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中国农学通报 ›› 2017, Vol. 33 ›› Issue (20): 90-94.doi: 10.11924/j.issn.1000-6850.casb16070043

所属专题: 农业气象

• 资源 环境 生态 土壤 气象 • 上一篇    下一篇

多普勒雷达产品在两次短时强降水过程中的对比分析

文海松,杨辉,王恪,赵卓勋   

  1. 湖北省荆州市气象局,湖北省鄂州市气象局,湖北省荆州市气象局,湖北省荆州市气象局
  • 收稿日期:2016-07-08 修回日期:2016-11-18 接受日期:2016-11-23 出版日期:2017-07-18 发布日期:2017-07-18
  • 通讯作者: 杨辉
  • 基金资助:

Comparison of Two Short-time Heavy Precipitation Processes from Doppler Weather Radar Products

  • Received:2016-07-08 Revised:2016-11-18 Accepted:2016-11-23 Online:2017-07-18 Published:2017-07-18

摘要: 为了提高荆州地区强对流天气的预报预警能力,提升气象服务农业生产水平,利用2015年荆州多普勒雷达资料,对比分析发生于2015年5月15日和2015年6月1日的2次短时强降水过程。结果发现:(1)2次过程的雷达回波最大反射率强度均在50 dBz以上,并且比较稳定,回波移动过程中均产生了“列车效应”;(2)2次过程均出现中尺度辐合,速度图上中尺度辐合区与强回波位置一致;(3)2次过程中的风暴云底高度大部分时间在2~3 km,云顶高度在12 km附近。风暴生成前期均存在明显的VIL跃增和回波顶高跃增现象,VIL跃增量分别为10、20 kg/m2,顶高跃增为3 km和9 km;(4)风暴发展阶段垂直积分液态含水量均比较稳定,分别为40~50 kg/m2和30~40 kg/m2。回波质心高度和最大反射率高度除6月1日出现下沉以外,其余大部时间2次过程回波质心高度均在4~5 km,最大反射率高度在3~6 km;(5)经过风暴追踪等信息的综合分析推断,6月1日可能还出现下击暴流。

关键词: 番茄早疫, 番茄早疫, 微生物防治, 茄链格孢菌属

Abstract: To improve the forecasting and early-warming ability of severe convection weather in Jingzhou, and enhance meteorological service for agricultural production, the authors analyzed two short- time strong precipitation processes occurred on May 15 and June 1, 2015, by using Doppler radar data in Jingzhou. The results showed that: (1) the maximum radar echo intensity of these two processes were more than 50 dBz andstable, and“train effect”occurred during the moving of radar echo; (2) mesoscale convergence occurred in both processes, and the location of strong echo was consistent with the location of mesoscale convergence in velocity field; (3) most of the time, the cloud base height of these two processes were 2-3 km, and the cloud top height were around 12 km; obvious jump of echo top height and vertically integrated liquid (VIL) existed before the generation of storm; the VIL increments of the two processes were 10 kg/m2 and 20 kg/m2 and the increments of echo top height were 3 km and 9 km, respectively; (4) the vertical integrated liquid water contents were relatively stable in the storm development phase, were 40- 50 kg/m2 and 30- 40 kg/m2, respectively; the echo mass center height of the two processes were 4-5 km, and the maximum reflectivity height were 3-6 km at most of the time except June 1, when the sinking movement occurred; (5) downburst probably occurred on June 1 according to comprehensive analysis of the information of storm tracking.