Technical Notes: Recent submissions

  • Haque, M. E.; Kumar, Rakesh (National Institute of Hydrology, 1990)
    In order to develop agriculture based economy and to meet the demands of growing population; in terms of irrigation, drinking water, hydropower generation and industrial use etc. a sound ...
  • Jain, S. K. (National Institute of Hydrology, 1990)
    Flood forecasting is required for a number of purposes, e.g. , flood control, flood damage reduction, and reservoir operation. Significant improvements in operation of water resources systems ...
  • Seth, S. M. (National Institute of Hydrology, 1990)
    The study of past or ancient flood events which occurred prior to the time of human observation or direct measurement by modern hydrologic procedures, is termed as paleoflood hydrology. ...
  • Divya; Sharma, M. K. (National Institute of Hydrology, 1989)
    Droughts of great magnitude in various tropical and sub-tropical regions have been a matter of concern in the recent past. Their socio-economic consequences have resulted in the studies ...
  • Divya (National Institute of Hydrology, 1992)
    Acid rain, generally described as a European and North American problem caused largely by anthropogenic emissions of the oxides of sulphur and nitrogen during burning of fossil fuels, is spreading ...
  • Divya (National Institute of Hydrology, 1992)
    Concentrations of greenhouse gases in the atmosphere carbon dioxide, methane, nitrous oxide, chlorofluorocarbons have increased considerably from pre-industrial levels and are increasing at an ...
  • Kumar, Rakesh; Haque, M. E. (National Institute of Hydrology, 1992)
    The time distribution of the runoff and the estimation of the peak flood constitute very important component of the planning and design as well as operation and maintenance of a water resources ...
  • Goel, M. K. (National Institute of Hydrology, 1991)
    Multipurpose reservoir projects with the objectives of conservation of water and flood control are quite common. The conservation purposes, which include irrigation, hydroelectric power generation, ...
  • Shukla, M. K.; Soni, B. (National Institute of Hydrology, 1991)
    Urbanization which may be broadly defined as the process* of expanding urban influence, has been taking place for more than 6000 years, its pace has increased markedly since the beginning of the ...
  • Tyagi, Aditya (National Institute of Hydrology, 1989)
    Increasing development of towns and industries has resulted in an increase in water consumption and waste water volume. Therefore, the danger of pollution has become greater for natural ...
  • Divya; Sharma, M. K. (National Institute of Hydrology, 1989)
    Atmospheric models are coupled to the land surface through the hydrological cycle, rain carries water from the atmosphere and evapotranspiration returns it to the atmosphere. The studies of ...
  • Divya; Seth, S. M.; Sharma, M. K. (National Institute of Hydrology, 1988)
    The General Circulation Models (GCM) synthesize the large scale distribution of the climate by application of the physical laws governing the atmospheric structure and behaviour. These ...
  • Divya; Seth, S. M.; Sharma, M. K. (National Institute of Hydrology, 1988)
    Monsoons, which affect the largest land masses, have been the subject of study on every scale from simple local studies to circulation simulation on giant computers (the so-called fifth ...
  • Jain, C. K. (National Institute of Hydrology, 1988)
    Soil moisture content is an important variable that determines the response of a soil plant system to any water input. Continual monitoring is therefore, of significance in irrigation management. ...
  • Jain, C. K. (National Institute of Hydrology, 1988)
    Groundwater recharge is that amount of surface water which reaches the permanent water table either by direct contact in the riparian zone or by downward percolation through the overlying ...
  • Goyal, V. C. (National Institute of Hydrology, 1988)
    Soil salinity problem in agricultural fields arises due to excessive soluble salts present in the soil, the inorganic electrolytes in the soil solution being the major contributors. ...
  • Kumar, Sudhir; Singh, Yatveer; Goyal, Rakesh; Abbas, Zafar; Sapra, T. R. (National Institute of Hydrology, 1988)
    The subsurface is the medium through which pollu- tants move from the soil surface to groundwater. Polluting substances are subjected to complex physical, chemical and biological ...
  • Lohani, Vinay K.; Raghuwanshi, N. S. (National Institute of Hydrology, 1988)
    Forest influences on groundwater storage can be estimated from evapo- transpiration and discharge relationships. Studies have been done in various countries to establish relationship between forests and ...
  • Goyal, R. K.; Soni, B. (National Institute of Hydrology, 1988)
    In the last few decades, the world has witnessed rapid urbanisation. One of the many complex problems which have come up with increased urbanisation is that of quick drainage of ...
  • Kamal; Deepti; Mishra, G. C. (National Institute of Hydrology, 1988)
    Considering the large number and variety of pollutants that may be released to the subsurface and the wide range of environmental situations (geological, hydrological, chemical. and biological) that may encounter, ...

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