highatmosphere
The high atmosphere refers to the upper layers of Earth's atmosphere, typically above the troposphere and extending up to the exosphere. This region is characterized by its thin air and extreme conditions, making it a challenging environment for both human exploration and scientific study. The high atmosphere is divided into several layers, each with distinct properties.
The stratosphere begins at the tropopause, around 10-15 kilometers above sea level, and extends up to about
Above the mesosphere lies the thermosphere, which extends from 85 to 600 kilometers. This layer is characterized
The high atmosphere plays a crucial role in Earth's climate and weather systems. It influences the distribution
Despite its importance, the high atmosphere remains one of the least explored regions of Earth's atmosphere.