A chunk of floating ice that weighs more than a trillion metric tons broke away from the Antarctic Peninsula, producing one of the largest icebergs ever recorded and providing a glimpse of how the Antarctic ice sheet might ultimately start to fall apart.
A crack more than 120 miles long had developed over several years in a floating ice shelf called Larsen C, and scientists who have been monitoring it confirmed on Wednesday that the huge iceberg had finally broken free.
There is no scientific consensus over whether global warming is to blame. But the landscape of the Antarctic Peninsula has been fundamentally changed, according to Project Midas, a research team from Swansea University and Aberystwyth University in Britain that had been monitoring the rift since 2014.
全球变暖是否是这次断裂的罪魁祸首，目前科学上尚无共识。但来自英国斯旺西大学(Swansea University)和阿伯斯威斯特大学(Aberystwyth University)的迈达斯计划(Project Midas)研究小组说，南极半岛的形状已经彻底改变，该小组自2014年起，一直在监测这条裂缝。
“The remaining shelf will be at its smallest ever known size,” said Adrian Luckman, a lead researcher for Project Midas. “This is a big change. Maps will need to be redrawn.”
Larsen C, like two smaller ice shelves that collapsed before it, was holding back relatively little land ice, and it is not expected to contribute much to the rise of the sea. But in other parts of Antarctica, similar shelves are holding back enormous amounts of ice, and scientists fear that their future collapse could dump enough ice into the ocean to raise the sea level by many feet. How fast this could happen is unclear.
In the late 20th century, the Antarctic Peninsula, which juts out from the main body of Antarctica and points toward South America, was one of the fastest-warming places in the world. That warming had slowed or perhaps reversed slightly in the 21st century, but scientists believe the ice is still catching up to the higher temperatures.
Some climate scientists believe the warming in the region was at least in part a consequence of human-caused climate change, while others have disputed that, seeing a large role for natural variability — and noting that icebergs have been breaking away from ice shelves for many millions of years. But the two camps agree that the breakup of ice shelves in the peninsula region may be a preview of what is in store for the main part of Antarctica as the world continues heating up as a result of human activity.
“While it might not be caused by global warming, it’s at least a natural laboratory to study how breakups will occur at other ice shelves to improve the theoretical basis for our projections of future sea level rise,” said Thomas P. Wagner, who leads NASA’s efforts to study the polar regions.
在美国宇航局领导极地研究项目的托马斯·P·瓦格纳(Thomas P. Wagner)说：“虽然这可能不是全球变暖造成的，但它至少为研究其他冰架将如何崩解提供了一个自然实验室，有助于改进我们预测未来海平面上升的理论基础。”
In frigid regions, ice shelves form as the long rivers of ice called glaciers flow from land into the sea. The result is a bit like a clog in a drain pipe, slowing the flow of the glaciers feeding them. When an ice shelf collapses, the glaciers behind it can accelerate, as though the drain pipe had suddenly cleared.
At the remaining part of Larsen C, the edge is now much closer to a line that scientists call the compressive arch, which is critical for structural support. If the front retreats past that line, the northernmost part of the shelf could collapse within months.
“At that point in time, the glaciers will react,” said Eric Rignot, a climate scientist at the University of California, Irvine, who has done extensive research on polar ice. “If the ice shelf breaks apart, it will remove a buttressing force on the glaciers that flow into it. The glaciers will feel less resistance to flow, effectively removing a cork in front of them.”
Scientists also fear that two crucial anchor points will be lost.
According to Dr. Rignot, the stability of the whole ice shelf is threatened, as the shelf front thins.
“You have these two anchors on the side of Larsen C that play a critical role in holding the ice shelf where it is,” he said. “If the shelf is getting thinner, it will be more breakable, and it will lose contact with the ice rises.”
Ice rises are islands that are overridden by the ice shelf, allowing them to shoulder more of the weight of the shelf. Scientists have yet to determine the extent of thinning around the Bawden and Gipps ice rises, though Dr. Rignot noted that the Bawden ice rise was more vulnerable.
“We’re not even sure how it’s hanging on there,” he said. “But if you take away Bawden, the whole shelf will feel it.”
The Antarctic Peninsula may be a canary in a coal mine.
The collapse of the peninsula’s ice shelves can be interpreted as fulfilling a prophecy made in 1978 by a renowned geologist named John H. Mercer of Ohio State University. In a classic paper, Dr. Mercer warned that the western part of Antarctica was so vulnerable to human-induced climate warming as to pose a “threat of disaster” from rising seas.
南极半岛冰架的崩解可以被解释为俄亥俄州立大学著名地质学家约翰·H·默瑟(John H. Mercer)1978年所做预言的兑现。默瑟在一篇经典论文中警告说，南极西部对人类造成的气候变暖如此之脆弱，以至于该地区构成对海平面上升所致“灾难的威胁”。
He said that humanity would know the calamity had begun when ice shelves started breaking up along the peninsula, with the breakups moving progressively southward.
The Larsen A ice shelf broke up over several years starting in 1995; the Larsen B underwent a dramatic collapse in 2002; and now, scientists fear, the calving of the giant iceberg could be the first stage in the breakup of Larsen C.
“As climate warming progresses farther south,” Dr. Rignot said, “it will affect larger and larger ice shelves, holding back bigger and bigger glaciers, so that their collapse will contribute more to sea-level rise.”