Enhanced Atlantic subpolar gyre variability through baroclinic threshold in a coarse resolution model

Direct observations, satellite measurements and paleo records reveal strong variability in the Atlantic subpolar gyre on various time scales. Here we show that variations of comparable amplitude can only be simulated in a coupled climate model in the proximity of a dynamical threshold. The threshold...

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Main Authors: Mengel, M., Levermann, A., Schleussner, C.-F., Born, A.
Format: Article in Journal/Newspaper
Language:English
Published: München : European Geopyhsical Union 2012
Subjects:
550
Online Access:https://doi.org/10.34657/931
https://oa.tib.eu/renate/handle/123456789/722
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spelling ftleibnizopen:oai:oai.leibnizopen.de:VRN2DYsBBwLIz6xGqehC 2023-11-05T03:43:43+01:00 Enhanced Atlantic subpolar gyre variability through baroclinic threshold in a coarse resolution model Mengel, M. Levermann, A. Schleussner, C.-F. Born, A. 2012 application/pdf https://doi.org/10.34657/931 https://oa.tib.eu/renate/handle/123456789/722 eng eng München : European Geopyhsical Union CC BY 3.0 Unported https://creativecommons.org/licenses/by/3.0/ Earth System Dynamics, Volume 3, Issue 2, Page 189-197 Atmosphere models Atmospheric variability Baroclinic Climate variability Coarse-resolution model Coupled climate model Deep convection Dynamical threshold Model system North Atlantic North Atlantic Ocean Ocean general circulation models Salt transport Satellite measurements Self-amplification Small amplitude Subpolar gyres Time-scales Statistical-dynamical 550 article Text 2012 ftleibnizopen https://doi.org/10.34657/931 2023-10-08T23:09:54Z Direct observations, satellite measurements and paleo records reveal strong variability in the Atlantic subpolar gyre on various time scales. Here we show that variations of comparable amplitude can only be simulated in a coupled climate model in the proximity of a dynamical threshold. The threshold and the associated dynamic response is due to a positive feedback involving increased salt transport in the subpolar gyre and enhanced deep convection in its centre. A series of sensitivity experiments is performed with a coarse resolution ocean general circulation model coupled to a statistical-dynamical atmosphere model which in itself does not produce atmospheric variability. To simulate the impact of atmospheric variability, the model system is perturbed with freshwater forcing of varying, but small amplitude and multi-decadal to centennial periodicities and observational variations in wind stress. While both freshwater and wind-stress-forcing have a small direct effect on the strength of the subpolar gyre, the magnitude of the gyre's response is strongly increased in the vicinity of the threshold. Our results indicate that baroclinic self-amplification in the North Atlantic ocean can play an important role in presently observed SPG variability and thereby North Atlantic climate variability on multi-decadal scales. publishedVersion Article in Journal/Newspaper North Atlantic LeibnizOpen (The Leibniz Association)
institution Open Polar
collection LeibnizOpen (The Leibniz Association)
op_collection_id ftleibnizopen
language English
topic Atmosphere models
Atmospheric variability
Baroclinic
Climate variability
Coarse-resolution model
Coupled climate model
Deep convection
Dynamical threshold
Model system
North Atlantic
North Atlantic Ocean
Ocean general circulation models
Salt transport
Satellite measurements
Self-amplification
Small amplitude
Subpolar gyres
Time-scales
Statistical-dynamical
550
spellingShingle Atmosphere models
Atmospheric variability
Baroclinic
Climate variability
Coarse-resolution model
Coupled climate model
Deep convection
Dynamical threshold
Model system
North Atlantic
North Atlantic Ocean
Ocean general circulation models
Salt transport
Satellite measurements
Self-amplification
Small amplitude
Subpolar gyres
Time-scales
Statistical-dynamical
550
Mengel, M.
Levermann, A.
Schleussner, C.-F.
Born, A.
Enhanced Atlantic subpolar gyre variability through baroclinic threshold in a coarse resolution model
topic_facet Atmosphere models
Atmospheric variability
Baroclinic
Climate variability
Coarse-resolution model
Coupled climate model
Deep convection
Dynamical threshold
Model system
North Atlantic
North Atlantic Ocean
Ocean general circulation models
Salt transport
Satellite measurements
Self-amplification
Small amplitude
Subpolar gyres
Time-scales
Statistical-dynamical
550
description Direct observations, satellite measurements and paleo records reveal strong variability in the Atlantic subpolar gyre on various time scales. Here we show that variations of comparable amplitude can only be simulated in a coupled climate model in the proximity of a dynamical threshold. The threshold and the associated dynamic response is due to a positive feedback involving increased salt transport in the subpolar gyre and enhanced deep convection in its centre. A series of sensitivity experiments is performed with a coarse resolution ocean general circulation model coupled to a statistical-dynamical atmosphere model which in itself does not produce atmospheric variability. To simulate the impact of atmospheric variability, the model system is perturbed with freshwater forcing of varying, but small amplitude and multi-decadal to centennial periodicities and observational variations in wind stress. While both freshwater and wind-stress-forcing have a small direct effect on the strength of the subpolar gyre, the magnitude of the gyre's response is strongly increased in the vicinity of the threshold. Our results indicate that baroclinic self-amplification in the North Atlantic ocean can play an important role in presently observed SPG variability and thereby North Atlantic climate variability on multi-decadal scales. publishedVersion
format Article in Journal/Newspaper
author Mengel, M.
Levermann, A.
Schleussner, C.-F.
Born, A.
author_facet Mengel, M.
Levermann, A.
Schleussner, C.-F.
Born, A.
author_sort Mengel, M.
title Enhanced Atlantic subpolar gyre variability through baroclinic threshold in a coarse resolution model
title_short Enhanced Atlantic subpolar gyre variability through baroclinic threshold in a coarse resolution model
title_full Enhanced Atlantic subpolar gyre variability through baroclinic threshold in a coarse resolution model
title_fullStr Enhanced Atlantic subpolar gyre variability through baroclinic threshold in a coarse resolution model
title_full_unstemmed Enhanced Atlantic subpolar gyre variability through baroclinic threshold in a coarse resolution model
title_sort enhanced atlantic subpolar gyre variability through baroclinic threshold in a coarse resolution model
publisher München : European Geopyhsical Union
publishDate 2012
url https://doi.org/10.34657/931
https://oa.tib.eu/renate/handle/123456789/722
genre North Atlantic
genre_facet North Atlantic
op_source Earth System Dynamics, Volume 3, Issue 2, Page 189-197
op_rights CC BY 3.0 Unported
https://creativecommons.org/licenses/by/3.0/
op_doi https://doi.org/10.34657/931
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