Dynamic Impact of the Southern Annular Mode on the Antarctic Ozone Hole Area

This study investigates the impact of dynamic variability of the Southern Hemisphere (SH) polar middle atmosphere on the ozone hole area. We analyze the influence of the southern annular mode (SAM) and planetary waves (PWs) on ozone depletion from 19 years (2005–2023) of aura microwave limb sounder...

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Published in:Remote Sensing
Main Authors: Jae N. Lee, Dong L. Wu
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2025
Subjects:
Online Access:https://doi.org/10.3390/rs17050835
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author Jae N. Lee
Dong L. Wu
author_facet Jae N. Lee
Dong L. Wu
author_sort Jae N. Lee
collection MDPI Open Access Publishing
container_issue 5
container_start_page 835
container_title Remote Sensing
container_volume 17
description This study investigates the impact of dynamic variability of the Southern Hemisphere (SH) polar middle atmosphere on the ozone hole area. We analyze the influence of the southern annular mode (SAM) and planetary waves (PWs) on ozone depletion from 19 years (2005–2023) of aura microwave limb sounder (MLS) geopotential height (GPH) measurements. We employ empirical orthogonal function (EOF) analysis to decompose the GPH variability into distinct spatial patterns. EOF analysis reveals a strong relationship between the first EOF (representing the SAM) and the Antarctic ozone hole area (γ = 0.91). A significant negative lag correlation between the August principal component of the second EOF (PC2) and the September SAM index (γ = −0.76) suggests that lower stratospheric wave activity in August can precondition the polar vortex strength in September. The minor sudden stratospheric warming (SSW) event in 2019 is an example of how strong wave activity can disrupt the polar vortex, leading to significant temperature anomalies and reduced ozone depletion. The coupling of PWs is evident in the lag correlation analysis between different altitudes. A “bottom-up” propagation of PWs from the lower stratosphere to the mesosphere and a potential “top-down” influence from the mesosphere to the lower stratosphere are observed with time lags of 21–30 days. These findings highlight the complex dynamics of PW propagation and their potential impact on the SAM and ozone layer. Further analysis of these correlations could improve one-month lead predictions of the SAM and the ozone hole area.
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spelling ftmdpi:oai:mdpi.com:/2072-4292/17/5/835/ 2025-03-30T14:55:29+00:00 Dynamic Impact of the Southern Annular Mode on the Antarctic Ozone Hole Area Jae N. Lee Dong L. Wu agris 2025-02-27 application/pdf https://doi.org/10.3390/rs17050835 eng eng Multidisciplinary Digital Publishing Institute https://dx.doi.org/10.3390/rs17050835 https://creativecommons.org/licenses/by/4.0/ Remote Sensing Volume 17 Issue 5 Pages: 835 ozone hole area southern annular mode planetary wave SAM stratospheric southern warming Text 2025 ftmdpi https://doi.org/10.3390/rs17050835 2025-03-03T15:30:50Z This study investigates the impact of dynamic variability of the Southern Hemisphere (SH) polar middle atmosphere on the ozone hole area. We analyze the influence of the southern annular mode (SAM) and planetary waves (PWs) on ozone depletion from 19 years (2005–2023) of aura microwave limb sounder (MLS) geopotential height (GPH) measurements. We employ empirical orthogonal function (EOF) analysis to decompose the GPH variability into distinct spatial patterns. EOF analysis reveals a strong relationship between the first EOF (representing the SAM) and the Antarctic ozone hole area (γ = 0.91). A significant negative lag correlation between the August principal component of the second EOF (PC2) and the September SAM index (γ = −0.76) suggests that lower stratospheric wave activity in August can precondition the polar vortex strength in September. The minor sudden stratospheric warming (SSW) event in 2019 is an example of how strong wave activity can disrupt the polar vortex, leading to significant temperature anomalies and reduced ozone depletion. The coupling of PWs is evident in the lag correlation analysis between different altitudes. A “bottom-up” propagation of PWs from the lower stratosphere to the mesosphere and a potential “top-down” influence from the mesosphere to the lower stratosphere are observed with time lags of 21–30 days. These findings highlight the complex dynamics of PW propagation and their potential impact on the SAM and ozone layer. Further analysis of these correlations could improve one-month lead predictions of the SAM and the ozone hole area. Text Antarc* Antarctic MDPI Open Access Publishing Antarctic The Antarctic Remote Sensing 17 5 835
spellingShingle ozone hole area
southern annular mode
planetary wave
SAM
stratospheric southern warming
Jae N. Lee
Dong L. Wu
Dynamic Impact of the Southern Annular Mode on the Antarctic Ozone Hole Area
title Dynamic Impact of the Southern Annular Mode on the Antarctic Ozone Hole Area
title_full Dynamic Impact of the Southern Annular Mode on the Antarctic Ozone Hole Area
title_fullStr Dynamic Impact of the Southern Annular Mode on the Antarctic Ozone Hole Area
title_full_unstemmed Dynamic Impact of the Southern Annular Mode on the Antarctic Ozone Hole Area
title_short Dynamic Impact of the Southern Annular Mode on the Antarctic Ozone Hole Area
title_sort dynamic impact of the southern annular mode on the antarctic ozone hole area
topic ozone hole area
southern annular mode
planetary wave
SAM
stratospheric southern warming
topic_facet ozone hole area
southern annular mode
planetary wave
SAM
stratospheric southern warming
url https://doi.org/10.3390/rs17050835