Simulated Glacier Sliding over an Obstacle

Abstract The sliding of temperate ice over two obstacles with sine-wave profiles (wavelength, 0.53 m; maximum slope, 0.22) and low thermal conductivity has been reproduced at full scale within a steel chamber. As expected, large cavities form between the ice and the obstacles so that the drag is lim...

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Published in:Journal of Glaciology
Main Author: Brepson, R.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1979
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000029798
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000029798
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spelling crcambridgeupr:10.1017/s0022143000029798 2024-04-28T08:26:45+00:00 Simulated Glacier Sliding over an Obstacle Brepson, R. 1979 http://dx.doi.org/10.1017/s0022143000029798 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000029798 en eng Cambridge University Press (CUP) Journal of Glaciology volume 23, issue 89, page 143-156 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1979 crcambridgeupr https://doi.org/10.1017/s0022143000029798 2024-04-09T06:56:14Z Abstract The sliding of temperate ice over two obstacles with sine-wave profiles (wavelength, 0.53 m; maximum slope, 0.22) and low thermal conductivity has been reproduced at full scale within a steel chamber. As expected, large cavities form between the ice and the obstacles so that the drag is limited. However, the delayed elasticity of bubbly ice modifies the expected behaviour. At the base of the ice a fine-grained, bubble-free blue ice layer develops. The shear strain concentrates on the up-stream side of bumps and in the blue ice layer. Tap-water ions enhance tertiary creep-rates. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 23 89 143 156
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Earth-Surface Processes
spellingShingle Earth-Surface Processes
Brepson, R.
Simulated Glacier Sliding over an Obstacle
topic_facet Earth-Surface Processes
description Abstract The sliding of temperate ice over two obstacles with sine-wave profiles (wavelength, 0.53 m; maximum slope, 0.22) and low thermal conductivity has been reproduced at full scale within a steel chamber. As expected, large cavities form between the ice and the obstacles so that the drag is limited. However, the delayed elasticity of bubbly ice modifies the expected behaviour. At the base of the ice a fine-grained, bubble-free blue ice layer develops. The shear strain concentrates on the up-stream side of bumps and in the blue ice layer. Tap-water ions enhance tertiary creep-rates.
format Article in Journal/Newspaper
author Brepson, R.
author_facet Brepson, R.
author_sort Brepson, R.
title Simulated Glacier Sliding over an Obstacle
title_short Simulated Glacier Sliding over an Obstacle
title_full Simulated Glacier Sliding over an Obstacle
title_fullStr Simulated Glacier Sliding over an Obstacle
title_full_unstemmed Simulated Glacier Sliding over an Obstacle
title_sort simulated glacier sliding over an obstacle
publisher Cambridge University Press (CUP)
publishDate 1979
url http://dx.doi.org/10.1017/s0022143000029798
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000029798
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source Journal of Glaciology
volume 23, issue 89, page 143-156
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s0022143000029798
container_title Journal of Glaciology
container_volume 23
container_issue 89
container_start_page 143
op_container_end_page 156
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