Measurement report: The influence of particle number size distribution and hygroscopicity on the microphysical properties of cloud droplets at a mountain site

Abstract. An automatic switched inlet system, incorporating a ground-based counterflow virtual impactor (GCVI) and a PM2.5 impactor, was developed and employed to investigate the particle number size distributions (PNSDs) and chemical composition for cloud-free (CF), cloud interstitial (CI), and cloud residual (CR) particles at Mt. Daming in the Yangtze River Delta, China, throughout a 1-month period in spring 2023. The PNSDs of CF particles were primarily characterized by a significant Aitken mode alongside a secondary accumulation mode. In contrast, CI and CR particles exhibited unimodal distribution with Aitken and accumulation modes, peaking at 56 and 220 nm, respectively. With the fast changes of PNSDs during the onset stage of the observed four typical cloud processes, it can be inferred that the critical diameters activated as cloud droplets ranging from 133–325 nm. Particularly noteworthy was the higher hygroscopicity parameter, κ value observed in CR particles (0.32±0.06), associated with a larger mass fraction of nitrate, compared to the lower κ value in CI particles (0.23±0.08), with higher fraction of black carbon. For a typical cloud process, the hygroscopicity of CI particles was found to influence cloud droplet properties, with higher κ values corresponding to lower droplet number concentration, reduced liquid water content, and smaller effective cloud droplet diameters. This suggests that these CI particles are capable of absorbing ambient water vapour, thereby restricting further droplet growth. This investigation contributes to understanding aerosol–cloud interactions by assessing the impact of aerosol particles on cloud microphysics, thus enhancing overall comprehension of these complex atmospheric dynamics. However, it is noted that long-term observations are necessary to capture more cloud processes and yield statistically significant findings.

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Publication Details

Journal
Atmospheric chemistry and physics
Published
2025-06-11
DOI
https://doi.org/10.5194/acp-25-5711-2025
Citations
3
Primary Topic
Atmospheric aerosols and clouds
Type
article
Field-Weighted Citation Impact
3.32

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article

Measurement report: The influence of particle number size distribution and hygroscopicity on the microphysical properties of cloud droplets at a mountain site

Lujie Han, Qianli Ma, Aoyuan Yu, Lei Liu et al.
3 citations
Atmospheric chemistry and physics
Atmospheric aerosols and clouds
3.32
article

Measurement report: The influence of particle number size distribution and hygroscopicity on the microphysical properties of cloud droplets at a mountain site

Lujie Han, Qianli Ma, Aoyuan Yu, Lei Liu, Quan Liu, Xiaojing Shen, Huizheng Che, Linlin Liang, Jiayuan Lu, Bing Qi, Xinyao Hu, Junying Sun, Shuo Liu, Xiaoye Zhang, Yangmei Zhang, Wanlin Kong
article en
3 citations

Abstract

Abstract. An automatic switched inlet system, incorporating a ground-based counterflow virtual impactor (GCVI) and a PM2.5 impactor, was developed and employed to investigate the particle number size distributions (PNSDs) and chemical composition for cloud-free (CF), cloud interstitial (CI), and cloud residual (CR) particles at Mt. Daming in the Yangtze River Delta, China, throughout a 1-month period in spring 2023. The PNSDs of CF particles were primarily characterized by a significant Aitken mode alongside a secondary accumulation mode. In contrast, CI and CR particles exhibited unimodal distribution with Aitken and accumulation modes, peaking at 56 and 220 nm, respectively. With the fast changes of PNSDs during the onset stage of the observed four typical cloud processes, it can be inferred that the critical diameters activated as cloud droplets ranging from 133–325 nm. Particularly noteworthy was the higher hygroscopicity parameter, κ value observed in CR particles (0.32±0.06), associated with a larger mass fraction of nitrate, compared to the lower κ value in CI particles (0.23±0.08), with higher fraction of black carbon. For a typical cloud process, the hygroscopicity of CI particles was found to influence cloud droplet properties, with higher κ values corresponding to lower droplet number concentration, reduced liquid water content, and smaller effective cloud droplet diameters. This suggests that these CI particles are capable of absorbing ambient water vapour, thereby restricting further droplet growth. This investigation contributes to understanding aerosol–cloud interactions by assessing the impact of aerosol particles on cloud microphysics, thus enhancing overall comprehension of these complex atmospheric dynamics. However, it is noted that long-term observations are necessary to capture more cloud processes and yield statistically significant findings.

Atmospheric chemistry and physicsVol. 25(11)
Chinese Academy of Meteorological Sciences (CN), Zhejiang Meteorological Bureau (CN)
National Natural Science Foundation of China, Chinese Academy of Meteorological Sciences, National Key Research and Development Program of China
Openalex Percentile: Top 8%
Atmospheric aerosols and clouds
3.32
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