Crack propagation speeds in weak snowpack layers

For the release of a slab avalanche, crack propagation within a weak snowpack layer below a cohesive snow slab is required. As crack speed measurements can give insight into underlying processes, we analysed three crack propagation events that occurred in similar snowpacks and covered all scales rel...

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Main Authors: Bergfeld, Bastian, van Herwijnen, Alec, Bobillier, Grégoire, Larose, Eric, Moreau, Ludovic, Trottet, Bertil, Gaume, Johan, Cathomen, Janic, Dual, Jürg, id_orcid:0 000-0001-5861-9058, Schweizer, Jürg, id_orcid:0 000-0001-5076-2968
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press 2022
Subjects:
Online Access:https://hdl.handle.net/20.500.11850/523719
https://doi.org/10.3929/ethz-b-000523719
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author Bergfeld, Bastian
van Herwijnen, Alec
Bobillier, Grégoire
Larose, Eric
Moreau, Ludovic
Trottet, Bertil
Gaume, Johan
Cathomen, Janic
Dual, Jürg
id_orcid:0 000-0001-5861-9058
Schweizer, Jürg
id_orcid:0 000-0001-5076-2968
author_facet Bergfeld, Bastian
van Herwijnen, Alec
Bobillier, Grégoire
Larose, Eric
Moreau, Ludovic
Trottet, Bertil
Gaume, Johan
Cathomen, Janic
Dual, Jürg
id_orcid:0 000-0001-5861-9058
Schweizer, Jürg
id_orcid:0 000-0001-5076-2968
author_sort Bergfeld, Bastian
collection ETH Zürich Research Collection
description For the release of a slab avalanche, crack propagation within a weak snowpack layer below a cohesive snow slab is required. As crack speed measurements can give insight into underlying processes, we analysed three crack propagation events that occurred in similar snowpacks and covered all scales relevant for avalanche release. For the largest scale, up to 400 m, we estimated crack speed from an avalanche movie; for scales between 5 and 25 m, we used accelerometers placed on the snow surface and for scales below 5 m, we performed a propagation saw test. The mean crack speeds ranged from 36 ± 6 to 49 ± 5 m s−1, and did not exhibit scale dependence. Using the discrete element method and the material point method, we reproduced the measured crack speeds reasonably well, in particular the terminal crack speed observed at smaller scales. Finally, we used a finite element model to assess the speed of different elastic waves in a layered snowpack. Results suggest that the observed cracks propagated as mixed mode closing cracks and that the flexural wave of the slab is responsible for the energy transfer to the crack tip. ISSN:0022-1430 ISSN:1727-5652
format Article in Journal/Newspaper
genre Journal of Glaciology
genre_facet Journal of Glaciology
id ftethz:oai:www.research-collection.ethz.ch:20.500.11850/523719
institution Open Polar
language English
op_collection_id ftethz
op_doi https://doi.org/20.500.11850/52371910.3929/ethz-b-00052371910.1017/jog.2021.118
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1017/jog.2021.118
info:eu-repo/semantics/altIdentifier/wos/000736116100001
http://hdl.handle.net/20.500.11850/523719
op_rights info:eu-repo/semantics/openAccess
http://creativecommons.org/licenses/by/4.0/
Creative Commons Attribution 4.0 International
op_source Journal of Glaciology, 68 (269)
publishDate 2022
publisher Cambridge University Press
record_format openpolar
spelling ftethz:oai:www.research-collection.ethz.ch:20.500.11850/523719 2025-03-30T15:17:08+00:00 Crack propagation speeds in weak snowpack layers Bergfeld, Bastian van Herwijnen, Alec Bobillier, Grégoire Larose, Eric Moreau, Ludovic Trottet, Bertil Gaume, Johan Cathomen, Janic Dual, Jürg id_orcid:0 000-0001-5861-9058 Schweizer, Jürg id_orcid:0 000-0001-5076-2968 2022-06 application/application/pdf https://hdl.handle.net/20.500.11850/523719 https://doi.org/10.3929/ethz-b-000523719 en eng Cambridge University Press info:eu-repo/semantics/altIdentifier/doi/10.1017/jog.2021.118 info:eu-repo/semantics/altIdentifier/wos/000736116100001 http://hdl.handle.net/20.500.11850/523719 info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/4.0/ Creative Commons Attribution 4.0 International Journal of Glaciology, 68 (269) Avalanches snow snow mechanics info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2022 ftethz https://doi.org/20.500.11850/52371910.3929/ethz-b-00052371910.1017/jog.2021.118 2025-03-05T22:09:15Z For the release of a slab avalanche, crack propagation within a weak snowpack layer below a cohesive snow slab is required. As crack speed measurements can give insight into underlying processes, we analysed three crack propagation events that occurred in similar snowpacks and covered all scales relevant for avalanche release. For the largest scale, up to 400 m, we estimated crack speed from an avalanche movie; for scales between 5 and 25 m, we used accelerometers placed on the snow surface and for scales below 5 m, we performed a propagation saw test. The mean crack speeds ranged from 36 ± 6 to 49 ± 5 m s−1, and did not exhibit scale dependence. Using the discrete element method and the material point method, we reproduced the measured crack speeds reasonably well, in particular the terminal crack speed observed at smaller scales. Finally, we used a finite element model to assess the speed of different elastic waves in a layered snowpack. Results suggest that the observed cracks propagated as mixed mode closing cracks and that the flexural wave of the slab is responsible for the energy transfer to the crack tip. ISSN:0022-1430 ISSN:1727-5652 Article in Journal/Newspaper Journal of Glaciology ETH Zürich Research Collection
spellingShingle Avalanches
snow
snow mechanics
Bergfeld, Bastian
van Herwijnen, Alec
Bobillier, Grégoire
Larose, Eric
Moreau, Ludovic
Trottet, Bertil
Gaume, Johan
Cathomen, Janic
Dual, Jürg
id_orcid:0 000-0001-5861-9058
Schweizer, Jürg
id_orcid:0 000-0001-5076-2968
Crack propagation speeds in weak snowpack layers
title Crack propagation speeds in weak snowpack layers
title_full Crack propagation speeds in weak snowpack layers
title_fullStr Crack propagation speeds in weak snowpack layers
title_full_unstemmed Crack propagation speeds in weak snowpack layers
title_short Crack propagation speeds in weak snowpack layers
title_sort crack propagation speeds in weak snowpack layers
topic Avalanches
snow
snow mechanics
topic_facet Avalanches
snow
snow mechanics
url https://hdl.handle.net/20.500.11850/523719
https://doi.org/10.3929/ethz-b-000523719