Please use this identifier to cite or link to this item: http://nopr.niscpr.res.in/handle/123456789/38574
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dc.contributor.authorBahulayan, N-
dc.contributor.authorVaradachari, V V R-
dc.date.accessioned2016-12-14T05:44:33Z-
dc.date.available2016-12-14T04:46:33Z-
dc.date.issued1986-03-
dc.identifier.issn0975-1033 (Online); 0379-5136 (Print)-
dc.identifier.urihttp://nopr.niscair.res.in/handle/123456789/38574-
dc.description8-12en_US
dc.description.abstractWind-driven circulation in the Bay of Bengal, generated by a southwest wind of constant speed (10 m.sec -1) and direction (225ᵒTN), is presented. A non-linear hydrodynamic model is used for the simulation of circulation. Numerical experiments have shown that when a uniform wind stress in suddenly imposed over the sea surface, a steady circulation is generated after 50 h of numerical integration of model equations. The sensitivity of this model to bathymetry and coastal configuration is also discussed. The study shows that maximum current speed is observed near the coastal region as anticipated and it generally tends to follow the idealised bottom contours.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(1) [March 1986]en_US
dc.titleNumerical model for wind-driven circulation in the Bay of Bengalen_US
dc.typeArticleen_US
Appears in Collections:IJMS Vol.15(1) [March 1986]

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