Methane GWP for the IPCC Method #118
Replies: 3 comments
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We are using data from Table 7.SM.7 (pdf here), which was pulled directly from here. The difference seems to mostly stem from:
You are correct that we did defer to the non-fossil factor for methane. see #97 I welcome @Andrew809 to chime in here on the choice of table for these data. |
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if you are curious, the raw data was compiled into a single csv here. We could probably do a better job linking those back to the specific tables used in each case. |
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Thanks for pointing out the difference and the csv version! I'm sure it would've been helpful to us before now. I welcome whatever other information you can provide on the choice of table (factor) here. The 7.SM.7 looks like it's the GWP from a pure radiative forcing perspective, and I think makes sense if your goal is to provide a single value for methane, regardless of source. FWIW, for AR5, I believe we were one of the few organizations using a 100-yr GWP value of 36 for methane, which included the climate carbon feedbacks and the +2 adder for fossil methane oxidation given that the vast majority of methane emissions in our life cycle models are from fossil sources (coal mines and natural gas). |
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Assuming I did this correctly, I get an AR6, 100-yr characterization factor 27.9, which aligns with the value in the data file. The 27.9 doesn't match up with any of the values provided in Table 7.15 of AR6:
Where did the 27.9 factor come from?
Secondly, I guess is the matter for which value gets mapped to FEDEFL emission/air/methane (for example). The AR5, 100-yr factor for methane in my mapping is 28, which suggests the "non-fossil" factor is being used there. So for AR6, would we expect the same mapping if there were separate fossil and non-fossil factors for methane?
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