Mass loss of the Greenland ice sheet until the year 3000 under a sustained late-21st-century climate
We conduct extended versions of the ISMIP6 future climate experiments for the Greenland ice sheet until the year 3000 with the model SICOPOLIS. Beyond 2100, the climate forcing is kept fixed at late-21st-century conditions. For the unabated warming pathway RCP8.5/SSP5-8.5, the ice sheet suffers a se...
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Cambridge University Press
2022
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Online Access: | https://doi.org/10.1017/jog.2022.9 https://doaj.org/article/a69e9574ffe44e8ca88d746c7ce32d76 |
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ftdoajarticles:oai:doaj.org/article:a69e9574ffe44e8ca88d746c7ce32d76 2023-05-15T15:04:19+02:00 Mass loss of the Greenland ice sheet until the year 3000 under a sustained late-21st-century climate Ralf Greve Christopher Chambers 2022-06-01T00:00:00Z https://doi.org/10.1017/jog.2022.9 https://doaj.org/article/a69e9574ffe44e8ca88d746c7ce32d76 EN eng Cambridge University Press https://www.cambridge.org/core/product/identifier/S0022143022000090/type/journal_article https://doaj.org/toc/0022-1430 https://doaj.org/toc/1727-5652 doi:10.1017/jog.2022.9 0022-1430 1727-5652 https://doaj.org/article/a69e9574ffe44e8ca88d746c7ce32d76 Journal of Glaciology, Vol 68, Pp 618-624 (2022) Arctic glaciology climate change ice and climate ice-sheet modelling Environmental sciences GE1-350 Meteorology. Climatology QC851-999 article 2022 ftdoajarticles https://doi.org/10.1017/jog.2022.9 2023-03-12T01:30:54Z We conduct extended versions of the ISMIP6 future climate experiments for the Greenland ice sheet until the year 3000 with the model SICOPOLIS. Beyond 2100, the climate forcing is kept fixed at late-21st-century conditions. For the unabated warming pathway RCP8.5/SSP5-8.5, the ice sheet suffers a severe mass loss, which amounts to ~ 1.8 m SLE (sea-level equivalent) for the 12-experiment mean, and ~ 3.5 m SLE (~ 50% of the entire mass) for the most sensitive experiment. For the reduced emissions pathway RCP2.6/SSP1-2.6, the mass loss is limited to a two-experiment mean of ~ 0.28 m SLE. Climate-change mitigation during the next decades will therefore be an efficient means for limiting the contribution of the Greenland ice sheet to sea-level rise in the long term. Article in Journal/Newspaper Arctic Climate change Greenland Ice Sheet Journal of Glaciology Directory of Open Access Journals: DOAJ Articles Arctic Greenland Journal of Glaciology 68 269 618 624 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
Arctic glaciology climate change ice and climate ice-sheet modelling Environmental sciences GE1-350 Meteorology. Climatology QC851-999 |
spellingShingle |
Arctic glaciology climate change ice and climate ice-sheet modelling Environmental sciences GE1-350 Meteorology. Climatology QC851-999 Ralf Greve Christopher Chambers Mass loss of the Greenland ice sheet until the year 3000 under a sustained late-21st-century climate |
topic_facet |
Arctic glaciology climate change ice and climate ice-sheet modelling Environmental sciences GE1-350 Meteorology. Climatology QC851-999 |
description |
We conduct extended versions of the ISMIP6 future climate experiments for the Greenland ice sheet until the year 3000 with the model SICOPOLIS. Beyond 2100, the climate forcing is kept fixed at late-21st-century conditions. For the unabated warming pathway RCP8.5/SSP5-8.5, the ice sheet suffers a severe mass loss, which amounts to ~ 1.8 m SLE (sea-level equivalent) for the 12-experiment mean, and ~ 3.5 m SLE (~ 50% of the entire mass) for the most sensitive experiment. For the reduced emissions pathway RCP2.6/SSP1-2.6, the mass loss is limited to a two-experiment mean of ~ 0.28 m SLE. Climate-change mitigation during the next decades will therefore be an efficient means for limiting the contribution of the Greenland ice sheet to sea-level rise in the long term. |
format |
Article in Journal/Newspaper |
author |
Ralf Greve Christopher Chambers |
author_facet |
Ralf Greve Christopher Chambers |
author_sort |
Ralf Greve |
title |
Mass loss of the Greenland ice sheet until the year 3000 under a sustained late-21st-century climate |
title_short |
Mass loss of the Greenland ice sheet until the year 3000 under a sustained late-21st-century climate |
title_full |
Mass loss of the Greenland ice sheet until the year 3000 under a sustained late-21st-century climate |
title_fullStr |
Mass loss of the Greenland ice sheet until the year 3000 under a sustained late-21st-century climate |
title_full_unstemmed |
Mass loss of the Greenland ice sheet until the year 3000 under a sustained late-21st-century climate |
title_sort |
mass loss of the greenland ice sheet until the year 3000 under a sustained late-21st-century climate |
publisher |
Cambridge University Press |
publishDate |
2022 |
url |
https://doi.org/10.1017/jog.2022.9 https://doaj.org/article/a69e9574ffe44e8ca88d746c7ce32d76 |
geographic |
Arctic Greenland |
geographic_facet |
Arctic Greenland |
genre |
Arctic Climate change Greenland Ice Sheet Journal of Glaciology |
genre_facet |
Arctic Climate change Greenland Ice Sheet Journal of Glaciology |
op_source |
Journal of Glaciology, Vol 68, Pp 618-624 (2022) |
op_relation |
https://www.cambridge.org/core/product/identifier/S0022143022000090/type/journal_article https://doaj.org/toc/0022-1430 https://doaj.org/toc/1727-5652 doi:10.1017/jog.2022.9 0022-1430 1727-5652 https://doaj.org/article/a69e9574ffe44e8ca88d746c7ce32d76 |
op_doi |
https://doi.org/10.1017/jog.2022.9 |
container_title |
Journal of Glaciology |
container_volume |
68 |
container_issue |
269 |
container_start_page |
618 |
op_container_end_page |
624 |
_version_ |
1766336111441870848 |