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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 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 ...
Estimation of evaporation rates over the Arabian Sea from Satellite data
(Indian Academy of Sciences, Bangalore, 1986)
Utilizing both the SAMIR brightness temperatures of Bhaskara 2 and GOSSTCOMP charts of NOAA satellite series, the evaporation rates over the Arabian Sea for June 1982 are estimated through the bulk aerodynamic method. The ...
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 ...
On the characteristics of multipeaked spectra of ocean surface waves
(Institute of Engineers�, 1986)