Glide-snow avalanches are considered unpredictable. It is presently unclear, where the water at the snow-soil interface comes from. By linking the two porous media, snow and soil, and assessing the mass and heat exchange across their interface, we will advance the predictability of glide avalanches.
Foundation Snow gliding, defined as slow downhill movement of the entire snow cover on the ground, may
https://www.slf.ch/de/mitarbeitende/carletti/
Doktorandin, SLF Davos, WSL-Institut für Schnee- und Lawinenforschung SLF, Flüelastrasse 11, 7260 Davos Dorf
Résumé May 2022 – Present PhD Student in Snow Hydrology, SLF (Davos, Switzerland) 2020 – 2022 Operational
https://www.slf.ch/de/mitarbeitende/vanherwi/
Gruppenleiter, SLF Davos, WSL Institute for Snow and Avalanche Research SLF, Flüelastrasse 11, 7260 Davos Dorf
General Assembly of the European Geophysical Union, 27 April – 2 May 2014, Vienna, Austria.
https://www.slf.ch/de/mitarbeitende/schneebm/
Gastwissenschafter, Schnee und Atmosphäre, SLF Davos, WSL-Institut für Schnee- und Lawinenforschung SLF, Flüelastrasse 11, 7260 Davos Dorf
(Environmental Engineering), ETH Zürich Head of Research Unit „Snow and Permafrost since May 2018 Invited
