Spring advection fog, radiation fog in winter.
春季为平流雾，冬季为辐射雾。
The way to forecast sea advection fog from evaporation duct
由海面蒸发波导预报平流海雾的方法
The inversion in the radiation fog is thick and strong, but weaker or no inversion in advection fogs.
辐射雾逆温厚而强，平流雾则为弱的逆温或无逆温。
The surface southeast wind is a condition for the generation of advection fog, but it contributes to the disappearance of radiation fog.
底层东南风是平流雾生成的条件, 却对应于辐射雾的消亡
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