| 武汉和宜昌地区降水的Z-R关系 |
| |
| 引用本文： | 许绍祖,朱国江,尹球,程箴荣,耿骠,庄荫模.武汉和宜昌地区降水的Z-R关系[J].大气科学学报,1990,13(4):572-575. |
| |
| 作者姓名： | 许绍祖 朱国江 尹球 程箴荣 耿骠 庄荫模 |
| |
| 作者单位： | 南京大学;南京大学;南京大学;南京大学;南京大学;南京大学 |
| |
| 摘 要： | 应用1987-1989年观测的850份雨滴谱资料,统计分析了武汉和宜昌地区降水的Z-R关系。得出武汉地区:层状云降水Z=200.7 R1.259 对流性降水Z=292.4R1.265 宜昌地区:层状云降水Z=259.3R1.407 对流性降水Z=361.9R1.477。
|
THE Z-R RELATIONSHIP OF PRECIPITATION IN WUHAN AND YICHANG AREAS |
| |
| Xu Shaozu,Zhu Guojiang,Yin Qiu,Cheng Zhenrong,Geng Biao and Zhuang Yinmo.THE Z-R RELATIONSHIP OF PRECIPITATION IN WUHAN AND YICHANG AREAS[J].大气科学学报,1990,13(4):572-575. |
| |
| Authors: | Xu Shaozu Zhu Guojiang Yin Qiu Cheng Zhenrong Geng Biao and Zhuang Yinmo |
| |
| Institution: | Affiliated with Nanjing University;Affiliated with Nanjing University;Affiliated with Nanjing University;Affiliated with Nanjing University;Affiliated with Nanjing University;Affiliated with Nanjing University |
| |
| Abstract: | Having analyzed 850 raindrop size data from 1987 to 1989, we obtain the following regressional formulas of radar reflectivity factor (Z) and precipitation intensity (R):(1) Wuhan Area:precipitation from stratiform clouds:Z=200.7R1.259precipitation from cumuliform clouds:Z=292.4R1.265(2) Yichang Area:precipitation from stratiform clouds:Z=259.3R1.407precipitation from cumuliform clouds:Z=361.9R1.477 |
| |
| Keywords: | |
|
| 点击此处可从《大气科学学报》浏览原始摘要信息 |
| 点击此处可从《大气科学学报》下载免费的PDF全文 |
