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dc.contributor.authorSadhuram, Y.
dc.contributor.authorRao, D.P.
dc.contributor.authorRao, B.P.
dc.date.accessioned2009-01-10T11:43:16Z
dc.date.available2009-01-10T11:43:16Z
dc.date.issued1999
dc.identifier.citationAdvanced Technologies in Meteorology. Symposium Proceedings. (TROPMET 1995), eds. Gupta, R.K.; Reddy, S.J. 285-289p.
dc.identifier.urihttp://drs.nio.org/drs/handle/2264/1831
dc.description.abstractSurface meteorological data collected onboard research vessels ORV Sagarkanya and Gaveshani during 1983-85 have been used in these studies. The analysis revealed that the Mean Sea surface temperature (SST was greater than 28 degrees C (designated as warm pool) except in North Bay of Bengal where it was less than 28 degrees C. SST was very high (greater than 30 degrees C) off Sri Lanka. Net total insolation (Q sub(1)) varied between 200 and 240 Wm sup(-2) over the warm pool, effective back radiation (Q sub(b)) was maximum off Sri Lanka which was associated with high SST. Sensible heat flux (Q sub(s)) varied between 8 and 5 Wm sup(-2) and latent heat flux (Q sub(e)) varied between 50 Wm sup(-2) (West of Andaman Islands) and 250 Wm sup(-2) (off Sri Lanka). The net heat exchange (Q sub(n)) was high and negative (-100 to -120 Wm sup(-2)) off Sri Lanka and central Bay of Bengal. Q sub(n) is positive and high (120-Wm sub(-2)) South of Port Blair and decreased sharply to 40 Wm sup(-2) within a few kms
dc.language.isoen
dc.publisherTata McGraw-Hill, New Delhi, India
dc.rightsCopyright [1999]. All efforts have been made to respect the copyright to the best of our knowledge. Inadvertent omissions, if brought to our notice, stand for correction and withdrawal of document from this repository.
dc.subjectmeteorological data
dc.subjectmeteorological observations
dc.subjectsurface temperature
dc.subjectheat budget
dc.subjectmonsoons
dc.subjectwind speed
dc.subjectatmospheric pressure
dc.titleMean surface fields of heat budget components over the warm pool in the Bay of Bengal during post-monsoon season
dc.typeConference Article


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