Maximum strain rates over the Amundsen Sea Embayment. Maximum strain rates were calculated by deriving the first principal stress component from strain rates derived from the 2D Sentinel-1 velocity data over 2014-2019, where negative/postive maximum strain rates result in healing/enhancement of damage respectively.

The data set contains a georeferenced tif file corresponding the PIG and THW study areas.

Please check for more information:
Lhermitte et al. (2020) Damage accelerates ice shelf instability and mass loss in Amundsen Sea Embayment. PNAS, www.pnas.org/cgi/doi/10.1073/pnas.1912890117  