On the limits of Köhler activation theory: how do collision and coalescence affect the activation of aerosols?
Activation is necessary to form a cloud droplet from an aerosol, and it is widely accepted that it occurs as soon as a wetted aerosol grows beyond its critical radius. Traditional Köhler theory assumes that this growth is driven by the diffusion of water vapor. However, if the wetted aerosols are...
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| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
Copernicus Publications
2017-07-01
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| coleção: | Atmospheric Chemistry and Physics |
| Acesso em linha: | https://www.atmos-chem-phys.net/17/8343/2017/acp-17-8343-2017.pdf |
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