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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 ...
Anomalous current structure in the eastern equatorial Indian Indian Ocean during the south-west monsoon of 1994
(CSIRO, Australia, 2001)
Analysis of hydrographic data collected along 80 degrees, 84 degrees and 88 degrees E between 5 degrees N and 3 degrees S during peak south-west monsoon (July-August) of the eastern equatorial Indian Ocean (EEIO) reveals ...
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 ...
Upper ocean stratification and circulation in the northern Bay of Bengal during southwest monsoon of 1991
(Pergamon, 2002)
During the southwest monsoon (July) of 1991 a large plume (300 x 250 km sup(2)) of warm (greater than 29 degrees C) and less saline (less than 29 PSU) water is noticed in the top 30 m to the east of 87.5 degrees E in the ...
Living coccolithophores during the northeast monsoon from the Equatorial Indian Ocean: Implications on hydrography
(Elsevier, 2005)
Water samples collected at five stations along 931E section (1 degrees N-4 degrees S) during the northeast monsoon (12-15 February 2000) at five depths (surface, 50, 100, 150 and 200 m) in the eastern equatorial Indian ...
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 ...
On the circulation in the Bay of Bengal during northern spring inter-monsoon (March-April 1987)
(Elsevier, 2003)
Temperature and salinity data collected from the Bay of Bengal 22 March-28 April 1987 (Northern spring inter-monsoon) identified the seasonal anticyclonic gyre (ACG) at 16 degrees N, 86 degrees E characterized by warm ...
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 ...