Frysningsnivå
Frysningsnivå, also known as the snow line or freezing level, refers to the altitude in the atmosphere at which the air temperature is 0 degrees Celsius (32 degrees Fahrenheit). Above this level, the temperature is consistently below freezing, while below it, temperatures are generally above freezing. This phenomenon is crucial in understanding atmospheric processes, particularly precipitation and cloud formation.
The frysningsnivå is not a fixed altitude but varies significantly depending on geographical location, season, and
The presence of the frysningsnivå dictates the form of precipitation. When precipitation forms above the frysningsnivå,