Temperature Measurements in a Temperate Glacier
Temperatures have been measured at two sites in a temperate glacier (Blue Glacier, Washington, U.S.A.) to depths of 192 and 76 m. The accuracy, which varies between about 0.002 and 0.005 deg, is about an order of magnitude better than previously obtained. Except near the surface, temperatures vary l...
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Language: | English |
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Cambridge University Press (CUP)
1975
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Online Access: | http://dx.doi.org/10.1017/s0022143000013356 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000013356 |
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crcambridgeupr:10.1017/s0022143000013356 2024-09-09T19:49:01+00:00 Temperature Measurements in a Temperate Glacier Harrison, W. D. 1975 http://dx.doi.org/10.1017/s0022143000013356 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000013356 en eng Cambridge University Press (CUP) Journal of Glaciology volume 14, issue 70, page 23-30 ISSN 0022-1430 1727-5652 journal-article 1975 crcambridgeupr https://doi.org/10.1017/s0022143000013356 2024-06-26T04:04:16Z Temperatures have been measured at two sites in a temperate glacier (Blue Glacier, Washington, U.S.A.) to depths of 192 and 76 m. The accuracy, which varies between about 0.002 and 0.005 deg, is about an order of magnitude better than previously obtained. Except near the surface, temperatures vary linearly with depth but are in disagreement with the simplest model of a temperate glacier, being about 0.02 deg colder near the surface and 0.04 deg colder at 192 m depth. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Blue Glacier ENVELOPE(164.167,164.167,-77.833,-77.833) Journal of Glaciology 14 70 23 30 |
institution |
Open Polar |
collection |
Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
description |
Temperatures have been measured at two sites in a temperate glacier (Blue Glacier, Washington, U.S.A.) to depths of 192 and 76 m. The accuracy, which varies between about 0.002 and 0.005 deg, is about an order of magnitude better than previously obtained. Except near the surface, temperatures vary linearly with depth but are in disagreement with the simplest model of a temperate glacier, being about 0.02 deg colder near the surface and 0.04 deg colder at 192 m depth. |
format |
Article in Journal/Newspaper |
author |
Harrison, W. D. |
spellingShingle |
Harrison, W. D. Temperature Measurements in a Temperate Glacier |
author_facet |
Harrison, W. D. |
author_sort |
Harrison, W. D. |
title |
Temperature Measurements in a Temperate Glacier |
title_short |
Temperature Measurements in a Temperate Glacier |
title_full |
Temperature Measurements in a Temperate Glacier |
title_fullStr |
Temperature Measurements in a Temperate Glacier |
title_full_unstemmed |
Temperature Measurements in a Temperate Glacier |
title_sort |
temperature measurements in a temperate glacier |
publisher |
Cambridge University Press (CUP) |
publishDate |
1975 |
url |
http://dx.doi.org/10.1017/s0022143000013356 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000013356 |
long_lat |
ENVELOPE(164.167,164.167,-77.833,-77.833) |
geographic |
Blue Glacier |
geographic_facet |
Blue Glacier |
genre |
Journal of Glaciology |
genre_facet |
Journal of Glaciology |
op_source |
Journal of Glaciology volume 14, issue 70, page 23-30 ISSN 0022-1430 1727-5652 |
op_doi |
https://doi.org/10.1017/s0022143000013356 |
container_title |
Journal of Glaciology |
container_volume |
14 |
container_issue |
70 |
container_start_page |
23 |
op_container_end_page |
30 |
_version_ |
1809918372239900672 |