Articles | Volume 19, issue 14
https://doi.org/10.5194/acp-19-9061-2019
https://doi.org/10.5194/acp-19-9061-2019
Research article
 | 
17 Jul 2019
Research article |  | 17 Jul 2019

Elucidating ice formation pathways in the aerosol–climate model ECHAM6-HAM2

Remo Dietlicher, David Neubauer, and Ulrike Lohmann

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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 Remo Dietlicher on behalf of the Authors (01 Nov 2018)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (05 Nov 2018) by Toshihiko Takemura
RR by Anonymous Referee #2 (04 Dec 2018)
RR by Anonymous Referee #1 (04 Dec 2018)
ED: Reconsider after major revisions (05 Dec 2018) by Toshihiko Takemura
AR by Remo Dietlicher on behalf of the Authors (15 Mar 2019)
ED: Referee Nomination & Report Request started (22 Mar 2019) by Toshihiko Takemura
RR by Anonymous Referee #1 (08 Jun 2019)
ED: Publish subject to minor revisions (review by editor) (08 Jun 2019) by Toshihiko Takemura
AR by Remo Dietlicher on behalf of the Authors (18 Jun 2019)  Author's response   Manuscript 
ED: Publish as is (20 Jun 2019) by Toshihiko Takemura
AR by Remo Dietlicher on behalf of the Authors (24 Jun 2019)  Manuscript 
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Short summary
Ice crystals in clouds cover a spectrum of shapes and sizes. We show the first results of a consistent representation of the cloud ice spectrum in the climate model ECHAM6-HAM2. The simulated cloud fields are linked to their sources by new diagnostics. We find that only a small fraction of ice clouds is initiated by freezing of cloud droplets in the mixed-phase temperature regime while most ice forms at temperatures colder than −35 °C.
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