Journal of Arid Meteorology
Previous Articles Next Articles
XU Juan,JI Fanhua,HAN Fengjun,LV Bo,WANG Jian, YI Xia
Online:
Published:
徐娟, 纪凡华,韩风军,吕博,王健, 衣霞
作者简介:
基金资助:
山东省气象局预报员专项(sdyby2012 -15)资助
Abstract:
:The paper analyzed the weather situation,physical quantity condition and the characteristics of satellite cloud images and radar echo on July 4 2012 in western Shandong Province by using conventional observation data, intensive observation of automatic weather station as well as satellite images and radar data. The results show that this short - term strong precipitation was caused by the lower cold air and the mesoscale weather system under the background of the propitious large - scale weather system. Abundant water vapor and the strong convergence ascending motion on the level of 925 hPa and 1 000 hPa were conducive to the occurrence of strong precipitation. The positive vorticity center was corresponding to the strong precipitation center, and the surface convergence line and cyclonic circulation touched off the short - term strong precipitation. The satellite cloud images and radar data revealed the occurrence and development of the mesoscale weather system. The position and the maintain time of the mesoscale convective cloud cluster were consistent with the mesoscale system,and the same as the short - term strong precipitation. Strong radar echo region with composite reflectivity factor more than 45 dBz corresponded with the area of the short - term strong precipitation. Appearance and maintenance of the convergence flow field in radar radial velocity product were associated with the mesoscale cyclonic circulation,as well as the echo top height rising. While appearance and maintenance of the divergence flow field,and decline of the echo top were associated with weakening of the mesoscale system. The peak of the vertical accumulated liquid water contend appeared at the early stage of the short -term strong precipitation,and the peak value occurred before the stronger precipitation.
Key words: short - term strong precipitation, mesoscale weather system, mesoscale convective cloud cluster, radar echo
摘要:
利用常规观测资料、 自动站加密观测资料、 卫星云图和雷达资料, 对 2012 年 7 月 4 日山东省西部一次短时强降水的天气形势、 物理量条件、 云图和雷达回波特征进行分析。结果表明:在有利降水的大尺度天气系统背景下, 低层冷空气和中尺度天气系统造成了本次短时强降水天气;低层 925 hPa 和 1 000 hPa 的充沛水汽和辐合上升运动有利于强降水天气的发生, 正涡度中心对应强降水中心;地面辐合线和低压环流造成本次短时强降水天气;中尺度对流云团和地面中尺度系统相对应, 其位置和维持时间与强降水的落区和时间基本一致。雷达组合反射率因子 > 45 dBZ 的强回波区与强降水落区基本吻合;雷达平均径向速度产品逆风区中辐合流场的出现和维持及回波顶高的上升对应地面中尺度气旋式环流的形成和维持;逆风区中辐散流场的出现和维持及回波顶高的下降, 对应地面中尺度气旋式环流的减弱;短时强降水出现的初期, 垂直累积液态水含量出现了一个峰值, 峰值出现时间提前于较强降水时段。
关键词: 短时强降水, 中尺度天气系统, 中尺度对流云团, 雷达回波
CLC Number:
P458. 1+ 21
XU Juan,JI Fanhua,HAN Fengjun,LV Bo,WANG Jian, YI Xia. Mechanism Analysis of a Short - term Strong Precipitation in Midsummer of 2012 in Western Shandong Province[J]. Journal of Arid Meteorology, DOI: 10. 11755/j. issn. 1006 -7639(2014) -03 -0439.
徐娟, 纪凡华,韩风军,吕博,王健, 衣霞. 2012 年盛夏山东西部一次短时强降水天气的形成机制[J]. 干旱气象, DOI: 10. 11755/j. issn. 1006 -7639(2014) -03 -0439.
0 / Recommend
Add to citation manager EndNote|Ris|BibTeX
URL: http://www.ghqx.org.cn/EN/10. 11755/j. issn. 1006 -7639(2014) -03 -0439
http://www.ghqx.org.cn/EN/Y2014/V32/I3/439
[ 1]姚莉, 李小泉, 张立梅. 我国 1 小时雨强的时空分布特征[J]. 气象, 2009, 35(2):80 -87.[ 2]杨诗芳, 郝世峰, 冯晓伟, 等. 杭州短时强降水特征分析及预报研究[J]. 科技通报, 2010(4):2378 -2390.[ 3]尹承美, 梁永礼, 冉桂平, 等. 济南市区短时强降水特征分析[J]. 气象科技, 2010, 30(2):262 -267.[ 4]彭九慧, 易永力, 吴显春, 等. 河北省承德市短时强降水的多普勒雷达特征分析[J]. 干旱气象, 2010, 28(2):184 -197.[ 5]王令, 王国荣, 孙秀忠, 等. 应用多种探测资料对比分析两次突发性局地强降水[J]. 气象, 2012, 38(3):281 -290.[ 6]郭虎, 段丽, 杨波, 等. 0679 香山局地大暴雨的中尺度天气分析[J]. 应用气象学报, 2008, 19(3):265 -276.[ 7]王志超, 王咏青, 马鸿青, 等. 华北中部一次切变线暴雨诊断分析[J]. 干旱气象, 2010, 28(4):422 -429.[ 8]苏军锋, 吕宏, 闫惠玲, 等. 一次暴雨过程的中尺度特征分析[J]. 干旱气象, 2013, 31(1):156 -162.[ 9]景怀玺, 吉慧敏, 王雅茹, 等. 甘肃白银市一次局地暴雨天气过程分析[J]. 干旱气象, 2012, 30(3):443 -450.[ 10]曲晓黎, 段宇辉, 秦宝国, 等. 河北省中南部一次 MCC 造成的暴雨过程分析[J]. 干旱气象, 2011, 29(1):69 -74.[ 11]王建兵, 杨建才, 汪治桂. 舟曲 “8. 8” 暴雨云团的中尺度特征[J]. 干旱气象, 2011, 29(4):466 -471.[ 12]愈小鼎, 姚秀萍, 熊廷南, 等. 多普勒天气雷达原理与业务应用[M]. 北京:气象出版社, 2006.