Yimin Huang1, Liuyi Zhang1,2, Yang Qiu3, Yang Chen2, Guangming Shi This email address is being protected from spambots. You need JavaScript enabled to view it.3, Tingzhen Li1, Lei Zhang1, Fumo Yang This email address is being protected from spambots. You need JavaScript enabled to view it.1,2,3

Key Laboratory of Water Environment Evolution and Pollution Control in Three Gorges Reservoir, Chongqing Three Gorges University, Chongqing 404100, China
Chongqing Institute of Green and Intelligent Technology, Chinese Academy of Sciences, Chongqing 400714, China
National Engineering Research Center for Flue Gas Desulfurization, Department of Environmental Science and Engineering, Sichuan University, Chengdu 610065, China


Received: January 2, 2020
Revised: April 25, 2020
Accepted: April 25, 2020

 Copyright The Author(s). This is an open access article distributed under the terms of the Creative Commons Attribution License (CC BY 4.0), which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are cited.

Download Citation: ||https://doi.org/10.4209/aaqr.2019.10.0516  

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Huang, Y., Zhang, L., Qiu, Y., Chen, Y., Shi, G., Li, T., Zhang, L. and Yang, F. (2020). Five-year Record of Black Carbon Concentrations in Urban Wanzhou, Sichuan Basin, China. Aerosol Air Qual. Res. 20: 1282–1293. https://doi.org/10.4209/aaqr.2019.10.0516


  • Temporal distribution of BC showed a distinct declining trend.
  • BC contamination in Wanzhou is still serious when compared to other urban areas.
  • The morning peak of BC concentration appeared later in winter than in other seasons.
  • BC concentration in Wanzhou is affected by traffic, industry and biomass combustion.


The atmospheric fine particle black carbon (BC) was measured from June 2013 till February 2018 in Wanzhou District, the second largest metropolitan area in Chongqing Municipality, China, which is located in the eastern Sichuan Basin. The average daily concentration ranged from 0.5 to 10.4 µg m–3, with a mean of 4.4 ± 2.2 µg m3, and the annual mean displayed a significantly decreasing trend, from 5.3 µg m3 in 2013 to 3.7 µg m3 in 2017. The frequency distribution of the average daily concentrations during the years 2014–2017 skewed toward lower values (compared to the rest of the study period), with over 60% falling between 1 and 5 µg m3. The BC exhibited a seasonal pattern, with the highest concentrations being reported during winter, followed by spring and fall, and the lowest ones during summer, as well as a double-peaked diel variability all year round, with a morning peak occurring between 07:00 and 09:00 and an evening peak between 19:00 and 21:00. Furthermore, the concentration was negatively correlated with the planetary boundary layer (PBL) height and influenced by the strong scavenging effect of precipitation. An inverse relationship between the concentration and the wind speed was observed when the latter was below 2.0 m s–1. The wind direction also affected the concentration, with easterly and southeasterly winds accompanying higher levels of BC regardless of the season.

Keywords: Black carbon; Seasonal variation; Diel variation; Meteorological parameters.


Black carbon (BC), primarily originating from incomplete combustion of fossil fuel and biomass burning, is one of the important components in atmospheric aerosol, and has strong absorption of light (Jacobson, 2001; Ramanathan and Carmichael, 2008; Chow et al., 2009; Tian et al., 2018). In recent years, BC has attracted extensive attention because of its important effects on climate (Jacobson, 2002; Chung and Seinfeld, 2005; Schmidt, 2011), environment (Ramachandran and Rajesh, 2007; Huang et al., 2012) and human health (Kopp and Mauzerall, 2010; Janssen et al., 2011; Farzad et al., 2020). According to researches on global climate change, absorption of BC accounts for 80–90% of aerosols’ contribution to global warming (Chung and Seinfeld, 2005; Kopp and Mauzerall, 2010; Rai et al., 2019). BC aerosol is considered to be the  second largest contributor to anthropogenic radiative forcing after CO2 (Jacobson, 2002; Panicker et al., 2013). In addition to enhancing the absorption of solar radiation, BC in clouds and aerosols also accelerates cloud evaporation rate, thus changing the duration of cloud existence (Quaas, 2011; Dalirian et al., 2018). BC can heat the air to alter the stability and vertical movement of the regional atmosphere, thus having an important impact on large-scale air circulation and water circulation with implication on crop yield reduction (Chameides et al., 1999; Menon et al., 2002; Richardson et al., 2018). BC is mainly present in fine particles in the urban environment, and can be inhaled into the human body and cause adverse health effects on the respiratory system (Sahu et al., 2011; Wang et al., 2011; Jung et al., 2017).

Research on BC has particular importance in China because the country has been regarded as the largest emitter of BC in the world (Novakov et al., 2003; Bond et al., 2007; Ramanathan and Carmichael, 2008; Zhou et al., 2018). BC emissions in China roughly accounted for one fourth of the global anthropogenic sources (Street et al., 2001). Numerous studies on BC have been conducted in Chinese megacities, such as Beijing (Chen et al., 2016; Ji et al., 2016; Wang et al., 2016; Ji et al., 2017, 2019b; Liu et al., 2019), Shanghai (Feng et al., 2014; Peng et al., 2019), Guangzhou (Chen et al., 2014; Sun et al., 2020), Nanjing (Zhuang et al., 2014; Xiao et al., 2016), Xi’an (Cao et al., 2009; Wang et al., 2015a; Zhang et al., 2015; Zhang et al., 2018). Collectively, these studies produced valuable data on the distribution of BC in China, and also provided results on BC’s optical property and radiative forcing. However, measurements from aforementioned studies were mostly short-term, and BC data of southwest China remains scarce.

