Stress Concentrations in Weak Snowpack Layers and Conditions for Slab Avalanche Release
Abstract Dry‐snow slab avalanches release due to the formation of a crack in a weak layer buried below cohesive snow slabs, followed by rapid crack propagation. The onset of rapid crack propagation occurs if stresses at the crack tip in the weak layer overcome its strength. In this study, we use the...
Guardado en:
| Autores principales: | , , , |
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| Formato: | Artigo |
| Lenguaje: | Inglês |
| Publicado: |
Wiley
2018-08-01
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| Colección: | Geophysical Research Letters |
| Materias: | |
| Acceso en línea: | https://doi.org/10.1029/2018GL078900 |
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