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Energy and generating mechanism of a subsurface, cold core eddy in the Bay of Bengal

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Title Energy and generating mechanism of a subsurface, cold core eddy in the Bay of Bengal
 
Creator Kumar, S Prasanna
Babu, M T
Rao, D P
 
Description 140-142
Computation of available potential energy (APE) of a recently observed cold core, subsurface eddy (centered at 17-degrees-40'N and 85-degrees-19'E) in the Bay of Bengal revealed that the energy maxima associated with the eddy was of the order of 1.31 x 10(2) J.m-3. The estimated Rosby radius of internal deformation compared well with the diameter of the eddy (congruent-to 200 km). The prevailing current system during the period of observation of the eddy was a southerly flow along the northwestern boundary forced by fresh water influx and a northerly flow along the southwestern boundary generated by wind forcing. The study showed that the energy density associated with the southward advective current (2.5 x 10(2) J.m-3) was more than twice of that in the northward flow (1.0 x 10(2) J.m-3). The study also indicated that the eddy obtained its energy from the APE produced mainly from the southward flowing boundary current.
 
Date 2016-12-01T11:15:19Z
2016-12-01T11:15:19Z
1992-06
 
Type Article
 
Identifier 0975-1033 (Online); 0379-5136 (Print)
http://nopr.niscair.res.in/handle/123456789/38036
 
Language en_US
 
Rights CC Attribution-Noncommercial-No Derivative Works 2.5 India
 
Publisher NISCAIR-CSIR, India
 
Source IJMS Vol.21(2) [June 1992]