The original aim of this research was to determine the best means of calculating the relative delay time parameter of the Laurenson runoff routing method of flood estimation. Early testing conducted as a part of achieving this end showed that the model could be quite insensitive to the means used to calculate relative delay. Model sensitivity to the means of calculating this parameter had apparently not yet been verified, and if it was insensitive, the best means of calculating the parameter was not required. Hence it was decided to test the thesis that the model was insensitive to the means of calculating the relative delay time parameter. The thesis was tested by applying the model to a range of flood sizes on two catchments using five di...
Flooding due to rivers overflowing have affected this year many countries in the world. The engender...
Abstract Natural flood management (NFM) techniques attract much interest in flood risk management sc...
Flood forecasting and warning is necessary as there will always be a residual risk against floods, n...
The original aim of this research was to determine the best means of calculating the relative delay ...
An investigation carried out into the values of lag time for catchment areas as measured from centr...
Published ArticleLarge errors in peak discharge estimates at catchment scales can be ascribed to err...
Time is an important element in hydrologic design. Most hydrologic models require a watershed charac...
Despite significant developments, the simple, lumped, conceptual, rainfall-runoff model is still wid...
The effect of the time step of calibration data on the performance of a hydrological model is examin...
Concentration times in small and medium-sized basins (∼10–1000 km2) are commonly less than 24 h. Flo...
Abstract: Most catchment-scale rainfall-runoff models represent as time-invariant such features of t...
Due to the character of the original source materials and the nature of batch digitization, quality ...
Time of concentration (TC) is a parameter in runoff estimation, used to study and design different t...
Lag time is an essential input to the most common synthetic unit-hydrograph models. The lag time for...
The study of generation process of subsurface stormflow, typical of well-drained and high permeable ...
Flooding due to rivers overflowing have affected this year many countries in the world. The engender...
Abstract Natural flood management (NFM) techniques attract much interest in flood risk management sc...
Flood forecasting and warning is necessary as there will always be a residual risk against floods, n...
The original aim of this research was to determine the best means of calculating the relative delay ...
An investigation carried out into the values of lag time for catchment areas as measured from centr...
Published ArticleLarge errors in peak discharge estimates at catchment scales can be ascribed to err...
Time is an important element in hydrologic design. Most hydrologic models require a watershed charac...
Despite significant developments, the simple, lumped, conceptual, rainfall-runoff model is still wid...
The effect of the time step of calibration data on the performance of a hydrological model is examin...
Concentration times in small and medium-sized basins (∼10–1000 km2) are commonly less than 24 h. Flo...
Abstract: Most catchment-scale rainfall-runoff models represent as time-invariant such features of t...
Due to the character of the original source materials and the nature of batch digitization, quality ...
Time of concentration (TC) is a parameter in runoff estimation, used to study and design different t...
Lag time is an essential input to the most common synthetic unit-hydrograph models. The lag time for...
The study of generation process of subsurface stormflow, typical of well-drained and high permeable ...
Flooding due to rivers overflowing have affected this year many countries in the world. The engender...
Abstract Natural flood management (NFM) techniques attract much interest in flood risk management sc...
Flood forecasting and warning is necessary as there will always be a residual risk against floods, n...