ilmastokerrosten

Ilimastokerrosten refers to the layered structure of Earth's atmosphere. These layers are primarily defined by their distinct temperature profiles, which change with altitude. The lowest layer, closest to the surface, is the troposphere, where temperature generally decreases with increasing height. This is where most weather phenomena occur. Above the troposphere is the stratosphere, characterized by a temperature increase with altitude due to the absorption of ultraviolet radiation by ozone. The mesosphere follows, where temperatures decrease again with height, reaching the coldest temperatures in the atmosphere. The thermosphere is above the mesosphere, and in this layer, temperatures increase significantly due to the absorption of high-energy solar radiation. Finally, the exosphere is the outermost layer, where the atmosphere gradually thins and merges with outer space. Each of these ilmastokerrosten plays a crucial role in regulating Earth's climate and protecting life from harmful solar radiation.