Articles | Volume 18, issue 19
https://doi.org/10.5194/acp-18-13987-2018
https://doi.org/10.5194/acp-18-13987-2018
Research article
 | 
02 Oct 2018
Research article |  | 02 Oct 2018

Composition of ice particle residuals in mixed-phase clouds at Jungfraujoch (Switzerland): enrichment and depletion of particle groups relative to total aerosol

Stine Eriksen Hammer, Stephan Mertes, Johannes Schneider, Martin Ebert, Konrad Kandler, and Stephan Weinbruch

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Latest update: 15 Apr 2024
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Short summary
It is important to study ice-nucleating particles in the environment to learn more about cloud formation. We studied the composition of ice particle residuals and total aerosol particles sampled in parallel during mixed-phase cloud events at Jungfraujoch and discovered that soot and complex secondary particles were not present. In contrast, silica, aluminosilicates, and other aluminosilicates were the most important ice particle residual groups at site temperatures between −11 and −18 °C.
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