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dc.contributor.authorRao, T.V.N.
dc.contributor.authorRao, D.P.
dc.contributor.authorRao, B.P.
dc.contributor.authorRamaRaju, V.S.
dc.date.accessioned1995-06-16T10:01:22Z
dc.date.accessioned2017-09-29T13:48:22Z
dc.date.available1995-06-16T10:01:22Z
dc.date.available2017-09-29T13:48:22Z
dc.date.issued1986
dc.identifier.citationIndian Journal of Marine Sciences, vol.15; 1986; 84-87
dc.identifier.issn0379-5136
dc.identifier.urihttp://drs.nio.org/drs/handle/2264/6273
dc.description.abstractStability and stratification of the water over the shelf disappear as cold saline waters characteristic of 60 m depth rise to the surface during March. Tilting of isopycnals and offshore displacement of isohalines suggest the surface divergence typical of a coastal upwelling driven by local wind stress. Upwelling is predominant off Visakhapatnam during premonsoon and monsoon periods. Waters from the deeper depths of the shelf appear to reach the surface causing considerable fall of temperature near the coast particularly during the premonsoon period
dc.languageen
dc.publisherCSIR-NISCAIR
dc.relation.ispartofIndian J Mar Sci
dc.relation.isreferencedbySCI
dc.subjectOceanography and Limnology
dc.subject.othermonsoons
dc.subject.otherstratification
dc.subject.othersinking
dc.subject.otherupwelling
dc.subject.otherISW, India, Andhra Pradesh, Visakhapatnam
dc.titleUpwelling and sinking along Visakhapatnam coast
dc.typeJournal Article


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