EGU24-16820, updated on 11 Mar 2024
https://doi.org/10.5194/egusphere-egu24-16820
EGU General Assembly 2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.

Building probabilistic projections of the Antarctic contribution to global sea level rise using a random forests emulato

Fiona Turner1, Jonathan Rougier2, Tamsin Edwards1, Violaine Coulon3, and Ann Kristin Klose4,5
Fiona Turner et al.
  • 1King's College London, Department of Geography, United Kingdom of Great Britain – England, Scotland, Wales (fiona.turner@kcl.ac.uk)
  • 2School of Mathematics, University of Bristol, Bristol, UK
  • 3Université libre de Bruxelles (ULB), Laboratoire de Glaciologie, Brussels, Belgium
  • 4Potsdam Institute for Climate Impact Research (PIK), Potsdam, Germany
  • 5Department of Physics and Astronomy, University of Potsdam, Potsdam, Germany

In order to predict future global sea level rise, it is key for us to have better understanding of the changes in the cryosphere, as is being done in the PROTECT project (https://protect-slr.eu). Large uncertainties exist around how these changes will present over the coming centuries, with the Antarctic ice sheet being the most uncertain component with regards to predicted mass changes. It is therefore necessary to turn to statistical techniques to create more robust predictions.

Here, we present results from a random forests emulator simultaneously trained on two ice sheet models, Kori and PISM, forced by four global climate models. We emulate the relationship between inputs, namely climate change and ice sheet model settings, and an output, sea level contribution. The use of random forests allows us to improve on previous Gaussian Process emulators (Edwards et al., 2021) in speed and the treatment of factor inputs. We also transform the multi-centennial output in order to allow us to model the whole time series, rather than each year individually. The emulator allows us to interpolate (and extrapolate slightly) in order to build probabilistic projections of sea level contribution to 2300 that include climate and ice sheet modelling uncertainties under all five Shared Socioeconomic Pathways (SSPs), despite only two being used in the ensemble of simulations.

References

Edwards, T. L., Nowicki, S., Marzeion, B., Hock, R., Goelzer, H., Seroussi, H., Jourdain, N. C., Slater, D. A., Turner, F. E., Smith, C. J., et al. (2021). Projected land ice contributions to twenty-first-century sea level rise. Nature, 593(7857):74–82.

How to cite: Turner, F., Rougier, J., Edwards, T., Coulon, V., and Klose, A. K.: Building probabilistic projections of the Antarctic contribution to global sea level rise using a random forests emulato, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-16820, https://doi.org/10.5194/egusphere-egu24-16820, 2024.