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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 |
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Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||||
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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
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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 |