Atmospheric Aerosols and Nucleation
DOI: 10.1007/3-540-50108-8_1145
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Phase transitions in an adsorbed water layer on aerosol particles

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“…In this case, a generalized heterogeneous nucleation equation was used, which takes into account the dependence of the interfacial specific surface energy on water vapor supersaturation. The issues of the formation of secondary ice crystals and the influence of particle sizes on the ice-forming activity of aerosol are considered [32,33].…”
Section: Introductionmentioning
confidence: 99%
“…In this case, a generalized heterogeneous nucleation equation was used, which takes into account the dependence of the interfacial specific surface energy on water vapor supersaturation. The issues of the formation of secondary ice crystals and the influence of particle sizes on the ice-forming activity of aerosol are considered [32,33].…”
Section: Introductionmentioning
confidence: 99%