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    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 ...
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    Circulation and watermass structure in the Central Arabian Sea during December 1982 

    Sarma, Y.V.B.; Murty, V.S.N.; Rao, D.P.; Sastry, J.S. (CSIR-NISCAIR, 1986)
    After the cessation of the SW monsoon over Arabian Sea, the North Equatorial Current sets strongly and the low saline waters from the Bay of Bengal and the equatorial Indian Ocean penetrate into the Arabian Sea. This results ...
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    Summer cooling of the Arabian sea - a review 

    Sastry, J.S.; RameshBabu, V. (Indian Academy of Sciences, Bangalore, 1985)
    The summer cooling of the Arabian Sea has been reviewed in relation to the dynamic and thermodynamic processes. The differences in the quantum of cooling in the coastal regions have been attributed to the variations in the ...
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    Estimation of evaporation rates over the Arabian Sea from Satellite data 

    Rao, M.V.; RameshBabu, V.; Rao, L.V.G.; Sastry, J.S. (Indian Academy of Sciences, Bangalore, 1986)
    Utilizing both the SAMIR brightness temperatures of Bhaskara 2 and GOSSTCOMP charts of NOAA satellite series, the evaporation rates over the Arabian Sea for June 1982 are estimated through the bulk aerodynamic method. The ...
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    Summer cooling in the east central Arabian Sea - a process of dynamic response to the southwest monsoon 

    RameshBabu, V.; Sastry, J.S. (India Meteorological Department, 1984)
    The cooling of the east central Arabian Sea during summer monsoon season is examined using data sets of MONEX '79 and MONSOON '77 programmes. These studies have revealed that downward transfer of heat due to the mixing of ...
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    A Comparative Study of Vertical Stabilities in the Arabian Sea and Bay of Bengal 

    Sastry, J.S.; Rao, D.P. (India Meteorological Department, 1981)
    Stabilities in the upper 300 m in the Arabian Sea and the Bay of Bengal are computed and presented seasonwise. The water column in the Bay of Bengal is more strongly stratified than that in the Arabian Sea. These studies ...

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    Author
    Sastry, J.S. (6)
    RameshBabu, V. (4)Rao, D.P. (2)Murty, V.S.N. (1)Rao, L.V.G. (1)Rao, M.V. (1)Sarma, Y.V.B. (1)Subject
    ISW, Arabian Sea (6)
    Oceanography and Limnology (6)
    monsoons (3)turbulent diffusion (2)air-water exchanges (1)anticyclones (1)Bengal Bay (1)bowen ratio (1)climatology (1)cooling (1)... View MoreDate Issued1981 (2)1986 (2)1984 (1)1985 (1)Has File(s)Yes (5)No (1)

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