Articles | Volume 22, issue 22
https://doi.org/10.5194/acp-22-14837-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/acp-22-14837-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Formation and impacts of nitryl chloride in Pearl River Delta
Haichao Wang
School of Atmospheric Sciences, Sun Yat-sen University, Zhuhai, 519082, China
Guangdong Provincial Observation and Research Station for Climate Environment and Air Quality Change in the Pearl River Estuary, Key Laboratory of Tropical Atmosphere-Ocean System, Ministry of Education, Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai), Zhuhai, 519082, China
Institute for Environmental and Climate Research, Jinan University, Guangzhou, 511443, China
Guangdong–Hong Kong–Macau Joint Laboratory of Collaborative Innovation for Environmental Quality, Guangzhou, 511443, China
E Zheng
Institute for Environmental and Climate Research, Jinan University, Guangzhou, 511443, China
Guangdong–Hong Kong–Macau Joint Laboratory of Collaborative Innovation for Environmental Quality, Guangzhou, 511443, China
Xiaoxiao Zhang
Institute for Environmental and Climate Research, Jinan University, Guangzhou, 511443, China
Guangdong–Hong Kong–Macau Joint Laboratory of Collaborative Innovation for Environmental Quality, Guangzhou, 511443, China
Jie Wang
School of Atmospheric Sciences, Sun Yat-sen University, Zhuhai, 519082, China
Keding Lu
State Key Joint Laboratory of Environmental Simulation and Pollution Control, College of Environmental Sciences and Engineering, Peking University, Beijing, 100871, China
The State Environmental Protection Key Laboratory of Atmospheric Ozone Pollution Control, College of Environmental Sciences and Engineering, Peking University, Beijing, 100871, China
Chenshuo Ye
Institute for Environmental and Climate Research, Jinan University, Guangzhou, 511443, China
Guangdong–Hong Kong–Macau Joint Laboratory of Collaborative Innovation for Environmental Quality, Guangzhou, 511443, China
Lei Yang
Institute for Environmental and Climate Research, Jinan University, Guangzhou, 511443, China
Guangdong–Hong Kong–Macau Joint Laboratory of Collaborative Innovation for Environmental Quality, Guangzhou, 511443, China
Shan Huang
Institute for Environmental and Climate Research, Jinan University, Guangzhou, 511443, China
Guangdong–Hong Kong–Macau Joint Laboratory of Collaborative Innovation for Environmental Quality, Guangzhou, 511443, China
Weiwei Hu
State Key Laboratory of Organic Geochemistry and Guangdong Key Laboratory of Environmental Protection and Resources Utilization, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China
Suxia Yang
Institute for Environmental and Climate Research, Jinan University, Guangzhou, 511443, China
Guangdong–Hong Kong–Macau Joint Laboratory of Collaborative Innovation for Environmental Quality, Guangzhou, 511443, China
Yuwen Peng
Institute for Environmental and Climate Research, Jinan University, Guangzhou, 511443, China
Guangdong–Hong Kong–Macau Joint Laboratory of Collaborative Innovation for Environmental Quality, Guangzhou, 511443, China
Jipeng Qi
Institute for Environmental and Climate Research, Jinan University, Guangzhou, 511443, China
Guangdong–Hong Kong–Macau Joint Laboratory of Collaborative Innovation for Environmental Quality, Guangzhou, 511443, China
Sihang Wang
Institute for Environmental and Climate Research, Jinan University, Guangzhou, 511443, China
Guangdong–Hong Kong–Macau Joint Laboratory of Collaborative Innovation for Environmental Quality, Guangzhou, 511443, China
Xianjun He
Institute for Environmental and Climate Research, Jinan University, Guangzhou, 511443, China
Guangdong–Hong Kong–Macau Joint Laboratory of Collaborative Innovation for Environmental Quality, Guangzhou, 511443, China
Yubin Chen
Institute for Environmental and Climate Research, Jinan University, Guangzhou, 511443, China
Guangdong–Hong Kong–Macau Joint Laboratory of Collaborative Innovation for Environmental Quality, Guangzhou, 511443, China
Tiange Li
Institute for Environmental and Climate Research, Jinan University, Guangzhou, 511443, China
Guangdong–Hong Kong–Macau Joint Laboratory of Collaborative Innovation for Environmental Quality, Guangzhou, 511443, China
Wenjie Wang
Institute for Environmental and Climate Research, Jinan University, Guangzhou, 511443, China
Multiphase Chemistry Department, Max Planck Institute for Chemistry, Mainz 55128, Germany
Yibo Huangfu
Institute for Environmental and Climate Research, Jinan University, Guangzhou, 511443, China
Guangdong–Hong Kong–Macau Joint Laboratory of Collaborative Innovation for Environmental Quality, Guangzhou, 511443, China
Xiaobing Li
Institute for Environmental and Climate Research, Jinan University, Guangzhou, 511443, China
Guangdong–Hong Kong–Macau Joint Laboratory of Collaborative Innovation for Environmental Quality, Guangzhou, 511443, China
Mingfu Cai
