Fig. 5: Comparisons of marine isoprene flux and AOD with monthly tropospheric column densities of NO2 and ozone in CEPO from August 2015 to December 2020. | npj Climate and Atmospheric Science

Fig. 5: Comparisons of marine isoprene flux and AOD with monthly tropospheric column densities of NO2 and ozone in CEPO from August 2015 to December 2020.

From: Geostationary satellite reveals increasing marine isoprene emissions in the center of the equatorial Pacific Ocean

Fig. 5

The data were grouped into 300 × 400 bins with data counts no less than 100 (Supplementary Fig. 7). a NO2 is likely to determine the enhancement rate of AOD from marine isoprene in CEPO. The dashed line represents the regression line of binned data with NO2 column densities higher than 2.5 × 1014 molecules cm−2, and the solid line represents that with NO2 column densities lower than 2.4 × 1014 molecules cm−2. b Lower ozone abundances were observed when marine isoprene emission and AOD were both higher.

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