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    Dynamics of the east India coastal current. 1. Analytic solutions forced by interior Ekman pumping and local alongshore winds 

    Shankar, D.; McCreary, J.P.; Han, W.; Shetye, S.R. (American Geophysical Union, 1996)
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    Tides in the Gulf of Kutch, India 

    Shetye, S.R. (Pergamon, 1999)
    In the Gulf of Kutch on the northwestern shelf of India the semi-diurnal constituents M sub(2) and S sub(2) get amplified approximately threefold. In contrast, amplification on the diurnal consituents K sub(1) and O sub(1) ...
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    Observed low-frequency currents in the deep mid-Arabian sea 

    Shetye, S.R.; Shenoi, S.S.C.; Sundar, D. (Pergamon, 1991)
    Current meter records form approximately 1000 and 3000 m at three moorings with a zonal separation of about 5 degrees along the 15 degrees N latitude in the mid-Arabian Sea during May 1986 to May 1987 have used to described ...
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    An examination of the factors that influence the monthly-mean sea level along the coast of India 

    Shetye, S.R.; Almeida, A.M. (IOC/Unesco, 1995)
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    West India coastal current and Lakshadweep High/Low 

    Shetye, S.R. (Indian Academy of Sciences, Bangalore, India, 1998)
    The West India Coastal Current (WICC) flows northward during November-February and southward during April-September. At the time of formation of the northward (southward) phase of the current, a high (low) in sea level - ...
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    Wind-driven coastal upwelling along the western boundary of the Bay of Bengal during the southwest monsoon 

    Shetye, S.R.; Shenoi, S.S.C.; Gouveia, A.D.; Michael, G.S.; Sundar, D.; Nampoothiri, G. (Pergamon, 1991)
    A hydrographic survey during the southwest monsoon (July-August 1989) showed that along most of the western boundary of the Bay of Bengal, in an approximately 40 km wide band, isopycnals from depths up to about 70 m surfaced ...
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    On the sea surface temperature high in the Lakshadweep Sea before the onset of the southwest monsoon 

    Shenoi, S.S.C.; Shankar, D.; Shetye, S.R. (American Geophysical Union, 1999)
    The north Indian Ocean becomes the warmest area of the world oceans prior to the onset of southwest monsoon in June. During this period a zonal band of high sea surface temperature (SST), the ``thermal equator'' (TE), moves ...
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    Satellite observations of the northeast monsoon coastal current 

    Shenoi, S.S.C.; Gouveia, A.D.; Shetye, S.R.; Rao, L.V.G. (PORSEC Secretariat, Shimizu, Japan, 1992)
    Satellite Infrared observations, from Advanced Very High Resolution Radiometer (AVHRR), during November 1987-February 1988 and hydrographic data from the eastern Arabian Sea are used to describe the poleward flowing coastal ...
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    Dynamics of the east India coastal current. 2. Numerical solutions 

    McCreary, J.P.; Han, W.; Shankar, D.; Shetye, S.R. (American Geophysical Union, 1996)
    A linear, continuously stratified model is used to investigate the dynamics of the East India Coastal Current (EICC). Solutions are found numerically in a basin that resembles the Indian Ocean basin north of 29 degrees S, ...
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    Does winter cooling lead to the subsurface salinity minimum off Saurashtra, India? 

    Shetye, S.R.; Gouveia, A.D.; Shenoi, S.S.C. (Oxford and IBH, New Delhi, 1992)
    Cold and dry winds of the northeast monsoon cool the northern Arabian Sea during November-January. The intensity of cooling is highest in the proximity of the peninsula of Saurashtra, India. Using hydrographic data, we ...
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    Shetye, S.R. (39)
    Gouveia, A.D. (18)Shenoi, S.S.C. (13)Michael, G.S. (10)Sundar, D. (9)Shankar, D. (7)Nampoothiri, G. (5)Almeida, A.M. (3)McCreary, J.P. (3)Unnikrishnan, A.S. (3)... View MoreSubjectcoastal currents (6)tidal propagation (6)monsoons (5)mathematical models (4)Indian Ocean (3)models (3)ocean circulation (3)runoff (3)seasonal variations (3)simulation (3)... View MoreDate Issued1999 (8)1991 (5)1992 (4)1993 (4)1996 (4)1998 (4)1994 (3)1997 (3)1990 (2)1995 (2)Has File(s)Yes (39)

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