting the ability of soil to store carbon. Our work explores trends of 26 years of experimental warming in temperate deciduous forest soils, which is associated with cycles of soil carbon degradation punctuated by periods of <span class="hlt">changes</span> in soil microbial dynamics. Using a combination of biogeochemistry and molecular analytical methods, we explore the hypotheses that substrate availability, community structure, altered temperature sensitivity of microbial turnover-growth efficiency tradeoff, and microbial evolution are responsible for observations of accelerated degradation of soil carbon over time. Amplicon sequencing of microbial communities suggests a small role of <span class="hlt">changing</span> microbial community composition over <span class="hlt">decades</span> of warming, but a sustained suppression of fungal biomass is accompanied by increased biomass of Actinobacteria, Actinobacteria, Alphaproteobacteria, Verrucomicrobia and Planctomycetes. Substrate availability plays an important role in microbial dynamics, with depleted labile carbon in the first <span class="hlt">decade</span> and depleted lignin in the second <span class="hlt">decade</span>. Increased lignin-degrading enzyme activity supports the suggestion that lignin-like organic matter is an important substrate in chronically warmed soils. Metatranscriptomics data support the suggestion that increased turnover is associated with long-term warming, with metagenomic signals of increased carbohydrate-degrading enzymes in the organic horizon but decreased in the mineral soils. Finally, traits analysis of over 200 cultivated isolates of bacterial species from heated and control soils suggests an expanded ability for degradation of cellulose and hemicellulose but not chitin, supporting the hypothesis that long-term warming is exerting evolutionary pressure on microbial</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>Predicting <span class="hlt">Decade</span>-to-Century Climate <span class="hlt">Change</span>: 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 climate models. In attempting to predict the climate 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 <span class="hlt">key</span> processes. Until we are able to incorporate adequate treatments of critical elements of the entire biogeophysical climate system, our models will remain subject to these uncertainties, and our scenarios of future climate <span class="hlt">change</span>, 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/2017AGUFM.C41E..05D','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFM.C41E..05D"><span>Multi-<span class="hlt">Decadal</span> Averages of Basal Melt for Ross Ice Shelf, Antarctica Using Airborne Observations</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Das, I.; Bell, R. E.; Tinto, K. J.; Frearson, N.; Kingslake, J.; Padman, L.; Siddoway, C. S.; Fricker, H. A.</p> <p>2017-12-01</p> <p><span class="hlt">Changes</span> in ice shelf mass balance are <span class="hlt">key</span> to the long term stability of the Antarctic Ice Sheet. Although the most extensive ice shelf mass loss currently is occurring in the Amundsen Sea sector of West Antarctica, many other ice shelves experience <span class="hlt">changes</span> in thickness on time scales from annual to ice age cycles. Here, we focus on the Ross Ice Shelf. An 18-year record (1994-2012) of satellite radar altimetry shows substantial variability in Ross Ice Shelf height on interannual time scales, complicating detection of potential long-term climate-<span class="hlt">change</span> signals in the mass budget of this ice shelf. Variability of radar signal penetration into the ice-shelf surface snow and firn layers further complicates assessment of mass <span class="hlt">changes</span>. We investigate Ross Ice Shelf mass balance using aerogeophysical data from the ROSETTA-Ice surveys using IcePod. We use two ice-penetrating radars; a 2 GHz unit that images fine-structure in the upper 400 m of the ice surface and a 360 MHz radar to identify the ice shelf base. We have identified internal layers that are continuous along flow from the grounding line to the ice shelf front. Based on layer continuity, we conclude that these layers must be the horizons between the continental ice of the outlet glaciers and snow accumulation once the ice is afloat. We use the Lagrangian <span class="hlt">change</span> in thickness of these layers, after correcting for strain rates derived using modern day InSAR velocities, to estimate multidecadal averaged basal melt rates. This method provides a novel way to quantify basal melt, avoiding the confounding impacts of spatial and short-timescale variability in surface accumulation and firn densification processes. Our estimates show elevated basal melt rates (> -1m/yr) around Byrd and Mullock glaciers within 100 km from the ice shelf front. We also compare modern InSAR velocity derived strain rates with estimates from the comprehensive ground-based RIGGS observations during 1973-1978 to estimate the potential magnitude of</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018GeoRL..45.2362Y','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018GeoRL..45.2362Y"><span>A First Look at <span class="hlt">Decadal</span> Hydrological Predictability by Land Surface Ensemble Simulations</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Yuan, Xing; Zhu, Enda</p> <p>2018-03-01</p> <p>The prediction of terrestrial hydrology at the <span class="hlt">decadal</span> scale is critical for managing water resources in the face of climate <span class="hlt">change</span>. Here we conducted an assessment by global land model simulations following the design of the fifth Coupled Model Intercomparison Project (CMIP5) <span class="hlt">decadal</span> hindcast experiments, specifically testing for the sensitivity to perfect initial or boundary conditions. The memory for terrestrial water storage (TWS) is longer than 6 years over 11% of global land areas where the deep soil moisture and aquifer water have a long memory and a nonnegligible variability. Ensemble <span class="hlt">decadal</span> predictions based on realistic initial conditions are skillful over 31%, 43%, and 59% of global land areas for TWS, deep soil moisture, and aquifer water, respectively. The fraction of skillful predictions for TWS increases by 10%-16% when conditioned on Pacific <span class="hlt">Decadal</span> Oscillation and Atlantic Multidecadal Oscillation indices. This study provides a first look at <span class="hlt">decadal</span> hydrological predictability, with an improved skill when incorporating low-frequency climate information.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018JHyd..556...61D','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018JHyd..556...61D"><span>Diverse multi-<span class="hlt">decadal</span> <span class="hlt">changes</span> in streamflow within a rapidly urbanizing region</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Diem, Jeremy E.; Hill, T. Chee; Milligan, Richard A.</p> <p>2018-01-01</p> <p>The impact of urbanization on streamflow depends on a variety of factors (e.g., climate, initial land cover, inter-basin transfers, water withdrawals, wastewater effluent, etc.). The purpose of this study is to examine trends in streamflow from 1986 to 2015 in a range of watersheds within the rapidly urbanizing Atlanta, GA metropolitan area. This study compares eight watersheds over three <span class="hlt">decades</span>, while minimizing the influence of inter-annual precipitation variability. Population and land-cover data were used to analyze <span class="hlt">changes</span> over approximately twenty years within the watersheds. Precipitation totals for the watersheds were estimated using precipitation totals at nearby weather stations. Multiple streamflow variables, such as annual streamflow, frequencies of high-flow days (HFDs), flashiness, and precipitation-adjusted streamflow, for the eight streams were calculated using daily streamflow data. Variables were tested for significant trends from 1986 to 2015 and significant differences between 1986-2000 and 2001-2015. Flashiness increased for all streams without municipal water withdrawals, and the four watersheds with the largest increase in developed land had significant increases in flashiness. Significant positive trends in precipitation-adjusted mean annual streamflow and HFDs occurred for the two watersheds (Big Creek and Suwanee Creek) that experienced the largest increases in development, and these were the only watersheds that went from majority forest land in 1986 to majority developed land in 2015. With a disproportionate increase in HFD occurrence during summer, Big Creek and Suwannee Creek also had a reduction in intra-annual variability of HFD occurrence. Watersheds that were already substantially developed at the beginning of the period and did not have wastewater discharge had declining streamflow. The most urbanized watershed (Peachtree Creek) had a significant decrease in streamflow, and a possible cause of the decrease was increasing</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://eric.ed.gov/?q=Sea+AND+level+AND+rise+AND+florida&id=EJ370938','ERIC'); return false;" href="https://eric.ed.gov/?q=Sea+AND+level+AND+rise+AND+florida&id=EJ370938"><span>The Geology of the Florida <span class="hlt">Keys</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>Shinn, Eugene A.</p> <p>1988-01-01</p> <p>Describes some of the ancient geologic history of the Florida <span class="hlt">Keys</span> from <span class="hlt">Key</span> Largo to <span class="hlt">Key</span> West including the effects of glaciers, sea level rise, reef distribution, spurs and grooves, backstepping and ecological zonation, growth rates and erosion. Predicts future <span class="hlt">changes</span> in this area. (CW)</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://files.eric.ed.gov/fulltext/ED522061.pdf','ERIC'); return false;" href="http://files.eric.ed.gov/fulltext/ED522061.pdf"><span>Education and <span class="hlt">Change</span> in Rich, Poor and National Minority Areas in China: Two <span class="hlt">Decades</span> of Transition. CREATE Pathways to Access. Research Monograph No. 61</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>Lewin, Keith M.; Lu, Wang</p> <p>2011-01-01</p> <p>This study traces education and <span class="hlt">change</span> over two <span class="hlt">decades</span> in three areas, Tongzhou on the periphery of Beijing chosen as one of the richest 300 counties in 1990; Ansai in Yan'an which was one of the poorest 300 counties and a famous base for the 8th Route Army at the end of the Long March, and Zhaojue a poor Yi national minority area in 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_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/2002JCli...15..586S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2002JCli...15..586S"><span>Anatomy of North Pacific <span class="hlt">Decadal</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>Schneider, Niklas; Miller, Arthur J.; Pierce, David W.</p> <p>2002-03-01</p> <p>A systematic analysis of North Pacific <span class="hlt">decadal</span> variability in a full-physics coupled ocean-atmosphere model is executed. The model is an updated and improved version of the coupled model studied by Latif and Barnett. Evidence is sought for determining the details of the mechanism responsible for the enhanced variance of some variables at 20-30-yr timescales. The possible mechanisms include a midlatitude gyre ocean-atmosphere feedback loop, stochastic forcing, remote forcing, or sampling error.<span class="hlt">Decadal</span> variability in the model is expressed most prominently in anomalies of upper-ocean streamfunction, sea surface temperature (SST), and latent surface heat flux in the Kuroshio-Oyashio extension (KOE) region off Japan. The <span class="hlt">decadal</span> signal off Japan is initiated by <span class="hlt">changes</span> in strength and position of the Aleutian low. The atmospheric perturbations excite SST anomalies in the central and eastern North Pacific (with opposing signs and canonical structure). The atmospheric perturbations also <span class="hlt">change</span> the Ekman pumping over the North Pacific, which excites equivalent barotropic Rossby waves that carry thermocline depth perturbations toward the west. This gyre adjustment results in a shift in the border between subtropical and subpolar gyres after about five years. This process consequently excites SST anomalies (bearing the same sign as the central North Pacific) in the KOE region. The SST anomalies are generated by subsurface temperature anomalies that are brought to the surface during winter by deep mixing and are damped by air-sea winter heat exchange (primarily latent heat flux). This forcing of the atmosphere by the ocean in the KOE region is associated with <span class="hlt">changes</span> of winter precipitation over the northwestern Pacific Ocean. The polarity of SST and Ekman pumping is such that warm central and cool eastern Pacific anomalies are associated with a deep thermocline, a poleward shift of the border between subtropical and subpolar gyres, and warm SST anomalies and an increase of</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/25158628','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/25158628"><span>Nucleosomal occupancy <span class="hlt">changes</span> locally over <span class="hlt">key</span> regulatory regions during cell differentiation and reprogramming.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>West, Jason A; Cook, April; Alver, Burak H; Stadtfeld, Matthias; Deaton, Aimee M; Hochedlinger, Konrad; Park, Peter J; Tolstorukov, Michael Y; Kingston, Robert E</p> <p>2014-08-27</p> <p>Chromatin structure determines DNA accessibility. We compare nucleosome occupancy in mouse and human embryonic stem cells (ESCs), induced-pluripotent stem cells (iPSCs) and differentiated cell types using MNase-seq. To address variability inherent in this technique, we developed a bioinformatic approach to identify regions of difference (RoD) in nucleosome occupancy between pluripotent and somatic cells. Surprisingly, most chromatin remains unchanged; a majority of rearrangements appear to affect a single nucleosome. RoDs are enriched at genes and regulatory elements, including enhancers associated with pluripotency and differentiation. RoDs co-localize with binding sites of <span class="hlt">key</span> developmental regulators, including the reprogramming factors Klf4, Oct4/Sox2 and c-Myc. Nucleosomal landscapes in ESC enhancers are extensively altered, exhibiting lower nucleosome occupancy in pluripotent cells than in somatic cells. Most <span class="hlt">changes</span> are reset during reprogramming. We conclude that <span class="hlt">changes</span> in nucleosome occupancy are a hallmark of cell differentiation and reprogramming and likely identify regulatory regions essential for these processes.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=20060037970&hterms=Mount+Rainier&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D50%26Ntt%3DMount%2BRainier','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=20060037970&hterms=Mount+Rainier&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D50%26Ntt%3DMount%2BRainier"><span>(abstract) Mount Rainier: New Remote Sensing Observations of a <span class="hlt">Decade</span> Volcano</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Realmuto, V. J.; Zebker, H. A.; Frank, D.</p> <p>1994-01-01</p> <p>Mount Rainier was selected as a <span class="hlt">Decade</span> Volcano by the International Association of Volcanology and Chemistry of the Earth's Interior. The purpose of this selection is to focus scientific and public attention on Mount Rainier during the current <span class="hlt">decade</span>, the United Nations-designated International <span class="hlt">Decade</span> of Natural Hazard Reduction. The Mount Rainier science plan calls for remote sensing surveys to monitor the volcano. To date, we have conducted airborne surveys with visible and near-infrared, thermal infrared, and interferometric radar instruments. Our preliminary analysis of some night-time time-series thermal infrared survey data sets of the summit suggests that, aside from seasonal variations in snow cover, there have been no qualitative <span class="hlt">changes</span> in the size or pattern of the summit hot spots. Day-time airborne surveys were done to record the current surface appearance of the volcano and map hydrothermal alteration in the summit region. An interferometric radar survey yielded a high-resolution digital elevation model (DEM) which serves as a base for the registration of the other remote sensing data sets. More importantly, the DEM documents the current topography of glaciers and valleys. Planned biannual radar survey of mount rainier will produce a data set from which seasonal <span class="hlt">changes</span> in glacier and valley topography can be characterized. Such characterization is essential if we are to recognize geothermally induced <span class="hlt">changes</span> in snow and ice cover.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013AGUFMGC11D1019L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013AGUFMGC11D1019L"><span>A decision analysis approach to climate adaptation: comparing multiple pathways for multi-<span class="hlt">decadal</span> decision making</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Lin, B. B.; Little, L.</p> <p>2013-12-01</p> <p>Policy planners around the world are required to consider the implications of adapting to climatic <span class="hlt">change</span> across spatial contexts and <span class="hlt">decadal</span> timeframes. However, local level information for planning is often poorly defined, even though climate adaptation decision-making is made at this scale. This is especially true when considering sea level rise and coastal impacts of climate <span class="hlt">change</span>. We present a simple approach using sea level rise simulations paired with adaptation scenarios to assess a range of adaptation options available to local councils dealing with issues of beach recession under present and future sea level rise and storm surge. Erosion and beach recession pose a large socioeconomic risk to coastal communities because of the loss of <span class="hlt">key</span> coastal infrastructure. We examine the well-known adaptation technique of beach nourishment and assess various timings and amounts of beach nourishment at <span class="hlt">decadal</span> time spans in relation to beach recession impacts. The objective was to identify an adaptation strategy that would allow for a low frequency of management interventions, the maintenance of beach width, and the ability to minimize variation in beach width over the 2010 to 2100 simulation period. 1000 replications of each adaptation option were produced against the 90 year simulation in order to model the ability each adaptation option to achieve the three <span class="hlt">key</span> objectives. Three sets of adaptation scenarios were identified. Within each scenario, a number of adaptation options were tested. The three scenarios were: 1) Fixed periodic beach replenishment of specific amounts at 20 and 50 year intervals, 2) Beach replenishment to the initial beach width based on trigger levels of recession (5m, 10m, 20m), and 3) Fixed period beach replenishment of a variable amount at <span class="hlt">decadal</span> intervals (every 10, 20, 30, 40, 50 years). For each adaptation option, we show the effectiveness of each beach replenishment scenario to maintain beach width and consider the implications of more</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/25985671','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/25985671"><span>[Agricultural policies and farming systems: A case study of landscape <span class="hlt">changes</span> in Shizuitou Village in the recent four <span class="hlt">decades</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, Xiao-jun; Zhou, Yang; Yan, Yan-bin; Li, Lei</p> <p>2015-01-01</p> <p>Agricultural policy in China's rural heartland is driving profound <span class="hlt">changes</span> to traditional farming systems. A case study covering four <span class="hlt">decades</span> mapped and recorded farming patterns and processes in Shizuitou Village, a rural village in northwest Shanxi. An integrated geospatial methodology from geography and anthropology was employed in the case study to record the <span class="hlt">changing</span> dynamics of farming systems in Shizuitou Village to discover the long-term impacts of China's agricultural policies on village farming systems. Positive and negative impacts of agricultural policies on village farming systems were mapped, inventoried and evaluated using Participatory Geographic Information Systems (PGIS). The results revealed traditional polycultures are being gradually replaced by industrialized monocultures. The driving forces behind these farming <span class="hlt">changes</span> come from a series of government agricultural policies aiming at modernization of farming systems in China. The goal of these policies was to spur rapid development of industrial agriculture under the guise of modernization but is leading to the decay of traditional farming systems in the village that maintained local food security with healthy land for hundreds of years. The paper concluded with a recommendation that in future, agricultural policy makers should strike a more reasonable balance between short-term agricultural profits and long-term farming sustainability based on the principles of ecological sustainable development under the context of global <span class="hlt">changes</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013EGUGA..15.4211B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013EGUGA..15.4211B"><span>Seasonal and <span class="hlt">decadal</span> information towards climate services: EUPORIAS</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Buontempo, Carlo; Hewitt, Chris</p> <p>2013-04-01</p> <p>Societies have always faced challenges and opportunities arising from variations in climate, and have often flourished or collapsed depending on their ability to adapt to such <span class="hlt">changes</span>. Recent advances in our understanding and ability to forecast climate variability and climate <span class="hlt">change</span> have meant that skilful predictions are beginning to be routinely made on seasonal to <span class="hlt">decadal</span> (s2d) timescales. Such forecasts have the potential to be of great value to a wide range of decision-making, where outcomes are strongly influenced by variations in the climate. The European Commission have recently commissioned a major four year long project (EUPORIAS) to develop prototype end-to-end climate impact prediction services operating on a seasonal to <span class="hlt">decadal</span> timescale, and assess their value in informing decision-making. EUPORIAS commenced on 1 November 2012, coordinated by the UK Met Office leading a consortium of 24 organisations representing world-class European climate research and climate service centres, expertise in impacts assessments and seasonal predictions, two United Nations agencies, specialists in new media, and commercial companies in climate-vulnerable sectors such as energy, water and tourism. The paper describes the setup of the project, its main outcome and some of the very preliminary results.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2005AGUFM.G41C0370D','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2005AGUFM.G41C0370D"><span>Historical Variations in Inner Core Rotation and Polar Motion at <span class="hlt">Decade</span> Timescales</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Dumberry, M.</p> <p>2005-12-01</p> <p>Exchanges of angular momentum between the mantle, the fluid core and the solid inner core result in <span class="hlt">changes</span> in the Earth's rotation. Torques in the axial direction produce <span class="hlt">changes</span> in amplitude, or <span class="hlt">changes</span> in length of day, while torques in the equatorial direction lead to <span class="hlt">changes</span> in orientation of the rotation vector with respect to the mantle, or polar motion. In this work, we explore the possibility that a combination of electromagnetic and gravitational torques on the inner core can reproduce the observed <span class="hlt">decadal</span> variations in polar motion known as the Markowitz wobble. Torsional oscillations, which involve azimuthal motions in the fluid core with typical periods of <span class="hlt">decades</span>, entrain the inner core by electromagnetic traction. When the inner core is axially rotated, its surfaces of constant density are no longer aligned with the gravitational potential from mantle density heterogeneities, and this results in a gravitational torque between the two. The axial component of this torque has been previously described and is believed to be partly responsible for <span class="hlt">decadal</span> <span class="hlt">changes</span> in length of day. In this work, we show that it has also an equatorial component, which produces a tilt of the inner core and results in polar motion. The polar motion produced by this mechanism depends on the density structure in the mantle, the rheology of the inner core, and the time-history of the angle of axial misalignment between the inner core and the mantle. We reconstruct the latter using a model of torsional oscillations derived from geomagnetic secular variation. From this time-history, and by using published models of mantle density structure, we show that we can reproduce the salient characteristics of the Markowitz wobble: an eccentric <span class="hlt">decadal</span> polar motion of 30-50 milliarcsecs oriented along a specific longitude. We discuss the implications of this result, noting that a match in both amplitude and phase of the observed Markowitz wobble allows the recovery of the historical</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/27896805','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/27896805"><span><span class="hlt">Key</span> Elements of a Family Intervention for Schizophrenia: A Qualitative Analysis of an RCT.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Grácio, Jaime; Gonçalves-Pereira, Manuel; Leff, Julian</p> <p>2018-03-01</p> <p>Schizophrenia is a complex biopsychosocial condition in which expressed emotion in family members is a robust predictor of relapse. Not surprisingly, family interventions are remarkably effective and thus recommended in current treatment guidelines. Their <span class="hlt">key</span> elements seem to be common therapeutic factors, followed by education and coping skills training. However, few studies have explored these <span class="hlt">key</span> elements and the process of the intervention itself. We conducted a qualitative and quantitative analysis of the records from a pioneering family intervention trial addressing expressed emotion, published by Leff and colleagues four <span class="hlt">decades</span> ago. Records were analyzed into categories and data explored using descriptive statistics. This was complemented by a narrative evaluation using an inductive approach based on emotional markers and markers of <span class="hlt">change</span>. The most used strategies in the intervention were addressing needs, followed by coping skills enhancement, advice, and emotional support. Dealing with overinvolvement and reframing were the next most frequent. Single-family home sessions seemed to augment the therapeutic work conducted in family groups. Overall the intervention seemed to promote cognitive and emotional <span class="hlt">change</span> in the participants, and therapists were sensitive to the emotional trajectory of each subject. On the basis of our findings, we developed a longitudinal framework for better understanding the process of this treatment approach. © 2016 Family Process Institute.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017EGUGA..19.2898W','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017EGUGA..19.2898W"><span>Tracking four-<span class="hlt">decade</span> inundation <span class="hlt">changes</span> with multi-temporal satellite images in China's largest freshwater lake</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Wu, Guiping</p> <p>2017-04-01</p> <p> certain extent for the Poyang Lake's area could be detected. The lake surface displayed comparatively low values ( 2000 km2) in wet periods of 1980, 2006, 2009 and 2011, corresponding to severe hydrological droughts in the lake. In addition, the water surface variation in Poyang Lake had a typical seasonal behavior. It mostly followed a unimodal cycle with area peaks appeared in the wet season. The earliest beginning of the inundation cycle was emerged in 2000 and the latest in 2006. In general, the <span class="hlt">change</span> of lake area is a synthetic result of climate <span class="hlt">change</span>, land-cover <span class="hlt">change</span> and construction of dykes. Our findings should be valuable to a comprehensive understanding of Poyang Lake's <span class="hlt">decadal</span> and seasonal variation, which is critical for flood/drought prevention, land use planning and lake ecological conservation.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19950005971','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19950005971"><span>Solar influences on global <span class="hlt">change</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>1994-01-01</p> <p>Monitoring of the Sun and the Earth has yielded new knowledge essential to this debate. There is now no doubt that the total radiative energy from the Sun that heats the Earth's surface <span class="hlt">changes</span> over <span class="hlt">decadal</span> time scales as a consequence of solar activity. Observations indicate as well that <span class="hlt">changes</span> in ultraviolet radiation and energetic particles from the Sun, also connected with the solar activity, modulate the layer of ozone that protects the biosphere from the solar ultraviolet radiation. This report reassesses solar influences on global <span class="hlt">change</span> in the light of this new knowledge of solar and atmospheric variability. Moreover, the report considers climate <span class="hlt">change</span> to be encompassed within the broader concept of global <span class="hlt">change</span>; thus the biosphere is recognized to be part of a larger, coupled Earth system. Implementing a program to continuously monitor solar irradiance over the next several <span class="hlt">decades</span> will provide the opportunity to estimate solar influences on global <span class="hlt">change</span>, assuming continued maintenance of observations of climate and other potential forcing mechanisms. In the lower atmosphere, an increase in solar radiation is expected to cause global warming. In the stratosphere, however, the two effects produce temperature <span class="hlt">changes</span> of opposite sign. A monitoring program that would augment long term observations of tropospheric parameters with similar observations of stratospheric parameters could separate these diverse climate perturbations and perhaps isolate a greenhouse footprint of climate <span class="hlt">change</span>. Monitoring global <span class="hlt">change</span> in the troposphere is a <span class="hlt">key</span> element of all facets of the United States Global <span class="hlt">Change</span> Research Program (USGCRP), not just of the study of solar influences on global <span class="hlt">change</span>. The need for monitoring the stratosphere is also important for global <span class="hlt">change</span> research in its own right because of the stratospheric ozone layer.</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 <span class="hlt">Decadal</span> Climate Prediction 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 <span class="hlt">Decadal</span> Climate Prediction Project (DCPP) is a coordinated multi-model investigation into <span class="hlt">decadal</span> climate prediction, predictability, and variability. The DCPP makes use of past experience in simulating and predicting <span class="hlt">decadal</span> variability and forced climate <span class="hlt">change</span> gained from the fifth Coupled Model Intercomparison Project (CMIP5) and elsewhere. It builds on recent improvements in models, in the reanalysis of climate data, in methods of initialization and ensemble generation, and in data treatment and analysis to propose an extended comprehensive <span class="hlt">decadal</span> prediction investigation as a contribution to CMIP6 (Eyring et al., 2016) and to the WCRP Grand Challenge on Near Term Climate 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 <span class="hlt">decadal</span> prediction skill, as a basis for improvements in all aspects of end-to-end <span class="hlt">decadal</span> prediction, and as a basis for forecasting on annual to <span class="hlt">decadal</span> 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 climate 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 <span class="hlt">Decadal</span> Climate Prediction Project addresses a range of scientific issues involving the ability of the climate system to be predicted on annual to <span class="hlt">decadal</span> 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://adsabs.harvard.edu/abs/2017EGUGA..19.1765R','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017EGUGA..19.1765R"><span><span class="hlt">Decadal</span> climate variation recorded in modern global carbonate archives (brachiopods, molluscs)</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Romanin, Marco; Zaki, Amir H.; Davis, Alyssa; Shaver, Kristen; Wang, Lisha; Aleksandra Bitner, Maria; Capraro, Luca; Preto, Nereo; Brand, Uwe</p> <p>2017-04-01</p> <p>The progress of the Earth's warming trend has rapidly accelerated in the last few <span class="hlt">decades</span> due to the increase in emission of anthropogenic greenhouse gases. The exchange of heat between the atmosphere and seawater has consequently elevated the rate of temperature buildup in the low and high latitude ocean. Records of the variation in seawater temperature in response to local and global <span class="hlt">changes</span> in climate are preserved within the carbonate structures of marine biogenic archives. Investigating the isotopic composition of the archives' growth increments documents the magnitude of sea surface temperature (SST) <span class="hlt">change</span>. A long-term (1956-2012) record of temperature <span class="hlt">change</span> in sub-tropical seawater was acquired from the giant clam Tridacna maxima collected from the Red Sea in conjunction with published results of the oyster Hyotissa hyotis (Titschack et al., 2010). Variation in polar-subpolar SST was obtained from the brachiopod Magellania venosa recovered from the coastal area of southern Chile, and from the proxy record of Hemithiris psittacea of Hudson Bay (Brand et al., 2014). The former reveals a long-term (1961-2012) time-series of Antarctic-induced oceanographic <span class="hlt">change</span> in the southern hemisphere, while the latter represents a trend of Hudson Bay seawater SST in the northern hemisphere. Evaluation of the isotopic compositions confirms the equilibrium incorporation of oxygen isotopes with respect to ambient seawater in brachiopods and some bivalves. A general trend of decreasing δ18O values in the Red Sea molluscs is observed, indicating an increase in tropical seawater temperature of about 0.79°C since 1988. The δ18O values of the polar-subpolar brachiopods display similar depletion slopes but of larger magnitudes than that of the Red Sea archives. This signifies a rise in seawater temperature of about 1.47°C in Hudson Bay since 1991, and about 2.08°C in southern Chile since 1988. The 2013 IPCC report suggests an increase in SST of +0.094°C per <span class="hlt">decade</span> (average</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012AGUFMPP33A2077P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012AGUFMPP33A2077P"><span>Solar Cycle Driven Environmental <span class="hlt">Changes</span> on <span class="hlt">Decadal</span> to Centennial Scale of Late Miocene Lake Sediments (tortonian, Lake Pannon, Central Europe)</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Piller, W. E.; Kern, A. K.; Harzhauser, M.; Soliman, A.; Mandic, O.</p> <p>2012-12-01</p> <p>High time resolution is a <span class="hlt">key</span> issue in reconstructing past climate systems. This is of particular importance when searching for model predictions of future climate <span class="hlt">change</span>, such as the warm Late Miocene. For this study we selected Lake Pannon, a paleo-ancient, alkaline, brackish lake in Europe during the Tortonian (early Late Miocene). On a continuous sediment core including the interval from ca. 10.5 - 10.4 Ma we show the power of high resolution multiproxy analyses for reconstructing paleoclimatology on a <span class="hlt">decadal</span> scale over several millennia of Late Miocene time. To demonstrate this high-resolution interpretation we selected a core from the western margin of Lake Pannon and studied it in respect to 2 different time resolutions. A continuous 6-m-core clearly displays regular fluctuations and modulations within three different environmental proxies (natural gamma radiation, magnetic susceptibility, total abundance of ostracods). Lomb-Scargle and REDFIT periodograms next to wavelet spectra of all data sets reveal distinct frequencies. Only few of these are deciphered in all proxy data sets at the same power, while some occur only in two or one proxies. A higher resolution study was conducted on a 1.5-m-long core interval based on pollen and dinoflagellate cysts, ostracod abundance, carbon and sulfur contents as well as magnetic susceptibility and natural gamma radiation. Based on an already established age model the study covers about two millennia of Late Miocene time with a resolution of ~13.7 years per sample. No major ecological turnovers are expected in respect to this very short interval. Thus, the pollen record suggests rather stable wetland vegetation with a forested hinterland. Shifts in the spectra can be mainly attributed to variations in transport mechanism, represented by few phases of fluvial input but mainly by <span class="hlt">changes</span> in wind intensity and probably also wind direction. Even within this short time span, dinoflagellates document rapid <span class="hlt">changes</span> between</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016DPS....4821406I','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016DPS....4821406I"><span>Enceladus Plumes: Causes of <span class="hlt">Decadal</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>Ingersoll, Andrew P.; Ewald, Shawn P.