Chongqing Municipality of southwestern China is known for its position at the hinterland of the Three Gorges Reservoir (TGR) on the Yangtze River. Wanzhou, situated in the eastern margin of the Sichuan Basin, is a district located 230 km away from downtown Chongqing. Wanzhou covers an area of 3457 km2 and has a registered population of approximately 1.8 million at the end of 2017 (Introduction to Wanzhou, http://www.wz.gov.cn/zjwz/wzjj/202003/t202
). In recent years, the acceleration of urbanization and energy consumption growth in Wanzhou together increased the amount of air pollutant emission, threatening local air quality. In 2013, Chinese government issued Air Pollution Prevention and Control Action Plan (2013–2017) with aggressive measures starting in October 2013. Since then, Chongqing Municipal Government has adopted a series of corresponding measures to improve the city’s air quality. Studying BC, a product of fossil fuel combustion and biomass burning, can shed light on the effectiveness of these emission control measures. However, to date no publicized data is available for BC aerosol in Wanzhou. In this study, we conducted continuous measurement of BC at an urban site in Wanzhou from June 1, 2013, to February 28, 2018. The purposes of this study are: 1) to evaluate the temporal variability of BC in Wanzhou, 2) to explore the correlation between BC and meteorological factors, and 3) to investigate the possible emission sources of BC.


Site Description

BC mass concentration was measured on the rooftop of the Experimental Building (30.79°N, 108.37°E) on Chongqing Three Georges University campus, at a height about 27 m above the ground (Fig. 1). Surrounding the site are residences, restaurants, and shops. At about 150 m east of the measurement site lies a major road, Shalong Road. There is no major stationary pollution source within 1 km around the sampling site. This site represents a mixed residential, traffic, and commercial environments of urban area in Wanzhou.

Fig. 1. Location of the sampling site in Wanzhou.Fig. 1. Location of the sampling site in Wanzhou.

Black Carbon Measurement

BC concentration was monitored using a Thermo Carusso Model 5012 Multi-Angle Absorption Photometer (MAAP). The MAAP was equipped with an additional impactor system removing particles with aerodynamic diameter larger than 2.5 µm. The sampling flow of the instrument was maintained at 16.7 L min–1 at ambient temperature and pressure. Briefly, the instrument collected aerosol particles on a glass-fiber tape and measured light attenuation caused by the sampled particles. More detailed information about the BC analysis protocol is provided in the study of Kanaya et al. (2013). The time of day (hour) referred to throughout this paper is the starting time of each hourly measurement at local time. The study period was June 1, 2013, to February 28, 2018. Yearly sampling campaigns were conducted during the following periods: June 2013 to February 28, 2014; March 1, 2014, to February 28, 2015; March 1, 2015, to February 29, 2016; March 1, 2016, to February 28, 2017; and March 1, 2017, to February 28, 2018. 

Meteorological Data

Meteorological parameters (wind speed and direction) were collected simultaneously with BC monitoring using a miniature weather instrument (WS500-UMB; Lufft Corp., Germany). No direct measurement was available for planetary boundary layer (PBL) heights and precipitation during the period of BC measurement; we used the closest grid value of the reanalysis PBL height and precipitation to the Wanzhou as the real PBL height and precipitation. The PBL heights and precipitation during the study period were calculated by the U.S. National Oceanic and Atmospheric Administration (NOAA) READY archived meteorological data (http://www.arl.noaa.gov/ready/hysplit4.html). The program used the archived dataset GDAS (1°, 3-h, global) based on the average value of Coordinated Universal Time (UTC), and the time series of calculated daily PBL heights were obtained. All UTC values were converted to local time.


BC Concentration and Variability

Daily average BC concentration from June 1, 2013, to February 28, 2018, in Wanzhou ranged from 0.5 to 10.4 µg m–3, with a mean level of 4.4 ± 2.2 µg m–3, implying a dramatic day-to-day variation (Fig. 2). The annual average concentration of BC is shown in Table 1. There was a decreasing trend of the annual mean BC concentration, which dropped from 5.3 µg m–3 in 2013 to 3.7 µg m–3 in 2017 (30% reduction). Overall, at the 95% confidence level, the annual mean BC decreased by 0.33 µg m–3 year–1 from 2013 to 2017. The decline in BC concentrations is closely associated with various policy interventions taken at Chongqing. As part of mitigation implementation to control traffic pollution, Chongqing eliminated 0.26 million yellow-label cars and outdated vehicles between 2013 and 2017, while adopting Chinese national Stage V standard for diesel and gasoline vehicles and eliminating the sale and use of substandard oil. Additionally, the government had designated prohibited areas (nearly 4000 m2) for high emission non-road mobile machinery (NRMM) and strengthened the supervision of NRMM usage in these areas. The total energy consumption in Chongqing accounted for 72.5 and 84.5 million tons of standard coal equivalent (SCE) in 2013 and 2017, respectively. However, the proportion of coal consumption in total energy consumption dropped from 63.2% in 2013 to 53.8% in 2017. Coal has been gradually replaced by natural gas and other cleaner energy in Chongqing (Chongqing environment statement in 2017, http://sthjj.cq.gov.cn/hjzl_249/hjzkgb/201912/P020191228643991023980.pdf). At the same time, Chongqing had closed some heavily polluting industries, had renovated coal-fired boilers with clean energy, and had promoted the ultra-low emission transformation of coal-fired power plants. Additional mitigation measures were applied for curbing domestic pollution. For example, it had reformed the lampblack emission from catering business and canteens of government and public institutions, and had intensified law enforcement on illegal activities such as burning straw, garbage, and barbecuing in the open air. It could be inferred that BC concentration reduction over the past few years in Wanzhou might be related to the implementation of these governmental mitigation measures. 

