Antarctic Ice Sheet and emission scenario controls on 21st-century extreme sea-level changes
There are significant uncertainties of how large sea level changes due to Antarctic Ice Sheet melting could be. Here, the authors quantify the impact of different greenhouse gas emission scenarios and different Antarctic contributions to changes to extreme sea-level events and find that even under l...
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ftdoajarticles:oai:doaj.org/article:ffc04314a3074b549febd93240e1dea8 2023-05-15T13:52:24+02:00 Antarctic Ice Sheet and emission scenario controls on 21st-century extreme sea-level changes Thomas Frederikse Maya K. Buchanan Erwin Lambert Robert E. Kopp Michael Oppenheimer D. J. Rasmussen Roderik S. W. van de Wal 2020-01-01T00:00:00Z https://doi.org/10.1038/s41467-019-14049-6 https://doaj.org/article/ffc04314a3074b549febd93240e1dea8 EN eng Nature Portfolio https://doi.org/10.1038/s41467-019-14049-6 https://doaj.org/toc/2041-1723 doi:10.1038/s41467-019-14049-6 2041-1723 https://doaj.org/article/ffc04314a3074b549febd93240e1dea8 Nature Communications, Vol 11, Iss 1, Pp 1-11 (2020) Science Q article 2020 ftdoajarticles https://doi.org/10.1038/s41467-019-14049-6 2022-12-31T07:08:05Z There are significant uncertainties of how large sea level changes due to Antarctic Ice Sheet melting could be. Here, the authors quantify the impact of different greenhouse gas emission scenarios and different Antarctic contributions to changes to extreme sea-level events and find that even under low emissions the occurrence of sea-level extremes could rise significantly due to Antarctic meltwater increase. Article in Journal/Newspaper Antarc* Antarctic Ice Sheet Directory of Open Access Journals: DOAJ Articles Antarctic Nature Communications 11 1 |
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Directory of Open Access Journals: DOAJ Articles |
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ftdoajarticles |
language |
English |
topic |
Science Q |
spellingShingle |
Science Q Thomas Frederikse Maya K. Buchanan Erwin Lambert Robert E. Kopp Michael Oppenheimer D. J. Rasmussen Roderik S. W. van de Wal Antarctic Ice Sheet and emission scenario controls on 21st-century extreme sea-level changes |
topic_facet |
Science Q |
description |
There are significant uncertainties of how large sea level changes due to Antarctic Ice Sheet melting could be. Here, the authors quantify the impact of different greenhouse gas emission scenarios and different Antarctic contributions to changes to extreme sea-level events and find that even under low emissions the occurrence of sea-level extremes could rise significantly due to Antarctic meltwater increase. |
format |
Article in Journal/Newspaper |
author |
Thomas Frederikse Maya K. Buchanan Erwin Lambert Robert E. Kopp Michael Oppenheimer D. J. Rasmussen Roderik S. W. van de Wal |
author_facet |
Thomas Frederikse Maya K. Buchanan Erwin Lambert Robert E. Kopp Michael Oppenheimer D. J. Rasmussen Roderik S. W. van de Wal |
author_sort |
Thomas Frederikse |
title |
Antarctic Ice Sheet and emission scenario controls on 21st-century extreme sea-level changes |
title_short |
Antarctic Ice Sheet and emission scenario controls on 21st-century extreme sea-level changes |
title_full |
Antarctic Ice Sheet and emission scenario controls on 21st-century extreme sea-level changes |
title_fullStr |
Antarctic Ice Sheet and emission scenario controls on 21st-century extreme sea-level changes |
title_full_unstemmed |
Antarctic Ice Sheet and emission scenario controls on 21st-century extreme sea-level changes |
title_sort |
antarctic ice sheet and emission scenario controls on 21st-century extreme sea-level changes |
publisher |
Nature Portfolio |
publishDate |
2020 |
url |
https://doi.org/10.1038/s41467-019-14049-6 https://doaj.org/article/ffc04314a3074b549febd93240e1dea8 |
geographic |
Antarctic |
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Antarctic |
genre |
Antarc* Antarctic Ice Sheet |
genre_facet |
Antarc* Antarctic Ice Sheet |
op_source |
Nature Communications, Vol 11, Iss 1, Pp 1-11 (2020) |
op_relation |
https://doi.org/10.1038/s41467-019-14049-6 https://doaj.org/toc/2041-1723 doi:10.1038/s41467-019-14049-6 2041-1723 https://doaj.org/article/ffc04314a3074b549febd93240e1dea8 |
op_doi |
https://doi.org/10.1038/s41467-019-14049-6 |
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Nature Communications |
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11 |
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1 |
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1766256674596716544 |