Articles | Volume 14, issue 9
https://doi.org/10.5194/tc-14-3033-2020
https://doi.org/10.5194/tc-14-3033-2020
Research article
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17 Sep 2020
Research article | Highlight paper |  | 17 Sep 2020

ISMIP6 Antarctica: a multi-model ensemble of the Antarctic ice sheet evolution over the 21st century

Hélène Seroussi, Sophie Nowicki, Antony J. Payne, Heiko Goelzer, William H. Lipscomb, Ayako Abe-Ouchi, Cécile Agosta, Torsten Albrecht, Xylar Asay-Davis, Alice Barthel, Reinhard Calov, Richard Cullather, Christophe Dumas, Benjamin K. Galton-Fenzi, Rupert Gladstone, Nicholas R. Golledge, Jonathan M. Gregory, Ralf Greve, Tore Hattermann, Matthew J. Hoffman, Angelika Humbert, Philippe Huybrechts, Nicolas C. Jourdain, Thomas Kleiner, Eric Larour, Gunter R. Leguy, Daniel P. Lowry, Chistopher M. Little, Mathieu Morlighem, Frank Pattyn, Tyler Pelle, Stephen F. Price, Aurélien Quiquet, Ronja Reese, Nicole-Jeanne Schlegel, Andrew Shepherd, Erika Simon, Robin S. Smith, Fiammetta Straneo, Sainan Sun, Luke D. Trusel, Jonas Van Breedam, Roderik S. W. van de Wal, Ricarda Winkelmann, Chen Zhao, Tong Zhang, and Thomas Zwinger

Data sets

CMIP6 ESFG https://esgf-node.llnl.gov/search/cmip6/

Results of ISMIP6 Antarctica: a multi-model ensemble of the Antarctic ice sheet evolution over the 21st century Helene Seroussi, Sophie Nowicki, Anthony P. Payne, Heiko Goelzer, William L. Lipscomb, Ayako Abe Ouchi, … and Thomas Zwinger https://doi.org/10.5281/zenodo.3940766

Scripts for "ISMIP6 Antarctica: a multi-model ensemble of the Antarctic ice sheet evolution over the 21st century" Helene Seroussi, Sophie Nowicki, Anthony P. Payne, Heiko Goelzer, William L. Lipscomb, Ayako Abe Ouchi, … and Thomas Zwinger https://doi.org/10.5281/zenodo.3940768

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Short summary
The Antarctic ice sheet has been losing mass over at least the past 3 decades in response to changes in atmospheric and oceanic conditions. This study presents an ensemble of model simulations of the Antarctic evolution over the 2015–2100 period based on various ice sheet models, climate forcings and emission scenarios. Results suggest that the West Antarctic ice sheet will continue losing a large amount of ice, while the East Antarctic ice sheet could experience increased snow accumulation.