migla

Migla refers to a specific type of dense fog that occurs in certain regions, particularly coastal areas and river valleys. It is characterized by its low visibility, often reducing it to a few meters or even less. The formation of migla is typically associated with conditions of high humidity and a significant temperature difference between the air and the ground or water surface. This can happen when warm, moist air moves over a cooler surface, causing water vapor to condense.

Geographically, migla is often reported in areas prone to fog, such as the Baltic Sea coast, parts of Eastern Europe, and river deltas. The term itself is of Slavic origin, with "migla" directly translating to fog or mist. The visual appearance of migla can vary, from a light haze to an opaque blanket that obscures all but the closest objects. Its presence can significantly impact transportation, leading to delays and hazards for road, sea, and air travel. While it can create atmospheric beauty, its practical implications are often disruptive. The duration of migla events can range from a few hours to several days, depending on the prevailing meteorological conditions.