EGU24-10661, updated on 08 Mar 2024
https://doi.org/10.5194/egusphere-egu24-10661
EGU General Assembly 2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.

Ice Borehole Thermometry: Paleo-Climate reconstruction using Bayesian modeling

Kshema Shaju1,4, Thomas Laepple1,2,3, and Peter Zaspel4
Kshema Shaju et al.
  • 1Alfred Wegener Institute, Potsdam, Germany (kshema.shaju@awi.de)
  • 2MARUM Center for Marine Environmental Sciences, University of Bremen, Bremen, Germany
  • 3Department of Geosciences, University of Bremen, Bremen, Germany
  • 4School of Mathematics and Natural Sciences, Bergische Universität Wuppertal, Wuppertal, Germany

In the quest of understanding the past and present climate system, we aim to reconstruct paleo-climate using Bayesian inversion from Antarctic borehole temperature profiles. We aim to develop a refined process for reconstructing the temperature evolution of Antarctica over the last century and millennia. Initially, a forward heat transfer model is implemented that simulates borehole temperature profiles for time-dependent surface temperatures. The forward model provides an approximate notion of the borehole depth at which a signal from the past may be obtained. Using forward simulations, a greedy approach is employed for the optimal placement of temperature sensors in the borehole to record temperature effectively. We invert the forward model to reconstruct past surface temperature evolution from borehole temperature measurements. For this, we apply Bayesian inference to optimally account for the uncertainty in the various influencing quantities. We model known uncertainties as priors and obtain the reconstructed surface temperatures with connected uncertainty information.

How to cite: Shaju, K., Laepple, T., and Zaspel, P.: Ice Borehole Thermometry: Paleo-Climate reconstruction using Bayesian modeling, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-10661, https://doi.org/10.5194/egusphere-egu24-10661, 2024.