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THE RELATIONSHIP BETWEEN THE THERMAL BELT ON THE SLOPE OF THE ICE SHEET ON THE SOYA COAST AND THE SURFACE INVERSION LAYER OVER SYOWA STATION
https://doi.org/10.15094/00003825
https://doi.org/10.15094/00003825d6ac4ebf-5267-4961-915e-15654764b1df
名前 / ファイル | ライセンス | アクション |
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KJ00000767933 (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 | 1994-11-01 | |||||
タイトル | ||||||
タイトル | THE RELATIONSHIP BETWEEN THE THERMAL BELT ON THE SLOPE OF THE ICE SHEET ON THE SOYA COAST AND THE SURFACE INVERSION LAYER OVER SYOWA STATION | |||||
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 | 10.15094/00003825 | |||||
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 | THE RELATIONSHIP BETWEEN THE THERMAL BELT ON THE SLOPE OF THE ICE SHEET ON THE SOYA COAST AND THE SURFACE INVERSION LAYER OVER SYOWA STATION | |||||
著者名よみ |
ナカガワ, キヨタカ
× ナカガワ, キヨタカ× シモドオリ, ヒロコ |
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著者名(英) |
NAKAGAWA, Kiyotaka
× NAKAGAWA, Kiyotaka× SHIMODOORI, Hiroko |
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著者所属(英) | ||||||
en | ||||||
Division of Science, Joetsu University of Education | ||||||
著者所属(英) | ||||||
en | ||||||
Division of Science, Joetsu University of Education | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | All the NOAA/AVHRR thermal infrared images received at Syowa Station from February 1990 to January 1991 were analyzed to make temperature distribution maps. From this analysis the warmer area in midslope, i.e. the so-called thermal belt (D. GREENLAND, The Encyclopedia of Climatology, ed. by OLIVER and FAIRBRIDGE, 594,1987), appeared on the ice sheet slope along the coast around Lutzow-Holm Bay, especially on the Soya Coast, frequently in winter. The relationship between the thermal belt on the Soya Coast and the surface inversion layer over Syowa Station was investigated. When the surface inversion layer thickness increased, the thermal belt was displaced toward the interior or higher part of the ice sheet slope. However, even if the surface inversion layer appeared over Syowa Staton, the thermal belt did not necessarily appear. The appearance or absence of the thermal belt on the ice sheet slope is considered to correspond to how the surface inversion layer over the ice sheet, a katabatic wind, connects with the surface inversion layer over the foot of the slope. | |||||
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. 53-65, 発行日 1994-11 |
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出版者 | ||||||
出版者 | National Institute of Polar Research |