East Antarctica significantly more at risk of melting than earlier thought

Antarctica is pictured in this undated image courtesy of NASA. Scientists found that a high ridge in the East Antarctic Plateau contains pockets of trapped air that dipped as low as minus 136 Fahrenheit (minus 93 degrees Celsius) on August 10, 2010, researchers said at the American Geophysical Union meeting in San Francisco on December 9, 2013. REUTERS/NASA/Handout via Reuters (ANTARCTICA - Tags: ENVIRONMENT) FOR EDITORIAL USE ONLY. NOT FOR SALE FOR MARKETING OR ADVERTISING CAMPAIGNS. THIS IMAGE HAS BEEN SUPPLIED BY A THIRD PARTY. IT IS DISTRIBUTED, EXACTLY AS RECEIVED BY REUTERS, AS A SERVICE TO CLIENTS - RTX16BO3
Antarctica is pictured in this undated image. (NASA/Reuters)

Scientists have long contended that some of the most vulnerable ice sheets are in the West Antarctic. In 1998, Nature published an article warning that the West Antarctic Ice Sheet “poses the most immediate threat of a large sea-level rise, owing to its potential instability.”

The reports have only gotten worse. In 2012, another paper said that temperatures in the West Antarctic had risen dramatically more than scientists had earlier thought — 4.4 degrees since 1958. Then just last month, more bad news hit: The West Antarctic is shedding ice at a faster rate than ever, with six regional glaciers disgorging roughly as much ice as the entire Greenland ice sheet.

Now comes the news that the West Antarctic isn’t the only concern. In fact, it may not even be the biggest one.

In the much larger East Antarctica, where melting has the potential to raise sea level by 53 meters (174 feet), there’s a small ice volume called the Wilkes Basin. It carries significance well beyond its size. According to a study published this week in Nature Climate Change, if it melts, it would trigger an “irreversible discharge” of the entire basin, causing an unstoppable sea level rise of up to 4 meters. “East Antarctica may become a large contributor to future sea-level rise on timescales beyond a century,” the study says.

“East Antarctica’s Wilkes Basin is like a bottle on a slant,” lead author Matthias Mengel said. “Once uncorked, it empties out.”

The most jarring conclusion? Once the ice begins its flow out of the broken “ice cork,” there’s no stopping it.


The Wilkes Basin, which is shaded blue, is the largest region with topography below sea level in East Antarctica, the study says. (Courtesy of the Potsdam Institute for Climate Impact Research.)

“Until recently, only West Antarctica was considered unstable, but now we know that its 10 times bigger counterpart in the East might also be at risk,” explained Anders Levermann, another author on the study.

The findings come at a time when scientists from the United Nations to the National Climate Assessment are warning of the looming effects of global warming. “Climate change, once considered an issue for a distant future, has moved firmly into the present,” a recent National Climate Assessment says.

Last month, the U.N. also released a report saying that it is nearly too late to reverse global warming. “The window is shutting very rapidly on [limiting global warming to] the 2 degrees target,” Johan Rockstrom, director of the Stockholm Resilience Centre, told Reuters. “The debate is drifting to ‘maybe we can adapt to 2 degrees, maybe 3 or even 4.’”

Until now the East Antarctic has been considered the more stable of the two. “The East Antarctic ice sheet has long been considered to be stable even under a warmer climate, in contrast to its West Antarctic counterpart,” Mengel said in a statement. “We have now shown that this may not be true. … The future sea-level contribution of the East Antarctic ice sheet may be significantly higher than previously estimated.”

“It sounds plausible,” Tony Payne, a professor of glaciology at Bristol University, told Reuters. East Antarctica “could contribute meters to sea level rise over thousands of years,” he said.

Indeed, the process, though significant, appears to be slow. The study found that it may take as many as 200 years for the cork to melt. And after it goes, it will take another several thousand years for the basin to empty into the sea.

Still, with many of the world’s most populous cities — Mumbai, Tokyo, New York — near the ocean, every inch in sea rise counts.

“Once started, it becomes unstoppable,” Levermann said. “At the moment it’s still stable but if it melts then the ice plug alone will result in a global sea-level rise of between 5 and 8 centimeters, but the ice that it will release is going to cause 80 times that amount of sea-level rise.”

Terrence McCoy is a foreign affairs writer at the Washington Post. He served in the U.S. Peace Corps in Cambodia and studied international politics at Columbia University. Follow him on Twitter here.
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