Articles | Volume 17, issue 9
https://doi.org/10.5194/tc-17-3761-2023
https://doi.org/10.5194/tc-17-3761-2023
Research article
 | 
07 Sep 2023
Research article |  | 07 Sep 2023

The stability of present-day Antarctic grounding lines – Part 2: Onset of irreversible retreat of Amundsen Sea glaciers under current climate on centennial timescales cannot be excluded

Ronja Reese, Julius Garbe, Emily A. Hill, Benoît Urruty, Kaitlin A. Naughten, Olivier Gagliardini, Gaël Durand, Fabien Gillet-Chaulet, G. Hilmar Gudmundsson, David Chandler, Petra M. Langebroek, and Ricarda Winkelmann

Data sets

Data and code for publication "The stability of present-day Antarctic grounding lines - Part B" Ronja Reese, Julius Garbe, Emily Hill, Benoit Urruty, Kaitlin Naughten, Olivier Gagliardini, Gael Durand, Fabien Gillet-Chaulet, G. Hilmar Gudmundsson, David Chandler, Petra M. Langebroek, Ricarda Winkelmann, and other PISM authors https://doi.org/10.5281/zenodo.8101891

Model code and software

Data and code for publication "The stability of present-day Antarctic grounding lines - Part B" Ronja Reese, Julius Garbe, Emily Hill, Benoit Urruty, Kaitlin Naughten, Olivier Gagliardini, Gael Durand, Fabien Gillet-Chaulet, G. Hilmar Gudmundsson, David Chandler, Petra M. Langebroek, Ricarda Winkelmann, and other PISM authors https://doi.org/10.5281/zenodo.8101891

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Short summary
We use an ice sheet model to test where current climate conditions in Antarctica might lead. We find that present-day ocean and atmosphere conditions might commit an irreversible collapse of parts of West Antarctica which evolves over centuries to millennia. Importantly, this collapse is not irreversible yet.