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Now showing items 21-30 of 34
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 ...
सफेद रेगिस्तान - अंटार्कटिका
(1986)
Sea surface temperature variability over North Indian Ocean - A study of two contrasting monsoon seasons
(Indian Academy of Sciences, Bangalore, 1986)
Using the satellite derived sea surface temperature (SST) data for 1979 (bad monsoon) and 1983 (good monsoon), the SST variability for two contrasting monsoon seasons is studied. The study indicates that large negative ...
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 ...
Thermohaline forcing of eastern boundary currents: With application to the circulation off the west coast of Australia
(Ingenta Connect Publication, 1986)
The linear, viscid, continuously stratified model of McCreary (1981) is extended to allow for thermohaline forcing by a specified, longitudinally independent, surface density field @ips@@. When the ocean is unbounded and ...
A model study of the seasonal cycle of the Arabian Sea surface temperature
(Ingenta Connect Publication, 1986)
The annual variation of the SST along a zonal strip from the coast of Somalia to the southwest coast of India was simulated using available data (monthly-mean heat and momentum fluxes across the air-sea interface, surface ...
Deep and bottom water characteristics in the Owen Fracture Zone, Western Arabian Sea
(CSIR-NISCAIR, 1986)
Hydro chemical studies at a station (10 degrees 34.l'N,56 degrees 31,7'E) in the Owen Fracture zone reveal an active movement of bottom water as approx 75 m thick, cold, low-salinity layer. Silicate profile exhibits a broad ...