Editing Agulhas Current (section)

===Retroflection===
In the southeast [[Atlantic Ocean]] the current [[retroflect]]s (turns back on itself) in the [[Agulhas Retroflection]] due to shear interactions with the strong [[Antarctic Circumpolar Current]], also known as the "[[West Wind Drift]]" despite referring to the ocean current rather than to the surface winds.  This water becomes the Agulhas Return Current, rejoining the [[Indian Ocean Gyre]]. It is estimated that up to 85 Sv (Sv) of the net transport is returned to the [[Indian Ocean]] through the retroflection.  The remaining water is transported into the [[South Atlantic Gyre]] in the Agulhas Leakage.  Along with direct branch currents, this leakage takes place in surface water filaments, and Agulhas Eddies.