Finite-Element Analysis of Snow on Slopes
Abstract This study describes the application of an incremental rheological law for snow in a finite-element model. The computation simulates the variation of strains and stresses in a layer of snow covering an inclined plane of variable slope. At the same time, a physical simulation was carried out...
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Language: | English |
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Cambridge University Press (CUP)
1980
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Online Access: | http://dx.doi.org/10.1017/s0022143000011072 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000011072 |
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crcambridgeupr:10.1017/s0022143000011072 2024-03-03T08:45:57+00:00 Finite-Element Analysis of Snow on Slopes Navarre, J. P. Desrues, J. 1980 http://dx.doi.org/10.1017/s0022143000011072 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000011072 en eng Cambridge University Press (CUP) Journal of Glaciology volume 26, issue 94, page 516 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1980 crcambridgeupr https://doi.org/10.1017/s0022143000011072 2024-02-08T08:40:23Z Abstract This study describes the application of an incremental rheological law for snow in a finite-element model. The computation simulates the variation of strains and stresses in a layer of snow covering an inclined plane of variable slope. At the same time, a physical simulation was carried out in a cold room to verify the results obtained with the model. This work illustrates the value of a finite-element model for snow, but also the complications attendant on its use. Indeed, the integration of the law may lead to oscillations due to the rate of variation of the stresses, and this means that the time increment must be modulated during the computation. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 26 94 516 |
institution |
Open Polar |
collection |
Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
topic |
Earth-Surface Processes |
spellingShingle |
Earth-Surface Processes Navarre, J. P. Desrues, J. Finite-Element Analysis of Snow on Slopes |
topic_facet |
Earth-Surface Processes |
description |
Abstract This study describes the application of an incremental rheological law for snow in a finite-element model. The computation simulates the variation of strains and stresses in a layer of snow covering an inclined plane of variable slope. At the same time, a physical simulation was carried out in a cold room to verify the results obtained with the model. This work illustrates the value of a finite-element model for snow, but also the complications attendant on its use. Indeed, the integration of the law may lead to oscillations due to the rate of variation of the stresses, and this means that the time increment must be modulated during the computation. |
format |
Article in Journal/Newspaper |
author |
Navarre, J. P. Desrues, J. |
author_facet |
Navarre, J. P. Desrues, J. |
author_sort |
Navarre, J. P. |
title |
Finite-Element Analysis of Snow on Slopes |
title_short |
Finite-Element Analysis of Snow on Slopes |
title_full |
Finite-Element Analysis of Snow on Slopes |
title_fullStr |
Finite-Element Analysis of Snow on Slopes |
title_full_unstemmed |
Finite-Element Analysis of Snow on Slopes |
title_sort |
finite-element analysis of snow on slopes |
publisher |
Cambridge University Press (CUP) |
publishDate |
1980 |
url |
http://dx.doi.org/10.1017/s0022143000011072 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000011072 |
genre |
Journal of Glaciology |
genre_facet |
Journal of Glaciology |
op_source |
Journal of Glaciology volume 26, issue 94, page 516 ISSN 0022-1430 1727-5652 |
op_doi |
https://doi.org/10.1017/s0022143000011072 |
container_title |
Journal of Glaciology |
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26 |
container_issue |
94 |
container_start_page |
516 |
_version_ |
1792501653895643136 |