The stratosphere, located between the troposphere and the mesosphere, is characterised by a temperature inversion, which means temperatures enhance with altitude. This area, dwelling to the ozone layer, performs a vital position in absorbing dangerous ultraviolet radiation from the solar. A notable instance of stratospheric phenomena is the formation of nacreous clouds, also called polar stratospheric clouds, that are composed of ice crystals and nitric acid and are sometimes noticed in polar areas throughout winter.
This atmospheric layer’s stability and distinctive temperature profile are essential for a number of causes. The ozone layer’s presence inside the stratosphere protects life on Earth from dangerous photo voltaic radiation, making it important for the existence of various ecosystems. Moreover, the steady situations inside the stratosphere affect long-range climate patterns and the worldwide circulation of air lots. Scientific exploration of this area, commencing with early balloon ascents within the early twentieth century, continues to yield beneficial insights into atmospheric chemistry, dynamics, and the influence of human actions.
