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. 2018 Sep 10;115(39):9720–9725. doi: 10.1073/pnas.1809276115

Fig. 1.

Fig. 1.

Average N2O and CH4 fluxes. The GWP of N2O is three and nine times higher than CH4 over 20 and 100 y, respectively. Therefore, the climate impacts of N2O are more dominant than those of CH4 in the longer term (i.e., 100 vs. 20 y). The error bars represent the ±95% confidence interval.