Articles | Volume 16, issue 5
https://doi.org/10.5194/tc-16-1719-2022
© 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-16-1719-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
06 May 2022
Research article |
| 06 May 2022
| 06 May 2022
Polarimetric radar reveals the spatial distribution of ice fabric at domes and divides in East Antarctica
M. Reza Ershadi
CORRESPONDING AUTHOR
Department of Geosciences, University of Tübingen, Tübingen, Germany
Reinhard Drews
Department of Geosciences, University of Tübingen, Tübingen, Germany
Carlos Martín
British Antarctic Survey, Natural Environment Research Council, Cambridge, UK
Olaf Eisen
Glaciology, Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven, Germany
Department of Geosciences, University of Bremen, Bremen, Germany
Catherine Ritz
IGE, Univ. Grenoble Alpes, CNRS, IRD, Grenoble INP, 38000 Grenoble, France
Hugh Corr
British Antarctic Survey, Natural Environment Research Council, Cambridge, UK
Julia Christmann
Glaciology, Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven, Germany
Institute of Applied Mechanics, University of Kaiserslautern, Kaiserslautern, Germany
Ole Zeising
Glaciology, Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven, Germany
Department of Geosciences, University of Bremen, Bremen, Germany
Angelika Humbert
Glaciology, Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven, Germany
Department of Geosciences, University of Bremen, Bremen, Germany
Robert Mulvaney
British Antarctic Survey, Natural Environment Research Council, Cambridge, UK
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Cited
13 citations as recorded by crossref.
- Simulating higher-order fabric structure in a coupled, anisotropic ice-flow model: application to Dome C D. Lilien et al. 10.1017/jog.2023.78
- ISMIP-HOM benchmark experiments using Underworld T. Sachau et al. 10.5194/gmd-15-8749-2022
- Improved estimation of the bulk ice crystal fabric asymmetry from polarimetric phase co-registration O. Zeising et al. 10.5194/tc-17-1097-2023
- Ultrasonic and seismic constraints on crystallographic preferred orientations of the Priestley Glacier shear margin, Antarctica F. Lutz et al. 10.5194/tc-16-3313-2022
- A newly digitized ice-penetrating radar data set acquired over the Greenland ice sheet in 1971–1979 N. Karlsson et al. 10.5194/essd-16-3333-2024
- Crystal orientation fabric anisotropy causes directional hardening of the Northeast Greenland Ice Stream T. Gerber et al. 10.1038/s41467-023-38139-8
- Multimaxima crystallographic fabrics (CPO) in warm, coarse-grained ice: New insights M. Disbrow-Monz et al. 10.1016/j.jsg.2024.105107
- Autonomous Rover Enables Radar Profiling of Ice-Fabric Properties in Antarctica M. Ershadi et al. 10.1109/TGRS.2024.3394594
- Paths forward in radioglaciology D. Schroeder 10.1017/aog.2023.3
- Radar Characterization of Ice Crystal Orientation Fabric and Anisotropic Viscosity Within an Antarctic Ice Stream T. Jordan et al. 10.1029/2022JF006673
- Rapid and accurate polarimetric radar measurements of ice crystal fabric orientation at the Western Antarctic Ice Sheet (WAIS) Divide ice core site T. Young et al. 10.5194/tc-15-4117-2021
- On the Limitations of Using Polarimetric Radar Sounding to Infer the Crystal Orientation Fabric of Ice Masses N. Rathmann et al. 10.1029/2021GL096244
- Inferring Ice Fabric From Birefringence Loss in Airborne Radargrams: Application to the Eastern Shear Margin of Thwaites Glacier, West Antarctica T. Young et al. 10.1029/2020JF006023
9 citations as recorded by crossref.
- Simulating higher-order fabric structure in a coupled, anisotropic ice-flow model: application to Dome C D. Lilien et al. 10.1017/jog.2023.78
- ISMIP-HOM benchmark experiments using Underworld T. Sachau et al. 10.5194/gmd-15-8749-2022
- Improved estimation of the bulk ice crystal fabric asymmetry from polarimetric phase co-registration O. Zeising et al. 10.5194/tc-17-1097-2023
- Ultrasonic and seismic constraints on crystallographic preferred orientations of the Priestley Glacier shear margin, Antarctica F. Lutz et al. 10.5194/tc-16-3313-2022
- A newly digitized ice-penetrating radar data set acquired over the Greenland ice sheet in 1971–1979 N. Karlsson et al. 10.5194/essd-16-3333-2024
- Crystal orientation fabric anisotropy causes directional hardening of the Northeast Greenland Ice Stream T. Gerber et al. 10.1038/s41467-023-38139-8
- Multimaxima crystallographic fabrics (CPO) in warm, coarse-grained ice: New insights M. Disbrow-Monz et al. 10.1016/j.jsg.2024.105107
- Autonomous Rover Enables Radar Profiling of Ice-Fabric Properties in Antarctica M. Ershadi et al. 10.1109/TGRS.2024.3394594
- Paths forward in radioglaciology D. Schroeder 10.1017/aog.2023.3
4 citations as recorded by crossref.
- Radar Characterization of Ice Crystal Orientation Fabric and Anisotropic Viscosity Within an Antarctic Ice Stream T. Jordan et al. 10.1029/2022JF006673
- Rapid and accurate polarimetric radar measurements of ice crystal fabric orientation at the Western Antarctic Ice Sheet (WAIS) Divide ice core site T. Young et al. 10.5194/tc-15-4117-2021
- On the Limitations of Using Polarimetric Radar Sounding to Infer the Crystal Orientation Fabric of Ice Masses N. Rathmann et al. 10.1029/2021GL096244
- Inferring Ice Fabric From Birefringence Loss in Airborne Radargrams: Application to the Eastern Shear Margin of Thwaites Glacier, West Antarctica T. Young et al. 10.1029/2020JF006023
Latest update: 26 Jul 2024
Short summary
Radio waves transmitted through ice split up and inform us about the ice sheet interior and orientation of single ice crystals. This can be used to infer how ice flows and improve projections on how it will evolve in the future. Here we used an inverse approach and developed a new algorithm to infer ice properties from observed radar data. We applied this technique to the radar data obtained at two EPICA drilling sites, where ice cores were used to validate our results.
Radio waves transmitted through ice split up and inform us about the ice sheet interior and...
