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Hydrography of the Andaman sea during late Winter

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Title Hydrography of the Andaman sea during late Winter
 
Creator Babu, V. Ramesh
Sastry, J. S.
 
Description 179-189
Distributions of temperature, salinity, density and dissolved oxygen during late winter in the Andaman Sea are presented by series of vertical sections and spatial distribution charts; study of the field of motion on dynamic computations is also included. Surface temperature exceeds 28°C over most of the northern Andaman Sea. Surface salinity increases from 31.0% in the northern regions to 32.8% in the southern regions. Density distribution in the upper 50 m is primarily controlled by the salinity distribution. Below the sill depth (1300 m), the water mass is characterized by uniform values of temperature, salinity and dissolved oxygen. Geostrophic circulation in the upper layer indicates the formation of cells (100-200 km), and the upper layer dynamics seem to be governed by the fresh water discharge into the region.
 
Date 2017-01-02T08:34:11Z
2017-01-02T08:34:11Z
1976-12
 
Type Article
 
Identifier 0975-1033 (Online); 0379-5136 (Print)
http://nopr.niscair.res.in/handle/123456789/39482
 
Language en_US
 
Rights CC Attribution-Noncommercial-No Derivative Works 2.5 India
 
Publisher NISCAIR-CSIR, India
 
Source IJMS Vol.05(2) [December 1976]