Fig. 2. Temporal variation of daily BC concentration (black line) from June 1, 2013, to February 28, 2018. The red dash line implies the linear regression trend of BC concentration.Fig. 2. Temporal variation of daily BC concentration (black line) from June 1, 2013, to February 28, 2018. The red dash line implies the linear regression trend of BC concentration. 

Fig. 3 shows the frequency distributions of daily BC concentrations between 2014 and 2017. BC concentration mostly occurred between 1 and 5 µg m3, accounting for 60% in 2014, 71% in 2015, 72% in 2016, and 73% in 2017. The maximum frequencies occurred at 4–5 µg m3, 3–4 µg m3, 2–3 µg m3, and 1–2 µg m3 between 2014 and 2017. These frequencies accounted for 20% of total BC concentrations in 2014, 26% in 2015, 24% in 2016, and 27% in 2017. The frequency of BC concentrations between 6 and 10 µg m3 decreased from 25% in 2014 to 14% in 2017. This suggests that daily BC distributions skewed towards lower concentrations from 2014 to 2017. 

Fig. 3. Frequency distributions of daily BC concentrations from 2014 to 2017.Fig. 3. Frequency distributions of daily BC concentrations from 2014 to 2017.

The mean BC concentration in Wanzhou was lower than that of downtown Chongqing and other major cities in China, e.g., Xi’an, Shijiazhuang, Chengdu, Guizhou, and Handan (Table 1). However, the BC concentration reported by this study was higher than the urban site of another district of Chongqing Municipality named Fuling (29.75°N, 107.27°E), which is about 157 km southwest of Wanzhou and comparable to Wanzhou with regard to traffic, population and economy. Moreover, BC concentration measured in this study was comparable with urban sites of Beijing and Nanjing. In comparison to global background site (Waliguan), BC pollution in Wanzhou was worse. Overall, BC concentration in Wanzhou was moderate compared to major cities in China; however, taking in consideration of Wanzhou’s city size, population, and economy, its BC contamination was concerning.

Seasonal Variations of BC Concentrations

Monthly and seasonal trends of BC during 2013–2017 were evident (Figs. 4 and 5). The lowest monthly average BC concentrations occurred in July or August, while the highest concentrations occurred in December or January. Monthly BC concentration varied by nearly fourfold, from a minimum of 2.3 ± 0.5 µg m3 (August 2017) to the maximum of 8.9 ± 1.6 µg m3 (January 2014). As shown in Fig. 4, a decreasing trend for BC was clear in all months; October and January are the main months that contributed to the decrease in annual average BC concentration. The decreasing trends in October and January are significant at the 95% confidence level. The peaks decreased at approximately 0.89 and 0.97 µg m3 year1 in October and January, respectively. Seasonal BC concentration was highest in winter, followed by fall and spring, with summer showing the lowest concentration. Similar seasonal variation of BC concentrations can be found in other Chinese sites (Chen et al., 2014; Feng et al., 2014; Ji et al., 2016; Chen et al., 2019). 

Fig. 4. Monthly average BC concentrations and BC concentration trend (blue curves) from 2013 to 2017.Fig. 4. Monthly average BC concentrations and BC concentration trend (blue curves) from 2013 to 2017. 

Fig. 5. Seasonal variation of BC average mass concentrations (in µg m–3) in Wanzhou from 2013–2018. The whiskers represent the standard deviation. Seasons are defined as: spring: March–May; summer: June–August; fall: September–November; winter: December–February.Fig. 5. Seasonal variation of BC average mass concentrations (in µg m3) in Wanzhou from 2013–2018. The whiskers represent the standard deviation. Seasons are defined as: spring: March–May; summer: June–August; fall: September–November; winter: December–February. 

Fig. 6. Hourly average BC changes throughout the day for each season, with seasons defined in Fig. 5.Fig. 6. Hourly average BC changes throughout the day for each season, with seasons defined in Fig. 5.

The seasonality of BC concentrations is mainly affected by meteorological factors and anthropogenic activities. Precipitation was usually abundant during summer (Fig. 7) and is an important mechanism that scavenges air pollutants, resulting in the lowest BC concentrations occurring in summer. At the same time, the PBL height was higher in summer which facilitated the dispersal of BC. Additionally, anthropogenic BC emission from fossil fuel over China was lower in summer while higher in winter (Zhuang et al., 2014; Zhang et al., 2009), also contributing to low BC concentrations in summer. High BC concentrations in fall might be due to the increased biomass burning such as burning of leftover crop residues (Huang et al., 2018). For spring, diffusion conditions were limited compared to those in summer, and could thus result in higher BC concentration than summer.

Diel Variations of BC Concentrations

The average diel BC mass concentrations measured in four seasons are shown in Fig. 6. In all seasons, a bimodal distribution of BC concentration was marked with a morning peak at 07:00–09:00 and an evening peak at 19:00–21:00. Meanwhile, the lowest BC concentration occurred between 14:00–15:00 for all seasons. This diel profile for BC is similar to those observed at different locations (Sahu et al., 2011; Chen et al., 2014; Feng et al., 2014). The morning peak results from morning rush hour traffic, suggesting an important role of vehicle emissions. In addition, atmospheric inversion in the morning can also lead to the high BC concentration. After sunrise, the increase in solar radiation promotes the development of daytime mixing layer, which facilitates the dispersion and dilution of pollutants, subsequently lowering BC concentration from morning hours. The BC evening peak could be attributed to afternoon traffic emissions and cooking, combined with low mixing heights. After midnight, due to the reduction of human activities and vehicle emissions, BC concentration decreased slightly, but remained at high levels. The BC concentrations at nighttime (00:00–06:00) maintained at 2.9–3.4 µg m3 in summer, 3.7–4.3 µg m3 in spring and fall, 5.5–6.2 µg m3 in winter, respectively. This may be attributed to the formation of a nocturnal boundary layer and stagnant air flow which favor the accumulation of pollutants.

