Rising temperatures will lead to a series of tipping points for Antarctica’s ice sheets, leading to practically irreversible melting, simulations suggest. Here, the Getz Ice Shelf in West Antarctica is shown.
Jeremy Harbeck/NASA
Rising temperatures will lead to a series of tipping points for Antarctica’s ice sheets, leading to practically irreversible melting, simulations suggest. Here, the Getz Ice Shelf in West Antarctica is shown.
Jeremy Harbeck/NASA