Improved estimation of the bulk ice crystal fabric asymmetry from polarimetric phase co-registration

The bulk crystal orientation in ice influences the flow of glaciers and ice streams. The ice c -axes fabric is most reliably derived from ice cores. Because these are sparse, the spatial and vertical distribution of the fabric in the Greenland and Antarctic ice sheets is largely unknown. In recent y...

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Published in:The Cryosphere
Main Authors: Zeising, Ole, Gerber, Tamara Annina, Eisen, Olaf, Ershadi, M. Reza, Stoll, Nicolas, Weikusat, Ilka, Humbert, Angelika
Format: Text
Language:English
Published: 2023
Subjects:
Online Access:https://doi.org/10.5194/tc-17-1097-2023
https://tc.copernicus.org/articles/17/1097/2023/
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spelling ftcopernicus:oai:publications.copernicus.org:tc106932 2023-05-15T13:31:14+02:00 Improved estimation of the bulk ice crystal fabric asymmetry from polarimetric phase co-registration Zeising, Ole Gerber, Tamara Annina Eisen, Olaf Ershadi, M. Reza Stoll, Nicolas Weikusat, Ilka Humbert, Angelika 2023-03-06 application/pdf https://doi.org/10.5194/tc-17-1097-2023 https://tc.copernicus.org/articles/17/1097/2023/ eng eng doi:10.5194/tc-17-1097-2023 https://tc.copernicus.org/articles/17/1097/2023/ eISSN: 1994-0424 Text 2023 ftcopernicus https://doi.org/10.5194/tc-17-1097-2023 2023-03-13T17:23:11Z The bulk crystal orientation in ice influences the flow of glaciers and ice streams. The ice c -axes fabric is most reliably derived from ice cores. Because these are sparse, the spatial and vertical distribution of the fabric in the Greenland and Antarctic ice sheets is largely unknown. In recent years, methods have been developed to determine fabric characteristics from polarimetric radar measurements. The aim of this paper is to present an improved method to infer the horizontal fabric asymmetry by precisely determining the travel-time difference using co-polarised phase-sensitive radar data. We applied this method to six radar measurements from the East Greenland Ice-core Project (EastGRIP) drill site on Greenland's largest ice stream to give a proof of concept by comparing the results with the horizontal asymmetry of the bulk crystal anisotropy derived from the ice core. This comparison shows an excellent agreement, which is a large improvement compared to previously used methods. Our approach is particularly useful for determining the vertical profile of the fabric asymmetry in higher resolution and over larger depths than was achievable with previous methods, especially in regions with strong asymmetry. Text Antarc* Antarctic East Greenland East Greenland Ice-core Project Greenland Greenland ice core Greenland Ice core Project ice core Copernicus Publications: E-Journals Antarctic Greenland The Cryosphere 17 3 1097 1105
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description The bulk crystal orientation in ice influences the flow of glaciers and ice streams. The ice c -axes fabric is most reliably derived from ice cores. Because these are sparse, the spatial and vertical distribution of the fabric in the Greenland and Antarctic ice sheets is largely unknown. In recent years, methods have been developed to determine fabric characteristics from polarimetric radar measurements. The aim of this paper is to present an improved method to infer the horizontal fabric asymmetry by precisely determining the travel-time difference using co-polarised phase-sensitive radar data. We applied this method to six radar measurements from the East Greenland Ice-core Project (EastGRIP) drill site on Greenland's largest ice stream to give a proof of concept by comparing the results with the horizontal asymmetry of the bulk crystal anisotropy derived from the ice core. This comparison shows an excellent agreement, which is a large improvement compared to previously used methods. Our approach is particularly useful for determining the vertical profile of the fabric asymmetry in higher resolution and over larger depths than was achievable with previous methods, especially in regions with strong asymmetry.
format Text
author Zeising, Ole
Gerber, Tamara Annina
Eisen, Olaf
Ershadi, M. Reza
Stoll, Nicolas
Weikusat, Ilka
Humbert, Angelika
spellingShingle Zeising, Ole
Gerber, Tamara Annina
Eisen, Olaf
Ershadi, M. Reza
Stoll, Nicolas
Weikusat, Ilka
Humbert, Angelika
Improved estimation of the bulk ice crystal fabric asymmetry from polarimetric phase co-registration
author_facet Zeising, Ole
Gerber, Tamara Annina
Eisen, Olaf
Ershadi, M. Reza
Stoll, Nicolas
Weikusat, Ilka
Humbert, Angelika
author_sort Zeising, Ole
title Improved estimation of the bulk ice crystal fabric asymmetry from polarimetric phase co-registration
title_short Improved estimation of the bulk ice crystal fabric asymmetry from polarimetric phase co-registration
title_full Improved estimation of the bulk ice crystal fabric asymmetry from polarimetric phase co-registration
title_fullStr Improved estimation of the bulk ice crystal fabric asymmetry from polarimetric phase co-registration
title_full_unstemmed Improved estimation of the bulk ice crystal fabric asymmetry from polarimetric phase co-registration
title_sort improved estimation of the bulk ice crystal fabric asymmetry from polarimetric phase co-registration
publishDate 2023
url https://doi.org/10.5194/tc-17-1097-2023
https://tc.copernicus.org/articles/17/1097/2023/
geographic Antarctic
Greenland
geographic_facet Antarctic
Greenland
genre Antarc*
Antarctic
East Greenland
East Greenland Ice-core Project
Greenland
Greenland ice core
Greenland Ice core Project
ice core
genre_facet Antarc*
Antarctic
East Greenland
East Greenland Ice-core Project
Greenland
Greenland ice core
Greenland Ice core Project
ice core
op_source eISSN: 1994-0424
op_relation doi:10.5194/tc-17-1097-2023
https://tc.copernicus.org/articles/17/1097/2023/
op_doi https://doi.org/10.5194/tc-17-1097-2023
container_title The Cryosphere
container_volume 17
container_issue 3
container_start_page 1097
op_container_end_page 1105
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