Now showing items 1-4 of 4

    • Contribution of mesoscale processes to nutrient budgets in the Arabian Sea 

      Resplandy, L.; Levy, M.; Madec, G.; Pous, S.; Aumont, O.; DileepKumar, M. (American Geophysical Union, 2011)
      We examine the impact of mesoscale dynamics on the seasonal cycle of primary production in the Arabian Sea with an eddy-resolving (1/12 degrees) bio-physical model. Comparison with observations indicates that the numerical ...
    • Controlling factors of the oxygen balance in the Arabian Sea's OMZ 

      Resplandy, L.; Levy, M.; Bopp, L.; Echevin, V.; Pous, S.; Sarma, V.V.S.S.; Kumar, M.D. (European Geosciences Union, 2012)
      The expansion of OMZs (oxygen minimum zones) due to climate change and their possible evolution and impacts on the ecosystems and the atmosphere are still debated, mostly because of the inability of global climate models ...
    • Oceanic mesoscale turbulence drives large biogeochemical interannual variability at middle and high latitudes 

      Levy, M.; Resplandy, L.; Lengaigne, M. (American Geophysical Union, 2014)
      Observed phytoplankton interannual variability has been commonly related to atmospheric variables and climate indices. Here we showed that such relation is highly hampered by internal variability associated with oceanic ...
    • Positive Indian ocean dipole events prevent anoxia off the west coast of India 

      Parvathi, V.; Suresh, I.; Lengaigne, M.; Ethe, C.; Vialard, J.; Levy, M.; Neetu, S.; Aumont, O.; Resplandy, L.; Naik, H.; Naqvi, S.W.A. (European Geosciences Union, 2017)
      The seasonal upwelling along the west coast of India (WCI) brings nutrient-rich, oxygen-poor subsurface waters to the continental shelf, favoring very low oxygen concentrations in the surface waters during late boreal ...