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Vertical Structure of Katabatic Winds in Mizuho Plateau
https://nipr.repo.nii.ac.jp/records/856
https://nipr.repo.nii.ac.jp/records/8560e22cd47-4f81-4163-8f3e-e086c69d97a8
名前 / ファイル | ライセンス | アクション |
---|---|---|
KJ00000011830.pdf (931.9 kB)
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Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
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公開日 | 1978-01-01 | |||||
タイトル | ||||||
言語 | en | |||||
タイトル | Vertical Structure of Katabatic Winds in Mizuho Plateau | |||||
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) |
Kobayashi, S.
× Kobayashi, S. |
|||||
著者所属(英) | ||||||
en | ||||||
The Institute of Low Temperature Science, Hokkaido University | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | Observation of vertical structure of katabatic winds blowing in Mizuho Plateau was made by means of radio sondes. It was found that the layer of the katabatic winds is roughly identical with the surface inversion layer. The surface inversion layer showed seasonal variations in thickness and intensity. The katabatic wind layer disappeared when a cyclone was passing over the ocean in the vicinity of Syowa Station, as noticed from the disarranged wind speed profiles. Wind vectors in the lowest few hundred metres of the katabatic wind layer showed that a thermal wind persisted in the surface inversion layer. Therefore, the katabatic winds in Mizuho Plateau may be called the "inversion winds", because they are essentially controlled by the thermal wind due to the existence of a sloped inversion layer. | |||||
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 7, p. 72-80, 発行日 1978-01 |