Predictable decadal forcing of the North Atlantic jet speed by sub-polar North Atlantic sea surface temperatures

It has been demonstrated that decadal variations in the North Atlantic Oscillation (NAO) can be predicted by current forecast models. While Atlantic Multidecadal Variability (AMV) in sea surface temperatures (SSTs) has been hypothesised as the source of this skill, the validity of this hypothesis an...

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Published in:Weather and Climate Dynamics
Main Authors: Strommen, Kristian, Woollings, Tim, Davini, Paolo, Ruggieri, Paolo, Simpson, Isla R.
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2023
Subjects:
Online Access:https://doi.org/10.5194/wcd-4-853-2023
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spelling ftnonlinearchiv:oai:noa.gwlb.de:cop_mods_00069184 2023-11-12T04:21:38+01:00 Predictable decadal forcing of the North Atlantic jet speed by sub-polar North Atlantic sea surface temperatures Strommen, Kristian Woollings, Tim Davini, Paolo Ruggieri, Paolo Simpson, Isla R. 2023-10 electronic https://doi.org/10.5194/wcd-4-853-2023 https://noa.gwlb.de/receive/cop_mods_00069184 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00067582/wcd-4-853-2023.pdf https://wcd.copernicus.org/articles/4/853/2023/wcd-4-853-2023.pdf eng eng Copernicus Publications Weather and Climate Dynamics -- https://www.weather-climate-dynamics.net/ -- 2698-4016 https://doi.org/10.5194/wcd-4-853-2023 https://noa.gwlb.de/receive/cop_mods_00069184 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00067582/wcd-4-853-2023.pdf https://wcd.copernicus.org/articles/4/853/2023/wcd-4-853-2023.pdf https://creativecommons.org/licenses/by/4.0/ uneingeschränkt info:eu-repo/semantics/openAccess article Verlagsveröffentlichung article Text doc-type:article 2023 ftnonlinearchiv https://doi.org/10.5194/wcd-4-853-2023 2023-10-15T23:22:18Z It has been demonstrated that decadal variations in the North Atlantic Oscillation (NAO) can be predicted by current forecast models. While Atlantic Multidecadal Variability (AMV) in sea surface temperatures (SSTs) has been hypothesised as the source of this skill, the validity of this hypothesis and the pathways involved remain unclear. We show, using reanalysis and data from two forecast models, that the decadal predictability of the NAO can be entirely accounted for by the predictability of decadal variations in the speed of the North Atlantic eddy-driven jet, with no predictability of decadal variations in the jet latitude. The sub-polar North Atlantic (SPNA) is identified as the only obvious common source of an SST-based signal across the models and reanalysis, and the predictability of the jet speed is shown to be consistent with a forcing from the SPNA visible already within a single season. The pathway is argued to be tropospheric in nature, with the SPNA-associated heating extending up to the mid-troposphere, which alters the meridional temperature gradient around the climatological jet core. The relative roles of anthropogenic aerosol emissions and the Atlantic Meridional Overturning Circulation (AMOC) at generating predictable SPNA variability are also discussed. The analysis is extensively supported by the novel use of a set of seasonal hindcasts spanning the 20th century and forced with prescribed SSTs. Article in Journal/Newspaper North Atlantic North Atlantic oscillation Niedersächsisches Online-Archiv NOA Weather and Climate Dynamics 4 4 853 874
institution Open Polar
collection Niedersächsisches Online-Archiv NOA
op_collection_id ftnonlinearchiv
language English
topic article
Verlagsveröffentlichung
spellingShingle article
Verlagsveröffentlichung
Strommen, Kristian
Woollings, Tim
Davini, Paolo
Ruggieri, Paolo
Simpson, Isla R.
Predictable decadal forcing of the North Atlantic jet speed by sub-polar North Atlantic sea surface temperatures
topic_facet article
Verlagsveröffentlichung
description It has been demonstrated that decadal variations in the North Atlantic Oscillation (NAO) can be predicted by current forecast models. While Atlantic Multidecadal Variability (AMV) in sea surface temperatures (SSTs) has been hypothesised as the source of this skill, the validity of this hypothesis and the pathways involved remain unclear. We show, using reanalysis and data from two forecast models, that the decadal predictability of the NAO can be entirely accounted for by the predictability of decadal variations in the speed of the North Atlantic eddy-driven jet, with no predictability of decadal variations in the jet latitude. The sub-polar North Atlantic (SPNA) is identified as the only obvious common source of an SST-based signal across the models and reanalysis, and the predictability of the jet speed is shown to be consistent with a forcing from the SPNA visible already within a single season. The pathway is argued to be tropospheric in nature, with the SPNA-associated heating extending up to the mid-troposphere, which alters the meridional temperature gradient around the climatological jet core. The relative roles of anthropogenic aerosol emissions and the Atlantic Meridional Overturning Circulation (AMOC) at generating predictable SPNA variability are also discussed. The analysis is extensively supported by the novel use of a set of seasonal hindcasts spanning the 20th century and forced with prescribed SSTs.
format Article in Journal/Newspaper
author Strommen, Kristian
Woollings, Tim
Davini, Paolo
Ruggieri, Paolo
Simpson, Isla R.
author_facet Strommen, Kristian
Woollings, Tim
Davini, Paolo
Ruggieri, Paolo
Simpson, Isla R.
author_sort Strommen, Kristian
title Predictable decadal forcing of the North Atlantic jet speed by sub-polar North Atlantic sea surface temperatures
title_short Predictable decadal forcing of the North Atlantic jet speed by sub-polar North Atlantic sea surface temperatures
title_full Predictable decadal forcing of the North Atlantic jet speed by sub-polar North Atlantic sea surface temperatures
title_fullStr Predictable decadal forcing of the North Atlantic jet speed by sub-polar North Atlantic sea surface temperatures
title_full_unstemmed Predictable decadal forcing of the North Atlantic jet speed by sub-polar North Atlantic sea surface temperatures
title_sort predictable decadal forcing of the north atlantic jet speed by sub-polar north atlantic sea surface temperatures
publisher Copernicus Publications
publishDate 2023
url https://doi.org/10.5194/wcd-4-853-2023
https://noa.gwlb.de/receive/cop_mods_00069184
https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00067582/wcd-4-853-2023.pdf
https://wcd.copernicus.org/articles/4/853/2023/wcd-4-853-2023.pdf
genre North Atlantic
North Atlantic oscillation
genre_facet North Atlantic
North Atlantic oscillation
op_relation Weather and Climate Dynamics -- https://www.weather-climate-dynamics.net/ -- 2698-4016
https://doi.org/10.5194/wcd-4-853-2023
https://noa.gwlb.de/receive/cop_mods_00069184
https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00067582/wcd-4-853-2023.pdf
https://wcd.copernicus.org/articles/4/853/2023/wcd-4-853-2023.pdf
op_rights https://creativecommons.org/licenses/by/4.0/
uneingeschränkt
info:eu-repo/semantics/openAccess
op_doi https://doi.org/10.5194/wcd-4-853-2023
container_title Weather and Climate Dynamics
container_volume 4
container_issue 4
container_start_page 853
op_container_end_page 874
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