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Thermohaline structure and circulation in the upper layers of the southern Bay of Bengal during BOBMEX-Pilot (October–November 1998)
Author(s) -
V. Ramesh Babu,
V. S. N. Murty,
L.V.G. Rao,
Charuta V. Prabhu,
V. Tilvi
Publication year - 2000
Publication title -
journal of earth system science
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.444
H-Index - 52
eISSN - 0973-774X
pISSN - 0253-4126
DOI - 10.1007/bf02702199
Subject(s) - bay , ocean gyre , geology , bengal , oceanography , thermohaline circulation , hydrography , monsoon , climatology , shutdown of thermohaline circulation , acoustic doppler current profiler , ocean current , intertropical convergence zone , current (fluid) , north atlantic deep water , subtropics , geography , meteorology , precipitation , fishery , biology
Hydrographic data collected on board ORV Sagar Kanya in the southern Bay of Bengal during the BOBMEX-Pilot programme (October–November 1998) have been used to describe the thermohaline structure and circulation in the upper 200 m water column of the study region. The presence of seasonal Inter-Tropical Convergence Zone (ITCZ) over the study area, typically characterized with enhanced cloudiness and flanked by the respective east/northeast winds on its northern part and west/southwest winds on its southern part, has led to net surface heat loss of about 55 W/m2. The sea surface dynamic topography relative to 500 db shows that the upper layer circulation is characterised by a cyclonic gyre encompassing the study area. The eastward flowing Indian Monsoon Current (IMC) between 5‡N and 7‡N in the south and its northward branching along 87‡E up to 13‡N appear to feed the cyclonic gyre. The Vessel-Mounted Acoustic Doppler Current Profiler (VM-ADCP) measured currents confirm the presence of the cyclonic gyre in the southern Bay of Bengal during the withdrawing phase of the southwest monsoon from the northern/central parts of the Bay of Bengal.

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