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Statistical characteristics of meso-scale vortex effects on the track of a tropical cyclone

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【作者】 罗哲贤孙治安平凡

【Author】 Luo Zhe-Xian a)d) ,Sun Zhi-An b) ,and Ping Fan c)d) a)Remote Sensing College,Nanjing University of Information Science and Technology,Nanjing 210044,China b)Center for Australian Weather and Climate Research,GPO Box 1289K,Melbourne,Australia c)Lab of Cloud-Precipitation Physics and Severe Storms (LACS),Institute of Atmospheric Physics,Chinese Academy of Science,Beijing 100029,China d)Wuxi Research Center for Environment Science and Technology,Wuxi 214031,China

【机构】 Remote Sensing College,Nanjing University of Information Science and TechnologyWuxi Research Center for Environment Science and TechnologyCenter for Australian Weather and Climate ResearchLab of Cloud-Precipitation Physics and Severe Storms (LACS),Institute of Atmospheric Physics,Chinese Academy of Science

【摘要】 This paper examines initial meso-scale vortex effects on the motion of a tropical cyclone (TC) in a system where coexisting two components of TC and meso-scale vortices with a barotropic vorticity equation model. The initial meso-scale vortices are generated stochastically by employing Reinaud’s method. The 62 simulations are performed and analysed in order to understand the statistical characteristics of the effects. Results show that the deflection of the TC track at t=24 h induced by the initial meso-scale vortices ranges from 2km to 37 km with the mean value of 13.4 km. A more significant deflection of the TC track can be reduced when several initial meso-scale vortices simultaneously appear in a smaller TC circulation area. It ranges from 22 km to 37 km with the mean value of 28 km,this fact implies that the initial meso-scale vortices-induced deflection may not be neglected sometimes.

【Abstract】 This paper examines initial meso-scale vortex effects on the motion of a tropical cyclone (TC) in a system where coexisting two components of TC and meso-scale vortices with a barotropic vorticity equation model. The initial meso-scale vortices are generated stochastically by employing Reinaud’s method. The 62 simulations are performed and analysed in order to understand the statistical characteristics of the effects. Results show that the deflection of the TC track at t=24 h induced by the initial meso-scale vortices ranges from 2km to 37 km with the mean value of 13.4 km. A more significant deflection of the TC track can be reduced when several initial meso-scale vortices simultaneously appear in a smaller TC circulation area. It ranges from 22 km to 37 km with the mean value of 28 km,this fact implies that the initial meso-scale vortices-induced deflection may not be neglected sometimes.

【基金】 supported by the National Natural Science Foundation of China (Grant Nos. 40775038,40875031 and 40975036);the Science Foundation of Wuxi Environment Science and Technology Research Center
  • 【文献出处】 Chinese Physics B ,中国物理B , 编辑部邮箱 ,2011年04期
  • 【分类号】P444
  • 【被引频次】2
  • 【下载频次】32
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