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...

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Published in:Earth System Dynamics
Main Authors: Ehlert, D., Levermann, Anders (Prof. Dr.)
Format: Article in Journal/Newspaper
Language:English
Published: 2014
Subjects:
Online Access:https://publishup.uni-potsdam.de/frontdoor/index/index/docId/38195
https://doi.org/10.5194/esd-5-383-2014
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spelling ftubpotsdam:oai:kobv.de-opus4-uni-potsdam:38195 2024-04-21T08:07:29+00:00 Mechanism for potential strengthening of Atlantic overturning prior to collapse Ehlert, D. Levermann, Anders (Prof. Dr.) 2014 https://publishup.uni-potsdam.de/frontdoor/index/index/docId/38195 https://doi.org/10.5194/esd-5-383-2014 eng eng https://publishup.uni-potsdam.de/frontdoor/index/index/docId/38195 https://doi.org/10.5194/esd-5-383-2014 info:eu-repo/semantics/closedAccess Institut für Physik und Astronomie article doc-type:article 2014 ftubpotsdam https://doi.org/10.5194/esd-5-383-2014 2024-03-27T15:02:48Z 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. Article in Journal/Newspaper North Atlantic Southern Ocean University of Potsdam: publish.UP Earth System Dynamics 5 2 383 397
institution Open Polar
collection University of Potsdam: publish.UP
op_collection_id ftubpotsdam
language English
topic Institut für Physik und Astronomie
spellingShingle Institut für Physik und Astronomie
Ehlert, D.
Levermann, Anders (Prof. Dr.)
Mechanism for potential strengthening of Atlantic overturning prior to collapse
topic_facet Institut für Physik und Astronomie
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.
format Article in Journal/Newspaper
author Ehlert, D.
Levermann, Anders (Prof. Dr.)
author_facet Ehlert, D.
Levermann, Anders (Prof. Dr.)
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
publishDate 2014
url https://publishup.uni-potsdam.de/frontdoor/index/index/docId/38195
https://doi.org/10.5194/esd-5-383-2014
genre North Atlantic
Southern Ocean
genre_facet North Atlantic
Southern Ocean
op_relation https://publishup.uni-potsdam.de/frontdoor/index/index/docId/38195
https://doi.org/10.5194/esd-5-383-2014
op_rights info:eu-repo/semantics/closedAccess
op_doi https://doi.org/10.5194/esd-5-383-2014
container_title Earth System Dynamics
container_volume 5
container_issue 2
container_start_page 383
op_container_end_page 397
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