
The scientists at the US National Snow and Ice Data Center (NSIDC) at the University of Colorado, USA, have based their calculation on the satellite imagery received by it.
The Wilkins Ice Shelf is a broad plate of permanent floating ice on the southwest Antarctic Peninsula, about 1,600 kilometers south of South America.
In the past 50 years, the western Antarctic Peninsula has experienced the biggest temperature increase on Earth, rising by 0.5 degree Celsius per decade.
Satellite images, scientists say, indicate that the Wilkins began its collapse on February 28 and a large iceberg, 41 by 2.5 kilometers, fell away from the ice shelf’s southwestern front, triggering a runaway disintegration of 405 square kilometers of the shelf interior.
The edge of the shelf crumbled into the sky-blue pattern of exposed deep glacial ice that has become characteristic of climate-induced ice shelf break-ups such as the Larsen B in 2002. A narrow beam of intact ice, just 6 kilometers wide was protecting the remaining shelf from further breakup as of March 23, they said.
Scientists track ice shelves and study collapses carefully because some of them hold back glaciers, which if unleashed, can accelerate and raise sea level.


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