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    Simulated seasonal and interannual variability of mixed layer heat budget in the northern Indian Ocean 

    DeBoyer Montegut, C.; Vialard, J.; Shenoi, S.S.C.; Shankar, D.; Durand, F.; Ethe, C.; Madec, G. (American Meteorological Society, 2007)
    A global Ocean General Circulation Model (OGCM) is used to investigate the mixed layer heat budget of the Northern Indian Ocean (NIO). The model is validated against observations and shows a fairly good agreement with mixed ...
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    Spatiotemporal structure of the East India Coastal Current from satellite altimetry 

    Durand, F.; Shankar, D.; Birol, F.; Shenoi, S.S.C. (American Geophysical Union, 2009)
    A newly processed altimeter data set to present a hitherto unprecedented description of the spatiotemporal structure of the East India Coastal Current (EICC) is used: the data set resolves timescales ranging from a few ...
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    Observational evidence for westward propagation of temperature inversions in the southeastern Arabian Sea 

    Shankar, D.; Gopalakrishna, V.V.; Shenoi, S.S.C.; Durand, F.; Shetye, S.R.; Rajan, C.K.; Johnson, Z.; Araligidad, N.; Michael, G.S. (American Geophysical Union, 2004)
    A warm pool forms in the southeastern Arabian Sea (SEAS) prior to the onset of the summer monsoon over India in early June; the core of this warm pool is in the Lakshadweep Sea (LS). XBT and surface salinity data collected ...
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    The monsoon currents in the north Indian Ocean 

    Shankar, D.; Vinayachandran, P.N.; Unnikrishnan, A.S. (Pergamon (Elsevier), 2002)
    The monsoon currents are the seasonally reversing, open-ocean currents that flow between the Arabian Sea and the Bay of Bengal, the two wings of the north Indian Ocean. The Summer Monsoon Current (SMC) flows eastward ...
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    Seasonal cycle of sea level and currents along the coast of India 

    Shankar, D. (Indian Academy of Sciences, 2000)
    A framework involving long baroclinic waves, which treats the north Indian Ocean as a single dynamical entity, has been remarkably successful in simulating the low-frequency, large-scale circulation in the ocean. It is, ...
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    Modeling the barrier-layer formation in the South-Eastern Arabian Sea 

    Durand, F.; Shankar, D.; DeBoyer Montegut, C.; Shenoi, S.S.C.; Blanke, B.; Madec, G. (American Meteorological Society, 2007)
    The effect of salinity on the formation of the barrier layer (BL) in the South-Eastern Arabian Sea (SEAS) is investigated using an ocean general circulation model. In accordance with previous studies, the runoff distribution ...

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    Shankar, D. (6)
    Durand, F. (4)Shenoi, S.S.C. (4)DeBoyer Montegut, C. (2)Madec, G. (2)Araligidad, N. (1)Birol, F. (1)Blanke, B. (1)Ethe, C. (1)Gopalakrishna, V.V. (1)... View MoreSubject
    Bay of Bengal (6)
    Arabian Sea (4)Air-sea interaction (3)Indian Ocean (3)Ocean circulation (3)Rossby waves (3)Lakshadweep Sea (2)Salinity (2)Upper ocean processes (2)West India Coastal Current (2)... View MoreDate Issued2007 (2)2000 (1)2002 (1)2004 (1)2009 (1)Has File(s)Yes (6)

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