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dc.contributor.authorShaji, C.
dc.contributor.authorBahulayan, N.
dc.contributor.authorDube, S.K.
dc.contributor.authorRao, A.D.
dc.date.accessioned2009-01-12T09:29:33Z
dc.date.available2009-01-12T09:29:33Z
dc.date.issued1997
dc.identifier.citationIndian Journal of Marine Sciences, Vol.26; 250-257p.
dc.identifier.urihttp://drs.nio.org/drs/handle/2264/2086
dc.description.abstractClimatic circulation in the upper levels of the Arabian Sea and western equatorial Indian Ocean are computed using a 3-dimensional, 33 level diagnostic circulation model. A steady state solution is obtained within 30 days of model integration. Model has been successful in computing all the major seasons. Computed currents are compared with available observations on currents at selected regions in the model area and it has been found that both agreed fairly well. Model results are also explained in terms of the forcing parameters and the dynamics considered in the model.
dc.language.isoen
dc.publisherNISCAIR, CSIR
dc.rightsCopyright [1997]. 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.subjectequatorial circulation
dc.subjectclimate
dc.subjectmathematical models
dc.subjectcomputation
dc.subjectsteady state
dc.subjectmonsoon reversal
dc.subjectdynamical oceanography
dc.titleNumerical experimentation of a diagnostic model of 3-D circulation in the Arabian Sea
dc.typeJournal Article


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