Over the last 16 years, the atmospheric CH4 level measured at Mauna Loa Observatory rose from 1.8431 ppmv in 2016 to 1.9135 ppmv in 2022, which is a mere 0.0704 ppmv change (= a 3.82% increase in 16 years). By my calculation, that increase caused a total radiative forcing of about 0.035 W/m². With feedbacks, that's enough to cause only about 0.02 °C of warming.
0.02 °C is about the temperature change you get from a ten foot change in elevation, or a 1.2 mile change in latitude. It's about 1/70-th of the "hysteresis" (a/k/a "dead zone" or "dead band") designed into a typical home thermostat. That's what space.com calls a "termination event."
For comparison, over the same 16-year period, the atmospheric CO2 concentration rose from 404.41 ppmv in 2016 to 418.56 ppmv in 2022, That's a 14.15 ppmv change (= a 3.50% increase in 16 years). That increase caused a total radiative forcing of about 0.15 W/m². With feedbacks, that's enough to cause about 0.1°C of warming.
Even if you don't burn it, methane in the atmosphere oxidizes fairly rapidly, changing ultimately into small amounts of CO2 and water:
CH4 + 2⋅O2 → CO2 + 2⋅H2O (caveat: that's very simplified!)
Various sources give the half-life of CH4 in the atmosphere as 6 to 8 years, which would make the average lifetime 1.4427 times that, yielding an average lifetime for a molecule of CH4 in the atmosphere of 8.7 to 11.5 years. The AMS gives a figure of 9.1 years. (That's from Pranther et al 2012, but Pranther actually reports it as 9.1±0.9 years.) However, Prof. Lyatt Jaeglé has identified a feedback mechanism which she believes effectively increases the atmospheric lifetime of additional CH4 to about 12 years.
So call it 8-12 years. That's pretty short. It means the only reason CH4 levels are as high as they are (about 1.9 ppmv = 5.58 Gt) is that total CH4 emissions (natural + anthropogenic) are already high (between 550 and 710 Mt/yr). There would have to be a very large, sustained increase in CH4 emissions to cause much increase in long-term average atmospheric CH4 levels.
CH4 removal processes (mainly oxidation) dwarf the rate of CH4 accumulation in the atmosphere, and they accelerate with increasing atmospheric methane concentration, making them negative (stabilizing) feedbacks. Assuming the Pranther atmospheric lifetime estimate (9.1±0.9 years), we can calculate that the rate of increase in CH4 level (which averages about 0.0044 ppmv/year) is less than 1/40-th of the rate of the CH4 removal processes, and less than 1/25-th the rate of anthropogenic emissions.
That's very different from CO2. Natural CO2 removal processes are also linearly related to the atmospheric CO2 concentration, but for CO2 the net natural removals are only about 50% of the rate of anthropogenic CO2 emissions, compared to 96% for CH4.
That means the CH4 does not accumulate in the atmosphere. Instead, the CH4 level responds quickly to changes in CH4 emission rate. If the total CH4 emission rate were to cease increasing then the level of CH4 in the atmosphere would rise at most only a few percent before plateauing.
It's a shame to see space.com publishing such misinformation.