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dc.contributor.authorMurty, V.S.N.
dc.contributor.authorRao, D.P.
dc.contributor.authorSastry, J.S.
dc.date.accessioned1995-05-13T10:00:57Z
dc.date.accessioned2017-09-29T13:48:37Z
dc.date.available1995-05-13T10:00:57Z
dc.date.available2017-09-29T13:48:37Z
dc.date.issued1983
dc.identifier.citationMahasagar, vol.16(1); 1983; 67-71
dc.identifier.issn0542-0938
dc.identifier.urihttp://drs.nio.org/drs/handle/2264/6571
dc.description.abstractAn analysis of thermal Structure in the East Central Arabian Sea associated with a moderate cyclone is presented. The heat storage and the heat budget components have been computed. Under the influence of the cyclone the Sea Surface Temperature (SST) decreased by 1.2 degrees C. The study has revealed that the lowering of SST was primarily due to the downward heat flux (58%) and secondarily due to the evaporative cooling (33%). The fluxes of sensible heat and effective back radiation across the sea surface account for only 9% of the total loss from the surface layer
dc.languageen
dc.publisherIndian Association for Limnology and Oceanography
dc.relation.ispartofMahasagar
dc.relation.isreferencedbyNON-SCI
dc.subjectMeteorology and Climatology
dc.subject.othersurface temperature
dc.subject.otherthermal structure
dc.subject.otherheat transfer
dc.subject.otherheat budget
dc.subject.otherheat balance
dc.subject.otherupwelling
dc.subject.otherupper ocean
dc.subject.othercyclones
dc.subject.otherISW, Arabian Sea
dc.titleThe Lowering of Sea Surface Temperature in the East Central Arabian Sea Associated with a Cyclone
dc.typeJournal Article
dc.affiliation.authorCSIR-National Institute of Oceanography, Dona Paula, Goa, India


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