Snow Forces

Abstract Snow forces are understood as forces originating from a very slow motion of the seasonal snow cover and acting on boundaries confining it. They depend on the total water-equivalent (a statistical magnitude with a certain probability of occurrence) and on mechanical characteristics of snow....

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Published in:Journal of Glaciology
Main Author: Salm, Bruno
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1977
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000029221
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000029221
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spelling crcambridgeupr:10.1017/s0022143000029221 2024-09-15T18:15:38+00:00 Snow Forces Salm, Bruno 1977 http://dx.doi.org/10.1017/s0022143000029221 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000029221 en eng Cambridge University Press (CUP) Journal of Glaciology volume 19, issue 81, page 67-100 ISSN 0022-1430 1727-5652 journal-article 1977 crcambridgeupr https://doi.org/10.1017/s0022143000029221 2024-07-24T04:03:49Z Abstract Snow forces are understood as forces originating from a very slow motion of the seasonal snow cover and acting on boundaries confining it. They depend on the total water-equivalent (a statistical magnitude with a certain probability of occurrence) and on mechanical characteristics of snow. The approximation of considering of snow as a Newtonian liquid fits the requirements for applications best. In this the only mechanical characteristics to be taken into account, besides density, are shear viscosity and Poisson’s ratio. They depend strongly on the snow structure. Generalizations are shown in which the snow cover is subdivided into layers having constant (Newtonian) properties. Non-Newtonian behaviour is also mentioned. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 19 81 67 100
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
description Abstract Snow forces are understood as forces originating from a very slow motion of the seasonal snow cover and acting on boundaries confining it. They depend on the total water-equivalent (a statistical magnitude with a certain probability of occurrence) and on mechanical characteristics of snow. The approximation of considering of snow as a Newtonian liquid fits the requirements for applications best. In this the only mechanical characteristics to be taken into account, besides density, are shear viscosity and Poisson’s ratio. They depend strongly on the snow structure. Generalizations are shown in which the snow cover is subdivided into layers having constant (Newtonian) properties. Non-Newtonian behaviour is also mentioned.
format Article in Journal/Newspaper
author Salm, Bruno
spellingShingle Salm, Bruno
Snow Forces
author_facet Salm, Bruno
author_sort Salm, Bruno
title Snow Forces
title_short Snow Forces
title_full Snow Forces
title_fullStr Snow Forces
title_full_unstemmed Snow Forces
title_sort snow forces
publisher Cambridge University Press (CUP)
publishDate 1977
url http://dx.doi.org/10.1017/s0022143000029221
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000029221
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source Journal of Glaciology
volume 19, issue 81, page 67-100
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s0022143000029221
container_title Journal of Glaciology
container_volume 19
container_issue 81
container_start_page 67
op_container_end_page 100
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