Generally, ozone is most ample at high latitudes, close to the poles, and least considerable within the tropics, close to the Equator. Basically, taking all that into account, you can imagine the atmosphere reaching equilibrium, a scenario during which the entire amounts of ozone and oxygen do not change. Ozone is definitely very uncommon—there’s hardly any of it, in comparison with the enormous quantities of unusual oxygen within the ambiance.
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