Characterization of dust-related new particle formation events based on long-term measurement in the North China Plain
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Published:2023-07-25
Issue:14
Volume:23
Page:8241-8257
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ISSN:1680-7324
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Container-title:Atmospheric Chemistry and Physics
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language:en
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Short-container-title:Atmos. Chem. Phys.
Author:
Shen Xiaojing, Sun Junying, Che HuizhengORCID, Zhang Yangmei, Zhou Chunhong, Gui KeORCID, Xu Wanyun, Liu QuanORCID, Zhong JuntingORCID, Xia Can, Hu Xinyao, Zhang Sinan, Wang Jialing, Liu Shuo, Lu Jiayuan, Yu Aoyuan, Zhang Xiaoye
Abstract
Abstract. Mineral dust is a major natural atmospheric aerosol that
impacts the Earth's radiation balance. The significant scavenging process of
fine particles by the strong wind during the dust episodes provided a
relatively clean environment that was favourable for new particle formation
(NPF) occurrence. In this study, the NPF occurred following the dust
episodes (dust-related NPF), and other cases under clean and polluted
conditions were classified based on the long-term particle number size
distribution (PNSD) in urban Beijing in spring from 2017 to 2021. It was
found that the observed formation (Jobs) and growth rate (GR) of dust-related
NPF events were approximately 50 % and 30 % lower than the values of
other NPF days, respectively. A typical severe dust storm that originated
from Mongolia and swept over northern China on 15–16 March 2021 was
analysed, to illustrate how the dust storm influences the NPF event. The
maximum hourly mean PM10 mass concentration reached
8000 µg m−3 during this dust storm. The occurrence of an NPF event after a dust
storm was facilitated due to the low condensation sink (∼ 0.005 s−1) caused by the strong dilution process of pre-existing
particles. However, a downward trend of particle hygroscopicity was found
during dust storm and NPF event as compared with the polluted episode,
resulting in an increasing trend of the critical diameter at different
supersaturations (ss), where aerosols are activated as cloud condensation
nuclei (CCN), although the NPF event occurred when dust faded. The critical
diameter was elevated by approximately 6 %–10 % (ss = 0.2 % and
0.7 %) during the dust storm, resulting in a lower CCN activation ratio,
especially at low supersaturation. Modifications of the nucleation and
growth process, as well as the particle-size distribution and hygroscopicity
of the dust particles, provide valuable information that reveals the
underlying climate and air quality effects of Asian mineral dust.
Funder
National Natural Science Foundation of China
Publisher
Copernicus GmbH
Subject
Atmospheric Science
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