The specific timing of BC’s diel variability was distinct among the seasons. The morning peak of BC concentration in winter appeared at 09:00, which was 1–2 hours later than other seasons. It could be associated with the inversion layer and the human activity regularity. During winter morning, the inversion phenomenon occurs more frequently and longer in mountain area (Wang et al., 2015b), which inhibits vertical diffusion and facilitates the accumulation of BC. Meanwhile, human activities were later than other seasons, leading to a delay in BC emission. In addition, the highest ratio between maximum and minimum of diel BC concentrations was found in summer (1.9), and the lowest in winter (1.3), reflecting the different diel variation of meteorological conditions in different seasons.

Relationships to Meteorological Conditions

PBL height, precipitation and wind speed are three important meteorological parameters affecting BC concentration. Monthly average BC mass concentration together with meteorological parameters in Wanzhou are plotted in Fig. 7. The PBL height determines the volume through which surface-emitted pollutants can be diluted and reflects boundary layer turbulence (Stull, 1988). It presented a strong seasonal variation in Wanzhou. The highest seasonal PBL height was observed in summer (465 m), which was 1.6 times higher than those measured in fall (289 m) and winter (297 m). A significant negative correlation coefficient (r = –0.58) was found between BC concentration and PBL height, as shown in Fig. 7(a). As mentioned in Section 3.2, the average BC concentrations were higher in winter (6.0 µg m3) than in fall (4.3 µg m3). However, the PBL height was almost the same in winter and fall. This result implies that PBL height was not the main reason for the higher BC concentration in winter.

Precipitation is an important mechanism of washing out particles as well as BC. As shown in Fig. 7(b), most of the precipitation occurred between June and October in Wanzhou, accounting for 59–66% of the annual precipitation (1198 mm). There was a significant negative correlation (r = –0.74) between precipitation and BC concentration. However, a poor correlation between BC and rainfall was found at Xi’an (r = –0.35), in northwestern China (Cao et al., 2009) and at Beijing (r = –0.27) in northern China (Chen et al., 2016). This distinct feature may be due to the more frequent precipitation in southwest of China compared to the northwest (Dai et al., 2014).

Among the meteorological parameters, wind speed is an important factor determining BC concentration (Chen et al., 2014; Park et al., 2015). Fig. 7(c) shows the monthly wind speed from 2013 to 2017. The wind speed is relatively low, with monthly averaged values generally ranged from 0.7 to 1.1 m s1. BC was observed to be negatively correlated with the wind speed (r = –0.64). This result is similar to the findings of many previous studies (Bhat et al., 2017; Kucbel et al., 2017). 

Fig. 7. Monthly average (a) planetary boundary layer (PBL) height, (b) rainfall, (c) wind speed, and (d) BC concentration in Wanzhou.Fig. 7. Monthly average (a) planetary boundary layer (PBL) height, (b) rainfall, (c) wind speed, and (d) BC concentration in Wanzhou.

The hourly wind speeds and corresponding BC concentrations are plotted in Fig. 8. The calm conditions (wind speeds < 0.5 m s1) occurred frequently in Wanzhou, accounting for 22% of the entire measurement period, during which the highest average BC concentration (5.5 µg m3) appeared. Wind speed between 0.5 and 1 m s1 was dominant (51%), and the corresponding average BC concentration was 4.4 µg m3. When wind speed reached 1.5–2.0 m s1, the average BC concentration dropped to 3.0 µg m3 (45% reduction). A clear inverse relationship between BC concentration and wind speed was found for wind speed lower than 2.0 m s1. However, when the wind speed was higher than 2.0 m s1, no clear relation between wind speed and BC concentrations could be seen. Similar relationship between BC and wind speed have also been reported for other urban locations globally, such as Helsinki, Finland (Pakkanen et al., 2000), and Urumqi, China (Li et al., 2012).

Fig. 8. BC concentration intervals grouped by wind speed. Box-and-whisker plot indicates median and 25% quartile (box), mean (square), 10/90% (whiskers).Fig. 8. BC concentration intervals grouped by wind speed. Box-and-whisker plot indicates median and 25% quartile (box), mean (square), 10/90% (whiskers).

The contribution of hourly BC from different wind directions is illustrated by wind rose plots in Fig. 9. The prevailing winds in Wanzhou were mainly from eastern and southeastern directions in different seasons. The main road, Shalong Road, is located to the east of the sampling site, so it can be speculated that the higher BC concentration from this direction may be affected by traffic emissions. Since the local industrial area lies in southeastern Wanzhou, relatively high BC concentration from this direction was likely due to the influence from industrial emissions. In addition, it is noteworthy that frequencies of wind directions between 180° to 270° increased in fall and winter, and BC concentration observed by these directions was considerably high. Patches of farmlands lie to the west of the sampling site; higher BC concentration from these directions could be attributed to the burning of crop residues on these farmlands. 

Fig. 9. Hourly BC concentrations with wind direction during four seasons. The scales display the percentage frequencies of wind directions. The legends display BC concentrations (µg m–3).Fig. 9. Hourly BC concentrations with wind direction during four seasons. The scales display the percentage frequencies of wind directions. The legends display BC concentrations (µg m3).

