The Sudden Stratospheric Warming Events in the Antarctic in 2024

Abstract In July and August 2024, two consecutive stratospheric sudden warming (SSW) events (termed SW07 and SW08) occurred over Antarctic, both featuring a rapid 17°C temperature rise at 10 hPa and significant stratospheric polar vortex (SPV) deceleration. SW07 occurred at the earliest winter time...

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Published in:Geophysical Research Letters
Main Authors: Yucheng Zi, Zhenxia Long, Jinyu Sheng, Gaopeng Lu, Will Perrie, Ziniu Xiao
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2025
Subjects:
Online Access:https://doi.org/10.1029/2025GL115257
https://doaj.org/article/f79471765ebd42b8bfedefecb69598a4
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author Yucheng Zi
Zhenxia Long
Jinyu Sheng
Gaopeng Lu
Will Perrie
Ziniu Xiao
author_facet Yucheng Zi
Zhenxia Long
Jinyu Sheng
Gaopeng Lu
Will Perrie
Ziniu Xiao
author_sort Yucheng Zi
collection Directory of Open Access Journals: DOAJ Articles
container_issue 7
container_title Geophysical Research Letters
container_volume 52
description Abstract In July and August 2024, two consecutive stratospheric sudden warming (SSW) events (termed SW07 and SW08) occurred over Antarctic, both featuring a rapid 17°C temperature rise at 10 hPa and significant stratospheric polar vortex (SPV) deceleration. SW07 occurred at the earliest winter time of the year recorded in the satellite era (1979 to present). The study found that, strong blocking highs affected stratospheric warming via nonlinear planetary wave prior to SW07, and the substantial sea ice loss over Antarctic Ross Sea and Amundsen Sea likely created favorable conditions for the formation of these blocking highs. Furthermore, the stratospheric preconditioning significantly amplified the intensity of the planetary waves. A downward‐propagating negative Southern Annular Mode (SAM) signal after SW07 supported blocking highs, creating a favorable circulation for planetary wave perturbations prior to SW08. In addition, enhanced ozone transport from low latitudes to the pole during SW07 and SW08 contributed to ozone recovery.
format Article in Journal/Newspaper
genre Amundsen Sea
Antarc*
Antarctic
Ross Sea
Sea ice
genre_facet Amundsen Sea
Antarc*
Antarctic
Ross Sea
Sea ice
geographic Amundsen Sea
Antarctic
Ross Sea
The Antarctic
geographic_facet Amundsen Sea
Antarctic
Ross Sea
The Antarctic
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op_doi https://doi.org/10.1029/2025GL115257
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doi:10.1029/2025GL115257
https://doaj.org/article/f79471765ebd42b8bfedefecb69598a4
op_source Geophysical Research Letters, Vol 52, Iss 7, Pp n/a-n/a (2025)
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spelling ftdoajarticles:oai:doaj.org/article:f79471765ebd42b8bfedefecb69598a4 2025-05-11T14:09:13+00:00 The Sudden Stratospheric Warming Events in the Antarctic in 2024 Yucheng Zi Zhenxia Long Jinyu Sheng Gaopeng Lu Will Perrie Ziniu Xiao 2025-04-01T00:00:00Z https://doi.org/10.1029/2025GL115257 https://doaj.org/article/f79471765ebd42b8bfedefecb69598a4 EN eng Wiley https://doi.org/10.1029/2025GL115257 https://doaj.org/toc/0094-8276 https://doaj.org/toc/1944-8007 doi:10.1029/2025GL115257 https://doaj.org/article/f79471765ebd42b8bfedefecb69598a4 Geophysical Research Letters, Vol 52, Iss 7, Pp n/a-n/a (2025) sudden stratospheric warming (SSW) stratospheric polar vortex (SPV) Antarctic sea ice stratospheric preconditioning southern annular mode (SAM) Geophysics. Cosmic physics QC801-809 article 2025 ftdoajarticles https://doi.org/10.1029/2025GL115257 2025-04-14T15:04:02Z Abstract In July and August 2024, two consecutive stratospheric sudden warming (SSW) events (termed SW07 and SW08) occurred over Antarctic, both featuring a rapid 17°C temperature rise at 10 hPa and significant stratospheric polar vortex (SPV) deceleration. SW07 occurred at the earliest winter time of the year recorded in the satellite era (1979 to present). The study found that, strong blocking highs affected stratospheric warming via nonlinear planetary wave prior to SW07, and the substantial sea ice loss over Antarctic Ross Sea and Amundsen Sea likely created favorable conditions for the formation of these blocking highs. Furthermore, the stratospheric preconditioning significantly amplified the intensity of the planetary waves. A downward‐propagating negative Southern Annular Mode (SAM) signal after SW07 supported blocking highs, creating a favorable circulation for planetary wave perturbations prior to SW08. In addition, enhanced ozone transport from low latitudes to the pole during SW07 and SW08 contributed to ozone recovery. Article in Journal/Newspaper Amundsen Sea Antarc* Antarctic Ross Sea Sea ice Directory of Open Access Journals: DOAJ Articles Amundsen Sea Antarctic Ross Sea The Antarctic Geophysical Research Letters 52 7
spellingShingle sudden stratospheric warming (SSW)
stratospheric polar vortex (SPV)
Antarctic sea ice
stratospheric preconditioning
southern annular mode (SAM)
Geophysics. Cosmic physics
QC801-809
Yucheng Zi
Zhenxia Long
Jinyu Sheng
Gaopeng Lu
Will Perrie
Ziniu Xiao
The Sudden Stratospheric Warming Events in the Antarctic in 2024
title The Sudden Stratospheric Warming Events in the Antarctic in 2024
title_full The Sudden Stratospheric Warming Events in the Antarctic in 2024
title_fullStr The Sudden Stratospheric Warming Events in the Antarctic in 2024
title_full_unstemmed The Sudden Stratospheric Warming Events in the Antarctic in 2024
title_short The Sudden Stratospheric Warming Events in the Antarctic in 2024
title_sort sudden stratospheric warming events in the antarctic in 2024
topic sudden stratospheric warming (SSW)
stratospheric polar vortex (SPV)
Antarctic sea ice
stratospheric preconditioning
southern annular mode (SAM)
Geophysics. Cosmic physics
QC801-809
topic_facet sudden stratospheric warming (SSW)
stratospheric polar vortex (SPV)
Antarctic sea ice
stratospheric preconditioning
southern annular mode (SAM)
Geophysics. Cosmic physics
QC801-809
url https://doi.org/10.1029/2025GL115257
https://doaj.org/article/f79471765ebd42b8bfedefecb69598a4