Regelation and the Deformation of Wet Snow

Abstract The thermodynamics of phase equilibrium control the temperature distribution around the ice particles in wet snow. When the snow is stressed, pressure melting occurs at the inter-particle contacts and the snow densifies. Densification is described by a physical model which simulates the hea...

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Bibliographic Details
Published in:Journal of Glaciology
Main Authors: Colbeck, S. C., Parssinen, N.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1978
Subjects:
Online Access:http://dx.doi.org/10.1017/s002214300003375x
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S002214300003375X
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spelling crcambridgeupr:10.1017/s002214300003375x 2024-03-03T08:46:08+00:00 Regelation and the Deformation of Wet Snow Colbeck, S. C. Parssinen, N. 1978 http://dx.doi.org/10.1017/s002214300003375x https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S002214300003375X en eng Cambridge University Press (CUP) Journal of Glaciology volume 21, issue 85, page 639-650 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1978 crcambridgeupr https://doi.org/10.1017/s002214300003375x 2024-02-08T08:47:47Z Abstract The thermodynamics of phase equilibrium control the temperature distribution around the ice particles in wet snow. When the snow is stressed, pressure melting occurs at the inter-particle contacts and the snow densifies. Densification is described by a physical model which simulates the heat flow, meltwater flow, and particle geometry. The effects of ionic impurities, liquid saturation, and particle size are demonstrated. Typical values of the temperature difference, inter-particle film size, and density are calculated as functions of time. The calculated rates of compaction are too large, hence, at some later time, the effects of simultaneous grain growth must be added to the model. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 21 85 639 650
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Earth-Surface Processes
spellingShingle Earth-Surface Processes
Colbeck, S. C.
Parssinen, N.
Regelation and the Deformation of Wet Snow
topic_facet Earth-Surface Processes
description Abstract The thermodynamics of phase equilibrium control the temperature distribution around the ice particles in wet snow. When the snow is stressed, pressure melting occurs at the inter-particle contacts and the snow densifies. Densification is described by a physical model which simulates the heat flow, meltwater flow, and particle geometry. The effects of ionic impurities, liquid saturation, and particle size are demonstrated. Typical values of the temperature difference, inter-particle film size, and density are calculated as functions of time. The calculated rates of compaction are too large, hence, at some later time, the effects of simultaneous grain growth must be added to the model.
format Article in Journal/Newspaper
author Colbeck, S. C.
Parssinen, N.
author_facet Colbeck, S. C.
Parssinen, N.
author_sort Colbeck, S. C.
title Regelation and the Deformation of Wet Snow
title_short Regelation and the Deformation of Wet Snow
title_full Regelation and the Deformation of Wet Snow
title_fullStr Regelation and the Deformation of Wet Snow
title_full_unstemmed Regelation and the Deformation of Wet Snow
title_sort regelation and the deformation of wet snow
publisher Cambridge University Press (CUP)
publishDate 1978
url http://dx.doi.org/10.1017/s002214300003375x
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S002214300003375X
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source Journal of Glaciology
volume 21, issue 85, page 639-650
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s002214300003375x
container_title Journal of Glaciology
container_volume 21
container_issue 85
container_start_page 639
op_container_end_page 650
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