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...
Published in: | Atmosphere |
---|---|
Main Author: | |
Format: | Text |
Language: | English |
Published: |
Multidisciplinary Digital Publishing Institute
2023
|
Subjects: | |
Online Access: | https://doi.org/10.3390/atmos14061011 |
id |
ftmdpi:oai:mdpi.com:/2073-4433/14/6/1011/ |
---|---|
record_format |
openpolar |
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 |
_version_ |
1774720390481838080 |