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Influence of the monsoon trough on air-sea interaction in the head of the Bay of Bengal during the southwest monsoon of 1990 (monsoon trough boundary layer experiment - 90)
(Kluwer, 1997)
The analysis of 3-hourly time-series data on surface meteorological parameters collected at 20 degrees N, 89 degrees E in the head of the Bay of Bengal during the southwest monsoon period (18 August - 19 Spetember) of 1990 ...
T-S variability and volume transport in the central Bay of Bengal during southwest monsoon
(NISCAIR, CSIR, 1996)
The variability of temperature and salinity along 11 degrees N and 12 degrees N sections in the Bay of Bengal during southwest monsoon months (July-September) was found to be large in the upper 200 m west of 83 degrees E ...
Physical oceanography of the Bay of Bengal and Andaman Sea
(George Allen and Unwin. London, UK, 1996)
Physical oceanography of the Bay of Bengal and Andaman Sea is reviewed for the first time. All available information for over 50 years is consolidated in this review. To begin with, information on peripheral or related ...
Transport and potential vorticity in the Bay of Bengal during the southwest monsoon
(Andhra University, Visakhapatnam (India), 1996)
In the Bay of Bengal, the water transport and potential vorticity (PV) during the southwest monsoon are examined through the prevailing thermohaline and wind-driven circulation. The Indian Monsoon Current (IMC) and the ...
Surface circulation off Somalia and western equatorial Indian Ocean during summer monsoon of 1988 from Geosat altimeter data
(Taylor and Francis, 1996)
The sea level variability derived from repeating tracks of the Geosat altimeter data during the late phase (August-September) of the summer monsoon of 1988 revealed the presence of multiple meso-scale eddy features with ...
Variability of the oceanic boundary layer characteristics in the Northern Bay of Bengal during MONTBLEX-90
(Indian Academy of Sciences, Bangalore, India, 1996)
Variability of the ocean surface boundary layer characteristics on daily time-scale is studied utilizing the 3-hourly hydrographic data collected at a stationary location (20 degrees N, 89 degrees E) in the Bay of Bengal ...