Chemical characteristics of cloud water and the impacts on aerosol properties at a subtropical mountain site in Hong Kong SAR
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Published:2020-01-13
Issue:1
Volume:20
Page:391-407
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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:
Li Tao, Wang ZheORCID, Wang Yaru, Wu Chen, Liang Yiheng, Xia MenORCID, Yu Chuan, Yun Hui, Wang WeihaoORCID, Wang Yan, Guo Jia, Herrmann HartmutORCID, Wang TaoORCID
Abstract
Abstract. To investigate the cloud water chemistry and the effects
of cloud processing on aerosol properties, comprehensive field observations
of cloud water, aerosols, and gas-phase species were conducted at a
mountaintop site in Hong Kong SAR in October and November 2016. The chemical
composition of cloud water including water-soluble ions, dissolved organic
matter (DOM), carbonyl compounds (refer to aldehydes and acetone),
carboxylic acids, and trace metals was quantified. The measured cloud water
was very acidic with a mean pH of 3.63, as the ammonium (174 µeq L−1) was insufficient for neutralizing the dominant sulfate (231 µeq L−1) and nitrate (160 µeq L−1). Substantial DOM
(9.3 mgC L−1) was found in cloud water, with carbonyl compounds and carboxylic
acids accounting for 18 % and 6 % in carbon molar concentrations,
respectively. Different from previous observations, concentrations of
methylglyoxal (19.1 µM; µM is equal to µmol L−1) and glyoxal (6.72 µM) were higher than
that of formaldehyde (1.59 µM). The partitioning of carbonyls between
cloud water and the gas phase was also investigated. The measured aqueous
fractions of dicarbonyls were comparable to the theoretical estimations,
while significant aqueous-phase supersaturation was found for less soluble
monocarbonyls. Both organics and sulfate were significantly produced in
cloud water, and the aqueous formation of organics was more enhanced by
photochemistry and under less acidic conditions. Moreover, elevated sulfate
and organics were measured in the cloud-processed aerosols, and they were
expected to contribute largely to the increase in droplet-mode aerosol mass
fraction. This study demonstrates the significant role of clouds in altering
the chemical compositions and physical properties of aerosols via scavenging
and aqueous chemical processing, providing valuable information about
gas–cloud–aerosol interactions in subtropical and coastal regions.
Funder
National Natural Science Foundation of China
Publisher
Copernicus GmbH
Subject
Atmospheric Science
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