the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Measurement report: Characterizing O3-NOₓ-VOC sensitivity and O3 formation in a heavily polluted central China megacity using multi-methods during 2019–2021 warm seasons
Abstract. This study investigated the high ozone pollution in Zhengzhou City from 2019 to 2021 using observational data and model simulations, focusing on volatile organic compound (VOC) pollution and its impact on ozone formation. Using online VOC data and statistical analyses, the results showed that VOC concentration increased with ozone pollution level, with average values of 84.7±51.0, 96.6±53.4 and 105.3±59.4 µg/m3 for non-pollution, mildly polluted and moderately polluted periods, respectively. Source apportionment of ozone and its precursor VOCs was performed using CMAQ and PMF models. The results demonstrated that reducing vehicle emissions should be prioritized to mitigate ozone pollution in Zhengzhou, as ransportation emissions accounted for 64 % and 31 % of ozone and VOC emissions, respectively. In addition, local ozone production rates and HOx base budgets were calculated using an observation-based model (OBM). The ozone production rates on non-pollution, mildly polluted, and moderately polluted days were respectively 2.0, 4.5, and 6.9 ppbv/h on average. The HOx radical concentration on polluted days was 1.5–6.4 times higher than that on non-pollution days, which is indicative of more efficient radical cycling during photochemical pollution. The O3-NOx-VOC sensitivity was analyzed using the OBM model, CMAQ model and ratio method. The results showed that ozone generation in Zhengzhou was mainly limited by VOCs, suggesting that the reduction of VOCs should be focused on aromatic hydrocarbons and olefins. The optimal reduction ratio of anthropogenic VOCs to NOx was about 2.9:1. This study will offer deeper insights for formulating effective ozone pollution prevention and control strategies.
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Status: open (until 03 Jan 2026)
- RC1: 'Comment on egusphere-2025-4519', Anonymous Referee #1, 27 Nov 2025 reply
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RC2: 'Comment on egusphere-2025-4519', Anonymous Referee #2, 15 Dec 2025
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In “Measurement report: Characterizing O3-NOₓ-VOC sensitivity and O3 formation in a heavily polluted central China megacity using multi-methods during 2019–2021 warm seasons” Yu et al. investigate the sensitivity of O3 formation in Zhengzhou City between 2019 and 2021 based on VOC in-situ observations, several models and machine learning tools. The authors find that O3 formation in the Chinese megacity is limited by the availability of VOCs and recommend a focus on VOC emission reductions with simultaneous NOx control.
While the investigation of O3 pollution generally remains a highly important topic, I have major concerns regarding the implementation and results presented in this study. The large number of methods, that often seem redundant, the use of many abbreviations (often not defined) and changes between units makes it difficult to follow the line of argument. The lack of presenting NOx measurements and a detailed discussion on the role of NOx in O3 formation makes it additionally challenging to understand how the authors reach their scientific conclusions. Unfortunately, I therefore cannot recommend this manuscript for publication in ACP.
Major Comments:
- Manuscript type: The manuscript type “Measurement Report” does not seem appropriate to me. A measurement report should “present substantial new results from measurements of atmospheric properties and processes from field and laboratory experiments” (https://www.atmospheric-chemistry-and-physics.net/about/manuscript_types.html). While it can be accompanied by model results, the focus should be on the presentation of a unique dataset rather than a pool of different methods, including modeling and machine learning tools.
- Number of methods: The authors use a large number of different methods to investigate O3 formation sensitivity. It is not clearly established why all these methods are needed and what their added value is. The questions posed could be answered with a reliable set of in-situ observations and an appropriate model to simulate missing trace gases. Instead, the introduction of all these methods is confusing and makes it difficult to follow the central line of argument.
- Measurements: From the results section, I understand that besides VOCs, measurements of NOx and O3 are available. However, there are no details presented in the methods section.
- NOx: Besides VOCs, Nitrogen Oxides are important precursors to tropospheric O3. However, the role of NOx seems to be mostly neglected in this study. A detailed description and discussion of the role of NOx are missing and I wonder how the authors reached their conclusions on O3 formation sensitivity, without accounting for NOx. E.g. the authors state that chemistry is VOC-limited in Zhengzhou, but suggest that VOC control is more important than NOx. VOC-limited chemistry is characterized by a large excess of NOx, which requires drastic emission cuts to improve long-term air quality.
