Now showing items 1-10 of 28
Convergence of Ekman wind driven layer and surface circulation in the Arabian sea during southwest monsoon
(Indian Association for Limnology and Oceanography, 1979)
Hydrological characteristics and transequatorial transport in the west Indian Ocean
Circulation and watermass structure in the Central Arabian Sea during December 1982
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 ...
Surface circulation over the shelf off the east coast of India during the south west monsoon
From the hydrographic data collected on board R V Gaveshani in the Western Bay of Bengal during August-September 1978, fields of temperature, salinity have been constructed and the probable flow regime has been deduced. ...
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 ...