Global warming due to loss of large ice masses and Arctic summer sea ice

Several large-scale cryosphere elements such as the Arctic summer sea ice, the mountain glaciers, the Greenland and West Antarctic Ice Sheet have changed substantially during the last century due to anthropogenic global warming. However, the impacts of their possible future disintegration on global...

Full description

Bibliographic Details
Main Authors: Wunderling, Nico, Willeit, Matteo, Donges, Jonathan, Winkelmann, Ricarda
Format: Article in Journal/Newspaper
Language:English
Published: Humboldt-Universität zu Berlin 2020
Subjects:
Online Access:http://edoc.hu-berlin.de/18452/27867
https://nbn-resolving.org/urn:nbn:de:kobv:11-110-18452/27867-9
https://doi.org/10.1038/s41467-020-18934-3
https://doi.org/10.18452/27211
id fthuberlin:oai:edoc.hu-berlin.de:18452/27867
record_format openpolar
spelling fthuberlin:oai:edoc.hu-berlin.de:18452/27867 2023-12-03T10:08:50+01:00 Global warming due to loss of large ice masses and Arctic summer sea ice Wunderling, Nico Willeit, Matteo Donges, Jonathan Winkelmann, Ricarda 2020-10-27 application/pdf http://edoc.hu-berlin.de/18452/27867 https://nbn-resolving.org/urn:nbn:de:kobv:11-110-18452/27867-9 https://doi.org/10.1038/s41467-020-18934-3 https://doi.org/10.18452/27211 eng eng Humboldt-Universität zu Berlin http://edoc.hu-berlin.de/18452/27867 urn:nbn:de:kobv:11-110-18452/27867-9 doi:10.1038/s41467-020-18934-3 http://dx.doi.org/10.18452/27211 2041-1723 (CC BY 4.0) Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/ Climate and Earth system modelling Cryospheric science Projection and prediction 550 Geowissenschaften ddc:550 article doc-type:article publishedVersion 2020 fthuberlin https://doi.org/10.1038/s41467-020-18934-310.18452/27211 2023-11-05T23:36:21Z Several large-scale cryosphere elements such as the Arctic summer sea ice, the mountain glaciers, the Greenland and West Antarctic Ice Sheet have changed substantially during the last century due to anthropogenic global warming. However, the impacts of their possible future disintegration on global mean temperature (GMT) and climate feedbacks have not yet been comprehensively evaluated. Here, we quantify this response using an Earth system model of intermediate complexity. Overall, we find a median additional global warming of 0.43 °C (interquartile range: 0.39−0.46 °C) at a CO2 concentration of 400 ppm. Most of this response (55%) is caused by albedo changes, but lapse rate together with water vapour (30%) and cloud feedbacks (15%) also contribute significantly. While a decay of the ice sheets would occur on centennial to millennial time scales, the Arctic might become ice-free during summer within the 21st century. Our findings imply an additional increase of the GMT on intermediate to long time scales. Deutsche Forschungsgemeinschaft (German Research Foundation) https://doi.org/10.13039/501100001659 Leibniz-Gemeinschaft (Leibniz Association) https://doi.org/10.13039/501100001664 Bundesministerium für Bildung und Forschung (Federal Ministry of Education and Research) https://doi.org/10.13039/501100002347 EC | EU Framework Programme for Research and Innovation H2020 | H2020 Priority Excellent Science | H2020 European Research Council (H2020 Excellent Science - European Research Council) https://doi.org/10.13039/100010663 Earth League https://doi.org/10.13039/501100010065 Peer Reviewed Article in Journal/Newspaper albedo Antarc* Antarctic Arctic Global warming Greenland Ice Sheet Sea ice Open-Access-Publikationsserver der Humboldt-Universität: edoc-Server Antarctic Arctic Greenland West Antarctic Ice Sheet
institution Open Polar
collection Open-Access-Publikationsserver der Humboldt-Universität: edoc-Server
