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The Effect of Asymmetric Wind Structures of Tropical Cyclones on Their Tracks
作者姓名:XIANG Jie  WU Rongsheng
作者单位:Key Laboratory of Mesoscale Severe Weather/MOE,Department of Atmospheric Sciences,Nanjing University,Nanjing 210093 Institute of Meteorology,PLA University of Science and Engineering,Nanjing 211101,Key Laboratory of Mesoscale Severe Weather/MOE,Department of Atmospheric Sciences,Nanjing University,Nanjing 210093
基金项目:This research is jointly supported by the National Natural Science Foundation of China under Grant Nos. 40075011 and40633030, and the State Key Basic Program: CHERES.
摘    要:1. IntroductionStudies on the tracks of tropical cyclones (TCs)have been one of the core problems in TC dynamics.In earlier researches, TCs are often viewed aspoint vortices, Rankine vortices. For example, Yeh(1950) and Kuo (1969), adopting dynamical methods,studied the motions of TCs and the effects of environ-ments. Their findings indicated that the motion tracksof TCs are characterized by cyclonic trochoidal oscil-lations.Syono (1955), by solving the barotropic vorticityequation, obta…

收稿时间:2003/9/12 0:00:00
修稿时间:2004/4/21 0:00:00

The Effect of Asymmetric Wind Structures of Tropical Cyclones on Their Tracks
XIANG Jie,WU Rongsheng.The Effect of Asymmetric Wind Structures of Tropical Cyclones on Their Tracks[J].Acta Meteorologica Sinica,2005,19(1):52-59.
Authors:XIANG Jie WU Rongsheng
Institution:Key Laboratory of Mesoscale Severe Weather/MOE, Department of Atmospheric Sciences, Nanjing University, Nanjing 210093;Institute of Meteorology, PLA University of Science and Engineering, Nanjing 211101 Key Laboratory of Mesoscale Severe Weather/MOE, Department of Atmospheric Sciences, Nanjing University, Nanjing 210093
Abstract:A model is proposed relating a variety of factors of tropical cyclones (TCs) to their tracks, and attentions are paid to the influence of the asymmetric wind structures of TCs. Ideal numerical calculation shows that the asymmetric wind structures of TCs have conspicuous influence on their motion tracks. When moving due westward initially, an axisymmetric TC will deflect right, and the overall trend is eastward. When it is asymmetric but the asymmetry is not sharp, wherever the area of maximum wind is, the TC deflects northwest first, and then, to various areas depending on the positions of the areas of maximum wind, i.e. for the area of maximum wind in Quadrant I, to the southeast; for in Quadrant to the northeast; for in Quadrant to the northwest; for in Quadrant to the southwest. And in the above four cases, the TC tracks are all accompanied by clockwise looping motions. With the asymmetry of the TC intensifiying, the track of the TC motion will be stretched further. For the area of maximum wind in Quadrants the TC tracks are still accompanied by clockwise looping motions; for the area of maximum wind in Quadrants the TC tracks become oscillatory, without clockwise looping motions.
Keywords:tropical cyclone  asymmetric wind structure  tracks of tropical cyclones
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