Articles | Volume 16, issue 5
https://doi.org/10.5194/tc-16-2009-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/tc-16-2009-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
25 May 2022
Research article |
| 25 May 2022
| 25 May 2022
Can changes in deformation regimes be inferred from crystallographic preferred orientations in polar ice?
Maria-Gema Llorens
CORRESPONDING AUTHOR
Geosciencies Barcelona CSIC, Lluis Sole i Sabaris s/n, 08028
Barcelona, Spain
Albert Griera
Departament de Geologia, Universitat Autònoma de Barcelona, 08193
Cerdanyola del Vallès, Barcelona, Spain
Paul D. Bons
Department of Geosciences, Eberhard Karls University Tübingen,
Wilhemstr. 56, 72074 Tübingen, Germany
School of Earth Sciences and Resources, China University of Geosciences, Beijing, China
Ilka Weikusat
Department of Geosciences, Eberhard Karls University Tübingen,
Wilhemstr. 56, 72074 Tübingen, Germany
Alfred Wegener Institute Helmholtz Centre for Polar and Marine
Research, Bremerhaven, Germany
David J. Prior
Department of Geology, University of Otago, 362 Leith Street,
Dunedin 9016, New Zealand
Enrique Gomez-Rivas
Departament de Mineralogia, Petrologia i Geologia Aplicada,
Facultat de Ciències de la Terra, Universitat de Barcelona, Martí i
Franquès s/n, 08028 Barcelona, Spain
Tamara de Riese
Department of Geosciences, Eberhard Karls University Tübingen,
Wilhemstr. 56, 72074 Tübingen, Germany
Ivone Jimenez-Munt
Geosciencies Barcelona CSIC, Lluis Sole i Sabaris s/n, 08028
Barcelona, Spain
Daniel García-Castellanos
Geosciencies Barcelona CSIC, Lluis Sole i Sabaris s/n, 08028
Barcelona, Spain
Ricardo A. Lebensohn
Theoretical Division, Los Alamos National Laboratory, Los Alamos,
NM, 87545, USA
Viewed
Total article views: 3,410 (including HTML, PDF, and XML)
Cumulative views and downloads
(calculated since 17 Sep 2021)
| HTML | XML | Total | Supplement | BibTeX | EndNote | |
|---|---|---|---|---|---|---|
| 2,556 | 758 | 96 | 3,410 | 78 | 77 | 81 |
- HTML: 2,556
- PDF: 758
- XML: 96
- Total: 3,410
- Supplement: 78
- BibTeX: 77
- EndNote: 81
Total article views: 1,777 (including HTML, PDF, and XML)
Cumulative views and downloads
(calculated since 25 May 2022)
| HTML | XML | Total | Supplement | BibTeX | EndNote | |
|---|---|---|---|---|---|---|
| 1,356 | 355 | 66 | 1,777 | 78 | 51 | 54 |
- HTML: 1,356
- PDF: 355
- XML: 66
- Total: 1,777
- Supplement: 78
- BibTeX: 51
- EndNote: 54
Total article views: 1,633 (including HTML, PDF, and XML)
Cumulative views and downloads
(calculated since 17 Sep 2021)
| HTML | XML | Total | BibTeX | EndNote | |
|---|---|---|---|---|---|
| 1,200 | 403 | 30 | 1,633 | 26 | 27 |
- HTML: 1,200
- PDF: 403
- XML: 30
- Total: 1,633
- BibTeX: 26
- EndNote: 27
Viewed (geographical distribution)
Total article views: 3,410 (including HTML, PDF, and XML)
Thereof 3,146 with geography defined
and 264 with unknown origin.
Total article views: 1,777 (including HTML, PDF, and XML)
Thereof 1,643 with geography defined
and 134 with unknown origin.
Total article views: 1,633 (including HTML, PDF, and XML)
Thereof 1,503 with geography defined
and 130 with unknown origin.
| Country | # | Views | % |
|---|
| Country | # | Views | % |
|---|
| Country | # | Views | % |
|---|
| Total: | 0 |
| HTML: | 0 |
| PDF: | 0 |
| XML: | 0 |
- 1
1
| Total: | 0 |
| HTML: | 0 |
| PDF: | 0 |
| XML: | 0 |
- 1
1
| Total: | 0 |
| HTML: | 0 |
| PDF: | 0 |
| XML: | 0 |
- 1
1
Cited
8 citations as recorded by crossref.
- Firn on ice sheets C. Amory et al. 10.1038/s43017-023-00507-9
- Microstructure-sensitive crystal plasticity and phase-field modeling of deformation and fracture in polycrystalline ice S. Motahari et al. 10.1016/j.actamat.2024.120512
- The influence of kinematics of deformation on polycrystalline halite dynamic recrystallization: Full-field simulation of simple shear versus pure shear B. Hao et al. 10.1016/j.jsg.2025.105424
- Progresses in studies on crystallographic preferred orientations in experimentally deformed ice Q. WANG & C. QI 10.3724/j.issn.1007-2802.20240103
- Bridging the Gap Between Experimental and Natural Fabrics: Modeling Ice Stream Fabric Evolution and its Comparison With Ice‐Core Data D. Richards et al. 10.1029/2023JB027245
- Icequakes and Large Shear Wave Velocity Drop in the Kuoqionggangri Glacier of Tibetan Plateau Observed with Fiber Optic Seismometer Array Y. Li et al. 10.3390/rs15051282
- Crystal orientation fabric anisotropy causes directional hardening of the Northeast Greenland Ice Stream T. Gerber et al. 10.1038/s41467-023-38139-8
- On the Limitations of Using Polarimetric Radar Sounding to Infer the Crystal Orientation Fabric of Ice Masses N. Rathmann et al. 10.1029/2021GL096244
7 citations as recorded by crossref.
- Firn on ice sheets C. Amory et al. 10.1038/s43017-023-00507-9
- Microstructure-sensitive crystal plasticity and phase-field modeling of deformation and fracture in polycrystalline ice S. Motahari et al. 10.1016/j.actamat.2024.120512
- The influence of kinematics of deformation on polycrystalline halite dynamic recrystallization: Full-field simulation of simple shear versus pure shear B. Hao et al. 10.1016/j.jsg.2025.105424
- Progresses in studies on crystallographic preferred orientations in experimentally deformed ice Q. WANG & C. QI 10.3724/j.issn.1007-2802.20240103
- Bridging the Gap Between Experimental and Natural Fabrics: Modeling Ice Stream Fabric Evolution and its Comparison With Ice‐Core Data D. Richards et al. 10.1029/2023JB027245
- Icequakes and Large Shear Wave Velocity Drop in the Kuoqionggangri Glacier of Tibetan Plateau Observed with Fiber Optic Seismometer Array Y. Li et al. 10.3390/rs15051282
- Crystal orientation fabric anisotropy causes directional hardening of the Northeast Greenland Ice Stream T. Gerber et al. 10.1038/s41467-023-38139-8
Latest update: 23 Apr 2025
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.
Polar ice is formed by ice crystals, which form fabrics that are utilised to interpret how ice...
