Sample records for advanced hydrologic prediction

  1. Observational breakthroughs lead the way to improved hydrological predictions

    NASA Astrophysics Data System (ADS)

    Lettenmaier, Dennis P.

    2017-04-01

    New data sources are revolutionizing the hydrological sciences. The capabilities of hydrological models have advanced greatly over the last several decades, but until recently model capabilities have outstripped the spatial resolution and accuracy of model forcings (atmospheric variables at the land surface) and the hydrologic state variables (e.g., soil moisture; snow water equivalent) that the models predict. This has begun to change, as shown in two examples here: soil moisture and drought evolution over Africa as predicted by a hydrology model forced with satellite-derived precipitation, and observations of snow water equivalent at very high resolution over a river basin in California's Sierra Nevada.

  2. The Hydrologic Ensemble Prediction Experiment (HEPEX)

    NASA Astrophysics Data System (ADS)

    Wood, A. W.; Thielen, J.; Pappenberger, F.; Schaake, J. C.; Hartman, R. K.

    2012-12-01

    The Hydrologic Ensemble Prediction Experiment was established in March, 2004, at a workshop hosted by the European Center for Medium Range Weather Forecasting (ECMWF). With support from the US National Weather Service (NWS) and the European Commission (EC), the HEPEX goal was to bring the international hydrological and meteorological communities together to advance the understanding and adoption of hydrological ensemble forecasts for decision support in emergency management and water resources sectors. The strategy to meet this goal includes meetings that connect the user, forecast producer and research communities to exchange ideas, data and methods; the coordination of experiments to address specific challenges; and the formation of testbeds to facilitate shared experimentation. HEPEX has organized about a dozen international workshops, as well as sessions at scientific meetings (including AMS, AGU and EGU) and special issues of scientific journals where workshop results have been published. Today, the HEPEX mission is to demonstrate the added value of hydrological ensemble prediction systems (HEPS) for emergency management and water resources sectors to make decisions that have important consequences for economy, public health, safety, and the environment. HEPEX is now organised around six major themes that represent core elements of a hydrologic ensemble prediction enterprise: input and pre-processing, ensemble techniques, data assimilation, post-processing, verification, and communication and use in decision making. This poster presents an overview of recent and planned HEPEX activities, highlighting case studies that exemplify the focus and objectives of HEPEX.

  3. Advancements in Hydrology and Erosion Process Understanding and Post-Fire Hydrologic and Erosion Model Development for Semi-Arid Landscapes

    NASA Astrophysics Data System (ADS)

    Williams, C. Jason; Pierson, Frederick B.; Al-Hamdan, Osama Z.; Robichaud, Peter R.; Nearing, Mark A.; Hernandez, Mariano; Weltz, Mark A.; Spaeth, Kenneth E.; Goodrich, David C.

    2017-04-01

    Fire activity continues to increase in semi-arid regions around the globe. Private and governmental land management entities are challenged with predicting and mitigating post-fire hydrologic and erosion responses on these landscapes. For more than a decade, a team of scientists with the US Department of Agriculture has collaborated on extensive post-fire hydrologic field research and the application of field research to development of post-fire hydrology and erosion predictive technologies. Experiments funded through this research investigated the impacts of fire on vegetation and soils and the effects of these fire-induced changes on infiltration, runoff generation, erodibility, and soil erosion processes. The distribution of study sites spans diverse topography across grassland, shrubland, and woodland landscapes throughout the western United States. Knowledge gleaned from the extensive field experiments was applied to develop and enhance physically-based models for hillslope- to watershed-scale runoff and erosion prediction. Our field research and subsequent data syntheses have identified key knowledge gaps and challenges regarding post-fire hydrology and erosion modeling. Our presentation details some consistent trends across a diverse domain and varying landscape conditions based on our extensive field campaigns. We demonstrate how field data have advanced our understanding of post-fire hydrology and erosion for semi-arid landscapes and highlight remaining key knowledge gaps. Lastly, we briefly show how our well-replicated experimental methodologies have contributed to advancements in hydrologic and erosion model development for the post-fire environment.

  4. The Hydrologic Ensemble Prediction Experiment (HEPEX)

    NASA Astrophysics Data System (ADS)

    Wood, Andy; Wetterhall, Fredrik; Ramos, Maria-Helena

    2015-04-01

    The Hydrologic Ensemble Prediction Experiment was established in March, 2004, at a workshop hosted by the European Center for Medium Range Weather Forecasting (ECMWF), and co-sponsored by the US National Weather Service (NWS) and the European Commission (EC). The HEPEX goal was to bring the international hydrological and meteorological communities together to advance the understanding and adoption of hydrological ensemble forecasts for decision support. HEPEX pursues this goal through research efforts and practical implementations involving six core elements of a hydrologic ensemble prediction enterprise: input and pre-processing, ensemble techniques, data assimilation, post-processing, verification, and communication and use in decision making. HEPEX has grown through meetings that connect the user, forecast producer and research communities to exchange ideas, data and methods; the coordination of experiments to address specific challenges; and the formation of testbeds to facilitate shared experimentation. In the last decade, HEPEX has organized over a dozen international workshops, as well as sessions at scientific meetings (including AMS, AGU and EGU) and special issues of scientific journals where workshop results have been published. Through these interactions and an active online blog (www.hepex.org), HEPEX has built a strong and active community of nearly 400 researchers & practitioners around the world. This poster presents an overview of recent and planned HEPEX activities, highlighting case studies that exemplify the focus and objectives of HEPEX.

  5. Hydrologic Predictions in the Anthropocene: A Research Framework Based on a Co-evolutionary Socio-hydrologic Perspective

    NASA Astrophysics Data System (ADS)

    Sivapalan, M.; Bloeschl, G.

    2012-12-01

    The world is facing a water management crisis, in the context of fast rising demand for water due to growth of human populations and changing lifestyles, and depletion of freshwater resources. In many parts of the world, poor distribution of freshwater in relation to demand is already the cause of serious water scarcity, exacerbated by climate change. Cumulatively, these result in increased human appropriation of water resources, significant modification of landscapes, and a strong human imprint on water cycle dynamics from local to global scales. Hydrologic predictions in such a fast changing environment face significant challenges. Traditional models for predictions treat the hydrologic system as a simple input-output system, and propagate variability of external inputs or disturbances through the various hydrologic subsystems, but assuming stationarity. However, in a fast changing world, none of the subsystems can be assumed to be stationary, but as co-evolving parts of a complex system. The role of humans takes on an important role, which can no longer be assumed to independent of the natural system. We need new socio-hydrologic frameworks to observe, monitor, understand and predict the co-evolution of coupled human-natural systems. In this talk, using examples from one or more real-world settings (from Australia and Europe) involving human interactions with hydrologic systems, we will present new theoretical frameworks that should be adopted to advance the emergent new sub-discipline of socio-hydrology. The proposed research agenda is organized under (i) process socio-hydrology, (ii) comparative socio-hydrology, and (iii) historical socio-hydrology.

  6. OpenDA-WFLOW framework for improving hydrologic predictions using distributed hydrologic models

    NASA Astrophysics Data System (ADS)

    Weerts, Albrecht; Schellekens, Jaap; Kockx, Arno; Hummel, Stef

    2017-04-01

    Data assimilation (DA) holds considerable potential for improving hydrologic predictions (Liu et al., 2012) and increase the potential for early warning and/or smart water management. However, advances in hydrologic DA research have not yet been adequately or timely implemented in operational forecast systems to improve the skill of forecasts for better informed real-world decision making. The objective of this work is to highlight the development of a generic linkage of the open source OpenDA package and the open source community hydrologic modeling framework Openstreams/WFLOW and its application in operational hydrological forecasting on various spatial scales. The coupling between OpenDA and Openstreams/wflow framework is based on the emerging standard Basic Model Interface (BMI) as advocated by CSDMS using cross-platform webservices (i.e. Apache Thrift) developed by Hut et al. (2016). The potential application of the OpenDA-WFLOW for operational hydrologic forecasting including its integration with Delft-FEWS (used by more than 40 operational forecast centers around the world (Werner et al., 2013)) is demonstrated by the presented case studies. We will also highlight the possibility to give real-time insight into the working of the DA methods applied for supporting the forecaster as mentioned as one of the burning issues by Liu et al., (2012).

  7. Advances in Applications of Hierarchical Bayesian Methods with Hydrological Models

    NASA Astrophysics Data System (ADS)

    Alexander, R. B.; Schwarz, G. E.; Boyer, E. W.

    2017-12-01

    Mechanistic and empirical watershed models are increasingly used to inform water resource decisions. Growing access to historical stream measurements and data from in-situ sensor technologies has increased the need for improved techniques for coupling models with hydrological measurements. Techniques that account for the intrinsic uncertainties of both models and measurements are especially needed. Hierarchical Bayesian methods provide an efficient modeling tool for quantifying model and prediction uncertainties, including those associated with measurements. Hierarchical methods can also be used to explore spatial and temporal variations in model parameters and uncertainties that are informed by hydrological measurements. We used hierarchical Bayesian methods to develop a hybrid (statistical-mechanistic) SPARROW (SPAtially Referenced Regression On Watershed attributes) model of long-term mean annual streamflow across diverse environmental and climatic drainages in 18 U.S. hydrological regions. Our application illustrates the use of a new generation of Bayesian methods that offer more advanced computational efficiencies than the prior generation. Evaluations of the effects of hierarchical (regional) variations in model coefficients and uncertainties on model accuracy indicates improved prediction accuracies (median of 10-50%) but primarily in humid eastern regions, where model uncertainties are one-third of those in arid western regions. Generally moderate regional variability is observed for most hierarchical coefficients. Accounting for measurement and structural uncertainties, using hierarchical state-space techniques, revealed the effects of spatially-heterogeneous, latent hydrological processes in the "localized" drainages between calibration sites; this improved model precision, with only minor changes in regional coefficients. Our study can inform advances in the use of hierarchical methods with hydrological models to improve their integration with stream

  8. Improving Permafrost Hydrology Prediction Through Data-Model Integration

    NASA Astrophysics Data System (ADS)

    Wilson, C. J.; Andresen, C. G.; Atchley, A. L.; Bolton, W. R.; Busey, R.; Coon, E.; Charsley-Groffman, L.

    2017-12-01

    The CMIP5 Earth System Models were unable to adequately predict the fate of the 16GT of permafrost carbon in a warming climate due to poor representation of Arctic ecosystem processes. The DOE Office of Science Next Generation Ecosystem Experiment, NGEE-Arctic project aims to reduce uncertainty in the Arctic carbon cycle and its impact on the Earth's climate system by improved representation of the coupled physical, chemical and biological processes that drive how much buried carbon will be converted to CO2 and CH4, how fast this will happen, which form will dominate, and the degree to which increased plant productivity will offset increased soil carbon emissions. These processes fundamentally depend on permafrost thaw rate and its influence on surface and subsurface hydrology through thermal erosion, land subsidence and changes to groundwater flow pathways as soil, bedrock and alluvial pore ice and massive ground ice melts. LANL and its NGEE colleagues are co-developing data and models to better understand controls on permafrost degradation and improve prediction of the evolution of permafrost and its impact on Arctic hydrology. The LANL Advanced Terrestrial Simulator was built using a state of the art HPC software framework to enable the first fully coupled 3-dimensional surface-subsurface thermal-hydrology and land surface deformation simulations to simulate the evolution of the physical Arctic environment. Here we show how field data including hydrology, snow, vegetation, geochemistry and soil properties, are informing the development and application of the ATS to improve understanding of controls on permafrost stability and permafrost hydrology. The ATS is being used to inform parameterizations of complex coupled physical, ecological and biogeochemical processes for implementation in the DOE ACME land model, to better predict the role of changing Arctic hydrology on the global climate system. LA-UR-17-26566.

  9. Predicting Hydrologic Function With Aquatic Gene Fragments

    NASA Astrophysics Data System (ADS)

    Good, S. P.; URycki, D. R.; Crump, B. C.

    2018-03-01

    Recent advances in microbiology techniques, such as genetic sequencing, allow for rapid and cost-effective collection of large quantities of genetic information carried within water samples. Here we posit that the unique composition of aquatic DNA material within a water sample contains relevant information about hydrologic function at multiple temporal scales. In this study, machine learning was used to develop discharge prediction models trained on the relative abundance of bacterial taxa classified into operational taxonomic units (OTUs) based on 16S rRNA gene sequences from six large arctic rivers. We term this approach "genohydrology," and show that OTU relative abundances can be used to predict river discharge at monthly and longer timescales. Based on a single DNA sample from each river, the average Nash-Sutcliffe efficiency (NSE) for predicted mean monthly discharge values throughout the year was 0.84, while the NSE for predicted discharge values across different return intervals was 0.67. These are considerable improvements over predictions based only on the area-scaled mean specific discharge of five similar rivers, which had average NSE values of 0.64 and -0.32 for seasonal and recurrence interval discharge values, respectively. The genohydrology approach demonstrates that genetic diversity within the aquatic microbiome is a large and underutilized data resource with benefits for prediction of hydrologic function.

  10. Advances in the use of observed spatial patterns of catchment hydrological response

    NASA Astrophysics Data System (ADS)

    Grayson, Rodger B.; Blöschl, Günter; Western, Andrew W.; McMahon, Thomas A.

    Over the past two decades there have been repeated calls for the collection of new data for use in developing hydrological science. The last few years have begun to bear fruit from the seeds sown by these calls, through increases in the availability and utility of remote sensing data, as well as the execution of campaigns in research catchments aimed at providing new data for advancing hydrological understanding and predictive capability. In this paper we discuss some philosophical considerations related to model complexity, data availability and predictive performance, highlighting the potential of observed patterns in moving the science and practice of catchment hydrology forward. We then review advances that have arisen from recent work on spatial patterns, including in the characterisation of spatial structure and heterogeneity, and the use of patterns for developing, calibrating and testing distributed hydrological models. We illustrate progress via examples using observed patterns of snow cover, runoff occurrence and soil moisture. Methods for the comparison of patterns are presented, illustrating how they can be used to assess hydrologically important characteristics of model performance. These methods include point-to-point comparisons, spatial relationships between errors and landscape parameters, transects, and optimal local alignment. It is argued that the progress made to date augers well for future developments, but there is scope for improvements in several areas. These include better quantitative methods for pattern comparisons, better use of pattern information in data assimilation and modelling, and a call for improved archiving of data from field studies to assist in comparative studies for generalising results and developing fundamental understanding.

  11. Hydrological partitioning in the critical zone: Recent advances and opportunities for developing transferable understanding of water cycle dynamics: CRITICAL ZONE HYDROLOGY

    DOE PAGES

    Brooks, Paul D.; Chorover, Jon; Fan, Ying; ...

    2015-09-01

    Hydrology is an integrative discipline linking the broad array of water‐related research with physical, ecological, and social sciences. The increasing breadth of hydrological research, often where subdisciplines of hydrology partner with related sciences, reflects the central importance of water to environmental science, while highlighting the fractured nature of the discipline itself. This lack of coordination among hydrologic subdisciplines has hindered the development of hydrologic theory and integrated models capable of predicting hydrologic partitioning across time and space. The recent development of the concept of the critical zone (CZ), an open system extending from the top of the canopy to themore » base of groundwater, brings together multiple hydrological subdisciplines with related physical and ecological sciences. Observations obtained by CZ researchers provide a diverse range of complementary process and structural data to evaluate both conceptual and numerical models. Consequently, a cross‐site focus on “critical zone hydrology” has potential to advance the discipline of hydrology and to facilitate the transition of CZ observatories into a research network with immediate societal relevance. Here we review recent work in catchment hydrology and hydrochemistry, hydrogeology, and ecohydrology that highlights a common knowledge gap in how precipitation is partitioned in the critical zone: “how is the amount, routing, and residence time of water in the subsurface related to the biogeophysical structure of the CZ?” Addressing this question will require coordination among hydrologic subdisciplines and interfacing sciences, and catalyze rapid progress in understanding current CZ structure and predicting how climate and land cover changes will affect hydrologic partitioning.« less

  12. Predicting hydrologic function with the streamwater mircobiome

    NASA Astrophysics Data System (ADS)

    Good, S. P.; URycki, D. R.; Crump, B. C.

    2017-12-01

    Recent advances in microbiology allow for rapid and cost-effective determination of the presence of a nearly limitless number of bacterial (and other) species within a water sample. Here, we posit that the quasi-unique taxonomic composition of the aquatic microbiome is an emergent property of a catchment that contains information about hydrologic function at multiple temporal and spatial scales, and term this approach `genohydrolgy.' As first a genohydrology case study, we show that the relative abundance of bacterial species within different operational taxonomic units (OTUs) from six large arctic rivers can be used to predict river discharge at monthly and longer timescales. Using only OTU abundance information and a machine-learning algorithm trained on OTU and discharge data from the other five rivers, our genohydrology approach is able to predict mean monthly discharge values throughout the year with an average Nash-Sutcliffe efficiency (NSE) of 0.50, while the recurrence interval of extreme flows at longer times scales in these rivers was predicted with an NSE of 0.04. This approach demonstrates considerable improvement over prediction of these quantities in each river based only on discharge data from the other five (our null hypothesis), which had average NSE values of -1.19 and -5.50 for the seasonal and recurrence interval discharge values, respectively. Overall the genohydrology approach demonstrates that bacterial diversity within the aquatic microbiome is a large and underutilized data resource with benefits for prediction of hydrologic function.

  13. Advancing Data Assimilation in Operational Hydrologic Forecasting: Progresses, Challenges, and Emerging Opportunities

    NASA Technical Reports Server (NTRS)

    Liu, Yuqiong; Weerts, A.; Clark, M.; Hendricks Franssen, H.-J; Kumar, S.; Moradkhani, H.; Seo, D.-J.; Schwanenberg, D.; Smith, P.; van Dijk, A. I. J. M.; hide

    2012-01-01

    Data assimilation (DA) holds considerable potential for improving hydrologic predictions as demonstrated in numerous research studies. However, advances in hydrologic DA research have not been adequately or timely implemented in operational forecast systems to improve the skill of forecasts for better informed real-world decision making. This is due in part to a lack of mechanisms to properly quantify the uncertainty in observations and forecast models in real-time forecasting situations and to conduct the merging of data and models in a way that is adequately efficient and transparent to operational forecasters. The need for effective DA of useful hydrologic data into the forecast process has become increasingly recognized in recent years. This motivated a hydrologic DA workshop in Delft, the Netherlands in November 2010, which focused on advancing DA in operational hydrologic forecasting and water resources management. As an outcome of the workshop, this paper reviews, in relevant detail, the current status of DA applications in both hydrologic research and operational practices, and discusses the existing or potential hurdles and challenges in transitioning hydrologic DA research into cost-effective operational forecasting tools, as well as the potential pathways and newly emerging opportunities for overcoming these challenges. Several related aspects are discussed, including (1) theoretical or mathematical aspects in DA algorithms, (2) the estimation of different types of uncertainty, (3) new observations and their objective use in hydrologic DA, (4) the use of DA for real-time control of water resources systems, and (5) the development of community-based, generic DA tools for hydrologic applications. It is recommended that cost-effective transition of hydrologic DA from research to operations should be helped by developing community-based, generic modeling and DA tools or frameworks, and through fostering collaborative efforts among hydrologic modellers, DA

  14. Recent advances in understanding Antarctic subglacial lakes and hydrology

    PubMed Central

    Siegert, Martin J.; Ross, Neil; Le Brocq, Anne M.

    2016-01-01

    It is now well documented that over 400 subglacial lakes exist across the bed of the Antarctic Ice Sheet. They comprise a variety of sizes and volumes (from the approx. 250 km long Lake Vostok to bodies of water less than 1 km in length), relate to a number of discrete topographic settings (from those contained within valleys to lakes that reside in broad flat terrain) and exhibit a range of dynamic behaviours (from ‘active’ lakes that periodically outburst some or all of their water to those isolated hydrologically for millions of years). Here we critique recent advances in our understanding of subglacial lakes, in particular since the last inventory in 2012. We show that within 3 years our knowledge of the hydrological processes at the ice-sheet base has advanced considerably. We describe evidence for further ‘active’ subglacial lakes, based on satellite observation of ice-surface changes, and discuss why detection of many ‘active’ lakes is not resolved in traditional radio-echo sounding methods. We go on to review evidence for large-scale subglacial water flow in Antarctica, including the discovery of ancient channels developed by former hydrological processes. We end by predicting areas where future discoveries may be possible, including the detection, measurement and significance of groundwater (i.e. water held beneath the ice-bed interface). PMID:26667914

  15. Recent advances in understanding Antarctic subglacial lakes and hydrology.

    PubMed

    Siegert, Martin J; Ross, Neil; Le Brocq, Anne M

    2016-01-28

    It is now well documented that over 400 subglacial lakes exist across the bed of the Antarctic Ice Sheet. They comprise a variety of sizes and volumes (from the approx. 250 km long Lake Vostok to bodies of water less than 1 km in length), relate to a number of discrete topographic settings (from those contained within valleys to lakes that reside in broad flat terrain) and exhibit a range of dynamic behaviours (from 'active' lakes that periodically outburst some or all of their water to those isolated hydrologically for millions of years). Here we critique recent advances in our understanding of subglacial lakes, in particular since the last inventory in 2012. We show that within 3 years our knowledge of the hydrological processes at the ice-sheet base has advanced considerably. We describe evidence for further 'active' subglacial lakes, based on satellite observation of ice-surface changes, and discuss why detection of many 'active' lakes is not resolved in traditional radio-echo sounding methods. We go on to review evidence for large-scale subglacial water flow in Antarctica, including the discovery of ancient channels developed by former hydrological processes. We end by predicting areas where future discoveries may be possible, including the detection, measurement and significance of groundwater (i.e. water held beneath the ice-bed interface). © 2015 The Authors.

  16. Acting, predicting and intervening in a socio-hydrological world

    NASA Astrophysics Data System (ADS)

    Lane, S. N.

    2014-03-01

    This paper asks a simple question: if humans and their actions co-evolve with hydrological systems (Sivapalan et al., 2012), what is the role of hydrological scientists, who are also humans, within this system? To put it more directly, as traditionally there is a supposed separation of scientists and society, can we maintain this separation as socio-hydrologists studying a socio-hydrological world? This paper argues that we cannot, using four linked sections. The first section draws directly upon the concern of science-technology studies to make a case to the (socio-hydrological) community that we need to be sensitive to constructivist accounts of science in general and socio-hydrology in particular. I review three positions taken by such accounts and apply them to hydrological science, supported with specific examples: (a) the ways in which scientific activities frame socio-hydrological research, such that at least some of the knowledge that we obtain is constructed by precisely what we do; (b) the need to attend to how socio-hydrological knowledge is used in decision-making, as evidence suggests that hydrological knowledge does not flow simply from science into policy; and (c) the observation that those who do not normally label themselves as socio-hydrologists may actually have a profound knowledge of socio-hydrology. The second section provides an empirical basis for considering these three issues by detailing the history of the practice of roughness parameterisation, using parameters like Manning's n, in hydrological and hydraulic models for flood inundation mapping. This history sustains the third section that is a more general consideration of one type of socio-hydrological practice: predictive modelling. I show that as part of a socio-hydrological analysis, hydrological prediction needs to be thought through much more carefully: not only because hydrological prediction exists to help inform decisions that are made about water management; but also because

  17. Hydrological regionalisation based on available hydrological information for runoff prediction at catchment scale

    NASA Astrophysics Data System (ADS)

    Li, Qiaoling; Li, Zhijia; Zhu, Yuelong; Deng, Yuanqian; Zhang, Ke; Yao, Cheng

    2018-06-01

    Regionalisation provides a way of transferring hydrological information from gauged to ungauged catchments. The past few decades has seen several kinds of regionalisation approaches for catchment classification and runoff predictions. The underlying assumption is that catchments having similar catchment properties are hydrological similar. This requires the appropriate selection of catchment properties, particularly the inclusion of observed hydrological information, to explain the similarity of hydrological behaviour. We selected observable catchments properties and flow duration curves to reflect the hydrological behaviour, and to regionalize rainfall-runoff response for runoff prediction. As a case study, we investigated 15 catchments located in the Yangtze and Yellow River under multiple hydro-climatic conditions. A clustering scheme was developed to separate the catchments into 4 homogeneous regions by employing catchment properties including hydro-climatic attributes, topographic attributes and land cover etc. We utilized daily flow duration curves as the indicator of hydrological response and interpreted hydrological similarity by root mean square errors. The combined analysis of similarity in catchment properties and hydrological response suggested that catchments in the same homogenous region were hydrological similar. A further validation was conducted by establishing a rainfall-runoff coaxial correlation diagram for each catchment. A common coaxial correlation diagram was generated for each homogenous region. The performances of most coaxial correlation diagrams met the national standard. The coaxial correlation diagram can be transferred within the homogeneous region for runoff prediction in ungauged catchments at an hourly time scale.

  18. Multi-model analysis in hydrological prediction

    NASA Astrophysics Data System (ADS)

    Lanthier, M.; Arsenault, R.; Brissette, F.

    2017-12-01

    Hydrologic modelling, by nature, is a simplification of the real-world hydrologic system. Therefore ensemble hydrological predictions thus obtained do not present the full range of possible streamflow outcomes, thereby producing ensembles which demonstrate errors in variance such as under-dispersion. Past studies show that lumped models used in prediction mode can return satisfactory results, especially when there is not enough information available on the watershed to run a distributed model. But all lumped models greatly simplify the complex processes of the hydrologic cycle. To generate more spread in the hydrologic ensemble predictions, multi-model ensembles have been considered. In this study, the aim is to propose and analyse a method that gives an ensemble streamflow prediction that properly represents the forecast probabilities and reduced ensemble bias. To achieve this, three simple lumped models are used to generate an ensemble. These will also be combined using multi-model averaging techniques, which generally generate a more accurate hydrogram than the best of the individual models in simulation mode. This new predictive combined hydrogram is added to the ensemble, thus creating a large ensemble which may improve the variability while also improving the ensemble mean bias. The quality of the predictions is then assessed on different periods: 2 weeks, 1 month, 3 months and 6 months using a PIT Histogram of the percentiles of the real observation volumes with respect to the volumes of the ensemble members. Initially, the models were run using historical weather data to generate synthetic flows. This worked for individual models, but not for the multi-model and for the large ensemble. Consequently, by performing data assimilation at each prediction period and thus adjusting the initial states of the models, the PIT Histogram could be constructed using the observed flows while allowing the use of the multi-model predictions. The under-dispersion has been

  19. It takes a community to raise a hydrologist: the Modular Curriculum for Hydrologic Advancement (MOCHA)

    NASA Astrophysics Data System (ADS)

    Wagener, T.; Kelleher, C.; Weiler, M.; McGlynn, B.; Gooseff, M.; Marshall, L.; Meixner, T.; McGuire, K.; Gregg, S.; Sharma, P.; Zappe, S.

    2012-09-01

    Protection from hydrological extremes and the sustainable supply of hydrological services in the presence of changing climate and lifestyles as well as rocketing population pressure in many parts of the world are the defining societal challenges for hydrology in the 21st century. A review of the existing literature shows that these challenges and their educational consequences for hydrology were foreseeable and were even predicted by some. However, surveys of the current educational basis for hydrology also clearly demonstrate that hydrology education is not yet ready to prepare students to deal with these challenges. We present our own vision of the necessary evolution of hydrology education, which we implemented in the Modular Curriculum for Hydrologic Advancement (MOCHA). The MOCHA project is directly aimed at developing a community-driven basis for hydrology education. In this paper we combine literature review, community survey, discussion and assessment to provide a holistic baseline for the future of hydrology education. The ultimate objective of our educational initiative is to enable educators to train a new generation of "renaissance hydrologists," who can master the holistic nature of our field and of the problems we encounter.

  20. A seasonal hydrologic ensemble prediction system for water resource management

    NASA Astrophysics Data System (ADS)

    Luo, L.; Wood, E. F.

    2006-12-01

    A seasonal hydrologic ensemble prediction system, developed for the Ohio River basin, has been improved and expanded to several other regions including the Eastern U.S., Africa and East Asia. The prediction system adopts the traditional Extended Streamflow Prediction (ESP) approach, utilizing the VIC (Variable Infiltration Capacity) hydrological model as the central tool for producing ensemble prediction of soil moisture, snow and streamflow with lead times up to 6-month. VIC is forced by observed meteorology to estimate the hydrological initial condition prior to the forecast, but during the forecast period the atmospheric forcing comes from statistically downscaled, seasonal forecast from dynamic climate models. The seasonal hydrologic ensemble prediction system is currently producing realtime seasonal hydrologic forecast for these regions on a monthly basis. Using hindcasts from a 19-year period (1981-1999), during which seasonal hindcasts from NCEP Climate Forecast System (CFS) and European Union DEMETER project are available, we evaluate the performance of the forecast system over our forecast regions. The evaluation shows that the prediction system using the current forecast approach is able to produce reliable and accurate precipitation, soil moisture and streamflow predictions. The overall skill is much higher then the traditional ESP. In particular, forecasts based on multiple climate model forecast are more skillful than single model-based forecast. This emphasizes the significant need for producing seasonal climate forecast with multiple climate models for hydrologic applications. Forecast from this system is expected to provide very valuable information about future hydrologic states and associated risks for end users, including water resource management and financial sectors.

  1. Hydrological partitioning in the critical zone: Recent advances and opportunities for developing transferable understanding of water cycle dynamics

    NASA Astrophysics Data System (ADS)

    Brooks, Paul D.; Chorover, Jon; Fan, Ying; Godsey, Sarah E.; Maxwell, Reed M.; McNamara, James P.; Tague, Christina

    2015-09-01

    Hydrology is an integrative discipline linking the broad array of water-related research with physical, ecological, and social sciences. The increasing breadth of hydrological research, often where subdisciplines of hydrology partner with related sciences, reflects the central importance of water to environmental science, while highlighting the fractured nature of the discipline itself. This lack of coordination among hydrologic subdisciplines has hindered the development of hydrologic theory and integrated models capable of predicting hydrologic partitioning across time and space. The recent development of the concept of the critical zone (CZ), an open system extending from the top of the canopy to the base of groundwater, brings together multiple hydrological subdisciplines with related physical and ecological sciences. Observations obtained by CZ researchers provide a diverse range of complementary process and structural data to evaluate both conceptual and numerical models. Consequently, a cross-site focus on "critical zone hydrology" has potential to advance the discipline of hydrology and to facilitate the transition of CZ observatories into a research network with immediate societal relevance. Here we review recent work in catchment hydrology and hydrochemistry, hydrogeology, and ecohydrology that highlights a common knowledge gap in how precipitation is partitioned in the critical zone: "how is the amount, routing, and residence time of water in the subsurface related to the biogeophysical structure of the CZ?" Addressing this question will require coordination among hydrologic subdisciplines and interfacing sciences, and catalyze rapid progress in understanding current CZ structure and predicting how climate and land cover changes will affect hydrologic partitioning.

  2. Accelerating advances in continental domain hydrologic modeling

    USGS Publications Warehouse

    Archfield, Stacey A.; Clark, Martyn; Arheimer, Berit; Hay, Lauren E.; McMillan, Hilary; Kiang, Julie E.; Seibert, Jan; Hakala, Kirsti; Bock, Andrew R.; Wagener, Thorsten; Farmer, William H.; Andreassian, Vazken; Attinger, Sabine; Viglione, Alberto; Knight, Rodney; Markstrom, Steven; Over, Thomas M.

    2015-01-01

    In the past, hydrologic modeling of surface water resources has mainly focused on simulating the hydrologic cycle at local to regional catchment modeling domains. There now exists a level of maturity among the catchment, global water security, and land surface modeling communities such that these communities are converging toward continental domain hydrologic models. This commentary, written from a catchment hydrology community perspective, provides a review of progress in each community toward this achievement, identifies common challenges the communities face, and details immediate and specific areas in which these communities can mutually benefit one another from the convergence of their research perspectives. Those include: (1) creating new incentives and infrastructure to report and share model inputs, outputs, and parameters in data services and open access, machine-independent formats for model replication or reanalysis; (2) ensuring that hydrologic models have: sufficient complexity to represent the dominant physical processes and adequate representation of anthropogenic impacts on the terrestrial water cycle, a process-based approach to model parameter estimation, and appropriate parameterizations to represent large-scale fluxes and scaling behavior; (3) maintaining a balance between model complexity and data availability as well as uncertainties; and (4) quantifying and communicating significant advancements toward these modeling goals.

  3. Hydrological partitioning in the critical zone: Recent advances and opportunities for developing transferable understanding of water cycle dynamics

    DOE PAGES

    Brooks, Paul D.; Chorover, Jon; Fan, Ying; ...

    2015-08-07

    Here, hydrology is an integrative discipline linking the broad array of water–related research with physical, ecological, and social sciences. The increasing breadth of hydrological research, often where subdisciplines of hydrology partner with related sciences, reflects the central importance of water to environmental science, while highlighting the fractured nature of the discipline itself. This lack of coordination among hydrologic subdisciplines has hindered the development of hydrologic theory and integrated models capable of predicting hydrologic partitioning across time and space. The recent development of the concept of the critical zone (CZ), an open system extending from the top of the canopy tomore » the base of groundwater, brings together multiple hydrological subdisciplines with related physical and ecological sciences. Observations obtained by CZ researchers provide a diverse range of complementary process and structural data to evaluate both conceptual and numerical models. Consequently, a cross–site focus on “critical zone hydrology” has potential to advance the discipline of hydrology and to facilitate the transition of CZ observatories into a research network with immediate societal relevance. Here we review recent work in catchment hydrology and hydrochemistry, hydrogeology, and ecohydrology that highlights a common knowledge gap in how precipitation is partitioned in the critical zone: “how is the amount, routing, and residence time of water in the subsurface related to the biogeophysical structure of the CZ?” Addressing this question will require coordination among hydrologic subdisciplines and interfacing sciences, and catalyze rapid progress in understanding current CZ structure and predicting how climate and land cover changes will affect hydrologic partitioning.« less

  4. A Hydrological Perspective to Advance Understanding of the Water Cycle

    NASA Astrophysics Data System (ADS)

    Berghuijs, W.

    2014-12-01

    In principle hydrologists are scientists that study relationships within the water cycle. Yet, current technology makes it tempting for hydrology students to lose their "hydrological perspective" and become instead full-time computer programmers or statisticians. I assert that students should ensure their hydrological perspective thrives, notwithstanding the importance and possibilities of current technology. This perspective is necessary to advance the science of hydrology. As other hydrologists have pondered similar views before, I make no claims of originality here. I just hope that in presenting my perspective on this issue I may spark the interest of other early career hydrologists.

  5. Multi-model ensemble hydrologic prediction using Bayesian model averaging

    NASA Astrophysics Data System (ADS)

    Duan, Qingyun; Ajami, Newsha K.; Gao, Xiaogang; Sorooshian, Soroosh

    2007-05-01

    Multi-model ensemble strategy is a means to exploit the diversity of skillful predictions from different models. This paper studies the use of Bayesian model averaging (BMA) scheme to develop more skillful and reliable probabilistic hydrologic predictions from multiple competing predictions made by several hydrologic models. BMA is a statistical procedure that infers consensus predictions by weighing individual predictions based on their probabilistic likelihood measures, with the better performing predictions receiving higher weights than the worse performing ones. Furthermore, BMA provides a more reliable description of the total predictive uncertainty than the original ensemble, leading to a sharper and better calibrated probability density function (PDF) for the probabilistic predictions. In this study, a nine-member ensemble of hydrologic predictions was used to test and evaluate the BMA scheme. This ensemble was generated by calibrating three different hydrologic models using three distinct objective functions. These objective functions were chosen in a way that forces the models to capture certain aspects of the hydrograph well (e.g., peaks, mid-flows and low flows). Two sets of numerical experiments were carried out on three test basins in the US to explore the best way of using the BMA scheme. In the first set, a single set of BMA weights was computed to obtain BMA predictions, while the second set employed multiple sets of weights, with distinct sets corresponding to different flow intervals. In both sets, the streamflow values were transformed using Box-Cox transformation to ensure that the probability distribution of the prediction errors is approximately Gaussian. A split sample approach was used to obtain and validate the BMA predictions. The test results showed that BMA scheme has the advantage of generating more skillful and equally reliable probabilistic predictions than original ensemble. The performance of the expected BMA predictions in terms of

  6. Probabilistic flood inundation prediction within a coupled hydrodynamic, distributed hydrologic modeling framework

    NASA Astrophysics Data System (ADS)

    Adams, T. E.

    2016-12-01

    Accurate and timely predictions of the lateral exent of floodwaters and water level depth in floodplain areas are critical globally. This paper demonstrates the coupling of hydrologic ensembles, derived from the use of numerical weather prediction (NWP) model forcings as input to a fully distributed hydrologic model. Resulting ensemble output from the distributed hydrologic model are used as upstream flow boundaries and lateral inflows to a 1-D hydrodynamic model. An example is presented for the Potomac River in the vicinity of Washington, DC (USA). The approach taken falls within the broader goals of the Hydrologic Ensemble Prediction EXperiment (HEPEX).

  7. Assessing predictability of a hydrological stochastic-dynamical system

    NASA Astrophysics Data System (ADS)

    Gelfan, Alexander

    2014-05-01

    The water cycle includes the processes with different memory that creates potential for predictability of hydrological system based on separating its long and short memory components and conditioning long-term prediction on slower evolving components (similar to approaches in climate prediction). In the face of the Panta Rhei IAHS Decade questions, it is important to find a conceptual approach to classify hydrological system components with respect to their predictability, define predictable/unpredictable patterns, extend lead-time and improve reliability of hydrological predictions based on the predictable patterns. Representation of hydrological systems as the dynamical systems subjected to the effect of noise (stochastic-dynamical systems) provides possible tool for such conceptualization. A method has been proposed for assessing predictability of hydrological system caused by its sensitivity to both initial and boundary conditions. The predictability is defined through a procedure of convergence of pre-assigned probabilistic measure (e.g. variance) of the system state to stable value. The time interval of the convergence, that is the time interval during which the system losses memory about its initial state, defines limit of the system predictability. The proposed method was applied to assess predictability of soil moisture dynamics in the Nizhnedevitskaya experimental station (51.516N; 38.383E) located in the agricultural zone of the central European Russia. A stochastic-dynamical model combining a deterministic one-dimensional model of hydrothermal regime of soil with a stochastic model of meteorological inputs was developed. The deterministic model describes processes of coupled heat and moisture transfer through unfrozen/frozen soil and accounts for the influence of phase changes on water flow. The stochastic model produces time series of daily meteorological variables (precipitation, air temperature and humidity), whose statistical properties are similar

  8. The efficacy of calibrating hydrologic model using remotely sensed evapotranspiration and soil moisture for streamflow prediction

    NASA Astrophysics Data System (ADS)

    Kunnath-Poovakka, A.; Ryu, D.; Renzullo, L. J.; George, B.

    2016-04-01

    Calibration of spatially distributed hydrologic models is frequently limited by the availability of ground observations. Remotely sensed (RS) hydrologic information provides an alternative source of observations to inform models and extend modelling capability beyond the limits of ground observations. This study examines the capability of RS evapotranspiration (ET) and soil moisture (SM) in calibrating a hydrologic model and its efficacy to improve streamflow predictions. SM retrievals from the Advanced Microwave Scanning Radiometer-EOS (AMSR-E) and daily ET estimates from the CSIRO MODIS ReScaled potential ET (CMRSET) are used to calibrate a simplified Australian Water Resource Assessment - Landscape model (AWRA-L) for a selection of parameters. The Shuffled Complex Evolution Uncertainty Algorithm (SCE-UA) is employed for parameter estimation at eleven catchments in eastern Australia. A subset of parameters for calibration is selected based on the variance-based Sobol' sensitivity analysis. The efficacy of 15 objective functions for calibration is assessed based on streamflow predictions relative to control cases, and relative merits of each are discussed. Synthetic experiments were conducted to examine the effect of bias in RS ET observations on calibration. The objective function containing the root mean square deviation (RMSD) of ET result in best streamflow predictions and the efficacy is superior for catchments with medium to high average runoff. Synthetic experiments revealed that accurate ET product can improve the streamflow predictions in catchments with low average runoff.

  9. Advances in river ice hydrology 1999-2003

    NASA Astrophysics Data System (ADS)

    Morse, Brian; Hicks, Faye

    2005-01-01

    In the period 1999 to 2003, river ice has continued to have important socio-economic impacts in Canada and other Nordic countries. Concurrently, there have been many important advances in all areas of Canadian research into river ice engineering and hydrology. For example: (1) River ice processes were highlighted in two special journal issues (Canadian Journal of Civil Engineering in 2003 and Hydrological Processes in 2002) and at five conferences (Canadian Committee on River Ice Processes and the Environment in 1999, 2001 and 2003, and International Association of Hydraulic Research in 2000 and 2002). (2) A number of workers have clearly advanced our understanding of river ice processes by bringing together disparate information in comprehensive review articles. (3) There have been significant advances in river ice modelling. For example, both one-dimensional (e.g. RIVICE, RIVJAM, ICEJAM, HEC-RAS, etc.) and two-dimensional (2-D; www.river2d.ca) public-domain ice-jam models are now available. Work is ongoing to improve RIVER2D, and a commercial 2-D ice-process model is being developed. (4) The 1999-2003 period is notable for the number of distinctly hydrological and ecological studies. On the quantitative side, many are making efforts to determine streamflow during the winter period. On the ecological side, some new publications have addressed the link to water quality (temperature, dissolved oxygen, nutrients and pollutants), and others have dealt with sediment transport and geomorphology (particularly as it relates to break-up), stream ecology (plants, food cycle, etc.) and fish habitat.There is the growing recognition, that these types of study require collaborative efforts. In our view, the main areas requiring further work are: (1) to interface geomorphological and habitat models with quantitative river ice hydrodynamic models; (2) to develop a manager's toolbox (database management, remote sensing, forecasting, intervention methodologies, etc.) to enable

  10. Reduction Continuous Rank Probability Score for Hydrological Ensemble Prediction System

    NASA Astrophysics Data System (ADS)

    Trinh, Nguyen Bao; Thielen Del-Pozo, Jutta; Pappenberger, Florian; Cloke, Hannah L.; Bogner, Konrad

    2010-05-01

    Ensemble Prediction System (EPS), calculated operationally by the weather services for various lead-times, are increasingly used as input to hydrological models to extend warning times from short- to medium and even long-range. Although the general skill of EPS has been demonstrated to increase continuously over the past decades, it remains comparatively low for precipitation, one of the driving forces of hydrological processes. Due to the non-linear integrating nature of river runoff and the complexities of catchment runoff processes, one cannot assume that the skill of the hydrological forecasts is necessarily similar to the skill of the meteorological predictions. Furthermore, due to the integrating nature of discharge, which accumulates effects from upstream catchment and slow-responding groundwater processes, commonly applied skill scores in meteorology may not be fully adapted to describe the skill of probabilistic discharge predictions. For example, while for hydrological applications it may be interesting to compare the forecast skill between upstream and downstream stations, meteorological applications focus more on climatologically relevant regions. In this paper, a range of widely used probabilistic skill scores for assessing reliability, spread-skill, sharpness and bias are calculated for a 12 months case study in the Danube river basin. The Continuous Rank Probability Score (CRPS) is demonstrated to have deficiencies when comparing skill of discharge forecast for different hydrological stations. Therefore, we propose a modified CRPS that allows this comparison and is therefore particularly useful for hydrological applications.

  11. Seamless hydrological predictions for a monsoon driven catchment in North-East India

    NASA Astrophysics Data System (ADS)

    Köhn, Lisei; Bürger, Gerd; Bronstert, Axel

    2016-04-01

    Improving hydrological forecasting systems on different time scales is interesting and challenging with regards to humanitarian as well as scientific aspects. In meteorological research, short-, medium-, and long-term forecasts are now being merged to form a system of seamless weather and climate predictions. Coupling of these meteorological forecasts with a hydrological model leads to seamless predictions of streamflow, ranging from one day to a season. While there are big efforts made to analyse the uncertainties of probabilistic streamflow forecasts, knowledge of the single uncertainty contributions from meteorological and hydrological modeling is still limited. The overarching goal of this project is to gain knowledge in this subject by decomposing and quantifying the overall predictive uncertainty into its single factors for the entire seamless forecast horizon. Our study area is the Mahanadi River Basin in North-East India, which is prone to severe floods and droughts. Improved streamflow forecasts on different time scales would contribute to early flood warning as well as better water management operations in the agricultural sector. Because of strong inter-annual monsoon variations in this region, which are, unlike the mid-latitudes, partly predictable from long-term atmospheric-oceanic oscillations, the Mahanadi catchment represents an ideal study site. Regionalized precipitation forecasts are obtained by applying the method of expanded downscaling to the ensemble prediction systems of ECMWF and NCEP. The semi-distributed hydrological model HYPSO-RR, which was developed in the Eco-Hydrological Simulation Environment ECHSE, is set up for several sub-catchments of the Mahanadi River Basin. The model is calibrated automatically using the Dynamically Dimensioned Search algorithm, with a modified Nash-Sutcliff efficiency as objective function. Meteorological uncertainty is estimated from the existing ensemble simulations, while the hydrological uncertainty is

  12. Hydrological-niche models predict water plant functional group distributions in diverse wetland types.

    PubMed

    Deane, David C; Nicol, Jason M; Gehrig, Susan L; Harding, Claire; Aldridge, Kane T; Goodman, Abigail M; Brookes, Justin D

    2017-06-01

    Human use of water resources threatens environmental water supplies. If resource managers are to develop policies that avoid unacceptable ecological impacts, some means to predict ecosystem response to changes in water availability is necessary. This is difficult to achieve at spatial scales relevant for water resource management because of the high natural variability in ecosystem hydrology and ecology. Water plant functional groups classify species with similar hydrological niche preferences together, allowing a qualitative means to generalize community responses to changes in hydrology. We tested the potential for functional groups in making quantitative prediction of water plant functional group distributions across diverse wetland types over a large geographical extent. We sampled wetlands covering a broad range of hydrogeomorphic and salinity conditions in South Australia, collecting both hydrological and floristic data from 687 quadrats across 28 wetland hydrological gradients. We built hydrological-niche models for eight water plant functional groups using a range of candidate models combining different surface inundation metrics. We then tested the predictive performance of top-ranked individual and averaged models for each functional group. Cross validation showed that models achieved acceptable predictive performance, with correct classification rates in the range 0.68-0.95. Model predictions can be made at any spatial scale that hydrological data are available and could be implemented in a geographical information system. We show the response of water plant functional groups to inundation is consistent enough across diverse wetland types to quantify the probability of hydrological impacts over regional spatial scales. © 2017 by the Ecological Society of America.

  13. Advancing the Implementation of Hydrologic Models as Web-based Applications

    NASA Astrophysics Data System (ADS)

    Dahal, P.; Tarboton, D. G.; Castronova, A. M.

    2017-12-01

    Advanced computer simulations are required to understand hydrologic phenomenon such as rainfall-runoff response, groundwater hydrology, snow hydrology, etc. Building a hydrologic model instance to simulate a watershed requires investment in data (diverse geospatial datasets such as terrain, soil) and computer resources, typically demands a wide skill set from the analyst, and the workflow involved is often difficult to reproduce. This work introduces a web-based prototype infrastructure in the form of a web application that provides researchers with easy to use access to complete hydrological modeling functionality. This includes creating the necessary geospatial and forcing data, preparing input files for a model by applying complex data preprocessing, running the model for a user defined watershed, and saving the results to a web repository. The open source Tethys Platform was used to develop the web app front-end Graphical User Interface (GUI). We used HydroDS, a webservice that provides data preparation processing capability to support backend computations used by the app. Results are saved in HydroShare, a hydrologic information system that supports the sharing of hydrologic data, model and analysis tools. The TOPographic Kinematic APproximation and Integration (TOPKAPI) model served as the example for which we developed a complete hydrologic modeling service to demonstrate the approach. The final product is a complete modeling system accessible through the web to create input files, and run the TOPKAPI hydrologic model for a watershed of interest. We are investigating similar functionality for the preparation of input to Regional Hydro-Ecological Simulation System (RHESSys). Key Words: hydrologic modeling, web services, hydrologic information system, HydroShare, HydroDS, Tethys Platform

  14. Role-play games, experiments, workshops, blog posts: how community activities in HEPEX contribute to advance hydrologic ensemble prediction

    NASA Astrophysics Data System (ADS)

    Ramos, Maria-Helena; Wetterhall, Fredrik; Wood, Andy; Wang, Qj; Pappenberger, Florian; Verkade, Jan

    2017-04-01

    Since 2004, HEPEX (Hydrologic Ensemble Prediction Experiment) has been fostering a community of researchers and practitioners around the world. Through the years, it has contributed to establish a more integrative view of hydrological forecasting, where data assimilation, hydro-meteorological modelling chains, post-processing techniques, expert knowledge, and decision support systems are connected to enhance operational systems and water management applications. Here we present the community activities in HEPEX that have contributed to strengthening this unfunded/volunteer effort for more than a decade. It includes the organization of workshops, conference sessions, testbeds and inter-comparison experiments. More recently, HEPEX has also prompted the development of several publicly available role-play games and, since 2013, it has been running a blog portal (www.hepex.org), which is used as an intersection point for members. Through this website, members can continuously share their research, make announcements, report on workshops, projects and meetings, and hear about related research and operational challenges. It also creates a platform for early career scientists to become increasingly involved in hydrological forecasting science and applications.

  15. Passive microwave (SSM/I) satellite predictions of valley glacier hydrology, Matanuska Glacier, Alaska

    USGS Publications Warehouse

    Kopczynski, S.E.; Ramage, J.; Lawson, D.; Goetz, S.; Evenson, E.; Denner, J.; Larson, G.

    2008-01-01

    We advance an approach to use satellite passive microwave observations to track valley glacier snowmelt and predict timing of spring snowmelt-induced floods at the terminus. Using 37 V GHz brightness temperatures (Tb) from the Special Sensor Microwave hnager (SSM/I), we monitor snowmelt onset when both Tb and the difference between the ascending and descending overpasses exceed fixed thresholds established for Matanuska Glacier. Melt is confirmed by ground-measured air temperature and snow-wetness, while glacier hydrologic responses are monitored by a stream gauge, suspended-sediment sensors and terminus ice velocity measurements. Accumulation area snowmelt timing is correlated (R2 = 0.61) to timing of the annual snowmelt flood peak and can be predicted within ??5 days. Copyright 2008 by the American Geophysical Union.

  16. Designing hydrologic monitoring networks to maximize predictability of hydrologic conditions in a data assimilation system: a case study from South Florida, U.S.A

    NASA Astrophysics Data System (ADS)

    Flores, A. N.; Pathak, C. S.; Senarath, S. U.; Bras, R. L.

    2009-12-01

    Robust hydrologic monitoring networks represent a critical element of decision support systems for effective water resource planning and management. Moreover, process representation within hydrologic simulation models is steadily improving, while at the same time computational costs are decreasing due to, for instance, readily available high performance computing resources. The ability to leverage these increasingly complex models together with the data from these monitoring networks to provide accurate and timely estimates of relevant hydrologic variables within a multiple-use, managed water resources system would substantially enhance the information available to resource decision makers. Numerical data assimilation techniques provide mathematical frameworks through which uncertain model predictions can be constrained to observational data to compensate for uncertainties in the model forcings and parameters. In ensemble-based data assimilation techniques such as the ensemble Kalman Filter (EnKF), information in observed variables such as canal, marsh and groundwater stages are propagated back to the model states in a manner related to: (1) the degree of certainty in the model state estimates and observations, and (2) the cross-correlation between the model states and the observable outputs of the model. However, the ultimate degree to which hydrologic conditions can be accurately predicted in an area of interest is controlled, in part, by the configuration of the monitoring network itself. In this proof-of-concept study we developed an approach by which the design of an existing hydrologic monitoring network is adapted to iteratively improve the predictions of hydrologic conditions within an area of the South Florida Water Management District (SFWMD). The objective of the network design is to minimize prediction errors of key hydrologic states and fluxes produced by the spatially distributed Regional Simulation Model (RSM), developed specifically to simulate the

  17. Predicting the natural flow regime: Models for assessing hydrological alteration in streams

    USGS Publications Warehouse

    Carlisle, D.M.; Falcone, J.; Wolock, D.M.; Meador, M.R.; Norris, R.H.

    2009-01-01

    Understanding the extent to which natural streamflow characteristics have been altered is an important consideration for ecological assessments of streams. Assessing hydrologic condition requires that we quantify the attributes of the flow regime that would be expected in the absence of anthropogenic modifications. The objective of this study was to evaluate whether selected streamflow characteristics could be predicted at regional and national scales using geospatial data. Long-term, gaged river basins distributed throughout the contiguous US that had streamflow characteristics representing least disturbed or near pristine conditions were identified. Thirteen metrics of the magnitude, frequency, duration, timing and rate of change of streamflow were calculated using a 20-50 year period of record for each site. We used random forests (RF), a robust statistical modelling approach, to develop models that predicted the value for each streamflow metric using natural watershed characteristics. We compared the performance (i.e. bias and precision) of national- and regional-scale predictive models to that of models based on landscape classifications, including major river basins, ecoregions and hydrologic landscape regions (HLR). For all hydrologic metrics, landscape stratification models produced estimates that were less biased and more precise than a null model that accounted for no natural variability. Predictive models at the national and regional scale performed equally well, and substantially improved predictions of all hydrologic metrics relative to landscape stratification models. Prediction error rates ranged from 15 to 40%, but were 25% for most metrics. We selected three gaged, non-reference sites to illustrate how predictive models could be used to assess hydrologic condition. These examples show how the models accurately estimate predisturbance conditions and are sensitive to changes in streamflow variability associated with long-term land-use change. We also

  18. Hydrological Predictability for the Peruvian Amazon

    NASA Astrophysics Data System (ADS)

    Towner, Jamie; Stephens, Elizabeth; Cloke, Hannah; Bazo, Juan; Coughlan, Erin; Zsoter, Ervin

    2017-04-01

    Population growth in the Peruvian Amazon has prompted the expansion of livelihoods further into the floodplain and thus increasing vulnerability to the annual rise and fall of the river. This growth has coincided with a period of increasing hydrological extremes with more frequent severe flood events. The anticipation and forecasting of these events is crucial for mitigating vulnerability. Forecast-based Financing (FbF) an initiative of the German Red Cross implements risk reducing actions based on threshold exceedance within hydrometeorological forecasts using the Global Flood Awareness System (GloFAS). However, the lead times required to complete certain actions can be long (e.g. several weeks to months ahead to purchase materials and reinforce houses) and are beyond the current capabilities of GloFAS. Therefore, further calibration of the model is required in addition to understanding the climatic drivers and associated hydrological response for specific flood events, such as those observed in 2009, 2012 and 2015. This review sets out to determine the current capabilities of the GloFAS model while exploring the limits of predictability for the Amazon basin. More specifically, how the temporal patterns of flow within the main coinciding tributaries correspond to the overall Amazonian flood wave under various climatic and meteorological influences. Linking the source areas of flow to predictability within the seasonal forecasting system will develop the ability to expand the limit of predictability of the flood wave. This presentation will focus on the Iquitos region of Peru, while providing an overview of the new techniques and current challenges faced within seasonal flood prediction.

  19. A Dynamic Hydrology-Critical Zone Framework for Rainfall-triggered Landslide Hazard Prediction

    NASA Astrophysics Data System (ADS)

    Dialynas, Y. G.; Foufoula-Georgiou, E.; Dietrich, W. E.; Bras, R. L.

    2017-12-01

    Watershed-scale coupled hydrologic-stability models are still in their early stages, and are characterized by important limitations: (a) either they assume steady-state or quasi-dynamic watershed hydrology, or (b) they simulate landslide occurrence based on a simple one-dimensional stability criterion. Here we develop a three-dimensional landslide prediction framework, based on a coupled hydrologic-slope stability model and incorporation of the influence of deep critical zone processes (i.e., flow through weathered bedrock and exfiltration to the colluvium) for more accurate prediction of the timing, location, and extent of landslides. Specifically, a watershed-scale slope stability model that systematically accounts for the contribution of driving and resisting forces in three-dimensional hillslope segments was coupled with a spatially-explicit and physically-based hydrologic model. The landslide prediction framework considers critical zone processes and structure, and explicitly accounts for the spatial heterogeneity of surface and subsurface properties that control slope stability, including soil and weathered bedrock hydrological and mechanical characteristics, vegetation, and slope morphology. To test performance, the model was applied in landslide-prone sites in the US, the hydrology of which has been extensively studied. Results showed that both rainfall infiltration in the soil and groundwater exfiltration exert a strong control on the timing and magnitude of landslide occurrence. We demonstrate the extent to which three-dimensional slope destabilizing factors, which are modulated by dynamic hydrologic conditions in the soil-bedrock column, control landslide initiation at the watershed scale.

  20. New Hydrologic Insights to Advance Geophysical Investigation of the Unsaturated Zone

    NASA Astrophysics Data System (ADS)

    Nimmo, J. R.; Perkins, K. S.

    2015-12-01

    Advances in hydrology require information from the unsaturated zone, especially for problems related to groundwater contamination, water-supply sustainability, and ecohydrology. Unsaturated-zone processes are notoriously difficult to quantify; soils and rocks are visually opaque, spatially variable in the extreme, and easily disturbed by instrument installation. Thus there is great value in noninvasive techniques that produce water-related data of high density in space and time. Methods based on resistivity and electromagnetic waves have already produced significant new understanding of percolation processes, root-zone water retention, influences of evapotranspiration on soil-water, and effects of preferential flow. Further developments are underway for such purposes as noninvasive application to greater depths, increased resolution, adaptation for lab-scale experiments, and calibration in heterogeneous media. Beyond these, however, there is need for a stronger marriage of hydrologic and geophysical knowledge and perspective. Possible means to greater and faster progress include: Apply the latest hydrologic understanding, both pore-scale and macroscopic, to the detection of preferential flow paths and their degree of activation. In the continuing advancement of hardware and techniques, draw creatively from developments in such fields as high-energy physics, medical imaging, astrogeology, high-tech semiconductors, and bioinstrumentation. Sidestep the imaging process where possible to measure essential properties and fluxes more directly. Pose questions that have a strong end-use character, like "how does storm intensity relate to aquifer recharge rate" rather than "what is the shape of the wetting front". The greatest advances in geophysical investigation of the unsaturated zone will come from methods informed by the latest understanding of unsaturated systems and processes, and aimed as directly as possible at the answers to important hydrologic questions.

  1. Consortium of Universities for the Advancement of Hydrologic Science Inc. (CUAHSI) Science Plan: A Community-based Infrastructure Initiative

    NASA Astrophysics Data System (ADS)

    Wilson, J. L.; Dressler, K.; Hooper, R. P.

    2005-12-01

    The river basin is a fundamental unit of the landscape and water in that defined landscape plays a central role in shaping the land surface, in dissolving minerals, in transporting chemicals, and in determining species distribution. Therefore, the river basin is a natural observatory for examining hydrologic phenomena and the complex interaction of physical, chemical, and biological processes that control them. CUAHSI, incorporated in 2001, is a community-based research infrastructure initiative formed to mobilize the hydrologic community through addressing key science questions and leveraging nationwide hydrologic resources from its member institutions and collaborative partners. Through an iterative community-based process, it has been previously proposed to develop a network of hydrologic infrastructure that organizes around scales on the order of 10,000 km2 to examine critical interfaces such as the land-surface, atmosphere, and human impact. Data collection will characterize the stores, fluxes, physical pathways, and residence time distributions of water, sediment, nutrients, and contaminants coherently at nested scales. These fundamental properties can be used by a wide range of scientific disciplines to address environmental questions. This more complete characterization will enable new linkages to be identified and hypotheses to be tested more incisively. With such a research platform, hydrologic science can advance beyond measuring streamflow or precipitation input to understanding how the river basin functions in both its internal processes and in responding to environmental stressors. That predictive understanding is needed to make informed decisions as development and even natural pressures stress existing water supplies and competing demands for water require non-traditional solutions that take into consideration economic, environmental, and social factors. Advanced hydrologic infrastructure will enable research for a broad range of multidisciplinary

  2. Practical guidance on representing the heteroscedasticity of residual errors of hydrological predictions

    NASA Astrophysics Data System (ADS)

    McInerney, David; Thyer, Mark; Kavetski, Dmitri; Kuczera, George

    2016-04-01

    Appropriate representation of residual errors in hydrological modelling is essential for accurate and reliable probabilistic streamflow predictions. In particular, residual errors of hydrological predictions are often heteroscedastic, with large errors associated with high runoff events. Although multiple approaches exist for representing this heteroscedasticity, few if any studies have undertaken a comprehensive evaluation and comparison of these approaches. This study fills this research gap by evaluating a range of approaches for representing heteroscedasticity in residual errors. These approaches include the 'direct' weighted least squares approach and 'transformational' approaches, such as logarithmic, Box-Cox (with and without fitting the transformation parameter), logsinh and the inverse transformation. The study reports (1) theoretical comparison of heteroscedasticity approaches, (2) empirical evaluation of heteroscedasticity approaches using a range of multiple catchments / hydrological models / performance metrics and (3) interpretation of empirical results using theory to provide practical guidance on the selection of heteroscedasticity approaches. Importantly, for hydrological practitioners, the results will simplify the choice of approaches to represent heteroscedasticity. This will enhance their ability to provide hydrological probabilistic predictions with the best reliability and precision for different catchment types (e.g. high/low degree of ephemerality).

  3. Assimilation of remote sensing observations into a continuous distributed hydrological model: impacts on the hydrologic cycle

    NASA Astrophysics Data System (ADS)

    Laiolo, Paola; Gabellani, Simone; Campo, Lorenzo; Cenci, Luca; Silvestro, Francesco; Delogu, Fabio; Boni, Giorgio; Rudari, Roberto

    2015-04-01

    The reliable estimation of hydrological variables (e.g. soil moisture, evapotranspiration, surface temperature) in space and time is of fundamental importance in operational hydrology to improve the forecast of the rainfall-runoff response of catchments and, consequently, flood predictions. Nowadays remote sensing can offer a chance to provide good space-time estimates of several hydrological variables and then improve hydrological model performances especially in environments with scarce in-situ data. This work investigates the impact of the assimilation of different remote sensing products on the hydrological cycle by using a continuous physically based distributed hydrological model. Three soil moisture products derived by ASCAT (Advanced SCATterometer) are used to update the model state variables. The satellite-derived products are assimilated into the hydrological model using different assimilation techniques: a simple nudging and the Ensemble Kalman Filter. Moreover two assimilation strategies are evaluated to assess the impact of assimilating the satellite products at model spatial resolution or at the satellite scale. The experiments are carried out for three Italian catchments on multi year period. The benefits on the model predictions of discharge, LST, evapotranspiration and soil moisture dynamics are tested and discussed.

  4. Predicting hydrological response to forest changes by simple statistical models: the selection of the best indicator of forest changes with a hydrological perspective

    NASA Astrophysics Data System (ADS)

    Ning, D.; Zhang, M.; Ren, S.; Hou, Y.; Yu, L.; Meng, Z.

    2017-01-01

    Forest plays an important role in hydrological cycle, and forest changes will inevitably affect runoff across multiple spatial scales. The selection of a suitable indicator for forest changes is essential for predicting forest-related hydrological response. This study used the Meijiang River, one of the headwaters of the Poyang Lake as an example to identify the best indicator of forest changes for predicting forest change-induced hydrological responses. Correlation analysis was conducted first to detect the relationships between monthly runoff and its predictive variables including antecedent monthly precipitation and indicators for forest changes (forest coverage, vegetation indices including EVI, NDVI, and NDWI), and by use of the identified predictive variables that were most correlated with monthly runoff, multiple linear regression models were then developed. The model with best performance identified in this study included two independent variables -antecedent monthly precipitation and NDWI. It indicates that NDWI is the best indicator of forest change in hydrological prediction while forest coverage, the most commonly used indicator of forest change is insignificantly related to monthly runoff. This highlights the use of vegetation index such as NDWI to indicate forest changes in hydrological studies. This study will provide us with an efficient way to quantify the hydrological impact of large-scale forest changes in the Meijiang River watershed, which is crucial for downstream water resource management and ecological protection in the Poyang Lake basin.

  5. Improving Robustness of Hydrologic Ensemble Predictions Through Probabilistic Pre- and Post-Processing in Sequential Data Assimilation

    NASA Astrophysics Data System (ADS)

    Wang, S.; Ancell, B. C.; Huang, G. H.; Baetz, B. W.

    2018-03-01

    Data assimilation using the ensemble Kalman filter (EnKF) has been increasingly recognized as a promising tool for probabilistic hydrologic predictions. However, little effort has been made to conduct the pre- and post-processing of assimilation experiments, posing a significant challenge in achieving the best performance of hydrologic predictions. This paper presents a unified data assimilation framework for improving the robustness of hydrologic ensemble predictions. Statistical pre-processing of assimilation experiments is conducted through the factorial design and analysis to identify the best EnKF settings with maximized performance. After the data assimilation operation, statistical post-processing analysis is also performed through the factorial polynomial chaos expansion to efficiently address uncertainties in hydrologic predictions, as well as to explicitly reveal potential interactions among model parameters and their contributions to the predictive accuracy. In addition, the Gaussian anamorphosis is used to establish a seamless bridge between data assimilation and uncertainty quantification of hydrologic predictions. Both synthetic and real data assimilation experiments are carried out to demonstrate feasibility and applicability of the proposed methodology in the Guadalupe River basin, Texas. Results suggest that statistical pre- and post-processing of data assimilation experiments provide meaningful insights into the dynamic behavior of hydrologic systems and enhance robustness of hydrologic ensemble predictions.

  6. Reducing hydrologic model uncertainty in monthly streamflow predictions using multimodel combination

    NASA Astrophysics Data System (ADS)

    Li, Weihua; Sankarasubramanian, A.

    2012-12-01

    Model errors are inevitable in any prediction exercise. One approach that is currently gaining attention in reducing model errors is by combining multiple models to develop improved predictions. The rationale behind this approach primarily lies on the premise that optimal weights could be derived for each model so that the developed multimodel predictions will result in improved predictions. A new dynamic approach (MM-1) to combine multiple hydrological models by evaluating their performance/skill contingent on the predictor state is proposed. We combine two hydrological models, "abcd" model and variable infiltration capacity (VIC) model, to develop multimodel streamflow predictions. To quantify precisely under what conditions the multimodel combination results in improved predictions, we compare multimodel scheme MM-1 with optimal model combination scheme (MM-O) by employing them in predicting the streamflow generated from a known hydrologic model (abcd model orVICmodel) with heteroscedastic error variance as well as from a hydrologic model that exhibits different structure than that of the candidate models (i.e., "abcd" model or VIC model). Results from the study show that streamflow estimated from single models performed better than multimodels under almost no measurement error. However, under increased measurement errors and model structural misspecification, both multimodel schemes (MM-1 and MM-O) consistently performed better than the single model prediction. Overall, MM-1 performs better than MM-O in predicting the monthly flow values as well as in predicting extreme monthly flows. Comparison of the weights obtained from each candidate model reveals that as measurement errors increase, MM-1 assigns weights equally for all the models, whereas MM-O assigns higher weights for always the best-performing candidate model under the calibration period. Applying the multimodel algorithms for predicting streamflows over four different sites revealed that MM-1 performs

  7. Recent advances in catchment hydrology

    NASA Astrophysics Data System (ADS)

    van Meerveld, I. H. J.

    2017-12-01

    Despite the consensus that field observations and catchment studies are imperative to understand hydrological processes, to determine the impacts of global change, to quantify the spatial and temporal variability in hydrological fluxes, and to refine and test hydrological models, there is a decline in the number of field studies. This decline and the importance of fieldwork for catchment hydrology have been described in several recent opinion papers. This presentation will summarize these commentaries, describe how catchment studies have evolved over time, and highlight the findings from selected recent studies published in Water Resources Research.

  8. Extending medium-range predictability of extreme hydrological events in Europe

    PubMed Central

    Lavers, David A.; Pappenberger, Florian; Zsoter, Ervin

    2014-01-01

    Widespread flooding occurred across northwest Europe during the winter of 2013/14, resulting in large socioeconomic damages. In the historical record, extreme hydrological events have been connected with intense water vapour transport. Here we show that water vapour transport has higher medium-range predictability compared with precipitation in the winter 2013/14 forecasts from the European Centre for Medium-Range Weather Forecasts. Applying the concept of potential predictability, the transport is found to extend the forecast horizon by 3 days in some European regions. Our results suggest that the breakdown in precipitation predictability is due to uncertainty in the horizontal mass convergence location, an essential mechanism for precipitation generation. Furthermore, the predictability increases with larger spatial averages. Given the strong association between precipitation and water vapour transport, especially for extreme events, we conclude that the higher transport predictability could be used as a model diagnostic to increase preparedness for extreme hydrological events. PMID:25387309

  9. The utility of satellite precipitation products for hydrologic prediction in topographically complex regions: The Chehalis River Basin, WA as a case study

    NASA Astrophysics Data System (ADS)

    Cao, Q.; Mehran, A.; Lettenmaier, D. P.; Mass, C.; Johnson, N.

    2015-12-01

    Accurate measurements of precipitation are of great importance in hydrologic predictions especially for floods, which are a pervasive natural hazard. One of the primary objectives of Global Precipitation Measurement (GPM) mission is to provide a basis for hydrologic predictions using satellite sensors. A major advance in GPM relative to the Tropical Rainfall Measuring Mission (TRMM) is that it observes atmospheric river (AR) events, most of which have landfall too far north to be tracked by TRMM. These events are responsible for most major floods along the U.S. West Coast. We address the question of whether, for hydrologic modeling purposes, it is better to use precipitation products derived directly from GPM and/or other precipitation fields from weather models that have assimilated satellite data. Our overall strategy is to compare different methods for prediction of flood and/or high flow events by different forcings on the hydrologic model. We examine four different configurations of the Distroibute Hydrology Soil Vegetation Model (DHSVM) over the Chehalis River Basin that use a) precipitation forcings based on gridded station data; b) precipitation forcings based on NWS WSR-88D data, c) forcings based from short-term precipitation forecasts using the Weather Research and Forecasting (WRF) mesoscale atmospheric model, and d) satellite-based precipitation estimates (TMPA and IMERG). We find that in general, biases in the radar and satellite products result in much larger errors than with either gridded station data or WRF forcings, but if these biases are removed, comparable performance in flood predictions can be achieved by Satellite-based precipitation estimates (TMPA and IMERG).

  10. Prediction of Hydrologic Characteristics for Ungauged Catchments to Support Hydroecological Modeling

    NASA Astrophysics Data System (ADS)

    Bond, Nick R.; Kennard, Mark J.

    2017-11-01

    Hydrologic variability is a fundamental driver of ecological processes and species distribution patterns within river systems, yet the paucity of gauges in many catchments means that streamflow data are often unavailable for ecological survey sites. Filling this data gap is an important challenge in hydroecological research. To address this gap, we first test the ability to spatially extrapolate hydrologic metrics calculated from gauged streamflow data to ungauged sites as a function of stream distance and catchment area. Second, we examine the ability of statistical models to predict flow regime metrics based on climate and catchment physiographic variables. Our assessment focused on Australia's largest catchment, the Murray-Darling Basin (MDB). We found that hydrologic metrics were predictable only between sites within ˜25 km of one another. Beyond this, correlations between sites declined quickly. We found less than 40% of fish survey sites from a recent basin-wide monitoring program (n = 777 sites) to fall within this 25 km range, thereby greatly limiting the ability to utilize gauge data for direct spatial transposition of hydrologic metrics to biological survey sites. In contrast, statistical model-based transposition proved effective in predicting ecologically relevant aspects of the flow regime (including metrics describing central tendency, high- and low-flows intermittency, seasonality, and variability) across the entire gauge network (median R2 ˜ 0.54, range 0.39-0.94). Modeled hydrologic metrics thus offer a useful alternative to empirical data when examining biological survey data from ungauged sites. More widespread use of these statistical tools and modeled metrics could expand our understanding of flow-ecology relationships.

  11. Global-Scale Hydrology: Simple Characterization of Complex Simulation

    NASA Technical Reports Server (NTRS)

    Koster, Randal D.

    1999-01-01

    Atmospheric general circulation models (AGCMS) are unique and valuable tools for the analysis of large-scale hydrology. AGCM simulations of climate provide tremendous amounts of hydrological data with a spatial and temporal coverage unmatched by observation systems. To the extent that the AGCM behaves realistically, these data can shed light on the nature of the real world's hydrological cycle. In the first part of the seminar, I will describe the hydrological cycle in a typical AGCM, with some emphasis on the validation of simulated precipitation against observations. The second part of the seminar will focus on a key goal in large-scale hydrology studies, namely the identification of simple, overarching controls on hydrological behavior hidden amidst the tremendous amounts of data produced by the highly complex AGCM parameterizations. In particular, I will show that a simple 50-year-old climatological relation (and a recent extension we made to it) successfully predicts, to first order, both the annual mean and the interannual variability of simulated evaporation and runoff fluxes. The seminar will conclude with an example of a practical application of global hydrology studies. The accurate prediction of weather statistics several months in advance would have tremendous societal benefits, and conventional wisdom today points at the use of coupled ocean-atmosphere-land models for such seasonal-to-interannual prediction. Understanding the hydrological cycle in AGCMs is critical to establishing the potential for such prediction. Our own studies show, among other things, that soil moisture retention can lead to significant precipitation predictability in many midlatitude and tropical regions.

  12. Geostatistical enhancement of european hydrological predictions

    NASA Astrophysics Data System (ADS)

    Pugliese, Alessio; Castellarin, Attilio; Parajka, Juraj; Arheimer, Berit; Bagli, Stefano; Mazzoli, Paolo; Montanari, Alberto; Blöschl, Günter

    2016-04-01

    Geostatistical Enhancement of European Hydrological Prediction (GEEHP) is a research experiment developed within the EU funded SWITCH-ON project, which proposes to conduct comparative experiments in a virtual laboratory in order to share water-related information and tackle changes in the hydrosphere for operational needs (http://www.water-switch-on.eu). The main objective of GEEHP deals with the prediction of streamflow indices and signatures in ungauged basins at different spatial scales. In particular, among several possible hydrological signatures we focus in our experiment on the prediction of flow-duration curves (FDCs) along the stream-network, which has attracted an increasing scientific attention in the last decades due to the large number of practical and technical applications of the curves (e.g. hydropower potential estimation, riverine habitat suitability and ecological assessments, etc.). We apply a geostatistical procedure based on Top-kriging, which has been recently shown to be particularly reliable and easy-to-use regionalization approach, employing two different type of streamflow data: pan-European E-HYPE simulations (http://hypeweb.smhi.se/europehype) and observed daily streamflow series collected in two pilot study regions, i.e. Tyrol (merging data from Austrian and Italian stream gauging networks) and Sweden. The merger of the two study regions results in a rather large area (~450000 km2) and might be considered as a proxy for a pan-European application of the approach. In a first phase, we implement a bidirectional validation, i.e. E-HYPE catchments are set as training sites to predict FDCs at the same sites where observed data are available, and vice-versa. Such a validation procedure reveals (1) the usability of the proposed approach for predicting the FDCs over the entire river network of interest using alternatively observed data and E-HYPE simulations and (2) the accuracy of E-HYPE-based predictions of FDCs in ungauged sites. In a

  13. Integrating SMOS brightness temperatures with a new conceptual spatially distributed hydrological model for improving flood and drought predictions at large scale.

    NASA Astrophysics Data System (ADS)

    Hostache, Renaud; Rains, Dominik; Chini, Marco; Lievens, Hans; Verhoest, Niko E. C.; Matgen, Patrick

    2017-04-01

    Motivated by climate change and its impact on the scarcity or excess of water in many parts of the world, several agencies and research institutions have taken initiatives in monitoring and predicting the hydrologic cycle at a global scale. Such a monitoring/prediction effort is important for understanding the vulnerability to extreme hydrological events and for providing early warnings. This can be based on an optimal combination of hydro-meteorological models and remote sensing, in which satellite measurements can be used as forcing or calibration data or for regularly updating the model states or parameters. Many advances have been made in these domains and the near future will bring new opportunities with respect to remote sensing as a result of the increasing number of spaceborn sensors enabling the large scale monitoring of water resources. Besides of these advances, there is currently a tendency to refine and further complicate physically-based hydrologic models to better capture the hydrologic processes at hand. However, this may not necessarily be beneficial for large-scale hydrology, as computational efforts are therefore increasing significantly. As a matter of fact, a novel thematic science question that is to be investigated is whether a flexible conceptual model can match the performance of a complex physically-based model for hydrologic simulations at large scale. In this context, the main objective of this study is to investigate how innovative techniques that allow for the estimation of soil moisture from satellite data can help in reducing errors and uncertainties in large scale conceptual hydro-meteorological modelling. A spatially distributed conceptual hydrologic model has been set up based on recent developments of the SUPERFLEX modelling framework. As it requires limited computational efforts, this model enables early warnings for large areas. Using as forcings the ERA-Interim public dataset and coupled with the CMEM radiative transfer model

  14. Fundamental concepts and research priorities for advancing the science of urban stormwater hydrology and flood management

    NASA Astrophysics Data System (ADS)

    Nytch, C. J.; Meléndez-Ackerman, E. J.; Vivoni, E. R.; Grove, J. M.; Ortiz, J.

    2016-12-01

    In cities, hydrologic processes are drastically altered by human interventions. Modification of land cover and the enhancement of hydraulic efficiency have been documented as root causes of augmented stormwater runoff in urban watersheds, contributing to higher magnitude discharge events that pose flood risks for human communities. Climate change is expected to accelerate the hydrologic cycle, leading to more extreme events and increased flood risk. We present a synthesis of the physical and conceptual components and processes that govern urban stormwater runoff, and highlight key areas for future research. There is limited understanding about the fine-scale spatio-temporal relationships between gray, green, brown, and blue land cover features, the underlying social-ecological mechanisms responsible for their distribution, and the resulting effects on runoff dynamics. Horizontal and vertical complexity of urban morphological features and connectivity with the network of stormwater management infrastructure leads to heterogeneous and non-linear runoff responses that confound efforts for accurately predicting flood hazards. Quantitative analysis is needed to understand how urban drainage network structure varies across stream orders, and illuminate the landscape-scale patterns that potentially serve as organizing principles for generating hydrologic processes across diverse socio-bio-climatic domains and scales. Field-based and modeling studies are also needed to quantify the individual hydrologic capacities of urban structural elements and their cumulative effects at the watershed scale, particularly in developing regions. Integrated, transdisciplinary, multi-scalar approaches to framing and investigating complex socio-eco-techno-hydrologic systems are essential for advancing the science of urban stormwater hydrology, and developing resilient, multifunctional management solutions appropriate to the challenges of urban flooding in the twenty-first century.

  15. Towards the development of a multimodel hydrological ensemble prediction system for La Mojana, Colombia

    NASA Astrophysics Data System (ADS)

    Brochero, D.; Peña, J.; Anctil, F.; Boucher, M. A.; Nogales, J.; Reyes, N.

    2016-12-01

    The impacts of floods in Colombia during 2010 and 2011 as a result of ENSO in its cold phase (La Niña) marked a milestone in Colombian politics. In La Mojana region the balance was around 100,000 homeless and 3 km2 of flooded crops. We model the upstream basin of La Mojana (3600 km2 and a mean annual precipitation from 1000mm in valleys to 4500 mm in mountains). A forecasting system of at least three days in advance was judged prudent. This basin receives an streamflow highly regulated by multiple reservoirs that we model with a recurrent neural networks from 1 to 3-days ahead. For hydrological modeling purposes we use the GR4J, HBV, and SIMHYD models, records of daily precipitation, temperature, and streamflows, and 110 prediction scenarios of precipitation and temperature from Canada, USA, Brazil, and Europe extracted from the TIGGE database (MEPS). Calibration period is between January 2004 and August 2011. Validation from September to December 2011, taking as meteorological input the MEPS. We analised four alternative for the 3-day Hydrological Ensemble Prediction System (HEPS) Calibration: 1) only the GR4J model and observed values, 2). as 1 but HBV and SIMHYD are included, 3). Simultaneous optimization of the three hydrological models based on the reliability maximisation and the CRPS minimisation using the multiobjective calibration, observed and forecasted temperature and precipitation from the MEPS and, 4). as 3 but adding the daily streamflow data assimilation. Results show that the use of multiple hydrological models is clearly advantageous but even more performing the simultaneous optimization of hydrological models in the probabilistic context directly. The results evolution of the MAE on the reliability diagram (MAE-RD) are 43%, 27%, 17% and 15% respectively for the four alternatives. Regarding CRPS, MAE results show that the probabilistic prediction improves the deterministic estimate based on the daily mean HEPS scenario, despite the improvement in

  16. A blueprint for using climate change predictions in an eco-hydrological study

    NASA Astrophysics Data System (ADS)

    Caporali, E.; Fatichi, S.; Ivanov, V. Y.

    2009-12-01

    There is a growing interest to extend climate change predictions to smaller, catchment-size scales and identify their implications on hydrological and ecological processes. Small scale processes are, in fact, expected to mediate climate changes, producing local effects and feedbacks that can interact with the principal consequences of the change. This is particularly applicable, when a complex interaction, such as the inter-relationship between the hydrological cycle and vegetation dynamics, is considered. This study presents a blueprint methodology for studying climate change impacts, as inferred from climate models, on eco-hydrological dynamics at the catchment scale. Climate conditions, present or future, are imposed through input hydrometeorological variables for hydrological and eco-hydrological models. These variables are simulated with an hourly weather generator as an outcome of a stochastic downscaling technique. The generator is parameterized to reproduce the climate of southwestern Arizona for present (1961-2000) and future (2081-2100) conditions. The methodology provides the capability to generate ensemble realizations for the future that take into account the heterogeneous nature of climate predictions from different models. The generated time series of meteorological variables for the two scenarios corresponding to the current and mean expected future serve as input to a coupled hydrological and vegetation dynamics model, “Tethys-Chloris”. The hydrological model reproduces essential components of the land-surface hydrological cycle, solving the mass and energy budget equations. The vegetation model parsimoniously parameterizes essential plant life-cycle processes, including photosynthesis, phenology, carbon allocation, and tissue turnover. The results for the two mean scenarios are compared and discussed in terms of changes in the hydrological balance components, energy fluxes, and indices of vegetation productivity The need to account for

  17. Identifying influential data points in hydrological model calibration and their impact on streamflow predictions

    NASA Astrophysics Data System (ADS)

    Wright, David; Thyer, Mark; Westra, Seth

    2015-04-01

    Highly influential data points are those that have a disproportionately large impact on model performance, parameters and predictions. However, in current hydrological modelling practice the relative influence of individual data points on hydrological model calibration is not commonly evaluated. This presentation illustrates and evaluates several influence diagnostics tools that hydrological modellers can use to assess the relative influence of data. The feasibility and importance of including influence detection diagnostics as a standard tool in hydrological model calibration is discussed. Two classes of influence diagnostics are evaluated: (1) computationally demanding numerical "case deletion" diagnostics; and (2) computationally efficient analytical diagnostics, based on Cook's distance. These diagnostics are compared against hydrologically orientated diagnostics that describe changes in the model parameters (measured through the Mahalanobis distance), performance (objective function displacement) and predictions (mean and maximum streamflow). These influence diagnostics are applied to two case studies: a stage/discharge rating curve model, and a conceptual rainfall-runoff model (GR4J). Removing a single data point from the calibration resulted in differences to mean flow predictions of up to 6% for the rating curve model, and differences to mean and maximum flow predictions of up to 10% and 17%, respectively, for the hydrological model. When using the Nash-Sutcliffe efficiency in calibration, the computationally cheaper Cook's distance metrics produce similar results to the case-deletion metrics at a fraction of the computational cost. However, Cooks distance is adapted from linear regression with inherit assumptions on the data and is therefore less flexible than case deletion. Influential point detection diagnostics show great potential to improve current hydrological modelling practices by identifying highly influential data points. The findings of this

  18. Toward an Online Community of Educators: The Modular Curriculum for Hydrologic Advancement (MOCHA)

    NASA Astrophysics Data System (ADS)

    Kelleher, C.; Wagener, T.; Gooseff, M. N.; Gregg, S.; McGlynn, B. L.; Sharma, P.; Meixner, T.; Marshall, L. A.; McGuire, K. J.; Weiler, M.

    2009-12-01

    The field of hydrology encompasses a wide range of departments and disciplines, ranging from civil engineering to geography to geosciences. As a consequence, in-class hydrology education is often strongly biased towards the background of a single instructor, limiting the educational experience of the students and not allowing for a holistic approach to hydrology education. Recently established, the Modular Curriculum for Hydrologic Advancement (MOCHA) creates an online community of hydrologists from a range of backgrounds and disciplines to define the boundaries of an unbiased hydrology education and to jointly develop resources to overcome previous instructional limitations (http://www.mocha.psu.edu/). Our first objective is to create an evolving core curriculum for hydrology education freely available to, developed, evolved and reviewed by the worldwide hydrologic community. On a larger scale, we hope to raise the standard of hydrology education and to foster international collaboration and exchange. Our work began with an initial survey including over 100 hydrology educators to assess the state of current hydrology education. Based on the survey results, the MOCHA project was designed and implemented, and initial teaching material and pedagogical guidelines for good practice in teaching were prepared. This past fall and spring, we piloted the website and teaching material across several universities. The web-based MOCHA project has recently been opened to solicit contributions from the global hydrology community. Our presentation will focus on the overall vision behind MOCHA, lessons learned from our initial piloting, and current steps to achieve our vision.

  19. Opportunities and challenges for extended-range predictions of tropical cyclone impacts on hydrological predictions

    NASA Astrophysics Data System (ADS)

    Tsai, Hsiao-Chung; Elsberry, Russell L.

    2013-12-01

    SummaryAn opportunity exists to extend support to the decision-making processes of water resource management and hydrological operations by providing extended-range tropical cyclone (TC) formation and track forecasts in the western North Pacific from the 51-member ECMWF 32-day ensemble. A new objective verification technique demonstrates that the ECMWF ensemble can predict most of the formations and tracks of the TCs during July 2009 to December 2010, even for most of the tropical depressions. Due to the relatively large number of false-alarm TCs in the ECMWF ensemble forecasts that would cause problems for support of hydrological operations, characteristics of these false alarms are discussed. Special attention is given to the ability of the ECMWF ensemble to predict periods of no-TCs in the Taiwan area, since water resource management decisions also depend on the absence of typhoon-related rainfall. A three-tier approach is proposed to provide support for hydrological operations via extended-range forecasts twice weekly on the 30-day timescale, twice-daily on the 15-day timescale, and up to four times a day with a consensus of high-resolution deterministic models.

  20. Nonlinear Prediction Model for Hydrologic Time Series Based on Wavelet Decomposition

    NASA Astrophysics Data System (ADS)

    Kwon, H.; Khalil, A.; Brown, C.; Lall, U.; Ahn, H.; Moon, Y.

    2005-12-01

    Traditionally forecasting and characterizations of hydrologic systems is performed utilizing many techniques. Stochastic linear methods such as AR and ARIMA and nonlinear ones such as statistical learning theory based tools have been extensively used. The common difficulty to all methods is the determination of sufficient and necessary information and predictors for a successful prediction. Relationships between hydrologic variables are often highly nonlinear and interrelated across the temporal scale. A new hybrid approach is proposed for the simulation of hydrologic time series combining both the wavelet transform and the nonlinear model. The present model employs some merits of wavelet transform and nonlinear time series model. The Wavelet Transform is adopted to decompose a hydrologic nonlinear process into a set of mono-component signals, which are simulated by nonlinear model. The hybrid methodology is formulated in a manner to improve the accuracy of a long term forecasting. The proposed hybrid model yields much better results in terms of capturing and reproducing the time-frequency properties of the system at hand. Prediction results are promising when compared to traditional univariate time series models. An application of the plausibility of the proposed methodology is provided and the results conclude that wavelet based time series model can be utilized for simulating and forecasting of hydrologic variable reasonably well. This will ultimately serve the purpose of integrated water resources planning and management.

  1. Benchmarking hydrological model predictive capability for UK River flows and flood peaks.

    NASA Astrophysics Data System (ADS)

    Lane, Rosanna; Coxon, Gemma; Freer, Jim; Wagener, Thorsten

    2017-04-01

    Data and hydrological models are now available for national hydrological analyses. However, hydrological model performance varies between catchments, and lumped, conceptual models are not able to produce adequate simulations everywhere. This study aims to benchmark hydrological model performance for catchments across the United Kingdom within an uncertainty analysis framework. We have applied four hydrological models from the FUSE framework to 1128 catchments across the UK. These models are all lumped models and run at a daily timestep, but differ in the model structural architecture and process parameterisations, therefore producing different but equally plausible simulations. We apply FUSE over a 20 year period from 1988-2008, within a GLUE Monte Carlo uncertainty analyses framework. Model performance was evaluated for each catchment, model structure and parameter set using standard performance metrics. These were calculated both for the whole time series and to assess seasonal differences in model performance. The GLUE uncertainty analysis framework was then applied to produce simulated 5th and 95th percentile uncertainty bounds for the daily flow time-series and additionally the annual maximum prediction bounds for each catchment. The results show that the model performance varies significantly in space and time depending on catchment characteristics including climate, geology and human impact. We identify regions where models are systematically failing to produce good results, and present reasons why this could be the case. We also identify regions or catchment characteristics where one model performs better than others, and have explored what structural component or parameterisation enables certain models to produce better simulations in these catchments. Model predictive capability was assessed for each catchment, through looking at the ability of the models to produce discharge prediction bounds which successfully bound the observed discharge. These results

  2. Predicting Epileptic Seizures in Advance

    PubMed Central

    Moghim, Negin; Corne, David W.

    2014-01-01

    Epilepsy is the second most common neurological disorder, affecting 0.6–0.8% of the world's population. In this neurological disorder, abnormal activity of the brain causes seizures, the nature of which tend to be sudden. Antiepileptic Drugs (AEDs) are used as long-term therapeutic solutions that control the condition. Of those treated with AEDs, 35% become resistant to medication. The unpredictable nature of seizures poses risks for the individual with epilepsy. It is clearly desirable to find more effective ways of preventing seizures for such patients. The automatic detection of oncoming seizures, before their actual onset, can facilitate timely intervention and hence minimize these risks. In addition, advance prediction of seizures can enrich our understanding of the epileptic brain. In this study, drawing on the body of work behind automatic seizure detection and prediction from digitised Invasive Electroencephalography (EEG) data, a prediction algorithm, ASPPR (Advance Seizure Prediction via Pre-ictal Relabeling), is described. ASPPR facilitates the learning of predictive models targeted at recognizing patterns in EEG activity that are in a specific time window in advance of a seizure. It then exploits advanced machine learning coupled with the design and selection of appropriate features from EEG signals. Results, from evaluating ASPPR independently on 21 different patients, suggest that seizures for many patients can be predicted up to 20 minutes in advance of their onset. Compared to benchmark performance represented by a mean S1-Score (harmonic mean of Sensitivity and Specificity) of 90.6% for predicting seizure onset between 0 and 5 minutes in advance, ASPPR achieves mean S1-Scores of: 96.30% for prediction between 1 and 6 minutes in advance, 96.13% for prediction between 8 and 13 minutes in advance, 94.5% for prediction between 14 and 19 minutes in advance, and 94.2% for prediction between 20 and 25 minutes in advance. PMID:24911316

  3. Seasonal Drought Prediction: Advances, Challenges, and Future Prospects

    NASA Astrophysics Data System (ADS)

    Hao, Zengchao; Singh, Vijay P.; Xia, Youlong

    2018-03-01

    Drought prediction is of critical importance to early warning for drought managements. This review provides a synthesis of drought prediction based on statistical, dynamical, and hybrid methods. Statistical drought prediction is achieved by modeling the relationship between drought indices of interest and a suite of potential predictors, including large-scale climate indices, local climate variables, and land initial conditions. Dynamical meteorological drought prediction relies on seasonal climate forecast from general circulation models (GCMs), which can be employed to drive hydrological models for agricultural and hydrological drought prediction with the predictability determined by both climate forcings and initial conditions. Challenges still exist in drought prediction at long lead time and under a changing environment resulting from natural and anthropogenic factors. Future research prospects to improve drought prediction include, but are not limited to, high-quality data assimilation, improved model development with key processes related to drought occurrence, optimal ensemble forecast to select or weight ensembles, and hybrid drought prediction to merge statistical and dynamical forecasts.

  4. Predicting Phosphorus Dynamics Across Physiographic Regions Using a Mixed Hortonian Non-Hortonian Hydrology Model

    NASA Astrophysics Data System (ADS)

    Collick, A.; Easton, Z. M.; Auerbach, D.; Buchanan, B.; Kleinman, P. J. A.; Fuka, D.

    2017-12-01

    Predicting phosphorus (P) loss from agricultural watersheds depends on accurate representation of the hydrological and chemical processes governing P mobility and transport. In complex landscapes, P predictions are complicated by a broad range of soils with and without restrictive layers, a wide variety of agricultural management, and variable hydrological drivers. The Soil and Water Assessment Tool (SWAT) is a watershed model commonly used to predict runoff and non-point source pollution transport, but is commonly only used with Hortonian (traditional SWAT) or non-Hortonian (SWAT-VSA) initializations. Many shallow soils underlain by a restricting layer commonly generate saturation excess runoff from variable source areas (VSA), which is well represented in a re-conceptualized version, SWAT-VSA. However, many watersheds exhibit traits of both infiltration excess and saturation excess hydrology internally, based on the hydrologic distance from the stream, distribution of soils across the landscape, and characteristics of restricting layers. The objective of this research is to provide an initial look at integrating distributed predictive capabilities that consider both Hortonian and Non-Hortonian solutions simultaneously within a single SWAT-VSA initialization. We compare results from all three conceptual watershed initializations against measured surface runoff and stream P loads and to highlight the model's ability to drive sub-field management of P. All three initializations predict discharge similarly well (daily Nash-Sutcliffe Efficiencies above 0.5), but the new conceptual SWAT-VSA initialization performed best in predicting P export from the watershed, while also identifying critical source areas - those areas generating large runoff and P losses at the sub field level. These results support the use of mixed Hortonian non-Hortonian SWAT-VSA initializations in predicting watershed-scale P losses and identifying critical source areas of P loss in landscapes

  5. How do I know if my forecasts are better? Using benchmarks in hydrological ensemble prediction

    NASA Astrophysics Data System (ADS)

    Pappenberger, F.; Ramos, M. H.; Cloke, H. L.; Wetterhall, F.; Alfieri, L.; Bogner, K.; Mueller, A.; Salamon, P.

    2015-03-01

    The skill of a forecast can be assessed by comparing the relative proximity of both the forecast and a benchmark to the observations. Example benchmarks include climatology or a naïve forecast. Hydrological ensemble prediction systems (HEPS) are currently transforming the hydrological forecasting environment but in this new field there is little information to guide researchers and operational forecasters on how benchmarks can be best used to evaluate their probabilistic forecasts. In this study, it is identified that the forecast skill calculated can vary depending on the benchmark selected and that the selection of a benchmark for determining forecasting system skill is sensitive to a number of hydrological and system factors. A benchmark intercomparison experiment is then undertaken using the continuous ranked probability score (CRPS), a reference forecasting system and a suite of 23 different methods to derive benchmarks. The benchmarks are assessed within the operational set-up of the European Flood Awareness System (EFAS) to determine those that are 'toughest to beat' and so give the most robust discrimination of forecast skill, particularly for the spatial average fields that EFAS relies upon. Evaluating against an observed discharge proxy the benchmark that has most utility for EFAS and avoids the most naïve skill across different hydrological situations is found to be meteorological persistency. This benchmark uses the latest meteorological observations of precipitation and temperature to drive the hydrological model. Hydrological long term average benchmarks, which are currently used in EFAS, are very easily beaten by the forecasting system and the use of these produces much naïve skill. When decomposed into seasons, the advanced meteorological benchmarks, which make use of meteorological observations from the past 20 years at the same calendar date, have the most skill discrimination. They are also good at discriminating skill in low flows and for all

  6. From catchment scale hydrologic processes to numerical models and robust predictions of climate change impacts at regional scales

    NASA Astrophysics Data System (ADS)

    Wagener, T.

    2017-12-01

    Current societal problems and questions demand that we increasingly build hydrologic models for regional or even continental scale assessment of global change impacts. Such models offer new opportunities for scientific advancement, for example by enabling comparative hydrology or connectivity studies, and for improved support of water management decision, since we might better understand regional impacts on water resources from large scale phenomena such as droughts. On the other hand, we are faced with epistemic uncertainties when we move up in scale. The term epistemic uncertainty describes those uncertainties that are not well determined by historical observations. This lack of determination can be because the future is not like the past (e.g. due to climate change), because the historical data is unreliable (e.g. because it is imperfectly recorded from proxies or missing), or because it is scarce (either because measurements are not available at the right scale or there is no observation network available at all). In this talk I will explore: (1) how we might build a bridge between what we have learned about catchment scale processes and hydrologic model development and evaluation at larger scales. (2) How we can understand the impact of epistemic uncertainty in large scale hydrologic models. And (3) how we might utilize large scale hydrologic predictions to understand climate change impacts, e.g. on infectious disease risk.

  7. Toward seamless hydrologic predictions across spatial scales

    NASA Astrophysics Data System (ADS)

    Samaniego, Luis; Kumar, Rohini; Thober, Stephan; Rakovec, Oldrich; Zink, Matthias; Wanders, Niko; Eisner, Stephanie; Müller Schmied, Hannes; Sutanudjaja, Edwin H.; Warrach-Sagi, Kirsten; Attinger, Sabine

    2017-09-01

    Land surface and hydrologic models (LSMs/HMs) are used at diverse spatial resolutions ranging from catchment-scale (1-10 km) to global-scale (over 50 km) applications. Applying the same model structure at different spatial scales requires that the model estimates similar fluxes independent of the chosen resolution, i.e., fulfills a flux-matching condition across scales. An analysis of state-of-the-art LSMs and HMs reveals that most do not have consistent hydrologic parameter fields. Multiple experiments with the mHM, Noah-MP, PCR-GLOBWB, and WaterGAP models demonstrate the pitfalls of deficient parameterization practices currently used in most operational models, which are insufficient to satisfy the flux-matching condition. These examples demonstrate that J. Dooge's 1982 statement on the unsolved problem of parameterization in these models remains true. Based on a review of existing parameter regionalization techniques, we postulate that the multiscale parameter regionalization (MPR) technique offers a practical and robust method that provides consistent (seamless) parameter and flux fields across scales. Herein, we develop a general model protocol to describe how MPR can be applied to a particular model and present an example application using the PCR-GLOBWB model. Finally, we discuss potential advantages and limitations of MPR in obtaining the seamless prediction of hydrological fluxes and states across spatial scales.