The conditional probability function (CPF) was used to identify the likely locations of local emission sources affecting concentrations of BC in sampling site. BC data obtained at wind speeds < 1.0 m s1 were excluded in the CPF analysis due to the isotropic behavior of wind vane under low wind speeds. Fig. 10 shows the CPF concentration plots of BC when the threshold was set at the upper 25th percentile of the concentrations. The emission sources are likely located in the directions that have high conditional probability values. There was a clear indication of higher probability for these concentrations from the southeast, i.e., in the direction of industrial emissions. Additionally, there was high probability to the west, corresponding to the direction where some farmlands lie. Combining Fig. 10 with Fig. 9 produces an interesting feature: The highest concentration occurred under very low wind speed conditions from all wind directions, particularly the east, corresponding to the direction where the main road lies. Thus, it is suggestive that BC concentration was mainly affected by traffic emissions at low wind speed (< 1.0 m s1), while BC concentration was affected by transport from industrial emissions and biomass burning at high wind speed (> 1.0 m s1). 

Fig. 10. CPF plots for BC at 75% percentile in different seasons.Fig. 10. CPF plots for BC at 75% percentile in different seasons.


In this study, BC was measured in Wanzhou metropolitan area from June 2013 till February 2018 in order to investigate its temporal variability and potential sources. The average daily concentration ranged from 0.5 to 10.4 µg m3, with a mean of 4.4 ± 2.2 µg m3, and the average annual concentration exhibited a declining trend, decreasing from 5.3 µg m3 in 2013 to 3.7 µg m3 in 2017. Although these values qualify as moderate in China, BC contamination is nevertheless an issue when considering the size, population, and economy of Wanzhou. The seasonality of the BC—specifically, the occurrence of the minimum and maximum concentrations during summer and winter, respectively—can be attributed to changes in the emission sources and variability in the ambient meteorological conditions, especially the low precipitation and shallow PBL height during winter. The concentrations peaked during the morning between 07:00 and 09:00 and again during the evening between 19:00 and 21:00, likely as a result of anthropogenic activities, including traffic, and dropped to their lowest daily values between 14:00 and 15:00, which can be ascribed to the development of the PBL.

The BC concentration was found to be negatively correlated with the PBL height (r = –0.58), rainfall (r = –0.74), and wind speed (r = –0.64). Furthermore, winds blowing from the east and southeast, the most frequent directions, were accompanied by higher concentrations during all of the seasons, and CPF analysis indicated a high probability of sources to the southeast, where industry is located, and to the west, where farmlands lie. Thus, at low wind speeds (< 1.0 m s1), traffic emissions may have been the primary factor influencing the BC concentration, whereas at high wind speeds (> 1.0 m s1), industrial emissions and biomass burning potentially played the largest roles.


This research was funded by the National Natural Science Foundation of China (41375123), Fundamental Research Funds for the Central Universities (YJ201891), Science and Technology Commission of Chongqing Project (Grant No. cstc2018jcyjAX0236), Scientific and Technological Research Program of Chongqing Municipal Education Commission, and Chongqing Three Gorges University project (Grant No. 19QN03).


  1. Bhat, M.A., Romshoo, S.A. and Beig, G. (2017). Aerosol black carbon at an urban site-Srinagar, Northwestern Himalaya, India: Seasonality, sources, meteorology and radiative forcing. Atmos. Environ. 165: 336–348. [Publisher Site]

  2. Bond, T.C., Bhardwaj, E., Dong, R., Jogani, R., Jung, S.K., Roden, C., Streets, D.G. and Trautmann, N.M. (2007). Historical emissions of black and organic carbon aerosol from energy-related combustion, 1850–2000. Global Biogeochem. Cycles 21: GB2018. [Publisher Site]

  3. Cao, J.J., Zhu, C.S., Chow, J.C., Watson, J.G., Han, Y.M., Wang, G.H., Shen, Z.X. and An, Z.S. (2009). Black carbon relationships with emissions and meteorology in Xi'an, China. Atmos. Environ. 94: 194–202. [Publisher Site]

  4. Chameides, W.L., Yu, H., Liu, S.C., Bergin, M., Zhou, X., Mearns, L., Wang, G., Kiang, C.S., Saylor, R.D., Luo, C., Huang, Y., Steiner, A. and Giorgi, F. (1999). Case study of the effects of atmospheric aerosols and regional haze onagriculture: an opportunity to enhance crop yields in China through emission controls? Proc. Natl. Acad. Sci. U.S.A. 96: 13626–13633. [Publisher Site]

  5. Chen, W., Tian, H. and Qin, K. (2019). Black carbon aerosol in the industrial city of Xuzhou, China: Temporal characteristics and source appointment. Aerosol Air Qual. Res. 19: 794–811. [Publisher Site]

  6. Chen, X.C., Zhang, Z.S., Engling, G., Zhang, R.J., Tao, J., Lin, M., Sang, X.F., Chan, C.Y., Li, S.Y. and Li, Y.P. (2014). Characterization of fine particulate black carbon in Guangzhou, a megacity of south China. Atmos. Pollut. Res. 5: 361–370. [Publisher Site]

  7. Chen, Y., Schleicher, N., Fricker, M., Cen, K., Liu, X.L., Kaminski, U., Yang, Y., Xue, F.W. and Norra, S. (2016). Long-term variation of black carbon and PM2.5 in Beijing, China with respect to meteorological conditions and governmental measures. Environ. Pollut. 212: 269–278. [Publisher Site]

  8. Chow, J.C., Watson, J.G., Doraiswamy, P., Chen, L.W.A., Sodeman, D.A., Lowenthal, D.H., Park, K., Arnott, W.P. and Motallebi, N. (2009). Aerosol light absorption, black carbon, and elemental carbon at the Fresno Supersite, California. Atmos. Res. 93: 874–887. [Publisher Site]

  9. Chung, S.H. and Seinfeld, J.H. (2005). Climate response of direct radiative forcing of anthropogenic black carbon. J. Geophys. Res. 110: D11102. [Publisher Site]

  10. Dai, Z.Y., Jiang, J. and Xiao, M.K. (2014). Autocorrelation analysis on China’s rainfall based on the improved spatio-temporal Moran’s I. J. Huazhong Normal Univ. 48: 924–929.

