Dynamic regimes of the Greenland Ice Sheet emerging from interacting melt–elevation and glacial isostatic adjustment feedbacks ...
The stability of the Greenland Ice Sheet under global warming is governed by a number of dynamic processes and interacting feedback mechanisms in the ice sheet, atmosphere and solid Earth. Here we study the long-term effects due to the interplay of the competing melt-elevation and glacial isostatic...
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Göttingen : Copernicus Publ.
2022
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Online Access: | https://dx.doi.org/10.34657/10899 https://oa.tib.eu/renate/handle/123456789/11866 |
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ftdatacite:10.34657/10899 2023-06-11T04:09:31+02:00 Dynamic regimes of the Greenland Ice Sheet emerging from interacting melt–elevation and glacial isostatic adjustment feedbacks ... Zeitz, Maria Haacker, Jan M. Donges, Jonathan F. Albrecht, Torsten Winkelmann, Ricarda 2022 https://dx.doi.org/10.34657/10899 https://oa.tib.eu/renate/handle/123456789/11866 unknown Göttingen : Copernicus Publ. Creative Commons Attribution 4.0 International CC BY 4.0 Unported https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 Arctic Greenland Greenland Ice Sheet Earth atmosphere Glacial geology 550 article-journal ScholarlyArticle Text article 2022 ftdatacite https://doi.org/10.34657/10899 2023-05-02T09:36:04Z The stability of the Greenland Ice Sheet under global warming is governed by a number of dynamic processes and interacting feedback mechanisms in the ice sheet, atmosphere and solid Earth. Here we study the long-term effects due to the interplay of the competing melt-elevation and glacial isostatic adjustment (GIA) feedbacks for different temperature step forcing experiments with a coupled ice-sheet and solid-Earth model. Our model results show that for warming levels above 2 C, Greenland could become essentially ice-free within several millennia, mainly as a result of surface melting and acceleration of ice flow. These ice losses are mitigated, however, in some cases with strong GIA feedback even promoting an incomplete recovery of the Greenland ice volume. We further explore the full-factorial parameter space determining the relative strengths of the two feedbacks: our findings suggest distinct dynamic regimes of the Greenland Ice Sheets on the route to destabilization under global warming - from ... Text Arctic Global warming Greenland Ice Sheet DataCite Metadata Store (German National Library of Science and Technology) Arctic Greenland |
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DataCite Metadata Store (German National Library of Science and Technology) |
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ftdatacite |
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unknown |
topic |
Arctic Greenland Greenland Ice Sheet Earth atmosphere Glacial geology 550 |
spellingShingle |
Arctic Greenland Greenland Ice Sheet Earth atmosphere Glacial geology 550 Zeitz, Maria Haacker, Jan M. Donges, Jonathan F. Albrecht, Torsten Winkelmann, Ricarda Dynamic regimes of the Greenland Ice Sheet emerging from interacting melt–elevation and glacial isostatic adjustment feedbacks ... |
topic_facet |
Arctic Greenland Greenland Ice Sheet Earth atmosphere Glacial geology 550 |
description |
The stability of the Greenland Ice Sheet under global warming is governed by a number of dynamic processes and interacting feedback mechanisms in the ice sheet, atmosphere and solid Earth. Here we study the long-term effects due to the interplay of the competing melt-elevation and glacial isostatic adjustment (GIA) feedbacks for different temperature step forcing experiments with a coupled ice-sheet and solid-Earth model. Our model results show that for warming levels above 2 C, Greenland could become essentially ice-free within several millennia, mainly as a result of surface melting and acceleration of ice flow. These ice losses are mitigated, however, in some cases with strong GIA feedback even promoting an incomplete recovery of the Greenland ice volume. We further explore the full-factorial parameter space determining the relative strengths of the two feedbacks: our findings suggest distinct dynamic regimes of the Greenland Ice Sheets on the route to destabilization under global warming - from ... |
format |
Text |
author |
Zeitz, Maria Haacker, Jan M. Donges, Jonathan F. Albrecht, Torsten Winkelmann, Ricarda |
author_facet |
Zeitz, Maria Haacker, Jan M. Donges, Jonathan F. Albrecht, Torsten Winkelmann, Ricarda |
author_sort |
Zeitz, Maria |
title |
Dynamic regimes of the Greenland Ice Sheet emerging from interacting melt–elevation and glacial isostatic adjustment feedbacks ... |
title_short |
Dynamic regimes of the Greenland Ice Sheet emerging from interacting melt–elevation and glacial isostatic adjustment feedbacks ... |
title_full |
Dynamic regimes of the Greenland Ice Sheet emerging from interacting melt–elevation and glacial isostatic adjustment feedbacks ... |
title_fullStr |
Dynamic regimes of the Greenland Ice Sheet emerging from interacting melt–elevation and glacial isostatic adjustment feedbacks ... |
title_full_unstemmed |
Dynamic regimes of the Greenland Ice Sheet emerging from interacting melt–elevation and glacial isostatic adjustment feedbacks ... |
title_sort |
dynamic regimes of the greenland ice sheet emerging from interacting melt–elevation and glacial isostatic adjustment feedbacks ... |
publisher |
Göttingen : Copernicus Publ. |
publishDate |
2022 |
url |
https://dx.doi.org/10.34657/10899 https://oa.tib.eu/renate/handle/123456789/11866 |
geographic |
Arctic Greenland |
geographic_facet |
Arctic Greenland |
genre |
Arctic Global warming Greenland Ice Sheet |
genre_facet |
Arctic Global warming Greenland Ice Sheet |
op_rights |
Creative Commons Attribution 4.0 International CC BY 4.0 Unported https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 |
op_doi |
https://doi.org/10.34657/10899 |
_version_ |
1768383457198604288 |