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The role of cloud glaciation in modulating aerosol susceptibility: insights from cold-air outbreak stratiform clouds over the Northwest Pacific

Year: 2025
Type: article
Abstract: Aerosol susceptibility (AS) of clouds refers to their sensitivity to increases in condensation nuclei (CN) concentration. This study investigates AS in marine boundary layer clouds that occur during cold-air outbreaks, where ice particles are often present. In warm clouds, the AS of cloud albedo (precipitation) remains positive (negative); however, this sensitivity weakens as CN concentration increases. In mixed-phase clouds, AS becomes less pronounced and does not follow a consistent trend due to the positive response of snow growth to rising CN levels. Aside from microphysical responses, cloud fraction -- a macro-physical feature -- also shows susceptibility to aerosol effects. As CN increases, cloud fraction tends to decrease, which can mitigate up to one-third of the cloud albedo AS in warm clouds and three-fourths in mixed-phase clouds.
Language: English
Open Access status: gold
Estimated APC paid: $1,390
OpenAlex ID: W4414600910
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Cites: 58
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