the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
| 08 Apr 2022
A comprehensive study about the in-cloud processing of nitrate through coupled measurements of individual cloud residuals and cloud water
Guohua Zhang
Xiaodong Hu
Wei Sun
Yuxiang Yang
Ziyong Guo
Yuzhen Fu
Haichao Wang
Shengzhen Zhou
Mingjin Tang
Zongbo Shi
Duohong Chen
Xinming Wang
Abstract. While the formation and evolution of nitrate in airborne particles are extensively investigated, little is known about the processing of nitrate in clouds. Here we present a detailed investigation on the in-cloud formation of nitrate, based on the size-resolved mixing state of nitrate in the individual cloud residual and cloud-free particles obtained by single particle mass spectrometry, and also the mass concentrations of nitrate in the cloud water and PM2.5 at a mountain site (1690 m a.s.l.) in southern China. The results show a significant enhancement of nitrate mass fraction and relative intensity of nitrate in cloud water and the cloud residual particles, respectively, reflecting a critical role of in-cloud processing in the formation of nitrate. We first exclude the gas phase scavenging of HNO3 and the facilitated activation of nitrate-containing particles as the major contribution for the enhanced nitrate, according to the size distribution of nitrate in individual particles. Based on regression analysis and theoretical calculations, we then reveal a critical role of in-cloud formation of nitrate via N2O5 hydrolysis, even during the daytime, attributed to the diminished light in clouds. Nitrate is highly related (R2 = ~0.6) to the variation of [NOx][O3], temperature and droplet surface area in clouds. Accounting for droplet surface area greatly enhances the predictability of the observed nitrate compared with using [NOx][O3] and temperature. The substantial contribution of N2O5 hydrolysis to nitrate in clouds during the daytime was reproduced by a multiphase chemical box model. Assuming that the photolysis rate is 30 % of the default setting, the overall contribution of N2O5 hydrolysis pathway to nitrate formation increases by ~20 % in clouds. Given that N2O5 hydrolysis acts as a major sink of NOx in the atmosphere, further model updates would improve our understanding about the processes contributing to nitrate production in cloud and the cycling of odd nitrogen.
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The requested preprint has a corresponding peer-reviewed final revised paper. You are encouraged to refer to the final revised version.
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Preprint
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The requested preprint has a corresponding peer-reviewed final revised paper. You are encouraged to refer to the final revised version.
- Preprint
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Supplement
(731 KB) - BibTeX
- EndNote
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Journal article(s) based on this preprint
Guohua Zhang et al.
Interactive discussion
Status: closed
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RC1: 'Comment on egusphere-2022-178', Anonymous Referee #1, 29 Apr 2022
Review comments for Zhang et al
This paper aims to investigate the formation and evolution of nitrate in clouds, which has been rarely studied, based on the size-resolved mixing state of nitrate in the individual cloud residual and cloud-free particles by single particle mass spectrometry and the mass concentrations of nitrate in the cloud water and PM2.5 in southern China. The data show the direct observational evidence for the enhanced nitrate formation in the cloud water and residual particles, which is attributed to the enhanced hydrolysis of N2O5. Such a comprehensive dataset is quite robust for discussions and conclusions. Given that the in-cloud process is critical to accurately evaluating the evolution and oxidative impacts of nitrate, which is increasingly important, the manuscript is worthy of publication after considering my suggestions.
Major Comments:
(1) The authors first exclude the scavenging of gas-phase HNO3 as a major pathway through the analysis of the size distribution of nitrate RPA and RPA ratio (nitrate/sulfate). However, the discussions based on such data are not clear enough. More detailed comparison and/or theoretical basis should be included to support the discussion.
(2) The authors show that the hydrolysis of N2O5 explains ~1-3% increase in the nitrate mass fraction in clouds, whereas the in-cloud processing contributed to > 5% increase, and two possible explanations were provided. I wonder if it is possible to reveal the most important factor and if there are other possibilities since the consideration of these explanations may still not fully explain the observation.(3) In Fig. S1, I noticed that the relative humidity is close to 100% during cloud events, but RH inevitably declines during the cloud-free period. Given that RH has a certain impact on the hydrolysis of N2O5 and the scavenging of gas-phase HNO3, which is worth to have some discussions on it.
