Please use this identifier to cite or link to this item: http://nopr.niscair.res.in/handle/123456789/38763
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dc.contributor.authorKrishna, V V Gopala-
dc.contributor.authorSastry, J S-
dc.date.accessioned2016-12-16T06:02:41Z-
dc.date.available2016-12-16T06:02:41Z-
dc.date.issued1985-06-
dc.identifier.issn0975-1033 (Online); 0379-5136 (Print)-
dc.identifier.urihttp://nopr.niscair.res.in/handle/123456789/38763-
dc.description62-65en_US
dc.description.abstractV V Gopala Krishna & J S Sastry From 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.en_US
dc.language.isoen_USen_US
dc.publisherNISCAIR-CSIR, Indiaen_US
dc.rights CC Attribution-Noncommercial-No Derivative Works 2.5 Indiaen_US
dc.sourceIJMS Vol.14(2) [June 1985]en_US
dc.titleSurface Circulation over the Shelf Off the East Coast of India during the Southwest Monsoonen_US
dc.typeArticleen_US
Appears in Collections:IJMS Vol.14(2) [June 1985]

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