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dc.contributor.authorGopalakrishna, V.V.
dc.contributor.authorSastry, J.S.
dc.date.accessioned1995-05-19T10:01:08Z
dc.date.accessioned2017-09-29T13:48:27Z
dc.date.available1995-05-19T10:01:08Z
dc.date.available2017-09-29T13:48:27Z
dc.date.issued1985
dc.identifier.citationIndian Journal of Marine Sciences, vol.14; 1985; 62-65
dc.identifier.issn0379-5136
dc.identifier.urihttp://drs.nio.org/drs/handle/2264/6380
dc.description.abstractFrom the hydrographic data collected on board R V Gaveshani in the Western Bay of Bengal during August-September 1978, fields of temperature, salinity have been constructed and the probable flow regime has been deduced. The studies indicate strong upwelling in the southern regions off the East Coast of India. Vertical temperature and salinity structures north of Visakhapatnam show a predominant estuarine character and upwelling is not evident. In the northern regions, the flow is directed south and is consonant with that derived from wind stress curl distribution
dc.languageen
dc.publisherCSIR-NISCAIR
dc.relation.ispartofIndian J Mar Sci
dc.relation.isreferencedbySCI
dc.subjectOceanography and Limnology
dc.subject.othermonsoons
dc.subject.otherwings
dc.subject.othercorrelation
dc.subject.othershelf dynamics
dc.subject.otherocean circulation
dc.subject.othersurface circulation
dc.subject.otherISW, India, East Coast
dc.titleSurface circulation over the shelf off the east coast of India during the south west monsoon
dc.typeJournal Article


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