</p> <p>2016-10-01</p> <p>The Enceladus plumes have decreased over the <span class="hlt">decade</span> that Cassini has been observing them. This long-term variation is superposed on the much shorter-term variation tied to the position of Enceladus in its orbit around Saturn. The observations are ISS and VIMS images, which reveal the particles in the plumes but not the gas. The <span class="hlt">decadal</span> variability largely consists of a 2-fold decline in the mass of plume material, but there is a hint of a recent turnaround. Here we offer three hypotheses, each with its strengths and weaknesses, to explain the long-term variability. The first is seasonal <span class="hlt">change</span>, from summer to fall in the southern hemisphere. The loss of sunlight could increase the build-up of ice around the tiger stripes. The weakness is that the sunlight is likely to have a small effect, e.g., decreasing the sublimation rate of the ice by only ~1 cm/year. The second hypothesis is a statistical fluctuation in the number of active plumes, which tend to turn themselves off due to build-up of ice at the throat of the vent. The weakness is that the plumes are likely to fluctuate independently, and if there are ~100 plumes, their sum will only fluctuate by 10%. The third hypothesis is that the variation is part of a well-known <span class="hlt">decadal</span> cycle of orbital eccentricity, which varies by ±2.5% around a mean of 0.0047. The peak eccentricity occurred in 2009-2010, and the minimum occurred in 2015. Since eccentricity controls the short-term orbital cycle variations, it could also control the longer-term <span class="hlt">decadal</span> variations. The weakness is that the eccentricity variation is small, from 0.0046 to 0.0048. It is not certain that such a small variation could cause a 2-fold variation in the strength of the plumes. An independent study, still in its infancy, is the possibility that liquid water reaches the surface during part of the orbital cycle.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/15563646','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/15563646"><span>Cities and health: history, approaches, and <span class="hlt">key</span> questions.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Vlahov, David; Gibble, Emily; Freudenberg, Nicholas; Galea, Sandro</p> <p>2004-12-01</p> <p>The majority of the world's population will live in cities in the next few years, and the pace of urbanization worldwide will continue to accelerate over the coming <span class="hlt">decades</span>. Such a dramatic demographic shift can be expected to have an impact on population health. Although there has been historic interest in how city living is associated with health, this interest has waxed and waned and a cogent framework has yet to evolve that encompasses <span class="hlt">key</span> issues in urban health. In this article, the authors discuss three alternate approaches to the study of urban health today; these include considering urban health from the perspective of a presumed urban health penalty, from an urban sprawl perspective, and more comprehensively, considering how urban living conditions may be associated with health. The authors also propose three <span class="hlt">key</span> questions that may help guide the study and practice of urban health in coming <span class="hlt">decades</span>. These include considering what specific features of cities are causally related to health, the extent to which these features are unique to a particular city or are different between cities, and ultimately, to what extent these features of cities are modifiable in order to allow interventions that can improve the health of urban populations.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018GMD....11..351P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018GMD....11..351P"><span>Parametric <span class="hlt">decadal</span> climate forecast recalibration (DeFoReSt 1.0)</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Pasternack, Alexander; Bhend, Jonas; Liniger, Mark A.; Rust, Henning W.; Müller, Wolfgang A.; Ulbrich, Uwe</p> <p>2018-01-01</p> <p>Near-term climate predictions such as <span class="hlt">decadal</span> climate forecasts are increasingly being used to guide adaptation measures. For near-term probabilistic predictions to be useful, systematic errors of the forecasting systems have to be corrected. While methods for the calibration of probabilistic forecasts are readily available, these have to be adapted to the specifics of <span class="hlt">decadal</span> climate forecasts including the long time horizon of <span class="hlt">decadal</span> climate forecasts, lead-time-dependent systematic errors (drift) and the errors in the representation of long-term <span class="hlt">changes</span> and variability. These features are compounded by small ensemble sizes to describe forecast uncertainty and a relatively short period for which typically pairs of reforecasts and observations are available to estimate calibration parameters. We introduce the <span class="hlt">Decadal</span> Climate Forecast Recalibration Strategy (DeFoReSt), a parametric approach to recalibrate <span class="hlt">decadal</span> ensemble forecasts that takes the above specifics into account. DeFoReSt optimizes forecast quality as measured by the continuous ranked probability score (CRPS). Using a toy model to generate synthetic forecast observation pairs, we demonstrate the positive effect on forecast quality in situations with pronounced and limited predictability. Finally, we apply DeFoReSt to <span class="hlt">decadal</span> surface temperature forecasts from the MiKlip prototype system and find consistent, and sometimes considerable, improvements in forecast quality compared with a simple calibration of the lead-time-dependent systematic errors.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2009AGUFMSH14A..01F','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2009AGUFMSH14A..01F"><span>Solar <span class="hlt">Changes</span> and Climate <span class="hlt">Changes</span>. (Invited)</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Feynman, J.</p> <p>2009-12-01</p> <p>During the early <span class="hlt">decades</span> of the Space Age there was general agreement in the scientific community on two facts: (1) sunspot cycles continued without interruption; (2) <span class="hlt">decadal</span> timescale variations in the solar output has no effect on Earth’s climate. Then in 1976 Jack Eddy published a paper called ‘The Maunder Minimum” in Science magazine arguing that neither of these two established facts was true. He reviewed the observations from the 17th century that show the Sun did not appear to cycle for several <span class="hlt">decades</span> and he related that to the cold winters in Northern Europe at that time. The paper has caused three <span class="hlt">decades</span> of hot discussions. When Jack Eddy died on June 10th of this year the arguments were sill going on, and there were no sunspots that day. The Sun was in the longest and deepest solar minimum since 1900. In this talk I will describe the <span class="hlt">changes</span> in the solar output that have taken place over the last few <span class="hlt">decades</span> and put them in their historical context. I will also review recent work on the influence of <span class="hlt">decadal</span> and century scale solar variations on the Earth’s climate. It is clear that this long, deep “solar minimum” is an opportunity to make fundamental progress on our understanding of the solar dynamo and to separate climate <span class="hlt">change</span> due to the Sun from anthropogenic climate <span class="hlt">change</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5686539','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5686539"><span><span class="hlt">Key</span> Metabolites and Mechanistic <span class="hlt">Changes</span> for Salt Tolerance in an Experimentally Evolved Sulfate-Reducing Bacterium, Desulfovibrio vulgaris</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Zhou, Aifen; Lau, Rebecca; Baran, Richard; Ma, Jincai; von Netzer, Frederick; Shi, Weiling; Gorman-Lewis, Drew; Kempher, Megan L.; He, Zhili; Qin, Yujia; Shi, Zhou; Zane, Grant M.; Wu, Liyou; Bowen, Benjamin P.; Northen, Trent R.; Hillesland, Kristina L.; Stahl, David A.; Wall, Judy D.; Arkin, Adam P.</p> <p>2017-01-01</p> <p>ABSTRACT Rapid genetic and phenotypic adaptation of the sulfate-reducing bacterium Desulfovibrio vulgaris Hildenborough to salt stress was observed during experimental evolution. In order to identify <span class="hlt">key</span> metabolites important for salt tolerance, a clone, ES10-5, which was isolated from population ES10 and allowed to experimentally evolve under salt stress for 5,000 generations, was analyzed and compared to clone ES9-11, which was isolated from population ES9 and had evolved under the same conditions for 1,200 generations. These two clones were chosen because they represented the best-adapted clones among six independently evolved populations. ES10-5 acquired new mutations in genes potentially involved in salt tolerance, in addition to the preexisting mutations and different mutations in the same genes as in ES9-11. Most basal abundance <span class="hlt">changes</span> of metabolites and phospholipid fatty acids (PLFAs) were lower in ES10-5 than ES9-11, but an increase of glutamate and branched PLFA i17:1ω9c under high-salinity conditions was persistent. ES9-11 had decreased cell motility compared to the ancestor; in contrast, ES10-5 showed higher cell motility under both nonstress and high-salinity conditions. Both genotypes displayed better growth energy efficiencies than the ancestor under nonstress or high-salinity conditions. Consistently, ES10-5 did not display most of the basal transcriptional <span class="hlt">changes</span> observed in ES9-11, but it showed increased expression of genes involved in glutamate biosynthesis, cation efflux, and energy metabolism under high salinity. These results demonstrated the role of glutamate as a <span class="hlt">key</span> osmolyte and i17:1ω9c as the major PLFA for salt tolerance in D. vulgaris. The mechanistic <span class="hlt">changes</span> in evolved genotypes suggested that growth energy efficiency might be a <span class="hlt">key</span> factor for selection. PMID:29138306</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://eric.ed.gov/?q=zulu&pg=7&id=EJ876978','ERIC'); return false;" href="https://eric.ed.gov/?q=zulu&pg=7&id=EJ876978"><span><span class="hlt">Key</span> Dimensions of Effective Leadership for <span class="hlt">Change</span>: A Focus on Township and Rural Schools in South Africa</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>Ngcobo, Thandi; Tikly, Leon Paul</p> <p>2010-01-01</p> <p>The article identifies <span class="hlt">key</span> dimensions of effective leadership for <span class="hlt">change</span> in historically disadvantaged, township and rural schools in South Africa. It is based on original case study research in 13 schools in Kwa-Zulu Natal. Although the sample included mainly township and rural primary and secondary schools it also included a smaller sample of…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017ERL....12i5003W','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017ERL....12i5003W"><span>Potential climate <span class="hlt">change</span> impacts on fire intensity and <span class="hlt">key</span> wildfire suppression thresholds in Canada</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Wotton, B. M.; Flannigan, M. D.; Marshall, G. A.</p> <p>2017-09-01</p> <p>Much research has been carried out on the potential impacts of climate <span class="hlt">change</span> on forest fire activity in the boreal forest. Indeed, there is a general consensus that, while <span class="hlt">change</span> will vary regionally across the vast extent of the boreal, in general the fire environment will become more conducive to fire. Land management agencies must consider ways to adapt to these new conditions. This paper examines the impact of that <span class="hlt">changed</span> fire environment on overall wildfire suppression capability. We use multiple General Circulation Models and carbon emission pathways to generate future fire environment scenarios for Canada’s forested region. We then use these scenarios with the Canadian Forest Fire Behaviour Prediction System and spatial coverages of the current forest fuel composition across the landscape to examine potential variation in <span class="hlt">key</span> fire behaviour outputs that influence whether fire management resources can effectively suppress fire. Specifically, we evaluate how the potential for crown fire occurrence and active growth of fires <span class="hlt">changes</span> with the <span class="hlt">changing</span> climate. We also examine future fire behaviour through the lens of operational fire intensity thresholds used to guide decisions about resources effectiveness. Results indicate that the proportion of days in fire seasons with the potential for unmanageable fire will increase across Canada’s forest, more than doubling in some regions in northern and eastern boreal forest.</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://pubs.er.usgs.gov/publication/70034795','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70034795"><span>Tree die-off in response to global <span class="hlt">change</span>-type drought: Mortality insights from a <span class="hlt">decade</span> of plant water potential measurements</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Breshears, D.D.; Myers, O.B.; Meyer, Clifton W.; Barnes, F.J.; Zou, C.B.; Allen, Craig D.; McDowell, N.G.; Pockman, W. T.</p> <p>2009-01-01</p> <p>Global climate <span class="hlt">change</span> is projected to produce warmer, longer, and more frequent droughts, referred to here as “global <span class="hlt">change</span>-type droughts”, which have the potential to trigger widespread tree die-off. However, drought-induced tree mortality cannot be predicted with confidence, because long-term field observations of plant water stress prior to, and culminating in, mortality are rare, precluding the development and testing of mechanisms. Here, we document plant water stress in two widely distributed, co-occurring species, piñon pine (Pinus edulis) and juniper (Juniperus monosperma), over more than a <span class="hlt">decade</span>, leading up to regional-scale die-off of piñon pine trees in response to global <span class="hlt">change</span>-related drought. Piñon leaf water potentials remained substantially below their zero carbon assimilation point for at least 10 months prior to dying, in contrast to those of juniper, which rarely dropped below their zero-assimilation point. These data suggest that piñon mortality was driven by protracted water stress, leading to carbon starvation and associated increases in susceptibility to other disturbances (eg bark beetles), a finding that should help to improve predictions of mortality during drought.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://eric.ed.gov/?q=early+AND+child&pg=5&id=EJ1167963','ERIC'); return false;" href="https://eric.ed.gov/?q=early+AND+child&pg=5&id=EJ1167963"><span>Breastfeeding Duration Predicts Greater Maternal Sensitivity over the Next <span class="hlt">Decade</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>Weaver, Jennifer M.; Schofield, Thomas J.; Papp, Lauren M.</p> <p>2018-01-01</p> <p>The current study represents the first longitudinal investigation of the potential effects of breastfeeding duration on maternal sensitivity over the following <span class="hlt">decade</span>. This study also examined whether infant attachment security at 24 months would mediate longitudinal relations between breastfeeding duration and <span class="hlt">changes</span> in maternal sensitivity over…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://files.eric.ed.gov/fulltext/ED276069.pdf','ERIC'); return false;" href="http://files.eric.ed.gov/fulltext/ED276069.pdf"><span>Media Coverage of International Women's <span class="hlt">Decade</span>: Feminism and Conflict.</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>Cooper, Anne; Davenport, Lucinda</p> <p></p> <p>A study examined <span class="hlt">changes</span> in the treatment of women's issues and feminism from 1975 to 1985--the United Nations (UN) designated "Women's <span class="hlt">Decade</span>"--by two nationally circulated newspapers. The purpose was to find out how much and what kind of news was reported during the three UN World conferences for women held in 1975, 1980, and 1985;…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017EGUGA..1913575P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017EGUGA..1913575P"><span>Calibration of <span class="hlt">decadal</span> ensemble predictions</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Pasternack, Alexander; Rust, Henning W.; Bhend, Jonas; Liniger, Mark; Grieger, Jens; Müller, Wolfgang; Ulbrich, Uwe</p> <p>2017-04-01</p> <p><span class="hlt">Decadal</span> climate predictions are of great socio-economic interest due to the corresponding planning horizons of several political and economic decisions. Due to uncertainties of weather and climate, forecasts (e.g. due to initial condition uncertainty), they are issued in a probabilistic way. One issue frequently observed for probabilistic forecasts is that they tend to be not reliable, i.e. the forecasted probabilities are not consistent with the relative frequency of the associated observed events. Thus, these kind of forecasts need to be re-calibrated. While re-calibration methods for seasonal time scales are available and frequently applied, these methods still have to be adapted for <span class="hlt">decadal</span> time scales and its characteristic problems like climate trend and lead time dependent bias. Regarding this, we propose a method to re-calibrate <span class="hlt">decadal</span> ensemble predictions that takes the above mentioned characteristics into account. Finally, this method will be applied and validated to <span class="hlt">decadal</span> forecasts from the MiKlip system (Germany's initiative for <span class="hlt">decadal</span> prediction).</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2010AGUFM.V43E..01F','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2010AGUFM.V43E..01F"><span>Looking Backward and Forward: A <span class="hlt">Decadal</span> View of Volcanology</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Fink, J. H.</p> <p>2010-12-01</p> <p>In many scientific fields, <span class="hlt">decades</span> are the time intervals of choice for retrospective and prospective reflections and speculations. AGU Session V02 seeks to apply this perspective to the assessment of where volcanology has been since 2000 and where it is headed in the next ten years. Most sciences progress through incremental observational, experimental and theoretical steps, accelerated by the identification of new socially-relevant applications, technological breakthroughs or conceptual insights, and jolted by largely unanticipated events. Volcanology is unusual in the dominant role that unpredictable eruptive observations play in controlling the evolution of the discipline. As a result, the most important constraints on how the field will <span class="hlt">change</span> are virtually unknowable. At a session at the Fall AGU meeting in 2000 on "Volcanology 2010" a dozen talks sought to forecast how volcano science and policy would <span class="hlt">change</span> in the next ten years, focusing on such topics as seismology, petrology, remote sensing, deformation, volcano-tectonic interactions, communications, graduate education, international cooperation, numerical modeling, database querying, and networking of observatories. While progress occurred in many of these areas, what was perhaps the most important influence on volcanology was not mentioned: for the first 9.5 years of the <span class="hlt">decade</span>, there were no eruptions disastrous or novel enough to garner global public or political attention, with associated prioritization by funding agencies. The notable exception was the eruption of Eyjafjallajökull in mid-2010, which captured the western world’s attention due to the magnitude of the disruption, the frustrating inability of scientists to provide guidance, and the fortunate lack of casualties. We can expect continuing technical advances in all aspects of geoscience to improve the understanding of volcanic processes in the coming <span class="hlt">decade</span>. However, another natural disaster in 2010 might hold more relevance for how</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/26017453','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/26017453"><span>Ocean impact on <span class="hlt">decadal</span> Atlantic climate variability revealed by sea-level observations.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>McCarthy, Gerard D; Haigh, Ivan D; Hirschi, Joël J-M; Grist, Jeremy P; Smeed, David A</p> <p>2015-05-28</p> <p><span class="hlt">Decadal</span> variability is a notable feature of the Atlantic Ocean and the climate of the regions it influences. Prominently, this is manifested in the Atlantic Multidecadal Oscillation (AMO) in sea surface temperatures. Positive (negative) phases of the AMO coincide with warmer (colder) North Atlantic sea surface temperatures. The AMO is linked with <span class="hlt">decadal</span> climate fluctuations, such as Indian and Sahel rainfall, European summer precipitation, Atlantic hurricanes and variations in global temperatures. It is widely believed that ocean circulation drives the phase <span class="hlt">changes</span> of the AMO by controlling ocean heat content. However, there are no direct observations of ocean circulation of sufficient length to support this, leading to questions about whether the AMO is controlled from another source. Here we provide observational evidence of the widely hypothesized link between ocean circulation and the AMO. We take a new approach, using sea level along the east coast of the United States to estimate ocean circulation on <span class="hlt">decadal</span> timescales. We show that ocean circulation responds to the first mode of Atlantic atmospheric forcing, the North Atlantic Oscillation, through circulation <span class="hlt">changes</span> between the subtropical and subpolar gyres--the intergyre region. These circulation <span class="hlt">changes</span> affect the <span class="hlt">decadal</span> evolution of North Atlantic heat content and, consequently, the phases of the AMO. The Atlantic overturning circulation is declining and the AMO is moving to a negative phase. This may offer a brief respite from the persistent rise of global temperatures, but in the coupled system we describe, there are compensating effects. In this case, the negative AMO is associated with a continued acceleration of sea-level rise along the northeast coast of the United States.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/27280629','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/27280629"><span>Resilience of <span class="hlt">Key</span> Biological Parameters of the Senegalese Flat Sardinella to Overfishing and Climate <span class="hlt">Change</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Ba, Kamarel; Thiaw, Modou; Lazar, Najih; Sarr, Alassane; Brochier, Timothée; Ndiaye, Ismaïla; Faye, Alioune; Sadio, Oumar; Panfili, Jacques; Thiaw, Omar Thiom; Brehmer, Patrice</p> <p>2016-01-01</p> <p>The stock of the Senegalese flat sardinella, Sardinella maderensis, is highly exploited in Senegal, West Africa. Its growth and reproduction parameters are <span class="hlt">key</span> biological indicators for improving fisheries management. This study reviewed these parameters using landing data from small-scale fisheries in Senegal and literature information dated back more than 25 years. Age was estimated using length-frequency data to calculate growth parameters and assess the growth performance index. With global climate <span class="hlt">change</span> there has been an increase in the average sea surface temperature along the Senegalese coast but the length-weight parameters, sex ratio, size at first sexual maturity, period of reproduction and condition factor of S. maderensis have not <span class="hlt">changed</span> significantly. The above parameters of S. maderensis have hardly <span class="hlt">changed</span>, despite high exploitation and fluctuations in environmental conditions that affect the early development phases of small pelagic fish in West Africa. This lack of plasticity of the species regarding of the biological parameters studied should be considered when planning relevant fishery management plans.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://rosap.ntl.bts.gov/view/dot/12198','DOTNTL'); return false;" href="https://rosap.ntl.bts.gov/view/dot/12198"><span>Climate <span class="hlt">change</span> effects on central New Mexico's land use, transportation system and <span class="hlt">key</span> natural resources : task 1.1 memo.</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>2014-12-01</p> <p>This report summarizes potential climate <span class="hlt">change</span> effects on the availability of water, land use, transportation infrastructure, and <span class="hlt">key</span> natural resources in central New Mexico. This work is being done as part of the Interagency Transportation, Land Us...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/27573049','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/27573049"><span><span class="hlt">Decadal</span>-Scale Forecasting of Climate Drivers for Marine Applications.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Salinger, J; Hobday, A J; Matear, R J; O'Kane, T J; Risbey, J S; Dunstan, P; Eveson, J P; Fulton, E A; Feng, M; Plagányi, É E; Poloczanska, E S; Marshall, A G; Thompson, P A</p> <p></p> <p>Climate influences marine ecosystems on a range of time scales, from weather-scale (days) through to climate-scale (hundreds of years). Understanding of interannual to <span class="hlt">decadal</span> climate variability and impacts on marine industries has received less attention. Predictability up to 10 years ahead may come from large-scale climate modes in the ocean that can persist over these time scales. In Australia the <span class="hlt">key</span> drivers of climate variability affecting the marine environment are the Southern Annular Mode, the Indian Ocean Dipole, the El Niño/Southern Oscillation, and the Interdecadal Pacific Oscillation, each has phases that are associated with different ocean circulation patterns and regional environmental variables. The roles of these drivers are illustrated with three case studies of extreme events-a marine heatwave in Western Australia, a coral bleaching of the Great Barrier Reef, and flooding in Queensland. Statistical and dynamical approaches are described to generate forecasts of climate drivers that can subsequently be translated to useful information for marine end users making decisions at these time scales. Considerable investment is still needed to support <span class="hlt">decadal</span> forecasting including improvement of ocean-atmosphere models, enhancement of observing systems on all scales to support initiation of forecasting models, collection of important biological data, and integration of forecasts into decision support tools. Collaboration between forecast developers and marine resource sectors-fisheries, aquaculture, tourism, biodiversity management, infrastructure-is needed to support forecast-based tactical and strategic decisions that reduce environmental risk over annual to <span class="hlt">decadal</span> time scales. © 2016 Elsevier Ltd. All rights reserved.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://eric.ed.gov/?q=DISEASES+AND+OF+AND+TRANSMISSION+AND+SEXUAL&pg=2&id=EJ873699','ERIC'); return false;" href="https://eric.ed.gov/?q=DISEASES+AND+OF+AND+TRANSMISSION+AND+SEXUAL&pg=2&id=EJ873699"><span>Mobilizing Communities around HIV Prevention for Youth: How Three Coalitions Applied <span class="hlt">Key</span> Strategies to Bring about Structural <span class="hlt">Changes</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>Chutuape, Kate S.; Willard, Nancy; Sanchez, Kenia; Straub, Diane M.; Ochoa, Tara N.; Howell, Kourtney; Rivera, Carmen; Ramos, Ibrahim; Ellen, Jonathan M.</p> <p>2010-01-01</p> <p>Increasingly, HIV prevention efforts must focus on altering features of the social and physical environment to reduce risks associated with HIV acquisition and transmission. Community coalitions provide a vehicle for bringing about sustainable structural <span class="hlt">changes</span>. This article shares lessons and <span class="hlt">key</span> strategies regarding how three community…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2006CorRe..25..287H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2006CorRe..25..287H"><span>Fragment generation, survival, and attachment of Dictyota spp. at Conch Reef in the Florida <span class="hlt">Keys</span>, USA</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Herren, L. W.; Walters, L. J.; Beach, K. S.</p> <p>2006-05-01</p> <p>During the past <span class="hlt">decade</span>, the relative abundance of the brown macroalgae Dictyota spp. has been high in the Florida <span class="hlt">Keys</span>. Recent studies have shown that members of this genus successfully reproduce via vegetative fragmentation. To investigate the importance of fragmentation on the reef community, this study examined: (1) the degree of epiphytism on benthic organisms, (2) the rate of fragment production through fish foraging activities, (3) the likelihood of fragment entanglement, and (4) the fragment attachment and success rate. It was found that reef fish contributed substantially to the fragment pool; furthermore, most fish-produced fragments produced rhizoids and attached to sand grains within 24 h in the field. Fragments of Dictyota spp. most commonly became entangled around and then attached themselves to the green alga Halimeda tuna, and other Dictyota spp. These results suggest that vegetative fragmentation of Dictyota spp. plays an important role in the <span class="hlt">changing</span> community structure on the Florida <span class="hlt">Keys</span> reef tract.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=20150008549&hterms=purpose+science&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D50%26Ntt%3Dpurpose%2Bscience','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=20150008549&hterms=purpose+science&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D50%26Ntt%3Dpurpose%2Bscience"><span>Solar System Planetary Science <span class="hlt">Decadal</span> Survey and Missions in the Next <span class="hlt">Decade</span>, 2013-2022</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Reh, Kim</p> <p>2011-01-01</p> <p>In 2010, the National Research Council Space Studies Board established a <span class="hlt">decadal</span> survey committee to develop a comprehensive science, mission, and technology strategy for planetary science that updates and extends the Board's 2003 Solar System Exploration <span class="hlt">Decadal</span> Survey, "New Frontiers in the Solar System: An Integrated Exploration Strategy." The scope of the survey encompasses the inner planets (Mercury, Venus, and Mars), the Earth's Moon, the giant planets (Jupiter, Saturn, Uranus, and Neptune), the moons of the giant planets, dwarf planets and small bodies, primitive bodies including comets and Kuiper Belt objects, and astrobiology. Over this past year, the <span class="hlt">decadal</span> survey committee has interacted with the broad solar system science community to determine the current state of knowledge and to identify the most important scientific questions expected to face the community during the interval 2013-2022. The survey has identified candidate missions that address the most important science questions and has conducted, through NASA sponsorship, concept studies to assess the cost of such missions as well as technology needs. The purpose of this paper is to provide an overview of the 2012 Solar System Planetary Science <span class="hlt">Decadal</span> Survey study approach and missions that were studied for implementation in the upcoming <span class="hlt">decade</span>. Final results of the <span class="hlt">decadal</span> survey, including studies that were completed and the specific science, programmatic, and technology recommendations will be disclosed publically in the spring of 2011 and are not the subject of this paper.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70010032','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70010032"><span>Near-<span class="hlt">decadal</span> <span class="hlt">changes</span> in nitrate and pesticide concentrations in the South Platte River alluvial aquifer, 1993-2004</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Paschke, S.S.; Schaffrath, K.R.; Mashbum, S.L.</p> <p>2008-01-01</p> <p>The lower South Platte River basin of Colorado and Nebraska is an area of intense agriculture supported by surface-water diversions from the river and ground-water pumping from a valley-fill alluvial aquifer. Two well networks consisting of 45 wells installed in the South Platte alluvial aquifer were sampled in the early 1990s and again in the early 2000s to examine near-<span class="hlt">decadal</span> ground-water quality <span class="hlt">changes</span> in irrigated agricultural areas. Ground-water age generally increases and dissolved-oxygen content decreases with distance along flow paths and with depdi below the water table, and denitrification is an important natural mitigation mechanism for nitrate in downgradient areas. Ground-water travel time from upland areas to the river ranges from 12 to 31 yr on the basis of apparent ground-water ages. Ground-water nitrate concentrations for agricultural land-use wells increased significantly for oxidized samples over the <span class="hlt">decade</span>, and nitrogen isotope ratios for oxidized samples indicate synthetic fertilizer as the predominant nitrate source. Ground-water concentrations of atrazine, DEA, and prometon decreased significandy. The decrease in pesticide concentrations and a significant increase in the ratio of DEA to atrazine suggest decreases in pesticide concentrations are likely caused by local decreases in application rates and/or degradation processes and that atrazine degradation is promoted by oxidizing conditions. The difference between results for oxidizing and nitrate-reducing conditions indicates redox state is an important variable to consider when evaluating ground-water quality trends for redox-sensitive constituents such as nitrate and pesticides in the South Platte alluvial aquifer. Copyright ?? 2008 by the American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America. All rights reserved.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=19810048508&hterms=information+technology+development&qs=N%3D0%26Ntk%3DAll%26Ntx%3Dmode%2Bmatchall%26Ntt%3Dinformation%2Btechnology%2Bdevelopment','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=19810048508&hterms=information+technology+development&qs=N%3D0%26Ntk%3DAll%26Ntx%3Dmode%2Bmatchall%26Ntt%3Dinformation%2Btechnology%2Bdevelopment"><span>The information systems heritage. [overview of technology developments over past five <span class="hlt">decades</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Kurzhals, P. R.; Bricker, R. W.; Jensen, A. S.; Smith, A. T.</p> <p>1981-01-01</p> <p>This paper addresses <span class="hlt">key</span> developments in the evolution of information systems over the past five <span class="hlt">decades</span>. Major areas covered include the growth of imaging sensors from such pioneering devices as the iconoscope and orthicon which ushered in television, through a wide range of vidicon tubes, to the solid-state arrays which characterize current systems; the phenomenal expansion of electronic communications from telegraph and telephone wires, through the introduction of broadcast and microwave relay services, to the present era of worldwide satellite communications and data networks; and the <span class="hlt">key</span> role of digital computers from their ancient precursors like the abacus and the mechanical calculating engines, through the appearance of the first large-scale electronic computers and their transistorized successors, to the rapid proliferation of miniaturized processors which impact every aspect of aerospace systems today.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=20010078968&hterms=landfill&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D10%26Ntt%3Dlandfill','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=20010078968&hterms=landfill&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D10%26Ntt%3Dlandfill"><span>Contribution of <span class="hlt">Changing</span> Sources and Sinks to the Growth Rate of Atmospheric Methane Concentrations for the Last Two <span class="hlt">Decades</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Matthews, Elaine; Walter, B.; Bogner, J.; Sarma, D.; Portmey, G.; Travis, Larry (Technical Monitor)</p> <p>2001-01-01</p> <p>In situ measurements of atmospheric methane concentrations begun in the early 1980s show <span class="hlt">decadal</span> trends, as well as large interannual variations, in growth rate. Recent research indicates that while wetlands can explain several of the large growth anomalies for individual years, the <span class="hlt">decadal</span> trend may be the combined effect of increasing sinks, due to increases in tropospheric OH, and stabilizing sources. We discuss new 20-year histories of annual, global source strengths for all major methane sources, i.e., natural wetlands, rice cultivation, ruminant animals, landfills, fossil fuels, and biomass burning. We also present estimates of the temporal pattern of the sink required to reconcile these sources and atmospheric concentrations over this time period. Analysis of the individual emission sources, together with model-derived estimates of the OH sink strength, indicates that the growth rate of atmospheric methane observed over the last 20 years can only be explained by a combination of <span class="hlt">changes</span> in source emissions and an increasing tropospheric sink. Direct validation of the global sources and the terrestrial sink is not straightforward, in part because some sources/sinks are relatively small and diffuse (e.g., landfills and soil consumption), as well as because the atmospheric record integrates multiple and substantial sources and tropospheric sinks in regions such as the tropics. We discuss ways to develop and test criteria for rejecting and/or accepting a suite of scenarios for the methane budget.