Asymmetry of AMOC Hysteresis in a State‐Of‐The‐Art Global Climate Model

Abstract We study hysteresis properties of the Atlantic Meridional Overturning Circulation (AMOC) under a slowly‐varying North Atlantic (20°N–50°N) freshwater flux forcing in state‐of‐the‐art global climate model (GCM), the Community Earth System Model. Results are presented of a full hysteresis sim...

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Published in:Geophysical Research Letters
Main Authors: René M. vanWesten, Henk A. Dijkstra
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2023
Subjects:
Online Access:https://doi.org/10.1029/2023GL106088
https://doaj.org/article/0dc1d032882a4e22aeee4ff517cf6882
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spelling ftdoajarticles:oai:doaj.org/article:0dc1d032882a4e22aeee4ff517cf6882 2024-09-09T19:55:34+00:00 Asymmetry of AMOC Hysteresis in a State‐Of‐The‐Art Global Climate Model René M. vanWesten Henk A. Dijkstra 2023-11-01T00:00:00Z https://doi.org/10.1029/2023GL106088 https://doaj.org/article/0dc1d032882a4e22aeee4ff517cf6882 EN eng Wiley https://doi.org/10.1029/2023GL106088 https://doaj.org/toc/0094-8276 https://doaj.org/toc/1944-8007 1944-8007 0094-8276 doi:10.1029/2023GL106088 https://doaj.org/article/0dc1d032882a4e22aeee4ff517cf6882 Geophysical Research Letters, Vol 50, Iss 22, Pp n/a-n/a (2023) ocean circulation tipping CESM hysteresis sea‐ice Geophysics. Cosmic physics QC801-809 article 2023 ftdoajarticles https://doi.org/10.1029/2023GL106088 2024-08-05T17:49:23Z Abstract We study hysteresis properties of the Atlantic Meridional Overturning Circulation (AMOC) under a slowly‐varying North Atlantic (20°N–50°N) freshwater flux forcing in state‐of‐the‐art global climate model (GCM), the Community Earth System Model. Results are presented of a full hysteresis simulation (4,400 model years) and show that there is a hysteresis width of about 0.4 Sv. This demonstrates that an AMOC collapse and recovery do not only occur in conceptual and idealized climate models, but also in a state‐of‐the‐art GCM. The AMOC recovery is about a factor six faster than the AMOC collapse and this asymmetry is due to the major effect of the North Atlantic sea‐ice distribution on the AMOC recovery. The results have implications for projections of possible future AMOC behavior and for explaining relatively rapid climate transitions in the geological past. Article in Journal/Newspaper North Atlantic Sea ice Directory of Open Access Journals: DOAJ Articles Geophysical Research Letters 50 22
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic ocean circulation
tipping
CESM
hysteresis
sea‐ice
Geophysics. Cosmic physics
QC801-809
spellingShingle ocean circulation
tipping
CESM
hysteresis
sea‐ice
Geophysics. Cosmic physics
QC801-809
René M. vanWesten
Henk A. Dijkstra
Asymmetry of AMOC Hysteresis in a State‐Of‐The‐Art Global Climate Model
topic_facet ocean circulation
tipping
CESM
hysteresis
sea‐ice
Geophysics. Cosmic physics
QC801-809
description Abstract We study hysteresis properties of the Atlantic Meridional Overturning Circulation (AMOC) under a slowly‐varying North Atlantic (20°N–50°N) freshwater flux forcing in state‐of‐the‐art global climate model (GCM), the Community Earth System Model. Results are presented of a full hysteresis simulation (4,400 model years) and show that there is a hysteresis width of about 0.4 Sv. This demonstrates that an AMOC collapse and recovery do not only occur in conceptual and idealized climate models, but also in a state‐of‐the‐art GCM. The AMOC recovery is about a factor six faster than the AMOC collapse and this asymmetry is due to the major effect of the North Atlantic sea‐ice distribution on the AMOC recovery. The results have implications for projections of possible future AMOC behavior and for explaining relatively rapid climate transitions in the geological past.
format Article in Journal/Newspaper
author René M. vanWesten
Henk A. Dijkstra
author_facet René M. vanWesten
Henk A. Dijkstra
author_sort René M. vanWesten
title Asymmetry of AMOC Hysteresis in a State‐Of‐The‐Art Global Climate Model
title_short Asymmetry of AMOC Hysteresis in a State‐Of‐The‐Art Global Climate Model
title_full Asymmetry of AMOC Hysteresis in a State‐Of‐The‐Art Global Climate Model
title_fullStr Asymmetry of AMOC Hysteresis in a State‐Of‐The‐Art Global Climate Model
title_full_unstemmed Asymmetry of AMOC Hysteresis in a State‐Of‐The‐Art Global Climate Model
title_sort asymmetry of amoc hysteresis in a state‐of‐the‐art global climate model
publisher Wiley
publishDate 2023
url https://doi.org/10.1029/2023GL106088
https://doaj.org/article/0dc1d032882a4e22aeee4ff517cf6882
genre North Atlantic
Sea ice
genre_facet North Atlantic
Sea ice
op_source Geophysical Research Letters, Vol 50, Iss 22, Pp n/a-n/a (2023)
op_relation https://doi.org/10.1029/2023GL106088
https://doaj.org/toc/0094-8276
https://doaj.org/toc/1944-8007
1944-8007
0094-8276
doi:10.1029/2023GL106088
https://doaj.org/article/0dc1d032882a4e22aeee4ff517cf6882
op_doi https://doi.org/10.1029/2023GL106088
container_title Geophysical Research Letters
container_volume 50
container_issue 22
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