Articles | Volume 22, issue 7
https://doi.org/10.5194/acp-22-4951-2022
© Author(s) 2022. This work is distributed under the Creative Commons Attribution 4.0 License.
Formation, radiative forcing, and climatic effects of severe regional haze
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- Final revised paper (published on 14 Apr 2022)
- Supplement to the final revised paper
- Preprint (discussion started on 29 Oct 2021)
- 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 acp-2021-799', Anonymous Referee #1, 22 Nov 2021
- AC1: 'Reply on RC1', Renyi Zhang, 16 Feb 2022
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RC2: 'Comment on acp-2021-799', Anonymous Referee #3, 28 Jan 2022
- AC2: 'Reply on RC2', Renyi Zhang, 16 Feb 2022
Peer review completion
AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
AR by Renyi Zhang on behalf of the Authors (16 Feb 2022)
Author's response
Author's tracked changes
Manuscript
ED: Referee Nomination & Report Request started (17 Feb 2022) by Zhanqing Li
RR by Anonymous Referee #1 (28 Feb 2022)
RR by Anonymous Referee #3 (07 Mar 2022)
ED: Publish subject to technical corrections (17 Mar 2022) by Zhanqing Li
AR by Renyi Zhang on behalf of the Authors (21 Mar 2022)
Author's response
Manuscript
General comments:
Using in situ measurements, satellite observations and the WRF modelï¼the authors investigated the contributions of chemical and physical processes to the evolution of haze extremes. Findings show that chemical process that plays a leading role in PM production varies with the development stage of the haze event. And the haze-PBL interactions accelerate the accumulation of aerosol particles and water vapor at the ground level, amplifying the haze severity. The findings help to demonstrate the potential for achieving co-benefits for air quality and climate via black carbon mitigation. I recommend it to be accepted after minor revision.
Technical comments: