Scale Height is playing a big role once the atmosphere passes a certain mass relative to the planet's mass.
The atmosphere layer's thickness.
The more massive a planet is the more atmosphere it takes to get the atmosphere reach higher above the surface, because of gravity. For the same reason the pressure will go up with more atmosphere mass.
Pressure and gravity are working against each other and it's only at and above a certain Matmosphere / Mplanet ratio that gravity gets the upper hand. Below that ratio, gases would simply escape.
Infrared Emissivity mostly refers to your planet cooling down and not so much to reflecting light of IR wavelength. With a thick layer of atmosphere containing reflective stuff the IR light of both sources will hit the surface more often, bouncing between surface and greenhouse contributors. Also while (visible) light is escaping the planet it's wavelength slightly shifts towards red and eventually infrared, contributing to the effect because visible light is also reflected and hence bounces as well, shifting a little towards red each time it goes "up".