the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
The driving factors of new particle formation and growth in the polluted boundary layer
Mao Xiao
Christopher R. Hoyle
Lubna Dada
Dominik Stolzenburg
Andreas Kürten
Mingyi Wang
Houssni Lamkaddam
Olga Garmash
Bernhard Mentler
Ugo Molteni
Andrea Baccarini
Mario Simon
Xu-Cheng He
Katrianne Lehtipalo
Lauri R. Ahonen
Rima Baalbaki
Paulus S. Bauer
Lisa Beck
David Bell
Federico Bianchi
Sophia Brilke
Dexian Chen
Randall Chiu
António Dias
Jonathan Duplissy
Henning Finkenzeller
Hamish Gordon
Victoria Hofbauer
Changhyuk Kim
Theodore K. Koenig
Janne Lampilahti
Chuan Ping Lee
Huajun Mai
Vladimir Makhmutov
Hanna E. Manninen
Ruby Marten
Serge Mathot
Roy L. Mauldin
Wei Nie
Antti Onnela
Eva Partoll
Tuukka Petäjä
Joschka Pfeifer
Veronika Pospisilova
Lauriane L. J. Quéléver
Matti Rissanen
Siegfried Schobesberger
Simone Schuchmann
Yuri Stozhkov
Christian Tauber
Yee Jun Tham
António Tomé
Miguel Vazquez-Pufleau
Andrea C. Wagner
Robert Wagner
Yonghong Wang
Lena Weitz
Daniela Wimmer
Yusheng Wu
Penglin Ye
Qiaozhi Zha
Xueqin Zhou
Antonio Amorim
Ken Carslaw
Joachim Curtius
Armin Hansel
Rainer Volkamer
Paul M. Winkler
Richard C. Flagan
Markku Kulmala
Douglas R. Worsnop
Jasper Kirkby
Neil M. Donahue
Urs Baltensperger
Josef Dommen
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- Final revised paper (published on 27 Sep 2021)
- Supplement to the final revised paper
- Preprint (discussion started on 20 Jan 2021)
- Supplement to the preprint
Interactive discussion
Status: closed
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RC1: 'Comment on acp-2020-1323', Anonymous Referee #1, 19 Feb 2021
Review of "The Driving Factors of New Particle Formation and Growth in the Polluted Boundary Layer" by M. Xiao et al.
This is a well-written and extremely interesting manuscript describing a comprehensive set of experiments on the chemical mechanisms of new particle formation (NPF) in an environment representative of a polluted urban atmosphere. The study provides an explanation for the occurrence of NPF when there is very strong competition for precursor vapors by high concentrations of pre-existing aerosol particles. The successful nucleation and growth of particles in these environments is important, because it distributes aerosol mass to smaller sizes, changing the interaction of these particles with sunlight, the numbers of cloud-nucleating particles, and the fate of the aerosol mass in the human respiratory system. These topics have broad interest, and the manuscript is definitely suitable for publication in ACP.
The investigators demonstrate that sulfuric acid + dimethylamine and other bases like ammonia dominate NPF in polluted atmospheres, even in the presence of high concentrations of oxidation products of aromatics, which can have quite low volatility. The growth of the newly formed particles to larger sizes involves many other compounds, including organics. There is a very strong temperature dependence to the NPF.
This work employs cutting-edge research instruments and the CERN CLOUD chamber to make these measurements. The results are well described and the interpretation is clear. The methods are also well described, and earlier work is appropriately referenced and discussed. The manuscript is very well written. I believe it is suitable for publication with only minor technical changes.
Comments:
1) Throughout the PDF manuscript, following a capital "A" there is a space and the remainder of the word is shifted to the right. This must be some sort of PDF conversion problem, but the authors and copy editors should carefully proof the online and print versions of the final manuscript to see if this issue still exists.
2) It's a bit odd in ACP to have the Methods following the Results. This is more common in journals such as Nature and Science, where a wide audience is presumed and the methods are relegated to an appendix-like attachment, with a smaller font. I don't have a problem with this structure for ACP, but wish to call attention to it in the event there are editorial norms that would suggest moving the Methods toward the front.
3) Line 134: define "GR"
4) Line 138: For clarity, perhaps say "cluster self-coagulation dominates the growth." It took me a moment to understand what the authors were meaning.
5) Line 144: "The multicomponent system used in the simulations. . . ." What simulations? Stolzenburg et al. (2020)?
6) Line 168: The chamber simulations do reproduce observed urban GRs; however, it is probably worth noting here that the more complex chemistry of the ambient urban atmosphere may lead to other species contributing to particle growth than are investigated at the CLOUD chamber. One should not presume that the relatively simple mixtures explored here can replicate the full complexity of atmospheric processes.
7) Line 214: In the previous paragraph you state that the experiments were at the CLOUD chamber; no need to repeat that here.
8) Line 240: DMA is already defined.
9) Line 244: No mention here of how OH was determined; this appears later in the manuscript (Eq. 5) but would logically be verbally described here.
10) Line 265: Replace "DMA-train" with "differential mobility analyzer train". Too many "DMA"s.
11) Lines 266-7: Define PSM, SMPS, and CPC.
