On The Use of Tensiometers in Snow Hydrology
Abstract The construction and use of snow-water tensiometers is gerscribed. Water pressure at the base of a shallow, Arctic snow-pack was measured to illustrate the response of the basal layer to water percolation. Water tension above an ice layer and water flux through the ice layer were measured i...
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Language: | English |
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Cambridge University Press (CUP)
1976
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Online Access: | http://dx.doi.org/10.1017/s0022143000030793 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000030793 |
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crcambridgeupr:10.1017/s0022143000030793 2024-03-03T08:41:52+00:00 On The Use of Tensiometers in Snow Hydrology Colbeck, S. C. 1976 http://dx.doi.org/10.1017/s0022143000030793 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000030793 en eng Cambridge University Press (CUP) Journal of Glaciology volume 17, issue 75, page 135-140 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1976 crcambridgeupr https://doi.org/10.1017/s0022143000030793 2024-02-08T08:32:56Z Abstract The construction and use of snow-water tensiometers is gerscribed. Water pressure at the base of a shallow, Arctic snow-pack was measured to illustrate the response of the basal layer to water percolation. Water tension above an ice layer and water flux through the ice layer were measured in glacial snow. The gravity flow theory is used to explain the close agreement between these parameters. This suggests that the ice layer has little effect on the flow field and that gravity (rather than tension gradients) controls the flow. Further work on water tensions is neegerd to igerntify the role of tension gradients in ripening and shallow snow covers. Article in Journal/Newspaper Arctic Journal of Glaciology Cambridge University Press Arctic Journal of Glaciology 17 75 135 140 |
institution |
Open Polar |
collection |
Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
topic |
Earth-Surface Processes |
spellingShingle |
Earth-Surface Processes Colbeck, S. C. On The Use of Tensiometers in Snow Hydrology |
topic_facet |
Earth-Surface Processes |
description |
Abstract The construction and use of snow-water tensiometers is gerscribed. Water pressure at the base of a shallow, Arctic snow-pack was measured to illustrate the response of the basal layer to water percolation. Water tension above an ice layer and water flux through the ice layer were measured in glacial snow. The gravity flow theory is used to explain the close agreement between these parameters. This suggests that the ice layer has little effect on the flow field and that gravity (rather than tension gradients) controls the flow. Further work on water tensions is neegerd to igerntify the role of tension gradients in ripening and shallow snow covers. |
format |
Article in Journal/Newspaper |
author |
Colbeck, S. C. |
author_facet |
Colbeck, S. C. |
author_sort |
Colbeck, S. C. |
title |
On The Use of Tensiometers in Snow Hydrology |
title_short |
On The Use of Tensiometers in Snow Hydrology |
title_full |
On The Use of Tensiometers in Snow Hydrology |
title_fullStr |
On The Use of Tensiometers in Snow Hydrology |
title_full_unstemmed |
On The Use of Tensiometers in Snow Hydrology |
title_sort |
on the use of tensiometers in snow hydrology |
publisher |
Cambridge University Press (CUP) |
publishDate |
1976 |
url |
http://dx.doi.org/10.1017/s0022143000030793 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000030793 |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic Journal of Glaciology |
genre_facet |
Arctic Journal of Glaciology |
op_source |
Journal of Glaciology volume 17, issue 75, page 135-140 ISSN 0022-1430 1727-5652 |
op_doi |
https://doi.org/10.1017/s0022143000030793 |
container_title |
Journal of Glaciology |
container_volume |
17 |
container_issue |
75 |
container_start_page |
135 |
op_container_end_page |
140 |
_version_ |
1792497425955422208 |