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dc.contributor.authorMcCreary, J.P.
dc.contributor.authorHan, W.
dc.contributor.authorShankar, D.
dc.contributor.authorShetye, S.R.
dc.date.accessioned2009-01-21T11:25:27Z
dc.date.available2009-01-21T11:25:27Z
dc.date.issued1996
dc.identifier.citationJournal of Geophysical Research (C: Oceans), Vol.101; 13993-14010p.
dc.identifier.urihttp://drs.nio.org/drs/handle/2264/2270
dc.description.abstractA 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, and they are forced by Hellerman and Rosenstein (1983) winds. Effects due to the following four forcing meachnisms are isolated: local alongshore winds adjacent to the east coasts of India and Sri Lanka, remote alongshore winds adjacent to the northern and eastern boundaries of the Bay, remotely forced signals propagating from the equator, and interior Ekman pumping. Each process contributes significantly to the EICC surface flow at some locations and at some times during the year. Along the Indian coast (north of 10 degrees N), the surface EICC flows northeastward from February until September, with a strong peak in March-April and waker flow from June to September; interior Ekman pumping, remote alongshore winds and equatorial forcing all contribute to the springtime peak, whereas local alongshore winds are the primary driving force of the weaker summertime flow. Along Sri Lanka (south of 10 degrees N) the surface EICC flows northward only during March and April; tha absence of northward flow at other times is due to interior Ekman pumping which drives a strong southward current for much of the year (April to December). Along both coasts there is southward flow from October to January that is driven by interior Ekman pumping and local alongshore winds. The EICC also has significant subsurface flow on several occasions. Along the Indian coast, there is southwestward flow extending to depths greater than 1000 m from May to July that is driven primarily by equatorial forcing. From July to September the southwestward flow forms a shallow subsurface counterflow (a coastal underwater); its cause is primarily equatorial forcing and interior Ekman pumping, not the local alongshore winds, as might be expected
dc.language.isoen
dc.publisherAmerican Geophysical Union
dc.rightsCopyright [1996]. All efforts have been made to respect the copyright to the best of our knowledge. Inadvertent omissions, if brought to our notice, stand for correction and withdrawal of document from this repository.
dc.subjectcoastal currents
dc.subjectmodels
dc.subjectdynamics
dc.subjectwinds
dc.subjectekman pumping
dc.subjectcounter currents
dc.subjectnumerical analysis
dc.titleDynamics of the east India coastal current. 2. Numerical solutions
dc.typeJournal Article


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