Tropospheric ozone is recognized as the third most important contributor to the positive radiative forcing, based on its increases since 1750, following carbon dioxide (CO 2) and methane (CH 4 ; Myhre et al., 2013). Ozone is a secondary air pollutant, which is not emitted directly, but is produced through chemical reactions of precursor gases in the atmosphere, such as nitrogen oxides (NO x), carbon monoxide (CO), methane, and non-methane volatile organic compounds (NMVOCs). Ozone precursors are mainly emitted by human activities, such as fossil fuel combustion, residential burning, oil and gas production, agriculture, and biomass burning. Observations from aircraft, ozonesondes, and different satellites show that the tropospheric ozone burden has been increasing in the second half of the 20th century (Gaudel et al., 2018; Hemispheric Transport of Air Pollution [HTAP], 2010). Both satellite ozone measurements and global chemical transport models have found that the largest ozone burden increases-about +6 to +7 Dobson units (i.e., ∼15%-20% of average background ozone) from 1980 to 2016-are over India, Southeast Asia, and East Asia (Ziemke et al., 2019). Previous studies have demonstrated that methane emissions affect global ozone with little dependence on the location of emissions (Fiore et al., 2008). For short-lived ozone precursors, the global tropospheric ozone burden (B O3) responds differently to emission changes from different world regions, with generally