What type of fog is likened to sea fog?

Advection fog is formed when warm, moist air moves horizontally over a colder surface, typically water, which cools the air mass and causes condensation to occur. This type of fog is commonly associated with coastal areas, particularly where warm ocean currents meet cooler air masses. As such, it is indeed likened to sea fog because both types are generated by the interaction between moist air and cooler surfaces, creating a thick fog that can significantly reduce visibility.

In coastal regions, the warmer air from the sea can create conditions favorable for the formation of advection fog, especially when it drifts over cooler sea waters. This is particularly common in the early morning or late evening when temperature differences are most pronounced. The resemblance to sea fog lies in its reliance on similar environmental conditions and processes, making advection fog a specific type of fog commonly observed along coastlines.