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dc.contributor.authorSastry, J.S.
dc.contributor.authorRameshBabu, V.
dc.date.accessioned1995-05-21T10:01:10Z
dc.date.accessioned2017-09-29T13:48:27Z
dc.date.available1995-05-21T10:01:10Z
dc.date.available2017-09-29T13:48:27Z
dc.date.issued1985
dc.identifier.citationProceedings of the Indian Academy of Sciences (Earth and Planetary Sciences), vol.94; 1985; 117-128
dc.identifier.issn0253-4126
dc.identifier.urihttp://drs.nio.org/drs/handle/2264/6379
dc.description.abstractThe summer cooling of the Arabian Sea has been reviewed in relation to the dynamic and thermodynamic processes. The differences in the quantum of cooling in the coastal regions have been attributed to the variations in the strength of coastal upwelling along the respective coasts. In the central portions of the Arabian Sea, the thickness of the surface layer and the thermal structure appear to be predominantly governed by the turbulent mixing of cold waters entrained into the surface layer in association with the deepening of current shear zone. The surface heat losses during the passage of a cyclone over the east central Arabian Sea account for only 40% of the total heat change in the surface layer while the rest is lost into the interior. Also presented are climatological mean patterns of the forcing parameters and their variations during certain years
dc.languageen
dc.publisherIndian Academy of Sciences, Bangalore
dc.relation.ispartofP Indian As-Earth
dc.relation.isreferencedbySCI
dc.subjectOceanography and Limnology
dc.subject.otherclimatology
dc.subject.otherheat flow
dc.subject.otherturbulent diffusion
dc.subject.othersummer
dc.subject.othertemperature
dc.subject.othersea water
dc.subject.otherISW, Arabian Sea
dc.titleSummer cooling of the Arabian sea - a review
dc.typeJournal Article


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