Apparent Short-Term Glacier Velocity Variations
Abstract In connection with a glacier-hydrological project at a sub-polar glacier in West Greenland, short-term glacier velocity variations were measured. Both the horizontal and the vertical velocity components showed distinct diurnal variations. Close examination indicates that these variations ar...
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Language: | English |
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Cambridge University Press (CUP)
1985
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Online Access: | http://dx.doi.org/10.1017/s0022143000004986 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000004986 |
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crcambridgeupr:10.1017/s0022143000004986 2024-03-03T08:44:35+00:00 Apparent Short-Term Glacier Velocity Variations Andreasen, Jørn-Ole 1985 http://dx.doi.org/10.1017/s0022143000004986 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000004986 en eng Cambridge University Press (CUP) Journal of Glaciology volume 31, issue 107, page 49-53 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1985 crcambridgeupr https://doi.org/10.1017/s0022143000004986 2024-02-08T08:40:37Z Abstract In connection with a glacier-hydrological project at a sub-polar glacier in West Greenland, short-term glacier velocity variations were measured. Both the horizontal and the vertical velocity components showed distinct diurnal variations. Close examination indicates that these variations are caused by the change in atmospheric refraction during the day, with the vertical component as the most important. Article in Journal/Newspaper glacier Greenland Journal of Glaciology Cambridge University Press Greenland Journal of Glaciology 31 107 49 53 |
institution |
Open Polar |
collection |
Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
topic |
Earth-Surface Processes |
spellingShingle |
Earth-Surface Processes Andreasen, Jørn-Ole Apparent Short-Term Glacier Velocity Variations |
topic_facet |
Earth-Surface Processes |
description |
Abstract In connection with a glacier-hydrological project at a sub-polar glacier in West Greenland, short-term glacier velocity variations were measured. Both the horizontal and the vertical velocity components showed distinct diurnal variations. Close examination indicates that these variations are caused by the change in atmospheric refraction during the day, with the vertical component as the most important. |
format |
Article in Journal/Newspaper |
author |
Andreasen, Jørn-Ole |
author_facet |
Andreasen, Jørn-Ole |
author_sort |
Andreasen, Jørn-Ole |
title |
Apparent Short-Term Glacier Velocity Variations |
title_short |
Apparent Short-Term Glacier Velocity Variations |
title_full |
Apparent Short-Term Glacier Velocity Variations |
title_fullStr |
Apparent Short-Term Glacier Velocity Variations |
title_full_unstemmed |
Apparent Short-Term Glacier Velocity Variations |
title_sort |
apparent short-term glacier velocity variations |
publisher |
Cambridge University Press (CUP) |
publishDate |
1985 |
url |
http://dx.doi.org/10.1017/s0022143000004986 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000004986 |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
glacier Greenland Journal of Glaciology |
genre_facet |
glacier Greenland Journal of Glaciology |
op_source |
Journal of Glaciology volume 31, issue 107, page 49-53 ISSN 0022-1430 1727-5652 |
op_doi |
https://doi.org/10.1017/s0022143000004986 |
container_title |
Journal of Glaciology |
container_volume |
31 |
container_issue |
107 |
container_start_page |
49 |
op_container_end_page |
53 |
_version_ |
1792500082880282624 |