Articles | Volume 26, issue 3
https://doi.org/10.5194/acp-26-2083-2026
https://doi.org/10.5194/acp-26-2083-2026
Research article
 | 
10 Feb 2026
Research article |  | 10 Feb 2026

Separating the Twomey effect and the semi-direct effect in absorbing aerosol environments through the cloud-aerosol mixing ratio

Po-Hsun Lin, Sheng-Hsiang Wang, Otto Klemm, and Neng-Huei Lin

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Cited articles

Albrecht, B. A.: Aerosols, Cloud Microphysics, and Fractional Cloudiness, Science, 245, 1227–1230, https://doi.org/10.1126/science.245.4923.1227, 1989. 
Ardon-Dryer, K., Kelley, M. C., Xueting, X., and Dryer, Y.: The Aerosol Research Observation Station (AEROS), Atmos. Meas. Tech., 15, 2345–2360, https://doi.org/10.5194/amt-15-2345-2022, 2022. 
Bender, F. A. M., Frey, L., McCoy, D. T., Grosvenor, D. P., and Mohrmann, J. K.: Assessment of aerosol–cloud–radiation correlations in satellite observations, climate models and reanalysis, Clim. Dynam., 52, 4371–4392, https://doi.org/10.1007/s00382-018-4384-z, 2019. 
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This study used in-situ observations to explore how long-range transported biomass-burning aerosols affect the development of warm clouds in Southeast Asia. Our findings provide evidence of the nonlinear responses of cloud systems to absorbing aerosols. When liquid water is relatively abundant compared to aerosol concentration, increased aerosols tend to enhance droplet formation; otherwise, aerosols may suppress cloud development by altering the surrounding environment.
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