Near-surface circulation and kinetic energy in the tropical Indian Ocean derived from Lagrangian drifters

Trajectories of 412 satellite-tracked drifting buoys deployed in the tropic al Indian Ocean have been analyzed to document the surface circulation and kinetic energy field. Only drifters drogued at 15 m depth and having drag a rea ratio greater than 35 are used to estimate current velocities. Unlike i n earlier studies, the widening of the Equatorial Jet in the eastern equato rial Indian Ocean and the westward flow at the equator during July-August a re apparent in the present data set. The comparison of drifter data with th e seasonal mean dynamic topography (0/1000 db) shows that the surface circu lation pattern inferred from dynamic topography does not always represent t he surface currents in the Indian Ocean. Both compare well for the South Eq uatorial Current, the Equatorial Counter Current, and the southwestward cur rent along the Indonesian Islands; they differ in the Bay of Bengal during the southwest monsoon, but are similar during the northeast monsoon. Maps o f mean and eddy kinetic energy show maxima in the regions of western bounda ry currents and equatorial currents and minima in the Arabian Sea, the Bay of Bengal, and south of 20 degrees S.