Rapid formation of an ice doline on Amery Ice Shelf, East Antarctica

• Main Authors: Warner, R, Fricker, H, Adusumilli, S, Arndt, P, Kingslake, J, Spergel, J
• Format: Conference Object
• Language: English
• Published: Copernicus GmbH 2022
• Subjects: Earth Sciences; Physical geography and environmental geoscience; Glaciology; East Antarctica; Amery; Amery Ice Shelf; Midwinter; New Lake; Antarc*; Antarctica; Ice Shelf; Ice Shelves
• Online Access: https://doi.org/10.5194/egusphere-egu21-14157; http://ecite.utas.edu.au/154120

Surface meltwater accumulating on Antarcticas floating ice shelves can drive fractures through to the ocean and potentially cause their collapse, leading to enhanced ice discharge from the continent. Surface melting in Antarctica is predicted to increase significantly during coming decades, but the implications for ice shelf stability are unknown. We are still learning how meltwater forms, flows and alters the surface, and that rapid water-driven changes are not limited to summer. The southern Amery Ice Shelf in East Antarctica already has an extensive surface meltwater system and provides us with an opportunity to study melt processes in detail. We present high-resolution satellite data (imagery, ICESat-2 altimetry and elevation models from WorldView stereo-photogrammetry) revealing an abrupt change extending across ~60 km 2 of the ice shelf surface in June 2019 (midwinter). We interpret this as drainage of an englacial lake through to the ocean below in less than three days. This left an uneven depression in the ice shelf surface, 11 km 2 in area and as much as 80 m deep, with a bed of fractured ice: an ice doline. The englacial lake had lain beneath the perennially ice-covered portion of a 20 km 2 meltwater lake. The reduced mass loading on the floating ice shelf after the drainage event resulted in flexure, with uplift of up to 36 m around the former lake. Applying an elastic flexural model to the uplift profiles suggests the loss of 0.75km 3 of water to the ocean. In summer 2020, we observed meltwater accumulating in a new lake basin created by the flexure. ICESat-2 observations profiled a new narrow meltwater channel (20m wide and 3m deep), rapidly incised inside the doline as meltwater spilled over from the new lake and started refilling the depression. This study demonstrates how high-resolution geodetic measurements from ICESat-2 and WorldView can explore critical fine-scale ice shelf processes. The insights gained will greatly improve our ability to model these processes, ultimately improving the ...