CAJ | 학술논문

通过对2008年10月12—15日海南省特大暴雨过程特征分析，表明海南“0810”特大暴雨是热带低压和冷空气相互作用的结果，特大暴雨的发生发展及减弱与偏东和偏南风急流的加强和减弱有较好的对应关系：东风急流造成海南岛东部降雨明显大于西部。副热带高压对北上热带低压的阻拦和形成的环流对降水起到了加强和维持的作用：雷达回波为典型的积层混合型降水回波；长时间的低层辐合、高空强辐散，有利于强降雨的发生和维持。
통과대2008년10월12—15일해남성특대폭우과정특정분석，표명해남“0810”특대폭우시열대저압화랭공기상호작용적결과，특대폭우적발생발전급감약여편동화편남풍급류적가강화감약유교호적대응관계：동풍급류조성해남도동부강우명현대우서부。부열대고압대북상열대저압적조란화형성적배류대강수기도료가강화유지적작용：뢰체회파위전형적적층혼합형강수회파；장시간적저층복합、고공강복산，유리우강강우적발생화유지。
Based on the characteristic analysis of torrential rain process on OCT12-15, 2008 in Hainan, it shows that this process is the result of interaction between tropical depression and cold air. There is a correspondent relation between the occurrence development or weakness of torrential rain and the rapids or decrease of east and south jet, and the heavier rain in the east of Hainan is caused by the east jet. Moreover, the rain was enhanced and maintained by the prevention of subtropical high to Tropical depression towards north and the circulation. The radar echo is the typical accumulated layer mixed precipitation echo. Long time lower convergence and high altitude strong divergence are helpful for the occurrence and maintenance of heavy rainfall.