Fresh understanding of West Antarctica has revealed how the region's ice sheet could become unstable in a warming world.
Scientists studying the region's landscape have determined how it reacted to a period of warming after the coldest point of the most recent Ice Age, some 21,000 years ago.
As the Earth warmed, the West Antarctic Ice Sheet reached a tipping point after which it thinned relatively quickly, losing 400m of thickness in 3,000 years, researchers found. This caused sea levels around the world to increase by up to two metres.