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作 者:才奎志[1,2] 袁子鹏[1] 孙晓巍[1] 桑明刚[1] 曲荣强[1]
机构地区:[1]南京大学大气科学学院,江苏南京210009 [2]辽宁省气象台,辽宁沈阳110016
出 处:《Meteorological and Environmental Research》2010年第8期55-57,104,共4页气象与环境研究(英文版)
摘 要:Based on the data of satellite cloud image and Doppler radar,the rainstorm process from July 31st,2007 to August 1st,2007 in Liaoning was analyzed.The precipitation in Fushun and Haicheng was more than 100 mm,and 6 h precipitation in Fushun and Dandong was more than 50 mm.Through the analysis of strong precipitation period,the structure of clouds had a little decline from the stage of development to maturity.The gray value and gradient degree around were both larger in the center of heavy precipitation.Based on the data of satellite cloud image and Doppler radar,the rainstorm process from July 31st,2007 to August 1st,2007 in Liaoning was analyzed.The precipitation in Fushun and Haicheng was more than 100 mm,and 6 h precipitation in Fushun and Dandong was more than 50 mm.Through the analysis of strong precipitation period,the structure of clouds had a little decline from the stage of development to maturity.The gray value and gradient degree around were both larger in the center of heavy precipitation.
关 键 词:Satellite cloud image Doppler radar Gray value Echo intensity China
分 类 号:P458.121.1[天文地球—大气科学及气象学]
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