Urbanization and development of lands have increased significantly in last few years to fulfil the requirements of increasing population and economic and infrastructure development in India. The hydrological response of ...

Sedimentation of the reservoir is a function of soil erosion rate of the river catchment area which reduces the water storage capacity of reservoir and availability of water for its designated use. Erosion of topsoil ...

In this paper, an attempt has been made to compare the revised capacities of Rajaval and Kharo reservoirs of southern Gujarat (India). The image analysis technique of remote sensing data was used to estimate the revised ...

Drought duration, frequency and severity of low flow of the past events occurred in the Kharun river basin in Chhattisgarh state are analyzed using daily stream flow data. Stream flow drought severity is the total deficit ...

Estimates of trends of climatic changes at basin and state scales are required for developing adaptation strategies related to planning, development and management of water resources. In the present study, seasonal and ...

Runoff is a key component of hydrological cycle and it is relevant for the basin planning and management programme for conservation and development or natural resources. This implies the need to develop and test hydrological ...

Freshwater resources are becoming increasingly limited day by day and policy makers are in demand for new and effective tools for the monitoring of water consumption rates.

आदिकाल से ही मानसून और चौमासा भारतीय संस्कृति के अभिन्न अंग रहें हैं। हमारे यहाँ कुल जितना पानी बरसता है उसका 70-90 प्रतिशत चौमासे में ही गिर जाता है।

Watershed development and management plans are very important for harnessing surface water and groundwater resources. To prepare a comprehensive watershed development plan, it becomes necessary to understand the topography, ...

Reliable prediction of the runoff generation and its routing to the outlets represents one of the most basic challenging and important aspect of the hydrology,