What meteorological phenomenon is likely to occur on the leeward side of a lake when warm air moves over it?

When warm air moves over the cooler waters of a lake, a common meteorological phenomenon that can occur is the formation of fog. This happens because the warm air can hold more moisture than cooler air. As it moves over the cooler lake surface, the temperature of the air is reduced, leading to condensation. The moisture in the air cools and condenses into tiny water droplets, forming fog. This phenomenon is particularly pronounced when the air is significantly warmer than the water, enhancing the likelihood of condensation and fog development.

In contrast, rain would typically require more dynamic weather conditions such as frontal lifting or significant moisture accumulation in the atmosphere, which are not specifically induced by simply moving warm air over a lake. Snow is a cold-weather phenomenon that requires temperatures to be at or below freezing. Thunderstorms usually develop in conditions that involve rising warm, moist air leading to convection, a more complex scenario than merely moving over a lake.