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Descending motion of Antarctic stratospheric aerosol layer in winter: Possible effect on stratospheric water vapor budget
https://nipr.repo.nii.ac.jp/records/2071
https://nipr.repo.nii.ac.jp/records/207139e76436-48ad-45fd-99e7-497e05e79f89
名前 / ファイル | ライセンス | アクション |
---|---|---|
KJ00000012624.pdf (1.1 MB)
|
Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
---|---|---|---|---|---|---|
公開日 | 1986-12-01 | |||||
タイトル | ||||||
言語 | en | |||||
タイトル | Descending motion of Antarctic stratospheric aerosol layer in winter: Possible effect on stratospheric water vapor budget | |||||
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) |
Iwasaka, Yasunobu
× Iwasaka, Yasunobu |
|||||
著者所属(英) | ||||||
en | ||||||
Water Research Institute, Nagoya University | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | Lidar measurements at Syowa Station (69°00′S, 39°35′E) revealed that the centroid of aerosol layer descended at the rate of 0.8mm/s during winter. If this motion is a substantial movement of aerosol particles, the mass of water transported into the troposphere is about 5×(10)^7t/winter, and the Antarctic winter stratosphere is an important sink of stratospheric water vapor. If it is a downword air motion carrying small ice crystals, the value is reduced to 5×(10)^4t/winter. | |||||
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 45, p. 13-18, 発行日 1986-12 |