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adjustments to wind patterns, temperature and precipitation throughout the Southern Hemisphere decreasing the oceans potential to behave as a carbon sink (less sequestering of carbon). Conversely, says the 2015 report, local weather change may improve the manufacturing in marine environments of brief-lived halogens (e.g., methylene chloride, bromoform) that cause depletion of ozone in the stratosphere and troposphere.Different modifications in local weather associated with ozone layer depletion embrace adjustments to wind patterns, temperature and precipitation across the Southern Hemisphere. The solar UV radiation has the potential to contribute to climate change via its stimulation of

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