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dc.contributor.authorBabu, M.T.
dc.contributor.authorHeblekar, A.K.
dc.contributor.authorMurty, C.S.
dc.date.accessioned1995-08-14T10:01:52Z
dc.date.accessioned2017-09-30T01:30:02Z
dc.date.available1995-08-14T10:01:52Z
dc.date.available2017-09-30T01:30:02Z
dc.date.issued1989
dc.identifier.citationIndian Journal of Marine Sciences, vol.18; 1989; 223-227
dc.identifier.issn0379-5136
dc.identifier.urihttp://drs.nio.org/drs/handle/2264/7322
dc.description.abstractWind distribution observed during southwest monsoon of 1984 has used to derive the mean wind stress for the season at every 1 degree square grid and curl over the Bay of Bengal. Two regions of maximum wind stress are present over the Bay of Bengal. Variability of wind components is compared with that derived from the wind field, given in the climatological atlas. Zonal component of the climatological and observed wind field has a maximum stress along 15 degrees N lat. along which the computed vertical velocity field present a negative maximum (sinking). The possible mechanisms influencing the surface layer dynamics have been discussed
dc.languageen
dc.publisherCSIR-NISCAIR
dc.relation.ispartofIndian J Mar Sci
dc.relation.isreferencedbySCI
dc.subjectOceanography and Limnology
dc.subject.othermonsoons
dc.subject.otherwind fields
dc.subject.otherwind stress curl
dc.subject.otherwind stress
dc.subject.othersurface layers
dc.subject.otherISW, Bengal Bay
dc.titleWind stress, curl and vertical velocity in the Bay of Bengal during southwest monsoon, 1984
dc.typeJournal Article
dc.affiliation.authorCSIR-National Institute of Oceanography, Dona Paula, Goa, India


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