Crystal-orientation fabric variations on the sub-metre scale in cold Alpine ice
The macroscopic flow of a glacier is substantially influenced by the plastic anisotropy of individual ice crystals on the microscale. A preferred crystal orientation fabric (COF) develops with depth in a glacier and is subjected to the influence of the temperature, deformation and recrystallisation...
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ftawi:oai:epic.awi.de:45499 2024-09-15T18:11:58+00:00 Crystal-orientation fabric variations on the sub-metre scale in cold Alpine ice Kerch, Johanna Weikusat, Ilka Diez, Anja Bohleber, Pascal Eisen, Olaf 2017-02-13 https://epic.awi.de/id/eprint/45499/ https://hdl.handle.net/10013/epic.51615 unknown Kerch, J. orcid:0000-0002-7200-6837 , Weikusat, I. orcid:0000-0002-3023-6036 , Diez, A. , Bohleber, P. and Eisen, O. orcid:0000-0002-6380-962X (2017) Crystal-orientation fabric variations on the sub-metre scale in cold Alpine ice , International Symposium on the Cryosphere in a Changing Climate, Wellington, Neuseeland, 12 February 2017 - 17 February 2017 . hdl:10013/epic.51615 EPIC3International Symposium on the Cryosphere in a Changing Climate, Wellington, Neuseeland, 2017-02-12-2017-02-17 Conference notRev 2017 ftawi 2024-06-24T04:18:50Z The macroscopic flow of a glacier is substantially influenced by the plastic anisotropy of individual ice crystals on the microscale. A preferred crystal orientation fabric (COF) develops with depth in a glacier and is subjected to the influence of the temperature, deformation and recrystallisation regime as well as the climate-dependent impurity load in the ice. Detailed knowledge about the crystal anisotropy in a glacier is thus required to better constrain the response of ice sheets in a changing climate. While the gradual change in anisotropy on a large scale of tens to hundreds of metres can mostly be explained, this is not the case for changes in the anisotropic fabric on a shorter scale of centimetres to decimetres. It is therefore essential to improve the understanding of how and why the anisotropic COF changes on a sub-metre scale in a glacier. Fabric data from an ice core of 72 m length, drilled at the high-altitude Alpine site Colle Gnifetti in Switzerland, were measured in continuously sampled sections of ca. 1 m length, covering 10 % of the entire core length. The eigenvalues of the second-order orientation tensor describing the distribution of crystal axes were analysed in high-resolution together with impurity data from meltwater analysis. It is found that the fabric anisotropy exhibits a strong variability on the short scale in all depths of the ice core with extreme eigenvalue differences within one metre of up to 0.2, often associated with small- or large-grained layers. The observation of a clear connection between the grain size variation and the impurity content leads to the conclusion that the influence of impurities on short-scale fabric variations is partially conveyed by the impurity-controlled grain size in combination with the local deformation regime. Conference Object ice core The Cryosphere Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) |
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Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) |
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ftawi |
language |
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description |
The macroscopic flow of a glacier is substantially influenced by the plastic anisotropy of individual ice crystals on the microscale. A preferred crystal orientation fabric (COF) develops with depth in a glacier and is subjected to the influence of the temperature, deformation and recrystallisation regime as well as the climate-dependent impurity load in the ice. Detailed knowledge about the crystal anisotropy in a glacier is thus required to better constrain the response of ice sheets in a changing climate. While the gradual change in anisotropy on a large scale of tens to hundreds of metres can mostly be explained, this is not the case for changes in the anisotropic fabric on a shorter scale of centimetres to decimetres. It is therefore essential to improve the understanding of how and why the anisotropic COF changes on a sub-metre scale in a glacier. Fabric data from an ice core of 72 m length, drilled at the high-altitude Alpine site Colle Gnifetti in Switzerland, were measured in continuously sampled sections of ca. 1 m length, covering 10 % of the entire core length. The eigenvalues of the second-order orientation tensor describing the distribution of crystal axes were analysed in high-resolution together with impurity data from meltwater analysis. It is found that the fabric anisotropy exhibits a strong variability on the short scale in all depths of the ice core with extreme eigenvalue differences within one metre of up to 0.2, often associated with small- or large-grained layers. The observation of a clear connection between the grain size variation and the impurity content leads to the conclusion that the influence of impurities on short-scale fabric variations is partially conveyed by the impurity-controlled grain size in combination with the local deformation regime. |
format |
Conference Object |
author |
Kerch, Johanna Weikusat, Ilka Diez, Anja Bohleber, Pascal Eisen, Olaf |
spellingShingle |
Kerch, Johanna Weikusat, Ilka Diez, Anja Bohleber, Pascal Eisen, Olaf Crystal-orientation fabric variations on the sub-metre scale in cold Alpine ice |
author_facet |
Kerch, Johanna Weikusat, Ilka Diez, Anja Bohleber, Pascal Eisen, Olaf |
author_sort |
Kerch, Johanna |
title |
Crystal-orientation fabric variations on the sub-metre scale in cold Alpine ice |
title_short |
Crystal-orientation fabric variations on the sub-metre scale in cold Alpine ice |
title_full |
Crystal-orientation fabric variations on the sub-metre scale in cold Alpine ice |
title_fullStr |
Crystal-orientation fabric variations on the sub-metre scale in cold Alpine ice |
title_full_unstemmed |
Crystal-orientation fabric variations on the sub-metre scale in cold Alpine ice |
title_sort |
crystal-orientation fabric variations on the sub-metre scale in cold alpine ice |
publishDate |
2017 |
url |
https://epic.awi.de/id/eprint/45499/ https://hdl.handle.net/10013/epic.51615 |
genre |
ice core The Cryosphere |
genre_facet |
ice core The Cryosphere |
op_source |
EPIC3International Symposium on the Cryosphere in a Changing Climate, Wellington, Neuseeland, 2017-02-12-2017-02-17 |
op_relation |
Kerch, J. orcid:0000-0002-7200-6837 , Weikusat, I. orcid:0000-0002-3023-6036 , Diez, A. , Bohleber, P. and Eisen, O. orcid:0000-0002-6380-962X (2017) Crystal-orientation fabric variations on the sub-metre scale in cold Alpine ice , International Symposium on the Cryosphere in a Changing Climate, Wellington, Neuseeland, 12 February 2017 - 17 February 2017 . hdl:10013/epic.51615 |
_version_ |
1810449559527096320 |