Preprints
https://doi.org/10.5194/egusphere-2024-2519
https://doi.org/10.5194/egusphere-2024-2519
09 Sep 2024
 | 09 Sep 2024

Brief communication: Reduced bandwidth improves the depth limit of the radar coherence method for detecting ice crystal fabric asymmetry

Ole Zeising, Álvaro Arenas-Pingarrón, Alex M. Brisbourne, and Carlos Martín

Abstract. Ice crystal orientation fabric strongly affects the viscous deformation of glacier ice. A popular technique to investigate ice fabric is radar polarimetry, often analysed using the coherence method. However, in fast-flowing areas with strong anisotropy, this method provides information of shallow areas below the surface only. This study proposes reducing radar bandwidth to enhance the depth limit for fabric asymmetry detection. Using data from two ice streams, we demonstrate that reduced bandwidth significantly increases the depth limit, depending on the centre frequency. This approach aims to improve the understanding of the spatial distribution of fabric, crucial for ice dynamics in fast-flowing regions.

Competing interests: At least one of the (co-)authors is a member of the editorial board of The Cryosphere. The peer-review process was guided by an independent editor, and the authors also have no other competing interests to declare.

Publisher's note: Copernicus Publications remains neutral with regard to jurisdictional claims made in the text, published maps, institutional affiliations, or any other geographical representation in this preprint. The responsibility to include appropriate place names lies with the authors.
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Journal article(s) based on this preprint

02 Jul 2025
Brief communication: Reduced bandwidth improves the depth limit of the radar coherence method for detecting ice crystal fabric asymmetry
Ole Zeising, Álvaro Arenas-Pingarrón, Alex M. Brisbourne, and Carlos Martín
The Cryosphere, 19, 2355–2363, https://doi.org/10.5194/tc-19-2355-2025,https://doi.org/10.5194/tc-19-2355-2025, 2025
Short summary
Ole Zeising, Álvaro Arenas-Pingarrón, Alex M. Brisbourne, and Carlos Martín

Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on egusphere-2024-2519', Anonymous Referee #1, 21 Oct 2024
    • AC1: 'Reply on RC1', Ole Zeising, 09 Jan 2025
  • RC2: 'Comment on egusphere-2024-2519', John Paden, 06 Dec 2024
    • AC2: 'Reply on RC2', Ole Zeising, 09 Jan 2025

Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on egusphere-2024-2519', Anonymous Referee #1, 21 Oct 2024
    • AC1: 'Reply on RC1', Ole Zeising, 09 Jan 2025
  • RC2: 'Comment on egusphere-2024-2519', John Paden, 06 Dec 2024
    • AC2: 'Reply on RC2', Ole Zeising, 09 Jan 2025

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
ED: Publish subject to minor revisions (review by editor) (03 Feb 2025) by Huw Horgan
AR by Ole Zeising on behalf of the Authors (13 Feb 2025)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (09 Apr 2025) by Huw Horgan
AR by Ole Zeising on behalf of the Authors (10 Apr 2025)  Manuscript 

Journal article(s) based on this preprint

02 Jul 2025
Brief communication: Reduced bandwidth improves the depth limit of the radar coherence method for detecting ice crystal fabric asymmetry
Ole Zeising, Álvaro Arenas-Pingarrón, Alex M. Brisbourne, and Carlos Martín
The Cryosphere, 19, 2355–2363, https://doi.org/10.5194/tc-19-2355-2025,https://doi.org/10.5194/tc-19-2355-2025, 2025
Short summary
Ole Zeising, Álvaro Arenas-Pingarrón, Alex M. Brisbourne, and Carlos Martín

Data sets

Polarimetric phase-sensitive radar measurements at EastGRIP drill site, 2019 Ole Zeising and Angelika Humbert https://doi.org/10.1594/PANGAEA.951267

Crystal c-axes (fabric analyser G50) of ice core samples (vertical thin sections) collected from the polar ice core EGRIP, 111-1714 m depth Ilka Weikusat, Nicolas Stoll, Johanna Kerch, Jan Eichler, Daniela Jansen, and Sepp Kipfstuhl https://doi.org/10.1594/PANGAEA.949248

Radar characterization of ice crystal orientation fabric and anisotropic rheology within Rutford Ice Stream, 2017-2019 T. Jordan, C. Martín, A. Brisbourne, D. Schroeder, and A. Smith https://doi.org/10.5285/D5B7E5A1-B04D-48D8-A440-C010658EC146

Ole Zeising, Álvaro Arenas-Pingarrón, Alex M. Brisbourne, and Carlos Martín

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Latest update: 02 Jul 2025
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Short summary
Ice crystal orientation influence how glacier ice deforms. Radar polarimetry is commonly used to study the bulk ice crystal orientation, but the often used coherence method only provides information of the shallow ice in fast-flowing areas. This study shows that reducing the bandwidth of high-bandwidth radar data significantly enhances the depth limit of the coherence method. This improvement helps us to better understand ice dynamics in fast-flowing ice streams.
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