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dc.contributor.authorRao, Lakshmana G.R.
dc.contributor.authorVeenaDevi, Y.
dc.contributor.authorReddy, Gopala K.
dc.contributor.authorPrasad, A.L.N.
dc.date.accessioned2007-01-12T09:57:18Z
dc.date.accessioned2017-09-29T13:48:46Z
dc.date.available2007-01-12T09:57:18Z
dc.date.available2017-09-29T13:48:46Z
dc.date.issued1981
dc.identifier.citationIndian Journal of Marine Sciences, vol.10(4); 1981; 337-340
dc.identifier.issn0379-5136
dc.identifier.urihttp://drs.nio.org/drs/handle/2264/6764
dc.description.abstractEvaporation from the surface of the North Indian Ocean is estimated following the aerodynamic approach The influence of the southwest monsoon and the northeast monsoon is significant giving rise to maximum evaporation from the sea surface due to strong wind field and high saturation deficit respectively An annual maximum evaporation of 160 cm is observed in the southern regions Due to the advancement of the southwest monsoon evaporation maximum in the Arabian Sea is reached earlier by 1 month than in the Bay of Bengal while the reverse is the case during the northeast monsoon
dc.languageen
dc.publisherCSIR-NISCAIR
dc.relation.ispartofIndian J Mar Sci
dc.relation.isreferencedbySCI
dc.subjectOceanography and Limnology
dc.subjectMeteorology and Climatology
dc.subject.otherevaporation
dc.subject.othersea surface
dc.subject.otherseasonal variations
dc.subject.othermonsoons
dc.subject.otherISW, North Indian Ocean
dc.titleStudies on Evaporation from the North Indian Ocean
dc.typeJournal Article
dc.affiliation.authorAndhra University, Visakhapatnam, Andhra Pradesh, India


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