The spatial variability of snow resistance on potential avalanche slopes

Abstract Since snow avalanches are believed to release from zones of localized weakness, knowledge of snow-strength patterns is important for determining slope stability and for applying effective avalanche-control measures. In this study, the spatial variability of snow resistance (an index of snow...

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Published in:Journal of Glaciology
Main Authors: Birkeland, K. W., Hansen, K.J., Brown, R. L.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1995
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000017871
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000017871
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spelling crcambridgeupr:10.1017/s0022143000017871 2024-04-07T07:53:42+00:00 The spatial variability of snow resistance on potential avalanche slopes Birkeland, K. W. Hansen, K.J. Brown, R. L. 1995 http://dx.doi.org/10.1017/s0022143000017871 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000017871 en eng Cambridge University Press (CUP) Journal of Glaciology volume 41, issue 137, page 183-190 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1995 crcambridgeupr https://doi.org/10.1017/s0022143000017871 2024-03-08T00:36:25Z Abstract Since snow avalanches are believed to release from zones of localized weakness, knowledge of snow-strength patterns is important for determining slope stability and for applying effective avalanche-control measures. In this study, the spatial variability of snow resistance (an index of snow strength) and depth were measured and compared with terrain features on two inclined slopes. A refined instrument allowed the strength of an entire snow slab to be characterized in a short time. The spatial pattern of trees appeared to affect the pattern of snow depth at one site, where a significant linear relationship was found between snow depth and average snow resistance. These results suggest that localized snow-depth variations may be important in snow-strength genesis. Although a linear relationship existed at that site, additional factors may be critically relevant. A second site with more complex terrain features and less localized wind drifting did not show a linear relationship between depth and average resistance. Instead, complex patterns of resistance demonstrated that many factors contribute to snow resistance. In particular, die snow overlying rocks was found to have significantly weaker resistance than that in adjacent areas not over rocks. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 41 137 183 190
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Earth-Surface Processes
spellingShingle Earth-Surface Processes
Birkeland, K. W.
Hansen, K.J.
Brown, R. L.
The spatial variability of snow resistance on potential avalanche slopes
topic_facet Earth-Surface Processes
description Abstract Since snow avalanches are believed to release from zones of localized weakness, knowledge of snow-strength patterns is important for determining slope stability and for applying effective avalanche-control measures. In this study, the spatial variability of snow resistance (an index of snow strength) and depth were measured and compared with terrain features on two inclined slopes. A refined instrument allowed the strength of an entire snow slab to be characterized in a short time. The spatial pattern of trees appeared to affect the pattern of snow depth at one site, where a significant linear relationship was found between snow depth and average snow resistance. These results suggest that localized snow-depth variations may be important in snow-strength genesis. Although a linear relationship existed at that site, additional factors may be critically relevant. A second site with more complex terrain features and less localized wind drifting did not show a linear relationship between depth and average resistance. Instead, complex patterns of resistance demonstrated that many factors contribute to snow resistance. In particular, die snow overlying rocks was found to have significantly weaker resistance than that in adjacent areas not over rocks.
format Article in Journal/Newspaper
author Birkeland, K. W.
Hansen, K.J.
Brown, R. L.
author_facet Birkeland, K. W.
Hansen, K.J.
Brown, R. L.
author_sort Birkeland, K. W.
title The spatial variability of snow resistance on potential avalanche slopes
title_short The spatial variability of snow resistance on potential avalanche slopes
title_full The spatial variability of snow resistance on potential avalanche slopes
title_fullStr The spatial variability of snow resistance on potential avalanche slopes
title_full_unstemmed The spatial variability of snow resistance on potential avalanche slopes
title_sort spatial variability of snow resistance on potential avalanche slopes
publisher Cambridge University Press (CUP)
publishDate 1995
url http://dx.doi.org/10.1017/s0022143000017871
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000017871
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source Journal of Glaciology
volume 41, issue 137, page 183-190
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s0022143000017871
container_title Journal of Glaciology
container_volume 41
container_issue 137
container_start_page 183
op_container_end_page 190
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