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赣东一次对流性暴雨成因及漏报原因分析

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利用自动加密观测资料和雷达云图等资料对2016年6月29日赣东对流性暴雨成因和漏报原因进行了分析,结果表明:这是一次典型的低层急流配合垂直抽吸作用使副热带高压边缘产生强降水过程,露点锋上激发出对流性降水是此次过程最主要原因。另外,强降水落区与发展旺盛的中尺度对流云团、强雷达反射率因子的强度和中气旋有较好的对应关系。此外漏报主要原因是对低空急流核和高空辐散的分析得不够深入,对误差较大的模式预报未进行不断的订正,以及对中尺度物理量资料和雷达卫星云图资料等未能充分使用。
Cause Analysis of Convective Rainstorm in Gandong and its Missing Prediction
Based on intensive observation data,radar,and satellite images,the causes of a local sud-den convective rainstorm process in Gandong on June 29 ,2016 and its missing prediction were ana-lyzed. The results showed that,this was a typical low-level jet with the vertical suction effect of the subtropical high-pressure edge of the process of heavy precipitation,which the most important reason was the convective precipitation induced by the dew point. However,there was a good correlation be-tween the strong precipitation area and the intensity of mesoscale convective cloud,strong radar re-flectivity factor and mesocyclone. In addition,the main cause of the rainstorm process missing predic-tion was that the analysis of the low-level jet nucleus and the high-level divergence was not deep e-nough,the model predictions with large errors were not constantly revised,as well as the small-scale physical data and radar satellite images were not fully used,etc.

MCSconvective rainstormjet streakupper divergencemissing prediction cause

董玲、郑劲光、周湘萍

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抚州市气象台,344000,江西,抚州

MCS 对流性暴雨 急流核 高空辐散 漏报原因

2013年江西省气象局面上项目

2016

江西科学
江西省科学院

江西科学

影响因子:0.286
ISSN:1001-3679
年,卷(期):2016.34(6)
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