Studies on evaporation from the north Indian Ocean

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dc.contributor.author Rao, Lakshmana G.R.
dc.contributor.author VeenaDevi, Y.
dc.contributor.author Reddy, Gopala K.
dc.contributor.author Prasad, A.L.N.
dc.date.accessioned 2007-01-12T09:57:18Z
dc.date.accessioned 2017-09-29T13:48:46Z
dc.date.available 2007-01-12T09:57:18Z
dc.date.available 2017-09-29T13:48:46Z
dc.date.issued 1981
dc.identifier.citation Indian Journal of Marine Sciences, vol.10(4); 1981; 337-340
dc.identifier.issn 0379-5136
dc.identifier.uri http://drs.nio.org/drs/handle/2264/6764
dc.description.abstract Evaporation 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.language en
dc.publisher CSIR-NISCAIR
dc.relation.ispartof Indian J Mar Sci
dc.relation.isreferencedby SCI
dc.subject Oceanography and Limnology
dc.subject Meteorology and Climatology
dc.subject.other evaporation
dc.subject.other sea surface
dc.subject.other seasonal variations
dc.subject.other monsoons
dc.subject.other ISW, North Indian Ocean
dc.title Studies on evaporation from the north Indian Ocean
dc.type Journal Article
dc.affiliation.author Andhra University, Visakhapatnam, Andhra Pradesh, India


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