Evaporation fog
(Section 3.2.1.1.1)
- Evaporation fog (or cold advection fog) is formed when cold, stable air moves over a much warmer body of water. Evaporation from the warm body of water saturates the cold air above; water vapour condenses in the cold air producing “steam fog” or “sea smoke”, or, in polar regions, “Arctic sea smoke”.
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