  8. Developing predictive insight into changing water systems: use-inspired hydrologic science for the Anthropocene

    NASA Astrophysics Data System (ADS)

    Thompson, S. E.; Sivapalan, M.; Harman, C. J.; Srinivasan, V.; Hipsey, M. R.; Reed, P.; Montanari, A.; Blöschl, G.

    2013-06-01

    Globally, many different kinds of water resources management issues call for policy and infrastructure based responses. Yet responsible decision making about water resources management raises a fundamental challenge for hydrologists: making predictions about water resources on decadal-to-century long timescales. Obtaining insight into hydrologic futures over 100 yr timescales forces researchers to address internal and exogenous changes in the properties of hydrologic systems. To do this, new hydrologic research must identify, describe and model feedbacks between water and other changing, coupled environmental subsystems. These models must be constrained to yield useful insights, despite the many likely sources of uncertainty in their predictions. Chief among these uncertainties are the impacts of the increasing role of human intervention in the global water cycle - a defining challenge for hydrology in the Anthropocene. Here we present a research agenda that proposes a suite of strategies to address these challenges. The research agenda focuses on the development of co-evolutionary hydrologic modeling to explore coupling across systems, and to address the implications of this coupling on the long-time behavior of the coupled systems. Three research directions support the development of these models: hydrologic reconstruction, comparative hydrology and model-data learning. These strategies focus on understanding hydrologic processes and feedbacks over long timescales, across many locations, and through strategic coupling of observational and model data in specific systems. We highlight the value of use-inspired and team-based science that is motivated by real-world hydrologic problems but targets improvements in fundamental understanding to support decision-making and management.

  9. Stochastic Residual-Error Analysis For Estimating Hydrologic Model Predictive Uncertainty

    EPA Science Inventory

    A hybrid time series-nonparametric sampling approach, referred to herein as semiparametric, is presented for the estimation of model predictive uncertainty. The methodology is a two-step procedure whereby a distributed hydrologic model is first calibrated, then followed by brute ...

  10. Advancing Drought Understanding, Monitoring and Prediction

    NASA Technical Reports Server (NTRS)

    Mariotti, Annarita; Schubert, Siegfried D.; Mo, Kingtse; Peters-Lidard, Christa; Wood, Andy; Pulwarty, Roger; Huang, Jin; Barrie, Dan

    2013-01-01

    Having the capacity to monitor droughts in near-real time and providing accurate drought prediction from weeks to seasons in advance can greatly reduce the severity of social and economic damage caused by drought, a leading natural hazard for North America. The congressional mandate to establish the National Integrated Drought Information System (NIDIS; Public Law 109-430) in 2006 was a major impulse to develop, integrate, and provide drought information to meet the challenges posed by this hazard. Significant progress has been made on many fronts. On the research front, efforts by the broad scientific community have resulted in improved understanding of North American droughts and improved monitoring and forecasting tools. We now have a better understanding of the droughts of the twentieth century including the 1930s "Dust Bowl"; we have developed a broader array of tools and datasets that enhance the official North American Drought Monitor based on different methodologies such as state-of-the-art land surface modeling (e.g., the North American Land Data Assimilation System) and remote sensing (e.g., the evaporative stress index) to better characterize the occurrence and severity of drought in its multiple manifestations. In addition, we have new tools for drought prediction [including the new National Centers for Environmental Prediction (NCEP) Climate Forecast System, version 2, for operational prediction and an experimental National Multimodel Ensemble] and have explored diverse methodologies including ensemble hydrologic prediction approaches. Broad NIDIS-inspired progress is influencing the development of a Global Drought Information System (GDIS) under the auspices of the World Climate Research Program. Despite these advances, current drought monitoring and forecasting capabilities still fall short of users' needs, especially the need for skillful and reliable drought forecasts at regional and local scales. To tackle this outstanding challenging problem

  11. A polynomial chaos ensemble hydrologic prediction system for efficient parameter inference and robust uncertainty assessment

    NASA Astrophysics Data System (ADS)

    Wang, S.; Huang, G. H.; Baetz, B. W.; Huang, W.

    2015-11-01

    This paper presents a polynomial chaos ensemble hydrologic prediction system (PCEHPS) for an efficient and robust uncertainty assessment of model parameters and predictions, in which possibilistic reasoning is infused into probabilistic parameter inference with simultaneous consideration of randomness and fuzziness. The PCEHPS is developed through a two-stage factorial polynomial chaos expansion (PCE) framework, which consists of an ensemble of PCEs to approximate the behavior of the hydrologic model, significantly speeding up the exhaustive sampling of the parameter space. Multiple hypothesis testing is then conducted to construct an ensemble of reduced-dimensionality PCEs with only the most influential terms, which is meaningful for achieving uncertainty reduction and further acceleration of parameter inference. The PCEHPS is applied to the Xiangxi River watershed in China to demonstrate its validity and applicability. A detailed comparison between the HYMOD hydrologic model, the ensemble of PCEs, and the ensemble of reduced PCEs is performed in terms of accuracy and efficiency. Results reveal temporal and spatial variations in parameter sensitivities due to the dynamic behavior of hydrologic systems, and the effects (magnitude and direction) of parametric interactions depending on different hydrological metrics. The case study demonstrates that the PCEHPS is capable not only of capturing both expert knowledge and probabilistic information in the calibration process, but also of implementing an acceleration of more than 10 times faster than the hydrologic model without compromising the predictive accuracy.

  12. Predicting changes in hydrologic retention in an evolving semi-arid alluvial stream

    USGS Publications Warehouse

    Harvey, J.W.; Conklin, M.H.; Koelsch, R.S.

    2003-01-01

    Hydrologic retention of solutes in hyporheic zones or other slowly moving waters of natural channels is thought to be a significant control on biogeochemical cycling and ecology of streams. To learn more about factors affecting hydrologic retention, we repeated stream-tracer injections for 5 years in a semi-arid alluvial stream (Pinal Creek, Ariz.) during a period when streamflow was decreasing, channel width increasing, and coverage of aquatic macrophytes expanding. Average stream velocity at Pinal Creek decreased from 0.8 to 0.2 m/s, average stream depth decreased from 0.09 to 0.04 m, and average channel width expanded from 3 to 13 m. Modeling of tracer experiments indicated that the hydrologic retention factor (Rh), a measure of the average time that solute spends in storage per unit length of downstream transport, increased from 0.02 to 8 s/m. At the same time the ratio of cross-sectional area of storage zones to main channel cross-sectional area (As/A) increased from 0.2 to 0.8 m2/m2, and average water residence time in storage zones (ts) increased from 5 to 24 min. Compared with published data from four other streams in the US, Pinal Creek experienced the greatest change in hydrologic retention for a given change in streamflow. The other streams differed from Pinal Creek in that they experienced a change in streamflow between tracer experiments without substantial geomorphic or vegetative adjustments. As a result, a regression of hydrologic retention on streamflow developed for the other streams underpredicted the measured increases in hydrologic retention at Pinal Creek. The increase in hydrologic retention at Pinal Creek was more accurately predicted when measurements of the Darcy-Weisbach friction factor were used (either alone or in addition to streamflow) as a predictor variable. We conclude that relatively simple measurements of channel friction are useful for predicting the response of hydrologic retention in streams to major adjustments in channel

  13. The state of the art of flood forecasting - Hydrological Ensemble Prediction Systems

    NASA Astrophysics Data System (ADS)

    Thielen-Del Pozo, J.; Pappenberger, F.; Salamon, P.; Bogner, K.; Burek, P.; de Roo, A.

    2010-09-01

    Flood forecasting systems form a key part of ‘preparedness' strategies for disastrous floods and provide hydrological services, civil protection authorities and the public with information of upcoming events. Provided the warning leadtime is sufficiently long, adequate preparatory actions can be taken to efficiently reduce the impacts of the flooding. Because of the specific characteristics of each catchment, varying data availability and end-user demands, the design of the best flood forecasting system may differ from catchment to catchment. However, despite the differences in concept and data needs, there is one underlying issue that spans across all systems. There has been an growing awareness and acceptance that uncertainty is a fundamental issue of flood forecasting and needs to be dealt with at the different spatial and temporal scales as well as the different stages of the flood generating processes. Today, operational flood forecasting centres change increasingly from single deterministic forecasts to probabilistic forecasts with various representations of the different contributions of uncertainty. The move towards these so-called Hydrological Ensemble Prediction Systems (HEPS) in flood forecasting represents the state of the art in forecasting science, following on the success of the use of ensembles for weather forecasting (Buizza et al., 2005) and paralleling the move towards ensemble forecasting in other related disciplines such as climate change predictions. The use of HEPS has been internationally fostered by initiatives such as "The Hydrologic Ensemble Prediction Experiment" (HEPEX), created with the aim to investigate how best to produce, communicate and use hydrologic ensemble forecasts in hydrological short-, medium- und long term prediction of hydrological processes. The advantages of quantifying the different contributions of uncertainty as well as the overall uncertainty to obtain reliable and useful flood forecasts also for extreme events

  14. Developing predictive insight into changing water systems: use-inspired hydrologic science for the Anthropocene

    NASA Astrophysics Data System (ADS)

    Thompson, S. E.; Sivapalan, M.; Harman, C. J.; Srinivasan, V.; Hipsey, M. R.; Reed, P.; Montanari, A.; Blöschl, G.

    2013-12-01

    Globally, many different kinds of water resources management issues call for policy- and infrastructure-based responses. Yet responsible decision-making about water resources management raises a fundamental challenge for hydrologists: making predictions about water resources on decadal- to century-long timescales. Obtaining insight into hydrologic futures over 100 yr timescales forces researchers to address internal and exogenous changes in the properties of hydrologic systems. To do this, new hydrologic research must identify, describe and model feedbacks between water and other changing, coupled environmental subsystems. These models must be constrained to yield useful insights, despite the many likely sources of uncertainty in their predictions. Chief among these uncertainties are the impacts of the increasing role of human intervention in the global water cycle - a defining challenge for hydrology in the Anthropocene. Here we present a research agenda that proposes a suite of strategies to address these challenges from the perspectives of hydrologic science research. The research agenda focuses on the development of co-evolutionary hydrologic modeling to explore coupling across systems, and to address the implications of this coupling on the long-time behavior of the coupled systems. Three research directions support the development of these models: hydrologic reconstruction, comparative hydrology and model-data learning. These strategies focus on understanding hydrologic processes and feedbacks over long timescales, across many locations, and through strategic coupling of observational and model data in specific systems. We highlight the value of use-inspired and team-based science that is motivated by real-world hydrologic problems but targets improvements in fundamental understanding to support decision-making and management. Fully realizing the potential of this approach will ultimately require detailed integration of social science and physical science

  15. A First Look at Decadal Hydrological Predictability by Land Surface Ensemble Simulations

    NASA Astrophysics Data System (ADS)

    Yuan, Xing; Zhu, Enda

    2018-03-01

    The prediction of terrestrial hydrology at the decadal scale is critical for managing water resources in the face of climate change. Here we conducted an assessment by global land model simulations following the design of the fifth Coupled Model Intercomparison Project (CMIP5) decadal 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 decadal 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 Decadal Oscillation and Atlantic Multidecadal Oscillation indices. This study provides a first look at decadal hydrological predictability, with an improved skill when incorporating low-frequency climate information.

  16. Impact of different satellite soil moisture products on the predictions of a continuous distributed hydrological model

    NASA Astrophysics Data System (ADS)

    Laiolo, P.; Gabellani, S.; Campo, L.; Silvestro, F.; Delogu, F.; Rudari, R.; Pulvirenti, L.; Boni, G.; Fascetti, F.; Pierdicca, N.; Crapolicchio, R.; Hasenauer, S.; Puca, S.

    2016-06-01

    The reliable estimation of hydrological variables in space and time is of fundamental importance in operational hydrology to improve the flood predictions and hydrological cycle description. Nowadays remotely sensed data can offer a chance to improve hydrological models especially in environments with scarce ground based data. The aim of this work is to update the state variables of a physically based, distributed and continuous hydrological model using four different satellite-derived data (three soil moisture products and a land surface temperature measurement) and one soil moisture analysis to evaluate, even with a non optimal technique, the impact on the hydrological cycle. The experiments were carried out for a small catchment, in the northern part of Italy, for the period July 2012-June 2013. The products were pre-processed according to their own characteristics and then they were assimilated into the model using a simple nudging technique. The benefits on the model predictions of discharge were tested against observations. The analysis showed a general improvement of the model discharge predictions, even with a simple assimilation technique, for all the assimilation experiments; the Nash-Sutcliffe model efficiency coefficient was increased from 0.6 (relative to the model without assimilation) to 0.7, moreover, errors on discharge were reduced up to the 10%. An added value to the model was found in the rainfall season (autumn): all the assimilation experiments reduced the errors up to the 20%. This demonstrated that discharge prediction of a distributed hydrological model, which works at fine scale resolution in a small basin, can be improved with the assimilation of coarse-scale satellite-derived data.

  17. Predictive Models of the Hydrological Regime of Unregulated Streams in Arizona

    USGS Publications Warehouse

    Anning, David W.; Parker, John T.C.

    2009-01-01

    Three statistical models were developed by the U.S. Geological Survey in cooperation with the Arizona Department of Environmental Quality to improve the predictability of flow occurrence in unregulated streams throughout Arizona. The models can be used to predict the probabilities of the hydrological regime being one of four categories developed by this investigation: perennial, which has streamflow year-round; nearly perennial, which has streamflow 90 to 99.9 percent of the year; weakly perennial, which has streamflow 80 to 90 percent of the year; or nonperennial, which has streamflow less than 80 percent of the year. The models were developed to assist the Arizona Department of Environmental Quality in selecting sites for participation in the U.S. Environmental Protection Agency's Environmental Monitoring and Assessment Program. One model was developed for each of the three hydrologic provinces in Arizona - the Plateau Uplands, the Central Highlands, and the Basin and Range Lowlands. The models for predicting the hydrological regime were calibrated using statistical methods and explanatory variables of discharge, drainage-area, altitude, and location data for selected U.S. Geological Survey streamflow-gaging stations and a climate index derived from annual precipitation data. Models were calibrated on the basis of streamflow data from 46 stations for the Plateau Uplands province, 82 stations for the Central Highlands province, and 90 stations for the Basin and Range Lowlands province. The models were developed using classification trees that facilitated the analysis of mixed numeric and factor variables. In all three models, a threshold stream discharge was the initial variable to be considered within the classification tree and was the single most important explanatory variable. If a stream discharge value at a station was below the threshold, then the station record was determined as being nonperennial. If, however, the stream discharge was above the threshold

  18. Getting the right answers for the right reasons: Linking measurements, analyses, and models to advance the science of hydrology

    NASA Astrophysics Data System (ADS)

    Kirchner, James W.

    2006-03-01

    The science of hydrology is on the threshold of major advances, driven by new hydrologic measurements, new methods for analyzing hydrologic data, and new approaches to modeling hydrologic systems. Here I suggest several promising directions forward, including (1) designing new data networks, field observations, and field experiments, with explicit recognition of the spatial and temporal heterogeneity of hydrologic processes, (2) replacing linear, additive "black box" models with "gray box" approaches that better capture the nonlinear and non-additive character of hydrologic systems, (3) developing physically based governing equations for hydrologic behavior at the catchment or hillslope scale, recognizing that they may look different from the equations that describe the small-scale physics, (4) developing models that are minimally parameterized and therefore stand some chance of failing the tests that they are subjected to, and (5) developing ways to test models more comprehensively and incisively. I argue that scientific progress will mostly be achieved through the collision of theory and data, rather than through increasingly elaborate and parameter-rich models that may succeed as mathematical marionettes, dancing to match the calibration data even if their underlying premises are unrealistic. Thus advancing the science of hydrology will require not only developing theories that get the right answers but also testing whether they get the right answers for the right reasons.

  19. Advances in Canadian forest hydrology, 1995-1998

    NASA Astrophysics Data System (ADS)

    Buttle, J. M.; Creed, I. F.; Pomeroy, J. W.

    2000-06-01

    Approximately 42% of Canada is covered by forests, which in turn can be subdivided into nine distinct forest ecozones. Many forested ecozones are located in northern Canada, where cold winters and cool summers provide forest environments that are less well-understood than those in more temperate locations. A number of major developments in recent years have stressed the need for enhanced understanding of hydrological processes in these forest landscapes. These include an increased emphasis on sustainable forest management in Canada as well as major scientific initiatives (e.g. BOREAS) examining water, carbon and energy fluxes in forest ecosystems, with a particular focus on boreal and subarctic forests. Recent progress in our understanding of forest hydrology across Canada is reviewed. Studies of hydrological processes across the spectrum of forest ecozones are highlighted, as well as work on hydrological responses to forest disturbance and recovery. Links between studies of hydrological processes in Canada's forests and other fields of research are examined, with particular attention paid to ongoing efforts to model hydrological impacts and interactions with the climate, biogeochemistry, geomorphology and ecology of forested landscapes.

  20. Life history theory predicts fish assemblage response to hydrologic regimes.

    PubMed

    Mims, Meryl C; Olden, Julian D

    2012-01-01

    The hydrologic regime is regarded as the primary driver of freshwater ecosystems, structuring the physical habitat template, providing connectivity, framing biotic interactions, and ultimately selecting for specific life histories of aquatic organisms. In the present study, we tested ecological theory predicting directional relationships between major dimensions of the flow regime and life history composition of fish assemblages in perennial free-flowing rivers throughout the continental United States. Using long-term discharge records and fish trait and survey data for 109 stream locations, we found that 11 out of 18 relationships (61%) tested between the three life history strategies (opportunistic, periodic, and equilibrium) and six hydrologic metrics (two each describing flow variability, predictability, and seasonality) were statistically significant (P < or = 0.05) according to quantile regression. Our results largely support a priori hypotheses of relationships between specific flow indices and relative prevalence of fish life history strategies, with 82% of all significant relationships observed supporting predictions from life history theory. Specifically, we found that (1) opportunistic strategists were positively related to measures of flow variability and negatively related to predictability and seasonality, (2) periodic strategists were positively related to high flow seasonality and negatively related to variability, and (3) the equilibrium strategists were negatively related to flow variability and positively related to predictability. Our study provides important empirical evidence illustrating the value of using life history theory to understand both the patterns and processes by which fish assemblage structure is shaped by adaptation to natural regimes of variability, predictability, and seasonality of critical flow events over broad biogeographic scales.

  1. Use of hydrologic landscape classification to diagnose streamflow predictability in Oregon

    EPA Science Inventory

    We implement a spatially lumped rainfall-runoff model to predict daily streamflow at 88 catchments within Oregon, USA and analyze its performance within the context of Oregon Hydrologic Landscapes (OHL) classification. OHL classification is used to characterize the physio-climat...

  2. Copula Entropy coupled with Wavelet Neural Network Model for Hydrological Prediction

    NASA Astrophysics Data System (ADS)

    Wang, Yin; Yue, JiGuang; Liu, ShuGuang; Wang, Li

    2018-02-01

    Artificial Neural network(ANN) has been widely used in hydrological forecasting. in this paper an attempt has been made to find an alternative method for hydrological prediction by combining Copula Entropy(CE) with Wavelet Neural Network(WNN), CE theory permits to calculate mutual information(MI) to select Input variables which avoids the limitations of the traditional linear correlation(LCC) analysis. Wavelet analysis can provide the exact locality of any changes in the dynamical patterns of the sequence Coupled with ANN Strong non-linear fitting ability. WNN model was able to provide a good fit with the hydrological data. finally, the hybrid model(CE+WNN) have been applied to daily water level of Taihu Lake Basin, and compared with CE ANN, LCC WNN and LCC ANN. Results showed that the hybrid model produced better results in estimating the hydrograph properties than the latter models.

  3. Snow multivariable data assimilation for hydrological predictions in Alpine sites

    NASA Astrophysics Data System (ADS)

    Piazzi, Gaia; Thirel, Guillaume; Campo, Lorenzo; Gabellani, Simone; Stevenin, Hervè

    2017-04-01

    Snowpack dynamics (snow accumulation and ablation) strongly impacts on hydrological processes in Alpine areas. During the winter season the presence of snow cover (snow accumulation) reduces the drainage in the basin with a resulting lower watershed time of concentration in case of possible rainfall events. Moreover, the release of the significant water volume stored in winter (snowmelt) considerably contributes to the total discharge during the melting period. Therefore when modeling hydrological processes in snow-dominated catchments the quality of predictions deeply depends on how the model succeeds in catching snowpack dynamics. The integration of a hydrological model with a snow module allows improving predictions of river discharges. Besides the well-known modeling limitations (uncertainty in parameterizations; possible errors affecting both meteorological forcing data and initial conditions; approximations in boundary conditions), there are physical factors that make an exhaustive reconstruction of snow dynamics complicated: snow intermittence in space and time, stratification and slow phenomena like metamorphism processes, uncertainty in snowfall evaluation, wind transportation, etc. Data Assimilation (DA) techniques provide an objective methodology to combine several independent snow-related data sources (model simulations, ground-based measurements and remote sensed observations) in order to obtain the most likely estimate of snowpack state. This study presents SMASH (Snow Multidata Assimilation System for Hydrology), a multi-layer snow dynamic model strengthened by a multivariable DA framework for hydrological purposes. The model is physically based on mass and energy balances and can be used to reproduce the main physical processes occurring within the snowpack: accumulation, density dynamics, melting, sublimation, radiative balance, heat and mass exchanges. The model is driven by observed forcing meteorological data (air temperature, wind velocity

  4. A framework for human-hydrologic system model development integrating hydrology and water management: application to the Cutzamala water system in Mexico

    NASA Astrophysics Data System (ADS)

    Wi, S.; Freeman, S.; Brown, C.

    2017-12-01

    This study presents a general approach to developing computational models of human-hydrologic systems where human modification of hydrologic surface processes are significant or dominant. A river basin system is represented by a network of human-hydrologic response units (HHRUs) identified based on locations where river regulations happen (e.g., reservoir operation and diversions). Natural and human processes in HHRUs are simulated in a holistic framework that integrates component models representing rainfall-runoff, river routing, reservoir operation, flow diversion and water use processes. We illustrate the approach in a case study of the Cutzamala water system (CWS) in Mexico, a complex inter-basin water transfer system supplying the Mexico City Metropolitan Area (MCMA). The human-hydrologic system model for CWS (CUTZSIM) is evaluated in terms of streamflow and reservoir storages measured across the CWS and to water supplied for MCMA. The CUTZSIM improves the representation of hydrology and river-operation interaction and, in so doing, advances evaluation of system-wide water management consequences under altered climatic and demand regimes. The integrated modeling framework enables evaluation and simulation of model errors throughout the river basin, including errors in representation of the human component processes. Heretofore, model error evaluation, predictive error intervals and the resultant improved understanding have been limited to hydrologic processes. The general framework represents an initial step towards fuller understanding and prediction of the many and varied processes that determine the hydrologic fluxes and state variables in real river basins.

  5. Diagnosis of streamflow prediction skills in Oregon using Hydrologic Landscape Classification

    EPA Science Inventory

    A complete understanding of why rainfall-runoff models provide good streamflow predictions at catchments in some regions, but fail to do so in other regions, has still not been achieved. Here, we argue that a hydrologic classification system is a robust conceptual tool that is w...

  6. Extending data worth methods to select multiple observations targeting specific hydrological predictions of interest

    NASA Astrophysics Data System (ADS)

    Vilhelmsen, Troels N.; Ferré, Ty P. A.

    2016-04-01

    Hydrological models are often developed to forecasting future behavior in response due to natural or human induced changes in stresses affecting hydrologic systems. Commonly, these models are conceptualized and calibrated based on existing data/information about the hydrological conditions. However, most hydrologic systems lack sufficient data to constrain models with adequate certainty to support robust decision making. Therefore, a key element of a hydrologic study is the selection of additional data to improve model performance. Given the nature of hydrologic investigations, it is not practical to select data sequentially, i.e. to choose the next observation, collect it, refine the model, and then repeat the process. Rather, for timing and financial reasons, measurement campaigns include multiple wells or sampling points. There is a growing body of literature aimed at defining the expected data worth based on existing models. However, these are almost all limited to identifying single additional observations. In this study, we present a methodology for simultaneously selecting multiple potential new observations based on their expected ability to reduce the uncertainty of the forecasts of interest. This methodology is based on linear estimates of the predictive uncertainty, and it can be used to determine the optimal combinations of measurements (location and number) established to reduce the uncertainty of multiple predictions. The outcome of the analysis is an estimate of the optimal sampling locations; the optimal number of samples; as well as a probability map showing the locations within the investigated area that are most likely to provide useful information about the forecasting of interest.

  7. Hydrologic impacts of thawing permafrost—A review

    USGS Publications Warehouse

    Walvoord, Michelle Ann; Kurylyk, Barret L.

    2016-01-01

    Where present, permafrost exerts a primary control on water fluxes, flowpaths, and distribution. Climate warming and related drivers of soil thermal change are expected to modify the distribution of permafrost, leading to changing hydrologic conditions, including alterations in soil moisture, connectivity of inland waters, streamflow seasonality, and the partitioning of water stored above and below ground. The field of permafrost hydrology is undergoing rapid advancement with respect to multiscale observations, subsurface characterization, modeling, and integration with other disciplines. However, gaining predictive capability of the many interrelated consequences of climate change is a persistent challenge due to several factors. Observations of hydrologic change have been causally linked to permafrost thaw, but applications of process-based models needed to support and enhance the transferability of empirical linkages have often been restricted to generalized representations. Limitations stem from inadequate baseline permafrost and unfrozen hydrogeologic characterization, lack of historical data, and simplifications in structure and process representation needed to counter the high computational demands of cryohydrogeologic simulations. Further, due in part to the large degree of subsurface heterogeneity of permafrost landscapes and the nonuniformity in thaw patterns and rates, associations between various modes of permafrost thaw and hydrologic change are not readily scalable; even trajectories of change can differ. This review highlights promising advances in characterization and modeling of permafrost regions and presents ongoing research challenges toward projecting hydrologic and ecologic consequences of permafrost thaw at time and spatial scales that are useful to managers and researchers.

  8. Advances in Canadian forest hydrology, 1999-2003

    NASA Astrophysics Data System (ADS)

    Buttle, J. M.; Creed, I. F.; Moore, R. D.

    2005-01-01

    Understanding key hydrological processes and properties is critical to sustaining the ecological, economic, social and cultural roles of Canada's varied forest types. This review examines recent progress in studying the hydrology of Canada's forest landscapes. Work in some areas, such as snow interception, accumulation and melt under forest cover, has led to modelling tools that can be readily applied for operational purposes. Our understanding in other areas, such as the link between runoff-generating processes in different forest landscapes and hydrochemical fluxes to receiving waters, is much more tentative. The 1999-2003 period saw considerable research examining hydrological and biogeochemical responses to natural and anthropogenic disturbance of forest landscapes, spurred by major funding initiatives at the provincial and federal levels. This work has provided valuable insight; however, application of the findings beyond the experimental site is often restricted by such issues as a limited consideration of the background variability of hydrological systems, incomplete appreciation of hydrological aspects at the experiment planning stage, and experimental design problems that often bedevil studies of basin response to disturbance. Overcoming these constraints will require, among other things, continued support for long-term hydroecological monitoring programmes, the embedding of process measurement and modelling studies within these programmes, and greater responsiveness to the vagaries of policy directions related to Canada's forest resources. Progress in these and related areas will contribute greatly to the development of hydrological indicators of sustainable forest management in Canada. Copyright

  9. Hydrological analysis in R: Topmodel and beyond

    NASA Astrophysics Data System (ADS)

    Buytaert, W.; Reusser, D.

    2011-12-01

    R is quickly gaining popularity in the hydrological sciences community. The wide range of statistical and mathematical functionality makes it an excellent tool for data analysis, modelling and uncertainty analysis. Topmodel was one of the first hydrological models being implemented as an R package and distributed through R's own distribution network CRAN. This facilitated pre- and postprocessing of data such as parameter sampling, calculation of prediction bounds, and advanced visualisation. However, apart from these basic functionalities, the package did not use many of the more advanced features of the R environment, especially from R's object oriented functionality. With R's increasing expansion in arenas such as high performance computing, big data analysis, and cloud services, we revisit the topmodel package, and use it as an example of how to build and deploy the next generation of hydrological models. R provides a convenient environment and attractive features to build and couple hydrological - and in extension other environmental - models, to develop flexible and effective data assimilation strategies, and to take the model beyond the individual computer by linking into cloud services for both data provision and computing. However, in order to maximise the benefit of these approaches, it will be necessary to adopt standards and ontologies for model interaction and information exchange. Some of those are currently being developed, such as the OGC web processing standards, while other will need to be developed.

  10. Advances in variable selection methods II: Effect of variable selection method on classification of hydrologically similar watersheds in three Mid-Atlantic ecoregions

    EPA Science Inventory

    Hydrological flow predictions in ungauged and sparsely gauged watersheds use regionalization or classification of hydrologically similar watersheds to develop empirical relationships between hydrologic, climatic, and watershed variables. The watershed classifications may be based...

  11. Advancing reservoir operation description in physically based hydrological models

    NASA Astrophysics Data System (ADS)

    Anghileri, Daniela; Giudici, Federico; Castelletti, Andrea; Burlando, Paolo

    2016-04-01

    Last decades have seen significant advances in our capacity of characterizing and reproducing hydrological processes within physically based models. Yet, when the human component is considered (e.g. reservoirs, water distribution systems), the associated decisions are generally modeled with very simplistic rules, which might underperform in reproducing the actual operators' behaviour on a daily or sub-daily basis. For example, reservoir operations are usually described by a target-level rule curve, which represents the level that the reservoir should track during normal operating conditions. The associated release decision is determined by the current state of the reservoir relative to the rule curve. This modeling approach can reasonably reproduce the seasonal water volume shift due to reservoir operation. Still, it cannot capture more complex decision making processes in response, e.g., to the fluctuations of energy prices and demands, the temporal unavailability of power plants or varying amount of snow accumulated in the basin. In this work, we link a physically explicit hydrological model with detailed hydropower behavioural models describing the decision making process by the dam operator. In particular, we consider two categories of behavioural models: explicit or rule-based behavioural models, where reservoir operating rules are empirically inferred from observational data, and implicit or optimization based behavioural models, where, following a normative economic approach, the decision maker is represented as a rational agent maximising a utility function. We compare these two alternate modelling approaches on the real-world water system of Lake Como catchment in the Italian Alps. The water system is characterized by the presence of 18 artificial hydropower reservoirs generating almost 13% of the Italian hydropower production. Results show to which extent the hydrological regime in the catchment is affected by different behavioural models and reservoir

  12. ARCHES: Advancing Research & Capacity in Hydrologic Education and Science

    NASA Astrophysics Data System (ADS)

    Milewski, A.; Fryar, A. E.; Durham, M. C.; Schroeder, P.; Agouridis, C.; Hanley, C.; Rotz, R. R.

    2013-12-01

    Educating young scientists and building capacity on a global scale is pivotal towards better understanding and managing our water resources. Based on this premise the ARCHES (Advancing Research & Capacity in Hydrologic Education and Science) program has been established. This abstract provides an overview of the program, links to access information, and describes the activities and outcomes of student participants from the Middle East and North Africa. The ARCHES program (http://arches.wrrs.uga.edu) is an integrated hydrologic education approach using online courses, field programs, and various hands-on workshops. The program aims to enable young scientists to effectively perform the high level research that will ultimately improve quality of life, enhance science-based decision making, and facilitate collaboration. Three broad, interlinked sets of activities are incorporated into the ARCHES program: (A1) the development of technical expertise, (A2) the development of professional contacts and skills, and (A3) outreach and long-term sustainability. The development of technical expertise (A1) is implemented through three progressive instructional sections. Section 1: Students were guided through a series of online lectures and exercises (Moodle: http://wrrs.uga.edu/moodle) covering three main topics (Remote Sensing, GIS, and Hydrologic Modeling). Section 2: Students participated in a hands-on workshop hosted at the University of Georgia's Water Resources and Remote Sensing Laboratory (WRRSL). Using ENVI, ArcGIS, and ArcSWAT, students completed a series of lectures and real-world applications (e.g., Development of Hydrologic Models). Section 3: Students participated in field studies (e.g., measurements of infiltration, recharge, streamflow, and water-quality parameters) conducted by U.S. partners and international collaborators in the participating countries. The development of professional contacts and skills (A2) was achieved through the promotion of networking

  13. Hydrology

    NASA Astrophysics Data System (ADS)

    Brutsaert, Wilfried

    2005-08-01

    Water in its different forms has always been a source of wonder, curiosity and practical concern for humans everywhere. Hydrology - An Introduction presents a coherent introduction to the fundamental principles of hydrology, based on the course that Wilfried Brutsaert has taught at Cornell University for the last thirty years. Hydrologic phenomena are dealt with at spatial and temporal scales at which they occur in nature. The physics and mathematics necessary to describe these phenomena are introduced and developed, and readers will require a working knowledge of calculus and basic fluid mechanics. The book will be invaluable as a textbook for entry-level courses in hydrology directed at advanced seniors and graduate students in physical science and engineering. In addition, the book will be more broadly of interest to professional scientists and engineers in hydrology, environmental science, meteorology, agronomy, geology, climatology, oceanology, glaciology and other earth sciences. Emphasis on fundamentals Clarification of the underlying physical processes Applications of fluid mechanics in the natural environment

  14. Timing and Prediction of Climate Change and Hydrological Impacts: Periodicity in Natural Variations

    EPA Science Inventory

    Hydrological impacts from climate change are of principal interest to water resource policy-makers and practicing engineers, and predictive climatic models have been extensively investigated to quantify the impacts. In palaeoclmatic investigations, climate proxy evidence has une...

  15. Satellite-derived potential evapotranspiration for distributed hydrologic runoff modeling

    NASA Astrophysics Data System (ADS)

    Spies, R. R.; Franz, K. J.; Bowman, A.; Hogue, T. S.; Kim, J.

    2012-12-01

    Distributed models have the ability of incorporating spatially variable data, especially high resolution forcing inputs such as precipitation, temperature and evapotranspiration in hydrologic modeling. Use of distributed hydrologic models for operational streamflow prediction has been partially hindered by a lack of readily available, spatially explicit input observations. Potential evapotranspiration (PET), for example, is currently accounted for through PET input grids that are based on monthly climatological values. The goal of this study is to assess the use of satellite-based PET estimates that represent the temporal and spatial variability, as input to the National Weather Service (NWS) Hydrology Laboratory Research Distributed Hydrologic Model (HL-RDHM). Daily PET grids are generated for six watersheds in the upper Mississippi River basin using a method that applies only MODIS satellite-based observations and the Priestly Taylor formula (MODIS-PET). The use of MODIS-PET grids will be tested against the use of the current climatological PET grids for simulating basin discharge. Gridded surface temperature forcing data are derived by applying the inverse distance weighting spatial prediction method to point-based station observations from the Automated Surface Observing System (ASOS) and Automated Weather Observing System (AWOS). Precipitation data are obtained from the Climate Prediction Center's (CPC) Climatology-Calibrated Precipitation Analysis (CCPA). A-priori gridded parameters for the Sacramento Soil Moisture Accounting Model (SAC-SMA), Snow-17 model, and routing model are initially obtained from the Office of Hydrologic Development and further calibrated using an automated approach. The potential of the MODIS-PET to be used in an operational distributed modeling system will be assessed with the long-term goal of promoting research to operations transfers and advancing the science of hydrologic forecasting.

  16. Water Cycle Dynamics in a Changing Environment: Advancing Hydrologic Science through Synthesis

    NASA Astrophysics Data System (ADS)

    Sivapalan, M.; Kumar, P.; Rhoads, B. L.; Wuebbles, D.

    2007-12-01

    As one ponders a changing environment -- climate, hydrology, land use, biogeochemical cycles, human dynamics -- there is an increasing need to understand the long term evolution of the linked component systems (e.g., climatic, hydrologic and ecological) through conceptual and quantitative models. The most challenging problem toward this goal is to understand and incorporate the rich dynamics of multiple linked systems with weak and strong coupling, and with many internal variables that exhibit multi-scale interactions. The richness of these interactions leads to fluctuations in one variable that in turn drive the dynamics of other related variables. The key question then becomes: Do these complexities lend an inherently stochastic character to the system, rendering deterministic prediction and modeling of limited value, or do they translate into constrained self- organization through which emerges order, and a limited group of "active" processes (that may change from time to time) that determine the general evolution of the system through a series of structured states with a distinct signature? This is a grand challenge for predictability and therefore requires community effort. The interconnectivity and hence synthesis of knowledge across the fields should be natural for hydrologists since the global water cycle and its regional manifestations directly correspond to the information flows for mass and energy transformations across the media, and across the disciplines. Further, the rich history of numerical, conceptual and stochastic modeling in hydrology provides the training and breadth for addressing the multi- scale, complex system dynamics challenges posed by the evolution question. Theory and observational analyses that necessitate stepping back from the existing knowledge paradigms and looking at the integrated system are needed. In this talk we will present the outlines of a new NSF-funded community effort that attempts to forge inter- disciplinary

  17. Impact of vegetation dynamics on hydrological processes in a semi-arid basin by using a land surface-hydrology coupled model

    NASA Astrophysics Data System (ADS)

    Jiao, Yang; Lei, Huimin; Yang, Dawen; Huang, Maoyi; Liu, Dengfeng; Yuan, Xing

    2017-08-01

    Land surface models (LSMs) are widely used to understand the interactions between hydrological processes and vegetation dynamics, which is important for the attribution and prediction of regional hydrological variations. However, most LSMs have large uncertainties in their representations of eco-hydrological processes due to deficiencies in hydrological parameterizations. In this study, the Community Land Model version 4 (CLM4) LSM was modified with an advanced runoff generation and flow routing scheme, resulting in a new land surface-hydrology coupled model, CLM-GBHM. Both models were implemented in the Wudinghe River Basin (WRB), which is a semi-arid basin located in the middle reaches of the Yellow River, China. Compared with CLM, CLM-GBHM increased the Nash Sutcliffe efficiency for daily river discharge simulation (1965-1969) from -0.03 to 0.23 and reduced the relative bias in water table depth simulations (2010-2012) from 32.4% to 13.4%. The CLM-GBHM simulations with static, remotely sensed and model-predicted vegetation conditions showed that the vegetation in the WRB began to recover in the 2000s due to the Grain for Green Program but had not reached the same level of vegetation cover as regions in natural eco-hydrological equilibrium. Compared with a simulation using remotely sensed vegetation cover, the simulation with a dynamic vegetation model that considers only climate-induced change showed a 10.3% increase in evapotranspiration, a 47.8% decrease in runoff, and a 62.7% and 71.3% deceleration in changing trend of the outlet river discharge before and after the year 2000, respectively. This result suggests that both natural and anthropogenic factors should be incorporated in dynamic vegetation models to better simulate the eco-hydrological cycle.

  18. Improving hydrologic predictions of a catchment model via assimilation of surface soil moisture

    USDA-ARS?s Scientific Manuscript database

    This paper examines the potential for improving Soil and Water Assessment Tool (SWAT) hydrologic predictions within the 341 km2 Cobb Creek Watershed in southwestern Oklahoma through the assimilation of surface soil moisture observations using an Ensemble Kalman filter (EnKF). In a series of synthet...

  19. Performance of two predictive uncertainty estimation approaches for conceptual Rainfall-Runoff Model: Bayesian Joint Inference and Hydrologic Uncertainty Post-processing

    NASA Astrophysics Data System (ADS)

    Hernández-López, Mario R.; Romero-Cuéllar, Jonathan; Camilo Múnera-Estrada, Juan; Coccia, Gabriele; Francés, Félix

    2017-04-01

    It is noticeably important to emphasize the role of uncertainty particularly when the model forecasts are used to support decision-making and water management. This research compares two approaches for the evaluation of the predictive uncertainty in hydrological modeling. First approach is the Bayesian Joint Inference of hydrological and error models. Second approach is carried out through the Model Conditional Processor using the Truncated Normal Distribution in the transformed space. This comparison is focused on the predictive distribution reliability. The case study is applied to two basins included in the Model Parameter Estimation Experiment (MOPEX). These two basins, which have different hydrological complexity, are the French Broad River (North Carolina) and the Guadalupe River (Texas). The results indicate that generally, both approaches are able to provide similar predictive performances. However, the differences between them can arise in basins with complex hydrology (e.g. ephemeral basins). This is because obtained results with Bayesian Joint Inference are strongly dependent on the suitability of the hypothesized error model. Similarly, the results in the case of the Model Conditional Processor are mainly influenced by the selected model of tails or even by the selected full probability distribution model of the data in the real space, and by the definition of the Truncated Normal Distribution in the transformed space. In summary, the different hypotheses that the modeler choose on each of the two approaches are the main cause of the different results. This research also explores a proper combination of both methodologies which could be useful to achieve less biased hydrological parameter estimation. For this approach, firstly the predictive distribution is obtained through the Model Conditional Processor. Secondly, this predictive distribution is used to derive the corresponding additive error model which is employed for the hydrological parameter

  20. Hydrological model parameter dimensionality is a weak measure of prediction uncertainty

    NASA Astrophysics Data System (ADS)

    Pande, S.; Arkesteijn, L.; Savenije, H.; Bastidas, L. A.

    2015-04-01

    This paper shows that instability of hydrological system representation in response to different pieces of information and associated prediction uncertainty is a function of model complexity. After demonstrating the connection between unstable model representation and model complexity, complexity is analyzed in a step by step manner. This is done measuring differences between simulations of a model under different realizations of input forcings. Algorithms are then suggested to estimate model complexity. Model complexities of the two model structures, SAC-SMA (Sacramento Soil Moisture Accounting) and its simplified version SIXPAR (Six Parameter Model), are computed on resampled input data sets from basins that span across the continental US. The model complexities for SIXPAR are estimated for various parameter ranges. It is shown that complexity of SIXPAR increases with lower storage capacity and/or higher recession coefficients. Thus it is argued that a conceptually simple model structure, such as SIXPAR, can be more complex than an intuitively more complex model structure, such as SAC-SMA for certain parameter ranges. We therefore contend that magnitudes of feasible model parameters influence the complexity of the model selection problem just as parameter dimensionality (number of parameters) does and that parameter dimensionality is an incomplete indicator of stability of hydrological model selection and prediction problems.

  1. Impact of vegetation dynamics on hydrological processes in a semi-arid basin by using a land surface-hydrology coupled model

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

    Jiao, Yang; Lei, Huimin; Yang, Dawen

    Land surface models (LSMs) are widely used to understand the interactions between hydrological processes and vegetation dynamics, which is important for the attribution and prediction of regional hydrological variations. However, most LSMs have large uncertainties in their representations of ecohydrological processes due to deficiencies in hydrological parameterizations. In this study, the Community Land Model version 4 (CLM4) LSM was modified with an advanced runoff generation and flow routing scheme, resulting in a new land surface-hydrology coupled model, CLM-GBHM. Both models were implemented in the Wudinghe River Basin (WRB), which is a semi-arid basin located in the middle reaches of themore » Yellow River, China. Compared with CLM, CLM-GBHM increased the Nash Sutcliffe efficiency for daily river discharge simulation (1965–1969) from 0.03 to 0.23 and reduced the relative bias in water table depth simulations (2010–2012) from 32.4% to 13.4%. The CLM-GBHM simulations with static, remotely sensed and model-predicted vegetation conditions showed that the vegetation in the WRB began to recover in the 2000s due to the Grain for Green Program but had not reached the same level of vegetation cover as regions in natural eco-hydrological equilibrium. Compared with a simulation using remotely sensed vegetation cover, the simulation with a dynamic vegetation model that considers only climate-induced change showed a 10.3% increase in evapotranspiration, a 47.8% decrease in runoff, and a 62.7% and 71.3% deceleration in changing trend of the outlet river discharge before and after the year 2000, respectively. This result suggests that both natural and anthropogenic factors should be incorporated in dynamic vegetation models to better simulate the eco-hydrological cycle.« less

  2. Advancing Collaboration through Hydrologic Data and Model Sharing

    NASA Astrophysics Data System (ADS)

    Tarboton, D. G.; Idaszak, R.; Horsburgh, J. S.; Ames, D. P.; Goodall, J. L.; Band, L. E.; Merwade, V.; Couch, A.; Hooper, R. P.; Maidment, D. R.; Dash, P. K.; Stealey, M.; Yi, H.; Gan, T.; Castronova, A. M.; Miles, B.; Li, Z.; Morsy, M. M.

    2015-12-01

    HydroShare is an online, collaborative system for open sharing of hydrologic data, analytical tools, and models. It supports the sharing of and collaboration around "resources" which are defined primarily by standardized metadata, content data models for each resource type, and an overarching resource data model based on the Open Archives Initiative's Object Reuse and Exchange (OAI-ORE) standard and a hierarchical file packaging system called "BagIt". HydroShare expands the data sharing capability of the CUAHSI Hydrologic Information System by broadening the classes of data accommodated to include geospatial and multidimensional space-time datasets commonly used in hydrology. HydroShare also includes new capability for sharing models, model components, and analytical tools and will take advantage of emerging social media functionality to enhance information about and collaboration around hydrologic data and models. It also supports web services and server/cloud based computation operating on resources for the execution of hydrologic models and analysis and visualization of hydrologic data. HydroShare uses iRODS as a network file system for underlying storage of datasets and models. Collaboration is enabled by casting datasets and models as "social objects". Social functions include both private and public sharing, formation of collaborative groups of users, and value-added annotation of shared datasets and models. The HydroShare web interface and social media functions were developed using the Django web application framework coupled to iRODS. Data visualization and analysis is supported through the Tethys Platform web GIS software stack. Links to external systems are supported by RESTful web service interfaces to HydroShare's content. This presentation will introduce the HydroShare functionality developed to date and describe ongoing development of functionality to support collaboration and integration of data and models.

  3. Hydrological resiliency in the Western Boreal Plains: classification of hydrological responses using wavelet analysis to assess landscape resilience

    NASA Astrophysics Data System (ADS)

    Probert, Samantha; Kettridge, Nicholas; Devito, Kevin; Hannah, David; Parkin, Geoff

    2017-04-01

    The Boreal represents a system of substantial resilience to climate change, with minimal ecological change over the past 6000 years. However, unprecedented climatic warming, coupled with catchment disturbances could exceed thresholds of hydrological function in the Western Boreal Plains. Knowledge of ecohydrological and climatic feedbacks that shape the resilience of boreal forests has advanced significantly in recent years, but this knowledge is yet to be applied and understood at landscape scales. Hydrological modelling at the landscape scale is challenging in the WBP due to diverse, non-topographically driven hydrology across the mosaic of terrestrial and aquatic ecosystems. This study functionally divides the geologic and ecological components of the landscape into Hydrologic Response Areas (HRAs) and wetland, forestland, interface and pond Hydrologic Units (HUs) to accurately characterise water storage and infer transmission at multiple spatial and temporal scales. Wavelet analysis is applied to pond and groundwater levels to describe the patterns of water storage in response to climate signals; to isolate dominant controls on hydrological responses and to assess the relative importance of physical controls between wet and dry climates. This identifies which components of the landscape exhibit greater magnitude and frequency of variability to wetting and drying trends, further to testing the hierarchical framework for hydrological storage controls of: climate, bedrock geology, surficial geology, soil, vegetation, and topography. Classifying HRA and HU hydrological function is essential to understand and predict water storage and redistribution through drought cycles and wet periods. This work recognises which landscape components are most sensitive under climate change and disturbance and also creates scope for hydrological resiliency research in Boreal systems by recognising critical landscape components and their role in landscape collapse or catastrophic

  4. Regional frameworks applied to hydrology: can landscape-based frameworks capture the hydrologic variability?

    Treesearch

    R. McManamay; D. Orth; C. Dolloff; E. Frimpong

    2011-01-01

    Regional frameworks have been used extensively in recent years to aid in broad-scale management. Widely used landscape-based regional frameworks, such as hydrologic landscape regions (HLRs) and physiographic provinces, may provide predictive tools of hydrologic variability. However, hydrologic-based regional frameworks, created using only streamflow data, are also...

  5. Understanding, management and modelling of urban hydrology and its consequences for receiving waters: A state of the art

    NASA Astrophysics Data System (ADS)

    Fletcher, T. D.; Andrieu, H.; Hamel, P.

    2013-01-01

    Urban hydrology has evolved to improve the way urban runoff is managed for flood protection, public health and environmental protection. There have been significant recent advances in the measurement and prediction of urban rainfall, with technologies such as radar and microwave networks showing promise. The ability to predict urban hydrology has also evolved, to deliver models suited to the small temporal and spatial scales typical of urban and peri-urban applications. Urban stormwater management increasingly consider the needs of receiving environments as well as those of humans. There is a clear trend towards approaches that attempt to restore pre-development flow-regimes and water quality, with an increasing recognition that restoring a more natural water balance benefits not only the environment, but enhances the liveability of the urban landscape. Once regarded only as a nuisance, stormwater is now increasingly regarded as a resource. Despite the advances, many important challenges in urban hydrology remain. Further research into the spatio-temporal dynamics of urban rainfall is required to improve short-term rainfall prediction. The performance of stormwater technologies in restoring the water balance and in removing emerging priority pollutants remain poorly quantified. All of these challenges are overlaid by the uncertainty of climate change, which imposes a requirement to ensure that stormwater management systems are adaptable and resilient to changes. Urban hydrology will play a critical role in addressing these challenges.

  6. Communication of uncertainty in hydrological predictions: a user-driven example web service for Europe

    NASA Astrophysics Data System (ADS)

    Fry, Matt; Smith, Katie; Sheffield, Justin; Watts, Glenn; Wood, Eric; Cooper, Jon; Prudhomme, Christel; Rees, Gwyn

    2017-04-01

    Water is fundamental to society as it impacts on all facets of life, the economy and the environment. But whilst it creates opportunities for growth and life, it can also cause serious damages to society and infrastructure through extreme hydro-meteorological events such as floods or droughts. Anticipation of future water availability and extreme event risks would both help optimise growth and limit damage through better preparedness and planning, hence providing huge societal benefits. Recent scientific research advances make it now possible to provide hydrological outlooks at monthly to seasonal lead time, and future projections up to the end of the century accounting for climatic changes. However, high uncertainty remains in the predictions, which varies depending on location, time of the year, prediction range and hydrological variable. It is essential that this uncertainty is fully understood by decision makers so they can account for it in their planning. Hence, the challenge is to finds ways to communicate such uncertainty for a range of stakeholders with different technical background and environmental science knowledge. The project EDgE (End-to end Demonstrator for improved decision making in the water sector for Europe) funded by the Copernicus programme (C3S) is a proof-of-concept project that develops a unique service to support decision making for the water sector at monthly to seasonal and to multi-decadal lead times. It is a mutual effort of co-production between hydrologists and environmental modellers, computer scientists and stakeholders representative of key decision makers in Europe for the water sector. This talk will present the iterative co-production process of a web service that serves the need of the user community. Through a series of Focus Group meetings in Spain, Norway and the UK, options for visualising the hydrological predictions and associated uncertainties are presented and discussed first as mock-up dash boards, off-line tools

  7. Hydrologic Predictions in the Anthropocene: Exploration with Co-evolutionary Socio-hydrologic Models

    NASA Astrophysics Data System (ADS)

    Sivapalan, Murugesu; Tian, Fuqiang; Liu, Dengfeng

    2013-04-01

    Socio-hydrology studies the co-evolution and self-organization of humans in the hydrologic landscape, which requires a thorough understanding of the complex interactions between humans and water. On the one hand, the nature of water availability greatly impacts the development of society. On the other hand, humans can significantly alter the spatio-temporal distribution of water and in this way provide feedback to the society itself. The human-water system functions underlying such complex human-water interactions are not well understood. Exploratory models with the appropriate level of simplification in any given area can be valuable to understand these functions and the self-organization associated with socio-hydrology. In this study, a simple coupled modeling framework for socio-hydrology co-evolution is developed, and is used to illustrate the explanatory power of such models. In the Tarim River, humans depend heavily on agricultural production (other industries can be ignored for a start), and the social processes can be described principally by two variables, i.e., irrigated-area and human population. The eco-hydrological processes are expressed in terms of area under natural vegetation and stream discharge. The study area is the middle and the lower reaches of the Tarim River, which is divided into two modeling units, i.e. middle reach and lower reach. In each modeling unit, four ordinary differential equations are used to simulate the dynamics of the hydrological system represented by stream discharge, ecological system represented by area under natural vegetation, the economic system represented by irrigated area under agriculture and social system represented by human population. The four dominant variables are coupled together by several internal variables. For example, the stream discharge is coupled to irrigated area by the colonization rate and mortality rate of the irrigated area in the middle reach and the irrigated area is coupled to stream

  8. Hypothesis testing in hydrology: Theory and practice

    NASA Astrophysics Data System (ADS)

    Kirchner, James; Pfister, Laurent

    2017-04-01

    Well-posed hypothesis tests have spurred major advances in hydrological theory. However, a random sample of recent research papers suggests that in hydrology, as in other fields, hypothesis formulation and testing rarely correspond to the idealized model of the scientific method. Practices such as "p-hacking" or "HARKing" (Hypothesizing After the Results are Known) are major obstacles to more rigorous hypothesis testing in hydrology, along with the well-known problem of confirmation bias - the tendency to value and trust confirmations more than refutations - among both researchers and reviewers. Hypothesis testing is not the only recipe for scientific progress, however: exploratory research, driven by innovations in measurement and observation, has also underlain many key advances. Further improvements in observation and measurement will be vital to both exploratory research and hypothesis testing, and thus to advancing the science of hydrology.

  9. Hydrological modelling in forested systems

    EPA Science Inventory

    This chapter provides a brief overview of forest hydrology modelling approaches for answering important global research and management questions. Many hundreds of hydrological models have been applied globally across multiple decades to represent and predict forest hydrological p...

  10. Arid Zone Hydrology

    USDA-ARS?s Scientific Manuscript database

    Arid zone hydrology encompasses a wide range of topics and hydro-meteorological and ecological characteristics. Although arid and semi-arid watersheds perform the same functions as those in humid environments, their hydrology and sediment transport characteristics cannot be readily predicted by inf...

  11. [Advance in researches on the effect of forest on hydrological process].

    PubMed

    Zhang, Zhiqiang; Yu, Xinxiao; Zhao, Yutao; Qin, Yongsheng

    2003-01-01

    According to the effects of forest on hydrological process, forest hydrology can be divided into three related aspects: experimental research on the effects of forest changing on hydrological process quantity and water quality; mechanism study on the effects of forest changing on hydrological cycle, and establishing and exploitating physical-based distributed forest hydrological model for resource management and engineering construction. Orientation experiment research can not only support the first-hand data for forest hydrological model, but also make clear the precipitation-runoff mechanisms. Research on runoff mechanisms can be valuable for the exploitation and improvement of physical based hydrological models. Moreover, the model can also improve the experimental and runoff mechanism researches. A review of above three aspects are summarized in this paper.

  12. Characterizing the utility of the TMPA real-time product for hydrologic predictions over global river basins across scales

    NASA Astrophysics Data System (ADS)

    Gao, H.; Zhang, S.; Nijssen, B.; Zhou, T.; Voisin, N.; Sheffield, J.; Lee, K.; Shukla, S.; Lettenmaier, D. P.

    2017-12-01

    Despite its errors and uncertainties, the Tropical Rainfall Measuring Mission (TRMM) Multi-satellite Precipitation Analysis real-time product (TMPA-RT) has been widely used for hydrological monitoring and forecasting due to its timely availability for real-time applications. To evaluate the utility of TMPA-RT in hydrologic predictions, many studies have compared modeled streamflows driven by TMPA-RT against gauge data. However, because of the limited availability of streamflow observations in data sparse regions, there is still a lack of comprehensive comparisons for TMPA-RT based hydrologic predictions at the global scale. Furthermore, it is expected that its skill is less optimal at the subbasin scale than the basin scale. In this study, we evaluate and characterize the utility of the TMPA-RT product over selected global river basins during the period of 1998 to 2015 using the TMPA research product (TMPA-RP) as a reference. The Variable Infiltration Capacity (VIC) model, which was calibrated and validated previously, is adopted to simulate streamflows driven by TMPA-RT and TMPA-RP, respectively. The objective of this study is to analyze the spatial and temporal characteristics of the hydrologic predictions by answering the following questions: (1) How do the precipitation errors associated with the TMPA-RT product transform into streamflow errors with respect to geographical and climatological characteristics? (2) How do streamflow errors vary across scales within a basin?

  13. Scaling, Similarity, and the Fourth Paradigm for Hydrology

    NASA Technical Reports Server (NTRS)

    Peters-Lidard, Christa D.; Clark, Martyn; Samaniego, Luis; Verhoest, Niko E. C.; van Emmerik, Tim; Uijlenhoet, Remko; Achieng, Kevin; Franz, Trenton E.; Woods, Ross

    2017-01-01

    In this synthesis paper addressing hydrologic scaling and similarity, we posit that roadblocks in the search for universal laws of hydrology are hindered by our focus on computational simulation (the third paradigm), and assert that it is time for hydrology to embrace a fourth paradigm of data-intensive science. Advances in information-based hydrologic science, coupled with an explosion of hydrologic data and advances in parameter estimation and modelling, have laid the foundation for a data-driven framework for scrutinizing hydrological scaling and similarity hypotheses. We summarize important scaling and similarity concepts (hypotheses) that require testing, describe a mutual information framework for testing these hypotheses, describe boundary condition, state flux, and parameter data requirements across scales to support testing these hypotheses, and discuss some challenges to overcome while pursuing the fourth hydrological paradigm. We call upon the hydrologic sciences community to develop a focused effort towards adopting the fourth paradigm and apply this to outstanding challenges in scaling and similarity.

  14. Hydrological Aspects of Weather Prediction and Flood Warnings: Report of the Ninth Prospectus Development Team of the U.S. Weather Research Program

    USGS Publications Warehouse

    Droegemeier, K.K.; Smith, J.D.; Businger, S.; Doswell, C.; Doyle, J.; Duffy, C.; Foufoula-Georgiou, E.; Graziano, T.; James, L.D.; Krajewski, V.; LeMone, M.; Lettenmaier, D.; Mass, C.; Pielke, R.; Ray, P.; Rutledge, S.; Schaake, J.; Zipser, E.

    2000-01-01

    Among the many natural disasters that disrupt human and industrial activity in the United States each year, including tornadoes, hurricanes, extreme temperatures, and lightning, floods are among the most devastating and rank second in the loss of life. Indeed, the societal impact of floods has increased during the past few years and shows no sign of abating. Although the scientific questions associated with flooding and its accurate prediction are many and complex, an unprecedented opportunity now exists - in light of new observational and computing systems and infrastructures, a much improved understanding of small-scale meteorological and hydrological processes, and the availability of sophisticated numerical models and data assimilation systems - to attack the flood forecasting problem in a comprehensive manner that will yield significant new scientific insights and corresponding practical benefits. The authors present herein a set of recommendations for advancing our understanding of floods via the creation of natural laboratories situated in a variety of local meteorological and hydrological settings. Emphasis is given to floods caused by convection and cold season events, fronts and extratropical cyclones, orographic forcing, and hurricanes and tropical cyclones following landfall. Although the particular research strategies applied within each laboratory setting will necessarily vary, all will share the following principal elements: (a) exploitation of those couplings important to flooding that exist between meteorological and hydrological processes and models; (b) innovative use of operational radars, research radars, satellites, and rain gauges to provide detailed spatial characterizations of precipitation fields and rates, along with the use of this information in hydrological models and for improving and validating microphysical algorithms in meteorological models; (c) comparisons of quantitative precipitation estimation algorithms from both research

  15. Hydrological Aspects of Weather Prediction and Flood Warnings: Report of the Ninth Prospectus Development Team of the U.S. Weather Research Program.

    NASA Astrophysics Data System (ADS)

    Droegemeier, K. K.; Smith, J. D.; Businger, S.; Doswell, C., III; Doyle, J.; Duffy, C.; Foufoula-Georgiou, E.; Graziano, T.; James, L. D.; Krajewski, V.; Lemone, M.; Lettenmaier, D.; Mass, C.; Pielke, R., Sr.; Ray, P.; Rutledge, S.; Schaake, J.; Zipser, E.

    2000-11-01

    Among the many natural disasters that disrupt human and industrial activity in the United States each year, including tornadoes, hurricanes, extreme temperatures, and lightning, floods are among the most devastating and rank second in the loss of life. Indeed, the societal impact of floods has increased during the past few years and shows no sign of abating. Although the scientific questions associated with flooding and its accurate prediction are many and complex, an unprecedented opportunity now exists-in light of new observational and computing systems and infrastructures, a much improved understanding of small-scale meteorological and hydrological processes, and the availability of sophisticated numerical models and data assimilation systems-to attack the flood forecasting problem in a comprehensive manner that will yield significant new scientific insights and corresponding practical benefits. The authors present herein a set of recommendations for advancing our understanding of floods via the creation of natural laboratories situated in a variety of local meteorological and hydrological settings. Emphasis is given to floods caused by convection and cold season events, fronts and extratropical cyclones, orographic forcing, and hurricanes and tropical cyclones following landfall. Although the particular research strategies applied within each laboratory setting will necessarily vary, all will share the following principal elements: (a) exploitation of those couplings important to flooding that exist between meteorological and hydrological processes and models; (b) innovative use of operational radars, research radars, satellites, and rain gauges to provide detailed spatial characterizations of precipitation fields and rates, along with the use of this information in hydrological models and for improving and validating microphysical algorithms in meteorological models; (c) comparisons of quantitative precipitation estimation algorithms from both research

  16. Quantitative predictions of streamflow variability in the Susquehanna River Basin

    NASA Astrophysics Data System (ADS)

    Alexander, R.; Boyer, E. W.; Leonard, L. N.; Duffy, C.; Schwarz, G. E.; Smith, R. A.

    2012-12-01

    Hydrologic researchers and water managers have increasingly sought an improved understanding of the major processes that control fluxes of water and solutes across diverse environmental settings and large spatial scales. Regional analyses of observed streamflow data have led to advances in our knowledge of relations among land use, climate, and streamflow, with methodologies ranging from statistical assessments of multiple monitoring sites to the regionalization of the parameters of catchment-scale mechanistic simulation models. However, gaps remain in our understanding of the best ways to transfer the knowledge of hydrologic response and governing processes among locations, including methods for regionalizing streamflow measurements and model predictions. We developed an approach to predict variations in streamflow using the SPARROW (SPAtially Referenced Regression On Watershed attributes) modeling infrastructure, with mechanistic functions, mass conservation constraints, and statistical estimation of regional and sub-regional parameters. We used the model to predict discharge in the Susquehanna River Basin (SRB) under varying hydrological regimes that are representative of contemporary flow conditions. The resulting basin-scale water balance describes mean monthly flows in stream reaches throughout the entire SRB (represented at a 1:100,000 scale using the National Hydrologic Data network), with water supply and demand components that are inclusive of a range of hydrologic, climatic, and cultural properties (e.g., precipitation, evapotranspiration, soil and groundwater storage, runoff, baseflow, water use). We compare alternative models of varying complexity that reflect differences in the number and types of explanatory variables and functional expressions as well as spatial and temporal variability in the model parameters. Statistical estimation of the models reveals the levels of complexity that can be uniquely identified, subject to the information content

  17. Critical Hydrologic and Atmospheric Measurements in Complex Alpine Regions

    NASA Astrophysics Data System (ADS)

    Parlange, M. B.; Bou-Zeid, E.; Barrenetxea, G.; Krichane, M.; Ingelrest, F.; Couach, O.; Luyet, V.; Vetterli, M.; Lehning, M.; Duffy, C.; Tobin, C.; Selker, J.; Kumar, M.

    2007-12-01

    The Alps are often referred to as the « Water Towers of Europe » and as such play an essential role in European water resources. The impact of climatic change is expected to be particularly pronounced in the Alps and the lack of detailed hydrologic field observations is problematic for predictions of hydrologic and hazard assessment. Advances in information technology and communications provide important possibilities to improve the situation with relatively few measurements. We will present sensorscope technology (arrays of wireless weather stations including soil moisture, pressure, and temperature) that has now been deployed at the Le Genepi and Grand St. Bernard pass. In addition, a Distributed Temperature Sensor array on the stream beds has been deployed and stream discharge monitored. The high spatial resolution data collected in these previously "ungaged" regions are used in conjunction with new generation hydrologic models. The framework as to what is possible today with sensor arrays and modeling in extreme mountain environments is discussed.

  18. A Local to National Scale Catchment Model Simulation Framework for Hydrological Predictions and Impact Assessments Under Uncertainty

    NASA Astrophysics Data System (ADS)

    Freer, Jim; Coxon, Gemma; Quinn, Niall; Dunne, Toby; Lane, Rosie; Bates, Paul; Wagener, Thorsten; Woods, Ross; Neal, Jeff; Howden, Nicholas; Musuuza, Jude

    2017-04-01

    There is a huge challenge in developing hydrological model structures that can be used for hypothesis testing, prediction, impact assessment and risk analyses over a wide range of spatial scales. There are many reasons why this is the case, from computational demands, to how we define and characterize different features and pathway connectivities in the landscape, that differ depending on the objectives of the study. However there is certainly a need more than ever to explore the trade-offs between the complexity of modelling applied (i.e. spatial discretization, levels of process representation, complexity of landscape representation) compared to the benefits realized in terms of predictive capability and robustness of these predictions during hydrological extremes and during change. Furthermore, there is a further balance, particularly associated with prediction uncertainties, in that it is not desirable to have modelling systems that are too complex compared to the observed data that would ever be available to apply them. This is particularly the case when models are applied to quantify national impact assessments, especially if these are based on validation assessments from smaller more detailed case studies. Therefore the hydrological community needs modelling tools and approaches that enable these trade-offs to be explored and to understand the level of representation needed in models to be 'fit-for-purpose' for a given application. This paper presents a catchment scale national modelling framework based on Dynamic-TOPMODEL specifically setup to fulfil these aims. A key component of the modelling framework is it's structural flexibility, as is the ability to assess model outputs using Monte Carlo simulation techniques. The model build has been automated to work at any spatial scale to the national scale, and within that to control the level of spatial discretisation and connectivity of locally accounted landscape elements in the form of hydrological response

  19. Debates—Hypothesis testing in hydrology: Pursuing certainty versus pursuing uberty

    NASA Astrophysics Data System (ADS)

    Baker, Victor R.

