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...
Published in: | Journal of Glaciology |
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Cambridge University Press
2022
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Online Access: | https://doi.org/10.1017/jog.2021.118 https://doaj.org/article/2bd78ff53b7643b48a3b4cb550536a78 |
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ftdoajarticles:oai:doaj.org/article:2bd78ff53b7643b48a3b4cb550536a78 2023-05-15T16:57:34+02:00 Crack propagation speeds in weak snowpack layers Bastian Bergfeld Alec van Herwijnen Grégoire Bobillier Eric Larose Ludovic Moreau Bertil Trottet Johan Gaume Janic Cathomen Jürg Dual Jürg Schweizer 2022-06-01T00:00:00Z https://doi.org/10.1017/jog.2021.118 https://doaj.org/article/2bd78ff53b7643b48a3b4cb550536a78 EN eng Cambridge University Press https://www.cambridge.org/core/product/identifier/S0022143021001180/type/journal_article https://doaj.org/toc/0022-1430 https://doaj.org/toc/1727-5652 doi:10.1017/jog.2021.118 0022-1430 1727-5652 https://doaj.org/article/2bd78ff53b7643b48a3b4cb550536a78 Journal of Glaciology, Vol 68, Pp 557-570 (2022) Avalanches snow snow mechanics Environmental sciences GE1-350 Meteorology. Climatology QC851-999 article 2022 ftdoajarticles https://doi.org/10.1017/jog.2021.118 2023-03-12T01:30:54Z 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. Article in Journal/Newspaper Journal of Glaciology Directory of Open Access Journals: DOAJ Articles Journal of Glaciology 68 269 557 570 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
Avalanches snow snow mechanics Environmental sciences GE1-350 Meteorology. Climatology QC851-999 |
spellingShingle |
Avalanches snow snow mechanics Environmental sciences GE1-350 Meteorology. Climatology QC851-999 Bastian Bergfeld Alec van Herwijnen Grégoire Bobillier Eric Larose Ludovic Moreau Bertil Trottet Johan Gaume Janic Cathomen Jürg Dual Jürg Schweizer Crack propagation speeds in weak snowpack layers |
topic_facet |
Avalanches snow snow mechanics Environmental sciences GE1-350 Meteorology. Climatology QC851-999 |
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. |
format |
Article in Journal/Newspaper |
author |
Bastian Bergfeld Alec van Herwijnen Grégoire Bobillier Eric Larose Ludovic Moreau Bertil Trottet Johan Gaume Janic Cathomen Jürg Dual Jürg Schweizer |
author_facet |
Bastian Bergfeld Alec van Herwijnen Grégoire Bobillier Eric Larose Ludovic Moreau Bertil Trottet Johan Gaume Janic Cathomen Jürg Dual Jürg Schweizer |
author_sort |
Bastian Bergfeld |
title |
Crack propagation speeds in weak snowpack layers |
title_short |
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_sort |
crack propagation speeds in weak snowpack layers |
publisher |
Cambridge University Press |
publishDate |
2022 |
url |
https://doi.org/10.1017/jog.2021.118 https://doaj.org/article/2bd78ff53b7643b48a3b4cb550536a78 |
genre |
Journal of Glaciology |
genre_facet |
Journal of Glaciology |
op_source |
Journal of Glaciology, Vol 68, Pp 557-570 (2022) |
op_relation |
https://www.cambridge.org/core/product/identifier/S0022143021001180/type/journal_article https://doaj.org/toc/0022-1430 https://doaj.org/toc/1727-5652 doi:10.1017/jog.2021.118 0022-1430 1727-5652 https://doaj.org/article/2bd78ff53b7643b48a3b4cb550536a78 |
op_doi |
https://doi.org/10.1017/jog.2021.118 |
container_title |
Journal of Glaciology |
container_volume |
68 |
container_issue |
269 |
container_start_page |
557 |
op_container_end_page |
570 |
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1766049133987102720 |