Hydrological processes in a watershed consist of multiple sub-processes (such as plant growth, evapotranspiration, water yield, and soil–water balance) that have complex interactions. The common practice of calibrating hydrological models against only a single variable (e.g., streamflow) can lead to parameter uncertainty (also known as equifinality), resulting in significant uncertainties in the representation and simulation of sub-processes. As multi-variable calibration can be a potential solution to this issue, we tested the integration of spatially and temporally gridded remotely sensed evapotranspiration (RS-ET) data with the Soil and Water Assessment Tool (SWAT) hydrological model. This approach was intended to reduce equifinality by ...
Uncertainty is inherent in any hydrologic prediction; an apparently well-performing model can be pse...
The accuracy of hydrological model predictions is limited by uncertainties in model structure and pa...
In this study, streamflow (Qs) and satellite-based actual evapotranspiration (ETa) are used in a mul...
ABSTRACT Although intrinsic, uncertainty for hydrological model estimation is not always reported. T...
In this paper, evapotranspiration (ET) and leaf area index (LAI) were used to calibrate the SWAT mod...
In this paper, evapotranspiration (ET) and leaf area index (LAI) were used to calibrate the SWAT mod...
In this paper, evapotranspiration (ET) and leaf area index (LAI) were used to calibrate the SWAT mod...
Conventional calibration methods adopted in hydrological modelling are based on streamflow data meas...
Historically, many watershed studies have been based on using the streamflow flux, typically from a ...
Spatially distributed hydrologic models are useful for understanding the water balance dynamics of c...
Model calibration and validation are challenging in poorly gauged basins. We developed and applied a...
Calibrating a spatially distributed hydrological model of a region with complex and highly diverse a...
Conventional calibration methods used in hydrological modelling are based on runoff observations at ...
Food, energy, and water (FEW) nexus studies require reliable estimates of water availability, use, a...
Hydrological models are usually calibrated against observed streamflow (Qobs), which is not applicab...
Uncertainty is inherent in any hydrologic prediction; an apparently well-performing model can be pse...
The accuracy of hydrological model predictions is limited by uncertainties in model structure and pa...
In this study, streamflow (Qs) and satellite-based actual evapotranspiration (ETa) are used in a mul...
ABSTRACT Although intrinsic, uncertainty for hydrological model estimation is not always reported. T...
In this paper, evapotranspiration (ET) and leaf area index (LAI) were used to calibrate the SWAT mod...
In this paper, evapotranspiration (ET) and leaf area index (LAI) were used to calibrate the SWAT mod...
In this paper, evapotranspiration (ET) and leaf area index (LAI) were used to calibrate the SWAT mod...
Conventional calibration methods adopted in hydrological modelling are based on streamflow data meas...
Historically, many watershed studies have been based on using the streamflow flux, typically from a ...
Spatially distributed hydrologic models are useful for understanding the water balance dynamics of c...
Model calibration and validation are challenging in poorly gauged basins. We developed and applied a...
Calibrating a spatially distributed hydrological model of a region with complex and highly diverse a...
Conventional calibration methods used in hydrological modelling are based on runoff observations at ...
Food, energy, and water (FEW) nexus studies require reliable estimates of water availability, use, a...
Hydrological models are usually calibrated against observed streamflow (Qobs), which is not applicab...
Uncertainty is inherent in any hydrologic prediction; an apparently well-performing model can be pse...
The accuracy of hydrological model predictions is limited by uncertainties in model structure and pa...
In this study, streamflow (Qs) and satellite-based actual evapotranspiration (ETa) are used in a mul...