A region of Earth's stratosphere that absorbs most of the Sun's harmful ultraviolet radiation.The ozone layer is a region of Earth's stratosphere, roughly 15 to 35 kilometers above the surface, that contains a relatively high concentration of ozone (O₃) molecules. Its primary role is to absorb most of the Sun's harmful ultraviolet (UV) radiation, particularly the most energetic UV-B and UV-C bands. Without this shield, life on Earth's surface would be exposed to radiation levels capable of causing severe DNA damage, skin cancer, and disruption of ecosystems.
The ozone layer's existence was discovered by French physicists Charles Fabry and Henri Buisson in 1913, and its role in absorbing UV radiation was identified by Gordon Dobson in the 1920s. The severe depletion of the layer by chlorofluorocarbons (CFCs) was announced by British Antarctic Survey scientists in 1985, leading to the Montreal Protocol in 1987.
Ozone molecules absorb UV photons through a photochemical cycle. When UV radiation strikes an O₃ molecule, it splits into an O₂ molecule and a single oxygen atom, converting the photon's energy into heat. This process, and the subsequent recombination of oxygen atoms with O₂ to reform ozone, continuously converts dangerous high-energy UV into harmless thermal energy, effectively acting as a protective filter in the stratosphere.
The ozone layer is essential for protecting human health and agriculture; its monitoring guides international policy on ozone-depleting substances, and its recovery is tracked via satellite and ground-based instruments.
The ozone layer, if compressed to sea-level pressure, would be only about 3 millimeters thick.

















