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TCM-90现场科学试验台风FLO“β陀螺”“通风流”非对称动力结构特征 总被引:9,自引:3,他引:6
采用TCM-90台风现场科学试验期间加密观测资料,揭示出目标台风Flo非对称动力、热力结构及其转向运动的特征,尤其通过分离处理的偏差场,突出了TCM-90现场试验有关飞机下投(dropsonde)加密探测资料对台风Flo内部非对称结构物理图象的描述,提出了实际台风动力结构存在类似Gray认为的非对称偶极子型,即中低层“β陀螺”偶极子型(β-topdipole),及其“通风流”(Ventilationflow)特征,高层辐合-辐散结构的变形偶极子系统概念模型,并认为这类三维非对称结构对台风运动(转向现象)有一定“引导”作用。文中还强调了“β陀螺”偶极子非对称结构的垂直差异,并揭示了目标台风暖心结构及其热力非对称结构特征。 相似文献
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INTERACTION BETWEEN TROPICAL CYCLONE AND MEIYU FRONT 总被引:3,自引:0,他引:3
Generally speaking,the convection activities are inactive over western Pacific warm pool andtropical cyclone(TC)activity seldom occurs over the offshore of East Asia during the period ofMeiyu rainfall.However,if a TC is active in this area,the Meiyu rainfall will often weaken or endup.Based on a statistical study with the data from 1980 to 1995,it is found that about 91% of 23TC activities affected the intensity of Meiyu rainfall,and 50% of the end-up of Meiyu events wererelated to the active TCs and the change of subtropical high.The present paper simulates the effectof TC on Meiyu circulation by using MM4 model,and the results agree with the observations.From the point of view of vapor and energy transport,the landing of TC cuts not only thetransport of the water vapor to Changjiang-Huaihe River basin from the Bay of Bengal but also theconversion of the mean flow energy to the Meiyu circulation because of the TC forcing to the zonalcirculation.These two effects make the convection and perturbation existing in Meiyu region lackthe supply of the vapor and energy for their maintenance and lead to the end of Meiyu rainfall. 相似文献
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