Basal friction of Ice Stream E, West Antarctica
Abstract We use surface velocity derived from sequential Landsat imagery and a control method to estimate the basal-friction distribution of a major West Antarctic ice stream. The area-averaged basal stress is approximately 1.4 × 10 4 Pa, or about 29% of the area-averaged driving stress of 4.9 × 10...
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Language: | English |
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Cambridge University Press (CUP)
1995
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Online Access: | http://dx.doi.org/10.1017/s0022143000016154 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000016154 |
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crcambridgeupr:10.1017/s0022143000016154 2024-04-28T07:58:26+00:00 Basal friction of Ice Stream E, West Antarctica MacAyeal, Douglas R. Bindschadler, Robert A. Scambos, Theodore A. 1995 http://dx.doi.org/10.1017/s0022143000016154 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000016154 en eng Cambridge University Press (CUP) Journal of Glaciology volume 41, issue 138, page 247-262 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1995 crcambridgeupr https://doi.org/10.1017/s0022143000016154 2024-04-09T06:54:42Z Abstract We use surface velocity derived from sequential Landsat imagery and a control method to estimate the basal-friction distribution of a major West Antarctic ice stream. The area-averaged basal stress is approximately 1.4 × 10 4 Pa, or about 29% of the area-averaged driving stress of 4.9 × 10 4 Pa. Uncertainty of the derived area-averaged basal stress is difficult to assess and depends primarily on spatial variation of the flow-law rate factor in the constitutive law. Spatial variation associated with depth-averaged temperature variation gives an uncertainty of approximately ±10 3 Pa. Approximately 60% of the ice stream has a basal-stress magnitude less than 10 4 Pa, and approximately 30% has less than 10 3 Pa. These characteristics suggest the presence of a mechanically weak, water-charged subglacial till. Small-scale sticky spots where basal friction exceeds the area-averaged driving stress are scattered irregularly across the subglacial regime and comprise approximately 15% of the ice-stream area. Sticky spots cluster in regions where Landsat imagery suggests structural features in the underlying bedrock. Article in Journal/Newspaper Antarc* Antarctic Antarctica Ice Stream E Journal of Glaciology West Antarctica Cambridge University Press Journal of Glaciology 41 138 247 262 |
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Open Polar |
collection |
Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
topic |
Earth-Surface Processes |
spellingShingle |
Earth-Surface Processes MacAyeal, Douglas R. Bindschadler, Robert A. Scambos, Theodore A. Basal friction of Ice Stream E, West Antarctica |
topic_facet |
Earth-Surface Processes |
description |
Abstract We use surface velocity derived from sequential Landsat imagery and a control method to estimate the basal-friction distribution of a major West Antarctic ice stream. The area-averaged basal stress is approximately 1.4 × 10 4 Pa, or about 29% of the area-averaged driving stress of 4.9 × 10 4 Pa. Uncertainty of the derived area-averaged basal stress is difficult to assess and depends primarily on spatial variation of the flow-law rate factor in the constitutive law. Spatial variation associated with depth-averaged temperature variation gives an uncertainty of approximately ±10 3 Pa. Approximately 60% of the ice stream has a basal-stress magnitude less than 10 4 Pa, and approximately 30% has less than 10 3 Pa. These characteristics suggest the presence of a mechanically weak, water-charged subglacial till. Small-scale sticky spots where basal friction exceeds the area-averaged driving stress are scattered irregularly across the subglacial regime and comprise approximately 15% of the ice-stream area. Sticky spots cluster in regions where Landsat imagery suggests structural features in the underlying bedrock. |
format |
Article in Journal/Newspaper |
author |
MacAyeal, Douglas R. Bindschadler, Robert A. Scambos, Theodore A. |
author_facet |
MacAyeal, Douglas R. Bindschadler, Robert A. Scambos, Theodore A. |
author_sort |
MacAyeal, Douglas R. |
title |
Basal friction of Ice Stream E, West Antarctica |
title_short |
Basal friction of Ice Stream E, West Antarctica |
title_full |
Basal friction of Ice Stream E, West Antarctica |
title_fullStr |
Basal friction of Ice Stream E, West Antarctica |
title_full_unstemmed |
Basal friction of Ice Stream E, West Antarctica |
title_sort |
basal friction of ice stream e, west antarctica |
publisher |
Cambridge University Press (CUP) |
publishDate |
1995 |
url |
http://dx.doi.org/10.1017/s0022143000016154 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000016154 |
genre |
Antarc* Antarctic Antarctica Ice Stream E Journal of Glaciology West Antarctica |
genre_facet |
Antarc* Antarctic Antarctica Ice Stream E Journal of Glaciology West Antarctica |
op_source |
Journal of Glaciology volume 41, issue 138, page 247-262 ISSN 0022-1430 1727-5652 |
op_doi |
https://doi.org/10.1017/s0022143000016154 |
container_title |
Journal of Glaciology |
container_volume |
41 |
container_issue |
138 |
container_start_page |
247 |
op_container_end_page |
262 |
_version_ |
1797569500657221632 |