Texture of the Upper 1000 m in the GRIP and NorthGRIP Ice Cores

In this study we discuss new and published profiles of c-axis fabric and size distributions of a large number of crystals in the upper 1000 m of the Greenland GRIP and NorthGRIP ice cores as obtained with an automatic c-axis fabric analyzer. We show that in both cores the fabric is strongly anisotro...

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Main Authors: Svensson, Anders, Durand, Gaël, Mathiesen, Joachim, Persson, Asbjørn, Dahl-Jensen, Dorthe
Format: Article in Journal/Newspaper
Language:English
Published: Institute of Low Temperature Science, Hokkaido University
Subjects:
400
Online Access:http://hdl.handle.net/2115/45437
id fthokunivhus:oai:eprints.lib.hokudai.ac.jp:2115/45437
record_format openpolar
spelling fthokunivhus:oai:eprints.lib.hokudai.ac.jp:2115/45437 2023-05-15T16:27:10+02:00 Texture of the Upper 1000 m in the GRIP and NorthGRIP Ice Cores Svensson, Anders Durand, Gaël Mathiesen, Joachim Persson, Asbjørn Dahl-Jensen, Dorthe http://hdl.handle.net/2115/45437 eng eng Institute of Low Temperature Science, Hokkaido University Physics of Ice Core Records II : Papers collected after the 2nd International Workshop on Physics of Ice Core Records, held in Sapporo, Japan, 2-6 February 2007. Edited by Takeo Hondoh http://hdl.handle.net/2115/45437 ice core ice crystal texture fabric Greenland 400 bulletin (article) fthokunivhus 2022-11-18T01:02:09Z In this study we discuss new and published profiles of c-axis fabric and size distributions of a large number of crystals in the upper 1000 m of the Greenland GRIP and NorthGRIP ice cores as obtained with an automatic c-axis fabric analyzer. We show that in both cores the fabric is strongly anisotropic already just below the firn (about 110 m depth) with a degree of orientation around 30%. We determine the mean crystal area profiles which are somewhat contrasting to earlier findings based on manual measurements. The crystal size distributions are compared to a simple ID model which takes into account crystal growth and polygonization (rotation recrystallization). The model suggests that the crystal size distribution develops into a Bessel type distribution that differs from the commonly applied log normal distribution. Finally. we combine the fabric and microstructure results to determine the sub-grain boundaries in the GRIP samples. Both the size distribution model and the sub-grain study suggest that polygonization is significant already below the firn and that the physical processes governing the conventionally adapted 'normal grain growth' and 'polygonization' regimes are identical. The new measurements provide a dataset for ice sheet models that take into account the anisotropy of the Greenland ice sheet. I. Microphysical properties, deformation, texture and grain growth Article in Journal/Newspaper Greenland GRIP ice core Ice Sheet Hokkaido University Collection of Scholarly and Academic Papers (HUSCAP) Greenland
institution Open Polar
collection Hokkaido University Collection of Scholarly and Academic Papers (HUSCAP)
op_collection_id fthokunivhus
language English
topic ice core
ice crystal
texture
fabric
Greenland
400
spellingShingle ice core
ice crystal
texture
fabric
Greenland
400
Svensson, Anders
Durand, Gaël
Mathiesen, Joachim
Persson, Asbjørn
Dahl-Jensen, Dorthe
Texture of the Upper 1000 m in the GRIP and NorthGRIP Ice Cores
topic_facet ice core
ice crystal
texture
fabric
Greenland
400
description In this study we discuss new and published profiles of c-axis fabric and size distributions of a large number of crystals in the upper 1000 m of the Greenland GRIP and NorthGRIP ice cores as obtained with an automatic c-axis fabric analyzer. We show that in both cores the fabric is strongly anisotropic already just below the firn (about 110 m depth) with a degree of orientation around 30%. We determine the mean crystal area profiles which are somewhat contrasting to earlier findings based on manual measurements. The crystal size distributions are compared to a simple ID model which takes into account crystal growth and polygonization (rotation recrystallization). The model suggests that the crystal size distribution develops into a Bessel type distribution that differs from the commonly applied log normal distribution. Finally. we combine the fabric and microstructure results to determine the sub-grain boundaries in the GRIP samples. Both the size distribution model and the sub-grain study suggest that polygonization is significant already below the firn and that the physical processes governing the conventionally adapted 'normal grain growth' and 'polygonization' regimes are identical. The new measurements provide a dataset for ice sheet models that take into account the anisotropy of the Greenland ice sheet. I. Microphysical properties, deformation, texture and grain growth
format Article in Journal/Newspaper
author Svensson, Anders
Durand, Gaël
Mathiesen, Joachim
Persson, Asbjørn
Dahl-Jensen, Dorthe
author_facet Svensson, Anders
Durand, Gaël
Mathiesen, Joachim
Persson, Asbjørn
Dahl-Jensen, Dorthe
author_sort Svensson, Anders
title Texture of the Upper 1000 m in the GRIP and NorthGRIP Ice Cores
title_short Texture of the Upper 1000 m in the GRIP and NorthGRIP Ice Cores
title_full Texture of the Upper 1000 m in the GRIP and NorthGRIP Ice Cores
title_fullStr Texture of the Upper 1000 m in the GRIP and NorthGRIP Ice Cores
title_full_unstemmed Texture of the Upper 1000 m in the GRIP and NorthGRIP Ice Cores
title_sort texture of the upper 1000 m in the grip and northgrip ice cores
publisher Institute of Low Temperature Science, Hokkaido University
url http://hdl.handle.net/2115/45437
geographic Greenland
geographic_facet Greenland
genre Greenland
GRIP
ice core
Ice Sheet
genre_facet Greenland
GRIP
ice core
Ice Sheet
op_relation Physics of Ice Core Records II : Papers collected after the 2nd International Workshop on Physics of Ice Core Records, held in Sapporo, Japan, 2-6 February 2007. Edited by Takeo Hondoh
http://hdl.handle.net/2115/45437
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