International Snow Science Workshop Proceedings - Montana State University Library

Item: SUPERSHEAR CRACK PROPAGATION IN SNOW SLAB AVALANCHE RELEASE: NEW INSIGHTS FROM NUMERICAL SIMULATIONS AND FIELD MEASUREMENTS

• • Title: SUPERSHEAR CRACK PROPAGATION IN SNOW SLAB AVALANCHE RELEASE: NEW INSIGHTS FROM NUMERICAL SIMULATIONS AND FIELD MEASUREMENTS

    Proceedings: International Snow Science Workshop Proceedings 2023, Bend, Oregon

    Authors:

    • Grégoire Bobillier  [ WSL Institute for Snow and Avalanche Research SLF, Davos, Switzerland ]  [ Climate Change, Extremes, and Natural Hazards in Alpine Regions Research Center CERC, Davos, Switzerland ]
    • Bertil Trottet  [ École Polytechnique Fédérale de Lausanne, Switzerland ]
    • Bastian Bergfeld  [ WSL Institute for Snow and Avalanche Research SLF, Davos, Switzerland ]
    • Ron Simenhois  [ Colorado Avalanche Information Center, Boulder, CO, USA ]
    • Alec van Herwijnen  [ WSL Institute for Snow and Avalanche Research SLF, Davos, Switzerland ]
    • Jürg Schweizer  [ WSL Institute for Snow and Avalanche Research SLF, Davos, Switzerland ]
    • Johan Gaume  [ WSL Institute for Snow and Avalanche Research SLF, Davos, Switzerland ]  [ Climate Change, Extremes, and Natural Hazards in Alpine Regions Research Center CERC, Davos, Switzerland ]  [ Institute for Geotechnical Engineering, ETH Zurich, Switzerland ]

    Date: 2023-10-08

    Abstract: The release process of dry-snow slab avalanches begins with a localized failure within a porous, weak snow layer that lies 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, to 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 one 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 fails 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.

    Object ID: ISSW2023_O2.01.pdf

    Language of Article: English

    Presenter(s): Grégoire Bobillier

    Keywords: supershear crack propagation, numerical modeling, dry-snow slab avalanche release

    Page Number(s): 38 - 42

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