Articles | Volume 22, issue 9
Atmos. Chem. Phys., 22, 6275–6289, 2022
https://doi.org/10.5194/acp-22-6275-2022
Atmos. Chem. Phys., 22, 6275–6289, 2022
https://doi.org/10.5194/acp-22-6275-2022
Research article
16 May 2022
Research article | 16 May 2022

A process-oriented evaluation of CAMS reanalysis ozone during tropopause folds over Europe for the period 2003–2018

Dimitris Akritidis et al.

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Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on acp-2021-998', Anonymous Referee #1, 11 Jan 2022
  • RC2: 'Comment on acp-2021-998', Anonymous Referee #2, 17 Jan 2022

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Dimitris Akritidis on behalf of the Authors (18 Mar 2022)  Author's response    Author's tracked changes    Manuscript
ED: Referee Nomination & Report Request started (23 Mar 2022) by Andreas Petzold
RR by Anonymous Referee #2 (29 Mar 2022)
RR by Anonymous Referee #1 (01 Apr 2022)
ED: Publish subject to minor revisions (review by editor) (05 Apr 2022) by Andreas Petzold
AR by Dimitris Akritidis on behalf of the Authors (10 Apr 2022)  Author's response    Author's tracked changes    Manuscript
ED: Publish subject to technical corrections (20 Apr 2022) by Andreas Petzold
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Short summary
We perform a process-oriented evaluation of Copernicus Atmosphere Monitoring Service (CAMS) reanalysis (CAMSRA) O3 over Europe using WOUDC (World Ozone and Ultraviolet Radiation Data Centre) ozonesondes and IAGOS (In-service Aircraft for a Global Observing System) aircraft measurements. Chemical data assimilation assists CAMSRA to reproduce the observed O3 increases in the troposphere during the examined folding events, but it mostly results in O3 overestimation in the upper troposphere.
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