Stratospheric chemistry refers to the study and understanding of chemical processes that occur in the stratosphere, which is a layer of Earth's atmosphere located between 10 and 50 kilometers above sea level. This region plays an important role in regulating our planet’s climate by absorbing some of the Sun's ultraviolet radiation through the ozone layer. Stratospheric chemistry involves studying how various chemical reactions, such as those involving ozone depletion and the formation of other atmospheric gases like nitrous oxide (N2O) and halocarbons, occur in this region. Understanding these processes is crucial for predicting future climate changes and developing strategies to mitigate their impacts on our planet's environment.