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    A study on the characteristics of temperature inversions in active and break phases of Indian summer monsoon 

    Muraleedharan, P.M.; Mohankumar, K.; Sivakumar, K.U. (Elsevier, 2013)
    The thermal inversion characteristics during active and break cycles of two consecutive and contrasting monsoon years were studied using GPS radiosonde profiles in Goa (15 degrees 46′ N; 73 degrees 08′ E), located on the ...
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    Distribution and abundance of mysid shrimps (Crustacea: Mysidacea) in the Northern Indian Ocean. 

    Biju, A.; Jagadeesan, L.; Panampunnayil, S.U. (Taylor & Francis, 2014)
    The distribution and abundance of mysids were studied based on materials collected from the upper 1000 m of the Northern Indian Ocean (Exclusive Economic Zone (EEZ) of India) during the period 2002–2006. A greater abundance ...
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    On the spatial structure and time evolution of shamal winds over the Arabian Sea – a case study through numerical modelling. 

    VinodKumar, K.; Seemanth, M.; Vethamony, P.; Aboobacker, V.M. (Royal Meteorological Society, 2014)
    Shamal events are extra-tropical weather systems which occur in winter (cold and dry winds) as well as summer (hot and humid winds) with strong northwesterly or northerly winds blowing over the Arabian Peninsula. We have ...
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    Bimodal character of cyclone climatology in the Bay of Bengal modulated by monsoon seasonal cycle 

    Li, Z.; Yu, W.; Li, T.; Murty, V.S.N.; Fredolin, T. (American Meteorological Society, 2013)
    The annual cycle of tropical cyclone (TC) frequency over the Bay of Bengal (BoB) exhibits a notable bimodal character, different from a single peak in other basins. The causes of this peculiar feature were investigated ...
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    Change in the intensity of low-salinity water inflow from the Bay of Bengal into the Eastern Arabian Sea from the Last Glacial Maximum to the Holocene: Implications for monsoon variations 

    Mahesh, B.S.; Banakar, V.K. (Elsevier, 2014)
    A 100–400 km wide region of the coastal Eastern Arabian Sea (EAS), off the west-coast of India, is characterized by a low-salinity tongue formed by the inflow of low-salinity surface water from the Bay of Bengal (BoB). ...
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    Coupling between suboxic condition in sediments of the western Bay of Bengal and southwest monsoon intensification: A geochemical study 

    Pattan, J.N.; Mir, I.A.; Parthiban, G.; Karapurkar, S.G.; Matta, V.M.; Naidu, P.D.; Naqvi, S.W.A. (Elsevier, 2013)
    Reconstruction of paleo-redox conditions in a radiocarbon (14C) dated sediment core (SK-218/1), covering the past 45 ka (thousand calendar years), collected from the western Bay of Bengal (Lat: 14 degrees 02′N; Long: 82 ...
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    Distribution and air–sea exchange of nitrous oxide in the coastal Bay of Bengal during peak discharge period (southwest monsoon) 

    Rao, G.D.; Rao, V.D.; Sarma, V.V.S.S. (Elsevier, 2013)
    In order to examine the impact of river discharge from the Indian subcontinent on the concentration and air–sea exchange of nitrous oxide (N sub(2)O) a study was conducted during peak discharge period in the coastal Bay ...
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    Does SW Monsoon Influence Total Suspended Matter Flux into the Arabian Sea? 

    Raghavan, B.R.; Chauhan, O.S. (Coastal Education and Reserch Foundation, 2013)
    Seasonal enhancement in the flux of total suspended matter (TSM) has been attributed to climatology of the SW monsoon (SWM) in time-series trap experiments conducted in the Arabian Sea. To determine the influence of climate ...
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    Is an onset vortex important for monsoon onset over Kerala? 

    RameshKumar, M.R.; Sankar, S.; Reason, C. (Springer, 2012)
    Inter-annual variability in the formation of the mini warm pool [sea-surface temperature (SST) more than 30 degrees C] over the south eastern Arabian Sea (SEAS) and its role in the formation of the monsoon onset vortex ...
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    Variation in the Indian summer monsoon intensity during the Bolling-Allerod and Holocene 

    Kessarkar, P.M.; Rao, V.P.; Naqvi, S.W.A.; Karapurkar, S.G. (American Geophysical Union, 2013)
    Variations in the Indian summer monsoon (ISM) intensity during the last 16.7 ka have been studied using organic carbon (C<sub>org</sub>), delta <sup>15</sup>N of sedimentary organic matter, CaCO<sub>3</sub>, sediment ...
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    AuthorNaidu, P.D. (3)Vethamony, P. (3)Chauhan, O.S. (2)Gupta, A.K. (2)Karapurkar, S.G. (2)Naqvi, S.W.A. (2)Raghavan, B.R. (2)RameshKumar, M.R. (2)Saraswat, R. (2)Aboobacker, V.M. (1)... View MoreSubject
    monsoons (23)
    nutrients (mineral) (3)palaeoclimatology (3)foraminifera (2)micropalaeontology (2)organic carbon (2)palaeosalinity (2)salinity (2)surface temperature (2)suspended particulate matter (2)... View MoreDate Issued2014 (8)2013 (7)2012 (6)2010 (1)2011 (1)Has File(s)Yes (23)

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