Fig. 4: Observed and simulated atmospheric CH4 and δ13C-CH4 from TM5 atmospheric modeling. | Communications Earth & Environment

Fig. 4: Observed and simulated atmospheric CH4 and δ13C-CH4 from TM5 atmospheric modeling.

From: Improved global wetland carbon isotopic signatures support post-2006 microbial methane emission increase

Fig. 4

a, b Model-data comparison of long-term trend of (a) atmospheric CH4 from 1985 to 2016 (in ppb) and (b) δ13C-CH4 from 1999 to 2016 (in ‰) by observation (gray) and simulations from Scenario A (yellow), B (red), C (blue), and D (skyblue). c Model-data comparison of normalized north–south gradient of atmospheric δ13C-CH4 for Scenario A (yellow), B (red), and C (blue) in 2012. The north–south δ13C-CH4 was calculated by zonally-averaging the surface δ13C-CH4 and normalized based on the mean δ13C-CH4 at 60–90 °S. The normalized north–south δ13C-CH4 for other years is in Supplementary Fig. 20 and Supplementary Table 9. d Histogram of the difference between simulated and observed δ13C-CH4 for Scenario A (yellow), B (red), and C (blue) for 6 measurement sites located in the northern hemisphere. The histogram plots for all measurement sites are in Supplementary Fig. 22. Information about Scenarios A–D is in Table 1.

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