Evaporation Fog: Warm water evaporates into cooler air above it. This adds moisture to the air, which can then condense into fog. For fog to dissipate, we need to separate the air temperature away ...
Fog, a cloud of water droplets or ice crystals that form close to the earth’s surface, occurs as a result of the air temperature reaching its dew point, which is its maximum water saturation.
The cool surface of the water brings the air temperature down to the dew point, allowing fog to form. Then, Grigsby said, you need just enough wind to blow the fog inland without lifting it too ...