Please use this identifier to cite or link to this item: http://nopr.niscpr.res.in/handle/123456789/38982
Full metadata record
DC FieldValueLanguage
dc.contributor.authorRadhakrishna, K-
dc.contributor.authorThiri, P M A Bhatia-
dc.contributor.authorDevassy, V P-
dc.date.accessioned2016-12-21T05:43:38Z-
dc.date.available2016-12-21T05:43:38Z-
dc.date.issued1982-12-
dc.identifier.issn0975-1033 (Online); 0379-5136 (Print)-
dc.identifier.urihttp://nopr.niscair.res.in/handle/123456789/38982-
dc.description287-291en_US
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.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.11(4) [December 1982]en_US
dc.titleChlorophyll a, phaeopigments and particulate organic carbon in the Northern and Western Bay of Bengalen_US
dc.typeArticleen_US
Appears in Collections:IJMS Vol.11(4) [December 1982]

Files in This Item:
File Description SizeFormat 
IJMS 11(4) 287-291.pdf483.53 kBAdobe PDFView/Open


Items in NOPR are protected by copyright, with all rights reserved, unless otherwise indicated.