    2017-03-01

    Modern hydrology places nearly all its emphasis on science-as-knowledge, the hypotheses of which are increasingly expressed as physical models, whose predictions are tested by correspondence to quantitative data sets. Though arguably appropriate for applications of theory to engineering and applied science, the associated emphases on truth and degrees of certainty are not optimal for the productive and creative processes that facilitate the fundamental advancement of science as a process of discovery. The latter requires an investigative approach, where the goal is uberty, a kind of fruitfulness of inquiry, in which the abductive mode of inference adds to the much more commonly acknowledged modes of deduction and induction. The resulting world-directed approach to hydrology provides a valuable complement to the prevailing hypothesis- (theory-) directed paradigm.Plain Language SummaryThis commentary suggests that a world-directed, investigative approach to <span class="hlt">hydrology</span> may serve as a productive complement to the prevailing hypothesis- (theory-) directed, approaches. The emphasis of the former on discovery has the potential to be transformative for investigative <span class="hlt">hydrology</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20010000028','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20010000028"><span>A Primer In <span class="hlt">Advanced</span> Fatigue Life <span class="hlt">Prediction</span> Methods</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Halford, Gary R.</p> <p>2000-01-01</p> <p>Metal fatigue has plagued structural components for centuries, and it remains a critical durability issue in today's aerospace hardware. This is true despite vastly improved and <span class="hlt">advanced</span> materials, increased mechanistic understanding, and development of accurate structural analysis and <span class="hlt">advanced</span> fatigue life <span class="hlt">prediction</span> tools. Each <span class="hlt">advance</span> is quickly taken advantage of to produce safer, more reliable more cost effective, and better performing products. In other words, as the envelop is expanded, components are then designed to operate just as close to the newly expanded envelop as they were to the initial one. The problem is perennial. The economic importance of addressing structural durability issues early in the design process is emphasized. Tradeoffs with performance, cost, and legislated restrictions are pointed out. Several aspects of structural durability of <span class="hlt">advanced</span> systems, <span class="hlt">advanced</span> materials and <span class="hlt">advanced</span> fatigue life <span class="hlt">prediction</span> methods are presented. Specific items include the basic elements of durability analysis, conventional designs, barriers to be overcome for <span class="hlt">advanced</span> systems, high-temperature life <span class="hlt">prediction</span> for both creep-fatigue and thermomechanical fatigue, mean stress effects, multiaxial stress-strain states, and cumulative fatigue damage accumulation assessment.</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://www.ars.usda.gov/research/publications/publication/?seqNo115=338072','TEKTRAN'); return false;" href="http://www.ars.usda.gov/research/publications/publication/?seqNo115=338072"><span>The Rangeland <span class="hlt">Hydrology</span> and Erosion Model: A dynamic approach for <span class="hlt">predicting</span> soil loss on rangelands</span></a></p> <p><a target="_blank" href="https://www.ars.usda.gov/research/publications/find-a-publication/">USDA-ARS?s Scientific Manuscript database</a></p> <p></p> <p></p> <p>In this study we present the improved Rangeland <span class="hlt">Hydrology</span> and Erosion Model (RHEM V2.3), a process-based erosion <span class="hlt">prediction</span> tool specific for rangeland application. The article provides the mathematical formulation of the model and parameter estimation equations. Model performance is assessed agains...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFM.H51Q..03O','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFM.H51Q..03O"><span>Hyper-resolution <span class="hlt">hydrological</span> modeling: Completeness of Formulation, Appropriateness of Descritization, and Physical LImits of <span class="hlt">Predictability</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Ogden, F. L.</p> <p>2017-12-01</p> <p>HIgh performance computing and the widespread availabilities of geospatial physiographic and forcing datasets have enabled consideration of flood impact <span class="hlt">predictions</span> with longer lead times and more detailed spatial descriptions. We are now considering multi-hour flash flood forecast lead times at the subdivision level in so-called hydroblind regions away from the National Hydrography network. However, the computational demands of such models are high, necessitating a nested simulation approach. Research on hyper-resolution <span class="hlt">hydrologic</span> modeling over the past three decades have illustrated some fundamental limits on <span class="hlt">predictability</span> that are simultaneously related to runoff generation mechanism(s), antecedent conditions, rates and total amounts of precipitation, discretization of the model domain, and complexity or completeness of the model formulation. This latter point is an acknowledgement that in some ways <span class="hlt">hydrologic</span> understanding in key areas related to land use, land cover, tillage practices, seasonality, and biological effects has some glaring deficiencies. This presentation represents a review of what is known related to the interacting effects of precipitation amount, model spatial discretization, antecedent conditions, physiographic characteristics and model formulation completeness for runoff <span class="hlt">predictions</span>. These interactions define a region in multidimensional forcing, parameter and process space where there are in some cases clear limits on <span class="hlt">predictability</span>, and in other cases diminished uncertainty.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012EGUGA..14.6900L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012EGUGA..14.6900L"><span>Understanding seasonal variability of uncertainty in <span class="hlt">hydrological</span> <span class="hlt">prediction</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Li, M.; Wang, Q. J.</p> <p>2012-04-01</p> <p>Understanding uncertainty in <span class="hlt">hydrological</span> <span class="hlt">prediction</span> can be highly valuable for improving the reliability of streamflow <span class="hlt">prediction</span>. In this study, a monthly water balance model, WAPABA, in a Bayesian joint probability with error models are presented to investigate the seasonal dependency of <span class="hlt">prediction</span> error structure. A seasonal invariant error model, analogous to traditional time series analysis, uses constant parameters for model error and account for no seasonal variations. In contrast, a seasonal variant error model uses a different set of parameters for bias, variance and autocorrelation for each individual calendar month. Potential connection amongst model parameters from similar months is not considered within the seasonal variant model and could result in over-fitting and over-parameterization. A hierarchical error model further applies some distributional restrictions on model parameters within a Bayesian hierarchical framework. An iterative algorithm is implemented to expedite the maximum a posterior (MAP) estimation of a hierarchical error model. Three error models are applied to forecasting streamflow at a catchment in southeast Australia in a cross-validation analysis. This study also presents a number of statistical measures and graphical tools to compare the <span class="hlt">predictive</span> skills of different error models. From probability integral transform histograms and other diagnostic graphs, the hierarchical error model conforms better to reliability when compared to the seasonal invariant error model. The hierarchical error model also generally provides the most accurate mean <span class="hlt">prediction</span> in terms of the Nash-Sutcliffe model efficiency coefficient and the best probabilistic <span class="hlt">prediction</span> in terms of the continuous ranked probability score (CRPS). The model parameters of the seasonal variant error model are very sensitive to each cross validation, while the hierarchical error model produces much more robust and reliable model parameters. Furthermore, the result of the</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFM.H53B1683K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFM.H53B1683K"><span>Detecting Human <span class="hlt">Hydrologic</span> Alteration from Diversion Hydropower Requires Universal Flow <span class="hlt">Prediction</span> Tools: A Proposed Framework for Flow <span class="hlt">Prediction</span> in Poorly-gauged, Regulated Rivers</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Kibler, K. M.; Alipour, M.</p> <p>2016-12-01</p> <p>Achieving the universal energy access Sustainable Development Goal will require great investment in renewable energy infrastructure in the developing world. Much growth in the renewable sector will come from new hydropower projects, including small and diversion hydropower in remote and mountainous regions. Yet, human impacts to <span class="hlt">hydrological</span> systems from diversion hydropower are poorly described. Diversion hydropower is often implemented in ungauged rivers, thus detection of impact requires flow analysis tools suited to <span class="hlt">prediction</span> in poorly-gauged and human-altered catchments. We conduct a comprehensive analysis of <span class="hlt">hydrologic</span> alteration in 32 rivers developed with diversion hydropower in southwestern China. As flow data are sparse, we devise an approach for estimating streamflow during pre- and post-development periods, drawing upon a decade of research into <span class="hlt">prediction</span> in ungauged basins. We apply a rainfall-runoff model, parameterized and forced exclusively with global-scale data, in <span class="hlt">hydrologically</span>-similar gauged and ungauged catchments. Uncertain "soft" data are incorporated through fuzzy numbers and confidence-based weighting, and a multi-criteria objective function is applied to evaluate model performance. Testing indicates that the proposed framework returns superior performance (NSE = 0.77) as compared to models parameterized by rote calibration (NSE = 0.62). Confident that the models are providing `the right answer for the right reasons', our analysis of <span class="hlt">hydrologic</span> alteration based on simulated flows indicates statistically significant <span class="hlt">hydrologic</span> effects of diversion hydropower across many rivers. Mean annual flows, 7-day minimum and 7-day maximum flows decreased. Frequency and duration of flow exceeding Q25 decreased while duration of flows sustained below the Q75 increased substantially. Hydrograph rise and fall rates and flow constancy increased. The proposed methodology may be applied to improve diversion hydropower design in data-limited regions.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017EGUGA..19.8724N','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017EGUGA..19.8724N"><span>Towards improved <span class="hlt">hydrologic</span> <span class="hlt">predictions</span> using data assimilation techniques for water resource management at the continental scale</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Naz, Bibi; Kurtz, Wolfgang; Kollet, Stefan; Hendricks Franssen, Harrie-Jan; Sharples, Wendy; Görgen, Klaus; Keune, Jessica; Kulkarni, Ketan</p> <p>2017-04-01</p> <p>More accurate and reliable <span class="hlt">hydrologic</span> simulations are important for many applications such as water resource management, future water availability projections and <span class="hlt">predictions</span> of extreme events. However, simulation of spatial and temporal variations in the critical water budget components such as precipitation, snow, evaporation and runoff is highly uncertain, due to errors in e.g. model structure and inputs (<span class="hlt">hydrologic</span> parameters and forcings). In this study, we use data assimilation techniques to improve the <span class="hlt">predictability</span> of continental-scale water fluxes using in-situ measurements along with remotely sensed information to improve <span class="hlt">hydrologic</span> predications for water resource systems. The Community Land Model, version 3.5 (CLM) integrated with the Parallel Data Assimilation Framework (PDAF) was implemented at spatial resolution of 1/36 degree (3 km) over the European CORDEX domain. The modeling system was forced with a high-resolution reanalysis system COSMO-REA6 from Hans-Ertel Centre for Weather Research (HErZ) and ERA-Interim datasets for time period of 1994-2014. A series of data assimilation experiments were conducted to assess the efficiency of assimilation of various observations, such as river discharge data, remotely sensed soil moisture, terrestrial water storage and snow measurements into the CLM-PDAF at regional to continental scales. This setup not only allows to quantify uncertainties, but also improves streamflow <span class="hlt">predictions</span> by updating simultaneously model states and parameters utilizing observational information. The results from different regions, watershed sizes, spatial resolutions and timescales are compared and discussed in this study.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017EGUGA..19.7722P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017EGUGA..19.7722P"><span>What is the relative role of initial <span class="hlt">hydrological</span> conditions and meteorological forcing to the seasonal <span class="hlt">hydrological</span> forecasting skill? Analysis along Europe's hydro-climatic gradient</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Pechlivanidis, Ilias; Crochemore, Louise</p> <p>2017-04-01</p> <p>Recent <span class="hlt">advances</span> in understanding and forecasting of climate have led into skilful seasonal meteorological <span class="hlt">predictions</span>, which can consequently increase the confidence of <span class="hlt">hydrological</span> prognosis. The majority of seasonal impact modelling has commonly been conducted at only one or a limited number of basins limiting the potential to understand large systems. Nevertheless, there is a necessity to develop operational seasonal forecasting services at the pan-European scale, capable of addressing the end-user needs. The skill of such forecasting services is subject to a number of sources of uncertainty, i.e. model structure, parameters, and forcing input. In here, we complement the "deep" knowledge from basin based modelling by investigating the relative contributions of initial <span class="hlt">hydrological</span> conditions (IHCs) and meteorological forcing (MF) to the skill of a seasonal pan-European <span class="hlt">hydrological</span> forecasting system. We use the Ensemble Streamflow <span class="hlt">Prediction</span> (ESP) and reverse ESP (revESP) procedure to show a proxy of <span class="hlt">hydrological</span> forecasting uncertainty due to MF and IHC uncertainties respectively. We further calculate the critical lead time (CLT), as a proxy of the river memory, after which the importance of MFs surpasses the importance of IHCs. We analyze these results in the context of prevailing hydro-climatic conditions for about 35000 European basins. Both model state initialisation (level in surface water, i.e. reservoirs, lakes and wetlands, soil moisture, snow depth) and provision of climatology are based on forcing input derived from the WFDEI product for the period 1981-2010. The analysis shows that the contribution of ICs and MFs to the <span class="hlt">hydrological</span> forecasting skill varies considerably according to location, season and lead time. This analysis allows clustering of basins in which <span class="hlt">hydrological</span> forecasting skill may be improved by better estimation of IHCs, e.g. via data assimilation of in-situ and/or satellite observations; whereas in other basins skill improvement</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017EGUGA..1914367P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017EGUGA..1914367P"><span>Probabilistic <span class="hlt">hydrological</span> nowcasting using radar based nowcasting techniques and distributed <span class="hlt">hydrological</span> models: application in the Mediterranean area</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Poletti, Maria Laura; Pignone, Flavio; Rebora, Nicola; Silvestro, Francesco</p> <p>2017-04-01</p> <p>The exposure of the urban areas to flash-floods is particularly significant to Mediterranean coastal cities, generally densely-inhabited. Severe rainfall events often associated to intense and organized thunderstorms produced, during the last century, flash-floods and landslides causing serious damages to urban areas and in the worst events led to human losses. The temporal scale of these events has been observed strictly linked to the size of the catchments involved: in the Mediterranean area a great number of catchments that pass through coastal cities have a small drainage area (less than 100 km2) and a corresponding <span class="hlt">hydrologic</span> response timescale in the order of a few hours. A suitable nowcasting chain is essential for the on time forecast of this kind of events. In fact meteorological forecast systems are unable to <span class="hlt">predict</span> precipitation at the scale of these events, small both at spatial (few km) and temporal (hourly) scales. Nowcasting models, covering the time interval of the following two hours starting from the observation try to extend the <span class="hlt">predictability</span> limits of the forecasting models in support of real-time flood alert system operations. This work aims to present the use of <span class="hlt">hydrological</span> models coupled with nowcasting techniques. The nowcasting model PhaSt furnishes an ensemble of equi-probable future precipitation scenarios on time horizons of 1-3 h starting from the most recent radar observations. The coupling of the nowcasting model PhaSt with the <span class="hlt">hydrological</span> model Continuum allows to forecast the flood with a few hours in <span class="hlt">advance</span>. In this way it is possible to generate different discharge <span class="hlt">prediction</span> for the following hours and associated return period maps: these maps can be used as a support in the decisional process for the warning system.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013HESSD..10.6407H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013HESSD..10.6407H"><span>Darwinian <span class="hlt">hydrology</span>: can the methodology Charles Darwin pioneered help <span class="hlt">hydrologic</span> science?</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Harman, C.; Troch, P. A.</p> <p>2013-05-01</p> <p>There have been repeated calls for a Darwinian approach to <span class="hlt">hydrologic</span> science or for a synthesis of Darwinian and Newtonian approaches, to deepen understanding the <span class="hlt">hydrologic</span> system in the larger landscape context, and so develop a better basis for <span class="hlt">predictions</span> now and in an uncertain future. But what exactly makes a Darwinian approach to <span class="hlt">hydrology</span> "Darwinian"? While there have now been a number of discussions of Darwinian approaches, many referencing Harte (2002), the term is potentially a source of confusion while its connections to Darwin remain allusive rather than explicit. Here we discuss the methods that Charles Darwin pioneered to understand a variety of complex systems in terms of their historical processes of change. We suggest that the Darwinian approach to <span class="hlt">hydrology</span> follows his lead by focusing attention on the patterns of variation in populations, seeking hypotheses that explain these patterns in terms of the mechanisms and conditions that determine their historical development, using deduction and modeling to derive consequent hypotheses that follow from a proposed explanation, and critically testing these hypotheses against new observations. It is not sufficient to catalogue the patterns or <span class="hlt">predict</span> them statistically. Nor is it sufficient for the explanations to amount to a "just-so" story not subject to critical analysis. Darwin's theories linked present-day variation to mechanisms that operated over history, and could be independently test and falsified by comparing new observations to the <span class="hlt">predictions</span> of corollary hypotheses they generated. With a Darwinian framework in mind it is easy to see that a great deal of <span class="hlt">hydrologic</span> research has already been done that contributes to a Darwinian <span class="hlt">hydrology</span> - whether deliberately or not. The various heuristic methods that Darwin used to develop explanatory theories - extrapolating mechanisms, space for time substitution, and looking for signatures of history - have direct application in <span class="hlt">hydrologic</span> science. Some</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013HESSD..10.8875H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013HESSD..10.8875H"><span>Impact of modellers' decisions on <span class="hlt">hydrological</span> a priori <span class="hlt">predictions</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Holländer, H. M.; Bormann, H.; Blume, T.; Buytaert, W.; Chirico, G. B.; Exbrayat, J.-F.; Gustafsson, D.; Hölzel, H.; Krauße, T.; Kraft, P.; Stoll, S.; Blöschl, G.; Flühler, H.</p> <p>2013-07-01</p> <p>The purpose of this paper is to stimulate a re-thinking of how we, the catchment hydrologists, could become reliable forecasters. A group of catchment modellers <span class="hlt">predicted</span> the <span class="hlt">hydrological</span> response of a man-made 6 ha catchment in its initial phase (Chicken Creek) without having access to the observed records. They used conceptually different model families. Their modelling experience differed largely. The <span class="hlt">prediction</span> exercise was organized in three steps: (1) for the 1st <span class="hlt">prediction</span> modellers received a basic data set describing the internal structure of the catchment (somewhat more complete than usually available to a priori <span class="hlt">predictions</span> in ungauged catchments). They did not obtain time series of stream flow, soil moisture or groundwater response. (2) Before the 2nd improved <span class="hlt">prediction</span> they inspected the catchment on-site and attended a workshop where the modellers presented and discussed their first attempts. (3) For their improved 3rd <span class="hlt">prediction</span> they were offered additional data by charging them pro forma with the costs for obtaining this additional information. Holländer et al. (2009) discussed the range of <span class="hlt">predictions</span> obtained in step 1. Here, we detail the modeller's decisions in accounting for the various processes based on what they learned during the field visit (step 2) and add the final outcome of step 3 when the modellers made use of additional data. We document the <span class="hlt">prediction</span> progress as well as the learning process resulting from the availability of added information. For the 2nd and 3rd step, the progress in <span class="hlt">prediction</span> quality could be evaluated in relation to individual modelling experience and costs of added information. We learned (i) that soft information such as the modeller's system understanding is as important as the model itself (hard information), (ii) that the sequence of modelling steps matters (field visit, interactions between differently experienced experts, choice of model, selection of available data, and methods for parameter guessing</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017WRR....53.1792P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017WRR....53.1792P"><span>Debates—Hypothesis testing in <span class="hlt">hydrology</span>: Theory and practice</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Pfister, Laurent; Kirchner, James W.</p> <p>2017-03-01</p> <p>The basic structure of the scientific method—at least in its idealized form—is widely championed as a recipe for scientific progress, but the day-to-day practice may be different. Here, we explore the spectrum of current practice in hypothesis formulation and testing in <span class="hlt">hydrology</span>, based on a random sample of recent research papers. This analysis suggests that in <span class="hlt">hydrology</span>, as in other fields, hypothesis formulation and testing rarely correspond to the idealized model of the scientific method. Practices such as "p-hacking" or "HARKing" (Hypothesizing After the Results are Known) are major obstacles to more rigorous hypothesis testing in <span class="hlt">hydrology</span>, along with the well-known problem of confirmation bias—the tendency to value and trust confirmations more than refutations—among both researchers and reviewers. Nonetheless, as several examples illustrate, hypothesis tests have played an essential role in spurring major <span class="hlt">advances</span> in <span class="hlt">hydrological</span> theory. Hypothesis testing is not the only recipe for scientific progress, however. Exploratory research, driven by innovations in measurement and observation, has also underlain many key <span class="hlt">advances</span>. Further improvements in observation and measurement will be vital to both exploratory research and hypothesis testing, and thus to <span class="hlt">advancing</span> the science of <span class="hlt">hydrology</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2011HESSD...8.3743B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2011HESSD...8.3743B"><span><span class="hlt">Prediction</span> of future <span class="hlt">hydrological</span> regimes in poorly gauged high altitude basins: the case study of the upper Indus, Pakistan</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Bocchiola, D.; Diolaiuti, G.; Soncini, A.; Mihalcea, C.; D'Agata, C.; Mayer, C.; Lambrecht, A.; Rosso, R.; Smiraglia, C.</p> <p>2011-04-01</p> <p>In the mountain regions of the Hindu Kush, Karakoram and Himalaya (HKH) the "third polar ice cap" of our planet, glaciers play the role of "water towers" by providing significant amount of melt water, especially in the dry season, essential for agriculture, drinking purposes, and hydropower production. Recently, most glaciers in the HKH have been retreating and losing mass, mainly due to significant regional warming, thus calling for assessment of future water resources availability for populations down slope. However, <span class="hlt">hydrology</span> of these high altitude catchments is poorly studied and little understood. Most such catchments are poorly gauged, thus posing major issues in flow <span class="hlt">prediction</span> therein, and representing in facts typical grounds of application of PUB concepts, where simple and portable <span class="hlt">hydrological</span> modeling based upon scarce data amount is necessary for water budget estimation, and <span class="hlt">prediction</span> under climate change conditions. In this preliminarily study, future (2060) <span class="hlt">hydrological</span> flows in a particular watershed (Shigar river at Shigar, ca. 7000 km2), nested within the upper Indus basin and fed by seasonal melt from major glaciers, are investigated. The study is carried out under the umbrella of the SHARE-Paprika project, aiming at evaluating the impact of climate change upon <span class="hlt">hydrology</span> of the upper Indus river. We set up a minimal <span class="hlt">hydrological</span> model, tuned against a short series of observed ground climatic data from a number of stations in the area, in situ measured ice ablation data, and remotely sensed snow cover data. The future, locally adjusted, precipitation and temperature fields for the reference decade 2050-2059 from CCSM3 model, available within the IPCC's panel, are then fed to the <span class="hlt">hydrological</span> model. We adopt four different glaciers' cover scenarios, to test sensitivity to decreased glacierized areas. The projected flow duration curves, and some selected flow descriptors are evaluated. The uncertainty of the results is then addressed, and use of</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2011HESS...15.2059B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2011HESS...15.2059B"><span><span class="hlt">Prediction</span> of future <span class="hlt">hydrological</span> regimes in poorly gauged high altitude basins: the case study of the upper Indus, Pakistan</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Bocchiola, D.; Diolaiuti, G.; Soncini, A.; Mihalcea, C.; D'Agata, C.; Mayer, C.; Lambrecht, A.; Rosso, R.; Smiraglia, C.</p> <p>2011-07-01</p> <p>In the mountain regions of the Hindu Kush, Karakoram and Himalaya (HKH) the "third polar ice cap" of our planet, glaciers play the role of "water towers" by providing significant amount of melt water, especially in the dry season, essential for agriculture, drinking purposes, and hydropower production. Recently, most glaciers in the HKH have been retreating and losing mass, mainly due to significant regional warming, thus calling for assessment of future water resources availability for populations down slope. However, <span class="hlt">hydrology</span> of these high altitude catchments is poorly studied and little understood. Most such catchments are poorly gauged, thus posing major issues in flow <span class="hlt">prediction</span> therein, and representing in fact typical grounds of application of PUB concepts, where simple and portable <span class="hlt">hydrological</span> modeling based upon scarce data amount is necessary for water budget estimation, and <span class="hlt">prediction</span> under climate change conditions. In this preliminarily study, future (2060) <span class="hlt">hydrological</span> flows in a particular watershed (Shigar river at Shigar, ca. 7000 km2), nested within the upper Indus basin and fed by seasonal melt from major glaciers, are investigated. The study is carried out under the umbrella of the SHARE-Paprika project, aiming at evaluating the impact of climate change upon <span class="hlt">hydrology</span> of the upper Indus river. We set up a minimal <span class="hlt">hydrological</span> model, tuned against a short series of observed ground climatic data from a number of stations in the area, in situ measured ice ablation data, and remotely sensed snow cover data. The future, locally adjusted, precipitation and temperature fields for the reference decade 2050-2059 from CCSM3 model, available within the IPCC's panel, are then fed to the <span class="hlt">hydrological</span> model. We adopt four different glaciers' cover scenarios, to test sensitivity to decreased glacierized areas. The projected flow duration curves, and some selected flow descriptors are evaluated. The uncertainty of the results is then addressed, and use of the</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70029825','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70029825"><span>Enhancing water cycle measurements for future <span class="hlt">hydrologic</span> research</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Loescher, H.W.; Jacobs, J.M.; Wendroth, O.; Robinson, D.A.; Poulos, G.S.; McGuire, K.; Reed, P.; Mohanty, B.P.; Shanley, J.B.; Krajewski, W.</p> <p>2007-01-01</p> <p>The Consortium of Universities for the <span class="hlt">Advancement</span> of <span class="hlt">Hydrologic</span> Sciences, Inc., established the <span class="hlt">Hydrologic</span> Measurement Facility to transform watershed-scale <span class="hlt">hydrologic</span> research by facilitating access to <span class="hlt">advanced</span> instrumentation and expertise that would not otherwise be available to individual investigators. We outline a committee-based process that determined which suites of instrumentation best fit the needs of the <span class="hlt">hydrological</span> science community and a proposed mechanism for the governance and distribution of these sensors. Here, we also focus on how these proposed suites of instrumentation can be used to address key scientific challenges, including scaling water cycle science in time and space, broadening the scope of individual subdisciplines of water cycle science, and developing mechanistic linkages among these subdisciplines and spatio-temporal scales. ?? 2007 American Meteorological Society.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19820011758','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19820011758"><span>Agricultural soil moisture experiment, Colby, Kansas 1978: Measured and <span class="hlt">predicted</span> <span class="hlt">hydrological</span> properties of the soil</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Arya, L. M. (Principal Investigator)</p> <p>1980-01-01</p> <p><span class="hlt">Predictive</span> procedures for developing soil <span class="hlt">hydrologic</span> properties (i.e., relationships of soil water pressure and hydraulic conductivity to soil water content) are presented. Three models of the soil water pressure-water content relationship and one model of the hydraulic conductivity-water content relationship are discussed. Input requirements for the models are indicated, and computational procedures are outlined. Computed <span class="hlt">hydrologic</span> properties for Keith silt loam, a soil typer near Colby, Kansas, on which the 1978 Agricultural Soil Moisture Experiment was conducted, are presented. A comparison of computed results with experimental data in the dry range shows that analytical models utilizing a few basic hydrophysical parameters can produce satisfactory data for large-scale applications.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFM.H33H1666P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFM.H33H1666P"><span>Merging Station Observations with Large-Scale Gridded Data to Improve <span class="hlt">Hydrological</span> <span class="hlt">Predictions</span> over Chile</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Peng, L.; Sheffield, J.; Verbist, K. M. J.</p> <p>2016-12-01</p> <p><span class="hlt">Hydrological</span> <span class="hlt">predictions</span> at regional-to-global scales are often hampered by the lack of meteorological forcing data. The use of large-scale gridded meteorological data is able to overcome this limitation, but these data are subject to regional biases and unrealistic values at local scale. This is especially challenging in regions such as Chile, where climate exhibits high spatial heterogeneity as a result of long latitude span and dramatic elevation changes. However, regional station-based observational datasets are not fully exploited and have the potential of constraining biases and spatial patterns. This study aims at adjusting precipitation and temperature estimates from the Princeton University global meteorological forcing (PGF) gridded dataset to improve <span class="hlt">hydrological</span> simulations over Chile, by assimilating 982 gauges from the Dirección General de Aguas (DGA). To merge station data with the gridded dataset, we use a state-space estimation method to produce optimal gridded estimates, considering both the error of the station measurements and the gridded PGF product. The PGF daily precipitation, maximum and minimum temperature at 0.25° spatial resolution are adjusted for the period of 1979-2010. Precipitation and temperature gauges with long and continuous records (>70% temporal coverage) are selected, while the remaining stations are used for validation. The leave-one-out cross validation verifies the robustness of this data assimilation approach. The merged dataset is then used to force the Variable Infiltration Capacity (VIC) <span class="hlt">hydrological</span> model over Chile at daily time step which are compared to the observations of streamflow. Our initial results show that the station-merged PGF precipitation effectively captures drizzle and the spatial pattern of storms. Overall the merged dataset has significant improvements compared to the original PGF with reduced biases and stronger inter-annual variability. The invariant spatial pattern of errors between the station</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018HESS...22.1831S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018HESS...22.1831S"><span>Relative effects of statistical preprocessing and postprocessing on a regional <span class="hlt">hydrological</span> ensemble <span class="hlt">prediction</span> system</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Sharma, Sanjib; Siddique, Ridwan; Reed, Seann; Ahnert, Peter; Mendoza, Pablo; Mejia, Alfonso</p> <p>2018-03-01</p> <p>The relative roles of statistical weather preprocessing and streamflow postprocessing in <span class="hlt">hydrological</span> ensemble forecasting at short- to medium-range forecast lead times (day 1-7) are investigated. For this purpose, a regional <span class="hlt">hydrologic</span> ensemble <span class="hlt">prediction</span> system (RHEPS) is developed and implemented. The RHEPS is comprised of the following components: (i) hydrometeorological observations (multisensor precipitation estimates, gridded surface temperature, and gauged streamflow); (ii) weather ensemble forecasts (precipitation and near-surface temperature) from the National Centers for Environmental <span class="hlt">Prediction</span> 11-member Global Ensemble Forecast System Reforecast version 2 (GEFSRv2); (iii) NOAA's <span class="hlt">Hydrology</span> Laboratory-Research Distributed <span class="hlt">Hydrologic</span> Model (HL-RDHM); (iv) heteroscedastic censored logistic regression (HCLR) as the statistical preprocessor; (v) two statistical postprocessors, an autoregressive model with a single exogenous variable (ARX(1,1)) and quantile regression (QR); and (vi) a comprehensive verification strategy. To implement the RHEPS, 1 to 7 days weather forecasts from the GEFSRv2 are used to force HL-RDHM and generate raw ensemble streamflow forecasts. Forecasting experiments are conducted in four nested basins in the US Middle Atlantic region, ranging in size from 381 to 12 362 km2. Results show that the HCLR preprocessed ensemble precipitation forecasts have greater skill than the raw forecasts. These improvements are more noticeable in the warm season at the longer lead times (> 3 days). Both postprocessors, ARX(1,1) and QR, show gains in skill relative to the raw ensemble streamflow forecasts, particularly in the cool season, but QR outperforms ARX(1,1). The scenarios that implement preprocessing and postprocessing separately tend to perform similarly, although the postprocessing-alone scenario is often more effective. The scenario involving both preprocessing and postprocessing consistently outperforms the other scenarios. In some cases</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015AGUFMGC53B1205J','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015AGUFMGC53B1205J"><span>Comparison of global optimization approaches for robust calibration of <span class="hlt">hydrologic</span> model parameters</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Jung, I. W.</p> <p>2015-12-01</p> <p>Robustness of the calibrated parameters of <span class="hlt">hydrologic</span> models is necessary to provide a reliable <span class="hlt">prediction</span> of future performance of watershed behavior under varying climate conditions. This study investigated calibration performances according to the length of calibration period, objective functions, <span class="hlt">hydrologic</span> model structures and optimization methods. To do this, the combination of three global optimization methods (i.e. SCE-UA, Micro-GA, and DREAM) and four <span class="hlt">hydrologic</span> models (i.e. SAC-SMA, GR4J, HBV, and PRMS) was tested with different calibration periods and objective functions. Our results showed that three global optimization methods provided close calibration performances under different calibration periods, objective functions, and <span class="hlt">hydrologic</span> models. However, using the agreement of index, normalized root mean square error, Nash-Sutcliffe efficiency as the objective function showed better performance than using correlation coefficient and percent bias. Calibration performances according to different calibration periods from one year to seven years were hard to generalize because four <span class="hlt">hydrologic</span> models have different levels of complexity and different years have different information content of <span class="hlt">hydrological</span> observation. Acknowledgements This research was supported by a grant (14AWMP-B082564-01) from <span class="hlt">Advanced</span> Water Management Research Program funded by Ministry of Land, Infrastructure and Transport of Korean government.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015AGUFMNH31C..05E','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015AGUFMNH31C..05E"><span>Towards a <span class="hlt">Predictive</span> Theory of Malaria: Connections to Spatio-temporal Variability of Climate and <span class="hlt">Hydrology</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Endo, N.; Eltahir, E. A. B.</p> <p>2015-12-01</p> <p>Malaria transmission is closely linked to climatology, <span class="hlt">hydrology</span>, environment, and the biology of local vectors. These factors interact with each other and non-linearly influence malaria transmission dynamics, making <span class="hlt">prediction</span> and prevention challenging. Our work attempts to find a universality in the multi-dimensional system of malaria transmission and to develop a theory to <span class="hlt">predict</span> emergence of malaria given a limited set of environmental and biological inputs.A credible malaria transmission dynamics model, HYDREMATS (Bomblies et al., 2008), was used under hypothetical settings to investigate the role of spatial and temporal distribution of vector breeding pools. HYDREMATS is a mechanistic model and capable of simulating the basic reproduction rate (Ro) without bold assumptions even under dynamic conditions. The spatial distribution of pools is mainly governed by <span class="hlt">hydrological</span> factors; the impact of pool persistence and rainy season length on malaria transmission were investigated. Also analyzed was the impact of the temporal distribution of pools relative to human houses. We developed non-dimensional variables combining the <span class="hlt">hydrological</span> and biological parameters. Simulated values of Ro from HYDREMATS are presented in a newly-introduced non-dimensional plane, which leads to a some-what universal theory describing the condition for sustainable malaria transmission. The findings were tested against observations both from the West Africa and the Ethiopian Highland, representing diverse hydroclimatological conditions. Predicated Ro values from the theory over the two regions are in good agreement with the observed malaria transmission data.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70027139','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70027139"><span>Statistical procedures for evaluating daily and monthly <span class="hlt">hydrologic</span> model <span class="hlt">predictions</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>Coffey, M.E.; Workman, S.R.; Taraba, J.L.; Fogle, A.W.</p> <p>2004-01-01</p> <p>The overall study objective was to evaluate the applicability of different qualitative and quantitative methods for comparing daily and monthly SWAT computer model <span class="hlt">hydrologic</span> streamflow <span class="hlt">predictions</span> to observed data, and to recommend statistical methods for use in future model evaluations. Statistical methods were tested using daily streamflows and monthly equivalent runoff depths. The statistical techniques included linear regression, Nash-Sutcliffe efficiency, nonparametric tests, t-test, objective functions, autocorrelation, and cross-correlation. None of the methods specifically applied to the non-normal distribution and dependence between data points for the daily <span class="hlt">predicted</span> and observed data. Of the tested methods, median objective functions, sign test, autocorrelation, and cross-correlation were most applicable for the daily data. The robust coefficient of determination (CD*) and robust modeling efficiency (EF*) objective functions were the preferred methods for daily model results due to the ease of comparing these values with a fixed ideal reference value of one. <span class="hlt">Predicted</span> and observed monthly totals were more normally distributed, and there was less dependence between individual monthly totals than was observed for the corresponding <span class="hlt">predicted</span> and observed daily values. More statistical methods were available for comparing SWAT model-<span class="hlt">predicted</span> and observed monthly totals. The 1995 monthly SWAT model <span class="hlt">predictions</span> and observed data had a regression Rr2 of 0.70, a Nash-Sutcliffe efficiency of 0.41, and the t-test failed to reject the equal data means hypothesis. The Nash-Sutcliffe coefficient and the R r2 coefficient were the preferred methods for monthly results due to the ability to compare these coefficients to a set ideal value of one.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014HESS...18.2065H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014HESS...18.2065H"><span>Impact of modellers' decisions on <span class="hlt">hydrological</span> a priori <span class="hlt">predictions</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Holländer, H. M.; Bormann, H.; Blume, T.; Buytaert, W.; Chirico, G. B.; Exbrayat, J.-F.; Gustafsson, D.; Hölzel, H.; Krauße, T.; Kraft, P.; Stoll, S.; Blöschl, G.; Flühler, H.</p> <p>2014-06-01</p> <p>In practice, the catchment hydrologist is often confronted with the task of <span class="hlt">predicting</span> discharge without having the needed records for calibration. Here, we report the discharge <span class="hlt">predictions</span> of 10 modellers - using the model of their choice - for the man-made Chicken Creek catchment (6 ha, northeast Germany, Gerwin et al., 2009b) and we analyse how well they improved their <span class="hlt">prediction</span> in three steps based on adding information prior to each following step. The modellers <span class="hlt">predicted</span> the catchment's <span class="hlt">hydrological</span> response in its initial phase without having access to the observed records. They used conceptually different physically based models and their modelling experience differed largely. Hence, they encountered two problems: (i) to simulate discharge for an ungauged catchment and (ii) using models that were developed for catchments, which are not in a state of landscape transformation. The <span class="hlt">prediction</span> exercise was organized in three steps: (1) for the first <span class="hlt">prediction</span> the modellers received a basic data set describing the catchment to a degree somewhat more complete than usually available for a priori <span class="hlt">predictions</span> of ungauged catchments; they did not obtain information on stream flow, soil moisture, nor groundwater response and had therefore to guess the initial conditions; (2) before the second <span class="hlt">prediction</span> they inspected the catchment on-site and discussed their first <span class="hlt">prediction</span> attempt; (3) for their third <span class="hlt">prediction</span> they were offered additional data by charging them pro forma with the costs for obtaining this additional information. Holländer et al. (2009) discussed the range of <span class="hlt">predictions</span> obtained in step (1). Here, we detail the modeller's assumptions and decisions in accounting for the various processes. We document the <span class="hlt">prediction</span> progress as well as the learning process resulting from the availability of added information. For the second and third steps, the progress in <span class="hlt">prediction</span> quality is evaluated in relation to individual modelling experience and costs of</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_5");'>5</a></li> <li><a href="#" onclick='return showDiv("page_6");'>6</a></li> <li class="active"><span>7</span></li> <li><a href="#" onclick='return showDiv("page_8");'>8</a></li> <li><a href="#" onclick='return showDiv("page_9");'>9</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_7 --> <div id="page_8" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_6");'>6</a></li> <li><a href="#" onclick='return showDiv("page_7");'>7</a></li> <li class="active"><span>8</span></li> <li><a href="#" onclick='return showDiv("page_9");'>9</a></li> <li><a href="#" onclick='return showDiv("page_10");'>10</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="141"> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2005AGUFM.H34E..03W','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2005AGUFM.H34E..03W"><span>CLEANER-<span class="hlt">Hydrologic</span> Observatory Joint Science Plan</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Welty, C.; Dressler, K.; Hooper, R.</p> <p>2005-12-01</p> <p>The CLEANER-<span class="hlt">Hydrologic</span> Observatory* initiative is a distributed network for research on complex environmental systems that focuses on the intersecting water-related issues of both the CUAHSI and CLEANER communities. It emphasizes research on the nation's water resources related to human-dominated natural and built environments. The network will be comprised of: interacting field sites with an integrated cyberinfrastructure; a centralized technical resource staff and management infrastructure to support interdisciplinary research through data collection from <span class="hlt">advanced</span> sensor systems, data mining and aggregation from multiple sources and databases; cyber-tools for analysis, visualization, and <span class="hlt">predictive</span> multi-scale modeling that is dynamically driven. As such, the network will transform 21st century workforce development in the water-related intersection of environmental science and engineering, as well as enable substantial educational and engagement opportunities for all age levels. The scientific goal and strategic intent of the CLEANER-<span class="hlt">Hydrologic</span> Observatory Network is to transform our understanding of the earth's water cycle and associated biogeochemical cycles across spatial and temporal scales-enabling quantitative forecasts of critical water-related processes, especially those that affect and are affected by human activities. This strategy will develop scientific and engineering tools that will enable more effective adaptive approaches for resource management. The need for the network is based on three critical deficiencies in current abilities to understand large-scale environmental processes and thereby develop more effective management strategies. First we lack basic data and the infrastructure to collect them at the needed resolution. Second, we lack the means to integrate data across scales from different media (paper records, electronic worksheets, web-based) and sources (observations, experiments, simulations). Third, we lack sufficiently accurate</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.nws.noaa.gov/ohd/index.html','SCIGOVWS'); return false;" href="http://www.nws.noaa.gov/ohd/index.html"><span>National Weather Service - Office of <span class="hlt">Hydrologic</span> Development</span></a></p> <p><a target="_blank" href="http://www.science.gov/aboutsearch.html">Science.gov Websites</a></p> <p></p> <p></p> <p><span class="hlt">Prediction</span> System (CHPS) National <em>Water</em> Center NWS <span class="hlt">Hydrology</span> Science <em>Research</em> and Collaboration Strategic Storymap The Office of <span class="hlt">Hydrologic</span> Development reorganized into the Office of <em>Water</em> <span class="hlt">Prediction</span> with through the infusion of new science and technology. This service improves flood warnings and <em>water</em></p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/biblio/1049659-value-medium-range-weather-forecasts-improvement-seasonal-hydrologic-prediction-skill','SCIGOV-STC'); return false;" href="https://www.osti.gov/biblio/1049659-value-medium-range-weather-forecasts-improvement-seasonal-hydrologic-prediction-skill"><span>Value of medium range weather forecasts in the improvement of seasonal <span class="hlt">hydrologic</span> <span class="hlt">prediction</span> skill</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>Shukla, Shraddhanand; Voisin, Nathalie; Lettenmaier, D. P.</p> <p>2012-08-15</p> <p>We investigated the contribution of medium range weather forecasts with lead times up to 14 days to seasonal <span class="hlt">hydrologic</span> <span class="hlt">prediction</span> skill over the Conterminous United States (CONUS). Three different Ensemble Streamflow <span class="hlt">Prediction</span> (ESP)-based experiments were performed for the period 1980-2003 using the Variable Infiltration Capacity (VIC) <span class="hlt">hydrology</span> model to generate forecasts of monthly runoff and soil moisture (SM) at lead-1 (first month of the forecast period) to lead-3. The first experiment (ESP) used a resampling from the retrospective period 1980-2003 and represented full climatological uncertainty for the entire forecast period. In the second and third experiments, the first 14 daysmore » of each ESP ensemble member were replaced by either observations (perfect 14-day forecast) or by a deterministic 14-day weather forecast. We used Spearman rank correlations of forecasts and observations as the forecast skill score. We estimated the potential and actual improvement in baseline skill as the difference between the skill of experiments 2 and 3 relative to ESP, respectively. We found that useful runoff and SM forecast skill at lead-1 to -3 months can be obtained by exploiting medium range weather forecast skill in conjunction with the skill derived by the knowledge of initial <span class="hlt">hydrologic</span> conditions. Potential improvement in baseline skill by using medium range weather forecasts, for runoff (SM) forecasts generally varies from 0 to 0.8 (0 to 0.5) as measured by differences in correlations, with actual improvement generally from 0 to 0.8 of the potential improvement. With some exceptions, most of the improvement in runoff is for lead-1 forecasts, although some improvement in SM was achieved at lead-2.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.fs.usda.gov/treesearch/pubs/52877','TREESEARCH'); return false;" href="https://www.fs.usda.gov/treesearch/pubs/52877"><span>iTree-Hydro: Snow <span class="hlt">hydrology</span> update for the urban forest <span class="hlt">hydrology</span> model</span></a></p> <p><a target="_blank" href="http://www.fs.usda.gov/treesearch/">Treesearch</a></p> <p>Yang Yang; Theodore A. Endreny; David J. Nowak</p> <p>2011-01-01</p> <p>This article presents snow <span class="hlt">hydrology</span> updates made to iTree-Hydro, previously called the Urban Forest Effects—<span class="hlt">Hydrology</span> model. iTree-Hydro Version 1 was a warm climate model developed by the USDA Forest Service to provide a process-based planning tool with robust water quantity and quality <span class="hlt">predictions</span> given data limitations common to most urban areas. Cold climate...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018GeoRL..45..346B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018GeoRL..45..346B"><span>Improved Seasonal <span class="hlt">Prediction</span> of European Summer Temperatures With New Five-Layer Soil-<span class="hlt">Hydrology</span> Scheme</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Bunzel, Felix; Müller, Wolfgang A.; Dobrynin, Mikhail; Fröhlich, Kristina; Hagemann, Stefan; Pohlmann, Holger; Stacke, Tobias; Baehr, Johanna</p> <p>2018-01-01</p> <p>We evaluate the impact of a new five-layer soil-<span class="hlt">hydrology</span> scheme on seasonal hindcast skill of 2 m temperatures over Europe obtained with the Max Planck Institute Earth System Model (MPI-ESM). Assimilation experiments from 1981 to 2010 and 10-member seasonal hindcasts initialized on 1 May each year are performed with MPI-ESM in two soil configurations, one using a bucket scheme and one a new five-layer soil-<span class="hlt">hydrology</span> scheme. We find the seasonal hindcast skill for European summer temperatures to improve with the five-layer scheme compared to the bucket scheme and investigate possible causes for these improvements. First, improved indirect soil moisture assimilation allows for enhanced soil moisture-temperature feedbacks in the hindcasts. Additionally, this leads to improved <span class="hlt">prediction</span> of anomalies in the 500 hPa geopotential height surface, reflecting more realistic atmospheric circulation patterns over Europe.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017JHyd..548..484W','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017JHyd..548..484W"><span>Towards robust quantification and reduction of uncertainty in <span class="hlt">hydrologic</span> <span class="hlt">predictions</span>: Integration of particle Markov chain Monte Carlo and factorial polynomial chaos expansion</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Wang, S.; Huang, G. H.; Baetz, B. W.; Ancell, B. C.</p> <p>2017-05-01</p> <p>The particle filtering techniques have been receiving increasing attention from the <span class="hlt">hydrologic</span> community due to its ability to properly estimate model parameters and states of nonlinear and non-Gaussian systems. To facilitate a robust quantification of uncertainty in <span class="hlt">hydrologic</span> <span class="hlt">predictions</span>, it is necessary to explicitly examine the forward propagation and evolution of parameter uncertainties and their interactions that affect the <span class="hlt">predictive</span> performance. This paper presents a unified probabilistic framework that merges the strengths of particle Markov chain Monte Carlo (PMCMC) and factorial polynomial chaos expansion (FPCE) algorithms to robustly quantify and reduce uncertainties in <span class="hlt">hydrologic</span> <span class="hlt">predictions</span>. A Gaussian anamorphosis technique is used to establish a seamless bridge between the data assimilation using the PMCMC and the uncertainty propagation using the FPCE through a straightforward transformation of posterior distributions of model parameters. The unified probabilistic framework is applied to the Xiangxi River watershed of the Three Gorges Reservoir (TGR) region in China to demonstrate its validity and applicability. Results reveal that the degree of spatial variability of soil moisture capacity is the most identifiable model parameter with the fastest convergence through the streamflow assimilation process. The potential interaction between the spatial variability in soil moisture conditions and the maximum soil moisture capacity has the most significant effect on the performance of streamflow <span class="hlt">predictions</span>. In addition, parameter sensitivities and interactions vary in magnitude and direction over time due to temporal and spatial dynamics of <span class="hlt">hydrologic</span> processes.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017WRR....53.5204C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017WRR....53.5204C"><span>Celebrating <span class="hlt">hydrologic</span> science: The "Science is Essential" collection</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Clark, Martyn P.; Luce, Charles H.; van Meerveld, H. J. (Ilja)</p> <p>2017-07-01</p> <p>Water Resources Research published nine commentaries in the AGU "Science is Essential" collection. The goal of these papers is to celebrate the <span class="hlt">advances</span> in <span class="hlt">hydrologic</span> science, to show how <span class="hlt">hydrologic</span> science is essential for society, and to illustrate how <span class="hlt">hydrologic</span> science has influenced policies. Here we provide a brief introduction to these papers, to encourage you to explore them in full.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013ECSS..118...11S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013ECSS..118...11S"><span><span class="hlt">Predictive</span> occurrence models for coastal wetland plant communities: Delineating <span class="hlt">hydrologic</span> response surfaces with multinomial logistic regression</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Snedden, Gregg A.; Steyer, Gregory D.</p> <p>2013-02-01</p> <p>Understanding plant community zonation along estuarine stress gradients is critical for effective conservation and restoration of coastal wetland ecosystems. We related the presence of plant community types to estuarine <span class="hlt">hydrology</span> at 173 sites across coastal Louisiana. Percent relative cover by species was assessed at each site near the end of the growing season in 2008, and hourly water level and salinity were recorded at each site Oct 2007-Sep 2008. Nine plant community types were delineated with k-means clustering, and indicator species were identified for each of the community types with indicator species analysis. An inverse relation between salinity and species diversity was observed. Canonical correspondence analysis (CCA) effectively segregated the sites across ordination space by community type, and indicated that salinity and tidal amplitude were both important drivers of vegetation composition. Multinomial logistic regression (MLR) and Akaike's Information Criterion (AIC) were used to <span class="hlt">predict</span> the probability of occurrence of the nine vegetation communities as a function of salinity and tidal amplitude, and probability surfaces obtained from the MLR model corroborated the CCA results. The weighted kappa statistic, calculated from the confusion matrix of <span class="hlt">predicted</span> versus actual community types, was 0.7 and indicated good agreement between observed community types and model <span class="hlt">predictions</span>. Our results suggest that models based on a few key <span class="hlt">hydrologic</span> variables can be valuable tools for <span class="hlt">predicting</span> vegetation community development when restoring and managing coastal wetlands.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/28241378','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/28241378"><span>An experimental test of fitness variation across a <span class="hlt">hydrologic</span> gradient <span class="hlt">predicts</span> willow and poplar species distributions.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Wei, Xiaojing; Savage, Jessica A; Riggs, Charlotte E; Cavender-Bares, Jeannine</p> <p>2017-05-01</p> <p>Environmental filtering is an important community assembly process influencing species distributions. Contrasting species abundance patterns along environmental gradients are commonly used to provide evidence for environmental filtering. However, the same abundance patterns may result from alternative or concurrent assembly processes. Experimental tests are an important means to decipher whether species fitness varies with environment, in the absence of dispersal constraints and biotic interactions, and to draw conclusions about the importance of environmental filtering in community assembly. We performed an experimental test of environmental filtering in 14 closely related willow and poplar species (family Salicaceae) by transplanting cuttings of each species into 40 common gardens established along a natural <span class="hlt">hydrologic</span> gradient in the field, where competition was minimized and herbivory was controlled. We analyzed species fitness responses to the <span class="hlt">hydrologic</span> environment based on cumulative growth and survival over two years using aster fitness models. We also examined variation in nine drought and flooding tolerance traits expected to contribute to performance based on a priori understanding of plant function in relation to water availability and stress. We found substantial evidence that environmental filtering along the <span class="hlt">hydrologic</span> gradient played a critical role in determining species distributions. Fitness variation of each species in the field experiment was used to model their water table depth optima. These optima <span class="hlt">predicted</span> 68% of the variation in species realized <span class="hlt">hydrologic</span> niches based on peak abundance in naturally assembled communities in the surrounding region. Multiple traits associated with water transport efficiency and water stress tolerance were correlated with species <span class="hlt">hydrologic</span> niches, but they did not necessarily covary with each other. As a consequence, species occupying similar <span class="hlt">hydrologic</span> niches had different combinations of trait values</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2001JHyd..249....2K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2001JHyd..249....2K"><span>The case for probabilistic forecasting in <span class="hlt">hydrology</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Krzysztofowicz, Roman</p> <p>2001-08-01</p> <p>That forecasts should be stated in probabilistic, rather than deterministic, terms has been argued from common sense and decision-theoretic perspectives for almost a century. Yet most operational <span class="hlt">hydrological</span> forecasting systems produce deterministic forecasts and most research in operational <span class="hlt">hydrology</span> has been devoted to finding the 'best' estimates rather than quantifying the <span class="hlt">predictive</span> uncertainty. This essay presents a compendium of reasons for probabilistic forecasting of <span class="hlt">hydrological</span> variates. Probabilistic forecasts are scientifically more honest, enable risk-based warnings of floods, enable rational decision making, and offer additional economic benefits. The growing demand for information about risk and the rising capability to quantify <span class="hlt">predictive</span> uncertainties create an unparalleled opportunity for the <span class="hlt">hydrological</span> profession to dramatically enhance the forecasting paradigm.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFM.H51F1343C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFM.H51F1343C"><span>Modeling alpine grasslands with two integrated <span class="hlt">hydrologic</span> models: a comparison of the different process representation in CATHY and GEOtop</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Camporese, M.; Bertoldi, G.; Bortoli, E.; Wohlfahrt, G.</p> <p>2017-12-01</p> <p>Integrated <span class="hlt">hydrologic</span> surface-subsurface models (IHSSMs) are increasingly used as <span class="hlt">prediction</span> tools to solve simultaneously states and fluxes in and between multiple terrestrial compartments (e.g., snow cover, surface water, groundwater), in an attempt to tackle environmental problems in a holistic approach. Two such models, CATHY and GEOtop, are used in this study to investigate their capabilities to reproduce <span class="hlt">hydrological</span> processes in alpine grasslands. The two models differ significantly in the complexity of the representation of the surface energy balance and the solution of Richards equation for water flow in the variably saturated subsurface. The main goal of this research is to show how these differences in process representation can lead to different <span class="hlt">predictions</span> of <span class="hlt">hydrologic</span> states and fluxes, in the simulation of an experimental site located in the Venosta Valley (South Tyrol, Italy). Here, a large set of relevant <span class="hlt">hydrological</span> data (e.g., evapotranspiration, soil moisture) has been collected, with ground and remote sensing observations. The area of interest is part of a Long-Term Ecological Research (LTER) site, a mountain steep, heterogeneous slope, where the predominant land use types are meadow, pasture, and forest. The comparison between data and model <span class="hlt">predictions</span>, as well as between simulations with the two IHSSMs, contributes to <span class="hlt">advance</span> our understanding of the tradeoffs between different complexities in modeĺs process representation, model accuracy, and the ability to explain observed <span class="hlt">hydrological</span> dynamics in alpine environments.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2010WRR....4610511K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2010WRR....4610511K"><span>Ancient numerical daemons of conceptual <span class="hlt">hydrological</span> modeling: 2. Impact of time stepping schemes on model analysis and <span class="hlt">prediction</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Kavetski, Dmitri; Clark, Martyn P.</p> <p>2010-10-01</p> <p>Despite the widespread use of conceptual <span class="hlt">hydrological</span> models in environmental research and operations, they remain frequently implemented using numerically unreliable methods. This paper considers the impact of the time stepping scheme on model analysis (sensitivity analysis, parameter optimization, and Markov chain Monte Carlo-based uncertainty estimation) and <span class="hlt">prediction</span>. It builds on the companion paper (Clark and Kavetski, 2010), which focused on numerical accuracy, fidelity, and computational efficiency. Empirical and theoretical analysis of eight distinct time stepping schemes for six different <span class="hlt">hydrological</span> models in 13 diverse basins demonstrates several critical conclusions. (1) Unreliable time stepping schemes, in particular, fixed-step explicit methods, suffer from troublesome numerical artifacts that severely deform the objective function of the model. These deformations are not rare isolated instances but can arise in any model structure, in any catchment, and under common hydroclimatic conditions. (2) Sensitivity analysis can be severely contaminated by numerical errors, often to the extent that it becomes dominated by the sensitivity of truncation errors rather than the model equations. (3) Robust time stepping schemes generally produce "better behaved" objective functions, free of spurious local optima, and with sufficient numerical continuity to permit parameter optimization using efficient quasi Newton methods. When implemented within a multistart framework, modern Newton-type optimizers are robust even when started far from the optima and provide valuable diagnostic insights not directly available from evolutionary global optimizers. (4) Unreliable time stepping schemes lead to inconsistent and biased inferences of the model parameters and internal states. (5) Even when interactions between <span class="hlt">hydrological</span> parameters and numerical errors provide "the right result for the wrong reason" and the calibrated model performance appears adequate, unreliable</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2003AGUFM.H12I..02R','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2003AGUFM.H12I..02R"><span><span class="hlt">Hydrologic</span> Observatories: Design, Operation, and the Neuse Basin Prototype</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Reckhow, K.; Band, L.</p> <p>2003-12-01</p> <p><span class="hlt">Hydrologic</span> observatories are conceived as major research facilities that will be available to the full <span class="hlt">hydrologic</span> community, to facilitate comprehensive, cross-disciplinary and multi-scale measurements necessary to address the current and next generation of critical science and management issues. A network of <span class="hlt">hydrologic</span> observatories is proposed that both develop national comparable, multidisciplinary data sets and provide study areas to allow scientists, through their own creativity, to make scientific breakthroughs that would be impossible without the proposed observatories. The core objective of an observatory is to improve <span class="hlt">predictive</span> understanding of the flow paths, fluxes, and residence times of water, sediment and nutrients (the "core data") across a range of spatial and temporal scales across `interfaces'. To assess attainment of this objective, a benchmark will be established in the first year, and evaluated periodically. The benchmark should provide an estimate of <span class="hlt">prediction</span> uncertainty at points in the stream across scale; the general principle is that <span class="hlt">predictive</span> understanding must be demonstrated internal to the catchment as well as its outlet. The core data will be needed for practically any <span class="hlt">hydrologic</span> study, yet absence of these data has been a barrier to larger scale studies in the past. However, <span class="hlt">advancement</span> of <span class="hlt">hydrologic</span> science facilitated by the network of <span class="hlt">hydrologic</span> observatories is expected to focus on a set of science drivers, drawn from the major scientific questions posed by the set of NRC reports and refined into CUAHSI themes. These hypotheses will be tested at all observatories and will be used in the design to ensure the sufficiency of the data set. To make the observatories a national (and international) resource, a key aspect of the operation is the support of remote PI's. This support will include a resident staff of scientists and technicians on the order of 10 FTE's, availability of dormitory, laboratory, workshop space for all</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2006AGUFM.H21F1441M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2006AGUFM.H21F1441M"><span>CUAHSI <span class="hlt">Hydrologic</span> Information Systems</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Maidment, D.; Zaslavsky, I.; Tarboton, D.; Piasecki, M.; Goodall, J.</p> <p>2006-12-01</p> <p>The Consortium of Universities for the <span class="hlt">Advancement</span> of <span class="hlt">Hydrologic</span> Science, Inc (CUAHSI) has a <span class="hlt">Hydrologic</span> Information System (HIS) project, which is supported by NSF to develop infrastructure and services to support the <span class="hlt">advance</span> of <span class="hlt">hydrologic</span> science in the United States. This paper provides an overview of the HIS project. A set of web services called WaterOneFlow is being developed to provide better access to water observations data (point measurements of streamflow, water quality, climate and groundwater levels) from government agencies and individual investigator projects. Successful partnerships have been created with the USGS National Water Information System, EPA Storet and the NCDC Climate Data Online. Observations catalogs have been created for stations in the measurement networks of each of these data systems so that they can be queried in a uniform manner through CUAHSI HIS, and data delivered from them directly to the user via web services. A CUAHSI Observations Data Model has been designed for storing individual investigator data and an equivalent set of web services created for that so that individual investigators can publish their data onto the internet in the same format CUAHSI is providing for the federal agency data. These data will be accessed through HIS Servers hosted at the national level by CUAHSI and also by research centers and academic departments for regional application of HIS. An individual user application called HIS Analyst will enable individual <span class="hlt">hydrologic</span> scientists to access the information from the network of HIS Servers. The present focus is on water observations data but later development of this system will include weather and climate grid information, GIS data, remote sensing data and linkages between data and <span class="hlt">hydrologic</span> simulation models.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://cfpub.epa.gov/si/si_public_record_report.cfm?direntryid=336564','PESTICIDES'); return false;" href="https://cfpub.epa.gov/si/si_public_record_report.cfm?direntryid=336564"><span><span class="hlt">Hydrological</span> modelling in forested systems | Science ...</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>This chapter provides a brief overview of forest <span class="hlt">hydrology</span> modelling approaches for answering important global research and management questions. Many hundreds of <span class="hlt">hydrological</span> models have been applied globally across multiple decades to represent and <span class="hlt">predict</span> forest <span class="hlt">hydrological</span> processes. The focus of this chapter is on process-based models and approaches, specifically 'forest <span class="hlt">hydrology</span> models'; that is, physically based simulation tools that quantify compartments of the forest <span class="hlt">hydrological</span> cycle. Physically based models can be considered those that describe the conservation of mass, momentum and/or energy. The purpose of this chapter is to provide a brief overview of forest <span class="hlt">hydrology</span> modeling approaches for answering important global research and management questions. The focus of this chapter is on process-based models and approaches, specifically “forest <span class="hlt">hydrology</span> models”, i.e., physically-based simulation tools that quantify compartments of the forest <span class="hlt">hydrological</span> cycle.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFM.H32B..08C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFM.H32B..08C"><span>Using Unsupervised Learning to Unlock the Potential of <span class="hlt">Hydrologic</span> Similarity</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Chaney, N.; Newman, A. J.</p> <p>2017-12-01</p> <p>By clustering environmental data into representative <span class="hlt">hydrologic</span> response units (HRUs), <span class="hlt">hydrologic</span> similarity aims to harness the covariance between a system's physical environment and its <span class="hlt">hydrologic</span> response to create reduced-order models. This is the primary approach through which sub-grid <span class="hlt">hydrologic</span> processes are represented in large-scale models (e.g., Earth System Models). Although the possibilities of <span class="hlt">hydrologic</span> similarity are extensive, its practical implementations have been limited to 1-d bins of oversimplistic metrics of <span class="hlt">hydrologic</span> response (e.g., topographic index)—this is a missed opportunity. In this presentation we will show how unsupervised learning is unlocking the potential of <span class="hlt">hydrologic</span> similarity; clustering methods enable generalized frameworks to effectively and efficiently harness the petabytes of global environmental data to robustly characterize sub-grid heterogeneity in large-scale models. To illustrate the potential that unsupervised learning has towards <span class="hlt">advancing</span> <span class="hlt">hydrologic</span> similarity, we introduce a hierarchical clustering algorithm (HCA) that clusters very high resolution (30-100 meters) elevation, soil, climate, and land cover data to assemble a domain's representative HRUs. These HRUs are then used to parameterize the sub-grid heterogeneity in land surface models; for this study we use the GFDL LM4 model—the land component of the GFDL Earth System Model. To explore HCA and its impacts on the <span class="hlt">hydrologic</span> system we use a ¼ grid cell in southeastern California as a test site. HCA is used to construct an ensemble of 9 different HRU configurations—each configuration has a different number of HRUs; for each ensemble member LM4 is run between 2002 and 2014 with a 26 year spinup. The analysis of the ensemble of model simulations show that: 1) clustering the high-dimensional environmental data space leads to a robust representation of the role of the physical environment in the coupled water, energy, and carbon cycles at a relatively low</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017EGUGA..19.9837P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017EGUGA..19.9837P"><span>An approach to <span class="hlt">predict</span> water quality in data-sparse catchments using <span class="hlt">hydrological</span> catchment similarity</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Pohle, Ina; Glendell, Miriam; Stutter, Marc I.; Helliwell, Rachel C.</p> <p>2017-04-01</p> <p>An understanding of catchment response to climate and land use change at a regional scale is necessary for the assessment of mitigation and adaptation options addressing diffuse nutrient pollution. It is well documented that the physicochemical properties of a river ecosystem respond to change in a non-linear fashion. This is particularly important when threshold water concentrations, relevant to national and EU legislation, are exceeded. Large scale (regional) model assessments required for regulatory purposes must represent the key processes and mechanisms that are more readily understood in catchments with water quantity and water quality data monitored at high spatial and temporal resolution. While daily discharge data are available for most catchments in Scotland, nitrate and phosphorus are mostly available on a monthly basis only, as typified by regulatory monitoring. However, high resolution (hourly to daily) water quantity and water quality data exist for a limited number of research catchments. To successfully implement adaptation measures across Scotland, an upscaling from data-rich to data-sparse catchments is required. In addition, the widespread availability of spatial datasets affecting <span class="hlt">hydrological</span> and biogeochemical responses (e.g. soils, topography/geomorphology, land use, vegetation etc.) provide an opportunity to transfer <span class="hlt">predictions</span> between data-rich and data-sparse areas by linking processes and responses to catchment attributes. Here, we develop a framework of catchment typologies as a prerequisite for transferring information from data-rich to data-sparse catchments by focusing on how <span class="hlt">hydrological</span> catchment similarity can be used as an indicator of grouped behaviours in water quality response. As indicators of <span class="hlt">hydrological</span> catchment similarity we use flow indices derived from observed discharge data across Scotland as well as <span class="hlt">hydrological</span> model parameters. For the latter, we calibrated the lumped rainfall-runoff model TUWModel using multiple</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016EGUGA..1811991F','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016EGUGA..1811991F"><span>Quantifying uncertainties in streamflow <span class="hlt">predictions</span> through signature based inference of <span class="hlt">hydrological</span> model parameters</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Fenicia, Fabrizio; Reichert, Peter; Kavetski, Dmitri; Albert, Calro</p> <p>2016-04-01</p> <p>The calibration of <span class="hlt">hydrological</span> models based on signatures (e.g. Flow Duration Curves - FDCs) is often advocated as an alternative to model calibration based on the full time series of system responses (e.g. hydrographs). Signature based calibration is motivated by various arguments. From a conceptual perspective, calibration on signatures is a way to filter out errors that are difficult to represent when calibrating on the full time series. Such errors may for example occur when observed and simulated hydrographs are shifted, either on the "time" axis (i.e. left or right), or on the "streamflow" axis (i.e. above or below). These shifts may be due to errors in the precipitation input (time or amount), and if not properly accounted in the likelihood function, may cause biased parameter estimates (e.g. estimated model parameters that do not reproduce the recession characteristics of a hydrograph). From a practical perspective, signature based calibration is seen as a possible solution for making <span class="hlt">predictions</span> in ungauged basins. Where streamflow data are not available, it may in fact be possible to reliably estimate streamflow signatures. Previous research has for example shown how FDCs can be reliably estimated at ungauged locations based on climatic and physiographic influence factors. Typically, the goal of signature based calibration is not the <span class="hlt">prediction</span> of the signatures themselves, but the <span class="hlt">prediction</span> of the system responses. Ideally, the <span class="hlt">prediction</span> of system responses should be accompanied by a reliable quantification of the associated uncertainties. Previous approaches for signature based calibration, however, do not allow reliable estimates of streamflow <span class="hlt">predictive</span> distributions. Here, we illustrate how the Bayesian approach can be employed to obtain reliable streamflow <span class="hlt">predictive</span> distributions based on signatures. A case study is presented, where a <span class="hlt">hydrological</span> model is calibrated on FDCs and additional signatures. We propose an approach where the likelihood</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70044582','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70044582"><span><span class="hlt">Predictive</span> occurrence models for coastal wetland plant communities: delineating <span class="hlt">hydrologic</span> response surfaces with multinomial logistic regression</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Snedden, Gregg A.; Steyer, Gregory D.</p> <p>2013-01-01</p> <p>Understanding plant community zonation along estuarine stress gradients is critical for effective conservation and restoration of coastal wetland ecosystems. We related the presence of plant community types to estuarine <span class="hlt">hydrology</span> at 173 sites across coastal Louisiana. Percent relative cover by species was assessed at each site near the end of the growing season in 2008, and hourly water level and salinity were recorded at each site Oct 2007–Sep 2008. Nine plant community types were delineated with k-means clustering, and indicator species were identified for each of the community types with indicator species analysis. An inverse relation between salinity and species diversity was observed. Canonical correspondence analysis (CCA) effectively segregated the sites across ordination space by community type, and indicated that salinity and tidal amplitude were both important drivers of vegetation composition. Multinomial logistic regression (MLR) and Akaike's Information Criterion (AIC) were used to <span class="hlt">predict</span> the probability of occurrence of the nine vegetation communities as a function of salinity and tidal amplitude, and probability surfaces obtained from the MLR model corroborated the CCA results. The weighted kappa statistic, calculated from the confusion matrix of <span class="hlt">predicted</span> versus actual community types, was 0.7 and indicated good agreement between observed community types and model <span class="hlt">predictions</span>. Our results suggest that models based on a few key <span class="hlt">hydrologic</span> variables can be valuable tools for <span class="hlt">predicting</span> vegetation community development when restoring and managing coastal wetlands.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.fs.usda.gov/treesearch/pubs/48829','TREESEARCH'); return false;" href="https://www.fs.usda.gov/treesearch/pubs/48829"><span>Comparing large-scale <span class="hlt">hydrological</span> model <span class="hlt">predictions</span> with observed streamflow in the Pacific Northwest: effects of climate and groundwater</span></a></p> <p><a target="_blank" href="http://www.fs.usda.gov/treesearch/">Treesearch</a></p> <p>Mohammad Safeeq; Guillaume S. Mauger; Gordon E. Grant; Ivan Arismendi; Alan F. Hamlet; Se-Yeun Lee</p> <p>2014-01-01</p> <p>Assessing uncertainties in <span class="hlt">hydrologic</span> models can improve accuracy in <span class="hlt">predicting</span> future streamflow. Here, simulated streamflows using the Variable Infiltration Capacity (VIC) model at coarse (1/16°) and fine (1/120°) spatial resolutions were evaluated against observed streamflows from 217 watersheds. In...</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('http://adsabs.harvard.edu/abs/2017EGUGA..1910805N','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017EGUGA..1910805N"><span><span class="hlt">Predicting</span> <span class="hlt">hydrological</span> and erosional risks in fire-affected watersheds: recent <span class="hlt">advances</span> and research gaps</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Nunes, João Pedro; Keizer, Jan Jacob</p> <p>2017-04-01</p> <p>Models can be invaluable tools to assess and manage the impacts of forest fires on <span class="hlt">hydrological</span> and erosion processes. Immediately after fires, models can be used to identify priority areas for post-fire interventions or assess the risks of flooding and downstream contamination. In the long term, models can be used to evaluate the long-term implications of a fire regime for soil protection, surface water quality and potential management risks, or determine how changes to fire regimes, caused e.g. by climate change, can impact soil and water quality. However, several challenges make post-fire modelling particularly difficult: • Fires change vegetation cover and properties, such as by changing soil water repellency or by adding an ash layer over the soil; these processes, however are not described in currently used models, so that existing models need to be modified and tested. • Vegetation and soils recover with time since fire, changing important model parameters, so that the recovery processes themselves also need to be simulated, including the role of post-fire interventions. • During the window of vegetation and soil disturbance, particular weather conditions, such as the occurrence of severe droughts or extreme rainfall events, can have a large impact on the amount of runoff and erosion produced in burnt areas, so that models that smooth out these peak responses and rather simulate "long-term" average processes are less useful. • While existing models can simulate reasonable well slope-scale runoff generation and associated sediment losses and their catchment-scale routing, few models can accommodate the role of the ash layer or its transport by overland flow, in spite of its importance for soil fertility losses and downstream contamination. This presentation will provide an overview of the importance of post-fire <span class="hlt">hydrological</span> and erosion modelling as well as of the challenges it faces and of recent efforts made to overcome these challenges. It will</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014AGUFMED54A3510B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014AGUFMED54A3510B"><span>Using <span class="hlt">Advances</span> in Research on Louisiana Coastal Restoration and Protection to Develop Undergraduate <span class="hlt">Hydrology</span> Education Experiences Delivered via a Web Interface</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Bodin, M.; Habib, E. H.; Meselhe, E. A.; Visser, J.; Chimmula, S.</p> <p>2014-12-01</p> <p>Utilizing <span class="hlt">advances</span> in <span class="hlt">hydrologic</span> research and technology, learning modules can be developed to deliver visual, case-based, data and simulation driven educational experiences. This paper focuses on the development of web modules based on case studies in Coastal Louisiana, one of three ecosystems that comprise an ongoing <span class="hlt">hydrology</span> education online system called HydroViz. The Chenier Plain ecosystem in Coastal Louisiana provides an abundance of concepts and scenarios appropriate for use in many undergraduate water resource and <span class="hlt">hydrology</span> curricula. The modules rely on a set of <span class="hlt">hydrologic</span> data collected within the Chenier Plain along with inputs and outputs of eco-<span class="hlt">hydrology</span> and vegetation-change simulation models that were developed to analyze different restoration and protection projects within the 2012 Louisiana Costal Master Plan. The modules begin by investigating the basic features of the basin and it <span class="hlt">hydrologic</span> characteristics. The eco-<span class="hlt">hydrology</span> model is then introduced along with its governing equations, numerical solution scheme and how it represents the study domain. Concepts on water budget in a coastal basin are then introduced using the simulation model inputs, outputs and boundary conditions. The complex relationships between salinity, water level and vegetation changes are then investigated through the use of the simulation models and associated field data. Other student activities focus on using the simulation models to evaluate tradeoffs and impacts of actual restoration and protection projects that were proposed as part of 2012 Louisiana Master Plan. The hands-on learning activities stimulate student learning of <span class="hlt">hydrologic</span> and water management concepts by providing real-world context and opportunity to build fundamental knowledge as well as practical skills. The modules are delivered through a carefully designed user interface using open source and free technologies which enable wide dissemination and encourage adaptation by others.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFM.H54A..06M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFM.H54A..06M"><span>The Canadian <span class="hlt">Hydrological</span> Model (CHM): A multi-scale, variable-complexity <span class="hlt">hydrological</span> model for cold regions</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Marsh, C.; Pomeroy, J. W.; Wheater, H. S.</p> <p>2016-12-01</p> <p>There is a need for <span class="hlt">hydrological</span> land surface schemes that can link to atmospheric models, provide <span class="hlt">hydrological</span> <span class="hlt">prediction</span> at multiple scales and guide the development of multiple objective water <span class="hlt">predictive</span> systems. Distributed raster-based models suffer from an overrepresentation of topography, leading to wasted computational effort that increases uncertainty due to greater numbers of parameters and initial conditions. The Canadian <span class="hlt">Hydrological</span> Model (CHM) is a modular, multiphysics, spatially distributed modelling framework designed for representing <span class="hlt">hydrological</span> processes, including those that operate in cold-regions. Unstructured meshes permit variable spatial resolution, allowing coarse resolutions at low spatial variability and fine resolutions as required. Model uncertainty is reduced by lessening the necessary computational elements relative to high-resolution rasters. CHM uses a novel multi-objective approach for unstructured triangular mesh generation that fulfills <span class="hlt">hydrologically</span> important constraints (e.g., basin boundaries, water bodies, soil classification, land cover, elevation, and slope/aspect). This provides an efficient spatial representation of parameters and initial conditions, as well as well-formed and well-graded triangles that are suitable for numerical discretization. CHM uses high-quality open source libraries and high performance computing paradigms to provide a framework that allows for integrating current state-of-the-art process algorithms. The impact of changes to model structure, including individual algorithms, parameters, initial conditions, driving meteorology, and spatial/temporal discretization can be easily tested. Initial testing of CHM compared spatial scales and model complexity for a spring melt period at a sub-arctic mountain basin. The meshing algorithm reduced the total number of computational elements and preserved the spatial heterogeneity of <span class="hlt">predictions</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014AGUFM.H24B..03S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014AGUFM.H24B..03S"><span>Water and the Earth System in the Anthropocene: Evolution of Socio-<span class="hlt">Hydrology</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Sivapalan, M.; Bloeschl, G.</p> <p>2014-12-01</p> <p>Over the past century, <span class="hlt">hydrological</span> science has evolved through distinct eras as judged by ideas, information sources, technological <span class="hlt">advances</span> and societal influences: Empirical Era which was data based with little theory, Systems Era that focused on input-output relationships, Process Era with a focus on processes, and the Geosciences Era where <span class="hlt">hydrology</span> was considered an Earth System science. We argue that as the human footprint on earth becomes increasingly dominant, we are moving into a Co-evolution Era. Co-evolution implies that the components of the Earth system are intimately intertwined at many time scales - fast scales of immediate feedbacks that translate into slow scale interdependencies and trends. These involve feedbacks between the atmosphere, biota, soils and landforms, mediated by water flow and transport processes. The human factor is becoming a key component of this coupled system. While there is a long tradition of considering effects of water on humans, and vice versa, the new thrust on socio-<span class="hlt">hydrology</span> has a number of defining characteristics that sets it apart from traditional approaches: - Capturing feedbacks of human-natural water system in a dynamic way (slow and fast processes) to go beyond prescribing human factors as mere boundary conditions. These feedbacks will be essential to understand how the system may evolve in the future into new, perhaps previously unobserved, states. - Quantifying system dynamics in a generalizable way. So far, water resources assessment has been context dependent, tied to local conditions. While for immediate decision making this is undoubtedly essential, for more scientific inquiry, a more uniform knowledge base is indispensable. - Not necessarily <span class="hlt">predictive</span>. The coupled human-nature system is inherently non-linear, which may prohibit <span class="hlt">predictability</span> in the traditional sense. The socio-<span class="hlt">hydrologic</span> approach may still be <span class="hlt">predictive</span> in a statistical sense and, perhaps even more importantly, it may yet reveal</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFM.H33C1688P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFM.H33C1688P"><span><span class="hlt">Hydrologic</span> classification of rivers based on cluster analysis of dimensionless <span class="hlt">hydrologic</span> signatures: Applications for environmental instream flows</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Praskievicz, S. J.; Luo, C.</p> <p>2017-12-01</p> <p>Classification of rivers is useful for a variety of purposes, such as generating and testing hypotheses about watershed controls on <span class="hlt">hydrology</span>, <span class="hlt">predicting</span> <span class="hlt">hydrologic</span> variables for ungaged rivers, and setting goals for river management. In this research, we present a bottom-up (based on machine learning) river classification designed to investigate the underlying physical processes governing rivers' <span class="hlt">hydrologic</span> regimes. The classification was developed for the entire state of Alabama, based on 248 United States Geological Survey (USGS) stream gages that met criteria for length and completeness of records. Five dimensionless <span class="hlt">hydrologic</span> signatures were derived for each gage: slope of the flow duration curve (indicator of flow variability), baseflow index (ratio of baseflow to average streamflow), rising limb density (number of rising limbs per unit time), runoff ratio (ratio of long-term average streamflow to long-term average precipitation), and streamflow elasticity (sensitivity of streamflow to precipitation). We used a Bayesian clustering algorithm to classify the gages, based on the five <span class="hlt">hydrologic</span> signatures, into distinct <span class="hlt">hydrologic</span> regimes. We then used classification and regression trees (CART) to <span class="hlt">predict</span> each gaged river's membership in different <span class="hlt">hydrologic</span> regimes based on climatic and watershed variables. Using existing geospatial data, we applied the CART analysis to classify ungaged streams in Alabama, with the National Hydrography Dataset Plus (NHDPlus) catchment (average area 3 km2) as the unit of classification. The results of the classification can be used for meeting management and conservation objectives in Alabama, such as developing statewide standards for environmental instream flows. Such <span class="hlt">hydrologic</span> classification approaches are promising for contributing to process-based understanding of river systems.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013AGUFMED31C0753H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013AGUFMED31C0753H"><span>Adaptable Web Modules to Stimulate Active Learning in Engineering <span class="hlt">Hydrology</span> using Data and Model Simulations of Three Regional <span class="hlt">Hydrologic</span> Systems</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Habib, E. H.; Tarboton, D. G.; Lall, U.; Bodin, M.; Rahill-Marier, B.; Chimmula, S.; Meselhe, E. A.; Ali, A.; Williams, D.; Ma, Y.</p> <p>2013-12-01</p> <p>The <span class="hlt">hydrologic</span> community has long recognized the need for broad reform in <span class="hlt">hydrologic</span> education. A paradigm shift is critically sought in undergraduate <span class="hlt">hydrology</span> and water resource education by adopting context-rich, student-centered, and active learning strategies. Hydrologists currently deal with intricate issues rooted in complex natural ecosystems containing a multitude of interconnected processes. <span class="hlt">Advances</span> in the multi-disciplinary field include observational settings such as Critical Zone and Water, Sustainability and Climate Observatories, <span class="hlt">Hydrologic</span> Information Systems, instrumentation and modeling methods. These research <span class="hlt">advances</span> theory and practices call for similar efforts and improvements in <span class="hlt">hydrologic</span> education. The typical, text-book based approach in <span class="hlt">hydrologic</span> education has focused on specific applications and/or unit processes associated with the <span class="hlt">hydrologic</span> cycle with idealizations, rather than the contextual relations in the physical processes and the spatial and temporal dynamics connecting climate and ecosystems. An appreciation of the natural variability of these processes will lead to graduates with the ability to develop independent learning skills and understanding. This appreciation cannot be gained in curricula where field components such as observational and experimental data are deficient. These types of data are also critical when using simulation models to create environments that support this type of learning. Additional sources of observations in conjunction with models and field data are key to students understanding of the challenges associated with using models to represent such complex systems. Recent <span class="hlt">advances</span> in scientific visualization and web-based technologies provide new opportunities for the development of active learning techniques utilizing ongoing research. The overall goal of the current study is to develop visual, case-based, data and simulation driven learning experiences to instructors and students through a web</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015JHyd..531..231S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015JHyd..531..231S"><span><span class="hlt">Hydrologic</span> applications of weather radar</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Seo, Dong-Jun; Habib, Emad; Andrieu, Hervé; Morin, Efrat</p> <p>2015-12-01</p> <p>By providing high-resolution quantitative precipitation information (QPI), weather radars have revolutionized <span class="hlt">hydrology</span> in the last two decades. With the aid of GIS technology, radar-based quantitative precipitation estimates (QPE) have enabled routine high-resolution <span class="hlt">hydrologic</span> modeling in many parts of the world. Given the ever-increasing need for higher-resolution <span class="hlt">hydrologic</span> and water resources information for a wide range of applications, one may expect that the use of weather radar will only grow. Despite the tremendous progress, a number of significant scientific, technological and engineering challenges remain to realize its potential. New challenges are also emerging as new areas of applications are discovered, explored and pursued. The purpose of this special issue is to provide the readership with some of the latest <span class="hlt">advances</span>, lessons learned, experiences gained, and science issues and challenges related to <span class="hlt">hydrologic</span> applications of weather radar. The special issue features 20 contributions on various topics which reflect the increasing diversity as well as the areas of focus in radar <span class="hlt">hydrology</span> today. The contributions may be grouped as follows:</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19940011422','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19940011422"><span>Recent scientific <span class="hlt">advances</span> in the use of radar in scientific <span class="hlt">hydrology</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Engman, Edwin T.</p> <p>1993-01-01</p> <p>The data needs in scientific <span class="hlt">hydrology</span> involve measurements of system states and fluxes. The microwave region is particularly well suited for measuring the system states of soil moisture and snow and the major flux into the earth as rainfall. This paper discusses the unique data needs of <span class="hlt">hydrology</span> and presents some recent examples from AIRSAR experiments.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018HESS...22.1665S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018HESS...22.1665S"><span>From engineering <span class="hlt">hydrology</span> to Earth system science: milestones in the transformation of <span class="hlt">hydrologic</span> science</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Sivapalan, Murugesu</p> <p>2018-03-01</p> <p><span class="hlt">Hydrology</span> has undergone almost transformative changes over the past 50 years. Huge strides have been made in the transition from early empirical approaches to rigorous approaches based on the fluid mechanics of water movement on and below the land surface. However, progress has been hampered by problems posed by the presence of heterogeneity, including subsurface heterogeneity present at all scales. The inability to measure or map the heterogeneity everywhere prevented the development of balance equations and associated closure relations at the scales of interest, and has led to the virtual impasse we are presently in, in terms of development of physically based models needed for <span class="hlt">hydrologic</span> <span class="hlt">predictions</span>. An alternative to the mapping of heterogeneity everywhere is a new Earth system science view, which sees the heterogeneity as the end result of co-evolutionary <span class="hlt">hydrological</span>, geomorphological, ecological, and pedological processes, each operating at a different rate, which help to shape the landscapes that we find in nature, including the heterogeneity that we do not readily see. The expectation is that instead of specifying exact details of the heterogeneity in our models, we can replace it (without loss of information) with the ecosystem function that they perform. Guided by this new Earth system science perspective, development of <span class="hlt">hydrologic</span> science is now addressing new questions using novel holistic co-evolutionary approaches as opposed to the physical, fluid mechanics based reductionist approaches that we inherited from the recent past. In the emergent Anthropocene, the co-evolutionary view has expanded further to involve interactions and feedbacks with human-social processes as well. In this paper, I present my own perspective of key milestones in the transformation of <span class="hlt">hydrologic</span> science from engineering <span class="hlt">hydrology</span> to Earth system science, drawn from the work of several students and colleagues of mine, and discuss their implication for <span class="hlt">hydrologic</span> observations</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2011AGUFMNG23B1500N','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2011AGUFMNG23B1500N"><span>Sequential data assimilation for a distributed <span class="hlt">hydrologic</span> model considering different time scale of internal processes</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Noh, S.; Tachikawa, Y.; Shiiba, M.; Kim, S.</p> <p>2011-12-01</p> <p>Applications of the sequential data assimilation methods have been increasing in <span class="hlt">hydrology</span> to reduce uncertainty in the model <span class="hlt">prediction</span>. In a distributed <span class="hlt">hydrologic</span> model, there are many types of state variables and each variable interacts with each other based on different time scales. However, the framework to deal with the delayed response, which originates from different time scale of <span class="hlt">hydrologic</span> processes, has not been thoroughly addressed in the <span class="hlt">hydrologic</span> data assimilation. In this study, we propose the lagged filtering scheme to consider the lagged response of internal states in a distributed <span class="hlt">hydrologic</span> model using two filtering schemes; particle filtering (PF) and ensemble Kalman filtering (EnKF). The EnKF is one of the widely used sub-optimal filters implementing an efficient computation with limited number of ensemble members, however, still based on Gaussian approximation. PF can be an alternative in which the propagation of all uncertainties is carried out by a suitable selection of randomly generated particles without any assumptions about the nature of the distributions involved. In case of PF, <span class="hlt">advanced</span> particle regularization scheme is implemented together to preserve the diversity of the particle system. In case of EnKF, the ensemble square root filter (EnSRF) are implemented. Each filtering method is parallelized and implemented in the high performance computing system. A distributed <span class="hlt">hydrologic</span> model, the water and energy transfer processes (WEP) model, is applied for the Katsura River catchment, Japan to demonstrate the applicability of proposed approaches. Forecasted results via PF and EnKF are compared and analyzed in terms of the <span class="hlt">prediction</span> accuracy and the probabilistic adequacy. Discussions are focused on the prospects and limitations of each data assimilation method.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=19990103011&hterms=seasonal+forecast&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D50%26Ntt%3Dseasonal%2Bforecast','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=19990103011&hterms=seasonal+forecast&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D50%26Ntt%3Dseasonal%2Bforecast"><span>Upper Limits of <span class="hlt">Predictability</span> in Long-Range Climate/<span class="hlt">Hydrologic</span> Forecasts</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Koster, R. D.; Suarez, M. J.; Heiser, M.</p> <p>1998-01-01</p> <p>The accurate forecasting of el nino or la nina conditions in the tropical Pacific can potentially lead to valuable <span class="hlt">predictions</span> of <span class="hlt">hydrological</span> anomalies over land at seasonal to interannual timescales. Even with highly accurate earth system models, though, our ability to generate these continental forecasts will always be limited by the chaotic nature of the atmospheric circulation. The nature of this fundamental limitation is explored through the use of 16-member ensembles of multi-decade GCM simulations. In each simulation of the first ensemble, sea surface temperatures (SSTs) are given the same realistic interannual variations over a 45-year period, and land surface state is allowed to evolve with that of the atmosphere. Analysis of the results shows that the SSTs control the temporal organization of continental precipitation anomalies to a significant extent in the tropics and to a much smaller extent in midlatitudes. In each simulation of the second ensemble, we prescribe SSTs as before, but we also prescribe interannual variations in the low frequency component of evaporation efficiency over land. Thus, in the second ensemble, we effectively make the extreme assumption that surface boundary conditions across the globe are perfectly <span class="hlt">predictable</span>, and we quantify the consistency with which the atmosphere (particularly precipitation) responds to these boundary conditions. The resulting "absolute upper limit" on the <span class="hlt">predictability</span> of precipitation is found to be quite high in the tropics yet only moderate in many midlatitude regions.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017EGUGA..19.9014T','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017EGUGA..19.9014T"><span>Observing <span class="hlt">hydrological</span> processes: recent <span class="hlt">advancements</span> in surface flow monitoring through image analysis</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Tauro, Flavia; Grimaldi, Salvatore</p> <p>2017-04-01</p> <p>Recently, several efforts have been devoted to the design and development of innovative, and often unintended, approaches for the acquisition of <span class="hlt">hydrological</span> data. Among such pioneering techniques, this presentation reports recent <span class="hlt">advancements</span> towards the establishment of a novel noninvasive and potentially continuous methodology based on the acquisition and analysis of images for spatially distributed observations of the kinematics of surface waters. The approach aims at enabling rapid, affordable, and accurate surface flow monitoring of natural streams. Flow monitoring is an integral part of <span class="hlt">hydrological</span> sciences and is essential for disaster risk reduction and the comprehension of natural phenomena. However, water processes are inherently complex to observe: they are characterized by multiscale and highly heterogeneous phenomena which have traditionally demanded sophisticated and costly measurement techniques. Challenges in the implementation of such techniques have also resulted in lack of <span class="hlt">hydrological</span> data during extreme events, in difficult-to-access environments, and at high temporal resolution. By combining low-cost yet high-resolution images and several velocimetry algorithms, noninvasive flow monitoring has been successfully conducted at highly heterogeneous scales, spanning from rills to highly turbulent streams, and medium-scale rivers, with minimal supervision by external users. Noninvasive image data acquisition has also afforded observations in high flow conditions. Latest novelties towards continuous flow monitoring at the catchment scale have entailed the development of a remote gauge-cam station on the Tiber River and integration of flow monitoring through image analysis with unmanned aerial systems (UASs) technology. The gauge-cam station and the UAS platform both afford noninvasive image acquisition and calibration through an innovative laser-based setup. Compared to traditional point-based instrumentation, images allow for generating surface</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70040844','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70040844"><span>Reference <span class="hlt">hydrologic</span> networks II. Using reference <span class="hlt">hydrologic</span> networks to assess climate-driven changes in streamflow</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Burn, Donald H.; Hannaford, Jamie; Hodgkins, Glenn A.; Whitfield, Paul H.; Thorne, Robin; Marsh, Terry</p> <p>2012-01-01</p> <p>Reference <span class="hlt">hydrologic</span> networks (RHNs) can play an important role in monitoring for changes in the <span class="hlt">hydrological</span> regime related to climate variation and change. Currently, the literature concerning <span class="hlt">hydrological</span> response to climate variations is complex and confounded by the combinations of many methods of analysis, wide variations in <span class="hlt">hydrology</span>, and the inclusion of data series that include changes in land use, storage regulation and water use in addition to those of climate. Three case studies that illustrate a variety of approaches to the analysis of data from RHNs are presented and used, together with a summary of studies from the literature, to develop approaches for the investigation of changes in the <span class="hlt">hydrological</span> regime at a continental or global scale, particularly for international comparison. We present recommendations for an analysis framework and the next steps to <span class="hlt">advance</span> such an initiative. There is a particular focus on the desirability of establishing standardized procedures and methodologies for both the creation of new national RHNs and the systematic analysis of data derived from a collection of RHNs.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2005AGUFM.H13J..02H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2005AGUFM.H13J..02H"><span>Monitoring Precipitation from Space: targeting <span class="hlt">Hydrology</span> Community?</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Hong, Y.; Turk, J.</p> <p>2005-12-01</p> <p>During the past decades, <span class="hlt">advances</span> in space, sensor and computer technology have made it possible to estimate precipitation nearly globally from a variety of observations in a relatively direct manner. The success of Tropical Precipitation Measuring Mission (TRMM) has been a significant <span class="hlt">advance</span> for modern precipitation estimation algorithms to move toward daily quarter degree measurements, while the need for precipitation data at temporal-spatial resolutions compatible with <span class="hlt">hydrologic</span> modeling has been emphasized by the end user: <span class="hlt">hydrology</span> community. Can the future deployment of Global Precipitation Measurement constellation of low-altitude orbiting satellites (covering 90% of the global with a sampling interval of less than 3-hours), in conjunction with the existing suite of geostationary satellites, results in significant improvements in scale and accuracy of precipitation estimates suitable for <span class="hlt">hydrology</span> applications? This presentation will review the current state of satellite-derived precipitation estimation and demonstrate the early results and primary barriers to full global high-resolution precipitation coverage. An attempt to facilitate the communication between data producers and users will be discussed by developing an 'end-to-end' uncertainty propagation analysis framework to quantify both the precipitation estimation error structure and the error influence on <span class="hlt">hydrological</span> modeling.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2004AGUFM.H31C0389H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2004AGUFM.H31C0389H"><span>The Platte River <span class="hlt">Hydrologic</span> Observatory (PRIVHO)</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Harvey, F.; Ramirez, J. A.; Thurow, T. L.</p> <p>2004-12-01</p> <p>The Platte River <span class="hlt">Hydrologic</span> Observatory (PRIVHO), located within the Platte River Basin, of the U.S. central Great Plains, affords excellent interdisciplinary and multi-disciplinary research opportunities for scientists to examine the impacts of scaling, to investigate forcing feedbacks and coupling of various interconnected <span class="hlt">hydrological</span>, geological, climatological and biological systems, and to test the applicability and limits of <span class="hlt">prediction</span> in keeping with all five of CUAHSI's priority science criteria; linking <span class="hlt">hydrologic</span> and biogeochemical cycles, sustainability of water resources, <span class="hlt">hydrologic</span> and ecosystem interactions, <span class="hlt">hydrologic</span> extremes, and fate and transport of contaminants. In addition, PRIVHO is uniquely positioned to investigate many human dimension questions such as those related to interstate and intrastate conflicts over water use, evolution of water policy and law in the wake of <span class="hlt">advancing</span> science, societal and economic changes that are driven by water use, availability and management, and human impacts on climate and land use changes. The Platte River traverses several important environmental gradients, including temperature and precipitation-to-evaporation ratio, is underlain by the High Plains Aquifer under much of its reach, crosses a number of terrestrial ecoregions, and in central Nebraska, serves as a vital link in the Central Flyway, providing habitat for 300 species of migratory birds and many threatened or endangered species. The Platte River flows through metropolitan, urban and agricultural settings and is impacted by both point and non-point pollution. The Platte River is one of the most over-appropriated rivers in the country with 15 major dams, hundreds of small reservoirs, and thousands of irrigation wells. The river provides municipal and industrial water supplies for about 3.5 million people, irrigation water for millions of acres of farmland, and generates millions of dollars of hydroelectric power. PRIVHO will allow researchers to</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.fs.usda.gov/treesearch/pubs/39275','TREESEARCH'); return false;" href="https://www.fs.usda.gov/treesearch/pubs/39275"><span>Chapter 2: Sampling strategies in forest <span class="hlt">hydrology</span> and biogeochemistry</span></a></p> <p><a target="_blank" href="http://www.fs.usda.gov/treesearch/">Treesearch</a></p> <p>Roger C. Bales; Martha H. Conklin; Branko Kerkez; Steven Glaser; Jan W. Hopmans; Carolyn T. Hunsaker; Matt Meadows; Peter C. Hartsough</p> <p>2011-01-01</p> <p>Many aspects of forest <span class="hlt">hydrology</span> have been based on accurate but not necessarily spatially representative measurements, reflecting the measurement capabilities that were traditionally available. Two developments are bringing about fundamental changes in sampling strategies in forest <span class="hlt">hydrology</span> and biogeochemistry: (a) technical <span class="hlt">advances</span> in measurement capability, as is...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.fs.usda.gov/treesearch/pubs/44370','TREESEARCH'); return false;" href="https://www.fs.usda.gov/treesearch/pubs/44370"><span>Response of <span class="hlt">hydrology</span> to climate change in the southern Appalachian mountains using Bayesian inference</span></a></p> <p><a target="_blank" href="http://www.fs.usda.gov/treesearch/">Treesearch</a></p> <p>Wei Wu; James S. Clark; James M. Vose</p> <p>2012-01-01</p> <p><span class="hlt">Predicting</span> long-term consequences of climate change on <span class="hlt">hydrologic</span> processes has been limited due to the needs to accommodate the uncertainties in <span class="hlt">hydrological</span> measurements for calibration, and to account for the uncertainties in the models that would ingest those calibrations and uncertainties in climate <span class="hlt">predictions</span> as basis for <span class="hlt">hydrological</span> <span class="hlt">predictions</span>. We implemented...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFM.H53E1505D','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFM.H53E1505D"><span>Daily Streamflow <span class="hlt">Predictions</span> in an Ungauged Watershed in Northern California Using the Precipitation-Runoff Modeling System (PRMS): Calibration Challenges when nearby Gauged Watersheds are <span class="hlt">Hydrologically</span> Dissimilar</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Dhakal, A. S.; Adera, S.</p> <p>2017-12-01</p> <p>Accurate daily streamflow <span class="hlt">prediction</span> in ungauged watersheds with sparse information is challenging. The ability of a <span class="hlt">hydrologic</span> model calibrated using nearby gauged watersheds to <span class="hlt">predict</span> streamflow accurately depends on <span class="hlt">hydrologic</span> similarities between the gauged and ungauged watersheds. This study examines daily streamflow <span class="hlt">predictions</span> using the Precipitation-Runoff Modeling System (PRMS) for the largely ungauged San Antonio Creek watershed, a 96 km2 sub-watershed of the Alameda Creek watershed in Northern California. The process-based PRMS model is being used to improve the accuracy of recent San Antonio Creek streamflow <span class="hlt">predictions</span> generated by two empirical methods. Although San Antonio Creek watershed is largely ungauged, daily streamflow data exists for <span class="hlt">hydrologic</span> years (HY) 1913 - 1930. PRMS was calibrated for HY 1913 - 1930 using streamflow data, modern-day land use and PRISM precipitation distribution, and gauged precipitation and temperature data from a nearby watershed. The PRMS model was then used to generate daily streamflows for HY 1996-2013, during which the watershed was ungauged, and <span class="hlt">hydrologic</span> responses were compared to two nearby gauged sub-watersheds of Alameda Creek. Finally, the PRMS-<span class="hlt">predicted</span> daily flows between HY 1996-2013 were compared to the two empirically-<span class="hlt">predicted</span> streamflow time series: (1) the reservoir mass balance method and (2) correlation of historical streamflows from 80 - 100 years ago between San Antonio Creek and a nearby sub-watershed located in Alameda Creek. While the mass balance approach using reservoir storage and transfers is helpful for estimating inflows to the reservoir, large discrepancies in daily streamflow estimation can arise. Similarly, correlation-based <span class="hlt">predicted</span> daily flows which rely on a relationship from flows collected 80-100 years ago may not represent current watershed <span class="hlt">hydrologic</span> conditions. This study aims to develop a method of streamflow <span class="hlt">prediction</span> in the San Antonio Creek watershed by examining PRMS</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014AGUFM.H34E..03V','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014AGUFM.H34E..03V"><span><span class="hlt">Hydrologic</span> Design in the Anthropocene</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Vogel, R. M.; Farmer, W. H.; Read, L.</p> <p>2014-12-01</p> <p>In an era dubbed the Anthropocene, the natural world is being transformed by a myriad of human influences. As anthropogenic impacts permeate <span class="hlt">hydrologic</span> systems, hydrologists are challenged to fully account for such changes and develop new methods of <span class="hlt">hydrologic</span> design. Deterministic watershed models (DWM), which can account for the impacts of changes in land use, climate and infrastructure, are becoming increasing popular for the design of flood and/or drought protection measures. As with all models that are calibrated to existing datasets, DWMs are subject to model error or uncertainty. In practice, the model error component of DWM <span class="hlt">predictions</span> is typically ignored yet DWM simulations which ignore model error produce model output which cannot reproduce the statistical properties of the observations they are intended to replicate. In the context of <span class="hlt">hydrologic</span> design, we demonstrate how ignoring model error can lead to systematic downward bias in flood quantiles, upward bias in drought quantiles and upward bias in water supply yields. By reincorporating model error, we document how DWM models can be used to generate results that mimic actual observations and preserve their statistical behavior. In addition to use of DWM for improved <span class="hlt">predictions</span> in a changing world, improved communication of the risk and reliability is also needed. Traditional statements of risk and reliability in <span class="hlt">hydrologic</span> design have been characterized by return periods, but such statements often assume that the annual probability of experiencing a design event remains constant throughout the project horizon. We document the general impact of nonstationarity on the average return period and reliability in the context of <span class="hlt">hydrologic</span> design. Our analyses reveal that return periods do not provide meaningful expressions of the likelihood of future <span class="hlt">hydrologic</span> events. Instead, knowledge of system reliability over future planning horizons can more effectively prepare society and communicate the likelihood</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017HESS...21.5477Y','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017HESS...21.5477Y"><span>Understanding and seasonal forecasting of <span class="hlt">hydrological</span> drought in the Anthropocene</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; Zhang, Miao; Wang, Linying; Zhou, Tian</p> <p>2017-11-01</p> <p><span class="hlt">Hydrological</span> drought is not only caused by natural hydroclimate variability but can also be directly altered by human interventions including reservoir operation, irrigation, groundwater exploitation, etc. Understanding and forecasting of <span class="hlt">hydrological</span> drought in the Anthropocene are grand challenges due to complicated interactions among climate, <span class="hlt">hydrology</span> and humans. In this paper, five decades (1961-2010) of naturalized and observed streamflow datasets are used to investigate <span class="hlt">hydrological</span> drought characteristics in a heavily managed river basin, the Yellow River basin in north China. Human interventions decrease the correlation between <span class="hlt">hydrological</span> and meteorological droughts, and make the <span class="hlt">hydrological</span> drought respond to longer timescales of meteorological drought. Due to large water consumptions in the middle and lower reaches, there are 118-262 % increases in the <span class="hlt">hydrological</span> drought frequency, up to 8-fold increases in the drought severity, 21-99 % increases in the drought duration and the drought onset is earlier. The non-stationarity due to anthropogenic climate change and human water use basically decreases the correlation between meteorological and <span class="hlt">hydrological</span> droughts and reduces the effect of human interventions on <span class="hlt">hydrological</span> drought frequency while increasing the effect on drought duration and severity. A set of 29-year (1982-2010) hindcasts from an established seasonal <span class="hlt">hydrological</span> forecasting system are used to assess the forecast skill of <span class="hlt">hydrological</span> drought. In the naturalized condition, the climate-model-based approach outperforms the climatology method in <span class="hlt">predicting</span> the 2001 severe <span class="hlt">hydrological</span> drought event. Based on the 29-year hindcasts, the former method has a Brier skill score of 11-26 % against the latter for the probabilistic <span class="hlt">hydrological</span> drought forecasting. In the Anthropocene, the skill for both approaches increases due to the dominant influence of human interventions that have been implicitly incorporated by the <span class="hlt">hydrological</span> post</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/2010WRR....46.9513W','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2010WRR....46.9513W"><span>Macroscale <span class="hlt">hydrologic</span> modeling of ecologically relevant flow metrics</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Wenger, Seth J.; Luce, Charles H.; Hamlet, Alan F.; Isaak, Daniel J.; Neville, Helen M.