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Maëva Cathala

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Articles

Predisposing, triggering and runout processes at a permafrost‐affected rock avalanche site in the French Alps (Étache, June 2020)

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By Florence Magnin, Ludovic Ravanel, Maëva Cathala, Josué Bock
| Wiley Online Library Verified
1 INTRODUCTION In the European Alps, the air temperature has increased by 2°C on average between the end of the 19th and the beginning of the 21st century, with an acceleration since 1980 (Beniston et al., 2018; Böhm et al., 2010; Nigrelli & Chiarle, 2023). High mountain environments are highly sensitive to this rapid climate change and the degradation of mountain permafrost is one of the consequences (Etzelmüller et al., 2020; Magnin et al., 2024).
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