Enhanced atmospheric oxidation toward carbon neutrality reduces methane's climate forcing.

By contrast, the global OH abundance in the SSP370 scenario exhibits a decreasing trend of 0.037‒0.15% yr −1 ( P < 0.001) over 2015‒2100 among these models, together with an increase in tropospheric O 3 of 0.11‒0.17% yr −1 ( P < 0.001) (Supplementary Figs. 3 and 4 ).

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