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.usgs.gov/fs/2015/3062/pdf/fs20153062.pdf','USGSPUBS'); return false;" href="https://pubs.usgs.gov/fs/2015/3062/pdf/fs20153062.pdf"><span><span class="hlt">Changing</span> arctic ecosystems—What is causing the rapid increase of snow geese in northern Alaska?</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Hupp, Jerry W.; Ward, David H.; Whalen, Mary E.; Pearce, John M.</p> <p>2015-09-10</p> <p>Through the <span class="hlt">Changing</span> Arctic Ecosystems (CAE) initiative, the U.S. Geological Survey (USGS) informs <span class="hlt">key</span> resource management decisions for Arctic Alaska by providing scientific information on current and future ecosystem response to a warming climate. The Arctic Coastal Plain (ACP) of northern Alaska is a <span class="hlt">key</span> study area within the USGS CAE initiative. This region has experienced a warming trend over the past <span class="hlt">decades</span>, leading to decreased sea ice, permafrost thaw, and an advancement of spring phenology. The number of birds on the ACP also is <span class="hlt">changing</span>, marked by increased populations of the four species of geese that nest in the region. The Snow Goose (Chen caerulescens) is the most rapidly increasing of these species. USGS CAE research is quantifying these <span class="hlt">changes</span> and their implications for management agencies.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3491282','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3491282"><span><span class="hlt">Changing</span> trends in the prevalence of blindness and visual impairment in a rural district of India: Systematic observations over a <span class="hlt">decade</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>Khanna, Rohit C; Marmamula, Srinivas; Krishnaiah, Sannapaneni; Giridhar, Pyda; Chakrabarti, Subhabrata; Rao, Gullapalli N</p> <p>2012-01-01</p> <p>Context: Globally, limited data are available on <span class="hlt">changing</span> trends of blindness from a single region. Aims: To report the <span class="hlt">changing</span> trends in the prevalence of blindness, visual impairment (VI), and visual outcomes of cataract surgery in a rural district of Andhra Pradesh, India, over period of one <span class="hlt">decade</span>. Settings and Design: Rural setting; cross-sectional study. Materials and Methods: Using a validated Rapid Assessment of Cataract Surgical Services (RACSS) method, population-based, cross-sectional survey was done in a rural district in the state of Andhra Pradesh, India. Two-stage sampling procedure was used to select participants ≥50 years of age. Further, a comparative analysis was done with participants ≥50 years from the previously concluded Andhra Pradesh Eye Disease Study (APEDS) study, who belonged to the same district. Statistical Analysis: Done using 11th version of Stata. Results: Using RACSS, 2160/2300 (93.9%) participants were examined as compared with the APEDS dataset (n=521). Age and sex adjusted prevalence of blindness in RACSS and APEDS was 8% (95% CI, 6.9–9.1%) and 11% (95% CI, 8.3–13.7%), while that of VI was 13.6% (95% CI, 12.2–15.1%) and 40.3% (95% CI, 36.1–44.5%), respectively. Cataract was the major cause of blindness in both the studies. There was a significant reduction in blindness following cataract surgery as observed through RACSS (17.3%; 95% CI, 13.5–21.8%) compared with APEDS (34%; 95% CI, 20.9–49.3%). Conclusion: There was a significant reduction in prevalence of blindness and VI in this rural district of India over a <span class="hlt">decade</span>. PMID:22944766</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/22944766','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/22944766"><span><span class="hlt">Changing</span> trends in the prevalence of blindness and visual impairment in a rural district of India: systematic observations over a <span class="hlt">decade</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Khanna, Rohit C; Marmamula, Srinivas; Krishnaiah, Sannapaneni; Giridhar, Pyda; Chakrabarti, Subhabrata; Rao, Gullapalli N</p> <p>2012-01-01</p> <p>Context : Globally, limited data are available on <span class="hlt">changing</span> trends of blindness from a single region. Aims : To report the <span class="hlt">changing</span> trends in the prevalence of blindness, visual impairment (VI), and visual outcomes of cataract surgery in a rural district of Andhra Pradesh, India, over period of one <span class="hlt">decade</span>. Settings and Design : Rural setting; cross-sectional study. Materials and Methods : Using a validated Rapid Assessment of Cataract Surgical Services (RACSS) method, population-based, cross-sectional survey was done in a rural district in the state of Andhra Pradesh, India. Two-stage sampling procedure was used to select participants ≥50 years of age. Further, a comparative analysis was done with participants ≥50 years from the previously concluded Andhra Pradesh Eye Disease Study (APEDS) study, who belonged to the same district. Statistical Analysis : Done using 11 th version of Stata. Results : Using RACSS, 2160/2300 (93.9%) participants were examined as compared with the APEDS dataset (n=521). Age and sex adjusted prevalence of blindness in RACSS and APEDS was 8% (95% CI, 6.9-9.1%) and 11% (95% CI, 8.3-13.7%), while that of VI was 13.6% (95% CI, 12.2-15.1%) and 40.3% (95% CI, 36.1-44.5%), respectively. Cataract was the major cause of blindness in both the studies. There was a significant reduction in blindness following cataract surgery as observed through RACSS (17.3%; 95% CI, 13.5-21.8%) compared with APEDS (34%; 95% CI, 20.9-49.3%). Conclusion : There was a significant reduction in prevalence of blindness and VI in this rural district of India over a <span class="hlt">decade</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20140017824','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20140017824"><span><span class="hlt">Changes</span> in Arctic and Antarctic Sea Ice as a Microcosm of Global Climate <span class="hlt">Change</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Parkinson, Claire L.</p> <p>2014-01-01</p> <p>Polar sea ice is a <span class="hlt">key</span> element of the climate system and has now been monitored through satellite observations for over three and a half <span class="hlt">decades</span>. The satellite observations reveal considerable information about polar ice and its <span class="hlt">changes</span> since the late 1970s, including a prominent downward trend in Arctic sea ice coverage and a much lesser upward trend in Antarctic sea ice coverage, illustrative of the important fact that climate <span class="hlt">change</span> entails spatial contrasts. The decreasing ice coverage in the Arctic corresponds well with contemporaneous Arctic warming and exhibits particularly large decreases in the summers of 2007 and 2012, influenced by both preconditioning and atmospheric conditions. The increasing ice coverage in the Antarctic is not as readily explained, but spatial differences in the Antarctic trends suggest a possible connection with atmospheric circulation <span class="hlt">changes</span> that have perhaps been influenced by the Antarctic ozone hole. The <span class="hlt">changes</span> in the polar ice covers and the issues surrounding those <span class="hlt">changes</span> have many commonalities with broader climate <span class="hlt">changes</span> and their surrounding issues, allowing the sea ice <span class="hlt">changes</span> to be viewed in some important ways as a microcosm of global climate <span class="hlt">change</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/24104436','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/24104436"><span>Nitride micro-LEDs and beyond--a <span class="hlt">decade</span> progress review.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Jiang, H X; Lin, J Y</p> <p>2013-05-06</p> <p>Since their inception, micro-size light emitting diode (µLED) arrays based on III-nitride semiconductors have emerged as a promising technology for a range of applications. This paper provides an overview on a <span class="hlt">decade</span> progresses on realizing III-nitride µLED based high voltage single-chip AC/DC-LEDs without power converters to address the <span class="hlt">key</span> compatibility issue between LEDs and AC power grid infrastructure; and high-resolution solid-state self-emissive microdisplays operating in an active driving scheme to address the need of high brightness, efficiency and robustness of microdisplays. These devices utilize the photonic integration approach by integrating µLED arrays on-chip. Other applications of nitride µLED arrays are also discussed.</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('http://hdl.handle.net/2060/20150021889','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20150021889"><span>WFIRST-AFTA Presentation to the NRC Mid-<span class="hlt">Decadal</span> Panel</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Gehrels, Neil; Grady, Kevin; Ruffa, John; Melton, Mark; Content, Dave; Zhao, Feng</p> <p>2015-01-01</p> <p>Over the past two years, increased funding has enabled significant progress in technology matura1on as well as addi1onal fidelity in the design reference mission. WFIRST with the 2.4-­-m telescope and coronagraph provides an exci1ng science program, superior to that recommended by NWNH and also advances exoplanet imaging technology (the highest ranked medium-­-class NWNH recommenda1on). Great opportunity for astronomy and astrophysics discoveries. Broad community support for WFIRST. <span class="hlt">Key</span> development areas are anchored in a <span class="hlt">decade</span> of investments in JPL's HCIT and GSFC's DCL. Great progress made in pre-­-formula1on, ready for KDP-­-A and launch in mid-­-2020s.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/22330391','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/22330391"><span>Color discrimination across four life <span class="hlt">decades</span> assessed by the Cambridge Colour Test.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Paramei, Galina V</p> <p>2012-02-01</p> <p>Color discrimination was estimated using the Cambridge Colour Test (CCT) in 160 normal trichromats of four life <span class="hlt">decades</span>, 20-59 years of age. For each age cohort, medians and tolerance limits of the CCT parameters are tabulated. Compared across the age cohorts (Kruskal-Wallis test), the Trivector test showed increases in the three vectors, Protan, Deutan, and Tritan, with advancing age; the Ellipses test revealed significant elongation of the major axes of all three ellipses but no <span class="hlt">changes</span> in either the axis ratio or the angle of the ellipse major axis. Multiple comparisons (Mann-Whitney test) between the cohorts of four age <span class="hlt">decades</span> (20+,…,50+) revealed initial benign deterioration of color discrimination in the 40+ <span class="hlt">decade</span>, as an incremental loss of discrimination along the Deutan axis (Trivector test), and in the 50+ <span class="hlt">decade</span>, as an elongation of the major axes of all three ellipses (Ellipses test). © 2012 Optical Society of America</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/20384414','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/20384414"><span>Two-digit number comparison: <span class="hlt">Decade</span>-unit and unit-<span class="hlt">decade</span> produce the same compatibility effect with number words.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Macizo, Pedro; Herrera, Amparo</p> <p>2010-03-01</p> <p>This study explored the processing of 2-digit number words by examining the unit-<span class="hlt">decade</span> compatibility effect in Spanish. Participants were required to choose the larger of 2-digit number words presented in verbal notation. In compatible trials the <span class="hlt">decade</span> and unit comparisons led to the same response (e.g., 53-68) while in incompatible trials the <span class="hlt">decade</span> and unit comparisons led to different responses (e.g., 59-74). Participants were slower on compatible trials as compared to incompatible trials. In Experiments 2 and 3, we evaluated whether the reverse compatibility effect in Spanish was only due to a pure left-to-right encoding which favours the <span class="hlt">decade</span> processing in this language (<span class="hlt">decade</span>-unit order). When participants processed 2-digit number words presented in reverse form (in the unit-<span class="hlt">decade</span> order), the same reverse compatibility effect was found. This pattern of results suggests that participants have learnt a language-dependent process for analysing written numbers which is used irrespective of the specific arrangement of units and <span class="hlt">decades</span> in the comparison task. 2010 APA, all rights reserved.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AdWR..109..236K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AdWR..109..236K"><span>Four <span class="hlt">decades</span> of microwave satellite soil moisture observations: Part 2. Product validation and inter-satellite comparisons</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Karthikeyan, L.; Pan, Ming; Wanders, Niko; Kumar, D. Nagesh; Wood, Eric F.</p> <p>2017-11-01</p> <p>Soil moisture is widely recognized as an important land surface variable that provides a deeper knowledge of land-atmosphere interactions and climate <span class="hlt">change</span>. Space-borne passive and active microwave sensors have become valuable and essential sources of soil moisture observations at global scales. Over the past four <span class="hlt">decades</span>, several active and passive microwave sensors have been deployed, along with the recent launch of two fully dedicated missions (SMOS and SMAP). Signifying the four <span class="hlt">decades</span> of microwave remote sensing of soil moisture, this Part 2 of the two-part review series aims to present an overview of how our knowledge in this field has improved in terms of the design of sensors and their accuracy for retrieving soil moisture. The first part discusses the developments made in active and passive microwave soil moisture retrieval algorithms. We assess the evolution of the products of various sensors over the last four <span class="hlt">decades</span>, in terms of daily coverage, temporal performance, and spatial performance, by comparing the products of eight passive sensors (SMMR, SSM/I, TMI, AMSR-E, WindSAT, AMSR2, SMOS and SMAP), two active sensors (ERS-Scatterometer, MetOp-ASCAT), and one active/passive merged soil moisture product (ESA-CCI combined product) with the International Soil Moisture Network (ISMN) in-situ stations and the Variable Infiltration Capacity (VIC) land surface model simulations over the Contiguous United States (CONUS). In the process, the regional impacts of vegetation conditions on the spatial and temporal performance of soil moisture products are investigated. We also carried out inter-satellite comparisons to study the roles of sensor design and algorithms on the retrieval accuracy. We find that substantial improvements have been made over recent years in this field in terms of daily coverage, retrieval accuracy, and temporal dynamics. We conclude that the microwave soil moisture products have significantly evolved in the last four <span class="hlt">decades</span> and will</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/28261462','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/28261462"><span>Long-term monitoring of tropical alpine habitat <span class="hlt">change</span>, Andean anurans, and chytrid fungus in the Cordillera Vilcanota, Peru: Results from a <span class="hlt">decade</span> of study.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Seimon, Tracie A; Seimon, Anton; Yager, Karina; Reider, Kelsey; Delgado, Amanda; Sowell, Preston; Tupayachi, Alfredo; Konecky, Bronwen; McAloose, Denise; Halloy, Stephan</p> <p>2017-03-01</p> <p>The Cordillera Vilcanota in southern Peru is the second largest glacierized range in the tropics and home to one of the largest high-alpine lakes, Sibinacocha (4,860 m). Here, Telmatobius marmoratus (marbled water frog), Rhinella spinulosa (Andean toad), and Pleurodema marmoratum (marbled four-eyed frog) have expanded their range vertically within the past century to inhabit newly formed ponds created by ongoing deglaciation. These anuran populations, geographically among the highest (5,200-5,400 m) recorded globally, are being impacted by the chytrid fungus Batrachochytrium dendrobatidis ( Bd ), and the disease it causes, chytridiomycosis. In this study, we report results from over a <span class="hlt">decade</span> of monitoring these three anuran species, their habitat, and Bd infection status. Our observations reveal dynamic <span class="hlt">changes</span> in habitat including ongoing rapid deglaciation (18.4 m/year widening of a corridor between retreating glaciers from 2005 to 2015), new pond formation, <span class="hlt">changes</span> in vegetation in amphibian habitat, and widespread occurrence of Bd in amphibians in seven sites. Three of these sites have tested positive for Bd over a 9- to 12-year period. In addition, we observed a widespread reduction in T. marmoratus encounters in the Vilcanota in 2008, 2009, and 2012, while encounters increased in 2013 and 2015. Despite the rapid and dynamic <span class="hlt">changes</span> in habitat under a warming climate, continued presence of Bd in the environment for over a <span class="hlt">decade</span>, and a reduction in one of three anuran species, we document that these anurans continue to breed and survive in this high Andean environment. High variability in anuran encounters across sites and plasticity in these populations across habitats, sites, and years are all factors that could favor repopulation postdecline. Preserving the connectivity of wetlands in the Cordillera Vilcanota is therefore essential in ensuring that anurans continue to breed and adapt as climate <span class="hlt">change</span> continues to reshape the environment.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016cosp...41E.983K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016cosp...41E.983K"><span>Tracking forest cover <span class="hlt">change</span> of Margalla Hills over a period of two <span class="hlt">decades</span> (1992-2011): A remote sensing perspective</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Khalid, Noora; Ullah, Saleem</p> <p>2016-07-01</p> <p>Forests play a critical role in balancing the ecological soundness of a region and in the facilitation of essential forest resources. Depletion of forest cover is a serious environmental problem throughout the world including Pakistan where a striking degradation of forest reserves has been an ecological concern for quite some time. Remote sensing techniques have been used to monitor land use and forest cover <span class="hlt">changes</span>. The present study aims at exploring the potential impacts of climate <span class="hlt">change</span> in the decline of forest reserves on Margalla Hills National Park (MHNP), since it remains the primary culprit behind this depletion. Landsat images for 1992, 2000 and 2011 were manipulated for the spatial and temporal analysis, interpretation and computation of the <span class="hlt">change</span> and shift that has occurred over the past two <span class="hlt">decades</span>. The analysis revealed a great increase in the built-up area, barren soil and agricultural land. Though other classes such as water body, lower vegetation, scrub and conifer forest showed a diminishing trend. The rise in temperature and relative humidity, the depletion in annual precipitation, frequent wild fires and the boost in urbanization and agricultural practices are the climatic conditions and causative agents chiefly responsible for the decline shown by the vegetation of the area. The degrading condition of the forest is below par and requires conservation practices to be carried out in order to avoid ecological disturbances.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/biblio/21036869-history-science-politics-climate-change-role-intergovernmental-panel-climate-change','SCIGOV-STC'); return false;" href="https://www.osti.gov/biblio/21036869-history-science-politics-climate-change-role-intergovernmental-panel-climate-change"><span>A history of the science and politics of climate <span class="hlt">change</span>: the role of the Intergovernmental Panel on Climate <span class="hlt">Change</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>Bolin, B.</p> <p>2007-11-15</p> <p>In response to growing concern about human-induced global climate <span class="hlt">change</span>, the UN Intergovernmental Panel on Climate <span class="hlt">Change</span> (IPCC) was formed in 1988. Written by its first Chairman, this book is a unique overview of the history of the IPCC. It describes and evaluates the intricate interplay between <span class="hlt">key</span> factors in the science and politics of climate <span class="hlt">change</span>, the strategy that has been followed, and the regretfully slow pace in getting to grips with the uncertainties that have prevented earlier action being taken. The book also highlights the emerging conflict between establishing a sustainable global energy system and preventing a seriousmore » <span class="hlt">change</span> in global climate. Contents are: Part I. The Early History of the Climate <span class="hlt">Change</span> Issue: 1. Nineteenth century discoveries; 2. The natural carbon cycle and life on earth; 3. Global research initiatives in meteorology and climatology; 4. Early international assessments of climate <span class="hlt">change</span>; Part II. The Climate <span class="hlt">Change</span> Issue Becomes One of Global Concern: 5. Setting the stage; 6. The scientific basis for a climate convention; 7. Serving the Intergovernmental Negotiating Committee; 8. The Second IPP Assessment Report; 9. In the aftermath of the IPCC Second Assessment; 10. The Kyoto Protocol is agreed and a third assessment begun; 11. A <span class="hlt">decade</span> of hesitance and slow progress; Part III. A Turning Point in Addressing Climate <span class="hlt">Change</span>?: 12. <span class="hlt">Key</span> scientific finding of prime political relevance; 13. Climate <span class="hlt">change</span> and the future global energy supply system; Concluding remarks. 9 figs.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2007AGUSMOS34B..06M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2007AGUSMOS34B..06M"><span>How <span class="hlt">Changing</span> Human Lifestyles are Shaping Europe's Regional Seas</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Mee, L. D.; Lowe, C. D.; Langmead, O.; McQuatters-Gollop, A.; Attrill, M.; Cooper, P.; Gilbert, A.; Knudsen, S.; Garnacho, E.</p> <p>2007-05-01</p> <p>European society is experiencing unprecedented <span class="hlt">changes</span> triggered by expansion of the European Union, the fall of Communism, economic growth and the onset of globalisation. Europe's regional seas, the Baltic, Black Sea, Mediterranean and North-East Atlantic (including the North Sea), provide <span class="hlt">key</span> goods and services to the human population but have suffered from severe degradation in past <span class="hlt">decades</span>. Their integrity as coupled social and ecological systems depends on how humanity will anticipate potential problems and deal with its ecological footprint in the future. We report the outcome of an EU-funded 15-country, 28 institution project entitled European Lifestyles and Marine Ecosystems (ELME). Our studies were designed to inform new EU policy and legislation that incorporates Ecosystem-Based Management. ELME has modelled the <span class="hlt">key</span> relationships between economic and social drivers (D), environmental pressures (P) and <span class="hlt">changes</span> in the state of the environment (S) in Europe's regional seas. We examined four <span class="hlt">key</span> issues in each sea: habitat <span class="hlt">change</span>, eutrophication, chemical pollution and fisheries. We developed conceptual models for each regional sea and employed a novel stochastic modelling technique to examine the interrelationship between <span class="hlt">key</span> components of the conceptual models. We used the models to examine 2-3 <span class="hlt">decade</span> projections of current trends in D, P and S and how a number of alternative development scenarios might modify these trends. These simulations demonstrate the vulnerability of Europe's seas to human pressure. As affluence increases in countries acceding to the EU, so does the demand for marine goods and services. There are `winners' and `losers' amongst marine species; the winners are often species that are opportunistic invaders or those with low economic value. In the case of eutrophication, semi-enclosed seas such as the Baltic or Black Sea are already affected by the `legacy of the past'; nutrients that have accumulated in soils, ground waters and</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014AGUFMGC54A..08F','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014AGUFMGC54A..08F"><span>Variability of western Amazon dry-season precipitation extremes: importance of <span class="hlt">decadal</span> fluctuations and implications for predictability</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Fernandes, K.; Baethgen, W.; Verchot, L. V.; Giannini, A.; Pinedo-Vasquez, M.</p> <p>2014-12-01</p> <p>A complete assessment of climate <span class="hlt">change</span> projections requires understanding the combined effects of <span class="hlt">decadal</span> variability and long-term trends and evaluating the ability of models to simulate them. The western Amazon severe droughts of the 2000s were the result of a modest drying trend enhanced by reduced moisture transport from the tropical Atlantic. Most of the WA dry-season precipitation <span class="hlt">decadal</span> variability is attributable to <span class="hlt">decadal</span> fluctuations of the north-south gradient (NSG) in Atlantic sea surface temperature (SST). The observed WA and NSG <span class="hlt">decadal</span> co-variability is well reproduced in Global Climate Models (GCMs) pre-industrial control (PIC) and historical (HIST) experiments that were part of the Intergovernmental Panel on Climate <span class="hlt">Change</span> fifth assessment report (IPCC-AR5). This suggests that unforced or natural climate variability, characteristic of the PIC simulations, determines the nature of this coupling, as the results from HIST simulations (forced with greenhouse gases (GHG) and natural and anthropogenic aerosols) are comparable in magnitude and spatial distribution. <span class="hlt">Decadal</span> fluctuation in the NSG also determines shifts in the probability of repeated droughts and pluvials in WA, as there is a 65% chance of 3 or more years of droughts per <span class="hlt">decade</span> when NSG>0 compared to 18% when NSG<0. The HIST and PIC model simulations also reproduce the observed shifts in probability distribution of droughts and pluvials as a function of the NSG <span class="hlt">decadal</span> phase, suggesting there is great potential for <span class="hlt">decadal</span> predictability based on GCMs. Persistence of the current NSG positive phase may lead to continuing above normal frequencies of western Amazon dry-season droughts.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017DSRI..119...58A','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017DSRI..119...58A"><span>Seasonal to multi-<span class="hlt">decadal</span> trends in apparent optical properties in the Sargasso Sea</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Allen, James G.; Nelson, Norman B.; Siegel, David A.</p> <p>2017-01-01</p> <p>Multi-<span class="hlt">decadal</span>, monthly observations of optical and biogeochemical properties, made as part of the Bermuda Bio-Optics Project (BBOP) at the Bermuda Atlantic Time-series Study (BATS) site in the Sargasso Sea, allow for the examination of temporal trends in vertical light attenuation and their potential controls. Trends in the magnitude of the diffuse attenuation coefficient, Kd(λ), and a proxy for its spectral shape reflect <span class="hlt">changes</span> in phytoplankton and chromophoric dissolved organic matter (CDOM) characteristics. The length and methodological consistency of this time series provide an excellent opportunity to extend analyses of seasonal cycles of apparent optical properties to interannual and <span class="hlt">decadal</span> time scales. Here, we characterize <span class="hlt">changes</span> in the magnitude and spectral shape proxy of diffuse attenuation coefficient spectra and compare them to available biological and optical data from the BATS time series program. The time series analyses reveal a 1.01%±0.18% annual increase of the magnitude of the diffuse attenuation coefficient at 443 nm over the upper 75 m of the water column while showing no significant <span class="hlt">change</span> in selected spectral characteristics over the study period. These and other observations indicate that <span class="hlt">changes</span> in phytoplankton rather than <span class="hlt">changes</span> in CDOM abundance are the primary driver for the diffuse attenuation trends on multi-year timescales for this region. Our findings are inconsistent with previous <span class="hlt">decadal</span>-scale global ocean water clarity and global satellite ocean color analyses yet are consistent with recent analyses of the BATS time series and highlight the value of long-term consistent observation at ocean time series sites.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/19965473','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/19965473"><span>Climate-driven basin-scale <span class="hlt">decadal</span> oscillations of oceanic phytoplankton.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Martinez, Elodie; Antoine, David; D'Ortenzio, Fabrizio; Gentili, Bernard</p> <p>2009-11-27</p> <p>Phytoplankton--the microalgae that populate the upper lit layers of the ocean--fuel the oceanic food web and affect oceanic and atmospheric carbon dioxide levels through photosynthetic carbon fixation. Here, we show that multidecadal <span class="hlt">changes</span> in global phytoplankton abundances are related to basin-scale oscillations of the physical ocean, specifically the Pacific <span class="hlt">Decadal</span> Oscillation and the Atlantic Multidecadal Oscillation. This relationship is revealed in approximately 20 years of satellite observations of chlorophyll and sea surface temperature. Interaction between the main pycnocline and the upper ocean seasonal mixed layer is one mechanism behind this correlation. Our findings provide a context for the interpretation of contemporary <span class="hlt">changes</span> in global phytoplankton and should improve predictions of their future evolution with climate <span class="hlt">change</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016NatGe...9..871Z','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016NatGe...9..871Z"><span>Impact of <span class="hlt">decadal</span> cloud variations on the Earth's energy budget</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Zhou, Chen; Zelinka, Mark D.; Klein, Stephen A.</p> <p>2016-12-01</p> <p>Feedbacks of clouds on climate <span class="hlt">change</span> strongly influence the magnitude of global warming. Cloud feedbacks, in turn, depend on the spatial patterns of surface warming, which vary on <span class="hlt">decadal</span> timescales. Therefore, the magnitude of the <span class="hlt">decadal</span> cloud feedback could deviate from the long-term cloud feedback. Here we present climate model simulations to show that the global mean cloud feedback in response to <span class="hlt">decadal</span> temperature fluctuations varies dramatically due to time variations in the spatial pattern of sea surface temperature. We find that cloud anomalies associated with these patterns significantly modify the Earth's energy budget. Specifically, the <span class="hlt">decadal</span> cloud feedback between the 1980s and 2000s is substantially more negative than the long-term cloud feedback. This is a result of cooling in tropical regions where air descends, relative to warming in tropical ascent regions, which strengthens low-level atmospheric stability. Under these conditions, low-level cloud cover and its reflection of solar radiation increase, despite an increase in global mean surface temperature. These results suggest that sea surface temperature pattern-induced low cloud anomalies could have contributed to the period of reduced warming between 1998 and 2013, and offer a physical explanation of why climate sensitivities estimated from recently observed trends are probably biased low.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/17455476','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/17455476"><span>Nanophase <span class="hlt">change</span> for data storage applications.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Shi, L P; Chong, T C</p> <p>2007-01-01</p> <p>Phase <span class="hlt">change</span> materials are widely used for date storage. The most widespread and important applications are rewritable optical disc and Phase <span class="hlt">Change</span> Random Access Memory (PCRAM), which utilizes the light and electric induced phase <span class="hlt">change</span> respectively. For <span class="hlt">decades</span>, miniaturization has been the major driving force to increase the density. Now the working unit area of the current data storage media is in the order of nano-scale. On the nano-scale, extreme dimensional and nano-structural constraints and the large proportion of interfaces will cause the deviation of the phase <span class="hlt">change</span> behavior from that of bulk. Hence an in-depth understanding of nanophase <span class="hlt">change</span> and the related issues has become more and more important. Nanophase <span class="hlt">change</span> can be defined as: phase <span class="hlt">change</span> at the scale within nano range of 100 nm, which is size-dependent, interface-dominated and surrounding materials related. Nanophase <span class="hlt">change</span> can be classified into two groups, thin film related and structure related. Film thickness and clapping materials are <span class="hlt">key</span> factors for thin film type, while structure shape, size and surrounding materials are critical parameters for structure type. In this paper, the recent development of nanophase <span class="hlt">change</span> is reviewed, including crystallization of small element at nano size, thickness dependence of crystallization, effect of clapping layer on the phase <span class="hlt">change</span> of phase <span class="hlt">change</span> thin film and so on. The applications of nanophase <span class="hlt">change</span> technology on data storage is introduced, including optical recording such as super lattice like optical disc, initialization free disc, near field, super-RENS, dual layer, multi level, probe storage, and PCRAM including, superlattice-like structure, side edge structure, and line type structure. Future <span class="hlt">key</span> research issues of nanophase <span class="hlt">change</span> are also discussed.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFM.H43O..08S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFM.H43O..08S"><span><span class="hlt">Changes</span> in precipitation-streamflow transformation around the world: interdecadal variability and trends.</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Saft, M.; Peel, M. C.; Andreassian, V.; Parajka, J.; Coxon, G.; Freer, J. E.; Woods, R. A.</p> <p>2017-12-01</p> <p>Accurate prediction of hydrologic response to potentially <span class="hlt">changing</span> climatic forcing is a <span class="hlt">key</span> current challenge in hydrology. Recent studies exploring <span class="hlt">decadal</span> to multidecadal climate drying in the African Sahel and south-eastern and south-western Australia demonstrated that long dry periods also had an indirect cumulative impact on streamflow via altered catchment biophysical properties. As a result, hydrologic response to persisting <span class="hlt">change</span> in climatic conditions, i.e. precipitation, cannot be confidently inferred from the hydrologic response to short-term interannual climate fluctuations of similar magnitude. This study aims to characterise interdecadal <span class="hlt">changes</span> in precipitation-runoff conversion processes globally. The analysis is based on long continuous records from near-natural baseline catchments in North America, Europe, and Australia. We used several complimentary metrics characterising precipitation-runoff relationship to assess how partitioning <span class="hlt">changed</span> over recent <span class="hlt">decades</span>. First, we explore the hypothesis that during particularly dry or wet <span class="hlt">decades</span> the precipitation elasticity of streamflow increases over what can be expected from inter-annual variability. We found this hypothesis holds for both wet and dry periods in some regions, but not everywhere. Interestingly, trend-like behaviour in the precipitation-runoff partitioning, unrelated to precipitation <span class="hlt">changes</span>, offset the impact of persisting precipitation <span class="hlt">change</span> in some regions. Therefore, in the second part of this study we explored longer-term trends in precipitation-runoff partitioning, and related them to climate and streamflow <span class="hlt">changes</span>. We found significant <span class="hlt">changes</span> in precipitation-runoff relationship around the world, which implies that runoff response to a given precipitation can vary over <span class="hlt">decades</span> even in near-natural catchments. When significant <span class="hlt">changes</span> occur, typically less runoff is generated for a given precipitation over time - even when precipitation is increasing. We discuss the consistency</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://eric.ed.gov/?q=governance+AND+meta&pg=2&id=EJ1042013','ERIC'); return false;" href="https://eric.ed.gov/?q=governance+AND+meta&pg=2&id=EJ1042013"><span>Higher Education Research Agendas for the Coming <span class="hlt">Decade</span>: A UK Perspective on the Policy-Research Nexus</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>Middlehurst, Robin</p> <p>2014-01-01</p> <p>From the perspective of the UK, this paper addresses two main themes. It presents a higher education (HE) research agenda for the next <span class="hlt">decade</span> linked to <span class="hlt">key</span> policy challenges and reflects on the dynamics of the research-policy landscape. The paper begins by identifying four dimensions of the UK that will continue to be important as a focus for…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2009AGUFM.P52A..09B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2009AGUFM.P52A..09B"><span>Rings Research in the Next <span class="hlt">Decade</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Burns, J. A.; Tiscareno, M. S.