The world will warm more than expected due to future changes in ozone, which protects the Earth from harmful sun rays but also traps heat as it is a greenhouse gas.



Summary

Future ozone depletion in the upper atmosphere, particularly over the tropics and mid-latitudes, will lead to less warming than previously predicted, as less heat will be trapped there. However, increases in ozone in the lower atmosphere will have the opposite effect, trapping more heat and exceeding prior warming expectations. This shift is due to changes in atmospheric circulation patterns driven by climate change itself, which are redistributing ozone. Overall, the net effect suggests a greater warming potential than previously estimated, highlighting the complex interplay between ozone and global climate change.

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