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SURFACE MASS BALANCE, SUBLIMATION AND SNOW TEMPERATURES AT DOME FUJI STATION, ANTARCTICA, IN 1995
https://doi.org/10.15094/00003967
https://doi.org/10.15094/00003967c02144c9-f79f-48be-b5d8-611f353480ae
名前 / ファイル | ライセンス | アクション |
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KJ00001014930 (1.3 MB)
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Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
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公開日 | 1997-11-01 | |||||
タイトル | ||||||
タイトル | SURFACE MASS BALANCE, SUBLIMATION AND SNOW TEMPERATURES AT DOME FUJI STATION, ANTARCTICA, IN 1995 | |||||
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 | 10.15094/00003967 | |||||
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) | |||||
論文名よみ | ||||||
その他のタイトル | SURFACE MASS BALANCE, SUBLIMATION AND SNOW TEMPERATURES AT DOME FUJI STATION, ANTARCTICA, IN 1995 | |||||
著者名よみ |
カメダ, タカオ
× カメダ, タカオ× アズマ, ノブヒコ× フルカワ, テルオ× アゲタ, ユタカ× タカハシ, シュウヘイ |
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著者名(英) |
KAMEDA, Takao
× KAMEDA, Takao× AZUMA, Nobuhiko× FURUKAWA, Teruo× AGETA, Yutaka× TAKAHASHI, Shuhei |
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著者所属(英) | ||||||
en | ||||||
Kitami Institute of Technology | ||||||
著者所属(英) | ||||||
en | ||||||
Nagaoka University of Technology | ||||||
著者所属(英) | ||||||
en | ||||||
National Institute of Polar Research | ||||||
著者所属(英) | ||||||
en | ||||||
Institute of Hydrospheric-Atmospheric Sciences, Nagoya University | ||||||
著者所属(英) | ||||||
en | ||||||
Kitami Institute of Technology | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | This paper focuses on the first year-round observations of surface mass balance, sublimation and snow temperatures at Dome Fuji Station. This station was newly established at the highest point (77°19′01″S, 39°42′12″E; 3810m) in Queen Maud Land, Antarctica by the Japanese Antarctic Research Expedition. It was found that average surface mass balance by the stake method was +2.5g(cm)^<-2> from 25 January 1995 to 30 January 1996 (370 days), of which about 95% of the positive balance was obtained from February to the middle of October (eight and half months). Sublimation from atmosphere to snow surface (mass input : +0.55g(cm)^<-2>) was predominant in winter (March to October) and sublimation from snow surface to atmosphere (mass output : -0.39g(cm)^<-2>) was predominant in summer (November to February). In the annual balance, sublimation from atmosphere to snow surface (+0.16g(cm)^<-2>) prevailed. This corresponds to about 6% of the annual surface mass balance. The snow temperature at 10m depth varied from -57.0 to -57.8℃, and the annual mean 10m snow temperature was -57.3℃. | |||||
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 11, p. 24-34, 発行日 1997-11 |
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出版者 | ||||||
出版者 | National Institute of Polar Research |