Supporting data for the paper of this title, published in Geophysical Research Letters https://agupubs.onlinelibrary.wiley.com/doi/abs/10.1029/2021GL094513. Please cite as:
Golledge NR, Clark PU, He F, Dutton A, Turney CS, Fogwill CJ, Naish TR, Levy RH, McKay RM, Lowry DP, Bertler NA, Dunbar, GB and Carlson, AE. Retreat of the Antarctic Ice Sheet during the Last Interglaciation and implications for future change. Geophysical Research Letters. 2021 Sep 16;48(17):e2021GL094513.
There are two files, for Termination 1 ('T1') and Termination 2 ('T2').
They contain spatial fields for ice thickness, ice surface elevation, bedrock elevation, surface and basal velocity, and mask.
The T1 outputs are every 500 years, whereas the T2 outputs are every 100 years.
The spatial resolution of both is 20 km.
Sea-level-equivalent mass loss can be calculated from these outputs, but is also provided here in a text file for convenience.
