Stratoszferikus

Stratoszferikus is a term used to describe the stratosphere, which is a layer of the Earth's atmosphere that is situated above the troposphere. The stratosphere is a relatively stable layer of the atmosphere, extending from the upper troposphere to the lower mesosphere, approximately 15 kilometers or 9 miles high. This layer is characterized by a decrease in temperature with altitude, which is in contrast to the troposphere, where temperatures generally increase with height.

The stratosphere is divided into two sub-layers: the lower stratosphere, which is the portion of the layer closest to the troposphere, and the upper stratosphere, which is the upper portion of the layer closest to the mesosphere. The lower stratosphere is characterized by a low level of atmospheric circulation and relatively stable weather conditions. The upper stratosphere is characterized by a high level of atmospheric circulation and variable weather conditions.

The stratosphere plays a crucial role in the Earth's climate system, as it is the layer in which the ozone layer is found. The ozone layer, which is a critical component of the stratosphere, absorbs the majority of the sun's ultraviolet radiation and prevents it from reaching the Earth's surface. The stratosphere is also an important factor in the formation of high-altitude clouds and the generation of weather patterns. Overall, the stratosphere is a vital component of the Earth's atmosphere and plays a significant role in the planet's climate system.