  11. Dalirian, M., Ylisirniö, A., Buchholz, A., Schlesinger, D., Ström, J., Virtanen, A. and Riipinen, I. (2017). Cloud droplet activation of black carbon particles coated with organic compounds of varying solubility. Atmos. Chem. Phys. 18: 12477–12489. [Publisher Site]

  12. arzad, K., Khorsandi, B., Khorsandi, M., Bouamra, O. and Maknoon, R. (2020). A study of cardiorespiratory related mortality as a result of exposure to black carbon. Sci. Total Environ. 725: 138422. [Publisher Site]

  13. Feng, J., Zhong, M., Xu, B., Du, Y., Wu, M., Wang, H. and Chen, C. (2014). Concentrations, seasonal and diurnal variations of black carbon in PM2.5 in Shanghai, China. Atmos. Res. 147–148: 1–9. [Publisher Site]

  14. Huang, X.F., Sun, T.L., Zeng, L.W., Yu, G.H. and Luan, S.J. (2012). Black carbon aerosol characterization in a coastal city in South China using a single particle soot photometer. Atmos. Environ. 51: 21–28. [Publisher Site]

  15. Huang, Y.M., Liu, Y., Zhang, L.Y., Peng, C. and Yang, F.M. (2018). Characteristics of carbonaceous aerosol in PM2.5 at Wanzhou in the southwest of China. Atmoshpere 9: 37. [Publisher Site]

  16. Jacobson, M.Z. (2001). Strong radiative heating due to mixing state of black carbon in atmospheric aerosol. Nature. 409: 695–697. [Publisher Site]

  17. Jacobson, M.Z. (2002). Control of fossil-fuel particulate black carbon and organic matter, possibly the most effective method of slowing global warming. J. Geophys. Res. 107. [Publisher Site]

  18. Janssen, N.A.H., Hoek, G., Simic-Lawson, M., Fischer, P., Bree, L.V., Brink, H.T., Keuken, M., Atikinson, R.W., Anderson, H.R., Brunekreef, B. and Flemming, R. (2011). Black carbon as an additional indicator of the adverse health effects of airborne particles compared with PM10 and PM2.5. Environ. Health Perspect. 119: 1691–1699. [Publisher Site]

  19. Ji, D., Zhang, J., He, J., Wang, X., Pang, B., Liu, Z., Wang, L. and Wang, Y. (2016). Characteristics of atmospheric organic and elemental carbon aerosols in urban Beijing, China. Atmos. Environ. 125: 293–306. [Publisher Site]

  20. Ji, D., Li, L., Pang, B., Xue, P., Wang, L., Wu, Y., Zhang, H. and Wang, Y. (2017). Characterization of black carbon in an urban-rural fringe area of Beijing. Environ. Pollut. 223: 524–534. [Publisher Site]

  21. Ji, D., Gao, M., Maenhaut, W., He, J., Wu, C., Cheng, L., Gao, W., Sun, Y., Sun, J., Xin, J., Wang, L. and Wang, Y. (2019a). The carbonaceous aerosol levels still remain a challenge in the Beijing-Tianjin-Hebei region of China: insights from continuous high temporal resolution measurements in multiple cities. Environ. Int. 126: 171–183. [Publisher Site]

  22. Ji, D., Gao, W., Maenhaut, W., He, J., Wang, Z., Li, J., Du, W., Wang, L., Sun, Y., Xin, J., Hu, B. and Wang, Y. (2019b). Impact of air pollution control measures and regional transport on carbonaceous aerosols in fine particulate matter in urban Beijing, China: insights gained from long-term measurement. Atmos. Chem. Phys. 19: 8569–8590. [Publisher Site]

  23. Jung, K.H., Lovinsky-Desir, S., Yan, B., Torrone, D., Lawrence, J., Jezioro, J.R., Perzanowski, M., Perera, F.P., Chillrud, S.N. and Miller, R.L. (2017). Effect of personal exposure to black carbon on changes in allergic asthma gene methylation measured 5 days later in urban children: Importance of allergic sensitization. Clin. Epigenet. 9: 61. [Publisher Site]

  24. Kanaya, Y., Taketani, F., Komazaki, Y., Liu, X., Kondo, Y., Sahu, L.K., Irie, H. and Takashima, H. (2013). Comparison of black carbon mass concentrations observed by Multi-Angle Absorption Photometer (MAAP) and Continuous Soot-Monitoring System (COSMOS) on Fukue Island and in Tokyo, Japan. Aerosol Sci. Technol. 47: 1–10. [Publisher Site]

  25. Kopp, R.E. and Mauzerall, D.L. (2010). Assessing the climatic benefits of black carbon mitigation. Proc. Natl. Acad. Sci. U.S.A. 107: 11703–11708. [Publisher Site]

