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    Antibacterial Activity of 2- (2',4'- Dibromophenoxy) -4, 6 - dibromophenol from Dysidea granulose 

    DivyaShridhar, M.P.; Mahajan, G.B.; Kamat, V.P.; Naik, C.G.; Parab, R.R.; Thakur, N.R.; Mishra, P.D. (Molecular Diversity Preservation International, 2009)
    2 - (2',4'- Dibromophenoxy) - 4, 6 - dibromophenol isolated from the marine sponge Dysidea granulosa (Bergquist) collected off the coast of Lakshadweep islands, Indian Ocean, exhibited potent and broad spectrum in-vitro ...
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    Biogeochemistry of the North Indian Ocean 

    DileepKumar, M. (Indian National Science Academy, 2006)
    Biogeochemistry is a subject wherein geochemical and biological processes occurring in the upper layers of the Earth, including atmosphere, are studied together. Many of the climatically important gases influencing the ...
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    Observational evidence for westward propagation of temperature inversions in the southeastern Arabian Sea 

    Shankar, D.; Gopalakrishna, V.V.; Shenoi, S.S.C.; Durand, F.; Shetye, S.R.; Rajan, C.K.; Johnson, Z.; Araligidad, N.; Michael, G.S. (American Geophysical Union, 2004)
    A warm pool forms in the southeastern Arabian Sea (SEAS) prior to the onset of the summer monsoon over India in early June; the core of this warm pool is in the Lakshadweep Sea (LS). XBT and surface salinity data collected ...
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    Climate fluctuations of tropical coupled systems — The role of ocean dynamics 

    Chang, P.; Yamagata, T.; Schopf, P.; Behera, S.K.; Carton, J.; Kessler, W.S.; Meyers, G.; Qu, T.; Schott, F.; Shetye, S.R.; Xie, S.P. (American Meteorological Society, 2006)
    The tropical oceans have long been recognized as the most important region for large-scale ocean-atmosphere interactions, giving rise to coupled climate variations on several time scales. During the TOGA decade, the focus ...
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    Quantitative characteristics of the Indian Ocean seafloor relief using fractal dimension 

    Chakraborty, B.; Mahale, V.; Shashikumar, K.; Srinivas, K. (NISCAIR, CSIR, 2007)
    In this paper spectral technique has been applied for seafioor topographic data analyses from three seafioor provinces of the Indian Ocean. Study sites include West of the Andaman Island (WAT), Western Continental Margins ...
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    A petrogenetic model of basalts from the Northern Central Indian Ridge: 3-11°S 

    Ray, Dwijesh; Iyer, S.D.; Banerjee, R.; Misra, S.; Widdowson, M. (Geological Society of China, 2007)
    Mid-Ocean Ridge Basalts (MORB) from Northern Central Indian Ridge (NCIR) were recovered between latitudes 30 and 110S and are olivine tholeiite with higher abundances of K and Rb. They are of typical transitional MORB ...
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    RAMA: The Research Moored Array for African-Asian-Australian Monsoon Analysis and Prediction (including supplement) 

    McPhaden, M.J.; Meyers, G.; Ando, K.; Masumoto, Y.; Murty, V.S.N.; Ravichandran, M.; Syamsudin, F.; Vialard, J.; Yu, L.; Yu, W. (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, ...
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    Response of deep-sea macrobenthos to a small-scale environmental disturbance 

    Ingole, B.S.; Ansari, Z.A.; Rathod, V.; Rodrigues, N. (Elsevier, 2001)
    To assess the possible effect of nodule mining on deep-sea environment, the Indian deep-sea environment experiment (INDEX) was undertaken in the Indian Basin. The present investigation is a part of the disturbance and ...
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    18 Ka BP records of climatic changes, Bay of Bengal: Isotopic and sedimentological evidences 

    Chauhan, O.S.; Suneethi, J. (Indian Academy of Sciences, 2001)
    Based upon the oxygen isotopic records of Globigerinoide sacculifer, the clay mineral assemblages and aridity indicator chlorite/illite (C/I) ratio, the palaeoclimatic changes during the past 18 Ka BP have been archived. ...
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    Why is mean sea level along the Indian coast higher in the Bay of Bengal than in the Arabian Sea? 

    Shankar, D.; Shetye, S.R. (Americal Geophysical Union, 2001)
    Levelling observations conducted during the Great Trigonometrical Survey of India (1858-1909) and subsequent observations showed that mean sea level along the coast of India is higher in the Bay of Bengal than in the Arabian ...
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    AuthorShankar, D. (12)Naqvi, S.W.A. (10)Ingole, B.S. (8)Shetye, S.R. (8)Shenoi, S.S.C. (7)Murty, V.S.N. (6)Saraswat, R. (6)Iyer, S.D. (5)RameshKumar, M.R. (5)Vialard, J. (5)... View MoreSubject
    Indian Ocean (122)
    Bay of Bengal (10)Arabian Sea (7)Monsoon (4)monsoon (4)Rossby waves (4)sediments (4)West India Coastal Current (4)Air-sea interaction (3)Central Indian Ocean Basin (3)... View MoreDate Issued2010 - 2011 (27)2000 - 2009 (95)Has File(s)Yes (122)

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