Crystallographic analysis of temperate ice on Rhonegletscher, Swiss Alps ...

Crystal orientation fabric (COF) analysis provides information about the c-axis orientation of ice grains and the associated anisotropy and microstructural information about deformation and recrystallisation processes within the glacier. This information can be used to introduce modules that fully d...

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Main Authors: Hellmann, Sebastian, Kerch, Johanna, Weikusat, Ilka, Bauder, Andreas, Grab, Melchior, Jouvet, Guillaume, Schwikowski, Margit, Maurer, Hansruedi
Format: Article in Journal/Newspaper
Language:English
Published: ETH Zurich 2021
Subjects:
Online Access:https://dx.doi.org/10.3929/ethz-b-000474292
http://hdl.handle.net/20.500.11850/474292
id ftdatacite:10.3929/ethz-b-000474292
record_format openpolar
spelling ftdatacite:10.3929/ethz-b-000474292 2024-04-28T08:24:16+00:00 Crystallographic analysis of temperate ice on Rhonegletscher, Swiss Alps ... Hellmann, Sebastian Kerch, Johanna Weikusat, Ilka Bauder, Andreas Grab, Melchior Jouvet, Guillaume Schwikowski, Margit Maurer, Hansruedi 2021 application/pdf https://dx.doi.org/10.3929/ethz-b-000474292 http://hdl.handle.net/20.500.11850/474292 en eng ETH Zurich info:eu-repo/semantics/openAccess Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 article-journal Text ScholarlyArticle Journal Article 2021 ftdatacite https://doi.org/10.3929/ethz-b-000474292 2024-04-02T12:34:54Z Crystal orientation fabric (COF) analysis provides information about the c-axis orientation of ice grains and the associated anisotropy and microstructural information about deformation and recrystallisation processes within the glacier. This information can be used to introduce modules that fully describe the microstructural anisotropy or at least direction-dependent enhancement factors for glacier modelling. The COF was studied at an ice core that was obtained from the temperate Rhonegletscher, located in the central Swiss Alps. Seven samples, extracted at depths between 2 and 79 m, were analysed with an automatic fabric analyser. The COF analysis revealed conspicuous four-maxima patterns of the c-axis orientations at all depths. Additional data, such as microstructural images, produced during the ice sample preparation process, were considered to interpret these patterns. Furthermore, repeated high-precision global navigation satellite system (GNSS) surveying allowed the local glacier flow direction to be ... : The Cryosphere, 15 (2) ... Article in Journal/Newspaper ice core DataCite Metadata Store (German National Library of Science and Technology)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
description Crystal orientation fabric (COF) analysis provides information about the c-axis orientation of ice grains and the associated anisotropy and microstructural information about deformation and recrystallisation processes within the glacier. This information can be used to introduce modules that fully describe the microstructural anisotropy or at least direction-dependent enhancement factors for glacier modelling. The COF was studied at an ice core that was obtained from the temperate Rhonegletscher, located in the central Swiss Alps. Seven samples, extracted at depths between 2 and 79 m, were analysed with an automatic fabric analyser. The COF analysis revealed conspicuous four-maxima patterns of the c-axis orientations at all depths. Additional data, such as microstructural images, produced during the ice sample preparation process, were considered to interpret these patterns. Furthermore, repeated high-precision global navigation satellite system (GNSS) surveying allowed the local glacier flow direction to be ... : The Cryosphere, 15 (2) ...
format Article in Journal/Newspaper
author Hellmann, Sebastian
Kerch, Johanna
Weikusat, Ilka
Bauder, Andreas
Grab, Melchior
Jouvet, Guillaume
Schwikowski, Margit
Maurer, Hansruedi
spellingShingle Hellmann, Sebastian
Kerch, Johanna
Weikusat, Ilka
Bauder, Andreas
Grab, Melchior
Jouvet, Guillaume
Schwikowski, Margit
Maurer, Hansruedi
Crystallographic analysis of temperate ice on Rhonegletscher, Swiss Alps ...
author_facet Hellmann, Sebastian
Kerch, Johanna
Weikusat, Ilka
Bauder, Andreas
Grab, Melchior
Jouvet, Guillaume
Schwikowski, Margit
Maurer, Hansruedi
author_sort Hellmann, Sebastian
title Crystallographic analysis of temperate ice on Rhonegletscher, Swiss Alps ...
title_short Crystallographic analysis of temperate ice on Rhonegletscher, Swiss Alps ...
title_full Crystallographic analysis of temperate ice on Rhonegletscher, Swiss Alps ...
title_fullStr Crystallographic analysis of temperate ice on Rhonegletscher, Swiss Alps ...
title_full_unstemmed Crystallographic analysis of temperate ice on Rhonegletscher, Swiss Alps ...
title_sort crystallographic analysis of temperate ice on rhonegletscher, swiss alps ...
publisher ETH Zurich
publishDate 2021
url https://dx.doi.org/10.3929/ethz-b-000474292
http://hdl.handle.net/20.500.11850/474292
genre ice core
genre_facet ice core
op_rights info:eu-repo/semantics/openAccess
Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
cc-by-4.0
op_doi https://doi.org/10.3929/ethz-b-000474292
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