Now showing items 1-4 of 4

    • Heat storage in the Andaman Sea 

      RameshBabu, V.; Sastry, J.S. (India Meteorological Department, 1981)
      Heat storage in the Andaman Sea in upper 20 m, where a strong halocline seems to inhibit vertical heat transport has been evaluated and discussed in relation to the other parameters of heat budget. Estimation of annual ...
    • Hydrography and circulation in the western Bay of Bengal during the northeast monsoon 

      Shetye, S.R.; Gouveia, A.D.; Shankar, D.; Shenoi, S.S.C.; Vinayachandran, P.N.; Sundar, D.; Michael, G.S.; Nampoothiri, G. (American Geophysical Union, 1996)
      The Bay of Bengal, a semienclosed tropical basin that comes under the influence of monsoonal wind and freshwater influx, is distinguished by a strongly stratified surface layer and a seasonally reversing circulation. We ...
    • Some Physical Characteristics of Andaman Sea Waters during Winter 

      RamaRaju, D.V.; Gouveia, A.D.; Murty, C.S. (CSIR-NISCAIR, 1981)
      Based on the data collected during the cruises of R V Gaveshani in Jan-Feb of 1979 and 1980 around the Andaman Islands, 6 transects are selected, along which the present study on some physical properties of the waters ...
    • Surface layer temperature inversion in the Bay of Bengal 

      Pankajakshan, T.; Gopalakrishna, V.V.; Muraleedharan, P.M.; Reddy, G.V.; Araligidad, N.; Shenoy, Shrikant (Pergamon, 2002)
      Surface layer temperature inversion occurring in the Bay of Bengal has been addressed. Hydrographic data archived in the Indian Oceanographic Data Center are used to understand various aspects of the temperature inversion ...