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Atmospheric Chemistry and Physics An interactive open-access journal of the European Geosciences Union
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Volume 16, issue 14
Atmos. Chem. Phys., 16, 9421–9433, 2016
https://doi.org/10.5194/acp-16-9421-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
Atmos. Chem. Phys., 16, 9421–9433, 2016
https://doi.org/10.5194/acp-16-9421-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 29 Jul 2016

Research article | 29 Jul 2016

Conditions for super-adiabatic droplet growth after entrainment mixing

Fan Yang et al.

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AR by Anna Wenzel on behalf of the Authors (09 Jun 2016)  Author's response
ED: Publish as is (08 Jul 2016) by Timothy Garrett
Publications Copernicus
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Short summary
When dry air is mixed into a cloud, droplets evaporate. If the diluted cloud mixture continues to rise, the remaining droplets will grow. In this work we show theoretically and computationally that a critical height exists, above which the droplets in a mixed, diluted cloud volume become larger than those in an undiluted volume. An environment that is humid and aerosol free is most favorable for producing such large droplets, which may contribute to the onset of precipitation formation.
When dry air is mixed into a cloud, droplets evaporate. If the diluted cloud mixture continues...
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