Institute for Environmental and Climate Research, Jinan University, Guangzhou, 511443, China
Guangdong–Hong Kong–Macau Joint Laboratory of Collaborative Innovation for Environmental Quality, Guangzhou, 511443, China
Xuemei Wang
Institute for Environmental and Climate Research, Jinan University, Guangzhou, 511443, China
Guangdong–Hong Kong–Macau Joint Laboratory of Collaborative Innovation for Environmental Quality, Guangzhou, 511443, China
Min Shao
Institute for Environmental and Climate Research, Jinan University, Guangzhou, 511443, China
Guangdong–Hong Kong–Macau Joint Laboratory of Collaborative Innovation for Environmental Quality, Guangzhou, 511443, China
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- Final revised paper (published on 22 Nov 2022)
- Preprint (discussion started on 08 Aug 2022)
Interactive discussion
Status: closed
Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor
| : Report abuse
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RC1: 'Comment on acp-2022-408', Anonymous Referee #2, 17 Aug 2022
The comment was uploaded in the form of a supplement: https://acp.copernicus.org/preprints/acp-2022-408/acp-2022-408-RC1-supplement.pdf
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AC1: 'Reply on RC1', Haichao Wang, 12 Oct 2022
The comment was uploaded in the form of a supplement: https://acp.copernicus.org/preprints/acp-2022-408/acp-2022-408-AC1-supplement.pdf
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AC1: 'Reply on RC1', Haichao Wang, 12 Oct 2022
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RC2: 'Comment on acp-2022-408', Anonymous Referee #1, 30 Aug 2022
This work conducted continuous field measurements of ClNO2 and N2O5 and performed comprehensive evaluation on the ClNO2 chemistry as well as its contributions to radical and ozone formation under different transport pathways. The results highlight the N2O5-uptake-limited ClNO2 formation and overall low contributions to RO2 radical and O3 formation in autumn in South China. The manuscript is generally well written with clear logic, deep analysis, and full discussion e. It can be considered to accept after addressing the following minor comments.
Specific comments:
- Line 76-77, 78-79, etc., blanks are missed in the middle of different citations. The same suggestion is given to other parts of the main text.
- Line 87-88, the sentence requires modification. e.g., “the challenge to accurately predict ClNO2 and particulate nitration production”.
- Line 148, “seldom disturbs the sampling” can be written as “to have little influence on the sampling”.
- Line 151, it’s better to add “sometimes” after the word “are”.
- Line 157, add “approximately” after the word “was”.
- Line 203, with and without the constrains of the observed ClNO2, or with and without taking ClNO2 as the source of Cl radicals?
- Line 204-205, this operation will lead to overestimation on the contributions from ClNO2 chemistry. The potential uncertainty should be described here or somewhere else.
- Line 209, the average lifetime or a constant lifetime?
- Line 210, the “was” should be “were”.
- Line 209-212, this sentence is not very clear. Is there any reference to support such lifetime setting?
- Line 249-250, what are the reasons for the lower abundances in 2019 than 2017? Smaller source strengths or larger sinks?
- Line 258, 500 m AMSL or AGL? Are the trajectories at 100 m similar to those at 500 m?
- Figure 5, a RMA correlation coefficient may be better for comparing the consistent.
- Line 401, add “in this study” before “than”.
- Figure 6 and Figure 7, suggest indicating the p values of the linear correlations.
- Line 468, 470, 473, “power plants emissions” should be coal-fired power plant emissions.
- Line 618, what does the “AH” mean? Double check the unit mmol/mmol.
Citation: https://doi.org/10.5194/acp-2022-408-RC2 -
AC2: 'Reply on RC2', Haichao Wang, 12 Oct 2022
The comment was uploaded in the form of a supplement: https://acp.copernicus.org/preprints/acp-2022-408/acp-2022-408-AC2-supplement.pdf
Peer review completion
AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
AR by Haichao Wang on behalf of the Authors (12 Oct 2022)
Author's response
Author's tracked changes
Manuscript
ED: Publish as is (21 Oct 2022) by Timothy Bertram
AR by Haichao Wang on behalf of the Authors (24 Oct 2022)
Short summary
We present intensive field measurement of ClNO2 in the Pearl River Delta in 2019. Large variation in the level, formation, and atmospheric impacts of ClNO2 was found in different air masses. ClNO2 formation was limited by the particulate chloride (Cl−) and aerosol surface area. Our results reveal that Cl− originated from various anthropogenic emissions rather than sea sources and show minor contribution to the O3 pollution and photochemistry.
We present intensive field measurement of ClNO2 in the Pearl River Delta in 2019. Large...
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