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dc.contributor.authorRameshKumar, M.R.
dc.contributor.authorSathyendranath, S.
dc.contributor.authorViswambharan, N.K.
dc.contributor.authorRao, L.V.G.
dc.date.accessioned1995-06-12T10:01:19Z
dc.date.accessioned2017-09-29T13:48:21Z
dc.date.available1995-06-12T10:01:19Z
dc.date.available2017-09-29T13:48:21Z
dc.date.issued1986
dc.identifier.citationProceedings of the Indian Academy of Sciences (Earth and Planetary Sciences), vol.95; 1986; 435-446
dc.identifier.issn0253-4126
dc.identifier.urihttp://drs.nio.org/drs/handle/2264/6247
dc.description.abstractUsing the satellite derived sea surface temperature (SST) data for 1979 (bad monsoon) and 1983 (good monsoon), the SST variability for two contrasting monsoon seasons is studied. The study indicates that large negative anomalies off the Somali and Arabian coasts are associated with good monsoon rainfall over India. The strong monsoonal cooling in these regions can be attributed to strong low level winds and intense upwelling. The reappearance of 27 degrees C isotherm off Somali coast in May/June coincides with the onset of southwest monsoon over India. Further, the influence of zonal anomaly of SST off Somali Coast (SCZASST) and Central Indian Ocean Zonal Anomaly of SST (CIOZASST) with monsoon rainfall over India is brought out. The former is negatively related to the monsoon rainfall over western and central parts of India, whilst CIOZASST is positively related
dc.languageen
dc.publisherIndian Academy of Sciences, Bangalore
dc.relation.ispartofP Indian As-Earth
dc.relation.isreferencedbySCI
dc.subjectOceanography and Limnology
dc.subject.otherequatorial trough
dc.subject.otherwinds
dc.subject.othersatellite sensing
dc.subject.othermonsoons
dc.subject.othersurface temperature
dc.subject.otherISW, North Indian Ocean
dc.titleSea surface temperature variability over North Indian Ocean - A study of two contrasting monsoon seasons
dc.typeJournal Article
dc.affiliation.authorCSIR-National Institute of Oceanography, Dona Paula, Goa, India


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