New research on a relatively unmonitored part of Antarctica shows that the ice in the area has been melting at a faster pace —and for longer— than previously thought. The study, which appears in the journal Geophysical Research Letters, provides insight on the implications of ice loss in Antarctica for sea level rise (for a brief compilation on the topic, check this article).
Satellite reviews of West Antarctica over the past two decades show the rapid increase of ice-loss. The ice shelves —blocks of floating ice that flow from Antarctica’s glaciers to the ocean— are shrinking and disappearing, this leaves way for warm waters to gnaw at the glaciers’ grounding line, which separates land-bound ice from the floating ice. As a consequence, the grounding line in West Antarctica’s glaciers has started to receed and expose thicker, older ice; thus increasing the flow of the glaciers. In some cases, this acceleration in flow has reached the point of no-return.
Put in perspective, if all glaciers in West Antarctica were to melt, sea level rise would be of 10 to 13 feet. Read the full article from Seeker below:
OVERLOOKED AREA OF ANTARCTICA SEES MAJOR ICE LOSS
A relatively little studied part of West Antarctica has seen considerable ice loss over a longer period of time than previously thought.
Over the past few years, the evidence has piled up that glaciers in parts of Antarctica have been melting and retreating at an increasingly worrying — and potentially unstoppable — pace.
Now, new research shows that glaciers in a region of West Antarctica that has received relatively little attention to date have lost a considerable amount of ice. And that ice melt and retreat has been going on for decades, longer than previously thought.
The findings, detailed in the journal Geophysical Research Letters, have implications for understanding the potential sea level rise that the vast icy expanse of Antarctica could unleash as the Earth’s temperature continues to rise.
“I think this study just underscores that West Antarctica, in general, is not only exceptionally vulnerable to retreat triggered by ocean melting at the coastline, but that it is happening now and it is showing no sign of slowing down,” study co-author Robert Bingham of the University of Edinburgh said in an email. “This whole process is pretty pervasive.”
West Antarctica Ice Loss
Since satellites first began looking down on Antarctica in the 1990s, polar scientists have noticed rapid changes in the ice of West Antarctica, particularly along its coastlines. It is here that the massive glaciers — essentially rivers of ice — that flow from the continent’s interior meet the sea and the ice begins to float.
The floating sections, known as ice shelves, help regulate the flow of the glaciers behind them. As those ice shelves shrink or collapse, the flow of the glaciers speeds up, increasing the amount of previously land-bound ice that is added to the world’s oceans, like ice cubes to a glass of water.
Warm ocean water is circulating under these ice shelves, eating away at them and causing them to thin, as well as pushing back the grounding line, or the point where land-bound ice begins to float. As the grounding line retreats, it exposes thicker and thicker portions of the glacier, increasing its flow.
Several major ice shelves have collapsed in the last two decades, and the speeds of several crucial glaciers, such as Pine Island Glacier, have accelerated. Recent studies suggest some have even reached a point of no return.
All told, the West Antarctic Ice Sheet contains enough ice to add 10 to 13 feet to global sea level rise were it all to melt; even an incomplete melt would imperial low-lying coastal areasaround the planet. One sector, the Amundsen Sea Embayment, contains several of the most worrisome glaciers. It alone currently accounts for about 10 percent of sea level rise.
But close behind it is a neighboring area, called the Bellingshausen Sea or the South Antarctica Peninsula. It accounts for about one third of the ice loss from the entire West Antarctic Ice Sheet (the Amundsen accounts for nearly half), and a study last year showed its glaciers have sped up considerably since 2009. But it has been relatively little studied, especially compared to the more attention-grabbing parts of the Amundsen.
During a 2009-2010 field mission, Bingham looked to shed more light on the region by scanning the ground below one of the fastest-moving Bellingshausen glaciers, the Ferrigno Ice Stream. He found a huge canyon underneath that is likely funneling warm ocean water under the ice.
“This only served to highlight to me that there is so much about the Bellingshausen Sea sector of West Antarctica that has gone unmonitored while most of the world’s eyes (glaciologically speaking) were looking beyond to Pine Island Glacier,” Bingham said.
To get a better picture of the overall ice loss in the area, Bingham and his Ph.D. student Frazer Christie, analyzed hundreds of satellite images of the area going back to 1975 and tracked the position of the grounding line along 1,240 miles of coast.
They found that 65 percent of the coastline had seen grounding line retreat since 1990, while only 7 percent had seen an advance. The total amount of ice lost over the last 40 years is about 390 square miles, an area about the size of Dallas.
The results “show that this whole coastline has been in a state of retreat since records began in the early 1970s,” Bingham said. That contrasts with previous thinking that only certain glaciers, like the Ferrigno Ice Stream, were seeing significant ice loss while the rest were fairly stable.
“The study illustrates that Antarctica is not immune to changes and that some of what we are seeing today started decades ago,” Eric Rignot, a NASA glaciologist who was not involved with the work, said in an email.
One notable oddity was the Venable Ice Shelf, which has thinned, but hasn’t retreated much. The researchers think it is pinned to a ridge on the seafloor that is keeping it stable for now. Scientists think the same was true of Pine Island Glacier — for a while.
Exactly what the pervasive ice loss in the Bellingshausen Sea area means for future global sea level rise isn’t entirely clear, in part because of the paucity of data from the area. Bingham says that researchers need a better idea of the topography underlying the ice so they can better model how it will change in the future.
“The Bellingshausen Sea region of West Antarctica stands as one of the least surveyed regions of ice and ocean on the planet,” he said.
Also needed is a clearer picture of ocean circulation there and in the entire West Antarctic region.
“The Antarctic Peninsula certainly does not receive as much attention as it should,” Rignot said. “I would recommend more work in this area, which is illustrative of what will happen farther south as climate gets warmer.”