Potential and challenges of depth-resolved three-dimensional MPM simulations: a case study of the 2019 ‘Salezer’ snow avalanche in Davos

Abstract Avalanche modeling is an essential tool to assess snow avalanche hazard. Today, most popular numerical approaches adopt depth-averaged equations. These methods are computationally efficient but limited in capturing processes occurring in the flow depth direction, e.g. erosion or deposition,...

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Published in:Annals of Glaciology
Main Authors: Kyburz, Michael Lukas, Sovilla, Betty, Bühler, Yves, Gaume, Johan
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 2024
Subjects:
Online Access:http://dx.doi.org/10.1017/aog.2024.14
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0260305524000144
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spelling crcambridgeupr:10.1017/aog.2024.14 2024-09-30T14:22:45+00:00 Potential and challenges of depth-resolved three-dimensional MPM simulations: a case study of the 2019 ‘Salezer’ snow avalanche in Davos Kyburz, Michael Lukas Sovilla, Betty Bühler, Yves Gaume, Johan 2024 http://dx.doi.org/10.1017/aog.2024.14 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0260305524000144 en eng Cambridge University Press (CUP) http://creativecommons.org/licenses/by/4.0/ Annals of Glaciology page 1-14 ISSN 0260-3055 1727-5644 journal-article 2024 crcambridgeupr https://doi.org/10.1017/aog.2024.14 2024-09-04T04:04:18Z Abstract Avalanche modeling is an essential tool to assess snow avalanche hazard. Today, most popular numerical approaches adopt depth-averaged equations. These methods are computationally efficient but limited in capturing processes occurring in the flow depth direction, e.g. erosion or deposition, which are often considered using ad hoc parameterizations or neglected completely. However, processes such as snow erosion, can crucially influence flow dynamics and run-out and are often not negligible. We address these issues by using a new three-dimensional (3-D) model, based on the material point method and finite strain elastoplasticity. To assess the possibilities and challenges associated with these highly detailed but computationally expensive calculations, we simulated the ‘Salezer’ snow avalanche that released in Davos, Switzerland in 2019. To reproduce the event in our simulations, we use the release areas mapped in a photogrammetric drone survey and estimate the snow conditions on the day of the event. We compare macroscopic features, such as flow outline and snow deposition of the simulated avalanche to field observations. An in-depth analysis of transient 3-D flow structures at the avalanche head not only demonstrates the degree of physical detail in the model, but also highlights challenges which still need to be addressed. Article in Journal/Newspaper Annals of Glaciology Cambridge University Press Annals of Glaciology 1 35
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
description Abstract Avalanche modeling is an essential tool to assess snow avalanche hazard. Today, most popular numerical approaches adopt depth-averaged equations. These methods are computationally efficient but limited in capturing processes occurring in the flow depth direction, e.g. erosion or deposition, which are often considered using ad hoc parameterizations or neglected completely. However, processes such as snow erosion, can crucially influence flow dynamics and run-out and are often not negligible. We address these issues by using a new three-dimensional (3-D) model, based on the material point method and finite strain elastoplasticity. To assess the possibilities and challenges associated with these highly detailed but computationally expensive calculations, we simulated the ‘Salezer’ snow avalanche that released in Davos, Switzerland in 2019. To reproduce the event in our simulations, we use the release areas mapped in a photogrammetric drone survey and estimate the snow conditions on the day of the event. We compare macroscopic features, such as flow outline and snow deposition of the simulated avalanche to field observations. An in-depth analysis of transient 3-D flow structures at the avalanche head not only demonstrates the degree of physical detail in the model, but also highlights challenges which still need to be addressed.
format Article in Journal/Newspaper
author Kyburz, Michael Lukas
Sovilla, Betty
Bühler, Yves
Gaume, Johan
spellingShingle Kyburz, Michael Lukas
Sovilla, Betty
Bühler, Yves
Gaume, Johan
Potential and challenges of depth-resolved three-dimensional MPM simulations: a case study of the 2019 ‘Salezer’ snow avalanche in Davos
author_facet Kyburz, Michael Lukas
Sovilla, Betty
Bühler, Yves
Gaume, Johan
author_sort Kyburz, Michael Lukas
title Potential and challenges of depth-resolved three-dimensional MPM simulations: a case study of the 2019 ‘Salezer’ snow avalanche in Davos
title_short Potential and challenges of depth-resolved three-dimensional MPM simulations: a case study of the 2019 ‘Salezer’ snow avalanche in Davos
title_full Potential and challenges of depth-resolved three-dimensional MPM simulations: a case study of the 2019 ‘Salezer’ snow avalanche in Davos
title_fullStr Potential and challenges of depth-resolved three-dimensional MPM simulations: a case study of the 2019 ‘Salezer’ snow avalanche in Davos
title_full_unstemmed Potential and challenges of depth-resolved three-dimensional MPM simulations: a case study of the 2019 ‘Salezer’ snow avalanche in Davos
title_sort potential and challenges of depth-resolved three-dimensional mpm simulations: a case study of the 2019 ‘salezer’ snow avalanche in davos
publisher Cambridge University Press (CUP)
publishDate 2024
url http://dx.doi.org/10.1017/aog.2024.14
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0260305524000144
genre Annals of Glaciology
genre_facet Annals of Glaciology
op_source Annals of Glaciology
page 1-14
ISSN 0260-3055 1727-5644
op_rights http://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.1017/aog.2024.14
container_title Annals of Glaciology
container_start_page 1
op_container_end_page 35
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