Jalvigyan Sameeksha: Recent submissions

  • Aggarwal, P. K. (National Institute of Hydrology, 2007)
    The Intergovernmental Panel on Climate Change has projected that the global mean surface temperature will rise by 2.0 - 4.5°C by 2100 due to increase in carbon dioxide concentration in the atmosphere. Climate variability ...
  • Goel, N. K.; Arya, D. S.; Gangwar, S. K. (National Institute of Hydrology, 2007)
    This paper attempts to bring out patterns of trend over different subdivisions in India through analysis of long (1872-2005) annual rainfall records. Modified Mann-Kendall test has been applied for assessment of trends. ...
  • Purohit, S.; Kesarkar, A.; Kaginalkar, A. (National Institute of Hydrology, 2007)
    Improvements in the mathematical model performance of weather and climate have been complemented by the development of supercomputing infrastructure and technological advancement in scientific data management, data ...
  • Goel, Malti (National Institute of Hydrology, 2007)
    The Himalayan-Karakoram Mountain chain forms an important mountain region between the Indian ocean basin and the highland of Tibet. The summer monsoon rainfall and the strong high pressure field called 'Tibetan high' have ...
  • Kulkarni, A. V. (National Institute of Hydrology, 2007)
    In the Himalayas, a large area is covered by glaciers and seasonal snow and changes in its extent can influence availability of water in the Himalayan Rivers. This paper discusses changes in glacial extent, glacial mass ...
  • Singh, P.; Arora, Manohar (National Institute of Hydrology, 2007)
    The concentration of several greenhouse gases has increased over time. Human activity increases the greenhouse gases effect primarily through release of carbon dioxide, but human influences on other greenhouse gases is ...
  • Pal, P. K.; Rakesh, V.; Singh, R.; Joshi, P. C. (National Institute of Hydrology, 2007)
    It is well established that mesoscale models have a pronounced skill in reproducing regional climate as compared to global models. The objective of this study is to assess the impact of improved land surface representation ...
  • Mall, R. K.; Bhatla, R.; Pandey, S. N. (National Institute of Hydrology, 2007)
    There is now clear evidence for an observed change in global surface temperature, rainfall, evaporation and extreme events since the start of 20th century. In recent times, several studies around the globe have shown that ...
  • Singh, A. K.; Yadava, M. G.; Ramesh, R. (National Institute of Hydrology, 2007)
    Impact of global climate change on the future water resources of India is intimately coupled with the variation of monsoon wind and monsoon rainfall. In this paper, the differences in paleo records from different areas ...
  • Contents 
    National Institute of Hydrology (National Institute of Hydrology, 2006)
  • Behera, G.; Bhanumurthy, V.; Raju, P. V.; Jonna, S.; Rao, V. Venkateshwar; Rao, G. S.; Murthy, C. S.; Sankar, E. Siva; Hakeem, K. Abdul; Rao, K. H. V. Durga (National Institute of Hydrology, 2006)
    Remote sensing is a reliable and cost-effective tool for managing extreme water conditions such as floods and droughts. The timeliness of satellite data is critical in flood management, rescue operations, damage assessment, ...
  • Ramesh, K. J.; Reddy, K. Mruthyunjaya; Nagaraju, A. Ramakrishna; Ramanamurthy, M. V.; Rao, G. Prasad; Ramesh, Y. (National Institute of Hydrology, 2006)
    An appropriate real-time hydrometeorological observational network is designed and established for developing a full-scale hazard mitigation modeling system in respect of floods covering 24 rivers with an objective to ...
  • Sharda, V. N.; Ojasvi, P. R. (National Institute of Hydrology, 2006)
    Frequent occurrence of floods and droughts in the country is a cause of serious concern for the planners, policy makers, hydrologists, conservationists and environmentalists. Spatial and temporal distribution of rainfall ...
  • Mishra, P. K.; Adhikari, R. N.; Patil, S. L. (National Institute of Hydrology, 2006)
    In the semi-arid regions of South India, droughts are more common and occur either due to failure of South-West or North-East monsoon. Drought impacts on agriculture are managed by taking appropriate preventive measures ...
  • Desai, V. R.; Mishra, A. K. (National Institute of Hydrology, 2006)
    Drought forecasting plays an important role in the planning and management of natural resources including water resource-systems of a river basin, since drought has severe effect when it persists over a longer period ...
  • Nagarajan, R. (National Institute of Hydrology, 2006)
    The perception' of drought varies with people engaged in different fields (e.g. meteorology, water resources, agriculture, socio-economy etc). Indicators of the impending droughts need to evaluated and categorized so that ...
  • National Institute of Hydrology (National Institute of Hydrology, 2006)
  • 8-News 
    National Institute of Hydrology (National Institute of Hydrology, 2006)
  • Contents 
    National Institute of Hydrology (National Institute of Hydrology, 2005)
  • Mohan, S.; Pramada, S. K. (National Institute of Hydrology, 2005)
    Many coastal areas in the world are dependent on local fresh groundwater resources because of heavy urbanization. Due to constant pumping and improper management, the South Chennai aquifer is facing a severe threat of being ...

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