Articles | Volume 19, issue 24
https://doi.org/10.5194/acp-19-15285-2019
https://doi.org/10.5194/acp-19-15285-2019
Research article
 | 
16 Dec 2019
Research article |  | 16 Dec 2019

Lateral facet growth of ice and snow – Part 1: Observations and applications to secondary habits

Jon Nelson and Brian D. Swanson

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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 Jon Nelson on behalf of the Authors (27 Jul 2019)  Manuscript 
ED: Referee Nomination & Report Request started (12 Aug 2019) by Thorsten Bartels-Rausch
RR by Anonymous Referee #1 (15 Aug 2019)
RR by Anonymous Referee #4 (23 Aug 2019)
ED: Publish subject to minor revisions (review by editor) (28 Aug 2019) by Thorsten Bartels-Rausch
AR by Jon Nelson on behalf of the Authors (19 Sep 2019)  Author's response   Manuscript 
ED: Publish as is (23 Oct 2019) by Thorsten Bartels-Rausch
AR by Jon Nelson on behalf of the Authors (11 Nov 2019)  Author's response   Manuscript 
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Short summary
Ice crystals in clouds have a wide variety. But many crystal forms are inexplicable using the common approach of modeling the growth rates normal to the crystal faces. Instead of using only this normal-growth approach, we suggest including lateral facet growth processes. Using such lateral processes, backed up by new experiments, we give explanations for some of these puzzling forms. The forms include the center droxtal in stellar crystals, scrolls, capped columns, sheath bundles, and trigonals.
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