</p> <p>2009-12-01</p> <p>The study of planetary ring systems forms a <span class="hlt">key</span> component of planetary science for several reasons: 1) The evolution and current states of planets and their satellites are affected in many ways by rings, while 2) conversely, properties of planets and moons and other solar system populations are revealed by their effects on rings; 3) highly structured and apparently delicate ring systems may be bellwethers, constraining various theories of the origin and evolution of their entire planetary system; and finally, 4) planetary rings provide an easily observable analogue to other astrophysical disk systems, enabling real “ground truth” results applicable to disks much more remote in space and/or time, including proto-planetary disks, circum-stellar disks, and even galaxies. Significant advances have been made in rings science in the past <span class="hlt">decade</span>. The highest-priority rings research recommendations of the last Planetary Science <span class="hlt">Decadal</span> Survey were to operate and extend the Cassini orbiter mission at Saturn; this has been done with tremendous success, accounting for much of the progress made on <span class="hlt">key</span> science questions, as we will describe. Important progress in understanding the rings of Saturn and other planets has also come from Earth-based observational and theoretical work, again as prioritized by the last <span class="hlt">Decadal</span> Survey. However, much important work remains to be done. At Saturn, the Cassini Solstice Mission must be brought to a successful completion. Priority should also be placed on sending spacecraft to Neptune and/or Uranus, now unvisited for more than 20 years. At Jupiter and Pluto, opportunities afforded by visiting spacecraft capable of studying rings should be exploited. On Earth, the need for continued research and analysis remains strong, including in-depth analysis of rings data already obtained, numerical and theoretical modeling work, laboratory analysis of materials and processes analogous to those found in the outer solar system, and continued Earth</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/28771931','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/28771931"><span>Microbial technology with major potentials for the urgent environmental needs of the next <span class="hlt">decades</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Verstraete, Willy; De Vrieze, Jo</p> <p>2017-09-01</p> <p>Several needs in the context of the water-energy-food nexus will become more prominent in the next <span class="hlt">decades</span>. It is crucial to delineate these challenges and to find opportunities for innovative microbial technologies in the framework of sustainability and climate <span class="hlt">change</span>. Here, we focus on four <span class="hlt">key</span> issues, that is the imbalance in the nitrogen cycle, the diffuse emission of methane, the necessity for carbon capture and the deterioration of freshwater reserves. We suggest a set of microbial technologies to deal with each of these issues, such as (i) the production of microbial protein as food and feed, (ii) the control of methanogenic archaea and better use of methanotrophic consortia, (iii) the avoidance of nitrification and (iv) the upgrading of CO 2 to microbial bioproducts. The central message is that instead of using crude methods to exploit microorganisms for degradations, the potentials of the microbiomes should be used to create processes and products that fit the demands of the cyclic market economy. © 2017 The Authors. Microbial Biotechnology published by Society for Applied Microbiology and John Wiley & Sons Ltd.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/26989826','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/26989826"><span>Heat, Human Performance, and Occupational Health: A <span class="hlt">Key</span> Issue for the Assessment of Global Climate <span class="hlt">Change</span> Impacts.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Kjellstrom, Tord; Briggs, David; Freyberg, Chris; Lemke, Bruno; Otto, Matthias; Hyatt, Olivia</p> <p>2016-01-01</p> <p>Ambient heat exposure is a well-known health hazard, which reduces human performance and work capacity at heat levels already common in tropical and subtropical areas. Various health problems have been reported. Increasing heat exposure during the hottest seasons of each year is a <span class="hlt">key</span> feature of global climate <span class="hlt">change</span>. Heat exhaustion and reduced human performance are often overlooked in climate <span class="hlt">change</span> health impact analysis. Later this century, many among the four billion people who live in hot areas worldwide will experience significantly reduced work capacity owing to climate <span class="hlt">change</span>. In some areas, 30-40% of annual daylight hours will become too hot for work to be carried out. The social and economic impacts will be considerable, with global gross domestic product (GDP) losses greater than 20% by 2100. The analysis to date is piecemeal. More analysis of climate <span class="hlt">change</span>-related occupational health impact assessments is greatly needed.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015JGRC..120.4226K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015JGRC..120.4226K"><span><span class="hlt">Decadal</span> and seasonal <span class="hlt">changes</span> in temperature, salinity, nitrate, and chlorophyll in inshore and offshore waters along southeast Australia</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Kelly, Paige; Clementson, Lesley; Lyne, Vincent</p> <p>2015-06-01</p> <p>Sixty years of oceanographic in situ data at Port Hacking (34°S) and Maria Island (42°S) and 15 years of satellite-derived chlorophyll a (chl a) in inshore and offshore waters of southeast Australia show <span class="hlt">changes</span> in the seasonality and trend of water properties consistent with long-term intensification and southerly extensions of East Australian Current (EAC) water. <span class="hlt">Decadal</span> analyses reveal that the EAC extension water at Maria Island increased gradually from the 1940s to 1980s, followed by a rapid increase since the 1990s. This acceleration coincided with enhanced winter nitrate, implying increased injections of subantarctic water at Maria Island. Satellite-derived chl a at six coastal sites and offshore companion sites in the western Tasman Sea showed significant inshore-offshore variations in seasonal cycle and long-term trend. After 2004-2005, the Maria Island seasonal cycle became increasingly similar to those of Bass Strait and St. Helens, suggesting that the EAC extension water was extending further southward. Comparative analyses of inshore-offshore sites showed that the presence of EAC extension water declined offshore. Seasonal cycles at Maria Island show a recent shift away from the traditional spring bloom, toward increased winter biomass, and enhanced primary productivity consistent with extensions of warm, energetic EAC extension water and more frequent injections of cooler, fresher nitrate-replete waters. Overall, we find complex temporal, latitudinal, and inshore-offshore <span class="hlt">changes</span> in multiple water masses, particularly at Maria Island, and <span class="hlt">changes</span> in primary productivity that will profoundly impact fisheries and ecosystems.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5467267','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5467267"><span>Tightening of tropical ascent and high clouds <span class="hlt">key</span> to precipitation <span class="hlt">change</span> in a warmer climate</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Su, Hui; Jiang, Jonathan H.; Neelin, J. David; Shen, T. Janice; Zhai, Chengxing; Yue, Qing; Wang, Zhien; Huang, Lei; Choi, Yong-Sang; Stephens, Graeme L.; Yung, Yuk L.</p> <p>2017-01-01</p> <p>The <span class="hlt">change</span> of global-mean precipitation under global warming and interannual variability is predominantly controlled by the <span class="hlt">change</span> of atmospheric longwave radiative cooling. Here we show that tightening of the ascending branch of the Hadley Circulation coupled with a decrease in tropical high cloud fraction is <span class="hlt">key</span> in modulating precipitation response to surface warming. The magnitude of high cloud shrinkage is a primary contributor to the intermodel spread in the <span class="hlt">changes</span> of tropical-mean outgoing longwave radiation (OLR) and global-mean precipitation per unit surface warming (dP/dTs) for both interannual variability and global warming. Compared to observations, most Coupled Model Inter-comparison Project Phase 5 models underestimate the rates of interannual tropical-mean dOLR/dTs and global-mean dP/dTs, consistent with the muted tropical high cloud shrinkage. We find that the five models that agree with the observation-based interannual dP/dTs all predict dP/dTs under global warming higher than the ensemble mean dP/dTs from the ∼20 models analysed in this study. PMID:28589940</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('https://www.osti.gov/pages/biblio/1406822-baseline-projections-latin-america-base-year-assumptions-key-drivers-greenhouse-emissions','SCIGOV-DOEP'); return false;" href="https://www.osti.gov/pages/biblio/1406822-baseline-projections-latin-america-base-year-assumptions-key-drivers-greenhouse-emissions"><span>Baseline projections for Latin America: base-year assumptions, <span class="hlt">key</span> drivers and greenhouse emissions</span></a></p> <p><a target="_blank" href="http://www.osti.gov/pages">DOE PAGES</a></p> <p>van Ruijven, Bas J.; Daenzer, Katie; Fisher-Vanden, Karen; ...</p> <p>2016-02-14</p> <p>This article provides an overview of the base-year assumptions and core baseline projections for the set of models participating in the LAMP and CLIMACAP projects. Here we present the range in core baseline projections for Latin America, and identify <span class="hlt">key</span> differences between model projections including how these projections compare to historic trends. We find relatively large differences across models in base year assumptions related to population, GDP, energy and CO 2 emissions due to the use of different data sources, but also conclude that this does not influence the range of projections. We find that population and GDP projections acrossmore » models span a broad range, comparable to the range represented by the set of Shared Socioeconomic Pathways (SSPs). Kaya-factor decomposition indicates that the set of core baseline scenarios mirrors trends experienced over the past <span class="hlt">decades</span>. Emissions in Latin America are projected to rise as result of GDP and population growth and a minor shift in the energy mix toward fossil fuels. Most scenarios assume a somewhat higher GDP growth than historically observed and continued decline of population growth. Minor <span class="hlt">changes</span> in energy intensity or energy mix are projected over the next few <span class="hlt">decades</span>.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018ACP....18.6121I','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018ACP....18.6121I"><span><span class="hlt">Key</span> drivers of ozone <span class="hlt">change</span> and its radiative forcing over 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>Iglesias-Suarez, Fernando; Kinnison, Douglas E.; Rap, Alexandru; Maycock, Amanda C.; Wild, Oliver; Young, Paul J.</p> <p>2018-05-01</p> <p>Over the 21st century <span class="hlt">changes</span> in both tropospheric and stratospheric ozone are likely to have important consequences for the Earth's radiative balance. In this study, we investigate the radiative forcing from future ozone <span class="hlt">changes</span> using the Community Earth System Model (CESM1), with the Whole Atmosphere Community Climate Model (WACCM), and including fully coupled radiation and chemistry schemes. Using year 2100 conditions from the Representative Concentration Pathway 8.5 (RCP8.5) scenario, we quantify the individual contributions to ozone radiative forcing of (1) climate <span class="hlt">change</span>, (2) reduced concentrations of ozone depleting substances (ODSs), and (3) methane increases. We calculate future ozone radiative forcings and their standard error (SE; associated with inter-annual variability of ozone) relative to year 2000 of (1) 33 ± 104 m Wm-2, (2) 163 ± 109 m Wm-2, and (3) 238 ± 113 m Wm-2 due to climate <span class="hlt">change</span>, ODSs, and methane, respectively. Our best estimate of net ozone forcing in this set of simulations is 430 ± 130 m Wm-2 relative to year 2000 and 760 ± 230 m Wm-2 relative to year 1750, with the 95 % confidence interval given by ±30 %. We find that the overall long-term tropospheric ozone forcing from methane chemistry-climate feedbacks related to OH and methane lifetime is relatively small (46 m Wm-2). Ozone radiative forcing associated with climate <span class="hlt">change</span> and stratospheric ozone recovery are robust with regard to background climate conditions, even though the ozone response is sensitive to both <span class="hlt">changes</span> in atmospheric composition and climate. <span class="hlt">Changes</span> in stratospheric-produced ozone account for ˜ 50 % of the overall radiative forcing for the 2000-2100 period in this set of simulations, highlighting the <span class="hlt">key</span> role of the stratosphere in determining future ozone radiative forcing.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/27532758','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/27532758"><span><span class="hlt">Changes</span> in beverage consumption among adolescents from public schools in the first <span class="hlt">decade</span> of the century XXI.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Monteiro, Luana Silva; Vasconcelos, Thaís Meirelles de; Veiga, Gloria Valéria da; Pereira, Rosângela Alves</p> <p>2016-01-01</p> <p>To evaluate the <span class="hlt">changes</span> in beverage consumption among adolescents between 2003 and 2008. Two school-based cross-sectional studies were carried out with public school students (12 to 19 years-old) from Niterói, Rio de Janeiro, Brazil. Data from three food records were used to estimate daily, weekdays and weekend average consumption (volume and percent contribution for total daily energy intake) of milk and milk-based beverages, sugar sweetened beverages, fresh squeezed fruit juices, caffeinated and alcoholic beverages. Beverage consumption age-adjusted means for weekdays and weekends were compared using linear regression (Generalized Linear Models - GLM). A total of 433 adolescents were examined in 2003, and 510 in 2008. The prevalence of overweight was 17% in 2003 and 22% in 2008 (p > 0.05). Milk was the most consumed beverage, being reported by 89% of adolescents, followed by sodas (75%). In general, in the five-year period, there was an increase in the prevalence of consumption of alcoholic drinks, guarana syrup refreshment, and processed fruit drinks, especially on weekdays. The soft drink was the largest contributor to the total energy consumption, corresponding on average to 4% of daily energy intake. The main <span class="hlt">changes</span> in the beverage consumption among adolescents from Niterói, in the first <span class="hlt">decade</span> of the XXI century, were the tendency to reduce the consumption of milk and the increase in the consumption of processed and alcoholic beverages.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/27524630','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/27524630"><span>Five <span class="hlt">Decades</span>: From Challenge to Acclaim.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Melina, Vesanto</p> <p>2016-09-01</p> <p>What can make your work as a dietitian so meaningful that you begin each day with enthusiasm, and if you so choose, retain that joy in your work for 5 <span class="hlt">decades</span> or more? Three themes are: (i) doing work that profoundly makes sense to you, (ii) inspiring others (and yourself) to make healthful choices, and (iii) moving through challenges to success. Initially it can be challenging to make a living through work that is most deeply meaningful or closest to your heart. Yet it is well worth finding the balance between practicality and movement in the desired direction. Other challenges faced by dietitians involve helping others to adopt new, more healthful lifestyle choices. As health professionals, our attitudes towards plant-based diets have <span class="hlt">changed</span> dramatically during these past <span class="hlt">decades</span>. This article examines our evolving perspectives of plant-based diets, and uses this as an example of movement through challenges to success and acclaim. Vegetarian and vegan diets that were considered entirely inappropriate for many stages of the life cycle in the 1970s are now seen to confer health benefits. This applies to well-designed plant-based diets, thus offering a significant role for dietitians as creative leaders in this field.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/26439678','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/26439678"><span>How will the semi-natural vegetation of the UK have <span class="hlt">changed</span> by 2030 given likely <span class="hlt">changes</span> in nitrogen deposition?</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Stevens, Carly J; Payne, Richard J; Kimberley, Adam; Smart, Simon M</p> <p>2016-01-01</p> <p>Nitrogen deposition is known to have major impacts on contemporary ecosystems but few studies have addressed how these impacts will develop over coming <span class="hlt">decades</span>. We consider likely <span class="hlt">changes</span> to British semi-natural vegetation up to the year 2030 both qualitatively, based on knowledge of species responses from experimental and gradient studies, and quantitatively, based on modelling of species relationships in national monitoring data. We used historical N deposition trends and national predictions of <span class="hlt">changing</span> deposition to calculate cumulative deposition from 1900 to 2030. Data from the Countryside Survey (1978, 1990 and 1998) was used to parameterise models relating cumulative N deposition to Ellenberg N which were then applied to expected future deposition trends. <span class="hlt">Changes</span> to habitat suitability for <span class="hlt">key</span> species of grassland, heathland and bog, and broadleaved woodland to 2030 were predicted using the MultiMOVE model. In UK woodlands by 2030 there is likely to be reduced occurrence of lichens, increased grass cover and a shift towards more nitrophilic vascular plant species. In grasslands we expect <span class="hlt">changing</span> species composition with reduced occurrence of terricolous lichens and, at least in acid grasslands, reduced species richness. In heaths and bogs we project overall reductions in species richness with decreased occurrence of terricolous lichens and some bryophytes, reduced cover of dwarf shrubs and small increases in grasses. Our study clearly suggests that <span class="hlt">changes</span> in vegetation due to nitrogen deposition are likely to continue through coming <span class="hlt">decades</span>. Copyright © 2015 Elsevier Ltd. All rights reserved.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29138306','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29138306"><span><span class="hlt">Key</span> Metabolites and Mechanistic <span class="hlt">Changes</span> for Salt Tolerance in an Experimentally Evolved Sulfate-Reducing Bacterium, Desulfovibrio vulgaris.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Zhou, Aifen; Lau, Rebecca; Baran, Richard; Ma, Jincai; von Netzer, Frederick; Shi, Weiling; Gorman-Lewis, Drew; Kempher, Megan L; He, Zhili; Qin, Yujia; Shi, Zhou; Zane, Grant M; Wu, Liyou; Bowen, Benjamin P; Northen, Trent R; Hillesland, Kristina L; Stahl, David A; Wall, Judy D; Arkin, Adam P; Zhou, Jizhong</p> <p>2017-11-14</p> <p>Rapid genetic and phenotypic adaptation of the sulfate-reducing bacterium Desulfovibrio vulgaris Hildenborough to salt stress was observed during experimental evolution. In order to identify <span class="hlt">key</span> metabolites important for salt tolerance, a clone, ES10-5, which was isolated from population ES10 and allowed to experimentally evolve under salt stress for 5,000 generations, was analyzed and compared to clone ES9-11, which was isolated from population ES9 and had evolved under the same conditions for 1,200 generations. These two clones were chosen because they represented the best-adapted clones among six independently evolved populations. ES10-5 acquired new mutations in genes potentially involved in salt tolerance, in addition to the preexisting mutations and different mutations in the same genes as in ES9-11. Most basal abundance <span class="hlt">changes</span> of metabolites and phospholipid fatty acids (PLFAs) were lower in ES10-5 than ES9-11, but an increase of glutamate and branched PLFA i17:1ω9c under high-salinity conditions was persistent. ES9-11 had decreased cell motility compared to the ancestor; in contrast, ES10-5 showed higher cell motility under both nonstress and high-salinity conditions. Both genotypes displayed better growth energy efficiencies than the ancestor under nonstress or high-salinity conditions. Consistently, ES10-5 did not display most of the basal transcriptional <span class="hlt">changes</span> observed in ES9-11, but it showed increased expression of genes involved in glutamate biosynthesis, cation efflux, and energy metabolism under high salinity. These results demonstrated the role of glutamate as a <span class="hlt">key</span> osmolyte and i17:1ω9c as the major PLFA for salt tolerance in D. vulgaris The mechanistic <span class="hlt">changes</span> in evolved genotypes suggested that growth energy efficiency might be a <span class="hlt">key</span> factor for selection. IMPORTANCE High salinity (e.g., elevated NaCl) is a stressor that affects many organisms. Salt tolerance, a complex trait involving multiple cellular pathways, is attractive for</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017EGUGA..1914563S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017EGUGA..1914563S"><span>Understanding three <span class="hlt">decades</span> of land use <span class="hlt">changes</span> and a cloudburst in Phewa Lake Watershed, Western Nepal</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Sudmeier-Rieux, Karen; Tonini, Marj; Vulliez, Cindy; Sanjaya, Devkota; Derron, Marc-Henri; Jaboyedoff, Michel</p> <p>2017-04-01</p> <p>This paper details an extreme rainfall event, or cloudburst (315 mm/ 24 hours) which occurred on July 29-30, 2015 in the Phewa Lake Watershed, Western Nepal, three months after the April 25, 2015 Gorkha Earthquake. The event triggered over 170 landslides and debris flows, caused 8 deaths and considerable damage to livelihoods. The fatal debris flow started from one of the numerous rural roads, which have proliferated exponentially over the past <span class="hlt">decades</span>. In addition to mapping landslides due to this extreme rainfall event, our study sought to document and analyze underlying natural and human land use factors that may have impacted the occurrence of landsliding (Vulliez et al submitted). To do so, our study analyzed land cover/ land use <span class="hlt">changes</span> for the period 1979-2016 based on an interpretation of aerial photos and satellite images, combined with ground truthing. We studied how land use / land cover <span class="hlt">changes</span> have resulted in a shift of active erosion zones from overgrazing around streams and forests to an exponential number of small failures along unplanned earthen rural roads, or "bulldozer roads". With several hundred small failures documented along roadsides (Leibundgut et al., 2016) as compared to only 14 landslides prior to 2015 extreme rainfall event - and none triggered by the 2015 earthquake - roads are thus a major driver of active erosion zones and small failures in the watershed. More effective management of the current unsustainable mode of rural road construction is required to reduce further environmental and economic impacts on vulnerable populations in Nepal. Leibundgut, G., Sudmeier-Rieux, K. Devkota, S., Jaboyedoff, M., Derron, M-H., Penna, I. Nguyen, L. (2016). Rural earthen roads impact assessment in Phewa watershed, Western region, Nepal. Geoenvironmental Disasters (2016) 3:13. DOI 10.1186/s40677-016-0047-8 Vulliez, C, Tonini, M., Sudmeier-Rieux, K. Devkota, S., Derron, M-H, Jaboyedoff, M. (submitted) Land use <span class="hlt">changes</span>, landslides and roads in the</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/17210177','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/17210177"><span>Collaboration, integration and <span class="hlt">change</span> in children's services: critical issues and <span class="hlt">key</span> ingredients.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Horwath, Jan; Morrison, Tony</p> <p>2007-01-01</p> <p>Government and state policy, irrespective of jurisdiction, increasingly require and indeed specify the nature of collaboration with regard to the delivery of child welfare services for maltreated children. The rationale for collaboration appears obvious in as much as it is aimed at promoting multidisciplinary practice in order to meet the needs of the vulnerable child. However, collaboration, whilst a useful and motivating concept, is in reality far from straightforward and contains complexities and ambiguities. The aim of this paper is to explore these complexities and ambiguities to provide an overview of <span class="hlt">key</span> developmental frameworks relevant to the creation and maintenance of strategic high-level multiagency partnerships. The authors begin by exploring the characteristic features of different levels of multiagency collaboration that is communication, co-operation, co-ordination, coalition, and integration. As the emphasis in a variety of jurisdictions in the Western world is on the highest levels of collaboration namely coalition and service integration this is the focus of the paper. The authors synthesize the main literature in the field to consider the critical elements for effective collaborative endeavors at this level including predisposing factors, mandate, leadership, machinery, process, and outcomes. The paper concludes by recognizing that the drive towards integrated services is occurring in a climate of continuing <span class="hlt">change</span>. The need to identify the impact of such an environment when managing multiagency partnerships is explored using five steps to <span class="hlt">change</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFMGC32A..08P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFMGC32A..08P"><span>Taimyr Reindeer and Environmental <span class="hlt">Change</span>: Monitoring Wild Reindeer Migration in <span class="hlt">Changing</span> Natural and Social Environments</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Petrov, A. N.</p> <p>2016-12-01</p> <p>The Taimyr Reindeer Herd (TRH) is both the largest and the longest monitored wild reindeer herd in Eurasia. An important part of Arctic ecosystems and Indigenous livelihood, wild reindeer have been continuously monitored for almost 50 years. During this time, herds have exhibited large <span class="hlt">changes</span> in size and these <span class="hlt">changes</span> have been recorded in almost all herds across the animal's range. An increasing number of wild reindeer in the Soviet times was followed by a significant population loss in the last <span class="hlt">decade</span>. In addition, recent monitoring revealed substantial shifts in the distribution of wild populations. The decline in wild reindeer is likely related to natural cycles and <span class="hlt">changes</span> in the Arctic environment caused by climate variability and anthropogenic activity. This study investigates patterns and possible drives of reindeer population dynamics in space and time. We identify <span class="hlt">key</span> climatic factors, possible relationships with biomass dynamics, as well as with hunting practices and other human impacts.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2009JHyd..375..114H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2009JHyd..375..114H"><span>Sahelian rangeland response to <span class="hlt">changes</span> in rainfall over two <span class="hlt">decades</span> in the Gourma region, Mali</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Hiernaux, Pierre; Mougin, Eric; Diarra, Lassine; Soumaguel, Nogmana; Lavenu, François; Tracol, Yann; Diawara, Mamadou</p> <p>2009-08-01</p> <p> the refusal scenario is more frequent. Because grazing promotes short cycle species, grazed rangelands respond faster to droughts. Year to year <span class="hlt">changes</span> in species composition are abrupt as expected from the transient soil seed stock. However, some <span class="hlt">decadal</span> trends in species composition are identified, with a wave of pioneer species following the 1983-1984 droughts, and a more progressive diversification and return to typical Sahel flora from 1992 onwards.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/22847100','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/22847100"><span>Checklists <span class="hlt">change</span> communication about <span class="hlt">key</span> elements of patient care.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Newkirk, Michelle; Pamplin, Jeremy C; Kuwamoto, Roderick; Allen, David A; Chung, Kevin K</p> <p>2012-08-01</p> <p>Combat casualty care is distributed across professions and echelons of care. Communication within it is fragmented, inconsistent, and prone to failure. Daily checklists used during intensive care unit (ICU) rounds have been shown to improve compliance with evidence-based practices, enhance communication, promote consistency of care, and improve outcomes. Checklists are criticized because it is difficult to establish a causal link between them and their effect on outcomes. We investigated how checklists used during ICU rounds affect communication. We conducted this project in two military ICUs (burn and surgical/trauma). Checklists contained up to 21 questions grouped according to patient population. We recorded which checklist items were discussed during rounds before and after implementation of a "must address" checklist and compared the frequency of discussing items before checklist prompting. Patient discussions addressed more checklist items before prompting at the end of the 2-week evaluation compared with the 2-week preimplementation period (surgical trauma ICU, 36% vs. 77%, p < 0.0001; burn ICU, 47% vs. 72 %, p < 0.001). Most items were addressed more frequently in both ICUs after implementation. <span class="hlt">Key</span> items such as central line removal, reduction of laboratory testing, medication reconciliation, medication interactions, bowel movements, sedation holidays, breathing trials, and lung protective ventilation showed significant improvements. Checklists modify communication patterns. Improved communication facilitated by checklists may be one mechanism behind their effectiveness. Checklists are powerful tools that can rapidly alter patient care delivery. Implementing checklists could facilitate the rapid dissemination of clinical practice <span class="hlt">changes</span>, improve communication between echelons of care and between individuals involved in patient care, and reduce missed information.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017xru..conf..114K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017xru..conf..114K"><span>XMM-Newton mission operations - ready for its third <span class="hlt">decade</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Kirsch, M.; Finn, T.; Godard, T.; v. Krusenstiern, N.; Pfeil, N.; Salt, D.; Toma, L.; Webert, D.; Weissmann, U.</p> <p>2017-10-01</p> <p>The XMM-Newton X-ray space observatory is approaching its third <span class="hlt">decade</span> of operations. The spacecraft and payload are operating without major degradation and scientific demand is continuously very high. With the <span class="hlt">change</span> to a new way of using the Attitude and Orbit control System in 2013 the fuel consumption was reduced by a factor of two, additionally this has reduced stress on the reaction wheels. The challenge for the next <span class="hlt">decade</span> is now to ensure that the saved fuel is available for continuous usage. We will describe the process of the so called 'fuel migration and replenishment' activities needed to keep the spacecraft operational potentially up to 2029+. We provide as well an overall health status of the mission, the evolution of the ground segment and concepts on streamlining mission operations with continued high safety requirements using automation tools.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://eric.ed.gov/?q=ftp%3a&pg=3&id=EJ523699','ERIC'); return false;" href="https://eric.ed.gov/?q=ftp%3a&pg=3&id=EJ523699"><span><span class="hlt">Decade</span> of <span class="hlt">Change</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>Hunter, Leslie Gene</p> <p>1995-01-01</p> <p>Discusses advancements in the field of history-related computer-assisted instruction and research. Describes the components of Historiography and Methods of Research, a class that introduces history students to such practical applications as the World Wide Web (WWW), File Transfer Protocol (FTP), listservs, archival access, and others. Briefly…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/24467425','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/24467425"><span>Low and decreasing self-esteem during adolescence predict adult depression two <span class="hlt">decades</span> later.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Steiger, Andrea E; Allemand, Mathias; Robins, Richard W; Fend, Helmut A</p> <p>2014-02-01</p> <p>Previous studies revealed that low self-esteem is prospectively associated with depression. However, self-esteem has been shown to <span class="hlt">change</span> over time. We thus hypothesized that not only level but also <span class="hlt">change</span> in self-esteem affect depression. Using data from a 23-year longitudinal study (N = 1,527), we therefore examined the prospective effects of global and domain-specific self-esteem (physical attractiveness, academic competence) level and <span class="hlt">change</span> on depressive symptoms 2 <span class="hlt">decades</span> later. Self-esteem was assessed annually from age 12 to 16, and depression was assessed at age 16 and 35. Results from latent growth curve analyses demonstrated that both level and <span class="hlt">change</span> in self-esteem served as predictors for adult depression. Individuals who entered adolescence with low self-esteem, and/or whose self-esteem declined further during the adolescent years, were more likely to exhibit symptoms of depression 2 <span class="hlt">decades</span> later as adults; this pattern held both for global and domain-specific self-esteem. These findings highlight the importance of adolescent self-esteem development for mental health outcomes in adulthood. PsycINFO Database Record (c) 2014 APA, all rights reserved.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017JGRD..122.5808Z','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017JGRD..122.5808Z"><span>Wetting and greening Tibetan Plateau in early summer in recent <span class="hlt">decades</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, Wenxia; Zhou, Tianjun; Zhang, Lixia</p> <p>2017-06-01</p> <p>The Tibetan Plateau (TP) plays an essential role in the global hydrological cycle. Unlike the well-recognized surface warming, <span class="hlt">changes</span> in precipitation over the TP and the underlying mechanisms remain ambiguous. A significant increase in the amount of precipitation over the southeastern TP in May over 1979-2014 (13.46% <span class="hlt">decade</span>-1 of the climatology) is identified in this study, based on homogenized daily rain gauge data. Both the increased precipitation frequency and intensity have contributions. The coherent increases in soil moisture content and vegetation activities further confirm the precipitation trend, indicating a wetting and greening TP in the early summer in recent <span class="hlt">decades</span>. The moisture budget analysis shows that this wetting trend in the past four <span class="hlt">decades</span> is dominated by the increased water vapor convergence due to circulation <span class="hlt">changes</span>, while increases in specific humidity play a minor role. The wetting trend over the TP in May results directly from the earlier onset of the South Asian summer monsoon (ASM) since the late 1970s associated with the phase transition of Interdecadal Pacific Oscillation around the late 1990s. The earlier onset of the ASM triggers low-level southwesterly anomalies over the northern Indian Ocean, promoting moisture convergence and increased precipitation over the TP in May. Specifically, the increased amount of precipitation after the onset of the ASM explains 95% of the increase in the total amount of precipitation in May.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/27532511','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/27532511"><span>Trends in Type of Original Psoriasis Publications by <span class="hlt">Decade</span>, 1960 to 2010.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Sako, Eric; Famenini, Shannon; Wu, Jashin J</p> <p>2016-01-01</p> <p>Research investigating psoriasis has spanned <span class="hlt">decades</span>, and as our understanding of the disease has evolved, the focus of publications has <span class="hlt">changed</span>. We sought to characterize the trends in original psoriasis-related research from 1960 to 2010 chronologically by <span class="hlt">decade</span>. A literature review was performed using the keyword psoriasis in the MEDLINE database. All original psoriasis-related articles published at the beginning of each <span class="hlt">decade</span> were searched and categorized by study type and topic. Number of articles per topic. A total of 869 original psoriasis-related articles were found. The number of publications increased 18 fold over 5 <span class="hlt">decades</span>. The immunology and pathogenesis of psoriasis was the most frequently researched topic (36%), and retrospective studies were the most common study type (37%). Recent highly published topics included biologic therapy, genetics, and psoriasis-associated cardiovascular disease. Original psoriasis-related publications have grown substantially since 1960. Basic science research into the immunology and pathogenesis has been and continues to be the mainstay of psoriasis research. Recent research trends suggest the focus has expanded to topics such as psoriasis-associated cardiovascular disease, genetics, and biologic therapy.