The weak cold advection or the water evaporation from the wet surface after sunrise during the dense fog episode is apt to cause the burst broadening of the fog droplet spectrum.
结果指出,雾滴谱爆发性拓宽是在降温速率加大(即过饱和度加大)条件下出现的,浓雾阶段地面的弱冷平流及日出后湿地表水分蒸发都易引起雾滴谱爆发性拓宽。
参考来源 - 辐射雾雾滴谱拓宽的微物理过程和宏观条件·2,447,543篇论文数据,部分数据来源于NoteExpress
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