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the lower environment, have an effect on ozone by reducing stratospheric temperatures and by strengthening the stratospheric circulation. The observed international ozone depletion prior to now four a long time is attributable to increases in reactive halogen gases in the stratosphere (see Q13).Satellite tv for pc devices have been routinely monitoring ozone, reactive chlorine gases, and temperatures in the world stratosphere. Reactive gases containing the halogens chlorine and bromine lead to the chemical destruction of stratospheric ozone. The source gases, which embrace ozone-depleting substances (ODSs), are emitted at Earth’s surface by natural processes and by human actions (see Q6).

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