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29153315','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29153315"><span>What are the <span class="hlt">keys</span> to a longer, happier life? Answers from five <span class="hlt">decades</span> of health psychology research.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Johnson, Blair T; Acabchuk, Rebecca L</p> <p>2018-01-01</p> <p>It has long been known that factors of the mind and of interpersonal relationships influence health, but it is only in the last 50 years that an independent scientific field of health psychology appeared, dedicated to understanding psychological and behavioral processes in health, illness, and healthcare. This article (a) reviews important research that answers the question of how human beings can have longer, happier lives; and (b) highlights trends in health psychology featuring articles in Social Science & Medicine as well as other related literature. Since the 1970s, health psychology has embraced a biopsychosocial model such that biological factors interact and are affected by psychological and social elements. This model has illuminated all subjects of health, ranging from interventions to lower stress and/or to improve people's ability to cope with stressors, to mental and physical health. Importantly, a health psychology perspective is behavioral: The majority of chronic diseases of today can be avoided or reduced through healthy lifestyles (e.g., sufficient exercise, proper diet, sufficient sleep). Thus, behavior <span class="hlt">change</span> is the <span class="hlt">key</span> target to help reduce the immense public health burden of chronic lifestyle illnesses. Health psychology also focuses on how social patterns influence health behavior and outcomes, in the form of patient-provider interactions or as social forces in communities where people live, work, and play. Health psychology is congenial to other health sciences, especially when allied with ecological perspectives that incorporate factors upstream from individual behavior, such as networks linked to individuals (e.g., peer groups, communities). Over its history, health psychology research has been responsive to societal and medical needs and has routinely focused on understanding health disparities. By relying on a strong interdisciplinary approach, research in health psychology provides a remarkably comprehensive perspective on how people</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/27115062','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/27115062"><span>Secular <span class="hlt">Changes</span> in Postfracture Outcomes Over 2 <span class="hlt">Decades</span> in Australia: A Time-Trend Comparison of Excess Postfracture Mortality in Two Birth Controls Over Two <span class="hlt">Decades</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Bliuc, Dana; Tran, Thach; Alarkawi, Dunia; Nguyen, Tuan V; Eisman, John A; Center, Jacqueline R</p> <p>2016-06-01</p> <p>Hip fracture incidence has been declining and life expectancy improving. However, trends of postfracture outcomes are unknown. The objective of the study was to compare the refracture risk and excess mortality after osteoporotic fracture between two birth cohorts, over 2 <span class="hlt">decades</span>. Prospective birth cohorts were followed up over 2 <span class="hlt">decades</span> (1989-2004 and 2000-2014). The study was conducted in community-dwelling participants in Dubbo, Australia. Women and men aged 60-80 years, participating in Dubbo Osteoporosis Epidemiology Study 1 (DOES 1; born before 1930) and Dubbo Osteoporosis Epidemiology Study 2 (DOES 2; born after 1930) participated in the study. Age-standardized fracture and mortality over two time intervals: (1989-2004 [DOES 1] and 2000-2014 [DOES 2]) were measured. The DOES 2 cohort had higher body mass index and bone mineral density and lower initial fracture rate than DOES 1, but similar refracture rates [age-standardized refracture rates per 1000 person-years: women: 53 (95% confidence interval [CI] 42-63) and 51 (95% CI 41-60) and men: 53 (95% CI 38-69) and 55 (95% CI 40-71) for DOES 2 and DOES 1, respectively). Absolute postfracture mortality rates declined in DOES 2 compared with DOES 1, mirroring the improvement in general-population life expectancy. However, when compared with period-specific general-population mortality, there was a similar 2.1- to 2.6-fold increased mortality risk after a fracture in both cohorts (age-adjusted standardized mortality ratio, women: 2.05 [95% CI 1.43-2.83] and 2.43 [95% CI 1.95-2.99] and men: 2.56 [95% CI 1.78-3.58] and 2.48 [95% CI 1.87-3.22] for DOES 2 and DOES 1, respectively). Over the 2 <span class="hlt">decades</span>, despite the decline in the prevalence of fracture risk factors, general-population mortality, and initial fracture incidence, there was no improvement in postfracture outcomes. Refracture rates were similar and fracture-associated mortality was 2-fold higher than expected. These data indicate that the low postfracture</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018ERL....13c4006L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018ERL....13c4006L"><span>Increase of surface solar irradiance across East China related to <span class="hlt">changes</span> in aerosol properties during the past <span class="hlt">decade</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Li, Jing; Jiang, Yiwei; Xia, Xiangao; Hu, Yongyun</p> <p>2018-03-01</p> <p>Previously, it was widely documented that an overall decrease in surface solar radiation occurred in China at least until 2005, in contrast to the general background of ‘global brightening’. Increased anthropogenic aerosol emissions were speculated to be the source of the reduction. In this study, we extend the trend analysis to the most recent <span class="hlt">decade</span> from 2005-2015 and find that surface solar radiation has shifted from ‘dimming’ to ‘brightening’ over East China, with the largest increase over the northeast and southeast parts. Meanwhile, satellite and ground observation both indicate a reduction in aerosol optical depth (AOD) during the same period, whereas no significant trends in cloud amount show up. Detailed analysis using co-located radiation and aerosol observation at the XiangHe station in North China suggests that both AOD and single scattering albedo (SSA) <span class="hlt">changes</span> contribute to the radiation trends. AOD reduction contributes to the increase of direct solar radiation, also decreasing the diffuse radiation, while the increase of SSA serves to increase the diffuse fraction. Simple calculations using a radiative transfer model confirm that the two effects combined explain <span class="hlt">changes</span> in the global solar radiation and its components effectively. Our results have implications for potential climate effects with the reduction of China’s aerosol emissions, and the necessity to monitor aerosol composition in addition to its loading.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2010EGUGA..12.8430S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2010EGUGA..12.8430S"><span>Analyzing phenological extreme events over the past five <span class="hlt">decades</span> in Germany</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Schleip, Christoph; Menzel, Annette; Estrella, Nicole; Graeser, Philipp</p> <p>2010-05-01</p> <p>As climate <span class="hlt">change</span> may alter the frequency and intensity of extreme temperatures, we analysed whether warming of the last 5 <span class="hlt">decades</span> has already <span class="hlt">changed</span> the statistics of phenological extreme events. In this context, two extreme value statistical concepts are discussed and applied to existing phenological datasets of German Weather Service (DWD) in order to derive probabilities of occurrence for extreme early or late phenological events. We analyse four phenological groups; "begin of flowering, "leaf foliation", "fruit ripening" and "leaf colouring" as well as DWD indicator phases of the "phenological year". Additionally we put an emphasis on a between-species analysis; a comparison of differences in extreme onsets between three common northern conifers. Furthermore we conducted a within-species analysis with different phases of horse chestnut throughout a year. The first statistical approach fits data to a Gaussian model using traditional statistical techniques, and then analyses the extreme quantile. The <span class="hlt">key</span> point of this approach is the adoption of an appropriate probability density function (PDF) to the observed data and the assessment of the PDF parameters <span class="hlt">change</span> in time. The full analytical description in terms of the estimated PDF for defined time steps of the observation period allows probability assessments of extreme values for e.g. annual or <span class="hlt">decadal</span> time steps. Related with this approach is the possibility of counting out the onsets which fall in our defined extreme percentiles. The estimation of the probability of extreme events on the basis of the whole data set is in contrast to analyses with the generalized extreme value distribution (GEV). The second approach deals with the extreme PDFs itself and fits the GEV distribution to annual minima of phenological series to provide useful estimates about return levels. For flowering and leaf unfolding phases exceptionally early extremes are seen since the mid 1980s and especially for the single years 1961</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('http://adsabs.harvard.edu/abs/2015ACP....1511931Y','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015ACP....1511931Y"><span>Distinguishing the drivers of trends in land carbon fluxes and plant volatile emissions over the past 3 <span class="hlt">decades</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Yue, X.; Unger, N.; Zheng, Y.</p> <p>2015-10-01</p> <p>The terrestrial biosphere has experienced dramatic <span class="hlt">changes</span> in recent <span class="hlt">decades</span>. Estimates of historical trends in land carbon fluxes remain uncertain because long-term observations are limited on the global scale. Here, we use the Yale Interactive terrestrial Biosphere (YIBs) model to estimate <span class="hlt">decadal</span> trends in land carbon fluxes and emissions of biogenic volatile organic compounds (BVOCs) and to identify the <span class="hlt">key</span> drivers for these <span class="hlt">changes</span> during 1982-2011. Driven by hourly meteorology from WFDEI (WATCH forcing data methodology applied to ERA-Interim data), the model simulates an increasing trend of 297 Tg C a-2 in gross primary productivity (GPP) and 185 Tg C a-2 in the net primary productivity (NPP). CO2 fertilization is the main driver for the flux <span class="hlt">changes</span> in forest ecosystems, while meteorology dominates the <span class="hlt">changes</span> in grasslands and shrublands. Warming boosts summer GPP and NPP at high latitudes, while drought dampens carbon uptake in tropical regions. North of 30° N, increasing temperatures induce a substantial extension of 0.22 day a-1 for the growing season; however, this phenological <span class="hlt">change</span> alone does not promote regional carbon uptake and BVOC emissions. Nevertheless, increases of leaf area index at peak season accounts for ~ 25 % of the trends in GPP and isoprene emissions at the northern lands. The net land sink shows statistically insignificant increases of only 3 Tg C a-2 globally because of simultaneous increases in soil respiration. Global BVOC emissions are calculated using two schemes. With the photosynthesis-dependent scheme, the model predicts increases of 0.4 Tg C a-2 in isoprene emissions, which are mainly attributed to warming trends because CO2 fertilization and inhibition effects offset each other. Using the MEGAN (Model of Emissions of Gases and Aerosols from Nature) scheme, the YIBs model simulates global reductions of 1.1 Tg C a-2 in isoprene and 0.04 Tg C a-2 in monoterpene emissions in response to the CO2 inhibition effects. Land use</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=1653985','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=1653985"><span>A <span class="hlt">decade</span> of international <span class="hlt">change</span> in abortion law: 1967-1977.</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Cook, R J; Dickens, B M</p> <p>1978-01-01</p> <p>Modern thinking on abortion, reflected in recent legal developments around the world, has turned from concentration upon criminality in favor of female and family well-being. New laws enacted during the last <span class="hlt">decade</span> are coming to focus upon conditions of health and social welfare of women and their existing families as indications for lawful termination of pregnancy. Regulations governing the delivery of services may be restrictive, however, so as to limit in practice access to means of safe, legal abortion made available in theory. Requirements may be imposed that only medical personnel with unduly high qualifications perform procedures, or that they be undertaken only in institutions meeting standards higher than similar health care requires. Approval procedures may be established involving second medical opinions or committees to monitor observance of the law, which may delay abortions and therefore increase their hazards. Parental and spousal consent requirements may exist in addition with the same effects, or to veto a pregnant female's request. Regulations may be employed more positively, however, to encourage contraceptive practice. A disappointment with legislative reform is that it may fail to improve circumstances if public resources are not applied to achieve the supply of services newly rendered legitimate, and illegal practice may persist. PMID:665881</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/18543369','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/18543369"><span><span class="hlt">Key</span> future research questions on mediators and moderators of behaviour <span class="hlt">change</span> processes for substance abuse.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Rehm, Jürgen</p> <p>2008-06-01</p> <p>In summarizing the <span class="hlt">key</span> themes and results of the second meeting of the German Addiction Research Network 'Understanding Addiction: Mediators and Moderators of Behaviour <span class="hlt">Change</span> Process', the following concrete steps forward were laid out to improve knowledge. The steps included pleas to (1) redefine substance abuse disorders, especially redefine the concept of abuse and harmful use; (2) increase the use of longitudinal and life-course studies with more adequate statistical methods such as latent growth modelling; (3) empirically test more specific and theoretically derived common factors and mechanisms of behavioural <span class="hlt">change</span> processes; (4) better exploit cross-regional and cross-cultural differences.Funding agencies are urged to support these developments by specifically supporting interdisciplinary research along the lines specified above. This may include improved forms of international funding of groups of researchers from different countries, where each national group conducts a specific part of an integrated proposal. 2008 John Wiley & Sons, Ltd</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/24066418','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/24066418"><span>Social <span class="hlt">change</span> and women's health.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>McDonough, Peggy; Worts, Diana; McMunn, Anne; Sacker, Amanda</p> <p>2013-01-01</p> <p>Over the past five <span class="hlt">decades</span>, the organization of women's lives has <span class="hlt">changed</span> dramatically. Throughout the industrialized world, paid work and family biographies have been altered as the once-dominant role of homemaker has given way to the role of secondary, dual, or even primary wage-earner. The attendant <span class="hlt">changes</span> represent a mix of gains and losses for women, in which not all women have benefited (or suffered) equally. But little is known about the health consequences. This article addresses that gap. It develops a "situated biographies" model to conceptualize how life course <span class="hlt">change</span> may influence women's health. The model stresses the role of time, both as individual aging and as the anchoring of lives in particular historical periods. "Situating" biographies in this way highlights two <span class="hlt">key</span> features of social <span class="hlt">change</span> in women's lives: the ambiguous implications for the health of women as a group, and the probable connections to growing social and economic disparities in health among them. This approach lays the groundwork for more integrated and productive population-based research about how historical transformations may affect women's health.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFMED41C..07D','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFMED41C..07D"><span><span class="hlt">Key</span> Ideas for Making and Using Virtual Fieldwork Experiences</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Duggan-Haas, D.; Ross, R. M.</p> <p>2016-12-01</p> <p>Fieldwork is a signature pedagogy for the geosciences, but can be challenging to manage and challenging to bring to certain settings, like large lecture courses or K-12 classrooms. Virtual Fieldwork Experiences (VFEs) are helpful in meeting these challenges, though we do not suggest that VFEs replace actual fieldwork. In designing and using VFEs, for providing related professional development, and for designing and implementing actual fieldwork, <span class="hlt">key</span> questions to consider are: What are the most important features and results of fieldwork? What aspects can be replicated through the use of multimedia? To what extent? How can the creation of VFEs be used to catalyze, extend, document, and share what is learned from doing actual fieldwork? A <span class="hlt">decade</span> ago, we began developing curriculum materials and offering professional development programming in which VFEs are a <span class="hlt">key</span> feature. Over the last ten years, both the technologies available and our pedagogical approaches have <span class="hlt">changed</span> substantially. Technologically, things that used to take hours to create can now be done in minutes, and other things that were simply not practical have become simple for users to create. The rate of <span class="hlt">change</span> of pedagogy is slower. Our initial goal of creating VFEs that offer a true inquiry experience by themselves has been tempered over time. While VFEs can offer inquiry experiences for students, a shorter route to inquiry is framing VFEs as models for student-created VFEs that document fieldwork done by students. The effective creation and use of VFEs is dependent upon Technological Pedagogical and Content Knowledge (TPACK), the suite of understandings and skills that educators apply to teaching scientific content with technology. Educators working with VFEs often find themselves pushing their limits in one or more of the different realms of TPACK. Pushing limits is fundamental to professional growth. Our work has led to three <span class="hlt">key</span> ideas for VFE development and use: There are questions that can be</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFM.C31C..01D','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFM.C31C..01D"><span>Scenarios of Earth system <span class="hlt">change</span> in western Canada: Conceptual understanding and process insights from the <span class="hlt">Changing</span> Cold Regions Network</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>DeBeer, C. M.; Wheater, H. S.; Pomeroy, J. W.; Stewart, R. E.; Turetsky, M. R.; Baltzer, J. L.; Pietroniro, A.; Marsh, P.; Carey, S.; Howard, A.; Barr, A.; Elshamy, M.</p> <p>2017-12-01</p> <p>The interior of western Canada has been experiencing rapid, widespread, and severe hydroclimatic <span class="hlt">change</span> in recent <span class="hlt">decades</span>, and this is projected to continue in the future. To better assess future hydrological, cryospheric and ecological states and fluxes under future climates, a regional hydroclimate project was formed under the auspices of the Global Energy and Water Exchanges (GEWEX) project of the World Climate Research Programme; the <span class="hlt">Changing</span> Cold Regions Network (CCRN; www.ccrnetwork.ca) aims to understand, diagnose, and predict interactions among the <span class="hlt">changing</span> Earth system components at multiple spatial scales over the Mackenzie and Saskatchewan River basins of western Canada. A particular challenge is in applying land surface and hydrological models under future climates, as system <span class="hlt">changes</span> and cold regions process interactions are not often straightforward, and model structures and parameterizations based on historical observations and understanding of contemporary system functioning may not adequately capture these complexities. To address this and provide guidance and direction to the modelling community, CCRN has drawn insights from a multi-disciplinary perspective on the process controls and system trajectories to develop a set of feasible scenarios of <span class="hlt">change</span> for the 21st century across the region. This presentation will describe CCRN's efforts towards formalizing these insights and applying them in a large-scale modelling context. This will address what are seen as the most critical processes and <span class="hlt">key</span> drivers affecting hydrological, cryospheric and ecological <span class="hlt">change</span>, how these will most likely evolve in the coming <span class="hlt">decades</span>, and how these are parameterized and incorporated as future scenarios for terrestrial ecology, hydrological functioning, permafrost state, glaciers, agriculture, and water management.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/21295811','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/21295811"><span>Resident education in 2011: three <span class="hlt">key</span> challenges on the road ahead.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Van Eaton, Erik G; Tarpley, John L; Solorzano, Carmen C; Cho, Clifford S; Weber, Sharon M; Termuhlen, Paula M</p> <p>2011-04-01</p> <p>Two important <span class="hlt">changes</span> in the past <span class="hlt">decade</span> have altered the landscape of graduate medical education (GME) in the U.S. The national restrictions on trainee duty hours mandated by the Accreditation Council for Graduate Medical Education (ACGME) were the most visible and generated much controversy. Equally important is the ACGME Outcome Project, which mandates competency-based training. Both of these <span class="hlt">changes</span> have unique implications for surgery trainees, who traditionally spent long hours caring for patients in the hospital, and who must be assessed in 2 broad domains: their medical care of pre- and postoperative patients, and their technical skill with procedures in and out of the operating room. This article summarizes 3 <span class="hlt">key</span> challenges that lie ahead for surgical educators. First, the <span class="hlt">changes</span> in duty hours in the past 7 years are summarized, and the conversation about added restrictions planned for July 2011 is reviewed. Next, the current state of the assessment of competency among surgical trainees is reviewed, with an outline of the challenges that need to be overcome to achieve widespread, competency-based training in surgery. Finally, the article summarizes the problems caused by increased reliance on handoffs among trainees as they compensate for decreased time in the hospital, and suggests <span class="hlt">changes</span> that need to be made to improve safety and efficiency, including how to use handoffs as part of our educational evaluation of residents. Copyright © 2011 Mosby, Inc. All rights reserved.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/22829324','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/22829324"><span>Mapping human dimensions of climate <span class="hlt">change</span> research in the Canadian Arctic.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Ford, James D; Bolton, Kenyon; Shirley, Jamal; Pearce, Tristan; Tremblay, Martin; Westlake, Michael</p> <p>2012-12-01</p> <p>This study maps current understanding and research trends on the human dimensions of climate <span class="hlt">change</span> (HDCC) in the eastern and central Canadian Arctic. Developing a systematic literature review methodology, 117 peer reviewed articles are identified and examined using quantitative and qualitative methods. The research highlights the rapid expansion of HDCC studies over the last <span class="hlt">decade</span>. Early scholarship was dominated by work documenting Inuit observations of climate <span class="hlt">change</span>, with research employing vulnerability concepts and terminology now common. Adaptation studies which seek to identify and evaluate opportunities to reduce vulnerability to climate <span class="hlt">change</span> and take advantage of new opportunities remain in their infancy. Over the last 5 years there has been an increase social science-led research, with many studies employing <span class="hlt">key</span> principles of community-based research. We currently have baseline understanding of climate <span class="hlt">change</span> impacts, adaptation, and vulnerability in the region, but <span class="hlt">key</span> gaps are evident. Future research needs to target significant geographic disparities in understanding, consider risks and opportunities posed by climate <span class="hlt">change</span> outside of the subsistence hunting sector, complement case study research with regional analyses, and focus on identifying and characterizing sustainable and feasible adaptation interventions.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016NatSR...621251D','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016NatSR...621251D"><span>The Footprint of the Inter-<span class="hlt">decadal</span> Pacific Oscillation in Indian Ocean Sea Surface Temperatures</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Dong, Lu; Zhou, Tianjun; Dai, Aiguo; Song, Fengfei; Wu, Bo; Chen, Xiaolong</p> <p>2016-02-01</p> <p>Superimposed on a pronounced warming trend, the Indian Ocean (IO) sea surface temperatures (SSTs) also show considerable <span class="hlt">decadal</span> variations that can cause regional climate oscillations around the IO. However, the mechanisms of the IO <span class="hlt">decadal</span> variability remain unclear. Here we perform numerical experiments using a state-of-the-art, fully coupled climate model in which the external forcings with or without the observed SSTs in the tropical eastern Pacific Ocean (TEP) are applied for 1871-2012. Both the observed timing and magnitude of the IO <span class="hlt">decadal</span> variations are well reproduced in those experiments with the TEP SSTs prescribed to observations. Although the external forcings account for most of the warming trend, the <span class="hlt">decadal</span> variability in IO SSTs is dominated by internal variability that is induced by the TEP SSTs, especially the Inter-<span class="hlt">decadal</span> Pacific Oscillation (IPO). The IPO weakens (enhances) the warming of the external forcings by about 50% over the IO during IPO’s cold (warm) phase, which contributes about 10% to the recent global warming hiatus since 1999. The <span class="hlt">decadal</span> variability in IO SSTs is modulated by the IPO-induced atmospheric adjustment through <span class="hlt">changing</span> surface heat fluxes, sea surface height and thermocline depth.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/26884089','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/26884089"><span>The Footprint of the Inter-<span class="hlt">decadal</span> Pacific Oscillation in Indian Ocean Sea Surface Temperatures.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Dong, Lu; Zhou, Tianjun; Dai, Aiguo; Song, Fengfei; Wu, Bo; Chen, Xiaolong</p> <p>2016-02-17</p> <p>Superimposed on a pronounced warming trend, the Indian Ocean (IO) sea surface temperatures (SSTs) also show considerable <span class="hlt">decadal</span> variations that can cause regional climate oscillations around the IO. However, the mechanisms of the IO <span class="hlt">decadal</span> variability remain unclear. Here we perform numerical experiments using a state-of-the-art, fully coupled climate model in which the external forcings with or without the observed SSTs in the tropical eastern Pacific Ocean (TEP) are applied for 1871-2012. Both the observed timing and magnitude of the IO <span class="hlt">decadal</span> variations are well reproduced in those experiments with the TEP SSTs prescribed to observations. Although the external forcings account for most of the warming trend, the <span class="hlt">decadal</span> variability in IO SSTs is dominated by internal variability that is induced by the TEP SSTs, especially the Inter-<span class="hlt">decadal</span> Pacific Oscillation (IPO). The IPO weakens (enhances) the warming of the external forcings by about 50% over the IO during IPO's cold (warm) phase, which contributes about 10% to the recent global warming hiatus since 1999. The <span class="hlt">decadal</span> variability in IO SSTs is modulated by the IPO-induced atmospheric adjustment through <span class="hlt">changing</span> surface heat fluxes, sea surface height and thermocline depth.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017JGRD..122.3214A','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017JGRD..122.3214A"><span>Tracking the Pacific <span class="hlt">Decadal</span> Precession</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Anderson, Bruce T.; Furtado, Jason C.; Di Lorenzo, Emanuele; Short Gianotti, Daniel J.</p> <p>2017-03-01</p> <p>Events of recent years—including extended droughts across California, record fires across western Canada, and destabilization of marine ecosystems—highlight the profound impact of multiannual to <span class="hlt">decadal</span>-scale climate shifts upon physical, biological, and socioeconomic systems. While previous research has focused on the influence of <span class="hlt">decadal</span>-scale climate oscillations such as the Atlantic Multidecadal Oscillation and the Pacific <span class="hlt">Decadal</span> Oscillation/Interdecadal Pacific Oscillation, recent research has revealed the presence of a quasi-<span class="hlt">decadal</span> mode of climate variability that, unlike the quasi-stationary standing wave-like structure of the oscillatory modes, involves a progression of atmospheric pressure anomalies around the North Pacific, which has been termed the Pacific <span class="hlt">Decadal</span> Precession (PDP). In this paper we develop a set of methods to track the spatial and temporal evolutions of the PDP within historical observations as well as numerical model simulations. In addition, we provide a method that approximates the time evolution of the PDP across the full period of available data for real-time monitoring of the PDP. Through the development of these tracking methods, we hope to provide the community with a consistent framework for future analysis and diagnosis of the PDP's characteristics and underlying processes, thereby avoiding the use of different, and disparate, phenomenological- and mathematical-based indices that can confound our understanding of the PDP and its evolution.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2005JGRB..110.9405G','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2005JGRB..110.9405G"><span>Atmospheric and oceanic excitation of <span class="hlt">decadal</span>-scale Earth orientation variations</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Gross, Richard S.; Fukumori, Ichiro; Menemenlis, Dimitris</p> <p>2005-09-01</p> <p>The contribution of atmospheric wind and surface pressure and oceanic current and bottom pressure variations during 1949-2002 to exciting <span class="hlt">changes</span> in the Earth's orientation on <span class="hlt">decadal</span> timescales is investigated using an atmospheric angular momentum series computed from the National Centers for Environmental Prediction/National Center for Atmospheric Research (NCEP/NCAR) reanalysis project and an oceanic angular momentum series computed from a near-global ocean model that was forced by surface fluxes from the NCEP/NCAR reanalysis project. Not surprisingly, since <span class="hlt">decadal</span>-scale variations in the length of day are caused mainly by interactions between the mantle and core, the effect of the atmosphere and oceans is found to be only about 14% of that observed. More surprisingly, it is found that the effect of atmospheric and oceanic processes on <span class="hlt">decadal</span>-scale <span class="hlt">changes</span> in polar motion is also only about 20% (x component) and 38% (y component) of that observed. Therefore redistribution of mass within the atmosphere and oceans does not appear to be the main cause of the Markowitz wobble. It is also found that on timescales between 10 days and 4 years the atmospheric and oceanic angular momentum series used here have very little skill in explaining Earth orientation variations before the mid to late 1970s. This is attributed to errors in both the Earth orientation observations prior to 1976 when measurements from the accurate space-geodetic techniques became available and to errors in the modeled atmospheric fields prior to 1979 when the satellite era of global weather observing systems began.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/28474142','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/28474142"><span>The Gastroenterology Fellowship Match: A <span class="hlt">Decade</span> Later.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Huang, Robert J; Triadafilopoulos, George; Limsui, David</p> <p>2017-06-01</p> <p>Following a period of uncertainty and disorganization, the gastroenterology (GI) national leadership decided to reinstitute the fellowship match (the Match) under the auspices of the National Residency Matching Program (NRMP) in 2006. Although it has now been a <span class="hlt">decade</span> since the rebirth of the Match, there have been limited data published regarding progress made. In this piece, we discuss reasons for the original collapse of the GI Match, including most notably a perceived oversupply of GI physicians and a poor job market. We discuss the negative impacts the absence of the Match had on programs and on applicants, as well as the impetus to reorganize the Match under the NRMP. We then utilize data published annually by the NRMP to demonstrate that in the <span class="hlt">decade</span> since its rebirth, the GI Match has been remarkably successful in terms of attracting the participation of applicants and programs. We show that previous misguided concerns of an oversupply of GI physicians were not realized, and that GI fellowship positions remain highly competitive for internal medicine applicants. Finally, we discuss possible implications of recent <span class="hlt">changes</span> in the healthcare landscape on the GI Match.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017EGUGA..19.4103L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017EGUGA..19.4103L"><span>A Possible Cause for Recent <span class="hlt">Decadal</span> Atlantic Meridional Overturning Circulation Decline</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Latif, Mojib; Park, Taewook; Park, Wonsun</p> <p>2017-04-01</p> <p>The Atlantic Meridional Overturning Circulation (AMOC) is a major oceanic current system with widespread climate impacts. AMOC influences have been discussed among others with regard to Atlantic hurricane activity, regional sea level variability, and surface air temperature and precipitation <span class="hlt">changes</span> on land areas adjacent to the North Atlantic Ocean. Most climate models project significant AMOC slowing during the 21st century, if atmospheric greenhouse gas concentrations continue to rise unabatedly. Recently, a marked <span class="hlt">decadal</span> decline in AMOC strength has been observed, which was followed by strongly reduced oceanic poleward heat transport and record low sea surface temperature in parts of the North Atlantic. Here, we provide evidence from observations, re-analyses and climate models that the AMOC decline was due to the combined action of the North Atlantic Oscillation and East Atlantic Pattern, the two leading modes of North Atlantic atmospheric surface pressure variability, which prior to the decline both transitioned into their negative phases. This <span class="hlt">change</span> in atmospheric circulation diminished oceanic heat loss over the Labrador Sea and forced ocean circulation <span class="hlt">changes</span> lowering upper ocean salinity transport into that region. As a consequence, Labrador Sea deep convection weakened, which eventually slowed the AMOC. This study suggests a new mechanism for <span class="hlt">decadal</span> AMOC variability, which is important to multiyear climate predictability and climate <span class="hlt">change</span> detection in the North Atlantic sector.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.fs.usda.gov/treesearch/pubs/53154','TREESEARCH'); return false;" href="https://www.fs.usda.gov/treesearch/pubs/53154"><span>Pyrodiversity promotes avian diversity over the <span class="hlt">decade</span> following forest fire</span></a></p> <p><a target="_blank" href="http://www.fs.usda.gov/treesearch/">Treesearch</a></p> <p>Morgan W. Tingley; Viviana Ruiz-Gutiérrez; Robert L. Wilkerson; Christine A. Howell; Rodney B. Siegel</p> <p>2016-01-01</p> <p>An emerging hypothesis in fire ecology is that pyrodiversity increases species diversity.We test whether pyrodiversity—defined as the standard deviation of fire severity—increases avian biodiversity at two spatial scales, and whether and how this relationship may <span class="hlt">change</span> in the <span class="hlt">decade</span> following fire. We use a dynamic Bayesian community model applied to a multi-year...