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Browsing Review Note by Issue Date

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  • Mishra, G. C.; Chachadi, A. G. (National Institute of Hydrology, 1982)
    The command of Upper Ganga Canal (UGC) system covers an area of about 24,500 sq.km. located between the rivers Ganga and Yamuna and forms a part of the Gangetic alluvial plain. The area is characterised ...
  • 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 ...
  • 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.; 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.; Perumal, M. (National Institute of Hydrology, 1984)
    Flood routing is used to simulate flood wave movement through river reaches and reservoirs. There are two types of flood routing methods used in practice viz., hydraulic flood ...
  • 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 ...
  • Mishra, G. C.; Chachadi, A. G. (National Institute of Hydrology, 1984)
    The wide use of large-diameter wells for groundwater abstraction especially in hard rock areas calls for a thorough understanding of the flow dynamics in these wells for better management and ...
  • Soni, B.; Mishra, G. C. (National Institute of Hydrology, 1984)
    Hydrologic soil classification refers to a group of soil series that can be considered homogeneous in respect of soil characteristics. Hydrologic soil classification is useful for estimation of runoff. ...
  • 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 ...
  • 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.; Goel, N. K. (National Institute of Hydrology, 1984)
    The basic requirement of flood frequency analysis is to know the probability with which a flow Q is exceeded during a stated design life of a particular project. The partial duration series ...
  • Seth, S. M.; Goyal, V. C. (National Institute of Hydrology, 1984)
    The report reviews the various systems of data collection and transmission in hydrology and hydrometeorology. Data on precipitation, evaporation temperature, humidity, wind velocity, sunshine hours, water level, ...
  • Seethapathi, P. V.; Jain, S. K. (National Institute of Hydrology, 1984)
    Optimization is one of the most powerful and popular technique for solving various problems associated with the operation of a reservoir. During the past few years, its use has grown tremendously due to wider availability ...
  • 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 ...
  • 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 ...
  • Perumal, M.; Kumar, Ravi (National Institute of Hydrology, 1985)
    Flash floods occurs suddenly and it is usually difficult forecast because of short time available between their causative event and their actual occurrence. Flash floods generally result ...
  • Kamal (National Institute of Hydrology, 1985)
    In a general sense, factors that must be considered in conjunctive use analyses have been identified and discussed. The factors have been distilled from the work of many authors who have examined ...
  • 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 ...
  • 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 ...

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