A Flow Law for Temperate Glacier Ice
Abstract Uniaxial compressive creep tests were performed on polycrystalline samples of glacier ice at stresses ranging from 0.06 bar to 1.0 bar under conditions similar to those actually occurring in a temperate glacier. Tests were conducted in an ice tunnel on the Blue Glacier, Mt Olympus, Washingt...
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Language: | English |
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Cambridge University Press (CUP)
1973
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Online Access: | http://dx.doi.org/10.1017/s0022143000022711 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000022711 |
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crcambridgeupr:10.1017/s0022143000022711 2024-09-15T18:15:38+00:00 A Flow Law for Temperate Glacier Ice Colbeck, S. C. Evans, R. J. 1973 http://dx.doi.org/10.1017/s0022143000022711 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000022711 en eng Cambridge University Press (CUP) Journal of Glaciology volume 12, issue 64, page 71-86 ISSN 0022-1430 1727-5652 journal-article 1973 crcambridgeupr https://doi.org/10.1017/s0022143000022711 2024-08-14T04:02:07Z Abstract Uniaxial compressive creep tests were performed on polycrystalline samples of glacier ice at stresses ranging from 0.06 bar to 1.0 bar under conditions similar to those actually occurring in a temperate glacier. Tests were conducted in an ice tunnel on the Blue Glacier, Mt Olympus, Washington, U.S.A., thus ensuring that the temperature remained at the pressure melting point. The flow law proposed as an appropriate one-dimensional flow law for temperate glacier ice is a polynomial expression containing linear, cubic and fifth-order terms. This law provides a good fit to the data and is also consistent with the quasi-viscous creep data of Glen (1955). Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 12 64 71 86 |
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Open Polar |
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Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
description |
Abstract Uniaxial compressive creep tests were performed on polycrystalline samples of glacier ice at stresses ranging from 0.06 bar to 1.0 bar under conditions similar to those actually occurring in a temperate glacier. Tests were conducted in an ice tunnel on the Blue Glacier, Mt Olympus, Washington, U.S.A., thus ensuring that the temperature remained at the pressure melting point. The flow law proposed as an appropriate one-dimensional flow law for temperate glacier ice is a polynomial expression containing linear, cubic and fifth-order terms. This law provides a good fit to the data and is also consistent with the quasi-viscous creep data of Glen (1955). |
format |
Article in Journal/Newspaper |
author |
Colbeck, S. C. Evans, R. J. |
spellingShingle |
Colbeck, S. C. Evans, R. J. A Flow Law for Temperate Glacier Ice |
author_facet |
Colbeck, S. C. Evans, R. J. |
author_sort |
Colbeck, S. C. |
title |
A Flow Law for Temperate Glacier Ice |
title_short |
A Flow Law for Temperate Glacier Ice |
title_full |
A Flow Law for Temperate Glacier Ice |
title_fullStr |
A Flow Law for Temperate Glacier Ice |
title_full_unstemmed |
A Flow Law for Temperate Glacier Ice |
title_sort |
flow law for temperate glacier ice |
publisher |
Cambridge University Press (CUP) |
publishDate |
1973 |
url |
http://dx.doi.org/10.1017/s0022143000022711 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000022711 |
genre |
Journal of Glaciology |
genre_facet |
Journal of Glaciology |
op_source |
Journal of Glaciology volume 12, issue 64, page 71-86 ISSN 0022-1430 1727-5652 |
op_doi |
https://doi.org/10.1017/s0022143000022711 |
container_title |
Journal of Glaciology |
container_volume |
12 |
container_issue |
64 |
container_start_page |
71 |
op_container_end_page |
86 |
_version_ |
1810453511593263104 |