1. Cooler water temperatures. The temperature of the water near the coast is often cooler than the temperature of the land. When warm, moist air from the land moves over the cooler water, it cools and condenses into fog. This is why fog is most common in the morning and evening, when the temperature difference between the land and the water is greatest.
2. Wind direction. The prevailing wind direction in coastal areas is often from the ocean. This means that the moist air from the ocean is constantly being blown over the land, where it can cool and condense into fog.
3. Geographic features. The geography of coastal areas can also contribute to fog formation. For example, cliffs and headlands can help to channel the flow of moist air from the ocean, which can lead to fog formation.
These factors all contribute to the fact that cities near the coast have more fog than inland areas.
Here are some additional factors that can contribute to fog formation in coastal areas:
Pollution: Air pollution from vehicles, factories, and other sources can increase the number of particles in the air, which can act as nucleation centers for water droplets to form on. This can lead to an increase in fog formation.
Upwelling: Upwelling is a process that brings cold water from the depths of the ocean to the surface. When this cold water reaches the surface, it can cool the air above it and lead to fog formation.
El Niño: El Niño is a climate pattern that causes the Pacific Ocean to become warmer than usual. This warm water can lead to an increase in fog formation along the coast of California and other parts of the Pacific Ocean.