Fig. 3: Correlation of δ18O-NO3− values with ozone, BrO and day length in the Northern and Southern Hemispheres. | npj Climate and Atmospheric Science

Fig. 3: Correlation of δ18O-NO3 values with ozone, BrO and day length in the Northern and Southern Hemispheres.

From: Hemispherical scale mechanisms of nitrate formation in global marine aerosols

Fig. 3

Panels af show the relationship between δ18O-NO3 and O3 (a and b), BrO (c and d), and day length (e and f), respectively. The monthly average O3 from 2006 to 2021 (the time range of all field observation cruises) for eight latitude bands (0–10°N, 10–30°N, 30–60°N, 60–90°N, 0–10°S, 10–30°S, 30–60°S, and 60–90°S) were obtained from National Aeronautics and Space Administration Ozone Watch (NASA Ozone Watch, https://ozonewatch.gsfc.nasa.gov/). The correlation between δ18O-NO3 and O3 is the average O3 value in a certain latitude range (one out of the eight bands) in a specific month corresponds to the average δ18O-NO3 value in that latitude range during that month. The monthly average BrO for eight latitude bands were obtained from the GOME-2 satellite instrument28 and the data presented by Schmidt et al.20. Each sample corresponds to a day length value according to the sampling date and latitude. Solid lines represent the linear regressions and the light shading represents the 95% confidence intervals.

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