ICE FLOW BEHAVIOR AT DYE 3,GREENLAND

P(論文) To understand the flow behavior of large polar ice masses, mechanical property studies have been conducted on deep ice core samples obtained at Dye 3,Greenland during the GISP field operations from 1979 to 1981. A strain rate enhancement factor profile obtained by making uniaxial compression t...

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Main Authors: ショウジ, ヒトシ /, SHOJI, Hitoshi, LANGWAY, Chester C.
Language:English
Published: National Institute of Polar Research 1990
Subjects:
Online Access:https://nipr.repo.nii.ac.jp/record/3621/files/KJ00000767827.pdf
https://doi.org/10.15094/00003621
https://nipr.repo.nii.ac.jp/records/3621
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author ショウジ, ヒトシ /
SHOJI, Hitoshi
LANGWAY, Chester C.
author_facet ショウジ, ヒトシ /
SHOJI, Hitoshi
LANGWAY, Chester C.
author_sort ショウジ, ヒトシ /
collection National Institute of Polar Research Repository, Japan
description P(論文) To understand the flow behavior of large polar ice masses, mechanical property studies have been conducted on deep ice core samples obtained at Dye 3,Greenland during the GISP field operations from 1979 to 1981. A strain rate enhancement factor profile obtained by making uniaxial compression tests shows (1) much higher enhancement factor values for Wisconsin age ice compared with Holocene ice and (2) characteristic changes in the enhancement factor value for the Wisconsin ice depth zone. These results were incorporated to calculate both horizontal and vertical flow velocity profiles of ice which are in good agreement with the results of borehole tilting measurements and computer models of flow dynamics. The finding of depth changes in enhancement factor value leads to a consideration of possible formation of boudinage structure. Further studies are required to fully understand the differential flow behavior of large ice sheets. departmental bulletin paper
genre Dye 3
Dye-3
GISP
Greenland
ice core
Polar meteorology and glaciology
Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology
genre_facet Dye 3
Dye-3
GISP
Greenland
ice core
Polar meteorology and glaciology
Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology
geographic Greenland
Tilting
geographic_facet Greenland
Tilting
id ftnipr:oai:nipr.repo.nii.ac.jp:00003621
institution Open Polar
language English
long_lat ENVELOPE(-54.065,-54.065,49.700,49.700)
op_collection_id ftnipr
op_doi https://doi.org/10.15094/00003621
op_relation Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology
3
105
AA10756213
https://nipr.repo.nii.ac.jp/record/3621/files/KJ00000767827.pdf
https://doi.org/10.15094/00003621
https://nipr.repo.nii.ac.jp/records/3621
publishDate 1990
publisher National Institute of Polar Research
record_format openpolar
spelling ftnipr:oai:nipr.repo.nii.ac.jp:00003621 2025-04-13T14:17:59+00:00 ICE FLOW BEHAVIOR AT DYE 3,GREENLAND ショウジ, ヒトシ / SHOJI, Hitoshi LANGWAY, Chester C. 1990-01 application/pdf https://nipr.repo.nii.ac.jp/record/3621/files/KJ00000767827.pdf https://doi.org/10.15094/00003621 https://nipr.repo.nii.ac.jp/records/3621 eng eng National Institute of Polar Research Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology 3 105 AA10756213 https://nipr.repo.nii.ac.jp/record/3621/files/KJ00000767827.pdf https://doi.org/10.15094/00003621 https://nipr.repo.nii.ac.jp/records/3621 1990 ftnipr https://doi.org/10.15094/00003621 2025-03-19T10:19:56Z P(論文) To understand the flow behavior of large polar ice masses, mechanical property studies have been conducted on deep ice core samples obtained at Dye 3,Greenland during the GISP field operations from 1979 to 1981. A strain rate enhancement factor profile obtained by making uniaxial compression tests shows (1) much higher enhancement factor values for Wisconsin age ice compared with Holocene ice and (2) characteristic changes in the enhancement factor value for the Wisconsin ice depth zone. These results were incorporated to calculate both horizontal and vertical flow velocity profiles of ice which are in good agreement with the results of borehole tilting measurements and computer models of flow dynamics. The finding of depth changes in enhancement factor value leads to a consideration of possible formation of boudinage structure. Further studies are required to fully understand the differential flow behavior of large ice sheets. departmental bulletin paper Other/Unknown Material Dye 3 Dye-3 GISP Greenland ice core Polar meteorology and glaciology Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology National Institute of Polar Research Repository, Japan Greenland Tilting ENVELOPE(-54.065,-54.065,49.700,49.700)
spellingShingle ショウジ, ヒトシ /
SHOJI, Hitoshi
LANGWAY, Chester C.
ICE FLOW BEHAVIOR AT DYE 3,GREENLAND
title ICE FLOW BEHAVIOR AT DYE 3,GREENLAND
title_full ICE FLOW BEHAVIOR AT DYE 3,GREENLAND
title_fullStr ICE FLOW BEHAVIOR AT DYE 3,GREENLAND
title_full_unstemmed ICE FLOW BEHAVIOR AT DYE 3,GREENLAND
title_short ICE FLOW BEHAVIOR AT DYE 3,GREENLAND
title_sort ice flow behavior at dye 3,greenland
url https://nipr.repo.nii.ac.jp/record/3621/files/KJ00000767827.pdf
https://doi.org/10.15094/00003621
https://nipr.repo.nii.ac.jp/records/3621