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锋生锋消对于梅雨锋附近有无降水起到了重要的作用。Frontogenesis and frontolysis have decisive effect on the precipitation near Meiyu front.

用一个具有解析解的二维动力锋生成过程算例，对比自适应网格方案和固定网格方案的优劣。A two dimensional kinematic frontogenesis process is studied for examing the use of adaptive grids in numerical model.

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矢量锋生函数分析表明大气斜压性的作用不可忽视。Q vector frontogenesis function further indicated that the function of the atmospheric baroclinicity could not be overlooked.

最后探讨梅雨锋与对流之关系，及对流潜热释放在梅雨锋生过程所扮演之角色。Finally, the relation of the front and convection as well as the role of convective latent heating on the Meiyu frontogenesis was discussed.

在高空平直的西风环流下，沿南支西风急流带，有低压槽在冷空气垫之上东移，地面高气压区域中常有低压槽和锋生出现。At this time if a trough in the south branch of the westerlies moves eastward over this cold cushion, then there offen appears a trough and frontogenesis in the region surface high.

高低空急流的建立及维持，强锋生区的持续触发作用，是本次连续性暴雨维持的重要原因。The maintaining mechanisms of the heavy rainfall also include the establishment and maintenance of the upper- and lower-level jets, and the continual triggering of strong frontogenesis.

矢量锋生函数计算分析表明，该环流圈形成了暴雨区与东北远距离的西风带系统之间的能量转换机制。Q-vector frontogenesis function analysis indicated that such circulation cell generated energy transforming system between torrential rain area and the distant westerly to the northeast.

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锋生使得湿等熵面倾斜，在锋区前侧产生显著的正垂直涡度变化，切变线得到快速发展。The frontogenesis tilts the wet isentropic surface and produces significant positive vertical vorticity change in front of the frontal zone, which results in the fast development of shear line.

结果表明，温度平流和涡度平流、沿岸锋生以及高空急流的动力作用对气旋暴发性发展有重要贡献。The results show that the dynamic functions of thermal advection, vorticity advection, coastal frontogenesis and air jet stream made great contribution to the explosive development of the cyclone.

利用假湿绝热假定，导得简化的半地转湿锋生模式，利用该模式讨论大尺度凝结加热对暖锋锋生过程的影响。A simplified semigeostrophic frontogenesis model with inclusion of large-scale condensation latent heat is derived and the effects of latent heat release on frontogenesis of warm front are discussed.