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実スケール雲生成実験による上昇風速及びエアロゾルが雲水生成に与える影響の解明に関する研究
https://doi.org/10.24789/00001228
https://doi.org/10.24789/00001228e8c7e2b8-6419-4689-8e70-a2d48a5a253c
名前 / ファイル | ライセンス | アクション |
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本文を見る(PDFファイル) (504.9 kB)
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Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||
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公開日 | 2012-10-01 | |||||
タイトル | ||||||
タイトル | 実スケール雲生成実験による上昇風速及びエアロゾルが雲水生成に与える影響の解明に関する研究 | |||||
タイトル | ||||||
言語 | en | |||||
タイトル | A Study of the vertical velocity and aerosol effects on cloud formation using quasi-prototype experiment of cloud physics | |||||
言語 | ||||||
言語 | jpn | |||||
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 | 10.24789/00001228 | |||||
ID登録タイプ | JaLC | |||||
著者 |
土屋, 修一
× 土屋, 修一× 岡田, 将治× 山田, 正 |
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著者別名(英) | ||||||
姓名 | TSUCHIYA, Shuichi | |||||
言語 | en | |||||
著者別名(英) | ||||||
姓名 | OKADA, Masaharu | |||||
言語 | en | |||||
著者別名(英) | ||||||
姓名 | YAMADA, Tadashi | |||||
言語 | en | |||||
抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | The purpose of this study is to propose a numerical model of rainfall consideringthe effects of cloud microphysics and aerosols. In order to compare the theory of cloud physics and the phenomena occurringin cloud, we constructed experimental facilities with prototype scale usingthe longv ertical shaft of an abandoned mine. Usingthis facility, data such as temperature, relative humidity, air pressure, updraft velocity, cloud particle and aerosol particle consistency have been observed at different height. In this shaft it was found that clouds occurred before the air reaches the saturation level. We observed condensational growth of water vapor from vertical distribution of each diameter particle number. Through the experiments, we found the new type mechanism related to occurrence of clouds. The followingresults were obtained; 1)The result of linear relation between updraft velocity and amount of cloud water was obtained. 2)The result of Logarithmic relation between solution consistency and amount of cloud water was obtained. 3)The result of Logarithmic relation between supplied aerosol number and cloud water was obtained. 4) Too much supplied aerosol number and solution of consistency lets increasingcloud water restrai. | |||||
内容記述 | ||||||
内容記述タイプ | Other | |||||
内容記述 | 【査読有】 | |||||
書誌情報 |
中央大学理工学研究所論文集 巻 10, p. 15-20, 発行日 2005-03-31 |
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出版者 | ||||||
出版者 | 中央大学理工学研究所 | |||||
ISSN | ||||||
収録物識別子タイプ | ISSN | |||||
収録物識別子 | 1343-0068 | |||||
権利 | ||||||
権利情報 | この資料の著作権は、資料の著作者または学校法人中央大学に帰属します。著作権法が定める私的利用・引用を超える使用を希望される場合には、掲載誌発行部局へお問い合わせください。 | |||||
フォーマット | ||||||
内容記述タイプ | Other | |||||
内容記述 | application/pdf | |||||
著者版フラグ | ||||||
出版タイプ | VoR | |||||
出版タイプResource | http://purl.org/coar/version/c_970fb48d4fbd8a85 |