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dc.contributor.authorAnto, A.F.
dc.contributor.authorSomayajulu, Y.K.
dc.date.accessioned1995-05-18T10:01:07Z
dc.date.accessioned2017-09-29T13:48:27Z
dc.date.available1995-05-18T10:01:07Z
dc.date.available2017-09-29T13:48:27Z
dc.date.issued1985
dc.identifier.citationMausam, vol.36; 1985; 519-524
dc.identifier.issn0252-9416
dc.identifier.urihttp://drs.nio.org/drs/handle/2264/6371
dc.description.abstractBased on the hourly BT and six hourly CSTD data, collected from two stations in the western Bay of Bengal during July 1979, the diurnal variations of temperature in the oceanic mixed layer (OML) were analysed as a function of the prevailing surface layer conditions of the overlying atmosphere. Structure of OML, as delineated with respect to the diurnal variation of temperature with depth, revealed three sub-layers: wave mixed, diurnal thermocline and transition layer. The first two sub-layers of OML showed immediate responses to the changes in surface meteorological forcings. Surface were mixing, convective activity and internal waves were found to be the main physical processes to effect the thickness of wave mixed, diurnal thermocline and transition layer respectively
dc.languageen
dc.publisherIndia Meteorological Department
dc.relation.ispartofMausam
dc.relation.isreferencedbySCI
dc.subjectOceanography and Limnology
dc.subject.othermeteorology
dc.subject.otherinternal waves
dc.subject.otherdiurnal thermocline
dc.subject.otheratmosphere
dc.subject.othersurface layers
dc.subject.otherdiurnal variations
dc.subject.othermonsoons
dc.subject.othermixed layer
dc.subject.otherISW, Bengal Bay
dc.titleStructure of the oceanic mixed layer in western Bay of Bengal during MONEX
dc.typeJournal Article
dc.affiliation.authorCSIR-National Institute of Oceanography, Dona Paula, Goa, India


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