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underneath the auspices of the United Nations Framework Convention on Local weather Change (UNFCCC). Halocarbons within the atmosphere contribute to both ozone depletion and local weather change.
Tropospheric ozone will increase consequence from the emission of air pollutants and lead to surface warming whereas stratospheric ozone depletion results in a small forcing that most probably cools the floor. Will increase within the abundances of those gases from human actions cause extra outgoing infrared radiation to be absorbed and reemitted back to the

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