Browsing by Author "Prasad, T.G."
Now showing items 1-9 of 9
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An atlas of precipitation over the tropical Indian Ocean using satellite data
RameshKumar, M.R.; Prasad, T.G. (1995) -
Annual and interannual variation of precipitation over the tropical Indian Ocean
RameshKumar, M.R.; Prasad, T.G. (American Geophysical Union, 1997)The annual and interannual variability of precipitation over the tropical Indian Ocean is studied for the period June 1986 to December 1990 using the data retrieved from the Indian National Satellite (INSAT). The seasonal ... -
Annual and seasonal mean buoyancy fluxes for the tropical Indian Ocean
Prasad, T.G. (Current Science Association, Bangalore, 1997)INSAT-derived monthly mean precipitation, combined with estimates of evaporation from COADS, are used to prepare the annual mean and seasonal distributions of evaporation-precipitation (E-P)) and buoyancy fluxes for the ... -
Formation and spreading of Arabian Sea high-salinity water mass
PrasannaKumar, S.; Prasad, T.G. (American Geophysical Union, 1999)The formation and seasonal spreading of the Arabian Sea High-Salinity Water (ASHSW) mass were studied based on the monthly mean climatology of temperature and salinity in the Arabian Sea, north of the equator and west of ... -
Mixed layer depth and thermocline climatology atlas of the Arabian Sea and Western Indian Ocean
Prasad, T.G.; Bahulayan, N. (1995) -
Mixed layer depth and thermocline climatology of the Arabian Sea and western equatorial Indian Ocean
Prasad, T.G.; Bahulayan, N. (NISCAIR, CSIR, 1996)A band of zonally oriented ridge of mixed layer depth and thermocline base extending from African Coast to the Central Indian Ocean is observed between 5 degrees S and 10 degrees S throughout hte year. Mixed layer depth ... -
Seasonal spreading of the Persian Gulf water mass in the Arabian Sea
Prasad, T.G.; Ikeda, M.; PrasannaKumar, S. (American Geophysical Union, 2001)The characteristics of the subsurface salinity maximum associated with the Persian Gulf Water mass (PGW) are used to quantify the spreading and mixing of PGW in the thermocline of the Arabian Sea based on a bimonthly ... -
Why is the Bay of Bengal less productive during summer monsoon compared to the Arabian Sea?
PrasannaKumar, S.; Muraleedharan, P.M.; Prasad, T.G.; Gauns, M.; Ramaiah, N.; DeSouza, S.N.; Sardessai, S.; Madhupratap, M. (American Geophysical Union, 2002)The Bay of Bengal is traditionally considered to be a less productive basin compared to the Arabian Sea. We explore the reasons for this in the central Bay during summer when both are subjected to strong monsoon forcing. ... -
Winter cooling in the northern Arabian Sea
PrasannaKumar, S.; Prasad, T.G. (Current Science Association, Bangalore, India, 1996)The upper thermo-haline structure and the surface meteorological parameters of the central and eastern Arabian Sea during the inter-monsoon (April-May, 1994) and winter monsoon (February-March, 1995) periods, were analysed ...