Preprints
https://doi.org/10.5194/egusphere-2026-4265
https://doi.org/10.5194/egusphere-2026-4265
24 Aug 2026
 | 24 Aug 2026
Status: this preprint is open for discussion and under review for Atmospheric Chemistry and Physics (ACP).

Tropical cyclone amplifies anthropogenic influences on aerosol-cloud interactions over the South China Sea

Hengjia Ou, Mingfu Cai, Haichao Wang, Xue Ni, Shixin Mai, Qibin Sun, Baoling Liang, Kunpeng Chen, Tao Deng, Sun Jiaren, Shengzhen Zhou, and Jun Zhao

Abstract. Tropical cyclones can influence marine aerosol-cloud interactions by transporting continental anthropogenic pollutants over the ocean. However, this process and its impact remain poorly understood due to lack of direct measurements. Using shipborne measurements over the South China Sea (SCS) from 22 June to 5 July 2022, we investigated how a typical TC Chaba altered aerosol physicochemical properties and cloud microphysical responses. As TC Chaba developed, its circulation altered regional transport pathways, shifting air masses from local marine origin to long-range transport from the Indochina Peninsula and causing pronounced increases in non-refractory submicron particulate matter (NR-PM1) concentrations. Organic aerosol (OA) increased from 14.6 % to 44.9 % of NR-PM1 after the influence of TC Chaba, mainly due to enhanced oxygenated OA (OOA) from long-range transport together with enhanced local heterogeneous oxidation, as indicated by the higher OA oxidation state and increasing OOA concentrations with Ox and relative humidity. These changes led to a ~60 % decrease in aerosol hygroscopicity (κ), while an ~27 % increase in κOA, which outweighed the modest particle size increase and resulted in a lower bulk activation ratio. Furthermore, CCN concentrations increased by up to sixfold because of enhanced aerosol concentrations. Combined observations and cloud parcel simulations indicate that the aerosol perturbations decreased cloud droplet effective radius by 11–37 % and increased the autoconversion radius by 6–26 %, enhancing cloud reflectivity and suppressing warm-rain formation. Satellite observations further confirmed smaller cloud droplets. These results demonstrate a strong TC influence on marine cloud microphysics and radiative effects.

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Hengjia Ou, Mingfu Cai, Haichao Wang, Xue Ni, Shixin Mai, Qibin Sun, Baoling Liang, Kunpeng Chen, Tao Deng, Sun Jiaren, Shengzhen Zhou, and Jun Zhao

Status: open (until 05 Oct 2026)

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Hengjia Ou, Mingfu Cai, Haichao Wang, Xue Ni, Shixin Mai, Qibin Sun, Baoling Liang, Kunpeng Chen, Tao Deng, Sun Jiaren, Shengzhen Zhou, and Jun Zhao
Hengjia Ou, Mingfu Cai, Haichao Wang, Xue Ni, Shixin Mai, Qibin Sun, Baoling Liang, Kunpeng Chen, Tao Deng, Sun Jiaren, Shengzhen Zhou, and Jun Zhao
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Short summary
This study investigates how tropical cyclones transport anthropogenic pollutants into the marine atmosphere, substantially increasing organic aerosol and enhancing secondary aerosol formation. These changes reduced bulk aerosol hygroscopicity despite enhanced organic aerosol hygroscopicity, weakening cloud condensation nuclei activity. However, higher aerosol number concentrations produced more and smaller cloud droplets, enhancing cloud reflectivity and suppressing warm-rain formation.
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