2013
DOI: 10.1002/hyp.9867
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Storage dynamics simulations in prairie wetland hydrology models: evaluation and parameterization

Abstract: Abstract:The contributing areas of streams in the Prairie regions of Canada and the northern U.S. are dominated by complexes of wetlands which store and release water. Prior research has suggested the existence of hysteresis between the total volume of water stored in prairie wetlands within a drainage basin and the basin's contributing area. To simulate the relationship between storage and contributing area in a way that accounts for hysteresis, two wetland hydrology models with vastly different levels of com… Show more

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Cited by 107 publications
(136 citation statements)
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“…The size and extent of water bodies across Canada vary both geographically and temporally throughout the year. This variation depends significantly on local climate and topography: the prairie region has many shallow water depressions (prairie potholes) that are filled through snow redistribution, snow melt, infiltration, and precipitation, and can evaporate quickly and exhibit "spill and fill" movement [45]. Due to local topography, small amounts of contributed water influence the areal extent of water bodies significantly.…”
Section: Discussionmentioning
confidence: 99%
“…The size and extent of water bodies across Canada vary both geographically and temporally throughout the year. This variation depends significantly on local climate and topography: the prairie region has many shallow water depressions (prairie potholes) that are filled through snow redistribution, snow melt, infiltration, and precipitation, and can evaporate quickly and exhibit "spill and fill" movement [45]. Due to local topography, small amounts of contributed water influence the areal extent of water bodies significantly.…”
Section: Discussionmentioning
confidence: 99%
“…Pomeroy et al (2010) and Pomeroy et al (2014) utilized the Prairie Hydrological Model (PHM), a modified version of the Cold Regions Hydrological Model (Pomeroy et al, 2007), to simulate the hydrologic influence of prairie pothole depressions within the Canadian plains. Pomeroy et al (2014) incorporated a conceptual, network-based model of synthetic wetlands parameterized via the separate physically-based Wetland Digital Elevation Model Ponding Model (Shook et al, 2013;Pomeroy et al, 2014). Pomeroy et al (2014) demonstrated that removal of all simulated depressions within the PHM resulted in a 55% increase in total flow volumes throughout their simulation period.…”
Section: Introductionmentioning
confidence: 99%
“…Improved terrain representation has helped characterize hysteretic relationships between water storage and contributing area in large wetland complexes within parameterized runoff models (Shook et al, 2013), improved mapping in and along river channels to parameterize network-level structure and flood inundation models (French, 2003;Kinzel et al, 2007;Snyder, 2009;Bates, 2012), and expanded investigation of geomorphological change in floodplains (Thoma et al, 2005;Jones et al, 2007). Lidar provides vertical information that permits the direct retrieval of forest attributes such as tree height and canopy structure (Hyyppä et al, 2012;Vosselman and Maas, 2010) that can be used to model canopy volume (Palminteri et al, 2012), biomass (Zhao et al, 2009), and the transmittance of solar radiation (Essery et al, 2008;Musselman et al, 2013;von Bode et al, 2014).…”
Section: Model Parameterization and Verificationmentioning
confidence: 99%