rannikuoludes
Rannikuoludes, a term originating from Estonian, translates to "coastal fog" or "sea fog." It refers to a meteorological phenomenon characterized by a dense layer of fog that forms over or near coastal areas. This type of fog typically arises when warm, moist air moves over a colder sea surface. The cooling of the air to its dew point causes water vapor to condense into tiny water droplets, forming the visible fog.
Coastal fog is a common occurrence in many parts of the world with significant coastlines, particularly in
The formation and persistence of rannikuoludes are influenced by several factors, including wind direction and speed,