  26. Kucbel, M., Corsaro, A., Švédová, B., Raclavská, H., Raclavský, K. and Juchelková, D. (2017). Temporal and seasonal variations of black carbon in a highly polluted Europeas city: apportionment of potential sources and the effect of meteorological conditions. J. Environ. Manage. 203: 1178–1189. [Publisher Site]

  27. Li, S., Guo, Z.Z., Hu, L.Q., He, Q. and Xu, Z.D. (2012). Preliminary study on black carbon aerosol pollution over Urumqi in Winter. Arid Zone Res. 29: 728–734. (in Chinese with English Abstract)

  28. Liu, Z.R., Gao, W.K., Yu, Y.C., Hu, B., Xin, J.Y., Sun, Y., Wang, L.L., Wang, G.H., Bi, X.H., Zhang, G.H., Xu, H.H., Cong, Z.Y., He, J., Xu, J.S. and Wang, Y.S. (2018). Characteristics of PM2.5 mass concentrations and chemical species in urban and background areas of China: Emerging results from the CARE-China network. Atmos. Chem. Phys. Discuss. 18: 1–34. [Publisher Site]

  29. Liu, Z.R., Hu, B., Ji, D.S., Cheng, M.T., Gao, W.K., Shi, S.Z., Xie, Y.Z., Yang, S.H., Gao, M., Fu, H.B., Chen, J.M. and Wang, Y.S. (2019). Characteristics of fine particle explosive growth events in Beijing, China: Seasonal variation, chemical evolution pattern and formation mechanism. Sci. Total Environ. 687: 1073–1086. [Publisher Site]

  30. Menon, S., Hansen, J., Nazarenko, L. and Luo, Y.F. (2002). Climate effects of black carbon aerosols in China and India. Science 297: 2250–2253. [Publisher Site]

  31. Novakov, T., Ramanathan, V., Hansen, J.E., Kirchstetter, T.W., Sato, M., Sinton, J.E. and Sathaye, J.A. (2003). Large historical changes of fossil-fuel black carbon aerosols. Geophys. Res. Lett. 30. [Publisher Site]

  32. Pakkanen, T.A., Kerminen, V.M., Ojanen, C.H., Hillamo, R.E., Aarnio, P. and Koskentalo, T. (2000). Atmospheric black carbon in Helsinki. Atmos. Environ. 34: 1497–1506. [Publisher Site]

  33. Panicker, A.S., Park, S.H., Lee, D.I., Kim, D.C., Jung, W.S., Jang, S.M., Jeong, J.H., Kim D.S., Yu, J. and Jeong, H. (2013). Observations of black carbon characteristics and radiative forcing over a global atmosphere watch supersite in Korea. Atmos. Environ. 77: 98–104. [Publisher Site]

  34. Park, S.S. and Lee, K.H. (2015). Characterization and sources of black carbon in PM2.5 at a site close to a roadway in Gwangju, Korea, during winter. Environ. Sci. Processes Impacts 17: 1794–805. [Publisher Site]

  35. Peng, X., Liu, M., Zhang, Y., Meng, Z., Achal, V., Zhou, T., Long, L. and She, Q. (2019). The characteristics and local-regional contributions of atmospheric black carbon over urban and suburban locations in Shanghai, China. Environ. Pollut. 255: 113188. [Publisher Site]

  36. Qi, M.Y., Wang, L.T., Zhang, C.Y., Ma, X., Zhao, L., Ji, S.P., Lu, X. and Wang, Y. (2018). Variation of black carbon aerosol concentration and its influencing factors in Handan City, Hebei Province. Acta Sci. Circumat. 38: 1751–1758. (in Chinese with English Abstract)
  37. Quaas, J. (2011). The soot factor. Nature 471: 456–457. [Publisher Site]

  38. Rai, M., Mahapatra, S.P., Gul. C., Kayastha, R.B., Panday, A.K. and Puppala, S.P. (2019). Aerosol radiative forcing estimation over a remote high-altitude location (~4900 masl) near Yala Glacier, Nepal. Aerosol Air Qual. Res. 19: 1872–1891. [Publisher Site]

  39. Ramachandran, S. and Rajesh, T.A. (2007). Black carbon aerosol mass concentrations over Ahmedabad, an urban location in western India: comparison with urban sites in Asia, Europe, Canada, and the United States. J. Geophys. Res. 112: D06211. [Publisher Site]

  40. Ramanathan, V. and Carmichael, G. (2008). Global and regional climate changes due to black carbon. Nat. Geosci. 1: 221–227. [Publisher Site]

  41. Richardson, T.B., Forster, P.M., Andrews, T., Boucher, O., Faluvegi, G., Fläschner, D., Hodnebrog, Ø., Kasoar, M., Kirkevåg, A., Lamarque, J.F. Myhre, G., Olivié, D., Samset, B.H., Shawki, D., Shindell, D., Takemura, T. and Voulgarakis, A. (2018). Drivers of precipitation change: An energetic understanding. J. Clim. 31: 9641–9657. [Publisher Site]

  42. Sahu, L.K., Kondo, Y., Miyazaki, Y., Pongkiatkul, P. and Oanh, N.T.K. (2011). Seasonal and diurnal variations of black carbon and organic carbon aerosols in Bangkok. J. Geophys. Res. 116: D15302. [Publisher Site]
  43. Schmidt, C.W. (2011). Black carbon: The dark horse of climate change drivers. Environ. Health Perspect. 119: 172–175. [Publisher Site]

  44. Streets, D.G., Gupta, S., Waldhoff, S.T., Wang, M.Q., Bond, T.C. and Yiyun, B. (2001). Black carbon emissions in China. Atmos. Environ. 35: 4281–4296. [Publisher Site]

