Deduction of Glacier Flow from the Distribution of Elongated Bubbles

Abstract The elongation of air bubbles discovered in a wide area of a glacier surface covered by supraglacial debris does not coincide with the direction of flow. When ice samples including elongated bubbles were subjected to simple-shear experiments, the elongated bubbles deformed passively with ic...

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Published in:Journal of Glaciology
Main Author: Nakawo, Masayoshi
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1979
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000014921
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000014921
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spelling crcambridgeupr:10.1017/s0022143000014921 2024-03-03T08:45:59+00:00 Deduction of Glacier Flow from the Distribution of Elongated Bubbles Nakawo, Masayoshi 1979 http://dx.doi.org/10.1017/s0022143000014921 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000014921 en eng Cambridge University Press (CUP) Journal of Glaciology volume 24, issue 90, page 457-467 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1979 crcambridgeupr https://doi.org/10.1017/s0022143000014921 2024-02-08T08:37:11Z Abstract The elongation of air bubbles discovered in a wide area of a glacier surface covered by supraglacial debris does not coincide with the direction of flow. When ice samples including elongated bubbles were subjected to simple-shear experiments, the elongated bubbles deformed passively with ice and their final orientation was a good indicator of the strain induced in the ice. Based on these experimental results, the strain and the velocity field of the glacier were deduced from the distribution pattern of the elongated bubbles. The results agreed with the measured flow velocity. The bubble foliation pattern could also be explained in terms of the passive deformation. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 24 90 457 467
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Earth-Surface Processes
spellingShingle Earth-Surface Processes
Nakawo, Masayoshi
Deduction of Glacier Flow from the Distribution of Elongated Bubbles
topic_facet Earth-Surface Processes
description Abstract The elongation of air bubbles discovered in a wide area of a glacier surface covered by supraglacial debris does not coincide with the direction of flow. When ice samples including elongated bubbles were subjected to simple-shear experiments, the elongated bubbles deformed passively with ice and their final orientation was a good indicator of the strain induced in the ice. Based on these experimental results, the strain and the velocity field of the glacier were deduced from the distribution pattern of the elongated bubbles. The results agreed with the measured flow velocity. The bubble foliation pattern could also be explained in terms of the passive deformation.
format Article in Journal/Newspaper
author Nakawo, Masayoshi
author_facet Nakawo, Masayoshi
author_sort Nakawo, Masayoshi
title Deduction of Glacier Flow from the Distribution of Elongated Bubbles
title_short Deduction of Glacier Flow from the Distribution of Elongated Bubbles
title_full Deduction of Glacier Flow from the Distribution of Elongated Bubbles
title_fullStr Deduction of Glacier Flow from the Distribution of Elongated Bubbles
title_full_unstemmed Deduction of Glacier Flow from the Distribution of Elongated Bubbles
title_sort deduction of glacier flow from the distribution of elongated bubbles
publisher Cambridge University Press (CUP)
publishDate 1979
url http://dx.doi.org/10.1017/s0022143000014921
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000014921
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source Journal of Glaciology
volume 24, issue 90, page 457-467
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s0022143000014921
container_title Journal of Glaciology
container_volume 24
container_issue 90
container_start_page 457
op_container_end_page 467
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