Warm,moist air blowing over cold water can result in

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When warm, moist air blows over cold water, the moisture in the air can condense to form fog. This is because the colder water cools the air, reducing its ability to hold moisture, which causes the water vapor to condense into tiny droplets that make up fog. Adiabatic cooling is the cooling of air as it rises due to expansion, but it is not directly related to the scenario described. Dry adiabatic rate and orographic lifting are not applicable to this situation.

Warm,moist Air Blowing Over Cold Water Can Result in