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...
Main Authors: | , , , , , , , , , , , |
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Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Cambridge University Press
2022
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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 |