op_collection_id fthuberlin
language English
topic Climate and Earth system modelling
Cryospheric science
Projection and prediction
550 Geowissenschaften
ddc:550
spellingShingle Climate and Earth system modelling
Cryospheric science
Projection and prediction
550 Geowissenschaften
ddc:550
Wunderling, Nico
Willeit, Matteo
Donges, Jonathan
Winkelmann, Ricarda
Global warming due to loss of large ice masses and Arctic summer sea ice
topic_facet Climate and Earth system modelling
Cryospheric science
Projection and prediction
550 Geowissenschaften
ddc:550
description Several large-scale cryosphere elements such as the Arctic summer sea ice, the mountain glaciers, the Greenland and West Antarctic Ice Sheet have changed substantially during the last century due to anthropogenic global warming. However, the impacts of their possible future disintegration on global mean temperature (GMT) and climate feedbacks have not yet been comprehensively evaluated. Here, we quantify this response using an Earth system model of intermediate complexity. Overall, we find a median additional global warming of 0.43 °C (interquartile range: 0.39−0.46 °C) at a CO2 concentration of 400 ppm. Most of this response (55%) is caused by albedo changes, but lapse rate together with water vapour (30%) and cloud feedbacks (15%) also contribute significantly. While a decay of the ice sheets would occur on centennial to millennial time scales, the Arctic might become ice-free during summer within the 21st century. Our findings imply an additional increase of the GMT on intermediate to long time scales. Deutsche Forschungsgemeinschaft (German Research Foundation) https://doi.org/10.13039/501100001659 Leibniz-Gemeinschaft (Leibniz Association) https://doi.org/10.13039/501100001664 Bundesministerium für Bildung und Forschung (Federal Ministry of Education and Research) https://doi.org/10.13039/501100002347 EC | EU Framework Programme for Research and Innovation H2020 | H2020 Priority Excellent Science | H2020 European Research Council (H2020 Excellent Science - European Research Council) https://doi.org/10.13039/100010663 Earth League https://doi.org/10.13039/501100010065 Peer Reviewed
format Article in Journal/Newspaper
author Wunderling, Nico
Willeit, Matteo
Donges, Jonathan
Winkelmann, Ricarda
author_facet Wunderling, Nico
Willeit, Matteo
Donges, Jonathan
Winkelmann, Ricarda
author_sort Wunderling, Nico
title Global warming due to loss of large ice masses and Arctic summer sea ice
title_short Global warming due to loss of large ice masses and Arctic summer sea ice
title_full Global warming due to loss of large ice masses and Arctic summer sea ice
title_fullStr Global warming due to loss of large ice masses and Arctic summer sea ice
title_full_unstemmed Global warming due to loss of large ice masses and Arctic summer sea ice
title_sort global warming due to loss of large ice masses and arctic summer sea ice
publisher Humboldt-Universität zu Berlin
publishDate 2020
url http://edoc.hu-berlin.de/18452/27867
https://nbn-resolving.org/urn:nbn:de:kobv:11-110-18452/27867-9
https://doi.org/10.1038/s41467-020-18934-3
https://doi.org/10.18452/27211
geographic Antarctic
Arctic
Greenland
West Antarctic Ice Sheet
geographic_facet Antarctic
Arctic
Greenland
West Antarctic Ice Sheet
genre albedo
Antarc*
Antarctic
Arctic
Global warming
Greenland
Ice Sheet
Sea ice
genre_facet albedo
Antarc*
Antarctic
Arctic
Global warming
Greenland
Ice Sheet
Sea ice
op_relation http://edoc.hu-berlin.de/18452/27867
urn:nbn:de:kobv:11-110-18452/27867-9
doi:10.1038/s41467-020-18934-3
http://dx.doi.org/10.18452/27211
2041-1723
op_rights (CC BY 4.0) Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.1038/s41467-020-18934-310.18452/27211
_version_ 1784259917619658752