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Distribution of 10m Snow Temperatures in Mizuho Plateau
https://nipr.repo.nii.ac.jp/records/855
https://nipr.repo.nii.ac.jp/records/85520744183-94b5-4808-8251-556753e03211
名前 / ファイル | ライセンス | アクション |
---|---|---|
KJ00000011829.pdf (1.1 MB)
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Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
---|---|---|---|---|---|---|
公開日 | 1978-01-01 | |||||
タイトル | ||||||
言語 | en | |||||
タイトル | Distribution of 10m Snow Temperatures 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) |
Satow, K.
× Satow, K. |
|||||
著者所属(英) | ||||||
en | ||||||
Nagaoka Technical College | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | Measurements were made of snow temperature at a depth of 10m beneath the surface during the oversnow traverses in 1968-1975 in the region of Mizuho Plateau. The mean annual surface temperature estimated from the 10m snow temperature decreases gradually from the coast to the inland, which mean temperature gradient with elevation is close to the dry adiabatic lapse rate in the area between 0m and 3000m and its value in the area between 3000m and 3800m is larger than -2℃/100m. A map of mean annual isotherms shows that the isotherms are similar to elevation contours, especially in the area lower than 3000m. | |||||
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. 63-71, 発行日 1978-01 |