Wind-tunnel study of snowdrift around avalanche defence structures

Avalanche defence structures such as retarding dams and breaking mounds are widely used to protect residential areas and other kinds of infrastructure. The effect of the defence structures depends largely on their effective height relative to the velocity, volume and flow depth of the avalanche. Sno...

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Published in:Annals of Glaciology
Main Authors: Jaedicke, Christian, Naaim-Bouvet, Florence, Granig, Matthias
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press 2004
Subjects:
Online Access:https://hdl.handle.net/11250/3098803
https://doi.org/10.3189/172756404781814799
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spelling ftngi:oai:ngi.brage.unit.no:11250/3098803 2023-11-12T04:01:18+01:00 Wind-tunnel study of snowdrift around avalanche defence structures Jaedicke, Christian Naaim-Bouvet, Florence Granig, Matthias 2004 application/pdf https://hdl.handle.net/11250/3098803 https://doi.org/10.3189/172756404781814799 eng eng Cambridge University Press urn:issn:0260-3055 https://hdl.handle.net/11250/3098803 https://doi.org/10.3189/172756404781814799 The Author(s) 325-330 38 Annals of Glaciology Avalanche-RnD Snøskred-FoU Journal article 2004 ftngi https://doi.org/10.3189/172756404781814799 2023-11-01T23:48:58Z Avalanche defence structures such as retarding dams and breaking mounds are widely used to protect residential areas and other kinds of infrastructure. The effect of the defence structures depends largely on their effective height relative to the velocity, volume and flow depth of the avalanche. Snow depositions from earlier avalanches as well as from drifting snow can significantly alter the effective height of defence structures. Different designs of avalanche-breaking mounds and retarding dams were tested in the Cemagref (Grenoble, France) wind tunnel for their effect on drifting snow. Examples included dams and mounds of different sizes and heights. The models were tested in a wind tunnel with sand particles subjected to different wind directions. The resulting depositions were scanned with a laser system to obtain a three-dimensional picture of the accumulation pattern. The results show that the accumulated snow varies widely with the design of the structure for a given wind direction. Most snow is accumulated around narrow mounds, with least accumulation observed around mounds covering a smaller relative area of the avalanche path. The data obtained can be used to study the effect of the depositions on the retarding effect of the avalanche defence structures. However, because the similarity criteria for studying the interaction between structures and saltating particles in a wind tunnel cannot be met, the transfer of the results to reality must be performed with caution. Article in Journal/Newspaper Annals of Glaciology Norwegian Geotechnical Institute (NGI) Digital Archive Annals of Glaciology 38 325 330
institution Open Polar
collection Norwegian Geotechnical Institute (NGI) Digital Archive
op_collection_id ftngi
language English
topic Avalanche-RnD
Snøskred-FoU
spellingShingle Avalanche-RnD
Snøskred-FoU
Jaedicke, Christian
Naaim-Bouvet, Florence
Granig, Matthias
Wind-tunnel study of snowdrift around avalanche defence structures
topic_facet Avalanche-RnD
Snøskred-FoU
description Avalanche defence structures such as retarding dams and breaking mounds are widely used to protect residential areas and other kinds of infrastructure. The effect of the defence structures depends largely on their effective height relative to the velocity, volume and flow depth of the avalanche. Snow depositions from earlier avalanches as well as from drifting snow can significantly alter the effective height of defence structures. Different designs of avalanche-breaking mounds and retarding dams were tested in the Cemagref (Grenoble, France) wind tunnel for their effect on drifting snow. Examples included dams and mounds of different sizes and heights. The models were tested in a wind tunnel with sand particles subjected to different wind directions. The resulting depositions were scanned with a laser system to obtain a three-dimensional picture of the accumulation pattern. The results show that the accumulated snow varies widely with the design of the structure for a given wind direction. Most snow is accumulated around narrow mounds, with least accumulation observed around mounds covering a smaller relative area of the avalanche path. The data obtained can be used to study the effect of the depositions on the retarding effect of the avalanche defence structures. However, because the similarity criteria for studying the interaction between structures and saltating particles in a wind tunnel cannot be met, the transfer of the results to reality must be performed with caution.
format Article in Journal/Newspaper
author Jaedicke, Christian
Naaim-Bouvet, Florence
Granig, Matthias
author_facet Jaedicke, Christian
Naaim-Bouvet, Florence
Granig, Matthias
author_sort Jaedicke, Christian
title Wind-tunnel study of snowdrift around avalanche defence structures
title_short Wind-tunnel study of snowdrift around avalanche defence structures
title_full Wind-tunnel study of snowdrift around avalanche defence structures
title_fullStr Wind-tunnel study of snowdrift around avalanche defence structures
title_full_unstemmed Wind-tunnel study of snowdrift around avalanche defence structures
title_sort wind-tunnel study of snowdrift around avalanche defence structures
publisher Cambridge University Press
publishDate 2004
url https://hdl.handle.net/11250/3098803
https://doi.org/10.3189/172756404781814799
genre Annals of Glaciology
genre_facet Annals of Glaciology
op_source 325-330
38
Annals of Glaciology
op_relation urn:issn:0260-3055
https://hdl.handle.net/11250/3098803
https://doi.org/10.3189/172756404781814799
op_rights The Author(s)
op_doi https://doi.org/10.3189/172756404781814799
container_title Annals of Glaciology
container_volume 38
container_start_page 325
op_container_end_page 330
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