Leaving no more than 40 % as
Radiant Energy transfer, with 24 % of that 40 % as direct loss to Atmospheric Window.
However, if extra CO2 reduces the cooling rate of the Earth surface, and the rate of
radiant energy transfer from Sun to Earth surface is little changed, then the Earth surface will warm (other things being equal) from what it was before the increase in CO2.
Not exact matches
PS when molecular collisions are frequent relative to photon emissions and absorptions (as is generally the case in most of the mass of the atmosphere), the
radiant heat absorbed by any population of molecules is
transfered to the heat of the whole population within some volume, and molecules that emit photons can then gain
energy from other molecules.
It is the density, not the composition which gives more or less opportunities for such instances of
energy transfer between molecules whilst the incoming and outgoing
radiant energy is negotiating the atmosphere.
The
radiant heat we feel from a fire is the fire's thermal
energy, its heat
energy — we can feel heat
energy transferred by radiation (as well as by conduction and convection).
This is heat
energy transferred by radiation, direct to us who feel the heat on our skin and absorb it deeply and feel it internally as this aka
radiant heat heats up the water in us, heats our blood and flesh and bones..
No surface can emit
energy any faster than
energy can be
transferred to the
radiant surface.
If the average
radiant layer were 288K @ 390Wm - 2 and you didn't have to consider other non-
radiant means of
energy transfer, that would be a fair estimate.
Terrestrial radiation absorbed by CO2 is immediately thermalized, i.e. the
radiant energy absorbed by CO2 molecules is immediately (about 0.1 nanosecond)
transferred (in a process similar to thermal conduction) to other atmospheric molecules which outnumber CO2 molecules 2500 to 1.
Radiant energy accounts for all of the outbound
energy at the top of atmosphere, but only a fraction of the
energy transfer at the surface.
The main issue is an understanding of the physical processes regarding density and the
energy transfer along with the conversion of
radiant energy to mechanical
energy and the currents of the oceans.
The fundamental equation of radiative
transfer at the emitting surface of an astronomical body, relating changes in
radiant -
energy flux to changes in temperature, is the Stefan - Boltzmann equation --
whereF is
radiant -
energy flux at the emitting surface; εis emissivity, set at 1 for a blackbody that absorbs and emits all irradiance reaching its emitting surface (by Kirchhoff's law of radiative
transfer, absorption and emission are equal and simultaneous), 0 for a whitebody that reflects all irradiance, and (0, 1) for a graybody that partly absorbs / emits and partly reflects; and σ ≈ 5.67 x 10 — 8 is the Stefan - Boltzmann constant.
In the atmosphere, you do not have a closed system, so such thermal equilibrium can hardly be present, given that all manner of things, are driving
radiant energy into any volume of atmosphere, as well as conductive, and mass transport (convective)
energy transfers are taking place.