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MODELING OF POLAR STRATOSPHERIC CLOUDS
https://doi.org/10.15094/00003653
https://doi.org/10.15094/00003653ed9e77a3-1d57-4919-a14b-38df41db72aa
名前 / ファイル | ライセンス | アクション |
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KJ00000767856 (111.0 kB)
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Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
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公開日 | 1991-05-01 | |||||
タイトル | ||||||
タイトル | MODELING OF POLAR STRATOSPHERIC CLOUDS | |||||
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 | |||||
ID登録 | ||||||
ID登録 | 10.15094/00003653 | |||||
ID登録タイプ | JaLC | |||||
ページ属性 | ||||||
内容記述タイプ | Other | |||||
内容記述 | P(論文) | |||||
記事種別(英) | ||||||
en | ||||||
ABSTRACT | ||||||
論文名よみ | ||||||
その他のタイトル | MODELING OF POLAR STRATOSPHERIC CLOUDS | |||||
著者名よみ |
タナカ, ヒロシ
× タナカ, ヒロシ× オオタ, マサキ× ハヤシ, マサヒコ× ウシマル, シンジ× イワサカ, ヤスノブ |
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著者名(英) |
TANAKA, Hiroshi
× TANAKA, Hiroshi× OOTA, Masaki× HAYASHI, Masahiko× USHIMARU, Shinji× IWASAKA, Yasunobu |
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著者所属(英) | ||||||
en | ||||||
Water Research Institute, Nagoya University | ||||||
著者所属(英) | ||||||
en | ||||||
Water Research Institute, Nagoya University | ||||||
著者所属(英) | ||||||
en | ||||||
Solar Terrestrial Environment Laboratory, Nagoya University | ||||||
著者所属(英) | ||||||
en | ||||||
Water Research Institute, Nagoya University | ||||||
著者所属(英) | ||||||
en | ||||||
Solar Terrestrial Environment Laboratory, Nagoya University | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | Formation of polar stratospheric clouds (PSCs) is simulated assuming that they consist of H_2O ice particles. Stratospheric aerosols are assumed to work as the ice-forming nuclei if the supersaturation ratio exceeds the critical values determined from aerosol size. Growth of the PSC particles is computed using the condensation equations. Two cases of cooling rates of the atmosphere are tested. One is 1.0K/day, and the other is 0.25K/day. The number concentration of the PSC particles ranges between 0.1 and 0.4/(cm)^3,and the particle size ranges between 4 and 6μm. Further inspection shows that the particles are larger in number concentration but smaller in particle size when the larger cooling rate is used. A simulation is also carried out for the temperatures measured in the Antarctic winter of 1980 incorporating the fall effect of PSC particles. The result shows that growth of the PSC particles is restricted by the fall effect, particularly in the upper part of the PSC layer. | |||||
雑誌書誌ID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AA10756213 | |||||
書誌情報 |
Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology 巻 4, p. 121, 発行日 1991-05 |
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出版者 | ||||||
出版者 | National Institute of Polar Research |