Specific comments:
(1) Introduction: The authors summarized the previous studies on the in-cloud processing of nitrate and showed that the detailed observational investigations and the possible mechanisms governing nitrate behavior upon in-cloud processes are scarce. It would be better to include how these studies quantify the relative roles of each pathway for the formation of nitrate in clouds.
(2) Line 141: The predefined sampling cloud droplet size is 7.5-8.5 μm. So why is the mean droplet size assumed to be at 7 μm when calculating the SA?
(3) Line 284: More detailed discussion should be provided to indicate the fast heterogeneous uptake coefficient, and also the specific values.
(4) Line 356: The involvements of VOCs may impact the formation of nitrate through various mechanisms, e.g., direct reaction with NO3 or consumption the oxidants such as OH, which should be discussed in detail.
Figure 3: It will be easier to understand if the chemical formulas N2O5 and NO3- are written in the axes of the figure instead of “nitrate”.
SI line 47: It should be “Text S1”.
SI figure S4: It's difficult to understand this figure, can you describe the horizontal and vertical coordinates more clearly in the figure caption?
Citation: https://doi.org/10.5194/egusphere-2022-178-RC1 -
AC1: 'Reply on RC1', Xinhui Bi, 07 Jun 2022
The comment was uploaded in the form of a supplement: https://egusphere.copernicus.org/preprints/2022/egusphere-2022-178/egusphere-2022-178-AC1-supplement.pdf
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AC1: 'Reply on RC1', Xinhui Bi, 07 Jun 2022
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RC2: 'Comment on egusphere-2022-178', Anonymous Referee #2, 28 May 2022
This study provided deep insights into the in-cloud processing nitrate formation. Nitrate is becoming a dominated fraction in fine particle in China. Investigating the nitrate formation is important to understand haze formation. It can be published in ACP after considering the following issues:
The discussion about the chemistry processes in the sampling site should be strengthened: Why the ozone concentrations were kept a relatively high level, even during nighttime? In 2018, the ozone concentrations were above 80 ppb during the entire field campaign, and, above 100 ppb for 2020. An explanation is needed for such high ozone concentration in the sampling site, especially cloudy condition. Additionally, “substantial attenuation of the incident solar radiation by clouds” may suppress the ozone formation, thereby, affect the N2O5 formation. The N2O5 uptake is a major contributor to in-cloud formed nitrate, more explanations of N2O5 sources are also needed.
Citation: https://doi.org/10.5194/egusphere-2022-178-RC2 -
AC2: 'Reply on RC2', Xinhui Bi, 07 Jun 2022
The comment was uploaded in the form of a supplement: https://egusphere.copernicus.org/preprints/2022/egusphere-2022-178/egusphere-2022-178-AC2-supplement.pdf
-
AC2: 'Reply on RC2', Xinhui Bi, 07 Jun 2022
Interactive discussion
Status: closed
-
RC1: 'Comment on egusphere-2022-178', Anonymous Referee #1, 29 Apr 2022
Review comments for Zhang et al
This paper aims to investigate the formation and evolution of nitrate in clouds, which has been rarely studied, based on the size-resolved mixing state of nitrate in the individual cloud residual and cloud-free particles by single particle mass spectrometry and the mass concentrations of nitrate in the cloud water and PM2.5 in southern China. The data show the direct observational evidence for the enhanced nitrate formation in the cloud water and residual particles, which is attributed to the enhanced hydrolysis of N2O5. Such a comprehensive dataset is quite robust for discussions and conclusions. Given that the in-cloud process is critical to accurately evaluating the evolution and oxidative impacts of nitrate, which is increasingly important, the manuscript is worthy of publication after considering my suggestions.