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015AGUFMED51B0809C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015AGUFMED51B0809C"><span>Lessons Learned from a <span class="hlt">Decade</span> of Serving Data to Students and the Public</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Chambers, L. H.; Martin, A. M.; Riebeek, H.; Jackson, R.</p> <p>2015-12-01</p> <p>NASA holds petabytes of Earth science data from a fleet of satellites going back <span class="hlt">decades</span>. While these data can be invaluable for use in STEM education and communication (E/C), the simple fact that the archive is public is not enough. The <span class="hlt">key</span> to successful use is to provide technological tools in strategic combination with best practices to meet the needs of various audiences. Students and teachers need access points that are specifically tailored to meet the technology resources in the classroom; citizen scientists need to feel a connection to NASA, easy-to-use technological interfaces, and are motivated by contributing to real research activities; the general public needs short, focused, easily digested tidbits. NASA's Earth science E/C teams have developed strategies combining audience knowledge with new technical capabilities through programs like MY NASA DATA, S'COOL, Earth Observatory, Giovanni, climate.gov, etc. The capability to offer a range of resources targeted to specific audience needs has advanced along several fronts over the last <span class="hlt">decade</span> through use of the following <span class="hlt">key</span> strategies: Regularly publishing articles, fact sheets and image captions written with greater detail than media releases to connect basic science concepts with current NASA research. Providing for differing levels of engagement, with basic, intermediate and advanced data access tools as well as lesson plans for grades K-2 through high school. Facilitating the important scientific process of asking questions once students are actively engaged though exploration and manipulation of current Earth data delivered through desktop and mobile apps.. Providing curated data sets that students can more easily interpret. Assessing users' needs through ongoing formative evaluation. Using Analytics to make data-driven decisions about technologies and approaches. We will survey the range of approaches to enabling data use for STEM E/C and will share some of the <span class="hlt">key</span> lessons learned.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/22087617','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/22087617"><span>Five <span class="hlt">keys</span> to real transformation in health care.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Senzon, Simon A</p> <p>2011-11-01</p> <p>Transformation in health care requires a deeply holistic approach. Natural leaders of such a transformation are the complementary and alternative medicine practitioners who already share a vision of wellness, prevention, and optimal human function. Central to this shared vision is lifestyle <span class="hlt">change</span> for patients and practitioners. Yet, to <span class="hlt">change</span> a lifestyle is to <span class="hlt">change</span> a self. Assisting individuals to transform their very sense of self in order to live healthier, more fulfilling lives centered on flourishing requires several important <span class="hlt">keys</span>. Visionary and unified leaders are the first <span class="hlt">key</span>. Structural support through coordination of health clinics locally and nationally is the second <span class="hlt">key</span>. This can be optimized by utilizing initiatives of the new Affordable Health Care Act, because it provides a potential impetus for deep structural <span class="hlt">changes</span>. An expanded evidence base for multifactorial approaches to wellness lifestyles is the third <span class="hlt">key</span>. A reorganizational orientation with an emphasis on the right timing of transformation is the fourth <span class="hlt">key</span>. The fifth <span class="hlt">key</span> is an Integral map, which brings together the personal, behavioral, cultural, and social domains. By utilizing such a map, one ensures that no aspect of the transformative revolution at hand slips away due to any misplaced focus, such as emphasizing only on the things we can see with our eyes. By embracing the essence of transformation in terms of a wholeness to all reality, an evolutionary unifying field with interior depth and exterior expression, health care is redefined more authentically. © Mary Ann Liebert, Inc.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018GeoRL..45.4991J','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018GeoRL..45.4991J"><span>Arctic Ocean Freshwater Content and Its <span class="hlt">Decadal</span> Memory of Sea-Level Pressure</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Johnson, Helen L.; Cornish, Sam B.; Kostov, Yavor; Beer, Emma; Lique, Camille</p> <p>2018-05-01</p> <p>Arctic freshwater content (FWC) has increased significantly over the last two <span class="hlt">decades</span>, with potential future implications for the Atlantic meridional overturning circulation downstream. We investigate the relationship between Arctic FWC and atmospheric circulation in the control run of a coupled climate model. Multiple linear lagged regression is used to extract the response of total Arctic FWC to a hypothetical step increase in the principal components of sea-level pressure. The results demonstrate that the FWC adjusts on a <span class="hlt">decadal</span> timescale, consistent with the idea that wind-driven ocean dynamics and eddies determine the response of Arctic Ocean circulation and properties to a <span class="hlt">change</span> in surface forcing, as suggested by idealized models and theory. Convolving the response of FWC to a <span class="hlt">change</span> in sea-level pressure with historical sea-level pressure variations reveals that the recent observed increase in Arctic FWC is related to natural variations in sea-level pressure.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016GeoJI.207..228W','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016GeoJI.207..228W"><span><span class="hlt">Decadal</span> variability in core surface flows deduced from geomagnetic observatory monthly means</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Whaler, K. A.; Olsen, N.; Finlay, C. C.</p> <p>2016-10-01</p> <p>Monthly means of the magnetic field measurements at ground observatories are a <span class="hlt">key</span> data source for studying temporal <span class="hlt">changes</span> of the core magnetic field. However, when they are calculated in the usual way, contributions of external (magnetospheric and ionospheric) origin may remain, which make them less favourable for studying the field generated by dynamo action in the core. We remove external field predictions, including a new way of characterizing the magnetospheric ring current, from the data and then calculate revised monthly means using robust methods. The geomagnetic secular variation (SV) is calculated as the first annual differences of these monthly means, which also removes the static crustal field. SV time-series based on revised monthly means are much less scattered than those calculated from ordinary monthly means, and their variances and correlations between components are smaller. On the annual to <span class="hlt">decadal</span> timescale, the SV is generated primarily by advection in the fluid outer core. We demonstrate the utility of the revised monthly means by calculating models of the core surface advective flow between 1997 and 2013 directly from the SV data. One set of models assumes flow that is constant over three months; such models exhibit large and rapid temporal variations. For models of this type, less complex flows achieve the same fit to the SV derived from revised monthly means than those from ordinary monthly means. However, those obtained from ordinary monthly means are able to follow excursions in SV that are likely to be external field contamination rather than core signals. Having established that we can find models that fit the data adequately, we then assess how much temporal variability is required. Previous studies have suggested that the flow is consistent with torsional oscillations (TO), solid body-like oscillations of fluid on concentric cylinders with axes aligned along the Earth's rotation axis. TO have been proposed to explain <span class="hlt">decadal</span></p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/19500882','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/19500882"><span>[<span class="hlt">Changes</span> in structure and function of the family of the adolescent in the last <span class="hlt">decade</span> (1997-2007)].</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Pérez Milena, Alejandro; Martínez Fernández, María Luz; Mesa Gallardo, Inmaculada; Pérez Milena, Rafael; Leal Helmling, Francisco Javier; Jiménez Pulido, Idoia</p> <p>2009-09-01</p> <p>To find out the structure and functioning of the family of the adolescent and its <span class="hlt">changes</span> in the last <span class="hlt">decade</span>. Cross-sectional descriptive study using questionnaires. Pupils in obligatory secondary education and high-school in one rural (Granada) and one urban (Jaén) area. Self-administered questionnaire (years 1997-2001-2004-2007) in which details of age, sex, family structure and family-Apgar test were recorded. A total of 1356 adolescents participated, 1271 questionnaires valid (259, 386, 246 and 380 respectively per year). Ages 12-18 years, equality of sexes. The nuclear family structure was predominant (78-84%), followed by single parent family in (7-11%), extended (6-7%) and reconstituted (2%). The family function was mainly normal (70-76%), with 30% dysfunction (slight dysfunction 18-21% and severe dysfunction 5-10%). The structure and family function does not vary by sex or the year of study, it is influenced by age: adolescents 16 years with a higher percentage of family dysfunction in 1997/2001 than the rest of ages, declining in the years 2004/2007 (P <0.05 chi(2)), similar to other ages. While the nuclear family in 1997 had a greater number of adolescents with normal family function (P <0.05 chi(2)), in the remaining years there were no significant differences between different family structures. The perception of family function in adolescents has <span class="hlt">changed</span> and now does not depend on sex, age and structure. Family care during adolescence should focus on promoting positive family dynamics, regardless of family structure.</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.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4255941','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4255941"><span>Two <span class="hlt">Decades</span> of Structure Building</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Gernsbacher, Morton Ann</p> <p>2014-01-01</p> <p>During the past <span class="hlt">decade</span> I have been developing a very simple framework for describing the cognitive processes and mechanisms involved in discourse comprehension. I call this framework the Structure Building Framework, and it is based on evidence provided during the first <span class="hlt">decade</span> of discourse processing research. According to the Structure Building Framework, the goal of comprehension is to build coherent mental representations or structures. Comprehenders build each structure by first laying a foundation. Comprehenders develop mental structures by mapping on new information when that information coheres or relates to previous information. However, when the incoming information is less related, comprehenders shift and attach a new substructure. The building blocks of mental structures are memory nodes, which are activated by incoming stimuli and controlled by two cognitive mechanisms: suppression and enhancement. In this article, first I review the seminal work on which the Structure Building Framework is based (the first <span class="hlt">decade</span> of structure building research); then I recount the research I have conducted to test the Structure Building Framework (the second <span class="hlt">decade</span> of structure building research). PMID:25484476</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/24405514','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/24405514"><span>BMC Medicine: a <span class="hlt">decade</span> of open access medical research.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Alam, Sabina; Patel, Jigisha</p> <p>2014-01-09</p> <p>On 24 November 2003, BMC Medicine published its first article. Ten years and over 900 articles later we look back at some of the most notable milestones for the journal and discuss advances and innovations in medicine over the last <span class="hlt">decade</span>. Our editorial board members, Leslie Biesecker, Thomas Powles, Chris Del Mar, Robert Snow and David Moher, also comment on the <span class="hlt">changes</span> they expect to see in their fields over the coming years.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70124289','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70124289"><span>A century of ocean warming on Florida <span class="hlt">Keys</span> coral reefs: historic in situ observations</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Kuffner, Ilsa B.; Lidz, Barbara H.; Hudson, J. Harold; Anderson, Jeffery S.</p> <p>2015-01-01</p> <p>There is strong evidence that global climate <span class="hlt">change</span> over the last several <span class="hlt">decades</span> has caused shifts in species distributions, species extinctions, and alterations in the functioning of ecosystems. However, because of high variability on short (i.e., diurnal, seasonal, and annual) timescales as well as the recency of a comprehensive instrumental record, it is difficult to detect or provide evidence for long-term, site-specific trends in ocean temperature. Here we analyze five in situ datasets from Florida <span class="hlt">Keys</span> coral reef habitats, including historic measurements taken by lighthouse keepers, to provide three independent lines of evidence supporting approximately 0.8 °C of warming in sea surface temperature (SST) over the last century. Results indicate that the warming observed in the records between 1878 and 2012 can be fully accounted for by the warming observed in recent <span class="hlt">decades</span> (from 1975 to 2007), documented using in situ thermographs on a mid-shore patch reef. The magnitude of warming revealed here is similar to that found in other SST datasets from the region and to that observed in global mean surface temperature. The geologic context and significance of recent ocean warming to coral growth and population dynamics are discussed, as is the future prognosis for the Florida reef tract.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/pages/biblio/1336997-impact-decadal-cloud-variations-earths-energy-budget','SCIGOV-DOEP'); return false;" href="https://www.osti.gov/pages/biblio/1336997-impact-decadal-cloud-variations-earths-energy-budget"><span>Impact of <span class="hlt">decadal</span> cloud variations on the Earth’s energy budget</span></a></p> <p><a target="_blank" href="http://www.osti.gov/pages">DOE PAGES</a></p> <p>Zhou, Chen; Zelinka, Mark D.; Klein, Stephen A.</p> <p>2016-10-31</p> <p>Feedbacks of clouds on climate <span class="hlt">change</span> strongly influence the magnitude of global warming. Cloud feedbacks, in turn, depend on the spatial patterns of surface warming, which vary on <span class="hlt">decadal</span> timescales. Therefore, the magnitude of the <span class="hlt">decadal</span> cloud feedback could deviate from the long-term cloud feedback. We present climate model simulations to show that the global mean cloud feedback in response to <span class="hlt">decadal</span> temperature fluctuations varies dramatically due to time variations in the spatial pattern of sea surface temperature. Here, we find that cloud anomalies associated with these patterns significantly modify the Earth’s energy budget. Specifically, the <span class="hlt">decadal</span> cloud feedback betweenmore » the 1980s and 2000s is substantially more negative than the long-term cloud feedback. This is a result of cooling in tropical regions where air descends, relative to warming in tropical ascent regions, which strengthens low-level atmospheric stability. Under these conditions, low-level cloud cover and its reflection of solar radiation increase, despite an increase in global mean surface temperature. Our results suggest that sea surface temperature pattern-induced low cloud anomalies could have contributed to the period of reduced warming between 1998 and 2013, and o er a physical explanation of why climate sensitivities estimated from recently observed trends are probably biased low.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/servlets/purl/1336997','SCIGOV-STC'); return false;" href="https://www.osti.gov/servlets/purl/1336997"><span>Impact of <span class="hlt">decadal</span> cloud variations on the Earth’s energy budget</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>Zhou, Chen; Zelinka, Mark D.; Klein, Stephen A.</p> <p></p> <p>Feedbacks of clouds on climate <span class="hlt">change</span> strongly influence the magnitude of global warming. Cloud feedbacks, in turn, depend on the spatial patterns of surface warming, which vary on <span class="hlt">decadal</span> timescales. Therefore, the magnitude of the <span class="hlt">decadal</span> cloud feedback could deviate from the long-term cloud feedback. We present climate model simulations to show that the global mean cloud feedback in response to <span class="hlt">decadal</span> temperature fluctuations varies dramatically due to time variations in the spatial pattern of sea surface temperature. Here, we find that cloud anomalies associated with these patterns significantly modify the Earth’s energy budget. Specifically, the <span class="hlt">decadal</span> cloud feedback betweenmore » the 1980s and 2000s is substantially more negative than the long-term cloud feedback. This is a result of cooling in tropical regions where air descends, relative to warming in tropical ascent regions, which strengthens low-level atmospheric stability. Under these conditions, low-level cloud cover and its reflection of solar radiation increase, despite an increase in global mean surface temperature. Our results suggest that sea surface temperature pattern-induced low cloud anomalies could have contributed to the period of reduced warming between 1998 and 2013, and o er a physical explanation of why climate sensitivities estimated from recently observed trends are probably biased low.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://eric.ed.gov/?q=non-financial&pg=7&id=ED224347','ERIC'); return false;" href="https://eric.ed.gov/?q=non-financial&pg=7&id=ED224347"><span>The Future of ESL and Bilingual Education in the Next <span class="hlt">Decade</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>Santiago, Ramon L.</p> <p></p> <p>Developments occurring at the national, state, and local levels that could affect the future of bilingual education and English as a second Language (ESL) instruction in the next <span class="hlt">decade</span> are considered. Attention is also directed to (1) the philosophy of the Reagan administration regarding social and educational programs, (2) budgetary <span class="hlt">changes</span> in…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFM.B14A..08C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFM.B14A..08C"><span>Differentiating surface water <span class="hlt">change</span> from seasonal and inter-annual variability in North Western Canada using multi-<span class="hlt">decadal</span> time series of data</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Carroll, M.; Loboda, T. V.</p> <p>2017-12-01</p> <p>Over the last several <span class="hlt">decades</span>, warming in the Arctic has outpaced the already impressiveincreases in global mean temperatures. The impact of these increases in temperature has beenobserved in a multitude of ecological <span class="hlt">changes</span> in North American tundra including <span class="hlt">changes</span> invegetative cover, depth of active layer, and surface water extent. The low topographic relief andcontinuous permafrost create an ideal environment for the formation of small water bodies—adefinitive feature of tundra surface. In this study, water bodies in Nunavut territory in northernCanada were mapped using a long-term record of remotely sensed observations at 30 m spatialresolution from the Landsat suite of instruments. The temporal trajectories of water extent between1985 and 2015 were assessed. Over 675,000 water bodies have been identified over the 31-yearstudy period with over 168,000 showing a significant (p < 0.05) trend in surface area. Approximately55% of water bodies with a significant trend were increasing in size while the remaining 45% weredecreasing in size. The overall net trend for water bodies with a significant trend is 0.009 ha year 1per water body.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/servlets/purl/1432221','SCIGOV-STC'); return false;" href="https://www.osti.gov/servlets/purl/1432221"><span><span class="hlt">Key</span> Metabolites and Mechanistic <span class="hlt">Changes</span> for Salt Tolerance in an Experimentally Evolved Sulfate-Reducing Bacterium, Desulfovibrio vulgaris</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>Zhou, Aifen; Lau, Rebecca; Baran, Richard</p> <p></p> <p>ABSTRACT. Rapid genetic and phenotypic adaptation of the sulfate-reducing bacteriumDesulfovibrio vulgarisHildenborough to salt stress was observed during experimental evolution. In order to identify <span class="hlt">key</span> metabolites important for salt tolerance, a clone, ES10-5, which was isolated from population ES10 and allowed to experimentally evolve under salt stress for 5,000 generations, was analyzed and compared to clone ES9-11, which was isolated from population ES9 and had evolved under the same conditions for 1,200 generations. These two clones were chosen because they represented the best-adapted clones among six independently evolved populations. ES10-5 acquired new mutations in genes potentially involved in salt tolerance, inmore » addition to the preexisting mutations and different mutations in the same genes as in ES9-11. Most basal abundance <span class="hlt">changes</span> of metabolites and phospholipid fatty acids (PLFAs) were lower in ES10-5 than ES9-11, but an increase of glutamate and branched PLFA i17:1ω9c under high-salinity conditions was persistent. ES9-11 had decreased cell motility compared to the ancestor; in contrast, ES10-5 showed higher cell motility under both nonstress and high-salinity conditions. Both genotypes displayed better growth energy efficiencies than the ancestor under nonstress or high-salinity conditions. Consistently, ES10-5 did not display most of the basal transcriptional <span class="hlt">changes</span> observed in ES9-11, but it showed increased expression of genes involved in glutamate biosynthesis, cation efflux, and energy metabolism under high salinity. These results demonstrated the role of glutamate as a <span class="hlt">key</span> osmolyte and i17:1ω9c as the major PLFA for salt tolerance inD. vulgaris. The mechanistic <span class="hlt">changes</span> in evolved genotypes suggested that growth energy efficiency might be a <span class="hlt">key</span> factor for selection. IMPORTANCE. High salinity (e.g., elevated NaCl) is a stressor that affects many organisms. Salt tolerance, a complex trait involving multiple cellular pathways, is</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/pages/biblio/1432221-key-metabolites-mechanistic-changes-salt-tolerance-experimentally-evolved-sulfate-reducing-bacterium-desulfovibrio-vulgaris','SCIGOV-DOEP'); return false;" href="https://www.osti.gov/pages/biblio/1432221-key-metabolites-mechanistic-changes-salt-tolerance-experimentally-evolved-sulfate-reducing-bacterium-desulfovibrio-vulgaris"><span><span class="hlt">Key</span> Metabolites and Mechanistic <span class="hlt">Changes</span> for Salt Tolerance in an Experimentally Evolved Sulfate-Reducing Bacterium, Desulfovibrio vulgaris</span></a></p> <p><a target="_blank" href="http://www.osti.gov/pages">DOE PAGES</a></p> <p>Zhou, Aifen; Lau, Rebecca; Baran, Richard; ...</p> <p>2017-11-14</p> <p>ABSTRACT. Rapid genetic and phenotypic adaptation of the sulfate-reducing bacteriumDesulfovibrio vulgarisHildenborough to salt stress was observed during experimental evolution. In order to identify <span class="hlt">key</span> metabolites important for salt tolerance, a clone, ES10-5, which was isolated from population ES10 and allowed to experimentally evolve under salt stress for 5,000 generations, was analyzed and compared to clone ES9-11, which was isolated from population ES9 and had evolved under the same conditions for 1,200 generations. These two clones were chosen because they represented the best-adapted clones among six independently evolved populations. ES10-5 acquired new mutations in genes potentially involved in salt tolerance, inmore » addition to the preexisting mutations and different mutations in the same genes as in ES9-11. Most basal abundance <span class="hlt">changes</span> of metabolites and phospholipid fatty acids (PLFAs) were lower in ES10-5 than ES9-11, but an increase of glutamate and branched PLFA i17:1ω9c under high-salinity conditions was persistent. ES9-11 had decreased cell motility compared to the ancestor; in contrast, ES10-5 showed higher cell motility under both nonstress and high-salinity conditions. Both genotypes displayed better growth energy efficiencies than the ancestor under nonstress or high-salinity conditions. Consistently, ES10-5 did not display most of the basal transcriptional <span class="hlt">changes</span> observed in ES9-11, but it showed increased expression of genes involved in glutamate biosynthesis, cation efflux, and energy metabolism under high salinity. These results demonstrated the role of glutamate as a <span class="hlt">key</span> osmolyte and i17:1ω9c as the major PLFA for salt tolerance inD. vulgaris. The mechanistic <span class="hlt">changes</span> in evolved genotypes suggested that growth energy efficiency might be a <span class="hlt">key</span> factor for selection. IMPORTANCE. High salinity (e.g., elevated NaCl) is a stressor that affects many organisms. Salt tolerance, a complex trait involving multiple cellular pathways, is</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2010AIPC.1211.1623V','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2010AIPC.1211.1623V"><span>Evolution of the Ultrasonic Inspection Requirements of Heavy Rotor Forgings Over the Past <span class="hlt">Decades</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Vrana, J.; Zimmer, A.; Bailey, K.; Angal, R.; Zombo, P.; Büchner, U.; Buschmann, A.; Shannon, R. E.; Lohmann, H.-P.; Heinrich, W.</p> <p>2010-02-01</p> <p>Heavy rotor forgings for land-based power generation turbines and generators are inspected ultrasonically. Several <span class="hlt">decades</span> ago the first inspections were conducted using manual, straight beam, contact transducers with simple, non-descript reporting requirements. The development of ultrasonic inspection capabilities, the <span class="hlt">change</span> in design engineer requirements, improvements of fracture mechanics calculations, experience with turbine operation, experience with the inspection technology, and probability of detection drove the <span class="hlt">changes</span> that have resulted in the current day inspection requirements: sizing technologies were implemented, detection limits were lowered, angle and pitch/catch (dual crystal) scans were introduced, and most recently automated equipment for the inspection was required. Due to all these <span class="hlt">changes</span>, model based sizing techniques, like DGS, and modern ultrasonic techniques, like phased array, are being introduced globally. This paper describes the evolution of the ultrasonic inspection requirements over the last <span class="hlt">decades</span> and presents an outlook for tomorrow.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018GeoRL..45..916L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018GeoRL..45..916L"><span>Current and Future <span class="hlt">Decadal</span> Trends in the Oceanic Carbon Uptake Are Dominated by Internal Variability</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Li, Hongmei; Ilyina, Tatiana</p> <p>2018-01-01</p> <p>We investigate the internal <span class="hlt">decadal</span> variability of the ocean carbon uptake using 100 ensemble simulations based on the Max Planck Institute Earth system model (MPI-ESM). We find that on <span class="hlt">decadal</span> time scales, internal variability (ensemble spread) is as large as the forced temporal variability (ensemble mean), and the largest internal variability is found in major carbon sink regions, that is, the 50-65°S band of the Southern Ocean, the North Pacific, and the North Atlantic. The MPI-ESM ensemble produces both positive and negative 10 year trends in the ocean carbon uptake in agreement with observational estimates. Negative <span class="hlt">decadal</span> trends are projected to occur in the future under RCP4.5 scenario. Due to the large internal variability, the Southern Ocean and the North Pacific require the most ensemble members (more than 53 and 46, respectively) to reproduce the forced <span class="hlt">decadal</span> trends. This number increases up to 79 in future <span class="hlt">decades</span> as CO2 emission trajectory <span class="hlt">changes</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/26089521','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/26089521"><span>OCEAN CIRCULATION. Observing the Atlantic Meridional Overturning Circulation yields a <span class="hlt">decade</span> of inevitable surprises.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Srokosz, M A; Bryden, H L</p> <p>2015-06-19</p> <p>The importance of the Atlantic Meridional Overturning Circulation (AMOC) heat transport for climate is well acknowledged. Climate models predict that the AMOC will slow down under global warming, with substantial impacts, but measurements of ocean circulation have been inadequate to evaluate these predictions. Observations over the past <span class="hlt">decade</span> have <span class="hlt">changed</span> that situation, providing a detailed picture of variations in the AMOC. These observations reveal a surprising degree of AMOC variability in terms of the intraannual range, the amplitude and phase of the seasonal cycle, the interannual <span class="hlt">changes</span> in strength affecting the ocean heat content, and the decline of the AMOC over the <span class="hlt">decade</span>, both of the latter two exceeding the variations seen in climate models. Copyright © 2015, American Association for the Advancement of Science.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/28883963','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/28883963"><span>World Rabies Day - a <span class="hlt">decade</span> of raising awareness.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Balaram, Deepashree; Taylor, Louise H; Doyle, Kim A S; Davidson, Elizabeth; Nel, Louis H</p> <p>2016-01-01</p> <p>World Rabies Day was set up in 2007 to raise global awareness about rabies, to provide information on how to prevent the disease in at-risk communities and support advocacy for increased efforts in rabies control. It is held annually on September 28th, with events, media outreach and other initiatives carried out by individuals, professionals, organisations and governments from the local to the international level. The Global Alliance for Rabies Control coordinates World Rabies Day, amplifying the campaign's reach through the provision of a central event platform and resources to support events across the world, the promotion of messages through <span class="hlt">key</span> rabies stakeholders, and the implementation of specific activities to highlight particular issues. Over the last <span class="hlt">decade</span>, more than 1,700 registered events have been held across the world and shared with others in the global rabies community. Events in canine rabies endemic countries, particularly in Africa and Asia, have increased over time. Beyond the individual events, World Rabies Day has gained the support of governments and international agencies that recognise its value in supporting existing rabies control initiatives and advocating for improvements. As the rabies landscape has <span class="hlt">changed</span>, World Rabies Day remains a general day of awareness but has also become an integral part of national, regional and global rabies elimination strategies. The global adoption of 2030 as the goal for the elimination of rabies as a public health threat has led to even greater opportunities for World Rabies Day to make a sustainable impact on rabies, by bringing the attention of policy makers and donors to the ongoing situation and elimination efforts in rabies-endemic countries.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=2974405','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=2974405"><span><span class="hlt">Changing</span> Attitudes Toward Influenza Vaccination in U.S. Kidney Transplant Programs Over the Past <span class="hlt">Decade</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>Kadambi, Pradeep V.; Harland, Robert C.; Thistlethwaite, J. Richard; West, Bradford L.; Udani, Suneel; Poduval, Rajiv; Josephson, Michelle A.</p> <p>2010-01-01</p> <p>Background and objectives: Influenza infection in transplant recipients is often associated with significant morbidity. Surveys were conducted in 1999 and 2009 to find out if the influenza vaccination practices in the U.S. transplant programs had <span class="hlt">changed</span> over the past 10 years. Design, setting, participants, & measurements: In 1999, a survey of the 217 United Network for Organ Sharing-certified kidney and kidney-pancreas transplant centers in the U.S. was conducted regarding their influenza vaccination practice patterns. A <span class="hlt">decade</span> later, a second similar survey of 239 transplant programs was carried out. Results: The 2009 respondents, compared with 1999, were more likely to recommend vaccination for kidney (94.5% versus 84.4%, P = 0.02) and kidney-pancreas recipients (76.8% versus 48.5%, P < 0.001), family members of transplant recipients (52.5% versus 21.0%, P < 0.001), and medical staff caring for transplant patients (79.6% versus 40.7%, P < 0.001). Physicians and other members of the transplant team were more likely to have been vaccinated in 2009 compared with 1999 (84.2% versus 62.3% of physicians, P < 0.001 and 91.2% versus 50.3% of nonphysicians, P < 0.001). Conclusions: Our study suggests a greater adoption of the Centers for Disease Control and Prevention influenza vaccination guidelines by U.S. transplant programs in vaccinating solid-organ transplant recipients, close family contacts, and healthcare workers. PMID:20595695</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014EGUGA..1613964I','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014EGUGA..1613964I"><span>Uncertainties in <span class="hlt">Decadal</span> Model Evaluation due to the Choice of Different Reanalysis Products</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Illing, Sebastian; Kadow, Christopher; Kunst, Oliver; Cubasch, Ulrich</p> <p>2014-05-01</p> <p>In recent years <span class="hlt">decadal</span> predictions have become very popular in the climate science community. A major task is the evaluation and validation of a <span class="hlt">decadal</span> prediction system. Therefore hindcast experiments are performed and evaluated against observation based or reanalysis data-sets. That is, various metrics and skill scores like the anomaly correlation or the mean squared error skill score (MSSS) are calculated to estimate potential prediction skill of the model system. Our results will mostly feature the Baseline 1 hindcast experiments from the MiKlip <span class="hlt">decadal</span> prediction system. MiKlip (www.fona-miklip.de) is a project for medium-term climate prediction funded by the Federal Ministry of Education and Research in Germany (BMBF) and has the aim to create a model system that can provide reliable <span class="hlt">decadal</span> forecasts on climate and weather. There are various reanalysis and observation based products covering at least the last forty years which can be used for model evaluation, for instance the 20th Century Reanalysis from NOAA-CIRES, the Climate Forecast System Reanalysis from NCEP or the Interim Reanalysis from ECMWF. Each of them is based on different climate models and observations. We will show that the choice of the reanalysis product has a huge impact on the value of various skill metrics. In some cases this may actually lead to a <span class="hlt">change</span> in the interpretation of the results, e.g. when one tries to compare two model versions and the anomaly correlation difference <span class="hlt">changes</span> its sign for two different reanalysis products. We will also show first results of our studies investigating the influence and effect of this source of uncertainty for <span class="hlt">decadal</span> model evaluation. Furthermore we point out regions which are most affected by this uncertainty and where one has to cautious interpreting skill scores. In addition we introduce some strategies to overcome or at least reduce this source of uncertainty.