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 sun by ozone molecules in the stratosphere. This absorption process heats the air at these altitudes. The concentration of ozone is highest in the lower stratosphere, and this concentration gradually decreases as one ascends towards the stratopauzához. Consequently, the highest temperatures are found at or near this boundary.

The altitude of the stratopauzához varies depending on latitude and season. Generally, it is found at an average altitude of about 50 kilometers (31 miles) above the Earth's surface. However, it can be higher over the equator and lower over the poles. The temperature at the stratopauzához can reach approximately 0 degrees Celsius (32 degrees Fahrenheit), making it significantly warmer than the colder temperatures found at the top of the mesosphere. Understanding the stratopauzához is crucial for atmospheric research, particularly in studies related to ozone depletion and climate change.