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The shape of the domelike plateau (Valkyrjedomen), which is the second highest in Antarctica, and the position of ice divides have been known more than before. The highest place of this dome was found at 77°22′S, 39°37′E with an altitude of 3807m by the use of Navy Navigation Statellite System. The surface slope, net accumulation, configuration of snow surface, ram hardness, 10m snow temperature and others were observed. From these results, the characteristics of katabatic winds region were not found in the region higher than the altitude around 3400-3600m, which was about 400m higher than such altitude in the case of Mizuho Plateau. Surface slopes change to less than 2×(10)^\u003c-3\u003e in the higher area from such altitudinal boundaries in both cases of the present study and Mizuho Plateau. 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GLACIOLOGICAL CHARACTERISTICS OF AN ANTARCTIC INLAND PLATEAU
https://doi.org/10.15094/00003548
https://doi.org/10.15094/00003548047e1b5b-b70e-43e9-91da-a66b762014e1
名前 / ファイル | ライセンス | アクション |
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KJ00000767756 (148.7 kB)
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Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
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公開日 | 1987-09-01 | |||||
タイトル | ||||||
タイトル | GLACIOLOGICAL CHARACTERISTICS OF AN ANTARCTIC INLAND PLATEAU | |||||
言語 | ||||||
言語 | eng | |||||
資源タイプ | ||||||
資源タイプ識別子 | http://purl.org/coar/resource_type/c_6501 | |||||
資源タイプ | departmental bulletin paper | |||||
ID登録 | ||||||
ID登録 | 10.15094/00003548 | |||||
ID登録タイプ | JaLC | |||||
ページ属性 | ||||||
内容記述タイプ | Other | |||||
内容記述 | P(論文) | |||||
記事種別(英) | ||||||
en | ||||||
ABSTRACT | ||||||
論文名よみ | ||||||
その他のタイトル | GLACIOLOGICAL CHARACTERISTICS OF AN ANTARCTIC INLAND PLATEAU | |||||
著者名よみ |
アゲタ, ユタカ
× アゲタ, ユタカ× オクヒラ, フミオ× カミヤマ, コキチ× キクチ, トキオ |
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著者名(英) |
AGETA, Yutaka
× AGETA, Yutaka× OKUHIRA, Fumio× KAMIYAMA, Kokichi× KIKUCHI, Tokio |
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著者所属(英) | ||||||
en | ||||||
Water Research Institute, Nagoya Univesity | ||||||
著者所属(英) | ||||||
en | ||||||
Gifu Prefectural Research Institute for Environmental Pollution | ||||||
著者所属(英) | ||||||
en | ||||||
Geophysical Research Station, Kyoto University | ||||||
著者所属(英) | ||||||
en | ||||||
Faculty of Science, Kochi University | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | Glaciological observations on the high plateau were made along a route of the oversnow traverse by the 26th Japanese Antarctic Research Expedition in 1985. The shape of the domelike plateau (Valkyrjedomen), which is the second highest in Antarctica, and the position of ice divides have been known more than before. The highest place of this dome was found at 77°22′S, 39°37′E with an altitude of 3807m by the use of Navy Navigation Statellite System. The surface slope, net accumulation, configuration of snow surface, ram hardness, 10m snow temperature and others were observed. From these results, the characteristics of katabatic winds region were not found in the region higher than the altitude around 3400-3600m, which was about 400m higher than such altitude in the case of Mizuho Plateau. Surface slopes change to less than 2×(10)^<-3> in the higher area from such altitudinal boundaries in both cases of the present study and Mizuho Plateau. From the observation of surface configuration, it was known that the directions of prevailing winds changed from southeast in the katabatic winds region to northeast around the highest place of the dome. On the basis of these results, patterns of atmospheric circulation over the plateau and its relation with the glaciological aspects are briefly discussed. | |||||
雑誌書誌ID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AA10756213 | |||||
書誌情報 |
Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology 巻 1, p. 155-156, 発行日 1987-09 |
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出版者 | ||||||
出版者 | National Institute of Polar Research |