Articles | Volume 22, issue 1
https://doi.org/10.5194/cp-22-173-2026
https://doi.org/10.5194/cp-22-173-2026
Research article
 | 
21 Jan 2026
Research article |  | 21 Jan 2026

A continuous 6000 a age depth relationship for the remainder of the Weißseespitze summit glacier based on 39Ar and 14C dating

David Wachs, Azzurra Spagnesi, Pascal Bohleber, Andrea Fischer, Martin Stocker-Waldhuber, Alexander Junkermann, Carl Kindermann, Linus Langenbacher, Niclas Mandaric, Joshua Marks, Florian Meienburg, Theo M. Jenk, Markus K. Oberthaler, and Werner Aeschbach

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This preprint is open for discussion and under review for The Cryosphere (TC).
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Cited articles

Arck, Y., Meienburg, F., Wachs, D., Beyersdorfer, S., Kersting, A., Schmidt, M., Oberthaler, M., and Aeschbach, W.: Sampling and Purification Methods for Dating by Atom Trap Trace Analysis in Various Environmental Applications, ACS Earth Space Chem., 9, 1927–1937, https://doi.org/10.1021/acsearthspacechem.5c00128, 2025. 
Bohleber, P.: Alpine Ice Cores as Climate and Environmental Archives, in: Oxford Research Encyclopedia of Climate Science, Oxford University Press, https://doi.org/10.1093/acrefore/9780190228620.013.743, 2019. 
Bohleber, P., Erhardt, T., Spaulding, N., Hoffmann, H., Fischer, H., and Mayewski, P.: Temperature and mineral dust variability recorded in two low-accumulation Alpine ice cores over the last millennium, Clim. Past, 14, 21–37, https://doi.org/10.5194/cp-14-21-2018, 2018. 
Bohleber, P., Schwikowski, M., Stocker-Waldhuber, M., Fang, L., and Fischer, A.: New glacier evidence for ice-free summits during the life of the Tyrolean Iceman, Scientific Reports, 10, 20513, https://doi.org/10.1038/s41598-020-77518-9, 2020. 
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Short summary
This study presents an age profile of the summit glacier of Weißseespitze in the Austrian Alps. The ages were obtained by combining 14C dating with the novel atom trap trace analysis for 39Ar. The data was used to constrain glacier age models. The results show that the surface ice is ~400 a old due to recent ice loss. The remaining ice continuously covers ages up to 6000 a. This work underscores the utility of 39Ar dating in glaciology, enabling precise reconstruction of age-depth relationships.
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