Review Note: Recent submissions

  • Bhar, A.K. (National Institute of Hydrology, 1985)
    Snow and ice is a major component of Water Resources and it is hydrologically important in India because of the presence of mighty snow clad Himalayas. Major north Indian rivers originate from the ...
  • Goyal, V. C.; Seth, S. M. (National Institute of Hydrology, 1985)
    Microprocessors and microcomputers are increasingly being used in a number of hydrometeorological data collection systems. Almost all modern data acquisition systems use microprocessors for collection ...
  • Bhatia, K. K. S. (National Institute of Hydrology, 1985)
    Sedimentation is a natural process which occurs whenever the flow of a sediment carrying river is impounded by any kind of obstacle. Proper management of water resources often requires the construction of ...
  • Seethapathi, P. V.; Jain, S. K. (National Institute of Hydrology, 1985)
    The range analysis is a part of the general probability theory of storage. In this report the works dealing with the range analysis for storage related problems have been reviewed. In the beginning, ...
  • Chand, Ramesh; Seth, S. M. (National Institute of Hydrology, 1985)
    In this report it is proposed to review the status of applications of environmental isotopes in hydrological investigations. These include Tritium H³ Carbon-14(C14), naturally occurring isotopes and ...
  • Harikrishna, H.; Mishra, G. C. (National Institute of Hydrology, 1985)
    In irrigation practices, certain portion of the applied water, over and above the consumptive use, infiltrates into the ground to reach either an aquifer as deep percolation or to a nearby stream ...
  • Palaniappan, A. B.; Seth, S. M. (National Institute of Hydrology, 1985)
    Although a river occupies a small portion of the. catchment, its role in shaping the landscape is enormous. The river and the adjoining plains and as a matter of fact, the whole catchment undergoes ...
  • Palaniappan, A. B.; Seth, S. M. (National Institute of Hydrology, 1985)
    Because of ever increasing human activities in the flood plains, the river environment gets affected. The movement of flood along the flood plains is quite complex. The flood plains act as ...
  • Ramasastri, K. S.; Seth, S. M. (National Institute of Hydrology, 1985)
    For estimating dependable yield while planning and designing water resources development projects, long period series of stream flow are required. However, since the flow data are generally available ...
  • Seth, S. M.; Ramasastri, K. S. (National Institute of Hydrology, 1985)
    Measurement of precipitation with gauges dates back to more than 2000 years. With the development of civilization and science, the demand for intensity of precipitation and its distribution in ...
  • Seth, S. M.; Goel, N. K. (1985)
    Time series analysis belongs to major statistical techniques used in the extraction of information on hydrologic and water resources random variables from observed data.-This report gives a brief ...
  • Seth, S. M.; Singh, R. D. (National Institute of Hydrology, 1985)
    The estimation of runoff from the watershed is needed for comprehensive water resources planning, flood flow forecast, adequate design of hydraulic structures etc. The climatic and physical characteristics ...
  • Soni, B.; Mishra, G. C. (National Institute of Hydrology, 1985)
    Many investigators have studied rates of evaporation from soils where water table is at shallow depth. The rate of evaporation may be controlled by either the capacity of ...
  • Seth, S. M.; Singh, R. D. (National Institute of Hydrology, 1984)
    A lack of meteorological and hydrological data is one of the greatest obstacles to accurate estimation of design flood or volumes of runoff. The hydrologist is usually faced with the problem ...
  • Seth, S. M. (1984)
    The main objective of hydrological studies of floods is to develop appropriate procedures in order to arrive at desired design variable for the particular structure to be safe under extremes of ...
  • Seth, S. M.; Datta, Bhaskar; Singh, R. D. (National Institute of Hydrology, 1984)
    The rainfall runoff process in a catchment is a complex and complicated phenomenon governed by large number of known and unknown physiographic factors that vary both in ...
  • Seth, S. M.; Palaniappan, A. B. (National Institute of Hydrology, 1984)
    Routing of flood in open channel is one of the unsteady flow problem of importance to engineers. Flood routing is a computational procedure aiming at tracing of a flood wave incident ...
  • Seth, S. M.; Singh, R. D. (National Institute of Hydrology, 1984)
    Overland flow is defined as a thin sheet flow occurring before surface irregularities cause a gathering of runoff into discrete stream channels. The primary distinguishing characteristic of ...
  • Mishra, G. C. (National Institute of Hydrology, 1984)
    The understanding of land phase of the hydrologic cycle plays an important role in design of field drainage system. Physical features(topography, geology; soil characteristics) meteorological (temperature; ...
  • Chachadi, A. G.; Mishra, G. C. (National Institute of Hydrology, 1984)
    Frequently, the groundwater modeller faces with the problem of input parameters to-the model. Hydrogeological parameters like hydraulic conductivity, transmissivity, storativity and specific yield form ...

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