Transition to marine ice cliff instability controlled by ice thickness gradients and velocity
Cliff collapse Tall ice cliffs at the edges of ice sheets can collapse under their own weight in spectacular fashion, a process that can considerably hasten ice sheet mass loss. Bassis et al. used a dynamic ice model to demonstrate that this kind of collapse can be slowed either by upstream thinning...
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Online Access: | http://dx.doi.org/10.1126/science.abf6271 https://syndication.highwire.org/content/doi/10.1126/science.abf6271 https://www.science.org/doi/pdf/10.1126/science.abf6271 |
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craaas:10.1126/science.abf6271 2024-06-23T07:53:46+00:00 Transition to marine ice cliff instability controlled by ice thickness gradients and velocity Bassis, J. N. Berg, B. Crawford, A. J. Benn, D. I. National Science Foundation National Environmental Research Council 2021 http://dx.doi.org/10.1126/science.abf6271 https://syndication.highwire.org/content/doi/10.1126/science.abf6271 https://www.science.org/doi/pdf/10.1126/science.abf6271 en eng American Association for the Advancement of Science (AAAS) Science volume 372, issue 6548, page 1342-1344 ISSN 0036-8075 1095-9203 journal-article 2021 craaas https://doi.org/10.1126/science.abf6271 2024-06-13T04:01:17Z Cliff collapse Tall ice cliffs at the edges of ice sheets can collapse under their own weight in spectacular fashion, a process that can considerably hasten ice sheet mass loss. Bassis et al. used a dynamic ice model to demonstrate that this kind of collapse can be slowed either by upstream thinning of the ice sheet or by the resistive forces from sea ice and calved debris (see the Perspective by Golledge and Lowry). Conversely, when there is upstream ice thickening, a transition to catastrophic collapse can occur. Science , abf6271, this issue p. 1342 see also abj3266, p. 1266 Article in Journal/Newspaper Ice Sheet Sea ice AAAS Resource Center (American Association for the Advancement of Science) Lowry ENVELOPE(-64.150,-64.150,-84.550,-84.550) Science 372 6548 1342 1344 |
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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 |
Cliff collapse Tall ice cliffs at the edges of ice sheets can collapse under their own weight in spectacular fashion, a process that can considerably hasten ice sheet mass loss. Bassis et al. used a dynamic ice model to demonstrate that this kind of collapse can be slowed either by upstream thinning of the ice sheet or by the resistive forces from sea ice and calved debris (see the Perspective by Golledge and Lowry). Conversely, when there is upstream ice thickening, a transition to catastrophic collapse can occur. Science , abf6271, this issue p. 1342 see also abj3266, p. 1266 |
author2 |
National Science Foundation National Environmental Research Council |
format |
Article in Journal/Newspaper |
author |
Bassis, J. N. Berg, B. Crawford, A. J. Benn, D. I. |
spellingShingle |
Bassis, J. N. Berg, B. Crawford, A. J. Benn, D. I. Transition to marine ice cliff instability controlled by ice thickness gradients and velocity |
author_facet |
Bassis, J. N. Berg, B. Crawford, A. J. Benn, D. I. |
author_sort |
Bassis, J. N. |
title |
Transition to marine ice cliff instability controlled by ice thickness gradients and velocity |
title_short |
Transition to marine ice cliff instability controlled by ice thickness gradients and velocity |
title_full |
Transition to marine ice cliff instability controlled by ice thickness gradients and velocity |
title_fullStr |
Transition to marine ice cliff instability controlled by ice thickness gradients and velocity |
title_full_unstemmed |
Transition to marine ice cliff instability controlled by ice thickness gradients and velocity |
title_sort |
transition to marine ice cliff instability controlled by ice thickness gradients and velocity |
publisher |
American Association for the Advancement of Science (AAAS) |
publishDate |
2021 |
url |
http://dx.doi.org/10.1126/science.abf6271 https://syndication.highwire.org/content/doi/10.1126/science.abf6271 https://www.science.org/doi/pdf/10.1126/science.abf6271 |
long_lat |
ENVELOPE(-64.150,-64.150,-84.550,-84.550) |
geographic |
Lowry |
geographic_facet |
Lowry |
genre |
Ice Sheet Sea ice |
genre_facet |
Ice Sheet Sea ice |
op_source |
Science volume 372, issue 6548, page 1342-1344 ISSN 0036-8075 1095-9203 |
op_doi |
https://doi.org/10.1126/science.abf6271 |
container_title |
Science |
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372 |
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6548 |
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1342 |
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1344 |
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1802645575361888256 |