The role of föhn winds in eastern Antarctic Peninsula rapid ice shelf collapse

• Published in: The Cryosphere
• Main Authors: Laffin, Matthew K., Zender, Charles S., van Wessem, Melchior, Marinsek, Sebastián
• Format: Article in Journal/Newspaper
• Language: English
• Published: Copernicus Publications 2022
• Subjects: article; Verlagsveröffentlichung; Antarctic; Antarctic Peninsula; Scar Inlet; The Antarctic; Antarc*; Ice Shelf; Ice Shelves; Sea ice; The Cryosphere
• Online Access: https://doi.org/10.5194/tc-16-1369-2022; https://noa.gwlb.de/receive/cop_mods_00060660; https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00060263/tc-16-1369-2022.pdf; https://tc.copernicus.org/articles/16/1369/2022/tc-16-1369-2022.pdf

Ice shelf collapse reduces buttressing and enables grounded glaciers to contribute more rapidly to sea-level rise in a warming climate. The abrupt collapses of the Larsen A (1995) and B (2002) ice shelves on the Antarctic Peninsula (AP) occurred, at least for Larsen B, when long-period ocean swells damaged the calving front and the ice shelf was inundated with melt lakes that led to large-scale hydrofracture cascades. During collapse, field and satellite observations indicate föhn winds were present on both ice shelves. Here we use a regional climate model and machine learning analyses to evaluate the contributory roles of föhn winds and associated melt events prior to and during the collapses for ice shelves on the AP. Föhn winds caused about 25 % ± 3 % of the total annual melt in just 9 d on Larsen A prior to and during collapse and were present during the Larsen B collapse, which helped form extensive melt lakes. At the same time, the off-coast wind direction created by föhn winds helped melt and physically push sea ice away from the ice shelf calving fronts that allowed long-period ocean swells to reach and damage the front, which has been theorized to have ultimately triggered collapse. Collapsed ice shelves experienced enhanced surface melt driven by föhn winds over a large spatial extent and near the calving front, whereas SCAR inlet and the Larsen C ice shelves are affected less by föhn-wind-induced melt and do not experience large-scale melt ponds. These results suggest SCAR inlet and the Larsen C ice shelves may be less likely to experience rapid collapse due to föhn-driven melt so long as surface temperatures and föhn occurrence remain within historical bounds.