Review Note

 

Recent Submissions

  • Ram, Shobha (National Institute of Hydrology, 1996)
    Quantitative data on hydraulic characteristics of aquifers including transmissivity and storativity are essential to the understanding and solution of aquifer problems and the proper evaluation and utilization ...
  • Kumar, Avadhesh; Ramasastri, K. S. (National Institute of Hydrology, 1986)
    Runoff in mountainous regions results from rainfall, snowmelt and glacier-melt. The different components of runoff are generally considered to be surface run off, sub-surface runoff and ...
  • Kumar, Avadhesh; Ramasastri, K. S. (National Institute of Hydrology, 1986)
    Floods in mountainous areas are the catchment's response due to precipitation and are influenced not only by catchment and stream characteristics but also storm characteristics and vegetal and land use changes. More ...
  • Singh, Pratap (National Institute of Hydrology, 1986)
    The accurate forecasting of the volume of snowmelt runoff likely to occur is of great importance for water resources management, especially to those responsible for operation of multipurpose reservoirs. [he ...
  • Bhar, A.K. (National Institute of Hydrology, 1986)
    Monitoring of sediment load in water bodies is an integrated part of any water resources management programme. After the advent of satellite age, remote sensing technique with its unique synoptic and repetitive ...
  • Kumar, Avadhesh; Palaniappan, A. B.; Ramasastri, K. S. (National Institute of Hydrology, 1987)
    Hydrologic analysis of watershed response to rainfall carried, out using lumped models, or mathematical models are quite common. These models involve certain parameters determined from the historical data and are ...
  • Seth, S. M.; Kumar, Rakesh (National Institute of Hydrology, 1986)
    Network design enters into most aspects of hydrology. Meteorological and hydrological data characteristics of watersheds, provide the basis for all water studies and determine the major ...
  • Verma, P. K.; Sikka, A. K. (National Institute of Hydrology, 1986)
    In spite of the lack of a unified definition of drought among the community of scientific professionals, it is basically agreed to be a situation of prolonged water deficit for given use, caused due to ...
  • Sikka, A. K. (National Institute of Hydrology, 1986)
    Scores of drought definitions are available in the literature developed by a variety of disciplines because it affects so many economic and social sectors. Drought holds different connotations to different people. The ...
  • Bhar, A.K. (National Institute of Hydrology, 1986)
    Mankind is beset with flood problems from the very ancient time. Fury of flood leaves its crippling effect on the economy. Flood inundation is one of the basic data need to understand, combat ...
  • Singh, Pratap (National Institute of Hydrology, 1986)
    The rivers draining out of the Himalayan region derive a major portion runoff from snow and ice melt. For runoff forecasting, irrigation planning, supply of drinking water and industrial use etc. reliable and ...
  • Singh, R. D. (National Institute of Hydrology, 1986)
    Drought forms one extreme end of the hydrologic cycle. It represents a period of abnormally dry weather sufficiently prolonged for the lack of precipitation to cause a serious hydrological imbalance and connotations of ...
  • Sikka, A. K.; Lohani, Vinay K. (National Institute of Hydrology, 1985)
    Studies done in India and elsewhere have indicated that the vegetation management practices have a great potential in increasing water yield from a watershed. The vegetation management practices include ...
  • Seth, S. M.; Goel, N. K. (National Institute of Hydrology, 1985)
    A hydrological forecast is the prior estimate of the future state of hydrological phenomena based on the knowledge of underlying physical laws and the modifying effects of specific geographic conditions. The ...
  • 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 ...
  • Ramasastri, K. S.; Singh, Pratap (National Institute of Hydrology, 1985)
    Hydrological cycle encompasses in itself two major processes the atmosphere phase and the ocean-land surface phase. Mathematical and conceptual modelling of these two processes independently have been ...
  • Goyal, V. C.; Seth, S. M. (National Institute of Hydrology, 1985)
    Data transmission is an integral part of any data acquisition system. The link between the sensor and the recording system can be physical or telemetric i.e. signal from the sensor is converted into radio ...
  • Goyal, V. C.; Chand, Ramesh; Seth, S. M. (National Institute of Hydrology, 1985)
    Geophysical investigations are effectively utilized in various hydrological applications. They provide fast and economic means of handling hydro-geological problems like exploration for groundwater, studies on ...
  • 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 ...
  • Kumar, Anil; Nigam, A. K. (National Institute of Hydrology, 1985)
    Land use vegetal cover characteristics of a watershed has a significant influence on the quality and quantity of runoff available from it. Various hydrologic processes such as infiltration, evapotranspiration, ...

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