Articles | Volume 18, issue 4
https://doi.org/10.5194/tc-18-1653-2024
https://doi.org/10.5194/tc-18-1653-2024
Research article
 | 
09 Apr 2024
Research article |  | 09 Apr 2024

A rigorous approach to the specific surface area evolution in snow during temperature gradient metamorphism

Anna Braun, Kévin Fourteau, and Henning Löwe

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Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on egusphere-2023-1947', Z.R. Courville, 12 Oct 2023
    • AC2: 'Reply on RC1', Anna Braun, 22 Dec 2023
  • RC2: 'Comment on egusphere-2023-1947', Thomas Kaempfer, 16 Oct 2023
    • AC1: 'Reply on RC2', Anna Braun, 22 Dec 2023

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
ED: Publish subject to revisions (further review by editor and referees) (04 Jan 2024) by Masashi Niwano
AR by Anna Braun on behalf of the Authors (17 Jan 2024)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (19 Jan 2024) by Masashi Niwano
RR by Thomas Kaempfer (23 Jan 2024)
ED: Publish subject to minor revisions (review by editor) (09 Feb 2024) by Masashi Niwano
AR by Anna Braun on behalf of the Authors (16 Feb 2024)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (26 Feb 2024) by Masashi Niwano
AR by Anna Braun on behalf of the Authors (06 Mar 2024)  Manuscript 
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Short summary
The specific surface of snow dictates key physical properties and continuously evolves in natural snowpacks. This is referred to as metamorphism. This work develops a rigorous physical model for this evolution, which is able to reproduce X-ray tomography measurements without using unphysical tuning parameters. Our results emphasize that snow crystal growth at the micrometer scale ultimately controls the pace of metamorphism.