Hyper‐Resolution Continental‐Scale 3‐D Aquifer Parameterization for Groundwater Modeling
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Univ Arizona, Dept Hydrol & Atmospher SciIssue Date
2020-04-04
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AMER GEOPHYSICAL UNIONCitation
de Graaf, I., Condon, L., & Maxwell, R. (2020). Hyper‐Resolution Continental‐Scale 3‐D Aquifer Parameterization for Groundwater Modeling. Water Resources Research, 56(5), e2019WR026004.Journal
WATER RESOURCES RESEARCHRights
© 2020. The Authors. This is an open access article under the terms of the Creative Commons Attribution License.Collection Information
This item from the UA Faculty Publications collection is made available by the University of Arizona with support from the University of Arizona Libraries. If you have questions, please contact us at repository@u.library.arizona.edu.Abstract
Groundwater is the world's most important freshwater resource. Despite this importance, groundwater flow and interactions between groundwater and other parts of the hydrological cycle are often neglected or simplified in large-scale hydrological models. One of the challenges in simulating groundwater flow and continental to global scales is the lack of consistent globally available hydrogeological data. These input data are needed for a more realistic physical representation of the groundwater system, enabling the simulation of groundwater head dynamics and lateral flows. A realistic representation of the subsurface is especially important as large-scale hydrological models move to finer resolutions and aim to provide accurate and locally relevant hydrologic information everywhere. In this study, we aim at improving and extending on current available large-scale data sets providing information of the subsurface. We present a detailed aquifer representation for the continental United States and Canada at hyper resolution (250 x 250 m). We integrate local hydrogeological information, including observations of aquifer layer thickness, conductivity, and vertical structure, to obtain representative aquifer parameter values applicable to the continental scale. The methods used are simple and can be expanded to other parts of the world. Hydrological simulations were performed using the integrated hydrological model ParFlow and demonstrated improved model performance when using the new aquifer parameterization. Our results support that more detailed and accurate aquifer parameterization will advance our understanding of the groundwater system at larger scales.Note
Open access articleISSN
0043-1397EISSN
1944-7973Version
Final published versionae974a485f413a2113503eed53cd6c53
10.1029/2019wr026004
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Except where otherwise noted, this item's license is described as © 2020. The Authors. This is an open access article under the terms of the Creative Commons Attribution License.