Articles | Volume 23, issue 17
https://doi.org/10.5194/acp-23-9873-2023
https://doi.org/10.5194/acp-23-9873-2023
Research article
 | 
06 Sep 2023
Research article |  | 06 Sep 2023

Radiation fog properties in two consecutive events under polluted and clean conditions in the Yangtze River Delta, China: a simulation study

Naifu Shao, Chunsong Lu, Xingcan Jia, Yuan Wang, Yubin Li, Yan Yin, Bin Zhu, Tianliang Zhao, Duanyang Liu, Shengjie Niu, Shuxian Fan, Shuqi Yan, and Jingjing Lv

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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-2022-833', Anonymous Referee #1, 16 Feb 2023
  • RC2: 'Comment on acp-2022-833', Anonymous Referee #2, 27 Feb 2023
    • AC2: 'Reply on RC2', Naifu Shao, 28 Apr 2023
    • AC5: 'Reply on RC2', Naifu Shao, 16 May 2023
  • EC1: 'Comment on acp-2022-833', Graham Feingold, 28 Apr 2023
    • AC3: 'Reply on EC1', Naifu Shao, 16 May 2023

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
AR by Naifu Shao on behalf of the Authors (28 Apr 2023)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (11 May 2023) by Graham Feingold
RR by Anonymous Referee #2 (20 May 2023)
RR by Anonymous Referee #1 (15 Jun 2023)
ED: Reconsider after major revisions (02 Jul 2023) by Graham Feingold
AR by Naifu Shao on behalf of the Authors (16 Jul 2023)  Author's response   Author's tracked changes   Manuscript 
ED: Publish subject to technical corrections (22 Jul 2023) by Graham Feingold
AR by Naifu Shao on behalf of the Authors (25 Jul 2023)  Manuscript 
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Short summary
Fog is an important meteorological phenomenon that affects visibility. Aerosols and the planetary boundary layer (PBL) play critical roles in the fog life cycle. In this study, aerosol-induced changes in fog properties become more remarkable in the second fog (Fog2) than in the first fog (Fog1). The reason is that aerosol–cloud interaction (ACI) delays Fog1 dissipation, leading to the PBL meteorological conditions being more conducive to Fog2 formation and to stronger ACI in Fog2.
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