Wave Pattern of Flowing Snow Slabs

Abstract Equations are derived, using a total potential-energy formulation, which predict the wavelength of the dominant wave pattern of a flowing snow slab. Account is taken of the visco-elastic properties of an assumed surface layer of snow which overlays a distinct visco-elastic foundation layer...

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Bibliographic Details
Published in:Journal of Glaciology
Main Author: Lang, T. E.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1977
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000029397
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000029397
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spelling crcambridgeupr:10.1017/s0022143000029397 2024-03-03T08:46:03+00:00 Wave Pattern of Flowing Snow Slabs Lang, T. E. 1977 http://dx.doi.org/10.1017/s0022143000029397 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000029397 en eng Cambridge University Press (CUP) Journal of Glaciology volume 19, issue 81, page 365-373 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1977 crcambridgeupr https://doi.org/10.1017/s0022143000029397 2024-02-08T08:36:15Z Abstract Equations are derived, using a total potential-energy formulation, which predict the wavelength of the dominant wave pattern of a flowing snow slab. Account is taken of the visco-elastic properties of an assumed surface layer of snow which overlays a distinct visco-elastic foundation layer of snow. The predicted wave pattern is recognized as a precursory mechanism which influences the characteristics of the sawtooth flank fracture pattern that may remain following a snow avalanche, particularly on broad, uniform slopes. The parameters that influence the wave pattern are determined by an order-of-magnitu de reduction of the terms in the governing differential equation for visco-elastic slab response. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 19 81 365 373
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Earth-Surface Processes
spellingShingle Earth-Surface Processes
Lang, T. E.
Wave Pattern of Flowing Snow Slabs
topic_facet Earth-Surface Processes
description Abstract Equations are derived, using a total potential-energy formulation, which predict the wavelength of the dominant wave pattern of a flowing snow slab. Account is taken of the visco-elastic properties of an assumed surface layer of snow which overlays a distinct visco-elastic foundation layer of snow. The predicted wave pattern is recognized as a precursory mechanism which influences the characteristics of the sawtooth flank fracture pattern that may remain following a snow avalanche, particularly on broad, uniform slopes. The parameters that influence the wave pattern are determined by an order-of-magnitu de reduction of the terms in the governing differential equation for visco-elastic slab response.
format Article in Journal/Newspaper
author Lang, T. E.
author_facet Lang, T. E.
author_sort Lang, T. E.
title Wave Pattern of Flowing Snow Slabs
title_short Wave Pattern of Flowing Snow Slabs
title_full Wave Pattern of Flowing Snow Slabs
title_fullStr Wave Pattern of Flowing Snow Slabs
title_full_unstemmed Wave Pattern of Flowing Snow Slabs
title_sort wave pattern of flowing snow slabs
publisher Cambridge University Press (CUP)
publishDate 1977
url http://dx.doi.org/10.1017/s0022143000029397
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000029397
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source Journal of Glaciology
volume 19, issue 81, page 365-373
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s0022143000029397
container_title Journal of Glaciology
container_volume 19
container_issue 81
container_start_page 365
op_container_end_page 373
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