ENSO-driven abrupt phase shift in North Atlantic oscillation in early January

Abstract El Niño-Southern Oscillation (ENSO) teleconnections exhibit a strong dependency on seasonally and intraseasonally varying mean states, leading to impactful short-term variations in regional climate. The North Atlantic Oscillation (NAO)-ENSO relation is a typical example, in that its phase r...

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Published in:npj Climate and Atmospheric Science
Main Authors: Xin Geng, Jiuwei Zhao, Jong-Seong Kug
Format: Article in Journal/Newspaper
Language:English
Published: Nature Portfolio 2023
Subjects:
Online Access:https://doi.org/10.1038/s41612-023-00414-2
https://doaj.org/article/1b15a9b1b9324d9193f54c00e66147c6
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spelling ftdoajarticles:oai:doaj.org/article:1b15a9b1b9324d9193f54c00e66147c6 2023-07-30T04:05:12+02:00 ENSO-driven abrupt phase shift in North Atlantic oscillation in early January Xin Geng Jiuwei Zhao Jong-Seong Kug 2023-07-01T00:00:00Z https://doi.org/10.1038/s41612-023-00414-2 https://doaj.org/article/1b15a9b1b9324d9193f54c00e66147c6 EN eng Nature Portfolio https://doi.org/10.1038/s41612-023-00414-2 https://doaj.org/toc/2397-3722 doi:10.1038/s41612-023-00414-2 2397-3722 https://doaj.org/article/1b15a9b1b9324d9193f54c00e66147c6 npj Climate and Atmospheric Science, Vol 6, Iss 1, Pp 1-8 (2023) Environmental sciences GE1-350 Meteorology. Climatology QC851-999 article 2023 ftdoajarticles https://doi.org/10.1038/s41612-023-00414-2 2023-07-16T00:38:39Z Abstract El Niño-Southern Oscillation (ENSO) teleconnections exhibit a strong dependency on seasonally and intraseasonally varying mean states, leading to impactful short-term variations in regional climate. The North Atlantic Oscillation (NAO)-ENSO relation is a typical example, in that its phase relationship reverses systematically between the early and late winter. Here based on observations and an ensemble of atmosphere-only climate model simulations, we reveal that this NAO phase reversal occurs synchronously in early January, showing strong abruptness. We demonstrate that this abrupt NAO phase reversal is caused by the change in ENSO-induced Rossby wave-propagating direction from northeastward to southeastward over the northeastern North American region, which is largely governed by a climatological alteration of the local jet meridional shear. We also provide evidence that the North Atlantic intrinsic eddy–low-frequency flow feedback further amplifies the NAO responses. This ENSO-related abrupt NAO change offers an avenue for intraseasonal climate forecasting in the Euro-Atlantic region. Article in Journal/Newspaper North Atlantic North Atlantic oscillation Directory of Open Access Journals: DOAJ Articles npj Climate and Atmospheric Science 6 1
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
spellingShingle Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
Xin Geng
Jiuwei Zhao
Jong-Seong Kug
ENSO-driven abrupt phase shift in North Atlantic oscillation in early January
topic_facet Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
description Abstract El Niño-Southern Oscillation (ENSO) teleconnections exhibit a strong dependency on seasonally and intraseasonally varying mean states, leading to impactful short-term variations in regional climate. The North Atlantic Oscillation (NAO)-ENSO relation is a typical example, in that its phase relationship reverses systematically between the early and late winter. Here based on observations and an ensemble of atmosphere-only climate model simulations, we reveal that this NAO phase reversal occurs synchronously in early January, showing strong abruptness. We demonstrate that this abrupt NAO phase reversal is caused by the change in ENSO-induced Rossby wave-propagating direction from northeastward to southeastward over the northeastern North American region, which is largely governed by a climatological alteration of the local jet meridional shear. We also provide evidence that the North Atlantic intrinsic eddy–low-frequency flow feedback further amplifies the NAO responses. This ENSO-related abrupt NAO change offers an avenue for intraseasonal climate forecasting in the Euro-Atlantic region.
format Article in Journal/Newspaper
author Xin Geng
Jiuwei Zhao
Jong-Seong Kug
author_facet Xin Geng
Jiuwei Zhao
Jong-Seong Kug
author_sort Xin Geng
title ENSO-driven abrupt phase shift in North Atlantic oscillation in early January
title_short ENSO-driven abrupt phase shift in North Atlantic oscillation in early January
title_full ENSO-driven abrupt phase shift in North Atlantic oscillation in early January
title_fullStr ENSO-driven abrupt phase shift in North Atlantic oscillation in early January
title_full_unstemmed ENSO-driven abrupt phase shift in North Atlantic oscillation in early January
title_sort enso-driven abrupt phase shift in north atlantic oscillation in early january
publisher Nature Portfolio
publishDate 2023
url https://doi.org/10.1038/s41612-023-00414-2
https://doaj.org/article/1b15a9b1b9324d9193f54c00e66147c6
genre North Atlantic
North Atlantic oscillation
genre_facet North Atlantic
North Atlantic oscillation
op_source npj Climate and Atmospheric Science, Vol 6, Iss 1, Pp 1-8 (2023)
op_relation https://doi.org/10.1038/s41612-023-00414-2
https://doaj.org/toc/2397-3722
doi:10.1038/s41612-023-00414-2
2397-3722
https://doaj.org/article/1b15a9b1b9324d9193f54c00e66147c6
op_doi https://doi.org/10.1038/s41612-023-00414-2
container_title npj Climate and Atmospheric Science
container_volume 6
container_issue 1
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