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  2. The main features of the ocean currents include large anticyclonic flow in the Bay of Bengal surface waters during the northern hemisphere winter. This gyre decays into eddies in spring and then transitions into a weaker, cyclonic gyre by late summer.
    Author: James T. Potemra, Mark E. Luther, James J. O'Brien
    Publish Year: 1991
    agupubs.onlinelibrary.wiley.com/doi/abs/10.1029/91JC01045
    agupubs.onlinelibrary.wiley.com/doi/abs/10.1029/91JC01045
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