Instability of Atlantic Meridional Overturning Circulation: Observations, Modelling and Relevance to Present and Future

The Atlantic Meridional Overturning Circulation (AMOC) has changed dramatically during the glacial–interglacial cycle. One leading hypothesis for these abrupt changes is thermohaline instability. Here, I review recent progress towards understanding thermohaline instability in both observations and m...

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Published in:Atmosphere
Main Author: Zhengyu Liu
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2023
Subjects:
Online Access:https://doi.org/10.3390/atmos14061011
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spelling ftmdpi:oai:mdpi.com:/2073-4433/14/6/1011/ 2023-08-20T04:08:14+02:00 Instability of Atlantic Meridional Overturning Circulation: Observations, Modelling and Relevance to Present and Future Zhengyu Liu agris 2023-06-12 application/pdf https://doi.org/10.3390/atmos14061011 EN eng Multidisciplinary Digital Publishing Institute https://dx.doi.org/10.3390/atmos14061011 https://creativecommons.org/licenses/by/4.0/ Atmosphere; Volume 14; Issue 6; Pages: 1011 thermohaline instability model bias abrupt changes Text 2023 ftmdpi https://doi.org/10.3390/atmos14061011 2023-08-01T10:26:29Z The Atlantic Meridional Overturning Circulation (AMOC) has changed dramatically during the glacial–interglacial cycle. One leading hypothesis for these abrupt changes is thermohaline instability. Here, I review recent progress towards understanding thermohaline instability in both observations and modelling. Proxy records available seem to favor thermohaline instability as the cause of the abrupt climate changes during the glacial–deglacial period because the deep North Atlantic water mass and AMOC seemed to have changed before the North Atlantic climate. However, most fully Coupled General Circulation Models (CGCMs) so far seem to exhibit monostable AMOC, because (1) these models have failed to simulate abrupt AMOC changes unless they are forced by an abrupt change of external forcing and, (2) these models have shown opposite freshwater convergence from the current observations. This potential model bias in the AMOC stability leaves the model projection of the future AMOC change uncertain. Text North Atlantic MDPI Open Access Publishing Atmosphere 14 6 1011
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic thermohaline instability
model bias
abrupt changes
spellingShingle thermohaline instability
model bias
abrupt changes
Zhengyu Liu
Instability of Atlantic Meridional Overturning Circulation: Observations, Modelling and Relevance to Present and Future
topic_facet thermohaline instability
model bias
abrupt changes
description The Atlantic Meridional Overturning Circulation (AMOC) has changed dramatically during the glacial–interglacial cycle. One leading hypothesis for these abrupt changes is thermohaline instability. Here, I review recent progress towards understanding thermohaline instability in both observations and modelling. Proxy records available seem to favor thermohaline instability as the cause of the abrupt climate changes during the glacial–deglacial period because the deep North Atlantic water mass and AMOC seemed to have changed before the North Atlantic climate. However, most fully Coupled General Circulation Models (CGCMs) so far seem to exhibit monostable AMOC, because (1) these models have failed to simulate abrupt AMOC changes unless they are forced by an abrupt change of external forcing and, (2) these models have shown opposite freshwater convergence from the current observations. This potential model bias in the AMOC stability leaves the model projection of the future AMOC change uncertain.
format Text
author Zhengyu Liu
author_facet Zhengyu Liu
author_sort Zhengyu Liu
title Instability of Atlantic Meridional Overturning Circulation: Observations, Modelling and Relevance to Present and Future
title_short Instability of Atlantic Meridional Overturning Circulation: Observations, Modelling and Relevance to Present and Future
title_full Instability of Atlantic Meridional Overturning Circulation: Observations, Modelling and Relevance to Present and Future
title_fullStr Instability of Atlantic Meridional Overturning Circulation: Observations, Modelling and Relevance to Present and Future
title_full_unstemmed Instability of Atlantic Meridional Overturning Circulation: Observations, Modelling and Relevance to Present and Future
title_sort instability of atlantic meridional overturning circulation: observations, modelling and relevance to present and future
publisher Multidisciplinary Digital Publishing Institute
publishDate 2023
url https://doi.org/10.3390/atmos14061011
op_coverage agris
genre North Atlantic
genre_facet North Atlantic
op_source Atmosphere; Volume 14; Issue 6; Pages: 1011
op_relation https://dx.doi.org/10.3390/atmos14061011
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/atmos14061011
container_title Atmosphere
container_volume 14
container_issue 6
container_start_page 1011
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