</p> <p>2010-09-01</p> <p>Stream <span class="hlt">hydrology</span> strongly affects the structure of aquatic communities. Changes to air temperature and precipitation driven by increased greenhouse gas concentrations are shifting timing and volume of streamflows potentially affecting these communities. The variable infiltration capacity (VIC) macroscale <span class="hlt">hydrologic</span> model has been employed at regional scales to describe and forecast <span class="hlt">hydrologic</span> changes but has been calibrated and applied mainly to large rivers. An important question is how well VIC runoff simulations serve to answer questions about <span class="hlt">hydrologic</span> changes in smaller streams, which are important habitat for many fish species. To answer this question, we aggregated gridded VIC outputs within the drainage basins of 55 streamflow gages in the Pacific Northwest United States and compared modeled hydrographs and summary metrics to observations. For most streams, several ecologically relevant aspects of the <span class="hlt">hydrologic</span> regime were accurately modeled, including center of flow timing, mean annual and summer flows and frequency of winter floods. Frequencies of high and low flows in the summer were not well <span class="hlt">predicted</span>, however. <span class="hlt">Predictions</span> were worse for sites with strong groundwater influence, and some sites showed errors that may result from limitations in the forcing climate data. Higher resolution (1/16th degree) modeling provided small improvements over lower resolution (1/8th degree). Despite some limitations, the VIC model appears capable of representing several ecologically relevant <span class="hlt">hydrologic</span> characteristics in streams, making it a useful tool for understanding the effects of <span class="hlt">hydrology</span> in delimiting species distributions and <span class="hlt">predicting</span> the potential effects of climate shifts on aquatic organisms.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017EGUGA..19.8329N','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017EGUGA..19.8329N"><span>Recent <span class="hlt">advances</span> in the multimodel <span class="hlt">hydrologic</span> ensemble forecasting using the HydroProg system in the Nysa Klodzka river basin (southwestern Poland)</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Niedzielski, Tomasz; Mizinski, Bartlomiej; Swierczynska-Chlasciak, Malgorzata</p> <p>2017-04-01</p> <p>The HydroProg system, the real-time multimodel <span class="hlt">hydrologic</span> ensemble system elaborated at the University of Wroclaw (Poland) in frame of the research grant no. 2011/01/D/ST10/04171 financed by National Science Centre of Poland, has been experimentally launched in 2013 in the Nysa Klodzka river basin (southwestern Poland). Since that time the system has been working operationally to provide water level <span class="hlt">predictions</span> in real time. At present, depending on a <span class="hlt">hydrologic</span> gauge, up to eight <span class="hlt">hydrologic</span> models are run. They are data- and physically-based solutions, with the majority of them being the data-based ones. The paper aims to report on the performance of the implementation of the HydroProg system for the basin in question. We focus on several high flows episodes and discuss the skills of the individual models in forecasting them. In addition, we present the performance of the multimodel ensemble solution. We also introduce a new prognosis which is determined in the following way: for a given lead time we select the most skillful <span class="hlt">prediction</span> (from the set of all individual models running at a given gauge and their multimodel ensemble) using the performance statistics computed operationally in real time as a function of lead time.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012EGUGA..14.5274A','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012EGUGA..14.5274A"><span>An operational <span class="hlt">hydrological</span> ensemble <span class="hlt">prediction</span> system for the city of Zurich (Switzerland): assessing the added value of probabilistic forecasts</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Addor, N.; Jaun, S.; Fundel, F.; Zappa, M.</p> <p>2012-04-01</p> <p>The Sihl River flows through Zurich, Switzerland's most populated city, for which it represents the largest flood threat. To anticipate extreme discharge events and provide decision support in case of flood risk, a hydrometeorological ensemble <span class="hlt">prediction</span> system (HEPS) was launched operationally in 2008. This model chain relies on deterministic (COSMO-7) and probabilistic (COSMO-LEPS) atmospheric forecasts, which are used to force a semi-distributed <span class="hlt">hydrological</span> model (PREVAH) coupled to a hydraulic model (FLORIS). The resulting <span class="hlt">hydrological</span> forecasts are eventually communicated to the stakeholders involved in the Sihl discharge management. This fully operational setting provides a real framework with which we assessed the potential of deterministic and probabilistic discharge forecasts for flood mitigation. To study the suitability of HEPS for small-scale basins and to quantify the added value conveyed by the probability information, a 31-month reforecast was produced for the Sihl catchment (336 km2). Several metrics support the conclusion that the performance gain is of up to 2 days lead time for the catchment considered. Brier skill scores show that probabilistic <span class="hlt">hydrological</span> forecasts outperform their deterministic counterparts for all the lead times and event intensities considered. The small size of the Sihl catchment does not prevent skillful discharge forecasts, but makes them particularly dependent on correct precipitation forecasts. Our evaluation stresses that the capacity of the model to provide confident and reliable mid-term probability forecasts for high discharges is limited. We finally highlight challenges for making decisions on the basis of <span class="hlt">hydrological</span> <span class="hlt">predictions</span>, and discuss the need for a tool to be used in addition to forecasts to compare the different mitigation actions possible in the Sihl catchment.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2001EOSTr..82..611B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2001EOSTr..82..611B"><span>Snow and Glacier <span class="hlt">Hydrology</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Brubaker, Kaye</p> <p></p> <p>The study of snow and ice is rich in both fundamental science and practical applications. Snow and Glacier <span class="hlt">Hydrology</span> offers something for everyone, from resource practitioners in regions where water supply depends on seasonal snow pack or glaciers, to research scientists seeking to understand the role of the solid phase in the water cycle and climate. The book is aimed at the <span class="hlt">advanced</span> undergraduate or graduate-level student. A perusal of online documentation for snow <span class="hlt">hydrology</span> classes suggests that there is currently no single text or reference book on this topic in general use. Instructors rely on chapters from general <span class="hlt">hydrology</span> texts or operational manuals, collections of journal papers, or their own notes. This variety reflects the fact that snow and ice regions differ in climate, topography, language, water law, hazards, and resource use (hydropower, irrigation, recreation). Given this diversity, producing a universally applicable book is a challenge.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2011HESSD...8..715A','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2011HESSD...8..715A"><span>An operational <span class="hlt">hydrological</span> ensemble <span class="hlt">prediction</span> system for the city of Zurich (Switzerland): skill, case studies and scenarios</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Addor, N.; Jaun, S.; Zappa, M.</p> <p>2011-01-01</p> <p>The Sihl River flows through Zurich, Switzerland's most populated city, for which it represents the largest flood threat. To anticipate extreme discharge events and provide decision support in case of flood risk, a hydrometeorological ensemble <span class="hlt">prediction</span> system (HEPS) was launched operationally in 2008. This models chain relies on limited-area atmospheric forecasts provided by the deterministic model COSMO-7 and the probabilistic model COSMO-LEPS. These atmospheric forecasts are used to force a semi-distributed <span class="hlt">hydrological</span> model (PREVAH), coupled to a hydraulic model (FLORIS). The resulting <span class="hlt">hydrological</span> forecasts are eventually communicated to the stakeholders involved in the Sihl discharge management. This fully operational setting provides a real framework to compare the potential of deterministic and probabilistic discharge forecasts for flood mitigation. To study the suitability of HEPS for small-scale basins and to quantify the added-value conveyed by the probability information, a reforecast was made for the period June 2007 to December 2009 for the Sihl catchment (336 km2). Several metrics support the conclusion that the performance gain can be of up to 2 days lead time for the catchment considered. Brier skill scores show that COSMO-LEPS-based <span class="hlt">hydrological</span> forecasts overall outperform their COSMO-7 based counterparts for all the lead times and event intensities considered. The small size of the Sihl catchment does not prevent skillful discharge forecasts, but makes them particularly dependent on correct precipitation forecasts, as shown by comparisons with a reference run driven by observed meteorological parameters. Our evaluation stresses that the capacity of the model to provide confident and reliable mid-term probability forecasts for high discharges is limited. The two most intense events of the study period are investigated utilising a novel graphical representation of probability forecasts and used to generate high discharge scenarios. They</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70037295','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70037295"><span>Tuning stochastic matrix models with <span class="hlt">hydrologic</span> data to <span class="hlt">predict</span> the population dynamics of a riverine fish</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Sakaris, P.C.; Irwin, E.R.</p> <p>2010-01-01</p> <p>We developed stochastic matrix models to evaluate the effects of <span class="hlt">hydrologic</span> alteration and variable mortality on the population dynamics of a lotie fish in a regulated river system. Models were applied to a representative lotic fish species, the flathead catfish (Pylodictis olivaris), for which two populations were examined: a native population from a regulated reach of the Coosa River (Alabama, USA) and an introduced population from an unregulated section of the Ocmulgee River (Georgia, USA). Size-classified matrix models were constructed for both populations, and residuals from catch-curve regressions were used as indices of year class strength (i.e., recruitment). A multiple regression model indicated that recruitment of flathead catfish in the Coosa River was positively related to the frequency of spring pulses between 283 and 566 m3/s. For the Ocmulgee River population, multiple regression models indicated that year class strength was negatively related to mean March discharge and positively related to June low flow. When the Coosa population was modeled to experience five consecutive years of favorable <span class="hlt">hydrologic</span> conditions during a 50-year projection period, it exhibited a substantial spike in size and increased at an overall 0.2% annual rate. When modeled to experience five years of unfavorable <span class="hlt">hydrologic</span> conditions, the Coosa population initially exhibited a decrease in size but later stabilized and increased at a 0.4% annual rate following the decline. When the Ocmulgee River population was modeled to experience five years of favorable conditions, it exhibited a substantial spike in size and increased at an overall 0.4% annual rate. After the Ocmulgee population experienced five years of unfavorable conditions, a sharp decline in population size was <span class="hlt">predicted</span>. However, the population quickly recovered, with population size increasing at a 0.3% annual rate following the decline. In general, stochastic population growth in the Ocmulgee River was more</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/20405801','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/20405801"><span>Tuning stochastic matrix models with <span class="hlt">hydrologic</span> data to <span class="hlt">predict</span> the population dynamics of a riverine fish.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Sakaris, Peter C; Irwin, Elise R</p> <p>2010-03-01</p> <p>We developed stochastic matrix models to evaluate the effects of <span class="hlt">hydrologic</span> alteration and variable mortality on the population dynamics of a lotic fish in a regulated river system. Models were applied to a representative lotic fish species, the flathead catfish (Pylodictis olivaris), for which two populations were examined: a native population from a regulated reach of the Coosa River (Alabama, USA) and an introduced population from an unregulated section of the Ocmulgee River (Georgia, USA). Size-classified matrix models were constructed for both populations, and residuals from catch-curve regressions were used as indices of year class strength (i.e., recruitment). A multiple regression model indicated that recruitment of flathead catfish in the Coosa River was positively related to the frequency of spring pulses between 283 and 566 m3/s. For the Ocmulgee River population, multiple regression models indicated that year class strength was negatively related to mean March discharge and positively related to June low flow. When the Coosa population was modeled to experience five consecutive years of favorable <span class="hlt">hydrologic</span> conditions during a 50-year projection period, it exhibited a substantial spike in size and increased at an overall 0.2% annual rate. When modeled to experience five years of unfavorable <span class="hlt">hydrologic</span> conditions, the Coosa population initially exhibited a decrease in size but later stabilized and increased at a 0.4% annual rate following the decline. When the Ocmulgee River population was modeled to experience five years of favorable conditions, it exhibited a substantial spike in size and increased at an overall 0.4% annual rate. After the Ocmulgee population experienced five years of unfavorable conditions, a sharp decline in population size was <span class="hlt">predicted</span>. However, the population quickly recovered, with population size increasing at a 0.3% annual rate following the decline. In general, stochastic population growth in the Ocmulgee River was more</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017JHyd..555..371A','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017JHyd..555..371A"><span>On the incidence of meteorological and <span class="hlt">hydrological</span> processors: Effect of resolution, sharpness and reliability of <span class="hlt">hydrological</span> ensemble forecasts</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Abaza, Mabrouk; Anctil, François; Fortin, Vincent; Perreault, Luc</p> <p>2017-12-01</p> <p>Meteorological and <span class="hlt">hydrological</span> ensemble <span class="hlt">prediction</span> systems are imperfect. Their outputs could often be improved through the use of a statistical processor, opening up the question of the necessity of using both processors (meteorological and <span class="hlt">hydrological</span>), only one of them, or none. This experiment compares the <span class="hlt">predictive</span> distributions from four <span class="hlt">hydrological</span> ensemble <span class="hlt">prediction</span> systems (H-EPS) utilising the Ensemble Kalman filter (EnKF) probabilistic sequential data assimilation scheme. They differ in the inclusion or not of the Distribution Based Scaling (DBS) method for post-processing meteorological forecasts and the ensemble Bayesian Model Averaging (ensemble BMA) method for <span class="hlt">hydrological</span> forecast post-processing. The experiment is implemented on three large watersheds and relies on the combination of two meteorological reforecast products: the 4-member Canadian reforecasts from the Canadian Centre for Meteorological and Environmental <span class="hlt">Prediction</span> (CCMEP) and the 10-member American reforecasts from the National Oceanic and Atmospheric Administration (NOAA), leading to 14 members at each time step. Results show that all four tested H-EPS lead to resolution and sharpness values that are quite similar, with an advantage to DBS + EnKF. The ensemble BMA is unable to compensate for any bias left in the precipitation ensemble forecasts. On the other hand, it succeeds in calibrating ensemble members that are otherwise under-dispersed. If reliability is preferred over resolution and sharpness, DBS + EnKF + ensemble BMA performs best, making use of both processors in the H-EPS system. Conversely, for enhanced resolution and sharpness, DBS is the preferred method.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFM.H42F..02M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFM.H42F..02M"><span>Panta Rhei: Global Perspectives on <span class="hlt">Hydrology</span>, Society and Change</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>McMillan, H. K.; Van Loon, A.; Mejia, A.; Liu, J.</p> <p>2016-12-01</p> <p>In 2013, the International Association of <span class="hlt">Hydrological</span> Sciences - IAHS - launched the <span class="hlt">hydrological</span> decade 2013-2022 with the theme `Panta Rhei: Change in <span class="hlt">Hydrology</span> and Society'. The decade recognises the urgency of <span class="hlt">hydrological</span> research to understand and <span class="hlt">predict</span> the interactions of society and water, to support sustainable water resource use under changing climatic and environmental conditions. This presentation provides an overview of the first three years of Panta Rhei, describing the scope, progress and future direction of the initiative. We provide a summary of the new science being undertaken by the 31 Panta Rhei working groups, demonstrating the views of the more than 400 members on the most pressing research questions and how the <span class="hlt">hydrological</span> community is progressing towards those goals. We draw out interconnections between different strands of research, and reflect on the need to take a global view on <span class="hlt">hydrology</span> in a world strongly impacted by humans and undergoing environmental change. There are many challenges associated with understanding and <span class="hlt">predicting</span> change in <span class="hlt">hydrology</span> and society, and empowering communities to mitigate and adapt to those changes. Such challenges can only be met by the concerted and joint efforts of hydrologists and affected societies around the world.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017JHyd..555..257V','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017JHyd..555..257V"><span>Estimating <span class="hlt">predictive</span> <span class="hlt">hydrological</span> uncertainty by dressing deterministic and ensemble forecasts; a comparison, with application to Meuse and Rhine</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Verkade, J. S.; Brown, J. D.; Davids, F.; Reggiani, P.; Weerts, A. H.</p> <p>2017-12-01</p> <p>Two statistical post-processing approaches for estimation of <span class="hlt">predictive</span> <span class="hlt">hydrological</span> uncertainty are compared: (i) 'dressing' of a deterministic forecast by adding a single, combined estimate of both <span class="hlt">hydrological</span> and meteorological uncertainty and (ii) 'dressing' of an ensemble streamflow forecast by adding an estimate of <span class="hlt">hydrological</span> uncertainty to each individual streamflow ensemble member. Both approaches aim to produce an estimate of the 'total uncertainty' that captures both the meteorological and <span class="hlt">hydrological</span> uncertainties. They differ in the degree to which they make use of statistical post-processing techniques. In the 'lumped' approach, both sources of uncertainty are lumped by post-processing deterministic forecasts using their verifying observations. In the 'source-specific' approach, the meteorological uncertainties are estimated by an ensemble of weather forecasts. These ensemble members are routed through a <span class="hlt">hydrological</span> model and a realization of the probability distribution of <span class="hlt">hydrological</span> uncertainties (only) is then added to each ensemble member to arrive at an estimate of the total uncertainty. The techniques are applied to one location in the Meuse basin and three locations in the Rhine basin. Resulting forecasts are assessed for their reliability and sharpness, as well as compared in terms of multiple verification scores including the relative mean error, Brier Skill Score, Mean Continuous Ranked Probability Skill Score, Relative Operating Characteristic Score and Relative Economic Value. The dressed deterministic forecasts are generally more reliable than the dressed ensemble forecasts, but the latter are sharper. On balance, however, they show similar quality across a range of verification metrics, with the dressed ensembles coming out slightly better. Some additional analyses are suggested. Notably, these include statistical post-processing of the meteorological forecasts in order to increase their reliability, thus increasing the reliability</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017EGUGA..1917716H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017EGUGA..1917716H"><span>Benchmarking Ensemble Streamflow <span class="hlt">Prediction</span> Skill in the UK</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Harrigan, Shaun; Smith, Katie; Parry, Simon; Tanguy, Maliko; Prudhomme, Christel</p> <p>2017-04-01</p> <p> increasing complexity were produced, including better model representation of <span class="hlt">hydrological</span> processes and sub-sampling of historic climate sequences (e.g. NAO+/NAO- years). This work is part of the Improving <span class="hlt">Predictions</span> of Drought for User Decision Making (IMPETUS) project and provides insight to where <span class="hlt">advancements</span> in atmospheric <span class="hlt">predictability</span> is most needed in the UK in the context of water management.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014EGUGA..16.8615R','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014EGUGA..16.8615R"><span>A radar-based <span class="hlt">hydrological</span> model for flash flood <span class="hlt">prediction</span> in the dry regions of Israel</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Ronen, Alon; Peleg, Nadav; Morin, Efrat</p> <p>2014-05-01</p> <p>Flash floods are floods which follow shortly after rainfall events, and are among the most destructive natural disasters that strike people and infrastructures in humid and arid regions alike. Using a <span class="hlt">hydrological</span> model for the <span class="hlt">prediction</span> of flash floods in gauged and ungauged basins can help mitigate the risk and damage they cause. The sparsity of rain gauges in arid regions requires the use of radar measurements in order to get reliable quantitative precipitation estimations (QPE). While many <span class="hlt">hydrological</span> models use radar data, only a handful do so in dry climate. This research presents a robust radar-based hydro-meteorological model built specifically for dry climate. Using this model we examine the governing factors of flash floods in the arid and semi-arid regions of Israel in particular and in dry regions in general. The <span class="hlt">hydrological</span> model built is a semi-distributed, physically-based model, which represents the main <span class="hlt">hydrological</span> processes in the area, namely infiltration, flow routing and transmission losses. Three infiltration functions were examined - Initial & Constant, SCS-CN and Green&Ampt. The parameters for each function were found by calibration based on 53 flood events in three catchments, and validation was performed using 55 flood events in six catchments. QPE were obtained from a C-band weather radar and adjusted using a weighted multiple regression method based on a rain gauge network. Antecedent moisture conditions were calculated using a daily recharge assessment model (DREAM). We found that the SCS-CN infiltration function performed better than the other two, with reasonable agreement between calculated and measured peak discharge. Effects of storm characteristics were studied using synthetic storms from a high resolution weather generator (HiReS-WG), and showed a strong correlation between storm speed, storm direction and rain depth over desert soils to flood volume and peak discharge.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016WRR....52..954F','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016WRR....52..954F"><span>From spatially variable streamflow to distributed <span class="hlt">hydrological</span> models: Analysis of key modeling decisions</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Fenicia, Fabrizio; Kavetski, Dmitri; Savenije, Hubert H. G.; Pfister, Laurent</p> <p>2016-02-01</p> <p>This paper explores the development and application of distributed <span class="hlt">hydrological</span> models, focusing on the key decisions of how to discretize the landscape, which model structures to use in each landscape element, and how to link model parameters across multiple landscape elements. The case study considers the Attert catchment in Luxembourg—a 300 km2 mesoscale catchment with 10 nested subcatchments that exhibit clearly different streamflow dynamics. The research questions are investigated using conceptual models applied at <span class="hlt">hydrologic</span> response unit (HRU) scales (1-4 HRUs) on 6 hourly time steps. Multiple model structures are hypothesized and implemented using the SUPERFLEX framework. Following calibration, space/time model transferability is tested using a split-sample approach, with evaluation criteria including streamflow <span class="hlt">prediction</span> error metrics and <span class="hlt">hydrological</span> signatures. Our results suggest that: (1) models using geology-based HRUs are more robust and capture the spatial variability of streamflow time series and signatures better than models using topography-based HRUs; this finding supports the hypothesis that, in the Attert, geology exerts a stronger control than topography on streamflow generation, (2) streamflow dynamics of different HRUs can be represented using distinct and remarkably simple model structures, which can be interpreted in terms of the perceived dominant <span class="hlt">hydrologic</span> processes in each geology type, and (3) the same maximum root zone storage can be used across the three dominant geological units with no loss in model transferability; this finding suggests that the partitioning of water between streamflow and evaporation in the study area is largely independent of geology and can be used to improve model parsimony. The modeling methodology introduced in this study is general and can be used to <span class="hlt">advance</span> our broader understanding and <span class="hlt">prediction</span> of <span class="hlt">hydrological</span> behavior, including the landscape characteristics that control <span class="hlt">hydrologic</span> response, the</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/pages/biblio/1286697-hydrologic-filtering-fish-life-history-strategies-across-united-states-implications-stream-flow-alteration','SCIGOV-DOEP'); return false;" href="https://www.osti.gov/pages/biblio/1286697-hydrologic-filtering-fish-life-history-strategies-across-united-states-implications-stream-flow-alteration"><span><span class="hlt">Hydrologic</span> filtering of fish life history strategies across the United States: implications for stream flow alteration</span></a></p> <p><a target="_blank" href="http://www.osti.gov/pages">DOE PAGES</a></p> <p>McManamay, Ryan A.; Frimpong, Emmanuel A.</p> <p>2015-01-01</p> <p>Lotic fish have developed life history strategies adapted to the natural variation in stream flow regimes. The natural timing, duration, and magnitude of flow events has contributed to the diversity, production, and composition of fish assemblages over time. Studies evaluating the role of <span class="hlt">hydrology</span> in structuring fish assemblages have been more common at the local or regional scale with very few studies conducted at the continental scale. Furthermore, quantitative linkages between natural <span class="hlt">hydrologic</span> patterns and fish assemblages are rarely used to make <span class="hlt">predictions</span> of ecological consequences of <span class="hlt">hydrologic</span> alterations. We ask two questions: (1) what is the relative role ofmore » <span class="hlt">hydrology</span> in structuring fish assemblages at large scales? and (2) can relationships between fish assemblages and natural <span class="hlt">hydrology</span> be utilized to <span class="hlt">predict</span> fish assemblage responses to <span class="hlt">hydrologic</span> disturbance? We developed models to relate fish life histories and reproductive strategies to landscape and <span class="hlt">hydrologic</span> variables separately and then combined. Models were then used to <span class="hlt">predict</span> the ecological consequences of altered <span class="hlt">hydrology</span> due to dam regulation. Although <span class="hlt">hydrology</span> plays a considerable role in structuring fish assemblages, the performance of models using only <span class="hlt">hydrologic</span> variables was lower than that of models constructed using landscape variables. Isolating the relative importance of <span class="hlt">hydrology</span> in structuring fish assemblages at the continental scale is difficult since <span class="hlt">hydrology</span> is interrelated to many landscape factors. By applying models to dam-regulated <span class="hlt">hydrologic</span> data, we observed some consistent <span class="hlt">predicted</span> responses in fish life history strategies and modes of reproduction. In agreement with existing literature, equilibrium strategists are <span class="hlt">predicted</span> to increase following dam regulation, whereas opportunistic and periodic species are <span class="hlt">predicted</span> to decrease. In addition, dam regulation favors the selection of reproductive strategies with extended spawning seasons and preference for</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/servlets/purl/1286697','SCIGOV-STC'); return false;" href="https://www.osti.gov/servlets/purl/1286697"><span><span class="hlt">Hydrologic</span> filtering of fish life history strategies across the United States: implications for stream flow alteration</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>McManamay, Ryan A.; Frimpong, Emmanuel A.</p> <p></p> <p>Lotic fish have developed life history strategies adapted to the natural variation in stream flow regimes. The natural timing, duration, and magnitude of flow events has contributed to the diversity, production, and composition of fish assemblages over time. Studies evaluating the role of <span class="hlt">hydrology</span> in structuring fish assemblages have been more common at the local or regional scale with very few studies conducted at the continental scale. Furthermore, quantitative linkages between natural <span class="hlt">hydrologic</span> patterns and fish assemblages are rarely used to make <span class="hlt">predictions</span> of ecological consequences of <span class="hlt">hydrologic</span> alterations. We ask two questions: (1) what is the relative role ofmore » <span class="hlt">hydrology</span> in structuring fish assemblages at large scales? and (2) can relationships between fish assemblages and natural <span class="hlt">hydrology</span> be utilized to <span class="hlt">predict</span> fish assemblage responses to <span class="hlt">hydrologic</span> disturbance? We developed models to relate fish life histories and reproductive strategies to landscape and <span class="hlt">hydrologic</span> variables separately and then combined. Models were then used to <span class="hlt">predict</span> the ecological consequences of altered <span class="hlt">hydrology</span> due to dam regulation. Although <span class="hlt">hydrology</span> plays a considerable role in structuring fish assemblages, the performance of models using only <span class="hlt">hydrologic</span> variables was lower than that of models constructed using landscape variables. Isolating the relative importance of <span class="hlt">hydrology</span> in structuring fish assemblages at the continental scale is difficult since <span class="hlt">hydrology</span> is interrelated to many landscape factors. By applying models to dam-regulated <span class="hlt">hydrologic</span> data, we observed some consistent <span class="hlt">predicted</span> responses in fish life history strategies and modes of reproduction. In agreement with existing literature, equilibrium strategists are <span class="hlt">predicted</span> to increase following dam regulation, whereas opportunistic and periodic species are <span class="hlt">predicted</span> to decrease. In addition, dam regulation favors the selection of reproductive strategies with extended spawning seasons and preference for</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014AGUFM.H52F..01C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014AGUFM.H52F..01C"><span>Assessment of <span class="hlt">Hydrologic</span> Response to Variable Precipitation Forcing: Russian River Case Study</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Cifelli, R.; Hsu, C.; Johnson, L. E.</p> <p>2014-12-01</p> <p>NOAA Hydrometeorology Testbed (HMT) activities in California have involved deployment of <span class="hlt">advanced</span> sensor networks to better track atmospheric river (AR) dynamics and inland penetration of high water vapor air masses. Numerical weather <span class="hlt">prediction</span> models and decision support tools have been developed to provide forecasters a better basis for forecasting heavy precipitation and consequent flooding. The HMT also involves a joint project with California Department of Water Resources (CA-DWR) and the Scripps Institute for Oceanography (SIO) as part of CA-DWR's Enhanced Flood Response and Emergency Preparedness (EFREP) program. The HMT activities have included development and calibration of a distributed <span class="hlt">hydrologic</span> model, the NWS Office of <span class="hlt">Hydrologic</span> Development's (OHD) Research Distributed <span class="hlt">Hydrologic</span> Model (RDHM), to prototype the distributed approach for flood and other water resources applications. HMT has applied RDHM to the Russian-Napa watersheds for research assessment of gap-filling weather radars for precipitation and <span class="hlt">hydrologic</span> forecasting and for establishing a prototype to inform both the NWS Monterey Forecast Office and the California Nevada River Forecast Center (CNRFC) of RDHM capabilities. In this presentation, a variety of precipitation forcings generated with and without gap filling radar and rain gauge data are used as input to RDHM to assess the <span class="hlt">hydrologic</span> response for selected case study events. Both the precipitation forcing and <span class="hlt">hydrologic</span> model are run at different spatial and temporal resolution in order to examine the sensitivity of runoff to the precipitation inputs. Based on the timing of the events and the variations of spatial and temporal resolution, the parameters which dominate the <span class="hlt">hydrologic</span> response are identified. The assessment is implemented at two USGS stations (Ukiah near Russian River and Austin Creek near Cazadero) that are minimally influenced by managed flows and objective evaluation can thus be derived. The results are assessed</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/biblio/1159415-quantifying-generalizing-hydrologic-responses-dam-regulation-using-statistical-modeling-approach','SCIGOV-STC'); return false;" href="https://www.osti.gov/biblio/1159415-quantifying-generalizing-hydrologic-responses-dam-regulation-using-statistical-modeling-approach"><span>Quantifying and Generalizing <span class="hlt">Hydrologic</span> Responses to Dam Regulation using a Statistical Modeling Approach</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>McManamay, Ryan A</p> <p>2014-01-01</p> <p>Despite the ubiquitous existence of dams within riverscapes, much of our knowledge about dams and their environmental effects remains context-specific. <span class="hlt">Hydrology</span>, more than any other environmental variable, has been studied in great detail with regard to dam regulation. While much progress has been made in generalizing the <span class="hlt">hydrologic</span> effects of regulation by large dams, many aspects of <span class="hlt">hydrology</span> show site-specific fidelity to dam operations, small dams (including diversions), and regional <span class="hlt">hydrologic</span> regimes. A statistical modeling framework is presented to quantify and generalize <span class="hlt">hydrologic</span> responses to varying degrees of dam regulation. Specifically, the objectives were to 1) compare the effects ofmore » local versus cumulative dam regulation, 2) determine the importance of different regional <span class="hlt">hydrologic</span> regimes in influencing <span class="hlt">hydrologic</span> responses to dams, and 3) evaluate how different regulation contexts lead to error in <span class="hlt">predicting</span> <span class="hlt">hydrologic</span> responses to dams. Overall, model performance was poor in quantifying the magnitude of <span class="hlt">hydrologic</span> responses, but performance was sufficient in classifying <span class="hlt">hydrologic</span> responses as negative or positive. Responses of some <span class="hlt">hydrologic</span> indices to dam regulation were highly dependent upon <span class="hlt">hydrologic</span> class membership and the purpose of the dam. The opposing coefficients between local and cumulative-dam predictors suggested that <span class="hlt">hydrologic</span> responses to cumulative dam regulation are complex, and <span class="hlt">predicting</span> the <span class="hlt">hydrology</span> downstream of individual dams, as opposed to multiple dams, may be more easy accomplished using statistical approaches. Results also suggested that particular contexts, including multipurpose dams, high cumulative regulation by multiple dams, diversions, close proximity to dams, and certain <span class="hlt">hydrologic</span> classes are all sources of increased error when <span class="hlt">predicting</span> <span class="hlt">hydrologic</span> responses to dams. Statistical models, such as the ones presented herein, show promise in their ability to model the effects of dam regulation effects</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.fs.usda.gov/treesearch/pubs/43664','TREESEARCH'); return false;" href="https://www.fs.usda.gov/treesearch/pubs/43664"><span>Influence of forest roads standards and networks on water yield as <span class="hlt">predicted</span> by the distributed <span class="hlt">hydrology</span>-soil-vegetation model</span></a></p> <p><a target="_blank" href="http://www.fs.usda.gov/treesearch/">Treesearch</a></p> <p>Salli F. Dymond; W. Michael Aust; Steven P. Prisley; Mark H. Eisenbies; James M. Vose</p> <p>2013-01-01</p> <p>Throughout the country, foresters are continually looking at the effects of logging and forest roads on stream discharge and overall stream health. In the Pacific Northwest, a distributed <span class="hlt">hydrology</span>-soil-vegetation model (DHSVM) has been used to <span class="hlt">predict</span> the effects of logging on peak discharge in mountainous regions. DHSVM uses elevation, meteorological, vegetation, and...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013AGUFM.H21J1196S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013AGUFM.H21J1196S"><span>Uncertainty in <span class="hlt">Predicted</span> Neighborhood-Scale Green Stormwater Infrastructure Performance Informed by field monitoring of <span class="hlt">Hydrologic</span> Abstractions</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Smalls-Mantey, L.; Jeffers, S.; Montalto, F. A.</p> <p>2013-12-01</p> <p>Human alterations to the environment provide infrastructure for housing and transportation but have drastically changed local <span class="hlt">hydrology</span>. Excess stormwater runoff from impervious surfaces generates erosion, overburdens sewer infrastructure, and can pollute receiving bodies. Increased attention to green stormwater management controls is based on the premise that some of these issues can be mitigated by capturing or slowing the flow of stormwater. However, our ability to <span class="hlt">predict</span> actual green infrastructure facility performance using physical or statistical methods needs additional validation, and efforts to incorporate green infrastructure controls into <span class="hlt">hydrologic</span> models are still in their infancy stages. We use more than three years of field monitoring data to derive facility specific probability density functions characterizing the <span class="hlt">hydrologic</span> abstractions provided by a stormwater treatment wetland, streetside bioretention facility, and a green roof. The monitoring results are normalized by impervious area treated, and incorporated into a neighborhood-scale agent model allowing probabilistic comparisons of the stormwater capture outcomes associated with alternative urban greening scenarios. Specifically, we compare the uncertainty introduced into the model by facility performance (as represented by the variability in the abstraction), to that introduced by both precipitation variability, and spatial patterns of emergence of different types of green infrastructure. The modeling results are used to update a discussion about the potential effectiveness of urban green infrastructure implementation plans.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://eric.ed.gov/?q=HUMAN+AND+RESOURCE+AND+MANAGEMENT+AND+JOB&pg=4&id=EJ961639','ERIC'); return false;" href="https://eric.ed.gov/?q=HUMAN+AND+RESOURCE+AND+MANAGEMENT+AND+JOB&pg=4&id=EJ961639"><span><span class="hlt">Predicting</span> Career <span class="hlt">Advancement</span> with Structural Equation Modelling</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>Heimler, Ronald; Rosenberg, Stuart; Morote, Elsa-Sofia</p> <p>2012-01-01</p> <p>Purpose: The purpose of this paper is to use the authors' prior findings concerning basic employability skills in order to determine which skills best <span class="hlt">predict</span> career <span class="hlt">advancement</span> potential. Design/methodology/approach: Utilizing survey responses of human resource managers, the employability skills showing the largest relationships to career…</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/2014AGUFMED54A3508M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014AGUFMED54A3508M"><span>Integrating local research watersheds into <span class="hlt">hydrologic</span> education: Lessons from the Dry Creek Experimental Watershed</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>McNamara, J. P.; Aishlin, P. S.; Flores, A. N.; Benner, S. G.; Marshall, H. P.; Pierce, J. L.</p> <p>2014-12-01</p> <p>While a proliferation of instrumented research watersheds and new data sharing technologies has transformed <span class="hlt">hydrologic</span> research in recent decades, similar <span class="hlt">advances</span> have not been realized in <span class="hlt">hydrologic</span> education. Long-standing problems in <span class="hlt">hydrologic</span> education include discontinuity of <span class="hlt">hydrologic</span> topics from introductory to <span class="hlt">advanced</span> courses, inconsistency of content across academic departments, and difficulties in development of laboratory and homework assignments utilizing large time series and spatial data sets. <span class="hlt">Hydrologic</span> problems are typically not amenable to "back-of-the-chapter" examples. Local, long-term research watersheds offer solutions to these problems. Here, we describe our integration of research and monitoring programs in the Dry Creek Experimental Watershed into undergraduate and graduate <span class="hlt">hydrology</span> programs at Boise State University. We developed a suite of watershed-based exercises into courses and curriculums using real, tangible datasets from the watershed to teach concepts not amenable to traditional textbook and lecture methods. The aggregation of exercises throughout a course or degree allows for scaffolding of concepts with progressive exposure of <span class="hlt">advanced</span> concepts throughout a course or degree. The need for exercises of this type is growing as traditional lecture-based classes (passive learning from a local authoritative source) are being replaced with active learning courses that integrate many sources of information through situational factors.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.fs.usda.gov/treesearch/pubs/33822','TREESEARCH'); return false;" href="https://www.fs.usda.gov/treesearch/pubs/33822"><span><span class="hlt">Advancing</span> the science of Forest <span class="hlt">Hydrology</span></span></a></p> <p><a target="_blank" href="http://www.fs.usda.gov/treesearch/">Treesearch</a></p> <p>Devendra M. Amatya; R. Wayne Skaggs; Carl C. Trettin</p> <p>2009-01-01</p> <p>For more than a century, agricultural and biological engineers have provided major <span class="hlt">advances</span> in science, engineering, and technology to increase food and fiber production to meet the demands of a rapidly growing global population. The land base for these technological <span class="hlt">advances</span> has...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFM.H51P..01L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFM.H51P..01L"><span>Study of <span class="hlt">hydrological</span> extremes - floods and droughts in global river basins using satellite data and model output</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Lakshmi, V.; Fayne, J.; Bolten, J. D.</p> <p>2016-12-01</p> <p>We will use satellite data from TRMM (Tropical Rainfall Measurement Mission), AMSR (<span class="hlt">Advanced</span> Microwave Scanning Radiometer), GRACE (Gravity Recovery and Climate Experiment) and MODIS (Moderate Resolution Spectroradiometer) and model output from NASA GLDAS (Global Land Data Assimilation System) to understand the linkages between <span class="hlt">hydrological</span> variables. These <span class="hlt">hydrological</span> variables include precipitation soil moisture vegetation index surface temperature ET and total water. We will present results for major river basins such as Amazon, Colorado, Mississippi, California, Danube, Nile, Congo, Yangtze Mekong, Murray-Darling and Ganga-Brahmaputra.The major floods and droughts in these watersheds will be mapped in time and space using the satellite data and model outputs mentioned above. We will analyze the various <span class="hlt">hydrological</span> variables and conduct a synergistic study during times of flood and droughts. In order to compare <span class="hlt">hydrological</span> variables between river basins with vastly different climate and land use we construct an index that is scaled by the climatology. This allows us to compare across different climate, topography, soils and land use regimes. The analysis shows that the <span class="hlt">hydrological</span> variables derived from satellite data and NASA models clearly reflect the <span class="hlt">hydrological</span> extremes. This is especially true when data from different sensors are analyzed together - for example rainfall data from TRMM and total water data from GRACE. Such analyses will help to construct <span class="hlt">prediction</span> tools for water resources applications.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFM.H21B1447E','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFM.H21B1447E"><span>Modeling post-wildfire <span class="hlt">hydrological</span> processes with ParFlow</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Escobar, I. S.; Lopez, S. R.; Kinoshita, A. M.</p> <p>2017-12-01</p> <p>Wildfires alter the natural processes within a watershed, such as surface runoff, evapotranspiration rates, and subsurface water storage. Post-fire <span class="hlt">hydrologic</span> models are typically one-dimensional, empirically-based models or two-dimensional, conceptually-based models with lumped parameter distributions. These models are useful for modeling and <span class="hlt">predictions</span> at the watershed outlet; however, do not provide detailed, distributed <span class="hlt">hydrologic</span> processes at the point scale within the watershed. This research uses ParFlow, a three-dimensional, distributed <span class="hlt">hydrologic</span> model to simulate post-fire <span class="hlt">hydrologic</span> processes by representing the spatial and temporal variability of soil burn severity (via hydrophobicity) and vegetation recovery. Using this approach, we are able to evaluate the change in post-fire water components (surface flow, lateral flow, baseflow, and evapotranspiration). This work builds upon previous field and remote sensing analysis conducted for the 2003 Old Fire Burn in Devil Canyon, located in southern California (USA). This model is initially developed for a hillslope defined by a 500 m by 1000 m lateral extent. The subsurface reaches 12.4 m and is assigned a variable cell thickness to explicitly consider soil burn severity throughout the stages of recovery and vegetation regrowth. We consider four slope and eight hydrophobic layer configurations. Evapotranspiration is used as a proxy for vegetation regrowth and is represented by the satellite-based Simplified Surface Energy Balance (SSEBOP) product. The pre- and post-fire surface runoff, subsurface storage, and surface storage interactions are evaluated at the point scale. Results will be used as a basis for developing and fine-tuning a watershed-scale model. Long-term simulations will <span class="hlt">advance</span> our understanding of post-fire <span class="hlt">hydrological</span> partitioning between water balance components and the spatial variability of watershed processes, providing improved guidance for post-fire watershed management. In reference</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016EGUGA..1813385M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016EGUGA..1813385M"><span>Towards real-time assimilation of crowdsourced observations in <span class="hlt">hydrological</span> modeling</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Mazzoleni, Maurizio; Verlaan, Martin; Alfonso, Leonardo; Norbiato, Daniele; Monego, Martina; Ferri, Michele; Solomatine, Dimitri</p> <p>2016-04-01</p> <p>The continued technological <span class="hlt">advances</span> have stimulated the spread of low-cost sensors that can be used by citizens to provide crowdsourced observations (CO) of different <span class="hlt">hydrological</span> variables. An example of such low-cost sensors is a staff gauge connected to a QR code on which people can read the water level indication and send the measurement via a mobile phone application. The goal of this study is to assess the combined effect of the assimilation of CO coming from a distributed network of low-cost sensors, and the existing streamflow observations from physical sensors, on the performance of a semi-distributed <span class="hlt">hydrological</span> model. The methodology is applied to the Bacchiglione catchment, North East of Italy, where an early warning system is used by the Alto Adriatico Water Authority to issue forecasted water level along the river network which cross important cities such as Vicenza and Padua. In this study, forecasted precipitation values are used as input in the <span class="hlt">hydrological</span> model to estimate the simulated streamflow hydrograph used as boundary condition for the hydraulic model. Observed precipitation values are used to generate realistic synthetic streamflow values with various characteristics of arrival frequency and accuracy, to simulate CO coming at irregular time steps. These observations are assimilated into the semi-distributed model using a Kalman filter based method. The results of this study show that CO, asynchronous in time and with variable accuracy, can still improve flood <span class="hlt">prediction</span> when integrated in <span class="hlt">hydrological</span> models. When both physical and low-cost sensors are located at the same places, the assimilation of CO gives the same model improvement than the assimilation of physical observations only for high number of non-intermittent sensors. However, the integration of observations from low-cost sensors and single physical sensors can improve the flood <span class="hlt">prediction</span> even when small a number of intermittent CO are available. This study is part of the</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2011JHyd..403..186L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2011JHyd..403..186L"><span>Grid computing technology for <span class="hlt">hydrological</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>Lecca, G.; Petitdidier, M.; Hluchy, L.; Ivanovic, M.; Kussul, N.; Ray, N.; Thieron, V.</p> <p>2011-06-01</p> <p>Summary<span class="hlt">Advances</span> in e-Infrastructure promise to revolutionize sensing systems and the way in which data are collected and assimilated, and complex water systems are simulated and visualized. According to the EU Infrastructure 2010 work-programme, data and compute infrastructures and their underlying technologies, either oriented to tackle scientific challenges or complex problem solving in engineering, are expected to converge together into the so-called knowledge infrastructures, leading to a more effective research, education and innovation in the next decade and beyond. Grid technology is recognized as a fundamental component of e-Infrastructures. Nevertheless, this emerging paradigm highlights several topics, including data management, algorithm optimization, security, performance (speed, throughput, bandwidth, etc.), and scientific cooperation and collaboration issues that require further examination to fully exploit it and to better inform future research policies. The paper illustrates the results of six different surface and subsurface <span class="hlt">hydrology</span> applications that have been deployed on the Grid. All the applications aim to answer to strong requirements from the Civil Society at large, relatively to natural and anthropogenic risks. Grid technology has been successfully tested to improve flood <span class="hlt">prediction</span>, groundwater resources management and Black Sea <span class="hlt">hydrological</span> survey, by providing large computing resources. It is also shown that Grid technology facilitates e-cooperation among partners by means of services for authentication and authorization, seamless access to distributed data sources, data protection and access right, and standardization.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014AGUFMED54A3505A','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014AGUFMED54A3505A"><span>An Educational Model for Hands-On <span class="hlt">Hydrology</span> Education</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>AghaKouchak, A.; Nakhjiri, N.; Habib, E. H.</p> <p>2014-12-01</p> <p>This presentation provides an overview of a hands-on modeling tool developed for students in civil engineering and earth science disciplines to help them learn the fundamentals of <span class="hlt">hydrologic</span> processes, model calibration, sensitivity analysis, uncertainty assessment, and practice conceptual thinking in solving engineering problems. The toolbox includes two simplified <span class="hlt">hydrologic</span> models, namely HBV-EDU and HBV-Ensemble, designed as a complement to theoretical <span class="hlt">hydrology</span> lectures. The models provide an interdisciplinary application-oriented learning environment that introduces the <span class="hlt">hydrologic</span> phenomena through the use of a simplified conceptual <span class="hlt">hydrologic</span> model. The toolbox can be used for in-class lab practices and homework assignments, and assessment of students' understanding of <span class="hlt">hydrological</span> processes. Using this modeling toolbox, students can gain more insights into how <span class="hlt">hydrological</span> processes (e.g., precipitation, snowmelt and snow accumulation, soil moisture, evapotranspiration and runoff generation) are interconnected. The educational toolbox includes a MATLAB Graphical User Interface (GUI) and an ensemble simulation scheme that can be used for teaching more <span class="hlt">advanced</span> topics including uncertainty analysis, and ensemble simulation. Both models have been administered in a class for both in-class instruction and a final project, and students submitted their feedback about the toolbox. The results indicate that this educational software had a positive impact on students understanding and knowledge of <span class="hlt">hydrology</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/24569270','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/24569270"><span>Green roof <span class="hlt">hydrologic</span> performance and modeling: a review.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Li, Yanling; Babcock, Roger W</p> <p>2014-01-01</p> <p>Green roofs reduce runoff from impervious surfaces in urban development. This paper reviews the technical literature on green roof <span class="hlt">hydrology</span>. Laboratory experiments and field measurements have shown that green roofs can reduce stormwater runoff volume by 30 to 86%, reduce peak flow rate by 22 to 93% and delay the peak flow by 0 to 30 min and thereby decrease pollution, flooding and erosion during precipitation events. However, the effectiveness can vary substantially due to design characteristics making performance <span class="hlt">predictions</span> difficult. Evaluation of the most recently published study findings indicates that the major factors affecting green roof <span class="hlt">hydrology</span> are precipitation volume, precipitation dynamics, antecedent conditions, growth medium, plant species, and roof slope. This paper also evaluates the computer models commonly used to simulate <span class="hlt">hydrologic</span> processes for green roofs, including stormwater management model, soil water atmosphere and plant, SWMS-2D, HYDRUS, and other models that are shown to be effective for <span class="hlt">predicting</span> precipitation response and economic benefits. The review findings indicate that green roofs are effective for reduction of runoff volume and peak flow, and delay of peak flow, however, no tool or model is available to <span class="hlt">predict</span> expected performance for any given anticipated system based on design parameters that directly affect green roof <span class="hlt">hydrology</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017EGUGA..1919260S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017EGUGA..1919260S"><span>From Engineering <span class="hlt">Hydrology</span> to Earth System Science: Milestones in the Transformation of <span class="hlt">Hydrologic</span> Science (Alfred Wegener Medal Lecture)</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Sivapalan, Murugesu</p> <p>2017-04-01</p> <p><span class="hlt">Hydrologic</span> science has undergone almost transformative changes over the past 50 years. Huge strides have been made in the transition from early empirical approaches to rigorous approaches based on the fluid mechanics of water movement on and below the land surface. However, further progress has been hampered by problems posed by the presence of heterogeneity, especially subsurface heterogeneity, at all scales. The inability to measure or map subsurface heterogeneity everywhere prevented further development of balance equations and associated closure relations at the scales of interest, and has led to the virtual impasse we are presently in, in terms of development of physically based models needed for <span class="hlt">hydrologic</span> <span class="hlt">predictions</span>. An alternative to the mapping of subsurface heterogeneity everywhere is a new earth system science view, which sees the heterogeneity as the end result of co-evolutionary <span class="hlt">hydrological</span>, geomorphological, ecological and pedological processes, each operating at a different rate, which have helped to shape the landscapes that we see in nature, including the heterogeneity below that we do not see. The expectation is that instead of specifying exact details of the heterogeneity in our models, we can replace it, without loss of information, with the ecosystem function they perform. Guided by this new earth system science perspective, development of <span class="hlt">hydrologic</span> science is now guided by altogether new questions and new approaches to address them, compared to the purely physical, fluid mechanics based approaches that we inherited from the past. In the emergent Anthropocene, the co-evolutionary view is expanded further to involve interactions and feedbacks with human-social processes as well. In this lecture, I will present key milestones in the transformation of <span class="hlt">hydrologic</span> science from Engineering <span class="hlt">Hydrology</span> to Earth System Science, and what this means for <span class="hlt">hydrologic</span> observations, theory development and <span class="hlt">predictions</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017WRR....53.2972M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017WRR....53.2972M"><span>Hyphenated <span class="hlt">hydrology</span>: Interdisciplinary evolution of water resource science</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>McCurley, Kathryn L.; Jawitz, James W.</p> <p>2017-04-01</p> <p><span class="hlt">Hydrology</span> has <span class="hlt">advanced</span> considerably as a scientific discipline since its recognized inception in the mid-twentieth century. Modern water resource related questions have forced adaptation from exclusively physical or engineering science viewpoints toward a deliberate interdisciplinary context. Over the past few decades, many of the eventual manifestations of this evolution were foreseen by prominent expert hydrologists. However, their narrative descriptions have lacked substantial quantification. This study addressed that gap by measuring the prevalence of and analyzing the relationships between the terms most frequently used by hydrologists to define and describe their research. We analyzed 16,591 journal article titles from 1965-2015 in Water Resources Research, through which the scientific dialogue and its time-sensitive progression emerged. Our word frequency and term cooccurrence network results revealed the dynamic timing of the lateral movement of <span class="hlt">hydrology</span> across multiple disciplines as well as the deepening of scientific discourse with respect to traditional <span class="hlt">hydrologic</span> questions. The conversation among water resource scientists surrounding the <span class="hlt">hydrologic</span> subdisciplines of catchment-<span class="hlt">hydrology</span>, hydro-meteorology, socio-<span class="hlt">hydrology</span>, hydro-climatology, and eco-<span class="hlt">hydrology</span> gained statistically significant momentum in the analyzed time period, while that of hydro-geology and contaminant-<span class="hlt">hydrology</span> experienced periods of increase followed by significant decline. This study concludes that formerly exotic disciplines can potentially modify <span class="hlt">hydrology</span>, prompting new insights and inspiring unconventional perspectives on old questions that may have otherwise become obsolete.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014SGeo...35..491R','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014SGeo...35..491R"><span>Review of Understanding of Earth's <span class="hlt">Hydrological</span> Cycle: Observations, Theory and Modelling</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Rast, Michael; Johannessen, Johnny; Mauser, Wolfram</p> <p>2014-05-01</p> <p>Water is our most precious and arguably most undervalued natural resource. It is essential for life on our planet, for food production and economic development. Moreover, water plays a fundamental role in shaping weather and climate. However, with the growing global population, the planet's water resources are constantly under threat from overuse and pollution. In addition, the effects of a changing climate are thought to be leading to an increased frequency of extreme weather causing floods, landslides and drought. The need to understand and monitor our environment and its resources, including <span class="hlt">advancing</span> our knowledge of the <span class="hlt">hydrological</span> cycle, has never been more important and apparent. The best approach to do so on a global scale is from space. This paper provides an overview of the major components of the <span class="hlt">hydrological</span> cycle, the status of their observations from space and related data products and models for <span class="hlt">hydrological</span> variable retrievals. It also lists the current and planned satellite missions contributing to <span class="hlt">advancing</span> our understanding of the <span class="hlt">hydrological</span> cycle on a global scale. Further details of the <span class="hlt">hydrological</span> cycle are substantiated in several of the other papers in this Special Issue.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.cambridge.org/us/knowledge/isbn/item6885007/?site_locale=en_US','USGSPUBS'); return false;" href="http://www.cambridge.org/us/knowledge/isbn/item6885007/?site_locale=en_US"><span>Hillslope <span class="hlt">hydrology</span> and stability</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Lu, Ning; Godt, Jonathan</p> <p>2012-01-01</p> <p>Landslides are caused by a failure of the mechanical balance within hillslopes. This balance is governed by two coupled physical processes: <span class="hlt">hydrological</span> or subsurface flow and stress. The stabilizing strength of hillslope materials depends on effective stress, which is diminished by rainfall. This book presents a cutting-edge quantitative approach to understanding hydro-mechanical processes across variably saturated hillslope environments and to the study and <span class="hlt">prediction</span> of rainfall-induced landslides. Topics covered include historic synthesis of hillslope geomorphology and <span class="hlt">hydrology</span>, total and effective stress distributions, critical reviews of shear strength of hillslope materials and different bases for stability analysis. Exercises and homework problems are provided for students to engage with the theory in practice. This is an invaluable resource for graduate students and researchers in <span class="hlt">hydrology</span>, geomorphology, engineering geology, geotechnical engineering and geomechanics and for professionals in the fields of civil and environmental engineering and natural hazard analysis.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29341358','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29341358"><span>Thermal and <span class="hlt">hydrologic</span> responses to climate change <span class="hlt">predict</span> marked alterations in boreal stream invertebrate assemblages.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Mustonen, Kaisa-Riikka; Mykrä, Heikki; Marttila, Hannu; Sarremejane, Romain; Veijalainen, Noora; Sippel, Kalle; Muotka, Timo; Hawkins, Charles P</p> <p>2018-06-01</p> <p>Air temperature at the northernmost latitudes is <span class="hlt">predicted</span> to increase steeply and precipitation to become more variable by the end of the 21st century, resulting in altered thermal and <span class="hlt">hydrological</span> regimes. We applied five climate scenarios to <span class="hlt">predict</span> the future (2070-2100) benthic macroinvertebrate assemblages at 239 near-pristine sites across Finland (ca. 1200 km latitudinal span). We used a multitaxon distribution model with air temperature and modeled daily flow as predictors. As expected, projected air temperature increased the most in northernmost Finland. <span class="hlt">Predicted</span> taxonomic richness also increased the most in northern Finland, congruent with the <span class="hlt">predicted</span> northwards shift of many species' distributions. Compositional changes were <span class="hlt">predicted</span> to be high even without changes in richness, suggesting that species replacement may be the main mechanism causing climate-induced changes in macroinvertebrate assemblages. Northern streams were <span class="hlt">predicted</span> to lose much of the seasonality of their flow regimes, causing potentially marked changes in stream benthic assemblages. Sites with the highest loss of seasonality were <span class="hlt">predicted</span> to support future assemblages that deviate most in compositional similarity from the present-day assemblages. Macroinvertebrate assemblages were also <span class="hlt">predicted</span> to change more in headwaters than in larger streams, as headwaters were particularly sensitive to changes in flow patterns. Our results emphasize the importance of focusing protection and mitigation on headwater streams with high-flow seasonality because of their vulnerability to climate change. © 2018 John Wiley & Sons Ltd.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://cfpub.epa.gov/si/si_public_record_report.cfm?dirEntryId=227488&Lab=NERL&keyword=erickson&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=227488&Lab=NERL&keyword=erickson&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>Assessing Impacts of Landuse Changes on <span class="hlt">Hydrology</span> for the Upper San Pedro Watershed</span></a></p> <p><a target="_blank" href="http://oaspub.epa.gov/eims/query.page">EPA Science Inventory</a></p> <p></p> <p></p> <p>The assessment of landuse changes on <span class="hlt">hydrology</span> is essential for the development of sustainable water resource strategies. Specifically, understanding how each land use influences <span class="hlt">hydrological</span> processes will greatly improve <span class="hlt">predictability</span> of <span class="hlt">hydrological</span> consequences to landuse ch...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017JHyd..549..374G','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017JHyd..549..374G"><span><span class="hlt">Hydrological</span> effect of vegetation against rainfall-induced landslides</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Gonzalez-Ollauri, Alejandro; Mickovski, Slobodan B.</p> <p>2017-06-01</p> <p>The <span class="hlt">hydrological</span> effect of vegetation on rainfall-induced landslides has rarely been quantified and its integration into slope stability analysis methods remains a challenge. Our goal was to establish a reproducible, novel framework to evaluate the <span class="hlt">hydrological</span> effect of vegetation on shallow landslides. This was achieved by accomplishing three objectives: (i) quantification in situ of the <span class="hlt">hydrological</span> mechanisms by which woody vegetation (i.e. Salix sp.) might impact slope stability under wetting and drying conditions; (ii) to propose a new approach to <span class="hlt">predict</span> plant-derived matric suctions under drying conditions; and (iii) to evaluate the suitability of the unified effective stress principle and framework (UES) to quantify the <span class="hlt">hydrological</span> effect of vegetation against landslides. The results revealed that plant water uptake was the main <span class="hlt">hydrological</span> mechanism contributing to slope stability, as the vegetated slope was, on average, 12.84% drier and had matric suctions three times higher than the fallow slope. The plant-related mechanisms under wetting conditions had a minimal effect on slope stability. The plant aerial parts intercepted up to 26.73% of the rainfall and concentrated a further 10.78% of it around the stem. Our approach successfully <span class="hlt">predicted</span> the plant-derived matric suctions and UES proved to be adequate for evaluating the <span class="hlt">hydrological</span> effect of vegetation on landslides. Although the UES framework presented here sets the basis for effectively evaluating the <span class="hlt">hydrological</span> effect of vegetation on slope stability, it requires knowledge of the specific hydro-mechanical properties of plant-soil composites and this in itself needs further investigation.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFM.H42F..05Y','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFM.H42F..05Y"><span>Quantification of effective plant rooting depth: <span class="hlt">advancing</span> global <span class="hlt">hydrological</span> modelling</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Yang, Y.; Donohue, R. J.; McVicar, T.</p> <p>2017-12-01</p> <p>Plant rooting depth (Zr) is a key parameter in <span class="hlt">hydrological</span> and biogeochemical models, yet the global spatial distribution of Zr is largely unknown due to the difficulties in its direct measurement. Moreover, Zr observations are usually only representative of a single plant or several plants, which can differ greatly from the effective Zr over a modelling unit (e.g., catchment or grid-box). Here, we provide a global parameterization of an analytical Zr model that balances the marginal carbon cost and benefit of deeper roots, and produce a climatological (i.e., 1982-2010 average) global Zr map. To test the Zr estimates, we apply the estimated Zr in a highly transparent <span class="hlt">hydrological</span> model (i.e., the Budyko-Choudhury-Porporato (BCP) model) to estimate mean annual actual evapotranspiration (E) across the globe. We then compare the estimated E with both water balance-based E observations at 32 major catchments and satellite grid-box retrievals across the globe. Our results show that the BCP model, when implemented with Zr estimated herein, optimally reproduced the spatial pattern of E at both scales and provides improved model outputs when compared to BCP model results from two already existing global Zr datasets. These results suggest that our Zr estimates can be effectively used in state-of-the-art <span class="hlt">hydrological</span> models, and potentially biogeochemical models, where the determination of Zr currently largely relies on biome type-based look-up tables.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.fs.usda.gov/treesearch/pubs/25564','TREESEARCH'); return false;" href="https://www.fs.usda.gov/treesearch/pubs/25564"><span>Statistical control in <span class="hlt">hydrologic</span> forecasting.</span></a></p> <p><a target="_blank" href="http://www.fs.usda.gov/treesearch/">Treesearch</a></p> <p>H.G. Wilm</p> <p>1950-01-01</p> <p>With rapidly growing development and uses of water, a correspondingly great demand has developed for <span class="hlt">advance</span> estimates of the volumes or rates of flow which are supplied by streams. Therefore much attention is being devoted to <span class="hlt">hydrologic</span> forecasting, and numerous methods have been tested in efforts to make increasingly reliable estimates of future supplies.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012EGUGA..14.7280S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012EGUGA..14.7280S"><span>What are the main research challenges in <span class="hlt">hydrology</span>?</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Savenije, H. H. G.</p> <p>2012-04-01</p> <p>The science of <span class="hlt">hydrology</span> finds itself in a difficult situation. The PUB decade has told us that we are not very good at <span class="hlt">predicting</span> <span class="hlt">hydrological</span> behaviour in a data scarce environment. How good is our science if we are so uncertain about our <span class="hlt">predictions</span>? On the other hand experienced hydrologists may say that we know enough for most practical problems. We can apply standard approaches or models to a variety of situations and if we have enough data we can make reasonable <span class="hlt">predictions</span> of river flow, groundwater levels or water availability. In the world of applied <span class="hlt">hydrology</span> we have enough knowledge to design dams, well fields, embankments, irrigation schemes, water intakes, and the like. There are proofs galore of impressive hydraulic works, all around the world. But for a scientist these accomplishments are hardly satisfying. The fact that a model works is no proof that the theory is correct, or that we understand the processes behind it. A <span class="hlt">hydrological</span> scientist will rightly point out that there is still a lot that we don't understand. Although we can apply rainfall-runoff models to catchments, we fail to understand how exactly the water behaves, or how long it resides within the different compartments of the system. From a science perspective this is very unsatisfactory, even though engineers may argue that there is no problem as long as the models give reasonable outputs. So is our science adequate or are we still in the dark and do we fail to understand precisely how our <span class="hlt">hydrological</span> system functions, much like a clockmaker who can read the time from a watch, but fails to understand how precisely the clockwork works? <span class="hlt">Hydrology</span> is about the occurrence and flow of water (or moisture) through the Earth system. In that sense it is similar to other Earth sciences, such a climatology, oceanography or hydraulics. But this similarity is treacherous, because it is different in one fundamental aspect. Unlike other Earth sciences, in <span class="hlt">hydrology</span> the medium through which the</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29699579','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29699579"><span>Urinary biomarkers <span class="hlt">predict</span> <span class="hlt">advanced</span> acute kidney injury after cardiovascular surgery.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Wang, Jian-Jhong; Chi, Nai-Hsin; Huang, Tao-Min; Connolly, Rory; Chen, Liang Wen; Chueh, Shih-Chieh Jeff; Kan, Wei-Chih; Lai, Chih-Cheng; Wu, Vin-Cent; Fang, Ji-Tseng; Chu, Tzong-Shinn; Wu, Kwan-Dun</p> <p>2018-04-26</p> <p>Acute kidney injury (AKI) after cardiovascular surgery is a serious complication. Little is known about the ability of novel biomarkers in combination with clinical risk scores for <span class="hlt">prediction</span> of <span class="hlt">advanced</span> AKI. In this prospectively conducted multicenter study, urine samples were collected from 149 adults at 0, 3, 6, 12 and 24 h after cardiovascular surgery. We measured urinary hemojuvelin (uHJV), kidney injury molecule-1 (uKIM-1), neutrophil gelatinase-associated lipocalin (uNGAL), α-glutathione S-transferase (uα-GST) and π-glutathione S-transferase (uπ-GST). The primary outcome was <span class="hlt">advanced</span> AKI, under the definition of Kidney Disease: Improving Global Outcomes (KDIGO) stage 2, 3 and composite outcomes were KDIGO stage 2, 3 or 90-day mortality after hospital discharge. Patients with <span class="hlt">advanced</span> AKI had significantly higher levels of uHJV and uKIM-1 at 3, 6 and 12 h after surgery. When normalized by urinary creatinine level, uKIM-1 in combination with uHJV at 3 h post-surgery had a high <span class="hlt">predictive</span> ability for <span class="hlt">advanced</span> AKI and composite outcome (AUC = 0.898 and 0.905, respectively). The combination of this biomarker panel (normalized uKIM-1, uHJV at 3 h post-operation) and Liano's score was superior in <span class="hlt">predicting</span> <span class="hlt">advanced</span> AKI (AUC = 0.931, category-free net reclassification improvement of 1.149, and p <  0.001). When added to Liano's score, normalized uHJV and uKIM-1 levels at 3 h after cardiovascular surgery enhanced the identification of patients at higher risk of progression to <span class="hlt">advanced</span> AKI and composite outcomes.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014EGUGA..16.2602B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014EGUGA..16.2602B"><span>Significance of <span class="hlt">hydrological</span> model choice and land use changes when doing climate change impact assessment</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Bjørnholt Karlsson, Ida; Obel Sonnenborg, Torben; Refsgaard, Jens Christian; Høgh Jensen, Karsten</p> <p>2014-05-01</p> <p>Uncertainty in impact studies arises both from Global Climate Models (GCM), emission projections, statistical downscaling, Regional Climate Models (RCM), <span class="hlt">hydrological</span> models and calibration techniques (Refsgaard et al. 2013). Some of these uncertainties have been evaluated several times in the literature; however few studies have investigated the effect of <span class="hlt">hydrological</span> model choice on the assessment results (Boorman & Sefton 1997; Jiang et al. 2007; Bastola et al. 2011). These studies have found that model choice results in large differences, up to 70%, in the <span class="hlt">predicted</span> discharge changes depending on the climate input. The objective of the study is to investigate the impact of climate change on <span class="hlt">hydrology</span> of the Odense catchment, Denmark both in response to (a) different climate projections (GCM-RCM combinations); (b) different <span class="hlt">hydrological</span> models and (c) different land use scenarios. This includes: 1. Separation of the climate model signal; the <span class="hlt">hydrological</span> model signal and the land use signal 2. How do the different <span class="hlt">hydrological</span> components react under different climate and land use conditions for the different models 3. What land use scenario seems to provide the best adaptation for the challenges of the different future climate change scenarios from a <span class="hlt">hydrological</span> perspective? Four climate models from the ENSEMBLES project (Hewitt & Griggs 2004): ECHAM5 - HIRHAM5, ECHAM5 - RCA3, ARPEGE - RM5.1 and HadCM3 - HadRM3 are used, assessing the climate change impact in three periods: 1991-2010 (present), 2041-2060 (near future) and 2081-2100 (far future). The four climate models are used in combination with three <span class="hlt">hydrological</span> models with different conceptual layout: NAM, SWAT and MIKE SHE. Bastola, S., C. Murphy and J. Sweeney (2011). "The role of <span class="hlt">hydrological</span> modelling uncertainties in climate change impact assessments of Irish river catchments." <span class="hlt">Advances</span> in Water Resources 34: 562-576. Boorman, D. B. and C. E. M. Sefton (1997). "Recognising the uncertainty 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_9");'>9</a></li> <li><a href="#" onclick='return showDiv("page_10");'>10</a></li> <li class="active"><span>11</span></li> <li><a href="#" onclick='return showDiv("page_12");'>12</a></li> <li><a href="#" onclick='return showDiv("page_13");'>13</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_11 --> <div id="page_12" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_10");'>10</a></li> <li><a href="#" onclick='return showDiv("page_11");'>11</a></li> <li class="active"><span>12</span></li> <li><a href="#" onclick='return showDiv("page_13");'>13</a></li> <li><a href="#" onclick='return showDiv("page_14");'>14</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="221"> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFM.H51Q..02H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFM.H51Q..02H"><span>Findings and Challenges in Fine-Resolution Large-Scale <span class="hlt">Hydrological</span> Modeling</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Her, Y. G.</p> <p>2017-12-01</p> <p>Fine-resolution large-scale (FL) modeling can provide the overall picture of the <span class="hlt">hydrological</span> cycle and transport while taking into account unique local conditions in the simulation. It can also help develop water resources management plans consistent across spatial scales by describing the spatial consequences of decisions and <span class="hlt">hydrological</span> events extensively. FL modeling is expected to be common in the near future as global-scale remotely sensed data are emerging, and computing resources have been <span class="hlt">advanced</span> rapidly. There are several spatially distributed models available for <span class="hlt">hydrological</span> analyses. Some of them rely on numerical methods such as finite difference/element methods (FDM/FEM), which require excessive computing resources (implicit scheme) to manipulate large matrices or small simulation time intervals (explicit scheme) to maintain the stability of the solution, to describe two-dimensional overland processes. Others make unrealistic assumptions such as constant overland flow velocity to reduce the computational loads of the simulation. Thus, simulation efficiency often comes at the expense of precision and reliability in FL modeling. Here, we introduce a new FL continuous <span class="hlt">hydrological</span> model and its application to four watersheds in different landscapes and sizes from 3.5 km2 to 2,800 km2 at the spatial resolution of 30 m on an hourly basis. The model provided acceptable accuracy statistics in reproducing <span class="hlt">hydrological</span> observations made in the watersheds. The modeling outputs including the maps of simulated travel time, runoff depth, soil water content, and groundwater recharge, were animated, visualizing the dynamics of <span class="hlt">hydrological</span> processes occurring in the watersheds during and between storm events. Findings and challenges were discussed in the context of modeling efficiency, accuracy, and reproducibility, which we found can be improved by employing <span class="hlt">advanced</span> computing techniques and <span class="hlt">hydrological</span> understandings, by using remotely sensed <span class="hlt">hydrological</span></p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.usgs.gov/circ/1968/0554/report.pdf','USGSPUBS'); return false;" href="https://pubs.usgs.gov/circ/1968/0554/report.pdf"><span><span class="hlt">Hydrology</span> for urban land planning - A guidebook on the <span class="hlt">hydrologic</span> effects of urban land use</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Leopold, Luna Bergere</p> <p>1968-01-01</p> <p>The application of current knowledge of the <span class="hlt">hydrologic</span> effects of urbanization to the Brandywine should be viewed as a forecast of conditions which may be expected as urbanization proceeds. By making such forecasts in <span class="hlt">advance</span> of actual urban development, the methods can be tested, data can be extended, and procedures improved as verification becomes possible.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.ars.usda.gov/research/publications/publication/?seqNo115=330371','TEKTRAN'); return false;" href="http://www.ars.usda.gov/research/publications/publication/?seqNo115=330371"><span>Flexibility on storage-release based distributed <span class="hlt">hydrologic</span> modeling with object-oriented approach</span></a></p> <p><a target="_blank" href="https://www.ars.usda.gov/research/publications/find-a-publication/">USDA-ARS?s Scientific Manuscript database</a></p> <p></p> <p></p> <p>With the availability of <span class="hlt">advanced</span> <span class="hlt">hydrologic</span> data in the public domain such as remotely sensed and climate change scenario data, there is a need for a modeling framework that is capable of using these data to simulate and extend <span class="hlt">hydrologic</span> processes with multidisciplinary approaches for sustainable ...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2010AGUFM.H11E0864H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2010AGUFM.H11E0864H"><span><span class="hlt">Hydrologic</span> Process-oriented Optimization of Electrical Resistivity Tomography</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Hinnell, A.; Bechtold, M.; Ferre, T. A.; van der Kruk, J.</p> <p>2010-12-01</p> <p>Electrical resistivity tomography (ERT) is commonly used in <span class="hlt">hydrologic</span> investigations. <span class="hlt">Advances</span> in joint and coupled hydrogeophysical inversion have enhanced the quantitative use of ERT to construct and condition <span class="hlt">hydrologic</span> models (i.e. identify <span class="hlt">hydrologic</span> structure and estimate <span class="hlt">hydrologic</span> parameters). However the selection of which electrical resistivity data to collect and use is often determined by a combination of data requirements for geophysical analysis, intuition on the part of the hydrogeophysicist and logistical constraints of the laboratory or field site. One of the advantages of coupled hydrogeophysical inversion is the direct link between the <span class="hlt">hydrologic</span> model and the individual geophysical data used to condition the model. That is, there is no requirement to collect geophysical data suitable for independent geophysical inversion. The geophysical measurements collected can be optimized for estimation of <span class="hlt">hydrologic</span> model parameters rather than to develop a geophysical model. Using a synthetic model of drip irrigation we evaluate the value of individual resistivity measurements to describe the soil hydraulic properties and then use this information to build a data set optimized for characterizing <span class="hlt">hydrologic</span> processes. We then compare the information content in the optimized data set with the information content in a data set optimized using a Jacobian sensitivity analysis.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017EGUGA..19.6719H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017EGUGA..19.6719H"><span>Towards Reproducibility in Computational <span class="hlt">Hydrology</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Hutton, Christopher; Wagener, Thorsten; Freer, Jim; Han, Dawei; Duffy, Chris; Arheimer, Berit</p> <p>2017-04-01</p> <p>Reproducibility is a foundational principle in scientific research. The ability to independently re-run an experiment helps to verify the legitimacy of individual findings, and evolve (or reject) hypotheses and models of how environmental systems function, and move them from specific circumstances to more general theory. Yet in computational <span class="hlt">hydrology</span> (and in environmental science more widely) the code and data that produces published results are not regularly made available, and even if they are made available, there remains a multitude of generally unreported choices that an individual scientist may have made that impact the study result. This situation strongly inhibits the ability of our community to reproduce and verify previous findings, as all the information and boundary conditions required to set up a computational experiment simply cannot be reported in an article's text alone. In Hutton et al 2016 [1], we argue that a cultural change is required in the computational <span class="hlt">hydrological</span> community, in order to <span class="hlt">advance</span> and make more robust the process of knowledge creation and hypothesis testing. We need to adopt common standards and infrastructures to: (1) make code readable and re-useable; (2) create well-documented workflows that combine re-useable code together with data to enable published scientific findings to be reproduced; (3) make code and workflows available, easy to find, and easy to interpret, using code and code metadata repositories. To create change we argue for improved graduate training in these areas. In this talk we reflect on our progress in achieving reproducible, open science in computational <span class="hlt">hydrology</span>, which are relevant to the broader computational geoscience community. In particular, we draw on our experience in the Switch-On (EU funded) virtual water science laboratory (http://www.switch-on-vwsl.eu/participate/), which is an open platform for collaboration in <span class="hlt">hydrological</span> experiments (e.g. [2]). While we use computational <span class="hlt">hydrology</span> as</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2011HESS...15.2327A','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2011HESS...15.2327A"><span>An operational <span class="hlt">hydrological</span> ensemble <span class="hlt">prediction</span> system for the city of Zurich (Switzerland): skill, case studies and scenarios</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Addor, N.; Jaun, S.; Fundel, F.; Zappa, M.</p> <p>2011-07-01</p> <p>The Sihl River flows through Zurich, Switzerland's most populated city, for which it represents the largest flood threat. To anticipate extreme discharge events and provide decision support in case of flood risk, a hydrometeorological ensemble <span class="hlt">prediction</span> system (HEPS) was launched operationally in 2008. This model chain relies on limited-area atmospheric forecasts provided by the deterministic model COSMO-7 and the probabilistic model COSMO-LEPS. These atmospheric forecasts are used to force a semi-distributed <span class="hlt">hydrological</span> model (PREVAH), coupled to a hydraulic model (FLORIS). The resulting <span class="hlt">hydrological</span> forecasts are eventually communicated to the stakeholders involved in the Sihl discharge management. This fully operational setting provides a real framework with which to compare the potential of deterministic and probabilistic discharge forecasts for flood mitigation. To study the suitability of HEPS for small-scale basins and to quantify the added-value conveyed by the probability information, a reforecast was made for the period June 2007 to December 2009 for the Sihl catchment (336 km2). Several metrics support the conclusion that the performance gain can be of up to 2 days lead time for the catchment considered. Brier skill scores show that overall COSMO-LEPS-based <span class="hlt">hydrological</span> forecasts outperforms their COSMO-7-based counterparts for all the lead times and event intensities considered. The small size of the Sihl catchment does not prevent skillful discharge forecasts, but makes them particularly dependent on correct precipitation forecasts, as shown by comparisons with a reference run driven by observed meteorological parameters. Our evaluation stresses that the capacity of the model to provide confident and reliable mid-term probability forecasts for high discharges is limited. The two most intense events of the study period are investigated utilising a novel graphical representation of probability forecasts, and are used to generate high discharge</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70033262','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70033262"><span>Characterization of errors in a coupled snow <span class="hlt">hydrology</span>-microwave emission model</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Andreadis, K.M.; Liang, D.; Tsang, L.; Lettenmaier, D.P.; Josberger, E.G.</p> <p>2008-01-01</p> <p>Traditional approaches to the direct estimation of snow properties from passive microwave remote sensing have been plagued by limitations such as the tendency of estimates to saturate for moderately deep snowpacks and the effects of mixed land cover within remotely sensed pixels. An alternative approach is to assimilate satellite microwave emission observations directly, which requires embedding an accurate microwave emissions model into a <span class="hlt">hydrologic</span> <span class="hlt">prediction</span> scheme, as well as quantitative information of model and observation errors. In this study a coupled snow <span class="hlt">hydrology</span> [Variable Infiltration Capacity (VIC)] and microwave emission [Dense Media Radiative Transfer (DMRT)] model are evaluated using multiscale brightness temperature (TB) measurements from the Cold Land Processes Experiment (CLPX). The ability of VIC to reproduce snowpack properties is shown with the use of snow pit measurements, while TB model <span class="hlt">predictions</span> are evaluated through comparison with Ground-Based Microwave Radiometer (GBMR), air-craft [Polarimetric Scanning Radiometer (PSR)], and satellite [<span class="hlt">Advanced</span> Microwave Scanning Radiometer for the Earth Observing System (AMSR-E)] TB measurements. Limitations of the model at the point scale were not as evident when comparing areal estimates. The coupled model was able to reproduce the TB spatial patterns observed by PSR in two of three sites. However, this was mostly due to the presence of relatively dense forest cover. An interesting result occurs when examining the spatial scaling behavior of the higher-resolution errors; the satellite-scale error is well approximated by the mode of the (spatial) histogram of errors at the smaller scale. In addition, TB <span class="hlt">prediction</span> errors were almost invariant when aggregated to the satellite scale, while forest-cover fractions greater than 30% had a significant effect on TB <span class="hlt">predictions</span>. ?? 2008 American Meteorological Society.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012AGUFM.H21D1198J','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012AGUFM.H21D1198J"><span>A Hierarchical Approach Embedding <span class="hlt">Hydrologic</span> and Population Modeling for a West Nile Virus Vector <span class="hlt">Prediction</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Jian, Y.; Silvestri, S.; Marani, M.; Saltarin, A.; Chillemi, G.</p> <p>2012-12-01</p> <p>We applied a hierarchical state space model to <span class="hlt">predict</span> the abundance of Cx.pipiens (a West Nile Virus vector) in the Po River Delta Region, Northeastern Italy. The study area has large mosquito abundance, due to a favorable environment and climate as well as dense human population. Mosquito data were collected on a weekly basis at more than 20 sites from May to September in 2010 and 2011. Cx.pipiens was the dominant species in our samples, accounting for about 90% of the more than 300,000 total captures. The <span class="hlt">hydrological</span> component of the model accounted for evapotranspiration, infiltration and deep percolation to infer, in a 0D context, the local dynamics of soil moisture as a direct exogenous forcing of mosquito dynamics. The population model had a Gompertz structure, which included exogenous meteorological forcings and delayed internal dynamics. The models were coupled within a hierarchical statistical structure to overcome the relatively short length of the samples by exploiting the large number of concurrent observations available. The results indicated that Cx.pipiens abundance had significant density dependence at 1 week lag, which approximately matched its development time from larvae to adult. Among the exogenous controls, temperature, daylight hours, and soil moisture explained most of the dynamics. Longer daylight hours and lower soil moisture values resulted in higher abundance. The negative correlation of soil moisture and mosquito population can be explained with the abundance of water in the region (e.g. due to irrigation) and the preference for eutrophic habitats by Cx.pipien. Variations among sites were explained by land use factors as represented by distance to the nearest rice field and NDVI values: the carrying capacity decreased with increased distance to the nearest rice filed, while the maximum growth rate was positively related with NDVI. The model shows a satisfactory performance in <span class="hlt">predicting</span> (potentially one week in <span class="hlt">advance</span>) mosquito</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/1997EOSTr..78..528I','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/1997EOSTr..78..528I"><span><span class="hlt">Hydrology</span> for Engineers, Geologists, and Environmental Professionals</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Ince, Simon</p> <p></p> <p>For people who are involved in the applied aspects of <span class="hlt">hydrology</span>, it is refreshing to find a textbook that begins with a meaningful disclaimer, albeit in fine print on the back side of the frontispiece:“The present book and the accompanying software have been written according to the latest techniques in scientific <span class="hlt">hydrology</span>. However, <span class="hlt">hydrology</span> is at best an inexact science. A good book and a good computer software by themselves do not guarantee accurate or even realistic <span class="hlt">predictions</span>. Acceptable results in the applications of <span class="hlt">hydrologic</span> methods to engineering and environmental problems depend to a greater extend (sic) on the skills, logical assumptions, and practical experience of the user, and on the quantity and quality of long-term <span class="hlt">hydrologic</span> data available. Neither the author nor the publisher assumes any responsibility or any liability, explicitly or implicitly, on the results or the consequences of using the information contained in this book or its accompanying software.”</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70028170','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70028170"><span>Mountain <span class="hlt">hydrology</span> of the western United States</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Bales, Roger C.; Molotch, Noah P.; Painter, Thomas H; Dettinger, Michael D.; Rice, Robert; Dozier, Jeff</p> <p>2006-01-01</p> <p>Climate change and climate variability, population growth, and land use change drive the need for new <span class="hlt">hydrologic</span> knowledge and understanding. In the mountainous West and other similar areas worldwide, three pressing <span class="hlt">hydrologic</span> needs stand out: first, to better understand the processes controlling the partitioning of energy and water fluxes within and out from these systems; second, to better understand feedbacks between <span class="hlt">hydrological</span> fluxes and biogeochemical and ecological processes; and, third, to enhance our physical and empirical understanding with integrated measurement strategies and information systems. We envision an integrative approach to monitoring, modeling, and sensing the mountain environment that will improve understanding and <span class="hlt">prediction</span> of <span class="hlt">hydrologic</span> fluxes and processes. Here extensive monitoring of energy fluxes and <span class="hlt">hydrologic</span> states are needed to supplement existing measurements, which are largely limited to streamflow and snow water equivalent. Ground‐based observing systems must be explicitly designed for integration with remotely sensed data and for scaling up to basins and whole ranges.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3651603','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3651603"><span><span class="hlt">Advanced</span> Hepatocellular Carcinoma: Which Staging Systems Best <span class="hlt">Predict</span> Prognosis?</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Huitzil-Melendez, Fidel-David; Capanu, Marinela; O'Reilly, Eileen M.; Duffy, Austin; Gansukh, Bolorsukh; Saltz, Leonard L.; Abou-Alfa, Ghassan K.</p> <p>2010-01-01</p> <p>Purpose The purpose of cancer staging systems is to accurately <span class="hlt">predict</span> patient prognosis. The outcome of <span class="hlt">advanced</span> hepatocellular carcinoma (HCC) depends on both the cancer stage and the extent of liver dysfunction. Many staging systems that include both aspects have been developed. It remains unknown, however, which of these systems is optimal for <span class="hlt">predicting</span> patient survival. Patients and Methods Patients with <span class="hlt">advanced</span> HCC treated over a 5-year period at Memorial Sloan-Kettering Cancer Center were identified from an electronic medical record database. Patients with sufficient data for utilization in all staging systems were included. TNM sixth edition, Okuda, Barcelona Clinic Liver Cancer (BCLC), Cancer of the Liver Italian Program (CLIP), Chinese University Prognostic Index (CUPI), Japan Integrated Staging (JIS), and Groupe d'Etude et de Traitement du Carcinome Hepatocellulaire (GETCH) systems were ranked on the basis of their accuracy at <span class="hlt">predicting</span> survival by using concordance index (c-index). Other independent prognostic variables were also identified. Results Overall, 187 eligible patients were identified and were staged by using the seven staging systems. CLIP, CUPI, and GETCH were the three top-ranking staging systems. BCLC and TNM sixth edition lacked any meaningful prognostic discrimination. Performance status, AST, abdominal pain, and esophageal varices improved the discriminatory ability of CLIP. Conclusion In our selected patient population, CLIP, CUPI, and GETCH were the most informative staging systems in <span class="hlt">predicting</span> survival in patients with <span class="hlt">advanced</span> HCC. Prospective validation is required to determine if they can be accurately used to stratify patients in clinical trials and to direct the appropriate need for systemic therapy versus best supportive care. BCLC and TNM sixth edition were not helpful in <span class="hlt">predicting</span> survival outcome, and their use is not supported by our data. PMID:20458042</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/24684960','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/24684960"><span>Pretreatment tables <span class="hlt">predicting</span> pathologic stage of locally <span class="hlt">advanced</span> prostate cancer.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Joniau, Steven; Spahn, Martin; Briganti, Alberto; Gandaglia, Giorgio; Tombal, Bertrand; Tosco, Lorenzo; Marchioro, Giansilvio; Hsu, Chao-Yu; Walz, Jochen; Kneitz, Burkhard; Bader, Pia; Frohneberg, Detlef; Tizzani, Alessandro; Graefen, Markus; van Cangh, Paul; Karnes, R Jeffrey; Montorsi, Francesco; van Poppel, Hein; Gontero, Paolo</p> <p>2015-02-01</p> <p>Pretreatment tables for the <span class="hlt">prediction</span> of pathologic stage have been published and validated for localized prostate cancer (PCa). No such tables are available for locally <span class="hlt">advanced</span> (cT3a) PCa. To construct tables <span class="hlt">predicting</span> pathologic outcome after radical prostatectomy (RP) for patients with cT3a PCa with the aim to help guide treatment decisions in clinical practice. This was a multicenter retrospective cohort study including 759 consecutive patients with cT3a PCa treated with RP between 1987 and 2010. Retropubic RP and pelvic lymphadenectomy. Patients were divided into pretreatment prostate-specific antigen (PSA) and biopsy Gleason score (GS) subgroups. These parameters were used to construct tables <span class="hlt">predicting</span> pathologic outcome and the presence of positive lymph nodes (LNs) after RP for cT3a PCa using ordinal logistic regression. In the model <span class="hlt">predicting</span> pathologic outcome, the main effects of biopsy GS and pretreatment PSA were significant. A higher GS and/or higher PSA level was associated with a more unfavorable pathologic outcome. The validation procedure, using a repeated split-sample method, showed good <span class="hlt">predictive</span> ability. Regression analysis also showed an increasing probability of positive LNs with increasing PSA levels and/or higher GS. Limitations of the study are the retrospective design and the long study period. These novel tables <span class="hlt">predict</span> pathologic stage after RP for patients with cT3a PCa based on pretreatment PSA level and biopsy GS. They can be used to guide decision making in men with locally <span class="hlt">advanced</span> PCa. Our study might provide physicians with a useful tool to <span class="hlt">predict</span> pathologic stage in locally <span class="hlt">advanced</span> prostate cancer that might help select patients who may need multimodal treatment. Copyright © 2014 European Association of Urology. Published by Elsevier B.V. All rights reserved.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19990014052','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19990014052"><span>Surface <span class="hlt">Hydrology</span> in Global River Basins in the Off-Line Land-Surface GEOS Assimilation (OLGA) System</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Bosilovich, Michael G.; Yang, Runhua; Houser, Paul R.</p> <p>1998-01-01</p> <p>Land surface <span class="hlt">hydrology</span> for the Off-line Land-surface GEOS Analysis (OLGA) system and Goddard Earth Observing System (GEOS-1) Data Assimilation System (DAS) has been examined using a river routing model. The GEOS-1 DAS land-surface parameterization is very simple, using an energy balance <span class="hlt">prediction</span> of surface temperature and prescribed soil water. OLGA uses near-surface atmospheric data from the GEOS-1 DAS to drive a more comprehensive parameterization of the land-surface physics. The two global systems are evaluated using a global river routing model. The river routing model uses climatologic surface runoff from each system to simulate the river discharge from global river basins, which can be compared to climatologic river discharge. Due to the soil <span class="hlt">hydrology</span>, the OLGA system shows a general improvement in the simulation of river discharge compared to the GEOS-1 DAS. Snowmelt processes included in OLGA also have a positive effect on the annual cycle of river discharge and source runoff. Preliminary tests of a coupled land-atmosphere model indicate improvements to the <span class="hlt">hydrologic</span> cycle compared to the uncoupled system. The river routing model has provided a useful tool in the evaluation of the GCM <span class="hlt">hydrologic</span> cycle, and has helped quantify the influence of the more <span class="hlt">advanced</span> land surface model.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016GMD.....9.4491G','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016GMD.....9.4491G"><span>StreamFlow 1.0: an extension to the spatially distributed snow model Alpine3D for <span class="hlt">hydrological</span> modelling and deterministic stream temperature <span class="hlt">prediction</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Gallice, Aurélien; Bavay, Mathias; Brauchli, Tristan; Comola, Francesco; Lehning, Michael; Huwald, Hendrik</p> <p>2016-12-01</p> <p>Climate change is expected to strongly impact the <span class="hlt">hydrological</span> and thermal regimes of Alpine rivers within the coming decades. In this context, the development of <span class="hlt">hydrological</span> models accounting for the specific dynamics of Alpine catchments appears as one of the promising approaches to reduce our uncertainty of future mountain <span class="hlt">hydrology</span>. This paper describes the improvements brought to StreamFlow, an existing model for <span class="hlt">hydrological</span> and stream temperature <span class="hlt">prediction</span> built as an external extension to the physically based snow model Alpine3D. StreamFlow's source code has been entirely written anew, taking advantage of object-oriented programming to significantly improve its structure and ease the implementation of future developments. The source code is now publicly available online, along with a complete documentation. A special emphasis has been put on modularity during the re-implementation of StreamFlow, so that many model aspects can be represented using different alternatives. For example, several options are now available to model the advection of water within the stream. This allows for an easy and fast comparison between different approaches and helps in defining more reliable uncertainty estimates of the model forecasts. In particular, a case study in a Swiss Alpine catchment reveals that the stream temperature <span class="hlt">predictions</span> are particularly sensitive to the approach used to model the temperature of subsurface flow, a fact which has been poorly reported in the literature to date. Based on the case study, StreamFlow is shown to reproduce hourly mean discharge with a Nash-Sutcliffe efficiency (NSE) of 0.82 and hourly mean temperature with a NSE of 0.78.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.usgs.gov/of/2008/1173/pdf/OF08-1173_508.pdf','USGSPUBS'); return false;" href="https://pubs.usgs.gov/of/2008/1173/pdf/OF08-1173_508.pdf"><span><span class="hlt">Hydrologic</span> modeling strategy for the Islamic Republic of Mauritania, Africa</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Friedel, Michael J.</p> <p>2008-01-01</p> <p>The government of Mauritania is interested in how to maintain <span class="hlt">hydrologic</span> balance to ensure a long-term stable water supply for minerals-related, domestic, and other purposes. Because of the many complicating and competing natural and anthropogenic factors, hydrologists will perform quantitative analysis with specific objectives and relevant computer models in mind. Whereas various computer models are available for studying water-resource priorities, the success of these models to provide reliable <span class="hlt">predictions</span> largely depends on adequacy of the model-calibration process. <span class="hlt">Predictive</span> analysis helps us evaluate the accuracy and uncertainty associated with simulated dependent variables of our calibrated model. In this report, the <span class="hlt">hydrologic</span> modeling process is reviewed and a strategy summarized for future Mauritanian <span class="hlt">hydrologic</span> modeling studies.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFM.H43A1617M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFM.H43A1617M"><span><span class="hlt">Predicting</span> Geomorphic and <span class="hlt">Hydrologic</span> Risks after Wildfire Using Harmonic and Stochastic Analyses</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Mikesell, J.; Kinoshita, A. M.; Florsheim, J. L.; Chin, A.; Nourbakhshbeidokhti, S.</p> <p>2017-12-01</p> <p>Wildfire is a landscape-scale disturbance that often alters <span class="hlt">hydrological</span> processes and sediment flux during subsequent storms. Vegetation loss from wildfires induce changes to sediment supply such as channel erosion and sedimentation and streamflow magnitude or flooding. These changes enhance downstream hazards, threatening human populations and physical aquatic habitat over various time scales. Using Williams Canyon, a basin burned by the Waldo Canyon Fire (2012) as a case study, we utilize deterministic and statistical modeling methods (Fourier series and first order Markov chain) to assess pre- and post-fire geomorphic and <span class="hlt">hydrologic</span> characteristics, including of precipitation, enhanced vegetation index (EVI, a satellite-based proxy of vegetation biomass), streamflow, and sediment flux. Local precipitation, terrestrial Light Detection and Ranging (LiDAR) scanning, and satellite-based products are used for these time series analyses. We present a framework to assess variability of periodic and nonperiodic climatic and multivariate trends to inform development of a post-wildfire risk assessment methodology. To establish the extent to which a wildfire affects <span class="hlt">hydrologic</span> and geomorphic patterns, a Fourier series was used to fit pre- and post-fire geomorphic and <span class="hlt">hydrologic</span> characteristics to yearly temporal cycles and subcycles of 6, 4, 3, and 2.4 months. These cycles were analyzed using least-squares estimates of the harmonic coefficients or amplitudes of each sub-cycle's contribution to fit the overall behavior of a Fourier series. The stochastic variances of these characteristics were analyzed by composing first-order Markov models and probabilistic analysis through direct likelihood estimates. Preliminary results highlight an increased dependence of monthly post-fire <span class="hlt">hydrologic</span> characteristics on 12 and 6-month temporal cycles. This statistical and probabilistic analysis provides a basis to determine the impact of wildfires on the temporal dependence of</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFM.H53B1689M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFM.H53B1689M"><span>Hyphenated <span class="hlt">hydrology</span>: Multidisciplinary evolution of water resource science</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>McCurley, K. 4553; Jawitz, J. W.</p> <p>2016-12-01</p> <p><span class="hlt">Hydrology</span> has <span class="hlt">advanced</span> considerably as a scientific discipline since its recognized inception in the mid-20th century. While <span class="hlt">hydrology</span> may have evolved from the singular viewpoint of a more rigid physical or engineering science, modern water resource related questions have forced adaptation toward a deliberate interdisciplinary context. Over the past few decades, many of the eventual manifestations of this evolution have been foreseen by prominent expert hydrologists, though their narrative descriptions were not substantially quantified. This study addresses that gap by directly measuring and inspecting the words that hydrologists use to define and describe their research endeavors. We analyzed 16,591 journal article titles from 1965-2015 in Water Resources Research, through which the scientific dialogue and its time-sensitive progression emerges. Word frequency and term concurrence reveal the dynamic timing of the lateral movement of <span class="hlt">hydrology</span> across multiple disciplines and a deepening of scientific discourse with respect to traditional <span class="hlt">hydrologic</span> questions. This study concludes that formerly exotic disciplines are increasingly modifying <span class="hlt">hydrology</span>, prompting new insights as well as inspiring unconventional perspectives on old questions.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2011JHyd..409..483V','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2011JHyd..409..483V"><span>Real-world <span class="hlt">hydrologic</span> assessment of a fully-distributed <span class="hlt">hydrological</span> model in a parallel computing environment</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Vivoni, Enrique R.; Mascaro, Giuseppe; Mniszewski, Susan; Fasel, Patricia; Springer, Everett P.; Ivanov, Valeriy Y.; Bras, Rafael L.</p> <p>2011-10-01</p> <p>SummaryA major challenge in the use of fully-distributed <span class="hlt">hydrologic</span> models has been the lack of computational capabilities for high-resolution, long-term simulations in large river basins. In this study, we present the parallel model implementation and real-world <span class="hlt">hydrologic</span> assessment of the Triangulated Irregular Network (TIN)-based Real-time Integrated Basin Simulator (tRIBS). Our parallelization approach is based on the decomposition of a complex watershed using the channel network as a directed graph. The resulting sub-basin partitioning divides effort among processors and handles <span class="hlt">hydrologic</span> exchanges across boundaries. Through numerical experiments in a set of nested basins, we quantify parallel performance relative to serial runs for a range of processors, simulation complexities and lengths, and sub-basin partitioning methods, while accounting for inter-run variability on a parallel computing system. In contrast to serial simulations, the parallel model speed-up depends on the variability of <span class="hlt">hydrologic</span> processes. Load balancing significantly improves parallel speed-up with proportionally faster runs as simulation complexity (domain resolution and channel network extent) increases. The best strategy for large river basins is to combine a balanced partitioning with an extended channel network, with potential savings through a lower TIN resolution. Based on these <span class="hlt">advances</span>, a wider range of applications for fully-distributed <span class="hlt">hydrologic</span> models are now possible. This is illustrated through a set of ensemble forecasts that account for precipitation uncertainty derived from a statistical downscaling model.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2010AGUFMED23B0719H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2010AGUFMED23B0719H"><span>HydroViz: A web-based <span class="hlt">hydrologic</span> observatory for enhancing <span class="hlt">hydrology</span> and earth-science education</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Habib, E. H.; Ma, Y.; Williams, D.</p> <p>2010-12-01</p> <p>The main goal of this study is to develop a virtual <span class="hlt">hydrologic</span> observatory (HydroViz) that integrates <span class="hlt">hydrologic</span> field observations with numerical simulations by taking advantage of <span class="hlt">advances</span> in <span class="hlt">hydrologic</span> field & remote sensing data, computer modeling, scientific visualization, and web resources and internet accessibility. The HydroViz system is a web-based teaching tool that can run on any web browsers. It leverages the strength of Google Earth to provide authentic and hands-on activities to improve learning. Evaluation of the HydroViz was performed in three engineering courses (a senior level course and two Introductory courses at two different universities). Evaluation results indicate that HydroViz provides an improvement over existing engineering <span class="hlt">hydrology</span> curriculum. HydroViz was effective in facilitating students’ learning and understanding of <span class="hlt">hydrologic</span> concepts & increasing related skills. HydroViz was much more effective for students in engineering <span class="hlt">hydrology</span> classes rather than at the freshmen introduction to civil engineering class. We found that HydroViz has great potential for freshmen audience. Even though HydroViz was challenging to some freshmen, most of them still learned the key concepts and the tool increased the enthusiasm for half of the freshmen. The evaluation provided suggestions to create a simplified version of HydroViz for freshmen-level courses students. It identified concepts and tasks that might be too challenging or irrelevant to the freshmen and areas where we could provide more guidance in the tool. After the first round of evaluation, the development team has made significant improvements to HydroViz, which would further improve its effectiveness for next round of class applications which is planned for the Fall of 2010 to take place in 5 classes at 4 different institutions.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013ESRv..116..109S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013ESRv..116..109S"><span><span class="hlt">Hydrological</span> and geomorphological controls of malaria transmission</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Smith, M. W.; Macklin, M. G.; Thomas, C. J.</p> <p>2013-01-01</p> <p>Malaria risk is linked inextricably to the <span class="hlt">hydrological</span> and geomorphological processes that form vector breeding sites. Yet environmental controls of malaria transmission are often represented by temperature and rainfall amounts, ignoring <span class="hlt">hydrological</span> and geomorphological influences altogether. Continental-scale studies incorporate <span class="hlt">hydrology</span> implicitly through simple minimum rainfall thresholds, while community-scale coupled <span class="hlt">hydrological</span> and entomological models do not represent the actual diversity of the mosquito vector breeding sites. The greatest range of malaria transmission responses to environmental factors is observed at the catchment scale where seemingly contradictory associations between rainfall and malaria risk can be explained by <span class="hlt">hydrological</span> and geomorphological processes that govern surface water body formation and persistence. This paper extends recent efforts to incorporate ecological factors into malaria-risk models, proposing that the same detailed representation be afforded to <span class="hlt">hydrological</span> and, at longer timescales relevant for <span class="hlt">predictions</span> of climate change impacts, geomorphological processes. We review existing representations of environmental controls of malaria and identify a range of <span class="hlt">hydrologically</span> distinct vector breeding sites from existing literature. We illustrate the potential complexity of interactions among <span class="hlt">hydrology</span>, geomorphology and vector breeding sites by classifying a range of water bodies observed in a catchment in East Africa. Crucially, the mechanisms driving surface water body formation and destruction must be considered explicitly if we are to produce dynamic spatial models of malaria risk at catchment scales.</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('http://adsabs.harvard.edu/abs/2009EGUGA..1111469K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2009EGUGA..1111469K"><span>Seeking parsimony in <span class="hlt">hydrology</span> and water resources technology</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Koutsoyiannis, D.</p> <p>2009-04-01</p> <p>The principle of parsimony, also known as the principle of simplicity, the principle of economy and Ockham's razor, advises scientists to prefer the simplest theory among those that fit the data equally well. In this, it is an epistemic principle but reflects an ontological characterization that the universe is ultimately parsimonious. Is this principle useful and can it really be reconciled with, and implemented to, our modelling approaches of complex <span class="hlt">hydrological</span> systems, whose elements and events are extraordinarily numerous, different and unique? The answer underlying the mainstream <span class="hlt">hydrological</span> research of the last two decades seems to be negative. Hopes were invested to the power of computers that would enable faithful and detailed representation of the diverse system elements and the <span class="hlt">hydrological</span> processes, based on merely "first principles" and resulting in "physically-based" models that tend to approach in complexity the real world systems. Today the account of such research endeavour seems not positive, as it did not improve model <span class="hlt">predictive</span> capacity and processes comprehension. A return to parsimonious modelling seems to be again the promising route. The experience from recent research and from comparisons of parsimonious and complicated models indicates that the former can facilitate insight and comprehension, improve accuracy and <span class="hlt">predictive</span> capacity, and increase efficiency. In addition - and despite aspiration that "physically based" models will have lower data requirements and, even, they ultimately become "data-free" - parsimonious models require fewer data to achieve the same accuracy with more complicated models. Naturally, the concepts that reconcile the simplicity of parsimonious models with the complexity of <span class="hlt">hydrological</span> systems are probability theory and statistics. Probability theory provides the theoretical basis for moving from a microscopic to a macroscopic view of phenomena, by mapping sets of diverse elements and events of <span class="hlt">hydrological</span></p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19990013876','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19990013876"><span>Book Review: Regional <span class="hlt">Hydrological</span> Response to Climate Change</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Koster, Randal</p> <p>1998-01-01</p> <p>The book being reviewed, Regional <span class="hlt">Hydrological</span> Response to Climate Change, addresses the effects of global climate change, particularly global warming induced by greenhouse gas emissions, on <span class="hlt">hydrological</span> budgets at the regional scale. As noted in its preface, the book consists of peer-reviewed papers delivered at scientific meetings held by the International Geographical Union Working Group on Regional <span class="hlt">Hydrological</span> Response to Climate Change and Global Warming, supplemented with some additional chapters that round out coverage of the topic. The editors hope that this book will serve as "not only a record of current achievements, but also a stimulus to further <span class="hlt">hydrological</span> research as the detail and spatial resolution of Global Climate Models improves". The reviewer found the background material on regional climatology to be valuable and the methodologies presented to be of interest. The value of the book is significantly diminished, however by the dated nature of some of the material and by large uncertainties in the <span class="hlt">predictions</span> of regional precipitation change. The book would have been improved by a much more extensive documentation of the uncertainty associated with each step of the <span class="hlt">prediction</span> process.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017WRR....5310007M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017WRR....5310007M"><span>Disturbance <span class="hlt">Hydrology</span>: Preparing for an Increasingly Disturbed Future</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Mirus, Benjamin B.; Ebel, Brian A.; Mohr, Christian H.; Zegre, Nicolas</p> <p>2017-12-01</p> <p>This special issue is the result of several fruitful conference sessions on disturbance <span class="hlt">hydrology</span>, which started at the 2013 AGU Fall Meeting in San Francisco and have continued every year since. The stimulating presentations and discussions surrounding those sessions have focused on understanding both the disruption of <span class="hlt">hydrologic</span> functioning following discrete disturbances, as well as the subsequent recovery or change within the affected watershed system. Whereas some <span class="hlt">hydrologic</span> disturbances are directly linked to anthropogenic activities, such as resource extraction, the contributions to this special issue focus primarily on those with indirect or less pronounced human involvement, such as bark-beetle infestation, wildfire, and other natural hazards. However, human activities are enhancing the severity and frequency of these seemingly natural disturbances, thereby contributing to acute <span class="hlt">hydrologic</span> problems and hazards. Major research challenges for our increasingly disturbed planet include the lack of continuous pre and postdisturbance monitoring, <span class="hlt">hydrologic</span> impacts that vary spatially and temporally based on environmental and hydroclimatic conditions, and the preponderance of overlapping or compounding disturbance sequences. In addition, a conceptual framework for characterizing commonalities and differences among <span class="hlt">hydrologic</span> disturbances is still in its infancy. In this introduction to the special issue, we <span class="hlt">advance</span> the fusion of concepts and terminology from ecology and <span class="hlt">hydrology</span> to begin filling this gap. We briefly explore some preliminary approaches for comparing different disturbances and their <span class="hlt">hydrologic</span> impacts, which provides a starting point for further dialogue and research progress.