Articles | Volume 20, issue 14
Atmos. Chem. Phys., 20, 8627–8639, 2020
https://doi.org/10.5194/acp-20-8627-2020
Atmos. Chem. Phys., 20, 8627–8639, 2020
https://doi.org/10.5194/acp-20-8627-2020

Research article 22 Jul 2020

Research article | 22 Jul 2020

Analysis and attribution of total column ozone changes over the Tibetan Plateau during 1979–2017

Yajuan Li et al.

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AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Yajuan Li on behalf of the Authors (18 Apr 2020)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (05 May 2020) by Marc von Hobe
RR by Anonymous Referee #3 (20 May 2020)
RR by Anonymous Referee #1 (03 Jun 2020)
ED: Publish subject to minor revisions (review by editor) (05 Jun 2020) by Marc von Hobe
AR by Yajuan Li on behalf of the Authors (06 Jun 2020)  Author's response    Manuscript
ED: Publish as is (16 Jun 2020) by Marc von Hobe
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Short summary
The Tibetan Plateau (TP) exerts important thermal and dynamical effects on atmospheric circulation, climate change as well as the ozone distribution. In this study, we use updated observations and model simulations to investigate the ozone trends and variations over the TP. Wintertime TP ozone variations are largely controlled by tropical to high-latitude transport processes, whereas summertime concentrations are a combined effect of photochemical decay and tropical processes.
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