An experimental study of the glacier boundary layer over melting ice
Abstract The results of an experiment to examine the glacier boundary layer over melting ice are described. They show that the boundary layer, as defined by the applicability of the log—linear profile, is approximately 1 m thick. The boundary layer is a frequent, but not a dominant feature of the ai...
Published in: | Journal of Glaciology |
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Language: | English |
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Cambridge University Press (CUP)
1977
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Online Access: | http://dx.doi.org/10.1017/s0022143000021109 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000021109 |
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crcambridgeupr:10.1017/s0022143000021109 2024-10-20T14:09:52+00:00 An experimental study of the glacier boundary layer over melting ice Munro, D. S. Davies, J. A. 1977 http://dx.doi.org/10.1017/s0022143000021109 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000021109 en eng Cambridge University Press (CUP) Journal of Glaciology volume 18, issue 80, page 425-436 ISSN 0022-1430 1727-5652 journal-article 1977 crcambridgeupr https://doi.org/10.1017/s0022143000021109 2024-09-25T04:01:59Z Abstract The results of an experiment to examine the glacier boundary layer over melting ice are described. They show that the boundary layer, as defined by the applicability of the log—linear profile, is approximately 1 m thick. The boundary layer is a frequent, but not a dominant feature of the air close to the ice. The frequency of occurrence is relatively high in cases where wind speeds are mainly controlled by katabatic forces. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 18 80 425 436 |
institution |
Open Polar |
collection |
Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
description |
Abstract The results of an experiment to examine the glacier boundary layer over melting ice are described. They show that the boundary layer, as defined by the applicability of the log—linear profile, is approximately 1 m thick. The boundary layer is a frequent, but not a dominant feature of the air close to the ice. The frequency of occurrence is relatively high in cases where wind speeds are mainly controlled by katabatic forces. |
format |
Article in Journal/Newspaper |
author |
Munro, D. S. Davies, J. A. |
spellingShingle |
Munro, D. S. Davies, J. A. An experimental study of the glacier boundary layer over melting ice |
author_facet |
Munro, D. S. Davies, J. A. |
author_sort |
Munro, D. S. |
title |
An experimental study of the glacier boundary layer over melting ice |
title_short |
An experimental study of the glacier boundary layer over melting ice |
title_full |
An experimental study of the glacier boundary layer over melting ice |
title_fullStr |
An experimental study of the glacier boundary layer over melting ice |
title_full_unstemmed |
An experimental study of the glacier boundary layer over melting ice |
title_sort |
experimental study of the glacier boundary layer over melting ice |
publisher |
Cambridge University Press (CUP) |
publishDate |
1977 |
url |
http://dx.doi.org/10.1017/s0022143000021109 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000021109 |
genre |
Journal of Glaciology |
genre_facet |
Journal of Glaciology |
op_source |
Journal of Glaciology volume 18, issue 80, page 425-436 ISSN 0022-1430 1727-5652 |
op_doi |
https://doi.org/10.1017/s0022143000021109 |
container_title |
Journal of Glaciology |
container_volume |
18 |
container_issue |
80 |
container_start_page |
425 |
op_container_end_page |
436 |
_version_ |
1813449523713802240 |