- Correlation analysis: The presentation of correlations between different parameters in Section 3.1.1 seems random and does not follow a clear strategy, e.g. hypothesis – method – result – discussion. The set of in-situ observations is much more powerful than this: I recommend presenting trace gas levels (and if possible a longer time series), the characteristics of each season, diurnal cycles and the weekend effect for a sensitivity analysis. The application of machine learning tools is not necessary here or needs to be better justified.
- Abbreviations: Many abbreviations are used in this manuscript, and they are often not defined upon first use, which makes it difficult to follow. It is further concerning that the authors are in some cases not consistent with the abbreviations, e.g. “OBM” is an “observation-based model” in Line 41 and an “Ozone Box Model” in Line 128.
- Units: Many different units for trace gases are used throughout the text, including ppbv, ug/m3 and molecules/cm3. This makes it difficult to compare trace gas levels and I recommend choosing one unit (preferably mixing ratios) and using it throughout the entire manuscript.
- PM2.5: Why is PM2.5 relevant to this study? I recommend focusing on O3 and its precursors to avoid overloading this study.
Minor comments:
- 33 f.: This sounds like VOCs increase in response to O3 increases, while VOCs are precursors to O3.
- 34 f.: Do these values refer to VOC or O3 concentrations?
- 37: Please define abbreviations upon first use.
- 39: What is meant by “ozone emissions”? Ozone is not emitted but formed photochemically.
- 46: What’s the “ratio method”?
- 47: If ozone generation is limited by VOCs, it is highly important to control NOx. Of course, it remains important to reduce VOCs simultaneously, but long-term air quality improvements can only be reached through NOx reductions in that case.
- 55 ff.: Several things are missing in the introduction, i.a. how O3 is formed from its precursors and particularly what the role of NOx is.
- 65 ff.: Are the authors saying that they are the first to investigate O3 formation from increasing anthropogenic sources?
- 76 f.: This sounds like the range of VOC mixing ratios in China is 27 – 92 ppbv.
- 81 ff.: This section is difficult to follow due to the jumps between countries and continents.
- 83: Is BB the major VOC source throughout the entire year?
- 93 ff.: Are the authors talking about concentrations, emissions, formation rates or sensitivities?
- 115 ff.: Why not use a set of in-situ observations?
- 128: In the Abstract the authors state the OBM to be an observation-based model.
- 188: How were other trace gases and meteo parameters measured?
- 215: More details on the OBM are required.
- 223: The reaction of OH and NO2 does not destroy O3 but limits its formation. It should therefore be accounted for in Equation (3), rather than (4).
- 242: More details are needed on the WRF/CMAQ model.
- 248 ff.: What are all these abbreviations: FNL, SAPRC-99, AERO6, IC/BC, MEIC, REAS2?
- 262 f.: What are first- and second-order sensitivities of O3?
- 265 ff.: What exactly do these equations show?
- 277: Why is PM2.5 needed in this study?
- 283: Why would the model be better at simulating emitted species?
- 284: Only a small fraction of NO2 is emitted directly, most is formed photochemically from NO.
- 319: What’s MDL?
- 348: Why exactly is machine learning needed in this study?
- 425 / Fig. 1: Why is a smoothing applied? What exactly does it involve? Why is the time series not just averaged to the desired resolution?
- 426 ff.: All three numbers are the same. How exactly are the pollution levels defined?
- 432: What exactly do the percentage values relate to? If it’s years, the time period is too short for a trend analysis.
- 437: Why is O3 positively correlated with wind speed? Usually, higher wind speeds lead to less accumulation?
- 438: Because H2O contributes to O3 loss? These correlations need to be discussed in more detail.
- 476 / Fig. 2: Why is half the figure upside down?
- 482 f.: It should be specified what is meant by “affecting boundary layer structure” – the current term is very generic.
- 494: HO2 can be lost on aerosol surfaces, which inhibits O3 formation (opposite effect!)
