
Winds and continental drift unlocked the Antarctic Circumpolar Current
New simulations show the Antarctic Circumpolar Current formed around 34 million years ago only after Australia moved north and strong westerlies blew through the Tasman Gateway, aided by a CO2 drop from ~1,000 to ~600 ppm and Antarctic isolation. Once fully developed, the ACC helped stabilize global climate by linking ocean basins and keeping warmer waters away from the ice sheets. Today, climate warming may push the current southward and slow it by about 20% by 2050, risking biodiversity and ice-sheet stability.













