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that industrially produced chlorofluorocarbons (CFCs) decompose in the stratosphere and release chlorine atoms, resulting in catalytic ozone destruction.Ultraviolet radiation from the Solar is responsible for many complicated photochemical reactions characteristic of the upper environment; e.g., the formation of the ozone layer through ultraviolet dissociation of oxygen molecules followed by recombination to type ozone. That portion of the environment from Earth’s surface to the stratosphere; that is, the bottom 10 to twenty km of the atmosphere. A very powerful hint gases contributing to the greenhouse effect are water vapor, carbon dioxide, ozone, methane, ammonia, nitric acid, nitrous oxide, ethylene,

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