Some Results on Oxygen Isotope and Stratigraphic Analyses of Firn in Mizuho Plateau, East Antarctica
P(論文) Oxygen isotope (δ^<18>O) and stratigraphic analyses of the 2m deep pits and the 10m deep cores from the coast to the high-inland region of Mizuho Plateau have been done. A seasonal diagram of δ^<18>O of drifting snow in connection with the elevation was obtained from the δ^<18&g...
Main Authors: | , , |
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Language: | English |
Published: |
1981
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Online Access: | https://nipr.repo.nii.ac.jp/record/1188/files/KJ00000011714.pdf https://nipr.repo.nii.ac.jp/records/1188 |
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author | Watanabe, Okitsugu Kato, Kikuo Satow, Kazuhide |
author_facet | Watanabe, Okitsugu Kato, Kikuo Satow, Kazuhide |
author_sort | Watanabe, Okitsugu |
collection | National Institute of Polar Research Repository, Japan |
description | P(論文) Oxygen isotope (δ^<18>O) and stratigraphic analyses of the 2m deep pits and the 10m deep cores from the coast to the high-inland region of Mizuho Plateau have been done. A seasonal diagram of δ^<18>O of drifting snow in connection with the elevation was obtained from the δ^<18>O values of fallen snow and drifting snow. The regional characteristics of the relations between the δ^<18>O profiles and the firn layering structures were examined. The seasonal cycles of δ^<18>O are only found in the δ^<18>O profiles in the firn of the coastal region and in the specified places of the katabatic slope region. The δ^<18>O profile in the most of the katabatic slope region is largely controlled by the season of formation of the surface snow layer and the snow metamorphosis such as the formation of loose and hard depth hoar. Similar tendencies are found in the profiles of the running means of δ^<18>O in the cores of the costal region and of the katabatic slope region, respectively. These tendencies may reflect the change of glaciological environment spread over each region. departmental bulletin paper |
genre | Antarc* Antarctica East Antarctica Memoirs of National Institute of Polar Research Polar Research |
genre_facet | Antarc* Antarctica East Antarctica Memoirs of National Institute of Polar Research Polar Research |
geographic | East Antarctica Mizuho Mizuho Plateau |
geographic_facet | East Antarctica Mizuho Mizuho Plateau |
id | ftnipr:oai:nipr.repo.nii.ac.jp:00001188 |
institution | Open Polar |
language | English |
long_lat | ENVELOPE(44.317,44.317,-70.683,-70.683) ENVELOPE(40.000,40.000,-73.000,-73.000) |
op_collection_id | ftnipr |
op_relation | Memoirs of National Institute of Polar Research. Special issue 19 264 279 AA00733561 https://nipr.repo.nii.ac.jp/record/1188/files/KJ00000011714.pdf https://nipr.repo.nii.ac.jp/records/1188 |
publishDate | 1981 |
record_format | openpolar |
spelling | ftnipr:oai:nipr.repo.nii.ac.jp:00001188 2025-04-13T14:10:16+00:00 Some Results on Oxygen Isotope and Stratigraphic Analyses of Firn in Mizuho Plateau, East Antarctica Watanabe, Okitsugu Kato, Kikuo Satow, Kazuhide 1981-10 application/pdf https://nipr.repo.nii.ac.jp/record/1188/files/KJ00000011714.pdf https://nipr.repo.nii.ac.jp/records/1188 eng eng Memoirs of National Institute of Polar Research. Special issue 19 264 279 AA00733561 https://nipr.repo.nii.ac.jp/record/1188/files/KJ00000011714.pdf https://nipr.repo.nii.ac.jp/records/1188 1981 ftnipr 2025-03-19T10:19:56Z P(論文) Oxygen isotope (δ^<18>O) and stratigraphic analyses of the 2m deep pits and the 10m deep cores from the coast to the high-inland region of Mizuho Plateau have been done. A seasonal diagram of δ^<18>O of drifting snow in connection with the elevation was obtained from the δ^<18>O values of fallen snow and drifting snow. The regional characteristics of the relations between the δ^<18>O profiles and the firn layering structures were examined. The seasonal cycles of δ^<18>O are only found in the δ^<18>O profiles in the firn of the coastal region and in the specified places of the katabatic slope region. The δ^<18>O profile in the most of the katabatic slope region is largely controlled by the season of formation of the surface snow layer and the snow metamorphosis such as the formation of loose and hard depth hoar. Similar tendencies are found in the profiles of the running means of δ^<18>O in the cores of the costal region and of the katabatic slope region, respectively. These tendencies may reflect the change of glaciological environment spread over each region. departmental bulletin paper Other/Unknown Material Antarc* Antarctica East Antarctica Memoirs of National Institute of Polar Research Polar Research National Institute of Polar Research Repository, Japan East Antarctica Mizuho ENVELOPE(44.317,44.317,-70.683,-70.683) Mizuho Plateau ENVELOPE(40.000,40.000,-73.000,-73.000) |
spellingShingle | Watanabe, Okitsugu Kato, Kikuo Satow, Kazuhide Some Results on Oxygen Isotope and Stratigraphic Analyses of Firn in Mizuho Plateau, East Antarctica |
title | Some Results on Oxygen Isotope and Stratigraphic Analyses of Firn in Mizuho Plateau, East Antarctica |
title_full | Some Results on Oxygen Isotope and Stratigraphic Analyses of Firn in Mizuho Plateau, East Antarctica |
title_fullStr | Some Results on Oxygen Isotope and Stratigraphic Analyses of Firn in Mizuho Plateau, East Antarctica |
title_full_unstemmed | Some Results on Oxygen Isotope and Stratigraphic Analyses of Firn in Mizuho Plateau, East Antarctica |
title_short | Some Results on Oxygen Isotope and Stratigraphic Analyses of Firn in Mizuho Plateau, East Antarctica |
title_sort | some results on oxygen isotope and stratigraphic analyses of firn in mizuho plateau, east antarctica |
url | https://nipr.repo.nii.ac.jp/record/1188/files/KJ00000011714.pdf https://nipr.repo.nii.ac.jp/records/1188 |