Possibility for strong northern hemisphere high-latitude cooling under negative emissions

It is well established that a collapse or strong reduction of the Atlantic meridional overturning circulation (AMOC) would substantially cool the northern high latitudes. Here we show that there is a possibility that such cooling could be amplified under deliberate CO2 removal and result in a tempor...

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Published in:Nature Communications
Main Authors: Schwinger, Jörg, Asaadi, Ali, Goris, Nadine, Lee, Hanna
Format: Article in Journal/Newspaper
Language:English
Published: 2022
Subjects:
Ice
Online Access:https://hdl.handle.net/11250/3046968
https://doi.org/10.1038/s41467-022-28573-5
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spelling ftnorce:oai:norceresearch.brage.unit.no:11250/3046968 2023-05-15T16:37:38+02:00 Possibility for strong northern hemisphere high-latitude cooling under negative emissions Schwinger, Jörg Asaadi, Ali Goris, Nadine Lee, Hanna 2022 application/pdf https://hdl.handle.net/11250/3046968 https://doi.org/10.1038/s41467-022-28573-5 eng eng Norges forskningsråd: 294930 urn:issn:2041-1723 https://hdl.handle.net/11250/3046968 https://doi.org/10.1038/s41467-022-28573-5 cristin:1993920 Navngivelse 4.0 Internasjonal http://creativecommons.org/licenses/by/4.0/deed.no © The Author(s) 2022 CC-BY Nature Communications 13 1 Peer reviewed Journal article 2022 ftnorce https://doi.org/10.1038/s41467-022-28573-5 2023-02-01T23:46:34Z It is well established that a collapse or strong reduction of the Atlantic meridional overturning circulation (AMOC) would substantially cool the northern high latitudes. Here we show that there is a possibility that such cooling could be amplified under deliberate CO2 removal and result in a temporary undershoot of a targeted temperature level. We find this behaviour in Earth system models that show a strong AMOC decline in response to anthropogenic forcing. Idealized simulations of CO2 removal with one of these models indicate that the timing of negative emissions relative to AMOC decline and recovery is key in setting the strength of the temporary cooling. We show that the pronounced temperature-fluctuations at high northern latitudes found in these simulations would entail considerable consequences for sea-ice and permafrost extent as well as for high latitude ecosystems. publishedVersion Article in Journal/Newspaper Ice permafrost Sea ice NORCE vitenarkiv (Norwegian Research Centre) Nature Communications 13 1
institution Open Polar
collection NORCE vitenarkiv (Norwegian Research Centre)
op_collection_id ftnorce
language English
description It is well established that a collapse or strong reduction of the Atlantic meridional overturning circulation (AMOC) would substantially cool the northern high latitudes. Here we show that there is a possibility that such cooling could be amplified under deliberate CO2 removal and result in a temporary undershoot of a targeted temperature level. We find this behaviour in Earth system models that show a strong AMOC decline in response to anthropogenic forcing. Idealized simulations of CO2 removal with one of these models indicate that the timing of negative emissions relative to AMOC decline and recovery is key in setting the strength of the temporary cooling. We show that the pronounced temperature-fluctuations at high northern latitudes found in these simulations would entail considerable consequences for sea-ice and permafrost extent as well as for high latitude ecosystems. publishedVersion
format Article in Journal/Newspaper
author Schwinger, Jörg
Asaadi, Ali
Goris, Nadine
Lee, Hanna
spellingShingle Schwinger, Jörg
Asaadi, Ali
Goris, Nadine
Lee, Hanna
Possibility for strong northern hemisphere high-latitude cooling under negative emissions
author_facet Schwinger, Jörg
Asaadi, Ali
Goris, Nadine
Lee, Hanna
author_sort Schwinger, Jörg
title Possibility for strong northern hemisphere high-latitude cooling under negative emissions
title_short Possibility for strong northern hemisphere high-latitude cooling under negative emissions
title_full Possibility for strong northern hemisphere high-latitude cooling under negative emissions
title_fullStr Possibility for strong northern hemisphere high-latitude cooling under negative emissions
title_full_unstemmed Possibility for strong northern hemisphere high-latitude cooling under negative emissions
title_sort possibility for strong northern hemisphere high-latitude cooling under negative emissions
publishDate 2022
url https://hdl.handle.net/11250/3046968
https://doi.org/10.1038/s41467-022-28573-5
genre Ice
permafrost
Sea ice
genre_facet Ice
permafrost
Sea ice
op_source Nature Communications
13
1
op_relation Norges forskningsråd: 294930
urn:issn:2041-1723
https://hdl.handle.net/11250/3046968
https://doi.org/10.1038/s41467-022-28573-5
cristin:1993920
op_rights Navngivelse 4.0 Internasjonal
http://creativecommons.org/licenses/by/4.0/deed.no
© The Author(s) 2022
op_rightsnorm CC-BY
op_doi https://doi.org/10.1038/s41467-022-28573-5
container_title Nature Communications
container_volume 13
container_issue 1
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