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Greenland ice sheet cracking open quicker than before, say scientists

FILE PHOTO: Icebergs are seen at the Disko Bay close to Ilulissat, Greenland, September 14, 2021.   REUTERS/Hannibal Hanschke/File Photo
FILE PHOTO: Icebergs are seen at the Disko Bay close to Ilulissat, Greenland, September 14, 2021. REUTERS/Hannibal Hanschke/File Photo
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The world's second largest body of ice - the Greenland Ice Sheet - is cracking open quicker than previously,scientists have warned.


Using three-dimensional maps of its surface, researchers have found crevasses have got significantly wider and deeper at the sheet's fast-flowing edges between 2016 and 2021.


The study, published in the journal Nature Gioscience, will be used to improve models about the future behaviour of the Greenland Ice Sheet.


The loss of ice on Greenland has been behind a sea level rise of around 14 millimetres since 1992, scientists have said.


If the entire Greenland Ice Sheet were to melt, sea levels could rise by seven metres, they said.


Study lead author Dr Tom Chudley, of Durham University's Geography Department, said: "In a warming world, we would expect to see more crevasses forming.


FILE PHOTO: A view of Pituffik Space Base (formerly Thule Air Base) in Greenland, October 4, 2023.   Ritzau Scanpix/Thomas Traasdahl via REUTERS
FILE PHOTO: A view of Pituffik Space Base (formerly Thule Air Base) in Greenland, October 4, 2023. Ritzau Scanpix/Thomas Traasdahl via REUTERS


"This is because glaciers are accelerating in response to warmer ocean temperatures, and because melt water filling crevasses can force fractures deeper into the ice.


"However, until now we haven't had the data to show where and how fast this is happening across the entirety of the Greenland Ice Sheet.


"For the first time, we are able to see significant increases in the size and depth of crevasses at fast-flowing glaciers at the edges of the Greenland Ice Sheet, on timescales of five years and less.


"With this dataset we can see that it's not just that crevasse fields are extending into the ice sheet, as previously observed - instead,change is dominated by existing crevasse fields getting larger and deeper." —PA Media/dpa


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