What is a common location to observe Advection Fog?

Advection fog is commonly observed in coastal regions due to the movement of warm, moist air over a cooler surface, typically the ocean or cold land. This phenomenon occurs when the air temperature decreases to the dew point as it moves horizontally, causing condensation to form in the atmosphere. In coastal areas, the interplay between warm, moist maritime air and cooler ocean waters creates ideal conditions for the development of advection fog.

In contrast, desert areas generally have low humidity and sparse moisture, which makes fog formation unlikely. Mountain tops tend to have colder, drier conditions, leading to different types of fog, such as radiation fog. Forested regions may produce moisture-laden air, but the combination of temperature and moisture needed for advection fog is less common compared to coastal settings. Thus, coastal regions are the most representative and frequent locations where advection fog is observed.