Conference Proceedings: Recent submissions

  • 7.8-Simulation of flood flows in a mountainous catchment in western ghats (India) 
    Jain, M. K.; Ramasastri, K. S. (National Institute of Hydrology, 1992)
    Floods in the mountainous areas result from high intensity rains falling over steep slopes and transforming into runoff at outlet very rapidly due to less time of concentration. ...
  • 7.9-Flood frequency estimates for Sub-Himalayan region by regional flood frequency approach. 
    Kumar, Rakesh; Singh, R. D. (National Institute of Hydrology, 1992)
    In this paper, flood frequency analysis has been carried out for Sub-Himalayan region (Zone-7) using peak flood series data of ten small and medium catchments varying in size from 6 sq.kms. to ...
  • 8-Ground water and springs - General reporter's report 
    Raju, T. S. (National Institute of Hydrology, 1992)
  • 8.1-Aquifer characteristics in karst topography. 
    Somasundram, M. V.; Thayumanavan, S.; Supardi, Engkus (National Institute of Hydrology, 1992)
    The study describes briefly the variations in determining aquifer potential parameters in mountainous areas adjoining sea. The hydrogeology of the area is generally characterised by the maximum 100 m horizon pleistocene ...
  • 8.2-Ground water in mountainous area and forest vegetation. 
    Singhal, R. M.; Pant, S. P. (National Institute of Hydrology, 1992)
    There are much misaivinqs outside the hydrological discipline on the location and behaviour of the mountainous water table under forest vecietation and there are many conflicting assertions ...
  • 8.3-Hydrologic study of springs. 
    Bhar, A. K.; Mishra, G. C. (National Institute of Hydrology, 1992)
    Springs have been used as a dependable source of water supply since ancient time. They are part and parcel of the groundwater, There is enough scope for hydrologic study of springs including the ...
  • 8.4-Modelling the seepage from a lake using 3D groundwater model. 
    Singh, Sushil K. (National Institute of Hydrology, 1992)
    The analysis of unsteady seepage from a lake in a homogeneous and anisotropic aquifer has been done using a three dimensional ground water flow model. Hypothetical setting of boundaries have ...
  • Recommendations 
    National Institute of Hydrology (National Institute of Hydrology, 1992)
  • Chairmen and general reporters of various technical sessions 
    National Institute of Hydrology (National Institute of Hydrology, 1992)
  • Organising committee 
    National Institute of Hydrology (National Institute of Hydrology, 1992)
  • Contents 
    National Institute of Hydrology (National Institute of Hydrology, 1991)
  • Preface 
    Chandra, Satish (National Institute of Hydrology, 1991)
  • 1-Chapter-I-Hydrologic system 
    Seth, S. M. (National Institute of Hydrology, 1991)
    Any phenomena which undergoes continuous changes particularly with respect to time may be called a process.As particularly all hydrologic phenomena change with time, they are hydrologic processes. ...
  • 2-Chapter-II-Data for hydrological analysis 
    Ramasastri, K. S.; Haque, M. E.; Ghosh, N. C.; Kumar, Rakesh (National Institute of Hydrology, 1991)
    In the expanding modern economy, exploitation of natural resources if of primary importance. As water is one of the main natrual resource, extensive efforts are being made in every country to ...
  • 3-Chapter-III-Applications of modern techniques 
    Kumar, Bhishm; Rathore, D. S. (National Institute of Hydrology, 1991)
    The prime function and Hydrology is to provide scientific facts about water in hydrological cycle. This is being done using sophisticated scientific instruments and techniques for managing water ...
  • 4-Chapter-IV-Water resources assessment 
    Seth, S. M.; Kumar, Rakesh; Haque, M. E. (National Institute of Hydrology, 1991)
    One of the most important aspects in planning of a water resources development project is to assess the availability of water and its time distribution. Water availability is the life ...
  • 5-Chapter-V-Design flood studies 
    Singh, R. D.; Mishra, S. K. (National Institute of Hydrology, 1991)
    For the estimation of design flood for any water resources project, the hydrologist often needs to have a fairly reliable es1 1 a of design storm. Among the various methods used for ...
  • 6-Chapter-VI-Hydrologic design criteria 
    Sharma, R. K. (National Institute of Hydrology, 1991)
    Water Resources have always played a major role in human activities. Rapid industrialization, urbanization and increasing needs of agriculture for growing population have resulted in considerable ...
  • 7-Chapter-VII-Hydrological aspects in operation and maintenance 
    Bhatia, K. K. S.; Jain, S. K.; Haque, M. E. (National Institute of Hydrology, 1991)
    Reservoirs are one of the most important component of a water resources development project. A reservoir is created by constructing a dam across a stream. The principal function of a ...
  • Contents 
    National Institute of Hydrology (National Institute of Hydrology, 1993)

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