Now showing items 1-4 of 4

    • Biogeochemical budgets for Tapi Estuary 

      Bapardekar, M.V.; DeSousa, S.N.; Zingde, M.D. (IGBP, 2004)
      The Tapi estuary (21 degrees 10'N, 72 degrees 40'E) is a tidal estuary originating in the Multai Ghats in Madhya Pradesh at an elevation of 752 m. The 720 km long river, after passing through the 3 states of Madhya Pradesh, ...
    • Computation of diffusion coefficients for waters of Gauthami Godavari estuary using one-dimensional advection-diffusion model 

      Jyothi, D.; Murty, T.V.R.; Sarma, V.V.; Rao, D.P. (NISCAIR, CSIR, 2000)
      An analysis of salinity, salt budget and diffusion coefficients based on the salinity data of Gauthami Godavari Estuary, Andhra Pradesh, India for three different months (Nov.'95, Jan, 96, April '96) representing different ...
    • The role of salinity on the dynamics of the Arabian Sea mini warm pool 

      Nyadjro, E.S.; Subrahmanyam, B.; Murty, V.S.N.; Shriver, J.F. (American Geophysical Union, 2012)
      Warmer (more than 28 degrees C) sea surface temperature (SST) occurs in the South Eastern Arabian Sea (SEAS, 5 degrees N-13 degrees N, 65 degrees E-76 degrees during March-April, and is known as the Arabian Sea Mini Warm ...
    • Water and salt budget in the Azikode estuary during postmonsoon season 

      Revichandran, C.; Shyam, K.R.; Varma, P.U.; Pylee, A. (CSIR-NISCAIR, 1987)
      Computed values of flux showed that seaward Eulerian residual flow of water was the major factor influencing the salt and water budget in the Azikode Estuary. Depth integrated residual flow was seaward at all depths. ...