Journal of Glaciology (Dec 2020)

Antarctic ice sheet response to sudden and sustained ice-shelf collapse (ABUMIP)

  • Sainan Sun,
  • Frank Pattyn,
  • Erika G. Simon,
  • Torsten Albrecht,
  • Stephen Cornford,
  • Reinhard Calov,
  • Christophe Dumas,
  • Fabien Gillet-Chaulet,
  • Heiko Goelzer,
  • Nicholas R. Golledge,
  • Ralf Greve,
  • Matthew J. Hoffman,
  • Angelika Humbert,
  • Elise Kazmierczak,
  • Thomas Kleiner,
  • Gunter R. Leguy,
  • William H. Lipscomb,
  • Daniel Martin,
  • Mathieu Morlighem,
  • Sophie Nowicki,
  • David Pollard,
  • Stephen Price,
  • Aurélien Quiquet,
  • Hélène Seroussi,
  • Tanja Schlemm,
  • Johannes Sutter,
  • Roderik S. W. van de Wal,
  • Ricarda Winkelmann,
  • Tong Zhang

DOI
https://doi.org/10.1017/jog.2020.67
Journal volume & issue
Vol. 66
pp. 891 – 904

Abstract

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Antarctica's ice shelves modulate the grounded ice flow, and weakening of ice shelves due to climate forcing will decrease their ‘buttressing’ effect, causing a response in the grounded ice. While the processes governing ice-shelf weakening are complex, uncertainties in the response of the grounded ice sheet are also difficult to assess. The Antarctic BUttressing Model Intercomparison Project (ABUMIP) compares ice-sheet model responses to decrease in buttressing by investigating the ‘end-member’ scenario of total and sustained loss of ice shelves. Although unrealistic, this scenario enables gauging the sensitivity of an ensemble of 15 ice-sheet models to a total loss of buttressing, hence exhibiting the full potential of marine ice-sheet instability. All models predict that this scenario leads to multi-metre (1–12 m) sea-level rise over 500 years from present day. West Antarctic ice sheet collapse alone leads to a 1.91–5.08 m sea-level rise due to the marine ice-sheet instability. Mass loss rates are a strong function of the sliding/friction law, with plastic laws cause a further destabilization of the Aurora and Wilkes Subglacial Basins, East Antarctica. Improvements to marine ice-sheet models have greatly reduced variability between modelled ice-sheet responses to extreme ice-shelf loss, e.g. compared to the SeaRISE assessments.

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