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山东省2009年7月8~9日区域性暴雨成因分析(英文) 被引量:1
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作者 赵钢 杨瑞峰 +1 位作者 陈彬 许长山 《Meteorological and Environmental Research》 CAS 2010年第7期41-44,共4页
By using the data which included the conventional weather chart,the satellite cloud image,the regional automatic meteorological station and the new generation of weather radar,the regional strong precipitation process... By using the data which included the conventional weather chart,the satellite cloud image,the regional automatic meteorological station and the new generation of weather radar,the regional strong precipitation process which happened in Shandong Province during July 8-9 in 2009 was analyzed comprehensively.The results showed that Shandong Province was in the strong convergence zone of atmospheric vorticity in the low layer and the ascent zone of vertical velocity.The shear line was generated in the eastward process of northwest vortex,and the ground inverted trough extended to Shandong,which provided the dynamic condition for the formation of rainstorm.The coupling of jet stream in the high-low altitude enhanced the development of convection.The low-altitude jet stream was the main water vapor transportation channel,which provided the water vapor condition for the generation of rainstorm.The water vapor was mainly from the South China Sea and the Bay of Bengal. 展开更多
关键词 RAINSTORM Water vapor flux Jet stream pseudoequivalent potential temperature Meso-scale convective system China
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