Marine ice-cliff instability modeling shows mixed-mode ice-cliff failure and yields calving rate parameterization
Ice-cliff failure that leads to marine ice-cliff instability could accelerate Antarctic Ice Sheet retreat. Here, the authors use 3D glacier models to investigate ice-cliff failure, derive a retreat rate relationship, and quantify mélange back force necessary to suppress ice-cliff failure.
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ftdoajarticles:oai:doaj.org/article:76d98a26e5224cb38c552d6e93465f10 2023-05-15T13:37:25+02:00 Marine ice-cliff instability modeling shows mixed-mode ice-cliff failure and yields calving rate parameterization Anna J. Crawford Douglas I. Benn Joe Todd Jan A. Åström Jeremy N. Bassis Thomas Zwinger 2021-05-01T00:00:00Z https://doi.org/10.1038/s41467-021-23070-7 https://doaj.org/article/76d98a26e5224cb38c552d6e93465f10 EN eng Nature Portfolio https://doi.org/10.1038/s41467-021-23070-7 https://doaj.org/toc/2041-1723 doi:10.1038/s41467-021-23070-7 2041-1723 https://doaj.org/article/76d98a26e5224cb38c552d6e93465f10 Nature Communications, Vol 12, Iss 1, Pp 1-9 (2021) Science Q article 2021 ftdoajarticles https://doi.org/10.1038/s41467-021-23070-7 2022-12-31T07:10:44Z Ice-cliff failure that leads to marine ice-cliff instability could accelerate Antarctic Ice Sheet retreat. Here, the authors use 3D glacier models to investigate ice-cliff failure, derive a retreat rate relationship, and quantify mélange back force necessary to suppress ice-cliff failure. Article in Journal/Newspaper Antarc* Antarctic Ice Sheet Directory of Open Access Journals: DOAJ Articles Antarctic Nature Communications 12 1 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
Science Q |
spellingShingle |
Science Q Anna J. Crawford Douglas I. Benn Joe Todd Jan A. Åström Jeremy N. Bassis Thomas Zwinger Marine ice-cliff instability modeling shows mixed-mode ice-cliff failure and yields calving rate parameterization |
topic_facet |
Science Q |
description |
Ice-cliff failure that leads to marine ice-cliff instability could accelerate Antarctic Ice Sheet retreat. Here, the authors use 3D glacier models to investigate ice-cliff failure, derive a retreat rate relationship, and quantify mélange back force necessary to suppress ice-cliff failure. |
format |
Article in Journal/Newspaper |
author |
Anna J. Crawford Douglas I. Benn Joe Todd Jan A. Åström Jeremy N. Bassis Thomas Zwinger |
author_facet |
Anna J. Crawford Douglas I. Benn Joe Todd Jan A. Åström Jeremy N. Bassis Thomas Zwinger |
author_sort |
Anna J. Crawford |
title |
Marine ice-cliff instability modeling shows mixed-mode ice-cliff failure and yields calving rate parameterization |
title_short |
Marine ice-cliff instability modeling shows mixed-mode ice-cliff failure and yields calving rate parameterization |
title_full |
Marine ice-cliff instability modeling shows mixed-mode ice-cliff failure and yields calving rate parameterization |
title_fullStr |
Marine ice-cliff instability modeling shows mixed-mode ice-cliff failure and yields calving rate parameterization |
title_full_unstemmed |
Marine ice-cliff instability modeling shows mixed-mode ice-cliff failure and yields calving rate parameterization |
title_sort |
marine ice-cliff instability modeling shows mixed-mode ice-cliff failure and yields calving rate parameterization |
publisher |
Nature Portfolio |
publishDate |
2021 |
url |
https://doi.org/10.1038/s41467-021-23070-7 https://doaj.org/article/76d98a26e5224cb38c552d6e93465f10 |
geographic |
Antarctic |
geographic_facet |
Antarctic |
genre |
Antarc* Antarctic Ice Sheet |
genre_facet |
Antarc* Antarctic Ice Sheet |
op_source |
Nature Communications, Vol 12, Iss 1, Pp 1-9 (2021) |
op_relation |
https://doi.org/10.1038/s41467-021-23070-7 https://doaj.org/toc/2041-1723 doi:10.1038/s41467-021-23070-7 2041-1723 https://doaj.org/article/76d98a26e5224cb38c552d6e93465f10 |
op_doi |
https://doi.org/10.1038/s41467-021-23070-7 |
container_title |
Nature Communications |
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12 |
container_issue |
1 |
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1766091708880125952 |