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Seasonal variability of upper-layer geostrophic transport in the tropical Indian Ocean during 1992-1996 along TOGA-I XBT tracklines
(Pergamon, 2000)
Upper layer (0-400 m) geostrophic volume transport associated with the major current systems of the tropical Indian Ocean along the near-meridional TOGA-India XBT tracklines from Mumbai to Mauritius during 1992-1996 is ...
Intraseasonal meridional current variability in the eastern equatorial Indian Ocean
(American Geophysical Union, 2008)
Intraseasonal variability in meridional current in the eastern equatorial Indian Ocean is investigated by use of results from a high-resolution ocean general circulation model. Both the simulated and observed meridional ...
Estimation of sea surface salinity in the Bay of Bengal using Outgoing Longwave Radiation
(American Geophysical Union, 2002)
A new technique for retrieval of sea surface salinity (SSS) from space-borne satellite measurements of Outgoing Longwave Radiation (OLR) through the 'Effective Oceanic Layer (EOL)' is explained in this paper. The OLR is ...
Seasonal cyclogenesis and the role of near-surface stratified layer in the Bay of Bengal
(NIO, Dona Paula, Goa (India), 2000)
The role of the near-surface stratified layer developed due to the spread of low salinity waters under the influence of freshwater influx on the cyclogenesis over the Bay of Bengal is addressed. The seasonal variation of ...
Impact of freshwater influx on the cyclogenesis, tracks of cyclones and air-sea coupling over the Bay of Bengal
(National Institute of Oceanography, India, 2008)
Over the Bay of Bengal weather disturbances of considerable seasonal variability in their zones of genesis, intensity, frequency and path across the Bay generate during May-November. This variability in the zones of ...
First results of Indian - Current meter moorings along The equator: Vertical current structure variability at equator, 93 degrees E during February-December, 2000
(PORSEC 2002 Secretariat; Bogor; Indonesia, 2002)
The first results of time-series current data obtained from 6 levels at equator, 93 degrees E in the eastern equatorial Indian Ocean during February-December 2000 are analyzed. The top RCM was located at 135m. The mean ...