| 招远特大暴雨分析 |
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| 引用本文： | 杨金玲,高峰,丁锡强.招远特大暴雨分析[J].安徽农业科学,2009,37(31):15387-15388. |
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| 作者姓名： | 杨金玲 高峰 丁锡强 |
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| 作者单位： | 招远市气象局,山东招远,265400 |
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| 摘 要： | 2008年7月19～20日受弱冷空气和7号热带风暴“海鸥”外围暖湿气流共同影响，招远市区出现了1次特大暴雨天气过程，日降水总量接近历史极值。笔者利用常规气象资料对此次暴雨过程进行总结分析，结果表明，热带低压和中纬度系统相互作用是造成此次过程的重要原因。
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| 关 键 词： | 特大暴雨 环流背景 物理量 雷达回波 |
Analysis of Heavy Rainstorm in Zhaoyuan |
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| YANG Jin-ling et al.Analysis of Heavy Rainstorm in Zhaoyuan[J].Journal of Anhui Agricultural Sciences,2009,37(31):15387-15388. |
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| Authors: | YANG Jin-ling |
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| Institution: | YANG Jin-ling et al (Zhaoyuan Meteorological Bureau,Zhaoyuan,Sh,ong 265400) |
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| Abstract: | By the interactive effects of a weak cold air and the 7th tropical storm Seagull external warm air,Zhaoyuan urban areas presented an especially big rainstorm synoptic process on Juky 19-20th of 2008.The total amount of precipitation was close to the historical extremum.The conventional meteorological data were used to analyze the rainstorm process.The results showed that the interaction of mid-latitude and tropical low pressure system was the important reason caused by the process. |
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| Keywords: | Heavy rainstorm Circulation background Physical amount Radar echo |
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