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Circulation and watermass structure in the Central Arabian Sea during December 1982
(CSIR-NISCAIR, 1986)
After the cessation of the 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 ...
Watermass structure in the Bay of Bengal
(Indian Association for Limnology and Oceanography, 1985)
The distributions of temperature, salinity thermosteric anomaly, density flux function and stability along 88 degrees E in the Bay of Bengal are presented. The surface salinities showed strong gradients both horizontally ...
Watermass structure in the western Indian Ocean: Part 1. Watermasses and their thermohaline indices
(India Meteorological Department, 1986)
The concept of "Indian Ocean Common Watermass" is introduced and its characteristics are defined. The temperature-salinity structures which would result when one, two or more watermasses of different temperature and salinity ...
Watermass structure in the western Indian Ocean - Part 2. The spreading and transformation of the Persian Gulf water
(India Meteorological Department, 1986)
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 ...
Circulation and Distribution of some Hydrographical Properties during the late Winter in the Bay of Bengal
(Indian Association for Limnology and Oceanography, 1981)
Charts showing dynamic topography, mass distribution, temperature, salinity, dissolved oxygen and inorganic phosphate in the upper layers of the Bay of Bengal for the late winter period were analysed and presented. The ...