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Current structure and volume transport across 12 degrees N in the Bay of Bengal
(NISCAIR, New Delhi, 1993)
Geostrophic currents and the associated volume transport across 12 degrees N in the Bay of Bengal during early southwest monsoon (April), southwest monsoon (September) and early northeast monsoon (November) show flow ...
Impact of river discharge on the coastal water pH and pCO<sub>2</sub> levels during the Indian Ocean Dipole (IOD) years in the western Bay of Bengal
(Elsevier, 2015)
Monthly variations in inorganic carbon components during January 2010–December 2011 in the coastal Bay of Bengal (BoB) were studied in relation to the variations in Godavari River (GR) discharge using ship board measurements, ...
RAMA: The Research Moored Array for African-Asian-Australian Monsoon Analysis and Prediction (including supplement)
(American Meteorological Society, 2009)
The Indian Ocean is unique among the three tropical ocean basins in that it is blocked at 25 degrees N by the Asian landmass. Seasonal heating and cooling of the land sets the stage for dramatic monsoon wind reversals, ...
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 ...
VM-ADCP measured upper ocean currents in the southeastern Arabian Sea and Equatorial Indian Ocean during December, 2000
(PORSEC 2002 Secretariat; Bogor; Indonesia, 2002)
The Vessel-Mounted Acoustic Doppler Current Profiler (VM-ADCP) measured currents in the upper 200 m along the cruise track covering the southeastern Arabian Sea and the Eastern Equatorial Indian Ocean during northern winter ...
Upper ocean variability in the Bay of Bengal during the tropical cyclones Nargis and Laila
(Elsevier, 2012)
Upper ocean variability at different stages in the evolution of the tropical cyclones Nargis and Laila is evaluated over the Bay of Bengal (BoB) during May 2008 and May 2010 respectively. Nargis initially developed on 24 ...
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 ...
Potential vorticity field in the Bay of Bengal during southwest monsoon
(Indian Society for Physical Sciences of the Oceans, 1992)
The distribution of potential vorticity along potential density surfaces in the upper 500 m indicates the presence of a wind driven anticyclonic gyre between 10 degrees N and 14 degrees N in the eastern Bay during southwest ...
Diurnal variability of upper ocean temperature and heat budget in the southern Bay of Bengal during October-November, 1998 (BOBMEX-Pilot)
(Indian Academy of Sciences, 2000)
Time-series data on upper-ocean temperature, Vessel-Mounted Acoustic Doppler Current Profiler (VM-ADCP) measured currents and surface meteorological parameters have been obtained for the first time in the southern Bay of ...
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 ...