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70192815','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70192815"><span>Disturbance <span class="hlt">hydrology</span>: Preparing for an increasingly disturbed future</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Mirus, Benjamin B.; Ebel, Brian A.; Mohr, Christian H.; Zegre, Nicolas</p> <p>2017-01-01</p> <p>This special issue is the result of several fruitful conference sessions on disturbance <span class="hlt">hydrology</span>, which started at the 2013 AGU Fall Meeting in San Francisco and have continued every year since. The stimulating presentations and discussions surrounding those sessions have focused on understanding both the disruption of <span class="hlt">hydrologic</span> functioning following discrete disturbances, as well as the subsequent recovery or change within the affected watershed system. Whereas some <span class="hlt">hydrologic</span> disturbances are directly linked to anthropogenic activities, such as resource extraction, the contributions to this special issue focus primarily on those with indirect or less pronounced human involvement, such as bark-beetle infestation, wildfire, and other natural hazards. However, human activities are enhancing the severity and frequency of these seemingly natural disturbances, thereby contributing to acute <span class="hlt">hydrologic</span> problems and hazards. Major research challenges for our increasingly disturbed planet include the lack of continuous pre- and post-disturbance monitoring, <span class="hlt">hydrologic</span> impacts that vary spatially and temporally based on environmental and hydroclimatic conditions, and the preponderance of overlapping or compounding disturbance sequences. In addition, a conceptual framework for characterizing commonalities and differences among <span class="hlt">hydrologic</span> disturbances is still in its infancy. In this introduction to the special issue, we <span class="hlt">advance</span> the fusion of concepts and terminology from ecology and <span class="hlt">hydrology</span> to begin filling this gap. We briefly explore some preliminary approaches for comparing different disturbances and their <span class="hlt">hydrologic</span> impacts, which provides a starting point for further dialogue and research progress.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/27796507','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/27796507"><span>Plant colonization and survival along a <span class="hlt">hydrological</span> gradient: demography and niche dynamics.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Damgaard, Christian; Merlin, Amandine; Bonis, Anne</p> <p>2017-01-01</p> <p><span class="hlt">Predicting</span> the effect of a changing environment, e.g., caused by climate change, on realized niche dynamics, and consequently, biodiversity is a challenging scientific question that needs to be addressed. One promising approach is to use estimated demographic parameters for <span class="hlt">predicting</span> plant abundance and occurrence probabilities. Using longitudinal pinpoint cover data sampled along a <span class="hlt">hydrological</span> gradient in the Marais poitevin grasslands, France, the effect of the gradient on the demographic probabilities of colonization and survival was estimated. The estimated probabilities and calculated elasticities of survival and colonization covaried with the observed cover of the different species along the <span class="hlt">hydrological</span> gradient. For example, the flooding tolerant grass A. stolonifera showed a positive response in both colonization and survival to flooding, and the <span class="hlt">hydrological</span> gradient is clearly the most likely explanation for the occurrence pattern observed for A. stolonifera. The results suggest that knowledge on the processes of colonization and survival of the individual species along the <span class="hlt">hydrological</span> gradient is sufficient for at least a qualitative understanding of species occurrences along the gradient. The results support the hypothesis that colonization has a predominant role for determining the ecological success along the <span class="hlt">hydrological</span> gradient compared to survival. Importantly, the study suggests that it may be possible to <span class="hlt">predict</span> the realized niche of different species from demographic studies. This is encouraging for the important endeavor of <span class="hlt">predicting</span> realized niche dynamics.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.fs.usda.gov/treesearch/pubs/1148','TREESEARCH'); return false;" href="https://www.fs.usda.gov/treesearch/pubs/1148"><span><span class="hlt">Predicting</span> Post-Harvest Performance of <span class="hlt">Advance</span> Red Oak Reproduction in the Southern Appalachians</span></a></p> <p><a target="_blank" href="http://www.fs.usda.gov/treesearch/">Treesearch</a></p> <p>David L. Loftis</p> <p>1990-01-01</p> <p>Models are presented for <span class="hlt">predicting</span>: (1) height growth of red oak <span class="hlt">advance</span> reproduction after clearcutting, and (2) the probability of stems becoming dominants or codominants in new stands as a function of preharvest size of <span class="hlt">advance</span> reproduction andsitequafity. The second model permits silviculturists to <span class="hlt">predict</span>, prior to harvest, the contribution to a new stand of an...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFM.H43J1611K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFM.H43J1611K"><span><span class="hlt">Hydrological</span> alteration of the Upper Nakdong river under AR5 climate change scenarios</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Kim, S.; Park, Y.; Cha, W. Y.; Okjeong, L.; Choi, J.; Lee, J.</p> <p>2016-12-01</p> <p>One of the tasks faced to water engineers is how to consider the climate change impact in our water resources management. Especially in South Korea, where almost all drinking water is taken from major rivers, the public attention is focused on their eco-<span class="hlt">hydrologic</span> status. In this study, the effect of climate change on eco-<span class="hlt">hydrologic</span> regime in the Upper Nakdong river which is one of major rivers in South Korea is investigated using SWAT. The simulation results are measured using the indicators of <span class="hlt">hydrological</span> alteration (IHA) established by U.S. Nature Conservancy. Future climate information is obtained by scaling historical series, provided by Korean Meteorological Administration RCM (KMA RCM) and four RCP scenarios. KMA RCM has 12.5-km spatial resolution in Korean Peninsula and is produced by UK Hedley Centre regional climate model HadGEM3-RA. The RCM bias is corrected by the Kernel density distribution mapping (KDDM) method. The KDDM estimates the cumulative probability density function (CDF) of each dataset using kernel density estimation, and is implemented by quantile-mapping the CDF of a present climate variable obtained from the RCM onto that of the corresponding observed climate variable. Although the simulation results from different RCP scenarios show diverse <span class="hlt">hydrologic</span> responses in our watershed, the mainstream of future simulation results indicate that there will be more river flow in southeast Korea. The <span class="hlt">predicted</span> impacts of <span class="hlt">hydrological</span> alteration caused by climate change on the aquatic ecosystem in the Upper Nakdong river will be presented. Acknowledgement This research was supported by a grant(14AWMP-B082564-01) from <span class="hlt">Advanced</span> Water Management Research Program funded by Ministry of Land, Infrastructure and Transport of Korean government.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015WRR....51.7090P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015WRR....51.7090P"><span>Physically based modeling in catchment <span class="hlt">hydrology</span> at 50: Survey and outlook</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Paniconi, Claudio; Putti, Mario</p> <p>2015-09-01</p> <p>Integrated, process-based numerical models in <span class="hlt">hydrology</span> are rapidly evolving, spurred by novel theories in mathematical physics, <span class="hlt">advances</span> in computational methods, insights from laboratory and field experiments, and the need to better understand and <span class="hlt">predict</span> the potential impacts of population, land use, and climate change on our water resources. At the catchment scale, these simulation models are commonly based on conservation principles for surface and subsurface water flow and solute transport (e.g., the Richards, shallow water, and advection-dispersion equations), and they require robust numerical techniques for their resolution. Traditional (and still open) challenges in developing reliable and efficient models are associated with heterogeneity and variability in parameters and state variables; nonlinearities and scale effects in process dynamics; and complex or poorly known boundary conditions and initial system states. As catchment modeling enters a highly interdisciplinary era, new challenges arise from the need to maintain physical and numerical consistency in the description of multiple processes that interact over a range of scales and across different compartments of an overall system. This paper first gives an historical overview (past 50 years) of some of the key developments in physically based <span class="hlt">hydrological</span> modeling, emphasizing how the interplay between theory, experiments, and modeling has contributed to <span class="hlt">advancing</span> the state of the art. The second part of the paper examines some outstanding problems in integrated catchment modeling from the perspective of recent developments in mathematical and computational science.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFMPA23B0378H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFMPA23B0378H"><span>Transforming Atmospheric and Remotely-Sensed Information to <span class="hlt">Hydrologic</span> <span class="hlt">Predictability</span> in South Asia</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Hopson, T. M.; Riddle, E. E.; Broman, D.; Brakenridge, G. R.; Birkett, C. M.; Kettner, A.; Sampson, K. M.; Boehnert, J.; Priya, S.; Collins, D. C.; Rostkier-Edelstein, D.; Young, W.; Singh, D.; Islam, A. S.</p> <p>2017-12-01</p> <p>South Asia is a flashpoint for natural disasters with profound societal impacts for the region and globally. Although close to 40% of the world's population depends on the Greater Himalaya's great rivers, $20 Billion of GDP is affected by river floods each year. The frequent occurrence of floods, combined with large and rapidly growing populations with high levels of poverty, make South Asia highly susceptible to humanitarian disasters. The challenges of mitigating such devastating disasters are exacerbated by the limited availability of real-time rain and stream gauge measuring stations and transboundary data sharing, and by constrained institutional commitments to overcome these challenges. To overcome such limitations, India and the World Bank have committed resources to the National <span class="hlt">Hydrology</span> Project III, with the development objective to improve the extent, quality, and accessibility of water resources information and to strengthen the capacity of targeted water resources management institutions in India. The availability and application of remote sensing products and weather forecasts from ensemble <span class="hlt">prediction</span> systems (EPS) have transformed river forecasting capability over the last decade, and is of interest to India. In this talk, we review the potential <span class="hlt">predictability</span> of river flow contributed by some of the freely-available remotely-sensed and weather forecasting products within the framework of the physics of water migration through a watershed. Our specific geographical context is the Ganges, Brahmaputra, and Meghna river basin and a newly-available set of stream gauge measurements located over the region. We focus on satellite rainfall estimation, river height and width estimation, and EPS weather forecasts. For the later, we utilize the THORPEX-TIGGE dataset of global forecasts, and discuss how atmospheric <span class="hlt">predictability</span>, as measured by an EPS, is transformed into hydrometeorological <span class="hlt">predictability</span>. We provide an overview of the strengths and</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016WRR....52.9215R','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016WRR....52.9215R"><span>Debates - Stochastic subsurface <span class="hlt">hydrology</span> from theory to practice: Introduction</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Rajaram, Harihar</p> <p>2016-12-01</p> <p>This paper introduces the papers in the "Debates - Stochastic Subsurface <span class="hlt">Hydrology</span> from Theory to Practice" series. Beginning in the 1970s, the field of stochastic subsurface <span class="hlt">hydrology</span> has been an active field of research, with over 3500 journal publications, of which over 850 have appeared in Water Resources Research. We are fortunate to have insightful contributions from four groups of distinguished authors who discuss the reasons why the <span class="hlt">advanced</span> research framework established in stochastic subsurface <span class="hlt">hydrology</span> has not impacted the practice of groundwater flow and transport modeling and design significantly. There is reasonable consensus that a community effort aimed at developing "toolboxes" for applications of stochastic methods will make them more accessible and encourage practical applications.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017JHyd..552...44D','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017JHyd..552...44D"><span>The incorrect usage of singular spectral analysis and discrete wavelet transform in hybrid models to <span class="hlt">predict</span> <span class="hlt">hydrological</span> time series</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Du, Kongchang; Zhao, Ying; Lei, Jiaqiang</p> <p>2017-09-01</p> <p>In <span class="hlt">hydrological</span> time series <span class="hlt">prediction</span>, singular spectrum analysis (SSA) and discrete wavelet transform (DWT) are widely used as preprocessing techniques for artificial neural network (ANN) and support vector machine (SVM) predictors. These hybrid or ensemble models seem to largely reduce the <span class="hlt">prediction</span> error. In current literature researchers apply these techniques to the whole observed time series and then obtain a set of reconstructed or decomposed time series as inputs to ANN or SVM. However, through two comparative experiments and mathematical deduction we found the usage of SSA and DWT in building hybrid models is incorrect. Since SSA and DWT adopt 'future' values to perform the calculation, the series generated by SSA reconstruction or DWT decomposition contain information of 'future' values. These hybrid models caused incorrect 'high' <span class="hlt">prediction</span> performance and may cause large errors in practice.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4128719','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4128719"><span>A Four-Stage Hybrid Model for <span class="hlt">Hydrological</span> Time Series Forecasting</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Di, Chongli; Yang, Xiaohua; Wang, Xiaochao</p> <p>2014-01-01</p> <p><span class="hlt">Hydrological</span> time series forecasting remains a difficult task due to its complicated nonlinear, non-stationary and multi-scale characteristics. To solve this difficulty and improve the <span class="hlt">prediction</span> accuracy, a novel four-stage hybrid model is proposed for <span class="hlt">hydrological</span> time series forecasting based on the principle of ‘denoising, decomposition and ensemble’. The proposed model has four stages, i.e., denoising, decomposition, components <span class="hlt">prediction</span> and ensemble. In the denoising stage, the empirical mode decomposition (EMD) method is utilized to reduce the noises in the <span class="hlt">hydrological</span> time series. Then, an improved method of EMD, the ensemble empirical mode decomposition (EEMD), is applied to decompose the denoised series into a number of intrinsic mode function (IMF) components and one residual component. Next, the radial basis function neural network (RBFNN) is adopted to <span class="hlt">predict</span> the trend of all of the components obtained in the decomposition stage. In the final ensemble <span class="hlt">prediction</span> stage, the forecasting results of all of the IMF and residual components obtained in the third stage are combined to generate the final <span class="hlt">prediction</span> results, using a linear neural network (LNN) model. For illustration and verification, six <span class="hlt">hydrological</span> cases with different characteristics are used to test the effectiveness of the proposed model. The proposed hybrid model performs better than conventional single models, the hybrid models without denoising or decomposition and the hybrid models based on other methods, such as the wavelet analysis (WA)-based hybrid models. In addition, the denoising and decomposition strategies decrease the complexity of the series and reduce the difficulties of the forecasting. With its effective denoising and accurate decomposition ability, high <span class="hlt">prediction</span> precision and wide applicability, the new model is very promising for complex time series forecasting. This new forecast model is an extension of nonlinear <span class="hlt">prediction</span> models. PMID:25111782</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/25111782','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/25111782"><span>A four-stage hybrid model for <span class="hlt">hydrological</span> time series forecasting.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Di, Chongli; Yang, Xiaohua; Wang, Xiaochao</p> <p>2014-01-01</p> <p><span class="hlt">Hydrological</span> time series forecasting remains a difficult task due to its complicated nonlinear, non-stationary and multi-scale characteristics. To solve this difficulty and improve the <span class="hlt">prediction</span> accuracy, a novel four-stage hybrid model is proposed for <span class="hlt">hydrological</span> time series forecasting based on the principle of 'denoising, decomposition and ensemble'. The proposed model has four stages, i.e., denoising, decomposition, components <span class="hlt">prediction</span> and ensemble. In the denoising stage, the empirical mode decomposition (EMD) method is utilized to reduce the noises in the <span class="hlt">hydrological</span> time series. Then, an improved method of EMD, the ensemble empirical mode decomposition (EEMD), is applied to decompose the denoised series into a number of intrinsic mode function (IMF) components and one residual component. Next, the radial basis function neural network (RBFNN) is adopted to <span class="hlt">predict</span> the trend of all of the components obtained in the decomposition stage. In the final ensemble <span class="hlt">prediction</span> stage, the forecasting results of all of the IMF and residual components obtained in the third stage are combined to generate the final <span class="hlt">prediction</span> results, using a linear neural network (LNN) model. For illustration and verification, six <span class="hlt">hydrological</span> cases with different characteristics are used to test the effectiveness of the proposed model. The proposed hybrid model performs better than conventional single models, the hybrid models without denoising or decomposition and the hybrid models based on other methods, such as the wavelet analysis (WA)-based hybrid models. In addition, the denoising and decomposition strategies decrease the complexity of the series and reduce the difficulties of the forecasting. With its effective denoising and accurate decomposition ability, high <span class="hlt">prediction</span> precision and wide applicability, the new model is very promising for complex time series forecasting. This new forecast model is an extension of nonlinear <span class="hlt">prediction</span> models.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017HESS...21.3427C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017HESS...21.3427C"><span>The evolution of process-based <span class="hlt">hydrologic</span> models: historical challenges and the collective quest for physical realism</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Clark, Martyn P.; Bierkens, Marc F. P.; Samaniego, Luis; Woods, Ross A.; Uijlenhoet, Remko; Bennett, Katrina E.; Pauwels, Valentijn R. N.; Cai, Xitian; Wood, Andrew W.; Peters-Lidard, Christa D.</p> <p>2017-07-01</p> <p>The diversity in <span class="hlt">hydrologic</span> models has historically led to great controversy on the <q>correct</q> approach to process-based <span class="hlt">hydrologic</span> modeling, with debates centered on the adequacy of process parameterizations, data limitations and uncertainty, and computational constraints on model analysis. In this paper, we revisit key modeling challenges on requirements to (1) define suitable model equations, (2) define adequate model parameters, and (3) cope with limitations in computing power. We outline the historical modeling challenges, provide examples of modeling <span class="hlt">advances</span> that address these challenges, and define outstanding research needs. We illustrate how modeling <span class="hlt">advances</span> have been made by groups using models of different type and complexity, and we argue for the need to more effectively use our diversity of modeling approaches in order to <span class="hlt">advance</span> our collective quest for physically realistic <span class="hlt">hydrologic</span> models.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFM.H54D..02C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFM.H54D..02C"><span>The evolution of process-based <span class="hlt">hydrologic</span> models: historical challenges and the collective quest for physical realism</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Clark, M. P.; Nijssen, B.; Wood, A.; Mizukami, N.; Newman, A. J.</p> <p>2017-12-01</p> <p>The diversity in <span class="hlt">hydrologic</span> models has historically led to great controversy on the "correct" approach to process-based <span class="hlt">hydrologic</span> modeling, with debates centered on the adequacy of process parameterizations, data limitations and uncertainty, and computational constraints on model analysis. In this paper, we revisit key modeling challenges on requirements to (1) define suitable model equations, (2) define adequate model parameters, and (3) cope with limitations in computing power. We outline the historical modeling challenges, provide examples of modeling <span class="hlt">advances</span> that address these challenges, and define outstanding research needs. We illustrate how modeling <span class="hlt">advances</span> have been made by groups using models of different type and complexity, and we argue for the need to more effectively use our diversity of modeling approaches in order to <span class="hlt">advance</span> our collective quest for physically realistic <span class="hlt">hydrologic</span> models.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/26188405','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/26188405"><span>Eco-<span class="hlt">hydrologic</span> model cascades: Simulating land use and climate change impacts on <span class="hlt">hydrology</span>, hydraulics and habitats for fish and macroinvertebrates.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Guse, Björn; Kail, Jochem; Radinger, Johannes; Schröder, Maria; Kiesel, Jens; Hering, Daniel; Wolter, Christian; Fohrer, Nicola</p> <p>2015-11-15</p> <p>Climate and land use changes affect the hydro- and biosphere at different spatial scales. These changes alter <span class="hlt">hydrological</span> processes at the catchment scale, which impact hydrodynamics and habitat conditions for biota at the river reach scale. In order to investigate the impact of large-scale changes on biota, a cascade of models at different scales is required. Using scenario simulations, the impact of climate and land use change can be compared along the model cascade. Such a cascade of consecutively coupled models was applied in this study. Discharge and water quality are <span class="hlt">predicted</span> with a <span class="hlt">hydrological</span> model at the catchment scale. The hydraulic flow conditions are <span class="hlt">predicted</span> by hydrodynamic models. The habitat suitability under these hydraulic and water quality conditions is assessed based on habitat models for fish and macroinvertebrates. This modelling cascade was applied to <span class="hlt">predict</span> and compare the impacts of climate- and land use changes at different scales to finally assess their effects on fish and macroinvertebrates. Model simulations revealed that magnitude and direction of change differed along the modelling cascade. Whilst the <span class="hlt">hydrological</span> model <span class="hlt">predicted</span> a relevant decrease of discharge due to climate change, the hydraulic conditions changed less. Generally, the habitat suitability for fish decreased but this was strongly species-specific and suitability even increased for some species. In contrast to climate change, the effect of land use change on discharge was negligible. However, land use change had a stronger impact on the modelled nitrate concentrations affecting the abundances of macroinvertebrates. The scenario simulations for the two organism groups illustrated that direction and intensity of changes in habitat suitability are highly species-dependent. Thus, a joined model analysis of different organism groups combined with the results of <span class="hlt">hydrological</span> and hydrodynamic models is recommended to assess the impact of climate and land use changes on</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016JHyd..541..800M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016JHyd..541..800M"><span>Validation of a national <span class="hlt">hydrological</span> model</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>McMillan, H. K.; Booker, D. J.; Cattoën, C.</p> <p>2016-10-01</p> <p>Nationwide <span class="hlt">predictions</span> of flow time-series are valuable for development of policies relating to environmental flows, calculating reliability of supply to water users, or assessing risk of floods or droughts. This breadth of model utility is possible because various <span class="hlt">hydrological</span> signatures can be derived from simulated flow time-series. However, producing national <span class="hlt">hydrological</span> simulations can be challenging due to strong environmental diversity across catchments and a lack of data available to aid model parameterisation. A comprehensive and consistent suite of test procedures to quantify spatial and temporal patterns in performance across various parts of the hydrograph is described and applied to quantify the performance of an uncalibrated national rainfall-runoff model of New Zealand. Flow time-series observed at 485 gauging stations were used to calculate Nash-Sutcliffe efficiency and percent bias when simulating between-site differences in daily series, between-year differences in annual series, and between-site differences in <span class="hlt">hydrological</span> signatures. The procedures were used to assess the benefit of applying a correction to the modelled flow duration curve based on an independent statistical analysis. They were used to aid understanding of climatological, <span class="hlt">hydrological</span> and model-based causes of differences in <span class="hlt">predictive</span> performance by assessing multiple hypotheses that describe where and when the model was expected to perform best. As the procedures produce quantitative measures of performance, they provide an objective basis for model assessment that could be applied when comparing observed daily flow series with competing simulated flow series from any region-wide or nationwide <span class="hlt">hydrological</span> model. Model performance varied in space and time with better scores in larger and medium-wet catchments, and in catchments with smaller seasonal variations. Surprisingly, model performance was not sensitive to aquifer fraction or rain gauge density.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/26831449','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/26831449"><span>Small scale green infrastructure design to meet different urban <span class="hlt">hydrological</span> criteria.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Jia, Z; Tang, S; Luo, W; Li, S; Zhou, M</p> <p>2016-04-15</p> <p>As small scale green infrastructures, rain gardens have been widely advocated for urban stormwater management in the contemporary low impact development (LID) era. This paper presents a simple method that consists of <span class="hlt">hydrological</span> models and the matching plots of nomographs to provide an informative and practical tool for rain garden sizing and <span class="hlt">hydrological</span> evaluation. The proposed method considers design storms, infiltration rates and the runoff contribution area ratio of the rain garden, allowing users to size a rain garden for a specific site with <span class="hlt">hydrological</span> reference and <span class="hlt">predict</span> overflow of the rain garden under different storms. The nomographs provide a visual presentation on the sensitivity of different design parameters. Subsequent application of the proposed method to a case study conducted in a sub-humid region in China showed that, the method accurately <span class="hlt">predicted</span> the design storms for the existing rain garden, the <span class="hlt">predicted</span> overflows under large storm events were within 13-50% of the measured volumes. The results suggest that the nomographs approach is a practical tool for quick selection or assessment of design options that incorporate key <span class="hlt">hydrological</span> parameters of rain gardens or other infiltration type green infrastructure. The graphic approach as displayed by the nomographs allow urban planners to demonstrate the <span class="hlt">hydrological</span> effect of small scale green infrastructure and gain more support for promoting low impact development. Copyright © 2016 Elsevier Ltd. All rights reserved.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/13950','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/13950"><span>Application of seismic-refraction techniques to <span class="hlt">hydrologic</span> studies</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Haeni, F.P.</p> <p>1986-01-01</p> <p>During the past 30 years, seismic-refraction methods have been used extensively in petroleum, mineral, and engineering investigations, and to some extent for <span class="hlt">hydrologic</span> applications. Recent <span class="hlt">advances</span> in equipment, sound sources, and computer interpretation techniques make seismic refraction a highly effective and economical means of obtaining subsurface data in <span class="hlt">hydrologic</span> studies. Aquifers that can be defined by one or more high seismic-velocity surfaces, such as (1) alluvial or glacial deposits in consolidated rock valleys, (2) limestone or sandstone underlain by metamorphic or igneous rock, or (3) saturated unconsolidated deposits overlain by unsaturated unconsolidated deposits,are ideally suited for applying seismic-refraction methods. These methods allow the economical collection of subsurface data, provide the basis for more efficient collection of data by test drilling or aquifer tests, and result in improved <span class="hlt">hydrologic</span> studies.This manual briefly reviews the basics of seismic-refraction theory and principles. It emphasizes the use of this technique in <span class="hlt">hydrologic</span> investigations and describes the planning, equipment, field procedures, and intrepretation techniques needed for this type of study.Examples of the use of seismic-refraction techniques in a wide variety of <span class="hlt">hydrologic</span> studies are presented.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.usgs.gov/twri/twri2d2/','USGSPUBS'); return false;" href="https://pubs.usgs.gov/twri/twri2d2/"><span>Application of seismic-refraction techniques to <span class="hlt">hydrologic</span> studies</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Haeni, F.P.</p> <p>1988-01-01</p> <p>During the past 30 years, seismic-refraction methods have been used extensively in petroleum, mineral, and engineering investigations and to some extent for <span class="hlt">hydrologic</span> applications. Recent <span class="hlt">advances</span> in equipment, sound sources, and computer interpretation techniques make seismic refraction a highly effective and economical means of obtaining subsurface data in <span class="hlt">hydrologic</span> studies. Aquifers that can be defined by one or more high-seismic-velocity surface, such as (1) alluvial or glacial deposits in consolidated rock valleys, (2) limestone or sandstone underlain by metamorphic or igneous rock, or (3) saturated unconsolidated deposits overlain by unsaturated unconsolidated deposits, are ideally suited for seismic-refraction methods. These methods allow economical collection of subsurface data, provide the basis for more efficient collection of data by test drilling or aquifer tests, and result in improved <span class="hlt">hydrologic</span> studies. This manual briefly reviews the basics of seismic-refraction theory and principles. It emphasizes the use of these techniques in <span class="hlt">hydrologic</span> investigations and describes the planning, equipment, field procedures, and interpretation techniques needed for this type of study. Further-more, examples of the use of seismic-refraction techniques in a wide variety of <span class="hlt">hydrologic</span> studies are presented.</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_11");'>11</a></li> <li><a href="#" onclick='return showDiv("page_12");'>12</a></li> <li class="active"><span>13</span></li> <li><a href="#" onclick='return showDiv("page_14");'>14</a></li> <li><a href="#" onclick='return showDiv("page_15");'>15</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_13 --> <div id="page_14" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_12");'>12</a></li> <li><a href="#" onclick='return showDiv("page_13");'>13</a></li> <li class="active"><span>14</span></li> <li><a href="#" onclick='return showDiv("page_15");'>15</a></li> <li><a href="#" onclick='return showDiv("page_16");'>16</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="261"> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015AGUFM.H42A..07H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015AGUFM.H42A..07H"><span><span class="hlt">Hydrology</span> Domain Cyberinfrastructures: Successes, Challenges, and Opportunities</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Horsburgh, J. S.</p> <p>2015-12-01</p> <p>Anticipated changes to climate, human population, land use, and urban form will alter the <span class="hlt">hydrology</span> and availability of water within the water systems on which the world's population relies. Understanding the effects of these changes will be paramount in sustainably managing water resources, as well as maintaining associated capacity to provide ecosystem services (e.g., regulating flooding, maintaining instream flow during dry periods, cycling nutrients, and maintaining water quality). It will require better information characterizing both natural and human mediated <span class="hlt">hydrologic</span> systems and enhanced ability to generate, manage, store, analyze, and share growing volumes of observational data. Over the past several years, a number of <span class="hlt">hydrology</span> domain cyberinfrastructures have emerged or are currently under development that are focused on providing integrated access to and analysis of data for cross-domain synthesis studies. These include the Consortium of Universities for the <span class="hlt">Advancement</span> of <span class="hlt">Hydrologic</span> Science, Inc. (CUAHSI) <span class="hlt">Hydrologic</span> Information System (HIS), the Critical Zone Observatory Information System (CZOData), HyroShare, the BiG CZ software system, and others. These systems have focused on sharing, integrating, and analyzing <span class="hlt">hydrologic</span> observations data. This presentation will describe commonalities and differences in the cyberinfrastructure approaches used by these projects and will highlight successes and lessons learned in addressing the challenges of big and complex data. It will also identify new challenges and opportunities for next generation cyberinfrastructure and a next generation of cyber-savvy scientists and engineers as developers and users.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/28247928','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/28247928"><span><span class="hlt">Advancing</span> alternatives analysis: The role of <span class="hlt">predictive</span> toxicology in selecting safer chemical products and processes.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Malloy, Timothy; Zaunbrecher, Virginia; Beryt, Elizabeth; Judson, Richard; Tice, Raymond; Allard, Patrick; Blake, Ann; Cote, Ila; Godwin, Hilary; Heine, Lauren; Kerzic, Patrick; Kostal, Jakub; Marchant, Gary; McPartland, Jennifer; Moran, Kelly; Nel, Andre; Ogunseitan, Oladele; Rossi, Mark; Thayer, Kristina; Tickner, Joel; Whittaker, Margaret; Zarker, Ken</p> <p>2017-09-01</p> <p>Alternatives analysis (AA) is a method used in regulation and product design to identify, assess, and evaluate the safety and viability of potential substitutes for hazardous chemicals. It requires toxicological data for the existing chemical and potential alternatives. <span class="hlt">Predictive</span> toxicology uses in silico and in vitro approaches, computational models, and other tools to expedite toxicological data generation in a more cost-effective manner than traditional approaches. The present article briefly reviews the challenges associated with using <span class="hlt">predictive</span> toxicology in regulatory AA, then presents 4 recommendations for its <span class="hlt">advancement</span>. It recommends using case studies to <span class="hlt">advance</span> the integration of <span class="hlt">predictive</span> toxicology into AA, adopting a stepwise process to employing <span class="hlt">predictive</span> toxicology in AA beginning with prioritization of chemicals of concern, leveraging existing resources to <span class="hlt">advance</span> the integration of <span class="hlt">predictive</span> toxicology into the practice of AA, and supporting transdisciplinary efforts. The further incorporation of <span class="hlt">predictive</span> toxicology into AA would <span class="hlt">advance</span> the ability of companies and regulators to select alternatives to harmful ingredients, and potentially increase the use of <span class="hlt">predictive</span> toxicology in regulation more broadly. Integr Environ Assess Manag 2017;13:915-925. © 2017 SETAC. © 2017 SETAC.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=19920067700&hterms=propeller+noise&qs=N%3D0%26Ntk%3DAll%26Ntx%3Dmode%2Bmatchall%26Ntt%3Dpropeller%2Bnoise','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=19920067700&hterms=propeller+noise&qs=N%3D0%26Ntk%3DAll%26Ntx%3Dmode%2Bmatchall%26Ntt%3Dpropeller%2Bnoise"><span><span class="hlt">Advanced</span> propeller noise <span class="hlt">prediction</span> in the time domain</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Farassat, F.; Dunn, M. H.; Spence, P. L.</p> <p>1992-01-01</p> <p>The time domain code ASSPIN gives acousticians a powerful technique of <span class="hlt">advanced</span> propeller noise <span class="hlt">prediction</span>. Except for nonlinear effects, the code uses exact solutions of the Ffowcs Williams-Hawkings equation with exact blade geometry and kinematics. By including nonaxial inflow, periodic loading noise, and adaptive time steps to accelerate computer execution, the development of this code becomes complete.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFM.H34B..02B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFM.H34B..02B"><span>Using <span class="hlt">Predictive</span> Uncertainty Analysis to Assess <span class="hlt">Hydrologic</span> Model Performance for a Watershed in Oregon</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Brannan, K. M.; Somor, A.</p> <p>2016-12-01</p> <p>A variety of statistics are used to assess watershed model performance but these statistics do not directly answer the question: what is the uncertainty of my <span class="hlt">prediction</span>. Understanding <span class="hlt">predictive</span> uncertainty is important when using a watershed model to develop a Total Maximum Daily Load (TMDL). TMDLs are a key component of the US Clean Water Act and specify the amount of a pollutant that can enter a waterbody when the waterbody meets water quality criteria. TMDL developers use watershed models to estimate pollutant loads from nonpoint sources of pollution. We are developing a TMDL for bacteria impairments in a watershed in the Coastal Range of Oregon. We setup an HSPF model of the watershed and used the calibration software PEST to estimate HSPF <span class="hlt">hydrologic</span> parameters and then perform <span class="hlt">predictive</span> uncertainty analysis of stream flow. We used Monte-Carlo simulation to run the model with 1,000 different parameter sets and assess <span class="hlt">predictive</span> uncertainty. In order to reduce the chance of specious parameter sets, we accounted for the relationships among parameter values by using mathematically-based regularization techniques and an estimate of the parameter covariance when generating random parameter sets. We used a novel approach to select flow data for <span class="hlt">predictive</span> uncertainty analysis. We set aside flow data that occurred on days that bacteria samples were collected. We did not use these flows in the estimation of the model parameters. We calculated a percent uncertainty for each flow observation based 1,000 model runs. We also used several methods to visualize results with an emphasis on making the data accessible to both technical and general audiences. We will use the <span class="hlt">predictive</span> uncertainty estimates in the next phase of our work, simulating bacteria fate and transport in the watershed.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/27100019','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/27100019"><span>Sensitivity of river fishes to climate change: The role of <span class="hlt">hydrological</span> stressors on habitat range shifts.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Segurado, Pedro; Branco, Paulo; Jauch, Eduardo; Neves, Ramiro; Ferreira, M Teresa</p> <p>2016-08-15</p> <p>Climate change will <span class="hlt">predictably</span> change <span class="hlt">hydrological</span> patterns and processes at the catchment scale, with impacts on habitat conditions for fish. The main goal of this study is to assess how shifts in fish habitat favourability under climate change scenarios are affected by <span class="hlt">hydrological</span> stressors. The interplay between climate and <span class="hlt">hydrological</span> stressors has important implications in river management under climate change because management actions to control <span class="hlt">hydrological</span> parameters are more feasible than controlling climate. This study was carried out in the Tamega catchment of the Douro basin. A set of <span class="hlt">hydrological</span> stressor variables were generated through a process-based modelling based on current climate data (2008-2014) and also considering a high-end future climate change scenario. The resulting parameters, along with climatic and site-descriptor variables were used as explanatory variables in empirical habitat models for nine fish species using boosted regression trees. Models were calibrated for the whole Douro basin using 254 fish sampling sites and <span class="hlt">predictions</span> under future climate change scenarios were made for the Tamega catchment. Results show that models using climatic variables but not <span class="hlt">hydrological</span> stressors produce more stringent <span class="hlt">predictions</span> of future favourability, <span class="hlt">predicting</span> more distribution contractions or stronger range shifts. The use of <span class="hlt">hydrological</span> stressors strongly influences projections of habitat favourability shifts; the integration of these stressors in the models thinned shifts in range due to climate change. <span class="hlt">Hydrological</span> stressors were retained in the models for most species and had a high importance, demonstrating that it is important to integrate <span class="hlt">hydrology</span> in studies of impacts of climate change on freshwater fishes. This is a relevant result because it means that management actions to control <span class="hlt">hydrological</span> parameters in rivers will have an impact on the effects of climate change and may potentially be helpful to mitigate its negative</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://cfpub.epa.gov/si/si_public_record_report.cfm?direntryid=312410&keyword=climate%20change&subject=climate%20change%20research&showcriteria=2&fed_org_id=111&datebeginpublishedpresented=02/22/2012&dateendpublishedpresented=02/22/2017&sortby=pubdateyear','PESTICIDES'); return false;" href="https://cfpub.epa.gov/si/si_public_record_report.cfm?direntryid=312410&keyword=climate%20change&subject=climate%20change%20research&showcriteria=2&fed_org_id=111&datebeginpublishedpresented=02/22/2012&dateendpublishedpresented=02/22/2017&sortby=pubdateyear"><span>Applicability of <span class="hlt">Hydrologic</span> Landscapes for Model Calibration ...</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>The Pacific Northwest <span class="hlt">Hydrologic</span> Landscapes (PNW HL) at the assessment unit scale has provided a solid conceptual classification framework to relate and transfer <span class="hlt">hydrologically</span> meaningful information between watersheds without access to streamflow time series. A collection of techniques were applied to the HL assessment unit composition in watersheds across the Pacific Northwest to aggregate the <span class="hlt">hydrologic</span> behavior of the <span class="hlt">Hydrologic</span> Landscapes from the assessment unit scale to the watershed scale. This non-trivial solution both emphasizes HL classifications within the watershed that provide that majority of moisture surplus/deficit and considers the relative position (upstream vs. downstream) of these HL classifications. A clustering algorithm was applied to the HL-based characterization of assessment units within 185 watersheds to help organize watersheds into nine classes hypothesized to have similar <span class="hlt">hydrologic</span> behavior. The HL-based classes were used to organize and describe <span class="hlt">hydrologic</span> behavior information about watershed classes and both <span class="hlt">predictions</span> and validations were independently performed with regard to the general magnitude of six hydroclimatic signature values. A second cluster analysis was then performed using the independently calculated signature values as similarity metrics, and it was found that the six signature clusters showed substantial overlap in watershed class membership to those in the HL-based classes. One hypothesis set forward from thi</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/servlets/purl/1398930','SCIGOV-STC'); return false;" href="https://www.osti.gov/servlets/purl/1398930"><span>The evolution of process-based <span class="hlt">hydrologic</span> models: historical challenges and the collective quest for physical realism</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>Clark, Martyn P.; Bierkens, Marc F. P.; Samaniego, Luis</p> <p></p> <p>The diversity in <span class="hlt">hydrologic</span> models has historically led to great controversy on the correct approach to process-based <span class="hlt">hydrologic</span> modeling, with debates centered on the adequacy of process parameterizations, data limitations and uncertainty, and computational constraints on model analysis. Here, we revisit key modeling challenges on requirements to (1) define suitable model equations, (2) define adequate model parameters, and (3) cope with limitations in computing power. We outline the historical modeling challenges, provide examples of modeling <span class="hlt">advances</span> that address these challenges, and define outstanding research needs. We also illustrate how modeling <span class="hlt">advances</span> have been made by groups using models of different type and complexity,more » and we argue for the need to more effectively use our diversity of modeling approaches in order to <span class="hlt">advance</span> our collective quest for physically realistic <span class="hlt">hydrologic</span> models.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/pages/biblio/1398930-evolution-process-based-hydrologic-models-historical-challenges-collective-quest-physical-realism','SCIGOV-DOEP'); return false;" href="https://www.osti.gov/pages/biblio/1398930-evolution-process-based-hydrologic-models-historical-challenges-collective-quest-physical-realism"><span>The evolution of process-based <span class="hlt">hydrologic</span> models: historical challenges and the collective quest for physical realism</span></a></p> <p><a target="_blank" href="http://www.osti.gov/pages">DOE PAGES</a></p> <p>Clark, Martyn P.; Bierkens, Marc F. P.; Samaniego, Luis; ...</p> <p>2017-07-11</p> <p>The diversity in <span class="hlt">hydrologic</span> models has historically led to great controversy on the correct approach to process-based <span class="hlt">hydrologic</span> modeling, with debates centered on the adequacy of process parameterizations, data limitations and uncertainty, and computational constraints on model analysis. Here, we revisit key modeling challenges on requirements to (1) define suitable model equations, (2) define adequate model parameters, and (3) cope with limitations in computing power. We outline the historical modeling challenges, provide examples of modeling <span class="hlt">advances</span> that address these challenges, and define outstanding research needs. We also illustrate how modeling <span class="hlt">advances</span> have been made by groups using models of different type and complexity,more » and we argue for the need to more effectively use our diversity of modeling approaches in order to <span class="hlt">advance</span> our collective quest for physically realistic <span class="hlt">hydrologic</span> models.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2011AGUFMGC33C..03W','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2011AGUFMGC33C..03W"><span>Drought Monitoring and Forecasting Using the Princeton/U Washington National <span class="hlt">Hydrologic</span> Forecasting System</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Wood, E. F.; Yuan, X.; Roundy, J. K.; Lettenmaier, D. P.; Mo, K. C.; Xia, Y.; Ek, M. B.</p> <p>2011-12-01</p> <p>Extreme <span class="hlt">hydrologic</span> events in the form of droughts or floods are a significant source of social and economic damage in many parts of the world. Having sufficient warning of extreme events allows managers to prepare for and reduce the severity of their impacts. A <span class="hlt">hydrologic</span> forecast system can give seasonal <span class="hlt">predictions</span> that can be used by mangers to make better decisions; however there is still much uncertainty associated with such a system. Therefore it is important to understand the forecast skill of the system before transitioning to operational usage. Seasonal reforecasts (1982 - 2010) from the NCEP Climate Forecast System (both version 1 (CFS) and version 2 (CFSv2), Climate <span class="hlt">Prediction</span> Center (CPC) outlooks and the European Seasonal Interannual <span class="hlt">Prediction</span> (EUROSIP) system, are assessed for forecasting skill in drought <span class="hlt">prediction</span> across the U.S., both singularly and as a multi-model system The Princeton/U Washington national <span class="hlt">hydrologic</span> monitoring and forecast system is being implemented at NCEP/EMC via their Climate Test Bed as the experimental <span class="hlt">hydrological</span> forecast system to support U.S. operational drought <span class="hlt">prediction</span>. Using our system, the seasonal forecasts are biased corrected, downscaled and used to drive the Variable Infiltration Capacity (VIC) land surface model to give seasonal forecasts of <span class="hlt">hydrologic</span> variables with lead times of up to six months. Results are presented for a number of events, with particular focus on the Apalachicola-Chattahoochee-Flint (ACF) River Basin in the South Eastern United States, which has experienced a number of severe droughts in recent years and is a pilot study basin for the National Integrated Drought Information System (NIDIS). The performance of the VIC land surface model is evaluated using observational forcing when compared to observed streamflow. The effectiveness of the forecast system to <span class="hlt">predict</span> streamflow and soil moisture is evaluated when compared with observed streamflow and modeled soil moisture driven by</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014HESS...18.3301H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014HESS...18.3301H"><span>The importance of <span class="hlt">hydrological</span> uncertainty assessment methods in climate change impact studies</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Honti, M.; Scheidegger, A.; Stamm, C.</p> <p>2014-08-01</p> <p>Climate change impact assessments have become more and more popular in <span class="hlt">hydrology</span> since the middle 1980s with a recent boost after the publication of the IPCC AR4 report. From hundreds of impact studies a quasi-standard methodology has emerged, to a large extent shaped by the growing public demand for <span class="hlt">predicting</span> how water resources management or flood protection should change in the coming decades. The "standard" workflow relies on a model cascade from global circulation model (GCM) <span class="hlt">predictions</span> for selected IPCC scenarios to future catchment <span class="hlt">hydrology</span>. Uncertainty is present at each level and propagates through the model cascade. There is an emerging consensus between many studies on the relative importance of the different uncertainty sources. The prevailing perception is that GCM uncertainty dominates <span class="hlt">hydrological</span> impact studies. Our hypothesis was that the relative importance of climatic and <span class="hlt">hydrologic</span> uncertainty is (among other factors) heavily influenced by the uncertainty assessment method. To test this we carried out a climate change impact assessment and estimated the relative importance of the uncertainty sources. The study was performed on two small catchments in the Swiss Plateau with a lumped conceptual rainfall runoff model. In the climatic part we applied the standard ensemble approach to quantify uncertainty but in <span class="hlt">hydrology</span> we used formal Bayesian uncertainty assessment with two different likelihood functions. One was a time series error model that was able to deal with the complicated statistical properties of <span class="hlt">hydrological</span> model residuals. The second was an approximate likelihood function for the flow quantiles. The results showed that the expected climatic impact on flow quantiles was small compared to <span class="hlt">prediction</span> uncertainty. The choice of uncertainty assessment method actually determined what sources of uncertainty could be identified at all. This demonstrated that one could arrive at rather different conclusions about the causes behind</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.dtic.mil/docs/citations/ADA566501','DTIC-ST'); return false;" href="http://www.dtic.mil/docs/citations/ADA566501"><span>Early <span class="hlt">Prediction</span> of Lupus Nephritis Using <span class="hlt">Advanced</span> Proteomics</span></a></p> <p><a target="_blank" href="http://www.dtic.mil/">DTIC Science & Technology</a></p> <p></p> <p>2012-06-01</p> <p>urine samples for research were obtained, and information on the following laboratory measures was collected: BUN ( urea ), serum creatinine, serum... urine chemistry), medications and other clinical outcomes (overall disease activity, renal and overall damage). Specific Aim 2: <span class="hlt">Advanced</span> proteomic...measured by the external standards. We concluded that serial measurements of plasma and urine NGAL may be valuable in <span class="hlt">predicting</span> impending worsening of</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://cfpub.epa.gov/si/si_public_record_report.cfm?dirEntryId=203230&keyword=european+AND+union&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=203230&keyword=european+AND+union&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>Development of <span class="hlt">hydrologic</span> landscape regions for classifying <span class="hlt">hydrologic</span> permanace and <span class="hlt">hydrological</span>-ecological interactions</span></a></p> <p><a target="_blank" href="http://oaspub.epa.gov/eims/query.page">EPA Science Inventory</a></p> <p></p> <p></p> <p>In a 2001 paper, Winter proposed the concept of the <span class="hlt">hydrologic</span> landscape unit as a fundamental unit composed of an upland and lowland separated by a steeper slope. Winter suggested that this concept could be useful for <span class="hlt">hydrologic</span> research, data analysis, and comparing <span class="hlt">hydrologic</span>...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2008AGUFM.H51E0870L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2008AGUFM.H51E0870L"><span>Ensemble Analysis of Variational Assimilation of <span class="hlt">Hydrologic</span> and Hydrometeorological Data into Distributed <span class="hlt">Hydrologic</span> Model</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Lee, H.; Seo, D.; Koren, V.</p> <p>2008-12-01</p> <p>A prototype 4DVAR (four-dimensional variational) data assimilator for gridded Sacramento soil-moisture accounting and kinematic-wave routing models in the <span class="hlt">Hydrology</span> Laboratory's Research Distributed <span class="hlt">Hydrologic</span> Model (HL-RDHM) has been developed. The prototype assimilates streamflow and in-situ soil moisture data and adjusts gridded precipitation and climatological potential evaporation data to reduce uncertainty in the model initial conditions for improved monitoring and <span class="hlt">prediction</span> of streamflow and soil moisture at the outlet and interior locations within the catchment. Due to large degrees of freedom involved, data assimilation (DA) into distributed <span class="hlt">hydrologic</span> models is complex. To understand and assess sensitivity of the performance of DA to uncertainties in the model initial conditions and in the data, two synthetic experiments have been carried out in an ensemble framework. Results from the synthetic experiments shed much light on the potential and limitations with DA into distributed models. For initial real-world assessment, the prototype DA has also been applied to the headwater basin at Eldon near the Oklahoma-Arkansas border. We present these results and describe the next steps.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015EGUGA..17..713B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015EGUGA..17..713B"><span><span class="hlt">Prediction</span> of soil stability and erosion in semiarid regions using numerical <span class="hlt">hydrological</span> model (MCAT) and airborne hyperspectral imagery</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Brook, Anna; Wittenberg, Lea</p> <p>2015-04-01</p> <p>Long-term environmental monitoring is addressed to identify physical and biological changes and progresses taking place in the ecosystem. This basic action of landscape monitoring is an essential part of the systematic long-term surveillance, aiming to evaluate, assess and <span class="hlt">predict</span> the spatial change and progresses. Indeed, it provides a context for wide range of diverse studies and research frameworks from regional or global scale. Spatial-temporal trends and changes at various scales (massive to less certain) require establishing consistent baseline data over time. One of the spatial cases of landscape monitoring is dedicated to soil formation and pedological progresses. It is previously acknowledged that changes in soil affect the functionality of the environment, so monitoring changes recently become important cause considerable resources in areas such as environmental management, sustainability services, and protecting the environment healthy. Given the above, it can be concluded that monitoring changes in the base for sustainable development. The <span class="hlt">hydrological</span> response of bare soils and watersheds in semiarid regions to intense rainfall events is known to be complex due to multiply physical and structural impacts and feedbacks. As a result, the comprehensive evaluations of mathematical models including detailed consideration of uncertainties in the modeling of <span class="hlt">hydrological</span> and environmental systems are of increasing importance. The presented method incorporates means of remote sensing data, <span class="hlt">hydrological</span> and climate data and implementing dedicated and integrative Monte Carlo Analysis Toolbox (MCAT) model for semiarid region. Complexity of practical models to represent spatial systems requires an extensive understanding of the spatial phenomena, while providing realistic balance of sensitivity and corresponding uncertainty levels. Nowadays a large number of dedicated mathematical models applied to assess environmental <span class="hlt">hydrological</span> process. Among the most</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013AGUFM.H21M..04V','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013AGUFM.H21M..04V"><span>Fusing Unmanned Aerial Vehicle Imagery with High Resolution <span class="hlt">Hydrologic</span> Modeling (Invited)</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Vivoni, E. R.; Pierini, N.; Schreiner-McGraw, A.; Anderson, C.; Saripalli, S.; Rango, A.</p> <p>2013-12-01</p> <p>After decades of development and applications, high resolution <span class="hlt">hydrologic</span> models are now common tools in research and increasingly used in practice. More recently, high resolution imagery from unmanned aerial vehicles (UAVs) that provide information on land surface properties have become available for civilian applications. Fusing the two approaches promises to significantly <span class="hlt">advance</span> the state-of-the-art in terms of <span class="hlt">hydrologic</span> modeling capabilities. This combination will also challenge assumptions on model processes, parameterizations and scale as land surface characteristics (~0.1 to 1 m) may now surpass traditional model resolutions (~10 to 100 m). Ultimately, <span class="hlt">predictions</span> from high resolution <span class="hlt">hydrologic</span> models need to be consistent with the observational data that can be collected from UAVs. This talk will describe our efforts to develop, utilize and test the impact of UAV-derived topographic and vegetation fields on the simulation of two small watersheds in the Sonoran and Chihuahuan Deserts at the Santa Rita Experimental Range (Green Valley, AZ) and the Jornada Experimental Range (Las Cruces, NM). High resolution digital terrain models, image orthomosaics and vegetation species classification were obtained from a fixed wing airplane and a rotary wing helicopter, and compared to coarser analyses and products, including Light Detection and Ranging (LiDAR). We focus the discussion on the relative improvements achieved with UAV-derived fields in terms of terrain-<span class="hlt">hydrologic</span>-vegetation analyses and summer season simulations using the TIN-based Real-time Integrated Basin Simulator (tRIBS) model. Model simulations are evaluated at each site with respect to a high-resolution sensor network consisting of six rain gauges, forty soil moisture and temperature profiles, four channel runoff flumes, a cosmic-ray soil moisture sensor and an eddy covariance tower over multiple summer periods. We also discuss prospects for the fusion of high resolution models with novel</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29614852','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29614852"><span><span class="hlt">Advanced</span> Daily <span class="hlt">Prediction</span> Model for National Suicide Numbers with Social Media Data.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Lee, Kyung Sang; Lee, Hyewon; Myung, Woojae; Song, Gil-Young; Lee, Kihwang; Kim, Ho; Carroll, Bernard J; Kim, Doh Kwan</p> <p>2018-04-01</p> <p>Suicide is a significant public health concern worldwide. Social media data have a potential role in identifying high suicide risk individuals and also in <span class="hlt">predicting</span> suicide rate at the population level. In this study, we report an <span class="hlt">advanced</span> daily suicide <span class="hlt">prediction</span> model using social media data combined with economic/meteorological variables along with observed suicide data lagged by 1 week. The social media data were drawn from weblog posts. We examined a total of 10,035 social media keywords for suicide <span class="hlt">prediction</span>. We made <span class="hlt">predictions</span> of national suicide numbers 7 days in <span class="hlt">advance</span> daily for 2 years, based on a daily moving 5-year <span class="hlt">prediction</span> modeling period. Our model <span class="hlt">predicted</span> the likely range of daily national suicide numbers with 82.9% accuracy. Among the social media variables, words denoting economic issues and mood status showed high <span class="hlt">predictive</span> strength. Observed number of suicides one week previously, recent celebrity suicide, and day of week followed by stock index, consumer price index, and sunlight duration 7 days before the target date were notable predictors along with the social media variables. These results strengthen the case for social media data to supplement classical social/economic/climatic data in forecasting national suicide events.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70022063','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70022063"><span><span class="hlt">Hydrological</span> responses to dynamically and statistically downscaled climate model output</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Wilby, R.L.; Hay, L.E.; Gutowski, W.J.; Arritt, R.W.; Takle, E.S.; Pan, Z.; Leavesley, G.H.; Clark, M.P.</p> <p>2000-01-01</p> <p>Daily rainfall and surface temperature series were simulated for the Animas River basin, Colorado using dynamically and statistically downscaled output from the National Center for Environmental <span class="hlt">Prediction</span>/National Center for Atmospheric Research (NCEP/NCAR) re-analysis. A distributed <span class="hlt">hydrological</span> model was then applied to the downscaled data. Relative to raw NCEP output, downscaled climate variables provided more realistic stimulations of basin scale <span class="hlt">hydrology</span>. However, the results highlight the sensitivity of modeled processes to the choice of downscaling technique, and point to the need for caution when interpreting future <span class="hlt">hydrological</span> scenarios.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFMIN13B0070O','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFMIN13B0070O"><span>Quo vadis: <span class="hlt">Hydrologic</span> inverse analyses using high-performance computing and a D-Wave quantum annealer</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>O'Malley, D.; Vesselinov, V. V.</p> <p>2017-12-01</p> <p>Classical microprocessors have had a dramatic impact on <span class="hlt">hydrology</span> for decades, due largely to the exponential growth in computing power <span class="hlt">predicted</span> by Moore's law. However, this growth is not expected to continue indefinitely and has already begun to slow. Quantum computing is an emerging alternative to classical microprocessors. Here, we demonstrated cutting edge inverse model analyses utilizing some of the best available resources in both worlds: high-performance classical computing and a D-Wave quantum annealer. The classical high-performance computing resources are utilized to build an <span class="hlt">advanced</span> numerical model that assimilates data from O(10^5) observations, including water levels, drawdowns, and contaminant concentrations. The developed model accurately reproduces the <span class="hlt">hydrologic</span> conditions at a Los Alamos National Laboratory contamination site, and can be leveraged to inform decision-making about site remediation. We demonstrate the use of a D-Wave 2X quantum annealer to solve <span class="hlt">hydrologic</span> inverse problems. This work can be seen as an early step in quantum-computational <span class="hlt">hydrology</span>. We compare and contrast our results with an early inverse approach in classical-computational <span class="hlt">hydrology</span> that is comparable to the approach we use with quantum annealing. Our results show that quantum annealing can be useful for identifying regions of high and low permeability within an aquifer. While the problems we consider are small-scale compared to the problems that can be solved with modern classical computers, they are large compared to the problems that could be solved with early classical CPUs. Further, the binary nature of the high/low permeability problem makes it well-suited to quantum annealing, but challenging for classical computers.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.fs.usda.gov/treesearch/pubs/49779','TREESEARCH'); return false;" href="https://www.fs.usda.gov/treesearch/pubs/49779"><span>Representing northern peatland microtopography and <span class="hlt">hydrology</span> within the Community Land Model</span></a></p> <p><a target="_blank" href="http://www.fs.usda.gov/treesearch/">Treesearch</a></p> <p>X. Shi; P.E. Thornton; D.M. Ricciuto; P J. Hanson; J. Mao; Stephen Sebestyen; N.A. Griffiths; G. Bisht</p> <p>2015-01-01</p> <p><span class="hlt">Predictive</span> understanding of northern peatland <span class="hlt">hydrology</span> is a necessary precursor to understanding the fate of massive carbon stores in these systems under the influence of present and future climate change. Current models have begun to address microtopographic controls on peatland <span class="hlt">hydrology</span>, but none have included a prognostic calculation of peatland water table depth...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017ApWS....7.3323H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017ApWS....7.3323H"><span>Estimating <span class="hlt">hydrologic</span> budgets for six Persian Gulf watersheds, Iran</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Hosseini, Majid; Ghafouri, Mohammad; Tabatabaei, MahmoudReza; Goodarzi, Masoud; Mokarian, Zeinab</p> <p>2017-10-01</p> <p>Estimation of the major components of the <span class="hlt">hydrologic</span> budget is important for determining the impacts on the water supply and quality of either planned or proposed land management projects, vegetative changes, groundwater withdrawals, and reservoir management practices and plans. As acquisition of field data is costly and time consuming, models have been created to test various land use practices and their concomitant effects on the <span class="hlt">hydrologic</span> budget of watersheds. To simulate such management scenarios realistically, a model should be able to simulate the individual components of the <span class="hlt">hydrologic</span> budget. The main objective of this study is to perform the SWAT2012 model for estimation of <span class="hlt">hydrological</span> budget in six subbasin of Persian Gulf watershed; Golgol, Baghan, Marghab Shekastian, Tangebirim and Daragah, which are located in south and south west of Iran during 1991-2009. In order to evaluate the performance of the model, <span class="hlt">hydrological</span> data, soil map, land use map and digital elevation model (DEM) are obtained and prepared for each catchment to run the model. SWAT-CUP with SUFI2 program was used for simulation, uncertainty and validation with 95 Percent <span class="hlt">Prediction</span> Uncertainty. Coefficient of determination ( R 2) and Nash-Sutcliffe coefficient (NS) were used for evaluation of the model simulation results. Comparison of measured and <span class="hlt">predicted</span> values demonstrated that each component of the model gave reasonable output and that the interaction among components was realistic. The study has produced a technique with reliable capability for annual and monthly water budget components in Persian Gulf watershed.</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('http://adsabs.harvard.edu/abs/2006E%26PSL.242..143L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2006E%26PSL.242..143L"><span>Oscillations in land surface <span class="hlt">hydrological</span> cycle</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Labat, D.</p> <p>2006-02-01</p> <p><span class="hlt">Hydrological</span> cycle is the perpetual movement of water throughout the various component of the global Earth's system. Focusing on the land surface component of this cycle, the determination of the succession of dry and humid periods is of high importance with respect to water resources management but also with respect to global geochemical cycles. This knowledge requires a specified estimation of recent fluctuations of the land surface cycle at continental and global scales. Our approach leans towards a new estimation of freshwater discharge to oceans from 1875 to 1994 as recently proposed by Labat et al. [Labat, D., Goddéris, Y., Probst, JL, Guyot, JL, 2004. Evidence for global runoff increase related to climate warming. <span class="hlt">Advances</span> in Water Resources, 631-642]. Wavelet analyses of the annual freshwater discharge time series reveal an intermittent multiannual variability (4- to 8-y, 14- to 16-y and 20- to 25-y fluctuations) and a persistent multidecadal 30- to 40-y variability. Continent by continent, reasonable relationships between land-water cycle oscillations and climate forcing (such as ENSO, NAO or sea surface temperature) are proposed even though if such relationships or correlations remain very complex. The high intermittency of interannual oscillations and the existence of persistent multidecadal fluctuations make <span class="hlt">prediction</span> difficult for medium-term variability of droughts and high-flows, but lead to a more optimistic diagnostic for long-term fluctuations <span class="hlt">prediction</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/19700135','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/19700135"><span>Echocardiography and risk <span class="hlt">prediction</span> in <span class="hlt">advanced</span> heart failure: incremental value over clinical markers.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Agha, Syed A; Kalogeropoulos, Andreas P; Shih, Jeffrey; Georgiopoulou, Vasiliki V; Giamouzis, Grigorios; Anarado, Perry; Mangalat, Deepa; Hussain, Imad; Book, Wendy; Laskar, Sonjoy; Smith, Andrew L; Martin, Randolph; Butler, Javed</p> <p>2009-09-01</p> <p>Incremental value of echocardiography over clinical parameters for outcome <span class="hlt">prediction</span> in <span class="hlt">advanced</span> heart failure (HF) is not well established. We evaluated 223 patients with <span class="hlt">advanced</span> HF receiving optimal therapy (91.9% angiotensin-converting enzyme inhibitor/angiotensin receptor blocker, 92.8% beta-blockers, 71.8% biventricular pacemaker, and/or defibrillator use). The Seattle Heart Failure Model (SHFM) was used as the reference clinical risk <span class="hlt">prediction</span> scheme. The incremental value of echocardiographic parameters for event <span class="hlt">prediction</span> (death or urgent heart transplantation) was measured by the improvement in fit and discrimination achieved by addition of standard echocardiographic parameters to the SHFM. After a median follow-up of 2.4 years, there were 38 (17.0%) events (35 deaths; 3 urgent transplants). The SHFM had likelihood ratio (LR) chi(2) 32.0 and C statistic 0.756 for event <span class="hlt">prediction</span>. Left ventricular end-systolic volume, stroke volume, and severe tricuspid regurgitation were independent echocardiographic predictors of events. The addition of these parameters to SHFM improved LR chi(2) to 72.0 and C statistic to 0.866 (P < .001 and P=.019, respectively). Reclassifying the SHFM-<span class="hlt">predicted</span> risk with use of the echocardiography-added model resulted in improved prognostic separation. Addition of standard echocardiographic variables to the SHFM results in significant improvement in risk <span class="hlt">prediction</span> for patients with <span class="hlt">advanced</span> HF.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.fs.usda.gov/treesearch/pubs/52800','TREESEARCH'); return false;" href="https://www.fs.usda.gov/treesearch/pubs/52800"><span>Forest <span class="hlt">hydrology</span></span></a></p> <p><a target="_blank" href="http://www.fs.usda.gov/treesearch/">Treesearch</a></p> <p>Ge Sun; Devendra Amatya; Steve McNulty</p> <p>2016-01-01</p> <p>Forest <span class="hlt">hydrology</span> studies the distribution, storage, movement, and quality of water and the <span class="hlt">hydrological</span> processes in forest-dominated ecosystems. Forest <span class="hlt">hydrological</span> science is regarded as the foundation of modern integrated water¬shed management. This chapter provides an overview of the history of forest <span class="hlt">hydrology</span> and basic principles of this unique branch of...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014JHyd..519.1394S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014JHyd..519.1394S"><span>A comparative appraisal of <span class="hlt">hydrological</span> behavior of SRTM DEM at catchment level</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Sharma, Arabinda; Tiwari, K. N.</p> <p>2014-11-01</p> <p>The Shuttle Radar Topography Mission (SRTM) data has emerged as a global elevation data in the past one decade because of its free availability, homogeneity and consistent accuracy compared to other global elevation dataset. The present study explores the consistency in <span class="hlt">hydrological</span> behavior of the SRTM digital elevation model (DEM) with reference to easily available regional 20 m contour interpolated DEM (TOPO DEM). Analysis ranging from simple vertical accuracy assessment to <span class="hlt">hydrological</span> simulation of the studied Maithon catchment, using empirical USLE model and semidistributed, physical SWAT model, were carried out. Moreover, terrain analysis involving <span class="hlt">hydrological</span> indices was performed for comparative assessment of the SRTM DEM with respect to TOPO DEM. Results reveal that the vertical accuracy of SRTM DEM (±27.58 m) in the region is less than the specified standard (±16 m). Statistical analysis of <span class="hlt">hydrological</span> indices such as topographic wetness index (TWI), stream power index (SPI), slope length factor (SLF) and geometry number (GN) shows a significant differences in <span class="hlt">hydrological</span> properties of the two studied DEMs. Estimation of soil erosion potentials of the catchment and conservation priorities of microwatersheds of the catchment using SRTM DEM and TOPO DEM produce considerably different results. <span class="hlt">Prediction</span> of soil erosion potential using SRTM DEM is far higher than that obtained using TOPO DEM. Similarly, conservation priorities determined using the two DEMs are found to be agreed for only 34% of microwatersheds of the catchment. ArcSWAT simulation reveals that runoff <span class="hlt">predictions</span> are less sensitive to selection of the two DEMs as compared to sediment yield <span class="hlt">prediction</span>. The results obtained in the present study are vital to <span class="hlt">hydrological</span> analysis as it helps understanding the <span class="hlt">hydrological</span> behavior of the DEM without being influenced by the model structural as well as parameter uncertainty. It also reemphasized that SRTM DEM can be a valuable dataset for</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2009EGUGA..1113463T','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2009EGUGA..1113463T"><span>Integrating <span class="hlt">hydrology</span> into catchment scale studies - need for new paradigms?</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Teutsch, G.</p> <p>2009-04-01</p> <p>Until the seventies, scientific development in the field of groundwater <span class="hlt">hydrology</span> concentrated mainly on a better understanding of the physics of subsurface flow in homogeneous or simply stratified porous respectively fractured media. Then, since mid of the seventies, a much more complex vision of groundwater <span class="hlt">hydrology</span> gradually developed. A more realistic description of the subsurface including its heterogeneity, predominant physico-chemical-biological reactions and also technologies for the efficient clean-up of contaminants developed during the past 30 years, much facilitated by the <span class="hlt">advancement</span> in numerical modelling techniques and the boost in computer power. Even though the <span class="hlt">advancements</span> in this field have been very significant, a new grand challenge evolved during the past 10 years trying to bring together the fields needed to build Integrated Watershed Management Systems (IWMS). The fundamental conceptual question is: Do we need new approaches to groundwater <span class="hlt">hydrology</span>, maybe even new paradigms in order to successfully build IWMS - or can we simply extrapolate our existing concepts and tool-sets to the scale of catchments and watersheds and simply add some interfaces to adjacent disciplines like economy, ecology and others? This lecture tries to provide some of the answers by describing some successful examples.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/pages/biblio/1255652-representing-northern-peatland-microtopography-hydrology-within-community-land-model','SCIGOV-DOEP'); return false;" href="https://www.osti.gov/pages/biblio/1255652-representing-northern-peatland-microtopography-hydrology-within-community-land-model"><span>Representing northern peatland microtopography and <span class="hlt">hydrology</span> within the Community Land Model</span></a></p> <p><a target="_blank" href="http://www.osti.gov/pages">DOE PAGES</a></p> <p>Shi, Xiaoying; Thornton, Peter E.; Ricciuto, Daniel M.; ...</p> <p>2015-11-12</p> <p><span class="hlt">Predictive</span> understanding of northern peatland <span class="hlt">hydrology</span> is a necessary precursor to understanding the fate of massive carbon stores in these systems under the influence of present and future climate change. Current models have begun to address microtopographic controls on peatland <span class="hlt">hydrology</span>, but none have included a prognostic calculation of peatland water table depth for a vegetated wetland, independent of prescribed regional water tables. We introduce here a new configuration of the Community Land Model (CLM) which includes a fully prognostic water table calculation for a vegetated peatland. Our structural and process changes to CLM focus on modifications needed to representmore » the <span class="hlt">hydrologic</span> cycle of bogs environment with perched water tables, as well as distinct <span class="hlt">hydrologic</span> dynamics and vegetation communities of the raised hummock and sunken hollow microtopography characteristic of peatland bogs. The modified model was parameterized and independently evaluated against observations from an ombrotrophic raised-dome bog in northern Minnesota (S1-Bog), the site for the Spruce and Peatland Responses Under Climatic and Environmental Change experiment (SPRUCE). Simulated water table levels compared well with site-level observations. The new model <span class="hlt">predicts</span> <span class="hlt">hydrologic</span> changes in response to planned warming at the SPRUCE site. At present, standing water is commonly observed in bog hollows after large rainfall events during the growing season, but simulations suggest a sharp decrease in water table levels due to increased evapotranspiration under the most extreme warming level, nearly eliminating the occurrence of standing water in the growing season. Simulated soil energy balance was strongly influenced by reduced winter snowpack under warming simulations, with the warming influence on soil temperature partly offset by the loss of insulating snowpack in early and late winter. Furthermore, the new model provides improved <span class="hlt">predictive</span> capacity for seasonal <span class="hlt">hydrological</span></p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/pages/biblio/1209488-representing-northern-peatland-microtopography-hydrology-within-community-land-model','SCIGOV-DOEP'); return false;" href="https://www.osti.gov/pages/biblio/1209488-representing-northern-peatland-microtopography-hydrology-within-community-land-model"><span>Representing northern peatland microtopography and <span class="hlt">hydrology</span> within the Community Land Model</span></a></p> <p><a target="_blank" href="http://www.osti.gov/pages">DOE PAGES</a></p> <p>Shi, X.; Thornton, P. E.; Ricciuto, D. M.; ...</p> <p>2015-02-20</p> <p><span class="hlt">Predictive</span> understanding of northern peatland <span class="hlt">hydrology</span> is a necessary precursor to understanding the fate of massive carbon stores in these systems under the influence of present and future climate change. Current models have begun to address microtopographic controls on peatland <span class="hlt">hydrology</span>, but none have included a prognostic calculation of peatland water table depth for a vegetated wetland, independent of prescribed regional water tables. We introduce here a new configuration of the Community Land Model (CLM) which includes a fully prognostic water table calculation for a vegetated peatland. Our structural and process changes to CLM focus on modifications needed to representmore » the <span class="hlt">hydrologic</span> cycle of bogs environment with perched water tables, as well as distinct <span class="hlt">hydrologic</span> dynamics and vegetation communities of the raised hummock and sunken hollow microtopography characteristic of peatland bogs. The modified model was parameterized and independently evaluated against observations from an ombrotrophic raised-dome bog in northern Minnesota (S1-Bog), the site for the Spruce and Peatland Responses Under Climatic and Environmental Change experiment (SPRUCE). Simulated water table levels compared well with site-level observations. The new model <span class="hlt">predicts</span> significant <span class="hlt">hydrologic</span> changes in response to planned warming at the SPRUCE site. At present, standing water is commonly observed in bog hollows after large rainfall events during the growing season, but simulations suggest a sharp decrease in water table levels due to increased evapotranspiration under the most extreme warming level, nearly eliminating the occurrence of standing water in the growing season. Simulated soil energy balance was strongly influenced by reduced winter snowpack under warming simulations, with the warming influence on soil temperature partly offset by the loss of insulating snowpack in early and late winter. The new model provides improved <span class="hlt">predictive</span> capacity for seasonal <span class="hlt">hydrological</span></p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2009SPIE.7238E..0HS','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2009SPIE.7238E..0HS"><span>Virtual <span class="hlt">hydrology</span> observatory: an immersive visualization of <span class="hlt">hydrology</span> modeling</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Su, Simon; Cruz-Neira, Carolina; Habib, Emad; Gerndt, Andreas</p> <p>2009-02-01</p> <p>The Virtual <span class="hlt">Hydrology</span> Observatory will provide students with the ability to observe the integrated <span class="hlt">hydrology</span> simulation with an instructional interface by using a desktop based or immersive virtual reality setup. It is the goal of the virtual <span class="hlt">hydrology</span> observatory application to facilitate the introduction of field experience and observational skills into <span class="hlt">hydrology</span> courses through innovative virtual techniques that mimic activities during actual field visits. The simulation part of the application is developed from the integrated atmospheric forecast model: Weather Research and Forecasting (WRF), and the <span class="hlt">hydrology</span> model: Gridded Surface/Subsurface <span class="hlt">Hydrologic</span> Analysis (GSSHA). Both the output from WRF and GSSHA models are then used to generate the final visualization components of the Virtual <span class="hlt">Hydrology</span> Observatory. The various visualization data processing techniques provided by VTK are 2D Delaunay triangulation and data optimization. Once all the visualization components are generated, they are integrated into the simulation data using VRFlowVis and VR Juggler software toolkit. VR Juggler is used primarily to provide the Virtual <span class="hlt">Hydrology</span> Observatory application with fully immersive and real time 3D interaction experience; while VRFlowVis provides the integration framework for the <span class="hlt">hydrologic</span> simulation data, graphical objects and user interaction. A six-sided CAVETM like system is used to run the Virtual <span class="hlt">Hydrology</span> Observatory to provide the students with a fully immersive experience.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013EGUGA..15.6176H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013EGUGA..15.6176H"><span>Uncertainty of a <span class="hlt">hydrological</span> climate change impact assessment - Is it really all about climate uncertainty?</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Honti, Mark; Reichert, Peter; Scheidegger, Andreas; Stamm, Christian</p> <p>2013-04-01</p> <p>Climate change impact assessments have become more and more popular in <span class="hlt">hydrology</span> since the middle 1980's with another boost after the publication of the IPCC AR4 report. During hundreds of impact studies a quasi-standard methodology emerged, which is mainly shaped by the growing public demand for <span class="hlt">predicting</span> how water resources management or flood protection should change in the close future. The ``standard'' workflow considers future climate under a specific IPCC emission scenario simulated by global circulation models (GCMs), possibly downscaled by a regional climate model (RCM) and/or a stochastic weather generator. The output from the climate models is typically corrected for bias before feeding it into a calibrated <span class="hlt">hydrological</span> model, which is run on the past and future meteorological data to analyse the impacts of climate change on the <span class="hlt">hydrological</span> indicators of interest. The impact <span class="hlt">predictions</span> are as uncertain as any forecast that tries to describe the behaviour of an extremely complex system decades into the future. Future climate <span class="hlt">predictions</span> are uncertain due to the scenario uncertainty and the GCM model uncertainty that is obvious on finer resolution than continental scale. Like in any hierarchical model system, uncertainty propagates through the descendant components. Downscaling increases uncertainty with the deficiencies of RCMs and/or weather generators. Bias correction adds a strong deterministic shift to the input data. Finally the <span class="hlt">predictive</span> uncertainty of the <span class="hlt">hydrological</span> model ends the cascade that leads to the total uncertainty of the <span class="hlt">hydrological</span> impact assessment. There is an emerging consensus between many studies on the relative importance of the different uncertainty sources. The prevailing perception is that GCM uncertainty dominates <span class="hlt">hydrological</span> impact studies. There are only few studies, which found that the <span class="hlt">predictive</span> uncertainty of <span class="hlt">hydrological</span> models can be in the same range or even larger than climatic uncertainty. We carried out a</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017EGUGA..1915477O','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017EGUGA..1915477O"><span><span class="hlt">Advancing</span> land surface model development with satellite-based Earth observations</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Orth, Rene; Dutra, Emanuel; Trigo, Isabel F.; Balsamo, Gianpaolo</p> <p>2017-04-01</p> <p>The land surface forms an essential part of the climate system. It interacts with the atmosphere through the exchange of water and energy and hence influences weather and climate, as well as their <span class="hlt">predictability</span>. Correspondingly, the land surface model (LSM) is an essential part of any weather forecasting system. LSMs rely on partly poorly constrained parameters, due to sparse land surface observations. With the use of newly available land surface temperature observations, we show in this study that novel satellite-derived datasets help to improve LSM configuration, and hence can contribute to improved weather <span class="hlt">predictability</span>. We use the <span class="hlt">Hydrology</span> Tiled ECMWF Scheme of Surface Exchanges over Land (HTESSEL) and validate it comprehensively against an array of Earth observation reference datasets, including the new land surface temperature product. This reveals satisfactory model performance in terms of <span class="hlt">hydrology</span>, but poor performance in terms of land surface temperature. This is due to inconsistencies of process representations in the model as identified from an analysis of perturbed parameter simulations. We show that HTESSEL can be more robustly calibrated with multiple instead of single reference datasets as this mitigates the impact of the structural inconsistencies. Finally, performing coupled global weather forecasts we find that a more robust calibration of HTESSEL also contributes to improved weather forecast skills. In summary, new satellite-based Earth observations are shown to enhance the multi-dataset calibration of LSMs, thereby improving the representation of insufficiently captured processes, <span class="hlt">advancing</span> weather <span class="hlt">predictability</span> and understanding of climate system feedbacks. Orth, R., E. Dutra, I. F. Trigo, and G. Balsamo (2016): <span class="hlt">Advancing</span> land surface model development with satellite-based Earth observations. Hydrol. Earth Syst. Sci. Discuss., doi:10.5194/hess-2016-628</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/27879946','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/27879946"><span>Integrating Remote Sensing Information Into A Distributed <span class="hlt">Hydrological</span> Model for Improving Water Budget <span class="hlt">Predictions</span> in Large-scale Basins through Data Assimilation.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Qin, Changbo; Jia, Yangwen; Su, Z; Zhou, Zuhao; Qiu, Yaqin; Suhui, Shen</p> <p>2008-07-29</p> <p>This paper investigates whether remote sensing evapotranspiration estimates can be integrated by means of data assimilation into a distributed <span class="hlt">hydrological</span> model for improving the <span class="hlt">predictions</span> of spatial water distribution over a large river basin with an area of 317,800 km2. A series of available MODIS satellite images over the Haihe River basin in China are used for the year 2005. Evapotranspiration is retrieved from these 1×1 km resolution images using the SEBS (Surface Energy Balance System) algorithm. The physically-based distributed model WEP-L (Water and Energy transfer Process in Large river basins) is used to compute the water balance of the Haihe River basin in the same year. Comparison between model-derived and remote sensing retrieval basin-averaged evapotranspiration estimates shows a good piecewise linear relationship, but their spatial distribution within the Haihe basin is different. The remote sensing derived evapotranspiration shows variability at finer scales. An extended Kalman filter (EKF) data assimilation algorithm, suitable for non-linear problems, is used. Assimilation results indicate that remote sensing observations have a potentially important role in providing spatial information to the assimilation system for the spatially optical <span class="hlt">hydrological</span> parameterization of the model. This is especially important for large basins, such as the Haihe River basin in this study. Combining and integrating the capabilities of and information from model simulation and remote sensing techniques may provide the best spatial and temporal characteristics for <span class="hlt">hydrological</span> states/fluxes, and would be both appealing and necessary for improving our knowledge of fundamental <span class="hlt">hydrological</span> processes and for addressing important water resource management problems.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20140009993','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20140009993"><span>Assessment of Evolving TRMM-Based Real-Time Precipitation Estimation Methods and Their Impacts on <span class="hlt">Hydrologic</span> <span class="hlt">Prediction</span> in a High-Latitude Basin</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Yong, Bin; Hong, Yang; Ren, Li-Liang; Gourley, Jonathan; Huffman, George J.; Chen, Xi; Wang, Wen; Khan, Sadiq I.</p> <p>2013-01-01</p> <p>The real-time availability of satellite-derived precipitation estimates provides hydrologists an opportunity to improve current <span class="hlt">hydrologic</span> <span class="hlt">prediction</span> capability for medium to large river basins. Due to the availability of new satellite data and upgrades to the precipitation algorithms, the Tropical Rainfall Measuring Mission (TRMM) Multi-satellite Precipitation Analysis real-time estimates (TMPA-RT) have been undergoing several important revisions over the past ten years. In this study, the changes of the relative accuracy and <span class="hlt">hydrologic</span> potential of TMPA-RT estimates over its three major evolving periods were evaluated and inter-compared at daily, monthly and seasonal scales in the high-latitude Laohahe basin in China. Assessment results show that the performance of TMPA-RT in terms of precipitation estimation and streamflow simulation was significantly improved after 3 February 2005. Overestimation during winter months was noteworthy and consistent, which is suggested to be a consequence from interference of snow cover to the passive microwave retrievals. Rainfall estimated by the new version 6 of TMPA-RT starting from 1 October 2008 to present has higher correlations with independent gauge observations and tends to perform better in detecting rain compared to the prior periods, although it suffers larger mean error and relative bias. After a simple bias correction, this latest dataset of TMPA-RT exhibited the best capability in capturing <span class="hlt">hydrologic</span> response among the three tested periods. In summary, this study demonstrated that there is an increasing potential in the use of TMPA-RT in <span class="hlt">hydrologic</span> streamflow simulations over its three algorithm upgrade periods, but still with significant challenges during the winter snowing events.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3697185','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3697185"><span>Integrating Remote Sensing Information Into A Distributed <span class="hlt">Hydrological</span> Model for Improving Water Budget <span class="hlt">Predictions</span> in Large-scale Basins through Data Assimilation</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Qin, Changbo; Jia, Yangwen; Su, Z.(Bob); Zhou, Zuhao; Qiu, Yaqin; Suhui, Shen</p> <p>2008-01-01</p> <p>This paper investigates whether remote sensing evapotranspiration estimates can be integrated by means of data assimilation into a distributed <span class="hlt">hydrological</span> model for improving the <span class="hlt">predictions</span> of spatial water distribution over a large river basin with an area of 317,800 km2. A series of available MODIS satellite images over the Haihe River basin in China are used for the year 2005. Evapotranspiration is retrieved from these 1×1 km resolution images using the SEBS (Surface Energy Balance System) algorithm. The physically-based distributed model WEP-L (Water and Energy transfer Process in Large river basins) is used to compute the water balance of the Haihe River basin in the same year. Comparison between model-derived and remote sensing retrieval basin-averaged evapotranspiration estimates shows a good piecewise linear relationship, but their spatial distribution within the Haihe basin is different. The remote sensing derived evapotranspiration shows variability at finer scales. An extended Kalman filter (EKF) data assimilation algorithm, suitable for non-linear problems, is used. Assimilation results indicate that remote sensing observations have a potentially important role in providing spatial information to the assimilation system for the spatially optical <span class="hlt">hydrological</span> parameterization of the model. This is especially important for large basins, such as the Haihe River basin in this study. Combining and integrating the capabilities of and information from model simulation and remote sensing techniques may provide the best spatial and temporal characteristics for <span class="hlt">hydrological</span> states/fluxes, and would be both appealing and necessary for improving our knowledge of fundamental <span class="hlt">hydrological</span> processes and for addressing important water resource management problems. PMID:27879946</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2009AGUFM.H24D..03K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2009AGUFM.H24D..03K"><span>“Black Swans” of <span class="hlt">Hydrology</span>: Can our Models Address the Science of <span class="hlt">Hydrologic</span> Change?</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Kumar, P.</p> <p>2009-12-01</p> <p>Coupled models of terrestrial <span class="hlt">hydrology</span> and climate have grown in complexity leading to better understanding of the coupling between the hydrosphere, biosphere, and the climate system. During the past two decades, these models have evolved through generational changes as they have grown in sophistication in their ability to resolve spatial heterogeneity as well as vegetation dynamics and biogeochemistry. These developments have, in part, been driven by data collection efforts ranging from focused field campaigns to long-term observational networks, <span class="hlt">advances</span> in remote sensing and other measurement technologies, along with sophisticated estimation and assimilation methods. However, the <span class="hlt">hydrologic</span> cycle is changing leading to unexpected and unanticipated behavior through emergent dynamics and patterns that are not part of the historical milieu. Is there a new thinking that is needed to address this challenge? The goal of this talk is to draw from the modeling developments in the past two decades to foster a debate for moving forward.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5912497','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5912497"><span><span class="hlt">Advanced</span> Daily <span class="hlt">Prediction</span> Model for National Suicide Numbers with Social Media Data</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Lee, Kyung Sang; Lee, Hyewon; Myung, Woojae; Song, Gil-Young; Lee, Kihwang; Kim, Ho; Carroll, Bernard J.; Kim, Doh Kwan</p> <p>2018-01-01</p> <p>Objective Suicide is a significant public health concern worldwide. Social media data have a potential role in identifying high suicide risk individuals and also in <span class="hlt">predicting</span> suicide rate at the population level. In this study, we report an <span class="hlt">advanced</span> daily suicide <span class="hlt">prediction</span> model using social media data combined with economic/meteorological variables along with observed suicide data lagged by 1 week. Methods The social media data were drawn from weblog posts. We examined a total of 10,035 social media keywords for suicide <span class="hlt">prediction</span>. We made <span class="hlt">predictions</span> of national suicide numbers 7 days in <span class="hlt">advance</span> daily for 2 years, based on a daily moving 5-year <span class="hlt">prediction</span> modeling period. Results Our model <span class="hlt">predicted</span> the likely range of daily national suicide numbers with 82.9% accuracy. Among the social media variables, words denoting economic issues and mood status showed high <span class="hlt">predictive</span> strength. Observed number of suicides one week previously, recent celebrity suicide, and day of week followed by stock index, consumer price index, and sunlight duration 7 days before the target date were notable predictors along with the social media variables. Conclusion These results strengthen the case for social media data to supplement classical social/economic/climatic data in forecasting national suicide events. PMID:29614852</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/26312403','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/26312403"><span>Circulating CD147 <span class="hlt">predicts</span> mortality in <span class="hlt">advanced</span> hepatocellular carcinoma.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Lee, Aimei; Rode, Anthony; Nicoll, Amanda; Maczurek, Annette E; Lim, Lucy; Lim, Seok; Angus, Peter; Kronborg, Ian; Arachchi, Niranjan; Gorelik, Alexandra; Liew, Danny; Warner, Fiona J; McCaughan, Geoffrey W; McLennan, Susan V; Shackel, Nicholas A</p> <p>2016-02-01</p> <p>The glycoprotein CD147 has a role in tumor progression, is readily detectable in the circulation, and is abundantly expressed in hepatocellular carcinoma (HCC). <span class="hlt">Advanced</span> HCC patients are a heterogeneous group with some individuals having dismal survival. The aim of this study was to examine circulating soluble CD147 levels as a prognostic marker in HCC patients. CD147 was measured in 277 patients (110 HCC, 115 chronic liver disease, and 52 non-liver disease). Clinical data included etiology, tumor progression, Barcelona Clinic Liver Cancer (BCLC) stage, and treatment response. Patients with HCC were stratified into two groups based upon the 75th percentile of CD147 levels (24 ng/mL). CD147 in HCC correlated inversely with poor survival (P = 0.031). Increased CD147 <span class="hlt">predicted</span> poor survival in BCLC stages C and D (P = 0.045), and CD147 levels >24 ng/mL <span class="hlt">predicted</span> a significantly diminished 90-day and 180-day survival time (hazard ratio [HR] = 6.1; 95% confidence interval [CI]: 2.1-63.2; P = 0.0045 and HR = 2.8; 95% CI: 1.2-12.6; P = 0.028, respectively). In BCLC stage C, CD147 <span class="hlt">predicted</span> prognosis; levels >24 ng/mL were associated with a median survival of 1.5 months compared with 6.5 months with CD147 levels ≤24 ng/mL (P = 0.03). CD147 also identified patients with a poor prognosis independent from treatment frequency, modality, and tumor size. Circulating CD147 is an independent marker of survival in <span class="hlt">advanced</span> HCC. CD147 requires further evaluation as a potential new prognostic measure in HCC to identify patients with <span class="hlt">advanced</span> disease who have a poor prognosis. © 2015 Journal of Gastroenterology and Hepatology Foundation and John Wiley & Sons Australia, Ltd.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2004AGUFM.H31C0384G','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2004AGUFM.H31C0384G"><span>The Suwannee River <span class="hlt">Hydrologic</span> Observatory: A Subtropical Coastal Plain Watershed in Transition</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Graham, W. D.</p> <p>2004-12-01</p> <p>The Consortium of Universities for the <span class="hlt">Advancement</span> of <span class="hlt">Hydrologic</span> Sciences (CUAHSI) proposed to establish a network of 5-15 <span class="hlt">hydrologic</span> observatories (HO's) across North America is to support fundamental research for the <span class="hlt">hydrologic</span> science community into the next century. These HO's are projected to be 10,000 to 50,000 km2 and will include a broad range of <span class="hlt">hydrologic</span>, climatic, bio-geochemical and ecosystem processes, including the critical linkages and couplings. This network is envisioned as the natural laboratory for experimental <span class="hlt">hydrology</span> in support of scientific investigations focused on <span class="hlt">predictive</span> understanding at a scale that will include both atmospheric- and ecosystem-<span class="hlt">hydrologic</span> interaction, as well as the <span class="hlt">hydrologic</span> response to larger-scale climate variation and change. A group of researchers from Florida and Georgia plan to propose the Suwannee River watershed as a <span class="hlt">Hydrologic</span> Observatory. The Suwannee River flows through a diverse watershed relatively unimpacted by urbanization but in transition to more intense land-use practices. It thus provides excellent opportunities to study the effects of ongoing changes in land use and water supply on varied <span class="hlt">hydrological</span> processes. Much background information is available on the <span class="hlt">hydrology</span>, hydrogeology, geology, chemistry, and biology of the watershed. Several major on-going monitoring programs are supported by state and federal agencies. Four characteristics, discussed in greater detail below, make the Suwannee River watershed ideal for a <span class="hlt">Hydrologic</span> Observatory: Unregulated and rural - The Suwannee River is one of few major rivers in the United States with largely unregulated flow through rural areas and is relatively unimpaired with regard to water quality, leading to its designation as one of twelve National Showcase Watersheds. At Risk and in Transition - Land use is trending toward increased urbanization and intensive agriculture with an apparent coupled increase in nutrient loads and decline in water quality</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2010ESASP.684E..36F','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2010ESASP.684E..36F"><span>Project 5322 Mid-Term Report: Key Eco-<span class="hlt">Hydrological</span> Parameters Retrieval And Land Data Assimilation System Development In A Typical Inland River Basin Of Chinas Arid Region</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Faivre, R.; Colin, J.; Menenti, M.; Lindenbergh, R.; Van Den Bergh, L.; Yu, H.; Jia, L.; Xin, L.</p> <p>2010-10-01</p> <p>Improving the understanding and the monitoring of high elevation regions <span class="hlt">hydrology</span> is of major relevance from both societal and environmental points of view for many Asian countries, in particular in terms of flood and drought, but also in terms of food security in a chang- ing environment. Satellite and airborne remote sensing technologies are of utmost for such a challenge. Exist- ing imaging spectro-radiometers, radars, microwave ra- diometers and backscatter LIDAR provide a very com- prehensive suite of measurements over a wide rage of wavelengths, time frequencies and spatial resolu- tions. It is however needed to devise new algorithms to convert these radiometric measurements into useful eco-<span class="hlt">hydrological</span> quantitative parameters for <span class="hlt">hydrologi</span>- cal modeling and water management. The DRAGON II project entitled Key Eco-<span class="hlt">Hydrological</span> Parameters Re- trieval and Land Data Assimilation System Development in a Typical Inland River Basin of Chinas Arid Region (ID 5322) aims at improving the monitoring, understand- ing, and <span class="hlt">predictability</span> of <span class="hlt">hydrological</span> and ecological pro- cesses at catchment scale, and promote the applicability of quantitative remote sensing in watershed science. Ex- isting Earth Observation platforms provided by the Euro- pean Space Agency as well as prototype airborne systems developed in China - ENVISAT/AATSR, ALOS/PRISM and PALSAR, Airborne LIDAR - are used and combined to retrieve <span class="hlt">advanced</span> land surface physical properties over high elevation arid regions of China. The existing syn- ergies between this project, the CEOP-AEGIS project (FP7) and the WATER project (CAS) provide incentives for innovative studies. The investigations presented in the following report focus on the development of <span class="hlt">advanced</span> and innovative methodologies and algorithms to monitor both the state and the trend of key eco-<span class="hlt">hydrological</span> vari- ables: 3D vegetation properties, land surface evaporation, glacier mass balance and drought indicators.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.ars.usda.gov/research/publications/publication/?seqNo115=312632','TEKTRAN'); return false;" href="http://www.ars.usda.gov/research/publications/publication/?seqNo115=312632"><span>An eco-<span class="hlt">hydrological</span> approach to <span class="hlt">predicting</span> regional vegetation and groundwater response to ecological water convergence in dryland riparian ecosystems</span></a></p> <p><a target="_blank" href="https://www.ars.usda.gov/research/publications/find-a-publication/">USDA-ARS?s Scientific Manuscript database</a></p> <p></p> <p></p> <p>To improve the management strategy of riparian restoration, better understanding of the dynamic of eco-<span class="hlt">hydrological</span> system and its feedback between <span class="hlt">hydrological</span> and ecological components are needed. The fully distributed eco-<span class="hlt">hydrological</span> model coupled with a <span class="hlt">hydrology</span> component was developed based o...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017JGRG..122...65T','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017JGRG..122...65T"><span>GIS-based <span class="hlt">prediction</span> of stream chemistry using landscape composition, wet areas, and <span class="hlt">hydrological</span> flow pathways</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Tiwari, Tejshree; Lidman, Fredrik; Laudon, Hjalmar; Lidberg, William; Ågren, Anneli M.</p> <p>2017-01-01</p> <p>Landscape morphology exerts strong, scale-dependent controls on stream <span class="hlt">hydrology</span> and biogeochemistry in heterogeneous catchments. We applied three descriptors of landscape structure at different spatial scales based on new geographic information system tools to <span class="hlt">predict</span> variability in stream concentrations for a wide range of solutes (Al, Ba, Be, Ca, Fe, K, Mg, Na, S, Si, Sr, Sc, Co, Cr, Ni, Cu, As, Se, Rb, Y, Cd, Sb, Cs, La, Pb, Th, U, DOC, and Cl) using a linear regression analysis. Results showed that less reactive elements, which can be expected to behave more conservatively in the landscape (e.g., Na, K, Ca, Mg, Cl, and Si), generally were best <span class="hlt">predicted</span> from the broader-scale description of landscape composition (areal coverage of peat, tills, and sorted sediments). These results highlight the importance of mineral weathering as a source of some elements, which was best captured by landscape-scale descriptors of catchment structure. By contrast, more nonconservative elements (e.g., DOC, Al, Cd, Cs, Co, Th, Y, and U), were best <span class="hlt">predicted</span> by defining wet areas and/or flow path lengths of different patches in the landscape. This change in the <span class="hlt">predictive</span> models reflect the importance of peat deposits, such as organic-rich riparian zones and mire ecosystems, which are favorable environments for biogeochemical reactions of more nonconservative elements. As such, using this understanding of landscape influences on stream chemistry can provide improved mitigation strategies and management plans that specifically target source areas, so as to minimize mobilization of undesired elements into streams.</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_13");'>13</a></li> <li><a href="#" onclick='return showDiv("page_14");'>14</a></li> <li class="active"><span>15</span></li> <li><a href="#" onclick='return showDiv("page_16");'>16</a></li> <li><a href="#" onclick='return showDiv("page_17");'>17</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_15 --> <div id="page_16" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_14");'>14</a></li> <li><a href="#" onclick='return showDiv("page_15");'>15</a></li> <li class="active"><span>16</span></li> <li><a href="#" onclick='return showDiv("page_17");'>17</a></li> <li><a href="#" onclick='return showDiv("page_18");'>18</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="301"> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/28558050','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/28558050"><span>Citizen science: A new perspective to <span class="hlt">advance</span> spatial pattern evaluation in <span class="hlt">hydrology</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Koch, Julian; Stisen, Simon</p> <p>2017-01-01</p> <p>Citizen science opens new pathways that can complement traditional scientific practice. Intuition and reasoning often make humans more effective than computer algorithms in various realms of problem solving. In particular, a simple visual comparison of spatial patterns is a task where humans are often considered to be more reliable than computer algorithms. However, in practice, science still largely depends on computer based solutions, which inevitably gives benefits such as speed and the possibility to automatize processes. However, the human vision can be harnessed to evaluate the reliability of algorithms which are tailored to quantify similarity in spatial patterns. We established a citizen science project to employ the human perception to rate similarity and dissimilarity between simulated spatial patterns of several scenarios of a <span class="hlt">hydrological</span> catchment model. In total, the turnout counts more than 2500 volunteers that provided over 43000 classifications of 1095 individual subjects. We investigate the capability of a set of <span class="hlt">advanced</span> statistical performance metrics to mimic the human perception to distinguish between similarity and dissimilarity. Results suggest that more complex metrics are not necessarily better at emulating the human perception, but clearly provide auxiliary information that is valuable for model diagnostics. The metrics clearly differ in their ability to unambiguously distinguish between similar and dissimilar patterns which is regarded a key feature of a reliable metric. The obtained dataset can provide an insightful benchmark to the community to test novel spatial metrics.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5449172','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5449172"><span>Citizen science: A new perspective to <span class="hlt">advance</span> spatial pattern evaluation in <span class="hlt">hydrology</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>Stisen, Simon</p> <p>2017-01-01</p> <p>Citizen science opens new pathways that can complement traditional scientific practice. Intuition and reasoning often make humans more effective than computer algorithms in various realms of problem solving. In particular, a simple visual comparison of spatial patterns is a task where humans are often considered to be more reliable than computer algorithms. However, in practice, science still largely depends on computer based solutions, which inevitably gives benefits such as speed and the possibility to automatize processes. However, the human vision can be harnessed to evaluate the reliability of algorithms which are tailored to quantify similarity in spatial patterns. We established a citizen science project to employ the human perception to rate similarity and dissimilarity between simulated spatial patterns of several scenarios of a <span class="hlt">hydrological</span> catchment model. In total, the turnout counts more than 2500 volunteers that provided over 43000 classifications of 1095 individual subjects. We investigate the capability of a set of <span class="hlt">advanced</span> statistical performance metrics to mimic the human perception to distinguish between similarity and dissimilarity. Results suggest that more complex metrics are not necessarily better at emulating the human perception, but clearly provide auxiliary information that is valuable for model diagnostics. The metrics clearly differ in their ability to unambiguously distinguish between similar and dissimilar patterns which is regarded a key feature of a reliable metric. The obtained dataset can provide an insightful benchmark to the community to test novel spatial metrics. PMID:28558050</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013EGUGA..1514247S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013EGUGA..1514247S"><span>Towards a Seamless Framework for Drought Analysis and <span class="hlt">Prediction</span> from Seasonal to Climate Change Time Scales (Plinius Medal Lecture)</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Sheffield, Justin</p> <p>2013-04-01</p> <p>Droughts arguably cause the most impacts of all natural hazards in terms of the number of people affected and the long-term economic costs and ecosystem stresses. Recent droughts worldwide have caused humanitarian and economic problems such as food insecurity across the Horn of Africa, agricultural economic losses across the central US and loss of livelihoods in rural western India. The prospect of future increases in drought severity and duration driven by projected changes in precipitation patterns and increasing temperatures is worrisome. Some evidence for climate change impacts on drought is already being seen for some regions, such as the Mediterranean and east Africa. Mitigation of the impacts of drought requires <span class="hlt">advance</span> warning of developing conditions and enactment of drought plans to reduce vulnerability. A key element of this is a drought early warning system that at its heart is the capability to monitor evolving <span class="hlt">hydrological</span> conditions and water resources storage, and provide reliable and robust <span class="hlt">predictions</span> out to several months, as well as the capacity to act on this information. At longer time scales, planning and policy-making need to consider the potential impacts of climate change and its impact on drought risk, and do this within the context of natural climate variability, which is likely to dominate any climate change signal over the next few decades. There are several challenges that need to be met to <span class="hlt">advance</span> our capability to provide both early warning at seasonal time scales and risk assessment under climate change, regionally and globally. <span class="hlt">Advancing</span> our understanding of drought <span class="hlt">predictability</span> and risk requires knowledge of drought at all time scales. This includes understanding of past drought occurrence, from the paleoclimate record to the recent past, and understanding of drought mechanisms, from initiation, through persistence to recovery and translation of this understanding to <span class="hlt">predictive</span> models. Current approaches to monitoring and</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFM.H33G1625O','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFM.H33G1625O"><span>Mapping <span class="hlt">hydrological</span> signatures in the tropical Andes using a network of paired catchments</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Ochoa-Tocachi, B. F.; Buytaert, W.; De Bièvre, B.</p> <p>2016-12-01</p> <p>The complexity and data scarcity of tropical Andean catchments make regional <span class="hlt">hydrological</span> <span class="hlt">predictions</span> very challenging. The strong spatiotemporal patterns of the local climate contrast with the inadequate coverage, especially of remote areas, by the national monitoring networks. We present an approach to regionalize the <span class="hlt">hydrological</span> impacts of land-use and land-cover (LUC) using a network of 24 headwater catchments in a pairwise comparison approach. We monitored precipitation and streamflow through an informal partnership of stakeholders in the Andes, known as iMHEA. Using a `trading-space-for-time' approach, our design aims at strengthening the statistical significance of LUC signals. To test our hypothesis, we summarized the <span class="hlt">hydrological</span> responses using a set of indices, which are then regionalized against catchment properties including land-use. Lastly, the regionalization model is then used to generate distributed maps of <span class="hlt">hydrological</span> signatures in ungauged areas. Our results clearly reflect the dominant regional climate patterns of the tropical Andes and the associated wide spectrum of <span class="hlt">hydrological</span> responses. Although the <span class="hlt">hydrological</span> impacts of LUC are equally diverse, we find consistent trends within different biomes. Contrary to earlier studies, we find that incorporating LUC variables in the regionalization increases significantly the performance of the regression model and its <span class="hlt">predictive</span> capacity, which makes it possible to generate regional maps that <span class="hlt">predict</span> the dynamics and propagation of streamflow signatures in complex regions with an explicit report of uncertainty. We attribute the robust regionalization results to the regional pairwise setup that covers diverse physiographic characteristics, contrasting LUC types, and degrees of conservation/alteration. As such, it may be a useful strategy to optimize data collection, leverage commonly available geographical information, and understand the major controls of <span class="hlt">hydrological</span> response in data</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.ars.usda.gov/research/publications/publication/?seqNo115=235393','TEKTRAN'); return false;" href="http://www.ars.usda.gov/research/publications/publication/?seqNo115=235393"><span>WEB-DHM: A distributed biosphere <span class="hlt">hydrological</span> model developed by coupling a simple biosphere scheme with a hillslope <span class="hlt">hydrological</span> model</span></a></p> <p><a target="_blank" href="https://www.ars.usda.gov/research/publications/find-a-publication/">USDA-ARS?s Scientific Manuscript database</a></p> <p></p> <p></p> <p>The coupling of land surface models and <span class="hlt">hydrological</span> models potentially improves the land surface representation, benefiting both the streamflow <span class="hlt">prediction</span> capabilities as well as providing improved estimates of water and energy fluxes into the atmosphere. In this study, the simple biosphere model 2...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015EGUGA..1715248V','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015EGUGA..1715248V"><span>Global operational <span class="hlt">hydrological</span> forecasts through eWaterCycle</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>van de Giesen, Nick; Bierkens, Marc; Donchyts, Gennadii; Drost, Niels; Hut, Rolf; Sutanudjaja, Edwin</p> <p>2015-04-01</p> <p>Central goal of the eWaterCycle project (www.ewatercycle.org) is the development of an operational hyper-resolution <span class="hlt">hydrological</span> global model. This model is able to produce 14 day ensemble forecasts based on a <span class="hlt">hydrological</span> model and operational weather data (presently NOAA's Global Ensemble Forecast System). Special attention is paid to <span class="hlt">prediction</span> of situations in which water related issues are relevant, such as floods, droughts, navigation, hydropower generation, and irrigation stress. Near-real time satellite data will be assimilated in the <span class="hlt">hydrological</span> simulations, which is a feature that will be presented for the first time at EGU 2015. First, we address challenges that are mainly computer science oriented but have direct practical <span class="hlt">hydrological</span> implications. An important feature in this is the use of existing standards and open-source software to the maximum extent possible. For example, we use the Community Surface Dynamics Modeling System (CSDMS) approach to coupling models (Basic Model Interface (BMI)). The <span class="hlt">hydrological</span> model underlying the project is PCR-GLOBWB, built by Utrecht University. This is the motor behind the <span class="hlt">predictions</span> and state estimations. Parts of PCR-GLOBWB have been re-engineered to facilitate running it in a High Performance Computing (HPC) environment, run parallel on multiple nodes, as well as to use BMI. <span class="hlt">Hydrological</span> models are not very CPU intensive compared to, say, atmospheric models. They are, however, memory hungry due to the localized processes and associated effective parameters. To accommodate this memory need, especially in an ensemble setting, a variation on the traditional Ensemble Kalman Filter was developed that needs much less on-chip memory. Due to the operational nature, the coupling of the <span class="hlt">hydrological</span> model with hydraulic models is very important. The idea is not to run detailed hydraulic routing schemes over the complete globe but to have on-demand simulation prepared off-line with respect to topography and</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=20000038126&hterms=watershed&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D20%26Ntt%3Dwatershed','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=20000038126&hterms=watershed&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D20%26Ntt%3Dwatershed"><span>The Impact of Microwave-Derived Surface Soil Moisture on Watershed <span class="hlt">Hydrological</span> Modeling</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>ONeill, P. E.; Hsu, A. Y.; Jackson, T. J.; Wood, E. F.; Zion, M.</p> <p>1997-01-01</p> <p>The usefulness of incorporating microwave-derived soil moisture information in a semi-distributed <span class="hlt">hydrological</span> model was demonstrated for the Washita '92 experiment in the Little Washita River watershed in Oklahoma. Initializing the <span class="hlt">hydrological</span> model with surface soil moisture fields from the ESTAR airborne L-band microwave radiometer on a single wet day at the start of the study period produced more accurate model <span class="hlt">predictions</span> of soil moisture than a standard <span class="hlt">hydrological</span> initialization with streamflow data over an eight-day soil moisture drydown.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://cfpub.epa.gov/si/si_public_record_report.cfm?direntryid=22471','PESTICIDES'); return false;" href="https://cfpub.epa.gov/si/si_public_record_report.cfm?direntryid=22471"><span>EFFICIENT <span class="hlt">HYDROLOGICAL</span> TRACER-TEST DESIGN (EHTD ...