EGU2020-22129
https://doi.org/10.5194/egusphere-egu2020-22129
EGU General Assembly 2020
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.

Ice load-bedrock uplift feedback leads to self-sustained oscillations in the Greenland Ice Sheet on long time scales

Maria Zeitz1,2, Jan Haacker1,2,3, and Ricarda Winkelmann1,2
Maria Zeitz et al.
  • 1Potsdam Institute for Climate Impact Research, Potsdam, Germany (maria.zeitz@pik-potsdam.de)
  • 2Institute of Physics, Potsdam University, Potsdam, Germany
  • 3Civil Engineering and Geosciences, TU Delft, Delft, Netherlands

The Greenland ice sheet loses substantial amounts of mass, due to accelerating outlet glaciers and longer melting periods. Different positive feedback mechanisms, as the melt-elevation feedback and the ice-albedo feedback, introduce a non-linear evolution and may further accelerate mass loss. Negative feedbacks, such as the feedback between receding ice load and subsequent bedrock uplift, might counteract the accelerating positive feedbacks on long timescales. Roughly, the bedrock uplift amounts to 1/3 of the change in the ice sheet thickness on a timescale of millennia.

To explore the interplay of those feedbacks, we use simulations of the Greenland Ice Sheet with the Parallel Ice Sheet Model (PISM) including an Elastic Lithosphere Relaxing Asthenosphere (ELRA) model in an idealized warming scenario. In particular, we observe that depending on the temperature anomaly (and thus the retreat time) and the asthenosphere viscosity, three distinct responses of the ice sheet are possible:

How to cite: Zeitz, M., Haacker, J., and Winkelmann, R.: Ice load-bedrock uplift feedback leads to self-sustained oscillations in the Greenland Ice Sheet on long time scales, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-22129, https://doi.org/10.5194/egusphere-egu2020-22129, 2020

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