摘要
对1982年7月26~28日由500hPa高原低涡与850hPa四川盆地浅薄低涡耦合作用引发盆地低涡强烈发展与大面积特大暴雨天气发生的机理进行了诊断研究。结果表明,高原低涡东移到100°E附近时,其低涡东部的正涡度平流与负值非平衡强迫与850hPa四川盆地浅薄低涡发生垂直叠加时,两者之间发生耦合作用。导致盆地浅薄低涡与500hPa高原涡同时发展,四川盆地发生大面积暴雨。
The evolution of southwest vortex and the occurrence of heavy rain caused by the coupling interaction between Plateau and southwest vortexes during the period of 26~28 July 1982 are diagnosed. The results show that, when the Plateau vortex moving eastward near 100°E, the positive vorticity advection and the negative unbalanced force in the east part of the Plateau vortex on 500 hPa imposed on 850 hPa southwest vortex occurred the vertical superposition. The coupling interaction between both the vortexes leads to the development of the southwest vortex and the occurrence of heavy rain.
出处
《高原气象》
CSCD
北大核心
2004年第1期75-80,共6页
Plateau Meteorology
基金
中国气象局青年基金项目
四川省应用基础项目
国家自然科学基金项目(40275017)共同资助
关键词
高原低涡
西南低涡
相互作用
诊断分析
Plateau vortex
Southwest vortex
Coupling interaction
Diagnostic analysis