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...

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Main Authors: Watanabe, Okitsugu, Kato, Kikuo, Satow, Kazuhide
Language:English
Published: 1981
Subjects:
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