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Crevasses at Store Glacier, a marine-terminating outlet glacier of the western Greenland Ice Sheet. Photo Credit: Tom Chudley (Durham University) |
A new study published this week in Nature Geoscience reveals that in response to climate change, the Greenland Ice Sheet is developing significantly more surface crevasses in key regions – a change that may accelerate ice loss and contribute to rising sea levels.
The research was led by Thomas Chudley, a research assistant professor at Durham University and former research associate at The Ohio State University’s Byrd Polar and Climate Research Center. The study analyzed high-resolution 3D surface maps and found that crevasses – wedge-shaped fractures in ice – had significantly increased in size and depth at the ice sheet’s fast-flowing edges over the entire Greenland Ice Sheet between 2016 and 2021.