Numerical simulation of interaction of strong mesoscale convective cloud systems and formation of tropical cyclone
中尺度强对流云系相互作用与热带气旋形成的数值模拟

This paper is a sequel of the theory of Multi-scale Organization of Formation of Tropical Cyclone. The theory is supported by a new fact- numericalsimulation results. The results verify the presentation of "the amplification effect of the vortex in tropical atmosphere (AEVTA)" further. Moreover , the results also explain the formation of predepression of tropical cyclone in quantity.