Articles | Volume 25, issue 22
https://doi.org/10.5194/acp-25-17125-2025
https://doi.org/10.5194/acp-25-17125-2025
Research article
 | 
28 Nov 2025
Research article |  | 28 Nov 2025

Atmospheric new particle formation in the eastern region of China: an investigation on mechanism and influencing factors at multiple sites

Jiaqi Jin, Runlong Cai, Yiliang Liu, Gan Yang, Yueyang Li, Chuang Li, Lei Yao, Jingkun Jiang, Xiuhui Zhang, and Lin Wang

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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 egusphere-2025-2787', Anonymous Referee #1, 12 Aug 2025
    • AC1: 'Reply on RC1', Lin Wang, 09 Oct 2025
  • RC2: 'Comment on egusphere-2025-2787', Anonymous Referee #2, 29 Aug 2025
    • AC2: 'Reply on RC2', Lin Wang, 09 Oct 2025

Peer review completion

AR – Author's response | RR – Referee report | ED – Editor decision | EF – Editorial file upload
AR by Lin Wang on behalf of the Authors (09 Oct 2025)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (09 Oct 2025) by Ari Laaksonen
RR by Anonymous Referee #2 (13 Oct 2025)
RR by Anonymous Referee #1 (31 Oct 2025)
ED: Publish subject to minor revisions (review by editor) (31 Oct 2025) by Ari Laaksonen
AR by Lin Wang on behalf of the Authors (04 Nov 2025)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (05 Nov 2025) by Ari Laaksonen
AR by Lin Wang on behalf of the Authors (07 Nov 2025)  Manuscript 
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Short summary
Based on observed atmospheric new particle formation events at multiple sites in eastern China, we find that sulfuric acid and dimethylamine can explain the observed atmospheric nucleation and the differences in the nucleation intensity among campaigns can be largely attributed to temperature and precursor concentrations. Our results also show that oxygenated organic molecules can make a great contribution to the initial growth of freshly nucleated particles in the real atmosphere.
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