</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><span class="hlt">Hydrological</span> tracer testing is the most reliable diagnostic technique available for establishing flow trajectories and <span class="hlt">hydrologic</span> connections and for determining basic hydraulic and geometric parameters necessary for establishing operative solute-transport processes. Tracer-test design can be difficult because of a lack of prior knowledge of the basic hydraulic and geometric parameters desired and the appropriate tracer mass to release. A new efficient <span class="hlt">hydrologic</span> tracer-test design (EHTD) methodology has been developed that combines basic measured field parameters (e.g., discharge, distance, cross-sectional area) in functional relationships that describe solute-transport processes related to flow velocity and time of travel. The new method applies these initial estimates for time of travel and velocity to a hypothetical continuously stirred tank reactor as an analog for the <span class="hlt">hydrologic</span> flow system to develop initial estimates for tracer concentration and axial dispersion, based on a preset average tracer concentration. Root determination of the one-dimensional advection-dispersion equation (ADE) using the preset average tracer concentration then provides a theoretical basis for an estimate of necessary tracer mass.Application of the <span class="hlt">predicted</span> tracer mass with the hydraulic and geometric parameters in the ADE allows for an approximation of initial sample-collection time and subsequent sample-collection frequency where a maximum of 65 samples were determined to</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2011WRR....47.4517N','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2011WRR....47.4517N"><span><span class="hlt">Hydrologic</span> controls on equilibrium soil depths</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Nicótina, L.; Tarboton, D. G.; Tesfa, T. K.; Rinaldo, A.</p> <p>2011-04-01</p> <p>This paper deals with modeling the mutual feedbacks between runoff production and geomorphological processes and attributes that lead to patterns of equilibrium soil depth. Our primary goal is an attempt to describe spatial patterns of soil depth resulting from long-term interactions between <span class="hlt">hydrologic</span> forcings and soil production, erosion, and sediment transport processes under the framework of landscape dynamic equilibrium. Another goal is to set the premises for exploiting the role of soil depths in shaping the <span class="hlt">hydrologic</span> response of a catchment. The relevance of the study stems from the massive improvement in <span class="hlt">hydrologic</span> <span class="hlt">predictions</span> for ungauged basins that would be achieved by using directly soil depths derived from geomorphic features remotely measured and objectively manipulated. <span class="hlt">Hydrological</span> processes are here described by explicitly accounting for local soil depths and detailed catchment topography. Geomorphological processes are described by means of well-studied geomorphic transport laws. The modeling approach is applied to the semiarid Dry Creek Experimental Watershed, located near Boise, Idaho. Modeled soil depths are compared with field data obtained from an extensive survey of the catchment. Our results show the ability of the model to describe properly the mean soil depth and the broad features of the distribution of measured data. However, local comparisons show significant scatter whose origins are discussed.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013AGUFM.H52C..08S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013AGUFM.H52C..08S"><span>A Seamless Framework for Global Water Cycle Monitoring and <span class="hlt">Prediction</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Sheffield, J.; Wood, E. F.; Chaney, N.; Fisher, C. K.; Caylor, K. K.</p> <p>2013-12-01</p> <p>The Global Earth Observation System of Systems (GEOSS) Water Strategy ('From Observations to Decisions') recognizes that 'water is essential for ensuring food and energy security, for facilitating poverty reduction and health security, and for the maintenance of ecosystems and biodiversity', and that water cycle data and observations are critical for improved water management and water security - especially in less developed regions. The GEOSS Water Strategy has articulated a number of goals for improved water management, including flood and drought preparedness, that include: (i) facilitating the use of Earth Observations for water cycle observations; (ii) facilitating the acquisition, processing, and distribution of data products needed for effective management; (iii) providing expertise, information systems, and datasets to the global, regional, and national water communities. There are several challenges that must be met to <span class="hlt">advance</span> our capability to provide near real-time water cycle monitoring, early warning of <span class="hlt">hydrological</span> hazards (floods and droughts) and risk assessment under climate change, regionally and globally. Current approaches to monitoring and <span class="hlt">predicting</span> <span class="hlt">hydrological</span> hazards are limited in many parts of the world, and especially in developing countries where national capacity is limited and monitoring networks are inadequate. This presentation describes the development of a seamless monitoring and <span class="hlt">prediction</span> framework at all time scales that allows for consistent assessment of water variability from historic to current conditions, and from seasonal and decadal <span class="hlt">predictions</span> to climate change projections. At the center of the framework is an experimental, global water cycle monitoring and seasonal forecast system that has evolved out of regional and continental systems for the US and Africa. The system is based on land surface <span class="hlt">hydrological</span> modeling that is driven by satellite remote sensing precipitation to <span class="hlt">predict</span> current <span class="hlt">hydrological</span> conditions</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/25224937','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/25224937"><span>Do plasma concentrations of apelin <span class="hlt">predict</span> prognosis in patients with <span class="hlt">advanced</span> heart failure?</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Dalzell, Jonathan R; Jackson, Colette E; Chong, Kwok S; McDonagh, Theresa A; Gardner, Roy S</p> <p>2014-01-01</p> <p>Apelin is an endogenous vasodilator and inotrope, plasma concentrations of which are reduced in <span class="hlt">advanced</span> heart failure (HF). We determined the prognostic significance of plasma concentrations of apelin in <span class="hlt">advanced</span> HF. Plasma concentrations of apelin were measured in 182 patients with <span class="hlt">advanced</span> HF secondary to left ventricular systolic dysfunction. The <span class="hlt">predictive</span> value of apelin for the primary end point of all-cause mortality was assessed over a median follow-up period of 544 (IQR: 196-923) days. In total, 30 patients (17%) reached the primary end point. Of those patients with a plasma apelin concentration above the median, 14 (16%) reached the primary end point compared with 16 (17%) of those with plasma apelin levels below the median (p = NS). NT-proBNP was the most powerful prognostic marker in this population (log rank statistic: 10.37; p = 0.001). Plasma apelin concentrations do not <span class="hlt">predict</span> medium to long-term prognosis in patients with <span class="hlt">advanced</span> HF secondary to left ventricular systolic dysfunction.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.usgs.gov/fs/2009/3002/','USGSPUBS'); return false;" href="https://pubs.usgs.gov/fs/2009/3002/"><span>Integrated Science: Florida Manatees and Everglades <span class="hlt">Hydrology</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>Langtimm, Catherine A.; Swain, Eric D.; Stith, Bradley M.; Reid, James P.; Slone, Daniel H.; Decker, Jeremy; Butler, Susan M.; Doyle, Terry; Snow, R.W.</p> <p>2009-01-01</p> <p><span class="hlt">Predicting</span> and monitoring restoration effects on Florida manatees, which are known to make extended movements, will be incomplete if modeling and monitoring are limited to the smaller areas defined by the various res-toration components. U.S. Geological Survey (USGS) efforts, thus far, have focused on (1) collecting manatee movement data throughout the Ten Thousand Islands (TTI) region, and (2) developing an individual-based model for manatees to illustrate manatee responses to changes in <span class="hlt">hydrology</span> related to the Picayune Strand Restoration Project (PSRP). In 2006, new regional research was begun to extend an Everglades <span class="hlt">hydrology</span> model into the TTI region; extend the manatee movement model into the southern estuaries of Everglades National Park (ENP); and integrate <span class="hlt">hydrology</span> and manatee data, models, and monitoring across the TTI region and ENP. Currently (2008), three research tasks are underway to develop the necessary modeling components to assess restoration efforts across the Greater Everglades Ecosystem.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/biblio/1149386-associations-among-hydrologic-classifications-fish-traits-support-environmental-flow-standards','SCIGOV-STC'); return false;" href="https://www.osti.gov/biblio/1149386-associations-among-hydrologic-classifications-fish-traits-support-environmental-flow-standards"><span>Associations among <span class="hlt">hydrologic</span> classifications and fish traits to support environmental flow standards</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>McManamay, Ryan A; Bevelhimer, Mark S; Frimpong, Dr. Emmanuel A,</p> <p>2014-01-01</p> <p>Classification systems are valuable to ecological management in that they organize information into consolidated units thereby providing efficient means to achieve conservation objectives. Of the many ways classifications benefit management, hypothesis generation has been discussed as the most important. However, in order to provide templates for developing and testing ecologically relevant hypotheses, classifications created using environmental variables must be linked to ecological patterns. Herein, we develop associations between a recent US <span class="hlt">hydrologic</span> classification and fish traits in order to form a template for generating flow ecology hypotheses and supporting environmental flow standard development. Tradeoffs in adaptive strategies for fish weremore » observed across a spectrum of stable, perennial flow to unstable intermittent flow. In accordance with theory, periodic strategists were associated with stable, <span class="hlt">predictable</span> flow, whereas opportunistic strategists were more affiliated with intermittent, variable flows. We developed linkages between the uniqueness of <span class="hlt">hydrologic</span> character and ecological distinction among classes, which may translate into <span class="hlt">predictions</span> between losses in <span class="hlt">hydrologic</span> uniqueness and ecological community response. Comparisons of classification strength between <span class="hlt">hydrologic</span> classifications and other frameworks suggested that spatially contiguous classifications with higher regionalization will tend to explain more variation in ecological patterns. Despite explaining less ecological variation than other frameworks, we contend that <span class="hlt">hydrologic</span> classifications are still useful because they provide a conceptual linkage between <span class="hlt">hydrologic</span> variation and ecological communities to support flow ecology relationships. Mechanistic associations among fish traits and <span class="hlt">hydrologic</span> classes support the presumption that environmental flow standards should be developed uniquely for stream classes and ecological communities, therein.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017EGUGA..19.9718A','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017EGUGA..19.9718A"><span>On the information content of <span class="hlt">hydrological</span> signatures and their relationship to catchment attributes</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Addor, Nans; Clark, Martyn P.; Prieto, Cristina; Newman, Andrew J.; Mizukami, Naoki; Nearing, Grey; Le Vine, Nataliya</p> <p>2017-04-01</p> <p><span class="hlt">Hydrological</span> signatures, which are indices characterizing <span class="hlt">hydrologic</span> behavior, are increasingly used for the evaluation, calibration and selection of <span class="hlt">hydrological</span> models. Their key advantage is to provide more direct insights into specific <span class="hlt">hydrological</span> processes than aggregated metrics (e.g., the Nash-Sutcliffe efficiency). A plethora of signatures now exists, which enable characterizing a variety of hydrograph features, but also makes the selection of signatures for new studies challenging. Here we propose that the selection of signatures should be based on their information content, which we estimated using several approaches, all leading to similar conclusions. To explore the relationship between <span class="hlt">hydrological</span> signatures and the landscape, we extended a previously published data set of hydrometeorological time series for 671 catchments in the contiguous United States, by characterizing the climatic conditions, topography, soil, vegetation and stream network of each catchment. This new catchment attributes data set will soon be in open access, and we are looking forward to introducing it to the community. We used this data set in a data-learning algorithm (random forests) to explore whether <span class="hlt">hydrological</span> signatures could be inferred from catchment attributes alone. We find that some signatures can be <span class="hlt">predicted</span> remarkably well by random forests and, interestingly, the same signatures are well captured when simulating discharge using a conceptual <span class="hlt">hydrological</span> model. We discuss what this result reveals about our understanding of <span class="hlt">hydrological</span> processes shaping <span class="hlt">hydrological</span> signatures. We also identify which catchment attributes exert the strongest control on catchment behavior, in particular during extreme <span class="hlt">hydrological</span> events. Overall, climatic attributes have the most significant influence, and strongly condition how well <span class="hlt">hydrological</span> signatures can be <span class="hlt">predicted</span> by random forests and simulated by the <span class="hlt">hydrological</span> model. In contrast, soil characteristics at the</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2010AGUFM.H11D0827Y','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2010AGUFM.H11D0827Y"><span>Early warnings of the potential for malaria transmission in Rural Africa using the <span class="hlt">Hydrology</span>, Entomology and Malaria Transmission Simulator (HYDREMATS)</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Yamana, T. K.; Eltahir, E. A.</p> <p>2010-12-01</p> <p>Early warnings of malaria transmission allow health officials to better prepare for future epidemics. Monitoring rainfall is recognized as an important part of malaria early warning systems, as outlined by the Roll Back Malaria Initiative. The <span class="hlt">Hydrology</span>, Entomology and Malaria Simulator (HYDREMATS) is a mechanistic model that relates rainfall to malaria transmission, and could be used to provide early warnings of malaria epidemics. HYDREMATS is used to make <span class="hlt">predictions</span> of mosquito populations and vectorial capacity for 2005, 2006, and 2007 in Banizoumbou village in western Niger. HYDREMATS is forced by observed rainfall, followed by a rainfall <span class="hlt">prediction</span> based on the seasonal mean rainfall for a period two or four weeks into the future. <span class="hlt">Predictions</span> made using this method provided reasonable estimates of mosquito populations and vectorial capacity, two to four weeks in <span class="hlt">advance</span>. The <span class="hlt">predictions</span> were significantly improved compared to those made when HYDREMATS was forced with seasonal mean rainfall alone.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2010AdWR...33.1176R','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2010AdWR...33.1176R"><span><span class="hlt">Hydrologic</span> drought <span class="hlt">prediction</span> under climate change: Uncertainty modeling with Dempster-Shafer and Bayesian approaches</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Raje, Deepashree; Mujumdar, P. P.</p> <p>2010-09-01</p> <p>Representation and quantification of uncertainty in climate change impact studies are a difficult task. Several sources of uncertainty arise in studies of <span class="hlt">hydrologic</span> impacts of climate change, such as those due to choice of general circulation models (GCMs), scenarios and downscaling methods. Recently, much work has focused on uncertainty quantification and modeling in regional climate change impacts. In this paper, an uncertainty modeling framework is evaluated, which uses a generalized uncertainty measure to combine GCM, scenario and downscaling uncertainties. The Dempster-Shafer (D-S) evidence theory is used for representing and combining uncertainty from various sources. A significant advantage of the D-S framework over the traditional probabilistic approach is that it allows for the allocation of a probability mass to sets or intervals, and can hence handle both aleatory or stochastic uncertainty, and epistemic or subjective uncertainty. This paper shows how the D-S theory can be used to represent beliefs in some hypotheses such as <span class="hlt">hydrologic</span> drought or wet conditions, describe uncertainty and ignorance in the system, and give a quantitative measurement of belief and plausibility in results. The D-S approach has been used in this work for information synthesis using various evidence combination rules having different conflict modeling approaches. A case study is presented for <span class="hlt">hydrologic</span> drought <span class="hlt">prediction</span> using downscaled streamflow in the Mahanadi River at Hirakud in Orissa, India. Projections of n most likely monsoon streamflow sequences are obtained from a conditional random field (CRF) downscaling model, using an ensemble of three GCMs for three scenarios, which are converted to monsoon standardized streamflow index (SSFI-4) series. This range is used to specify the basic probability assignment (bpa) for a Dempster-Shafer structure, which represents uncertainty associated with each of the SSFI-4 classifications. These uncertainties are then combined across</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFMPP31D2311M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFMPP31D2311M"><span><span class="hlt">Predictable</span> oxygen isotope exchange of plant lipids improves our ability to understand <span class="hlt">hydrologic</span> shifts and partition evapotranspiration across scales</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Maxwell, T.; Silva, L. C. R.; Horwath, W. R.</p> <p>2016-12-01</p> <p>Understanding the partitioning of evapotranspiration is critical to assessing how changes in climate affect the terrestrial water cycle. N-alkyl lipids have been successfully used to integrate local to regional scale <span class="hlt">hydrologic</span> change through the integration of δD measured in specific compounds found in sediments. However, such studies are limited compared to contemporary <span class="hlt">hydrologic</span> studies which have the advantage of using dual isotope methods whereby δD and δ18O are used in conjunction to partition evapotranspiration. δD values in n-alkyl lipids have been established as resistant to exchange with environmental water and, this approach has allowed for routine measurement and reconstruction of plant water δD. In contrast, the use of δ18O in organic matter remains incipient because the low oxygen content of plant lipids makes it difficult to accurately measure δ18O. In the interest of addressing both fundamental and practical potential of a lipid δ18O proxy, we present the first evidence for <span class="hlt">predictable</span> exchange of δ18O between environmental water and hydrophobic bulk organic matter, neutral saponified lipids, and specific plant derived compounds Our data suggests that these different pools may be used to reconstruct the original source water δD/δ18O relationship from soil or sedimentary organic matter, which will help elucidate <span class="hlt">hydrologic</span> shifts in terrestrial systems. Our results bring new insight into methods by which organic compounds might be used to partition evapotranspiration across large spatial scales in both contemporary and reconstructed systems.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20110008056','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20110008056"><span><span class="hlt">Predicting</span> <span class="hlt">Hydrological</span> Drought: Relative Contributions of Soil Moisture and Snow Information to Seasonal Streamflow <span class="hlt">Prediction</span> Skill</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Koster, R.; Mahanama, S.; Livneh, B.; Lettenmaier, D.; Reichle, R.</p> <p>2011-01-01</p> <p>in this study we examine how knowledge of mid-winter snow accumulation and soil moisture conditions contribute to our ability to <span class="hlt">predict</span> streamflow months in <span class="hlt">advance</span>. A first "synthetic truth" analysis focuses on a series of numerical experiments with multiple sophisticated land surface models driven with a dataset of observations-based meteorological forcing spanning multiple decades and covering the continental United States. Snowpack information by itself obviously contributes to the skill attained in streamflow <span class="hlt">prediction</span>, particularly in the mountainous west. The isolated contribution of soil moisture information, however, is found to be large and significant in many areas, particularly in the west but also in region surrounding the Great Lakes. The results are supported by a supplemental, observations-based analysis using (naturalized) March-July streamflow measurements covering much of the western U.S. Additional forecast experiments using start dates that span the year indicate a strong seasonality in the skill contributions; soil moisture information, for example, contributes to kill at much longer leads for forecasts issued in winter than for those issued in summer.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19770018663','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19770018663"><span>Remote sensing inputs to landscape models which <span class="hlt">predict</span> future spatial land use patterns for <span class="hlt">hydrologic</span> models</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Miller, L. D.; Tom, C.; Nualchawee, K.</p> <p>1977-01-01</p> <p>A tropical forest area of Northern Thailand provided a test case of the application of the approach in more natural surroundings. Remote sensing imagery subjected to proper computer analysis has been shown to be a very useful means of collecting spatial data for the science of <span class="hlt">hydrology</span>. Remote sensing products provide direct input to <span class="hlt">hydrologic</span> models and practical data bases for planning large and small-scale <span class="hlt">hydrologic</span> developments. Combining the available remote sensing imagery together with available map information in the landscape model provides a basis for substantial improvements in these applications.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://cfpub.epa.gov/si/si_public_record_report.cfm?dirEntryId=248778&keyword=Groups+AND+networks&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=248778&keyword=Groups+AND+networks&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>Oregon <span class="hlt">Hydrologic</span> Landscapes: An Approach for Broadscale <span class="hlt">Hydrologic</span> Classification</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>Gaged streams represent only a small percentage of watershed <span class="hlt">hydrologic</span> conditions throughout the Unites States and globe, but there is a growing need for <span class="hlt">hydrologic</span> classification systems that can serve as the foundation for broad-scale assessments of the <span class="hlt">hydrologic</span> functions of...</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/2014EGUGA..1613372V','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014EGUGA..1613372V"><span>Ensemble catchment <span class="hlt">hydrological</span> modelling for climate change impact analysis</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Vansteenkiste, Thomas; Ntegeka, Victor; Willems, Patrick</p> <p>2014-05-01</p> <p>It is vital to investigate how the <span class="hlt">hydrological</span> model structure affects the climate change impact given that future changes not in the range for which the models were calibrated or validated are likely. Thus an ensemble modelling approach which involves a diversity of models with different structures such as spatial resolutions and process descriptions is crucial. The ensemble modelling approach was applied to a set of models: from the lumped conceptual models NAM, PDM and VHM, an intermediate detailed and distributed model WetSpa, to the highly detailed and fully distributed model MIKE-SHE. Explicit focus was given to the high and low flow extremes. All models were calibrated for sub flows and quick flows derived from rainfall and potential evapotranspiration (ETo) time series. In general, all models were able to produce reliable estimates of the flow regimes under the current climate for extreme peak and low flows. An intercomparison of the low and high flow changes under changed climatic conditions was made using climate scenarios tailored for extremes. Tailoring was important for two reasons. First, since the use of many scenarios was not feasible it was necessary to construct few scenarios that would reasonably represent the range of extreme impacts. Second, scenarios would be more informative as changes in high and low flows would be easily traced to changes of ETo and rainfall; the tailored scenarios are constructed using seasonal changes that are defined using different levels of magnitude (high, mean and low) for rainfall and ETo. After simulation of these climate scenarios in the five <span class="hlt">hydrological</span> models, close agreement was found among the models. The different models <span class="hlt">predicted</span> similar range of peak flow changes. For the low flows, however, the differences in the projected impact range by different <span class="hlt">hydrological</span> models was larger, particularly for the drier scenarios. This suggests that the <span class="hlt">hydrological</span> model structure is critical in low flow <span class="hlt">predictions</span></p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2011AGUFM.H21F1211F','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2011AGUFM.H21F1211F"><span>Replacing climatological potential evapotranspiration estimates with dynamic satellite-based observations in operational <span class="hlt">hydrologic</span> <span class="hlt">prediction</span> models</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Franz, K. J.; Bowman, A. L.; Hogue, T. S.; Kim, J.; Spies, R.</p> <p>2011-12-01</p> <p>In the face of a changing climate, growing populations, and increased human habitation in <span class="hlt">hydrologically</span> risky locations, both short- and long-range planners increasingly require robust and reliable streamflow forecast information. Current operational forecasting utilizes watershed-scale, conceptual models driven by ground-based (commonly point-scale) observations of precipitation and temperature and climatological potential evapotranspiration (PET) estimates. The PET values are derived from historic pan evaporation observations and remain static from year-to-year. The need for regional dynamic PET values is vital for improved operational forecasting. With the advent of satellite remote sensing and the adoption of a more flexible operational forecast system by the National Weather Service, incorporation of <span class="hlt">advanced</span> data products is now more feasible than in years past. In this study, we will test a previously developed satellite-derived PET product (UCLA MODIS-PET) in the National Weather Service forecast models and compare the model results to current methods. The UCLA MODIS-PET method is based on the Priestley-Taylor formulation, is driven with MODIS satellite products, and produces a daily, 250m PET estimate. The focus area is eight headwater basins in the upper Midwest U.S. There is a need to develop improved forecasting methods for this region that are able to account for climatic and landscape changes more readily and effectively than current methods. This region is highly flood prone yet sensitive to prolonged dry periods in late summer and early fall, and is characterized by a highly managed landscape, which has drastically altered the natural <span class="hlt">hydrologic</span> cycle. Our goal is to improve model simulations, and thereby, the initial conditions prior to the start of a forecast through the use of PET values that better reflect actual watershed conditions. The forecast models are being tested in both distributed and lumped mode.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/23338229','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/23338229"><span><span class="hlt">Predictive</span> factors for overall quality of life in patients with <span class="hlt">advanced</span> cancer.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Cramarossa, Gemma; Chow, Edward; Zhang, Liying; Bedard, Gillian; Zeng, Liang; Sahgal, Arjun; Vassiliou, Vassilios; Satoh, Takefumi; Foro, Palmira; Ma, Brigette B Y; Chie, Wei-Chu; Chen, Emily; Lam, Henry; Bottomley, Andrew</p> <p>2013-06-01</p> <p>This study examined which domains/symptoms from the European Organisation for Research and Treatment of Cancer (EORTC) Quality of Life Questionnaire Core 15 Palliative (QLQ-C15-PAL), an abbreviated version of the health-related EORTC QLQ-C30 questionnaire designed for palliative cancer patients, were <span class="hlt">predictive</span> of overall quality of life (QOL) in <span class="hlt">advanced</span> cancer patients. Patients with <span class="hlt">advanced</span> cancer from six countries completed the QLQ-C15-PAL at consultation and at one follow-up point. Univariate and multivariate regression analyses were conducted to determine the <span class="hlt">predictive</span> value of the EORTC QLQ-C15-PAL functional/symptom scores for global QOL (question 15). Three hundred forty-nine patients completed the EORTC QLQ-C15-PAL at baseline. In the total patient sample, worse emotional functioning, pain, and appetite loss were the most significant <span class="hlt">predictive</span> factors for worse QOL. In the subgroup of patients with bone metastases (n = 240), the domains mentioned above were also the most significant predictors, whereas in patients with brain metastases (n = 109), worse physical and emotional functioning most significantly <span class="hlt">predicted</span> worse QOL. One-month follow-up in 267 patients revealed that the significant predictors changed somewhat over time. For example, in the total patient sample, physical functioning, fatigue, and appetite loss were significant predictors at the follow-up point. A sub-analysis of <span class="hlt">predictive</span> factors affecting QOL by primary cancer (lung, breast, and prostate) was also conducted for the total patient sample. Deterioration of certain EORTC QLQ-C15-PAL functional/symptom scores significantly contributes to worse overall QOL. Special attention should be directed to managing factors most influential on overall QOL to ensure optimal management of <span class="hlt">advanced</span> cancer patients.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012AGUFM.H51I1476K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012AGUFM.H51I1476K"><span>Accounting for inter-annual and seasonal variability in regionalization of <span class="hlt">hydrologic</span> response in the Great Lakes basin</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Kult, J. M.; Fry, L. M.; Gronewold, A. D.</p> <p>2012-12-01</p> <p>Methods for <span class="hlt">predicting</span> streamflow in areas with limited or nonexistent measures of <span class="hlt">hydrologic</span> response typically invoke the concept of regionalization, whereby knowledge pertaining to gauged catchments is transferred to ungauged catchments. In this study, we identify watershed physical characteristics acting as primary drivers of <span class="hlt">hydrologic</span> response throughout the US portion of the Great Lakes basin. Relationships between watershed physical characteristics and <span class="hlt">hydrologic</span> response are generated from 166 catchments spanning a variety of climate, soil, land cover, and land form regimes through regression tree analysis, leading to a grouping of watersheds exhibiting similar <span class="hlt">hydrologic</span> response characteristics. These groupings are then used to <span class="hlt">predict</span> response in ungauged watersheds in an uncertainty framework. Results from this method are assessed alongside one historical regionalization approach which, while simple, has served as a cornerstone of Great Lakes regional <span class="hlt">hydrologic</span> research for several decades. Our approach expands upon previous research by considering multiple temporal characterizations of <span class="hlt">hydrologic</span> response. Due to the substantial inter-annual and seasonal variability in <span class="hlt">hydrologic</span> response observed over the Great Lakes basin, results from the regression tree analysis differ considerably depending on the level of temporal aggregation used to define the response. Specifically, higher levels of temporal aggregation for the response metric (for example, indices derived from long-term means of climate and streamflow observations) lead to improved watershed groupings with lower within-group variance. However, this perceived improvement in model skill occurs at the cost of understated uncertainty when applying the regression to time series simulations or as a basis for model calibration. In such cases, our results indicate that <span class="hlt">predictions</span> based on long-term characterizations of <span class="hlt">hydrologic</span> response can produce misleading conclusions when applied at shorter</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.ars.usda.gov/research/publications/publication/?seqNo115=241277','TEKTRAN'); return false;" href="http://www.ars.usda.gov/research/publications/publication/?seqNo115=241277"><span>Soil water repellency and ground cover effects on infiltration in response to prescribed burning of steeply-sloped sagebrush hillslopes</span></a></p> <p><a target="_blank" href="https://www.ars.usda.gov/research/publications/find-a-publication/">USDA-ARS?s Scientific Manuscript database</a></p> <p></p> <p></p> <p>Rangeland managers and scientists are in need of <span class="hlt">predictive</span> tools to accurately simulate post-fire <span class="hlt">hydrologic</span> responses and provide <span class="hlt">hydrologic</span> risk assessment. Rangeland <span class="hlt">hydrologic</span> modeling has <span class="hlt">advanced</span> in recent years; however, model <span class="hlt">advancements</span> have largely been associated with data from gently ...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/25062815','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/25062815"><span><span class="hlt">PREDICT</span>: a diagnostic accuracy study of a tool for <span class="hlt">predicting</span> mortality within one year: who should have an <span class="hlt">advance</span> healthcare directive?</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Richardson, Philip; Greenslade, Jaimi; Shanmugathasan, Sulochana; Doucet, Katherine; Widdicombe, Neil; Chu, Kevin; Brown, Anthony</p> <p>2015-01-01</p> <p>CARING is a screening tool developed to identify patients who have a high likelihood of death in 1 year. This study sought to validate a modified CARING tool (termed <span class="hlt">PREDICT</span>) using a population of patients presenting to the Emergency Department. In total, 1000 patients aged over 55 years who were admitted to hospital via the Emergency Department between January and June 2009 were eligible for inclusion in this study. Data on the six prognostic indicators comprising <span class="hlt">PREDICT</span> were obtained retrospectively from patient records. One-year mortality data were obtained from the State Death Registry. Weights were applied to each <span class="hlt">PREDICT</span> criterion, and its final score ranged from 0 to 44. Receiver operator characteristic analyses and diagnostic accuracy statistics were used to assess the accuracy of <span class="hlt">PREDICT</span> in identifying 1-year mortality. The sample comprised 976 patients with a median (interquartile range) age of 71 years (62-81 years) and a 1-year mortality of 23.4%. In total, 50% had ≥1 <span class="hlt">PREDICT</span> criteria with a 1-year mortality of 40.4%. Receiver operator characteristic analysis gave an area under the curve of 0.86 (95% confidence interval: 0.83-0.89). Using a cut-off of 13 points, <span class="hlt">PREDICT</span> had a 95.3% (95% confidence interval: 93.6-96.6) specificity and 53.9% (95% confidence interval: 47.5-60.3) sensitivity for <span class="hlt">predicting</span> 1-year mortality. <span class="hlt">PREDICT</span> was simpler than the CARING criteria and identified 158 patients per 1000 admitted who could benefit from <span class="hlt">advance</span> care planning. <span class="hlt">PREDICT</span> was successfully applied to the Australian healthcare system with findings similar to the original CARING study conducted in the United States. This tool could improve end-of-life care by identifying who should have <span class="hlt">advance</span> care planning or an <span class="hlt">advance</span> healthcare directive. © The Author(s) 2014.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/25406073','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/25406073"><span>High-speed limnology: using <span class="hlt">advanced</span> sensors to investigate spatial variability in biogeochemistry and <span class="hlt">hydrology</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Crawford, John T; Loken, Luke C; Casson, Nora J; Smith, Colin; Stone, Amanda G; Winslow, Luke A</p> <p>2015-01-06</p> <p><span class="hlt">Advanced</span> sensor technology is widely used in aquatic monitoring and research. Most applications focus on temporal variability, whereas spatial variability has been challenging to document. We assess the capability of water chemistry sensors embedded in a high-speed water intake system to document spatial variability. This new sensor platform continuously samples surface water at a range of speeds (0 to >45 km h(-1)) resulting in high-density, mesoscale spatial data. These novel observations reveal previously unknown variability in physical, chemical, and biological factors in streams, rivers, and lakes. By combining multiple sensors into one platform, we were able to detect terrestrial-aquatic <span class="hlt">hydrologic</span> connections in a small dystrophic lake, to infer the role of main-channel vs backwater nutrient processing in a large river and to detect sharp chemical changes across aquatic ecosystem boundaries in a stream/lake complex. Spatial sensor data were verified in our examples by comparing with standard lab-based measurements of selected variables. Spatial fDOM data showed strong correlation with wet chemistry measurements of DOC, and optical NO3 concentrations were highly correlated with lab-based measurements. High-frequency spatial data similar to our examples could be used to further understand aquatic biogeochemical fluxes, ecological patterns, and ecosystem processes, and will both inform and benefit from fixed-site data.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70182177','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70182177"><span>High-speed limnology: Using <span class="hlt">advanced</span> sensors to investigate spatial variability in biogeochemistry and <span class="hlt">hydrology</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>Crawford, John T.; Loken, Luke C.; Casson, Nora J.; Smith, Collin; Stone, Amanda G.; Winslow, Luke A.</p> <p>2015-01-01</p> <p><span class="hlt">Advanced</span> sensor technology is widely used in aquatic monitoring and research. Most applications focus on temporal variability, whereas spatial variability has been challenging to document. We assess the capability of water chemistry sensors embedded in a high-speed water intake system to document spatial variability. This new sensor platform continuously samples surface water at a range of speeds (0 to >45 km h–1) resulting in high-density, mesoscale spatial data. These novel observations reveal previously unknown variability in physical, chemical, and biological factors in streams, rivers, and lakes. By combining multiple sensors into one platform, we were able to detect terrestrial–aquatic <span class="hlt">hydrologic</span> connections in a small dystrophic lake, to infer the role of main-channel vs backwater nutrient processing in a large river and to detect sharp chemical changes across aquatic ecosystem boundaries in a stream/lake complex. Spatial sensor data were verified in our examples by comparing with standard lab-based measurements of selected variables. Spatial fDOM data showed strong correlation with wet chemistry measurements of DOC, and optical NO3 concentrations were highly correlated with lab-based measurements. High-frequency spatial data similar to our examples could be used to further understand aquatic biogeochemical fluxes, ecological patterns, and ecosystem processes, and will both inform and benefit from fixed-site data.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://cfpub.epa.gov/si/si_public_record_report.cfm?dirEntryId=47028&Lab=ORD&keyword=evapotranspiration&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=47028&Lab=ORD&keyword=evapotranspiration&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>EVALUATING CUMULATIVE EFFECTS OF DISTURBANCE ON THE <span class="hlt">HYDROLOGIC</span> FUNCTION OF BOGS, FENS, AND MIRES</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>Few quantitative studies have been done on the <span class="hlt">hydrology</span> of fens, bogs and mires, and consequently any <span class="hlt">predictions</span> of the cumulative impacts of disturbances on their <span class="hlt">hydrologic</span> functions is extremely difficult. or example, few data are available on the role of bogs and fens with ...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://eric.ed.gov/?q=drought&pg=6&id=EJ185405','ERIC'); return false;" href="https://eric.ed.gov/?q=drought&pg=6&id=EJ185405"><span><span class="hlt">Hydrology</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>Sharp, John M., Jr.</p> <p>1978-01-01</p> <p>The past year saw a re-emphasis on the practical aspects of <span class="hlt">hydrology</span> due to regional drought patterns, urban flooding, and agricultural and energy demands on water resources. Highlights of <span class="hlt">hydrologic</span> symposia, publications, and events are included. (MA)</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70191374','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70191374"><span>Modeling summer month <span class="hlt">hydrological</span> drought probabilities in the United States using antecedent flow conditions</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Austin, Samuel H.; Nelms, David L.</p> <p>2017-01-01</p> <p>Climate change raises concern that risks of <span class="hlt">hydrological</span> drought may be increasing. We estimate <span class="hlt">hydrological</span> drought probabilities for rivers and streams in the United States (U.S.) using maximum likelihood logistic regression (MLLR). Streamflow data from winter months are used to estimate the chance of <span class="hlt">hydrological</span> drought during summer months. Daily streamflow data collected from 9,144 stream gages from January 1, 1884 through January 9, 2014 provide <span class="hlt">hydrological</span> drought streamflow probabilities for July, August, and September as functions of streamflows during October, November, December, January, and February, estimating outcomes 5-11 months ahead of their occurrence. Few drought <span class="hlt">prediction</span> methods exploit temporal links among streamflows. We find MLLR modeling of drought streamflow probabilities exploits the explanatory power of temporally linked water flows. MLLR models with strong correct classification rates were produced for streams throughout the U.S. One ad hoc test of correct <span class="hlt">prediction</span> rates of September 2013 <span class="hlt">hydrological</span> droughts exceeded 90% correct classification. Some of the best-performing models coincide with areas of high concern including the West, the Midwest, Texas, the Southeast, and the Mid-Atlantic. Using <span class="hlt">hydrological</span> drought MLLR probability estimates in a water management context can inform understanding of drought streamflow conditions, provide warning of future drought conditions, and aid water management decision making.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013HESSD..1012905D','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013HESSD..1012905D"><span>Validating a spatially distributed <span class="hlt">hydrological</span> model with soil morphology data</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Doppler, T.; Honti, M.; Zihlmann, U.; Weisskopf, P.; Stamm, C.</p> <p>2013-10-01</p> <p>Spatially distributed <span class="hlt">hydrological</span> models are popular tools in <span class="hlt">hydrology</span> and they are claimed to be useful to support management decisions. Despite the high spatial resolution of the computed variables, calibration and validation is often carried out only on discharge time-series at specific locations due to the lack of spatially distributed reference data. Because of this restriction, the <span class="hlt">predictive</span> power of these models, with regard to <span class="hlt">predicted</span> spatial patterns, can usually not be judged. An example of spatial <span class="hlt">predictions</span> in <span class="hlt">hydrology</span> is the <span class="hlt">prediction</span> of saturated areas in agricultural catchments. These areas can be important source areas for the transport of agrochemicals to the stream. We set up a spatially distributed model to <span class="hlt">predict</span> saturated areas in a 1.2 km2 catchment in Switzerland with moderate topography. Around 40% of the catchment area are artificially drained. We measured weather data, discharge and groundwater levels in 11 piezometers for 1.5 yr. For broadening the spatially distributed data sets that can be used for model calibration and validation, we translated soil morphological data available from soil maps into an estimate of the duration of soil saturation in the soil horizons. We used redox-morphology signs for these estimates. This resulted in a data set with high spatial coverage on which the model <span class="hlt">predictions</span> were validated. In general, these saturation estimates corresponded well to the measured groundwater levels. We worked with a model that would be applicable for management decisions because of its fast calculation speed and rather low data requirements. We simultaneously calibrated the model to the groundwater levels in the piezometers and discharge. The model was able to reproduce the general <span class="hlt">hydrological</span> behavior of the catchment in terms of discharge and absolute groundwater levels. However, the accuracy of the groundwater level <span class="hlt">predictions</span> was not high enough to be used for the <span class="hlt">prediction</span> of saturated areas. The groundwater</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013AGUFMIN53A1549S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013AGUFMIN53A1549S"><span>Distributed <span class="hlt">Hydrologic</span> Modeling Apps for Decision Support in the Cloud</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Swain, N. R.; Latu, K.; Christiensen, S.; Jones, N.; Nelson, J.</p> <p>2013-12-01</p> <p><span class="hlt">Advances</span> in computation resources and greater availability of water resources data represent an untapped resource for addressing <span class="hlt">hydrologic</span> uncertainties in water resources decision-making. The current practice of water authorities relies on empirical, lumped <span class="hlt">hydrologic</span> models to estimate watershed response. These models are not capable of taking advantage of many of the spatial datasets that are now available. Physically-based, distributed <span class="hlt">hydrologic</span> models are capable of using these data resources and providing better <span class="hlt">predictions</span> through stochastic analysis. However, there exists a digital divide that discourages many science-minded decision makers from using distributed models. This divide can be spanned using a combination of existing web technologies. The purpose of this presentation is to present a cloud-based environment that will offer <span class="hlt">hydrologic</span> modeling tools or 'apps' for decision support and the web technologies that have been selected to aid in its implementation. Compared to the more commonly used lumped-parameter models, distributed models, while being more intuitive, are still data intensive, computationally expensive, and difficult to modify for scenario exploration. However, web technologies such as web GIS, web services, and cloud computing have made the data more accessible, provided an inexpensive means of high-performance computing, and created an environment for developing user-friendly apps for distributed modeling. Since many water authorities are primarily interested in the scenario exploration exercises with <span class="hlt">hydrologic</span> models, we are creating a toolkit that facilitates the development of a series of apps for manipulating existing distributed models. There are a number of hurdles that cloud-based <span class="hlt">hydrologic</span> modeling developers face. One of these is how to work with the geospatial data inherent with this class of models in a web environment. Supporting geospatial data in a website is beyond the capabilities of standard web frameworks and it</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/26259446','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/26259446"><span>[Socio-<span class="hlt">hydrology</span>: A review].</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Ding, Jing-yi; Zhao, Wen-wu; Fang, Xue-ning</p> <p>2015-04-01</p> <p>Socio-<span class="hlt">hydrology</span> is an interdiscipline of <span class="hlt">hydrology</span>, nature, society and humanity. It mainly explores the two-way feedbacks of coupled human-water system and its dynamic mechanism of co-evolution, and makes efforts to solve the issues that human faces today such as sustainable utilization of water resources. Starting from the background, formation process, and fundamental concept of socio-<span class="hlt">hydrology</span>, this paper summarized the features of socio-<span class="hlt">hydrology</span>. The main research content of socio-<span class="hlt">hydrology</span> was reduced to three aspects: The tradeoff in coupled human-water system, interests in water resources management and virtual water research in coupled human-water system. And its differences as well as relations with traditional <span class="hlt">hydrology</span>, eco-<span class="hlt">hydrology</span> and hydro-sociology were dwelled on. Finally, with hope to promote the development of socio-<span class="hlt">hydrology</span> researches in China, the paper made prospects for the development of the subject from following aspects: Completing academic content and deepening quantitative research, focusing on scale studies of socio-<span class="hlt">hydrology</span>, fusing socio-<span class="hlt">hydrology</span> and eco-<span class="hlt">hydrology</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2010ems..confE.329J','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2010ems..confE.329J"><span>Error discrimination of an operational <span class="hlt">hydrological</span> forecasting system at a national scale</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Jordan, F.; Brauchli, T.</p> <p>2010-09-01</p> <p>The use of operational <span class="hlt">hydrological</span> forecasting systems is recommended for hydropower production as well as flood management. However, the forecast uncertainties can be important and lead to bad decisions such as false alarms and inappropriate reservoir management of hydropower plants. In order to improve the forecasting systems, it is important to discriminate the different sources of uncertainties. To achieve this task, reanalysis of past <span class="hlt">predictions</span> can be realized and provide information about the structure of the global uncertainty. In order to discriminate between uncertainty due to the weather numerical model and uncertainty due to the rainfall-runoff model, simulations assuming perfect weather forecast must be realized. This contribution presents the spatial analysis of the weather uncertainties and their influence on the river discharge <span class="hlt">prediction</span> of a few different river basins where an operational forecasting system exists. The forecast is based on the RS 3.0 system [1], [2], which is also running the open Internet platform www.swissrivers.ch [3]. The uncertainty related to the <span class="hlt">hydrological</span> model is compared to the uncertainty related to the weather <span class="hlt">prediction</span>. A comparison between numerous weather <span class="hlt">prediction</span> models [4] at different lead times is also presented. The results highlight an important improving potential of both forecasting components: the <span class="hlt">hydrological</span> rainfall-runoff model and the numerical weather <span class="hlt">prediction</span> models. The <span class="hlt">hydrological</span> processes must be accurately represented during the model calibration procedure, while weather <span class="hlt">prediction</span> models suffer from a systematic spatial bias. REFERENCES [1] Garcia, J., Jordan, F., Dubois, J. & Boillat, J.-L. 2007. "Routing System II, Modélisation d'écoulements dans des systèmes hydrauliques", Communication LCH n° 32, Ed. Prof. A. Schleiss, Lausanne [2] Jordan, F. 2007. Modèle de prévision et de gestion des crues - optimisation des opérations des aménagements hydroélectriques à accumulation</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017WRR....53.3087A','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017WRR....53.3087A"><span>Simulation of the cumulative <span class="hlt">hydrological</span> response to green infrastructure</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Avellaneda, P. M.; Jefferson, A. J.; Grieser, J. M.; Bush, S. A.</p> <p>2017-04-01</p> <p>In this study, we evaluated the cumulative <span class="hlt">hydrologic</span> performance of green infrastructure in a residential area of the city of Parma, Ohio, draining to a tributary of the Cuyahoga River. Green infrastructure included the following spatially distributed devices: 16 street-side bioretention cells, 7 rain gardens, and 37 rain barrels. Data consisted of rainfall and outfall flow records for a wide range of storm events, including pretreatment and treatment periods. The Stormwater Management Model was calibrated and validated to <span class="hlt">predict</span> the <span class="hlt">hydrologic</span> response of green infrastructure. The calibrated model was used to quantify annual water budget alterations and discharge frequency over a 6 year simulation period. For the study catchment, we observed a treatment effect with increases of 1.4% in evaporation, 7.6% in infiltration, and a 9.0% reduction in surface runoff. The <span class="hlt">hydrologic</span> performance of green infrastructure was evaluated by comparing the flow duration curve for pretreatment and treatment outfall flow scenarios. The flow duration curve shifted downward for the green infrastructure scenario. Discharges with a 0.5, 1, 2, and 5 year return period were reduced by an average of 29%. Parameter and <span class="hlt">predictive</span> uncertainties were inspected by implementing a Bayesian statistical approach.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016EGUGA..1814158P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016EGUGA..1814158P"><span>Flash flood warning based on fully dynamic <span class="hlt">hydrology</span> modelling</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Pejanovic, Goran; Petkovic, Slavko; Cvetkovic, Bojan; Nickovic, Slobodan</p> <p>2016-04-01</p> <p>Numerical <span class="hlt">hydrologic</span> modeling has achieved limited success in the past due to, inter alia, lack of adequate input data. Over the last decade, data availability has improved substantially. For modelling purposes, high-resolution data on topography, river routing, and land cover and soil features have meanwhile become available, as well as the observations such as radar precipitation information. In our study, we have implemented the HYPROM model (<span class="hlt">Hydrology</span> Prognostic Model) to <span class="hlt">predict</span> a flash flood event at a smaller-scale basin in Southern Serbia. HYPROM is based on the full set of governing equations for surface <span class="hlt">hydrological</span> dynamics, in which momentum components, along with the equation of mass continuity, are used as full prognostic equations. HYPROM also includes a river routing module serving as a collector for the extra surface water. Such approach permits appropriate representation of different <span class="hlt">hydrology</span> scales ranging from flash floods to flows of large and slow river basins. The use of full governing equations, if not appropriately parameterized, may lead to numerical instability systems when the surface water in a model is vanishing. To resolve these modelling problems, an unconditionally stable numerical scheme and a method for height redistribution avoiding shortwave height noise have been developed in HYPROM, which achieve numerical convergence of u, v and h when surface water disappears. We have applied HYPROM, driven by radar-estimated precipitation, to <span class="hlt">predict</span> flash flooding occurred over smaller and medium-size river basins. Two torrential rainfall cases have been simulated to check the accuracy of the model: the exceptional flooding of May 2014 in Western Serbia, and the convective flash flood of January 2015 in Southern Serbia. The second episode has been successfully <span class="hlt">predicted</span> by HYPROM in terms of timing and intensity six hours before the event occurred. Such flash flood warning system is in preparation to be operationally implemented in the</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015WRR....51.4635H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015WRR....51.4635H"><span>Water conservation and <span class="hlt">hydrological</span> transitions in cities in the 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>Hornberger, George M.; Hess, David J.; Gilligan, Jonathan</p> <p>2015-06-01</p> <p>Cities across the world have had to diversify and expand their water supply systems in response to demand growth, groundwater depletion and pollution, and instability and inadequacy of regional surface freshwater sources. In the U.S., these problems plague not only the arid Western cities but increasingly also cities in the Eastern portions of the country. Although cities continue to seek out new sources of water via Promethean projects of long-distance supply systems, desalinization plants, and the recharge of aquifers with surface water, they also pursue water conservation because of its low cost and other benefits. We examine water conservation as a complex sociotechnical system comprising interactions of political, sociodemographic, economic, and hydroclimatological factors. We provide quantitative data on the factors that affect more and less <span class="hlt">advanced</span> transitions in water conservation regimes, and we show that water stress and other <span class="hlt">hydrological</span> data can only partially <span class="hlt">predict</span> the transition. We also provide qualitative case studies to identify institutional and political barriers to more <span class="hlt">advanced</span> water conservation regimes. This interdisciplinary, mixed methods approach typifies the need for knowledge that informs hydrologists about how their research may or may not be adopted by decision-makers.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014AGUFM.H24B..05H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014AGUFM.H24B..05H"><span>Water Conservation and <span class="hlt">Hydrological</span> Transitions in Cities</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Hornberger, G. M.; Gilligan, J. M.; Hess, D. J.</p> <p>2014-12-01</p> <p>A 2012 report by the National Research Council, Challenges and Opportunities in the <span class="hlt">Hydrologic</span> Sciences, called for the development of "translational <span class="hlt">hydrologic</span> science." Translational research in this context requires knowledge about the communication of science to decision makers and to the public but also improved understanding of the public by the scientists. This kind of knowledge is inherently interdisciplinary because it requires understanding of the complex sociotechnical dimensions of water, policy, and user relations. It is axiomatic that good governance of water resources and water infrastructure requires information about water resources themselves and about the institutions that govern water use. This "socio-<span class="hlt">hydrologic</span>" or "hydrosociological" knowledge is often characterized by complex dynamics between and among human and natural systems. Water Resources Research has provided a forum for presentation of interdisciplinary research in coupled natural-human systems since its inception 50 years ago. The evolution of ideas presented in the journal provides a basis for framing new work, an example of which is water conservation in cities. In particular, we explore the complex interactions of political, sociodemographic, economic, and hydroclimatological factors in affecting decisions that either <span class="hlt">advance</span> or retard the development of water conservation policies.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2001AGUFM.H42A0335S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2001AGUFM.H42A0335S"><span>The Upper Rio Grande Basin as a Long-Term <span class="hlt">Hydrologic</span> Observatory - Challenges and Opportunities</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Springer, E.; Duffy, C.; Phillips, F.; Hogan, J.; Winter, C. L.</p> <p>2001-12-01</p> <p>Long-term <span class="hlt">hydrologic</span> observatories (LTHO) have been identified as a key element to <span class="hlt">advance</span> <span class="hlt">hydrologic</span> science. Issues to be addressed are the size and locations of LTHOs to meet research needs and address water resources management concerns. To date, considerable small watershed research has been performed, and these have provided valuable insights into processes governing <span class="hlt">hydrologic</span> response on local scales. For <span class="hlt">hydrology</span> to <span class="hlt">advance</span> as a science, more complete and coherent data sets at larger scales are needed to tie together local studies and examine lower frequency long wavelength processes that may govern the water cycle at the scale of river basins and continents. The objective of this poster is to describe the potential opportunities and challenges for the upper Rio Grande as a LTHO. The presence of existing research programs and facilities can be leveraged by a LTHO to develop the required scientific measurements. Within the upper Rio Grande Basin, there are two Long-Term Ecological Research sites, Jornada and Sevilleta; Los Alamos National Laboratory, which monitors the atmosphere, surface water and groundwater; a groundwater study is being performed by the USGS in the Albuquerque Basin to examine recharge and water quality issues. Additionally, the upper Rio Grande basin served as an USGS-NAWQA study site starting in the early 1990's and is currently being studied by SAHRA (NSF-STC) to understand sources of salinity of the river system; such studies provide an existing framework on which to base long-term monitoring of water quality. The upper Rio Grande Basin has a wealth of existing long-term climate, <span class="hlt">hydrologic</span> and geochemical records on which to base an LTHO. Within the basin there are currently 122 discharge gages operated by the USGS; and many of these gages have long-term records of discharge. Other organizations operate additional surface water gages in the lower part of the basin. Long-term records of river chemistry have been kept by the USGS, U</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('https://pubs.er.usgs.gov/publication/70171425','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70171425"><span><span class="hlt">Hydrology</span> of the North Cascades region, Washington: 2. A proposed hydrometeorological streamflow <span class="hlt">prediction</span> method</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Tangborn, Wendell V.; Rasmussen, Lowell A.</p> <p>1976-01-01</p> <p>. This contribution decreases to nearly zero during the summer and then rises slightly for late summer <span class="hlt">predictions</span>. The reason for the smaller than expected effect of summer precipitation is thought to be due to the compensating effect of increased evaporative losses and increased infiltration when precipitation is greater than normal during the summer months. The error caused by the beginning winter month (assumed to be October in this study) not coinciding with the time of minimum storage was examined; it appears that October may be the best average beginning winter month for most drainages but that a more detailed study is needed. The optimum beginning of the winter season appears to vary from August to October when individual years are examined. These results demonstrate that standard precipitation and runoff measurements in the North Cascades region are adequate for constructing a <span class="hlt">predictive</span> <span class="hlt">hydrologic</span> model. This model can be used to make streamflow <span class="hlt">predictions</span> that compare favorably with current multiple regression methods based on mountain snow surveys. This method has the added advantages of <span class="hlt">predicting</span> the space and time distributions of storage and summer runoff.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016HESS...20.4775N','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016HESS...20.4775N"><span>The evolution of root-zone moisture capacities after deforestation: a step towards <span class="hlt">hydrological</span> <span class="hlt">predictions</span> under change?</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Nijzink, Remko; Hutton, Christopher; Pechlivanidis, Ilias; Capell, René; Arheimer, Berit; Freer, Jim; Han, Dawei; Wagener, Thorsten; McGuire, Kevin; Savenije, Hubert; Hrachowitz, Markus</p> <p>2016-12-01</p> <p>The core component of many <span class="hlt">hydrological</span> systems, the moisture storage capacity available to vegetation, is impossible to observe directly at the catchment scale and is typically treated as a calibration parameter or obtained from a priori available soil characteristics combined with estimates of rooting depth. Often this parameter is considered to remain constant in time. Using long-term data (30-40 years) from three experimental catchments that underwent significant land cover change, we tested the hypotheses that: (1) the root-zone storage capacity significantly changes after deforestation, (2) changes in the root-zone storage capacity can to a large extent explain post-treatment changes to the <span class="hlt">hydrological</span> regimes and that (3) a time-dynamic formulation of the root-zone storage can improve the performance of a <span class="hlt">hydrological</span> model.A recently introduced method to estimate catchment-scale root-zone storage capacities based on climate data (i.e. observed rainfall and an estimate of transpiration) was used to reproduce the temporal evolution of root-zone storage capacity under change. Briefly, the maximum deficit that arises from the difference between cumulative daily precipitation and transpiration can be considered as a proxy for root-zone storage capacity. This value was compared to the value obtained from four different conceptual <span class="hlt">hydrological</span> models that were calibrated for consecutive 2-year windows.It was found that water-balance-derived root-zone storage capacities were similar to the values obtained from calibration of the <span class="hlt">hydrological</span> models. A sharp decline in root-zone storage capacity was observed after deforestation, followed by a gradual recovery, for two of the three catchments. Trend analysis suggested <span class="hlt">hydrological</span> recovery periods between 5 and 13 years after deforestation. In a proof-of-concept analysis, one of the <span class="hlt">hydrological</span> models was adapted to allow dynamically changing root-zone storage capacities, following the observed changes due to</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29726210','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29726210"><span>[Gene method for inconsistent <span class="hlt">hydrological</span> frequency calculation. 2: Diagnosis system of <span class="hlt">hydrological</span> genes and method of <span class="hlt">hydrological</span> moment genes with inconsistent characters].</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Xie, Ping; Zhao, Jiang Yan; Wu, Zi Yi; Sang, Yan Fang; Chen, Jie; Li, Bin Bin; Gu, Hai Ting</p> <p>2018-04-01</p> <p>The analysis of inconsistent <span class="hlt">hydrological</span> series is one of the major problems that should be solved for engineering <span class="hlt">hydrological</span> calculation in changing environment. In this study, the diffe-rences of non-consistency and non-stationarity were analyzed from the perspective of composition of <span class="hlt">hydrological</span> series. The inconsistent <span class="hlt">hydrological</span> phenomena were generalized into <span class="hlt">hydrological</span> processes with inheritance, variability and evolution characteristics or regulations. Furthermore, the <span class="hlt">hydrological</span> genes were identified following the theory of biological genes, while their inheritance bases and variability bases were determined based on composition of <span class="hlt">hydrological</span> series under diffe-rent time scales. To identify and test the components of <span class="hlt">hydrological</span> genes, we constructed a diagnosis system of <span class="hlt">hydrological</span> genes. With the P-3 distribution as an example, we described the process of construction and expression of the moment genes to illustrate the inheritance, variability and evolution principles of <span class="hlt">hydrological</span> genes. With the annual minimum 1-month runoff series of Yunjinghong station in Lancangjiang River basin as an example, we verified the feasibility and practicability of <span class="hlt">hydrological</span> gene theory for the calculation of inconsistent <span class="hlt">hydrological</span> frequency. The results showed that the method could be used to reveal the evolution of inconsistent <span class="hlt">hydrological</span> series. Therefore, it provided a new research pathway for engineering <span class="hlt">hydrological</span> calculation in changing environment and an essential reference for the assessment of water security.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017EGUGA..19.6504W','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017EGUGA..19.6504W"><span>Some thoughts on building, evaluating and constraining <span class="hlt">hydrologic</span> models from catchment to continental scales</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Wagener, Thorsten</p> <p>2017-04-01</p> <p>We increasingly build and apply <span class="hlt">hydrologic</span> models that simulate systems beyond the catchment scale. Such models run at regional, national or even continental scales. They therefore offer opportunities for new scientific insights, for example by enabling comparative <span class="hlt">hydrology</span> or connectivity studies, and for water management, where we might better understand changes to water resources from larger scale activities like agriculture or from hazards such as droughts. However, these models also require us to rethink how we build and evaluate them given that some of the unsolved problems from the catchment scale have not gone away. So what role should such models play in scientific <span class="hlt">advancement</span> in <span class="hlt">hydrology</span>? What problems do we still have to resolve before they can fulfill their role? What opportunities for solving these problems are there, but have not yet been utilized? I will provide some thoughts on these issues in the context of the IAHS Panta Rhei initiative and the scientific challenges it has set out for <span class="hlt">hydrology</span> (Montanari et al., 2013, <span class="hlt">Hydrological</span> Sciences Journal; McMillan et al., 2016, <span class="hlt">Hydrological</span> Sciences Journal).</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2009AGUFMED23A0532M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2009AGUFMED23A0532M"><span>DEVELOPMENT OF <span class="hlt">HYDROLOGICAL</span> EDUCATION IN UKRAINE</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Manukalo, V.</p> <p>2009-12-01</p> <p>In order to protect water from deterioration, improve water-environmental quality require the use of <span class="hlt">advanced</span> science and technology, sufficient investment and appropriate management. All of these need effective and efficient education in different components of <span class="hlt">hydrology</span>. The <span class="hlt">hydrological</span> education is part of the national water - related activities in Ukraine. The needs in the quality of <span class="hlt">hydrological</span> education will increase with introduction of new ideas and techniques into practices of water resources planners and managers. The environmentally oriented water resources development, the climate change impact on waters have to be tackled worldwide by well trained engineers and scientist relying on modern technology. Ukraine has more than 70 years of experience in the training of hydrologists. At the present hydrologists of B.Sc., M. Sc. and Ph D levels are trained at the Odesa State Environmental University (on the engineering basis) and at the Faculty of Geography of the Kyiv National University (on the geographical basis). The total duration of B.Sc. training is 4 years and M.Sc. - 5 years. The Geographical training of hydrologists at the Kyiv National University provides deeper understanding of natural processes in rivers, lakes and reservoirs, to view them in geographical complex with other physiogeographical phenomena. For this purpose students study geology, geomorphology, biology, meteorology, soil science, physical geography etc. The graduate hydrologists work in the organizations of the State Hydrometeorological Service, the State Committee for Water Management, the Academy of Sciences, others governmental and private organizations. The requirements for hydrologists of all these organizations are different in context and scope. This leads to the conclusion that a level of training of hydrologists should have a wide-scope in education. This is achieved by the university-wide fundamental and general geographic training at the first 2 years and orientation on</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017WRR....53.9368H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017WRR....53.9368H"><span>The Rangeland <span class="hlt">Hydrology</span> and Erosion Model: A Dynamic Approach for <span class="hlt">Predicting</span> Soil Loss on Rangelands</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Hernandez, Mariano; Nearing, Mark A.; Al-Hamdan, Osama Z.; Pierson, Frederick B.; Armendariz, Gerardo; Weltz, Mark A.; Spaeth, Kenneth E.; Williams, C. Jason; Nouwakpo, Sayjro K.; Goodrich, David C.; Unkrich, Carl L.; Nichols, Mary H.; Holifield Collins, Chandra D.</p> <p>2017-11-01</p> <p>In this study, we present the improved Rangeland <span class="hlt">Hydrology</span> and Erosion Model (RHEM V2.3), a process-based erosion <span class="hlt">prediction</span> tool specific for rangeland application. The article provides the mathematical formulation of the model and parameter estimation equations. Model performance is assessed against data collected from 23 runoff and sediment events in a shrub-dominated semiarid watershed in Arizona, USA. To evaluate the model, two sets of primary model parameters were determined using the RHEM V2.3 and RHEM V1.0 parameter estimation equations. Testing of the parameters indicated that RHEM V2.3 parameter estimation equations provided a 76% improvement over RHEM V1.0 parameter estimation equations. Second, the RHEM V2.3 model was calibrated to measurements from the watershed. The parameters estimated by the new equations were within the lowest and highest values of the calibrated parameter set. These results suggest that the new parameter estimation equations can be applied for this environment to <span class="hlt">predict</span> sediment yield at the hillslope scale. Furthermore, we also applied the RHEM V2.3 to demonstrate the response of the model as a function of foliar cover and ground cover for 124 data points across Arizona and New Mexico. The dependence of average sediment yield on surface ground cover was moderately stronger than that on foliar cover. These results demonstrate that RHEM V2.3 <span class="hlt">predicts</span> runoff volume, peak runoff, and sediment yield with sufficient accuracy for broad application to assess and manage rangeland systems.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016JGRC..121.7308S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016JGRC..121.7308S"><span>Variability, trends, and <span class="hlt">predictability</span> of seasonal sea ice retreat and <span class="hlt">advance</span> in the Chukchi Sea</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Serreze, Mark C.; Crawford, Alex D.; Stroeve, Julienne C.; Barrett, Andrew P.; Woodgate, Rebecca A.</p> <p>2016-10-01</p> <p>As assessed over the period 1979-2014, the date that sea ice retreats to the shelf break (150 m contour) of the Chukchi Sea has a linear trend of -0.7 days per year. The date of seasonal ice <span class="hlt">advance</span> back to the shelf break has a steeper trend of about +1.5 days per year, together yielding an increase in the open water period of 80 days. Based on detrended time series, we ask how interannual variability in <span class="hlt">advance</span> and retreat dates relate to various forcing parameters including radiation fluxes, temperature and wind (from numerical reanalyses), and the oceanic heat inflow through the Bering Strait (from in situ moorings). Of all variables considered, the retreat date is most strongly correlated (r ˜ 0.8) with the April through June Bering Strait heat inflow. After testing a suite of statistical linear models using several potential predictors, the best model for <span class="hlt">predicting</span> the date of retreat includes only the April through June Bering Strait heat inflow, which explains 68% of retreat date variance. The best model <span class="hlt">predicting</span> the ice <span class="hlt">advance</span> date includes the July through September inflow and the date of retreat, explaining 67% of <span class="hlt">advance</span> date variance. We address these relationships by discussing heat balances within the Chukchi Sea, and the hypothesis of oceanic heat transport triggering ocean heat uptake and ice-albedo feedback. Developing an operational <span class="hlt">prediction</span> scheme for seasonal retreat and <span class="hlt">advance</span> would require timely acquisition of Bering Strait heat inflow data. <span class="hlt">Predictability</span> will likely always be limited by the chaotic nature of atmospheric circulation patterns.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016EGUGA..18.4506K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016EGUGA..18.4506K"><span>Avenues for crowd science in <span class="hlt">Hydrology</span>.</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Koch, Julian; Stisen, Simon</p> <p>2016-04-01</p> <p>Crowd science describes research that is conducted with the participation of the general public (the crowd) and gives the opportunity to involve the crowd in research design, data collection and analysis. In various fields, scientists have already drawn on underused human resources to <span class="hlt">advance</span> research at low cost, with high transparency and large acceptance of the public due to the bottom up structure and the participatory process. Within the <span class="hlt">hydrological</span> sciences, crowd research has quite recently become more established in the form of crowd observatories to generate <span class="hlt">hydrological</span> data on water quality, precipitation or river flow. These innovative observatories complement more traditional ways of monitoring <span class="hlt">hydrological</span> data and strengthen a community-based environmental decision making. However, the full potential of crowd science lies in internet based participation of the crowd and it is not yet fully exploited in the field of <span class="hlt">Hydrology</span>. New avenues that are not primarily based on the outsourcing of labor, but instead capitalize the full potential of human capabilities have to emerge. In multiple realms of solving complex problems, like image detection, optimization tasks, narrowing of possible solutions, humans still remain more effective than computer algorithms. The most successful online crowd science projects Foldit and Galaxy Zoo have proven that the collective of tens of thousands users could clearly outperform traditional computer based science approaches. Our study takes advantage of the well trained human perception to conduct a spatial sensitivity analysis of land-surface variables of a distributed <span class="hlt">hydrological</span> model to identify the most sensitive spatial inputs. True spatial performance metrics, that quantitatively compare patterns, are not trivial to choose and their applicability is often not universal. On the other hand humans can quickly integrate spatial information at various scales and are therefore a trusted competence. We selected</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018JHyd..556...39H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018JHyd..556...39H"><span>Evaluating the role of evapotranspiration remote sensing data in improving <span class="hlt">hydrological</span> modeling <span class="hlt">predictability</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Herman, Matthew R.; Nejadhashemi, A. Pouyan; Abouali, Mohammad; Hernandez-Suarez, Juan Sebastian; Daneshvar, Fariborz; Zhang, Zhen; Anderson, Martha C.; Sadeghi, Ali M.; Hain, Christopher R.; Sharifi, Amirreza</p> <p>2018-01-01</p> <p>As the global demands for the use of freshwater resources continues to rise, it has become increasingly important to insure the sustainability of this resources. This is accomplished through the use of management strategies that often utilize monitoring and the use of <span class="hlt">hydrological</span> models. However, monitoring at large scales is not feasible and therefore model applications are becoming challenging, especially when spatially distributed datasets, such as evapotranspiration, are needed to understand the model performances. Due to these limitations, most of the <span class="hlt">hydrological</span> models are only calibrated for data obtained from site/point observations, such as streamflow. Therefore, the main focus of this paper is to examine whether the incorporation of remotely sensed and spatially distributed datasets can improve the overall performance of the model. In this study, actual evapotranspiration (ETa) data was obtained from the two different sets of satellite based remote sensing data. One dataset estimates ETa based on the Simplified Surface Energy Balance (SSEBop) model while the other one estimates ETa based on the Atmosphere-Land Exchange Inverse (ALEXI) model. The <span class="hlt">hydrological</span> model used in this study is the Soil and Water Assessment Tool (SWAT), which was calibrated against spatially distributed ETa and single point streamflow records for the Honeyoey Creek-Pine Creek Watershed, located in Michigan, USA. Two different techniques, multi-variable and genetic algorithm, were used to calibrate the SWAT model. Using the aforementioned datasets, the performance of the <span class="hlt">hydrological</span> model in estimating ETa was improved using both calibration techniques by achieving Nash-Sutcliffe efficiency (NSE) values >0.5 (0.73-0.85), percent bias (PBIAS) values within ±25% (±21.73%), and root mean squared error - observations standard deviation ratio (RSR) values <0.7 (0.39-0.52). However, the genetic algorithm technique was more effective with the ETa calibration while significantly</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2005AGUFM.H54B..07B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2005AGUFM.H54B..07B"><span>Automatic Calibration of a Semi-Distributed <span class="hlt">Hydrologic</span> Model Using Particle Swarm Optimization</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Bekele, E. G.; Nicklow, J. W.</p> <p>2005-12-01</p> <p><span class="hlt">Hydrologic</span> simulation models need to be calibrated and validated before using them for operational <span class="hlt">predictions</span>. Spatially-distributed <span class="hlt">hydrologic</span> models generally have a large number of parameters to capture the various physical characteristics of a <span class="hlt">hydrologic</span> system. Manual calibration of such models is a very tedious and daunting task, and its success depends on the subjective assessment of a particular modeler, which includes knowledge of the basic approaches and interactions in the model. In order to alleviate these shortcomings, an automatic calibration model, which employs an evolutionary optimization technique known as Particle Swarm Optimizer (PSO) for parameter estimation, is developed. PSO is a heuristic search algorithm that is inspired by social behavior of bird flocking or fish schooling. The newly-developed calibration model is integrated to the U.S. Department of Agriculture's Soil and Water Assessment Tool (SWAT). SWAT is a physically-based, semi-distributed <span class="hlt">hydrologic</span> model that was developed to <span class="hlt">predict</span> the long term impacts of land management practices on water, sediment and agricultural chemical yields in large complex watersheds with varying soils, land use, and management conditions. SWAT was calibrated for streamflow and sediment concentration. The calibration process involves parameter specification, whereby sensitive model parameters are identified, and parameter estimation. In order to reduce the number of parameters to be calibrated, parameterization was performed. The methodology is applied to a demonstration watershed known as Big Creek, which is located in southern Illinois. Application results show the effectiveness of the approach and model <span class="hlt">predictions</span> are significantly improved.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFM.H23H1676S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFM.H23H1676S"><span>A toolkit for determining historical eco-<span class="hlt">hydrological</span> interactions</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Singer, M. B.; Sargeant, C. I.; Evans, C. M.; Vallet-Coulomb, C.</p> <p>2016-12-01</p> <p>Contemporary climate change is <span class="hlt">predicted</span> to result in perturbations to hydroclimatic regimes across the globe, with some regions forecast to become warmer and drier. Given that water is a primary determinant of vegetative health and productivity, we can expect shifts in the availability of this critical resource to have significant impacts on forested ecosystems. The subject is particularly complex in environments where multiple sources of water are potentially available to vegetation and which may also exhibit spatial and temporal variability. To anticipate how subsurface <span class="hlt">hydrological</span> partitioning may evolve in the future and impact overlying vegetation, we require well constrained, historical data and a modelling framework for assessing the dynamics of subsurface <span class="hlt">hydrology</span>. We outline a toolkit to retrospectively investigate dynamic water use by trees. We describe a synergistic approach, which combines isotope dendrochronology of tree ring cellulose with a biomechanical model, detailed climatic and isotopic data in endmember waters to assess the mean isotopic composition of source water used in annual tree rings. We identify the data requirements and suggest three versions of the toolkit based on data availability. We present sensitivity analyses in order to identify the key variables required to constrain model <span class="hlt">predictions</span> and then develop empirical relationships for constraining these parameters based on climate records. We demonstrate our methodology within a Mediterranean riparian forest site and show how it can be used along with subsurface <span class="hlt">hydrological</span> modelling to validate source water determinations, which are fundamental to understanding climatic fluctuations and trends in subsurface <span class="hlt">hydrology</span>. We suggest that the utility of our toolkit is applicable in riparian zones and in a range of forest environments where distinct isotopic endmembers are present.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015JHyd..529.1129W','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015JHyd..529.1129W"><span>A fractional factorial probabilistic collocation method for uncertainty propagation of <span class="hlt">hydrologic</span> model parameters in a reduced dimensional space</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Wang, S.; Huang, G. H.; Huang, W.; Fan, Y. R.; Li, Z.</p> <p>2015-10-01</p> <p>In this study, a fractional factorial probabilistic collocation method is proposed to reveal statistical significance of <span class="hlt">hydrologic</span> model parameters and their multi-level interactions affecting model outputs, facilitating uncertainty propagation in a reduced dimensional space. The proposed methodology is applied to the Xiangxi River watershed in China to demonstrate its validity and applicability, as well as its capability of revealing complex and dynamic parameter interactions. A set of reduced polynomial chaos expansions (PCEs) only with statistically significant terms can be obtained based on the results of factorial analysis of variance (ANOVA), achieving a reduction of uncertainty in <span class="hlt">hydrologic</span> <span class="hlt">predictions</span>. The <span class="hlt">predictive</span> performance of reduced PCEs is verified by comparing against standard PCEs and the Monte Carlo with Latin hypercube sampling (MC-LHS) method in terms of reliability, sharpness, and Nash-Sutcliffe efficiency (NSE). Results reveal that the reduced PCEs are able to capture <span class="hlt">hydrologic</span> behaviors of the Xiangxi River watershed, and they are efficient functional representations for propagating uncertainties in <span class="hlt">hydrologic</span> <span class="hlt">predictions</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014WRR....50.7153M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014WRR....50.7153M"><span>A significant nexus: Geographically isolated wetlands influence landscape <span class="hlt">hydrology</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>McLaughlin, Daniel L.; Kaplan, David A.; Cohen, Matthew J.</p> <p>2014-09-01</p> <p>Recent U.S. Supreme Court rulings have limited federal protections for geographically isolated wetlands (GIWs) except where a "significant nexus" to a navigable water body is demonstrated. Geographic isolation does not imply GIWs are <span class="hlt">hydrologically</span> disconnected; indeed, wetland-groundwater interactions may yield important controls on regional <span class="hlt">hydrology</span>. Differences in specific yield (Sy) between uplands and inundated GIWs drive differences in water level responses to precipitation and evapotranspiration, leading to frequent reversals in hydraulic gradients that cause GIWs to act as both groundwater sinks and sources. These reversals are <span class="hlt">predicted</span> to buffer surficial aquifer dynamics and thus base flow delivery, a process we refer to as landscape <span class="hlt">hydrologic</span> capacitance. To test this hypothesis, we connected models of soil moisture, upland water table, and wetland stage to simulate <span class="hlt">hydrology</span> of a low-relief landscape with GIWs, and explored the influences of total wetland area, individual wetland size, climate, and soil texture on water table and base flow variation. Increasing total wetland area and decreasing individual wetland size substantially decreased water table and base flow variation (e.g., reducing base flow standard deviation by as much as 50%). GIWs also decreased the frequency of extremely high and low water tables and base flow deliveries. For the same total wetland area, landscapes with fewer (i.e., larger) wetlands exhibited markedly lower <span class="hlt">hydrologic</span> capacitance than those with more (i.e., smaller) wetlands, highlighting the importance of small GIWs to regional <span class="hlt">hydrology</span>. Our results suggest that GIWs buffer dynamics of the surficial aquifer and stream base flow, providing an indirect but significant nexus to the regional <span class="hlt">hydrologic</span> system.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015WRR....51.5919B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015WRR....51.5919B"><span>Whither field <span class="hlt">hydrology</span>? The need for discovery science and outrageous <span class="hlt">hydrological</span> hypotheses</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Burt, T. P.; McDonnell, J. J.</p> <p>2015-08-01</p> <p>Field <span class="hlt">hydrology</span> is on the decline. Meanwhile, the need for new field-derived insight into the age, origin and pathway of water in the headwaters, where most runoff is generated, is more needed than ever. Water Resources Research (WRR) has included some of the most influential papers in field-based runoff process understanding, particularly in the formative years when the knowledge base was developing rapidly. Here we take advantage of this 50th anniversary of the journal to highlight a few of these important field-based papers and show how field scientists have posed strong and sometimes outrageous hypotheses—approaches so needed in an era of largely model-only research. We chronicle the decline in field work and note that it is not only the quantity of field work that is diminishing but its character is changing too: from discovery science to data collection for model parameterization. While the latter is a necessary activity, the loss of the former is a major concern if we are to <span class="hlt">advance</span> the science of watershed <span class="hlt">hydrology</span>. We outline a vision for field research to seek new fundamental understanding, new mechanistic explanations of how watershed systems work, particularly outside the regions of traditional focus.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFM.H53J..03K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFM.H53J..03K"><span>Modeling non-linear growth responses to temperature and <span class="hlt">hydrology</span> in wetland trees</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Keim, R.; Allen, S. T.</p> <p>2016-12-01</p> <p>Growth responses of wetland trees to flooding and climate variations are difficult to model because they depend on multiple, apparently interacting factors, but are a critical link in <span class="hlt">hydrological</span> control of wetland carbon budgets. To more generally understand tree growth to <span class="hlt">hydrological</span> forcing, we modeled non-linear responses of tree ring growth to flooding and climate at sub-annual time steps, using Vaganov-Shashkin response functions. We calibrated the model to six baldcypress tree-ring chronologies from two <span class="hlt">hydrologically</span> distinct sites in southern Louisiana, and tested several hypotheses of plasticity in wetlands tree responses to interacting environmental variables. The model outperformed traditional multiple linear regression. More importantly, optimized response parameters were generally similar among sites with varying <span class="hlt">hydrological</span> conditions, suggesting generality to the functions. Model forms that included interacting responses to multiple forcing factors were more effective than were single response functions, indicating the principle of a single limiting factor is not correct in wetlands and both climatic and <span class="hlt">hydrological</span> variables must be considered in <span class="hlt">predicting</span> responses to <span class="hlt">hydrological</span> or climate change.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2006AGUSM.H21C..01G','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2006AGUSM.H21C..01G"><span>Operational Precipitation <span class="hlt">prediction</span> in Support of Real-Time Flash Flood <span class="hlt">Prediction</span> and Reservoir Management</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Georgakakos, K. P.</p> <p>2006-05-01</p> <p>The presentation will outline the implementation and performance evaluation of a number of national and international projects pertaining to operational precipitation estimation and <span class="hlt">prediction</span> in the context of <span class="hlt">hydrologic</span> warning systems and reservoir management support. In all cases, uncertainty measures of the estimates and <span class="hlt">predictions</span> are an integral part of the precipitation models. Outstanding research issues whose resolution is likely to lead to improvements in the operational environment are presented. The presentation draws from the experience of the <span class="hlt">Hydrologic</span> Research Center (http://www.hrc-lab.org) prototype implementation projects at the Panama Canal, Central America, Northern California, and South-Central US. References: Carpenter, T.M, and K.P. Georgakakos, "Discretization Scale Dependencies of the Ensemble Flow Range versus Catchment Area Relationship in Distributed <span class="hlt">Hydrologic</span> Modeling," Journal of <span class="hlt">Hydrology</span>, 2006, in press. Carpenter, T.M., and K.P. Georgakakos, "Impacts of Parametric and Radar Rainfall Uncertainty on the Ensemble Streamflow Simulations of a Distributed <span class="hlt">Hydrologic</span> Model," Journal of <span class="hlt">Hydrology</span>, 298, 202-221, 2004. Georgakakos, K.P., Graham, N.E., Carpenter, T.M., Georgakakos, A.P., and H. Yao, "Integrating Climate- <span class="hlt">Hydrology</span> Forecasts and Multi-Objective Reservoir Management in Northern California," EOS, 86(12), 122,127, 2005. Georgakakos, K.P., and J.A. Sperfslage, "Operational Rainfall and Flow Forecasting for the Panama Canal Watershed," in The Rio Chagres: A Multidisciplinary Profile of a Tropical Watershed, R.S. Harmon, ed., Kluwer Academic Publishers, The Netherlands, Chapter 16, 323-334, 2005. Georgakakos, K. P., "Analytical results for operational flash flood guidance," Journal of <span class="hlt">Hydrology</span>, doi:10.1016/j.jhydrol.2005.05.009, 2005.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://cfpub.epa.gov/si/si_public_record_report.cfm?dirEntryId=248231&keyword=soil+AND+carbon+AND+climate&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=248231&keyword=soil+AND+carbon+AND+climate&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>Climate change effects on watershed <span class="hlt">hydrological</span> and biogeochemical processes</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>Projected changes in climate are widely expected to alter watershed processes. However, the extent of these changes is difficult to <span class="hlt">predict</span> because complex interactions among affected <span class="hlt">hydrological</span> and biogeochemical processes will likely play out over many decades and spatial sc...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/27879728','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/27879728"><span>Monitoring and <span class="hlt">Predicting</span> Land-use Changes and the <span class="hlt">Hydrology</span> of the Urbanized Paochiao Watershed in Taiwan Using Remote Sensing Data, Urban Growth Models and a <span class="hlt">Hydrological</span> Model.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Lin, Yu-Pin; Lin, Yun-Bin; Wang, Yen-Tan; Hong, Nien-Ming</p> <p>2008-02-04</p> <p>Monitoring and simulating urban sprawl and its effects on land-use patterns andhydrological processes in urbanized watersheds are essential in land-use and waterresourceplanning and management. This study applies a novel framework to the urbangrowth model Slope, Land use, Excluded land, Urban extent, Transportation, andHillshading (SLEUTH) and land-use change with the Conversion of Land use and itsEffects (CLUE-s) model using historical SPOT images to <span class="hlt">predict</span> urban sprawl in thePaochiao watershed in Taipei County, Taiwan. The historical and <span class="hlt">predicted</span> land-use datawas input into Patch Analyst to obtain landscape metrics. This data was also input to theGeneralized Watershed Loading Function (GWLF) model to analyze the effects of futureurban sprawl on the land-use patterns and watershed <span class="hlt">hydrology</span>. The landscape metrics ofthe historical SPOT images show that land-use patterns changed between 1990-2000. TheSLEUTH model accurately simulated historical land-use patterns and urban sprawl in thePaochiao watershed, and simulated future clustered land-use patterns (2001-2025). TheCLUE-s model also simulated land-use patterns for the same period and yielded historical trends in the metrics of land-use patterns. The land-use patterns <span class="hlt">predicted</span> by the SLEUTHand CLUE-s models show the significant impact urban sprawl will have on land-usepatterns in the Paochiao watershed. The historical and <span class="hlt">predicted</span> land-use patterns in thewatershed tended to fragment, had regular shapes and interspersion patterns, but wererelatively less isolated in 2001-2025 and less interspersed from 2005-2025 compared withland-use pattern in 1990. During the study, the variability and magnitude of hydrologicalcomponents based on the historical and <span class="hlt">predicted</span> land-use patterns were cumulativelyaffected by urban sprawl in the watershed; specifically, surface runoff increasedsignificantly by 22.0% and baseflow decreased by 18.0% during 1990-2025. The proposedapproach is an effective means of enhancing land</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013AGUFM.H43E1497K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013AGUFM.H43E1497K"><span>Lowering the Barrier for Standards-Compliant and Discoverable <span class="hlt">Hydrological</span> Data Publication</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Kadlec, J.</p> <p>2013-12-01</p> <p>The growing need for sharing and integration of <span class="hlt">hydrological</span> and climate data across multiple organizations has resulted in the development of distributed, services-based, standards-compliant <span class="hlt">hydrological</span> data management and data hosting systems. The problem with these systems is complicated set-up and deployment. Many existing systems assume that the data publisher has remote-desktop access to a locally managed server and experience with computer network setup. For corporate websites, shared web hosting services with limited root access provide an inexpensive, dynamic web presence solution using the Linux, Apache, MySQL and PHP (LAMP) software stack. In this paper, we hypothesize that a webhosting service provides an optimal, low-cost solution for <span class="hlt">hydrological</span> data hosting. We propose a software architecture of a standards-compliant, lightweight and easy-to-deploy <span class="hlt">hydrological</span> data management system that can be deployed on the majority of existing shared internet webhosting services. The architecture and design is validated by developing Hydroserver Lite: a PHP and MySQL-based <span class="hlt">hydrological</span> data hosting package that is fully standards-compliant and compatible with the Consortium of Universities for <span class="hlt">Advancement</span> of <span class="hlt">Hydrologic</span> Sciences (CUAHSI) <span class="hlt">hydrologic</span> information system. It is already being used for management of field data collection by students of the McCall Outdoor Science School in Idaho. For testing, the Hydroserver Lite software has been installed on multiple different free and low-cost webhosting sites including Godaddy, Bluehost and 000webhost. The number of steps required to set-up the server is compared with the number of steps required to set-up other standards-compliant <span class="hlt">hydrologic</span> data hosting systems including THREDDS, IstSOS and MapServer SOS.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017WRR....53.8137S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017WRR....53.8137S"><span>The Growth of <span class="hlt">Hydrological</span> Understanding: Technologies, Ideas, and Societal Needs Shape the Field</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Sivapalan, Murugesu; Blöschl, Günter</p> <p>2017-10-01</p> <p>Inspired by the work of Newton, Darwin, and Wegener, this paper tracks the drivers and dynamics that have shaped the growth of <span class="hlt">hydrological</span> understanding over the last century. On the basis of an interpretation of this history, the paper then speculates about what kind of future is in store for <span class="hlt">hydrology</span> and how we can better prepare for it. The historical narrative underpinning this analysis indicates that progress in <span class="hlt">hydrological</span> understanding is brought about by changing societal needs and technological opportunities: new ideas are generated by hydrologists through addressing societal needs with the technologies of their time. We suggest that progress in <span class="hlt">hydrological</span> understanding over the last century has expressed itself through repeated cycles of euphoria and disenchantment, which have served as stimuli for the progress. The progress, for it to happen, also needed inspirational leaders as well as a supportive scientific community that provided the backdrop to major <span class="hlt">advances</span> in the field. The paper concludes that, in a similar way to how Newton, Darwin, and Wegener conducted their research, <span class="hlt">hydrology</span> too can benefit from synthesis activities aimed at "connecting the dots."</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_16");'>16</a></li> <li><a href="#" onclick='return showDiv("page_17");'>17</a></li> <li class="active"><span>18</span></li> <li><a href="#" onclick='return showDiv("page_19");'>19</a></li> <li><a href="#" onclick='return showDiv("page_20");'>20</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_18 --> <div id="page_19" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_17");'>17</a></li> <li><a href="#" onclick='return showDiv("page_18");'>18</a></li> <li class="active"><span>19</span></li> <li><a href="#" onclick='return showDiv("page_20");'>20</a></li> <li><a href="#" onclick='return showDiv("page_21");'>21</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="361"> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/biblio/1184927-hydrological-sensitivity-global-warming-solar-geoengineering-derived-from-thermodynamic-constraints','SCIGOV-STC'); return false;" href="https://www.osti.gov/biblio/1184927-hydrological-sensitivity-global-warming-solar-geoengineering-derived-from-thermodynamic-constraints"><span>The <span class="hlt">Hydrological</span> Sensitivity to Global Warming and Solar Geoengineering Derived from Thermodynamic Constraints</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>Kleidon, Alex; Kravitz, Benjamin S.; Renner, Maik</p> <p>2015-01-16</p> <p>We derive analytic expressions of the transient response of the <span class="hlt">hydrological</span> cycle to surface warming from an extremely simple energy balance model in which turbulent heat fluxes are constrained by the thermodynamic limit of maximum power. For a given magnitude of steady-state temperature change, this approach <span class="hlt">predicts</span> the transient response as well as the steady-state change in surface energy partitioning and the <span class="hlt">hydrologic</span> cycle. We show that the transient behavior of the simple model as well as the steady state <span class="hlt">hydrological</span> sensitivities to greenhouse warming and solar geoengineering are comparable to results from simulations using highly complex models. Many ofmore » the global-scale <span class="hlt">hydrological</span> cycle changes can be understood from a surface energy balance perspective, and our thermodynamically-constrained approach provides a physically robust way of estimating global <span class="hlt">hydrological</span> changes in response to altered radiative forcing.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/27955707','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/27955707"><span>Desire for <span class="hlt">predictive</span> testing for Alzheimer's disease and impact on <span class="hlt">advance</span> care planning: a cross-sectional study.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Sheffrin, Meera; Stijacic Cenzer, Irena; Steinman, Michael A</p> <p>2016-12-13</p> <p>It is unknown whether older adults in the United States would be willing to take a test <span class="hlt">predictive</span> of future Alzheimer's disease, or whether testing would change behavior. Using a nationally representative sample, we explored who would take a free and definitive test <span class="hlt">predictive</span> of Alzheimer's disease, and examined how using such a test may impact <span class="hlt">advance</span> care planning. A cross-sectional study within the 2012 Health and Retirement Study of adults aged 65 years or older asked questions about a test <span class="hlt">predictive</span> of Alzheimer's disease (N = 874). Subjects were asked whether they would want to take a hypothetical free and definitive test <span class="hlt">predictive</span> of future Alzheimer's disease. Then, imagining they knew they would develop Alzheimer's disease, subjects rated the chance of completing <span class="hlt">advance</span> care planning activities from 0 to 100. We classified a score > 50 as being likely to complete that activity. We evaluated characteristics associated with willingness to take a test for Alzheimer's disease, and how such a test would impact completing an <span class="hlt">advance</span> directive and discussing health plans with loved ones. Overall, 75% (N = 648) of the sample would take a free and definitive test <span class="hlt">predictive</span> of Alzheimer's disease. Older adults willing to take the test had similar race and educational levels to those who would not, but were more likely to be ≤75 years old (odds ratio 0.71 (95% CI 0.53-0.94)). Imagining they knew they would develop Alzheimer's, 81% would be likely to complete an <span class="hlt">advance</span> directive, although only 15% had done so already. In this nationally representative sample, 75% of older adults would take a free and definitive test <span class="hlt">predictive</span> of Alzheimer's disease. Many participants expressed intent to increase activities of <span class="hlt">advance</span> care planning with this knowledge. This confirms high public interest in <span class="hlt">predictive</span> testing for Alzheimer's disease and suggests this may be an opportunity to engage patients in <span class="hlt">advance</span> care planning discussions.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=19850028733&hterms=propeller+noise+prediction&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D40%26Ntt%3Dpropeller%2Bnoise%2Bprediction','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=19850028733&hterms=propeller+noise+prediction&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D40%26Ntt%3Dpropeller%2Bnoise%2Bprediction"><span><span class="hlt">Predicted</span> changes in <span class="hlt">advanced</span> turboprop noise with shaft angle of attack</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Padula, S. L.; Block, P. J. W.</p> <p>1984-01-01</p> <p><span class="hlt">Advanced</span> turboprop blade designs and new propeller installation schemes motivated an effort to include unsteady loading effects in existing propeller noise <span class="hlt">prediction</span> computer programs. The present work validates the <span class="hlt">prediction</span> capability while studing the effects of shaft inclination on the radiated sound field. Classical methods of propeller performance analysis supply the time-dependent blade loading needed to calculate noise. Polar plots of the sound pressure level (SPL) of the first four harmonics and overall SPL are indicative of the change in directivity pattern as a function of propeller angle of attack. Noise <span class="hlt">predictions</span> are compared with newly available wind tunnel data and the accuracy and applicability of the <span class="hlt">prediction</span> method are discussed. It is concluded that unsteady blade loading caused by inclining the propeller with respect to the flow changes the directionality and the intensity of the radiated noise. These changes are well modeled by the present quasi-steady <span class="hlt">prediction</span> method.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=19990116524&hterms=Venkataraman&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D10%26Ntt%3DVenkataraman','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=19990116524&hterms=Venkataraman&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D10%26Ntt%3DVenkataraman"><span>Impact of the 1997-1998 El-Nino of Regional <span class="hlt">Hydrology</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Lakshmi, Venkataraman; Susskind, Joel</p> <p>1998-01-01</p> <p>The 1997-1998 El-Nino brought with it a range of severe local-regional <span class="hlt">hydrological</span> phenomena. Record high temperatures and extremely dry soil conditions in Texas is an example of this regional effect. The El-Nino and La-Nina change the continental weather patterns considerably. However, connections between continental weather anomalies and regional or local anomalies have not been established to a high degree of confidence. There are several unique features of the recent El-Nino and La-Nina. Due to the recognition of the present El-Nino well in <span class="hlt">advance</span>, there have been several coupled model studies on global and regional scales. Secondly, there is a near real-time monitoring of the situation using data from satellite sensors, namely, SeaWIFS, TOVS, AVHRR and GOES. Both observations and modeling characterize the large scale features of this El-Nino fairly well. However the connection to the local and regional <span class="hlt">hydrological</span> phenomenon still needs to be made. This paper will use satellite observations and analysis data to establish a relation between local <span class="hlt">hydrology</span> and large scale weather patterns. This will be the first step in using satellite data to perform regional <span class="hlt">hydrological</span> simulations of surface temperature and soil moisture.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015EGUGA..17.9460D','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015EGUGA..17.9460D"><span>Calibration of limited-area ensemble precipitation forecasts for <span class="hlt">hydrological</span> <span class="hlt">predictions</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Diomede, Tommaso; Marsigli, Chiara; Montani, Andrea; Nerozzi, Fabrizio; Paccagnella, Tiziana</p> <p>2015-04-01</p> <p>The main objective of this study is to investigate the impact of calibration for limited-area ensemble precipitation forecasts, to be used for driving discharge <span class="hlt">predictions</span> up to 5 days in <span class="hlt">advance</span>. A reforecast dataset, which spans 30 years, based on the Consortium for Small Scale Modeling Limited-Area Ensemble <span class="hlt">Prediction</span> System (COSMO-LEPS) was used for testing the calibration strategy. Three calibration techniques were applied: quantile-to-quantile mapping, linear regression, and analogs. The performance of these methodologies was evaluated in terms of statistical scores for the precipitation forecasts operationally provided by COSMO-LEPS in the years 2003-2007 over Germany, Switzerland, and the Emilia-Romagna region (northern Italy). The analog-based method seemed to be preferred because of its capability of correct position errors and spread deficiencies. A suitable spatial domain for the analog search can help to handle model spatial errors as systematic errors. However, the performance of the analog-based method may degrade in cases where a limited training dataset is available. A sensitivity test on the length of the training dataset over which to perform the analog search has been performed. The quantile-to-quantile mapping and linear regression methods were less effective, mainly because the forecast-analysis relation was not so strong for the available training dataset. A comparison between the calibration based on the deterministic reforecast and the calibration based on the full operational ensemble used as training dataset has been considered, with the aim to evaluate whether reforecasts are really worthy for calibration, given that their computational cost is remarkable. The verification of the calibration process was then performed by coupling ensemble precipitation forecasts with a distributed rainfall-runoff model. This test was carried out for a medium-sized catchment located in Emilia-Romagna, showing a beneficial impact of the analog</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014HESS...18.3481D','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014HESS...18.3481D"><span>Validating a spatially distributed <span class="hlt">hydrological</span> model with soil morphology data</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Doppler, T.; Honti, M.; Zihlmann, U.; Weisskopf, P.; Stamm, C.</p> <p>2014-09-01</p> <p>Spatially distributed models are popular tools in <span class="hlt">hydrology</span> claimed to be useful to support management decisions. Despite the high spatial resolution of the computed variables, calibration and validation is often carried out only on discharge time series at specific locations due to the lack of spatially distributed reference data. Because of this restriction, the <span class="hlt">predictive</span> power of these models, with regard to <span class="hlt">predicted</span> spatial patterns, can usually not be judged. An example of spatial <span class="hlt">predictions</span> in <span class="hlt">hydrology</span> is the <span class="hlt">prediction</span> of saturated areas in agricultural catchments. These areas can be important source areas for inputs of agrochemicals to the stream. We set up a spatially distributed model to <span class="hlt">predict</span> saturated areas in a 1.2 km2 catchment in Switzerland with moderate topography and artificial drainage. We translated soil morphological data available from soil maps into an estimate of the duration of soil saturation in the soil horizons. This resulted in a data set with high spatial coverage on which the model <span class="hlt">predictions</span> were validated. In general, these saturation estimates corresponded well to the measured groundwater levels. We worked with a model that would be applicable for management decisions because of its fast calculation speed and rather low data requirements. We simultaneously calibrated the model to observed groundwater levels and discharge. The model was able to reproduce the general <span class="hlt">hydrological</span> behavior of the catchment in terms of discharge and absolute groundwater levels. However, the the groundwater level <span class="hlt">predictions</span> were not accurate enough to be used for the <span class="hlt">prediction</span> of saturated areas. Groundwater level dynamics were not adequately reproduced and the <span class="hlt">predicted</span> spatial saturation patterns did not correspond to those estimated from the soil map. Our results indicate that an accurate <span class="hlt">prediction</span> of the groundwater level dynamics of the shallow groundwater in our catchment that is subject to artificial drainage would require a model that</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFM.H51B1267P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFM.H51B1267P"><span>Is there a `universal' dynamic zero-parameter <span class="hlt">hydrological</span> model? Evaluation of a dynamic Budyko model in US and India</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Patnaik, S.; Biswal, B.; Sharma, V. C.</p> <p>2017-12-01</p> <p>River flow varies greatly in space and time, and the single biggest challenge for hydrologists and ecologists around the world is the fact that most rivers are either ungauged or poorly gauged. Although it is relatively easier to <span class="hlt">predict</span> long-term average flow of a river using the `universal' zero-parameter Budyko model, lack of data hinders short-term flow <span class="hlt">prediction</span> at ungauged locations using traditional <span class="hlt">hydrological</span> models as they require observed flow data for model calibration. Flow <span class="hlt">prediction</span> in ungauged basins thus requires a dynamic 'zero-parameter' <span class="hlt">hydrological</span> model. One way to achieve this is to regionalize a dynamic <span class="hlt">hydrological</span> model's parameters. However, a regionalization method based zero-parameter dynamic <span class="hlt">hydrological</span> model is not `universal'. An alternative attempt was made recently to develop a zero-parameter dynamic model by defining an instantaneous dryness index as a function of antecedent rainfall and solar energy inputs with the help of a decay function and using the original Budyko function. The model was tested first in 63 US catchments and later in 50 Indian catchments. The median Nash-Sutcliffe efficiency (NSE) was found to be close to 0.4 in both the cases. Although improvements need to be incorporated in order to use the model for reliable <span class="hlt">prediction</span>, the main aim of this study was to rather understand <span class="hlt">hydrological</span> processes. The overall results here seem to suggest that the dynamic zero-parameter Budyko model is `universal.' In other words natural catchments around the world are strikingly similar to each other in the way they respond to <span class="hlt">hydrologic</span> inputs; we thus need to focus more on utilizing catchment similarities in <span class="hlt">hydrological</span> modelling instead of over parameterizing our models.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=20040171586&hterms=attention+span&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D60%26Ntt%3Dattention%2Bspan','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=20040171586&hterms=attention+span&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D60%26Ntt%3Dattention%2Bspan"><span>Time Changes of the European Gravity Field from GRACE: A Comparison with Ground Measurements from Superconducting Gravimeters and with <span class="hlt">Hydrology</span> Model <span class="hlt">Predictions</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Hinderer, J.; Lemoine, Frank G.; Crossley, D.; Boy, J.-P.</p> <p>2004-01-01</p> <p>We investigate the time-variable gravity changes in Europe retrieved from the initial GRACE monthly solutions spanning a 18 month duration from April 2002 to October 2003. Gravity anomaly maps are retrieved in Central Europe from the monthly satellite solutions we compare the fields according to various truncation levels (typically between degree 10 and 20) of the initial fields (expressed in spherical harmonics to degree 120). For these different degrees, an empirical orthogonal function (EOF) decomposition of the time-variable gravity field leads us to its main spatial and temporal characteristics. We show that the dominant signal is found to be annual with an amplitude and a phase both in agreement with <span class="hlt">predictions</span> in Europe modeled using snow and soil-moisture variations from recent <span class="hlt">hydrology</span> models. We compare these GRACE gravity field changes to surface gravity observations from 6 superconducting gravimeters of the GGP (Global Geodynamics Project) European sub-network, with a special attention to loading corrections. Initial results suggest that all 3 data sets (GRACE, <span class="hlt">hydrology</span> and GGP) are responding to annual changes in near-surface water in Europe of a few microGal (at length scales of approx.1000 km) that show a high value in winter and a summer minimum. We also point out that the GRACE gravity field evolution seems to indicate that there is a trend in gravity between summer 2002 and summer 2003 which can be related to the 2003 heatwave in Europe and its <span class="hlt">hydrological</span> consequences (drought). Despite the limited time span of our analysis and the uncertainties in retrieving a regional solution from the network of gravimeters, the calibration and validation aspects of the GRACE data processing based on the annual <span class="hlt">hydrology</span> cycle in Europe are in progress.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70094985','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70094985"><span><span class="hlt">Hydrology</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>Eisenbies, Mark H.; Hughes, W. Brian</p> <p>2000-01-01</p> <p><span class="hlt">Hydrologic</span> process are the main determinants of the type of wetland located on a site. Precipitation, groundwater, or flooding interact with soil properties and geomorphic setting to yield a complex matrix of conditions that control groundwater flux, water storage and discharge, water chemistry, biotic productivity, biodiversity, and biogeochemical cycling. Hydroperiod affects many abiotic factors that in turn determine plant and animal species composition, biodiversity, primary and secondary productivity, accumulation, of organic matter, and nutrient cycling. Because the <span class="hlt">hydrologic</span> regime has a major influence on wetland functioning, understanding how <span class="hlt">hydrologic</span> changes influence ecosystem processes is essential, especially in light of the pressures placed on remaining wetlands by society's demands for water resources and by potential global changes in climate.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014AGUFM.H42C..06H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014AGUFM.H42C..06H"><span>Recent <span class="hlt">advances</span> towards a theory of catchment <span class="hlt">hydrologic</span> transport: age-ranked storage and the Ω-functions</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Harman, C. J.</p> <p>2014-12-01</p> <p>Models that faithfully represent spatially-integrated <span class="hlt">hydrologic</span> transport through the critical zone at sub-watershed scales are essential building blocks for large-scale models of land use and climate controls on non-point source contaminant delivery. A particular challenge facing these models is the need to represent the delay between inputs of soluble contaminants (such as nitrate) at the field scale, and the solute load that appears in streams. Recent <span class="hlt">advances</span> in the theory of time-variable transit time distributions (e.g. Botter et al., GRL 38(L11403), 2011) have provided a rigorous framework for representing conservative solute transport and its coupling to <span class="hlt">hydrologic</span> variability and partitioning. Here I will present a reformulation of this framework that offers several distinct advantages over existing formulations: 1) the derivation of the governing conservation equation is simple and intuitive, 2) the closure relations are expressed in a convenient and physically meaningful way as probability distributions Ω(ST)Omega(S_T) over the storage ranked by age STS_T, and 3) changes in transport behavior determined by storage-dependent dilution and flow-path dynamics (as distinct from those due only to changes in the rates and partitioning of water flux) are completely encapsulated by these probability distributions. The framework has been implemented to model to the rich dataset of long-term stream and precipitation chloride from the Plynlimon watershed in Wales, UK. With suitable choices for the functional form of the closure relationships, only a small number of free parameters are required to reproduce the observed chloride dynamics as well as previous models with many more parameters, including reproducing the observed fractal 1/f filtering of the streamflow chloride variability. The modeled transport dynamics are sensitive to the input precipitation variability and water balance partitioning to evapotranspiration. Apparent storage-dependent age</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFMIN12B..02T','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFMIN12B..02T"><span>The HydroShare Collaborative Repository for the <span class="hlt">Hydrology</span> Community</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Tarboton, D. G.; Idaszak, R.; Horsburgh, J. S.; Ames, D. P.; Goodall, J. L.; Couch, A.; Hooper, R. P.; Dash, P. K.; Stealey, M.; Yi, H.; Bandaragoda, C.; Castronova, A. M.