Articles | Volume 22, issue 18
https://doi.org/10.5194/acp-22-12525-2022
https://doi.org/10.5194/acp-22-12525-2022
Research article
 | 
26 Sep 2022
Research article |  | 26 Sep 2022

Radical chemistry in the Pearl River Delta: observations and modeling of OH and HO2 radicals in Shenzhen in 2018

Xinping Yang, Keding Lu, Xuefei Ma, Yue Gao, Zhaofeng Tan, Haichao Wang, Xiaorui Chen, Xin Li, Xiaofeng Huang, Lingyan He, Mengxue Tang, Bo Zhu, Shiyi Chen, Huabin Dong, Limin Zeng, and Yuanhang Zhang

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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-2022-113', Anonymous Referee #1, 14 Mar 2022
    • AC1: 'Reply on RC1', Keding Lu, 26 May 2022
  • RC2: 'Comment on acp-2022-113', Anonymous Referee #2, 02 Apr 2022
    • AC2: 'Reply on RC2', Keding Lu, 26 May 2022
  • RC3: 'Comment on acp-2022-113', Anonymous Referee #3, 02 Apr 2022
    • AC3: 'Reply on RC3', Keding Lu, 26 May 2022

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
AR by Keding Lu on behalf of the Authors (26 May 2022)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (01 Jun 2022) by Lisa Whalley
RR by Anonymous Referee #1 (09 Jun 2022)
RR by Anonymous Referee #3 (14 Jun 2022)
RR by Anonymous Referee #2 (19 Jun 2022)
ED: Reconsider after major revisions (21 Jun 2022) by Lisa Whalley
AR by Keding Lu on behalf of the Authors (01 Aug 2022)  Author's response   Author's tracked changes   Manuscript 
ED: Publish subject to minor revisions (review by editor) (07 Aug 2022) by Lisa Whalley
AR by Keding Lu on behalf of the Authors (11 Aug 2022)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (15 Aug 2022) by Lisa Whalley
AR by Keding Lu on behalf of the Authors (23 Aug 2022)  Manuscript 
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Short summary
We present the OH and HO2 radical observations at the Shenzhen site (Pearl River Delta, China) in the autumn of 2018. The diurnal maxima were 4.5 × 106 cm−3 for OH and 4.2 × 108 cm−3 for HO2 (including an estimated interference of 23 %–28 % from RO2 radicals during the daytime). The OH underestimation was identified again, and it was attributable to the missing OH sources. HO2 heterogeneous uptake, ROx sources and sinks, and the atmospheric oxidation capacity were evaluated as well.
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