Latent ice-forming nuclei in the Pacific Northwest
作者： J. Rosinski
DOI: 10.1016/0169-8095(91)90041-T
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摘要: Abstract Some cloud condensation nuclei (CCN) constitute a reservoir of latent ice-forming (IFN) active by condensation-followed-by-freezing and sorption. Evaporated droplets occasionally left aerosol particles that acted as sorption IFN at temperatures high −5°C water vapor supersaturation over ice 0.2%. The newly formed (residues evaporated droplets) are all mixed particles. discovery produced from CCN promotes new insights into the process formation in clouds; an evaporating parcel rate will be enhanced continuous production IFN. Aerosol behind after evaporation may provide source for some cirrus clouds.
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