2017
DOI: 10.1016/j.agwat.2016.07.011
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Simulating hydrological and nonpoint source pollution processes in a karst watershed: A variable source area hydrology model evaluation

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Cited by 64 publications
(42 citation statements)
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“…TopoSWAT (Easton et al., 2008), a version of SWAT that incorporates topographic index as an input layer, was initialized over the resulting 29 subbasins using a 10‐m digital elevation model (DEM) resampled from 1‐m light detection and ranging (LiDAR) based data (PAMAP Program, 2006) and soils from the FAO‐United Nations Educational, Scientific and Cultural Organization (UNESCO) Digital Soil Map of the World (FAO‐UN Land and Water Division, 2007). TopoSWAT was used in this study on the basis of previous research in the northeastern United States that showed that TopoSWAT adequately captures the variable source hydrology of this region (Amin, Veith, Collick, Karsten, & Buda, 2017, 2018; Collick et al., 2014, 2016; Liu et al., 2017).…”
Section: Methodsmentioning
confidence: 99%
“…TopoSWAT (Easton et al., 2008), a version of SWAT that incorporates topographic index as an input layer, was initialized over the resulting 29 subbasins using a 10‐m digital elevation model (DEM) resampled from 1‐m light detection and ranging (LiDAR) based data (PAMAP Program, 2006) and soils from the FAO‐United Nations Educational, Scientific and Cultural Organization (UNESCO) Digital Soil Map of the World (FAO‐UN Land and Water Division, 2007). TopoSWAT was used in this study on the basis of previous research in the northeastern United States that showed that TopoSWAT adequately captures the variable source hydrology of this region (Amin, Veith, Collick, Karsten, & Buda, 2017, 2018; Collick et al., 2014, 2016; Liu et al., 2017).…”
Section: Methodsmentioning
confidence: 99%
“…Specifically, we delineated watershed boundary and drainage network based on a 10‐m digital elevation model (DEM) and created six subbasins by specifying subbasin outlets at the locations of the monitoring stream flumes. When creating HRUs, we overlaid a TI layer with the FAO‐UNESCO (United Nations Educational, Scientific and Cultural Organization) Digital Soil Map of the World layer (FAO, 2007) instead of conventional SWAT slope classes and soil layers (Collick et al, 2015; Amin et al, 2017). …”
Section: Methodsmentioning
confidence: 99%
“…(3) in the SWAT model, was run with the determined data and the data from the Environmental Protection Bureau of Xiangtan, and the Nash Sutcliffe efficiency coefficient (E ns ) and regression coefficient (R 2 ) can be calculated with the following formulas [26][27]…”
Section: Determining δ and Kmentioning
confidence: 99%