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


Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on egusphere-2022-701', Anonymous Referee #1, 23 Sep 2022
    • AC1: 'Reply on RC1', Arseniy Karagodin-Doyennel, 18 Oct 2022
  • RC2: 'Comment on egusphere-2022-701', Anonymous Referee #2, 27 Sep 2022
    • AC2: 'Reply on RC2', Arseniy Karagodin-Doyennel, 18 Oct 2022

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
AR by Arseniy Karagodin-Doyennel on behalf of the Authors (18 Oct 2022)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (21 Oct 2022) by Jayanarayanan Kuttippurath
RR by Anonymous Referee #2 (07 Nov 2022)
ED: Publish as is (13 Nov 2022) by Jayanarayanan Kuttippurath
AR by Arseniy Karagodin-Doyennel on behalf of the Authors (13 Nov 2022)  Manuscript 

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