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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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    Chemical oceanography of the Arabian Sea: Part 1 - Hydrochemical and hydrographical features of the Northern basin 

    SenGupta, R.; Fondekar, S.P.; Sankaranarayanan, V.N.; DeSousa, S.N. (CSIR-NISCAIR, 1975)
    Three water masses in the Arabian Sea have been identified from their physical and chemical characteristics: (i) water mass which originates in the surface layer and has high salinity,low oxygen and high pH ; (ii) water ...
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    Circulation and water masses of the Arabian Sea 

    Shetye, S.R.; Gouveia, A.D.; Shenoi, S.S.C. (Indian Academy of Sciences, Bangalore, 1994)
    The circulation in the coastal region off Oman is driven mainly by local winds and there is no remotely driven western boundary current. Local wind-driving is also important to the coastal circulation off western India ...

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    AuthorDeSousa, S.N. (1)Fondekar, S.P. (1)Gouveia, A.D. (1)Murty, V.S.N. (1)Rao, D.P. (1)Sankaranarayanan, V.N. (1)Sarma, Y.V.B. (1)Sastry, J.S. (1)SenGupta, R. (1)Shenoi, S.S.C. (1)... View MoreSubject
    ISW, Arabian Sea (3)
    Oceanography and Limnology (3)
    water masses (3)
    chemical Oceanography (1)coastal currents (1)dissolved oxygen (1)equatorial circulation (1)mixed layer (1)monsoons (1)nutrients (mineral) (1)... View MoreDate Issued1990 - 1994 (1)1980 - 1989 (1)1975 - 1979 (1)Has File(s)
    Yes (3)

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