New Site of Potential Instability in West Antarctic Ice Sheet

Bottom Image: This radar image of bedrock elevation reveals the new sub-glacial

Bottom Image: This radar image of bedrock elevation reveals the new sub-glacial basin (purple and blue regions). The basin is divided into two components (A and B) and lies just inland of the West Antarctic Ice Sheet's grounding line (black line), where streams of ice flowing toward the Weddell Sea begin to float. Top Image: White box indicates location of bottom image. Pine Island Glacier (PIG) and Thwaites Glacier--two parts of the West Antarctic Ice Sheet previously studied by the U.S. and U.K. researchers--drain into the Amundsen Sea.

AUSTIN, Texas — Using ice-penetrating radar instruments flown on aircraft, a team of scientists from the U.S. and U.K. have uncovered a previously unknown sub-glacial basin nearly the size of New Jersey beneath the West Antarctic Ice Sheet (WAIS) near the Weddell Sea. The location, shape and texture of the mile-deep basin suggest that this region of the ice sheet is at a greater risk of collapse than previously thought.

Team members at The University of Texas at Austin compared data about the newly discovered basin to data they previously collected from other parts of the WAIS that also appear highly vulnerable, including Pine Island Glacier and Thwaites Glacier. Although the amount of ice stored in the new basin is less than the ice stored in previously studied areas, it might be closer to a tipping point.

"If we were to invent a set of conditions conducive to retreat of the West Antarctic Ice Sheet, this would be it," said Don Blankenship , senior research scientist at The University of Texas at Austin’s Institute for Geophysics and co-author on the new paper. "With its smooth bed that slopes steeply toward the interior, we could find no other region in West Antarctica more poised for change than this newly discovered basin at the head of the Filchner-Ronne Ice Shelf. The only saving grace is that losing the ice over this new basin would only raise sea level by a small percentage of the several meters that would result if the entire West Antarctic Ice Sheet destabilized."

The study’s co-authors also included Duncan Young , research scientist associate at the Institute for Geophysics.

The study, published this week , was carried out in a collaboration led by the University of Edinburgh with the British Antarctic Survey and the Universities of Aberdeen, Exeter and York, as well as The University of Texas at Austin.

"This is a significant discovery in a region of Antarctica that at present we know little about," said Professor Martin Siegert of the University of Edinburgh, who led the project. "The area is on the brink of change, but it is impossible to predict what the impact of this change might be without further work enabling better understanding of how the West Antarctic Ice Sheet behaves."

The seaward edge of the newly discovered basin lies just inland of the ice sheet’s grounding line, where streams of ice flowing toward the sea begin to float.

Two features of the basin, which is entirely below sea level, are particularly worrisome to scientists: First, like a cereal bowl, its edges slope down steeply. If the grounding line begins to retreat upstream, seawater will replace it and more ice will begin to float. The study’s authors predict that this positive feedback mechanism would sustain retreat of the ice sheet until eventually all of the ice filling the basin goes afloat. Second, the bed of the basin on which the ice rests is smooth. There are few big bumps, or "pinning points," to hold back sliding ice.

The newly discovered basin covers 20,000 square kilometers (7,700 square miles), nearly the size of New Jersey, and is well below sea level, nearly 2 kilometers (about 1.2 miles) deep in places.

In a related paper published simultaneously in the journal Nature , computer models reveal that the Weddell Sea region may experience warmer ocean conditions at the end of the 21st century, which could provide the trigger for ice sheet change.

 
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