Technical note: Equilibrium droplet size distributions in a turbulent cloud chamber with uniform supersaturation

<p>In a laboratory cloud chamber that is undergoing Rayleigh–Bénard convection, supersaturation is produced by isobaric mixing. When aerosols (cloud condensation nuclei) are injected into the chamber at a constant rate, and the rate of droplet activation is balanced by the rate of droplet loss...

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Bibliographic Details
Main Author: S. K. Krueger
Format: Article
Language:English
Published: Copernicus Publications 2020-07-01
Series:Atmospheric Chemistry and Physics
Online Access:https://www.atmos-chem-phys.net/20/7895/2020/acp-20-7895-2020.pdf

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