Snow fracture in relation to slab avalanche release: critical state for the onset of crack propagation

The failure of a weak snow layer buried below cohesive slab layers is a necessary, but insufficient, condition for the release of a dry-snow slab avalanche. The size of the crack in the weak layer must also exceed a critical length to propagate across a slope. In contrast to pioneering shear-based a...

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Published in:The Cryosphere
Main Authors: Gaume, Johan, van Herwijnen, Alec, Chambon, Guillaume, Wever, Nander, Schweizer, Jürg
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2017
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Online Access:https://doi.org/10.5194/tc-11-217-2017
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spelling ftnonlinearchiv:oai:noa.gwlb.de:cop_mods_00010490 2023-05-15T18:32:32+02:00 Snow fracture in relation to slab avalanche release: critical state for the onset of crack propagation Gaume, Johan van Herwijnen, Alec Chambon, Guillaume Wever, Nander Schweizer, Jürg 2017-01 electronic https://doi.org/10.5194/tc-11-217-2017 https://noa.gwlb.de/receive/cop_mods_00010490 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00010447/tc-11-217-2017.pdf https://tc.copernicus.org/articles/11/217/2017/tc-11-217-2017.pdf eng eng Copernicus Publications The Cryosphere -- ˜Theœ Cryosphere -- http://www.bibliothek.uni-regensburg.de/ezeit/?2393169 -- http://www.the-cryosphere.net/ -- 1994-0424 https://doi.org/10.5194/tc-11-217-2017 https://noa.gwlb.de/receive/cop_mods_00010490 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00010447/tc-11-217-2017.pdf https://tc.copernicus.org/articles/11/217/2017/tc-11-217-2017.pdf uneingeschränkt info:eu-repo/semantics/openAccess article Verlagsveröffentlichung article Text doc-type:article 2017 ftnonlinearchiv https://doi.org/10.5194/tc-11-217-2017 2022-02-08T22:57:00Z The failure of a weak snow layer buried below cohesive slab layers is a necessary, but insufficient, condition for the release of a dry-snow slab avalanche. The size of the crack in the weak layer must also exceed a critical length to propagate across a slope. In contrast to pioneering shear-based approaches, recent developments account for weak layer collapse and allow for better explaining typical observations of remote triggering from low-angle terrain. However, these new models predict a critical length for crack propagation that is almost independent of slope angle, a rather surprising and counterintuitive result. Based on discrete element simulations we propose a new analytical expression for the critical crack length. This new model reconciles past approaches by considering for the first time the complex interplay between slab elasticity and the mechanical behavior of the weak layer including its structural collapse. The crack begins to propagate when the stress induced by slab loading and deformation at the crack tip exceeds the limit given by the failure envelope of the weak layer. The model can reproduce crack propagation on low-angle terrain and the decrease in critical length with increasing slope angle as modeled in numerical experiments. The good agreement of our new model with extensive field data and the ease of implementation in the snow cover model SNOWPACK opens a promising prospect for improving avalanche forecasting. Article in Journal/Newspaper The Cryosphere Niedersächsisches Online-Archiv NOA The Cryosphere 11 1 217 228
institution Open Polar
collection Niedersächsisches Online-Archiv NOA
op_collection_id ftnonlinearchiv
language English
topic article
Verlagsveröffentlichung
spellingShingle article
Verlagsveröffentlichung
Gaume, Johan
van Herwijnen, Alec
Chambon, Guillaume
Wever, Nander
Schweizer, Jürg
Snow fracture in relation to slab avalanche release: critical state for the onset of crack propagation
topic_facet article
Verlagsveröffentlichung
description The failure of a weak snow layer buried below cohesive slab layers is a necessary, but insufficient, condition for the release of a dry-snow slab avalanche. The size of the crack in the weak layer must also exceed a critical length to propagate across a slope. In contrast to pioneering shear-based approaches, recent developments account for weak layer collapse and allow for better explaining typical observations of remote triggering from low-angle terrain. However, these new models predict a critical length for crack propagation that is almost independent of slope angle, a rather surprising and counterintuitive result. Based on discrete element simulations we propose a new analytical expression for the critical crack length. This new model reconciles past approaches by considering for the first time the complex interplay between slab elasticity and the mechanical behavior of the weak layer including its structural collapse. The crack begins to propagate when the stress induced by slab loading and deformation at the crack tip exceeds the limit given by the failure envelope of the weak layer. The model can reproduce crack propagation on low-angle terrain and the decrease in critical length with increasing slope angle as modeled in numerical experiments. The good agreement of our new model with extensive field data and the ease of implementation in the snow cover model SNOWPACK opens a promising prospect for improving avalanche forecasting.
format Article in Journal/Newspaper
author Gaume, Johan
van Herwijnen, Alec
Chambon, Guillaume
Wever, Nander
Schweizer, Jürg
author_facet Gaume, Johan
van Herwijnen, Alec
Chambon, Guillaume
Wever, Nander
Schweizer, Jürg
author_sort Gaume, Johan
title Snow fracture in relation to slab avalanche release: critical state for the onset of crack propagation
title_short Snow fracture in relation to slab avalanche release: critical state for the onset of crack propagation
title_full Snow fracture in relation to slab avalanche release: critical state for the onset of crack propagation
title_fullStr Snow fracture in relation to slab avalanche release: critical state for the onset of crack propagation
title_full_unstemmed Snow fracture in relation to slab avalanche release: critical state for the onset of crack propagation
title_sort snow fracture in relation to slab avalanche release: critical state for the onset of crack propagation
publisher Copernicus Publications
publishDate 2017
url https://doi.org/10.5194/tc-11-217-2017
https://noa.gwlb.de/receive/cop_mods_00010490
https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00010447/tc-11-217-2017.pdf
https://tc.copernicus.org/articles/11/217/2017/tc-11-217-2017.pdf
genre The Cryosphere
genre_facet The Cryosphere
op_relation The Cryosphere -- ˜Theœ Cryosphere -- http://www.bibliothek.uni-regensburg.de/ezeit/?2393169 -- http://www.the-cryosphere.net/ -- 1994-0424
https://doi.org/10.5194/tc-11-217-2017
https://noa.gwlb.de/receive/cop_mods_00010490
https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00010447/tc-11-217-2017.pdf
https://tc.copernicus.org/articles/11/217/2017/tc-11-217-2017.pdf
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op_doi https://doi.org/10.5194/tc-11-217-2017
container_title The Cryosphere
container_volume 11
container_issue 1
container_start_page 217
op_container_end_page 228
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