The Indian Ocean gyre is composed of two major currents : the South Equatorial Current, and the West Australian Current.
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As the current approaches Western Australia, it turns north, parallel to the western coast of Australia, and becomes the West Australian Current.
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In addition to the West Australian Current flowing on the Western Australian Coast, the Leeuwin Current and Southern Australian Countercurrent, also flow along this coast, with the former flowing in the opposite direction.
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The West Australian Current and Southern Australian Countercurrent, which are produced by the West Wind Drift on the southern Indian Ocean and at Tasmania, respectively, flow in the opposite direction, producing one of the most interesting oceanic current systems in the world.
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