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A Historical Primer on WAIS Collapse, Pt. 2: Recent History August 4, 2014

Posted by Will Thomas in Commentary Track.
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This post continues my post from May, which was written to lend some historical background to the recently released news that the large marine glaciers emptying into the Amundsen Sea seem to have passed a point of no return, and will continue to collapse until they are gone, whereupon the rest of the West Antarctic Ice Sheeet (WAIS) may well follow. Total sea level rises should be 2–3m within a few centuries, though the exact timescales could be faster or slower.  The above video from the NASA Jet Propulsion Laboratory features Eric Rignot, one of the leaders of the two teams who have reached this conclusion.  (The other team is led by the University of Washington’s Ian Joughin, on whom more below.)

The history in Pt. 1 concluded circa 1980, when geologist John Mercer (1922-1987) connected the prospect of WAIS collapsing to global warming.  Shortly thereafter the University of Maine’s Terry Hughes—who had previously linked future WAIS collapse to an ongoing global retreat from the Last Glacial Maximum (18,000 years ago)—identified (pdf) the Amundsen Sea glaciers as WAIS’s “weak underbelly,” which would be the “mechanism for disintegration of [WAIS] during a proposed Super Interglaciation triggered by CO2-induced climatic warming.” This post addresses what occurred in the intervening decades to convince the glaciological community of the assertion.

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