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 R^(1.259) 对流性降水Z=292.4R^(1.265) 宜昌地区:层状云降水Z=259.3R^(1.407) 对流性降水Z=361.9R^(1.477)
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=200.7R^(1.259)
precipitation from cumuliform clouds: Z=292.4R^(1.265)
(2) Yichang Area:
precipitation from stratiform clouds: Z=259.3R^(1.407)
precipitation from cumuliform clouds: Z=361.9R^(1.477)
出处
《南京气象学院学报》
CSCD
1990年第4期572-575,共4页
Journal of Nanjing Institute of Meteorology