When sources describe global warming potential of different gasses, such as in this paper on radiative forcing, methane and tropospheric ozone respectively are given GWP values of around 29 and 65. However, when I look at spectra for the three gasses or diagrams showing outgoing blackbody radiation from the earth, it doesn't look like the radiative forcing effect for methane and tropospheric ozone should be that much higher than CO2. I've hunted around a bit, and have seen the same values for GWP of methane and ozone in many sources, but haven't been able to figure out why those gasses are so much more potent than CO2.
Why is the global warming potential of tropospheric ozone and methane so high?