EGU23-1062
https://doi.org/10.5194/egusphere-egu23-1062
EGU General Assembly 2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.

Automated ice ablation readings reveal the significance of summer heat waves for glacier melt

Aaron Cremona1,2, Matthias Huss1,2,3, Johannes Marian Landmann1,2,4, Joël Borner1,5, and Daniel Farinotti1,2
Aaron Cremona et al.
  • 1ETH Zurich, Laboratory of Hydraulics, Hydrology and Glaciology (VAW), D-BAUG, Zürich, Switzerland (cremona@vaw.baug.ethz.ch)
  • 2Swiss Federal Institute for Forest, Snow and Landscape Research (WSL), Birmensdorf, Switzerland
  • 3Department of Geosciences, University of Fribourg, Fribourg, Switzerland
  • 4Federal Office of Meteorology and Climatology, MeteoSwiss, Zurich-Airport, Switzerland
  • 5WSL Institute for Snow and Avalanche Research SLF, Davos, Switzerland

Summer heat waves have a substantial impact on glacier melt as emphasized by the extreme summer of 2022 that caused unprecedented mass losses to the Swiss glaciers. Despite the dramatic impact on glaciers, the summer of 2022 offered a unique opportunity to analyze the implications that such extraordinary events have on glacier melt and related runoff release.

This study presents a novel approach based on computer-vision techniques for automatically determining daily mass balance variations at the local scale. The approach is based on the automated recognition of color-taped ablation stakes from camera images acquired at six sites on three Alpine glaciers in the period 2019-2022. The validation of the method revealed an uncertainty of the automated readings of ±0.81 cm d-1. By comparing the automatically retrieved mass balances at the six sites with the average mass balance of the last decade derived from seasonal in situ observations, we detect extreme melt events in the summer seasons of 2019-2022.

The in-depth analysis of summer 2022 allows us to assess the impact that the summer heat waves have on glacier melt. With our approach we detect 23 days with extreme melt over the summer, emphasizing the strong correspondence between heat waves and extreme melt events. The Swiss-wide glacier mass loss during the 25 days of heat waves in 2022 is estimated as 1.27 ± 0.10 Gt, corresponding to 35% of the overall glacier mass loss in the summer of 2022. As compared to the 2010-2020 average glacier mass change, days with extreme melt in 2022 correspond to 56% of the mass change during the summer period, thus demonstrating the significance of heat waves for seasonal melt.

How to cite: Cremona, A., Huss, M., Landmann, J. M., Borner, J., and Farinotti, D.: Automated ice ablation readings reveal the significance of summer heat waves for glacier melt, EGU General Assembly 2023, Vienna, Austria, 24–28 Apr 2023, EGU23-1062, https://doi.org/10.5194/egusphere-egu23-1062, 2023.