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: O. Zeising, T. A. Gerber, O. Eisen, M. R. Ershadi, N. Stoll, I. Weikusat, A. Humbert
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2023
Subjects:
Online Access:https://doi.org/10.5194/tc-17-1097-2023
https://doaj.org/article/5b622539651046e793936e3aaa03c8eb
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spelling ftdoajarticles:oai:doaj.org/article:5b622539651046e793936e3aaa03c8eb 2023-05-15T14:13:30+02:00 Improved estimation of the bulk ice crystal fabric asymmetry from polarimetric phase co-registration O. Zeising T. A. Gerber O. Eisen M. R. Ershadi N. Stoll I. Weikusat A. Humbert 2023-03-01T00:00:00Z https://doi.org/10.5194/tc-17-1097-2023 https://doaj.org/article/5b622539651046e793936e3aaa03c8eb EN eng Copernicus Publications https://tc.copernicus.org/articles/17/1097/2023/tc-17-1097-2023.pdf https://doaj.org/toc/1994-0416 https://doaj.org/toc/1994-0424 doi:10.5194/tc-17-1097-2023 1994-0416 1994-0424 https://doaj.org/article/5b622539651046e793936e3aaa03c8eb The Cryosphere, Vol 17, Pp 1097-1105 (2023) Environmental sciences GE1-350 Geology QE1-996.5 article 2023 ftdoajarticles https://doi.org/10.5194/tc-17-1097-2023 2023-03-12T01:34:33Z 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. Article in Journal/Newspaper Antarc* Antarctic East Greenland East Greenland Ice-core Project Greenland Greenland ice core Greenland Ice core Project ice core The Cryosphere Directory of Open Access Journals: DOAJ Articles Antarctic Greenland The Cryosphere 17 3 1097 1105
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Environmental sciences
GE1-350
Geology
QE1-996.5
spellingShingle Environmental sciences
GE1-350
Geology
QE1-996.5
O. Zeising
T. A. Gerber
O. Eisen
M. R. Ershadi
N. Stoll
I. Weikusat
A. Humbert
Improved estimation of the bulk ice crystal fabric asymmetry from polarimetric phase co-registration
topic_facet Environmental sciences
GE1-350
Geology
QE1-996.5
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 Article in Journal/Newspaper
author O. Zeising
T. A. Gerber
O. Eisen
M. R. Ershadi
N. Stoll
I. Weikusat
A. Humbert
author_facet O. Zeising
T. A. Gerber
O. Eisen
M. R. Ershadi
N. Stoll
I. Weikusat
A. Humbert
author_sort O. Zeising
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
publisher Copernicus Publications
publishDate 2023
url https://doi.org/10.5194/tc-17-1097-2023
https://doaj.org/article/5b622539651046e793936e3aaa03c8eb
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
The Cryosphere
genre_facet Antarc*
Antarctic
East Greenland
East Greenland Ice-core Project
Greenland
Greenland ice core
Greenland Ice core Project
ice core
The Cryosphere
op_source The Cryosphere, Vol 17, Pp 1097-1105 (2023)
op_relation https://tc.copernicus.org/articles/17/1097/2023/tc-17-1097-2023.pdf
https://doaj.org/toc/1994-0416
https://doaj.org/toc/1994-0424
doi:10.5194/tc-17-1097-2023
1994-0416
1994-0424
https://doaj.org/article/5b622539651046e793936e3aaa03c8eb
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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