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...

Full description

Bibliographic Details
Published in:Weather and Climate Dynamics
Main Authors: Strommen, Kristian, Woollings, Tim, Davini, Paolo, Ruggieri, Paolo, Simpson, Isla R.
Format: Text
Language:English
Published: 2023
Subjects:
Online Access:https://doi.org/10.5194/wcd-4-853-2023
https://wcd.copernicus.org/articles/4/853/2023/
id ftcopernicus:oai:publications.copernicus.org:wcd109790
record_format openpolar
spelling ftcopernicus:oai:publications.copernicus.org:wcd109790 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. 2023-10-09 application/pdf https://doi.org/10.5194/wcd-4-853-2023 https://wcd.copernicus.org/articles/4/853/2023/ eng eng doi:10.5194/wcd-4-853-2023 https://wcd.copernicus.org/articles/4/853/2023/ eISSN: 2698-4016 Text 2023 ftcopernicus https://doi.org/10.5194/wcd-4-853-2023 2023-10-16T16:24:16Z 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. Text North Atlantic North Atlantic oscillation Copernicus Publications: E-Journals Weather and Climate Dynamics 4 4 853 874
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
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 Text
author Strommen, Kristian
Woollings, Tim
Davini, Paolo
Ruggieri, Paolo
Simpson, Isla R.
spellingShingle 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
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
publishDate 2023
url 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_source eISSN: 2698-4016
op_relation doi:10.5194/wcd-4-853-2023
https://wcd.copernicus.org/articles/4/853/2023/
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
_version_ 1782336958392958976