Review Note: Recent submissions

  • 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.; 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, ...
  • 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. ...
  • 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 ...
  • Ethirajan, K.; Mishra, G. C. (1985)
    The natural hydrological phenomenon of rainfall recharge is very complex to study, analyse, and evaluate due to the unpredictable unbounded random variable nature of its input ...
  • 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 ...
  • 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 ...
  • 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 ...

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