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Now showing items 201-210 of 223
Quaternary radiolarian faunal changes in the tropical Indian Ocean: Inferences to paleomonsoonal oscillation of the 10 degrees S hydrographic front
(Current Science Association, Bangalore, 1997)
The northern Indian Ocean is characterized by three distinct surface water masses, i.e. (1) highly saline (greater than 34.5 ppt) Arabian Sea, (2) low saline (less than 34.5 ppt) Bay of Bengal and (3) a moderate salinity ...
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 ...
Weekly observations on dispersal and sink pathways of the terrigenous flux of the Ganga-Brahmaputra in the Bay of Bengal during NE monsoon
(Elsevier, 2005)
The analyses of 64 sequential satellite images (October 1999-March 2001) of Indian Remote Sensing Satellite IRS-P4 ocean color monitor (OCM) (bands around 490, 555, and 670 nm) for total suspended matter (TSM), synchronous ...
Observed variability of sea surface salinity and thermal inversions in the Lakshadweep Sea during contrast monsoons
(AGU, 2005)
The sea surface salinity (SSS) of the Lakshadweep Sea (LS) shows large seasonal variability due to horizontal advection of low (high) salinity waters from south (north) during winter (summer) monsoon. The measurements made ...
Spatial distribution of upwelling off the central east coast of India
(Academic Press, 2002)
The spatial distribution of upwelling along the central east coast of India (13 degrees-18 degrees N) in the premonsoon and south-west monsoon seasons is described using data collected during cruises 193 (13-28 March 1988) ...
Monsoon oscillations of the Findlater Jet and coastal winds of India
(PORSEC 2002 Secretariat; Bogor; Indonesia, 2002)
Intraseasonal variability (ISV) of the Low Level Jet (LLJ) and its effects on coastal winds during the Indian summer monsoon are examined using National Centre for Environmental Prediction / National Centre for Atmospheric ...
Coastal processes at the southern tip of India during summer monsoon 2005
(School of Naval Oceanology and Meteorology, 2007)
In situ temperature and wind data, during summer monsoon 2005, bring out some interesting features like, the existence of a purely wind driven upweiling system at the southern tip (ST), very adjacent to another remotely ...
Dissolved aluminium in the surface microlayer of the eastern Arabian Sea
(Elsevier, 1993)
Measurements of dissolved aluminium (Al) in surface microlayer (SML) samples from the eastern Arabian Sea during the southwest (summer) and northwast (winter) monsoon periods have revealed much higher concentrations (23-657 ...
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 ...
Estimating boundary currents from satellite altimetry: A case study for the east coast of India
(The Oceanographic Society of Japan, 2008)
A methodology to derive surface geostrophic current from a newly released altimetric sea-level data set is presented. TOPEX/Poseidon data were first completely reprocessed from Geophysical Data Records using new algorithms ...