Articles | Volume 13, issue 4
https://doi.org/10.5194/tc-13-1349-2019
https://doi.org/10.5194/tc-13-1349-2019
Research article
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24 Apr 2019
Research article | Highlight paper |  | 24 Apr 2019

Uncertainty quantification of the multi-centennial response of the Antarctic ice sheet to climate change

Kevin Bulthuis, Maarten Arnst, Sainan Sun, and Frank Pattyn

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Cited articles

Adhikari, S., Ivins, E. R., Larour, E., Seroussi, H., Morlighem, M., and Nowicki, S.: Future Antarctic bed topography and its implications for ice sheet dynamics, Solid Earth, 5, 569–584, https://doi.org/10.5194/se-5-569-2014, 2014. a
An, M., Wiens, D. A., Zhao, Y., Feng, M., Nyblade, A., Kanao, M., Li, Y., Maggi, A., and Lévêque, J.-J.: Temperature, lithosphere-asthenosphere boundary, and heat flux beneath the Antarctic Plate inferred from seismic velocities, J. Geophys. Res.-Sol. Ea., 120, 8720–8742, https://doi.org/10.1002/2015jb011917, 2015. a, b
Arnst, M. and Ponthot, J.-P.: An overview of nonintrusive characterization, propagation, and sensitivity analysis of uncertainties in computational mechanics, Int. J. Uncertain. Quan., 4, 387–421, https://doi.org/10.1615/int.j.uncertaintyquantification.2014006990, 2014. a
Arthern, R. J. and Williams, C. R.: The sensitivity of West Antarctica to the submarine melting feedback, Geophys. Res. Lett., 44, 2352–2359, https://doi.org/10.1002/2017gl072514, 2017. a
Aschwanden, A., Fahnestock, M. A., and Truffer, M.: Complex Greenland outlet glacier flow captured, Nat. Commun., 7, 10524, https://doi.org/10.1038/ncomms10524, 2016. a
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Short summary
Using probabilistic methods, we quantify the uncertainty in the Antarctic ice-sheet response to climate change over the next millennium under the four RCP scenarios and parametric uncertainty. We find that the ice sheet is stable in RCP 2.6 regardless of parametric uncertainty, while West Antarctica undergoes disintegration in RCP 8.5 almost regardless of parametric uncertainty. We also show a high sensitivity of the ice-sheet response to uncertainty in sub-shelf melting and sliding conditions.
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