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dc.contributor.authorPrasad, T.G.
dc.contributor.authorBahulayan, N.
dc.date.accessioned2009-01-21T11:25:29Z
dc.date.available2009-01-21T11:25:29Z
dc.date.issued1996
dc.identifier.citationIndian Journal of Marine Sciences, Vol.25; 189-194p.
dc.identifier.urihttp://drs.nio.org/drs/handle/2264/2277
dc.description.abstractA band of zonally oriented ridge of mixed layer depth and thermocline base extending from African Coast to the Central Indian Ocean is observed between 5 degrees S and 10 degrees S throughout hte year. Mixed layer depth and thermocline base deepen during February and March in the vicinity of equator, off Kenya due to the convergence of northward flowing East African Coastal Current and southward flowing Somalin current. Power law has been used to calculate thermocline base. Characteristics of thermocline thickness resemble those of the thermocline base.
dc.language.isoen
dc.publisherNISCAIR, CSIR
dc.rightsCopyright [1996]. 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.subjectmixed layer depth
dc.subjectclimatology
dc.subjectthermocline
dc.subjectclimatological charts
dc.titleMixed layer depth and thermocline climatology of the Arabian Sea and western equatorial Indian Ocean
dc.typeJournal Article


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