stratopauzához
The stratopauzához, often referred to as the stratopause, is a boundary layer in Earth's atmosphere situated between the stratosphere and the mesosphere. This region is characterized by a significant temperature inversion, meaning temperature increases with altitude, a stark contrast to the layer below it. The stratopause marks the point where the temperature reaches its maximum within the stratosphere before beginning to decrease again in the mesosphere.
The existence of the stratopauzához is primarily due to the absorption of ultraviolet (UV) radiation from the
The altitude of the stratopauzához varies depending on latitude and season. Generally, it is found at an