2020
DOI: 10.3390/ijerph17249172
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Air Pollution Characteristics and Health Risks in the Yangtze River Economic Belt, China during Winter

Abstract: The air pollution characteristics of six ambient criteria pollutants, including particulate matter (PM) and trace gases, in 29 typical cities across the Yangtze River Economic Belt (YREB) from December 2017 to February 2018 are analyzed. The overall average mass concentrations of PM2.5, PM10, SO2, CO, NO2, and O3 are 73, 104, 16, 1100, 47, and 62 µg/m3, respectively. PM2.5, PM10, and NO2 are the dominant major pollutants to poor air quality, with nearly 83%, 86%, and 59%, exceeding the Chinese Ambient Air Qual… Show more

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Cited by 19 publications
(16 citation statements)
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“…While aerosol loading and air pollution situation can be revealed with the satellite data of daily aerosol optical depth (AOD) from moderate resolution imaging spectroradiometry (MODIS) Level 2 10 km × 10 km Collection V005, regional AOD distribution on the basis of the Giovanni map [29] over mid-eastern China is illustrated in Figure 1. An average AOD of ~1.0 at 550 nm during June 2012 is obtained over Hefei (see Figure 1a), and such high aerosol loading is probably attributed to severe haze and fog episodes contributed by synoptic patterns and anthropogenic emissions (e.g., straw biomass burning, and traffic exhausts) [30,31]. During the sampling period, a typical radiation fog event is observed in 11-12 June 2012, and an AOD of ~3.0 at 550 nm is even obtained (see Figure 1b), indicating strong aerosol extinction during fog episodes.…”
Section: Overview Of Aerosol Radiative Propertiesmentioning
confidence: 99%
See 1 more Smart Citation
“…While aerosol loading and air pollution situation can be revealed with the satellite data of daily aerosol optical depth (AOD) from moderate resolution imaging spectroradiometry (MODIS) Level 2 10 km × 10 km Collection V005, regional AOD distribution on the basis of the Giovanni map [29] over mid-eastern China is illustrated in Figure 1. An average AOD of ~1.0 at 550 nm during June 2012 is obtained over Hefei (see Figure 1a), and such high aerosol loading is probably attributed to severe haze and fog episodes contributed by synoptic patterns and anthropogenic emissions (e.g., straw biomass burning, and traffic exhausts) [30,31]. During the sampling period, a typical radiation fog event is observed in 11-12 June 2012, and an AOD of ~3.0 at 550 nm is even obtained (see Figure 1b), indicating strong aerosol extinction during fog episodes.…”
Section: Overview Of Aerosol Radiative Propertiesmentioning
confidence: 99%
“…The trajectories at Hefei during fog episodes are illustrated in Figure 6, and air masses are originated from the Yangtze Delta to the east of Hefei. The monsoon wind prevailing brings Hefei aerosol pollutions produced over the Yangtze Delta, besides local emissions [31]. These anthropogenic aerosol emissions from industry and fossil fuels, as well as biomass burning displayed in the MODIS wildfire maps (not shown), are favorable for radiation fog episodes, in addition to weather conditions (such as calm wind, few clouds, and high relative humidity).…”
Section: Comparison Of Aerosol Radiative Properties During Fog With Haze and Clear Periodsmentioning
confidence: 99%
“…A large number of studies have investigated the regularity of temporal variations and the spatial distribution of different air pollutants. Examples include sulfur dioxide (SO 2 ) [ 6 , 7 , 8 ], particulate matter with a median diameter less than 2.5 µm (PM 2.5 ) [ 9 , 10 , 11 ], and particulate matter with a median diameter less than 10 µm (PM 10 ) [ 12 , 13 ]. Research on the spatiotemporal regularity of air pollutants has been carried out extensively in single cities [ 12 , 14 ], urban agglomerations [ 15 ], hot regions [ 16 , 17 , 18 ], and even nationwide [ 19 ].…”
Section: Introductionmentioning
confidence: 99%
“…The former is usually concentrated in large-scale areas, such as the whole of China [13], the North China Plain [14] and so on. The latter has the characteristics of high monitoring frequency, which facilitates better exploration of seasonal and daily changes at the urban scale (such as small-and medium-sized areas) [15,16]. In addition, ground monitoring data are much more reliable and accurate than remote sensing inversion data [17].…”
Section: Introductionmentioning
confidence: 99%