Using video detection of snow surface movements to estimate weak layer crack propagation speeds

Abstract Dry-snow slab avalanches release due to crack propagation in a weak snow layer under a cohesive snow slab. Crack propagation speeds can provide insights into the potential size of avalanches and inform fracture and avalanche release models. Despite their importance, slope-scale crack speed...

Full description

Bibliographic Details
Published in:Annals of Glaciology
Main Authors: Simenhois, Ron, Birkeland, Karl W., Gaume, Johan, van Herwijnen, Alec, Bergfeld, Bastian, Trottet, Bertil, Greene, Ethan
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 2023
Subjects:
Online Access:http://dx.doi.org/10.1017/aog.2023.36
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0260305523000368
id crcambridgeupr:10.1017/aog.2023.36
record_format openpolar
spelling crcambridgeupr:10.1017/aog.2023.36 2024-06-09T07:38:27+00:00 Using video detection of snow surface movements to estimate weak layer crack propagation speeds Simenhois, Ron Birkeland, Karl W. Gaume, Johan van Herwijnen, Alec Bergfeld, Bastian Trottet, Bertil Greene, Ethan 2023 http://dx.doi.org/10.1017/aog.2023.36 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0260305523000368 en eng Cambridge University Press (CUP) http://creativecommons.org/licenses/by/4.0/ Annals of Glaciology page 1-11 ISSN 0260-3055 1727-5644 journal-article 2023 crcambridgeupr https://doi.org/10.1017/aog.2023.36 2024-05-15T13:13:07Z Abstract Dry-snow slab avalanches release due to crack propagation in a weak snow layer under a cohesive snow slab. Crack propagation speeds can provide insights into the potential size of avalanches and inform fracture and avalanche release models. Despite their importance, slope-scale crack speed measurements from real avalanches are limited. Further, most existing slope-scale measurements utilize the appearance of slab fractures on the snow surface. However, we have no evidence that the appearance of surface cracking is a good indicator of the weak layer crack propagation tip. Here we present a novel method to estimate crack propagation speed from snow surface movements in avalanche videos. Our technique uses changes in frame pixel intensity, allowing us to detect the location of weak layer cracks well before slab fractures appear on the snow surface. We use field experiments and numerical simulations to validate our method before applying it to five avalanches. Our estimates show that cracks propagate faster up and down the slope than in the cross-slope direction; this suggests that different propagation regimes likely govern crack propagation up/down the slope, cross-slope and in flat terrain. Article in Journal/Newspaper Annals of Glaciology Cambridge University Press Annals of Glaciology 1 11
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
description Abstract Dry-snow slab avalanches release due to crack propagation in a weak snow layer under a cohesive snow slab. Crack propagation speeds can provide insights into the potential size of avalanches and inform fracture and avalanche release models. Despite their importance, slope-scale crack speed measurements from real avalanches are limited. Further, most existing slope-scale measurements utilize the appearance of slab fractures on the snow surface. However, we have no evidence that the appearance of surface cracking is a good indicator of the weak layer crack propagation tip. Here we present a novel method to estimate crack propagation speed from snow surface movements in avalanche videos. Our technique uses changes in frame pixel intensity, allowing us to detect the location of weak layer cracks well before slab fractures appear on the snow surface. We use field experiments and numerical simulations to validate our method before applying it to five avalanches. Our estimates show that cracks propagate faster up and down the slope than in the cross-slope direction; this suggests that different propagation regimes likely govern crack propagation up/down the slope, cross-slope and in flat terrain.
format Article in Journal/Newspaper
author Simenhois, Ron
Birkeland, Karl W.
Gaume, Johan
van Herwijnen, Alec
Bergfeld, Bastian
Trottet, Bertil
Greene, Ethan
spellingShingle Simenhois, Ron
Birkeland, Karl W.
Gaume, Johan
van Herwijnen, Alec
Bergfeld, Bastian
Trottet, Bertil
Greene, Ethan
Using video detection of snow surface movements to estimate weak layer crack propagation speeds
author_facet Simenhois, Ron
Birkeland, Karl W.
Gaume, Johan
van Herwijnen, Alec
Bergfeld, Bastian
Trottet, Bertil
Greene, Ethan
author_sort Simenhois, Ron
title Using video detection of snow surface movements to estimate weak layer crack propagation speeds
title_short Using video detection of snow surface movements to estimate weak layer crack propagation speeds
title_full Using video detection of snow surface movements to estimate weak layer crack propagation speeds
title_fullStr Using video detection of snow surface movements to estimate weak layer crack propagation speeds
title_full_unstemmed Using video detection of snow surface movements to estimate weak layer crack propagation speeds
title_sort using video detection of snow surface movements to estimate weak layer crack propagation speeds
publisher Cambridge University Press (CUP)
publishDate 2023
url http://dx.doi.org/10.1017/aog.2023.36
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0260305523000368
genre Annals of Glaciology
genre_facet Annals of Glaciology
op_source Annals of Glaciology
page 1-11
ISSN 0260-3055 1727-5644
op_rights http://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.1017/aog.2023.36
container_title Annals of Glaciology
container_start_page 1
op_container_end_page 11
_version_ 1801373006232027136