Satellite altimetry analysis shows Bay of Bengal water parcels reach the southeastern Arabian Sea in 1.5-2 months, with 1.3x higher stirring along the western boundary during summer monsoons and a ~10% interannual increase in basin-scale geostrophic eddy kinetic energy.
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Influx of Bay of Bengal waters and stirring trends in the Arabian Sea based on satellite altimetry
Satellite altimetry analysis shows Bay of Bengal water parcels reach the southeastern Arabian Sea in 1.5-2 months, with 1.3x higher stirring along the western boundary during summer monsoons and a ~10% interannual increase in basin-scale geostrophic eddy kinetic energy.