Hemispheric asymmetry in recent stratospheric age of air changes

<p>Many stratospheric trace gases, including <span class="inline-formula">O<sub>3</sub></span>, <span class="inline-formula">HCl</span>, and <span class="inline-formula">NO<sub>y</sub></span>, have had op...

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Main Authors: K. Dubé, S. Tegtmeier, F. Ploeger, K. A. Walker
Format: Article
Language:English
Published: Copernicus Publications 2025-01-01
Series:Atmospheric Chemistry and Physics
Online Access:https://acp.copernicus.org/articles/25/1433/2025/acp-25-1433-2025.pdf
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author K. Dubé
S. Tegtmeier
F. Ploeger
K. A. Walker
author_facet K. Dubé
S. Tegtmeier
F. Ploeger
K. A. Walker
author_sort K. Dubé
collection DOAJ
description <p>Many stratospheric trace gases, including <span class="inline-formula">O<sub>3</sub></span>, <span class="inline-formula">HCl</span>, and <span class="inline-formula">NO<sub>y</sub></span>, have had opposing trends in the Southern Hemisphere (SH) compared to the Northern Hemisphere (NH) during the last 2 decades. Some of this difference is due to hemispherically asymmetric changes in the rate of transport by the Brewer–Dobson circulation (BDC), and some is due to ozone depletion and recovery. The mean age of air (AoA) is a common proxy for the transport rate by the BDC in models; however it cannot be directly measured. We use observations from the Atmospheric Chemistry Experiment Fourier transform spectrometer (ACE-FTS) along with results from the Chemical Lagrangian Model of the Stratosphere (CLaMS) to derive AoA anomalies and AoA trends. The AoA is derived using observations of <span class="inline-formula">N<sub>2</sub>O</span>, <span class="inline-formula">CH<sub>4</sub></span>, and CFC-12, all long-lived trace gases with tropospheric sources. We also consider CLaMS simulations driven with four different reanalyses (ERA5, ERA-Interim, JRA-55, MERRA-2). We find that, irrespective of which trace gas or reanalysis is used, air in the NH aged by up to 0.3 years per decade relative to the SH over 2004–2017. The maximum hemispheric difference in aging occurs in the middle stratosphere, near 30 hPa (<span class="inline-formula">∼</span> 24 km). We also show that the aging rate in the NH becomes smaller when the analysis is extended to 2021. The observed aging in the NH middle stratosphere contradicts model predictions of a decrease in stratospheric AoA in response to rising atmospheric greenhouse gas levels. However, the smaller aging rate during 2004–2021 compared to 2004–2017 provides some evidence that the NH aging is impacted by decadal variability and the limited length of the observation period.</p>
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spelling doaj-art-9d3d1c6511f04b079d0d937786d2026e2025-01-31T14:02:10ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242025-01-01251433144710.5194/acp-25-1433-2025Hemispheric asymmetry in recent stratospheric age of air changesK. Dubé0S. Tegtmeier1F. Ploeger2K. A. Walker3Institute of Space and Atmospheric Studies, University of Saskatchewan, Saskatoon, SK, CanadaInstitute of Space and Atmospheric Studies, University of Saskatchewan, Saskatoon, SK, CanadaInstitute for Energy and Climate Research: Stratosphere (IEK-7), Forschungszentrum Jülich, Jülich, GermanyDepartment of Physics, University of Toronto, Toronto, ON, Canada<p>Many stratospheric trace gases, including <span class="inline-formula">O<sub>3</sub></span>, <span class="inline-formula">HCl</span>, and <span class="inline-formula">NO<sub>y</sub></span>, have had opposing trends in the Southern Hemisphere (SH) compared to the Northern Hemisphere (NH) during the last 2 decades. Some of this difference is due to hemispherically asymmetric changes in the rate of transport by the Brewer–Dobson circulation (BDC), and some is due to ozone depletion and recovery. The mean age of air (AoA) is a common proxy for the transport rate by the BDC in models; however it cannot be directly measured. We use observations from the Atmospheric Chemistry Experiment Fourier transform spectrometer (ACE-FTS) along with results from the Chemical Lagrangian Model of the Stratosphere (CLaMS) to derive AoA anomalies and AoA trends. The AoA is derived using observations of <span class="inline-formula">N<sub>2</sub>O</span>, <span class="inline-formula">CH<sub>4</sub></span>, and CFC-12, all long-lived trace gases with tropospheric sources. We also consider CLaMS simulations driven with four different reanalyses (ERA5, ERA-Interim, JRA-55, MERRA-2). We find that, irrespective of which trace gas or reanalysis is used, air in the NH aged by up to 0.3 years per decade relative to the SH over 2004–2017. The maximum hemispheric difference in aging occurs in the middle stratosphere, near 30 hPa (<span class="inline-formula">∼</span> 24 km). We also show that the aging rate in the NH becomes smaller when the analysis is extended to 2021. The observed aging in the NH middle stratosphere contradicts model predictions of a decrease in stratospheric AoA in response to rising atmospheric greenhouse gas levels. However, the smaller aging rate during 2004–2021 compared to 2004–2017 provides some evidence that the NH aging is impacted by decadal variability and the limited length of the observation period.</p>https://acp.copernicus.org/articles/25/1433/2025/acp-25-1433-2025.pdf
spellingShingle K. Dubé
S. Tegtmeier
F. Ploeger
K. A. Walker
Hemispheric asymmetry in recent stratospheric age of air changes
Atmospheric Chemistry and Physics
title Hemispheric asymmetry in recent stratospheric age of air changes
title_full Hemispheric asymmetry in recent stratospheric age of air changes
title_fullStr Hemispheric asymmetry in recent stratospheric age of air changes
title_full_unstemmed Hemispheric asymmetry in recent stratospheric age of air changes
title_short Hemispheric asymmetry in recent stratospheric age of air changes
title_sort hemispheric asymmetry in recent stratospheric age of air changes
url https://acp.copernicus.org/articles/25/1433/2025/acp-25-1433-2025.pdf
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