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作 者:方兆宝[1] 林珲[2] 吴立新[1] 江吉喜[3] 黄签[3]
机构地区:[1]中国矿业大学,北京100083 [2]香港中文大学中科院地球信息科学联合实验室 [3]中国气象局国家卫星气象中心,北京100081
出 处:《大气科学》2004年第4期634-640,共7页Chinese Journal of Atmospheric Sciences
基 金:香港特别行政区政府研究资助项目CUHK 4132/99H
摘 要:中尺度对流系统 (MesoscaleConvectiveSystems,MCSs)的活动和演变 ,是造成致洪暴雨灾害性天气的主要因素之一。多年来 ,许多学者加大了对中尺度对流系统研究的力度。但是 ,中尺度对流系统的活动及其移动和传播的研究进展一直受到计算机自动识别和跟踪问题的制约。首先介绍了一种基于面积重叠法的MCSs自动跟踪技术 ,然后针对它存在的问题进行了改良 ,并应用改良后的面积重叠法对 1 998年 6月至 8月的青藏高原上空MCSs进行了识别与跟踪实验。实验结果表明 ,改良后的面积重叠法的跟踪准确率可达80 % ,比改良前提高了 1 0 %以上。The activities and evolvements of mesoscale convective systems (MCSs) is one of the mostly factors which heavy rainstorm arise from Many scholars have increased the interest in the study on MCSs from these years However, the progression on studying activities and evolvements of MCSs is restricted by the technology of automatic identifying and tracking MCSs The thesis first introduces area overlapped method of automatic tracking MCSs Then aiming at its shortage, the area overlapped method is improved Using improved based method, the experiments are performed with data of MCSs over the Tibetan Plateau and its surrounding area in summer of 1998 The experiments show that the precision of tracking MCSs is about 80% with improved based area overlapped method, it is increased more ten percents than before improvement
分 类 号:P445[天文地球—大气科学及气象学]
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