Snow stability during rain
Abstract The mechanical response of snowpacks to penetrating liquid water was observed over two winter seasons in the central Cascade Mountains, Washington, U.S.A. Following the onset of rain, three evolutionary regimes of snow behavior were identified: immediate avalanching, delayed avalanching, an...
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Language: | English |
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Cambridge University Press (CUP)
1993
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Online Access: | http://dx.doi.org/10.1017/s0022143000016531 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000016531 |
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crcambridgeupr:10.1017/s0022143000016531 2024-09-15T18:15:39+00:00 Snow stability during rain Conway, H. Raymond, C. F. 1993 http://dx.doi.org/10.1017/s0022143000016531 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000016531 en eng Cambridge University Press (CUP) Journal of Glaciology volume 39, issue 133, page 635-642 ISSN 0022-1430 1727-5652 journal-article 1993 crcambridgeupr https://doi.org/10.1017/s0022143000016531 2024-07-10T04:04:37Z Abstract The mechanical response of snowpacks to penetrating liquid water was observed over two winter seasons in the central Cascade Mountains, Washington, U.S.A. Following the onset of rain, three evolutionary regimes of snow behavior were identified: immediate avalanching, delayed avalanching, and return to stability. Immediate avalanching occurred within minutes to an hour after the onset of rain and the time of release could be predicted with an accuracy of less than an hour from meteorological forecasts of the transition from snow to rain. These avalanches usually slid on surfaces substantially deeper than the level to which water or associated thermal effects had penetrated. The mechanism by which alteration of a thin skin of surface snow can cause deep slab failure has not been identified, but several possibilities involving a redistribution of stress are discussed. Delayed avalanches released several hours after rain started. The delay varied, depending on the rate of increasing stress associated with the additional precipitation, and on the time taken for water to penetrate and weaken a potential sliding layer. It is difficult to define accurately the evolving distribution of liquid water in snow which makes it difficult to predict accurately the time of avalanching. Depth profiles of the rate of snow settlement showed that a wave of increased strain rate propagated into the snow in response to penetrating water. This type of measurement could prove useful for predicting when snow stability is reaching a critical condition. Avalanche activity was rare after continuation of rain for 15 h or more. This return to stability occurred after drainage structures had evolved and penetrated the full depth of the snowpack. Established drain channels route water away from potential sliding surfaces and are also relatively strong structures within a snowpack. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 39 133 635 642 |
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Cambridge University Press |
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English |
description |
Abstract The mechanical response of snowpacks to penetrating liquid water was observed over two winter seasons in the central Cascade Mountains, Washington, U.S.A. Following the onset of rain, three evolutionary regimes of snow behavior were identified: immediate avalanching, delayed avalanching, and return to stability. Immediate avalanching occurred within minutes to an hour after the onset of rain and the time of release could be predicted with an accuracy of less than an hour from meteorological forecasts of the transition from snow to rain. These avalanches usually slid on surfaces substantially deeper than the level to which water or associated thermal effects had penetrated. The mechanism by which alteration of a thin skin of surface snow can cause deep slab failure has not been identified, but several possibilities involving a redistribution of stress are discussed. Delayed avalanches released several hours after rain started. The delay varied, depending on the rate of increasing stress associated with the additional precipitation, and on the time taken for water to penetrate and weaken a potential sliding layer. It is difficult to define accurately the evolving distribution of liquid water in snow which makes it difficult to predict accurately the time of avalanching. Depth profiles of the rate of snow settlement showed that a wave of increased strain rate propagated into the snow in response to penetrating water. This type of measurement could prove useful for predicting when snow stability is reaching a critical condition. Avalanche activity was rare after continuation of rain for 15 h or more. This return to stability occurred after drainage structures had evolved and penetrated the full depth of the snowpack. Established drain channels route water away from potential sliding surfaces and are also relatively strong structures within a snowpack. |
format |
Article in Journal/Newspaper |
author |
Conway, H. Raymond, C. F. |
spellingShingle |
Conway, H. Raymond, C. F. Snow stability during rain |
author_facet |
Conway, H. Raymond, C. F. |
author_sort |
Conway, H. |
title |
Snow stability during rain |
title_short |
Snow stability during rain |
title_full |
Snow stability during rain |
title_fullStr |
Snow stability during rain |
title_full_unstemmed |
Snow stability during rain |
title_sort |
snow stability during rain |
publisher |
Cambridge University Press (CUP) |
publishDate |
1993 |
url |
http://dx.doi.org/10.1017/s0022143000016531 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000016531 |
genre |
Journal of Glaciology |
genre_facet |
Journal of Glaciology |
op_source |
Journal of Glaciology volume 39, issue 133, page 635-642 ISSN 0022-1430 1727-5652 |
op_doi |
https://doi.org/10.1017/s0022143000016531 |
container_title |
Journal of Glaciology |
container_volume |
39 |
container_issue |
133 |
container_start_page |
635 |
op_container_end_page |
642 |
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1810453534479482880 |