willem2 said:
That's certainly what I meant also. I got that quote from the wikipedia page about Kirchhoff's law of radiation.
Since the atmosphere does emit IR radiation, it must also be able to absorb it. There's plenty of radiation about. Why doesn't this happen? You still have given no reason why it doesn't happen.
Hi willem:
Thanks for your post. Sorry if I misunderstood your previous question.
It does happen. I confess that the concepts in my elaboration below are guesses, since I haven't studied anything in detail about this particular physical phenomenon.
When an atmospheric molecule interacts with another atmospheric molecule, a thermal photon will/may be emitted, and possibly two photons, one from each molecule. This would be characterized as stimulated emission. Such photons are subsequently likely to be absorbed by a similar molecule, and then soon after, spontaneously re-emitted. These re-emitted photons and then also likely to be absorbed by a similar molecule.
This emission -> absorption -> re-emission -> absorption ->... sequence will continue perhaps many times until instead of a photon:
(1) being absorbed, it will finally (a) hit the Earth, or (b) escape into space; or
(2) being re-emitted, the excited molecule will hit another molecule.
The number of photons that hit the Earth in this scenario is about the same as the number which escape into space. This is because such a re-emitted photon is equally likely to be headed downward as upward.
The next scenario is the normal (non-greenhouse) effect which increases the Earth's temperature from what it would be with no atmosphere. Following the heating of the atmosphere by conduction-convection, all of these emissions/re-emissions and absorption of the thermal black-body photons are non-thermal, in that a molecule's being excited from its absorption of a photon does not make the gas warmer. However, when two molecules collide, and no photon is emitted, the energy of the excited state will add to the kinetic energy of one or both of the colliding molecules, and this will make the atmosphere warmer. So, both the thermal and non-thermal re-emitted photons that hit the Earth return some of the energy from the Earth back to the Earth. This is NOT a violation the thermodynamics law about a cold body not being able to heat a warmer body. The warmer Earth is in thermal equilibrium with the cooler atmosphere, and there are net exchanges of heat from the Earth warming the atmosphere, with some of that heat being returned to the Earth, reducing what would otherwise be a warmer atmosphere.
When a greenhouse molecule absorbs a photon, it also is involved in a similar scenario of repeated re-missions and absorptions. Although it is rare for an excited molecule to collide before it re-emits a photon, it can happen. When it does, the small number of cases when it does results in some slight warming of the atmosphere.
So far I have ignored clouds. When a photon from Earth, or re-emitted from a water vapor molecule, hits a water droplet in a cloud, and is absorbed by a water molecule, the excited molecule is much more likely to collide before it re-emits a photon. This is because the molecules in a liquid drop are much closer together than they are in a gas. Therefore, these photons heat the water droplets, which in turn by conduction thermally warm the atmosphere gasses.
I hope this answers your question.
Regards,
Buzz