Articles | Volume 16, issue 17
https://doi.org/10.5194/acp-16-11107-2016
https://doi.org/10.5194/acp-16-11107-2016
Research article
 | 
08 Sep 2016
Research article |  | 08 Sep 2016

Effects of 20–100 nm particles on liquid clouds in the clean summertime Arctic

W. Richard Leaitch, Alexei Korolev, Amir A. Aliabadi, Julia Burkart, Megan D. Willis, Jonathan P. D. Abbatt, Heiko Bozem, Peter Hoor, Franziska Köllner, Johannes Schneider, Andreas Herber, Christian Konrad, and Ralf Brauner

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Latest update: 14 Dec 2024
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Short summary
Thought to be mostly unimportant for summertime Arctic liquid-water clouds, airborne observations show that atmospheric aerosol particles 50 nm in diameter or smaller and most likely from natural sources are often involved in cloud formation in the pristine Arctic summer. The result expands the reference for aerosol forcing of climate. Further, for extremely low droplet concentrations, no evidence is found for a connection between cloud liquid water and aerosol particle concentrations.
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