| 凝结反馈对云层垂直发展影响的一个线性理论 |
| |
| 引用本文： | 顾震潮,胡广兴.凝结反馈对云层垂直发展影响的一个线性理论[J].气象学报,1962,32(1):64-70. |
| |
| 作者姓名： | 顾震潮 胡广兴 |
| |
| 作者单位： | 中国科学院地球物理研究所
(顾震潮)，中国科学院地球物理研究所(胡广兴) |
| |
| 摘 要： | 根据小尺度垂直运动的线性分析,作者证明凝结反馈对云层的垂直发展有着很强的制约作用。这种制约作用在温度和湿度较大的情况下更为明显。作者引出了在凝结反馈作用下非定常运动中的频率公式和定常运动下的波速公式。这样,南方雨季中每次雨停时常常见到的云层迅速分层的现象得到了可能的理论解释。
|
| 收稿时间： | 1961/10/20 0:00:00 |
A LINEAR THEORY OF THE INFLUENCE OF CONDENSATION FEEDBACK ON THE DEVELOPMENT OF THE CLOUD |
| |
| Koo CHEN-CHAD and Ho K. WANG-SHING.A LINEAR THEORY OF THE INFLUENCE OF CONDENSATION FEEDBACK ON THE DEVELOPMENT OF THE CLOUD[J].Acta Meteorologica Sinica,1962,32(1):64-70. |
| |
| Authors: | Koo CHEN-CHAD and Ho K WANG-SHING |
| |
| Institution: | Institute. of Geophysics and Meteorology, Academia Sinica;Institute. of Geophysics and Meteorology, Academia Sinica |
| |
| Abstract: | Based on a linear analysisaof the small scale vertical motion the authors show that the feedback of condensation gives a strong control on the vertical development of the cloud. The frequency equation for the non-stationary case is given with the feedback of condensation taken into consideretion. A possible explanation of the appearence of mufti-layer cloud in the southern countries towards the ending of rain is presented. |
| |
| Keywords: | |
| 本文献已被 CNKI 等数据库收录！ |
| 点击此处可从《气象学报》浏览原始摘要信息 |
| 点击此处可从《气象学报》下载免费的PDF全文 |
