Now showing items 1-4 of 4

    • Dynamics of the east India coastal current. 2. Numerical solutions 

      McCreary, J.P.; Han, W.; Shankar, D.; Shetye, S.R. (American Geophysical Union, 1996)
      A linear, continuously stratified model is used to investigate the dynamics of the East India Coastal Current (EICC). Solutions are found numerically in a basin that resembles the Indian Ocean basin north of 29 degrees S, ...
    • Hydrography and circulation in the western Bay of Bengal during the northeast monsoon 

      Shetye, S.R.; Gouveia, A.D.; Shankar, D.; Shenoi, S.S.C.; Vinayachandran, P.N.; Sundar, D.; Michael, G.S.; Nampoothiri, G. (American Geophysical Union, 1996)
      The Bay of Bengal, a semienclosed tropical basin that comes under the influence of monsoonal wind and freshwater influx, is distinguished by a strongly stratified surface layer and a seasonally reversing circulation. We ...
    • Transport and potential vorticity in the Bay of Bengal during the southwest monsoon 

      Murty, V.S.N.; Murty, C.S.; Sarma, Y.V.B.; Rao, D.P.; Sastry, J.S.; Rao, G.R.L. (Andhra University, Visakhapatnam (India), 1996)
      In the Bay of Bengal, the water transport and potential vorticity (PV) during the southwest monsoon are examined through the prevailing thermohaline and wind-driven circulation. The Indian Monsoon Current (IMC) and the ...
    • Westward movement of eddies into the Gulf of Aden from the Arabian Sea 

      Al Saafani, M.A.; Shenoi, S.S.C.; Shankar, D.; Aparna, M.; Kurian, J.; Durand, F.; Vinayachandran, P.N. (American Geophysical Union, 2007)
      Sea level anomalies (SLA) from satellite altimetry (1993-2003) reveal the westward movement of mesoscale eddies in the Gulf of Aden. Inside the gulf the eddies move at a speed of approx. 6.0-8.5 cm s sup(-1), comparable ...