Now showing items 1-15 of 15

    • A new atlas of temperature and salinity for the North Indian Ocean 

      Chatterjee, A.; Shankar, D.; Shenoi, S.S.C.; Reddy, G.V.; Michael, G.S.; Ravichandran, M.; Gopalakrishna, V.V.; Rao, E.P.R.; UdayaBhaskar, T.V.S.; Sanjeevan, V.N. (Indian Academy of Sciences, 2012)
      The most used temperature and salinity climatology for the world ocean, including the Indian Ocean, is the World Ocean Atlas (WOA) because of the vast amount of data used in its preparation. The WOA climatology does not, ...
    • Aeolian sand transport and its effects on the stability of Miramar-Caranzalem beach 

      Reddy, G.V.; Sastry, J.S. (Indian Association for Limnology and Oceanography, 1988)
      Removal of sand by wind from the beach at Miramar-Caranzalem, Goa, has been found to effect its stability over a relatively longer time scale. This aeolian sand transport has been computed for this strip of the beach ...
    • Determination of dynamic heights in the Bay of Bengal from XBT profiles and climatological salinities 

      Ali, M.M.; Gopalakrishna, V.V.; Araligidad, N.; Reddy, G.V.; Salgaonkar, G. (Sears Foundation for Marine Research, 2005)
      Dynamic height (DH) computations are necessary for the estimation of geostrophic currents, heat transport studies, identification of eddies and to validate the altimeter sea surface height (SSH) observations. To compute ...
    • Gyres in the NW Bay of Bengal - Some observed evidences 

      Rao, K.H.; Antony, M.K.; Murty, C.S.; Reddy, G.V. (CSIR-NISCAIR, 1987)
      Continuous observations of temperature, salinity and the flow at 4 stations off the rivers of Krishna, Godavari, Mahanadi and off New Moore Island, along the east coast of India, were made prior to the onset of the SW ...
    • Observed seasonal variability of barrier layer in the Bay of Bengal 

      Pankajakshan, T.; Muraleedharan, P.M.; Rao, R.R.; Somayajulu, Y.K.; Reddy, G.V.; Revichandran, C. (American Geophysical Union, 2007)
      The observed formation of Barrier Layer (BL) and the seasonal variability of BL thickness (BLT) in the Bay of Bengal are examined utilizing the most comprehensive data set. Thick BL (~50m) first appears in the coastal ...
    • Oceanographic data and information network in the Indian Ocean 

      Sarupria, J.S.; Reddy, G.V. (Kochi: School of Naval Oceanology and Meteorology, Southern Naval Command, 2004)
      Intergovernmental Oceanographic Commission (IOC) committee on International Oceanographic Data Exchange (IODE) has developed a data center network by establishing 70 National Oceanographic Data centres (NODCs) in 70 IOC ...
    • Present status of oceanographic studies and characteristics of the Exclusive Economic Zone of India 

      Desai, B.N.; Bhargava, R.M.S.; Sarupria, J.S.; Reddy, G.V. (International Ocean Technology Congress, 1989)
      The EEZ of India includes four seas viz: Arabian Sea, Lakshadweep Sea, Bay of Bengal and Andaman & Nicobar Sea. All the seas except the Andaman and Nicobar Sea are extensively surveyed. The total number of cruises undertaken ...
    • Seasonal variability of the observed barrier layer in the Arabian Sea 

      Pankajakshan, T.; Thoppil, P.; Rao, R.R.; Muraleedharan, P.M.; Somayajulu, Y.K.; Gopalakrishna, V.V.; Murthugudde, R.; Reddy, G.V.; Revichandran, C. (American Meteorological Society, 2008)
      The formation mechanisms of the barrier layer (BL) and its seasonal variability in the Arabian Sea (AS) are studied using a comprehensive dataset of temperature and salinity profiles from Argo and other archives for the ...
    • Seasonal variation of sea surface temperature in the Bay of Bengal during 1992 as derived from NOAA-AVHRR SST data 

      Murty, V.S.N.; Subrahmanyam, B.; Rao, L.V.G.; Reddy, G.V. (Taylor and Francis, 1998)
      Monthly maps of sea surface temperature (SST) derived for NOAA (National Oceanic and Atmospheric Administration)-AVHRR (Advanced Very High Resolution Radiometer) data during 1992 for the Bay of Bengal are analysed and ...
    • Sub-surface temperature oscillations and associated flow in the Western Bay of Bengal 

      Antony, M.K.; Murty, C.S.; Reddy, G.V.; Rao, K.H. (Elsevier, 1985)
    • Surface layer temperature inversion in the Bay of Bengal 

      Pankajakshan, T.; Gopalakrishna, V.V.; Muraleedharan, P.M.; Reddy, G.V.; Araligidad, N.; Shenoy, Shrikant (Pergamon, 2002)
      Surface layer temperature inversion occurring in the Bay of Bengal has been addressed. Hydrographic data archived in the Indian Oceanographic Data Center are used to understand various aspects of the temperature inversion ...
    • Surface layer temperature inversion in the Bay of Bengal 

      Pankajakshan, T.; Gopalakrishna, V.V.; Muraleedharan, P.M.; Reddy, G.V.; Araligidad, N. (NIO, Dona Paula, Goa (India), 2000)
      Hydrographic and XBT data archived in the Indian Oceanographic Data Centre (IODC) are used to understand the process of temperature inversions occurring in the Bay of Bengal. The following aspects of the inversions are ...
    • Temperature error in digital bathythermograph data 

      Pankajakshan, T.; Reddy, G.V.; Ratnakaran, L.; Sarupria, J.S.; RameshBabu, V. (NISCAIR, CSIR, 2003)
      Simultaneous Digital Bathythermograph (DBT) and Nansen Cast data collected during two cruises of R.V. Gaveshani (GV-117 and GV-118) and archived in Indian Oceanographic Data Centre (IODC) are used to determine existing ...
    • Validation of argo data in the Indian Ocean 

      Pankajakshan, T.; Muraleedharan, P.M.; Gopalakrishna, V.V.; Reddy, G.V.; Ratnakaran, L.; Revichandran, C.; Murty, V.S.N. (Universidad de Concepcion, 2004)
      ARGO-salinity data from the Indian Ocean are validated using salinity from float-versus-float match-ups and also using CTD observations from three cruises. Validation data sets are selected in such a way that the float and ...
    • Watermass structure and current system in the equatorial western Indian Ocean during August, 1985 

      Suryanarayana, A.; Reddy, G.V.; Pankajakshan, T. (Hamburg : Das Institut, 1987)
      During the 17th cruise of ORV Sagar Kanya (3rd to 21st August, 1985), two meridional sections were occupied between 4 degrees N and 6 degrees n S in the equatorial Western Indian Ocean. The Dynamic Method was employed to ...