At about 90 km up, I note that the atmosphere of Venus cools down to very low temperatures in the vicinity of -112 deg C. I suspect this is the CO2 thermal
radiation escape altitude there.
Not exact matches
At lower
altitudes the repeated
radiation and absorbtion acts to reduce the
escape to one of diffusion.
Because the lapse rate is not zero, changing the
altitude near the top of the atmosphere where infrared
radiation escapes freely to space allows adjustment of the surface temperature by means of the addition of greenhouse gases.
The term «photosphere» for a star has essentially the same meaning as any of the six terms «Effective -LCB- Emission
Radiation Radiating -RCB--LCB- Height Level -RCB-» for the atmosphere of a planet, being the
altitude at which the gas above has an optical depth of 2/3, i.e. at which about 50 % of the
radiation leaving that
altitude vertically upwards
escapes to space.
So the thermal energy transported to high
altitudes, must be ultimately converted to Electro - magnetic
radiation, in order to
escape the planet.
The full picture is a bit more complex as some
radiation can
escape to space from all
altitudes of the atmosphere and the surface.
A small localized change in surface temperature can cause a convection burst (thunderstorm) and a large increase in convection height, improving both reflection of incoming solar
radiation, and conveying sensible heat to a higher
altitude where it can then
escape to space via radiative processes with far less interference.
The
radiation in the absorption spectrum of GHG's finally
escapes into outer space directly from higher
altitudes where the gases are cooler and the rate of radiaton is reduced.
This interpretation is essentially the converse of the point (made years earlier by Nils Ekholm) that
radiation escaping the atmosphere is controlled by the effective
altitude of the radiating layer.
With sufficient warming, the same radiative transfer equations show that upward IR will rise enough for sufficient quantities to
escape to space, albeit at a higher
altitude than before, warmed sufficiently so that its IR emissivity allows OLR to balance incoming absorbed
radiation.