Water Movement At The Base Of Ice Sheets
Abstract Flat-surfaced subglacial lakes, such as those discovered by Oswald (1975), can form where basal sliding velocities are low. As the glacier moves onto a subglacial lake, its underside retains the shape of the vertical relief at the lake edge. Differential heat transfer from the lake into hig...
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Language: | English |
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Cambridge University Press (CUP)
1979
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Online Access: | http://dx.doi.org/10.1017/s0022143000030070 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000030070 |
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crcambridgeupr:10.1017/s0022143000030070 2024-04-07T07:53:41+00:00 Water Movement At The Base Of Ice Sheets Whillans, I. M. 1979 http://dx.doi.org/10.1017/s0022143000030070 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000030070 en eng Cambridge University Press (CUP) Journal of Glaciology volume 23, issue 89, page 410 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1979 crcambridgeupr https://doi.org/10.1017/s0022143000030070 2024-03-08T00:34:10Z Abstract Flat-surfaced subglacial lakes, such as those discovered by Oswald (1975), can form where basal sliding velocities are low. As the glacier moves onto a subglacial lake, its underside retains the shape of the vertical relief at the lake edge. Differential heat transfer from the lake into high and low points in the interface flattens the surface by extra melting of the downward projections or freezing in the high areas. A time of the order of 10 3 years is required to flatten the fluting, and the down-glacier part of a subglacial lake can be flat-surfaced if the glacier takes longer than some 10 3 years to traverse the lake. Such a slow traverse time is expected near ice-drainage divides, and it is there that flat-surfaced lakes were discovered by radar sounding. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 23 89 410 |
institution |
Open Polar |
collection |
Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
topic |
Earth-Surface Processes |
spellingShingle |
Earth-Surface Processes Whillans, I. M. Water Movement At The Base Of Ice Sheets |
topic_facet |
Earth-Surface Processes |
description |
Abstract Flat-surfaced subglacial lakes, such as those discovered by Oswald (1975), can form where basal sliding velocities are low. As the glacier moves onto a subglacial lake, its underside retains the shape of the vertical relief at the lake edge. Differential heat transfer from the lake into high and low points in the interface flattens the surface by extra melting of the downward projections or freezing in the high areas. A time of the order of 10 3 years is required to flatten the fluting, and the down-glacier part of a subglacial lake can be flat-surfaced if the glacier takes longer than some 10 3 years to traverse the lake. Such a slow traverse time is expected near ice-drainage divides, and it is there that flat-surfaced lakes were discovered by radar sounding. |
format |
Article in Journal/Newspaper |
author |
Whillans, I. M. |
author_facet |
Whillans, I. M. |
author_sort |
Whillans, I. M. |
title |
Water Movement At The Base Of Ice Sheets |
title_short |
Water Movement At The Base Of Ice Sheets |
title_full |
Water Movement At The Base Of Ice Sheets |
title_fullStr |
Water Movement At The Base Of Ice Sheets |
title_full_unstemmed |
Water Movement At The Base Of Ice Sheets |
title_sort |
water movement at the base of ice sheets |
publisher |
Cambridge University Press (CUP) |
publishDate |
1979 |
url |
http://dx.doi.org/10.1017/s0022143000030070 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000030070 |
genre |
Journal of Glaciology |
genre_facet |
Journal of Glaciology |
op_source |
Journal of Glaciology volume 23, issue 89, page 410 ISSN 0022-1430 1727-5652 |
op_doi |
https://doi.org/10.1017/s0022143000030070 |
container_title |
Journal of Glaciology |
container_volume |
23 |
container_issue |
89 |
container_start_page |
410 |
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1795669757960126464 |