期刊文献+

对南海热带气旋近海加强机理个例模拟研究 被引量:19

A CASE SIMULATION STUDY ON OFFSHORE INTENSIFICATION MECHANISM OF TROPICAL CYCLONE IN SOUTH CHINA SEA
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摘要 利用具有完备物理过程的中尺度模式MM5对发生于南海的0214号热带气旋(TC)“黄蜂”进行高分辨率的数值模拟,以此来研究热带气旋在近海发展为强热带风暴过程中结构变化对强度的作用,并对近海加强的内部动力机理做一些探讨。模拟结果发现在加强阶段,气旋环流中存在类似于涡旋Rossby波性质的波动在西北侧对流激发下绕中心逆时针传播,波动与眼墙区对流带相耦合,使得眼区趋于闭合;中尺度涡旋系统的轴对称化过程,通过与对称环流系统非线性相互作用,向气旋环流提供能量,其自身也得到维持与发展。这些结构的变化对TC近海加强和登陆后迅速减弱都产生了重要的影响。 Full physical model MM5 has been used to simulate tropical cyclone “Huang-Feng” in August 2002. Adapting high resolution grids, the effect of structure changes on intensity in the process of intensification was investigated. The simulation catches evolution details to support further analysis. During the process of intensification, there exist two different synoptic systems in the two sides of TC circulation. One is deep subtropical high, which stretches westwards and led adequate vapor into inner core; the other is cold votex located in the west of TC, which induced cold air to surrounding of TC circulation through middle level to increase instability. These environmental conditions were favorable for TC intensification. According to vortex-Rossby waves (VRW) theory to explore the mechanism of TC intensification, the results confirm that there exists Vortex-Rossby like waves, which are initiated by convection as perturbation source in the northwest of TC circulation. Vortex-Rossby waves, coupled with eyewall convective band and spiral rain band outside, propagate cyclonically in the process of intensification. Ultimately the propagation of waves leads to form a complete eye structure in the minimum botton of sea level pressure. Mesoscale vortices axisymmetrization are found to transfer energy to parent vortex through nonlinear interaction. Meantime vortices also experience self-maintain and development process. These factors impact on the offshore intensification. After landfall, vapor channel is cut off and cold air penetrates low level to strengthen stability of troposphere. These unfavorable conditions weaken the convective activity and lead to decay of TC intensity.
出处 《气象学报》 CAS CSCD 北大核心 2005年第3期359-364,共6页 Acta Meteorologica Sinica
基金 国家自然科学基金重点项目(40231005)
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参考文献10

  • 1Montgomery M T, Kallenbach R J. A theory for votex Rossby-waves and its application to spiral bands and intensity change in hurricanes. Quart J Roy Meteor Soc, 1997, 123: 435-465
  • 2May P T, Holland G J. The role of spiral rainbands in tropical cyclones. J Atmos Sci. 1999, 56: 1224-1228
  • 3Montgomery M T, Enagonio J. Tropical cyclogenesis via convectively forced vortex Rossby waves in a three-dimensional quasigeostrophic model. J Atmos Sci,. 1998, 55: 3176-3207
  • 4Moller J D, Montgomery M T. Tropical cyclone evolution via potential vorticity anomalies in a three-dimensional balance model. J Atmos Sci, 2000, 57: 3366-3387
  • 5余志豪.台风螺旋雨带——涡旋Rossby波[J].气象学报,2002,60(4):502-507. 被引量:66
  • 6钟科,康建伟,余清平.飓风中的涡旋罗斯贝波[J].气象学报,2002,60(4):436-441. 被引量:12
  • 7MaCalpin J D. On the adjustment of azimuthally perturced vortices. J Geophy Resear, 1987, 92: 8213-8225
  • 8罗哲贤.台风轴对称环流和非轴对称扰动非线性相互作用的研究[J].中国科学(D辑),2003,33(7):686-694. 被引量:19
  • 9Chen Y, Yau M K. Spiral bands in a simulated hurricane. Part I: Vortex Rossby wave verification. J Atmos Sci,2001, 58: 2128-2145
  • 10Carr L E,Williams R T. Barotropic votex stability to perturbations from axisymmetry. J Atmos Sci, 1989, 46: 3177-3191

二级参考文献25

  • 1黄荣辉.冬季低纬度热源异常对北半球大气环流影响的物理机制[J].中国科学,1986,:89-103.
  • 2Anthes R A 李毓芳 等.热带气旋的发展、结构和影响[M].北京:气象出版社,1982.46-47.
  • 3Elsberry 陈联寿 等.热带气旋全球观[M].北京:气象出版社,1994.72-75.
  • 4钟科.飓风Andrew(1992)的中尺度扰动结构和动力诊断分析:(学位论文)[M].南京:中国人民解放军理工大学气象学院,2000.59.
  • 5曾庆存.旋转大气中运动的非线性相互作用和旋转适应过程[J].中国科学,1979,(10):986-995.
  • 6Zeng Qing-cun. On the evolution and interaction of disturbances and zonal flow in rotating barotropic atmosphere. J Meterorol Soc Japan, 1982, 60:24~31.
  • 7Elsberry R L. Global perspectives on tropical cyclones. World Meteorological Organization Technical Document, No 472,1995, 106~197.
  • 8Melander M V, McWilliams J C, Zabusky N J. Axisymmetrization and vorticity-gradient intensification of an isolated two-dimensional vortex through filamentation. J Fluid Mech, 1987, 178:137~159.
  • 9McCalpin J D. On the adjustment of azimuthally perturbed vortices. J Geophy Resear, 1987, 92:8213~8225.
  • 10Carr L E III, Williams R T. Barotropoic vortex stability to perturbations from axisymmetry. J Atmos Sci, 1989, 46:3177-3191.

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