Stratoshere

The Stratosphere

The stratosphere is a layer of the Earth’s atmosphere that starts above the tropopause (the boundary between the troposphere and stratosphere) and extends up to an altitude of approximately 160,000 feet. In this layer, temperatures increase with altitude due to the absorption of ultraviolet radiation by ozone in the ozone layer. The stratosphere is a crucial part of the Earth’s atmosphere that helps to protect life on Earth by absorbing most of the sun’s harmful UV rays. It is also where airplanes and weather balloons fly, and where phenomena such as the polar vortex and the ozone hole occur. The stratosphere is an important area of study in atmospheric science, as it plays a significant role in weather patterns and global climate. Overall, the stratosphere is a fascinating and complex layer of our atmosphere that helps to sustain life on Earth.