Please use this identifier to cite or link to this item: http://nopr.niscpr.res.in/handle/123456789/38700
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dc.contributor.authorSarma, Y V B-
dc.contributor.authorMurty, V S N-
dc.contributor.authorRao, D Panakala-
dc.contributor.authorSastry, J S-
dc.date.accessioned2016-12-15T06:53:52Z-
dc.date.available2016-12-15T06:53:52Z-
dc.date.issued1986-12-
dc.identifier.issn0975-1033 (Online); 0379-5136 (Print)-
dc.identifier.urihttp://nopr.niscair.res.in/handle/123456789/38700-
dc.description234-240en_US
dc.description.abstractAfter the cessation ofthe SW monsoon over Arabian Sea, the North Equatorial Current sets strongly and the low saline waters from the Bay of Bengal and the equatorial Indian Ocean penetrate into the Arabian Sea. This results in strong horizontal salinity gradients in the upper layers due to the mixing of the Persian Gulf, Bay of Bengal and Arabian Sea High Salinity Waters. The low salinity water is found to originate in the Andaman Sea and its thermohaline index has been derived as T= 18.6°C and S = 34.5 X 10-3 and can be traced on the 300 cl/t isanosteric surface. The mixing patterns in the central Arabian Sea have been studied by constructmg the triangles of mixing. It is found that, the vertical mixing is dominant along the core of the Persian Gulf Watermass.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.15(4) [December 1986]en_US
dc.titleCirculation &Watermass Structure in the Central Arabian Sea during December 1982en_US
dc.typeArticleen_US
Appears in Collections:IJMS Vol.15(4) [December 1986]

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