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dc.contributor.authorSomasundar, K.
dc.contributor.authorRajendran, A.
dc.contributor.authorDileepKumar, M.
dc.date.accessioned1995-06-16T10:01:31Z
dc.date.accessioned2017-09-29T13:48:13Z
dc.date.available1995-06-16T10:01:31Z
dc.date.available2017-09-29T13:48:13Z
dc.date.issued1987
dc.identifier.citationOceanologica Acta, vol.10; 1987; 293-299
dc.identifier.issn0399-1784
dc.identifier.urihttp://drs.nio.org/drs/handle/2264/6095
dc.description.abstractProperty-property relations, mostly of conservative chemical parameters, are used in this attempt in tracing various discontinuities in the Arabian Sea and to reveal in situ processes together with potential temperature-salinity plots. Plots of salinity, PO, NO, oxygen and water stability (E) against potential temperature reveal that two discontinuity layers, one at 22.2 degrees C (22 DD) and the other at 9.1 degrees C (9 DD) are found in the Arabian Sea. 22 DD seems to have been formed due to the mixing of shallow salinity maximum water (SSMW) and Persian Gulf water (PGW). This discontinuity is situated in the centre of the mixing depth interval. Red Sea water (RSW) mass contributes chiefly for 9 DD. Various physico-chemical characteristics of these two discontinuity layers are elucidated, along with those of other water masses and density surfaces
dc.languageen
dc.publisherElsevier
dc.relation.ispartofOceanol Acta
dc.relation.isreferencedbySCI
dc.subjectChemistry and Biogeochemistry
dc.subject.otherin situ measurements
dc.subject.otherphysicochemical properties
dc.subject.otherwater mixing
dc.subject.otherT/S diagrams
dc.subject.otherdiscontinuity layers
dc.subject.otherconservative properties
dc.subject.otherwater masses
dc.subject.otherhydrography
dc.subject.otherISW, Arabian Sea
dc.titleProperty-Property relations: 22 degree and 9 degree discontinuities in the Arabian Sea
dc.typeJournal Article
dc.affiliation.authorCSIR-National Institute of Oceanography, Dona Paula, Goa, India


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