the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Modeling organic aerosol over Central Europe: uncertainties linked to different chemical mechanisms, parameterizations, and boundary conditions
Abstract. This study explores the uncertainties in modeling organic aerosol (OA) over Central Europe, focusing on the roles of chemical mechanisms, emission parameterizations, and boundary conditions. Organic aerosols, particularly secondary organic aerosols (SOAs), significantly influence climate, health, and visibility, comprising up to 90 % of submicron particulate matter. Using the Comprehensive Air Quality Model with Extensions (CAMx) coupled with the Weather Research and Forecast Model, sensitivity analyses were conducted to assess the impact of intermediate-volatility organic compounds (IVOCs), semi-volatile organic compounds (SVOCs), and chemical boundary conditions on primary and secondary organic aerosol concentrations.
Results showed that including source-specific IVOC and SVOC emissions significantly improved CAMx's performance in reproducing observed OA levels, mainly when using the 1.5-dimensional Volatility Basis Set framework with activated chemical aging. For example, the domain-averaged SOA concentrations increased by up to 1.17 μg m-3 during summer when both IVOC and SVOC emissions were included. Furthermore, incorporating OA into the boundary conditions enhanced model predictions, with the accuracy of modeled organic carbon concentrations improving by up to 100 % during summer at some monitoring sites. Despite these improvements, challenges remain due to uncertainties in emission estimates, parameterization schemes, and the spatial resolution of the models.
The findings underscore the importance of refined parameterizations for IVOC and SVOC emissions, higher temporal and spatial resolution in chemical boundary conditions, and better representation of chemical aging. Addressing these gaps in future studies will further enhance the understanding and prediction of OA dynamics in regional air quality modeling.
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Status: final response (author comments only)
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RC1: 'Comment on egusphere-2025-167', Anonymous Referee #2, 07 May 2025
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AC2: 'Reply on RC1', Lukáš Bartík, 01 Aug 2025
The comment was uploaded in the form of a supplement: https://egusphere.copernicus.org/preprints/2025/egusphere-2025-167/egusphere-2025-167-AC2-supplement.pdf
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AC2: 'Reply on RC1', Lukáš Bartík, 01 Aug 2025
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RC2: 'Comment on egusphere-2025-167', Anonymous Referee #1, 15 May 2025
The manuscript “Modeling organic aerosol over Central Europe: uncertainties linked to different chemical mechanisms, parameterizations, and boundary conditions” by Bartík et al. combines CAMx model simulations with observations from sites located in Czech Republic. They investigate the sensitivity of organic aerosol concentrations simulated with CAMx on assumptions regarding IVOC and SVOC emissions and model boundary conditions. The topic fits within the scope of ACP. The model evaluation and sensitivity analysis presented in the manuscript are valuable work towards improving model representation of organic aerosols. However, the manuscript contains shortcomings in the description of methods and results and these should be addressed before the manuscript can be recommended for publication.
Major comments
1. The main aspects of the model related to the presented analysis should be included for the reader to be able to understand the work. I find that following aspects of the model should be described better:
- L121-126: Why were two chemistry mechanisms used? Could the authors please explain here some basics of what kind of chemistry these two mechanisms include and what are the main similarities/differences between them or otherwise explain the use of two mechanisms. For example, do the two mechanisms include essentially different precursors and/or reaction products?
- L127-134: Since aerosols are in focus in this study, please describe the basics of aerosol representation in the model, e.g.: What aerosol dynamics processes are included? Is condensation calculated based on equilibrium partitioning or some other way? It is said that ISORROPIA is used to predict composition and physical phase of inorganic aerosols. Are the organic and inorganic aerosols assumed externally mixed?
- L159-160: What are these concentrations of the chemical species based on?
- Table S1: The SOAP and VBS schemes seem to consider monoterpenes and sesquiterpenes but these species do not seem to be included in the boundary conditions. If that is the case, why is it so? At least the overall picture of what is and what isn't included in the boundary conditions should be described in the main text.
- L180-183: Authors should clarify here that the aging is included in CVb for POA and anthropogenic SOA. In appendix on L574 it is stated that "The gas-phase hydroxyl radical reaction rates for the chemical aging of POA and anthropogenic SOA, except those originating from biomass burning, are assumed to be 4×10−11 and 2×10−11 cm3 molecule−1 s−1, respectively. In contrast, the chemical aging of biogenic SOA and SOA originating from biomass burning (both anthropogenic and biogenic) is disabled." There authors should make it clear that this disabling of aging refers to the reference run, not for all runs with VBS scheme.
- L185-190: Why were different emissions used for simulations with different SOA mechanisms? Also, were all POA emissions really replaced with POM_SV emissions? Does that mean that all POA was assumed to be semivolatile? Use of POM_SV in the model is one of the main focus points in the manuscript and Table 2 lists parameterizations used for these, but explanation of how these POM_SV are treated in the model is missing. Does all POM_SV have same volatility in the model?
