The stratosphere is the atmospheric layer located above the troposphere, the place most climate phenomena happen. Extending from roughly 10 to 50 kilometers above the Earth’s floor, it’s characterised by a secure temperature gradient, rising with altitude because of the absorption of ultraviolet radiation by the ozone layer. This area is essential for safeguarding life on Earth from dangerous photo voltaic radiation.
This secure atmospheric area performs a significant function in world local weather and atmospheric circulation patterns. The ozone layer inside it absorbs the vast majority of the Solar’s dangerous ultraviolet-B (UV-B) radiation, shielding life beneath. Its distinct temperature stratification additionally influences the propagation of sound waves and the dispersion of volcanic aerosols. Understanding its composition and dynamics is essential for predicting long-term local weather tendencies and assessing the impression of human actions on atmospheric chemistry.
