Stromnessens

Stromnessens is a term that refers to a phenomenon observed in certain coastal regions, particularly in Scandinavia. It describes a specific type of fog that forms when cold, dry air moves over a warmer body of water. The moisture from the warmer water evaporates and condenses in the colder air, creating a dense fog. This fog is often characterized by its low-lying nature and its tendency to cling to the water's surface. Stromnessens can significantly reduce visibility, impacting maritime activities and coastal transportation. The term itself is derived from Swedish and is sometimes translated as "sea smoke" or "steam fog." The conditions necessary for stromnessens to form include a significant temperature difference between the air and the water, with the water being considerably warmer. This phenomenon is most common during the autumn and winter months when the sea retains heat longer than the surrounding air. While it can occur in various locations with similar meteorological conditions, it is most frequently associated with the Baltic Sea and the Norwegian coast. The visual appearance of stromnessens can be quite dramatic, with thick white plumes rising from the water.