What describes the formation of advection fog?

Advection fog forms when moist air moves horizontally over a colder surface, such as cool land or water. As the warm, moist air comes into contact with the cooler surface, the air's temperature decreases. If the temperature drops enough to reach the dew point, condensation occurs, resulting in the formation of fog. This process is distinctly different from the other options, which do not accurately capture the essential mechanism of advection fog.

For instance, dry air mixing with warm air typically leads to other phenomena, such as brief rain showers or turbulence, but does not create fog. Options related to high humidity during cold weather or saturated air over mountain ranges pertain to different weather formations, like radiation fog or orographic lifting, rather than directly describing the advection process leading to fog. Therefore, the correct answer highlights the crucial interaction between the moving moist air and the cooler surface that triggers the fog's formation.