New maps collected under the floating tongue of Thwaites Glacier and further offshore reveal deep (> 1000 m) and wide (> 20,000 m) channels that guide warm ocean water under the ice, accelerating melt that eventually may lead to collapse. Thwaites, part of the West Antarctic Ice Sheet (WAIS) is the size of Great Britain, and responsible for 55% of the yearly mass loss from the WAIS since 1992. These channels exert a fundamental control on warm water routing, on the stability of the glacier, and on the rest of the WAIS. A collapse of this single glacier would eventually lead to more than 65 cm of global sea level rise.
https://tc.copernicus.org/articles/14/2869/2020/
https://tc.copernicus.org/articles/14/2883/2020/
Compiled by Amy Imdieke
Dear Friends of the Cryosphere Pavilion and Cryosphere Capsule Readers! We are happy to announce…
Nature Communications, 21 July 2026 Rising sea levels driven by ocean warming and ice sheet…
Journal of Geophysical Research: Oceans, 26 June 2026 East Antarctica has long been considered less…
Geophysical Research Letters, 9 July 2026 Antarctic Bottom Water (AABW) is the cold, dense water…
PNAS, 20 July 2026 After several years in the early 2020s when Arctic winter sea…
Nature Communications, 16 July 2026 Temporarily exceeding global warming targets increases the risk of long-lasting…