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Secondary ice growth mechanism for ice nuclei in the atmosphere

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arxiv 2303.05239 v1 pith:3QRJOXI6 submitted 2023-03-09 cond-mat.mtrl-sci cond-mat.stat-mechhep-th

classification cond-mat.mtrl-scicond-mat.stat-mechhep-th
keywords nucleiatmosphericwatergrowthmechanismquantumaccumulationatmosphere
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abstract

The study of atmospheric ice nuclei is vital for understanding the formation of precipitation and the development of cloud systems as it reveals how these tiny particles grow. A mechanism of such growth when the nuclei are in a mixed ice/water phase and quantum vacuum fluctuation-induced Casimir-Lifshitz interaction highlights the complexity and interconnection of the atmospheric processes with quantum theory. Initially of the order of $0.1\sim10\rm\mu m$ in size, atmospheric ice nuclei can expand by the accumulation of water molecules from the surrounding water vapor.

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