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: Kristian Strommen, Tim Woollings, Paolo Davini, Paolo Ruggieri, Isla R. Simpson
Other Authors: Tim Woolling
Format: Article in Journal/Newspaper
Language:English
Published: 2023
Subjects:
Online Access:https://hdl.handle.net/11585/950376
https://doi.org/10.5194/wcd-4-853-2023
https://wcd.copernicus.org/articles/4/853/2023/
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spelling ftunibolognairis:oai:cris.unibo.it:11585/950376 2024-04-14T08:15:22+00:00 Predictable decadal forcing of the North Atlantic jet speed by sub-polar North Atlantic sea surface temperatures Kristian Strommen Tim Woollings Paolo Davini Paolo Ruggieri Isla R. Simpson Kristian Strommen Tim Woolling Paolo Davini Paolo Ruggieri Isla R. Simpson 2023 ELETTRONICO https://hdl.handle.net/11585/950376 https://doi.org/10.5194/wcd-4-853-2023 https://wcd.copernicus.org/articles/4/853/2023/ eng eng volume:4 issue:4 firstpage:853 lastpage:874 numberofpages:22 journal:WEATHER AND CLIMATE DYNAMICS (ONLINE) https://hdl.handle.net/11585/950376 doi:10.5194/wcd-4-853-2023 info:eu-repo/semantics/altIdentifier/scopus/2-s2.0-85178217260 https://wcd.copernicus.org/articles/4/853/2023/ info:eu-repo/semantics/openAccess Climate variability decadal predictions info:eu-repo/semantics/article 2023 ftunibolognairis https://doi.org/10.5194/wcd-4-853-2023 2024-03-21T17:04:58Z 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 IRIS Università degli Studi di Bologna (CRIS - Current Research Information System) Weather and Climate Dynamics 4 4 853 874
institution Open Polar
collection IRIS Università degli Studi di Bologna (CRIS - Current Research Information System)
op_collection_id ftunibolognairis
language English
topic Climate variability
decadal predictions
spellingShingle Climate variability
decadal predictions
Kristian Strommen
Tim Woollings
Paolo Davini
Paolo Ruggieri
Isla R. Simpson
Predictable decadal forcing of the North Atlantic jet speed by sub-polar North Atlantic sea surface temperatures
topic_facet Climate variability
decadal predictions
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.
author2 Kristian Strommen
Tim Woolling
Paolo Davini
Paolo Ruggieri
Isla R. Simpson
format Article in Journal/Newspaper
author Kristian Strommen
Tim Woollings
Paolo Davini
Paolo Ruggieri
Isla R. Simpson
author_facet Kristian Strommen
Tim Woollings
Paolo Davini
Paolo Ruggieri
Isla R. Simpson
author_sort Kristian Strommen
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
publishDate 2023
url https://hdl.handle.net/11585/950376
https://doi.org/10.5194/wcd-4-853-2023
https://wcd.copernicus.org/articles/4/853/2023/
genre North Atlantic
North Atlantic oscillation
genre_facet North Atlantic
North Atlantic oscillation
op_relation volume:4
issue:4
firstpage:853
lastpage:874
numberofpages:22
journal:WEATHER AND CLIMATE DYNAMICS (ONLINE)
https://hdl.handle.net/11585/950376
doi:10.5194/wcd-4-853-2023
info:eu-repo/semantics/altIdentifier/scopus/2-s2.0-85178217260
https://wcd.copernicus.org/articles/4/853/2023/
op_rights 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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