Mason Valley Groundwater Model: Linking Surface Water and Groundwater in the Walker River Basin,Nevada1 |
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Authors: | Rosemary WH Carroll Greg Pohll David McGraw Chris Garner Anna Knust Doug Boyle Tim Minor Scott Bassett Karl Pohlmann |
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Institution: | 1. Respectively, Assistant Research Hydrologist (Carroll, McGraw, Garner, and Knust), Associate Research Professor (Pohll and Boyle), and Associate Research Hydrologist (Pohlmann), Division of Hydrologic Sciences, Desert Research Institute, 2215 Raggio Parkway, Reno, Nevada 89512;2. Associate Research Scientist (Minor), Division of Earth and Ecosystem Science, Desert Research Institute, Reno, Nevada;3. and Assistant Professor (Bassett), Department of Geography, University of Nevada, Reno, Nevada. |
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Abstract: | Carroll, Rosemary W.H., Greg Pohll, David McGraw, Chris Garner, Anna Knust, Doug Boyle, Tim Minor, Scott Bassett, and Karl Pohlmann, 2010. Mason Valley Groundwater Model: Linking Surface Water and Groundwater in the Walker River Basin, Nevada. Journal of the American Water Resources Association (JAWRA) 46(3):554-573. DOI: 10.1111/j.1752-1688.2010.00434.x Abstract: An integrated surface water and groundwater model of Mason Valley, Nevada is constructed to replicate the movement of water throughout the different components of the demand side of water resources in the Walker River system. The Mason Valley groundwater surface water model (MVGSM) couples the river/drain network with agricultural demand areas and the groundwater system using MODFLOW, MODFLOW’s streamflow routing package, as well as a surface water linking algorithm developed for the project. The MVGSM is capable of simulating complex feedback mechanisms between the groundwater and surface water system that is not dependent on linearity among the related variables. The spatial scale captures important hydrologic components while the monthly stress periods allow for seasonal evaluation. A simulation spanning an 11-year record shows the methodology is robust under diverse climatic conditions. The basin-wide modeling approach predicts a river system generally gaining during the summer irrigation period but losing during winter months and extended periods of drought. River losses to the groundwater system approach 25% of the river’s annual budget. Reducing diversions to hydrologic response units will increase river flows exiting the model domain, but also has the potential to increase losses from the river to groundwater storage. |
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Keywords: | surface water and groundwater exchange water resources management numeric model semi-arid basin irrigated agriculture |
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