Mechanism for potential strengthening of Atlantic overturning prior to collapse
The Atlantic meridional overturning circulation (AMOC) carries large amounts of heat into the North Atlantic influencing climate regionally as well as globally. Palaeo-records and simulations with comprehensive climate models suggest that the positive salt-advection feedback may yield a threshold be...
Main Authors: | , |
---|---|
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
München : European Geopyhsical Union
2014
|
Subjects: | |
Online Access: | https://doi.org/10.34657/337 https://oa.tib.eu/renate/handle/123456789/3742 |
id |
ftleibnizopen:oai:oai.leibnizopen.de:R1u78IgBdbrxVwz6XZZI |
---|---|
record_format |
openpolar |
spelling |
ftleibnizopen:oai:oai.leibnizopen.de:R1u78IgBdbrxVwz6XZZI 2023-07-16T03:59:43+02:00 Mechanism for potential strengthening of Atlantic overturning prior to collapse Ehlert, D. Levermann, A. 2014 application/pdf https://doi.org/10.34657/337 https://oa.tib.eu/renate/handle/123456789/3742 eng eng München : European Geopyhsical Union CC BY 3.0 Unported https://creativecommons.org/licenses/by/3.0/ Earth System Dynamics, Volume 5, Issue 2, Page 383-397 Climate models Computer simulation Water Atlantic meridional overturning circulationsConceptual model Degree of freedom Density-dependent Eddy transports Freshwater fluxes Meridional overturning circulations North Atlantic 500 article Text 2014 ftleibnizopen https://doi.org/10.34657/337 2023-06-25T23:15:19Z The Atlantic meridional overturning circulation (AMOC) carries large amounts of heat into the North Atlantic influencing climate regionally as well as globally. Palaeo-records and simulations with comprehensive climate models suggest that the positive salt-advection feedback may yield a threshold behaviour of the system. That is to say that beyond a certain amount of freshwater flux into the North Atlantic, no meridional overturning circulation can be sustained. Concepts of monitoring the AMOC and identifying its vicinity to the threshold rely on the fact that the volume flux defining the AMOC will be reduced when approaching the threshold. Here we advance conceptual models that have been used in a paradigmatic way to understand the AMOC, by introducing a density-dependent parameterization for the Southern Ocean eddies. This additional degree of freedom uncovers a mechanism by which the AMOC can increase with additional freshwater flux into the North Atlantic, before it reaches the threshold and collapses: an AMOC that is mainly wind-driven will have a constant upwelling as long as the Southern Ocean winds do not change significantly. The downward transport of tracers occurs either in the northern sinking regions or through Southern Ocean eddies. If freshwater is transported, either atmospherically or via horizontal gyres, from the low to high latitudes, this would reduce the eddy transport and by continuity increase the northern sinking which defines the AMOC until a threshold is reached at which the AMOC cannot be sustained. If dominant in the real ocean this mechanism would have significant consequences for monitoring the AMOC. publishedVersion Article in Journal/Newspaper North Atlantic Southern Ocean LeibnizOpen (The Leibniz Association) Southern Ocean |
institution |
Open Polar |
collection |
LeibnizOpen (The Leibniz Association) |
op_collection_id |
ftleibnizopen |
language |
English |
topic |
Climate models Computer simulation Water Atlantic meridional overturning circulationsConceptual model Degree of freedom Density-dependent Eddy transports Freshwater fluxes Meridional overturning circulations North Atlantic 500 |
spellingShingle |
Climate models Computer simulation Water Atlantic meridional overturning circulationsConceptual model Degree of freedom Density-dependent Eddy transports Freshwater fluxes Meridional overturning circulations North Atlantic 500 Ehlert, D. Levermann, A. Mechanism for potential strengthening of Atlantic overturning prior to collapse |
topic_facet |
Climate models Computer simulation Water Atlantic meridional overturning circulationsConceptual model Degree of freedom Density-dependent Eddy transports Freshwater fluxes Meridional overturning circulations North Atlantic 500 |
description |
The Atlantic meridional overturning circulation (AMOC) carries large amounts of heat into the North Atlantic influencing climate regionally as well as globally. Palaeo-records and simulations with comprehensive climate models suggest that the positive salt-advection feedback may yield a threshold behaviour of the system. That is to say that beyond a certain amount of freshwater flux into the North Atlantic, no meridional overturning circulation can be sustained. Concepts of monitoring the AMOC and identifying its vicinity to the threshold rely on the fact that the volume flux defining the AMOC will be reduced when approaching the threshold. Here we advance conceptual models that have been used in a paradigmatic way to understand the AMOC, by introducing a density-dependent parameterization for the Southern Ocean eddies. This additional degree of freedom uncovers a mechanism by which the AMOC can increase with additional freshwater flux into the North Atlantic, before it reaches the threshold and collapses: an AMOC that is mainly wind-driven will have a constant upwelling as long as the Southern Ocean winds do not change significantly. The downward transport of tracers occurs either in the northern sinking regions or through Southern Ocean eddies. If freshwater is transported, either atmospherically or via horizontal gyres, from the low to high latitudes, this would reduce the eddy transport and by continuity increase the northern sinking which defines the AMOC until a threshold is reached at which the AMOC cannot be sustained. If dominant in the real ocean this mechanism would have significant consequences for monitoring the AMOC. publishedVersion |
format |
Article in Journal/Newspaper |
author |
Ehlert, D. Levermann, A. |
author_facet |
Ehlert, D. Levermann, A. |
author_sort |
Ehlert, D. |
title |
Mechanism for potential strengthening of Atlantic overturning prior to collapse |
title_short |
Mechanism for potential strengthening of Atlantic overturning prior to collapse |
title_full |
Mechanism for potential strengthening of Atlantic overturning prior to collapse |
title_fullStr |
Mechanism for potential strengthening of Atlantic overturning prior to collapse |
title_full_unstemmed |
Mechanism for potential strengthening of Atlantic overturning prior to collapse |
title_sort |
mechanism for potential strengthening of atlantic overturning prior to collapse |
publisher |
München : European Geopyhsical Union |
publishDate |
2014 |
url |
https://doi.org/10.34657/337 https://oa.tib.eu/renate/handle/123456789/3742 |
geographic |
Southern Ocean |
geographic_facet |
Southern Ocean |
genre |
North Atlantic Southern Ocean |
genre_facet |
North Atlantic Southern Ocean |
op_source |
Earth System Dynamics, Volume 5, Issue 2, Page 383-397 |
op_rights |
CC BY 3.0 Unported https://creativecommons.org/licenses/by/3.0/ |
op_doi |
https://doi.org/10.34657/337 |
_version_ |
1771547907447586816 |