Articles | Volume 18, issue 19
Atmos. Chem. Phys., 18, 13987–14003, 2018

Special issue: Results from the ice nucleation research unit (INUIT) (ACP/AMT...

Atmos. Chem. Phys., 18, 13987–14003, 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 et al.


Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Stine Eriksen-Hammer on behalf of the Authors (04 Sep 2018)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (08 Sep 2018) by Allan Bertram
RR by Anonymous Referee #1 (10 Sep 2018)
ED: Publish as is (10 Sep 2018) by Allan Bertram
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.
Final-revised paper