A simple model for the time evolution of the condensation sink in the atmosphere for intermediate Knudsen numbers

Transformation of the mass flux towards the particle from the kinetic regime to the continuum regime is often described by the Fuchs–Sutugin coefficient. Kinetic regime can be obtained as a limiting case when only one term of the expansion of the Fuchs–Sutugin coefficient at small 1 ∕ <i>K...

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Bibliographic Details
Main Authors: E. Ezhova, V.-M. Kerminen, K. E. J. Lehtinen, M. Kulmala
Format: Article
Language:English
Published: Copernicus Publications 2018-02-01
Series:Atmospheric Chemistry and Physics
Online Access:https://www.atmos-chem-phys.net/18/2431/2018/acp-18-2431-2018.pdf