海岸锋生 Coastal frontogenesis
The water vapor was carried from the lower to higher troposphere by the strong updraft,and enhanced the local precipitation. The heavy precipitation zone was located on the coastal front and its cold side.
强烈的上升气流携带低层水汽在空中辐合和凝结,使局地降雪增强,强降雪落区位于海岸锋及其冷区一侧。
参考来源 - 山东半岛一次暴雪过程的海岸锋三维结构特征·2,447,543篇论文数据，部分数据来源于NoteExpress
海洋热通量是海岸锋形成的关键因子， 其中感热通量使海陆温差加大是形成海岸锋锋生的重要条件。
The sensible and latent heat fluxes from the ocean are the key factors for the formation of coastal front, especially, the sensible heat flux is more important to the coastal frontogenesis.
这类天气系统包括雷暴，阵风锋，陆龙卷，沿海岸湖面或山脉的大风，大雪及冻雨。
Included in this category are thunderstorms, gust fronts, tornadoes, high winds especially along coasts, over lakes and mountains, heavy snow and freezing precipitation.
应用推荐