Vikaantuminen
Vikaantuminen, also known as inversion, is a meteorological phenomenon where a layer of warm air is situated above a layer of cooler air. This situation is the opposite of the normal atmospheric stratification, where temperature generally decreases with altitude. Inversion layers can form under various conditions, such as during the night when the ground cools rapidly, leading to a cooler layer of air near the surface. Inversions can also occur due to the presence of a warm air mass moving over a cooler surface, like a cold ocean current.
Inversions have significant impacts on weather patterns and air quality. They can trap pollutants near the
Inversions can be temporary or persistent, depending on the underlying causes. Temporary inversions often dissipate with