2022
DOI: 10.1029/2022wr032694
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The Numerical Formulation of Simple Hysteretic Models to Simulate the Large‐Scale Hydrological Impacts of Prairie Depressions

Abstract: Topographic depressions have large impacts on the hydrology, ecology, and biogeochemistry in prairie environments. In many prairie landscapes, there has not been sufficient energy, water, or time to carve conventional drainage networks, and, as a result, much of the landscape drains internally to millions of small topographic depressions. Topographic depressions control the hydrological flow regime through their role in storing water from precipitation and snow melt and the subsequent impacts of depression sto… Show more

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Cited by 5 publications
(3 citation statements)
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“…Thus, care must be taken with models that aggregate the bulk response of a wetland complex by representation as a single equivalent wetland (e.g., Liu et al, 2008;Yang et al, 2010); the emergent upscaled response could not be emulated using a single wetland, regardless of whether effective parameterization or calibration is used. This finding is consistent with other studies (e.g., Clark and Shook, 2022;Evenson et al, 2016;Pomeroy et al, 2014;Shook and Pomeroy, 2011) which emphasize that for modeling complex fill-and-spill dynamics in wetlands, a single "equivalent wetland" is insufficient. The capability of the UWFS model to consider the effects of local contributing area of wetlands and wetland cascading depth increases the ability of hydrological models to account for dynamics of fill-and-spill process in wetland complexes.…”
Section: Sensitivity Analysissupporting
confidence: 92%
“…Thus, care must be taken with models that aggregate the bulk response of a wetland complex by representation as a single equivalent wetland (e.g., Liu et al, 2008;Yang et al, 2010); the emergent upscaled response could not be emulated using a single wetland, regardless of whether effective parameterization or calibration is used. This finding is consistent with other studies (e.g., Clark and Shook, 2022;Evenson et al, 2016;Pomeroy et al, 2014;Shook and Pomeroy, 2011) which emphasize that for modeling complex fill-and-spill dynamics in wetlands, a single "equivalent wetland" is insufficient. The capability of the UWFS model to consider the effects of local contributing area of wetlands and wetland cascading depth increases the ability of hydrological models to account for dynamics of fill-and-spill process in wetland complexes.…”
Section: Sensitivity Analysissupporting
confidence: 92%
“…This forms a complicated hydrological condition, in which the hydrologic responses heavily depend on landscape feature detail (Fang et al, 2007;van der Kamp et al, 2003;Spence, 2010), and are subject to nonlinear hysteresis (Shook and Pomeroy, 2011). With few exceptions (Clark and Shook, 2022), current hydrological models do not represent dominant hydrological processes in prairie landscapes and fail in reproducing the observed runoff. Here we attempted to maximize the use of observed gauge information (Table S1) by implementing a data-driven reconstruction scheme.…”
Section: Streamflow Reconstruction Schemementioning
confidence: 99%
“…This forms a complicated hydrological condition, in which the hydrologic responses heavily depend on landscape feature detail (Fang et al, 2007;van der Kamp et al, 2003;Spence, 2010), and are subject to nonlinear hysteresis (Shook and Pomeroy, 2011). With few exceptions (Clark and Shook, 2022), current hydrological models do not represent dominant hydrological processes in prairie landscapes and fail in reproducing the observed runoff. Here we attempted to maximize the use of observed gauge information (Table S1) by implementing a data-driven reconstruction scheme.…”
Section: Streamflow Reconstruction Schemementioning
confidence: 99%