</p> <p>2017-12-01</p> <p>HydroShare is an online, collaboration system for sharing of <span class="hlt">hydrologic</span> data, analytical tools, and models. It supports the sharing of, and collaboration around, "resources" which are defined by standardized content types for data formats and models commonly used in <span class="hlt">hydrology</span>. With HydroShare you can: Share your data and models with colleagues; Manage who has access to the content that you share; Share, access, visualize and manipulate a broad set of <span class="hlt">hydrologic</span> data types and models; Use the web services application programming interface (API) to program automated and client access; Publish data and models and obtain a citable digital object identifier (DOI); Aggregate your resources into collections; Discover and access data and models published by others; Use web apps to visualize, analyze and run models on data in HydroShare. This presentation will describe the functionality and architecture of HydroShare highlighting our approach to making this system easy to use and serving the needs of the <span class="hlt">hydrology</span> community represented by the Consortium of Universities for the <span class="hlt">Advancement</span> of <span class="hlt">Hydrologic</span> Sciences, Inc. (CUAHSI). Metadata for uploaded files is harvested automatically or captured using easy to use web user interfaces. Users are encouraged to add or create resources in HydroShare early in the data life cycle. To encourage this we allow users to share and collaborate on HydroShare resources privately among individual users or groups, entering metadata while doing the work. HydroShare also provides enhanced functionality for users through web apps that provide tools and computational capability for actions on resources. HydroShare's architecture broadly is comprised of: (1) resource storage, (2) resource exploration website, and (3) web apps for actions on resources. System components are loosely coupled and interact through APIs, which enhances robustness, as components can be upgraded and <span class="hlt">advanced</span> relatively independently. The full power of this paradigm is the</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFM.C31C..07K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFM.C31C..07K"><span>Determining <span class="hlt">hydrological</span> changes in a small Arctic treeline basin using cold regions <span class="hlt">hydrological</span> modelling and a pseudo-global warming approach</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Krogh, S. A.; Pomeroy, J. W.</p> <p>2017-12-01</p> <p>Increasing temperatures are producing higher rainfall ratios, shorter snow-covered periods, permafrost thaw, more shrub coverage, more northerly treelines and greater interaction between groundwater and surface flow in Arctic basins. How these changes will impact the <span class="hlt">hydrology</span> of the Arctic treeline environment represents a great challenge. To diagnose the future <span class="hlt">hydrology</span> along the current Arctic treeline, a physically based cold regions model was used to simulate the <span class="hlt">hydrology</span> of a small basin near Inuvik, Northwest Territories, Canada. The <span class="hlt">hydrological</span> model includes <span class="hlt">hydrological</span> processes such as snow redistribution and sublimation by wind, canopy interception of snow/rain and sublimation/evaporation, snowmelt energy balance, active layer freeze/thaw, infiltration into frozen and unfrozen soils, evapotranspiration, horizontal flow through organic terrain and snowpack, subsurface flow and streamflow routing. The model was driven with weather simulated by a high-resolution (4 km) numerical weather <span class="hlt">prediction</span> model under two scenarios: (1) control run, using ERA-Interim boundary conditions (2001-2013) and (2) future, using a Pseudo-Global Warming (PGW) approach based on the RCP8.5 projections perturbing the control run. Transient changes in vegetation based on recent observations and ecological expectations were then used to re-parameterise the model. Historical <span class="hlt">hydrological</span> simulations were validated against daily streamflow, snow water equivalent and active layer thickness records, showing the model's suitability in this environment. Strong annual warming ( 6 °C) and more precipitation ( 20%) were simulated by the PGW scenario, with winter precipitation and fall temperature showing the largest seasonal increase. The joint impact of climate and transient vegetation changes on snow accumulation and redistribution, evapotranspiration, active layer development, runoff generation and hydrograph characteristics are analyzed and discussed.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5102348','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5102348"><span>Climate Change Impacts on the Upper Indus <span class="hlt">Hydrology</span>: Sources, Shifts and Extremes</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Immerzeel, W. W.; Kraaijenbrink, P. D. A.; Shrestha, A. B.; Bierkens, M. F. P.</p> <p>2016-01-01</p> <p>The Indus basin heavily depends on its upstream mountainous part for the downstream supply of water while downstream demands are high. Since downstream demands will likely continue to increase, accurate <span class="hlt">hydrological</span> projections for the future supply are important. We use an ensemble of statistically downscaled CMIP5 General Circulation Model outputs for RCP4.5 and RCP8.5 to force a cryospheric-<span class="hlt">hydrological</span> model and generate transient <span class="hlt">hydrological</span> projections for the entire 21st century for the upper Indus basin. Three methodological <span class="hlt">advances</span> are introduced: (i) A new precipitation dataset that corrects for the underestimation of high-altitude precipitation is used. (ii) The model is calibrated using data on river runoff, snow cover and geodetic glacier mass balance. (iii) An <span class="hlt">advanced</span> statistical downscaling technique is used that accounts for changes in precipitation extremes. The analysis of the results focuses on changes in sources of runoff, seasonality and <span class="hlt">hydrological</span> extremes. We conclude that the future of the upper Indus basin’s water availability is highly uncertain in the long run, mainly due to the large spread in the future precipitation projections. Despite large uncertainties in the future climate and long-term water availability, basin-wide patterns and trends of seasonal shifts in water availability are consistent across climate change scenarios. Most prominent is the attenuation of the annual hydrograph and shift from summer peak flow towards the other seasons for most ensemble members. In addition there are distinct spatial patterns in the response that relate to monsoon influence and the importance of meltwater. Analysis of future <span class="hlt">hydrological</span> extremes reveals that increases in intensity and frequency of extreme discharges are very likely for most of the upper Indus basin and most ensemble members. PMID:27828994</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/27828994','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/27828994"><span>Climate Change Impacts on the Upper Indus <span class="hlt">Hydrology</span>: Sources, Shifts and Extremes.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Lutz, A F; Immerzeel, W W; Kraaijenbrink, P D A; Shrestha, A B; Bierkens, M F P</p> <p>2016-01-01</p> <p>The Indus basin heavily depends on its upstream mountainous part for the downstream supply of water while downstream demands are high. Since downstream demands will likely continue to increase, accurate <span class="hlt">hydrological</span> projections for the future supply are important. We use an ensemble of statistically downscaled CMIP5 General Circulation Model outputs for RCP4.5 and RCP8.5 to force a cryospheric-<span class="hlt">hydrological</span> model and generate transient <span class="hlt">hydrological</span> projections for the entire 21st century for the upper Indus basin. Three methodological <span class="hlt">advances</span> are introduced: (i) A new precipitation dataset that corrects for the underestimation of high-altitude precipitation is used. (ii) The model is calibrated using data on river runoff, snow cover and geodetic glacier mass balance. (iii) An <span class="hlt">advanced</span> statistical downscaling technique is used that accounts for changes in precipitation extremes. The analysis of the results focuses on changes in sources of runoff, seasonality and <span class="hlt">hydrological</span> extremes. We conclude that the future of the upper Indus basin's water availability is highly uncertain in the long run, mainly due to the large spread in the future precipitation projections. Despite large uncertainties in the future climate and long-term water availability, basin-wide patterns and trends of seasonal shifts in water availability are consistent across climate change scenarios. Most prominent is the attenuation of the annual hydrograph and shift from summer peak flow towards the other seasons for most ensemble members. In addition there are distinct spatial patterns in the response that relate to monsoon influence and the importance of meltwater. Analysis of future <span class="hlt">hydrological</span> extremes reveals that increases in intensity and frequency of extreme discharges are very likely for most of the upper Indus basin and most ensemble members.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2008AGUFM.H11F0832B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2008AGUFM.H11F0832B"><span>Dam Dynamics in the Colonial Northeast and Chesapeake: <span class="hlt">Hydrologic</span> Implications</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Bain, D. J.; Salant, N. L.; Brandt, S. L.</p> <p>2008-12-01</p> <p>Recent work has highlighted the widespread presence of low-head dams for power generation during the 19th century. However, this work largely depends on census numbers tabulated in the mid-1800s, over 200 years after European activity began in North America. In order to compare the <span class="hlt">hydrologic</span> implications of colonial era low-head dam construction with the impacts of other simultaneous processes (e.g., expatriation of the beaver or forest clearance), we have compiled historical data on mills to reconstruct the temporal and spatial dynamics of low-head dam construction in the colonial northeastern United States (i.e., Virginia to Maine). This reconstruction, combined with the results of related work on beaver pond dynamics and deforestation, provides several insights into the distribution and impacts of human impoundments during this period. While the resulting <span class="hlt">hydrologic</span> changes are large, the addition of human dams to the system seems to be minimally offset and less important than changes arising from the expatriation of the beaver or the removal of trees during this early period. In addition, the spatial patterns of dam construction are complex, making <span class="hlt">prediction</span> of <span class="hlt">hydrologic</span> and associated responses more difficult to <span class="hlt">predict</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29720601','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29720601"><span>An approach to quantum-computational <span class="hlt">hydrologic</span> inverse analysis.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>O'Malley, Daniel</p> <p>2018-05-02</p> <p>Making <span class="hlt">predictions</span> about flow and transport in an aquifer requires knowledge of the heterogeneous properties of the aquifer such as permeability. Computational methods for inverse analysis are commonly used to infer these properties from quantities that are more readily observable such as hydraulic head. We present a method for computational inverse analysis that utilizes a type of quantum computer called a quantum annealer. While quantum computing is in an early stage compared to classical computing, we demonstrate that it is sufficiently developed that it can be used to solve certain subsurface flow problems. We utilize a D-Wave 2X quantum annealer to solve 1D and 2D <span class="hlt">hydrologic</span> inverse problems that, while small by modern standards, are similar in size and sometimes larger than <span class="hlt">hydrologic</span> inverse problems that were solved with early classical computers. Our results and the rapid progress being made with quantum computing hardware indicate that the era of quantum-computational <span class="hlt">hydrology</span> may not be too far in the future.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=20000032349&hterms=usle+soil&qs=N%3D0%26Ntk%3DAll%26Ntx%3Dmode%2Bmatchall%26Ntt%3Dusle%2Bsoil','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=20000032349&hterms=usle+soil&qs=N%3D0%26Ntk%3DAll%26Ntx%3Dmode%2Bmatchall%26Ntt%3Dusle%2Bsoil"><span>Development of a Coupled <span class="hlt">Hydrological</span>/Sediment Yield Model for a Watershed at Regional Level</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Rajbhandaril, Narayan; Crosson, William; Tsegaye, Teferi; Coleman, Tommy; Liu, Yaping; Soman, Vishwas</p> <p>1998-01-01</p> <p>Development of a <span class="hlt">hydrologic</span> model for the study of environmental conservation requires a comprehensive understanding of individual-storm affecting <span class="hlt">hydrologic</span> and sedimentologic processes. The <span class="hlt">hydrologic</span> models that we are currently coupling are the Simulator for <span class="hlt">Hydrology</span> and Energy Exchange at the Land Surface (SHEELS) and the Distributed Runoff Model (DRUM). SHEELS runs continuously to estimate surface energy fluxes and sub-surface soil water fluxes, while DRUM operates during and following precipitation events to <span class="hlt">predict</span> surface runoff and peak flow through channel routing. The lateral re-distribution of surface water determined by DRUM is passed to SHEELS, which then adjusts soil water contents throughout the profile. The model SHEELS is well documented in Smith et al. (1993) and Laymen and Crosson (1995). The model DRUM is well documented in Vieux et al. (1990) and Vieux and Gauer (1994). The coupled <span class="hlt">hydrologic</span> model, SHEELS/DRUM, does not simulate sedimentologic processes. The simulation of the sedimentologic process is important for environmental conservation planning and management. Therefore, we attempted to develop a conceptual frame work for coupling a sediment yield model with SHEELS/DRUM to estimate individual-storm sediment yield from a watershed at a regional level. The sediment yield model that will be used for this study is the Universal Soil Loss Equation (USLE) with some modifications to enable the model to <span class="hlt">predict</span> individual-storm sediment yield. The <span class="hlt">predicted</span> sediment yield does not include wind erosion and erosion caused by irrigation and snow melt. Units used for this study are those given by Foster et al. (1981) for SI units.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014AGUFM.C41D..04P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014AGUFM.C41D..04P"><span>Correcting Inadequate Model Snow Process Descriptions Dramatically Improves Mountain <span class="hlt">Hydrology</span> Simulations</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Pomeroy, J. W.; Fang, X.</p> <p>2014-12-01</p> <p>The vast effort in <span class="hlt">hydrology</span> devoted to parameter calibration as a means to improve model performance assumes that the models concerned are not fundamentally wrong. By focussing on finding optimal parameter sets and ascribing poor model performance to parameter or data uncertainty, these efforts may fail to consider the need to improve models with more intelligent descriptions of <span class="hlt">hydrological</span> processes. To test this hypothesis, a flexible physically based <span class="hlt">hydrological</span> model including a full suite of snow <span class="hlt">hydrology</span> processes as well as warm season, hillslope and groundwater <span class="hlt">hydrology</span> was applied to Marmot Creek Research Basin, Canadian Rocky Mountains where excellent driving meteorology and basin biophysical descriptions exist. Model parameters were set from values found in the basin or from similar environments; no parameters were calibrated. The model was tested against snow surveys and streamflow observations. The model used algorithms that describe snow redistribution, sublimation and forest canopy effects on snowmelt and evaporative processes that are rarely implemented in <span class="hlt">hydrological</span> models. To investigate the contribution of these processes to model <span class="hlt">predictive</span> capability, the model was "falsified" by deleting parameterisations for forest canopy snow mass and energy, blowing snow, intercepted rain evaporation, and sublimation. Model falsification by ignoring forest canopy processes contributed to a large increase in SWE errors for forested portions of the research basin with RMSE increasing from 19 to 55 mm and mean bias (MB) increasing from 0.004 to 0.62. In the alpine tundra portion, removing blowing processes resulted in an increase in model SWE MB from 0.04 to 2.55 on north-facing slopes and -0.006 to -0.48 on south-facing slopes. Eliminating these algorithms degraded streamflow <span class="hlt">prediction</span> with the Nash Sutcliffe efficiency dropping from 0.58 to 0.22 and MB increasing from 0.01 to 0.09. These results show dramatic model improvements by including snow</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.ars.usda.gov/research/publications/publication/?seqNo115=283836','TEKTRAN'); return false;" href="http://www.ars.usda.gov/research/publications/publication/?seqNo115=283836"><span>Introduction to <span class="hlt">hydrology</span></span></a></p> <p><a target="_blank" href="https://www.ars.usda.gov/research/publications/find-a-publication/">USDA-ARS?s Scientific Manuscript database</a></p> <p></p> <p></p> <p><span class="hlt">Hydrology</span> deals with the occurrence, movement, and storage of water in the Earth system. <span class="hlt">Hydrologic</span> science comprises understanding the underlying physical and stochastic processes involved and estimating the quantity and quality of water in the various phases and stores. The study of <span class="hlt">hydrology</span> als...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://cfpub.epa.gov/si/si_public_record_report.cfm?dirEntryId=277755&keyword=geology&actType=&TIMSType=+&TIMSSubTypeID=&DEID=&epaNumber=&ntisID=&archiveStatus=Both&ombCat=Any&dateBeginCreated=&dateEndCreated=&dateBeginPublishedPresented=&dateEndPublishedPresented=&dateBeginUpdated=&dateEndUpdated=&dateBeginCompleted=&dateEndCompleted=&personID=&role=Any&journalID=&publisherID=&sortBy=revisionDate&count=50','EPA-EIMS'); return false;" href="https://cfpub.epa.gov/si/si_public_record_report.cfm?dirEntryId=277755&keyword=geology&actType=&TIMSType=+&TIMSSubTypeID=&DEID=&epaNumber=&ntisID=&archiveStatus=Both&ombCat=Any&dateBeginCreated=&dateEndCreated=&dateBeginPublishedPresented=&dateEndPublishedPresented=&dateBeginUpdated=&dateEndUpdated=&dateBeginCompleted=&dateEndCompleted=&personID=&role=Any&journalID=&publisherID=&sortBy=revisionDate&count=50"><span>How does spatial variability of climate affect catchment streamflow <span class="hlt">predictions</span>?</span></a></p> <p><a target="_blank" href="http://oaspub.epa.gov/eims/query.page">EPA Science Inventory</a></p> <p></p> <p></p> <p>Spatial variability of climate can negatively affect catchment streamflow <span class="hlt">predictions</span> if it is not explicitly accounted for in <span class="hlt">hydrologic</span> models. In this paper, we examine the changes in streamflow <span class="hlt">predictability</span> when a <span class="hlt">hydrologic</span> model is run with spatially variable (distribute...</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://adsabs.harvard.edu/abs/2017EGUGA..1919009P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017EGUGA..1919009P"><span>Network analysis applications in <span class="hlt">hydrology</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Price, Katie</p> <p>2017-04-01</p> <p>Applied network theory has seen pronounced expansion in recent years, in fields such as epidemiology, computer science, and sociology. Concurrent development of analytical methods and frameworks has increased possibilities and tools available to researchers seeking to apply network theory to a variety of problems. While water and nutrient fluxes through stream systems clearly demonstrate a directional network structure, the <span class="hlt">hydrological</span> applications of network theory remain under­explored. This presentation covers a review of network applications in <span class="hlt">hydrology</span>, followed by an overview of promising network analytical tools that potentially offer new insights into conceptual modeling of <span class="hlt">hydrologic</span> systems, identifying behavioral transition zones in stream networks and thresholds of dynamical system response. Network applications were tested along an urbanization gradient in Atlanta, Georgia, USA. Peachtree Creek and Proctor Creek. Peachtree Creek contains a nest of five long­term USGS streamflow and water quality gages, allowing network application of long­term flow statistics. The watershed spans a range of suburban and heavily urbanized conditions. Summary flow statistics and water quality metrics were analyzed using a suite of network analysis techniques, to test the conceptual modeling and <span class="hlt">predictive</span> potential of the methodologies. Storm events and low flow dynamics during Summer 2016 were analyzed using multiple network approaches, with an emphasis on tomogravity methods. Results indicate that network theory approaches offer novel perspectives for understanding long­ term and event­based <span class="hlt">hydrological</span> data. Key future directions for network applications include 1) optimizing data collection, 2) identifying "hotspots" of contaminant and overland flow influx to stream systems, 3) defining process domains, and 4) analyzing dynamic connectivity of various system components, including groundwater­surface water interactions.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFM.H23C1665S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFM.H23C1665S"><span>Diagnosing the impact of alternative calibration strategies on coupled <span class="hlt">hydrologic</span> models</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Smith, T. J.; Perera, C.; Corrigan, C.</p> <p>2017-12-01</p> <p><span class="hlt">Hydrologic</span> models represent a significant tool for understanding, <span class="hlt">predicting</span>, and responding to the impacts of water on society and society on water resources and, as such, are used extensively in water resources planning and management. Given this important role, the validity and fidelity of <span class="hlt">hydrologic</span> models is imperative. While extensive focus has been paid to improving <span class="hlt">hydrologic</span> models through better process representation, better parameter estimation, and better uncertainty quantification, significant challenges remain. In this study, we explore a number of competing model calibration scenarios for simple, coupled snowmelt-runoff models to better understand the sensitivity / variability of parameterizations and its impact on model performance, robustness, fidelity, and transferability. Our analysis highlights the sensitivity of coupled snowmelt-runoff model parameterizations to alterations in calibration approach, underscores the concept of information content in <span class="hlt">hydrologic</span> modeling, and provides insight into potential strategies for improving model robustness / fidelity.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.usgs.gov/sir/2009/5049/pdf/Kepner.pdf','USGSPUBS'); return false;" href="https://pubs.usgs.gov/sir/2009/5049/pdf/Kepner.pdf"><span>Evaluating <span class="hlt">hydrological</span> response to forecasted land-use change—scenario testing with the automated geospatial watershed assessment (AGWA) tool</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Kepner, William G.; Semmens, Darius J.; Hernandez, Mariano; Goodrich, David C.</p> <p>2009-01-01</p> <p>Envisioning and evaluating future scenarios has emerged as a critical component of both science and social decision-making. The ability to assess, report, map, and forecast the life support functions of ecosystems is absolutely critical to our capacity to make informed decisions to maintain the sustainable nature of our ecosystem services now and into the future. During the past two decades, important <span class="hlt">advances</span> in the integration of remote imagery, computer processing, and spatial-analysis technologies have been used to develop landscape information that can be integrated with <span class="hlt">hydrologic</span> models to determine long-term change and make <span class="hlt">predictive</span> inferences about the future. Two diverse case studies in northwest Oregon (Willamette River basin) and southeastern Arizona (San Pedro River) were examined in regard to future land use scenarios relative to their impact on surface water conditions (e.g., sediment yield and surface runoff) using <span class="hlt">hydrologic</span> models associated with the Automated Geospatial Watershed Assessment (AGWA) tool. The base reference grid for land cover was modified in both study locations to reflect stakeholder preferences 20 to 60 yrs into the future, and the consequences of landscape change were evaluated relative to the selected future scenarios. The two studies provide examples of integrating <span class="hlt">hydrologic</span> modeling with a scenario analysis framework to evaluate plausible future forecasts and to understand the potential impact of landscape change on ecosystem services.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2005AGUFM.H41D0449M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2005AGUFM.H41D0449M"><span>Characteristics and Impact of Imperviousness From a GIS-based <span class="hlt">Hydrological</span> Perspective</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Moglen, G. E.; Kim, S.</p> <p>2005-12-01</p> <p>With the concern that imperviousness can be differently quantified depending on data sources and methods, this study assessed imperviousness estimates using two different data sources: land use and land cover. Year 2000 land use developed by the Maryland Department of Planning was utilized to estimate imperviousness by assigning imperviousness coefficients to unique land use categories. These estimates were compared with imperviousness estimates based on satellite-derived land cover from the 2001 National Land Cover Dataset. Our study developed the relationships between these two estimates in the form of regression equations to convert imperviousness derived from one data source to the other. The regression equations are considered reliable, based on goodness-of-fit measures. Furthermore, this study examined how quantitatively different imperviousness estimates affect the <span class="hlt">prediction</span> of <span class="hlt">hydrological</span> response both in the flow regime and in the thermal regime. We assessed the relationships between indicators of <span class="hlt">hydrological</span> response and imperviousness-descriptors. As indicators of flow variability, coefficient of variance, lag-one autocorrelation, and mean daily flow change were calculated based on measured mean daily stream flow from the water year 1997 to 2003. For thermal variability, indicators such as percent-days of surge, degree-day, and mean daily temperature difference were calculated base on measured stream temperature over several basins in Maryland. To describe imperviousness through the <span class="hlt">hydrological</span> process, GIS-based spatially distributed <span class="hlt">hydrological</span> models were developed based on a water-balance method and the SCS-CN method. Imperviousness estimates from land use and land cover were used as predictors in these models to examine the effect of imperviousness using different data sources on the <span class="hlt">prediction</span> of <span class="hlt">hydrological</span> response. Indicators of <span class="hlt">hydrological</span> response were also regressed on aggregate imperviousness. This allowed for identifying if</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018JHyd..558..255B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018JHyd..558..255B"><span>Daily river flow <span class="hlt">prediction</span> based on Two-Phase Constructive Fuzzy Systems Modeling: A case of <span class="hlt">hydrological</span> - meteorological measurements asymmetry</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Bou-Fakhreddine, Bassam; Mougharbel, Imad; Faye, Alain; Abou Chakra, Sara; Pollet, Yann</p> <p>2018-03-01</p> <p>Accurate daily river flow forecast is essential in many applications of water resources such as hydropower operation, agricultural planning and flood control. This paper presents a forecasting approach to deal with a newly addressed situation where <span class="hlt">hydrological</span> data exist for a period longer than that of meteorological data (measurements asymmetry). In fact, one of the potential solutions to resolve measurements asymmetry issue is data re-sampling. It is a matter of either considering only the <span class="hlt">hydrological</span> data or the balanced part of the hydro-meteorological data set during the forecasting process. However, the main disadvantage is that we may lose potentially relevant information from the left-out data. In this research, the key output is a Two-Phase Constructive Fuzzy inference hybrid model that is implemented over the non re-sampled data. The introduced modeling approach must be capable of exploiting the available data efficiently with higher <span class="hlt">prediction</span> efficiency relative to Constructive Fuzzy model trained over re-sampled data set. The study was applied to Litani River in the Bekaa Valley - Lebanon by using 4 years of rainfall and 24 years of river flow daily measurements. A Constructive Fuzzy System Model (C-FSM) and a Two-Phase Constructive Fuzzy System Model (TPC-FSM) are trained. Upon validating, the second model has shown a primarily competitive performance and accuracy with the ability to preserve a higher day-to-day variability for 1, 3 and 6 days ahead. In fact, for the longest lead period, the C-FSM and TPC-FSM were able of explaining respectively 84.6% and 86.5% of the actual river flow variation. Overall, the results indicate that TPC-FSM model has provided a better tool to capture extreme flows in the process of streamflow <span class="hlt">prediction</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2004AGUFM.H41B0295D','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2004AGUFM.H41B0295D"><span><span class="hlt">Prediction</span> of Mass Wasting, Erosion, and Sediment Transport With the Distributed <span class="hlt">Hydrology</span>-Soil-Vegetation Model</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Doten, C. O.; Lanini, J. S.; Bowling, L. C.; Lettenmaier, D. P.</p> <p>2004-12-01</p> <p>Erosion and sediment transport in a temperate forested watershed are <span class="hlt">predicted</span> with a new sediment module linked to the Distributed <span class="hlt">Hydrology</span>-Soil-Vegetation Model (DHSVM). The DHSVM sediment module represents the main sources of sediment generation in forested environments: mass wasting, hillslope erosion and road surface erosion. It produces failures based on a factor-of-safety analysis with the infinite slope model through use of stochastically generated soil and vegetation parameters. Failed material is routed downslope with a rule-based scheme that determines sediment delivery to streams. Sediment from hillslopes and road surfaces is also transported to the channel network. Basin sediment yield is <span class="hlt">predicted</span> with a simple channel sediment routing scheme. The model was applied to the Rainy Creek catchment, a tributary of the Wenatchee River which drains the east slopes of the Cascade Mountains, and Hard and Ware Creeks on the west slopes of the Cascades. In these initial applications, the model produced plausible sediment yield and ratios of landsliding and surface erosion , when compared to published rates for similar catchments in the Pacific Northwest. We have also used the model to examine the implications of fires and logging road removal on sediment generation in the Rainy Creek catchment. Generally, in absolute value, the <span class="hlt">predicted</span> changes (increased sediment generation) following fires, which are primarily associated with increased slope failures, are much larger than the modest changes (reductions in sediment yield) associated with road obliteration, although the small sensitivity to forest road obliteration may be due in part to the relatively low road density in the Rainy Creek catchment, and to mechanisms, such as culvert failure, that are not represented in the model.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017JGRG..122..966N','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017JGRG..122..966N"><span>Development of an <span class="hlt">advanced</span> eco-<span class="hlt">hydrologic</span> and biogeochemical coupling model aimed at clarifying the missing role of inland water in the global biogeochemical cycle</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Nakayama, Tadanobu</p> <p>2017-04-01</p> <p>Recent research showed that inland water including rivers, lakes, and groundwater may play some role in carbon cycling, although its contribution has remained uncertain due to limited amount of reliable data available. In this study, the author developed an <span class="hlt">advanced</span> model coupling eco-<span class="hlt">hydrology</span> and biogeochemical cycle (National Integrated Catchment-based Eco-<span class="hlt">hydrology</span> (NICE)-BGC). This new model incorporates complex coupling of <span class="hlt">hydrologic</span>-carbon cycle in terrestrial-aquatic linkages and interplay between inorganic and organic carbon during the whole process of carbon cycling. The model could simulate both horizontal transports (export from land to inland water 2.01 ± 1.98 Pg C/yr and transported to ocean 1.13 ± 0.50 Pg C/yr) and vertical fluxes (degassing 0.79 ± 0.38 Pg C/yr, and sediment storage 0.20 ± 0.09 Pg C/yr) in major rivers in good agreement with previous researches, which was an improved estimate of carbon flux from previous studies. The model results also showed global net land flux simulated by NICE-BGC (-1.05 ± 0.62 Pg C/yr) decreased carbon sink a little in comparison with revised Lund-Potsdam-Jena Wetland <span class="hlt">Hydrology</span> and Methane (-1.79 ± 0.64 Pg C/yr) and previous materials (-2.8 to -1.4 Pg C/yr). This is attributable to CO2 evasion and lateral carbon transport explicitly included in the model, and the result suggests that most previous researches have generally overestimated the accumulation of terrestrial carbon and underestimated the potential for lateral transport. The results further implied difference between inverse techniques and budget estimates suggested can be explained to some extent by a net source from inland water. NICE-BGC would play an important role in reevaluation of greenhouse gas budget of the biosphere, quantification of hot spots, and bridging the gap between top-down and bottom-up approaches to global carbon budget.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016EGUGA..1815918Z','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016EGUGA..1815918Z"><span><span class="hlt">Hydrological</span> response of a subhumid watershed after a greening-up process, an example in South East Spain</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Zema, Demetrio Antonio; Cataldo, Maria Francesca; Denisi, Pietro; Martino, Domenico; de Vente, Joris; Boix-Fayos, Carolina</p> <p>2016-04-01</p> <p>Many watersheds in the Mediterranean are subject to land use changes and <span class="hlt">hydrological</span> control works that can have important effects on their <span class="hlt">hydrological</span> and geomorphological response. In such contexts, a better understanding of the <span class="hlt">hydrological</span> processes and their linkage to the geomorphic evolutionary trends would help territory planners and other stakeholders to face off soil and water body degradation, optimising efficiency and cheapness of planned interventions. This study focuses on a catchment in SE Spain, Upper Taibilla (320 km2, Segura basin), which suffered an important greening-up process with increase of forest cover, decrease of agriculture activities and installation of <span class="hlt">hydrological</span> control works during the second half of XX century. The objective was to characterize the changes in the <span class="hlt">hydrological</span> response of the catchment in relation to the changes in their drainage area. Firstly, the actual <span class="hlt">hydrological</span> response to precipitation was analysed at aggregated (i.e. monthly, seasonal and annual) scale, using 15 years of the most recent runoff observations collected at the outlet of Upper Taibilla river (specifically at the inlet of Taibilla reservoir). Based on the actual distribution of soil land use and texture, the studied sub-basins were discretised by a GIS software in a system of homogenous <span class="hlt">hydrological</span> units, in order to identify the most critical areas producing surface runoff. This actual aptitude to produce runoff was compared to the sub-basin <span class="hlt">hydrological</span> response of 1930-1940s (that is before reforestation works and check-dam installation), in order to analyse the eventual presence of evolutionary trends in basin <span class="hlt">hydrology</span> and the whole efficiency of these works in mitigating runoff impacts. Furthermore, considering that computer <span class="hlt">prediction</span> models are important tools for planning land use changes and other management works in basins, the applicability of two <span class="hlt">hydrological</span> models for <span class="hlt">predicting</span> surface runoff in the studied sub-basins was</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19810004018','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19810004018"><span>Remote Sensing For Water Resources And <span class="hlt">Hydrology</span>. Recommended research emphasis for the 1980's</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p></p> <p>1980-01-01</p> <p>The problems and the areas of activity that the Panel believes should be emphasized in work on remote sensing for water resources and <span class="hlt">hydrology</span> in the 1980's are set forth. The Panel deals only with those activities and problems in water resources and <span class="hlt">hydrology</span> that the Panel considers important, and where, in the Panel's opinion, application of current remote sensing capability or <span class="hlt">advancements</span> in remote sensing capability can help meet urgent problems and provide large returns in practical benefits.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2005AtmRe..77..367C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2005AtmRe..77..367C"><span>Design storm <span class="hlt">prediction</span> and <span class="hlt">hydrologic</span> modeling using a web-GIS approach on a free-software platform</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Castrogiovanni, E. M.; La Loggia, G.; Noto, L. V.</p> <p>2005-09-01</p> <p>The aim of this work has been to implement a set of procedures useful to automatise the evaluation, the design storm <span class="hlt">prediction</span> and the flood discharge associated with a selected risk level. For this purpose a Geographic Information System has been implemented using Grass 5.0. One of the main topics of such a system is a georeferenced database of the highest intensity rainfalls and their assigned duration recorded in Sicily. This database contains the main characteristics for more than 250 raingauges, as well as the values of intense rainfall events recorded by these raingauges. These data are managed through the combined use of the PostgreSQL and GRASS-GIS 5.0 databases. Some of the best-known probability distributions have been implemented within the Geographical Information System in order to determine the point and/or areal rain values once duration and return period have been defined. The system also includes a <span class="hlt">hydrological</span> module necessary to compute the probable flow, for a selected risk level, at points chosen by the user. A peculiarity of the system is the possibility to querying the model using a web-interface. The assumption is that the rising needs of geographic information, and dealing with the rising importance of peoples participation in the decision process, requires new forms for the diffusion of territorial data. Furthermore, technicians as well as public administrators needs to get customized and specialist data to support planning, particularly in emergencies. In this perspective a Web-interface has been developed for the <span class="hlt">hydrologic</span> system. The aim is to allow remote users to access a centralized database and processing-power to serve the needs of knowledge without complex hardware/software infrastructures.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/pages/biblio/1376362-intermediate-scale-model-thermal-hydrology-low-relief-permafrost-affected-landscapes','SCIGOV-DOEP'); return false;" href="https://www.osti.gov/pages/biblio/1376362-intermediate-scale-model-thermal-hydrology-low-relief-permafrost-affected-landscapes"><span>An intermediate-scale model for thermal <span class="hlt">hydrology</span> in low-relief permafrost-affected landscapes</span></a></p> <p><a target="_blank" href="http://www.osti.gov/pages">DOE PAGES</a></p> <p>Jan, Ahmad; Coon, Ethan T.; Painter, Scott L.; ...</p> <p>2017-07-10</p> <p>Integrated surface/subsurface models for simulating the thermal <span class="hlt">hydrology</span> of permafrost-affected regions in a warming climate have recently become available, but computational demands of those new process-rich simu- lation tools have thus far limited their applications to one-dimensional or small two-dimensional simulations. We present a mixed-dimensional model structure for efficiently simulating surface/subsurface thermal <span class="hlt">hydrology</span> in low-relief permafrost regions at watershed scales. The approach replaces a full three-dimensional system with a two-dimensional overland thermal <span class="hlt">hydrology</span> system and a family of one-dimensional vertical columns, where each column represents a fully coupled surface/subsurface thermal <span class="hlt">hydrology</span> system without lateral flow. The system is then operatormore » split, sequentially updating the overland flow system without sources and the one-dimensional columns without lateral flows. We show that the app- roach is highly scalable, supports subcycling of different processes, and compares well with the corresponding fully three-dimensional representation at significantly less computational cost. Those <span class="hlt">advances</span> enable recently developed representations of freezing soil physics to be coupled with thermal overland flow and surface energy balance at scales of 100s of meters. Furthermore developed and demonstrated for permafrost thermal <span class="hlt">hydrology</span>, the mixed-dimensional model structure is applicable to integrated surface/subsurface thermal <span class="hlt">hydrology</span> in general.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFMED31B0874P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFMED31B0874P"><span>Indigenous Waters: Applying the SWAT <span class="hlt">Hydrological</span> Model to the Lumbee River Watershed</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Painter, J.; Singh, N.; Martin, K. L.; Vose, J. M.; Wear, D. N.; Emanuel, R. E.</p> <p>2016-12-01</p> <p><span class="hlt">Hydrological</span> modeling can reveal insight about how rainfall becomes streamflow in a watershed comprising heterogeneous soils, terrain and land cover. Modeling can also help disentangle <span class="hlt">predicted</span> impacts of climate and land use change on <span class="hlt">hydrological</span> processes. We applied a <span class="hlt">hydrological</span> model to the Lumbee River watershed, also known as the Lumber River Watershed, in the coastal plain of North Carolina (USA) to better understand how streamflow may be impacted by <span class="hlt">predicted</span> climate and land use change in the mid-21st century. The Lumbee River flows through a predominantly Native American community, which may be affected by changing water resources during this period. The long-term goal of our project is to <span class="hlt">predict</span> the effects of climate and land use change on the Lumbee River watershed and on the Native community that relies upon the river. We applied the Soil & Water Assessment Tool for ArcGIS (ArcSWAT), which was calibrated to historical climate and USGS streamflow data during the late 20th century, and we determined frequency distributions for key model parameters that best <span class="hlt">predicted</span> streamflow during this time period. After calibrating and validating the model during the historical period, we identified land use and climate projections to represent a range of future conditions in the watershed. Specifically, we selected downscaled climate forcing data from four general circulation models running the RCP8.5 scenario. We also selected land use projections from a cornerstone scenario of the USDA Forest Service's Southern Forest Futures Project. This presentation reports on our methods for propagating parameter and climatic uncertainty through model <span class="hlt">predictions</span>, and it reports on spatial patterns of land use change <span class="hlt">predicted</span> by the cornerstone scenario.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20140017451','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20140017451"><span>Thermal Model <span class="hlt">Predictions</span> of <span class="hlt">Advanced</span> Stirling Radioisotope Generator Performance</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Wang, Xiao-Yen J.; Fabanich, William Anthony; Schmitz, Paul C.</p> <p>2014-01-01</p> <p>This paper presents recent thermal model results of the <span class="hlt">Advanced</span> Stirling Radioisotope Generator (ASRG). The three-dimensional (3D) ASRG thermal power model was built using the Thermal Desktop(trademark) thermal analyzer. The model was correlated with ASRG engineering unit test data and ASRG flight unit <span class="hlt">predictions</span> from Lockheed Martin's (LM's) I-deas(trademark) TMG thermal model. The auxiliary cooling system (ACS) of the ASRG is also included in the ASRG thermal model. The ACS is designed to remove waste heat from the ASRG so that it can be used to heat spacecraft components. The performance of the ACS is reported under nominal conditions and during a Venus flyby scenario. The results for the nominal case are validated with data from Lockheed Martin. Transient thermal analysis results of ASRG for a Venus flyby with a representative trajectory are also presented. In addition, model results of an ASRG mounted on a Cassini-like spacecraft with a sunshade are presented to show a way to mitigate the high temperatures of a Venus flyby. It was <span class="hlt">predicted</span> that the sunshade can lower the temperature of the ASRG alternator by 20 C for the representative Venus flyby trajectory. The 3D model also was modified to <span class="hlt">predict</span> generator performance after a single <span class="hlt">Advanced</span> Stirling Convertor failure. The geometry of the Microtherm HT insulation block on the outboard side was modified to match deformation and shrinkage observed during testing of a prototypic ASRG test fixture by LM. Test conditions and test data were used to correlate the model by adjusting the thermal conductivity of the deformed insulation to match the post-heat-dump steady state temperatures. Results for these conditions showed that the performance of the still-functioning inboard ACS was unaffected.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017EGUGA..1917476K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017EGUGA..1917476K"><span>Flood <span class="hlt">Prediction</span> for the Tam Nong District in Mekong Delta Using <span class="hlt">Hydrological</span> Modelling and <span class="hlt">Hydrologic</span> Remote Sensing Technique</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Kappas, Martin; Nguyen Hong, Quang; Thanh, Nga Pham Thi; Thu, Hang Le Thi; Nguyen Vu, Giang; Degener, Jan; Rafiei Emam, Ammar</p> <p>2017-04-01</p> <p>There has been an increasing attention to the large trans-boundary Mekong river basin due to various problems related to water management and flood control, for instance. Vietnam Mekong delta is located at the downstream of the river basin where is affected most by this human-induced reduction in flows from the upstream. On the other hand, the flood plain of nine anastomosing channels is increasingly effected by the seawater intrusion due to sea level rising of climate change. This results in negative impacts of salinization, drought, and floods, while formerly flooding had frequently brought positive natural gain of irrigation water and alluvial aggradation. In this research, our aim is to <span class="hlt">predict</span> flooding for the better water management adaptation and control. We applied the model HEC-SSP 2.1 to analyze flood flow frequency, two-dimensional unsteady flow calculations in HEC-RAS 5.0 for simulating a floodplain inundation. Remote sensing-based water level (Jason-2) and inundation map were used for validation and comparison with the model simulations. The results revealed a reduction of water level at all the monitoring stations, particularly in the last decade. In addition, a trend of the inundation extension gradually declined, but in some periods it remained severe due to water release from upstream reservoirs during the rainy season (October-November). We found an acceptable agreement between the HEC-RAS and remote sensing flooding maps (around 70%). Based on the flood routine analysis, we could conclude that the water level will continue lower and lead to a trend of drought and salinization harsher in the near future. Keywords: Mekong delta, flood control, inundation, water management, <span class="hlt">hydrological</span> modelling, remote sensing</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://cfpub.epa.gov/si/si_public_record_report.cfm?direntryid=66073','PESTICIDES'); return false;" href="https://cfpub.epa.gov/si/si_public_record_report.cfm?direntryid=66073"><span>Tracer-Test Planning Using the Efficient <span class="hlt">Hydrologic</span> Tracer ...</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><span class="hlt">Hydrological</span> tracer testing is the most reliable diagnostic technique available for establishing flow trajectories and <span class="hlt">hydrologic</span> connections and for determining basic hydraulic and geometric parameters necessary for establishing operative solute-transport processes. Tracer-test design can be difficult because of a lack of prior knowledge of the basic hydraulic and geometric parameters desired and the appropriate tracer mass to release. A new efficient <span class="hlt">hydrologic</span> tracer-test design (EHTD) methodology has been developed that combines basic measured field parameters (e.g., discharge, distance, cross-sectional area) in functional relationships that describe solute-transport processes related to flow velocity and time of travel. The new method applies these initial estimates for time of travel and velocity to a hypothetical continuously stirred tank reactor as an analog for the <span class="hlt">hydrologic</span> flow system to develop initial estimates for tracer concentration and axial dispersion, based on a preset average tracer concentration. Root determination of the one-dimensional advection-dispersion equation (ADE) using the preset average tracer concentration then provides a theoretical basis for an estimate of necessary tracer mass.Application of the <span class="hlt">predicted</span> tracer mass with the hydraulic and geometric parameters in the ADE allows for an approximation of initial sample-collection time and subsequent sample-collection frequency where a maximum of 65 samples were determined to be</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2011AGUFM.H33H1410W','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2011AGUFM.H33H1410W"><span>A "total parameter estimation" method in the varification of distributed <span class="hlt">hydrological</span> models</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Wang, M.; Qin, D.; Wang, H.</p> <p>2011-12-01</p> <p>Conventionally <span class="hlt">hydrological</span> models are used for runoff or flood forecasting, hence the determination of model parameters are common estimated based on discharge measurements at the catchment outlets. With the <span class="hlt">advancement</span> in <span class="hlt">hydrological</span> sciences and computer technology, distributed <span class="hlt">hydrological</span> models based on the physical mechanism such as SWAT, MIKESHE, and WEP, have gradually become the mainstream models in <span class="hlt">hydrology</span> sciences. However, the assessments of distributed <span class="hlt">hydrological</span> models and model parameter determination still rely on runoff and occasionally, groundwater level measurements. It is essential in many countries, including China, to understand the local and regional water cycle: not only do we need to simulate the runoff generation process and for flood forecasting in wet areas, we also need to grasp the water cycle pathways and consumption process of transformation in arid and semi-arid regions for the conservation and integrated water resources management. As distributed <span class="hlt">hydrological</span> model can simulate physical processes within a catchment, we can get a more realistic representation of the actual water cycle within the simulation model. Runoff is the combined result of various <span class="hlt">hydrological</span> processes, using runoff for parameter estimation alone is inherits problematic and difficult to assess the accuracy. In particular, in the arid areas, such as the Haihe River Basin in China, runoff accounted for only 17% of the rainfall, and very concentrated during the rainy season from June to August each year. During other months, many of the perennial rivers within the river basin dry up. Thus using single runoff simulation does not fully utilize the distributed <span class="hlt">hydrological</span> model in arid and semi-arid regions. This paper proposed a "total parameter estimation" method to verify the distributed <span class="hlt">hydrological</span> models within various water cycle processes, including runoff, evapotranspiration, groundwater, and soil water; and apply it to the Haihe river basin in</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012JHyd..472..277B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012JHyd..472..277B"><span>Valuing <span class="hlt">hydrological</span> alteration in multi-objective water resources management</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Bizzi, Simone; Pianosi, Francesca; Soncini-Sessa, Rodolfo</p> <p>2012-11-01</p> <p>SummaryThe management of water through the impoundment of rivers by dams and reservoirs is necessary to support key human activities such as hydropower production, agriculture and flood risk mitigation. <span class="hlt">Advances</span> in multi-objective optimization techniques and ever growing computing power make it possible to design reservoir operating policies that represent Pareto-optimal tradeoffs between multiple interests. On the one hand, such optimization methods can enhance performances of commonly targeted objectives (such as hydropower production or water supply), on the other hand they risk strongly penalizing all the interests not directly (i.e. mathematically) included in the optimization algorithm. The alteration of the downstream <span class="hlt">hydrological</span> regime is a well established cause of ecological degradation and its evaluation and rehabilitation is commonly required by recent legislation (as the Water Framework Directive in Europe). However, it is rarely embedded in reservoir optimization routines and, even when explicitly considered, the criteria adopted for its evaluation are doubted and not commonly trusted, undermining the possibility of real implementation of environmentally friendly policies. The main challenges in defining and assessing <span class="hlt">hydrological</span> alterations are: how to define a reference state (referencing); how to define criteria upon which to build mathematical indicators of alteration (measuring); and finally how to aggregate the indicators in a single evaluation index (valuing) that can serve as objective function in the optimization problem. This paper aims to address these issues by: (i) discussing the benefits and constrains of different approaches to referencing, measuring and valuing <span class="hlt">hydrological</span> alteration; (ii) testing two alternative indices of <span class="hlt">hydrological</span> alteration, one based on the established framework of Indicators of <span class="hlt">Hydrological</span> Alteration (Richter et al., 1996), and one satisfying the mathematical properties required by widely used optimization</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19980017321','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19980017321"><span>Assessment of Required Accuracy of Digital Elevation Data for <span class="hlt">Hydrologic</span> Modeling</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Kenward, T.; Lettenmaier, D. P.</p> <p>1997-01-01</p> <p>The effect of vertical accuracy of Digital Elevation Models (DEMs) on <span class="hlt">hydrologic</span> models is evaluated by comparing three DEMs and resulting <span class="hlt">hydrologic</span> model <span class="hlt">predictions</span> applied to a 7.2 sq km USDA - ARS watershed at Mahantango Creek, PA. The high resolution (5 m) DEM was resempled to a 30 m resolution using method that constrained the spatial structure of the elevations to be comparable with the USGS and SIR-C DEMs. This resulting 30 m DEM was used as the reference product for subsequent comparisons. Spatial fields of directly derived quantities, such as elevation differences, slope, and contributing area, were compared to the reference product, as were <span class="hlt">hydrologic</span> model output fields derived using each of the three DEMs at the common 30 m spatial resolution.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016JHyd..541.1488B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016JHyd..541.1488B"><span><span class="hlt">Hydrologic</span> response to stormwater control measures in urban watersheds</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Bell, Colin D.; McMillan, Sara K.; Clinton, Sandra M.; Jefferson, Anne J.</p> <p>2016-10-01</p> <p>Stormwater control measures (SCMs) are designed to mitigate deleterious effects of urbanization on river networks, but our ability to <span class="hlt">predict</span> the cumulative effect of multiple SCMs at watershed scales is limited. The most widely used metric to quantify impacts of urban development, total imperviousness (TI), does not contain information about the extent of stormwater control. We analyzed the discharge records of 16 urban watersheds in Charlotte, NC spanning a range of TI (4.1-54%) and area mitigated with SCMs (1.3-89%). We then tested multiple watershed metrics that quantify the degree of urban impact and SCM mitigation to determine which best <span class="hlt">predicted</span> <span class="hlt">hydrologic</span> response across sites. At the event time scale, linear models showed TI to be the best predictor of both peak unit discharge and rainfall-runoff ratios across a range of storm sizes. TI was also a strong driver of both a watershed's capacity to buffer small (e.g., 1-10 mm) rain events, and the relationship between peak discharge and precipitation once that buffering capacity is exceeded. Metrics containing information about SCMs did not appear as primary predictors of event <span class="hlt">hydrologic</span> response, suggesting that the level of SCM mitigation in many urban watersheds is insufficient to influence <span class="hlt">hydrologic</span> response. Over annual timescales, impervious surfaces unmitigated by SCMs and tree coverage were best correlated with streamflow flashiness and water yield, respectively. The shift in controls from the event scale to the annual scale has important implications for water resource management, suggesting that overall limitation of watershed imperviousness rather than partial mitigation by SCMs may be necessary to alleviate the <span class="hlt">hydrologic</span> impacts of urbanization.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFM.B31H0562M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFM.B31H0562M"><span>Geochemical response to <span class="hlt">hydrologic</span> change along land-sea interfaces</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Michael, H. A.; Yu, X.; LeMonte, J. J.; Sparks, D. L.; Kim, K. H.; Heiss, J.; Ullman, W. J.; Guimond, J. A.; Seyfferth, A.</p> <p>2016-12-01</p> <p>Coastal groundwater-surface water interfaces are hotspots of geochemical activity, where reactants contributed by different sources come in contact. Reactions that occur along these land-sea boundaries have important effects on fluxes and cycling of carbon, nutrients, and contaminants. <span class="hlt">Hydrologic</span> perturbations can alter interactions by promoting mixing, changing redox state, and altering subsurface residence times during which reactions may occur. We present examples from field and modeling investigations along the Delaware coastline that illustrate the impacts of <span class="hlt">hydrologic</span> fluctuations on geochemical conditions and fluxes in different coastal environments. Along the highly populated Wilmington coastline, soils are contaminated with heavy metals from legacy industrial practices. We show with continuous redox monitoring and sampling over tidal to seasonal timescales that arsenic is mobilized and immobilized in response to <span class="hlt">hydrologic</span> change. Along a beach, modeling and long-term monitoring show the influence of tidal to seasonal changes in the mixing zone between discharging fresh groundwater and seawater in the intertidal beach aquifer and associated impacts on biogeochemical reactivity and denitrification. In a saltmarsh, <span class="hlt">hydrologic</span> changes alter carbon dynamics, with implications for the discharge of dissolved organic carbon to the ocean and export of carbon dioxide and methane to the atmosphere. Understanding the impacts of <span class="hlt">hydrologic</span> changes on both long and short timescales is essential for improving our ability to <span class="hlt">predict</span> the global biogeochemical impacts of a changing climate.</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.ncbi.nlm.nih.gov/pubmed/22097059','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/22097059"><span>Storm water infiltration in a monitored green roof for <span class="hlt">hydrologic</span> restoration.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Palla, A; Sansalone, J J; Gnecco, I; Lanza, L G</p> <p>2011-01-01</p> <p>The objectives of this study are to provide detailed information about green roof performance in the Mediterranean climate (retained volume, peak flow reduction, runoff delay) and to identify a suitable modelling approach for describing the associated <span class="hlt">hydrologic</span> response. Data collected during a 13-month monitoring campaign and a seasonal monitoring campaign (September-December 2008) at the green roof experimental site of the University of Genova (Italy) are presented together with results obtained in quantifying the green roof <span class="hlt">hydrologic</span> performance. In order to examine the green roof <span class="hlt">hydrologic</span> response, the SWMS_2D model, that solves the Richards' equation for two-dimensional saturated-unsaturated water flow, has been implemented. Modelling results confirm the suitability of the SWMS_2D model to properly describe the <span class="hlt">hydrologic</span> response of the green roofs. The model adequately reproduces the hydrographs; furthermore, the <span class="hlt">predicted</span> soil water content profile generally matches the observed values along a vertical profile where measurements are available.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017JHyd..550..685K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017JHyd..550..685K"><span>Diagnosis of the <span class="hlt">hydrology</span> of a small Arctic basin at the tundra-taiga transition using a physically based <span class="hlt">hydrological</span> model</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Krogh, Sebastian A.; Pomeroy, John W.; Marsh, Philip</p> <p>2017-07-01</p> <p>A better understanding of cold regions <span class="hlt">hydrological</span> processes and regimes in transitional environments is critical for <span class="hlt">predicting</span> future Arctic freshwater fluxes under climate and vegetation change. A physically based <span class="hlt">hydrological</span> model using the Cold Regions <span class="hlt">Hydrological</span> Model platform was created for a small Arctic basin in the tundra-taiga transition region. The model represents snow redistribution and sublimation by wind and vegetation, snowmelt energy budget, evapotranspiration, subsurface flow through organic terrain, infiltration to frozen soils, freezing and thawing of soils, permafrost and streamflow routing. The model was used to reconstruct the basin water cycle over 28 years to understand and quantify the mass fluxes controlling its <span class="hlt">hydrological</span> regime. Model structure and parameters were set from the current understanding of Arctic <span class="hlt">hydrology</span>, remote sensing, field research in the basin and region, and calibration against streamflow observations. Calibration was restricted to subsurface hydraulic and storage parameters. Multi-objective evaluation of the model using observed streamflow, snow accumulation and ground freeze/thaw state showed adequate simulation. Significant spatial variability in the winter mass fluxes was found between tundra, shrubs and forested sites, particularly due to the substantial blowing snow redistribution and sublimation from the wind-swept upper basin, as well as sublimation of canopy intercepted snow from the forest (about 17% of snowfall). At the basin scale, the model showed that evapotranspiration is the largest loss of water (47%), followed by streamflow (39%) and sublimation (14%). The models streamflow performance sensitivity to a set of parameter was analysed, as well as the mean annual mass balance uncertainty associated with these parameters.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://cfpub.epa.gov/si/si_public_record_report.cfm?dirEntryId=335890&Lab=NRMRL&keyword=State+AND+flow&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=335890&Lab=NRMRL&keyword=State+AND+flow&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>Wetland <span class="hlt">Hydrology</span></span></a></p> <p><a target="_blank" href="http://oaspub.epa.gov/eims/query.page">EPA Science Inventory</a></p> <p></p> <p></p> <p>This chapter discusses the state of the science in wetland <span class="hlt">hydrology</span> by touching upon the major hydraulic and <span class="hlt">hydrologic</span> processes in these complex ecosystems, their measurement/estimation techniques, and modeling methods. It starts with the definition of wetlands, their benefit...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012EGUGA..14.4946K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012EGUGA..14.4946K"><span>Identification of statistically independent climatic pattern in GRACE and <span class="hlt">hydrological</span> model data over West-Africa</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Kusche, J.; Forootan, E.; Eicker, A.; Hoffmann-Dobrev, H.</p> <p>2012-04-01</p> <p>West-African countries have been exposed to changes in rainfall patterns over the last decades, including a significant negative trend. This causes adverse effects on water resources, for instance reduced freshwater availability, and changes in the frequency, duration and magnitude of droughts and floods. Extracting the main patterns of water storage change in West Africa from remote sensing and linking them to climate variability, is therefore an essential step to understand the <span class="hlt">hydrological</span> aspects of the region. In this study, the higher order statistical method of Independent Component Analysis (ICA) is employed to extract statistically independent water storage patterns from monthly Gravity Recovery And Climate Experiment (GRACE), from the WaterGAP Global <span class="hlt">Hydrology</span> Model (WGHM) and from Tropical Rainfall Measuring Mission (TRMM) products over West Africa, for the period 2002-2012. Then, to reveal the influences of climatic teleconnections on the individual patterns, these results were correlated to the El Nino-Southern Oscillation (ENSO) and the Indian Ocean Dipole (IOD) indices. To study the <span class="hlt">predictability</span> of water storage changes, <span class="hlt">advanced</span> statistical methods were applied on the main independent Sea Surface Temperature (SST) patterns over the Atlantic and Indian Oceans for the period 2002-2012 and the ICA results. Our results show a water storage decrease over the coastal regions of West Africa (including Sierra Leone, Liberia, Togo and Nigeria), associated with rainfall decrease. The comparison between GRACE estimations and WGHM results indicates some inconsistencies that underline the importance of forcing data for <span class="hlt">hydrological</span> modeling of West Africa. Keywords: West Africa; GRACE-derived water storage; ICA; ENSO; IOD</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2007AGUFM.H13H1685W','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2007AGUFM.H13H1685W"><span>Data Access System for <span class="hlt">Hydrology</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Whitenack, T.; Zaslavsky, I.; Valentine, D.; Djokic, D.</p> <p>2007-12-01</p> <p>As part of the CUAHSI HIS (Consortium of Universities for the <span class="hlt">Advancement</span> of <span class="hlt">Hydrologic</span> Science, Inc., <span class="hlt">Hydrologic</span> Information System), the CUAHSI HIS team has developed Data Access System for <span class="hlt">Hydrology</span> or DASH. DASH is based on commercial off the shelf technology, which has been developed in conjunction with a commercial partner, ESRI. DASH is a web-based user interface, developed in ASP.NET developed using ESRI ArcGIS Server 9.2 that represents a mapping, querying and data retrieval interface over observation and GIS databases, and web services. This is the front end application for the CUAHSI <span class="hlt">Hydrologic</span> Information System Server. The HIS Server is a software stack that organizes observation databases, geographic data layers, data importing and management tools, and online user interfaces such as the DASH application, into a flexible multi- tier application for serving both national-level and locally-maintained observation data. The user interface of the DASH web application allows online users to query observation networks by location and attributes, selecting stations in a user-specified area where a particular variable was measured during a given time interval. Once one or more stations and variables are selected, the user can retrieve and download the observation data for further off-line analysis. The DASH application is highly configurable. The mapping interface can be configured to display map services from multiple sources in multiple formats, including ArcGIS Server, ArcIMS, and WMS. The observation network data is configured in an XML file where you specify the network's web service location and its corresponding map layer. Upon initial deployment, two national level observation networks (USGS NWIS daily values and USGS NWIS Instantaneous values) are already pre-configured. There is also an optional login page which can be used to restrict access as well as providing a alternative to immediate downloads. For large request, users would be notified via</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2008AGUFM.H51B0793B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2008AGUFM.H51B0793B"><span>Estimating the Uncertain Mathematical Structure of <span class="hlt">Hydrological</span> Model via Bayesian Data Assimilation</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Bulygina, N.; Gupta, H.; O'Donell, G.; Wheater, H.</p> <p>2008-12-01</p> <p>The structure of <span class="hlt">hydrological</span> model at macro scale (e.g. watershed) is inherently uncertain due to many factors, including the lack of a robust <span class="hlt">hydrological</span> theory at the macro scale. In this work, we assume that a suitable conceptual model for the <span class="hlt">hydrologic</span> system has already been determined - i.e., the system boundaries have been specified, the important state variables and input and output fluxes to be included have been selected, and the major <span class="hlt">hydrological</span> processes and geometries of their interconnections have been identified. The structural identification problem then is to specify the mathematical form of the relationships between the inputs, state variables and outputs, so that a computational model can be constructed for making simulations and/or <span class="hlt">predictions</span> of system input-state-output behaviour. We show how Bayesian data assimilation can be used to merge both prior beliefs in the form of pre-assumed model equations with information derived from the data to construct a posterior model. The approach, entitled Bayesian Estimation of Structure (BESt), is used to estimate a <span class="hlt">hydrological</span> model for a small basin in England, at hourly time scales, conditioned on the assumption of 3-dimensional state - soil moisture storage, fast and slow flow stores - conceptual model structure. Inputs to the system are precipitation and potential evapotranspiration, and outputs are actual evapotranspiration and streamflow discharge. Results show the difference between prior and posterior mathematical structures, as well as provide <span class="hlt">prediction</span> confidence intervals that reflect three types of uncertainty: due to initial conditions, due to input and due to mathematical structure.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/24708258','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/24708258"><span><span class="hlt">Predicting</span> survival time in noncurative patients with <span class="hlt">advanced</span> cancer: a prospective study in China.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Cui, Jing; Zhou, Lingjun; Wee, B; Shen, Fengping; Ma, Xiuqiang; Zhao, Jijun</p> <p>2014-05-01</p> <p>Accurate <span class="hlt">prediction</span> of prognosis for cancer patients is important for good clinical decision making in therapeutic and care strategies. The application of prognostic tools and indicators could improve <span class="hlt">prediction</span> accuracy. This study aimed to develop a new prognostic scale to <span class="hlt">predict</span> survival time of <span class="hlt">advanced</span> cancer patients in China. We prospectively collected items that we anticipated might influence survival time of <span class="hlt">advanced</span> cancer patients. Participants were recruited from 12 hospitals in Shanghai, China. We collected data including demographic information, clinical symptoms and signs, and biochemical test results. Log-rank tests, Cox regression, and linear regression were performed to develop a prognostic scale. Three hundred twenty patients with <span class="hlt">advanced</span> cancer were recruited. Fourteen prognostic factors were included in the prognostic scale: Karnofsky Performance Scale (KPS) score, pain, ascites, hydrothorax, edema, delirium, cachexia, white blood cell (WBC) count, hemoglobin, sodium, total bilirubin, direct bilirubin, aspartate aminotransferase (AST), and alkaline phosphatase (ALP) values. The score was calculated by summing the partial scores, ranging from 0 to 30. When using the cutoff points of 7-day, 30-day, 90-day, and 180-day survival time, the scores were calculated as 12, 10, 8, and 6, respectively. We propose a new prognostic scale including KPS, pain, ascites, hydrothorax, edema, delirium, cachexia, WBC count, hemoglobin, sodium, total bilirubin, direct bilirubin, AST, and ALP values, which may help guide physicians in <span class="hlt">predicting</span> the likely survival time of cancer patients more accurately. More studies are needed to validate this scale in the future.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70027144','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70027144"><span><span class="hlt">Hydrologic</span> aspects of marsh ponds during winter on the Gulf Coast Chenier Plain, USA: Effects of structural marsh management</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Bolduc, F.; Afton, A.D.</p> <p>2004-01-01</p> <p>The <span class="hlt">hydrology</span> of marsh ponds influences aquatic invertebrate and waterbird communities. <span class="hlt">Hydrologic</span> variables in marsh ponds of the Gulf Coast Chenier Plain are potentially affected by structural marsh management (SMM: levees, water control structures and impoundments) that has been implemented since the 1950s. Assuming that SMM restricts tidal flows and drainage of rainwater, we <span class="hlt">predicted</span> that SMM would increase water depth, and concomitantly decrease salinity and transparency in impounded marsh ponds. We also <span class="hlt">predicted</span> that SMM would increase seasonal variability in water depth in impounded marsh ponds because of the potential incapacity of water control structures to cope with large flooding events. In addition, we <span class="hlt">predicted</span> that SMM would decrease spatial variability in water depth. Finally, we <span class="hlt">predicted</span> that ponds of impounded freshwater (IF), oligohaline (IO), and mesohaline (IM) marshes would be similar in water depth, temperature, dissolved oxygen (O2), and transparency. Using a priori multivariate analysis of variance (MANOVA) contrast, we tested these <span class="hlt">predictions</span> by comparing <span class="hlt">hydrologic</span> variables within ponds of impounded and unimpounded marshes during winters 1997-1998 to 1999-2000 on Rockefeller State Wildlife Refuge, near Grand Chenier, Louisiana. Specifically, we compared <span class="hlt">hydrologic</span> variables (1) between IM and unimpounded mesohaline marsh ponds (UM); and (2) among IF, IO, and IM marshes ponds. As <span class="hlt">predicted</span>, water depth was higher and salinity and O2 were lower in IM than in UM marsh ponds. However, temperature and transparency did not differ between IM and UM marsh ponds. Water depth varied more among months in IM marsh ponds than within those of UM marshes, and variances among and within ponds were lower in IM than UM marshes. Finally, all <span class="hlt">hydrologic</span> variables, except salinity, were similar among IF, IO, and IM marsh ponds. <span class="hlt">Hydrologic</span> changes within marsh ponds due to SMM should (1) promote benthic invertebrate taxa that tolerate low levels of O2 and</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018HESS...22..171V','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018HESS...22..171V"><span>Comment on "Can assimilation of crowdsourced data in <span class="hlt">hydrological</span> modelling improve flood <span class="hlt">prediction</span>?" by Mazzoleni et al. (2017)</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Viero, Daniele P.</p> <p>2018-01-01</p> <p>Citizen science and crowdsourcing are gaining increasing attention among hydrologists. In a recent contribution, Mazzoleni et al. (2017) investigated the integration of crowdsourced data (CSD) into <span class="hlt">hydrological</span> models to improve the accuracy of real-time flood forecasts. The authors used synthetic CSD (i.e. not actually measured), because real CSD were not available at the time of the study. In their work, which is a proof-of-concept study, Mazzoleni et al. (2017) showed that assimilation of CSD improves the overall model performance; the impact of irregular frequency of available CSD, and that of data uncertainty, were also deeply assessed. However, the use of synthetic CSD in conjunction with (semi-)distributed <span class="hlt">hydrological</span> models deserves further discussion. As a result of equifinality, poor model identifiability, and deficiencies in model structure, internal states of (semi-)distributed models can hardly mimic the actual states of complex systems away from calibration points. Accordingly, the use of synthetic CSD that are drawn from model internal states under best-fit conditions can lead to overestimation of the effectiveness of CSD assimilation in improving flood <span class="hlt">prediction</span>. Operational flood forecasting, which results in decisions of high societal value, requires robust knowledge of the model behaviour and an in-depth assessment of both model structure and forcing data. Additional guidelines are given that are useful for the a priori evaluation of CSD for real-time flood forecasting and, hopefully, for planning apt design strategies for both model calibration and collection of CSD.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012AcMeS..26...93B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012AcMeS..26...93B"><span>Development and application of an atmospheric-<span class="hlt">hydrologic</span>-hydraulic flood forecasting model driven by TIGGE ensemble forecasts</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Bao, Hongjun; Zhao, Linna</p> <p>2012-02-01</p> <p>A coupled atmospheric-<span class="hlt">hydrologic</span>-hydraulic ensemble flood forecasting model, driven by The Observing System Research and <span class="hlt">Predictability</span> Experiment (THORPEX) Interactive Grand Global Ensemble (TIGGE) data, has been developed for flood forecasting over the Huaihe River. The incorporation of numerical weather <span class="hlt">prediction</span> (NWP) information into flood forecasting systems may increase forecast lead time from a few hours to a few days. A single NWP model forecast from a single forecast center, however, is insufficient as it involves considerable non-<span class="hlt">predictable</span> uncertainties and leads to a high number of false alarms. The availability of global ensemble NWP systems through TIGGE offers a new opportunity for flood forecast. The Xinanjiang model used for <span class="hlt">hydrological</span> rainfall-runoff modeling and the one-dimensional unsteady flow model applied to channel flood routing are coupled with ensemble weather <span class="hlt">predictions</span> based on the TIGGE data from the Canadian Meteorological Centre (CMC), the European Centre for Medium-Range Weather Forecasts (ECMWF), the UK Met Office (UKMO), and the US National Centers for Environmental <span class="hlt">Prediction</span> (NCEP). The developed ensemble flood forecasting model is applied to flood forecasting of the 2007 flood season as a test case. The test case is chosen over the upper reaches of the Huaihe River above Lutaizi station with flood diversion and retarding areas. The input flood discharge hydrograph from the main channel to the flood diversion area is estimated with the fixed split ratio of the main channel discharge. The flood flow inside the flood retarding area is calculated as a reservoir with the water balance method. The Muskingum method is used for flood routing in the flood diversion area. A probabilistic discharge and flood inundation forecast is provided as the end product to study the potential benefits of using the TIGGE ensemble forecasts. The results demonstrate satisfactory flood forecasting with clear signals of probability of floods up to a</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70171110','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70171110"><span>Toward improved simulation of river operations through integration with a <span class="hlt">hydrologic</span> model</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Morway, Eric D.; Niswonger, Richard G.; Triana, Enrique</p> <p>2016-01-01</p> <p><span class="hlt">Advanced</span> modeling tools are needed for informed water resources planning and management. Two classes of modeling tools are often used to this end–(1) distributed-parameter <span class="hlt">hydrologic</span> models for quantifying supply and (2) river-operation models for sorting out demands under rule-based systems such as the prior-appropriation doctrine. Within each of these two broad classes of models, there are many software tools that excel at simulating the processes specific to each discipline, but have historically over-simplified, or at worse completely neglected, aspects of the other. As a result, water managers reliant on river-operation models for administering water resources need improved tools for representing spatially and temporally varying groundwater resources in conjunctive-use systems. A new tool is described that improves the representation of groundwater/surface-water (GW-SW) interaction within a river-operations modeling context and, in so doing, <span class="hlt">advances</span> evaluation of system-wide <span class="hlt">hydrologic</span> consequences of new or altered management regimes.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012JGeo...62...40J','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012JGeo...62...40J"><span>Assessment of terrestrial water contributions to polar motion from GRACE and <span class="hlt">hydrological</span> models</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Jin, S. G.; Hassan, A. A.; Feng, G. P.</p> <p>2012-12-01</p> <p>The <span class="hlt">hydrological</span> contribution to polar motion is a major challenge in explaining the observed geodetic residual of non-atmospheric and non-oceanic excitations since <span class="hlt">hydrological</span> models have limited input of comprehensive global direct observations. Although global terrestrial water storage (TWS) estimated from the Gravity Recovery and Climate Experiment (GRACE) provides a new opportunity to study the <span class="hlt">hydrological</span> excitation of polar motion, the GRACE gridded data are subject to the post-processing de-striping algorithm, spatial gridded mapping and filter smoothing effects as well as aliasing errors. In this paper, the <span class="hlt">hydrological</span> contributions to polar motion are investigated and evaluated at seasonal and intra-seasonal time scales using the recovered degree-2 harmonic coefficients from all GRACE spherical harmonic coefficients and <span class="hlt">hydrological</span> models data with the same filter smoothing and recovering methods, including the Global Land Data Assimilation Systems (GLDAS) model, Climate <span class="hlt">Prediction</span> Center (CPC) model, the National Centers for Environmental <span class="hlt">Prediction</span>/National Center for Atmospheric Research (NCEP/NCAR) reanalysis products and European Center for Medium-Range Weather Forecasts (ECMWF) operational model (opECMWF). It is shown that GRACE is better in explaining the geodetic residual of non-atmospheric and non-oceanic polar motion excitations at the annual period, while the models give worse estimates with a larger phase shift or amplitude bias. At the semi-annual period, the GRACE estimates are also generally closer to the geodetic residual, but with some biases in phase or amplitude due mainly to some aliasing errors at near semi-annual period from geophysical models. For periods less than 1-year, the <span class="hlt">hydrological</span> models and GRACE are generally worse in explaining the intraseasonal polar motion excitations.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4579880','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4579880"><span><span class="hlt">Predictive</span> biomarkers of sorafenib efficacy in <span class="hlt">advanced</span> hepatocellular carcinoma: Are we getting there?</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Shao, Yu-Yun; Hsu, Chih-Hung; Cheng, Ann-Lii</p> <p>2015-01-01</p> <p>Sorafenib is the current standard treatment for <span class="hlt">advanced</span> hepatocellular carcinoma (HCC), but its efficacy is modest with low response rates and short response duration. <span class="hlt">Predictive</span> biomarkers for sorafenib efficacy are necessary. However, efforts to determine biomarkers for sorafenib have led only to potential candidates rather than clinically useful predictors. Studies based on patient cohorts identified the potential of blood levels of angiopoietin-2, hepatocyte growth factor, insulin-like growth factor-1, and transforming growth factor-β1 for <span class="hlt">predicting</span> sorafenib efficacy. Alpha-fetoprotein response, dynamic contrast-enhanced magnetic resonance imaging, and treatment-related side effects may serve as early surrogate markers. Novel approaches based on super-responders or experimental mouse models may provide new directions in biomarker research. These studies identified tumor amplification of FGF3/FGF4 or VEGFA and tumor expression of phospho-Mapk14 and phospho-Atf2 as possible <span class="hlt">predictive</span> markers that await validation. A group effort that considers various prognostic factors and proper collection of tumor tissues before treatment is imperative for the success of future biomarker research in <span class="hlt">advanced</span> HCC. PMID:26420960</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/26420960','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/26420960"><span><span class="hlt">Predictive</span> biomarkers of sorafenib efficacy in <span class="hlt">advanced</span> hepatocellular carcinoma: Are we getting there?</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Shao, Yu-Yun; Hsu, Chih-Hung; Cheng, Ann-Lii</p> <p>2015-09-28</p> <p>Sorafenib is the current standard treatment for <span class="hlt">advanced</span> hepatocellular carcinoma (HCC), but its efficacy is modest with low response rates and short response duration. <span class="hlt">Predictive</span> biomarkers for sorafenib efficacy are necessary. However, efforts to determine biomarkers for sorafenib have led only to potential candidates rather than clinically useful predictors. Studies based on patient cohorts identified the potential of blood levels of angiopoietin-2, hepatocyte growth factor, insulin-like growth factor-1, and transforming growth factor-β1 for <span class="hlt">predicting</span> sorafenib efficacy. Alpha-fetoprotein response, dynamic contrast-enhanced magnetic resonance imaging, and treatment-related side effects may serve as early surrogate markers. Novel approaches based on super-responders or experimental mouse models may provide new directions in biomarker research. These studies identified tumor amplification of FGF3/FGF4 or VEGFA and tumor expression of phospho-Mapk14 and phospho-Atf2 as possible <span class="hlt">predictive</span> markers that await validation. A group effort that considers various prognostic factors and proper collection of tumor tissues before treatment is imperative for the success of future biomarker research in <span class="hlt">advanced</span> HCC.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018WRR....54.2510M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018WRR....54.2510M"><span>Inspiring a Broader Socio-<span class="hlt">Hydrological</span> Negotiation Approach With Interdisciplinary Field-Based Experience</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Massuel, S.; Riaux, J.; Molle, F.; Kuper, M.; Ogilvie, A.; Collard, A.-L.; Leduc, C.; Barreteau, O.</p> <p>2018-04-01</p> <p>Socio-<span class="hlt">hydrology</span> <span class="hlt">advanced</span> the field of <span class="hlt">hydrology</span> by considering humans and their activities as part of the water cycle, rather than as external drivers. Models are used to infer reproducible trends in human interactions with water resources. However, defining and handling water problems in this way may restrict the scope of such modeling approaches. We propose an interdisciplinary socio-<span class="hlt">hydrological</span> approach to overcome this limit and complement modeling approaches. It starts from concrete field-based situations, combines disciplinary as well as local knowledge on water-society relationships, with the aim of broadening the hydrocentric analysis and modeling of water systems. The paper argues that an analysis of social dynamics linked to water is highly complementary to traditional <span class="hlt">hydrological</span> tools but requires a negotiated and contextualized interdisciplinary approach to the representation and analysis of socio-hydro systems. This reflection emerged from experience gained in the field where a water-budget modeling framework failed to adequately incorporate the multiplicity of (nonhydrological) factors that determine the volumes of withdrawals for irrigation. The pathway subsequently explored was to move away from the <span class="hlt">hydrologic</span> view of the phenomena and, in collaboration with social scientists, to produce a shared conceptualization of a coupled human-water system through a negotiated approach. This approach changed the way <span class="hlt">hydrological</span> research issues were addressed and limited the number of strong assumptions needed for simplification in modeling. The proposed socio-<span class="hlt">hydrological</span> approach led to a deeper understanding of the mechanisms behind local water-related problems and to debates on the interactions between social and political decisions and the dynamics of these problems.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://cfpub.epa.gov/si/si_public_record_report.cfm?dirEntryId=324712&Lab=NCEA&keyword=discrete&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=324712&Lab=NCEA&keyword=discrete&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">Hydrologic</span> Landscape Classification to Estimate Bristol Bay Watershed <span class="hlt">Hydrology</span></span></a></p> <p><a target="_blank" href="http://oaspub.epa.gov/eims/query.page">EPA Science Inventory</a></p> <p></p> <p></p> <p>The use of <span class="hlt">hydrologic</span> landscapes has proven to be a useful tool for broad scale assessment and classification of landscapes across the United States. These classification systems help organize larger geographical areas into areas of similar <span class="hlt">hydrologic</span> characteristics based on cl...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://cfpub.epa.gov/si/si_public_record_report.cfm?dirEntryId=318163&Lab=NHEERL&keyword=Clustering&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=318163&Lab=NHEERL&keyword=Clustering&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>On the Usefulness of <span class="hlt">Hydrologic</span> Landscapes for <span class="hlt">Hydrologic</span> Modeling and Water Management</span></a></p> <p><a target="_blank" href="http://oaspub.epa.gov/eims/query.page">EPA Science Inventory</a></p> <p></p> <p></p> <p><span class="hlt">Hydrologic</span> Landscapes (HLs) are units that can be used in aggregate to describe the watershed-scale <span class="hlt">hydrologic</span> response of an area through use of physical and climatic properties. The HL assessment unit is a useful classification tool to relate and transfer <span class="hlt">hydrologically</span> meaning...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://cfpub.epa.gov/si/si_public_record_report.cfm?dirEntryId=310709&Lab=NHEERL&keyword=Clustering&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=310709&Lab=NHEERL&keyword=Clustering&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>On the Usefulness of <span class="hlt">Hydrologic</span> Landscapes on <span class="hlt">Hydrologic</span> Model calibration and Selection</span></a></p> <p><a target="_blank" href="http://oaspub.epa.gov/eims/query.page">EPA Science Inventory</a></p> <p></p> <p></p> <p><span class="hlt">Hydrologic</span> Landscapes (HLs) are units that can be used in aggregate to describe the watershed-scale <span class="hlt">hydrologic</span> response of an area through use of physical and climatic properties. The HL assessment unit is a useful classification tool to relate and transfer <span class="hlt">hydrologically</span> meaning...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014cosp...40E3641W','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014cosp...40E3641W"><span><span class="hlt">Hydrological</span> excitation of polar motion by different variables of the GLDAS models</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Wińska, Małgorzata; Nastula, Jolanta</p> <p></p> <p>Continental <span class="hlt">hydrological</span> loading, by land water, snow, and ice, is an element that is strongly needed for a full understanding of the excitation of polar motion. In this study we compute different estimations of <span class="hlt">hydrological</span> excitation functions of polar motion (<span class="hlt">Hydrological</span> Angular Momentum - HAM) using various variables from the Global Land Data Assimilation System (GLDAS) models of land hydrosphere. The main aim of this study is to show the influence of different variables for example: total evapotranspiration, runoff, snowmelt, soil moisture to polar motion excitations in annual and short term scale. In our consideration we employ several realizations of the GLDAS model as: GLDAS Common Land Model (CLM), GLDAS Mosaic Model, GLDAS National Centers for Environmental <span class="hlt">Prediction</span>/Oregon State University/Air Force/<span class="hlt">Hydrologic</span> Research Lab Model (Noah), GLDAS Variable Infiltration Capacity (VIC) Model. <span class="hlt">Hydrological</span> excitation functions of polar motion, both global and regional, are determined by using selected variables of these GLDAS realizations. First we compare a timing, spectra and phase diagrams of different regional and global HAMs with each other. Next, we estimate, the <span class="hlt">hydrological</span> signal in geodetically observed polar motion excitation by subtracting the atmospheric -- AAM (pressure + wind) and oceanic -- OAM (bottom pressure + currents) contributions. Finally, the <span class="hlt">hydrological</span> excitations are compared to these <span class="hlt">hydrological</span> signal in observed polar motion excitation series. The results help us understand which variables of considered <span class="hlt">hydrological</span> models are the most important for the polar motion excitation and how well we can close polar motion excitation budget in the seasonal and inter-annual spectral ranges.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014AGUFM.H21F0785B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014AGUFM.H21F0785B"><span>Regionalisation of <span class="hlt">Hydrological</span> Indices to Assess Land-Use Change Impacts in the Tropical Andes</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Buytaert, W.; Ochoa Tocachi, B. F.</p> <p>2014-12-01</p> <p>Andean ecosystems are major water sources for cities and communities located in the Tropical Andes; however, there is a considerable lack of knowledge about their <span class="hlt">hydrology</span>. Two problems are especially important: (i) the lack of monitoring to assess the impacts of historical land-use and cover change and degradation (LUCCD) at catchment scale, and (ii) the high variability in climatic and <span class="hlt">hydrological</span> conditions that complicate the evaluation of land management practices. This study analyses how a reliable LUCCD impacts assessment can be performed in an environment of high variability combined with data-scarcity and low-quality records. We use data from participatory <span class="hlt">hydrological</span> monitoring activities in 20 catchments distributed along the tropical Andes. A set of 46 <span class="hlt">hydrological</span> indices is calculated and regionalized by relating them to 42 physical catchment properties. Principal Component Analysis (PCA) is performed to maximise available data while minimising redundancy in the sets of variables. <span class="hlt">Hydrological</span> model parameters are constrained by estimated indices, and different behavioural <span class="hlt">predictions</span> are assembled to provide a generalised response on which we assess LUCCD impacts. Results from this methodology show that the attributed effects of LUCCD in pair-wise catchment comparisons may be overstated or hidden by different sources of uncertainty, including measurement inaccuracies and model structural errors. We propose extrapolation and evaluation in ungauged catchments as a way to regionalize LUCCD <span class="hlt">predictions</span> and to provide statistically significant conclusions in the Andean region. These estimations may deliver reliable knowledge to evaluate the <span class="hlt">hydrological</span> impact of different watershed management practices.</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/2012AGUFM.H42C..04V','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012AGUFM.H42C..04V"><span>Balancing model complexity and measurements in <span class="hlt">hydrology</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Van De Giesen, N.; Schoups, G.; Weijs, S. V.</p> <p>2012-12-01</p> <p>The Data Processing Inequality implies that <span class="hlt">hydrological</span> modeling can only reduce, and never increase, the amount of information available in the original data used to formulate and calibrate <span class="hlt">hydrological</span> models: I(X;Z(Y)) ≤ I(X;Y). Still, hydrologists around the world seem quite content building models for "their" watersheds to move our discipline forward. <span class="hlt">Hydrological</span> models tend to have a hybrid character with respect to underlying physics. Most models make use of some well established physical principles, such as mass and energy balances. One could argue that such principles are based on many observations, and therefore add data. These physical principles, however, are applied to <span class="hlt">hydrological</span> models that often contain concepts that have no direct counterpart in the observable physical universe, such as "buckets" or "reservoirs" that fill up and empty out over time. These not-so-physical concepts are more like the Artificial Neural Networks and Support Vector Machines of the Artificial Intelligence (AI) community. Within AI, one quickly came to the realization that by increasing model complexity, one could basically fit any dataset but that complexity should be controlled in order to be able to <span class="hlt">predict</span> unseen events. The more data are available to train or calibrate the model, the more complex it can be. Many complexity control approaches exist in AI, with Solomonoff inductive inference being one of the first formal approaches, the Akaike Information Criterion the most popular, and Statistical Learning Theory arguably being the most comprehensive practical approach. In <span class="hlt">hydrology</span>, complexity control has hardly been used so far. There are a number of reasons for that lack of interest, the more valid ones of which will be presented during the presentation. For starters, there are no readily available complexity measures for our models. Second, some unrealistic simplifications of the underlying complex physics tend to have a smoothing effect on possible model</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016EGUGA..1812522A','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016EGUGA..1812522A"><span>Open <span class="hlt">hydrological</span> data at hypeweb.smhi.se</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Arheimer, Berit; Strömbäck, Lena; Andersson, Jafet; Donnelly, Chantal; Gustafsson, David; Pechlivianidis, Ilias; Strömqvist, Johan</p> <p>2016-04-01</p> <p>Following the EU open data strategy the Swedish Meteorological and <span class="hlt">Hydrological</span> Institute (SMHI) is providing large parts of the databases openly available. These data are ranging from historical observations to climate <span class="hlt">predictions</span> in various areas such as weather, oceanography and <span class="hlt">hydrology</span>. For the Water Service called Hypeweb (www.hypeweb.smhi.se), we provide data for water management. So far, the data has been used in: (i) Climate change impact assessments on water resources and dynamics; (ii) The European Water Framework Directive (WFD) for characterization and development of measure programs to improve the ecological status of water bodies; (iii) Design variables for infrastructure constructions; (iv) Spatial water-resource mapping; (v) Operational forecasts (1-10 days and seasonal) on floods and droughts; (vi) Input to oceanographic models for operational forecasts and marine status assessments; and (vii) Research. The data of Hypeweb is based on other open data sources that has been merged and re-purposed by using the <span class="hlt">Hydrological</span> <span class="hlt">Predictions</span> for the Environment (HYPE) model in world-wide applications with high resolution. HYPE is a dynamic, semi-distributed, process-based, and integrated catchment model. So far, the following regional domains have been modelled with different resolutions (number of subbasins within brackets): Sweden (37 000), Europe (35 000), Arctic basin (30 000), La Plata River (6 000), Niger River (800), Middle-East North-Africa (31 000), and the Indian subcontinent (6 000). The web site provides several interactive applications for exploring results from the models. The user can explore an overview of various water variables for historical and future conditions. Moreover the user can explore and download historical time series of discharge for each basin and explore the performance of the model towards observed river flow. The presentation will give an overview of the functionality of the web site and the available <span class="hlt">hydrological</span></p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://rosap.ntl.bts.gov/view/dot/32743','DOTNTL'); return false;" href="https://rosap.ntl.bts.gov/view/dot/32743"><span>Improving <span class="hlt">hydrologic</span> disaster forecasting and response for transportation by assimilating and fusing NASA and other data sets : final report.</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>2017-04-15</p> <p>In this 3-year project, the research team developed the <span class="hlt">Hydrologic</span> Disaster Forecast and Response (HDFR) system, a set of integrated software tools for end users that streamlines <span class="hlt">hydrologic</span> <span class="hlt">prediction</span> workflows involving automated retrieval of hetero...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017EGUGA..1915719A','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017EGUGA..1915719A"><span>A framework for improving a seasonal <span class="hlt">hydrological</span> forecasting system using sensitivity analysis</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Arnal, Louise; Pappenberger, Florian; Smith, Paul; Cloke, Hannah</p> <p>2017-04-01</p> <p>Seasonal streamflow forecasts are of great value for the socio-economic sector, for applications such as navigation, flood and drought mitigation and reservoir management for hydropower generation and water allocation to agriculture and drinking water. However, as we speak, the performance of dynamical seasonal <span class="hlt">hydrological</span> forecasting systems (systems based on running seasonal meteorological forecasts through a <span class="hlt">hydrological</span> model to produce seasonal <span class="hlt">hydrological</span> forecasts) is still limited in space and time. In this context, the ESP (Ensemble Streamflow <span class="hlt">Prediction</span>) remains an attractive forecasting method for seasonal streamflow forecasting as it relies on forcing a <span class="hlt">hydrological</span> model (starting from the latest observed or simulated initial <span class="hlt">hydrological</span> conditions) with historical meteorological observations. This makes it cheaper to run than a standard dynamical seasonal <span class="hlt">hydrological</span> forecasting system, for which the seasonal meteorological forecasts will first have to be produced, while still producing skilful forecasts. There is thus the need to focus resources and time towards improvements in dynamical seasonal <span class="hlt">hydrological</span> forecasting systems which will eventually lead to significant improvements in the skill of the streamflow forecasts generated. Sensitivity analyses are a powerful tool that can be used to disentangle the relative contributions of the two main sources of errors in seasonal streamflow forecasts, namely the initial <span class="hlt">hydrological</span> conditions (IHC; e.g., soil moisture, snow cover, initial streamflow, among others) and the meteorological forcing (MF; i.e., seasonal meteorological forecasts of precipitation and temperature, input to the <span class="hlt">hydrological</span> model). Sensitivity analyses are however most useful if they inform and change current operational practices. To this end, we propose a method to improve the design of a seasonal <span class="hlt">hydrological</span> forecasting system. This method is based on sensitivity analyses, informing the forecasters as to which element of</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2011WRR....4712529F','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2011WRR....4712529F"><span>Using discharge data to reduce structural deficits in a <span class="hlt">hydrological</span> model with a Bayesian inference approach and the implications for the <span class="hlt">prediction</span> of critical source areas</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Frey, M. P.; Stamm, C.; Schneider, M. K.; Reichert, P.</p> <p>2011-12-01</p> <p>A distributed <span class="hlt">hydrological</span> model was used to simulate the distribution of fast runoff formation as a proxy for critical source areas for herbicide pollution in a small agricultural catchment in Switzerland. We tested to what degree <span class="hlt">predictions</span> based on prior knowledge without local measurements could be improved upon relying on observed discharge. This learning process consisted of five steps: For the prior <span class="hlt">prediction</span> (step 1), knowledge of the model parameters was coarse and <span class="hlt">predictions</span> were fairly uncertain. In the second step, discharge data were used to update the prior parameter distribution. Effects of uncertainty in input data and model structure were accounted for by an autoregressive error model. This step decreased the width of the marginal distributions of parameters describing the lower boundary (percolation rates) but hardly affected soil hydraulic parameters. Residual analysis (step 3) revealed model structure deficits. We modified the model, and in the subsequent Bayesian updating (step 4) the widths of the posterior marginal distributions were reduced for most parameters compared to those of the prior. This incremental procedure led to a strong reduction in the uncertainty of the spatial <span class="hlt">prediction</span>. Thus, despite only using spatially integrated data (discharge), the spatially distributed effect of the improved model structure can be expected to improve the spatially distributed <span class="hlt">predictions</span> also. The fifth step consisted of a test with independent spatial data on herbicide losses and revealed ambiguous results. The comparison depended critically on the ratio of event to preevent water that was discharged. This ratio cannot be estimated from <span class="hlt">hydrological</span> data only. The results demonstrate that the value of local data is strongly dependent on a correct model structure. An iterative procedure of Bayesian updating, model testing, and model modification is suggested.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012AGUFM.H11J..06C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012AGUFM.H11J..06C"><span>National-Scale <span class="hlt">Hydrologic</span> Classification & Agricultural Decision Support: A Multi-Scale Approach</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Coopersmith, E. J.; Minsker, B.; Sivapalan, M.</p> <p>2012-12-01</p> <p>Classification frameworks can help organize catchments exhibiting similarity in <span class="hlt">hydrologic</span> and climatic terms. Focusing this assessment of "similarity" upon specific <span class="hlt">hydrologic</span> signatures, in this case the annual regime curve, can facilitate the <span class="hlt">prediction</span> of <span class="hlt">hydrologic</span> responses. Agricultural decision-support over a diverse set of catchments throughout the United States depends upon successful modeling of the wetting/drying process without necessitating separate model calibration at every site where such insights are required. To this end, a holistic classification framework is developed to describe both climatic variability (humid vs. arid, winter rainfall vs. summer rainfall) and the draining, storing, and filtering behavior of any catchment, including ungauged or minimally gauged basins. At the national scale, over 400 catchments from the MOPEX database are analyzed to construct the classification system, with over 77% of these catchments ultimately falling into only six clusters. At individual locations, soil moisture models, receiving only rainfall as input, produce correlation values in excess of 0.9 with respect to observed soil moisture measurements. By deploying physical models for <span class="hlt">predicting</span> soil moisture exclusively from precipitation that are calibrated at gauged locations, overlaying machine learning techniques to improve these estimates, then generalizing the calibration parameters for catchments in a given class, agronomic decision-support becomes available where it is needed rather than only where sensing data are located.lassifications of 428 U.S. catchments on the basis of <span class="hlt">hydrologic</span> regime data, Coopersmith et al, 2012.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2011AGUFM.H13D1246G','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2011AGUFM.H13D1246G"><span>Characterizing Satellite Rainfall Errors based on Land Use and Land Cover and Tracing Error Source in <span class="hlt">Hydrologic</span> 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>Gebregiorgis, A. S.; Peters-Lidard, C. D.; Tian, Y.; Hossain, F.</p> <p>2011-12-01</p> <p><span class="hlt">Hydrologic</span> modeling has benefited from operational production of high resolution satellite rainfall products. The global coverage, near-real time availability, spatial and temporal sampling resolutions have <span class="hlt">advanced</span> the application of physically based semi-distributed and distributed <span class="hlt">hydrologic</span> models for wide range of environmental decision making processes. Despite these successes, the existence of uncertainties due to indirect way of satellite rainfall estimates and <span class="hlt">hydrologic</span> models themselves remain a challenge in making meaningful and more evocative <span class="hlt">predictions</span>. This study comprises breaking down of total satellite rainfall error into three independent components (hit bias, missed precipitation and false alarm), characterizing them as function of land use and land cover (LULC), and tracing back the source of simulated soil moisture and runoff error in physically based distributed <span class="hlt">hydrologic</span> model. Here, we asked "on what way the three independent total bias components, hit bias, missed, and false precipitation, affect the estimation of soil moisture and runoff in physically based <span class="hlt">hydrologic</span> models?" To understand the clear picture of the outlined question above, we implemented a systematic approach by characterizing and decomposing the total satellite rainfall error as a function of land use and land cover in Mississippi basin. This will help us to understand the major source of soil moisture and runoff errors in <span class="hlt">hydrologic</span> model simulation and trace back the information to algorithm development and sensor type which ultimately helps to improve algorithms better and will improve application and data assimilation in future for GPM. For forest and woodland and human land use system, the soil moisture was mainly dictated by the total bias for 3B42-RT, CMORPH, and PERSIANN products. On the other side, runoff error was largely dominated by hit bias than the total bias. This difference occurred due to the presence of missed precipitation which is a major</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://cfpub.epa.gov/si/si_public_record_report.cfm?dirEntryId=311854&keyword=windows&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=311854&keyword=windows&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>Stream <span class="hlt">hydrologic</span> response to increased urbanization in Mid-Atlantic watersheds</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>Urban development alters stream <span class="hlt">hydrology</span>; resulting in increases in the Richard-Baker Flashiness index, peak flow, and the number of flood events for many watersheds throughout the U.S. To better understand and <span class="hlt">predict</span> the relationship between stream flow patterns and watershed ...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/pages/biblio/1438145-approach-quantum-computational-hydrologic-inverse-analysis','SCIGOV-DOEP'); return false;" href="https://www.osti.gov/pages/biblio/1438145-approach-quantum-computational-hydrologic-inverse-analysis"><span>An approach to quantum-computational <span class="hlt">hydrologic</span> inverse analysis</span></a></p> <p><a target="_blank" href="http://www.osti.gov/pages">DOE PAGES</a></p> <p>O'Malley, Daniel</p> <p>2018-05-02</p> <p>Making <span class="hlt">predictions</span> about flow and transport in an aquifer requires knowledge of the heterogeneous properties of the aquifer such as permeability. Computational methods for inverse analysis are commonly used to infer these properties from quantities that are more readily observable such as hydraulic head. We present a method for computational inverse analysis that utilizes a type of quantum computer called a quantum annealer. While quantum computing is in an early stage compared to classical computing, we demonstrate that it is sufficiently developed that it can be used to solve certain subsurface flow problems. We utilize a D-Wave 2X quantum annealermore » to solve 1D and 2D <span class="hlt">hydrologic</span> inverse problems that, while small by modern standards, are similar in size and sometimes larger than <span class="hlt">hydrologic</span> inverse problems that were solved with early classical computers. Our results and the rapid progress being made with quantum computing hardware indicate that the era of quantum-computational <span class="hlt">hydrology</span> may not be too far in the future.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/servlets/purl/1438145','SCIGOV-STC'); return false;" href="https://www.osti.gov/servlets/purl/1438145"><span>An approach to quantum-computational <span class="hlt">hydrologic</span> inverse analysis</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>O'Malley, Daniel</p> <p></p> <p>Making <span class="hlt">predictions</span> about flow and transport in an aquifer requires knowledge of the heterogeneous properties of the aquifer such as permeability. Computational methods for inverse analysis are commonly used to infer these properties from quantities that are more readily observable such as hydraulic head. We present a method for computational inverse analysis that utilizes a type of quantum computer called a quantum annealer. While quantum computing is in an early stage compared to classical computing, we demonstrate that it is sufficiently developed that it can be used to solve certain subsurface flow problems. We utilize a D-Wave 2X quantum annealermore » to solve 1D and 2D <span class="hlt">hydrologic</span> inverse problems that, while small by modern standards, are similar in size and sometimes larger than <span class="hlt">hydrologic</span> inverse problems that were solved with early classical computers. Our results and the rapid progress being made with quantum computing hardware indicate that the era of quantum-computational <span class="hlt">hydrology</span> may not be too far in the future.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/1990EOSTr..71Q.998.','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/1990EOSTr..71Q.998."><span>1990 <span class="hlt">Hydrology</span> Prize awarded</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p></p> <p></p> <p>The International Association of <span class="hlt">Hydrological</span> Sciences awarded its 1990 International <span class="hlt">Hydrology</span> Prize to Z. Kaczmarek of Warsaw, Poland. The award was presented on March 16 in Paris, France, during Unesco's Commemorative Symposium on 25 Years of the International <span class="hlt">Hydrological</span> Decade/International <span class="hlt">Hydrological</span> Program.The IAHS International <span class="hlt">Hydrology</span> Prize, a silver medal, was first approved in 1979 as an annual award to a person who has made an outstanding contribution to <span class="hlt">hydrology</span> and gives the candidate universal recognition of his international stature. The IAHS national committees give nominations to the IAHS Secretary General for consideration by a nominating committee, which consists of the IAHS president, the first and second vice presidents and representatives of Unesco and the World Meteorological Organization. The citation for the award to Kaczmarek, which was given by IAHS president Vit Klemes, follows.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015EGUGA..17.2394H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015EGUGA..17.2394H"><span>On how to avoid input and structural uncertainties corrupt the inference of <span class="hlt">hydrological</span> parameters using a Bayesian framework</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Hernández, Mario R.; Francés, Félix</p> <p>2015-04-01</p> <p>One phase of the <span class="hlt">hydrological</span> models implementation process, significantly contributing to the <span class="hlt">hydrological</span> <span class="hlt">predictions</span> uncertainty, is the calibration phase in which values of the unknown model parameters are tuned by optimizing an objective function. An unsuitable error model (e.g. Standard Least Squares or SLS) introduces noise into the estimation of the parameters. The main sources of this noise are the input errors and the <span class="hlt">hydrological</span> model structural deficiencies. Thus, the biased calibrated parameters cause the divergence model phenomenon, where the errors variance of the (spatially and temporally) forecasted flows far exceeds the errors variance in the fitting period, and provoke the loss of part or all of the physical meaning of the modeled processes. In other words, yielding a calibrated <span class="hlt">hydrological</span> model which works well, but not for the right reasons. Besides, an unsuitable error model yields a non-reliable <span class="hlt">predictive</span> uncertainty assessment. Hence, with the aim of prevent all these undesirable effects, this research focuses on the Bayesian joint inference (BJI) of both the <span class="hlt">hydrological</span> and error model parameters, considering a general additive (GA) error model that allows for correlation, non-stationarity (in variance and bias) and non-normality of model residuals. As <span class="hlt">hydrological</span> model, it has been used a conceptual distributed model called TETIS, with a particular split structure of the effective model parameters. Bayesian inference has been performed with the aid of a Markov Chain Monte Carlo (MCMC) algorithm called Dream-ZS. MCMC algorithm quantifies the uncertainty of the <span class="hlt">hydrological</span> and error model parameters by getting the joint posterior probability distribution, conditioned on the observed flows. The BJI methodology is a very powerful and reliable tool, but it must be used correctly this is, if non-stationarity in errors variance and bias is modeled, the Total Laws must be taken into account. The results of this research show that the</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.fs.usda.gov/treesearch/pubs/25345','TREESEARCH'); return false;" href="https://www.fs.usda.gov/treesearch/pubs/25345"><span>Modeling <span class="hlt">hydrology</span> and in-stream transport on drained forested lands in coastal Carolinas, U.S.A.</span></a></p> <p><a target="_blank" href="http://www.fs.usda.gov/treesearch/">Treesearch</a></p> <p>Devendra Amatya</p> <p>2005-01-01</p> <p>This study summarizes the successional development and testing of forest <span class="hlt">hydrologic</span> models based on DRAINMOD that <span class="hlt">predicts</span> the <span class="hlt">hydrology</span> of low-gradient poorly drained watersheds as affected by land management and climatic variation. The field scale (DRAINLOB) and watershed-scale in-stream routing (DRAINWAT) models were successfully tested with water table and outflow...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2010EGUGA..12.5280R','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2010EGUGA..12.5280R"><span>Communicating uncertainty in <span class="hlt">hydrological</span> forecasts: mission impossible?</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Ramos, Maria-Helena; Mathevet, Thibault; Thielen, Jutta; Pappenberger, Florian</p> <p>2010-05-01</p> <p>Cascading uncertainty in meteo-<span class="hlt">hydrological</span> modelling chains for forecasting and integrated flood risk assessment is an essential step to improve the quality of <span class="hlt">hydrological</span> forecasts. Although the best methodology to quantify the total <span class="hlt">predictive</span> uncertainty in <span class="hlt">hydrology</span> is still debated, there is a common agreement that one must avoid uncertainty misrepresentation and miscommunication, as well as misinterpretation of information by users. Several recent studies point out that uncertainty, when properly explained and defined, is no longer unwelcome among emergence response organizations, users of flood risk information and the general public. However, efficient communication of uncertain hydro-meteorological forecasts is far from being a resolved issue. This study focuses on the interpretation and communication of uncertain <span class="hlt">hydrological</span> forecasts based on (uncertain) meteorological forecasts and (uncertain) rainfall-runoff modelling approaches to decision-makers such as operational hydrologists and water managers in charge of flood warning and scenario-based reservoir operation. An overview of the typical flow of uncertainties and risk-based decisions in <span class="hlt">hydrological</span> forecasting systems is presented. The challenges related to the extraction of meaningful information from probabilistic forecasts and the test of its usefulness in assisting operational flood forecasting are illustrated with the help of two case-studies: 1) a study on the use and communication of probabilistic flood forecasting within the European Flood Alert System; 2) a case-study on the use of probabilistic forecasts by operational forecasters from the hydroelectricity company EDF in France. These examples show that attention must be paid to initiatives that promote or reinforce the active participation of expert forecasters in the forecasting chain. The practice of face-to-face forecast briefings, focusing on sharing how forecasters interpret, describe and perceive the model output forecasted</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29079764','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29079764"><span><span class="hlt">Prediction</span> of Indian Summer-Monsoon Onset Variability: A Season in <span class="hlt">Advance</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Pradhan, Maheswar; Rao, A Suryachandra; Srivastava, Ankur; Dakate, Ashish; Salunke, Kiran; Shameera, K S</p> <p>2017-10-27</p> <p>Monsoon onset is an inherent transient phenomenon of Indian Summer Monsoon and it was never envisaged that this transience can be <span class="hlt">predicted</span> at long lead times. Though onset is precipitous, its variability exhibits strong teleconnections with large scale forcing such as ENSO and IOD and hence may be <span class="hlt">predictable</span>. Despite of the tremendous skill achieved by the state-of-the-art models in <span class="hlt">predicting</span> such large scale processes, the <span class="hlt">prediction</span> of monsoon onset variability by the models is still limited to just 2-3 weeks in <span class="hlt">advance</span>. Using an objective definition of onset in a global coupled ocean-atmosphere model, it is shown that the skillful <span class="hlt">prediction</span> of onset variability is feasible under seasonal <span class="hlt">prediction</span> framework. The better representations/simulations of not only the large scale processes but also the synoptic and intraseasonal features during the evolution of monsoon onset are the comprehensions behind skillful simulation of monsoon onset variability. The changes observed in convection, tropospheric circulation and moisture availability prior to and after the onset are evidenced in model simulations, which resulted in high hit rate of early/delay in monsoon onset in the high resolution model.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2004AGUSM.H24B..04H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2004AGUSM.H24B..04H"><span>Designing Observatories for the <span class="hlt">Hydrologic</span> Sciences</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Hooper, R. P.</p> <p>2004-05-01</p> <p>The need for longer-term, multi-scale, coherent, and multi-disciplinary data to test hypotheses in <span class="hlt">hydrologic</span> science has been recognized by numerous prestigious review panels over the past decade (e.g. NRC's Basic Research Opportunities in Earth Science). Designing such observatories has proven to be a challenge not only on scientific, but also technological, economic and even sociologic levels. The Consortium of Universities for the <span class="hlt">Advancement</span> of <span class="hlt">Hydrologic</span> Science, Inc. (CUAHSI) has undertaken a "paper" prototype design of a <span class="hlt">hydrologic</span> observatory (HO) for the Neuse River Basin, NC and plans to solicit proposals and award grants to develop implementation plans for approximately 10 basins (which may be defined by topographic or groundwater divides) during the summer of 2004. These observatories are envisioned to be community resources with data available to all scientists, with support facilities to permit their use by both local and remote investigators. This paper presents the broad design concepts which were developed from a national team of scientists for the Neuse River Basin Prototype. There are three fundamental characteristics of a watershed or river basin that are critical for answering the major scientific questions proposed by the NRC to <span class="hlt">advance</span> <span class="hlt">hydrologic</span>, biogeochemical and ecological sciences: (1) the store and flux of water, sediment, nutrients and contaminants across interfaces at multiple scales must be identified; (2) the residence time of these constituents, and (3) their flowpaths and response spectra to forcing must be estimated. "Stores" consist of subsurface, land surface and atmospheric volumes partitioned over the watershed. The HO will require "core measurements" which will serve the communities of <span class="hlt">hydrologic</span> science for long range research questions. The core measurements will also provide context for shorter-term or hypothesis-driven research investigations. The HO will support "mobile measurement facilities" designed to support teams</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014NHESS..14.1417E','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014NHESS..14.1417E"><span>Flood design recipes vs. reality: can <span class="hlt">predictions</span> for ungauged basins be trusted?