Our analysis shows that reductions in OH during the COVID-19 period (2020–2021), followed by a recovery through 2023, accounted for ~80% of the interannual variations in the CH4 growth rate. These reductions were linked to declines in NOx and CO emissions from human activities during the COVID-19 lockdowns, which temporarily weakened the oxidizing capacity of the atmosphere. When OH rebounded, the methane sink strengthened, slowing the growth rate.
The study is here.