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Thermal oscillation induced by an interaction between sea ice and ocean in a numerical polar ice-ocean model
https://nipr.repo.nii.ac.jp/records/1360
https://nipr.repo.nii.ac.jp/records/13607b1f2c82-39bd-4e1a-9344-31e4f010c74b
名前 / ファイル | ライセンス | アクション |
---|---|---|
KJ00000011994 (1.4 MB)
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Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
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公開日 | 1982-12-01 | |||||
タイトル | ||||||
言語 | en | |||||
タイトル | Thermal oscillation induced by an interaction between sea ice and ocean in a numerical polar ice-ocean model | |||||
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 | |||||
ページ属性 | ||||||
内容記述タイプ | Other | |||||
内容記述 | P(論文) | |||||
著者名(英) |
Sakai, Satoshi
× Sakai, Satoshi× Imawaki, Shiro |
|||||
著者所属(英) | ||||||
en | ||||||
Institute of Earth Science, Kyoto University/Geophysical Institute, Kyoto University | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | A numerical model of simplified Arctic Ocean and Greenland-Norwegian Seas is presented. The essential effects of sea ice, river runoff, surface cooling, and water exchange between the Greenland-Norwegian Seas and the Atlantic Ocean are included. A thermal oscillation occurs due to an interaction between the sea ice and the ocean. The river runoff forms a low-salinity surface layer, which is essential to the oscillation. Parameters governing the time scale of the oscillation are also discussed. | |||||
雑誌書誌ID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AA00733561 | |||||
書誌情報 |
Memoirs of National Institute of Polar Research. Special issue 巻 24, p. 246-254, 発行日 1982-12 |