Antarctic ice melting faster than expected
Warmer air, less frigid water and gravity may combine to make parts of Antarctica's western ice sheet melt far faster than scientists had thought. Sea levels could rise much more than expected. It could happen by the end of the century. This is according to a study.
New physics-based computer simulations forecast dramatic increases in melting. The increases come in the vulnerable western edge of the continent. In a worst-case scenario, that could raise sea level in 2100 by 18 to 34 inches more than an international panel of climate scientists predicted. They made that prediction just three years ago.
And even if the countries of the world control heat-trapping gases at the moderate levels they pledged last year, it would still mean three to 12 inches higher seas than have been forecast. This is according to a study. It was published March 30 in the journal Nature.
By the year 2500, in the worst-case scenario, the simulations predict seas 42 feet higher. The increase would come purely from Antarctic melt.
"You're remapping the way the planet looks from space with those numbers," said study lead author Robert DeConto. He is a climate scientist at the University of Massachusetts.
This is all because Antarctica is one of the biggest wild cards when scientists try to assess the effects of man-made climate change. Scientists were caught by surprise when the western portion of the continent started showing signs of rapid ice loss in the last 10 years or so.
The United Nations' Intergovernmental Panel on Climate Change has not forecast much sea level rise from Antarctica. Its last report predicted just seven inches by 2100. For this century, the panel saw water expanding from heat, glacier melt and Greenland ice sheet loss as the bigger factors.
Instead of 7 inches, DeConto's simulations forecast dramatically higher levels. His estimates from Antarctica's melt alone could be 2 to 3 feet. That is the worst-case scenario. The estimate is 10 to 19 inches if greenhouse gas emissions are moderately controlled. And if the world cracks down more dramatically on heat-trapping gases, Antarctica would essentially not add anything to sea level rise, the study said.
Those figures are just worldwide averages. In many places on the East Coast, like Boston, it could be 25 percent more. That's because of geological conditions, DeConto said.
"North America has a lot to fear from ice loss from West Antarctica." That is where it all begins, DeConto said.
While other studies have looked at the effect of warming from water below ice sheets and the air that melts from above, DeConto adds in the effect of pooling water and giant ice cliffs. Those ice cliffs, which can be dozens and even hundreds of feet high, can then collapse from the sheer weight of ice. That hastens glacier and ice sheet retreat, he said.
Ted Scambos at the University of Colorado, who wasn't part of the new study, said it was plausible and used "a few simple yet under-appreciated factors regarding ice retreat."
Carnegie Institute climate scientist Chris Field said the study drives home the difference the world can make by controlling its greenhouse gas emissions. It's the difference between rising seas that can be managed and conditions that are "dangerously risky," he said.
CRITICAL THINKING QUESTION
Why is Antarctica “one of the biggest wildcards?”
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