Articles | Volume 16, issue 5
https://doi.org/10.5194/tc-16-2009-2022
https://doi.org/10.5194/tc-16-2009-2022
Research article
 | 
25 May 2022
Research article |  | 25 May 2022

Can changes in deformation regimes be inferred from crystallographic preferred orientations in polar ice?

Maria-Gema Llorens, Albert Griera, Paul D. Bons, Ilka Weikusat, David J. Prior, Enrique Gomez-Rivas, Tamara de Riese, Ivone Jimenez-Munt, Daniel García-Castellanos, and Ricardo A. Lebensohn

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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 tc-2021-224', Anonymous Referee #1, 06 Oct 2021
  • RC2: 'Comment on tc-2021-224', Chris Wilson, 08 Oct 2021
  • EC1: 'Inappropriate tone and language RC2', Nanna Bjørnholt Karlsson, 08 Oct 2021
  • RC3: 'Comment on tc-2021-224', Anonymous Referee #3, 04 Nov 2021

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) (06 Jan 2022) by Nanna Bjørnholt Karlsson
AR by Maria-Gema Llorens on behalf of the Authors (17 Feb 2022)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (28 Feb 2022) by Nanna Bjørnholt Karlsson
RR by Christine McCarthy (04 Mar 2022)
RR by Anonymous Referee #1 (07 Mar 2022)
ED: Publish subject to minor revisions (review by editor) (23 Mar 2022) by Nanna Bjørnholt Karlsson
AR by Maria-Gema Llorens on behalf of the Authors (08 Apr 2022)  Author's response   Author's tracked changes   Manuscript 
ED: Publish subject to technical corrections (25 Apr 2022) by Nanna Bjørnholt Karlsson
AR by Maria-Gema Llorens on behalf of the Authors (25 Apr 2022)  Manuscript 
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Short summary
Polar ice is formed by ice crystals, which form fabrics that are utilised to interpret how ice sheets flow. It is unclear whether fabrics result from the current flow regime or if they are inherited. To understand the extent to which ice crystals can be reoriented when ice flow conditions change, we simulate and evaluate multi-stage ice flow scenarios according to natural cases. We find that second deformation regimes normally overprint inherited fabrics, with a range of transitional fabrics.