0200 GMT December 14, 2018
At the end of the last ice age, warming temperatures caused ice masses in Antarctica to shrink. But, around 10,000 years ago, the West Antarctic Ice Sheet surprisingly rebounded, UPI wrote.
New research suggested the loss of mass allowed for crustal uplift. As the continent rose, the ice sheet began to self-stabilize.
Analysis of the phenomenon — detailed in the journal Nature —suggested such a reversal of fortune is unlikely to happen again.
Torsten Albrecht, researcher at the Potsdam Institute for Climate Impact Research, said, "Given the speed of current climate-change from burning fossil fuels, the mechanism we detected unfortunately does not work fast enough to save today's ice sheets from melting and causing seas to rise.”
Until now, scientists thought the retreat of the West Antarctic Ice Sheet was continuous. But new models showed the ice sheet's behavior was more complicated.
Albrecht said, "When I observed the re-growth in our numerical computer simulations of Western Antarctica, I first thought this might be a flaw — it looked so different from what you find in the text books.
"So I started figuring out the involved interactions between the ice, ocean and Earth and their typical time scales."
A radar survey of the ice sheet's ancient layers, led by Jonathan Kingslake and colleagues from Columbia University's Lamont-Doherty Earth Observatory, revealed cracks where scientists didn't expect them.
The cracks suggested the ice had been rapidly stretched and compressed, evidence of periods of retreat and regrowth.
When a team of scientists led by Reed Scherer from Northern Illinois University examined sediments from beneath the ancient ice layers, they arrived at a similar conclusion.
Researchers believe the rising peaks of the mountains beneath the West Antarctic Ice Sheet provided a ‘buttressing’ effect. This effect requires time to have an impact and encourage ice regrowth.
Scherer said, "What happened roughly 10,000 years ago might not dictate where we're going in our carbon dioxide-enhanced world, in which the oceans are rapidly warming in the Polar Regions.
"If the ice sheet were to dramatically retreat now, triggered by anthropogenic warming, the uplift process won't help regrow the ice sheet until long after coastal cities have felt the effects of sea level rise."