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The Cryosphere An interactive open-access journal of the European Geosciences Union
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TC | Volume 13, issue 5
The Cryosphere, 13, 1495-1511, 2019
https://doi.org/10.5194/tc-13-1495-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
The Cryosphere, 13, 1495-1511, 2019
https://doi.org/10.5194/tc-13-1495-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.

Research article 27 May 2019

Research article | 27 May 2019

Recrystallization processes, microstructure and crystallographic preferred orientation evolution in polycrystalline ice during high-temperature simple shear

Baptiste Journaux et al.
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Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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AR: Author's response | RR: Referee report | ED: Editor decision
AR by Baptiste Journaux on behalf of the Authors (27 Feb 2019)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (07 Mar 2019) by Martin Schneebeli
RR by David Prior (26 Mar 2019)
RR by Jacob Tielke (26 Mar 2019)
ED: Publish subject to minor revisions (review by editor) (02 Apr 2019) by Martin Schneebeli
AR by Baptiste Journaux on behalf of the Authors (09 Apr 2019)  Author's response    Manuscript
ED: Publish as is (19 Apr 2019) by Martin Schneebeli
Publications Copernicus
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Short summary
Ice mechanics is an important tool to better predict the response of glaciers or polar ice sheets to climate variations. Nevertheless our current predictive abilities are limited as the microscale mechanisms responsible for ice creep are poorly identified. We show in this study, using state-of-the-art experimental techniques, which recrystallization processes control ice deformation. This will allow realistic simulations, necessary to predict the long-term effects on ice landmasses.
Ice mechanics is an important tool to better predict the response of glaciers or polar ice...
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