| 2019年6月桂林三次强降水天气成因对比分析 |
| |
| 引用本文： | 王艳兰,伍静,唐桥义,王娟,王军君.2019年6月桂林三次强降水天气成因对比分析[J].湖北气象,2020,39(2):136-147. |
| |
| 作者姓名： | 王艳兰 伍静 唐桥义 王娟 王军君 |
| |
| 作者单位： | 广西桂林市气象局,桂林541001,广西桂林市气象局,桂林541001,广西桂林市气象局,桂林541001,广西桂林市气象局,桂林541001,广西桂林市气象局,桂林541001 |
| |
| 基金项目： | 广西区气象局科研计划项目;中国气象局预报员专项 |
| |
| 摘 要： | 利用多普勒雷达、气象卫星、自动气象站等监测数据以及NCEP再分析资料,对桂林2019年6月6-12日接连3次强降水天气过程的环流背景、影响系统与形成原因进行了对比分析。结果表明:(1)3次过程按影响系统分属暖区暴雨、低涡暴雨和锋面暴雨过程,均发生在高空急流右侧辐散、低空急流左侧辐合叠加区。(2)3次过程均受500 hPa短波槽和地面中尺度辐合线影响,但第1次过程中西南急流及地形等、第2次过程中低涡切变线、第3次过程中冷锋也起到重要作用。(3)3次过程的触发系统不同,第1次暖区暴雨过程迎风坡地形对其起触发作用,西南急流使得后向传播的对流云带维持;第2次低涡暴雨过程的触发系统为低层位于贵州一带的西南涡,西部冷空气侵入与西南急流加强是低涡对流云团维持较长时间的原因;第3次锋面暴雨的触发系统为冷锋,锋面配合锋前暖湿气流使对流云带加强。(4)第1次过程暖区暴雨MCS模态主要为线状后向扩建类,极端强降水出现在线对流中后端;第2次过程低涡暴雨MCS模态为涡旋类,极端强降水出现在涡旋中心附近;第3次过程锋面暴雨MCS模态由前期后部层云区线状对流转为层状云包裹对流系统,强降水发生在线对流弯曲或中心强回波处。
|
| 关 键 词： | 强降水 暖区暴雨 低涡暴雨 锋面暴雨 MCS模态 |
Comparative analysis on the cause of three heavy rainfall events in Guilin in June 2019 |
| |
| WANG Yanlan,WU Jing,TANG Qiaoyi,WANG Juan,WANG Junjun.Comparative analysis on the cause of three heavy rainfall events in Guilin in June 2019[J].Meteorology Journal of Hubei,2020,39(2):136-147. |
| |
| Authors: | WANG Yanlan WU Jing TANG Qiaoyi WANG Juan WANG Junjun |
| |
| Institution: | (Guilin Meteorological Office of Guangxi Zhuang Autonomous Region,Guilin 541001) |
| |
| Abstract: | Using the data collected from Doppler weather radar,FY satellite,automatic weather stations and NCEP reanalysis,we have conducted a comparative analysis of the three successive heavy rainfall events occurred in Guilin from June 6 to 12 in 2019 in terms of their circulation background,influence system and cause.The main results are as follow.(1)According to influence system the three events are warm-sector rainstorm,low-vortex rainstorm and frontal rainstorm,respectively,all of which occurred in the superimposed area of the divergence on the right side of upper-level jet and the convergence on the left side of low-level jet.(2)All three events are affected by short-wave troughs at 500 hPa and surface mesoscale convergence lines.In additon,the southwesterly low-level jet and terrain in the first event,the shear line with low vortex in the second event,and the cold front in the third event played an important role,respectively.(3)The trigger systems of the three events are different.The first warm-sector rainstorm event is triggered by windward slope terrain,and the southwest low-level jet maintains the convective clouds which is characterized by backward propagating.The second low-vortex rainstorm event is triggered by the southwest vortex in the low-level in Guizhou area,and in the event the intrusion of western cold air and the reinforcement of southwest low-level jets made the convective cloud with vortex last for a long time.The third frontal rainstorm event is triggered by cold front,which combined with warm and wet airflow in front of the front to strengthen the convective clouds.(4)The patterns of MCS that caused the first warm-sector rainstorm event are mainly the linear backward extension type,and the extremely precipitation occurred in the center and rear part of linear convection echoes.The pattern of MCS that induced the second vortex rainstorm event is the vorticity-stratiform type,and the extremely precipitation occurred near the center of vortex.The pattern of MCS that resulted in the third vortex rainstorm event is the convection system surrounded by stratiform cloud which is changed from linear convection in the rear of stratiform cloud area earlier stage,and the heavy rainfall occurred in the bend of linear convection or the center of strong echo. |
| |
| Keywords: | heavy rainfall warm-sector rainstorm low-vortex rainstorm frontal rainstorm MCS pattern |
| 本文献已被 维普 万方数据 等数据库收录！ |
|
