Supershear crack propagation in snow slab avalanche release: new insights from numerical simulations and field measurements
<p>The release process of dry-snow slab avalanches begins with a localized failure within a porous, weak snow layer beneath a cohesive slab. Subsequently, rapid crack propagation may occur within the weak layer, eventually leading to a tensile fracture across the slab, resulting, if the slope...
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Copernicus Publications
2025-07-01
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| Series: | Natural Hazards and Earth System Sciences |
| Online Access: | https://nhess.copernicus.org/articles/25/2215/2025/nhess-25-2215-2025.pdf |
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| author | G. Bobillier G. Bobillier B. Trottet B. Bergfeld R. Simenhois A. van Herwijnen J. Schweizer J. Gaume J. Gaume J. Gaume |
| author_facet | G. Bobillier G. Bobillier B. Trottet B. Bergfeld R. Simenhois A. van Herwijnen J. Schweizer J. Gaume J. Gaume J. Gaume |
| author_sort | G. Bobillier |
| collection | DOAJ |
| description | <p>The release process of dry-snow slab avalanches begins with a localized failure within a porous, weak snow layer beneath a cohesive slab. Subsequently, rapid crack propagation may occur within the weak layer, eventually leading to a tensile fracture across the slab, resulting, if the slope is steep enough, in its detachment and sliding. The dynamics of crack propagation is believed to influence the size of the release area. However, the relationship between crack propagation dynamics and avalanche size remains incompletely understood. Notably, crack propagation speeds estimated from avalanche video analysis are almost 1 order of magnitude larger than speeds typically measured in field experiments. To shed more light on this discrepancy and avalanche release processes, we used discrete (DEM: discrete element method) and continuum (MPM: material point method) numerical methods to simulate the so-called propagation saw test (PST). On low-angle terrain, our models showed that the weak layer failed mainly due to a compressive stress peak at the crack tip induced by weak layer collapse and the resulting slab bending. On steep slopes, we observed the emergence of a supershear crack propagation regime: the crack speed becomes higher than the slab shear wave speed. This transition occurs if the crack propagates over a distance larger than the super-critical crack length (approximately 5 m). Above the super-critical crack length, the fracture is mainly driven by the slope-parallel gravitational pull of the slab (tension) and, thus, shear stresses in the weak layer. These findings represent an essential additional piece in the dry-snow slab avalanche formation puzzle.</p> |
| format | Article |
| id | doaj-art-81dcd770ac3b4882a2e8b561cce4aa20 |
| institution | Kabale University |
| issn | 1561-8633 1684-9981 |
| language | English |
| publishDate | 2025-07-01 |
| publisher | Copernicus Publications |
| record_format | Article |
| series | Natural Hazards and Earth System Sciences |
| spelling | doaj-art-81dcd770ac3b4882a2e8b561cce4aa202025-08-20T03:28:33ZengCopernicus PublicationsNatural Hazards and Earth System Sciences1561-86331684-99812025-07-01252215222310.5194/nhess-25-2215-2025Supershear crack propagation in snow slab avalanche release: new insights from numerical simulations and field measurementsG. Bobillier0G. Bobillier1B. Trottet2B. Bergfeld3R. Simenhois4A. van Herwijnen5J. Schweizer6J. Gaume7J. Gaume8J. Gaume9WSL Institute for Snow and Avalanche Research SLF, Davos, SwitzerlandClimate Change, Extremes, and Natural Hazards in Alpine Regions Research Center CERC, Davos, SwitzerlandFaculty of Architecture, Civil and Environmental Engineering, École Polytechnique Fédérale de Lausanne, Lausanne, SwitzerlandWSL Institute for Snow and Avalanche Research SLF, Davos, SwitzerlandColorado Avalanche Information Center, Boulder, CO, USAWSL Institute for Snow and Avalanche Research SLF, Davos, SwitzerlandWSL Institute for Snow and Avalanche Research SLF, Davos, SwitzerlandWSL Institute for Snow and Avalanche Research SLF, Davos, SwitzerlandClimate Change, Extremes, and Natural Hazards in Alpine Regions Research Center CERC, Davos, SwitzerlandInstitute for Geotechnical Engineering, ETH Zurich, Zurich, Switzerland<p>The release process of dry-snow slab avalanches begins with a localized failure within a porous, weak snow layer beneath a cohesive slab. Subsequently, rapid crack propagation may occur within the weak layer, eventually leading to a tensile fracture across the slab, resulting, if the slope is steep enough, in its detachment and sliding. The dynamics of crack propagation is believed to influence the size of the release area. However, the relationship between crack propagation dynamics and avalanche size remains incompletely understood. Notably, crack propagation speeds estimated from avalanche video analysis are almost 1 order of magnitude larger than speeds typically measured in field experiments. To shed more light on this discrepancy and avalanche release processes, we used discrete (DEM: discrete element method) and continuum (MPM: material point method) numerical methods to simulate the so-called propagation saw test (PST). On low-angle terrain, our models showed that the weak layer failed mainly due to a compressive stress peak at the crack tip induced by weak layer collapse and the resulting slab bending. On steep slopes, we observed the emergence of a supershear crack propagation regime: the crack speed becomes higher than the slab shear wave speed. This transition occurs if the crack propagates over a distance larger than the super-critical crack length (approximately 5 m). Above the super-critical crack length, the fracture is mainly driven by the slope-parallel gravitational pull of the slab (tension) and, thus, shear stresses in the weak layer. These findings represent an essential additional piece in the dry-snow slab avalanche formation puzzle.</p>https://nhess.copernicus.org/articles/25/2215/2025/nhess-25-2215-2025.pdf |
| spellingShingle | G. Bobillier G. Bobillier B. Trottet B. Bergfeld R. Simenhois A. van Herwijnen J. Schweizer J. Gaume J. Gaume J. Gaume Supershear crack propagation in snow slab avalanche release: new insights from numerical simulations and field measurements Natural Hazards and Earth System Sciences |
| title | Supershear crack propagation in snow slab avalanche release: new insights from numerical simulations and field measurements |
| title_full | Supershear crack propagation in snow slab avalanche release: new insights from numerical simulations and field measurements |
| title_fullStr | Supershear crack propagation in snow slab avalanche release: new insights from numerical simulations and field measurements |
| title_full_unstemmed | Supershear crack propagation in snow slab avalanche release: new insights from numerical simulations and field measurements |
| title_short | Supershear crack propagation in snow slab avalanche release: new insights from numerical simulations and field measurements |
| title_sort | supershear crack propagation in snow slab avalanche release new insights from numerical simulations and field measurements |
| url | https://nhess.copernicus.org/articles/25/2215/2025/nhess-25-2215-2025.pdf |
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