Major Comments:
(1) The authors first exclude the scavenging of gas-phase HNO3 as a major pathway through the analysis of the size distribution of nitrate RPA and RPA ratio (nitrate/sulfate). However, the discussions based on such data are not clear enough. More detailed comparison and/or theoretical basis should be included to support the discussion.
(2) The authors show that the hydrolysis of N2O5 explains ~1-3% increase in the nitrate mass fraction in clouds, whereas the in-cloud processing contributed to > 5% increase, and two possible explanations were provided. I wonder if it is possible to reveal the most important factor and if there are other possibilities since the consideration of these explanations may still not fully explain the observation.(3) In Fig. S1, I noticed that the relative humidity is close to 100% during cloud events, but RH inevitably declines during the cloud-free period. Given that RH has a certain impact on the hydrolysis of N2O5 and the scavenging of gas-phase HNO3, which is worth to have some discussions on it.
Specific comments:
(1) Introduction: The authors summarized the previous studies on the in-cloud processing of nitrate and showed that the detailed observational investigations and the possible mechanisms governing nitrate behavior upon in-cloud processes are scarce. It would be better to include how these studies quantify the relative roles of each pathway for the formation of nitrate in clouds.
(2) Line 141: The predefined sampling cloud droplet size is 7.5-8.5 μm. So why is the mean droplet size assumed to be at 7 μm when calculating the SA?
(3) Line 284: More detailed discussion should be provided to indicate the fast heterogeneous uptake coefficient, and also the specific values.
(4) Line 356: The involvements of VOCs may impact the formation of nitrate through various mechanisms, e.g., direct reaction with NO3 or consumption the oxidants such as OH, which should be discussed in detail.
Figure 3: It will be easier to understand if the chemical formulas N2O5 and NO3- are written in the axes of the figure instead of “nitrate”.
SI line 47: It should be “Text S1”.
SI figure S4: It's difficult to understand this figure, can you describe the horizontal and vertical coordinates more clearly in the figure caption?
Citation: https://doi.org/10.5194/egusphere-2022-178-RC1 -
AC1: 'Reply on RC1', Xinhui Bi, 07 Jun 2022
The comment was uploaded in the form of a supplement: https://egusphere.copernicus.org/preprints/2022/egusphere-2022-178/egusphere-2022-178-AC1-supplement.pdf
-
AC1: 'Reply on RC1', Xinhui Bi, 07 Jun 2022
-
RC2: 'Comment on egusphere-2022-178', Anonymous Referee #2, 28 May 2022
This study provided deep insights into the in-cloud processing nitrate formation. Nitrate is becoming a dominated fraction in fine particle in China. Investigating the nitrate formation is important to understand haze formation. It can be published in ACP after considering the following issues:
The discussion about the chemistry processes in the sampling site should be strengthened: Why the ozone concentrations were kept a relatively high level, even during nighttime? In 2018, the ozone concentrations were above 80 ppb during the entire field campaign, and, above 100 ppb for 2020. An explanation is needed for such high ozone concentration in the sampling site, especially cloudy condition. Additionally, “substantial attenuation of the incident solar radiation by clouds” may suppress the ozone formation, thereby, affect the N2O5 formation. The N2O5 uptake is a major contributor to in-cloud formed nitrate, more explanations of N2O5 sources are also needed.
Citation: https://doi.org/10.5194/egusphere-2022-178-RC2 -
AC2: 'Reply on RC2', Xinhui Bi, 07 Jun 2022
The comment was uploaded in the form of a supplement: https://egusphere.copernicus.org/preprints/2022/egusphere-2022-178/egusphere-2022-178-AC2-supplement.pdf
-
AC2: 'Reply on RC2', Xinhui Bi, 07 Jun 2022
Peer review completion
Journal article(s) based on this preprint
Guohua Zhang et al.
Guohua Zhang et al.
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The requested preprint has a corresponding peer-reviewed final revised paper. You are encouraged to refer to the final revised version.
- Preprint
(706 KB) - Metadata XML
-
Supplement
(731 KB) - BibTeX
- EndNote
- Final revised paper