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, growing 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 an important function in world local weather and atmospheric circulation patterns. The ozone layer inside it absorbs nearly all of the Solar’s dangerous ultraviolet-B (UV-B) radiation, shielding life under. Its distinct temperature stratification additionally influences the propagation of sound waves and the dispersion of volcanic aerosols. Understanding its composition and dynamics is vital for predicting long-term local weather developments and assessing the influence of human actions on atmospheric chemistry.
