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The surface runoff model, based on the concept of uniform nonlinearity (Dooge 1967), has three parameters. It is shown that these parameters can be estimated from the informaion that can be easily o...
The converging overland flow model contains five parameters, three geometric and two kinematic. An attempt is made in this study to estimate these parameters utilizing watershed topographic characte...
An indirect method of determining flood plain aquifer parameters from estimated autocorrelation of groundwater table data is presented. For this purpose a stream-aquifer system is approximated by a ...
The interpretation of rain-runoff measurements from 6 small (less than 17 ha) urban catchments is described. The recording period covers mostly 1979-1983. Relations between rain- and runoff depths w...
Groundwater levels fluctuate as a result of changes in the relation between inflow and outflow to the aquifer, and the magnitude of the fluctuations are also depending on the geologic conditions in ...
Pumping and recovery test data in phyllite formations were analysed under linear flow conditions by incorporating modification in the method proposed by Sen (1986). Although the Sen (1986) method is...
Macro-scale hydrological modelling implies a repeated application of a model within an area using regional parameters. These parameters are based on climate and landscape characteristics, and they a...
Geostatistical analysis of some of the hydrogeological parameters viz., transmissivity, water level, and depth to the aquifer basement, has been carried out for an aquifer in the Vaippar basin in a we...
The parameters of hydrological models for catchments with few or no discharge records can be estimated using regional information. One can assume that catchments with similar characteristics show a si...
The estimation of hydrological model parameters is a challenging task. With increasing capacity of computational power several complex optimization algorithms have emerged, but none of the algorithms ...
An application of regression relationships depending on geomorphic parameters is proposed to predict the amount of the average annual suspended sediment yield at different sections of the drainage net...
There are two approaches available for mapping water retention parameters over the study area using a spatial interpolation method. (1) Retention models can be first fitted to retention curves availab...

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