the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Superimposed effects of typical local circulations driven by mountainous topography and aerosol-radiation interaction on heavy haze in the Beijing-Tianjin-Hebei central and southern plains in winter
Abstract. Although China’s air quality has substantially improved in recent years due to the vigorous emission reduction, the Beijing-Tianjin-Hebei (BTH) region, especially its central and southern plains at the eastern foot of the Taihang Mountains, has been the most polluted area in China with persistent and severe haze in winter. Combining meteorology-chemistry coupled model simulations and multiple observations, this study explored the causes of several heavy haze events in this area in January 2017, focusing on local circulations related to mountain terrain. The study results showed that on weather scale, the configuration of the upper, middle, and lower atmosphere provided favorable weather and water vapor transport conditions for the development of haze pollution. Under the weak weather-scale systems, local circulation played a dominant role in the regional distribution and extreme values of PM2.5. Influenced by the Taihang and Yanshan Mountains, vertical circulations and wind convergence zone were formed between the plain and mountain slopes. The vertical distribution of pollutants strongly depended on the intensity and location of the circulation. Strong and low circulation was more unfavorable to the vertical diffusion and horizontal transport of near-surface pollutants. More importantly, we found that aerosol-radiation interaction (ARI) significantly amplified the impacts of local vertical circulations on heavy haze by two mechanisms. First, ARI strengthened the vertical circulations at the lower levels, with the zonal wind speeds increasing by 0.2–0.8 m s-1. Meanwhile, ARI could cause a substantial downward shift of the vertical circulations (~100 m). Second, ARI weakened the horizontal transport of pollutants by reducing the westerly winds below 300 m and enhancing the wind convergence below 1000 m. Under these two mechanisms, pollutants could only recirculate in a limited space. This superposition of typical local circulation and ARI eventually contributed to the accumulation of pollutants and the consequent deterioration of haze pollution in the region.
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Notice on discussion status
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
(2838 KB)
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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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- Final revised paper
Journal article(s) based on this preprint
Interactive discussion
Status: closed
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RC1: 'Comment on egusphere-2022-780', I. Pérez, 03 Jan 2023
The current paper is focused on the air pollution by PM2.5 at the Beijing-Tianjin-Hebei region in China. The subject merits to be investigated due to the noticeable impact on the affected population. The period investigated is around January 2017, although only three days are selected. Measurements are considered together with modelling analysis. Observations are provided by the National Environmental Monitoring Center, 149 stations, and the Hebei Meteorological service, 210 stations. Moreover, two kind of modelling calculations are used, one of them with the aerosol-radiation interaction, and the second calculation without this interaction. The synoptic pattern is presented at varied pressure surfaces, and vertical cross-sections with the airflow and concentration are also shown. Although the subject and procedure are suitable for a publication, some restrictions of this research indicate that this paper could be accepted in a journal with low impact, but not in Atmospheric Chemistry and Physics.
The main inconvenience lies on the extremely low number of situations where the study is made, only three days, 6th, 17th, and 24th. Although the analysis is detailed, the readers should know if these days are representative enough for the pollution days at this site. Moreover, the readers should know if these conditions could be reproduced at different sites.
Since the pollution levels are affected by factors such as the emissions and the meteorological variables, some information about the patterns of both factors could be useful to focus the pollution problem at the site.
Figure 2 presents the concentration evolution. The authors should comment the reason to discard the first days of the month when the concentrations are even higher than those selected for the analysis.
Some statistics to contrast the measured and calculated concentrations should be introduced. If the correlation is made with the Pearson correlation coefficient, the authors should consider that a good value of this estimator could not indicate a good agreement between measured and calculated values. A better statistic for this calculation could be the index of agreement.
Minor remarks.
The names of mountain ranges and sea should be introduced in Fig. 1a (indicated in the text, l. 51), not in Fig. 1b.
