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中国农学通报 ›› 2016, Vol. 32 ›› Issue (17): 157-164.doi: 10.11924/j.issn.1000-6850.casb16030020

所属专题: 农业气象

• 资源 环境 生态 土壤 气象 • 上一篇    下一篇

一次锋前暖区暴雨成因分析

王洪霞,苗爱梅,郑皓文   

  1. 山西省气象台,山西省气象台,山西省气象台
  • 收稿日期:2016-03-02 修回日期:2016-05-19 接受日期:2016-03-18 出版日期:2016-06-20 发布日期:2016-06-20
  • 通讯作者: 王洪霞
  • 基金资助:
    山西省科技攻关项目“基于GIS的极端气象灾害预警与评估集成系统”(20090311083);中国气象局预报员专项“数值预报对山西几次切变线强降水天气的预报性能分析研究”(CMAYBY2016-012)、“2015年汛期山西3次非典型暴雨过程的对比分析”(CMAYBY2016-010)。

Cause Analysis of a Heavy Rainfall Process in Warm Sector Ahead of Cold Front

  • Received:2016-03-02 Revised:2016-05-19 Accepted:2016-03-18 Online:2016-06-20 Published:2016-06-20

摘要: 利用常规气象观测、自动站、区域雨量站、卫星、雷达、再分析等资料,对2015年8月发生的一次锋前暖区暴雨进行了综合分析,结果表明:此次暴雨发生在西风槽东移和副高东退南压的环流背景下,以热力条件为主导引发的锋前暖区强对流性降水是此次暴雨产生的主要贡献者;暴雨发生在高空急流右后侧的显著辐散区,700hPa暖式切变线、850hPa冷式切变线、地面干线以及SI<-2℃相重叠的区域;850hPa切变线上的中尺度气旋性涡旋、自动站极大风速风场切变线以及中尺度涡旋是本次暴雨的直接触发系统;由于数值模式850hPa切变线位置预报的偏差,使得中低层流型配置由前倾误导为后倾结构,直接影响了模式热力条件预报的准确性,其结果是增强了西部动力条件而弱化了东部热力条件,最终导致暴雨落区预报偏差;锋前暖区暴雨预报的关键是触发不稳定能量释放的条件,对于此类暴雨应多关注边界层风场的变化,加强新型监测资料的综合分析和应用。

关键词: 直播方式, 直播方式, 出苗状况, 生长发育, 产量

Abstract: Based on conventional meteorological observation, automatic stations, regional rainfall stations, satellite, radar and reanalysis data, a heavy rain in warm sector before cold front occurred in August 2015 were analyzed. The results showed that: This heavy rainfall process happened in the background of westerly trough eastward and the subtropical high southeast retreat, and the strong convective precipitation led by thermal condition in warm sector before cold front was the main contribution of the heavy rainfall. The rainstorm appeared in the overlapping area of the significant divergence zone at the right rear of the upper-level jet, warm shear line at 700hPa, cold shear line at 850hPa, surface dry line and the region where Showalter Index was less than -2℃. The mesoscale cyclone vortex on 850hPa shear line together with the shear lines of extreme wind of automatic stations and mesoscale vortex directly triggered the rainstorm. Due to the deviation error of the model forecast in position of the 850hPa shear line, the mid-lower flow configuration was misled from a forward-tilting to be a backward-tilting structure, which directly affected the model accuracy in thermal condition forecast, and the result was that enhanced the Western dynamic condition and weakened the Eastern thermal condition, which ended up with a deviation error of heavy rainfall area forecast. The key of heavy rainfall in warm sector before cold front forecast was the conditions of triggering the release of unstable energy. For such rainstorm forecast, we should pay more attention to the wind field changes in boundary layer and strengthen the comprehensive analysis and application of the monitoring data.

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