Articles | Volume 24, issue 6
https://doi.org/10.5194/acp-24-3613-2024
https://doi.org/10.5194/acp-24-3613-2024
Research article
 | 
22 Mar 2024
Research article |  | 22 Mar 2024

Quantifying the tropospheric ozone radiative effect and its temporal evolution in the satellite era

Richard J. Pope, Alexandru Rap, Matilda A. Pimlott, Brice Barret, Eric Le Flochmoen, Brian J. Kerridge, Richard Siddans, Barry G. Latter, Lucy J. Ventress, Anne Boynard, Christian Retscher, Wuhu Feng, Richard Rigby, Sandip S. Dhomse, Catherine Wespes, and Martyn P. Chipperfield

Viewed

Total article views: 2,696 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
2,044 582 70 2,696 151 84 91
  • HTML: 2,044
  • PDF: 582
  • XML: 70
  • Total: 2,696
  • Supplement: 151
  • BibTeX: 84
  • EndNote: 91
Views and downloads (calculated since 08 Sep 2023)
Cumulative views and downloads (calculated since 08 Sep 2023)

Viewed (geographical distribution)

Total article views: 2,696 (including HTML, PDF, and XML) Thereof 2,632 with geography defined and 64 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 06 Dec 2025
Download
Short summary
Tropospheric ozone is an important short-lived climate forcer which influences the incoming solar short-wave radiation and the outgoing long-wave radiation in the atmosphere (8–15 km) where the balance between the two yields a net positive (i.e. warming) effect at the surface. Overall, we find that the tropospheric ozone radiative effect ranges between 1.21 and 1.26 W m−2 with a negligible trend (2008–2017), suggesting that tropospheric ozone influences on climate have remained stable with time.
Share
Altmetrics
Final-revised paper
Preprint