Like a hot beverage melts ice cubes, scientists have determined that warm ocean currents are thinning Antarctic ice.
When it comes to melting ice shelves in Antarctica, the danger comes from below, new research suggests.
By discovering the anatomy of ice loss across this chilly expanse, research may be able to forecast how the continent will melt in the future — and also how much global seas may rise.
Team member David Vaughan, a scientist at the European Union initiative ice2sea, said this study "shows the key to predicting how the ice sheet will change in the future is in understanding the oceans."
Scientists have long known that the wide platforms of ice extending from the southernmost continent have been shrinking away. But what's behind the melting hasn't been clear — whether warm ocean currents or surface winds have a bigger impact on the ice.
Now, a new satellite survey of Antarctica places the blame largely on the water. "In most places in Antarctica, we can't explain the ice-shelf thinning through melting of snow at the surface," said study team member Hamish Pritchard of the British Antarctic Survey in a statement. "So it has to be driven by warm ocean currents melting them from below." [Images: Tracking a Retreating Glacier]
The team's results represent the culmination of a massive international effort to observe the loss of Antarctic ice from the skies. Using NASA's ICESat satellite, the researchers closely monitored how the thickness of West and East Antarctica's ice changed over time. In some cases, Pritchard said, shelves thinned by as much as several meters each year. And the pattern of that melting, he added, suggested that at least 20 out of 54 observed platforms of ice across the continent were being melted largely by the oceans below, much like a warm drink consuming ice cubes.