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Wrong way around. Tropospheric (ground level) ozone is a component of photochemical smog. It is made by the interaction of ultraviolet light, volatile hydrocarbons and nitrogen oxides. Other products of this reaction include polycyclic hydrocarbons (PAHs)

Stratospheric ozone (hig level) is made by the interaction of oxygen atoms and ultraviolet light.

The two locations only interact when stratospheric ozone is downwashed by the jet stream passing over high mountain into the troposphere.

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