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...

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Published in:Journal of Glaciology
Main Authors: Munro, D. S., Davies, J. A.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1977
Subjects:
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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spelling 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
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