Characterization of aerosol hygroscopicity, mixing state, and CCN activity at a suburban site in the central North China Plain
<p>This study investigates aerosol hygroscopicity, mixing state, and cloud condensation nucleation as part of the Atmosphere–Aerosol–Boundary Layer–Cloud Interaction Joint Experiment performed in the summer of 2016 at Xingtai (XT), a suburban site located in the center of the North China P...
Main Authors: | , , , , , , , , , , , , |
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Format: | Article |
Language: | English |
Published: |
Copernicus Publications
2018-08-01
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Series: | Atmospheric Chemistry and Physics |
Online Access: | https://www.atmos-chem-phys.net/18/11739/2018/acp-18-11739-2018.pdf |
Summary: | <p>This
study investigates aerosol hygroscopicity, mixing state, and cloud
condensation nucleation as part of the Atmosphere–Aerosol–Boundary
Layer–Cloud Interaction Joint Experiment performed in the summer of 2016 at
Xingtai (XT), a suburban site located in the center of the North China Plain
(NCP). In general, the probability density function (PDF) of the
hygroscopicity parameter (<i>κ</i>) for 40–200 nm particles had a unimodal
distribution, and mean <i>κ</i>-PDF patterns for different sizes were
similar, suggesting that the particles were highly aged and internally mixed
because of strong photochemical reactions. The <i>κ</i> calculated from the
hygroscopic growth factor in the daytime and at night suggests that
photochemical reactions largely enhanced the aerosol hygroscopicity. This
effect became weaker as the particle size increased. In addition, the aerosol
hygroscopicity was much larger at XT than at other sites in the NCP. This is
because new particle formation takes place much more frequently in the
central NCP, which is heavily polluted from industrial activities, than
elsewhere in the region. The evolution of the planetary boundary layer played
a dominant role in dictating aerosol mass concentration. Particle size was
the most important factor influencing the ability of aerosols to activate,
whereas the effect of chemical composition was secondary, especially when
supersaturation was high. Using a fixed value of <i>κ</i> = 0.31 to calculate
the cloud condensation nuclei number concentration in this region suffices.</p> |
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ISSN: | 1680-7316 1680-7324 |