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2011年7月黑龙江省西部罕见暴雨成因分析
引用本文:胡好莉,王承伟.2011年7月黑龙江省西部罕见暴雨成因分析[J].气象与环境学报,2013,29(3):15-20.
作者姓名:胡好莉  王承伟
作者单位:1. 齐齐哈尔市气象局,黑龙江 齐齐哈尔161006;2. 黑龙江省气象科技服务中心,黑龙江 哈尔滨150030
基金项目:基金项目:中国气象局预报员专项(CMAYBY2011-011)“黑龙江省局地暴雨天气过程研究”和“黑龙江省单站降水预报方法研究”课题共同资助.
摘    要:利用区域自动站和常规观测资料及卫星云图、多普勒雷达资料,对2011年7月31日黑龙江省西部大区域暴雨过程进行分析。结果表明:黑龙江省西部暴雨区位于高空西风急流出口区左侧、低空和超低空急流的左侧,高空辐散和低空辐合作用为暴雨过程提供了动力条件,低空和超低空急流为暴雨提供了水汽条件;在对流层中层有较强的干冷空气侵入,短时强降水落区位于干侵入边界,并且与TBB大梯度区有较好的对应关系;而在雷达回波中,短时强降水落区位于速度图中的风场不连续线附近。

关 键 词:暴雨  干侵入边界  TBB  风场不连续线  

Forming reason of a rare rainstorm on July of 2011 in the west of Heilongjiang province
HU Hao-li,WANG Cheng-wei.Forming reason of a rare rainstorm on July of 2011 in the west of Heilongjiang province[J].Journal of Meteorology and Environment,2013,29(3):15-20.
Authors:HU Hao-li  WANG Cheng-wei
Institution:1.Qiqihar Meteorological Service, Qiqihar 161006, China; 2. Heilongjiang Meteorological Service Center of science and Technology ,Harbin 150030, China
Abstract:Based on the data from the automatic weather stations, the conventional observation data, the data from the satellite cloud imagery and the Doppler radar, a rainstorm process on July 31,2011 in the west of Heilongjiang province was analyzed synthetically. The results show that the rainstorm falling areas are located in the left side of the upper-level westerly jet exit region and the ultral-low-level jet. The upper divergence and lower convergence, the low-level and ultra-low-level jets provide the dynamic conditions and the water vapor conditions for this process, respectively. The strong dry cold air invades in the middle level of troposphere. The falling area of short-time rainstorm is located in the dry intrusion boundary of the strong cold air in the middle level, and it has a very good corresponding relation with the TBB region of big grads. However, it is near the discontinuity line of wind field on the radar echo velocity chart.
Keywords:Rainstorm  Dry intrusion boundary  Black body temperature (TBB)  Wind field discontinuity line
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