Record Details

Watermass structure in the western Indian Ocean - Part 2. The spreading and transformation of the Persian Gulf water

DRS at CSIR-National Institute of Oceanography

View Archive Info
 
 
Field Value
 
Title Watermass structure in the western Indian Ocean - Part 2. The spreading and transformation of the Persian Gulf water
 
Creator Premchand, K.
Sastry, J.S.
Murty, C.S.
 
Subject Oceanography and Limnology
salt flux
heat transfer
isohalines
vertical mixing
core reefs
salinity
water masses
ISW, Persian Gulf
ISW, Indian Ocean
 
Description The spreading and the transformation of the Persian Gulf Watermass (PGW) in the Arabian Sea and the Indian Ocean have been presented. The core layer of this watermass is found in the depth range of 250-300 m over most of the Arabian Sea with a tendency to deepen southwards. The salinity at the core decreases from 37.9 ppt. in the Gulf of Oman to 35.1 ppt. at the equatorial regions. Its spreading is found to be mainly towards the west-coast of India and southerly off the Indian coast. Owing to intense vertical mixing, rapid transformation of this watermass takes place in the Gulf of Oman. Vertical mixing of this watermass with the Red Sea watermass along the Arabian Coast gives rise to an isohaline layer in the depth range of 250-800 m and this layer has been termed as 'Arabian Sea Intermediate Watermass'. The influence of PGW in the deeper layers is reflected by the relatively higher temperatures and salinities at all depths in the northern Arabian Sea. Downward fluxes of heat and salt as a result of vertical mixing are inferred all along the core of this watermass
 
Date 1995-06-12T10:01:19Z
2017-09-29T13:48:23Z
1995-06-12T10:01:19Z
2017-09-29T13:48:23Z
1986
 
Type Journal Article
 
Identifier Mausam, vol.37; 1986; 179-186
0252-9416
http://drs.nio.org/drs/handle/2264/6278
 
Language en
 
Relation Mausam
SCI
 
Publisher India Meteorological Department