How does radiation fog typically dissipate?

Radiation fog dissipates primarily because the sun heats the air, which in turn allows the moisture in the fog to evaporate. This phenomenon occurs during the daytime when solar radiation increases. As the sunlight warms the ground, it causes the temperature of the air just above it to rise. This warming process initiates the evaporation of water droplets that make up the fog, leading to a gradual clearing of the foggy conditions.

While factors like precipitation, wind shifts, and atmospheric pressure can affect fog and its persistence, they are not the primary mechanisms for the dissipation of radiation fog. Increased precipitation would typically contribute more to the formation of fog rather than its dissipation. Wind shifts can lead to changes in weather patterns but are not a direct cause of evaporating the fog. Changes in atmospheric pressure influence weather systems but do not directly interact with the fog's composition to lead to its dissipation. Thus, the most direct and effective mechanism for dissolving radiation fog is the heating of the air by sunlight, allowing the moisture to evaporate.