Implementation and evaluation of a monthly water balance model over the U.S. on an 800 m grid

We simulate the 1950-2010 water balance for the conterminous U.S. (CONUS) with a monthly water balance model (MWBM) using the 800 m Parameter-elevation Regression on Independent Slopes Model (PRISM) data set as model input. We employed observed snow and streamflow data sets to guide modification of...
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Autor*in:	Hostetler, S.W [verfasserIn] Alder, J.R

Format:	Artikel
Sprache:	Englisch

Erschienen:	2016

Übergeordnetes Werk:	Enthalten in: Water resources research - Hoboken, NJ : Wiley, 1965, 52(2016), 12, Seite 9600
Übergeordnetes Werk:	volume:52 ; year:2016 ; number:12 ; pages:9600

Links:	Volltext Link aufrufen

DOI / URN:	10.1002/2016WR018665

Katalog-ID:	OLC1987623347

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allfields	10.1002/2016WR018665 doi PQ20170206 (DE-627)OLC1987623347 (DE-599)GBVOLC1987623347 (PRQ)c650-c8dfe03ebbc34236c8f1648a4e8eceb4b9864b9a9c0337cf7dd33dbf2a3da9b60 (KEY)0046260820160000052001209600implementationandevaluationofamonthlywaterbalancem DE-627 ger DE-627 rakwb eng 550 DE-600 38.85 bkl Hostetler, S.W verfasserin aut Implementation and evaluation of a monthly water balance model over the U.S. on an 800 m grid 2016 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier We simulate the 1950-2010 water balance for the conterminous U.S. (CONUS) with a monthly water balance model (MWBM) using the 800 m Parameter-elevation Regression on Independent Slopes Model (PRISM) data set as model input. We employed observed snow and streamflow data sets to guide modification of the snow and potential evapotranspiration components in the default model and to evaluate model performance. Based on various metrics and sensitivity tests, the modified model yields reasonably good simulations of seasonal snowpack in the West (range of bias of ±50 mm at 68% of 713 SNOTEL sites), the gradients and magnitudes of actual evapotranspiration, and runoff (median correlation of 0.83 and median Nash-Sutcliff efficiency of 0.6 between simulated and observed annual time series at 1427 USGS gage sites). The model generally performs well along the Pacific Coast, the high elevations of the Basin and Range and over the Midwest and East, but not as well over the dry areas of the Southwest and upper Plains regions due, in part, to the apportioning of direct versus delayed runoff. Sensitivity testing and application of the MWBM to simulate the future water balance at four National Parks when driven by 30 climate models from the Climate Model Intercomparison Program Phase 5 (CMIP5) demonstrate that the model is useful for evaluating first-order, climate driven hydrologic change on monthly and annual time scales. Alder, J.R oth Enthalten in Water resources research Hoboken, NJ : Wiley, 1965 52(2016), 12, Seite 9600 (DE-627)129088285 (DE-600)5564-5 (DE-576)014422980 0043-1397 nnns volume:52 year:2016 number:12 pages:9600 http://dx.doi.org/10.1002/2016WR018665 Volltext http://search.proquest.com/docview/1859504530 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OLC-FOR SSG-OPC-GGO GBV_ILN_4219 38.85 AVZ AR 52 2016 12 9600
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title_sort	implementation and evaluation of a monthly water balance model over the u.s. on an 800 m grid
title_auth	Implementation and evaluation of a monthly water balance model over the U.S. on an 800 m grid
abstract	We simulate the 1950-2010 water balance for the conterminous U.S. (CONUS) with a monthly water balance model (MWBM) using the 800 m Parameter-elevation Regression on Independent Slopes Model (PRISM) data set as model input. We employed observed snow and streamflow data sets to guide modification of the snow and potential evapotranspiration components in the default model and to evaluate model performance. Based on various metrics and sensitivity tests, the modified model yields reasonably good simulations of seasonal snowpack in the West (range of bias of ±50 mm at 68% of 713 SNOTEL sites), the gradients and magnitudes of actual evapotranspiration, and runoff (median correlation of 0.83 and median Nash-Sutcliff efficiency of 0.6 between simulated and observed annual time series at 1427 USGS gage sites). The model generally performs well along the Pacific Coast, the high elevations of the Basin and Range and over the Midwest and East, but not as well over the dry areas of the Southwest and upper Plains regions due, in part, to the apportioning of direct versus delayed runoff. Sensitivity testing and application of the MWBM to simulate the future water balance at four National Parks when driven by 30 climate models from the Climate Model Intercomparison Program Phase 5 (CMIP5) demonstrate that the model is useful for evaluating first-order, climate driven hydrologic change on monthly and annual time scales.
abstractGer	We simulate the 1950-2010 water balance for the conterminous U.S. (CONUS) with a monthly water balance model (MWBM) using the 800 m Parameter-elevation Regression on Independent Slopes Model (PRISM) data set as model input. We employed observed snow and streamflow data sets to guide modification of the snow and potential evapotranspiration components in the default model and to evaluate model performance. Based on various metrics and sensitivity tests, the modified model yields reasonably good simulations of seasonal snowpack in the West (range of bias of ±50 mm at 68% of 713 SNOTEL sites), the gradients and magnitudes of actual evapotranspiration, and runoff (median correlation of 0.83 and median Nash-Sutcliff efficiency of 0.6 between simulated and observed annual time series at 1427 USGS gage sites). The model generally performs well along the Pacific Coast, the high elevations of the Basin and Range and over the Midwest and East, but not as well over the dry areas of the Southwest and upper Plains regions due, in part, to the apportioning of direct versus delayed runoff. Sensitivity testing and application of the MWBM to simulate the future water balance at four National Parks when driven by 30 climate models from the Climate Model Intercomparison Program Phase 5 (CMIP5) demonstrate that the model is useful for evaluating first-order, climate driven hydrologic change on monthly and annual time scales.
abstract_unstemmed	We simulate the 1950-2010 water balance for the conterminous U.S. (CONUS) with a monthly water balance model (MWBM) using the 800 m Parameter-elevation Regression on Independent Slopes Model (PRISM) data set as model input. We employed observed snow and streamflow data sets to guide modification of the snow and potential evapotranspiration components in the default model and to evaluate model performance. Based on various metrics and sensitivity tests, the modified model yields reasonably good simulations of seasonal snowpack in the West (range of bias of ±50 mm at 68% of 713 SNOTEL sites), the gradients and magnitudes of actual evapotranspiration, and runoff (median correlation of 0.83 and median Nash-Sutcliff efficiency of 0.6 between simulated and observed annual time series at 1427 USGS gage sites). The model generally performs well along the Pacific Coast, the high elevations of the Basin and Range and over the Midwest and East, but not as well over the dry areas of the Southwest and upper Plains regions due, in part, to the apportioning of direct versus delayed runoff. Sensitivity testing and application of the MWBM to simulate the future water balance at four National Parks when driven by 30 climate models from the Climate Model Intercomparison Program Phase 5 (CMIP5) demonstrate that the model is useful for evaluating first-order, climate driven hydrologic change on monthly and annual time scales.
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container_issue	12
title_short	Implementation and evaluation of a monthly water balance model over the U.S. on an 800 m grid
url	http://dx.doi.org/10.1002/2016WR018665 http://search.proquest.com/docview/1859504530
remote_bool	false
author2	Alder, J.R
author2Str	Alder, J.R
ppnlink	129088285
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author2_role	oth
doi_str	10.1002/2016WR018665
up_date	2024-07-03T14:42:38.700Z
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