Please use this identifier to cite or link to this item: http://nopr.niscpr.res.in/handle/123456789/35739
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dc.contributor.authorPal, P K-
dc.contributor.authorAli, M M-
dc.date.accessioned2016-10-18T09:33:41Z-
dc.date.available2016-10-18T09:33:41Z-
dc.date.issued1998-03-
dc.identifier.issn0975-1033 (Online); 0379-5136 (Print)-
dc.identifier.urihttp://nopr.niscair.res.in/handle/123456789/35739-
dc.description72-75en_US
dc.description.abstractSomali eddies have been simulated by reduced gravity, primitive equation thermodynamic model by converting the equatorial Pacific Ocean medel of Gent & Cane to the Arabian Sea. The cyclonic/anticyclonic patterns observed in the circulation are also reflected in the sea surface height elevations and in the mixed layer depth gradients. In the periphery of the anticyclonic eddies the depressions due to the upwelling is clearly seen.en_US
dc.language.isoen_USen_US
dc.publisherNISCAIR-CSIR, Indiaen_US
dc.rights CC Attribution-Noncommercial-No Derivative Works 2.5 Indiaen_US
dc.sourceIJMS Vol.27(1) [March 1998]en_US
dc.titleArabian Sea eddies simulated by an ocean model with thermodynamicsen_US
dc.typeArticleen_US
Appears in Collections:IJMS Vol.27(1) [March 1998]

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