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dc.contributor.authorSadhuram, Y.
dc.date.accessioned2009-05-12T10:40:32Z
dc.date.available2009-05-12T10:40:32Z
dc.date.issued1991
dc.identifier.citationBoundary-Layer Meteorology, Vol.54; 411-414p.
dc.identifier.urihttp://drs.nio.org/drs/handle/2264/3314
dc.description.abstractThe bulk transfer coefficient for latent heat flux (Ce) has been estimated over the Arabian Sea from the moisture budget during the pre-monsoon season of 1988. The computations have been made over two regions (A: 0-8 degrees N: 60-68 degrees E: B: 0-4 degrees N: 56-60 degrees E) with the upper computational boundary fixed at the 300 mb level. The precipitation amount (P) was negligible for region A while the observed values of P have been used for region B. The Ce estimates have been compared with those obtained with other available schemes (Kondo, 1975: Bunker, 1976), which are based on wind speed and atmospheric stability within the surface layer. Value of Ce is higher in region A and lower in region B than the other estimates.
dc.language.isoen
dc.publisherKluwer
dc.rightsCopyright [1991]. 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.titleEstimation of bulk transfer coefficient for latent heat flux (Ce)
dc.typeJournal Article


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