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CHARACTERISTICS OF EVAPORATION FROM SNOW AND TUNDRA SURFACE IN SPITSBERGEN IN THE SNOWMELT SEASON 1993
https://doi.org/10.15094/00003879
https://doi.org/10.15094/000038794f102f3b-9c15-4fb9-b39b-13f851a28430
名前 / ファイル | ライセンス | アクション |
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Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
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公開日 | 1995-09-01 | |||||
タイトル | ||||||
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 | 10.15094/00003879 | |||||
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 | CHARACTERISTICS OF EVAPORATION FROM SNOW AND TUNDRA SURFACE IN SPITSBERGEN IN THE SNOWMELT SEASON 1993 | |||||
著者名よみ |
タケウチ, ユカリ
× タケウチ, ユカリ× コダマ, ユウジ× ナカバヤシ, ヒロノリ |
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著者名(英) |
TAKEUCHI, Yukari
× TAKEUCHI, Yukari× KODAMA, Yuji× NAKABAYASHI, Hironori |
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著者所属(英) | ||||||
en | ||||||
Institute of Low Temperature Science, Hokkaido University | ||||||
著者所属(英) | ||||||
en | ||||||
Institute of Low Temperature Science, Hokkaido University | ||||||
著者所属(英) | ||||||
en | ||||||
Institute of Low Temperature Science, Hokkaido University | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | Meteorological conditions and evaporation from snow and tundra surfaces were measured in the tundra area in Spitsbergen from the end of May to the end of June in 1993. In this period, three types of ground surface were seen, i.e. dry snow, melting snow and snow-free tundra. Clear changes in evaporation as well as the meteorological conditions were seen with the changes in surface condition. During the dry snow period, evaporation predominated at the snow surface and the latent heat loss by evaporation suppressed the snowmelt. During the snowmelt period, the temperature of the snow cover was 0℃ from the surface to the bottom, and condensation predominated due to the increase of vapor pressure in the air. The latent heat by condensation contributed to the snowmelt. After the seasonal snow was gone and the meltwater was still abundant at the tundra surface, intense evaporation of about 3.7 mmday^<-1> occurred with the rapid surface temperature increase, while condensation occurred on the remaining snow surface. | |||||
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 9, p. 54-65, 発行日 1995-09 |
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出版者 | ||||||
出版者 | National Institute of Polar Research |