- 522 ff.: I cannot follow this logic. NO is lower for high O3 days because (a) O3 generation is VOC-limited or because (b) of the titration effect close to NOx sources (NO + O3 --> NO2 + O2)
- 556 ff.: It is important to control NOx when chemistry is VOC-limited.
- 559 ff: What exactly are these different phases? Is titration meant by suppression?
- 571: Is there a specific reason to investigate midnight concentrations? Maybe the analysis should be limited to daylight values.
- 652: These sources emit both VOCs and NOx.
- 656 ff.: How exactly were these factors identified? Why are there six factors? Additional explanations are needed here.
- 696 ff. / Fig. 6: There does not seem to be a relevant difference between the three cases. What’s the uncertainty? Are the differences even significant?
- 706 ff.: Please provide an explanation for speculations.
- 799 ff.: Sillman et al. suggested the HCHO to NO2 ratio for O3 sensitivity analysis.
- 803: What is MEM?
- 827: What is RIR?
- 944: It is not clear why the slope of the ridge could indicate the ratio at which VOCs and NOx need to decline. Wouldn’t it be important to reduce NOx as quickly as possible to move towards NOx limited chemistry?
- 961: What is meant by “high-resolution observations” – the hourly measurements?
Citation: https://doi.org/10.5194/egusphere-2025-4519-RC2 -
RC3: 'Comment on egusphere-2025-4519', Anonymous Referee #3, 23 Dec 2025
reply
This work discussed concerns ozone formation within ZhengZhou, China, a mega city with considerable anthropogenic activity. The authors use observations (2019-2021), a box model, CMAQ, and machine learning tools to investigate the emissions sectors and species contributing to ozone during the period.
Unfortunately, this manuscript is rambling and does not present a clear message. “Conclusions” discussed are not traceable, and basic concepts well established in the community about ozone formation are clearly not well understood by the authors. Inadequate discussion of key factors to the analysis, along with generic findings does not lend well to this work, in its current form, being useful to the community and therefore I do not recommend this manuscript for publication in ACP.
Section comments:
Methods: The manuscript uses a variety of models, and methods, many of which are confusing for the reader to understand and follow. The authors need to shorten the observations and methods section (10 pages is excessive), and more succinctly describe the methodology used for this analysis. Make use of supplemental information for details that are not as critical. The paper should convey the main points, the big concepts of this work.
Results: Many of the findings presented in the results section are not groundbreaking, or new, and rely on machine learning techniques which not well described and therefore are questionable at best for accurately accessing relationships between ozone and precursor species. Additionally, the authors mention PM2.5, like a buzz word – the scope of this paper needs to be made smaller and more impactful. The units should be mixing ratios when discussing gaseous species, not the variety of units that are currently mentioned in the paper. What are the criteria to classify non-polluted, lightly polluted, and moderately polluted days? Discussion of the ozone diurnal cycle are not fully accurate, basic knowledge of ozone formation is clearly lacking by the authors. No clear policy relevant message is conveyed – it seems the authors do not have a great handle on the differing results from the different methods used.
Conclusions: Nothing of consequence discussed here. No policies recommended, again, nothing novel presented.
Citation: https://doi.org/10.5194/egusphere-2025-4519-RC3
Data sets
VOCs Dataset S. Yu et al. https://doi.org/10.5281/zenodo.17214861
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- 1
This manuscript investigates O3–NOx–VOC sensitivity and O3 formation mechanisms in Zhengzhou (2019–2021) using a combination of online VOC measurements, OBM, CMAQ-DDM, source apportionment, PMF, and machine-learning (ML)/SHAP interpretation. While the dataset is valuable and the research direction is meaningful, the manuscript suffers from inconsistent methodology, unclear descriptions of model configurations, uncertainties and machine learning, no comparisons between different analytical models for the O3 formation mechanism, and very vague data interpretation. The manuscript is long and unreadable. Therefore, I suggest the manuscript be rejected.
Major Comment:
In addition, there is no cross-method comparison. A combined table is highly recommended to show the section contributions across PMF, CMAQ-DDM, and OBM RIR/EKMA. As a result, the manuscript reads like a report by stacking results (sensitivity diagnostics + VOC and O3 source apportionment + ML/SHAP), but with limited discussion.
Minor Comment:
Technical Comment: