副高西侧四川盆地两次极端暴雨过程分析

Analysis of Two Extreme Heavy Rain Processes at the Edge of West Pacific Subtropical High in Sichuan Basin

  • 摘要: 本文利用1×1°NCEP/NCAR再分析资料、FY2E卫星TBB资料及地面自动站资料,对2013年7月8~11日和7月17~19日四川盆地出现的两次极端暴雨过程的环流形势、中尺度环境条件和触发机制、水汽条件异常特征、地面能量和水汽压的分布及演变特征进行了诊断和对比分析,结果表明:(1)两次过程均发生在500h Pa为东高西低的形势下,暴雨落区位于低层低涡右侧、偏南气流左侧,高空急流入口区右侧。(2)副高外围偏南风持续向四川盆地上空输送暖湿气流,形成高能、高湿和层结不稳定的有利环境条件,500h Pa高原低值系统东移诱发低层正涡度辐合,造成对流强烈发展,是两次过程的共同特征,副高、低层低涡和辐合区位置、盆地内能量和水汽条件分布的差异是导致两次过程暴雨落区不同的主要原因。(3)两次过程都存在明显的水汽条件异常特征,其中降雨极端性更强的“7.8-11”过程标准化距平更大。(4)初始对流主要出现在地面水汽压的24h显著增量区域和地面能量锋偏低能区一侧,强降雨开始后,地面水汽压的演变趋势对降雨强度和强降雨持续时间也有一定的指示意义。

     

    Abstract: An Comparative Analysis of circulation situation,environmental conditions,trigger mechanism,anomaly characteristics of the water vapor condition,surface energy and vapor pressure's characteristics in two Extreme Heavy Rain Processes during 8 to 11 and 17 to 19 July 2013 in Sichuan basin is performed by using of the NCEP / NCAR 1°×1° reanalysis data,FY- 2E satellite observational data and ground intensive observational data. The results showed that:(1) The two heavy rainfall processes occur in the situation of east high west low on 500 h Pa,and the heavy rainfall appears on the vortex's right side,the south airflow's left side,the high jet entrance area's right side.(2) The warm moist air is continuous transported to the sichuan basin by the south airflow on the edge of subtropical high,the environmental conditions of high energy,high humidity and stratification instability are formatted,and the plateau low system induces the formation of the vortex,all they make the convective system develop strongly; the position of subtropical high,low vortex and convergence zone,and the distribution of the basin energy and water vapor condition difference are the main reasons for the different rainfall distribution in the two process.(3) The anomaly characteristics of the water vapor conditions are obvious in the two heavy rainfall processes,especially in the process of "7. 8- 11".(4) The initial convection mainly appears in the significant incremental area of the ground vapor pressure during 24 hours and the low side of energy front,the evolution's trend of the ground vapor pressure also has certain instruction significance to intensity and persistent time after the heavy rainfall begin.

     

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