Articles | Volume 16, issue 17
https://doi.org/10.5194/acp-16-11107-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/acp-16-11107-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Effects of 20–100 nm particles on liquid clouds in the clean summertime Arctic
W. Richard Leaitch
CORRESPONDING AUTHOR
Environment and Climate Change Canada, Toronto, Canada
Alexei Korolev
Environment and Climate Change Canada, Toronto, Canada
Amir A. Aliabadi
Environment and Climate Change Canada, Toronto, Canada
now at: Environmental Engineering, University of Guelph, Guelph, Canada
Julia Burkart
Department of Chemistry, University of Toronto, Toronto, Canada
Megan D. Willis
Department of Chemistry, University of Toronto, Toronto, Canada
Jonathan P. D. Abbatt
Department of Chemistry, University of Toronto, Toronto, Canada
Heiko Bozem
Institute for Atmospheric Physics, University of Mainz, Mainz, Germany
Peter Hoor
Institute for Atmospheric Physics, University of Mainz, Mainz, Germany
Franziska Köllner
Particle Chemistry Department, Max Planck Institute for Chemistry, Mainz,
Germany
Johannes Schneider
Particle Chemistry Department, Max Planck Institute for Chemistry, Mainz,
Germany
Andreas Herber
Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research, Bremerhaven,
Germany
Christian Konrad
Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research, Bremerhaven,
Germany
Ralf Brauner
Department of Maritime and Logistics Studies, Jade University, Elsfleth, Germany
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Latest update: 06 Dec 2025
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.
Thought to be mostly unimportant for summertime Arctic liquid-water clouds, airborne...
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