This article might benefit from a bit more numerical data: CO₂ Radiative Forcing:
1950: Approximately 0.58 W/m² @ 310 ppm
2020: Approximately 2.13 W/m² @ 414 ppm
CH₄ Radiative Forcing:
1950: Approximately 0.25 W/m² @ 1.15 ppm
2020: Approximately 0.59 W/m² @ 1.86 ppm
Methane in the atmosphere is oxidized to CO2 with about a 6-year halflife, so:20-year timescale: CH₄ is approximately 84-87 times more efficient than CO₂. 100-year timescale: CH₄ is approximately 28-34 times more efficient than CO₂. The other thing to keep in mind is the removal rate: > "Roughly 56% of annual fossil CO₂ emissions are absorbed by natural sinks—29% by the biosphere and 23% by the oceans—while 44% remains in the atmosphere, driving global climate change. For CH₄, 90% is removed by atmospheric oxidation within roughly a decade, with a small fraction absorbed by soils." The bottom line? If human civilization really wants to stabilize the concentration of CO2 and CH4 in the atmosphere - which ideally will lead to a stabilization of global temperature and a new climate normal (certainly warmer and wetter, much like Pliocene conditions of 2-5 mya), then elimination of fossil fuel combustion as an energy source really is the only plausible option. |
That's an interesting scaling. For a ~30% increase in ppm, it's ~400% in W/m^2