Hydrologic simulations of different models have direct impact on the accuracy of discharge prediction because of the diverse model structure. This study is an attempt to comprehend the uncertainty in discharge prediction of two models in the Ghatshila catchment, Subarnarekha Basin in India. A lumped Probability Distribution Model (PDM) and semi-distributed Soil and Water Assessment Tool (SWAT) were applied to simulate the discharge from 24 years of records (1982–2005), using gridded ground based meteorological variables. The results indicate a marginal outperformance of SWAT model with 0.69 Nash-Sutcliffe (NSE) for predicting discharge as compared to PDM with 0.62 NSE value. Extreme high flows are clearly depicted in the flow duration curve...
In flood-prone areas it is important to do the runoff prediction so that the early warning system ca...
Continuous simulation of flows for ungauged catchments is a methodology being developed for estimati...
An assessment of uncertainty in flood hydrograph features, e.g., peak discharge and flood volume due...
Hydrologic simulations of different models have direct impact on the accuracy of discharge predictio...
Hydrologic simulations of different models have direct impact on the accuracy of discharge predictio...
Uncertainty in hydrological model prediction stems from different sources such as parameter uncertai...
Rainfall runoff modeling has been a subject of interest for decades due to a need to understand a ca...
The generalised likelihood uncertainty estimation (GLUE) approach was applied to assess the performa...
The objective of this study was to assess the performance and predictive uncertainty of the Soil and...
Stream flow, which is a part of the integrated process of atmospheric and topographic processes, is ...
An assessment of uncertainty in flood hydrograph features, e.g., peak discharge and flood volume due...
An assessment of uncertainty in flood hydrograph features, e.g., peak discharge and flood volume due...
An assessment of uncertainty in flood hydrograph features, e.g., peak discharge and flood volume due...
In flood-prone areas it is important to do the runoff prediction so that the early warning system ca...
Assessing the impacts of Land Use (LU) and climate change on future streamflow projections is necess...
In flood-prone areas it is important to do the runoff prediction so that the early warning system ca...
Continuous simulation of flows for ungauged catchments is a methodology being developed for estimati...
An assessment of uncertainty in flood hydrograph features, e.g., peak discharge and flood volume due...
Hydrologic simulations of different models have direct impact on the accuracy of discharge predictio...
Hydrologic simulations of different models have direct impact on the accuracy of discharge predictio...
Uncertainty in hydrological model prediction stems from different sources such as parameter uncertai...
Rainfall runoff modeling has been a subject of interest for decades due to a need to understand a ca...
The generalised likelihood uncertainty estimation (GLUE) approach was applied to assess the performa...
The objective of this study was to assess the performance and predictive uncertainty of the Soil and...
Stream flow, which is a part of the integrated process of atmospheric and topographic processes, is ...
An assessment of uncertainty in flood hydrograph features, e.g., peak discharge and flood volume due...
An assessment of uncertainty in flood hydrograph features, e.g., peak discharge and flood volume due...
An assessment of uncertainty in flood hydrograph features, e.g., peak discharge and flood volume due...
In flood-prone areas it is important to do the runoff prediction so that the early warning system ca...
Assessing the impacts of Land Use (LU) and climate change on future streamflow projections is necess...
In flood-prone areas it is important to do the runoff prediction so that the early warning system ca...
Continuous simulation of flows for ungauged catchments is a methodology being developed for estimati...
An assessment of uncertainty in flood hydrograph features, e.g., peak discharge and flood volume due...