“…Being a secondary pollutant, the generation as well as mitigation of tropospheric O 3 largely depend on multiple factors, such as the dynamics of emission sources for precursor molecules, the ratio and saturation levels of the available precursor molecules, alteration of meteorological variables, and others [19][20][21]. Based on the source and sink mechanism, the precursors such as nitrogen oxides (NO X : NO and NO 2 ), volatile organic compounds (VOCs) including benzene, toluene, ethylbenzene, xylene (BTEX), the proportion of NO X to VOCs [19][20][21], along with the meteorological variables like solar radiation intensity, temperature, relative humidity, wind speed, and rainfall [22][23][24][25], play a key role in the synthesis of O 3 in the troposphere. Reshmi et al [26], while discussing the relations of precursor molecules with O 3 formation in the Kannur city, India, pointed towards a negative correlation with NO X, but positive correlation with carbon monoxide (CO).…”