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    Enhanced export of carbon by salps during the northeast monsoon period in the northern Arabian Sea 

    Ramaswamy, V.; Sarin, M.M.; Rengarajan, R. (Elsevier, 2005)
    A drifting sediment trap was deployed and sup(234)Th activity in the water column was measured to calculate export flux of carbon at a time-series station in the northern Arabian Sea (lat. 21 degrees 30 minutes N; long. ...
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    Seasonal sea surface temperature contrast between the Holocene and last glacial period in the western Arabian Sea (Ocean Drilling Project Site 723A): Modulated by monsoon upwelling 

    Naidu, P.D.; Malmgren, B.A. (AGU, 2005)
    Annual, summer, and winter sea surface temperatures (SSTs) in the western Arabian Sea were reconstructed through the last 22 kyr using artificial neural networks (ANNs) based on quantitative analyses of planktic foraminifera. ...
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    Summer monsoon rainfall prediction for India - Some new ideas 

    Varkey, M.J. (Narosa Publishing, 2005)
    Present methods of forecasting of mean Indian rainfall for summer monsoon season are critically examined. Considering the wide variations in mean seasonal rainfalls (more than 5 to less than 400 cm) and crops in various ...
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    Sediment texture, distribution and transport on the Ayeyarwady continental shelf, Andaman Sea 

    Rao, P.S.; Ramaswamy, V.; Thwin, S. (Elsevier, 2005)
    The Ayeyarwady continental shelf is a complex sedimentary system characterized by large sediment influx (N360 million ton/yr), a wide shelf (N170 km), a strong tidal regime (7 m maximum tidal range), and incised by the ...
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    The biology of the Arabian Sea and Bay of Bengal 

    Gauns, M. (Angkor, India, 2005)
    This article focusses on the variability in physics and chemistry of the region and investigate its influence on the biology. This article is largely based on the recent observations made during the India JGOFS and BOBPS ...
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    Weekly observations on dispersal and sink pathways of the terrigenous flux of the Ganga-Brahmaputra in the Bay of Bengal during NE monsoon 

    Chauhan, O.S.; Rajawat, A.S.; Pradhan, Y.; Suneethi, J.; Nayak, S.R. (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 ...
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    Observed variability of sea surface salinity and thermal inversions in the Lakshadweep Sea during contrast monsoons 

    Gopalakrishna, V.V.; Johnson, Z.; Salgaonkar, G.; Nisha, K.; Rajan, C.K.; Rao, R.R. (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 ...
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    Monsoon related changes in sea surface productivity and water column denitrification in the Eastern Arabian Sea during the last glacial cycle 

    Banakar, V.K.; Oba, T.; Chodankar, A.R.; Kuramoto, T.; Yamamoto, M.; Minagawa, M. (Elsevier, 2005)
    Sea surface salinity reconstruction for the Holocene and the Last Glacial Maximum (LGM) suggests that the LGM-Eastern Arabian Sea was more saline (by approx.5 psu) than the Holocene due to weakened freshwater flux to the ...
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    Seasonal variations in carbon biomass of bacteria, thraustochytrids and microzooplankton in the northern Arabian Sea 

    Ramaiah, N.; Raghukumar, S.; Gauns, M.; Madhupratap, M. (Elsevier, 2005)
    As a part of the JGOFS-India Programme, abundance of heterotrophic bacteria (Hbac; 0-2000 m), thraustochytrids (0-2000 m), microzooplankton (0-200m occasionally up to 300 m) as well as bacterial growth rates (0-500 m) were ...
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    Living coccolithophores during the northeast monsoon from the Equatorial Indian Ocean: Implications on hydrography 

    Guptha, M.V.S.; Mergulhao, L.P.; Murty, V.S.N.; Shenoy, D.M. (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 ...
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    AuthorGuptha, M.V.S. (3)Banakar, V.K. (2)Chodankar, A.R. (2)Gauns, M. (2)Ittekkot, V. (2)Madhupratap, M. (2)Murty, V.S.N. (2)Oba, T. (2)Ramaswamy, V. (2)Chauhan, O.S. (1)... View MoreSubject
    monsoons (16)
    palaeo studies (4)seasonal variations (4)upwelling (4)abundance (3)biogeochemical cycle (3)surface circulation (3)zooplankton (3)biogeochemical cycles (2)biomass (2)... View MoreDate Issued
    2005 (16)
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