According to two new studies, the collapse of much of the West Antarctic Ice Sheet may now be irreversible. That could ultimately mean 10 feet of sea level rise.
If you truly understand global warming, then you know it’s all about the ice. That’s what matters. Planet Earth has not always had great ice sheets at the poles, of the sort that currently exist atop Greenland and Antarctica. In other periods, much of that water has instead been in liquid form, in the oceans—and the oceans have been much higher.
How much? According to the National Academy of Sciences, the globe’s great ice sheets contain enough frozen water to raise sea levels worldwide by more than 60 meters. That’s about 200 feet. And it makes all the sea level rise that we’ve seen so far due to global warming appear piddly and insignificant.
That’s why scientists have long feared a day like this would come. Two new scientific papers, in the journals Science and Geophysical Research Letters, report that major glaciers that are part of the West Antarctic Ice Sheet appear to have become irrevocably destabilized. The whole process may still play out on the scale of centuries, but due to the particular dynamics of this ice sheet, the collapse of these major glaciers now “appears unstoppable,” according to NASA (whose researchers are behind one of the two studies).
The first study, by researchers at NASA and the University of California-Irvine, uses satellite radar to examine an array of large glaciers along the Amundsen Sea in West Antarctica, which collectively contain the equivalent of four feet of sea level rise. The result is the documentation of a “continuous and rapid retreat”—for instance, the Smith and Kohler glaciers have retreated 35 kilometers since 1992—and the researchers say that there is “no [major] obstacle that would prevent the glaciers from further retreat.” In the NASA press release, the researchers are still more vocal, with one of them noting that these glaciers “have passed the point of no return.”
The other group of researchers, based at the University of Washington, reach similar conclusions with their paper in Science. But they do so by using a computer model to study one of these glaciers in particular: The Thwaites Glacier, pictured above, which contains about two feet of sea level rise and is retreating rapidly. “The simulations indicate that early-stage collapse has begun,” notes their paper. What’s more, the Thwaites Glacier is a “linchpin” for the rest of the West Antarctic Ice Sheet; its rapid collapse would “probably spill over to adjacent catchments, undermining much of West Antarctica.” And considering that the entire West Antarctic Ice Sheet contains enough water to raise sea levels by 10 to 13 feet, that’s a really big deal.
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