The success of a hydrological model is primarily governed by the model parameters that are generally obtained through calibration and validation of the model against historical rainfall and runoff data. Therefore, calibration and validation are critical steps in hydrological modelling, which assist minimisation of uncertainty in runoff estimates. Calibration and validation of a hydrological model depends on various factors such as availability of necessary data, length and quality of the data and choice of optimisation technique. In this study, impact of data length to obtain the best set of calibrated parameters of a hydrological model, known as Australian Water Balance Model (AWBM) is investigated. Several combinations of calibration and ...
Six steps can be distinguished in the process of hydrological modelling: the perceptual model (decid...
Hydrologic models using water balance approaches typically use continuously observed streamflow data...
Applications of runoff models usually rely on long and continuous runoff time series for model calib...
In this study, a quantitative assessment of uncertainty was made in connection with the calibration ...
AbstractIn order to assess the effects of calibration data series length on the performance and opti...
Many calibrated hydrological models are inconsistent with the behavioral functions of catchments and...
The temporal split-sample approach is the most common method to allocate observed data into calibrat...
Conceptual rainfall‐runoff (CRR) models are widely used for runoff simulation and for prediction und...
Conceptual hydrological models often rely on calibration for the identification of their parameters....
Hydrologic rainfall-runoff models are usually calibrated with reference to a limited number of recor...
Copyright © 2008 ASCEIn many regions where rainfall runoff models are required, there is a lack of s...
[1] This paper investigates the actual extrapolation capacity of three hydrological models in differ...
Two problems are addressed which arise when using monthly water balance models as an aid to making d...
Hydrologic models using water balance approaches typically use continuously observed streamflow data...
Water scarcity which arose with the growth of population, industrialization, urbanization and climat...
Six steps can be distinguished in the process of hydrological modelling: the perceptual model (decid...
Hydrologic models using water balance approaches typically use continuously observed streamflow data...
Applications of runoff models usually rely on long and continuous runoff time series for model calib...
In this study, a quantitative assessment of uncertainty was made in connection with the calibration ...
AbstractIn order to assess the effects of calibration data series length on the performance and opti...
Many calibrated hydrological models are inconsistent with the behavioral functions of catchments and...
The temporal split-sample approach is the most common method to allocate observed data into calibrat...
Conceptual rainfall‐runoff (CRR) models are widely used for runoff simulation and for prediction und...
Conceptual hydrological models often rely on calibration for the identification of their parameters....
Hydrologic rainfall-runoff models are usually calibrated with reference to a limited number of recor...
Copyright © 2008 ASCEIn many regions where rainfall runoff models are required, there is a lack of s...
[1] This paper investigates the actual extrapolation capacity of three hydrological models in differ...
Two problems are addressed which arise when using monthly water balance models as an aid to making d...
Hydrologic models using water balance approaches typically use continuously observed streamflow data...
Water scarcity which arose with the growth of population, industrialization, urbanization and climat...
Six steps can be distinguished in the process of hydrological modelling: the perceptual model (decid...
Hydrologic models using water balance approaches typically use continuously observed streamflow data...
Applications of runoff models usually rely on long and continuous runoff time series for model calib...