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BOBMEX: The Bay of Bengal Monsoon Experiment
(American Meteorological Society, 2001)
The first observational experiment under the Indian Climate Research Programme, called the Bay of Bengal Monsoon Experiment (BOBMEX), was carried out during July-August 1999. BOBMEX was aimed at measurements of important ...
Observations of barrier layer formation in the Bay of Bengal during summer monsoon
(American Geophysical Union, 2002)
Time series of temperature and salinity in the upper ocean, measured at 17 degrees 30'N, 89 degrees E in the northern Bay of Bengal, from 27 July to 6 August 1999 captured an event of upper layer freshening. Initially, the ...
Warm pool thermodynamics from the Arabian Sea Monsoon Experiment (ARMEX)
(American Geophysical Union, 2008)
Before the onset of the south Asian summer monsoon, sea surface temperature (SST) of the north Indian Ocean warms to 30-32 degrees C. Climatological mean mixed layer depth in spring (March-May) is 10-20 m, and net surface ...
Bimodal character of cyclone climatology in the Bay of Bengal modulated by monsoon seasonal cycle
(American Meteorological Society, 2013)
The annual cycle of tropical cyclone (TC) frequency over the Bay of Bengal (BoB) exhibits a notable bimodal character, different from a single peak in other basins. The causes of this peculiar feature were investigated ...
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 ...
Anomalous circulation in the eastern equatorial Indian Ocean during southwest monsoon of 1994
(NIO, Dona Paula, Goa (India), 2000)
Geostrophic circulation derived from hydrographic data collected during July-August, 1994 along 80, 84 and 88E between 5N and 3S latitudinal belt in the eastern equatorial Indian Ocean is presented. A broad westward flow ...
Circulation and watermass structure in the Central Arabian Sea during December 1982
(CSIR-NISCAIR, 1986)
After the cessation of the SW monsoon over Arabian Sea, the North Equatorial Current sets strongly and the low saline waters from the Bay of Bengal and the equatorial Indian Ocean penetrate into the Arabian Sea. This results ...
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 ...