- L560-563: What does "more-volatile" and "less-volatile" mean concretely in terms of volatilities?
2. Description of the observational data used for the model evaluation would need more information:
- A map showing the locations of the observational sites would be helpful for a reader. This could be a separate map or the locations could be marked in e.g. in the Fig. 1.
- L237-238: According to the Table S6, the length of each of these measurement campaigns was only about one month. Please mention that in the main text.
- L250-252: Please mention how long time period was considered from these data.
3. Some clarifications or explanations would be needed in the results section:
- L367-368: Could you please explain why you have chosen different emission estimates?
- L430: What does the "similar conclusion" refer to here? Does it refer to the conclusion in the previous sentence about wind speed inaccuracy in the model being possibly the explanation for the underestimated OC? Why would that affect CVb and CVa most?
- Are the concentrations in the map figures (e.g. Fig. 4) surface level concentrations or, e.g., averaged through the vertical layers of the model?
- L493-495: “The observed impacts in these simulations are likely linked to changes in other pollutant(s) at the boundaries of the model domain, which influence SOA chemistry.” Could the authors please explain what these other pollutants are, how/why they changed and how that would affect the organic aerosol in the model?
- L495-496: “The spatial distributions of the mean seasonal impacts on SOA concentrations in Sp50s50 and Sp0s100 (and similarly in Vp50s50 and Vp0s100) exhibit structures akin to those observed for the mean seasonal impacts on POA concentrations in Sp50s50 and Sp100s0 (and likewise in Vp50s50 and Vp50s000) (Figs. 8c and d) during both seasons.” Could the authors please comment if this is an expected result? Or does this point towards the boundary conditions defining too much the concentrations over the simulated area?
- L522-529: Why does the improvement with adding the OA at boundaries differ between the stations and seasons? Also, is it reasonable to assume that the OA at boundaries is only or mostly POA, i.e. do the authors expect that adding the OA as POA at boundaries is getting model results closer to the measured values because it is making the model representation of organic aerosols more accurate, or is the agreement better just because there is a large underestimation in the reference simulation and adding the OA at boundaries as POA happens to increase OA concentration most?
4. This study includes sensitivity analysis on estimates of IVOC and SVOC emissions and OA boundary conditions, as well as comparisons using two different SOA schemes and chemistry schemes. Is it possible to conclude which of the analyzed factors/assumptions, or their uncertainties, are most important from the point of view of modelling OA in Central Europe with this model?
Minor comments
Please mention in the abstract that the evaluation of the model simulations is focused on Czech Republic. Currently the reader finds out quite late in the text that the evaluation is not for wider Central Europe but only for one country.
L21: “have an undoubted environmental footprint” Please check the choice of word. In my understanding environmental footprint term is used for the impact of e.g. organization or products on environment, so for the source of aerosols one could talk about environmental footprint, but not for aerosols themselves. I did not find the term “environmental footprint” from the reference given for this statement, therefore it is not clear what the authors mean by this term.
L136-137: I would suggest moving this essential information from the Appendix to the main text.
Some of the figures, e.g. Figure 2, are missing y-axis labels. I recommend adding y-axis labels.
Tables S3, S4 and S5 contain acronyms for surrogate SOA/POA species in the model. Please add explanation of what these species are.
Citation: https://doi.org/10.5194/egusphere-2025-167-RC2 -
AC1: 'Reply on RC2', Lukáš Bartík, 01 Aug 2025
The comment was uploaded in the form of a supplement: https://egusphere.copernicus.org/preprints/2025/egusphere-2025-167/egusphere-2025-167-AC1-supplement.pdf
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The study presents some key challenges in accurately modeling organic aerosol concentrations over Central Europe. By using an advanced regional model along with the different approaches for atmospheric aging of organic matter, it identifies the importance of including explicit SVOC and IVOC parameterizations in emission inventories to achieve higher agreement with observations. Moreover, it points out that the share between primary and secondary organic aerosol considered for the boundary conditions is a critical choice for accuracy. This study explores a region that has not been the main focus of air quality research in Europe and would therefore be a useful reference for the community. Before I can suggest it for final publication, there are some major and minor issues that should be first addressed. You can find them below :
Major Comments :
Minor Comments :
References
Meroni, A., Pirovano, G., Gilardoni, S., Lonati, G., Colombi, C., Gianelle, V., Paglione, M., Poluzzi, V., Riva, G., and Toppetti, A.: Investigating the role of chemical and physical processes on organic aerosol modelling with CAMx in the Po Valley during a winter episode, Atmospheric Environment, 171, 126–142, https://doi.org/10.1016/j.atmosenv.2017.10.004 , 2017.