Characterization of cm-scale variations of crystal orientation fabric in cold Alpine ice core from Colle Gnifetti
Crystal orientation fabric – i.e. the spatial distribution of crystal c-axes in a defined depth interval – and its evolution with depth contain information on deformation processes in the ice column. Recent pilot studies on Alpine and polar ice indicate that fabric evolution provides more informatio...
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ftawi:oai:epic.awi.de:40821 2024-09-15T18:11:54+00:00 Characterization of cm-scale variations of crystal orientation fabric in cold Alpine ice core from Colle Gnifetti Kerch, Johanna Weikusat, Ilka Eisen, Olaf Wagenbach, Dietmar Bohleber, Pascal Spaulding, Nicole 2015 https://epic.awi.de/id/eprint/40821/ https://hdl.handle.net/10013/epic.47836 unknown Kerch, J. orcid:0000-0002-7200-6837 , Weikusat, I. orcid:0000-0002-3023-6036 , Eisen, O. orcid:0000-0002-6380-962X , Wagenbach, D. , Bohleber, P. and Spaulding, N. (2015) Characterization of cm-scale variations of crystal orientation fabric in cold Alpine ice core from Colle Gnifetti , 26. Polartagung der Deutschen Gesellschaft für Polarforschung „Hohe Breiten und Hochgebirge: Treiber oder Getriebene im Globalen Wandel?“, Bayerische Akademie der Wissenschaften, München, 6 September 2015 - 11 September 2015 . hdl:10013/epic.47836 EPIC326. Polartagung der Deutschen Gesellschaft für Polarforschung „Hohe Breiten und Hochgebirge: Treiber oder Getriebene im Globalen Wandel?“, Bayerische Akademie der Wissenschaften, München, 2015-09-06-2015-09-11 Conference notRev 2015 ftawi 2024-06-24T04:14:20Z Crystal orientation fabric – i.e. the spatial distribution of crystal c-axes in a defined depth interval – and its evolution with depth contain information on deformation processes in the ice column. Recent pilot studies on Alpine and polar ice indicate that fabric evolution provides more information than just on deformation if examined on the sub-meter scale, where the interaction between climate-related impurities and fabric evolution, i.e. their mutual influence, comes into focus and needs to be investigated. We studied crystal orientation fabric from an Alpine ice core from Colle Gnifetti (4450 m asl, Monte Rosa, Switzerland), a small glacier saddle with low net accumulation which is uniquely suited as a test site for studies under polar conditions. We calculated orientation tensor eigenvalues as measure for fabric strength in cm-resolution for several depth ranges of about 1 m between the firn-ice-transition and bed rock of the 73 m long ice core drilled in 2013. We found significant variations of fabric strength occurring within only 10 cm in all assessed depth ranges, revealing a complex anisotropic ice structure. In order to understand the mechanisms that lead to the observed short-scale variability we evaluated impurity data in cm-resolution from continuous flow analysis of the ice core. As a new approach we collected sub-mm impurity data from several features of the ice microstructure, where fabric changes occur, by means of a new laser ablation-inductively coupled plasma-mass spectrometry technique to explore the direct comparison of sub-mm impurity data and ice microstructure. Conference Object ice core Polarforschung 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 |
Crystal orientation fabric – i.e. the spatial distribution of crystal c-axes in a defined depth interval – and its evolution with depth contain information on deformation processes in the ice column. Recent pilot studies on Alpine and polar ice indicate that fabric evolution provides more information than just on deformation if examined on the sub-meter scale, where the interaction between climate-related impurities and fabric evolution, i.e. their mutual influence, comes into focus and needs to be investigated. We studied crystal orientation fabric from an Alpine ice core from Colle Gnifetti (4450 m asl, Monte Rosa, Switzerland), a small glacier saddle with low net accumulation which is uniquely suited as a test site for studies under polar conditions. We calculated orientation tensor eigenvalues as measure for fabric strength in cm-resolution for several depth ranges of about 1 m between the firn-ice-transition and bed rock of the 73 m long ice core drilled in 2013. We found significant variations of fabric strength occurring within only 10 cm in all assessed depth ranges, revealing a complex anisotropic ice structure. In order to understand the mechanisms that lead to the observed short-scale variability we evaluated impurity data in cm-resolution from continuous flow analysis of the ice core. As a new approach we collected sub-mm impurity data from several features of the ice microstructure, where fabric changes occur, by means of a new laser ablation-inductively coupled plasma-mass spectrometry technique to explore the direct comparison of sub-mm impurity data and ice microstructure. |
format |
Conference Object |
author |
Kerch, Johanna Weikusat, Ilka Eisen, Olaf Wagenbach, Dietmar Bohleber, Pascal Spaulding, Nicole |
spellingShingle |
Kerch, Johanna Weikusat, Ilka Eisen, Olaf Wagenbach, Dietmar Bohleber, Pascal Spaulding, Nicole Characterization of cm-scale variations of crystal orientation fabric in cold Alpine ice core from Colle Gnifetti |
author_facet |
Kerch, Johanna Weikusat, Ilka Eisen, Olaf Wagenbach, Dietmar Bohleber, Pascal Spaulding, Nicole |
author_sort |
Kerch, Johanna |
title |
Characterization of cm-scale variations of crystal orientation fabric in cold Alpine ice core from Colle Gnifetti |
title_short |
Characterization of cm-scale variations of crystal orientation fabric in cold Alpine ice core from Colle Gnifetti |
title_full |
Characterization of cm-scale variations of crystal orientation fabric in cold Alpine ice core from Colle Gnifetti |
title_fullStr |
Characterization of cm-scale variations of crystal orientation fabric in cold Alpine ice core from Colle Gnifetti |
title_full_unstemmed |
Characterization of cm-scale variations of crystal orientation fabric in cold Alpine ice core from Colle Gnifetti |
title_sort |
characterization of cm-scale variations of crystal orientation fabric in cold alpine ice core from colle gnifetti |
publishDate |
2015 |
url |
https://epic.awi.de/id/eprint/40821/ https://hdl.handle.net/10013/epic.47836 |
genre |
ice core Polarforschung |
genre_facet |
ice core Polarforschung |
op_source |
EPIC326. Polartagung der Deutschen Gesellschaft für Polarforschung „Hohe Breiten und Hochgebirge: Treiber oder Getriebene im Globalen Wandel?“, Bayerische Akademie der Wissenschaften, München, 2015-09-06-2015-09-11 |
op_relation |
Kerch, J. orcid:0000-0002-7200-6837 , Weikusat, I. orcid:0000-0002-3023-6036 , Eisen, O. orcid:0000-0002-6380-962X , Wagenbach, D. , Bohleber, P. and Spaulding, N. (2015) Characterization of cm-scale variations of crystal orientation fabric in cold Alpine ice core from Colle Gnifetti , 26. Polartagung der Deutschen Gesellschaft für Polarforschung „Hohe Breiten und Hochgebirge: Treiber oder Getriebene im Globalen Wandel?“, Bayerische Akademie der Wissenschaften, München, 6 September 2015 - 11 September 2015 . hdl:10013/epic.47836 |
_version_ |
1810449486730756096 |