On the Flow of Avalanching Snow
Abstract Variation of flow depth of a flowing avalanche caused by a change in the slope angle is examined using Bernoulli’s energy equation, used in hydraulics to determine a non-uniform steady flow. This equation is modified for a material with internal friction and a strongly curved track. The cal...
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Language: | English |
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Cambridge University Press (CUP)
1977
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Online Access: | http://dx.doi.org/10.1017/s0022143000029385 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000029385 |
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crcambridgeupr:10.1017/s0022143000029385 2024-03-03T08:46:02+00:00 On the Flow of Avalanching Snow Heimgartner, M. 1977 http://dx.doi.org/10.1017/s0022143000029385 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000029385 en eng Cambridge University Press (CUP) Journal of Glaciology volume 19, issue 81, page 357-363 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1977 crcambridgeupr https://doi.org/10.1017/s0022143000029385 2024-02-08T08:37:11Z Abstract Variation of flow depth of a flowing avalanche caused by a change in the slope angle is examined using Bernoulli’s energy equation, used in hydraulics to determine a non-uniform steady flow. This equation is modified for a material with internal friction and a strongly curved track. The calculated flow depths are compared with those obtained by tests with a snow slide. In the flow model dry and turbulent friction are taken into account. Friction coefficients are estimated comparing calculated and measured flow depths. It appears that in wet snow they differ from those of dry snow. Finally, this model is used to calculate the runout distance of a natural avalanche. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 19 81 357 363 |
institution |
Open Polar |
collection |
Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
topic |
Earth-Surface Processes |
spellingShingle |
Earth-Surface Processes Heimgartner, M. On the Flow of Avalanching Snow |
topic_facet |
Earth-Surface Processes |
description |
Abstract Variation of flow depth of a flowing avalanche caused by a change in the slope angle is examined using Bernoulli’s energy equation, used in hydraulics to determine a non-uniform steady flow. This equation is modified for a material with internal friction and a strongly curved track. The calculated flow depths are compared with those obtained by tests with a snow slide. In the flow model dry and turbulent friction are taken into account. Friction coefficients are estimated comparing calculated and measured flow depths. It appears that in wet snow they differ from those of dry snow. Finally, this model is used to calculate the runout distance of a natural avalanche. |
format |
Article in Journal/Newspaper |
author |
Heimgartner, M. |
author_facet |
Heimgartner, M. |
author_sort |
Heimgartner, M. |
title |
On the Flow of Avalanching Snow |
title_short |
On the Flow of Avalanching Snow |
title_full |
On the Flow of Avalanching Snow |
title_fullStr |
On the Flow of Avalanching Snow |
title_full_unstemmed |
On the Flow of Avalanching Snow |
title_sort |
on the flow of avalanching snow |
publisher |
Cambridge University Press (CUP) |
publishDate |
1977 |
url |
http://dx.doi.org/10.1017/s0022143000029385 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000029385 |
genre |
Journal of Glaciology |
genre_facet |
Journal of Glaciology |
op_source |
Journal of Glaciology volume 19, issue 81, page 357-363 ISSN 0022-1430 1727-5652 |
op_doi |
https://doi.org/10.1017/s0022143000029385 |
container_title |
Journal of Glaciology |
container_volume |
19 |
container_issue |
81 |
container_start_page |
357 |
op_container_end_page |
363 |
_version_ |
1792501850666172416 |