Sub-glacial basin seen as potential trigger for ice shelf collapse
A sub-glacial basin beneath the West Antarctic Ice Sheet, near the Weddell Sea, could be a weak spot leading to potential collapse. PHOTO BY BOB BERWYN
The bottom image shows a 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. The top image shows a white box indicating the location of the bottom image. Pine Island Glacier and Thwaites Glacier — two parts of the West Antarctic Ice Sheet previously studied by the US and UK researchers — drain into the Amundsen Sea.
Credit: University of Edinburgh/British Antarctic Survey
By Summit Voice
SUMMIT COUNTY — Ice-penetrating radar has hlep scientists discover a mile-deep sub-glacial basin beneath the West Antarctic Ice Sheet near the Weddell Sea. The location, shape and texture of the basin — about the size of New Jersey — suggest that this region of the ice sheet is at a greater risk of collapse than previously thought.
“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 research team members at The University of Texas at Austin compared data from the newly discovered basin to data they previously collected from other parts of the West Antarctic Ice Sheet 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.
“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.” (more…)
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