Articles | Volume 18, issue 10
https://doi.org/10.5194/acp-18-7721-2018
https://doi.org/10.5194/acp-18-7721-2018
Research article
 | 
01 Jun 2018
Research article |  | 01 Jun 2018

Future changes in the stratosphere-to-troposphere ozone mass flux and the contribution from climate change and ozone recovery

Stefanie Meul, Ulrike Langematz, Philipp Kröger, Sophie Oberländer-Hayn, and Patrick Jöckel

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Latest update: 15 Jul 2024
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Short summary
Using a chemistry--climate model future changes in the stratosphere-to-troposphere ozone mass flux, their drivers, and the future distribution of stratospheric ozone in the troposphere are investigated. In an extreme greenhouse gas (GHG) scenario, the global influx of stratospheric ozone into the troposphere is projected to grow between 2000 and 2100 by 53%. The increase is due to the recovery of stratospheric ozone owing to declining halogens and GHG induced circulation and temperature changes.
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