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017EGUGA..1917465S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017EGUGA..1917465S"><span>Predicting bi-<span class="hlt">decadal</span> organic carbon mineralization in northwestern European soils with Rock-Eval pyrolysis</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Soucemarianadin, Laure; Barré, Pierre; Baudin, François; Chenu, Claire; Houot, Sabine; Kätterer, Thomas; Macdonald, Andy; van Oort, Folkert; Plante, Alain F.; Cécillon, Lauric</p> <p>2017-04-01</p> <p>The organic carbon reservoir of soils is a <span class="hlt">key</span> component of climate <span class="hlt">change</span>, calling for an accurate knowledge of the residence time of soil organic carbon (SOC). Existing proxies of the size of SOC labile pool such as SOC fractionation or respiration tests are time consuming and unable to consistently predict SOC mineralization over years to <span class="hlt">decades</span>. Similarly, models of SOC dynamics often yield unrealistic values of the size of SOC kinetic pools. Thermal analysis of bulk soil samples has recently been shown to provide useful and cost-effective information regarding the long-term in-situ decomposition of SOC. Barré et al. (2016) analyzed soil samples from long-term bare fallow sites in northwestern Europe using Rock-Eval 6 pyrolysis (RE6), and demonstrated that persistent SOC is thermally more stable and has less hydrogen-rich compounds (low RE6 HI parameter) than labile SOC. The objective of this study was to predict SOC loss over a 20-year period (i.e. the size of the SOC pool with a residence time lower than 20 years) using RE6 indicators. Thirty-six archive soil samples coming from 4 long-term bare fallow chronosequences (Grignon, France; Rothamsted, Great Britain; Ultuna, Sweden; Versailles, France) were used in this study. For each sample, the value of bi-<span class="hlt">decadal</span> SOC mineralization was obtained from the observed SOC dynamics of its long-term bare fallow plot (approximated by a spline function). Those values ranged from 0.8 to 14.3 gC·kg-1 (concentration data), representing 8.6 to 50.6% of total SOC (proportion data). All samples were analyzed using RE6 and simple linear regression models were used to predict bi-<span class="hlt">decadal</span> SOC loss (concentration and proportion data) from 4 RE6 parameters: HI, OI, PC/SOC and T50 CO2 oxidation. HI (the amount of hydrogen-rich effluents formed during the pyrolysis phase of RE6; mgCH.g-1SOC) and OI (the CO2 yield during the pyrolysis phase of RE6; mgCO2.g-1SOC) parameters describe SOC bulk chemistry. PC/SOC (the amount of organic</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.fs.usda.gov/treesearch/pubs/45034','TREESEARCH'); return false;" href="https://www.fs.usda.gov/treesearch/pubs/45034"><span>Impacts on South Carolina timber production over the last five <span class="hlt">decades</span>.</span></a></p> <p><a target="_blank" href="http://www.fs.usda.gov/treesearch/">Treesearch</a></p> <p>Jinglong Mo; Thomas Straka; Richard Harper</p> <p>2013-01-01</p> <p>Timberland ownership patterns and national forest timber harvesting policy have undergone significant <span class="hlt">changes</span> in South Carolina over the past five <span class="hlt">decades</span>. Timber output studies for the state commonly focused on short time frames and seldom addressed timberland ownership patterns in detail. We describe fifty-year timber output for South Carolina, allowing us to address...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/27196890','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/27196890"><span><span class="hlt">Key</span> Developments in Ionic Liquid Crystals.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Alvarez Fernandez, Alexandra; Kouwer, Paul H J</p> <p>2016-05-16</p> <p>Ionic liquid crystals are materials that combine the classes of liquid crystals and ionic liquids. The first one is based on the multi-billion-dollar flat panel display industry, whilst the latter quickly developed in the past <span class="hlt">decades</span> into a family of highly-tunable non-volatile solvents. The combination yields materials with a unique set of properties, but also with many challenges ahead. In this review, we provide an overview of the <span class="hlt">key</span> concepts in ionic liquid crystals, particularly from a molecular perspective. What are the important molecular parameters that determine the phase behavior? How should they be introduced into the molecules? Finally, which other tools does one have to realize specific properties in the material?</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4881553','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4881553"><span><span class="hlt">Key</span> Developments in Ionic Liquid Crystals</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Alvarez Fernandez, Alexandra; Kouwer, Paul H. J.</p> <p>2016-01-01</p> <p>Ionic liquid crystals are materials that combine the classes of liquid crystals and ionic liquids. The first one is based on the multi-billion-dollar flat panel display industry, whilst the latter quickly developed in the past <span class="hlt">decades</span> into a family of highly-tunable non-volatile solvents. The combination yields materials with a unique set of properties, but also with many challenges ahead. In this review, we provide an overview of the <span class="hlt">key</span> concepts in ionic liquid crystals, particularly from a molecular perspective. What are the important molecular parameters that determine the phase behavior? How should they be introduced into the molecules? Finally, which other tools does one have to realize specific properties in the material? PMID:27196890</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70029010','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70029010"><span><span class="hlt">Changes</span> toward earlier streamflow timing across western North America</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, I.T.; Cayan, D.R.; Dettinger, M.D.</p> <p>2005-01-01</p> <p>The highly variable timing of streamflow in snowmelt-dominated basins across western North America is an important consequence, and indicator, of climate fluctuations. <span class="hlt">Changes</span> in the timing of snowmelt-derived streamflow from 1948 to 2002 were investigated in a network of 302 western North America gauges by examining the center of mass for flow, spring pulse onset dates, and seasonal fractional flows through trend and principal component analyses. Statistical analysis of the streamflow timing measures with Pacific climate indicators identified local and <span class="hlt">key</span> large-scale processes that govern the regionally coherent parts of the <span class="hlt">changes</span> and their relative importance. Widespread and regionally coherent trends toward earlier onsets of springtime snowmelt and streamflow have taken place across most of western North America, affecting an area that is much larger than previously recognized. These timing <span class="hlt">changes</span> have resulted in increasing fractions of annual flow occurring earlier in the water year by 1-4 weeks. The immediate (or proximal) forcings for the spatially coherent parts of the year-to-year fluctuations and longer-term trends of streamflow timing have been higher winter and spring temperatures. Although these temperature <span class="hlt">changes</span> are partly controlled by the <span class="hlt">decadal</span>-scale Pacific climate mode [Pacific <span class="hlt">decadal</span> oscillation (PDO)], a separate and significant part of the variance is associated with a springtime warming trend that spans the PDO phases. ?? 2005 American Meteorological Society.</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('http://hdl.handle.net/2060/20140000917','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20140000917"><span>Climate <span class="hlt">Change</span>: A New Metric to Measure <span class="hlt">Changes</span> in the Frequency of Extreme Temperatures using Record Data</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Munasinghe, L.; Jun, T.; Rind, D. H.</p> <p>2012-01-01</p> <p>Consensus on global warming is the result of multiple and varying lines of evidence, and one <span class="hlt">key</span> ramification is the increase in frequency of extreme climate events including record high temperatures. Here we develop a metric- called "record equivalent draws" (RED)-based on record high (low) temperature observations, and show that <span class="hlt">changes</span> in RED approximate <span class="hlt">changes</span> in the likelihood of extreme high (low) temperatures. Since we also show that this metric is independent of the specifics of the underlying temperature distributions, RED estimates can be aggregated across different climates to provide a genuinely global assessment of climate <span class="hlt">change</span>. Using data on monthly average temperatures across the global landmass we find that the frequency of extreme high temperatures increased 10-fold between the first three <span class="hlt">decades</span> of the last century (1900-1929) and the most recent <span class="hlt">decade</span> (1999-2008). A more disaggregated analysis shows that the increase in frequency of extreme high temperatures is greater in the tropics than in higher latitudes, a pattern that is not indicated by <span class="hlt">changes</span> in mean temperature. Our RED estimates also suggest concurrent increases in the frequency of both extreme high and extreme low temperatures during 2002-2008, a period when we observe a plateauing of global mean temperature. Using daily extreme temperature observations, we find that the frequency of extreme high temperatures is greater in the daily minimum temperature time-series compared to the daily maximum temperature time-series. There is no such observable difference in the frequency of extreme low temperatures between the daily minimum and daily maximum.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/servlets/purl/1253370','SCIGOV-STC'); return false;" href="https://www.osti.gov/servlets/purl/1253370"><span>The footprint of the inter-<span class="hlt">decadal</span> Pacific oscillation in Indian Ocean sea surface temperatures</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>Dong, Lu; Zhou, Tianjun; Dai, Aiguo</p> <p></p> <p>Superimposed on a pronounced warming trend, the Indian Ocean (IO) sea surface temperatures (SSTs) also show considerable <span class="hlt">decadal</span> variations that can cause regional climate oscillations around the IO. However, the mechanisms of the IO <span class="hlt">decadal</span> variability remain unclear. Here we perform numerical experiments using a state-of-the-art, fully coupled climate model in which the external forcings with or without the observed SSTs in the tropical eastern Pacific Ocean (TEP) are applied for 1871–2012. Both the observed timing and magnitude of the IO <span class="hlt">decadal</span> variations are well reproduced in those experiments with the TEP SSTs prescribed to observations. Although the external forcingsmore » account for most of the warming trend, the <span class="hlt">decadal</span> variability in IO SSTs is dominated by internal variability that is induced by the TEP SSTs, especially the Inter-<span class="hlt">decadal</span> Pacific Oscillation (IPO). The IPO weakens (enhances) the warming of the external forcings by about 50% over the IO during IPO’s cold (warm) phase, which contributes about 10% to the recent global warming hiatus since 1999. As a result, the <span class="hlt">decadal</span> variability in IO SSTs is modulated by the IPO-induced atmospheric adjustment through <span class="hlt">changing</span> surface heat fluxes, sea surface height and thermocline depth.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/pages/biblio/1253370-footprint-inter-decadal-pacific-oscillation-indian-ocean-sea-surface-temperatures','SCIGOV-DOEP'); return false;" href="https://www.osti.gov/pages/biblio/1253370-footprint-inter-decadal-pacific-oscillation-indian-ocean-sea-surface-temperatures"><span>The footprint of the inter-<span class="hlt">decadal</span> Pacific oscillation in Indian Ocean sea surface temperatures</span></a></p> <p><a target="_blank" href="http://www.osti.gov/pages">DOE PAGES</a></p> <p>Dong, Lu; Zhou, Tianjun; Dai, Aiguo; ...</p> <p>2016-02-17</p> <p>Superimposed on a pronounced warming trend, the Indian Ocean (IO) sea surface temperatures (SSTs) also show considerable <span class="hlt">decadal</span> variations that can cause regional climate oscillations around the IO. However, the mechanisms of the IO <span class="hlt">decadal</span> variability remain unclear. Here we perform numerical experiments using a state-of-the-art, fully coupled climate model in which the external forcings with or without the observed SSTs in the tropical eastern Pacific Ocean (TEP) are applied for 1871–2012. Both the observed timing and magnitude of the IO <span class="hlt">decadal</span> variations are well reproduced in those experiments with the TEP SSTs prescribed to observations. Although the external forcingsmore » account for most of the warming trend, the <span class="hlt">decadal</span> variability in IO SSTs is dominated by internal variability that is induced by the TEP SSTs, especially the Inter-<span class="hlt">decadal</span> Pacific Oscillation (IPO). The IPO weakens (enhances) the warming of the external forcings by about 50% over the IO during IPO’s cold (warm) phase, which contributes about 10% to the recent global warming hiatus since 1999. As a result, the <span class="hlt">decadal</span> variability in IO SSTs is modulated by the IPO-induced atmospheric adjustment through <span class="hlt">changing</span> surface heat fluxes, sea surface height and thermocline depth.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014AGUFM.A31C3044P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014AGUFM.A31C3044P"><span>On the Mechanisms Linking Nitrogen Oxides to Trends in Ammonium Nitrate Aerosol over the Last <span class="hlt">Decade</span> in the San Joaquin Valley</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Pusede, S. E.; Zhang, Q.; Parworth, C.; Kim, H.; Shusterman, A.; Saleh, A.; Duffey, K.; Wooldridge, P. J.; Valin, L. C.; Fried, A.; Nowak, J. B.; Crawford, J. H.; Cohen, R. C.</p> <p>2014-12-01</p> <p>Nitrogen oxide (NOx) abundances across the U.S. have fallen steadily over the last fifteen years. Patterns in anthropogenic sources result in 2-fold lower NOx on weekends than weekdays largely without co-occurring <span class="hlt">changes</span> in other emissions. These trends taken together provide a near perfect NOx constraint on the nonlinear chemistry of ozone, on the <span class="hlt">key</span> oxidants nitrate radical (NO3) and hydroxyl radical (OH), and on secondary aerosol formation. We use this NOx constraint to interpret trends in wintertime PM2.5 over the last <span class="hlt">decade</span> in San Joaquin Valley, California, a location with severe aerosol pollution and where a large portion of the total aerosol mass is ammonium nitrate (NH4NO3). We combine the 12-year routine monitoring record and the air- and ground-based DISCOVER-AQ-2013 datasets to quantify the impact of NOx emission controls on the frequency of wintertime exceedances of the national PM2.5 standard. Nitrate ion (NO3-) is the oxidation product of NO2 and is formed by distinct daytime and nighttime pathways, both of which are nonlinear functions of the NO2 abundance. We present observationally derived <span class="hlt">decadal</span> trends in both pathways and show that NOx reductions have worked to simultaneously increase daytime and decrease nighttime NH4NO3 production over the last 15 years. The net effect has been a substantial decrease in NH4NO3 via decreased NO3-radical initiated production in the nocturnal residual layer, a layer largely separated from nighttime emissions at the surface. Whereas NO3- production in the nocturnal residual layer drove NH4NO3 chemistry over the last <span class="hlt">decade</span>, OH-initiated chemistry at the surface is poised to be the most important source of NH4NO3 in the next <span class="hlt">decade</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013EGUGA..15.1465Z','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013EGUGA..15.1465Z"><span>Climate <span class="hlt">change</span> scenarios and <span class="hlt">key</span> climate indices in the Swiss Alpine region</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Zubler, Elias; Croci-Maspoli, Mischa; Frei, Christoph; Liniger, Mark; Scherrer, Simon; Appenzeller, Christof</p> <p>2013-04-01</p> <p>For climate adaption and to support climate mitigation policy it is of outermost importance to demonstrate the consequences of climate <span class="hlt">change</span> on a local level and in user oriented quantities. Here, a framework is presented to apply the Swiss national climate <span class="hlt">change</span> scenarios CH2011 to climate indices with direct relevance to applications, such as tourism, transportation, agriculture and health. This framework provides results on a high spatial and temporal resolution and can also be applied in mountainous regions such as the Alps. Results are shown for some <span class="hlt">key</span> indices, such as the number of summer days and tropical nights, growing season length, number of frost days, heating and cooling degree days, and the number of days with fresh snow. Particular focus is given to <span class="hlt">changes</span> in the vertical distribution for the future periods 2020-2049, 2045-2074 and 2070-2099 relative to the reference period 1980-2009 for the A1B, A2 and RCP3PD scenario. The number of days with fresh snow is approximated using a combination of temperature and precipitation as proxies. Some findings for the latest scenario period are: (1) a doubling of the number of summer days by the end of the century under the business-as-usual scenario A2, (2) tropical nights appear above 1500 m asl, (3) the number of frost days may be reduced by more than 3 months at altitudes higher than 2500 m, (4) an overall reduction of heating degree days of about 30% by the end of the century, but on the other hand an increase in cooling degree days in warm seasons, and (5) the number of days with fresh snow tends to go towards zero at low altitudes. In winter, there is little <span class="hlt">change</span> in snowfall above 2000 m asl (roughly -3 days) in all scenarios. The largest impact on snowfall is found along the Northern Alpine flank and the Jura (-10 days or roughly -50% in A1B for the winter season). It is also highlighted that the future projections for all indices strongly depend on the chosen scenario and on model uncertainty</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://files.eric.ed.gov/fulltext/EJ1134458.pdf','ERIC'); return false;" href="http://files.eric.ed.gov/fulltext/EJ1134458.pdf"><span>The Impact of Cooperative Learning on CHC Students' Achievements and Its <span class="hlt">Changes</span> over the Past <span class="hlt">Decade</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>Chen, Qiuxian; Liu, Yuan</p> <p>2017-01-01</p> <p>Informed by emergent learning theories and multiple evidenced benefits, cooperative learning has developed into a widely accepted organization mode of class in the Western context. For the same reason, cooperative learning is transferred, during the past <span class="hlt">decade</span>, into classrooms of Confucian Heritage Culture (CHC) contexts. Concerns, however, are…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/1992EOSTr..73..177S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/1992EOSTr..73..177S"><span>Mount Rainier: A <span class="hlt">decade</span> volcano</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Swanson, Donald A.; Malone, Stephen D.; Samora, Barbara A.</p> <p></p> <p>Mount Rainier, the highest (4392 m) volcano in the Cascade Range, towers over a population of more than 2.5 million in the Seattle-Tacoma metropolitan area, and its drainage system via the Columbia River potentially affects another 500,000 residents of southwestern Washington and northwestern Oregon (Figure 1). Mount Rainier is the most hazardous volcano in the Cascades in terms of its potential for magma-water interaction and sector collapse. Major eruptions, or debris flows even without eruption, pose significant dangers and economic threats to the region. Despite such hazard and risk, Mount Rainier has received little study; such important topics as its petrologic and geochemical character, its proximal eruptive history, its susceptibility to major edifice failure, and its development over time have been barely investigated. This situation may soon <span class="hlt">change</span> because of Mount Rainier's recent designation as a “<span class="hlt">Decade</span> Volcano.”</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015AGUFMGC53G1288W','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015AGUFMGC53G1288W"><span>The Growth Periods Responses of Double-season Paddy Rice to Climate <span class="hlt">Change</span> in Hunan Province, China over the Past Two <span class="hlt">Decades</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Wang, Y.; Li, Y.; Yi, M.; Ye, T.</p> <p>2015-12-01</p> <p>The shifts of timing and length of the growing season (TLGS) are important indicators of crop response to climate <span class="hlt">change</span>. With the help of satellite image data, it becomes feasible to retrieve the TLGS in a spatially continuous manner, which also accommodates local variation of TGSs. In this article, the TGSs of paddy rice in Hunan Province, China since 1995 was retrieved using times-series curves of MODIS Normalized Difference Vegetation Index (NDVI), Enhanced Vegetation Index (EVI), and Land Surface Water Index (LSWI). The <span class="hlt">change</span> in TLGS and its connection to regional climate <span class="hlt">change</span> was discussed. The results showed the advance of TGSs of double-season paddy rice and the reduction of GSL in the past 20 years, which is believed to be linked to the rise in the temperature and precipitation in the growth periods. Understanding the local variation and trend of TLGS influenced by climate <span class="hlt">change</span> is essential for making agricultural adaptive policies to reduce the risk of crop damaged, also can provide <span class="hlt">key</span> information for studying how multi-hazards affect crop exposure.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=1747960','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=1747960"><span>Tobacco use in popular movies during the past <span class="hlt">decade</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>Mekemson, C; Glik, D; Titus, K; Myerson, A; Shaivitz, A; Ang, A; Mitchell, S</p> <p>2004-01-01</p> <p>Objective: The top 50 commercially successful films released per year from 1991 to 2000 were content coded to assess trends in tobacco use over time and attributes of films predictive of higher smoking rates. Design: This observational study used media content analysis methods to generate data about tobacco use depictions in films studied (n = 497). Films are the basic unit of analysis. Once films were coded and preliminary analysis completed, outcome data were transformed to approximate multivariate normality before being analysed with general linear models and longitudinal mixed method regression methods. Main outcome measures: Tobacco use per minute of film was the main outcome measure used. Predictor variables include attributes of films and actors. Tobacco use was defined as any cigarette, cigar, and chewing tobacco use as well as the display of smoke and cigarette paraphernalia such as ashtrays, brand names, or logos within frames of films reviewed. Results: Smoking rates in the top films fluctuated yearly over the <span class="hlt">decade</span> with an overall modest downward trend (p < 0.005), with the exception of R rated films where rates went up. Conclusions: The decrease in smoking rates found in films in the past <span class="hlt">decade</span> is modest given extensive efforts to educate the entertainment industry on this issue over the past <span class="hlt">decade</span>. Monitoring, education, advocacy, and policy <span class="hlt">change</span> to bring tobacco depiction rates down further should continue. PMID:15564625</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/15564625','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/15564625"><span>Tobacco use in popular movies during the past <span class="hlt">decade</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Mekemson, C; Glik, D; Titus, K; Myerson, A; Shaivitz, A; Ang, A; Mitchell, S</p> <p>2004-12-01</p> <p>The top 50 commercially successful films released per year from 1991 to 2000 were content coded to assess trends in tobacco use over time and attributes of films predictive of higher smoking rates. This observational study used media content analysis methods to generate data about tobacco use depictions in films studied (n = 497). Films are the basic unit of analysis. Once films were coded and preliminary analysis completed, outcome data were transformed to approximate multivariate normality before being analysed with general linear models and longitudinal mixed method regression methods. Tobacco use per minute of film was the main outcome measure used. Predictor variables include attributes of films and actors. Tobacco use was defined as any cigarette, cigar, and chewing tobacco use as well as the display of smoke and cigarette paraphernalia such as ashtrays, brand names, or logos within frames of films reviewed. Smoking rates in the top films fluctuated yearly over the <span class="hlt">decade</span> with an overall modest downward trend (p < 0.005), with the exception of R rated films where rates went up. The decrease in smoking rates found in films in the past <span class="hlt">decade</span> is modest given extensive efforts to educate the entertainment industry on this issue over the past <span class="hlt">decade</span>. Monitoring, education, advocacy, and policy <span class="hlt">change</span> to bring tobacco depiction rates down further should continue.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://files.eric.ed.gov/fulltext/ED420285.pdf','ERIC'); return false;" href="http://files.eric.ed.gov/fulltext/ED420285.pdf"><span>Georgia's Health Professions: A <span class="hlt">Decade</span> of <span class="hlt">Change</span>, 1985-1995.</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>Morris, Libby V.; Little, Catherine J.</p> <p></p> <p>This report examines the supply of and demand for health care professionals in the state of Georgia, including information on education, demographics, and workforce <span class="hlt">changes</span>. Supply data analyzed included licensure and certification records; a survey of Georgia's major health care institutions provided demand data. Additionally, institutions of…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFM.B43G2209F','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFM.B43G2209F"><span><span class="hlt">Decadal</span> <span class="hlt">changes</span> in peat carbon accrual rates in bogs in Northern Minnesota</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Fissore, C.; Nater, E. A.; McFarlane, K. J.</p> <p>2017-12-01</p> <p>Throughout the Holocene, peatland ecosystems have accumulated substantial amounts of carbon (C) and currently store about one third of all soil organic carbon (SOC) worldwide. Large uncertainty still persists on whether peatland ecosystems located in northern latitudes will continue to act as C sinks, or if the effects of global warming will have greater effects on decomposition processes than on net ecosystem production. We investigated <span class="hlt">decadal</span> C accrual rates of the top 25 cm of peats in three Sphagnum-rich peatlands located in Northern Minnesota (two ombrotrophic bogs and one fen). We used radiocarbon analysis of Sphagnum cellulose and model fitting to determine peat ages, and peat FTIR spectroscopy to determine humification indices and relative decomposition of peat samples with depth. We had the scope to detect whether recent warming has had an effect on peat decomposition and C accumulation rates. Modeled C accumulation rates in the three peatlands during the past five <span class="hlt">decades</span> ranged between 78 and 107 g C m-2 yr-1 in the top 25 cm analyzed in this study, values that are higher than the 22 to 29 g C m-2 yr-1 obtained for long-term (millennial) accumulations for the entire bog profiles. Peat IR spectra and C:N ratios confirm low levels of decomposition across the bog sites, especially in the uppermost parts of the peat. The fen site showed very limited decomposition across the entire sampled profile. Higher rates of C accumulation, combined with low decomposition rates close to the surface provide a good estimate of net primary productivity. As substrate decomposition progresses over time, net rates of accumulation decrease. Peat decomposition was more pronounced in the lower depths of the sampled cores in the two ombrotrophic bogs than in the fen, likely an effect of larger temporal variation in water table depth in the bogs than in the fen. Some of the variation in C accumulation and decomposition observed in our bogs and fen suggests that future C</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/19167061','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/19167061"><span>Managing the pursuit of health and wealth: the <span class="hlt">key</span> challenges.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Fidler, David P; Drager, Nick; Lee, Kelley</p> <p>2009-01-24</p> <p>This article forms part of a six-part Series on trade and health, and sets the stage for this Series by analysing <span class="hlt">key</span> aspects of the relationship between trade and health. The Series takes stock of this relation and provides timely analysis of the <span class="hlt">key</span> challenges facing efforts to achieve an appropriate balance between trade and health across a diverse range of issues. This introductory article reviews how trade and health have risen and expanded on global policy agendas in the past <span class="hlt">decade</span> in unprecedented ways, describes how trade and health issues are respectively governed in international relations, examines the ongoing search for policy coherence between the two policy spheres, and highlights the topics of the remaining articles in the Series.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=2726934','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=2726934"><span>Managing the pursuit of health and wealth: the <span class="hlt">key</span> challenges</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Fidler, David P; Drager, Nick; Lee, Kelley</p> <p>2009-01-01</p> <p>This article forms part of a six-part Series on trade and health, and sets the stage for this Series by analysing <span class="hlt">key</span> aspects of the relationship between trade and health. The Series takes stock of this relation and provides timely analysis of the <span class="hlt">key</span> challenges facing efforts to achieve an appropriate balance between trade and health across a diverse range of issues. This introductory article reviews how trade and health have risen and expanded on global policy agendas in the past <span class="hlt">decade</span> in unprecedented ways, describes how trade and health issues are respectively governed in international relations, examines the ongoing search for policy coherence between the two policy spheres, and highlights the topics of the remaining articles in the Series. PMID:19167061</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/24180757','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/24180757"><span><span class="hlt">Decadal</span> trends in Indian Ocean ambient sound.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Miksis-Olds, Jennifer L; Bradley, David L; Niu, Xiaoyue Maggie</p> <p>2013-11-01</p> <p>The increase of ocean noise documented in the North Pacific has sparked concern on whether the observed increases are a global or regional phenomenon. This work provides evidence of low frequency sound increases in the Indian Ocean. A <span class="hlt">decade</span> (2002-2012) of recordings made off the island of Diego Garcia, UK in the Indian Ocean was parsed into time series according to frequency band and sound level. Quarterly sound level comparisons between the first and last years were also performed. The combination of time series and temporal comparison analyses over multiple measurement parameters produced results beyond those obtainable from a single parameter analysis. The ocean sound floor has increased over the past <span class="hlt">decade</span> in the Indian Ocean. Increases were most prominent in recordings made south of Diego Garcia in the 85-105 Hz band. The highest sound level trends differed between the two sides of the island; the highest sound levels decreased in the north and increased in the south. Rate, direction, and magnitude of <span class="hlt">changes</span> among the multiple parameters supported interpretation of source functions driving the trends. The observed sound floor increases are consistent with concurrent increases in shipping, wind speed, wave height, and blue whale abundance in the Indian Ocean.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/28720170','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/28720170"><span>A <span class="hlt">DECADE</span> OF HEALTH TECHNOLOGY ASSESSMENT IN POLAND.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Lipska, Iga; McAuslane, Neil; Leufkens, Hubert; Hövels, Anke</p> <p>2017-01-01</p> <p>The objective of this study is to illustrate and provide a better understanding of the role of health technology assessment (HTA) processes in decision making for drug reimbursement in Poland and how this approach could be considered by other countries of limited resources. We analyzed the evolution of the HTA system and processes in Poland over the past <span class="hlt">decade</span> and current developments based on publicly available information. The role of HTA in drug-reimbursement process in Poland has increased substantially over the recent <span class="hlt">decade</span>, starting in 2005 with the formation the Agency for Health Technology Assessment and Tariff System (AOTMiT). The <span class="hlt">key</span> success factors in this development were effective capacity building based on the use of international expertise, the implementation of transparent criteria into the drug reimbursement processes, and the selective approach to the adoption of innovative medicines based on the cost-effectiveness threshold among other criteria. While Poland is regarded as a leader in Central and Eastern Europe, there is room for improvement, especially with regard to the quality of HTA processes and the consistency of HTA guidelines with reimbursement law. In the "pragmatic" HTA model use by AOTMiT, the pharmaceutical company is responsible for the preparation of a reimbursement dossier of good quality in line with HTA guidelines while the assessment team in AOTMiT is responsible for critical review of that dossier. Adoption of this model may be considered by other countries with limited resources to balance differing priorities and ensure transparent and objective access to medicines for patients who need them.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015AGUFM.U31A..03H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015AGUFM.U31A..03H"><span>Atmospheric Aerosols in a <span class="hlt">Changing</span> World</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Heald, C. L.</p> <p>2015-12-01</p> <p>Aerosols in the atmosphere impact human and environmental health, visibility, and climate. Exposure to air pollution is the leading environmental cause of premature mortality world-wide. The role of aerosols on the Earth's climate represents the single largest source of uncertainty in our understanding of global radiative forcing. Tremendous strides have been made to clean up the air in recent <span class="hlt">decades</span>, and yet poor air quality continues to plague many regions of the world, and our understanding of how global <span class="hlt">change</span> will feedback on to aerosol sources, formation, and impacts is limited. In this talk, I will use recent results from my research group to highlight some of the <span class="hlt">key</span> uncertainties and research topics in global aerosol lifecycle.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4299358','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4299358"><span>More Becomes Less: Management Strategy Has Definitely <span class="hlt">Changed</span> over the Past <span class="hlt">Decade</span> of Splenic Injury—A Nationwide Population-Based Study</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Soo, Kwan-Ming; Lin, Tsung-Ying; Chen, Chao-Wen; Kuo, Liang-Chi; Wang, Jaw-Yuan; Lee, Wei-Che; Lin, Hsing-Lin</p> <p>2015-01-01</p> <p>Background. Blunt spleen injury is generally taken as major trauma which is potentially lethal. However, the management strategy has progressively <span class="hlt">changed</span> to noninvasive treatment over the <span class="hlt">decade</span>. This study aimed to (1) find out the incidence and trend of strategy <span class="hlt">change</span>; (2) investigate the effect of <span class="hlt">change</span> on the mortality rate over the study period; and (3) evaluate the risk factors of mortality. Materials and Methods. We utilized nationwide population-based data to explore the incidence of BSI during a 12-year study period. The demographic characteristics, including gender, age, surgical intervention, blood transfusion, availability of CT scans, and numbers of coexisting injuries, were collected for analysis. Mortality, hospital length of stay, and cost were as outcome variables. Results. 578 splenic injuries were recorded with an estimated incidence of 48 per million per year. The average 12-year overall mortality rate during hospital stay was 5.28% (29/549). There is a trend of decreasing operative management in patients (X 2, P = 0.004). The risk factors for mortality in BSI from a multivariate logistic regression analysis were amount of transfusion (OR 1.033, P < 0.001, CI 1.017–1.049), with or without CT obtained (OR 0.347, P = 0.026, CI 0.158–0.889), and numbers of coexisting injuries (OR 1.346, P = 0.043, CI 1.010–1.842). Conclusion. Although uncommon of BSI, management strategy is obviously <span class="hlt">changed</span> to nonoperative treatment without increasing mortality and blood transfusion under the increase of CT utilization. Patients with more coexisting injuries and more blood transfusion had higher mortality. PMID:25629032</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016EGUGA..1814041S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016EGUGA..1814041S"><span>Potential impacts of a future Grand Solar Minimum on <span class="hlt">decadal</span> regional climate <span class="hlt">change</span> and interannual hemispherical climate variability</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Spiegl, Tobias; Langematz, Ulrike</p> <p>2016-04-01</p> <p>The political, technical and socio-economic developments of the next <span class="hlt">decades</span> will determine the magnitude of 21st century climate <span class="hlt">change</span>, since they are inextricably linked to future anthropogenic greenhouse gas emissions. To assess the range of uncertainty that is related to these developments, it is common to assume different emission scenarios for 21st climate projections. While the uncertainties associated with the anthropogenic greenhouse gas forcing have been studied intensely, the contribution of natural climate drivers (particularly solar variability) to recent and future climate <span class="hlt">change</span> are subject of intense debate. The past 1,000 years featured at least 5 excursions (lasting 60-100 years) of exceptionally low solar activity, induced by a weak magnetic field of the Sun, so called Grand Solar Minima. While the global temperature response to such a decrease in solar activity is assumed to be rather small, nonlinear mechanisms in the climate system might amplify the regional temperature signal. This hypothesis is supported by the last Grand Solar Minimum (the Maunder Minimum, 1645-1715) which coincides with the Little Ice Age, an epoch which is characterized by severe cold and hardship over Europe, North America and Asia. The long-lasting minimum of Solar Cycle 23 as well as the overall weak maximum of Cycle 24 reveal the possibility for a return to Grand Solar Minimum conditions within the next <span class="hlt">decades</span>. The quantification of the implications of such a projected decrease in solar forcing is of ultimate importance, given the on-going public discussion of the role of carbon dioxide emissions for global warming, and the possible role a cooling due to decreasing solar activity could be ascribed to. Since there is still no clear consensus about the actual strength of the Maunder Minimum, we used 3 acknowledged solar reconstruction datasets that show significant differences in both, total solar irradiance (TSI) and spectral irradiance (SSI) to simulate a future</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://images.nasa.gov/#/details-PIA03460.html','SCIGOVIMAGE-NASA'); return false;" href="https://images.nasa.gov/#/details-PIA03460.html"><span>Pacific <span class="hlt">Decadal</span> Oscillation</span></a></p> <p><a target="_blank" href="https://images.nasa.gov/">NASA Image and Video Library</a></p> <p></p> <p>2001-11-07</p> <p>Like fall and winter of 2000, this year NASA Topex/Poseidon satellite data shows that the Pacific ocean continues to be dominated by the strong Pacific <span class="hlt">Decadal</span> Oscillation, which is larger than the El Niño/La Niña pattern.