Articles | Volume 22, issue 6
Atmos. Chem. Phys., 22, 4005–4018, 2022
https://doi.org/10.5194/acp-22-4005-2022
Atmos. Chem. Phys., 22, 4005–4018, 2022
https://doi.org/10.5194/acp-22-4005-2022
Research article
 | Highlight paper
31 Mar 2022
Research article  | Highlight paper | 31 Mar 2022

Full latitudinal marine atmospheric measurements of iodine monoxide

Hisahiro Takashima 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-2021-680', Anonymous Referee #1, 06 Sep 2021
  • RC2: 'Comment on acp-2021-680', Anonymous Referee #2, 11 Nov 2021

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Hisahiro Takashima on behalf of the Authors (22 Dec 2021)  Author's response    Author's tracked changes    Manuscript
ED: Referee Nomination & Report Request started (01 Jan 2022) by Steven Brown
RR by Anonymous Referee #1 (14 Jan 2022)
RR by Anonymous Referee #2 (14 Jan 2022)
ED: Publish subject to minor revisions (review by editor) (15 Jan 2022) by Steven Brown
AR by Hisahiro Takashima on behalf of the Authors (03 Feb 2022)  Author's response    Author's tracked changes    Manuscript
ED: Publish as is (06 Feb 2022) by Steven Brown
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Short summary
We have undertaken atmospheric iodine monoxide (IO) observations in the global marine boundary layer with a wide latitudinal coverage and sea surface temperature (SST) range. We conclude that atmospheric iodine is abundant over the Western Pacific warm pool, appearing as an iodine fountain, where ozone (O3) minima occur. Our study also found negative correlations between IO and O3 concentrations over IO maxima, which requires reconsideration of the initiation process of halogen activation.
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