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dc.contributor.authorSastry, J.S.
dc.contributor.authorRao, D.P.
dc.date.accessioned1995-05-08T09:57:16Z
dc.date.accessioned2017-09-29T13:48:42Z
dc.date.available1995-05-08T09:57:16Z
dc.date.available2017-09-29T13:48:42Z
dc.date.issued1981
dc.identifier.citationMausam, vol.32; 1981; 159-164
dc.identifier.issn0252-9416
dc.identifier.urihttp://drs.nio.org/drs/handle/2264/6670
dc.description.abstractStabilities in the upper 300 m in the Arabian Sea and the Bay of Bengal are computed and presented seasonwise. The water column in the Bay of Bengal is more strongly stratified than that in the Arabian Sea. These studies suggest that the vertical transfer of subsurface nutrients into the surface layer in the Bay of Bengal is greatly inhibited
dc.languageen
dc.publisherIndia Meteorological Department
dc.relation.ispartofMausam
dc.relation.isreferencedbySCI
dc.subjectOceanography and Limnology
dc.subject.otherstratification
dc.subject.otherwater bodies
dc.subject.otherupwelling
dc.subject.othermonsoons
dc.subject.otherturbulent diffusion
dc.subject.otherhydrographic data
dc.subject.othervertical stability
dc.subject.otherBengal Bay
dc.subject.otherISW, Arabian Sea
dc.titleA Comparative Study of Vertical Stabilities in the Arabian Sea and Bay of Bengal
dc.typeJournal Article
dc.affiliation.authorCSIR-National Institute of Oceanography, Dona Paula, Goa, India


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