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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Cambridge University Press (CUP)
1990
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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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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 |
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Open Polar |
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Cambridge University Press |
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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 |
_version_ |
1810453507228041216 |