</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('http://www.osti.gov/accomplishments/documents/fullText/ACC0409.pdf','DOE-RDACC'); return false;" href="http://www.osti.gov/accomplishments/documents/fullText/ACC0409.pdf"><span><span class="hlt">Decades</span> of Discovery</span></a></p> <p><a target="_blank" href="http://www.osti.gov/accomplishments/fieldedsearch.html">DOE R&D Accomplishments Database</a></p> <p></p> <p>2011-06-01</p> <p>For the past two-and-a-half <span class="hlt">decades</span>, the Office of Science at the U.S. Department of Energy has been at the forefront of scientific discovery. Over 100 important discoveries supported by the Office of Science are represented in this document.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://files.eric.ed.gov/fulltext/EJ1055170.pdf','ERIC'); return false;" href="http://files.eric.ed.gov/fulltext/EJ1055170.pdf"><span>A <span class="hlt">Decade</span> of Evolution in the Practice Teaching Component of a Canadian Teacher Education Program: What Drove <span class="hlt">Change</span>, What Insights Were Gleaned, and What Challenges Lie Ahead</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>Benson, Fiona; Hooton, Kate</p> <p>2014-01-01</p> <p>This paper explores the many and diverse factors that have driven <span class="hlt">changes</span> to the field-based component of a program of teacher education in a large Canadian university over the past 10 years. We look at <span class="hlt">key</span> contexts of influence to any work in program <span class="hlt">change</span>; that of internal and external bodies at the institutional level, the operational or…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012EGUGA..1410863R','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012EGUGA..1410863R"><span>Human effects on estuarine shoreline <span class="hlt">decadal</span> evolution</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Rilo, A.; Freire, P.; Ceia, R.; Mendes, R. N.; Catalão, J.; Taborda, R.</p> <p>2012-04-01</p> <p>Due to their sheltered conditions and natural resources, estuaries were always attractive to human activities (industrial, agriculture, residential and recreation). Consequently, the complex interactions between anthropogenic and natural drivers increase estuarine shoreline vulnerability to climate <span class="hlt">changes</span> impacts. The environmental sustainability of these systems depends on a fragile balance between societal development and natural values that can be further disturbed by climate <span class="hlt">change</span> effects. This challenging task for scientific community, managers and stakeholders can only be accomplished with interdisplinary approaches. In this context, it seems clear that estuarine management plans should incorporate the concept of <span class="hlt">change</span> into the planning of policy decisions since these natural dynamic areas are often under human pressure and are recognized as sensitive to climate <span class="hlt">change</span> effects. Therefore, the knowledge about historical evolution of estuarine shoreline is important to provide new insights on the spatial and temporal dimensions of estuarine <span class="hlt">change</span>. This paper aims to present and discuss shoreline <span class="hlt">changes</span> due to human intervention in Tagus estuary, located on the west coast of Portugal. Detailed margins cartography, in a 550m fringe (drawn inland from the highest astronomical tide line), was performed based on 2007 orthophotos (spatial resolution of 0.5 m) analysis. Several classification categories were considered, as urbanized areas, industrial, port and airport facilities, agriculture spaces, green areas and natural zones. The estuarine bed (area bellow the highest astronomical tide line) was also mapped (including human occupation, natural habitats, morpho-sedimentary units) based on the geographic information above and LANSAT 7 TM+ images using image processing techniques. Aerial photographs dated from 1944, 1946, 1948, 1955 and 1958 were analyzed for a set of pilot zones in order to fully understand the <span class="hlt">decadal</span> shoreline <span class="hlt">change</span>. Estuarine bed presents</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/23311905','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/23311905"><span>Socially disempowered women as the <span class="hlt">key</span> to addressing <span class="hlt">change</span> in Malawi: how do they do it?</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Macintyre, Linda M; Rankin, Sally; Pinderhughes, Howard; Waters, Catherine M; Schell, Ellen; Fiedler, Rachel</p> <p>2013-01-01</p> <p>Malawi women are in the ironic juxtaposition of being socially disempowered while, at the same time, thought to hold the <span class="hlt">key</span> to shaping an effective community response to the HIV crisis. Based on this juxtaposition, a descriptive, qualitative study was conducted in Malawi and the United States where 26 participants from nongovernmental organizations (NGOs) and community-based organizations (CBOs) discussed the roles of Malawi women. Interviews were audiotaped, transcribed, and analyzed. We identified an improvement in women's economic status as the strongest factor in reducing gender inequities. Through providing stipends for rural Malawi women, one NGO created unintended <span class="hlt">changes</span> in gender roles.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/26406469','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/26406469"><span><span class="hlt">Changes</span> in the Prevalence of Rheumatic Diseases in Shantou, China, in the Past Three <span class="hlt">Decades</span>: A COPCORD Study.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Zeng, Shao-Ying; Gong, Yao; Zhang, Yu-Ping; Chen, Su-Biao; Chen, Jun-Yang; Lin, Chu-Qing; Peng, Jian-Hua; Hou, Zhi-Duo; Zhong, Jian-Qiu; Liang, Hong-Jin; Huang, Guo-Hai; Wang, Dan-Min; Lai, Huai-Yuan; Li, Li-Ping; Zeng, Qing Yu</p> <p>2015-01-01</p> <p>This study aimed to clarify <span class="hlt">changes</span> in the prevalence of rheumatic diseases in Shantou, China, in the past 3 <span class="hlt">decades</span> and validate whether stair-climbing is a risk factor for knee pain and knee osteoarthritis (KOA). The World Health Organization-International League Against Rheumatism Community Oriented Program for Control of Rheumatic Diseases (COPCORD) protocol was implemented. In all, 2337 adults living in buildings without elevators and 1719 adults living in buildings with elevators were surveyed. The prevalence of rheumatic pain at any site and in the knee was 15.7% and 10.2%, respectively; both types of pain had a significantly higher incidence in residents of buildings without elevators than was reported by people who lived in buildings with elevators (14.9% vs. 10.6% and 11.32% vs. 8.82%, respectively) (both P < 0.0001). The prevalence of rheumatic pain in the neck, lumbar spine, shoulder, elbow, and foot was 5.6%, 4.5%, 3.1%, 1.4%, and 1.8%, respectively; these findings were similar to the data from the 1987 rural survey, but were somewhat lower than data reported in the urban and suburban surveys of the 1990s, with the exception of neck and lumbar pain. The prevalence of KOA, gout, and fibromyalgia was 7.10%, 1.08%, and 0.07%, respectively, and their prevalence increased significantly compared with those in previous studies from the 20th century. There were no significant differences in the prevalence of rheumatoid arthritis (RA) (0.35%) or ankylosing spondylitis (AS) (0.31%) compared to that reported in prior surveys. The prevalence of KOA was higher in for residents of buildings without elevators than that in those who had access to elevators (16-64 years, 5.89% vs. 3.95%, P = 0.004; 16->85 years, 7.64% vs. 6.26%, P = 0.162). The prevalence of RA and AS remained stable, whereas that of KOA, gout, and fibromyalgia has increased significantly in Shantou, China, during the past 3 <span class="hlt">decades</span>. Stair-climbing might be an important risk factor for knee pain and</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2006SPIE.6241E..0SK','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2006SPIE.6241E..0SK"><span>Extending <span class="hlt">key</span> sharing: how to generate a <span class="hlt">key</span> tightly coupled to a network security policy</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Kazantzidis, Matheos</p> <p>2006-04-01</p> <p>Current state of the art security policy technologies, besides the small scale limitation and largely manual nature of accompanied management methods, are lacking a) in real-timeliness of policy implementation and b) vulnerabilities and inflexibility stemming from the centralized policy decision making; even if, for example, a policy description or access control database is distributed, the actual decision is often a centralized action and forms a system single point of failure. In this paper we are presenting a new fundamental concept that allows implement a security policy by a systematic and efficient <span class="hlt">key</span> distribution procedure. Specifically, we extend the polynomial Shamir <span class="hlt">key</span> splitting. According to this, a global <span class="hlt">key</span> is split into n parts, any k of which can re-construct the original <span class="hlt">key</span>. In this paper we present a method that instead of having "any k parts" be able to re-construct the original <span class="hlt">key</span>, the latter can only be reconstructed if <span class="hlt">keys</span> are combined as any access control policy describes. This leads into an easily deployable <span class="hlt">key</span> generation procedure that results a single <span class="hlt">key</span> per entity that "knows" its role in the specific access control policy from which it was derived. The system is considered efficient as it may be used to avoid expensive PKI operations or pairwise <span class="hlt">key</span> distributions as well as provides superior security due to its distributed nature, the fact that the <span class="hlt">key</span> is tightly coupled to the policy, and that policy <span class="hlt">change</span> may be implemented easier and faster.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.fs.usda.gov/treesearch/pubs/55859','TREESEARCH'); return false;" href="https://www.fs.usda.gov/treesearch/pubs/55859"><span>Overstory structure and surface cover dynamics in the <span class="hlt">decade</span> following the Hayman Fire, Colorado</span></a></p> <p><a target="_blank" href="http://www.fs.usda.gov/treesearch/">Treesearch</a></p> <p>Paula J. Fornwalt; Camille S. Stevens-Rumann; Byron J. Collins</p> <p>2018-01-01</p> <p>The 2002 Hayman Fire burned with mixed-severity across a 400-ha dry conifer study site in Colorado, USA, where overstory tree and surface cover attributes had been recently measured on 20 0.1-ha permanent plots. We remeasured these plots repeatedly during the first post-fire <span class="hlt">decade</span> to examine how the attributes <span class="hlt">changed</span> through time and whether <span class="hlt">changes</span> were influenced...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3529625','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3529625"><span>Rethinking health systems strengthening: <span class="hlt">key</span> systems thinking tools and strategies for transformational <span class="hlt">change</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>Swanson, R Chad; Cattaneo, Adriano; Bradley, Elizabeth; Chunharas, Somsak; Atun, Rifat; Abbas, Kaja M; Katsaliaki, Korina; Mustafee, Navonil; Mason Meier, Benjamin; Best, Allan</p> <p>2012-01-01</p> <p>While reaching consensus on future plans to address current global health challenges is far from easy, there is broad agreement that reductionist approaches that suggest a limited set of targeted interventions to improve health around the world are inadequate. We argue that a comprehensive systems perspective should guide health practice, education, research and policy. We propose <span class="hlt">key</span> ‘systems thinking’ tools and strategies that have the potential for transformational <span class="hlt">change</span> in health systems. Three overarching themes span these tools and strategies: collaboration across disciplines, sectors and organizations; ongoing, iterative learning; and transformational leadership. The proposed tools and strategies in this paper can be applied, in varying degrees, to every organization within health systems, from families and communities to national ministries of health. While our categorization is necessarily incomplete, this initial effort will provide a valuable contribution to the health systems strengthening debate, as the need for a more systemic, rigorous perspective in health has never been greater. PMID:23014154</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/23014154','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/23014154"><span>Rethinking health systems strengthening: <span class="hlt">key</span> systems thinking tools and strategies for transformational <span class="hlt">change</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Swanson, R Chad; Cattaneo, Adriano; Bradley, Elizabeth; Chunharas, Somsak; Atun, Rifat; Abbas, Kaja M; Katsaliaki, Korina; Mustafee, Navonil; Mason Meier, Benjamin; Best, Allan</p> <p>2012-10-01</p> <p>While reaching consensus on future plans to address current global health challenges is far from easy, there is broad agreement that reductionist approaches that suggest a limited set of targeted interventions to improve health around the world are inadequate. We argue that a comprehensive systems perspective should guide health practice, education, research and policy. We propose <span class="hlt">key</span> 'systems thinking' tools and strategies that have the potential for transformational <span class="hlt">change</span> in health systems. Three overarching themes span these tools and strategies: collaboration across disciplines, sectors and organizations; ongoing, iterative learning; and transformational leadership. The proposed tools and strategies in this paper can be applied, in varying degrees, to every organization within health systems, from families and communities to national ministries of health. While our categorization is necessarily incomplete, this initial effort will provide a valuable contribution to the health systems strengthening debate, as the need for a more systemic, rigorous perspective in health has never been greater.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/19491346','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/19491346"><span>Strategic management and organizational behavior in dental education: reflections on <span class="hlt">key</span> issues in an environment of <span class="hlt">change</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Dunning, David G; Durham, Timothy M; Lange, Brian M; Aksu, Mert N</p> <p>2009-06-01</p> <p>With issues such as shrinking revenue, access to care, faculty workloads, and graying faculty, dental schools are faced with difficult challenges that fall to dental school deans to manage. Do dental school deans have the organizational skill sets and ethical frameworks necessary to address the challenges now facing dental schools? The purpose of this article is to pose questions and suggestions regarding some of the <span class="hlt">key</span> issues in dental colleges today and to stimulate discussion in the dental community about needed <span class="hlt">changes</span> in dental education.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014AGUFM.C41B0347M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014AGUFM.C41B0347M"><span>Multi-<span class="hlt">Decadal</span> Comparison between Clean-Ice and Debris-Covered Glaciers in the Eastern Himalaya</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Maurer, J. M.; Rupper, S.</p> <p>2014-12-01</p> <p>Himalayan glaciers are important natural resources and climatic indicators. Many of these glaciers have debris-covered ablation zones, while others are mostly clean ice. Regarding glacier dynamics, it is expected that debris-covered glaciers will respond differently to atmospheric warming compared to clean ice glaciers. In the Bhutanese Himalaya, there are (1) north flowing clean-ice glaciers with high velocities, likely with large amounts of basal sliding, and (2) south flowing debris-covered glaciers with slow velocities, thermokarst features, and influenced more by the Indian Summer Monsoon. This region, therefore, is ideal for comparing the dynamical response of clean-ice versus debris-covered glaciers to climatic <span class="hlt">change</span>. In particular, previous studies have suggested the north flowing glaciers are likely adjusting more dynamically (i.e. retreating) in response to climate variations, while the south flowing glaciers are likely experiencing downwasting, with stagnant termini locations. We test this hypothesis by assessing glacier <span class="hlt">changes</span> over three <span class="hlt">decades</span> in the Bhutan region using a newly-developed workflow to extract DEMs and orthorectified imagery from both 1976 historical spy satellite images and 2006 ASTER images. DEM differencing for both debris-covered and clean glaciers allows for quantification of glacier surface elevation <span class="hlt">changes</span>, while orthorectified imagery allows for measuring <span class="hlt">changes</span> in glacier termini. The same stereo-matching, denoising, and georeferencing methodology is used on both datasets to ensure consistency, while the three <span class="hlt">decade</span> timespan allows for a better signal to noise ratio compared to studies performed on shorter timescales. The results of these analyses highlight the similarities and differences in the <span class="hlt">decadal</span> response of clean-ice and debris-covered glaciers to climatic <span class="hlt">change</span>, and provide insights into the complex dynamics of debris-covered glaciers in the monsoonal Himalayas.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4974611','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4974611"><span>Three-<span class="hlt">decade</span> long fertilization-induced soil organic carbon sequestration depends on edaphic characteristics in six typical croplands</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Liang, Feng; Li, Jianwei; Yang, Xueyun; Huang, Shaomin; Cai, Zejiang; Gao, Hongjun; Ma, Junyong; Cui, Xian; Xu, Minggang</p> <p>2016-01-01</p> <p>Fertilizations affect soil organic carbon (SOC) content but the relative influences of the edaphic and climate factors on SOC storage are rarely studied across wide spatiotemporal scales. This study synthesized long-term datasets of fertilization experiments in six typical Chinese croplands, and calculated annual C input from crops and manure amendments, <span class="hlt">changes</span> in SOC storage (ΔSOC) and C sequestration efficiency (i.e. the percentage of soil C <span class="hlt">change</span> per unit of C input, hereafter referred as CSE) in 0–20 cm soil over three <span class="hlt">decades</span>. Three fertilization treatments include no fertilization (CK), chemical nitrogen, phosphorus and potassium fertilizers (NPK) and combined chemical fertilizers and manure (NPKM). Results showed significant fertilization effects on C input and ΔSOC (NPKM>NPK>CK), and significantly higher CSE in Qiyang at Hunan than Zhengzhou at Henan and Heihe at Heilongjiang. The variance partitioning analysis (VPA) showed more variance of CSE can be explained by edaphic factors (up to 39.7%) than other factors. Furthermore, soil available N content and pH were identified as the major soil properties explaining CSE variance. This study demonstrated <span class="hlt">key</span> controls of soil fertility factors on SOC sequestration and informs the need to develop strategic soil management plan to promote soil carbon sequestration under long-term intensive fertilization. PMID:27492771</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016NatSR...630350L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016NatSR...630350L"><span>Three-<span class="hlt">decade</span> long fertilization-induced soil organic carbon sequestration depends on edaphic characteristics in six typical croplands</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Liang, Feng; Li, Jianwei; Yang, Xueyun; Huang, Shaomin; Cai, Zejiang; Gao, Hongjun; Ma, Junyong; Cui, Xian; Xu, Minggang</p> <p>2016-08-01</p> <p>Fertilizations affect soil organic carbon (SOC) content but the relative influences of the edaphic and climate factors on SOC storage are rarely studied across wide spatiotemporal scales. This study synthesized long-term datasets of fertilization experiments in six typical Chinese croplands, and calculated annual C input from crops and manure amendments, <span class="hlt">changes</span> in SOC storage (ΔSOC) and C sequestration efficiency (i.e. the percentage of soil C <span class="hlt">change</span> per unit of C input, hereafter referred as CSE) in 0-20 cm soil over three <span class="hlt">decades</span>. Three fertilization treatments include no fertilization (CK), chemical nitrogen, phosphorus and potassium fertilizers (NPK) and combined chemical fertilizers and manure (NPKM). Results showed significant fertilization effects on C input and ΔSOC (NPKM>NPK>CK), and significantly higher CSE in Qiyang at Hunan than Zhengzhou at Henan and Heihe at Heilongjiang. The variance partitioning analysis (VPA) showed more variance of CSE can be explained by edaphic factors (up to 39.7%) than other factors. Furthermore, soil available N content and pH were identified as the major soil properties explaining CSE variance. This study demonstrated <span class="hlt">key</span> controls of soil fertility factors on SOC sequestration and informs the need to develop strategic soil management plan to promote soil carbon sequestration under long-term intensive fertilization.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/27492771','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/27492771"><span>Three-<span class="hlt">decade</span> long fertilization-induced soil organic carbon sequestration depends on edaphic characteristics in six typical croplands.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Liang, Feng; Li, Jianwei; Yang, Xueyun; Huang, Shaomin; Cai, Zejiang; Gao, Hongjun; Ma, Junyong; Cui, Xian; Xu, Minggang</p> <p>2016-08-05</p> <p>Fertilizations affect soil organic carbon (SOC) content but the relative influences of the edaphic and climate factors on SOC storage are rarely studied across wide spatiotemporal scales. This study synthesized long-term datasets of fertilization experiments in six typical Chinese croplands, and calculated annual C input from crops and manure amendments, <span class="hlt">changes</span> in SOC storage (ΔSOC) and C sequestration efficiency (i.e. the percentage of soil C <span class="hlt">change</span> per unit of C input, hereafter referred as CSE) in 0-20 cm soil over three <span class="hlt">decades</span>. Three fertilization treatments include no fertilization (CK), chemical nitrogen, phosphorus and potassium fertilizers (NPK) and combined chemical fertilizers and manure (NPKM). Results showed significant fertilization effects on C input and ΔSOC (NPKM>NPK>CK), and significantly higher CSE in Qiyang at Hunan than Zhengzhou at Henan and Heihe at Heilongjiang. The variance partitioning analysis (VPA) showed more variance of CSE can be explained by edaphic factors (up to 39.7%) than other factors. Furthermore, soil available N content and pH were identified as the major soil properties explaining CSE variance. This study demonstrated <span class="hlt">key</span> controls of soil fertility factors on SOC sequestration and informs the need to develop strategic soil management plan to promote soil carbon sequestration under long-term intensive fertilization.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/27708152','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/27708152"><span>Pyrodiversity promotes avian diversity over the <span class="hlt">decade</span> following forest fire.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Tingley, Morgan W; Ruiz-Gutiérrez, Viviana; Wilkerson, Robert L; Howell, Christine A; Siegel, Rodney B</p> <p>2016-10-12</p> <p>An emerging hypothesis in fire ecology is that pyrodiversity increases species diversity. We test whether pyrodiversity-defined as the standard deviation of fire severity-increases avian biodiversity at two spatial scales, and whether and how this relationship may <span class="hlt">change</span> in the <span class="hlt">decade</span> following fire. We use a dynamic Bayesian community model applied to a multi-year dataset of bird surveys at 1106 points sampled across 97 fires in montane California. Our results provide strong support for a positive relationship between pyrodiversity and bird diversity. This relationship interacts with time since fire, with pyrodiversity having a greater effect on biodiversity at 10 years post-fire than at 1 year post-fire. Immediately after fires, patches of differing burn severities hold similar bird communities, but over the ensuing <span class="hlt">decade</span>, bird assemblages within patches of contrasting severities differentiate. When evaluated at the scale of individual fires, fires with a greater heterogeneity of burn severities hold substantially more species. High spatial heterogeneity in severity, sometimes called 'mixed-severity fire', is a natural part of wildfire regimes in western North America, but may be jeopardized by climate <span class="hlt">change</span> and a legacy of fire suppression. Forest management that encourages mixed-severity fire may be critical for sustaining biodiversity across fire-prone landscapes. © 2016 The Author(s).</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5069516','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5069516"><span>Pyrodiversity promotes avian diversity over the <span class="hlt">decade</span> following forest fire</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Ruiz-Gutiérrez, Viviana; Wilkerson, Robert L.; Howell, Christine A.; Siegel, Rodney B.</p> <p>2016-01-01</p> <p>An emerging hypothesis in fire ecology is that pyrodiversity increases species diversity. We test whether pyrodiversity—defined as the standard deviation of fire severity—increases avian biodiversity at two spatial scales, and whether and how this relationship may <span class="hlt">change</span> in the <span class="hlt">decade</span> following fire. We use a dynamic Bayesian community model applied to a multi-year dataset of bird surveys at 1106 points sampled across 97 fires in montane California. Our results provide strong support for a positive relationship between pyrodiversity and bird diversity. This relationship interacts with time since fire, with pyrodiversity having a greater effect on biodiversity at 10 years post-fire than at 1 year post-fire. Immediately after fires, patches of differing burn severities hold similar bird communities, but over the ensuing <span class="hlt">decade</span>, bird assemblages within patches of contrasting severities differentiate. When evaluated at the scale of individual fires, fires with a greater heterogeneity of burn severities hold substantially more species. High spatial heterogeneity in severity, sometimes called ‘mixed-severity fire', is a natural part of wildfire regimes in western North America, but may be jeopardized by climate <span class="hlt">change</span> and a legacy of fire suppression. Forest management that encourages mixed-severity fire may be critical for sustaining biodiversity across fire-prone landscapes. PMID:27708152</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFM.C44B..06G','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFM.C44B..06G"><span>Enhanced ASTER DEMs for <span class="hlt">Decadal</span> Measurements of Glacier Elevation <span class="hlt">Changes</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Girod, L.; Nuth, C.; Kääb, A.</p> <p>2016-12-01</p> <p>Elevation <span class="hlt">change</span> data is critical to the understanding of a number of geophysical processes, including glaciers through the measurement their volume <span class="hlt">change</span>. The Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) system on-board the Terra (EOS AM-1) satellite has been a unique source of systematic stereoscopic images covering the whole globe at 15m resolution and at a consistent quality for over 15 years. While satellite stereo sensors with significantly improved radiometric and spatial resolution are available today, the potential of ASTER data lies in its long consistent time series that is unrivaled, though not fully exploited for <span class="hlt">change</span> analysis due to lack of data accuracy and precision. ASTER data are strongly affected by attitude jitter, mainly of approximately 4 and 30 km wavelength, and improving the generation of ASTER DEMs requires removal of this effect. We developed MMASTER, an improved method for ASTER DEM generation and implemented it in the open source photogrammetric library and software suite MicMac. The method relies on the computation of a rational polynomial coefficients (RPC) model and the detection and correction of cross-track sensor jitter in order to compute DEMs. Our sensor modeling does not require ground control points and thus potentially allows for automatic processing of large data volumes. When compared to ground truth data, we have assessed a ±5m accuracy in DEM differencing when using our processing method, improved from the ±30m when using the AST14DMO DEM product. We demonstrate and discuss this improved ASTER DEM quality for a number of glaciers in Greenland (See figure attached), Alaska, and Svalbard. The quality of our measurements promises to further unlock the underused potential of ASTER DEMs for glacier volume <span class="hlt">change</span> time series on a global scale. The data produced by our method will thus help to better understand the response of glaciers to climate <span class="hlt">change</span> and their influence on runoff and sea level.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013AGUFM.B31H..06R','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013AGUFM.B31H..06R"><span>Last <span class="hlt">Decade</span> of <span class="hlt">Changes</span> in Ground Temperature and Active Layer Thickness in the High Canadian Arctic and in Barrow</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Romanovsky, V. E.; Cable, W.; Walker, D. A.; Yoshikawa, K.; Marchenko, S. S.</p> <p>2013-12-01</p> <p>The impact of climate warming on permafrost and the potential of climate feedbacks resulting from permafrost thawing have recently received a great deal of attention. Most of the permafrost observatories in the Northern Hemisphere show substantial warming of permafrost since circa 1980-1990. The magnitude of warming has varied with location, but was typically from 0.5 to 2°C. Permafrost is already thawing within the southern part of the permafrost domain. However, recent observations documented propagation of this process northward into the continuous permafrost zone. The close proximity of the exceptionally icy soil horizons to the ground surface, which is typical for the arctic tundra biome, makes tundra surfaces extremely sensitive to the natural and human-made <span class="hlt">changes</span> that may resulted in development of processes such as thermokarst, thermal erosion, and retrogressive thaw slumps that strongly affect the stability of ecosystems and infrastructure. In 2003-2005, three Ecological Permafrost Observatories where established in the High Canadian Arctic (Green Cabin on the Banks Island, Mould Bay on the Prince Patrick Island, and Isachsen on the Ellef Ringnes Island) as a part of the University of Alaska Fairbanks NSF funded Biocomplexity Project. These observatories represent the northern part of the North American Arctic Transect (NAAT) established as a result of this project. The climatic and ground temperature data collected at these observatories show a general warming trend similar to what has been observed at the other locations in the North American Arctic. An important result of this resent warming is a significant increase in the active layer thickness (ALT) during the last <span class="hlt">decade</span>. For example, ALT at the Isachsen observatory increased from 0.4-0.42 m in 2005 to 0.54 m in 2012. The maximum ALT of 0.58 m was recorded in 2008. In a shallow excavation across an ice wedge at the Isachsen site, we estimated that the top of the ice wedge ice was located at 42</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUOSPC14E2102M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUOSPC14E2102M"><span>Global <span class="hlt">decadal</span> climate variability driven by Southern Ocean convection</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Marinov, I.; Cabre, A.</p> <p>2016-02-01</p> <p>Here we suggest a set of new "teleconnections" by which the Southern Ocean (SO) can induce anomalies in the tropical oceans and atmosphere. A 5000-year long control simulation in a coupled atmosphere-ocean model (CM2Mc, a low-resolution GFDL model) shows a natural, highly regular multi-<span class="hlt">decadal</span> oscillation between periods of SO open sea convection and non-convective periods. This process happens naturally, with different frequencies and durations of convection across the majority of CMIP5 under preindustrial forcing (deLavergne et al., 2014). In our model, oscillations in Weddell Sea convection drive multidecadal variability in SO and global SSTs, as well as SO heat storage, with convective <span class="hlt">decades</span> warm due to the heat released from the Circumpolar Deep Water and non-convective <span class="hlt">decades</span> cold due to subsurface heat storage. Convective pulses drive local SST and sea ice variations south of 60S, immediately triggering <span class="hlt">changes</span> in the Ferrell and Hadley cells, atmospheric energy budget and cross-equatorial heat exchange, ultimately influencing the position of the Intertropical Convergence Zone and rain patterns in the tropics. Additionally, the SO convection pulse is propagated to the tropics and the North Atlantic MOC via oceanic pathways on relatively fast (<span class="hlt">decadal</span>) timescales, in agreement with recent observational constraints. Open sea convection is the major mode of Antarctic Bottom Water (AABW) formation in the CMIP5 models. Future improvements in the representation of shelf convection and sea-ice interaction in the SO are a clear necessity. These model improvements should render the AABW representation more realistic, and might influence (a) the connectivity of the SO with the rest of the planet, as described above and (b) the oceanic and global carbon cycle, of which the AABW is a fundamental conduit.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014AGUFMGC13B0633G','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014AGUFMGC13B0633G"><span>Water Stress on U.S. Power Production at <span class="hlt">Decadal</span> Time Horizons</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Ganguli, P.; Kumar, D.; Yun, J.; Short, G.; Klausner, J.; Ganguly, A. R.</p> <p>2014-12-01</p> <p>Thermoelectric power production at risk, owing to current and projected water scarcity and rising stream temperatures, is assessed for the continental United States (US) at <span class="hlt">decadal</span> scales. Regional water scarcity is driven by climate variability and <span class="hlt">change</span>, as well as by multi-sector water demand. While a planning horizon of zero to about thirty years is occasionally prescribed by stakeholders, the challenges to risk assessment at these scales include the difficulty in delineating <span class="hlt">decadal</span> climate trends from intrinsic natural or multiple model variability. Current generation global climate or earth system models are not credible at the spatial resolutions of power plants, especially for surface water quantity and stream temperatures, which further exacerbates the assessment challenge. Population <span class="hlt">changes</span>, which are anyway difficult to project, cannot serve as adequate proxies for <span class="hlt">changes</span> in the water demand across sectors. The hypothesis that robust assessments of power production at risks are possible, despite the uncertainties, has been examined as a proof of concept. An approach is presented for delineating water scarcity and temperature from climate models, observations and population storylines, as well as for assessing power production at risk by examining geospatial correlations of power plant locations within regions where the usable water supply for energy production happens to be scarcer and warmer. Acknowledgment: Funding provided by US DOE's ARPA-E through Award DE-AR0000374.</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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