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dc.contributor.authorRadhakrishna, K.
dc.contributor.authorBhattathiri, P.M.A.
dc.contributor.authorDevassy, V.P.
dc.date.accessioned1995-05-10T10:00:53Z
dc.date.accessioned2017-09-29T13:48:39Z
dc.date.available1995-05-10T10:00:53Z
dc.date.available2017-09-29T13:48:39Z
dc.date.issued1982
dc.identifier.citationIndian Journal of Marine Sciences, vol.11; 1982; 287-291
dc.identifier.issn0379-5136
dc.identifier.urihttp://drs.nio.org/drs/handle/2264/6597
dc.description.abstractDistribution of chl a at surface closely corresponds to the surface flow patterns. Integral mean concentration (IMC) of chl a in inshore waters (depth 200 m) is double than that in the offshore waters (depth 200 m) while IMC of particulate organic carbon from inshore and the offshore waters does not differ significantly. The euphotic zone lies within the upper homogeneous layer. Phaeopigment concentration increases with decrease in light intensity. For comparison of these parameters IMC is considered to be a more valid index than the integrated concentration
dc.languageen
dc.publisherCSIR-NISCAIR
dc.relation.ispartofIndian J Mar Sci
dc.relation.isreferencedbySCI
dc.subjectAquatic Ecology, Productivity
dc.subject.othereuphotic zone
dc.subject.othervertical distribution
dc.subject.otherparticulate organic carbon
dc.subject.otherpigments
dc.subject.otherchlorophylls
dc.subject.otherISW, Bengal Bay
dc.titleChlorophyll a, Phaeopigments and particulate Organic Carbon in the Northern and Western Bay of Bengal
dc.typeJournal Article
dc.affiliation.authorCSIR-National Institute of Oceanography, Dona Paula, Goa, India


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