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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Bibliographic Details
Published in:Journal of Glaciology
Main Author: Heimgartner, M.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1977
Subjects:
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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spelling 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
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