摘要
利用海口多普勒天气雷达、闪电定位和日本静止卫星0.05°×0.05°TBB资料,对1117号强台风"纳沙"造成的海南岛暴雨的中尺度特征进行了分析。结果表明:台风暴雨分布特征与TC环流和地形增幅密切相关;明显的辐合性暖平流和"列车效应"有利于暴雨的持续;最大回波强度和小时雨量间有很好的对应关系,建议了海口多普勒雷达TC估测降水产品使用公式Z=230R1.25;海南岛强降水时段TBB值普遍小于-70℃,但仍属于降水效率高的弱对流;西半部地区强降水出现时间与中尺度对流云团对应较好,而东半部地区中尺度对流云团的发展则超前于强降水出现时间。
Based on data of Haikou Doppler Radar,Hainan lightning locating system and 0. 05° × 0. 05°TBB data of Japanese stationary satellite,the mesoscale characteristic of rainstorm caused by violent typhoon ' Neast' in Hainan Island was analyzed in this paper. The results show that,the distribution features of typhoon rainstorm are closely related with TC circulation and terrain enhancement; the remarkable convergence warm advection and ' the train effect' both are beneficial to the lasting rainstorm; the strongest echo intensity and hourly rainfall match well; the function Z = 230R1. 25 is suggested to be used for TC estimating precipitation production of Haikou Doppler Radar;though the TBB of heavy rainfall in Hainan Island is normally less than- 70 ℃,the heavy rainfall still belongs to weak convection with high rainfall efficiency; the occurring time of heavy rainfall in west half area matches well with mesoscale convective clouds,while the mesoscale convective clouds develop earlier than heavy rainfall in east half area.
出处
《自然灾害学报》
CSCD
北大核心
2014年第4期134-141,共8页
Journal of Natural Disasters
基金
中国气象局预报员专项资助项目(CMAYBY2012-047)
国家科技支撑计划项目(2013BAK05B03)