Articles | Volume 22, issue 23
https://doi.org/10.5194/acp-22-15579-2022
https://doi.org/10.5194/acp-22-15579-2022
Research article
 | 
12 Dec 2022
Research article |  | 12 Dec 2022

Conditions favorable for secondary ice production in Arctic mixed-phase clouds

Julie Thérèse Pasquier, Jan Henneberger, Fabiola Ramelli, Annika Lauber, Robert Oscar David, Jörg Wieder, Tim Carlsen, Rosa Gierens, Marion Maturilli, and Ulrike Lohmann

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Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
AR by Julie Thérèse Pasquier on behalf of the Authors (24 Oct 2022)  Author's response   Author's tracked changes   Manuscript 
ED: Publish subject to minor revisions (review by editor) (24 Oct 2022) by Timothy Garrett
AR by Julie Thérèse Pasquier on behalf of the Authors (01 Nov 2022)  Author's response   Author's tracked changes   Manuscript 
ED: Publish subject to technical corrections (03 Nov 2022) by Timothy Garrett
AR by Julie Thérèse Pasquier on behalf of the Authors (03 Nov 2022)  Author's response   Manuscript 
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Short summary
It is important to understand how ice crystals and cloud droplets form in clouds, as their concentrations and sizes determine the exact radiative properties of the clouds. Normally, ice crystals form from aerosols, but we found evidence for the formation of additional ice crystals from the original ones over a large temperature range within Arctic clouds. In particular, additional ice crystals were formed during collisions of several ice crystals or during the freezing of large cloud droplets.
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