Articles | Volume 26, issue 6
https://doi.org/10.5194/acp-26-3995-2026
© Author(s) 2026. This work is distributed under the Creative Commons Attribution 4.0 License.
Life–cycle impacts of South Korean air pollution on tropospheric ozone and methane: sensitivity to dispersion time
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- Final revised paper (published on 23 Mar 2026)
- Supplement to the final revised paper
- Preprint (discussion started on 05 Dec 2025)
- Supplement to the preprint
Interactive discussion
Status: closed
Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor
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RC1: 'Comment on egusphere-2025-6012', Anonymous Referee #1, 23 Jan 2026
- AC1: 'Reply on RC1', Calum Wilson, 17 Feb 2026
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RC2: 'Comment on egusphere-2025-6012', Anonymous Referee #2, 26 Jan 2026
- AC2: 'Reply on RC2', Calum Wilson, 17 Feb 2026
Peer review completion
AR – Author's response | RR – Referee report | ED – Editor decision | EF – Editorial file upload
AR by Calum Wilson on behalf of the Authors (17 Feb 2026)
Author's response
Author's tracked changes
Manuscript
ED: Publish as is (26 Feb 2026) by Yves Balkanski
AR by Calum Wilson on behalf of the Authors (04 Mar 2026)
Manuscript
The manuscript by Wilson and Prather describes a quasi-three-dimensional modeling approach and employs the model to quantify the global net O3 production and CH4 loss from South Korean air pollution over 45 days in May-June 2016 during the KORUS-AQ campaign. The model consists of three stages: (1) a boundary layer-residual layer (BL-RL) stage, (2) an isolated pollution plume integration (PL) stage, and (3) a dispersed pollution (DP) stage. Taking a test case with South Korean air pollutant emissions compared to a control case with no anthropogenic and biomass burning emissions, the relative global CH4 loss and O3 production due to South Korean air pollution is diagnosed over the three model stages. Global modeling studies have typically diagnosed O3 production and loss from reaction rates for the odd-oxygen family. Here, the model developed by the authors explicitly resolves O3 perturbation lifetimes to more accurately calculate the O3 production term. This study offers a useful demonstration of this alternative approach to deriving O3 budget diagnostics. Further, the sensitivity of O3 and CH4 reactivity to plume aging times is assessed, providing valuable insight on the potential degree of overestimation of the anthropogenic contribution to global O3 and CH4 budgets resulting from rapid dispersion of air pollution in course resolution models.
I find that the manuscript is well written overall, provides a thorough detailing of the model, and fits well within the scope of ACP. I recommend publication of the manuscript after the authors address the following comments.
Comments:
Technical corrections: