CAJ | 학술논문

利用常规和加密自动气象站观测资料、卫星和雷达探测资料及NCEP再分析资料（1°×1°，6 h），对2013年8月15—16日辽宁黑山地区特大暴雨的中尺度对流条件和对流系统特征进行分析。结果表明：此次强降水由中—β尺度系统引起，短时大暴雨发生在能量舌边缘，地面偏东风和地形强迫抬升作用造成对流单体沿山脉东侧生成、发展和移动，最终导致持续对流性强降雨。东北低压冷锋前激发的中尺度切变和涡旋触发了局地大暴雨。黑山地区上游有两个对流单体生成，向东移动合并影响该地区，移动方向前侧的斜升气流和低质心回波提高了降水效率。
이용상규화가밀자동기상참관측자료、위성화뢰체탐측자료급NCEP재분석자료（1°×1°，6 h），대2013년8월15—16일료녕흑산지구특대폭우적중척도대류조건화대류계통특정진행분석。결과표명：차차강강수유중—β척도계통인기，단시대폭우발생재능량설변연，지면편동풍화지형강박태승작용조성대류단체연산맥동측생성、발전화이동，최종도치지속대류성강강우。동북저압랭봉전격발적중척도절변화와선촉발료국지대폭우。흑산지구상유유량개대류단체생성，향동이동합병영향해지구，이동방향전측적사승기류화저질심회파제고료강수효솔。
Based on data from conventional and automatic weather stations,satellite and radar,and the NCEP rean-alysis data (1 °×1 °,6 h),the mesoscale convective conditions and convective system characteristics of an extraor-dinary rainstorm process on August 15-16,2013 at Heishan of Liaoning province were analyzed.The results show that the severe precipitation process is caused by mesoscale-βconvectional systems.The short-term torrential rain area occurs at the edge of energy tongue.Surface eastward wind and topographic force are dominant factors that causes generation,development and movement of convection cells along the east side of mountain,which lead to the continuous and convectional precipitation.The mesoscale wind shear and vortex motivated by the northeast low-pressure cold front trigger the local torrential rain.Two separate convective cells generate in upper reaches of heavy rain areas,and merge together and then influence Heishan County.The oblique ascension airflow in front of echo moving direction and low heart echo both enhance precipitation efficiency.