Basal Drainage System Response to Increasing Surface Melt on the Greenland Ice Sheet
Draining Through Ice Water formed by surface melting of the Greenland Ice Sheet is transferred rapidly to the underlying bedrock, but how the water is then dispersed is less clear. This question is important because how the ice-rock interface is lubricated affects how fast the ice sheet moves. Exist...
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American Association for the Advancement of Science (AAAS)
2013
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Online Access: | http://dx.doi.org/10.1126/science.1235905 https://www.science.org/doi/pdf/10.1126/science.1235905 |
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craaas:10.1126/science.1235905 2024-06-09T07:46:17+00:00 Basal Drainage System Response to Increasing Surface Melt on the Greenland Ice Sheet Meierbachtol, T. Harper, J. Humphrey, N. 2013 http://dx.doi.org/10.1126/science.1235905 https://www.science.org/doi/pdf/10.1126/science.1235905 en eng American Association for the Advancement of Science (AAAS) Science volume 341, issue 6147, page 777-779 ISSN 0036-8075 1095-9203 journal-article 2013 craaas https://doi.org/10.1126/science.1235905 2024-05-16T12:53:35Z Draining Through Ice Water formed by surface melting of the Greenland Ice Sheet is transferred rapidly to the underlying bedrock, but how the water is then dispersed is less clear. This question is important because how the ice-rock interface is lubricated affects how fast the ice sheet moves. Existing conceptual models are based on observations of mountain glaciers, but Meierbachtol et al. (p. 777 see the Perspective by Lüthi ) now show that those ideas may not be applicable to the Greenland Ice Sheet. Measuring water pressures in a transect of 23 boreholes revealed that drainage structures differ between the edge, where large melt channels form, and further inland, where more distributed pathways are found. Article in Journal/Newspaper Greenland Ice Sheet AAAS Resource Center (American Association for the Advancement of Science) Greenland Science 341 6147 777 779 |
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Open Polar |
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AAAS Resource Center (American Association for the Advancement of Science) |
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craaas |
language |
English |
description |
Draining Through Ice Water formed by surface melting of the Greenland Ice Sheet is transferred rapidly to the underlying bedrock, but how the water is then dispersed is less clear. This question is important because how the ice-rock interface is lubricated affects how fast the ice sheet moves. Existing conceptual models are based on observations of mountain glaciers, but Meierbachtol et al. (p. 777 see the Perspective by Lüthi ) now show that those ideas may not be applicable to the Greenland Ice Sheet. Measuring water pressures in a transect of 23 boreholes revealed that drainage structures differ between the edge, where large melt channels form, and further inland, where more distributed pathways are found. |
format |
Article in Journal/Newspaper |
author |
Meierbachtol, T. Harper, J. Humphrey, N. |
spellingShingle |
Meierbachtol, T. Harper, J. Humphrey, N. Basal Drainage System Response to Increasing Surface Melt on the Greenland Ice Sheet |
author_facet |
Meierbachtol, T. Harper, J. Humphrey, N. |
author_sort |
Meierbachtol, T. |
title |
Basal Drainage System Response to Increasing Surface Melt on the Greenland Ice Sheet |
title_short |
Basal Drainage System Response to Increasing Surface Melt on the Greenland Ice Sheet |
title_full |
Basal Drainage System Response to Increasing Surface Melt on the Greenland Ice Sheet |
title_fullStr |
Basal Drainage System Response to Increasing Surface Melt on the Greenland Ice Sheet |
title_full_unstemmed |
Basal Drainage System Response to Increasing Surface Melt on the Greenland Ice Sheet |
title_sort |
basal drainage system response to increasing surface melt on the greenland ice sheet |
publisher |
American Association for the Advancement of Science (AAAS) |
publishDate |
2013 |
url |
http://dx.doi.org/10.1126/science.1235905 https://www.science.org/doi/pdf/10.1126/science.1235905 |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
Greenland Ice Sheet |
genre_facet |
Greenland Ice Sheet |
op_source |
Science volume 341, issue 6147, page 777-779 ISSN 0036-8075 1095-9203 |
op_doi |
https://doi.org/10.1126/science.1235905 |
container_title |
Science |
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341 |
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6147 |
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777 |
op_container_end_page |
779 |
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1801376073753034752 |