@article{oai:chuo-u.repo.nii.ac.jp:00001238,
 author = {土屋, 修一 and 岡田, 将治 and 山田, 正},
 journal = {中央大学理工学研究所論文集},
 month = {Mar},
 note = {application/pdf, 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., 【査読有】},
 pages = {15--20},
 title = {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},
 volume = {10},
 year = {2005},
 yomi = {ツチヤ, シュウイチ and オカダ, マサハル and ヤマダ, タダシ}
}