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Once within the stratosphere, the source gases–which alone don’t destroy ozone–chemically degrade to kind ozone-depleting chemicals, corresponding to chlorine and chlorine monoxide. No one knows for certain how much more ozone depletion will occur. There is a substantial time lag between the time when ODS emissions begin to decline and the point at which the ozone layer begins to recover. It takes years for CFCs and other ozone-depleting compounds to succeed in the stratosphere. Many of them can persist in the stratosphere for centuries; some have life spans of 25 to 400 Amazing national football league pittsburgh steelers full printing shirtyears. Almost all of the CFCs and halons ever released are still in the atmosphere and will proceed to destroy ozone for many years to return. Ozone depletion is immediately associated to the temperature within the stratosphere. This is as a result of stratospheric clouds, which have an necessary role within the chemical destruction of ozone, solely form at temperatures below -78°C. These polar stratospheric clouds contain ice crystals that can flip non-reactive compounds into reactive ones, which may then quickly destroy ozone as soon as light from the sun becomes out there to energise the chemical reactions.
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