Articles | Volume 19, issue 12
https://doi.org/10.5194/tc-19-6943-2025
https://doi.org/10.5194/tc-19-6943-2025
Research article
 | 
19 Dec 2025
Research article |  | 19 Dec 2025

A unified framework for large-scale fabric evolution models and anisotropic rheologies

Daniel H. Richards, Elisa Mantelli, Samuel S. Pegler, and Sandra Piazolo

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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
ED: Publish subject to revisions (further review by editor and referees) (08 Apr 2025) by Kaitlin Keegan
AR by Daniel Richards on behalf of the Authors (02 Jun 2025)  Author's response   Author's tracked changes   Manuscript 
ED: Publish subject to minor revisions (review by editor) (16 Oct 2025) by Kaitlin Keegan
AR by Daniel Richards on behalf of the Authors (17 Oct 2025)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (21 Oct 2025) by Kaitlin Keegan
AR by Daniel Richards on behalf of the Authors (22 Oct 2025)  Author's response   Manuscript 
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Short summary
Ice behaves differently depending on its crystal orientation, but how this affects its flow is unclear. We combine a range of previous models into a common equation to better understand crystal alignment. We tested a range of previous models on ice streams and divides, discovering that the best fit to observations comes from (a) assuming neighbouring crystals have the same stress, and (b) through describing the effect of crystal orientation on the flow in a way that allows directional variation.
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