Snow mechanical property variability at the slope scale – implication for snow mechanical modelling

Snow avalanches represent a natural hazard to infrastructure and backcountry recreationists. Risk assessment of avalanche hazard is difficult due to the sparse nature of available observations informing on snowpack mechanical and geophysical properties and overall stability. The spatial variability...

Full description

Bibliographic Details
Published in:The Cryosphere
Main Authors: F. Meloche, F. Gauthier, A. Langlois
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2024
Subjects:
Online Access:https://doi.org/10.5194/tc-18-1359-2024
https://doaj.org/article/69759425c3864ab3b70967feb19e3d51
id ftdoajarticles:oai:doaj.org/article:69759425c3864ab3b70967feb19e3d51
record_format openpolar
spelling ftdoajarticles:oai:doaj.org/article:69759425c3864ab3b70967feb19e3d51 2024-09-09T20:11:39+00:00 Snow mechanical property variability at the slope scale – implication for snow mechanical modelling F. Meloche F. Gauthier A. Langlois 2024-03-01T00:00:00Z https://doi.org/10.5194/tc-18-1359-2024 https://doaj.org/article/69759425c3864ab3b70967feb19e3d51 EN eng Copernicus Publications https://tc.copernicus.org/articles/18/1359/2024/tc-18-1359-2024.pdf https://doaj.org/toc/1994-0416 https://doaj.org/toc/1994-0424 doi:10.5194/tc-18-1359-2024 1994-0416 1994-0424 https://doaj.org/article/69759425c3864ab3b70967feb19e3d51 The Cryosphere, Vol 18, Pp 1359-1380 (2024) Environmental sciences GE1-350 Geology QE1-996.5 article 2024 ftdoajarticles https://doi.org/10.5194/tc-18-1359-2024 2024-08-05T17:49:46Z Snow avalanches represent a natural hazard to infrastructure and backcountry recreationists. Risk assessment of avalanche hazard is difficult due to the sparse nature of available observations informing on snowpack mechanical and geophysical properties and overall stability. The spatial variability of these properties also adds complexity to decision-making and route finding in avalanche terrain for mountain users. Snow cover models can simulate snow mechanical properties with good accuracy at fairly good spatial resolution (around 100 m). However, monitoring small-scale variability at the slope scale (5–50 m) remains critical, since slope stability and the possible size of an avalanche are governed by that scale. To better understand and estimate the spatial variability at the slope scale, this work explores links between snow mechanical properties and microtopographic indicators. Six spatial snow surveys were conducted in two study areas across Canada. Snow mechanical properties, such as snow density, elastic modulus and shear strength, were estimated from high-resolution snow penetrometer (SMP) profiles at multiple locations over several studied slopes, in Rogers Pass, British Columbia, and Mt. Albert, Québec. Point snow stability metrics, such as the skier crack length, critical propagation crack length and a skier stability index, were derived using the snow mechanical properties from SMP measurements. Microtopographic indicators, such as the topographic position index (TPI), vegetation height and proximity, wind-exposed slope index, and potential radiation index, were derived from unoccupied aerial vehicle (UAV) surveys with sub-metre resolution. We computed the variogram and the fractal dimension of the snow mechanical properties and stability metrics and compared them. The comparison showed some similarities in the correlation distances and fractal dimensions between the slab thickness and the slab snow density and also between the weak layer strength and the stability metrics. We then spatially modelled ... Article in Journal/Newspaper The Cryosphere Directory of Open Access Journals: DOAJ Articles Canada British Columbia ENVELOPE(-125.003,-125.003,54.000,54.000) The Cryosphere 18 3 1359 1380
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Environmental sciences
GE1-350
Geology
QE1-996.5
spellingShingle Environmental sciences
GE1-350
Geology
QE1-996.5
F. Meloche
F. Gauthier
A. Langlois
Snow mechanical property variability at the slope scale – implication for snow mechanical modelling
topic_facet Environmental sciences
GE1-350
Geology
QE1-996.5
description Snow avalanches represent a natural hazard to infrastructure and backcountry recreationists. Risk assessment of avalanche hazard is difficult due to the sparse nature of available observations informing on snowpack mechanical and geophysical properties and overall stability. The spatial variability of these properties also adds complexity to decision-making and route finding in avalanche terrain for mountain users. Snow cover models can simulate snow mechanical properties with good accuracy at fairly good spatial resolution (around 100 m). However, monitoring small-scale variability at the slope scale (5–50 m) remains critical, since slope stability and the possible size of an avalanche are governed by that scale. To better understand and estimate the spatial variability at the slope scale, this work explores links between snow mechanical properties and microtopographic indicators. Six spatial snow surveys were conducted in two study areas across Canada. Snow mechanical properties, such as snow density, elastic modulus and shear strength, were estimated from high-resolution snow penetrometer (SMP) profiles at multiple locations over several studied slopes, in Rogers Pass, British Columbia, and Mt. Albert, Québec. Point snow stability metrics, such as the skier crack length, critical propagation crack length and a skier stability index, were derived using the snow mechanical properties from SMP measurements. Microtopographic indicators, such as the topographic position index (TPI), vegetation height and proximity, wind-exposed slope index, and potential radiation index, were derived from unoccupied aerial vehicle (UAV) surveys with sub-metre resolution. We computed the variogram and the fractal dimension of the snow mechanical properties and stability metrics and compared them. The comparison showed some similarities in the correlation distances and fractal dimensions between the slab thickness and the slab snow density and also between the weak layer strength and the stability metrics. We then spatially modelled ...
format Article in Journal/Newspaper
author F. Meloche
F. Gauthier
A. Langlois
author_facet F. Meloche
F. Gauthier
A. Langlois
author_sort F. Meloche
title Snow mechanical property variability at the slope scale – implication for snow mechanical modelling
title_short Snow mechanical property variability at the slope scale – implication for snow mechanical modelling
title_full Snow mechanical property variability at the slope scale – implication for snow mechanical modelling
title_fullStr Snow mechanical property variability at the slope scale – implication for snow mechanical modelling
title_full_unstemmed Snow mechanical property variability at the slope scale – implication for snow mechanical modelling
title_sort snow mechanical property variability at the slope scale – implication for snow mechanical modelling
publisher Copernicus Publications
publishDate 2024
url https://doi.org/10.5194/tc-18-1359-2024
https://doaj.org/article/69759425c3864ab3b70967feb19e3d51
long_lat ENVELOPE(-125.003,-125.003,54.000,54.000)
geographic Canada
British Columbia
geographic_facet Canada
British Columbia
genre The Cryosphere
genre_facet The Cryosphere
op_source The Cryosphere, Vol 18, Pp 1359-1380 (2024)
op_relation https://tc.copernicus.org/articles/18/1359/2024/tc-18-1359-2024.pdf
https://doaj.org/toc/1994-0416
https://doaj.org/toc/1994-0424
doi:10.5194/tc-18-1359-2024
1994-0416
1994-0424
https://doaj.org/article/69759425c3864ab3b70967feb19e3d51
op_doi https://doi.org/10.5194/tc-18-1359-2024
container_title The Cryosphere
container_volume 18
container_issue 3
container_start_page 1359
op_container_end_page 1380
_version_ 1809946215418167296