Citation: https://doi.org/10.5194/egusphere-2022-780-RC1 -
AC2: 'Reply on RC1', Yue Peng, 09 Mar 2023
The comment was uploaded in the form of a supplement: https://egusphere.copernicus.org/preprints/2022/egusphere-2022-780/egusphere-2022-780-AC2-supplement.pdf
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AC2: 'Reply on RC1', Yue Peng, 09 Mar 2023
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RC2: 'Comment on egusphere-2022-780', Anonymous Referee #2, 03 Jan 2023
General comments:
The authors of the manuscript entitled: “Superimposed effects of typical local circulations driven by mountainous topography and aerosol-radiation interaction on heavy haze in the Beijing-Tianjin-Hebei central and southern plains in winter”, try to investigate the link between aerosol, local vertical circulation, and heavy haze pollution in the Beijing-Tianjin-Hebei plain in winter, by implementing the atmospheric chemistry model GRAPES_Meso5.1/CUACE in January 2017. In my opinion this is an interesting manuscript suitable for Atmospheric Chemistry and Physics journal, however some important issues need to be addressed before it can be further considered for possible publication.
Specific comments:
Lines 20-21: This phrase is not clear. Please revise.
Line 33: Please define PM2.5 based on their diameter.
Line 43: The expression “high concentration aerosols” is not clear. Please revise
Line 89: Why was this time period selected? This must be explained.
Figure 1: The abbreviation OBS is not defined in the legend. Please revise.
Line 127: Please define the type of these correlation coefficients.
Lines 128-129: The difference of the correlation coefficients (0.03) between the two numerical scenarios (CTL and EXP) is really low to support this statement. Please revise.
Lines 131-134: The justification for the selection of the three studied pollution periods (January 5–7, 16–18, and 23–26) is not adequate. Other extreme pollution periods are also indicated in Figure 2. In addition, the selection of January 6, 17, and 24 as the representatives of the three pollution periods is also not adequately justified. This is an important issue because biased results can be implied. Please include more convincing explanations. Moreover, in my opinion the authors should expand the implementation of their method in other time periods besides January 2017 to enhance their manuscript.
Figure 4: The quality of these images is very low and has to be improved. In addition, some elements are not defined the legend. More specifically: a) which images correspond at 500 hPa and which at 700 hPa? b) the red square indicates the BTH region?
Figure 5: A red square is also needed here to indicate the BTH region. Please add it.
Lines 231-232: This sentence is incomplete
Lines 238-242: This section is not clear especially for January 24. Please revise.
Line 248: The enhancement of northerly winds in the lower level on January 24 is not clear in Figure 9c. Please revise.
Line 253: A reference to Figure 10 (b, e) would be useful here
Figure 9: (g–i) is missing from the legend. Please include it.
Citation: https://doi.org/10.5194/egusphere-2022-780-RC2 -
AC1: 'Reply on RC2', Yue Peng, 09 Mar 2023
The comment was uploaded in the form of a supplement: https://egusphere.copernicus.org/preprints/2022/egusphere-2022-780/egusphere-2022-780-AC1-supplement.pdf
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AC1: 'Reply on RC2', Yue Peng, 09 Mar 2023
Interactive discussion
Status: closed
-
RC1: 'Comment on egusphere-2022-780', I. Pérez, 03 Jan 2023
The current paper is focused on the air pollution by PM2.5 at the Beijing-Tianjin-Hebei region in China. The subject merits to be investigated due to the noticeable impact on the affected population. The period investigated is around January 2017, although only three days are selected. Measurements are considered together with modelling analysis. Observations are provided by the National Environmental Monitoring Center, 149 stations, and the Hebei Meteorological service, 210 stations. Moreover, two kind of modelling calculations are used, one of them with the aerosol-radiation interaction, and the second calculation without this interaction. The synoptic pattern is presented at varied pressure surfaces, and vertical cross-sections with the airflow and concentration are also shown. Although the subject and procedure are suitable for a publication, some restrictions of this research indicate that this paper could be accepted in a journal with low impact, but not in Atmospheric Chemistry and Physics.
The main inconvenience lies on the extremely low number of situations where the study is made, only three days, 6th, 17th, and 24th. Although the analysis is detailed, the readers should know if these days are representative enough for the pollution days at this site. Moreover, the readers should know if these conditions could be reproduced at different sites.
