锋生是促使新锋面形成或原有锋面加强的过程。
在暴雨持续阶段，散度项锋生和形变项锋生作用旗鼓相当，倾斜项起锋消作用。
The continuous stage in the rainstorm, effects of divergence and deformation are equal in match or contest of strength, effect of tilting term is frontolysis.
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.
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.
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