12) Eq. 1: Perhaps have a subscript "dp" for the J and N variables, since you calculate these values for different size particles (e.g., 1.7 nm, 3 nm).
13) Line 305: Provide model number and company name for the H3O+ CIMS and state the method (e.g., cavity ringdown spectrometry), model number, and company name for the NH3 analyser.
14) Line 311: Is the PTR3 a custom-built instrument? If so, say this and if not, give model number and company name.
15) Line 314: Define STOF and give model number and company name for the "PTRS", which should be "PTRMS".
16) Line 359: Please reference the form of the Cunningham slip correction equation you are using; there are several and they do have some differences.
17) References: Please review the reference formatting and ensure it follows Copernicus guidelines. EndNote-style reference managers always make mistakes; for example, for Breitenlechner et al. the title of the paper is capitalized, and in Dunne et al. the page range is not completed. If you correct these errors now it will save the copy editors the effort of finding all them and asking you to fix them later.
18) Fig. 1. I used a pen to label all the lines and symbols because this is such a busy graph. I suggest you go ahead and do that to make it much easier to interpret.
19) Fig. 1 caption. The penultimate sentence should say that the nucleation rate of H2SO4+DMA at the kinetic limit is shown by the cyan curve.
20) Fig. 2 caption: In the last sentence there needs to be a space in bicycloalkylradicals.
21) Fig. 4 caption: What do you mean by, "At larger particle sizes, the contribution of organics will increase further."? What's the basis for this statement.
22) Fig. 4b: It's hard to distinguish the green and blue curves (biogenic with and without NO) from each other. Can you use a different line type for each?
23) Fig. 5: In the caption please list the name and country of each location indicated in the condensation sink box in the graph, as you did for Fig. 7.
24) Fig. 6. What information is conveyed by the size of the symbols?
Citation: https://doi.org/10.5194/acp-2020-1323-RC1 -
AC1: 'Reply on RC1', Mao Xiao, 24 May 2021
The comment was uploaded in the form of a supplement: https://acp.copernicus.org/preprints/acp-2020-1323/acp-2020-1323-AC1-supplement.pdf
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AC1: 'Reply on RC1', Mao Xiao, 24 May 2021
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RC2: 'Comment on acp-2020-1323', Anonymous Referee #2, 19 Mar 2021
Comments on “The driving factors of new particle formation and growth in the
polluted boundary layer” by Xiao et al.
Xiao et al. make an important contribution on nailing down the different role of precursors and environment factors (mainly temperature) on new particle formation and growth in contrast/diverse conditions in the atmosphere. In their controlled chamber experiments, large variability in NPF rate has been observed, which covers the observed variability in the real atmosphere. The results and conclusion will be very helpful on understanding and interpretating the ambient observations of NPF rates and growth, especially in polluted urban environment. The manuscript is well written, and plots are nicely crafted.
I recommend its publication and have following comments for improvements.
- As the main goal of this study is to explain the large variability of the NPF rate in the different environment, it would be nice if the related real atmospheric environment that can be clearly defined, for example, Beijing clean, Madrid, Nanjin, Nanjin Beijing transition, Beijing haze, SE US, SW US, Tartu, Xian, Zurich and so on. I see that the authors have somehow made such attempt by marking them in some plots (e.g., Figure 2A and Figure 5 etc.), but a table of concentrations ranges of the varied precursors, as well as the ambient temperature when the observations were made would be very helpful. I also suggest strengthening a bit the discussion on comparison between chamber conditions and real environmental conditions.
- “These conflicting observations are subject of intense scientific debate of late (Brean et al., 2020; Cai et al., 2020; Guo et al., 2020) and highlight…” It would be nice if the authors could elaborate a bit here what are the “scientific debate” here, and I believe it will help the readers to have a better overview and understanding of the motivation of this study.
- I understand that putting the Method section at the end is probably to obey the formatting requirement of letter, the authors may want to refer to sub-sections, descriptions and equations of the Method section in the main text, so the readers could cross check. For example, how are the “Organic fraction of GR” in Figure 4B derived?
- In Figure 3, organic seems having stronger effects when DMA is absent. Could the authors comment on it? For clarity, I suggest explaining that “Base” means both NH3 and DMA are present in the figure caption. There is an additional “Figure 3.” in the figure caption.
- In Figure 5, survival probability in Beijing haze condition seems extremely low. Here, CS6 is used, and I am wondering how pollute are the Nanjin Beijing transition and Beijing haze condition? E.g., PM1 or PM2.5 concentrations? A related question is that “polluted boundary layer” is with what PM1 or PM2.5 levels approximately?
- “We compare chamber simulations and atmospheric observations in Fig. 7 using sub-3 nm GR as a proxy for total condensable vapour concentrations…” It seems that total condensable vapor concentration in BJ is not high as marked in Figure 7. One would expect that high as the pollution level there is quite high. Could the authors comment on it?
Citation: https://doi.org/10.5194/acp-2020-1323-RC2 -
AC2: 'Reply on RC2', Mao Xiao, 24 May 2021
The comment was uploaded in the form of a supplement: https://acp.copernicus.org/preprints/acp-2020-1323/acp-2020-1323-AC2-supplement.pdf