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DYNAMICAL BEHAVIOR OF SHIRASE GLACIER IN RELATION TO DETERIORATION OF THE SHELF ICE
https://doi.org/10.15094/00003856
https://doi.org/10.15094/000038568e366322-fd13-4c04-9c8f-0709b1ea3dcc
名前 / ファイル | ライセンス | アクション |
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KJ00000767964 (58.4 kB)
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Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
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公開日 | 1994-11-01 | |||||
タイトル | ||||||
タイトル | DYNAMICAL BEHAVIOR OF SHIRASE GLACIER IN RELATION TO DETERIORATION OF THE SHELF ICE | |||||
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 | 10.15094/00003856 | |||||
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 | DYNAMICAL BEHAVIOR OF SHIRASE GLACIER IN RELATION TO DETERIORATION OF THE SHELF ICE | |||||
著者名よみ |
ナカワ, マサヨシ
× ナカワ, マサヨシ× カワイ, シンイチ |
|||||
著者名(英) |
NAKAWO, Masayoshi
× NAKAWO, Masayoshi× KAWAI, Shinichi |
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著者所属(英) | ||||||
en | ||||||
Institute for Hydrospheric-Atmospheric Sciences, Nagoya University | ||||||
著者所属(英) | ||||||
en | ||||||
National Research Institute for Earth Science and Disaster Prevention | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | Recent thinning of the Antarctic ice sheet has been found at the middle stream of the Shirase drainage basin, East Antarctica, through intermittent surveys in the last 20 years. The strain rate of the ice sheet, obtained in the observations, was about +10×(10)^<-5>/a and -3×(10)^<-5>/a along the longitudinal and vertical directions, respectively, near Mizuho Station in the middle stream of Shirase Basin. The strain rates for the last 9000 years, on the other hand, were found to be about +14×(10)^<-5>/a and -7×(10)^<-5>/a respectively, based upon analyses on an ice core retrieved at Mizuho Station. A steady state model calculation gave values for the strain rate intermediate between the survey data and the core data. These results have been explained, by a two dimensional non-steady state model, in terms of deterioration of the ice shelf at the exit of Shirase Basin, which could have taken place roughly 2000 years before the present. | |||||
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 8, p. 199, 発行日 1994-11 |
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出版者 | ||||||
出版者 | National Institute of Polar Research |