Strongly Depth‐Dependent Ice Fabric in a Fast‐Flowing Antarctic Ice Stream Revealed With Icequake Observations ...

The crystal orientation fabric of glacier ice impacts its strength and flow. Crystal fabric is therefore an important consideration when modeling ice flow. Here, we show that shear-wave splitting (SWS) measured with glacial microseismicity can be used to invert seismic anisotropy and ice fabric, if...

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Main Authors: Kufner, S.-K., Wookey, J., Brisbourne, A. M., Martín, C., Hudson, T. S., Kendall, J. M., Smith, A. M.
Format: Text
Language:English
Published: John Wiley and Sons 2023
Subjects:
Online Access:https://dx.doi.org/10.5445/ir/1000157738
https://publikationen.bibliothek.kit.edu/1000157738
id ftdatacite:10.5445/ir/1000157738
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spelling ftdatacite:10.5445/ir/1000157738 2023-06-11T04:04:07+02:00 Strongly Depth‐Dependent Ice Fabric in a Fast‐Flowing Antarctic Ice Stream Revealed With Icequake Observations ... Kufner, S.-K. Wookey, J. Brisbourne, A. M. Martín, C. Hudson, T. S. Kendall, J. M. Smith, A. M. 2023 https://dx.doi.org/10.5445/ir/1000157738 https://publikationen.bibliothek.kit.edu/1000157738 en eng John Wiley and Sons Creative Commons Namensnennung 4.0 International Embargoed Access info:eu-repo/semantics/embargoedAccess https://creativecommons.org/licenses/by/4.0/deed.de article-journal Text Journal Article ScholarlyArticle 2023 ftdatacite https://doi.org/10.5445/ir/1000157738 2023-05-02T10:22:32Z The crystal orientation fabric of glacier ice impacts its strength and flow. Crystal fabric is therefore an important consideration when modeling ice flow. Here, we show that shear-wave splitting (SWS) measured with glacial microseismicity can be used to invert seismic anisotropy and ice fabric, if represented in a statistical sense. Rutford Ice Stream (RIS) is a fast-flowing Antarctic ice stream, a setting crucial for informing large-scale ice sheet models. We present >200,000 SWS measurements from glacial microseismicity, registered at a 38-station seismic network located ∼40 km upstream of the grounding line. A representative subset of these data is inverted for ice fabric. Due to the character of SWS, which accumulates along the raypath, we include information on the depth structure from radar measurements. We find that the following three-layer configuration fits the data best: a broad vertical cone fabric near the base of RIS (500 m thick), a thick vertical girdle fabric, orientated perpendicular to ... Text Antarc* Antarctic Ice Sheet Ice Stream A Rutford Ice Stream DataCite Metadata Store (German National Library of Science and Technology) Antarctic Rutford ENVELOPE(-85.300,-85.300,-78.600,-78.600) Rutford Ice Stream ENVELOPE(-80.000,-80.000,-79.167,-79.167)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
description The crystal orientation fabric of glacier ice impacts its strength and flow. Crystal fabric is therefore an important consideration when modeling ice flow. Here, we show that shear-wave splitting (SWS) measured with glacial microseismicity can be used to invert seismic anisotropy and ice fabric, if represented in a statistical sense. Rutford Ice Stream (RIS) is a fast-flowing Antarctic ice stream, a setting crucial for informing large-scale ice sheet models. We present >200,000 SWS measurements from glacial microseismicity, registered at a 38-station seismic network located ∼40 km upstream of the grounding line. A representative subset of these data is inverted for ice fabric. Due to the character of SWS, which accumulates along the raypath, we include information on the depth structure from radar measurements. We find that the following three-layer configuration fits the data best: a broad vertical cone fabric near the base of RIS (500 m thick), a thick vertical girdle fabric, orientated perpendicular to ...
format Text
author Kufner, S.-K.
Wookey, J.
Brisbourne, A. M.
Martín, C.
Hudson, T. S.
Kendall, J. M.
Smith, A. M.
spellingShingle Kufner, S.-K.
Wookey, J.
Brisbourne, A. M.
Martín, C.
Hudson, T. S.
Kendall, J. M.
Smith, A. M.
Strongly Depth‐Dependent Ice Fabric in a Fast‐Flowing Antarctic Ice Stream Revealed With Icequake Observations ...
author_facet Kufner, S.-K.
Wookey, J.
Brisbourne, A. M.
Martín, C.
Hudson, T. S.
Kendall, J. M.
Smith, A. M.
author_sort Kufner, S.-K.
title Strongly Depth‐Dependent Ice Fabric in a Fast‐Flowing Antarctic Ice Stream Revealed With Icequake Observations ...
title_short Strongly Depth‐Dependent Ice Fabric in a Fast‐Flowing Antarctic Ice Stream Revealed With Icequake Observations ...
title_full Strongly Depth‐Dependent Ice Fabric in a Fast‐Flowing Antarctic Ice Stream Revealed With Icequake Observations ...
title_fullStr Strongly Depth‐Dependent Ice Fabric in a Fast‐Flowing Antarctic Ice Stream Revealed With Icequake Observations ...
title_full_unstemmed Strongly Depth‐Dependent Ice Fabric in a Fast‐Flowing Antarctic Ice Stream Revealed With Icequake Observations ...
title_sort strongly depth‐dependent ice fabric in a fast‐flowing antarctic ice stream revealed with icequake observations ...
publisher John Wiley and Sons
publishDate 2023
url https://dx.doi.org/10.5445/ir/1000157738
https://publikationen.bibliothek.kit.edu/1000157738
long_lat ENVELOPE(-85.300,-85.300,-78.600,-78.600)
ENVELOPE(-80.000,-80.000,-79.167,-79.167)
geographic Antarctic
Rutford
Rutford Ice Stream
geographic_facet Antarctic
Rutford
Rutford Ice Stream
genre Antarc*
Antarctic
Ice Sheet
Ice Stream A
Rutford Ice Stream
genre_facet Antarc*
Antarctic
Ice Sheet
Ice Stream A
Rutford Ice Stream
op_rights Creative Commons Namensnennung 4.0 International
Embargoed Access
info:eu-repo/semantics/embargoedAccess
https://creativecommons.org/licenses/by/4.0/deed.de
op_doi https://doi.org/10.5445/ir/1000157738
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