NASA scientists have discovered a gigantic cavity, almost 300 metres tall, growing at the bottom of the Thwaites Glacier in West Antarctica, indicating rapid decay of the ice sheet and acceleration in global sea levels due to climate change.
The findings, published in the journal Science Advances, highlight the need for detailed observations of Antarctic glaciers’ undersides in calculating how fast sea levels will rise in response to warming.
Researchers expected to find some gaps between ice and bedrock at Thwaites’ bottom where ocean water could flow in and melt the glacier from below, NASA said in a statement.
“Thanks to a new generation of satellites, we can finally see the detail,” said Rignot, who is also associated with NASA’s Jet Propulsion Laboratory (JPL).
The cavity was revealed by ice-penetrating radar in NASA’s Operation IceBridge, an airborne campaign beginning in 2010 that studies connections between the polar regions and the global climate.
The researchers also used data from a constellation of Italian and German space-borne synthetic aperture radars.
These very high-resolution data can be processed by a technique called radar interferometry to reveal how the ground surface below has moved between images.
“(The size of) a cavity under a glacier plays an important role in melting. As more heat and water get under the glacier, it melts faster,” said Pietro Milillo of JPL.
Thwaites Glacier is currently responsible for about four per cent of global sea level rise, researchers said.
It holds enough ice to raise the world ocean a little over 65 centimeters and backstops neighbouring glaciers that would raise sea levels an additional 2.4 metres if all the ice were lost, they said.
“We are discovering different mechanisms of retreat,” Millilo said.
Different processes at various parts of the 160-kilometer-long front of the glacier are putting the rates of grounding-line retreat and of ice loss out of sync, NASA said.
The huge cavity is under the main trunk of the glacier on its western side — the side farther from the West Antarctic Peninsula.
In this region, as the tide rises and falls, the grounding line retreats and advances across a zone of about three to five kilometers.
The glacier has been coming unstuck from a ridge in the bedrock at a steady rate of about 0.6 to 0.8 kilometers a year since 1992.