</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Efstratiadis, A.; Koussis, A. D.; Koutsoyiannis, D.; Mamassis, N.</p> <p>2014-06-01</p> <p>Despite the great scientific and technological <span class="hlt">advances</span> in flood <span class="hlt">hydrology</span>, everyday engineering practices still follow simplistic approaches that are easy to formally implement in ungauged areas. In general, these "recipes" have been developed many decades ago, based on field data from typically few experimental catchments. However, many of them have been neither updated nor validated across all hydroclimatic and geomorphological conditions. This has an obvious impact on the quality and reliability of <span class="hlt">hydrological</span> studies, and, consequently, on the safety and cost of the related flood protection works. Preliminary results, based on historical flood data from Cyprus and Greece, indicate that a substantial revision of many aspects of flood engineering procedures is required, including the regionalization formulas as well as the modelling concepts themselves. In order to provide a consistent design framework and to ensure realistic <span class="hlt">predictions</span> of the flood risk (a key issue of the 2007/60/EU Directive) in ungauged basins, it is necessary to rethink the current engineering practices. In this vein, the collection of reliable <span class="hlt">hydrological</span> data would be essential for re-evaluating the existing "recipes", taking into account local peculiarities, and for updating the modelling methodologies as needed.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/1992STIN...9223119T','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/1992STIN...9223119T"><span>Measured and <span class="hlt">predicted</span> rotor performance for the SERI <span class="hlt">advanced</span> wind turbine blades</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Tangler, J.; Smith, B.; Kelley, N.; Jager, D.</p> <p>1992-02-01</p> <p>Measured and <span class="hlt">predicted</span> rotor performance for the Solar Energy Research Institute (SERI) <span class="hlt">advanced</span> wind turbine blades were compared to assess the accuracy of <span class="hlt">predictions</span> and to identify the sources of error affecting both <span class="hlt">predictions</span> and measurements. An awareness of these sources of error contributes to improved <span class="hlt">prediction</span> and measurement methods that will ultimately benefit future rotor design efforts. Propeller/vane anemometers were found to underestimate the wind speed in turbulent environments such as the San Gorgonio Pass wind farm area. Using sonic or cup anemometers, good agreement was achieved between <span class="hlt">predicted</span> and measured power output for wind speeds up to 8 m/sec. At higher wind speeds an optimistic <span class="hlt">predicted</span> power output and the occurrence of peak power at wind speeds lower than measurements resulted from the omission of turbulence and yaw error. In addition, accurate two-dimensional (2-D) airfoil data prior to stall and a post stall airfoil data synthesization method that reflects three-dimensional (3-D) effects were found to be essential for accurate performance <span class="hlt">prediction</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/26860846','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/26860846"><span>Modified CLIP with objective liver reserve assessment retains prognosis <span class="hlt">prediction</span> for patients with <span class="hlt">advanced</span> hepatocellular carcinoma.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Shao, Yu-Yun; Liu, Tsung-Hao; Lee, Ying-Hui; Hsu, Chih-Hung; Cheng, Ann-Lii</p> <p>2016-07-01</p> <p>The Cancer of the Liver Italian Program (CLIP) score is a commonly used staging system for hepatocellular carcinoma (HCC) helpful with <span class="hlt">predicting</span> prognosis of <span class="hlt">advanced</span> HCC. CLIP uses the Child-Turcotte-Pugh (CTP) score to evaluate liver reserve. A new scoring system, the albumin-bilirubin (ALBI) grade, has been proposed as they objectively evaluate liver reserve. We examined whether the modification of CLIP with ALBI retained its prognosis <span class="hlt">prediction</span> for patients with <span class="hlt">advanced</span> HCC. We included patients who received first-line antiangiogenic therapy for <span class="hlt">advanced</span> HCC. Liver reserve was assessed using CTP and ALBI scores, which were then incorporated into CLIP and ALBI-CLIP, respectively. To assess their efficacies of prognostic <span class="hlt">prediction</span>, the Cox's proportional hazard model and concordance indexes were used. A total of 142 patients were included; 137 of them were classified CTP A and 5 patients CTP B. Patients could be divided into four or five groups with different prognosis according to CLIP and ALBI-CLIP, respectively. Higher R(2) (0.249 vs 0.216) and lower Akaike information criterion (995.0 vs 1001.1) were observed for ALBI-CLIP than for CLIP in the Cox's model <span class="hlt">predicting</span> overall survival. ALBI-CLIP remained an independent predictor for overall survival when CLIP and ALBI-CLIP were simultaneously incorporated in Cox's models allowing variable selection with adjustment for hepatitis etiology, treatment, and performance status. The concordance index was also higher for ALBI-CLIP than for CLIP (0.724 vs 0.703). Modification of CLIP scoring with ALBI, which objectively assesses liver reserve, retains and might have improved prognosis <span class="hlt">prediction</span> for <span class="hlt">advanced</span> HCC. © 2016 Journal of Gastroenterology and Hepatology Foundation and John Wiley & Sons Australia, Ltd.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012AGUFM.H13J..05G','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012AGUFM.H13J..05G"><span><span class="hlt">Hydrological</span> research in Ethiopia</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Gebremichael, M.</p> <p>2012-12-01</p> <p>Almost all major development problems in Ethiopia are water-related: food insecurity, low economic development, recurrent droughts, disastrous floods, poor health conditions, and low energy condition. In order to develop and manage existing water resources in a sustainable manner, knowledge is required about water availability, water quality, water demand in various sectors, and the impacts of water resource projects on health and the environment. The lack of ground-based data has been a major challenge for generating this knowledge. Current <span class="hlt">advances</span> in remote sensing and computer simulation technology could provide alternative source of datasets. In this talk, I will present the challenges and opportunities in using remote sensing datasets and <span class="hlt">hydrological</span> models in regions such as Africa where ground-based datasets are scarce.</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('http://adsabs.harvard.edu/abs/2011WRR....47.9510K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2011WRR....47.9510K"><span><span class="hlt">Predicting</span> foraging wading bird populations in Everglades National Park from seasonal <span class="hlt">hydrologic</span> statistics under different management scenarios</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Kwon, Hyun-Han; Lall, Upmanu; Engel, Vic</p> <p>2011-09-01</p> <p>The ability to map relationships between ecological outcomes and <span class="hlt">hydrologic</span> conditions in the Everglades National Park (ENP) is a key building block for their restoration program, a primary goal of which is to improve conditions for wading birds. This paper presents a model linking wading bird foraging numbers to <span class="hlt">hydrologic</span> conditions in the ENP. Seasonal <span class="hlt">hydrologic</span> statistics derived from a single water level recorder are well correlated with water depths throughout most areas of the ENP, and are effective as predictors of wading bird numbers when using a nonlinear hierarchical Bayesian model to estimate the conditional distribution of bird populations. Model parameters are estimated using a Markov chain Monte Carlo (MCMC) procedure. Parameter and model uncertainty is assessed as a byproduct of the estimation process. Water depths at the beginning of the nesting season, the average dry season water level, and the numbers of reversals from the dry season recession are identified as significant predictors, consistent with the <span class="hlt">hydrologic</span> conditions considered important in the production and concentration of prey organisms in this system. Long-term <span class="hlt">hydrologic</span> records at the index location allow for a retrospective analysis (1952-2006) of foraging bird numbers showing low frequency oscillations in response to decadal fluctuations in hydroclimatic conditions. Simulations of water levels at the index location used in the Bayesian model under alternative water management scenarios allow the posterior probability distributions of the number of foraging birds to be compared, thus providing a mechanism for linking management schemes to seasonal rainfall forecasts.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2010AGUFMEP41B0693B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2010AGUFMEP41B0693B"><span>How Does Decommissioning Forest Roads Effect <span class="hlt">Hydrologic</span> and Geomorphic Risk?</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Black, T.; Luce, C.; Cissel, R. M.; Nelson, N.; Staab, B.</p> <p>2010-12-01</p> <p>The US Forest Service is investigating road decommissioning projects to understand how treatments change <span class="hlt">hydrologic</span> and geomorphic risks. Road treatment effect was measured using a before after control impact design (BACI), using the Geomorphic Road Analysis and Inventory Package (http://www.fs.fed.us/GRAIP). This suite of inventory and analysis tools evaluates: road-stream <span class="hlt">hydrologic</span> connectivity, fine sediment production and delivery, shallow landslide risk, gully initiation risk, and risks associated with stream crossing failures. The Skokomish River study site is steep and wet and received a high intensity treatment including the removal of stream crossing pipes and fills, all ditch relief pipes and a full hillslope recontouring. Road to stream <span class="hlt">hydrologic</span> connectivity was reduced by 70%. The treatments reduced fine sediment delivery by 21.8 tons or 81%. The removal of the stream crossing culverts and large associated road fills eliminated the risk of pipe plugging related failures and the eventual erosion of over 4,000 m3 of fill. The slope stability risk was assessed using a modified version of SINMAP (Pack et al, 2005). Risk below drain point locations on the original road was reduced as water was redistributed across the hillslope to waterbars and diffuse drainage. It is unclear; however, if landslide risk was reduced across the entire treated road length because treatments slightly increased risk in some areas where new concentrated drainage features were added above steep slopes. Similarly, values of a gully index ESI (Istanbulluoglu et al, 2003), were reduced at many of the original drainage points, however some new drainage was added. ESI values still exceed a <span class="hlt">predicted</span> conservative initiation thresholds at some sites, therefore it is uncertain if gully risk will be changed. Mann Creek occupies a moderately steep mid-elevation site in Southern Idaho. The high intensity treatments removed all constructed road drainage features including stream crossing</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://pubs.water.usgs.gov/wsp2294','USGSPUBS'); return false;" href="http://pubs.water.usgs.gov/wsp2294"><span><span class="hlt">Hydrologic</span> unit maps</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Seaber, Paul R.; Kapinos, F. Paul; Knapp, George L.</p> <p>1987-01-01</p> <p>A set of maps depicting approved boundaries of, and numerical codes for, river-basin units of the United States has been developed by the U.S . Geological Survey. These '<span class="hlt">Hydrologic</span> Unit Maps' are four-color maps that present information on drainage, culture, hydrography, and <span class="hlt">hydrologic</span> boundaries and codes of (1) the 21 major water-resources regions and the 222 subregions designated by the U.S . Water Resources Council, (2) the 352 accounting units of the U.S. Geological Survey's National Water Data Network, and (3) the 2,149 cataloging units of the U.S . Geological Survey's 'Catalog of information on Water Data:' The maps are plotted on the Geological Survey State base-map series at a scale of 1 :500,000 and, except for Alaska, depict <span class="hlt">hydrologic</span> unit boundaries for all drainage basins greater than 700 square miles (1,813 square kilometers). A complete list of all the <span class="hlt">hydrologic</span> units, along with their drainage areas, their names, and the names of the States or outlying areas in which they reside, is contained in the report. These maps and associated codes provide a standardized base for use by water-resources organizations in locating, storing, retrieving, and exchanging <span class="hlt">hydrologic</span> data, in indexing and inventorying <span class="hlt">hydrologic</span> data and information, in cataloging water-data acquisition activities, and in a variety of other applications. Because the maps have undergone extensive review by all principal Federal, regional, and State water-resource agencies, they are widely accepted for use in planning and describing water-use and related land-use activities, and in geographically organizing <span class="hlt">hydrologic</span> data . Examples of these uses are given in the report . The <span class="hlt">hydrologic</span> unit codes shown on the maps have been approved as a Federal Information Processing Standard for use by the Federal establishment.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/27783639','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/27783639"><span>Genomic <span class="hlt">Prediction</span> of Seed Quality Traits Using <span class="hlt">Advanced</span> Barley Breeding Lines.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Nielsen, Nanna Hellum; Jahoor, Ahmed; Jensen, Jens Due; Orabi, Jihad; Cericola, Fabio; Edriss, Vahid; Jensen, Just</p> <p>2016-01-01</p> <p>Genomic selection was recently introduced in plant breeding. The objective of this study was to develop genomic <span class="hlt">prediction</span> for important seed quality parameters in spring barley. The aim was to <span class="hlt">predict</span> breeding values without expensive phenotyping of large sets of lines. A total number of 309 <span class="hlt">advanced</span> spring barley lines tested at two locations each with three replicates were phenotyped and each line was genotyped by Illumina iSelect 9Kbarley chip. The population originated from two different breeding sets, which were phenotyped in two different years. Phenotypic measurements considered were: seed size, protein content, protein yield, test weight and ergosterol content. A leave-one-out cross-validation strategy revealed high <span class="hlt">prediction</span> accuracies ranging between 0.40 and 0.83. <span class="hlt">Prediction</span> across breeding sets resulted in reduced accuracies compared to the leave-one-out strategy. Furthermore, <span class="hlt">predicting</span> across full and half-sib-families resulted in reduced <span class="hlt">prediction</span> accuracies. Additionally, <span class="hlt">predictions</span> were performed using reduced marker sets and reduced training population sets. In conclusion, using less than 200 lines in the training set can result in low <span class="hlt">prediction</span> accuracy, and the accuracy will then be highly dependent on the family structure of the selected training set. However, the results also indicate that relatively small training sets (200 lines) are sufficient for genomic <span class="hlt">prediction</span> in commercial barley breeding. In addition, our results indicate a minimum marker set of 1,000 to decrease the risk of low <span class="hlt">prediction</span> accuracy for some traits or some families.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5082657','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5082657"><span>Genomic <span class="hlt">Prediction</span> of Seed Quality Traits Using <span class="hlt">Advanced</span> Barley Breeding Lines</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Nielsen, Nanna Hellum; Jahoor, Ahmed; Jensen, Jens Due; Orabi, Jihad; Cericola, Fabio; Edriss, Vahid; Jensen, Just</p> <p>2016-01-01</p> <p>Genomic selection was recently introduced in plant breeding. The objective of this study was to develop genomic <span class="hlt">prediction</span> for important seed quality parameters in spring barley. The aim was to <span class="hlt">predict</span> breeding values without expensive phenotyping of large sets of lines. A total number of 309 <span class="hlt">advanced</span> spring barley lines tested at two locations each with three replicates were phenotyped and each line was genotyped by Illumina iSelect 9Kbarley chip. The population originated from two different breeding sets, which were phenotyped in two different years. Phenotypic measurements considered were: seed size, protein content, protein yield, test weight and ergosterol content. A leave-one-out cross-validation strategy revealed high <span class="hlt">prediction</span> accuracies ranging between 0.40 and 0.83. <span class="hlt">Prediction</span> across breeding sets resulted in reduced accuracies compared to the leave-one-out strategy. Furthermore, <span class="hlt">predicting</span> across full and half-sib-families resulted in reduced <span class="hlt">prediction</span> accuracies. Additionally, <span class="hlt">predictions</span> were performed using reduced marker sets and reduced training population sets. In conclusion, using less than 200 lines in the training set can result in low <span class="hlt">prediction</span> accuracy, and the accuracy will then be highly dependent on the family structure of the selected training set. However, the results also indicate that relatively small training sets (200 lines) are sufficient for genomic <span class="hlt">prediction</span> in commercial barley breeding. In addition, our results indicate a minimum marker set of 1,000 to decrease the risk of low <span class="hlt">prediction</span> accuracy for some traits or some families. PMID:27783639</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.dtic.mil/docs/citations/ADA464649','DTIC-ST'); return false;" href="http://www.dtic.mil/docs/citations/ADA464649"><span>Life <span class="hlt">Prediction</span> of Fretting Fatigue with <span class="hlt">Advanced</span> Surface Treatments (Preprint)</span></a></p> <p><a target="_blank" href="http://www.dtic.mil/">DTIC Science & Technology</a></p> <p></p> <p>2006-05-01</p> <p>surfaces and not the fretting pads. The chosen coatings included DLC, Ni-B, Molybdenum, and Nitride. These 4 coatings, their application to the titanium ...Article Preprint 5a. CONTRACT NUMBER In-house 5b. GRANT NUMBER 4 . TITLE AND SUBTITLE LIFE <span class="hlt">PREDICTION</span> OF FRETTING FATIGUE WITH <span class="hlt">ADVANCED</span> SURFACE...TREATMENTS (PREPRINT) 5c. PROGRAM ELEMENT NUMBER N/A 5d. PROJECT NUMBER M02R 5e. TASK NUMBER 30 6 . AUTHOR(S) Patrick J. Golden and Michael</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70155505','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70155505"><span>A comparison of <span class="hlt">hydrologic</span> models for ecological flows and water availability</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Caldwell, Peter V; Kennen, Jonathan G.; Sun, Ge; Kiang, Julie E.; Butcher, John B; Eddy, Michelle C; Hay, Lauren E.; LaFontaine, Jacob H.; Hain, Ernie F.; Nelson, Stacy C; McNulty, Steve G</p> <p>2015-01-01</p> <p>Robust <span class="hlt">hydrologic</span> models are needed to help manage water resources for healthy aquatic ecosystems and reliable water supplies for people, but there is a lack of comprehensive model comparison studies that quantify differences in streamflow <span class="hlt">predictions</span> among model applications developed to answer management questions. We assessed differences in daily streamflow <span class="hlt">predictions</span> by four fine-scale models and two regional-scale monthly time step models by comparing model fit statistics and bias in ecologically relevant flow statistics (ERFSs) at five sites in the Southeastern USA. Models were calibrated to different extents, including uncalibrated (level A), calibrated to a downstream site (level B), calibrated specifically for the site (level C) and calibrated for the site with adjusted precipitation and temperature inputs (level D). All models generally captured the magnitude and variability of observed streamflows at the five study sites, and increasing level of model calibration generally improved performance. All models had at least 1 of 14 ERFSs falling outside a +/−30% range of <span class="hlt">hydrologic</span> uncertainty at every site, and ERFSs related to low flows were frequently over-<span class="hlt">predicted</span>. Our results do not indicate that any specific <span class="hlt">hydrologic</span> model is superior to the others evaluated at all sites and for all measures of model performance. Instead, we provide evidence that (1) model performance is as likely to be related to calibration strategy as it is to model structure and (2) simple, regional-scale models have comparable performance to the more complex, fine-scale models at a monthly time step.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2008PhDT.......184D','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2008PhDT.......184D"><span>Modeling winter <span class="hlt">hydrological</span> processes under differing climatic conditions: Modifying WEPP</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Dun, Shuhui</p> <p></p> <p>Water erosion is a serious and continuous environmental problem worldwide. In cold regions, soil freeze and thaw has great impacts on infiltration and erosion. Rain or snowmelt on a thawing soil can cause severe water erosion. Of equal importance is snow accumulation and snowmelt, which can be the predominant <span class="hlt">hydrological</span> process in areas of mid- to high latitudes and forested watersheds. Modelers must properly simulate winter processes to adequately represent the overall <span class="hlt">hydrological</span> outcome and sediment and chemical transport in these areas. Modeling winter <span class="hlt">hydrology</span> is presently lacking in water erosion models. Most of these models are based on the functional Universal Soil Loss Equation (USLE) or its revised forms, e.g., Revised USLE (RUSLE). In RUSLE a seasonally variable soil erodibility factor (K) was used to account for the effects of frozen and thawing soil. Yet the use of this factor requires observation data for calibration, and such a simplified approach cannot represent the complicated transient freeze-thaw processes and their impacts on surface runoff and erosion. The Water Erosion <span class="hlt">Prediction</span> Project (WEPP) watershed model, a physically-based erosion <span class="hlt">prediction</span> software developed by the USDA-ARS, has seen numerous applications within and outside the US. WEPP simulates winter processes, including snow accumulation, snowmelt, and soil freeze-thaw, using an approach based on mass and energy conservation. However, previous studies showed the inadequacy of the winter routines in the WEPP model. Therefore, the objectives of this study were: (1) To adapt a modeling approach for winter <span class="hlt">hydrology</span> based on mass and energy conservation, and to implement this approach into a physically-oriented <span class="hlt">hydrological</span> model, such as WEPP; and (2) To assess this modeling approach through case applications to different geographic conditions. A new winter routine was developed and its performance was evaluated by incorporating it into WEPP (v2008.9) and then applying WEPP to</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.ars.usda.gov/research/publications/publication/?seqNo115=341516','TEKTRAN'); return false;" href="http://www.ars.usda.gov/research/publications/publication/?seqNo115=341516"><span>Evaluate the Role of Evapotranspiration Remote Sensing Data in Improving <span class="hlt">Hydrological</span> Modeling <span class="hlt">Predictability</span></span></a></p> <p><a target="_blank" href="https://www.ars.usda.gov/research/publications/find-a-publication/">USDA-ARS?s Scientific Manuscript database</a></p> <p></p> <p></p> <p>As the global demands for the use of freshwater resources continues to rise, it has become increasingly important to insure the sustainability of this resources. This is accomplished through the use of management strategies that often utilize monitoring and the use of <span class="hlt">hydrological</span> models. However, m...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016EGUGA..1812502P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016EGUGA..1812502P"><span>A multiple hypotheses uncertainty analysis in <span class="hlt">hydrological</span> modelling: about model structure, landscape parameterization, and numerical integration</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Pilz, Tobias; Francke, Till; Bronstert, Axel</p> <p>2016-04-01</p> <p>Until today a large number of competing computer models has been developed to understand <span class="hlt">hydrological</span> processes and to simulate and <span class="hlt">predict</span> streamflow dynamics of rivers. This is primarily the result of a lack of a unified theory in catchment <span class="hlt">hydrology</span> due to insufficient process understanding and uncertainties related to model development and application. Therefore, the goal of this study is to analyze the uncertainty structure of a process-based <span class="hlt">hydrological</span> catchment model employing a multiple hypotheses approach. The study focuses on three major problems that have received only little attention in previous investigations. First, to estimate the impact of model structural uncertainty by employing several alternative representations for each simulated process. Second, explore the influence of landscape discretization and parameterization from multiple datasets and user decisions. Third, employ several numerical solvers for the integration of the governing ordinary differential equations to study the effect on simulation results. The generated ensemble of model hypotheses is then analyzed and the three sources of uncertainty compared against each other. To ensure consistency and comparability all model structures and numerical solvers are implemented within a single simulation environment. First results suggest that the selection of a sophisticated numerical solver for the differential equations positively affects simulation outcomes. However, already some simple and easy to implement explicit methods perform surprisingly well and need less computational efforts than more <span class="hlt">advanced</span> but time consuming implicit techniques. There is general evidence that ambiguous and subjective user decisions form a major source of uncertainty and can greatly influence model development and application at all stages.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70179473','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70179473"><span><span class="hlt">Hydrologic</span> connectivity: Quantitative assessments of <span class="hlt">hydrologic</span>-enforced drainage structures in an elevation model</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Poppenga, Sandra K.; Worstell, Bruce B.</p> <p>2016-01-01</p> <p>Elevation data derived from light detection and ranging present challenges for <span class="hlt">hydrologic</span> modeling as the elevation surface includes bridge decks and elevated road features overlaying culvert drainage structures. In reality, water is carried through these structures; however, in the elevation surface these features impede modeled overland surface flow. Thus, a <span class="hlt">hydrologically</span>-enforced elevation surface is needed for hydrodynamic modeling. In the Delaware River Basin, <span class="hlt">hydrologic</span>-enforcement techniques were used to modify elevations to simulate how constructed drainage structures allow overland surface flow. By calculating residuals between unfilled and filled elevation surfaces, artificially pooled depressions that formed upstream of constructed drainage structure features were defined, and elevation values were adjusted by generating transects at the location of the drainage structures. An assessment of each <span class="hlt">hydrologically</span>-enforced drainage structure was conducted using field-surveyed culvert and bridge coordinates obtained from numerous public agencies, but it was discovered the disparate drainage structure datasets were not comprehensive enough to assess all remotely located depressions in need of <span class="hlt">hydrologic</span>-enforcement. Alternatively, orthoimagery was interpreted to define drainage structures near each depression, and these locations were used as reference points for a quantitative <span class="hlt">hydrologic</span>-enforcement assessment. The orthoimagery-interpreted reference points resulted in a larger corresponding sample size than the assessment between <span class="hlt">hydrologic</span>-enforced transects and field-surveyed data. This assessment demonstrates the viability of rules-based <span class="hlt">hydrologic</span>-enforcement that is needed to achieve <span class="hlt">hydrologic</span> connectivity, which is valuable for hydrodynamic models in sensitive coastal regions. <span class="hlt">Hydrologic</span>-enforced elevation data are also essential for merging with topographic/bathymetric elevation data that extend over vulnerable urbanized areas and dynamic coastal</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFM.H42B..04F','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFM.H42B..04F"><span>Towards a National <span class="hlt">Hydrological</span> Forecasting system for Canada : Lessons Learned from the Great Lakes and St. Lawrence <span class="hlt">Prediction</span> System</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Fortin, V.; Durnford, D.; Gaborit, E.; Davison, B.; Dimitrijevic, M.; Matte, P.</p> <p>2016-12-01</p> <p>Environment and Climate Change Canada has recently deployed a water cycle <span class="hlt">prediction</span> system for the Great Lakes and St. Lawrence River. The model domain includes both the Canadian and US portions of the watershed. It provides 84-h forecasts of weather elements, lake level, lake ice cover and surface currents based on two-way coupling of the GEM numerical weather <span class="hlt">prediction</span> (NWP) model with the NEMO ocean model. Streamflow of all the major tributaries of the Great Lakes and St. Lawrence River are estimated by the WATROUTE routing model, which routes the surface runoff forecasted by GEM's land-surface scheme and assimilates streamflow observations where available. Streamflow forecasts are updated twice daily and are disseminated through an OGC compliant web map service (WMS) and a web feature service (WFS). In this presentation, in addition to describing the system and documenting its forecast skill, we show how it is being used by clients for various environmental <span class="hlt">prediction</span> applications. We then discuss the importance of two-way coupling, land-surface and hillslope modelling and the impact of horizontal resolution on <span class="hlt">hydrological</span> <span class="hlt">prediction</span> skill. In the second portion of the talk, we discuss plans for implementing a similar system at the national scale, using what we have learned in the Great Lakes and St. Lawrence watershed. Early results obtained for the headwaters of the Saskatchewan River as well as for the whole Nelson-Churchill watershed are presented.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4488316','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4488316"><span><span class="hlt">Hydrologic</span>-Process-Based Soil Texture Classifications for Improved Visualization of Landscape Function</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Groenendyk, Derek G.; Ferré, Ty P.A.; Thorp, Kelly R.; Rice, Amy K.</p> <p>2015-01-01</p> <p>Soils lie at the interface between the atmosphere and the subsurface and are a key component that control ecosystem services, food production, and many other processes at the Earth’s surface. There is a long-established convention for identifying and mapping soils by texture. These readily available, georeferenced soil maps and databases are used widely in environmental sciences. Here, we show that these traditional soil classifications can be inappropriate, contributing to bias and uncertainty in applications from slope stability to water resource management. We suggest a new approach to soil classification, with a detailed example from the science of <span class="hlt">hydrology</span>. <span class="hlt">Hydrologic</span> simulations based on common meteorological conditions were performed using HYDRUS-1D, spanning textures identified by the United States Department of Agriculture soil texture triangle. We consider these common conditions to be: drainage from saturation, infiltration onto a drained soil, and combined infiltration and drainage events. Using a k-means clustering algorithm, we created soil classifications based on the modeled <span class="hlt">hydrologic</span> responses of these soils. The <span class="hlt">hydrologic</span>-process-based classifications were compared to those based on soil texture and a single hydraulic property, Ks. Differences in classifications based on <span class="hlt">hydrologic</span> response versus soil texture demonstrate that traditional soil texture classification is a poor predictor of <span class="hlt">hydrologic</span> response. We then developed a QGIS plugin to construct soil maps combining a classification with georeferenced soil data from the Natural Resource Conservation Service. The spatial patterns of <span class="hlt">hydrologic</span> response were more immediately informative, much simpler, and less ambiguous, for use in applications ranging from trafficability to irrigation management to flood control. The ease with which <span class="hlt">hydrologic</span>-process-based classifications can be made, along with the improved quantitative <span class="hlt">predictions</span> of soil responses and visualization of landscape</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/26121466','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/26121466"><span><span class="hlt">Hydrologic</span>-Process-Based Soil Texture Classifications for Improved Visualization of Landscape Function.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Groenendyk, Derek G; Ferré, Ty P A; Thorp, Kelly R; Rice, Amy K</p> <p>2015-01-01</p> <p>Soils lie at the interface between the atmosphere and the subsurface and are a key component that control ecosystem services, food production, and many other processes at the Earth's surface. There is a long-established convention for identifying and mapping soils by texture. These readily available, georeferenced soil maps and databases are used widely in environmental sciences. Here, we show that these traditional soil classifications can be inappropriate, contributing to bias and uncertainty in applications from slope stability to water resource management. We suggest a new approach to soil classification, with a detailed example from the science of <span class="hlt">hydrology</span>. <span class="hlt">Hydrologic</span> simulations based on common meteorological conditions were performed using HYDRUS-1D, spanning textures identified by the United States Department of Agriculture soil texture triangle. We consider these common conditions to be: drainage from saturation, infiltration onto a drained soil, and combined infiltration and drainage events. Using a k-means clustering algorithm, we created soil classifications based on the modeled <span class="hlt">hydrologic</span> responses of these soils. The <span class="hlt">hydrologic</span>-process-based classifications were compared to those based on soil texture and a single hydraulic property, Ks. Differences in classifications based on <span class="hlt">hydrologic</span> response versus soil texture demonstrate that traditional soil texture classification is a poor predictor of <span class="hlt">hydrologic</span> response. We then developed a QGIS plugin to construct soil maps combining a classification with georeferenced soil data from the Natural Resource Conservation Service. The spatial patterns of <span class="hlt">hydrologic</span> response were more immediately informative, much simpler, and less ambiguous, for use in applications ranging from trafficability to irrigation management to flood control. The ease with which <span class="hlt">hydrologic</span>-process-based classifications can be made, along with the improved quantitative <span class="hlt">predictions</span> of soil responses and visualization of landscape</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017EGUGA..1913288T','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017EGUGA..1913288T"><span><span class="hlt">Advanced</span> inflow forecasting for a hydropower plant in an Alpine hydropower regulated catchment - coupling of operational and <span class="hlt">hydrological</span> forecasts</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Tilg, Anna-Maria; Schöber, Johannes; Huttenlau, Matthias; Messner, Jakob; Achleitner, Stefan</p> <p>2017-04-01</p> <p>Hydropower is a renewable energy source which can help to stabilize fluctuations in the volatile energy market. Especially pumped-storage infrastructures in the European Alps play an important role within the European energy grid system. Today, the runoff of rivers in the Alps is often influenced by cascades of hydropower infrastructures where the operational procedures are triggered by energy market demands, water deliveries and flood control aspects rather than by hydro-meteorological variables. An example for such a highly hydropower regulated river is the catchment of the river Inn in the Eastern European Alps, originating in the Engadin (Switzerland). A new hydropower plant is going to be built as transboundary project at the boarder of Switzerland and Austria using the water of the Inn River. For the operation, a runoff forecast to the plant is required. The challenge in this case is that a high proportion of runoff is turbine water from an upstream situated hydropower cascade. The newly developed physically based <span class="hlt">hydrological</span> forecasting system is mainly capable to cover natural <span class="hlt">hydrological</span> runoff processes caused by storms and snow melt but can model only a small degree of human impact. These discontinuous parts of the runoff downstream of the pumped storage are described by means of an additional statistical model which has been developed. The main goal of the statistical model is to forecast the turbine water up to five days in <span class="hlt">advance</span>. The lead time of the data driven model exceeds the lead time of the used energy production forecast. Additionally, the amount of turbine water is linked to the need of electricity production and the electricity price. It has been shown that especially the parameters day-ahead prognosis of the energy production and turbine inflow of the previous week are good predictors and are therefore used as input parameters for the model. As the data is restricted due to technical conditions, so-called Tobit models have been used to</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2010EGUGA..1210643S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2010EGUGA..1210643S"><span>Strategies for <span class="hlt">Hydrology</span> Teaching for a Changing World</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Sivapalan, Murugesu</p> <p>2010-05-01</p> <p>, learning from case studies of nature's experiments with respect to climate change and land cover changes, <span class="hlt">predictions</span> using space for time substitution, models of interacting processes as opposed to models of individual processes, and models of human-nature interactions and feedbacks. Instead of, or in addition to, pooling together collections of <span class="hlt">hydrologic</span> recipes or tool sets, as we do now, there is a need for consensus building on a clear vision or philosophy of <span class="hlt">hydrology</span> teaching that is cognizant of where <span class="hlt">hydrology</span> presently is and where it is headed. This will enable experimentation of different methods of teaching to different audiences (e.g., engineers, earth scientists, even social scientists) while remaining within an agreed vision. In this way we can be satisfied that teaching methods will improve so that future practitioners carry forward a coherent philosophy of the science and possess the necessary skill sets.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012AGUFM.H43C1358C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012AGUFM.H43C1358C"><span>Operational validation of a multi-period and multi-criteria model conditioning approach for the <span class="hlt">prediction</span> of rainfall-runoff processes in small forest catchments</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Choi, H.; Kim, S.</p> <p>2012-12-01</p> <p> Limestone. The study is progressed based on the followings. Firstly, <span class="hlt">hydrological</span> time series of each catchment are sampled and clustered into multi-period having distinctly different temporal characteristics, and secondly, behavioural parameter distributions are determined in each multi-period based on the specification of multi-criteria model performance measures. Finally, behavioural parameter sets of each multi-period of single catchment are applied on the corresponding period of other catchments, and the cross-validations are conducted in this manner for all catchments The multi-period model conditioning approach is clearly effective to reduce the width of <span class="hlt">prediction</span> limits, giving better model performance against the temporal variability of <span class="hlt">hydrological</span> characteristics, and has enough potential to be the effective <span class="hlt">prediction</span> tool for ungauged catchments. However, more <span class="hlt">advanced</span> and continuous studies are needed to expand the application of this approach in <span class="hlt">prediction</span> of <span class="hlt">hydrological</span> responses in ungauged catchments,</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFMGC11B1146S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFMGC11B1146S"><span>Changes in <span class="hlt">Hydrological</span> Extremes and its Relation to Climate Variability in Mountainous Watershed: A Case Study from Gandaki River Basin, Nepal</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Shrestha, N. S.; Dahal, P.</p> <p>2016-12-01</p> <p>Changes in the <span class="hlt">hydrological</span> extreme are expected due to climate variability and are needed to assess at local and regional scales since these changes are not uniform over the globe. This study analyses the changes in intensity, frequency and persistence <span class="hlt">hydrological</span> extreme in Gandaki River Basin (GRB) Nepal over past and future and its relation to climate variability. <span class="hlt">Hydrological</span> data of 12 different <span class="hlt">hydrological</span> stations covering all the sub basins of Gandaki River Basin were analyzed. At least 1 <span class="hlt">hydrological</span> station in each sub basin to the maximum of 3 was taken into consideration for this study. Results show that <span class="hlt">hydrological</span> extreme have increased in intensity, frequency and persistence over recent year and are <span class="hlt">predicted</span> to increase in future (2030-2060). The time-series analysis revealed an increase in the magnitude, frequency and duration of flood and drought. The instantaneous maximum flow, flood events and duration of flood events are found to have increasing trend. The minimum discharge was observed to be decreasing which entails that the water availability in the driest time is decreasing. Trend analysis of seasonal flow revealed an increase in monsoon flows and decreasing in post monsoon. Changes in climate variability over the same period shows higher anomalies in both temperature and precipitation in recent decades (1990s and 2000s) compared to the baseline period (1970-2000). Model suggests an increasing trend in annual flows with the increase more pronounced in 2060s. Significant increase in extreme flows and subsequent decrease in dependable flows suggest increase in frequency of isolated extreme flows followed by prolonged dry spells. Data also showed that the mean temperature will be increasing from 1.9 0C to 3.1 0C and precipitation will be changing by -8% to +12% in 2031-2060 compared to the baseline period. For long-term planning and management of water resources, current trend and future change in the pattern of water availability should be</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017ApWS....7.1595T','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017ApWS....7.1595T"><span>Integrating remote sensing, geographic information systems and global positioning system techniques with <span class="hlt">hydrological</span> modeling</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Thakur, Jay Krishna; Singh, Sudhir Kumar; Ekanthalu, Vicky Shettigondahalli</p> <p>2017-07-01</p> <p>Integration of remote sensing (RS), geographic information systems (GIS) and global positioning system (GPS) are emerging research areas in the field of groundwater <span class="hlt">hydrology</span>, resource management, environmental monitoring and during emergency response. Recent <span class="hlt">advancements</span> in the fields of RS, GIS, GPS and higher level of computation will help in providing and handling a range of data simultaneously in a time- and cost-efficient manner. This review paper deals with <span class="hlt">hydrological</span> modeling, uses of remote sensing and GIS in <span class="hlt">hydrological</span> modeling, models of integrations and their need and in last the conclusion. After dealing with these issues conceptually and technically, we can develop better methods and novel approaches to handle large data sets and in a better way to communicate information related with rapidly decreasing societal resources, i.e. groundwater.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3205875','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3205875"><span>A Serum Protein Profile <span class="hlt">Predictive</span> of the Resistance to Neoadjuvant Chemotherapy in <span class="hlt">Advanced</span> Breast Cancers*</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Hyung, Seok-Won; Lee, Min Young; Yu, Jong-Han; Shin, Byunghee; Jung, Hee-Jung; Park, Jong-Moon; Han, Wonshik; Lee, Kyung-Min; Moon, Hyeong-Gon; Zhang, Hui; Aebersold, Ruedi; Hwang, Daehee; Lee, Sang-Won; Yu, Myeong-Hee; Noh, Dong-Young</p> <p>2011-01-01</p> <p><span class="hlt">Prediction</span> of the responses to neoadjuvant chemotherapy (NACT) can improve the treatment of patients with <span class="hlt">advanced</span> breast cancer. Genes and proteins <span class="hlt">predictive</span> of chemoresistance have been extensively studied in breast cancer tissues. However, noninvasive serum biomarkers capable of such <span class="hlt">prediction</span> have been rarely exploited. Here, we performed profiling of N-glycosylated proteins in serum from fifteen <span class="hlt">advanced</span> breast cancer patients (ten patients sensitive to and five patients resistant to NACT) to discover serum biomarkers of chemoresistance using a label-free liquid chromatography-tandem MS method. By performing a series of statistical analyses of the proteomic data, we selected thirteen biomarker candidates and tested their differential serum levels by Western blotting in 13 independent samples (eight patients sensitive to and five patients resistant to NACT). Among the candidates, we then selected the final set of six potential serum biomarkers (AHSG, APOB, C3, C9, CP, and ORM1) whose differential expression was confirmed in the independent samples. Finally, we demonstrated that a multivariate classification model using the six proteins could <span class="hlt">predict</span> responses to NACT and further <span class="hlt">predict</span> relapse-free survival of patients. In summary, global N-glycoproteome profile in serum revealed a protein pattern <span class="hlt">predictive</span> of the responses to NACT, which can be further validated in large clinical studies. PMID:21799047</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://adsabs.harvard.edu/abs/2018HESS...22..331I','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018HESS...22..331I"><span>Scale effect challenges in urban <span class="hlt">hydrology</span> highlighted with a distributed <span class="hlt">hydrological</span> model</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Ichiba, Abdellah; Gires, Auguste; Tchiguirinskaia, Ioulia; Schertzer, Daniel; Bompard, Philippe; Ten Veldhuis, Marie-Claire</p> <p>2018-01-01</p> <p><span class="hlt">Hydrological</span> models are extensively used in urban water management, development and evaluation of future scenarios and research activities. There is a growing interest in the development of fully distributed and grid-based models. However, some complex questions related to scale effects are not yet fully understood and still remain open issues in urban <span class="hlt">hydrology</span>. In this paper we propose a two-step investigation framework to illustrate the extent of scale effects in urban <span class="hlt">hydrology</span>. First, fractal tools are used to highlight the scale dependence observed within distributed data input into urban <span class="hlt">hydrological</span> models. Then an intensive multi-scale modelling work is carried out to understand scale effects on <span class="hlt">hydrological</span> model performance. Investigations are conducted using a fully distributed and physically based model, Multi-Hydro, developed at Ecole des Ponts ParisTech. The model is implemented at 17 spatial resolutions ranging from 100 to 5 m. Results clearly exhibit scale effect challenges in urban <span class="hlt">hydrology</span> modelling. The applicability of fractal concepts highlights the scale dependence observed within distributed data. Patterns of geophysical data change when the size of the observation pixel changes. The multi-scale modelling investigation confirms scale effects on <span class="hlt">hydrological</span> model performance. Results are analysed over three ranges of scales identified in the fractal analysis and confirmed through modelling. This work also discusses some remaining issues in urban <span class="hlt">hydrology</span> modelling related to the availability of high-quality data at high resolutions, and model numerical instabilities as well as the computation time requirements. The main findings of this paper enable a replacement of traditional methods of <q>model calibration</q> by innovative methods of <q>model resolution alteration</q> based on the spatial data variability and scaling of flows in urban <span class="hlt">hydrology</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19740019698','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19740019698"><span>Application of remote sensing to <span class="hlt">hydrology</span>. [for the formulation of watershed behavior models</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Ambaruch, R.; Simmons, J. W.</p> <p>1973-01-01</p> <p>Streamflow forecasting and <span class="hlt">hydrologic</span> modelling are considered in a feasibility assessment of using the data produced by remote observation from space and/or aircraft to reduce the time and expense normally involved in achieving the ability to <span class="hlt">predict</span> the <span class="hlt">hydrological</span> behavior of an ungaged watershed. Existing watershed models are described, and both stochastic and parametric techniques are discussed towards the selection of a suitable simulation model. Technical progress and applications are reported and recommendations are made for additional research.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/15601798','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/15601798"><span><span class="hlt">Advances</span> in the assessment and <span class="hlt">prediction</span> of interpersonal violence.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Mills, Jeremy F</p> <p>2005-02-01</p> <p>This article underscores the weakness of clinical judgment as a mechanism for <span class="hlt">prediction</span> with examples from other areas in the psychological literature. Clinical judgment has as its Achilles'heel the reliance on a person to incorporate multiple pieces of information while overcoming human judgment errors--a feat insurmountable thus far. The actuarial approach to risk assessment has overcome many of the weaknesses of clinical judgment and has been shown to be a much superior method. Nonetheless, the static/historical nature of the risk factors associated with most actuarial approaches is limiting. <span class="hlt">Advances</span> in risk <span class="hlt">prediction</span> will be found in part in the development of dynamic actuarial instruments that will measure both static/historical and changeable risk factors. The dynamic risk factors can be reevaluated on an ongoing basis, and it is proposed that the level of change in dynamic factors necessary to represent a significant change in overall risk will be an interactive function with static risk factors.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014EGUGA..1611346L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014EGUGA..1611346L"><span>Impact of the assimilation of satellite soil moisture and LST on the <span class="hlt">hydrological</span> cycle</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Laiolo, Paola; Gabellani, Simone; Delogu, Fabio; Silvestro, Francesco; Rudari, Roberto; Campo, Lorenzo; Boni, Giorgio</p> <p>2014-05-01</p> <p>The reliable estimation of <span class="hlt">hydrological</span> variables (e.g. soil moisture, evapotranspiration, surface temperature) in space and time is of fundamental importance in operational <span class="hlt">hydrology</span> to improve the forecast of the rainfall-runoff response of catchments and, consequently, flood <span class="hlt">predictions</span>. Nowadays remote sensing can offer a chance to provide good space-time estimates of several <span class="hlt">hydrological</span> variables and then improve <span class="hlt">hydrological</span> model performances especially in environments with scarce ground based data. The aim of this work is to investigate the impacts on the performances of a distributed <span class="hlt">hydrological</span> model (Continuum) of the assimilation of satellite-derived soil moisture products and Land Surface (LST). In this work three different soil moisture (SM) products, derived by ASCAT sensor, are used. These data are provided by the EUMETSAT's H-SAF (Satellite Application Facility on Support to Operational <span class="hlt">Hydrology</span> and Water Management) program. The considered soil moisture products are: large scale surface soil moisture (SM OBS 1 - H07), small scale surface soil moisture (SM OBS 2 - H08) and profile index in the roots region (SM DAS 2 - H14). These data are compared with soil moisture estimated by Continuum model on the Orba catchment (800 km2), in the northern part of Italy, for the period July 2012-June 2013. Different assimilation experiments have been performed. The first experiment consists in the assimilation of the SM products by using a simple Nudging technique; the second one is the assimilation of only LST data, derived from MSG satellite, and the third is the assimilation of both SM products and LST. The benefits on the model <span class="hlt">predictions</span> of discharge, LST and soil moisture dynamics were tested.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/28376283','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/28376283"><span>Modeled <span class="hlt">hydrologic</span> metrics show links between <span class="hlt">hydrology</span> and the functional composition of stream assemblages.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Patrick, Christopher J; Yuan, Lester L</p> <p>2017-07-01</p> <p>Flow alteration is widespread in streams, but current understanding of the effects of differences in flow characteristics on stream biological communities is incomplete. We tested hypotheses about the effect of variation in <span class="hlt">hydrology</span> on stream communities by using generalized additive models to relate watershed information to the values of different flow metrics at gauged sites. Flow models accounted for 54-80% of the spatial variation in flow metric values among gauged sites. We then used these models to <span class="hlt">predict</span> flow metrics in 842 ungauged stream sites in the mid-Atlantic United States that were sampled for fish, macroinvertebrates, and environmental covariates. Fish and macroinvertebrate assemblages were characterized in terms of a suite of metrics that quantified aspects of community composition, diversity, and functional traits that were expected to be associated with differences in flow characteristics. We related modeled flow metrics to biological metrics in a series of stressor-response models. Our analyses identified both drying and base flow instability as explaining 30-50% of the observed variability in fish and invertebrate community composition. Variations in community composition were related to variations in the prevalence of dispersal traits in invertebrates and trophic guilds in fish. The results demonstrate that we can use statistical models to <span class="hlt">predict</span> <span class="hlt">hydrologic</span> conditions at bioassessment sites, which, in turn, we can use to estimate relationships between flow conditions and biological characteristics. This analysis provides an approach to quantify the effects of spatial variation in flow metrics using readily available biomonitoring data. © 2017 by the Ecological Society of America.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://cfpub.epa.gov/si/si_public_record_report.cfm?dirEntryId=263239&keyword=service+AND+processes&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=263239&keyword=service+AND+processes&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">Hydrologic</span> Connections and Landscape Metrics to <span class="hlt">Advance</span> Ecosystem Goods and Services in Tampa Bay Watershed</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>Understanding the <span class="hlt">hydrological</span> characteristics of coastal wetlands across land use gradients ranging from natural to urban to agricultural is important for significantly enhancing our ability to utilize environmental data in interpreting ecosystem condition and processes. Here we...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2005AGUFM.H42B..04I','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2005AGUFM.H42B..04I"><span>Comprehensive Representation of <span class="hlt">Hydrologic</span> and Geomorphic Process Coupling in Numerical Models: Internal Dynamics and Basin Evolution</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Istanbulluoglu, E.; Vivoni, E. R.; Ivanov, V. Y.; Bras, R. L.</p> <p>2005-12-01</p> <p>Landscape morphology has an important control on the spatial and temporal organization of basin <span class="hlt">hydrologic</span> response to climate forcing, affecting soil moisture redistribution as well as vegetation function. On the other hand, erosion, driven by <span class="hlt">hydrology</span> and modulated by vegetation, produces landforms over geologic time scales that reflect characteristic signatures of the dominant land forming process. Responding to extreme climate events or anthropogenic disturbances of the land surface, infrequent but rapid forms of erosion (e.g., arroyo development, landsliding) can modify topography such that basin <span class="hlt">hydrology</span> is significantly influenced. Despite significant <span class="hlt">advances</span> in both <span class="hlt">hydrologic</span> and geomorphic modeling over the past two decades, the dynamic interactions between basin <span class="hlt">hydrology</span>, geomorphology and terrestrial ecology are not adequately captured in current model frameworks. In order to investigate <span class="hlt">hydrologic</span>-geomorphic-ecologic interactions at the basin scale we present initial efforts in integrating the CHILD landscape evolution model (Tucker et al. 2001) with the tRIBS <span class="hlt">hydrology</span> model (Ivanov et al. 2004), both developed in a common software environment. In this talk, we present preliminary results of the numerical modeling of the coupled evolution of basin hydro-geomorphic response and resulting landscape morphology in two sets of examples. First, we discuss the long-term evolution of both the <span class="hlt">hydrologic</span> response and the resulting basin morphology from an initially uplifted plateau. In the second set of modeling experiments, we implement changes in climate and land-use to an existing topography and compare basin <span class="hlt">hydrologic</span> response to the model results when landscape form is fixed (e.g. no coupling between <span class="hlt">hydrology</span> and geomorphology). Model results stress the importance of internal basin dynamics, including runoff generation mechanisms and <span class="hlt">hydrologic</span> states, in shaping <span class="hlt">hydrologic</span> response as well as the importance of employing comprehensive</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2009AGUFM.H42C..08P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2009AGUFM.H42C..08P"><span>Synthesizing International Understanding of Changes in the Arctic <span class="hlt">Hydrological</span> System</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Pundsack, J. W.; Vorosmarty, C. J.; Hinzman, L. D.</p> <p>2009-12-01</p> <p>There are several notable gaps in our current level of understanding of Arctic <span class="hlt">hydrological</span> systems. At the same time, rapidly emerging data sets, technologies, and modeling resources provide us with an unprecedented opportunity to move substantially forward. The Arctic Community-Wide <span class="hlt">Hydrological</span> Analysis and Monitoring Program (Arctic-CHAMP), funded by NSF/ARCSS, was established to initiate a major effort to improve our current monitoring of water cycle variables, and to foster collaboration with the many relevant U.S. and international arctic research initiatives. These projects, funded under ARCSS through the ‘Freshwater Integration (FWI) study’, links CHAMP, the Arctic/Subarctic Ocean Fluxes (ASOF) Programme, and SEARCH. As part of the overall synthesis and integration efforts of the NSF-ARCSS Freshwater Integration (FWI) study, the program carried-out a major International Synthesis Capstone Workshop in Fall 2009 as an International Polar Year (IPY) affiliated meeting. The workshop, "Synthesizing International Understanding of Changes in the Arctic <span class="hlt">Hydrological</span> System,” was held 30 September to 4 October 2009 in Stockholm at the Beijer Auditorium of the Royal Swedish Academy. The workshop was sponsored by the NSF-ARCSS Arctic-CHAMP Science Management Office (City College of New York / Univ. of New Hampshire), the International Study of Arctic Change (ISAC), and the International Arctic Research Center (IARC; Univ. of Alaska Fairbanks). The overarching goals of the meeting were to stage a post-IPY lessons-learned workshop with co-equal numbers of FWI, IPY, and ICARP-II researchers, using insights from recent scientific findings, data, and strategies to afford synthesis. The workshop aimed to: (1) take stock of recent <span class="hlt">advances</span> in our understanding of changes in the Arctic <span class="hlt">hydrological</span> system; (2) identify key remaining research gaps / unanswered questions; and (3) gather insight on where to focus future research efforts/initiatives (nationally and</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017HESS...21.3859C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017HESS...21.3859C"><span>Spatial and temporal variability of rainfall and their effects on <span class="hlt">hydrological</span> response in urban areas - a review</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Cristiano, Elena; ten Veldhuis, Marie-claire; van de Giesen, Nick</p> <p>2017-07-01</p> <p>In urban areas, <span class="hlt">hydrological</span> processes are characterized by high variability in space and time, making them sensitive to small-scale temporal and spatial rainfall variability. In the last decades new instruments, techniques, and methods have been developed to capture rainfall and <span class="hlt">hydrological</span> processes at high resolution. Weather radars have been introduced to estimate high spatial and temporal rainfall variability. At the same time, new models have been proposed to reproduce <span class="hlt">hydrological</span> response, based on small-scale representation of urban catchment spatial variability. Despite these efforts, interactions between rainfall variability, catchment heterogeneity, and <span class="hlt">hydrological</span> response remain poorly understood. This paper presents a review of our current understanding of <span class="hlt">hydrological</span> processes in urban environments as reported in the literature, focusing on their spatial and temporal variability aspects. We review recent findings on the effects of rainfall variability on <span class="hlt">hydrological</span> response and identify gaps where knowledge needs to be further developed to improve our understanding of and capability to <span class="hlt">predict</span> urban <span class="hlt">hydrological</span> response.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018ThApC.tmp....5A','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018ThApC.tmp....5A"><span>Quantifying the sources of uncertainty in an ensemble of <span class="hlt">hydrological</span> climate-impact projections</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Aryal, Anil; Shrestha, Sangam; Babel, Mukand S.</p> <p>2018-01-01</p> <p>The objective of this paper is to quantify the various sources of uncertainty in the assessment of climate change impact on <span class="hlt">hydrology</span> in the Tamakoshi River Basin, located in the north-eastern part of Nepal. Multiple climate and <span class="hlt">hydrological</span> models were used to simulate future climate conditions and discharge in the basin. The simulated results of future climate and river discharge were analysed for the quantification of sources of uncertainty using two-way and three-way ANOVA. The results showed that temperature and precipitation in the study area are projected to change in near- (2010-2039), mid- (2040-2069) and far-future (2070-2099) periods. Maximum temperature is likely to rise by 1.75 °C under Representative Concentration Pathway (RCP) 4.5 and by 3.52 °C under RCP 8.5. Similarly, the minimum temperature is expected to rise by 2.10 °C under RCP 4.5 and by 3.73 °C under RCP 8.5 by the end of the twenty-first century. Similarly, the precipitation in the study area is expected to change by - 2.15% under RCP 4.5 and - 2.44% under RCP 8.5 scenarios. The future discharge in the study area was projected using two <span class="hlt">hydrological</span> models, viz. Soil and Water Assessment Tool (SWAT) and <span class="hlt">Hydrologic</span> Engineering Center's <span class="hlt">Hydrologic</span> Modelling System (HEC-HMS). The SWAT model projected discharge is expected to change by small amount, whereas HEC-HMS model projected considerably lower discharge in future compared to the baseline period. The results also show that future climate variables and river <span class="hlt">hydrology</span> contain uncertainty due to the choice of climate models, RCP scenarios, bias correction methods and <span class="hlt">hydrological</span> models. During wet days, more uncertainty is observed due to the use of different climate models, whereas during dry days, the use of different <span class="hlt">hydrological</span> models has a greater effect on uncertainty. Inter-comparison of the impacts of different climate models reveals that the REMO climate model shows higher uncertainty in the <span class="hlt">prediction</span> of precipitation and</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=19820055670&hterms=landcover&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D30%26Ntt%3Dlandcover','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=19820055670&hterms=landcover&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D30%26Ntt%3Dlandcover"><span>Classification of simulated and actual NOAA-6 AVHRR data for <span class="hlt">hydrologic</span> land-surface feature definition. [<span class="hlt">Advanced</span> Very High Resolution Radiometer</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Ormsby, J. P.</p> <p>1982-01-01</p> <p>An examination of the possibilities of using Landsat data to simulate NOAA-6 <span class="hlt">Advanced</span> Very High Resolution Radiometer (AVHRR) data on two channels, as well as using actual NOAA-6 imagery, for large-scale <span class="hlt">hydrological</span> studies is presented. A running average was obtained of 18 consecutive pixels of 1 km resolution taken by the Landsat scanners were scaled up to 8-bit data and investigated for different gray levels. AVHRR data comprising five channels of 10-bit, band-interleaved information covering 10 deg latitude were analyzed and a suitable pixel grid was chosen for comparison with the Landsat data in a supervised classification format, an unsupervised mode, and with ground truth. Landcover delineation was explored by removing snow, water, and cloud features from the cluster analysis, and resulted in less than 10% difference. Low resolution large-scale data was determined useful for characterizing some landcover features if weekly and/or monthly updates are maintained.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2011AGUFMIN32A..03H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2011AGUFMIN32A..03H"><span><span class="hlt">Advancing</span> an Information Model for Environmental Observations</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Horsburgh, J. S.; Aufdenkampe, A. K.; Hooper, R. P.; Lehnert, K. A.; Schreuders, K.; Tarboton, D. G.; Valentine, D. W.; Zaslavsky, I.</p> <p>2011-12-01</p> <p> have been modified to support data management for the Critical Zone Observatories (CZOs). This paper will present limitations of the existing information model used by the CUAHSI HIS that have been uncovered through its deployment and use, as well as new <span class="hlt">advances</span> to the information model, including: better representation of both in situ observations from field sensors and observations derived from environmental samples, extensibility in attributes used to describe observations, and observation provenance. These <span class="hlt">advances</span> have been developed by the HIS team and the broader scientific community and will enable the information model to accommodate and better describe wider classes of environmental observations and to better meet the needs of the <span class="hlt">hydrologic</span> science and CZO communities.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29934651','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29934651"><span>Beyond Metrics? The Role of <span class="hlt">Hydrologic</span> Baseline Archetypes in Environmental Water Management.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Lane, Belize A; Sandoval-Solis, Samuel; Stein, Eric D; Yarnell, Sarah M; Pasternack, Gregory B; Dahlke, Helen E</p> <p>2018-06-22</p> <p>Balancing ecological and human water needs often requires characterizing key aspects of the natural flow regime and then <span class="hlt">predicting</span> ecological response to flow alterations. Flow metrics are generally relied upon to characterize long-term average statistical properties of the natural flow regime (<span class="hlt">hydrologic</span> baseline conditions). However, some key aspects of <span class="hlt">hydrologic</span> baseline conditions may be better understood through more complete consideration of continuous patterns of daily, seasonal, and inter-annual variability than through summary metrics. Here we propose the additional use of high-resolution dimensionless archetypes of regional stream classes to improve understanding of baseline <span class="hlt">hydrologic</span> conditions and inform regional environmental flows assessments. In an application to California, we describe the development and analysis of <span class="hlt">hydrologic</span> baseline archetypes to characterize patterns of flow variability within and between stream classes. We then assess the utility of archetypes to provide context for common flow metrics and improve understanding of linkages between aquatic patterns and processes and their <span class="hlt">hydrologic</span> controls. Results indicate that these archetypes may offer a distinct and complementary tool for researching mechanistic flow-ecology relationships, assessing regional patterns for streamflow management, or understanding impacts of changing climate.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://epi.grants.cancer.gov/events/pharm-2010/','NCI'); return false;" href="https://epi.grants.cancer.gov/events/pharm-2010/"><span>Cancer Pharmacogenomics: Integrating Discoveries in Basic, Clinical and Population Sciences to <span class="hlt">Advance</span> <span class="hlt">Predictive</span> Cancer Care</span></a></p> <p><a target="_blank" href="http://www.cancer.gov">Cancer.gov</a></p> <p></p> <p></p> <p>Cancer Pharmacogenomics: Integrating Discoveries in Basic, Clinical and Population Sciences to <span class="hlt">Advance</span> <span class="hlt">Predictive</span> Cancer Care, a 2010 workshop sponsored by the Epidemiology and Genomics Research Program.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012EGUGA..1411027B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012EGUGA..1411027B"><span>Valuing <span class="hlt">hydrological</span> alteration in Multi-Objective reservoir management</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Bizzi, S.; Pianosi, F.; Soncini-Sessa, R.</p> <p>2012-04-01</p> <p>Water management through dams and reservoirs is worldwide necessary to support key human-related activities ranging from hydropower production to water allocation for agricultural production, and flood risk mitigation. <span class="hlt">Advances</span> in multi-objectives (MO) optimization techniques and ever growing computing power make it possible to design reservoir operating policies that represent Pareto-optimal tradeoffs between the multiple interests analysed. These progresses if on one hand are likely to enhance performances of commonly targeted objectives (such as hydropower production or water supply), on the other risk to strongly penalize all the interests not directly (i.e. mathematically) optimized within the MO algorithm. Alteration of <span class="hlt">hydrological</span> regime, although is a well established cause of ecological degradation and its evaluation and rehabilitation are commonly required by recent legislation (as the Water Framework Directive in Europe), is rarely embedded as an objective in MO planning of optimal releases from reservoirs. Moreover, even when it is explicitly considered, the criteria adopted for its evaluation are doubted and not commonly trusted, undermining the possibility of real implementation of environmentally friendly policies. The main challenges in defining and assessing <span class="hlt">hydrological</span> alterations are: how to define a reference state (referencing); how to define criteria upon which to build mathematical indicators of alteration (measuring); and finally how to aggregate the indicators in a single evaluation index that can be embedded in a MO optimization problem (valuing). This paper aims to address these issues by: i) discussing benefits and constrains of different approaches to referencing, measuring and valuing <span class="hlt">hydrological</span> alteration; ii) testing two alternative indices of <span class="hlt">hydrological</span> alteration in the context of MO problems, one based on the established framework of Indices of <span class="hlt">Hydrological</span> Alteration (IHA, Richter et al., 1996), and a novel satisfying the</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/28104836','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/28104836"><span>Validating a <span class="hlt">Predictive</span> Model of Acute <span class="hlt">Advanced</span> Imaging Biomarkers in Ischemic Stroke.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Bivard, Andrew; Levi, Christopher; Lin, Longting; Cheng, Xin; Aviv, Richard; Spratt, Neil J; Lou, Min; Kleinig, Tim; O'Brien, Billy; Butcher, Kenneth; Zhang, Jingfen; Jannes, Jim; Dong, Qiang; Parsons, Mark</p> <p>2017-03-01</p> <p><span class="hlt">Advanced</span> imaging to identify tissue pathophysiology may provide more accurate prognostication than the clinical measures used currently in stroke. This study aimed to derive and validate a <span class="hlt">predictive</span> model for functional outcome based on acute clinical and <span class="hlt">advanced</span> imaging measures. A database of prospectively collected sub-4.5 hour patients with ischemic stroke being assessed for thrombolysis from 5 centers who had computed tomographic perfusion and computed tomographic angiography before a treatment decision was assessed. Individual variable cut points were derived from a classification and regression tree analysis. The optimal cut points for each assessment variable were then used in a backward logic regression to <span class="hlt">predict</span> modified Rankin scale (mRS) score of 0 to 1 and 5 to 6. The variables remaining in the models were then assessed using a receiver operating characteristic curve analysis. Overall, 1519 patients were included in the study, 635 in the derivation cohort and 884 in the validation cohort. The model was highly accurate at <span class="hlt">predicting</span> mRS score of 0 to 1 in all patients considered for thrombolysis therapy (area under the curve [AUC] 0.91), those who were treated (AUC 0.88) and those with recanalization (AUC 0.89). Next, the model was highly accurate at <span class="hlt">predicting</span> mRS score of 5 to 6 in all patients considered for thrombolysis therapy (AUC 0.91), those who were treated (0.89) and those with recanalization (AUC 0.91). The odds ratio of thrombolysed patients who met the model criteria achieving mRS score of 0 to 1 was 17.89 (4.59-36.35, P <0.001) and for mRS score of 5 to 6 was 8.23 (2.57-26.97, P <0.001). This study has derived and validated a highly accurate model at <span class="hlt">predicting</span> patient outcome after ischemic stroke. © 2017 American Heart Association, Inc.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017HESS...21.4681B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017HESS...21.4681B"><span>A national-scale seasonal <span class="hlt">hydrological</span> forecast system: development and evaluation over Britain</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Bell, Victoria A.; Davies, Helen N.; Kay, Alison L.; Brookshaw, Anca; Scaife, Adam A.</p> <p>2017-09-01</p> <p>Skilful winter seasonal <span class="hlt">predictions</span> for the North Atlantic circulation and northern Europe have now been demonstrated and the potential for seasonal <span class="hlt">hydrological</span> forecasting in the UK is now being explored. One of the techniques being used combines seasonal rainfall forecasts provided by operational weather forecast systems with <span class="hlt">hydrological</span> modelling tools to provide estimates of seasonal mean river flows up to a few months ahead. The work presented here shows how spatial information contained in a distributed <span class="hlt">hydrological</span> model typically requiring high-resolution (daily or better) rainfall data can be used to provide an initial condition for a much simpler forecast model tailored to use low-resolution monthly rainfall forecasts. Rainfall forecasts (<q>hindcasts</q>) from the GloSea5 model (1996 to 2009) are used to provide the first assessment of skill in these national-scale flow forecasts. The skill in the combined modelling system is assessed for different seasons and regions of Britain, and compared to what might be achieved using other approaches such as use of an ensemble of historical rainfall in a <span class="hlt">hydrological</span> model, or a simple flow persistence forecast. The analysis indicates that only limited forecast skill is achievable for Spring and Summer seasonal <span class="hlt">hydrological</span> forecasts; however, Autumn and Winter flows can be reasonably well forecast using (ensemble mean) rainfall forecasts based on either GloSea5 forecasts or historical rainfall (the preferred type of forecast depends on the region). Flow forecasts using ensemble mean GloSea5 rainfall perform most consistently well across Britain, and provide the most skilful forecasts overall at the 3-month lead time. Much of the skill (64 %) in the 1-month ahead seasonal flow forecasts can be attributed to the <span class="hlt">hydrological</span> initial condition (particularly in regions with a significant groundwater contribution to flows), whereas for the 3-month ahead lead time, GloSea5 forecasts account for ˜ 70 % of the</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016EGUGA..1812793N','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016EGUGA..1812793N"><span>Streamflow hindcasting in European river basins via multi-parametric ensemble of the mesoscale <span class="hlt">hydrologic</span> model (mHM)</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Noh, Seong Jin; Rakovec, Oldrich; Kumar, Rohini; Samaniego, Luis</p> <p>2016-04-01</p> <p>There have been tremendous improvements in distributed <span class="hlt">hydrologic</span> modeling (DHM) which made a process-based simulation with a high spatiotemporal resolution applicable on a large spatial scale. Despite of increasing information on heterogeneous property of a catchment, DHM is still subject to uncertainties inherently coming from model structure, parameters and input forcing. Sequential data assimilation (DA) may facilitate improved streamflow <span class="hlt">prediction</span> via DHM using real-time observations to correct internal model states. In conventional DA methods such as state updating, parametric uncertainty is, however, often ignored mainly due to practical limitations of methodology to specify modeling uncertainty with limited ensemble members. If parametric uncertainty related with routing and runoff components is not incorporated properly, <span class="hlt">predictive</span> uncertainty by DHM may be insufficient to capture dynamics of observations, which may deteriorate <span class="hlt">predictability</span>. Recently, a multi-scale parameter regionalization (MPR) method was proposed to make <span class="hlt">hydrologic</span> <span class="hlt">predictions</span> at different scales using a same set of model parameters without losing much of the model performance. The MPR method incorporated within the mesoscale <span class="hlt">hydrologic</span> model (mHM, http://www.ufz.de/mhm) could effectively represent and control uncertainty of high-dimensional parameters in a distributed model using global parameters. In this study, we present a global multi-parametric ensemble approach to incorporate parametric uncertainty of DHM in DA to improve streamflow <span class="hlt">predictions</span>. To effectively represent and control uncertainty of high-dimensional parameters with limited number of ensemble, MPR method is incorporated with DA. Lagged particle filtering is utilized to consider the response times and non-Gaussian characteristics of internal <span class="hlt">hydrologic</span> processes. The hindcasting experiments are implemented to evaluate impacts of the proposed DA method on streamflow <span class="hlt">predictions</span> in multiple European river basins</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.fs.usda.gov/treesearch/pubs/35323','TREESEARCH'); return false;" href="https://www.fs.usda.gov/treesearch/pubs/35323"><span>A comparison of MIKE SHE and DRAINMOD for modeling forested wetland <span class="hlt">hydrology</span> in coastal South Carolina, USA</span></a></p> <p><a target="_blank" href="http://www.fs.usda.gov/treesearch/">Treesearch</a></p> <p>Zhaohua Dai; Devendra M. Amatya; Ge Sun; Carl C. Trettin; Changsheng Li; Harbin Li</p> <p>2010-01-01</p> <p>Models are widely used to assess <span class="hlt">hydrologic</span> impacts of land-management, land-use change and climate change. Two <span class="hlt">hydrologic</span> models with different spatial scales, MIKE SHE (spatially distributed, watershed-scale) and DRAINMOD (lumped, fieldscale), were compared in terms of their performance in <span class="hlt">predicting</span> stream flow and water table depth in a first-order forested...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2010EGUGA..12.4929V','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2010EGUGA..12.4929V"><span>Comparison of the performance and reliability of 18 lumped <span class="hlt">hydrological</span> models driven by ECMWF rainfall ensemble forecasts: a case study on 29 French catchments</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Velázquez, Juan Alberto; Anctil, François; Ramos, Maria-Helena; Perrin, Charles</p> <p>2010-05-01</p> <p>An ensemble forecasting system seeks to assess and to communicate the uncertainty of <span class="hlt">hydrological</span> <span class="hlt">predictions</span> by proposing, at each time step, an ensemble of forecasts from which one can estimate the probability distribution of the <span class="hlt">predictant</span> (the probabilistic forecast), in contrast with a single estimate of the flow, for which no distribution is obtainable (the deterministic forecast). In the past years, efforts towards the development of probabilistic <span class="hlt">hydrological</span> <span class="hlt">prediction</span> systems were made with the adoption of ensembles of numerical weather <span class="hlt">predictions</span> (NWPs). The additional information provided by the different available Ensemble <span class="hlt">Prediction</span> Systems (EPS) was evaluated in a <span class="hlt">hydrological</span> context on various case studies (see the review by Cloke and Pappenberger, 2009). For example, the European ECMWF-EPS was explored in case studies by Roulin et al. (2005), Bartholmes et al. (2005), Jaun et al. (2008), and Renner et al. (2009). The Canadian EC-EPS was also evaluated by Velázquez et al. (2009). Most of these case studies investigate the ensemble <span class="hlt">predictions</span> of a given <span class="hlt">hydrological</span> model, set up over a limited number of catchments. Uncertainty from weather <span class="hlt">predictions</span> is assessed through the use of meteorological ensembles. However, uncertainty from the tested <span class="hlt">hydrological</span> model and statistical robustness of the forecasting system when coping with different hydro-meteorological conditions are less frequently evaluated. The aim of this study is to evaluate and compare the performance and the reliability of 18 lumped <span class="hlt">hydrological</span> models applied to a large number of catchments in an operational ensemble forecasting context. Some of these models were evaluated in a previous study (Perrin et al. 2001) for their ability to simulate streamflow. Results demonstrated that very simple models can achieve a level of performance almost as high (sometimes higher) as models with more parameters. In the present study, we focus on the ability of the <span class="hlt">hydrological</span> models to</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://adsabs.harvard.edu/abs/2017AGUFM.H31F1577A','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFM.H31F1577A"><span>Establishment of quantitative <span class="hlt">hydrological</span> indexes for studies of hydro-biogeochemical interactions at the subsurface.</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Alves Meira Neto, A.; Sengupta, A.; Wang, Y.; Volkmann, T.; Chorover, J.; Troch, P. A. A.</p> <p>2017-12-01</p> <p><span class="hlt">Advances</span> in the understanding of processes in the critical zone (CZ) are dependent on studies coupling the fields of <span class="hlt">hydrology</span>, microbiology, geochemistry and soil development. At the same time, better insights are needed to integrate <span class="hlt">hydrologic</span> information into biogeochemical analysis of subsurface environments. This study investigated potential <span class="hlt">hydrological</span> indexes that help explaining spatiotemporal biogeochemical patterns. The miniLEO is a 2 m3, 10 degree sloping lysimeter located at Biosphere 2 - University of Arizona. The lysimeter was initially filled with pristine basaltic soil and subject to intermittent rainfall applications throughout the period of 18 months followed by its excavation, resulting in a grid-based sample collection at 324 locations. As a result, spatially distributed microbiological and geochemical patterns as well as soil physical properties were obtained. A <span class="hlt">hydrologic</span> model was then developed in order to simulate the history of the system until the excavation. After being calibrated against sensor data to match its observed input-state-output behavior, the resulting distributed fields of flow velocities and moisture states were retrieved. These results were translated into several <span class="hlt">hydrological</span> indexes to be used in with distributed microbiological and geochemical signatures. Our study attempts at conciliating sound <span class="hlt">hydrological</span> modelling with an investigation of the subsurface biological signatures, thus providing a unique opportunity for understanding of fine-scale hydro-biological interactions.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29726209','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29726209"><span>[Gene method for inconsistent <span class="hlt">hydrological</span> frequency calculation. I: Inheritance, variability and evolution principles of <span class="hlt">hydrological</span> genes].</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Xie, Ping; Wu, Zi Yi; Zhao, Jiang Yan; Sang, Yan Fang; Chen, Jie</p> <p>2018-04-01</p> <p>A stochastic <span class="hlt">hydrological</span> process is influenced by both stochastic and deterministic factors. A <span class="hlt">hydrological</span> time series contains not only pure random components reflecting its inheri-tance characteristics, but also deterministic components reflecting variability characteristics, such as jump, trend, period, and stochastic dependence. As a result, the stochastic <span class="hlt">hydrological</span> process presents complicated evolution phenomena and rules. To better understand these complicated phenomena and rules, this study described the inheritance and variability characteristics of an inconsistent <span class="hlt">hydrological</span> series from two aspects: stochastic process simulation and time series analysis. In addition, several frequency analysis approaches for inconsistent time series were compared to reveal the main problems in inconsistency study. Then, we proposed a new concept of <span class="hlt">hydrological</span> genes origined from biological genes to describe the inconsistent hydrolocal processes. The <span class="hlt">hydrologi-cal</span> genes were constructed using moments methods, such as general moments, weight function moments, probability weight moments and L-moments. Meanwhile, the five components, including jump, trend, periodic, dependence and pure random components, of a stochastic <span class="hlt">hydrological</span> process were defined as five <span class="hlt">hydrological</span> bases. With this method, the inheritance and variability of inconsistent <span class="hlt">hydrological</span> time series were synthetically considered and the inheritance, variability and evolution principles were fully described. Our study would contribute to reveal the inheritance, variability and evolution principles in probability distribution of <span class="hlt">hydrological</span> elements.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013AGUFMIN33C..05E','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013AGUFMIN33C..05E"><span>Design and Implementation of <span class="hlt">Hydrologic</span> Process Knowledge-base Ontology: A case study for the Infiltration Process</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Elag, M.; Goodall, J. L.</p> <p>2013-12-01</p> <p><span class="hlt">Hydrologic</span> modeling often requires the re-use and integration of models from different disciplines to simulate complex environmental systems. Component-based modeling introduces a flexible approach for integrating physical-based processes across disciplinary boundaries. Several <span class="hlt">hydrologic</span>-related modeling communities have adopted the component-based approach for simulating complex physical systems by integrating model components across disciplinary boundaries in a workflow. However, it is not always straightforward to create these interdisciplinary models due to the lack of sufficient knowledge about a <span class="hlt">hydrologic</span> process. This shortcoming is a result of using informal methods for organizing and sharing information about a <span class="hlt">hydrologic</span> process. A knowledge-based ontology provides such standards and is considered the ideal approach for overcoming this challenge. The aims of this research are to present the methodology used in analyzing the basic <span class="hlt">hydrologic</span> domain in order to identify <span class="hlt">hydrologic</span> processes, the ontology itself, and how the proposed ontology is integrated with the Water Resources Component (WRC) ontology. The proposed ontology standardizes the definitions of a <span class="hlt">hydrologic</span> process, the relationships between <span class="hlt">hydrologic</span> processes, and their associated scientific equations. The objective of the proposed <span class="hlt">Hydrologic</span> Process (HP) Ontology is to <span class="hlt">advance</span> the idea of creating a unified knowledge framework for components' metadata by introducing a domain-level ontology for <span class="hlt">hydrologic</span> processes. The HP ontology is a step toward an explicit and robust domain knowledge framework that can be evolved through the contribution of domain users. Analysis of the <span class="hlt">hydrologic</span> domain is accomplished using the Formal Concept Approach (FCA), in which the infiltration process, an important <span class="hlt">hydrologic</span> process, is examined. Two infiltration methods, the Green-Ampt and Philip's methods, were used to demonstrate the implementation of information in the HP ontology. Furthermore, a SPARQL</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014AGUFM.H31M..05L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014AGUFM.H31M..05L"><span>Exploring the linkage between drought, high temperatures, and <span class="hlt">hydrologic</span> sensitivities: A case study of the 2012 Great Plains drought.</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Livneh, B.; Hoerling, M. P.</p> <p>2014-12-01</p> <p>The occurrence of drought is associated with agricultural loss, water supply shortfalls, and other economic impacts. Here we explore the physical relationships between precipitation deficits, high temperatures, and <span class="hlt">hydrologic</span> responses as a pathway to better anticipate drought impacts. Current methodologies to <span class="hlt">predict</span> <span class="hlt">hydrologic</span> scarcity include local monitoring of river flows, remote sensing of land-surface wetness, drought indices, expert judgment, climate indices (e.g. SST-relationships) and the application of <span class="hlt">hydrologic</span> models. At longer lead times, <span class="hlt">predictions</span> of drought have most frequently been made on the basis of GCM ensembles, with subsequent downscaling of those to scales over which <span class="hlt">hydrologic</span> <span class="hlt">predictions</span> can be made. This study focuses on two important aspects of drought. First, we explore the causal hydro-climatic timeline of a drought event, namely (a) the lack of precipitation, which serves to reduce soil moisture and produce (b) a skewed Bowen ratio, i.e. comparatively more sensible heating (warming) with less ET, resulting in (c) anomalously warm conditions. We seek to assess the extent to which the lack of precipitation contributes to warming temperatures, and the further effects of that warming on <span class="hlt">hydrology</span> and the severity of drought impacts. An ensemble of GCM simulations will be used to explore the evolution of the land surface energy budget during a recent Great Plains drought event, which will subsequently be used to drive a <span class="hlt">hydrologic</span> model. Second, we examine the impacts of the critical assumptions relating climatic variables with water demand, specifically the relationship between potential evapotranspiration (PET) and temperature. The common oversimplification in relating PET to temperature is explored against a more physically consistent energy balance estimate of PET, using the Penman-Monteith approach and the <span class="hlt">hydrologic</span> impacts are presented. Results from this work are anticipated to have broad relevance for future water management</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFM.H21E1444M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFM.H21E1444M"><span>Designing for knowledge: bridging socio-<span class="hlt">hydrological</span> monitoring and beyond</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Mao, F.; Clark, J.; Buytaert, W.; Ochoa-Tocachi, B. F.; Hannah, D. M.</p> <p>2016-12-01</p> <p>Many methods and applications have been developed to research socio-<span class="hlt">hydrological</span> systems, such as participatory monitoring, environmental big data processing and sensor network data transmission. However, these data-centred activities are insufficient to guarantee successful knowledge co-generation, decision making or governance. This research suggests a shift of attentions in designing socio-<span class="hlt">hydrological</span> monitoring tools, from designing for data to designing for knowledge (DfK). Compared to the former strategy, DfK has at least three features as follows. (1) Why monitor? DfK demands the data produced by the newly introduced monitoring application to have potentials to generate socio-<span class="hlt">hydrological</span> knowledge that supports decision making or management. It means that when designing a monitoring tool, we should not only answer how to collect data, but also questions such as how to best use the collected data in the form of knowledge. (2) What is the role of monitoring? DfK admits that the socio-<span class="hlt">hydrological</span> data and knowledge generated by monitoring is just one of many kinds to support decision making and management. It means that the importance of monitoring and scientific evidence should not be overestimated, and knowledge cogeneration and synthesis should be considered in <span class="hlt">advance</span> in the monitoring design process. (3) Who participate? DfK implies a wider engagement of stakeholders, which is not restricted between volunteers as data collectors and providers, and scientist and researcher communities as main data users. It requires a broader consideration of users, including not only data collectors, processors and interpreters, but also local and indigenous knowledge providers, and decision makers who use the knowledge and data. In summary, this research proposes a knowledge-centred strategy in designing participatory socio-<span class="hlt">hydrological</span> monitoring tools, in order to make monitoring more useful and effective.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016HESS...20.2649S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016HESS...20.2649S"><span>A retrospective streamflow ensemble forecast for an extreme <span class="hlt">hydrologic</span> event: a case study of Hurricane Irene and on the Hudson River basin</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Saleh, Firas; Ramaswamy, Venkatsundar; Georgas, Nickitas; Blumberg, Alan F.; Pullen, Julie</p> <p>2016-07-01</p> <p>This paper investigates the uncertainties in hourly streamflow ensemble forecasts for an extreme <span class="hlt">hydrological</span> event using a <span class="hlt">hydrological</span> model forced with short-range ensemble weather <span class="hlt">prediction</span> models. A state-of-the art, automated, short-term <span class="hlt">hydrologic</span> <span class="hlt">prediction</span> framework was implemented using GIS and a regional scale <span class="hlt">hydrological</span> model (HEC-HMS). The <span class="hlt">hydrologic</span> framework was applied to the Hudson River basin ( ˜ 36 000 km2) in the United States using gridded precipitation data from the National Centers for Environmental <span class="hlt">Prediction</span> (NCEP) North American Regional Reanalysis (NARR) and was validated against streamflow observations from the United States Geologic Survey (USGS). Finally, 21 precipitation ensemble members of the latest Global Ensemble Forecast System (GEFS/R) were forced into HEC-HMS to generate a retrospective streamflow ensemble forecast for an extreme <span class="hlt">hydrological</span> event, Hurricane Irene. The work shows that ensemble stream discharge forecasts provide improved <span class="hlt">predictions</span> and useful information about associated uncertainties, thus improving the assessment of risks when compared with deterministic forecasts. The uncertainties in weather inputs may result in false warnings and missed river flooding events, reducing the potential to effectively mitigate flood damage. The findings demonstrate how errors in the ensemble median streamflow forecast and time of peak, as well as the ensemble spread (uncertainty) are reduced 48 h pre-event by utilizing the ensemble framework. The methodology and implications of this work benefit efforts of short-term streamflow forecasts at regional scales, notably regarding the peak timing of an extreme <span class="hlt">hydrologic</span> event when combined with a flood threshold exceedance diagram. Although the modeling framework was implemented on the Hudson River basin, it is flexible and applicable in other parts of the world where atmospheric reanalysis products and streamflow data are available.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014HESS...18..417H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014HESS...18..417H"><span>What makes Darwinian <span class="hlt">hydrology</span> "Darwinian"? Asking a different kind of question about landscapes</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Harman, C.; Troch, P. A.</p> <p>2014-02-01</p> <p>There have been repeated calls for a Darwinian approach to <span class="hlt">hydrologic</span> science, or for a synthesis of Darwinian and Newtonian approaches, to deepen understanding of the <span class="hlt">hydrologic</span> system in the larger landscape context, and so develop a better basis for <span class="hlt">predictions</span> now and in an uncertain future. But what exactly makes a Darwinian approach to <span class="hlt">hydrology</span> "Darwinian"? While there have now been a number of discussions of Darwinian approaches, many referencing Harte (2002), the term is potentially a source of confusion because its connections to Darwin remain allusive rather than explicit. Here we suggest that the Darwinian approach to <span class="hlt">hydrology</span> follows the example of Charles Darwin by focusing attention on the patterns of variation in populations and seeking hypotheses that explain these patterns in terms of the mechanisms and conditions that determine their historical development. These hypotheses do not simply catalog patterns or <span class="hlt">predict</span> them statistically - they connect the present structure with processes operating in the past. Nor are they explanations presented without independent evidence or critical analysis - Darwin's hypotheses about the mechanisms underlying present-day variation could be independently tested and validated. With a Darwinian framework in mind, it is easy to see that a great deal of <span class="hlt">hydrologic</span> research has already been done that contributes to a Darwinian <span class="hlt">hydrology</span> - whether deliberately or not. We discuss some practical and philosophical issues with this approach to <span class="hlt">hydrologic</span> science: how are explanatory hypotheses generated? What constitutes a good hypothesis? How are hypotheses tested? "Historical" sciences - including paleohydrology - have long grappled with these questions, as must a Darwinian <span class="hlt">hydrologic</span> science. We can draw on Darwin's own example for some answers, though there are ongoing debates about the philosophical nature of his methods and reasoning. Darwin used a range of methods of historical reasoning to develop explanatory</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015EGUGA..17..690M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015EGUGA..17..690M"><span><span class="hlt">Hydrological</span> response of the Mediterranean catchments- A review</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Merheb, Mohammad; Moussa, Roger; Abdallah, Chadi; Colin, François; Perrin, Charles; Baghdadi, Nicolas</p> <p>2015-04-01</p> <p>-stressed region that witnesses long low-flows periods. <span class="hlt">Predictions</span> of runoff hydrograph give poor results. For flow duration curves and low flows regionalization, statistical and geo-statistical methods appear to outperform parametric approaches and regression respectively. Mixed results were found for regional flood analysis which appears to be the most common regionalization practice in the area. Finally, given the great heterogeneity in the <span class="hlt">hydrological</span> responses of Mediterranean catchments and the increasing anthropogenic and climatic pressures, the region appears to be in need for more detailed observations and new modeling techniques adapted to its specificities. Keywords: <span class="hlt">hydrology</span>, catchment, Mediterranean, modeling, regionalization, anthropogenic impact, climate change.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013EGUGA..15.7844R','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013EGUGA..15.7844R"><span>Open source data assimilation framework for <span class="hlt">hydrological</span> modeling</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Ridler, Marc; Hummel, Stef; van Velzen, Nils; Katrine Falk, Anne; Madsen, Henrik</p> <p>2013-04-01</p> <p>An open-source data assimilation framework is proposed for <span class="hlt">hydrological</span> modeling. Data assimilation (DA) in hydrodynamic and <span class="hlt">hydrological</span> forecasting systems has great potential to improve <span class="hlt">predictions</span> and improve model result. The basic principle is to incorporate measurement information into a model with the aim to improve model results by error minimization. Great strides have been made to assimilate traditional in-situ measurements such as discharge, soil moisture, hydraulic head and snowpack into <span class="hlt">hydrologic</span> models. More recently, remotely sensed data retrievals of soil moisture, snow water equivalent or snow cover area, surface water elevation, terrestrial water storage and land surface temperature have been successfully assimilated in <span class="hlt">hydrological</span> models. The assimilation algorithms have become increasingly sophisticated to manage measurement and model bias, non-linear systems, data sparsity (time & space) and undetermined system uncertainty. It is therefore useful to use a pre-existing DA toolbox such as OpenDA. OpenDA is an open interface standard for (and free implementation of) a set of tools to quickly implement DA and calibration for arbitrary numerical models. The basic design philosophy of OpenDA is to breakdown DA into a set of building blocks programmed in object oriented languages. To implement DA, a model must interact with OpenDA to create model instances, propagate the model, get/set variables (or parameters) and free the model once DA is completed. An open-source interface for <span class="hlt">hydrological</span> models exists capable of all these tasks: OpenMI. OpenMI is an open source standard interface already adopted by key <span class="hlt">hydrological</span> model providers. It defines a universal approach to interact with <span class="hlt">hydrological</span> models during simulation to exchange data during runtime, thus facilitating the interactions between models and data sources. The interface is flexible enough so that models can interact even if the model is coded in a different language, represent</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70023605','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70023605"><span>The concept of <span class="hlt">hydrologic</span> landscapes</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Winter, T.C.</p> <p>2001-01-01</p> <p><span class="hlt">Hydrologic</span> landscapes are multiples or variations of fundamental <span class="hlt">hydrologic</span> landscape units. A fundamental <span class="hlt">hydrologic</span> landscape unit is defined on the basis of land-surface form, geology, and climate. The basic land-surface form of a fundamental <span class="hlt">hydrologic</span> landscape unit is an upland separated from a lowland by an intervening steeper slope. Fundamental <span class="hlt">hydrologic</span> landscape units have a complete <span class="hlt">hydrologic</span> system consisting of surface runoff, ground-water flow, and interaction with atmospheric water. By describing actual landscapes in terms of land-surface slope, hydraulic properties of soils and geologic framework, and the difference between precipitation and evapotranspiration, the <span class="hlt">hydrologic</span> system of actual landscapes can be conceptualized in a uniform way. This conceptual framework can then be the foundation for design of studies and data networks, syntheses of information on local to national scales, and comparison of process research across small study units in a variety of settings. The Crow Wing River watershed in central Minnesota is used as an example of evaluating stream discharge in the context of <span class="hlt">hydrologic</span> landscapes. Lake-research watersheds in Wisconsin, Minnesota, North Dakota, and Nebraska are used as an example of using the <span class="hlt">hydrologic</span>-landscapes concept to evaluate the effect of ground water on the degree of mineralization and major-ion chemistry of lakes that lie within ground-water flow systems.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/27879861','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/27879861"><span><span class="hlt">Hydrologic</span> Remote Sensing and Land Surface Data Assimilation.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Moradkhani, Hamid</p> <p>2008-05-06</p> <p>Accurate, reliable and skillful forecasting of key environmental variables such as soil moisture and snow are of paramount importance due to their strong influence on many water resources applications including flood control, agricultural production and effective water resources management which collectively control the behavior of the climate system. Soil moisture is a key state variable in land surface-atmosphere interactions affecting surface energy fluxes, runoff and the radiation balance. Snow processes also have a large influence on land-atmosphere energy exchanges due to snow high albedo, low thermal conductivity and considerable spatial and temporal variability resulting in the dramatic change on surface and ground temperature. Measurement of these two variables is possible through variety of methods using ground-based and remote sensing procedures. Remote sensing, however, holds great promise for soil moisture and snow measurements which have considerable spatial and temporal variability. Merging these measurements with <span class="hlt">hydrologic</span> model outputs in a systematic and effective way results in an improvement of land surface model <span class="hlt">prediction</span>. Data Assimilation provides a mechanism to combine these two sources of estimation. Much success has been attained in recent years in using data from passive microwave sensors and assimilating them into the models. This paper provides an overview of the remote sensing measurement techniques for soil moisture and snow data and describes the <span class="hlt">advances</span> in data assimilation techniques through the ensemble filtering, mainly Ensemble Kalman filter (EnKF) and Particle filter (PF), for improving the model <span class="hlt">prediction</span> and reducing the uncertainties involved in <span class="hlt">prediction</span> process. It is believed that PF provides a complete representation of the probability distribution of state variables of interests (according to sequential Bayes law) and could be a strong alternative to EnKF which is subject to some limitations including the linear</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFM.H53I1601P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFM.H53I1601P"><span>Understanding the Amazon <span class="hlt">Hydrology</span> for Sustainable Hydropower Development</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Pokhrel, Y. N.; Chaudhari, S. N.</p> <p>2017-12-01</p> <p>Construction of 147 new hydropower dams, many of which are large, has been proposed in the Amazon river basin, despite the continuous stacking of negative impacts from the existing ones. These dams are continued to be built in a way that disrupts river ecology, causes large-scale deforestation, and negatively affects both the food systems nearby and downstream communities. In this study, we explore the impacts of the existing and proposed hydropower dams on the <span class="hlt">hydrological</span> fluxes across the Amazonian Basin by incorporating human impact modules in an extensively validated regional <span class="hlt">hydrological</span> model called LEAF-Hydro-Flood (LHF). We conduct two simulations, one in offline mode, forced by observed meteorological data for the historical period of 2000-2016 and the other in a coupled mode using the Weather Research and Forecasting (WRF) regional climate model. We mainly analyze terrestrial water storage and streamflow changes during the period of dam operations with and without human impacts. It is certain that the Amazon will undergo some major <span class="hlt">hydrological</span> changes such as decrease in streamflow downstream in the coming decades caused due to these proposed dams. This study helps us understand and represent processes in a <span class="hlt">predictable</span> manner, and provides the ability to evaluate future scenarios with dams and other major human influences while considering climate change in the basin. It also provides important insights on how to redesign the hydropower systems to make them truly renewable in terms of energy production, <span class="hlt">hydrology</span> and ecology.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/20010097890','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/20010097890"><span>Modeling and Analysis of Global and Regional Climate Change in Relation to Atmospheric <span class="hlt">Hydrologic</span> Processes</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Johnson, Donald R.</p> <p>2001-01-01</p> <p>This research was directed to the development and application of global isentropic modeling and analysis capabilities to describe <span class="hlt">hydrologic</span> processes and energy exchange in the climate system, and discern regional climate change. An additional objective was to investigate the accuracy and theoretical limits of global climate <span class="hlt">predictability</span> which are imposed by the inherent limitations of simulating trace constituent transport and the <span class="hlt">hydrologic</span> processes of condensation, precipitation and cloud life cycles.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014AGUFM.H34E..05S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014AGUFM.H34E..05S"><span>Socio-<span class="hlt">Hydrology</span>: Conceptual and Methodological Challenges in the Bidirectional Coupling of Human and Water Systems</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Scott, C. A.</p> <p>2014-12-01</p> <p>This presentation reviews conceptual <span class="hlt">advances</span> in the emerging field of socio-<span class="hlt">hydrology</span> that focuses on coupled human and water systems. An important current challenge is how to better couple the bidirectional influences between human and water systems, which lead to emergent dynamics. The interactions among (1) the structure and dynamics of systems with (2) human values and norms lead to (3) outcomes, which in turn influence subsequent interactions. Human influences on <span class="hlt">hydrological</span> systems are relatively well understood, chiefly resulting from developments in the field of water resources. The ecosystem-service concept of cultural value has expanded understanding of decision-making beyond economic rationality criteria. <span class="hlt">Hydrological</span> impacts on social processes are less well developed conceptually, but this is changing with growing attention to vulnerability, adaptation, and resilience, particularly in the face of climate change. Methodological limitations, especially in characterizing the range of human responses to <span class="hlt">hydrological</span> events and drivers, still pose challenges to modeling bidirectional human-water influences. Evidence from multiple case studies, synthesized in more broadly generic syndromes, helps surmount these methodological limitations and offers the potential to improve characterization and quantification of socio-<span class="hlt">hydrological</span> systems.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFM.H43S..04X','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFM.H43S..04X"><span>Understanding controls of <span class="hlt">hydrologic</span> processes across two headwater monolithological catchments using model-data synthesis</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Xiao, D.; Shi, Y.; Hoagland, B.; Del Vecchio, J.; Russo, T. A.; DiBiase, R. A.; Li, L.</p> <p>2017-12-01</p> <p>How do watershed <span class="hlt">hydrologic</span> processes differ in catchments derived from different lithology? This study compares two first order, deciduous forest watersheds in Pennsylvania, a sandstone watershed, Garner Run (GR, 1.34 km2), and a shale-derived watershed, Shale Hills (SH, 0.08 km2). Both watersheds are simulated using a combination of national datasets and field measurements, and a physics-based land surface <span class="hlt">hydrologic</span> model, Flux-PIHM. We aim to evaluate the effects of lithology on watershed <span class="hlt">hydrology</span> and assess if we can simulate a new watershed without intensive measurements, i.e., directly use calibration information from one watershed (SH) to reproduce <span class="hlt">hydrologic</span> dynamics of another watershed (GR). Without any calibration, the model at GR based on national datasets and calibration inforamtion from SH cannot capture some discharge peaks or the baseflow during dry periods. The model <span class="hlt">prediction</span> agrees well with the GR field discharge and soil moisture after calibrating the soil hydraulic parameters using the uncertainty based Hornberger-Spear-Young algorithm and the Latin Hypercube Sampling method. Agreeing with the field observation and national datasets, the difference in parameter values shows that the sandstone watershed has a larger averaged soil pore diameter, greater water storage created by porosity, lower water retention ability, and greater preferential flow. The water budget calculation shows that the riparian zone and the colluvial valley serves as buffer zones that stores water at GR. Using the same procedure, we compared Flux-PIHM simulations with and without a field measured surface boulder map at GR. When the boulder map is used, the <span class="hlt">prediction</span> of areal averaged soil moisture is improved, without performing extra calibration. When calibrated separately, the cases with or without boulder map yield different calibration values, but their <span class="hlt">hydrologic</span> <span class="hlt">predictions</span> are similar, showing equifinality. The calibrated soil hydraulic parameter values in the</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.ars.usda.gov/research/publications/publication/?seqNo115=263408','TEKTRAN'); return false;" href="http://www.ars.usda.gov/research/publications/publication/?seqNo115=263408"><span>SWAT ungauged: <span class="hlt">Hydrological</span> budget and crop yield <span class="hlt">predictions</span> in the Upper Mississippi River Basin</span></a></p> <p><a target="_blank" href="https://www.ars.usda.gov/research/publications/find-a-publication/">USDA-ARS?s Scientific Manuscript database</a></p> <p></p> <p></p> <p>Physically based, distributed <span class="hlt">hydrologic</span> models are increasingly used in assessments of water resources, best management practices, and climate and land use changes. Model performance evaluation in ungauged basins is an important research topic. In this study, we propose a framework for developing S...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015EGUGA..17.2730D','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015EGUGA..17.2730D"><span><span class="hlt">Hydrology</span> for everyone: Share your knowledge</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Dogulu, Nilay; Dogulu, Canay</p> <p>2015-04-01</p> <p><span class="hlt">Hydrology</span>, the science of water, plays a central role in understanding the function and behaviour of water on the earth. Given the increasingly complex, uncertain, and dynamic nature of this system, the study of <span class="hlt">hydrology</span> presents challenges in solving water-related problems in societies. While researchers in <span class="hlt">hydrologic</span> science and engineering embrace these challenges, it is important that we also realize our critical role in promoting the basic understanding of <span class="hlt">hydrology</span> concepts among the general public. <span class="hlt">Hydrology</span> is everywhere, yet, the general public often lacks the basic understanding of the <span class="hlt">hydrologic</span> environment surrounding them. Essentially, we believe that a basic level of knowledge on <span class="hlt">hydrology</span> is a must for everyone and that this knowledge might facilitate resilience of communities to <span class="hlt">hydrological</span> extremes. For instance, in case of flood and drought conditions, which are the most frequent and widespread <span class="hlt">hydrological</span> phenomena that societies live with, a key aspect of facilitating community resilience would be to create awareness on the <span class="hlt">hydrological</span>, meteorological, and climatological processes behind floods and droughts, and also on their potential implications on water resources management. Such knowledge awareness can lead to an increase in individuals' awareness on their role in water-related problems which in turn can potentially motivate them to adopt preparedness behaviours. For these reasons, embracing an approach that will increase <span class="hlt">hydrologic</span> literacy of the general public should be a common objective for the <span class="hlt">hydrologic</span> community. This talk, hopefully, will motivate researchers in <span class="hlt">hydrologic</span> science and engineering to share their knowledge with the general public. We, as early career hydrologists, should take this responsibility more than anybody else. Start teaching <span class="hlt">hydrology</span> now and share your knowledge with people around you - friends, family, relatives, neighbours, and others. There is <span class="hlt">hydrology</span> for everyone!</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19960001924','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19960001924"><span>Development of <span class="hlt">advanced</span> structural analysis methodologies for <span class="hlt">predicting</span> widespread fatigue damage in aircraft structures</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Harris, Charles E.; Starnes, James H., Jr.; Newman, James C., Jr.</p> <p>1995-01-01</p> <p>NASA is developing a 'tool box' that includes a number of <span class="hlt">advanced</span> structural analysis computer codes which, taken together, represent the comprehensive fracture mechanics capability required to <span class="hlt">predict</span> the onset of widespread fatigue damage. These structural analysis tools have complementary and specialized capabilities ranging from a finite-element-based stress-analysis code for two- and three-dimensional built-up structures with cracks to a fatigue and fracture analysis code that uses stress-intensity factors and material-property data found in 'look-up' tables or from equations. NASA is conducting critical experiments necessary to verify the <span class="hlt">predictive</span> capabilities of the codes, and these tests represent a first step in the technology-validation and industry-acceptance processes. NASA has established cooperative programs with aircraft manufacturers to facilitate the comprehensive transfer of this technology by making these <span class="hlt">advanced</span> structural analysis codes available to industry.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017EGUGA..1912576P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017EGUGA..1912576P"><span>Synchronising data sources and filling gaps by global <span class="hlt">hydrological</span> modelling</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Pimentel, Rafael; Crochemore, Louise; Hasan, Abdulghani; Pineda, Luis; Isberg, Kristina; Arheimer, Berit</p> <p>2017-04-01</p> <p>The <span class="hlt">advances</span> in remote sensing in the last decades combined with the creation of different open <span class="hlt">hydrological</span> databases have generated a very large amount of useful information for global <span class="hlt">hydrological</span> modelling. Working with this huge number of datasets to set up a global <span class="hlt">hydrological</span> model can constitute challenges such as multiple data formats and big heterogeneity on spatial and temporal resolutions. Different initiatives have made effort to homogenize some of these data sources, i.e. GRDC (Global Runoff Data Center), HYDROSHEDS (SHuttle Elevation Derivatives at multiple Scales), GLWD (Global Lake and Wetland Database) for runoff, watershed delineation and water bodies respectively. However, not all the related issues are covered or homogenously solved at the global scale and new information is continuously available to complete the current ones. This work presents synchronising efforts to make use of different global data sources needed to set up the semi-distributed <span class="hlt">hydrological</span> model HYPE (<span class="hlt">Hydrological</span> <span class="hlt">Predictions</span> for the Environment) at the global scale. These data sources included: topography for watershed delineation, gauging stations of river flow, and extention of lakes, flood plains and land cover classes. A new database with approximately 100 000 subbasins, with an average area of 1000 km2, was created. Subbasin delineation was done combining Global Width Database for Large River (GWD-LR), SRTM high-resolution elevation data and a number of forced points of interest (gauging station of river flow, lakes, reservoirs, urban areas, nuclear plants and areas with high risk of flooding). Regarding flow data, the locations of GRDC stations were checked or placed along the river network when necessary, and completed with available information from national water services in data-sparse regions. A screening of doublet stations and associated time series was necessary to efficiently combine the two types of data sources. A total number about 21 000 stations were</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013AGUFM.U41A..01B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013AGUFM.U41A..01B"><span>Making sense of Big Data in <span class="hlt">Hydrology</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>Booth, N.; Blodgett, D. L.; Briar, D.</p> <p>2013-12-01</p> <p>At the same time that "big data" promises to help provide new insights for understanding earth processes, budget challenges require we more effectively use data collected by organizations other than our own. Answering societally relevant questions related to water requires that we consider all natural and anthropogenic aspects of the <span class="hlt">hydrologic</span> cycle. How do we integrate across organizations and across water cycle components to satisfy these challenges and expectations? We now need to move beyond metadata that describe individual datasets to an ability to interrogate integrated collections of observations. Furthermore, we need to be able to query across obvious (yet elusive) dimensions including <span class="hlt">hydrologic</span> context and position while filtering for data of a known quality that meets our purpose. In addition, we need to traverse the climate/geography interface, efficiently attributing a climate signal to watersheds. We know that water flows downhill and that after heavy rain, streams flood. But we cannot systematically query for observations made during a flashy summer storm-related flood upstream from notable points on a river or stream such as water treatment intakes. USGS has long committed to providing real-time access to surface and groundwater monitoring networks across the United States. Of the over 45 million requests made for these data in a recent month, nearly a quarter were made via mobile devices. An additional 19.8 million requests were made to web services that provide content according to community and international data standards -- presumably to support other applications and mash ups. This presentation will describe ongoing efforts at the USGS on how we are working with the earth sciences and water resource management communities to develop and implement new techniques for both delivering and consuming <span class="hlt">hydrologic</span> data. Our strategy has been an "all-of-the-above" approach whereby we recognize and work to <span class="hlt">advance</span> best practices in various communities</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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