Articles | Volume 22, issue 23
Research article
05 Dec 2022
Research article |  | 05 Dec 2022

The historical ozone trends simulated with the SOCOLv4 and their comparison with observations and reanalyses

Arseniy Karagodin-Doyennel, Eugene Rozanov, Timofei Sukhodolov, Tatiana Egorova, Jan Sedlacek, William Ball, and Thomas Peter


Total article views: 1,414 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
1,097 287 30 1,414 17 14
  • HTML: 1,097
  • PDF: 287
  • XML: 30
  • Total: 1,414
  • BibTeX: 17
  • EndNote: 14
Views and downloads (calculated since 12 Aug 2022)
Cumulative views and downloads (calculated since 12 Aug 2022)

Viewed (geographical distribution)

Total article views: 1,414 (including HTML, PDF, and XML) Thereof 1,405 with geography defined and 9 with unknown origin.
Country # Views %
  • 1


Latest update: 02 Dec 2023

The requested paper has a corresponding corrigendum published. Please read the corrigendum first before downloading the article.

Short summary
Applying the dynamic linear model, we confirm near-global ozone recovery (55°N–55°S) in the mesosphere, upper and middle stratosphere, and a steady increase in the troposphere. We also show that modern chemistry–climate models (CCMs) like SOCOLv4 may reproduce the observed trend distribution of lower stratospheric ozone, despite exhibiting a lower magnitude and statistical significance. The obtained ozone trend pattern in SOCOLv4 is generally consistent with observations and reanalysis datasets.
Final-revised paper