2021
DOI: 10.1016/j.envsoft.2021.105131
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Calibration of hydrological models considering process interdependence: A case study of SWAT model

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Cited by 18 publications
(4 citation statements)
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“…It affects the partitioning of solar radiation into latent and sensible heat as well as the partitioning of precipitation into direct runoff and catchment storage (Duethmann et al, 2022). Accurate prediction of soil moisture is thus essential for simulating streamflow, evapotranspiration and percolation (Rajib et al, 2016;Rajat and Athira, 2021) and for constraining 355 the parameters of hydrological models. The role of groundwater in the seasonal and multi-year dynamics of streamflow is also essential: in many temperate catchments, groundwater stores water during wet periods and releases it throughout the year, thus contributing greatly to low flows (Pelletier and Andréassian, 2022).…”
Section: Model Calibration and Evaluationmentioning
confidence: 99%
“…It affects the partitioning of solar radiation into latent and sensible heat as well as the partitioning of precipitation into direct runoff and catchment storage (Duethmann et al, 2022). Accurate prediction of soil moisture is thus essential for simulating streamflow, evapotranspiration and percolation (Rajib et al, 2016;Rajat and Athira, 2021) and for constraining 355 the parameters of hydrological models. The role of groundwater in the seasonal and multi-year dynamics of streamflow is also essential: in many temperate catchments, groundwater stores water during wet periods and releases it throughout the year, thus contributing greatly to low flows (Pelletier and Andréassian, 2022).…”
Section: Model Calibration and Evaluationmentioning
confidence: 99%
“…The current study uses S as a calibration variable, and the parameters which are significant for streamflow generation are considered for calibration. The parameter Curve Number, CN2 is directly related to the surface runoff generation process (Rajat, 2021). The erosion and sediment yields are estimated for each HRU with Modified Universal Soil Loss Equation (MUSLE) (Williams, 1995), as in Eq.…”
Section: Analysis and Evaluationmentioning
confidence: 99%
“…Developing hydrological models at the basin scale is challenging due to the complexity of hydrological processes, spatial variability of soil, geology, and land use/cover characteristics, and spatial and temporal variability of climatic conditions. Hydrological models enable us to understand how physical or climatic changes could affect basinwide hydrological processes and predict basin response to natural or artificial changes (Gupta et al 2005;Rajat 2021).…”
Section: Introductionmentioning
confidence: 99%