Concentration and Physical Characteristics of Black Carbon in Winter Snow of Beijing in 2015

In Beijing, the probability of snowfall is decreasing as a result of global warming. At the same time, Beijing has suffered severe air pollution. In this paper, the concentration and particle size characteristics of BC (Black Carbon) in snow during the winter of 2015 in Beijing were analyzed by the...

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Bibliographic Details
Published inAtmosphere Vol. 12; no. 7; p. 816
Main Authors Zhao, Delong, Sheng, Jiujiang, Du, Yuanmou, Zhou, Wei, Wang, Fei, Xiao, Wei, Ding, Deping
Format Journal Article
LanguageEnglish
Published Basel MDPI AG 01.07.2021
Subjects
Aerosols
Air pollution
Beijing
Black carbon
Carbon
Carbon dioxide
Climate change
Efficiency
Global warming
Ice
Laboratories
Megacities
Meltwater
Meteorological conditions
Methods
Mountains
Optical properties
Particle size
Physical characteristics
Physical properties
Pollution levels
Polyethylene terephthalate
Probability theory
size distribution
Snow
Snow accumulation
Snow and ice
Snowfall
Snowmelt
SP2
Urban areas
Wind
Winter
Winter snow
Beijing China
China
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Summary:In Beijing, the probability of snowfall is decreasing as a result of global warming. At the same time, Beijing has suffered severe air pollution. In this paper, the concentration and particle size characteristics of BC (Black Carbon) in snow during the winter of 2015 in Beijing were analyzed by the SP2 method. The average concentration of BC in snow meltwater in Beijing is 82 ng/mL, with a minimum value of 62.9 ng/mL and a maximum of 210.6 ng/mL. The BC particle size in snow and ice in the Beijing area is mostly concentrated in the range of 70–400 nm. After log-normal, the BC particle size above 600 nm is still small, which should be closely related to the nature of the local BC emission source. The concentration of BC in snow is highly susceptible to meteorological conditions and local pollution levels. When Beijing is under the control of the east wind or the southeast wind, aerosols in the urban areas can easily accumulate in the northwestern mountains and then settle or participate in the snowfall process, resulting in an increase in BC aerosol accumulation in the snow, thus further changing the optical properties of snow in the Beijing area.
ISSN:2073-4433
2073-4433
DOI:10.3390/atmos12070816