The current study evaluates the impacts of various sources of uncertainty involved in hydrologic modeling on parameter behavior and regionalization utilizing different Bayesian likelihood functions and the Differential Evolution Adaptive Metropolis (DREAM) algorithm. The developed likelihood functions differ in their underlying assumptions and treatment of error sources. We apply the developed method to a snow accumulation and ablation model (National Weather Service SNOW17) and generate parameter ensembles to predict snow water equivalent (SWE). Observational data include precipitation and air temperature forcing along with SWE measurements from 24 sites with diverse hydroclimatic characteristics. A multiple linear regression model is used...
The simulation of snow water equivalent (SWE) remains difficult for regional climate models. Accurat...
The simulation of snow water equivalent (SWE) remains difficult for regional climate models. Accurat...
The simulation of snow water equivalent (SWE) remains difficult for regional climate models. Accurat...
The current study evaluates the impacts of various sources of uncertainty involved in hydrologic mod...
The National Weather Service (NWS) uses the SNOW17 model to forecast snow accumulation and ablation ...
Bayesian inference is used to study the effect of precipitation and model structural uncertainty on ...
The National Weather Service (NWS) uses the SNOW17 model to forecast snow accumulation and ablation ...
Physically based models provide insights into key hydrologic processes but are associated with unce...
Prediction of snow in regional and global hydrological models has been a difficult task due to error...
Mountainous watersheds have always remained a challenge for the modelers due to ample variations tak...
The impacts of climate change on water resources in snow- and glacier-dominated basins are of great ...
Parameter uncertainty estimation is one of the major challenges in hydrological modeling. Here we pr...
Parameter estimation in rainfall-runoff models is affected by uncertainties in the measured input/ou...
Accurate specification of the model error covariances in data assimilation systems is a challenging ...
Modeling snow hydrology for cold regions remains a problematic aspect of many hydro-environmental mo...
The simulation of snow water equivalent (SWE) remains difficult for regional climate models. Accurat...
The simulation of snow water equivalent (SWE) remains difficult for regional climate models. Accurat...
The simulation of snow water equivalent (SWE) remains difficult for regional climate models. Accurat...
The current study evaluates the impacts of various sources of uncertainty involved in hydrologic mod...
The National Weather Service (NWS) uses the SNOW17 model to forecast snow accumulation and ablation ...
Bayesian inference is used to study the effect of precipitation and model structural uncertainty on ...
The National Weather Service (NWS) uses the SNOW17 model to forecast snow accumulation and ablation ...
Physically based models provide insights into key hydrologic processes but are associated with unce...
Prediction of snow in regional and global hydrological models has been a difficult task due to error...
Mountainous watersheds have always remained a challenge for the modelers due to ample variations tak...
The impacts of climate change on water resources in snow- and glacier-dominated basins are of great ...
Parameter uncertainty estimation is one of the major challenges in hydrological modeling. Here we pr...
Parameter estimation in rainfall-runoff models is affected by uncertainties in the measured input/ou...
Accurate specification of the model error covariances in data assimilation systems is a challenging ...
Modeling snow hydrology for cold regions remains a problematic aspect of many hydro-environmental mo...
The simulation of snow water equivalent (SWE) remains difficult for regional climate models. Accurat...
The simulation of snow water equivalent (SWE) remains difficult for regional climate models. Accurat...
The simulation of snow water equivalent (SWE) remains difficult for regional climate models. Accurat...