CAJ | 학술논문

利用常规观测资料、卫星云图、自动站气象观测资料和多普勒雷达等资料，对2011年6月16日玉林市南部一次中尺度强降水过程进行天气动力学和中尺度分析，结果表明：这次暴雨是在有利的大尺度环流背景下．通过中尺度系统激发而产生的。高空低槽和低空切变辐合是强降水产生的前提条件，中尺度对流云团强烈发展是强降水产生的直接原因；分析红外云图的TBB、多普勒雷达反射率和基本速度、地形条件等方面，都很好地阐述了本次强降水的暴雨中心落区。
이용상규관측자료、위성운도、자동참기상관측자료화다보륵뢰체등자료，대2011년6월16일옥림시남부일차중척도강강수과정진행천기동역학화중척도분석，결과표명：저차폭우시재유리적대척도배류배경하．통과중척도계통격발이산생적。고공저조화저공절변복합시강강수산생적전제조건，중척도대류운단강렬발전시강강수산생적직접원인；분석홍외운도적TBB、다보륵뢰체반사솔화기본속도、지형조건등방면，도흔호지천술료본차강강수적폭우중심락구。
By using the conventional observational data, satellite cloud pictures, AWS data and Doppler radar data, a weather dynamics and mesoscale analysis for a heavy rain process occurred on june 16, 2011 in southern Yulin was made. It shows that this process is stimulated by mesoscale system under the favorable large-scale circulation, low slots and low shear convergence was the preconditions of rainfall, the mesoscale convective cloud cluster development is strong rainfall produce direct cause. Moreover, the center of this heavy rain is well described by TBB, Doppler radar reflectivity and base speed, terrain condition.