Ice 'theft' between neighbouring glaciers in Antarctica. The discovery thanks to Copernicus
The research is partly funded by the Science for Society section of Esa's FutureEO programme and the results have been published in Cryosphere
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Key points
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Esa researchers, thanks to Copernicus Sentinel-1, have discovered that a glacier in Antarctica is rapidly stealing ice from nearby streams, 'at a rate never seen before'. Almost a 'theft' if it were not a natural occurrence, but considered extraordinary, especially in light of ongoing climate change.
'Until now, researchers believed that this process in Antarctica took hundreds or even thousands of years,' writes the European space agency Esa in a note, 'but these latest findings clearly show that this is not always the case'.
The Kholer East Glacier and the "ice theft"
.The research, funded in part by the Science for Society section of Esa's FutureEO programme, was published in The Cryosphere and explains that 'the fast-flowing Kohler East glacier in West Antarctica is taking ice from a slower-flowing neighbour'.
As part of this research, a team of scientists, led by the University of Leeds in the UK, examined high-resolution images from satellites such as Sentinel-1, together with other satellite data covering the period from 2005 to 2022, to understand the flow velocity of eight ice streams in the Pope-Smith-Kohler region.
The Kohler glacier, Esa reconstructs, as well as the Pope and Smith glaciers, are among the most rapidly changing glaciers in West Antarctica, with some shifting and thinning more rapidly than others. These glaciers are located upstream of the Dotson and Crosson ice shelves.

