Articles | Volume 21, issue 6
https://doi.org/10.5194/acp-21-4809-2021
https://doi.org/10.5194/acp-21-4809-2021
Research article
 | 
29 Mar 2021
Research article |  | 29 Mar 2021

A three-dimensional-model inversion of methyl chloroform to constrain the atmospheric oxidative capacity

Stijn Naus, Stephen A. Montzka, Prabir K. Patra, and Maarten C. Krol

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AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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AR: Author's response | RR: Referee report | ED: Editor decision
AR by Stijn Naus on behalf of the Authors (23 Oct 2020)  Author's response   Manuscript 
ED: Reconsider after major revisions (30 Oct 2020) by Mathias Palm
AR by Stijn Naus on behalf of the Authors (10 Dec 2020)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (17 Dec 2020) by Mathias Palm
RR by Anonymous Referee #1 (08 Jan 2021)
RR by Anonymous Referee #2 (18 Jan 2021)
ED: Publish subject to minor revisions (review by editor) (05 Feb 2021) by Mathias Palm
AR by Stijn Naus on behalf of the Authors (18 Feb 2021)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (18 Feb 2021) by Mathias Palm
AR by Stijn Naus on behalf of the Authors (18 Feb 2021)
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Short summary
Following up on previous box model studies, we employ a 3D transport model to estimate variations in the hydroxyl radical (OH) from observations of methyl chloroform (MCF). We derive small interannual OH variations that are consistent with variations in the El Niño–Southern Oscillation. We also find evidence for the release of MCF from oceans in atmospheric gradients of MCF. Both findings highlight the added value of a 3D transport model since box model studies did not identify these effects.
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