台风中-α尺度重力惯性波的发展与暴雨增幅
THE RELATION BETWEEN THE DEVELOPMENT OF MESO-αSCALE INTERNAL INERTIAL GRAVITY WAVE AND THE ENHANCEMENT OF RAINSTORM
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摘要: 通过数值模拟和诊断研究得出,9216号台风暴雨的增幅过程与台风中-α尺度重力惯性波的发展、传播,非均匀层结的分布以及积云对流潜热反馈有关。大尺度非线性平流项的作用激发出大尺度的重力惯性波,积云对流潜热加热作用导致非地转风场扰动大大加强,从而使重力惯性波波幅加大,上升运动增强,暴雨加大。当重力惯性波向稳定度减小的方向传播时,波能量最易加强。Abstract: By numerical study and diagnostic analysis for Typhoon 9216,it is found that the process of the typhoon rainstorm is associated with the development and propagation of meso-α-scale intertial gravity wave(IGW),the distribution of heterogeno us stratification and the latent heat feedback of cumulus convection.The nonlinear advection for large scale excites the large scale IGW.The heating of cumulus convection latent heat feedback is responsible for the strengthening the ageostrophic wind,whose effect gives rise to the development of IGW amplitude,ascending motion and rainstorm.When IGW propagates along the direction in which the degree of stability is decreased,the IGW energy is reinforced easily.
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Key words:
- Typhoon /
- Cumulus convection /
- Internal inertial gravity wave /
- Rainstorm
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