East Antarctica more at risk than thought to long-term thaw
PART OF EAST ANTARCTICA is more vulnerable than expected to a thaw that could trigger an unstoppable slide of ice into the ocean and raise world sea levels for thousands of years, a study showed on Sunday.
The Wilkes Basin in East Antarctica, stretching more than 1,000 km inland, has enough ice to raise sea levels by three to four metres if it were to melt, the report said.
The Wilkes is vulnerable to warming associated with climate change because it is held in place by a small rim of ice, resting on bedrock below sea level by the coast of the frozen continent. That ‘ice plug’ might melt away in coming centuries if ocean waters warm up.
“East Antarctica’s Wilkes Basin is like a bottle on a slant. Once uncorked, it empties out,” Matthias Mengel of the Potsdam Institute for Climate Impact Research, lead author of the study in the journal Nature Climate Change, said in a statement.
Co-author Anders Levermann, also at the Potsdam Institute, said the main finding was that the ice flow would be irreversible, if set in motion. He said there was still time to limit warming to levels to keep the ice plug in place.
Almost 200 governments have promised to work out an international deal by the end of 2015 to curb increasing emissions of man-made greenhouse gases that a United Nations panel says will cause more droughts, heatwaves, downpours and rising sea levels.
Worries about rising seas that could swamp low-lying areas from Shanghai to Florida focus most on ice in Greenland and West Antarctica, as well as far smaller amounts of ice in mountain ranges from the Himalayas to the Andes.
Sunday’s study is among the first to gauge risks in East Antarctica, the biggest wedge of the continent and usually considered stable. “I would not be surprised if this (basin) is more vulnerable than West Antarctica,” Levermann said.
The Big Thaw
Antarctica holds enough ice to raise sea levels by some 57 metres if it ever all melted. The study indicated that it could take 200 years or more to melt the ice plug if ocean temperatures rise. Once removed, it could take between 5,000 and 10,000 years for ice in the Wilkes Basin to empty as gravity pulled the ice seawards.
“It sounds plausible,” Tony Payne, a professor of glaciology at Bristol University who was not involved in the study, said of the findings. The region is not an immediate threat, he said, but “could contribute metres to sea level rise over thousands of years.”
The United Nations panel on climate change says it is at least 95 per cent probable that human activities such as burning fossil fuels, rather than natural swings in the climate, are the dominant cause of warming since the 1950s.
Sea levels are likely to rise by between 26 and 82 centimetres by the late 21st century, after a rise of 19 cm since 1900, it says. Antarctica is the biggest uncertainty.
The Wilkes Basin in East Antarctica, stretching more than 1,000 km inland, has enough ice to raise sea levels by three to four metres if it were to melt, the report said.
The Wilkes is vulnerable to warming associated with climate change because it is held in place by a small rim of ice, resting on bedrock below sea level by the coast of the frozen continent. That ‘ice plug’ might melt away in coming centuries if ocean waters warm up.
“East Antarctica’s Wilkes Basin is like a bottle on a slant. Once uncorked, it empties out,” Matthias Mengel of the Potsdam Institute for Climate Impact Research, lead author of the study in the journal Nature Climate Change, said in a statement.
Co-author Anders Levermann, also at the Potsdam Institute, said the main finding was that the ice flow would be irreversible, if set in motion. He said there was still time to limit warming to levels to keep the ice plug in place.
Almost 200 governments have promised to work out an international deal by the end of 2015 to curb increasing emissions of man-made greenhouse gases that a United Nations panel says will cause more droughts, heatwaves, downpours and rising sea levels.
Worries about rising seas that could swamp low-lying areas from Shanghai to Florida focus most on ice in Greenland and West Antarctica, as well as far smaller amounts of ice in mountain ranges from the Himalayas to the Andes.
Sunday’s study is among the first to gauge risks in East Antarctica, the biggest wedge of the continent and usually considered stable. “I would not be surprised if this (basin) is more vulnerable than West Antarctica,” Levermann said.
The Big Thaw
Antarctica holds enough ice to raise sea levels by some 57 metres if it ever all melted. The study indicated that it could take 200 years or more to melt the ice plug if ocean temperatures rise. Once removed, it could take between 5,000 and 10,000 years for ice in the Wilkes Basin to empty as gravity pulled the ice seawards.
“It sounds plausible,” Tony Payne, a professor of glaciology at Bristol University who was not involved in the study, said of the findings. The region is not an immediate threat, he said, but “could contribute metres to sea level rise over thousands of years.”
The United Nations panel on climate change says it is at least 95 per cent probable that human activities such as burning fossil fuels, rather than natural swings in the climate, are the dominant cause of warming since the 1950s.
Sea levels are likely to rise by between 26 and 82 centimetres by the late 21st century, after a rise of 19 cm since 1900, it says. Antarctica is the biggest uncertainty.
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