A Model for Scaling Avalanche Speeds

Abstract Snow-avalanche speeds, run-out distances, and the concepts from dense granular flows are combined in a model for prediction of speeds along the incline. Field measurements indicate that speeds and run-out distances are nearly independent of path steepness once a length is chosen to scale th...

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Bibliographic Details
Published in:Journal of Glaciology
Main Author: Mcclung, D.M.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1990
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000009436
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000009436
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spelling crcambridgeupr:10.1017/s0022143000009436 2024-09-15T18:15:38+00:00 A Model for Scaling Avalanche Speeds Mcclung, D.M. 1990 http://dx.doi.org/10.1017/s0022143000009436 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000009436 en eng Cambridge University Press (CUP) Journal of Glaciology volume 36, issue 123, page 188-198 ISSN 0022-1430 1727-5652 journal-article 1990 crcambridgeupr https://doi.org/10.1017/s0022143000009436 2024-08-28T04:01:23Z Abstract Snow-avalanche speeds, run-out distances, and the concepts from dense granular flows are combined in a model for prediction of speeds along the incline. Field measurements indicate that speeds and run-out distances are nearly independent of path steepness once a length is chosen to scale them. Application of granular-flow concepts explains these results. The most important feature of the model (and the speed data) is the steep gradient of speeds in the run-out zone. These results emphasize the need for high precision in run-out prediction when construction or defences are contemplated. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 36 123 188 198
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
description Abstract Snow-avalanche speeds, run-out distances, and the concepts from dense granular flows are combined in a model for prediction of speeds along the incline. Field measurements indicate that speeds and run-out distances are nearly independent of path steepness once a length is chosen to scale them. Application of granular-flow concepts explains these results. The most important feature of the model (and the speed data) is the steep gradient of speeds in the run-out zone. These results emphasize the need for high precision in run-out prediction when construction or defences are contemplated.
format Article in Journal/Newspaper
author Mcclung, D.M.
spellingShingle Mcclung, D.M.
A Model for Scaling Avalanche Speeds
author_facet Mcclung, D.M.
author_sort Mcclung, D.M.
title A Model for Scaling Avalanche Speeds
title_short A Model for Scaling Avalanche Speeds
title_full A Model for Scaling Avalanche Speeds
title_fullStr A Model for Scaling Avalanche Speeds
title_full_unstemmed A Model for Scaling Avalanche Speeds
title_sort model for scaling avalanche speeds
publisher Cambridge University Press (CUP)
publishDate 1990
url http://dx.doi.org/10.1017/s0022143000009436
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000009436
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source Journal of Glaciology
volume 36, issue 123, page 188-198
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s0022143000009436
container_title Journal of Glaciology
container_volume 36
container_issue 123
container_start_page 188
op_container_end_page 198
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