Ongoing margin migration of Ice Stream B, Antarctica
Abstract The rate of margin migration of an ice stream can be determined using repeat measurements of the surface velocity profile within the marginal shear zone. The method relies on the assumption that the velocity profile is a characteristic feature of the margin, and that this profile is shifted...
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Language: | English |
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Cambridge University Press (CUP)
1999
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Online Access: | http://dx.doi.org/10.1017/s0022143000001866 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000001866 |
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crcambridgeupr:10.1017/s0022143000001866 2024-03-03T08:37:35+00:00 Ongoing margin migration of Ice Stream B, Antarctica Echelmeyer, K. A. Harrison, W. D. 1999 http://dx.doi.org/10.1017/s0022143000001866 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000001866 en eng Cambridge University Press (CUP) Journal of Glaciology volume 45, issue 150, page 361-369 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1999 crcambridgeupr https://doi.org/10.1017/s0022143000001866 2024-02-08T08:36:10Z Abstract The rate of margin migration of an ice stream can be determined using repeat measurements of the surface velocity profile within the marginal shear zone. The method relies on the assumption that the velocity profile is a characteristic feature of the margin, and that this profile is shifted laterally as the margin migrates. Application of the method to Ice Stream B, Antarctica, indicates that the southern margin is moving outward into the inland ice at a rate of at least 9.7 ± 1.1 m a −1 . Article in Journal/Newspaper Antarc* Antarctica Ice Stream B Journal of Glaciology Cambridge University Press Journal of Glaciology 45 150 361 369 |
institution |
Open Polar |
collection |
Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
topic |
Earth-Surface Processes |
spellingShingle |
Earth-Surface Processes Echelmeyer, K. A. Harrison, W. D. Ongoing margin migration of Ice Stream B, Antarctica |
topic_facet |
Earth-Surface Processes |
description |
Abstract The rate of margin migration of an ice stream can be determined using repeat measurements of the surface velocity profile within the marginal shear zone. The method relies on the assumption that the velocity profile is a characteristic feature of the margin, and that this profile is shifted laterally as the margin migrates. Application of the method to Ice Stream B, Antarctica, indicates that the southern margin is moving outward into the inland ice at a rate of at least 9.7 ± 1.1 m a −1 . |
format |
Article in Journal/Newspaper |
author |
Echelmeyer, K. A. Harrison, W. D. |
author_facet |
Echelmeyer, K. A. Harrison, W. D. |
author_sort |
Echelmeyer, K. A. |
title |
Ongoing margin migration of Ice Stream B, Antarctica |
title_short |
Ongoing margin migration of Ice Stream B, Antarctica |
title_full |
Ongoing margin migration of Ice Stream B, Antarctica |
title_fullStr |
Ongoing margin migration of Ice Stream B, Antarctica |
title_full_unstemmed |
Ongoing margin migration of Ice Stream B, Antarctica |
title_sort |
ongoing margin migration of ice stream b, antarctica |
publisher |
Cambridge University Press (CUP) |
publishDate |
1999 |
url |
http://dx.doi.org/10.1017/s0022143000001866 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000001866 |
genre |
Antarc* Antarctica Ice Stream B Journal of Glaciology |
genre_facet |
Antarc* Antarctica Ice Stream B Journal of Glaciology |
op_source |
Journal of Glaciology volume 45, issue 150, page 361-369 ISSN 0022-1430 1727-5652 |
op_doi |
https://doi.org/10.1017/s0022143000001866 |
container_title |
Journal of Glaciology |
container_volume |
45 |
container_issue |
150 |
container_start_page |
361 |
op_container_end_page |
369 |
_version_ |
1792499956276264960 |