  45. Stull, R.B. (1988). An introduction to boundary layer meteorology. Springer Netherlands.

  46. Sun, H.H., Ni, C.J. and Cui, L. (2016). Characteristics of black carbon aerosol pollution in Chengdu and the relationship between meteorological factors. Environ. Eng. 34: 11–124. (in Chinese with English Abstract)

  47. Sun, J.Y., Wu, C., Wu, D., Cheng, C., Li, M., Li, L., Deng, T., Yu, J.Z., Li, Y.J., Zhou, Q., Liang, Y., Sun, T., Song, L., Cheng, P., Yang, W., Pei, C., Chen, Y., Cen, Y., Nian, H. and Zhou, Z. (2020). Amplification of black carbon light absorption induced by atmospheric aging: temporal variation at seasonal and diel scales in urban Guangzhou. Atmos. Chem. Phys. 20: 2445–2470. [Publisher Site]

  48. Tian, P., Zhang, L., Ma, J., Tang, K., Xu, L., Wang, Y., Cao, X., Liang, J., Ji, Y., Jiang, J.H., Yung, Y.L. and Zhang, R.Y. (2018). Radiative absorption enhancement of dust mixed with anthropogenic pollution over East Asia. Atmos. Chem. Phys. 18: 7815–7825. [Publisher Site]

  49. Wang, Q., Huang, R., Cao, J., Tie, X., Shen, Z., Zhao, S., Han, Y., Li, G., Li, Z., Ni, H., Zhou, Y., Wang, M., Chen, Y. and Su, X. (2016). Contribution of regional transport to the black carbon aerosol during winter haze period in Beijing. Atmos. Environ. 132: 11–18. [Publisher Site]

  50. Wang, Q.Y., Liu, S.X., Zhou, Y.Q., Cao, J.J., Han, Y.M., Ni, H.Y., Zhang, N.N. and Huang, R.J. (2015a). Characteristics of black carbon aerosol during the Chinese Lunar Year and Weekdays in Xi’an, China. Atmosphere 6: 195–208. [Publisher Site]

  51. Wang, X., Zeng, Y. and Qiu, X.F. (2015b). Temperature inversion in mountain areas based on distributed simulation of monthly mean temperature under complex terrains. Sci. Technol. Eng. 15: 1–7. (in Chinese with English Abstract)

  52. Wang, Y., Hopke, P.K., Rattigan, O.V. and Zhu, Y. (2011). Characterization of ambient black carbon and wood burning particles in two urban areas. J. Environ. Monit. 13: 1919–1926. [Publisher Site]

  53. Xiao, S.H., Yu, X.N., Zhu, B. and He, J.Q. (2016). Characteristics of black carbon aerosol and influencing factors in northern suburbs of Nanjing. Environ. Sci. 37: 3280–3289. (in Chinese with English Abstract) [Publisher Site]

  54. Zhang, C., Zhou, Z.E., Zhai, C.Z., Chen, G.C., Zhang, D., Yu, J.Y., Zheng, J.J. and Wu, L.P. (2014). Characteristics and influencing factors of black carbon aerosol in Chongqing. Acta Sci. Circumat. 34: 812–818. (in Chinese with English Abstract)  [Publisher Site]

  55. Zhang, Q., Streets, D.G., Carmichael, G.R., He, K., Huo, H., Kannari, A., Klimont, Z., Park, I., Reddy, S., Fu, J.S., Chen, D., Duan, L., Lei, Y., Wang, L. and Yao, Z. (2009). Asian emissions in 2006 for the NASA INTEX-B mission. Atmos. Chem. Phys. 9: 5131–5153.  [Publisher Site]

  56. Zhang, Q., Shen, Z.X., Cao, J.J., Zhang, R.J., Zhang, L.M., Huang, R.J., Zheng, C.J., Wang, L.Q., Liu, S.X., Xu, H.M., Zheng, C. and Liu, P. (2015). Variations in PM2.5, TSP, BC, and trace gases (NO2, SO2, and O3) between haze and non-haze episodes in winter over Xi’an, China. Atmos. Environ. 112: 64–71. [Publisher Site]

  57. Zhang, Q., Shen, Z., Lei, Y., Wang, Y., Zeng, Y., Wang, Q., Ning, Z., Cao, J., Wang, L. and Xu, H. (2018). Variations of particle size distribution, black carbon, and brown carbon during a severe winter pollution event over Xi’an, China. Aerosol Air Qual. Res. 18: 1419–1430. [Publisher Site]

  58. Zhao, Y.C., Deli, G., Cai, Y.X., Zhang, Z.F. and Wen, Y.P. (2008). Variation of black-carbon aerosol concentration observed in Xining. J. Glaciol. Geocryol. 30: 789–794. (in Chinese with English Abstract)

  59. Zhou, B., Wang, Q., Zhou, Q., Zhang, Z., Wang, G., Fang, N., Li, M. and Cao, J. (2018). Seasonal characteristics of black carbon aerosol and its potential source regions in Baoji, China. Aerosol Air Qual. Res. 18: 397–406. [Publisher Site]

  60. Zhuang, B.L., Wang, T.J., Liu, J., Li, S., Xie, M., Yang, X.Q., Fu, C.B., Sun, J.N., Yin, C.Q., Liao, J.B., Zhu, J.L. and Zhang, Y. (2014). Continuous measurement of black carbon aerosol in urban Nanjing of Yangtze river delta, China. Atmos. Environ. 89: 415–424. [Publisher Site]

Aerosol Air Qual. Res. 20 :1282 -1293 . https://doi.org/10.4209/aaqr.2019.10.0516  

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