Since the pollution levels are affected by factors such as the emissions and the meteorological variables, some information about the patterns of both factors could be useful to focus the pollution problem at the site.
Figure 2 presents the concentration evolution. The authors should comment the reason to discard the first days of the month when the concentrations are even higher than those selected for the analysis.
Some statistics to contrast the measured and calculated concentrations should be introduced. If the correlation is made with the Pearson correlation coefficient, the authors should consider that a good value of this estimator could not indicate a good agreement between measured and calculated values. A better statistic for this calculation could be the index of agreement.
Minor remarks.
The names of mountain ranges and sea should be introduced in Fig. 1a (indicated in the text, l. 51), not in Fig. 1b.
Citation: https://doi.org/10.5194/egusphere-2022-780-RC1 -
AC2: 'Reply on RC1', Yue Peng, 09 Mar 2023
The comment was uploaded in the form of a supplement: https://egusphere.copernicus.org/preprints/2022/egusphere-2022-780/egusphere-2022-780-AC2-supplement.pdf
-
AC2: 'Reply on RC1', Yue Peng, 09 Mar 2023
-
RC2: 'Comment on egusphere-2022-780', Anonymous Referee #2, 03 Jan 2023
General comments:
The authors of the manuscript entitled: “Superimposed effects of typical local circulations driven by mountainous topography and aerosol-radiation interaction on heavy haze in the Beijing-Tianjin-Hebei central and southern plains in winter”, try to investigate the link between aerosol, local vertical circulation, and heavy haze pollution in the Beijing-Tianjin-Hebei plain in winter, by implementing the atmospheric chemistry model GRAPES_Meso5.1/CUACE in January 2017. In my opinion this is an interesting manuscript suitable for Atmospheric Chemistry and Physics journal, however some important issues need to be addressed before it can be further considered for possible publication.
Specific comments:
Lines 20-21: This phrase is not clear. Please revise.
Line 33: Please define PM2.5 based on their diameter.
Line 43: The expression “high concentration aerosols” is not clear. Please revise
Line 89: Why was this time period selected? This must be explained.
Figure 1: The abbreviation OBS is not defined in the legend. Please revise.
Line 127: Please define the type of these correlation coefficients.
Lines 128-129: The difference of the correlation coefficients (0.03) between the two numerical scenarios (CTL and EXP) is really low to support this statement. Please revise.
Lines 131-134: The justification for the selection of the three studied pollution periods (January 5–7, 16–18, and 23–26) is not adequate. Other extreme pollution periods are also indicated in Figure 2. In addition, the selection of January 6, 17, and 24 as the representatives of the three pollution periods is also not adequately justified. This is an important issue because biased results can be implied. Please include more convincing explanations. Moreover, in my opinion the authors should expand the implementation of their method in other time periods besides January 2017 to enhance their manuscript.
Figure 4: The quality of these images is very low and has to be improved. In addition, some elements are not defined the legend. More specifically: a) which images correspond at 500 hPa and which at 700 hPa? b) the red square indicates the BTH region?
Figure 5: A red square is also needed here to indicate the BTH region. Please add it.
Lines 231-232: This sentence is incomplete
Lines 238-242: This section is not clear especially for January 24. Please revise.
Line 248: The enhancement of northerly winds in the lower level on January 24 is not clear in Figure 9c. Please revise.
Line 253: A reference to Figure 10 (b, e) would be useful here
Figure 9: (g–i) is missing from the legend. Please include it.
Citation: https://doi.org/10.5194/egusphere-2022-780-RC2 -
AC1: 'Reply on RC2', Yue Peng, 09 Mar 2023
The comment was uploaded in the form of a supplement: https://egusphere.copernicus.org/preprints/2022/egusphere-2022-780/egusphere-2022-780-AC1-supplement.pdf
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AC1: 'Reply on RC2', Yue Peng, 09 Mar 2023
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Yue Peng
Xiaoye Zhang
Zhaodong Liu
Wenjie Zhang
Siting Li
Chen Han
Huizheng Che
The requested preprint has a corresponding peer-reviewed final revised paper. You are encouraged to refer to the final revised version.
- Preprint
(2838 KB) - Metadata XML