JDoolin said:
Aren't the mechanisms behind glass, and the mechanism behind greenhouse gasses the same in principle? The glass is transparent to visible light... It let's the visible light penetrate to the ground, which absorbs part of that light as heat. Then the ground re-emits the light (largely) in the infrared spectrum. The glass is opaque to the infrared spectrum so this heat cannot escape.
Heat can still escape through the glass, via conduction. But it can no longer escape via radiation.
Conceptually, I think this model is great, and almost perfectly analogous to greenhouse gasses. For greenhouse gasses, they are transparent to the incoming light, and then they are opaque to the outgoing light. Once they absorb 100% of that outgoing light, you're concerned about their heat-conductivity properties instead of their band-pass properties.
However the reason that the OP's experiment wouldn't work, if I'm right, is that whatever transparent container holds the gas will also interfere with the transparency and the conductivity of the gas. But in principle, if you had a perfectly transparent container material that wouldn't block any light at all in any wavelength... e.g. an "ideal glass" we could at least approach the idea "gedanken"-style... Am I right?
Greenhouses primary reason for heat trapping is that they stop convection circulation. Ordinarily, hot air rises and is replaced by cooler air. The glass enclosure stops that. So it is a bit wrong to say the mechanism is based on transmission limits in the infrared by the glass.
Let'sthink said:
As I understand and I think correctly, that Green house effect is in essence conversion of lower wavelengths in the Sun's energy to higher wavelength near infrared regions which can heat up the medium more efficiently.
That is almost right. The sunlight that hits the Earth is in a broad spectrum. The Earth re-radiates energy as black-body radiation. That black body radiation is SCATTERED and ABSORBED and RE-RADIATED. Those mechanisms trap some of the infrared energy. The black-body temperature of the Earth must be at a steady state, exactly re-radiating the Sun's incident energy back into space. If the Earth had no atmospheric blanket, the black-body temperature that balances the Sun's "solar constant" would be about 0-degrees F (IIRC). The Earth's average surface temperature is about 60-degrees-F. Changes to the Earth's atmospheric blanket will change the amount of energy that gets retained. That moves the black-body temperature higher, which moves the radiation profile (this is a physics board, someone probably even knows the formula off the top of their head, I use google). A new steady state is arrived at with a slightly higher temperature.
The experiment you describe is simply absorbance spectroscopy. Different gases have different absorption spectra. You could also fill two bottles, one with black paint and one with white paint, and put them in the same sun. One would have a higher black-body temperature (if I am using the words correctly) ... it would be the black one. It is somewhat trivial to deduce that absorption spectrum changes the steady state temperature. But just as you could mix one drop of the black paint into the white paint and see a slight change in temperature, if you mix a gas that has absorption in the spectrum passing thru that space into a gas that has less, there is a slight temperature increase.
I'm not sure if that precise experiment has been done. I considered something similar as a simple bit of work to propose to a group of kids as a science fair project.
But the step from absorption spectrum to energy re-distribution should be one which is strong theoretically.
The sun radiates as a body at a very high temperature. That is the spectrum hitting the Earth surface. The Earth radiates as a body at a much lower temperature. That is the spectrum leaving the Earth surface. In between, there is an atmosphere.
That bit of science is remarkably simple. There are a LOT of other things that matter though. The Earth's albedo ... how much sunlight is reflected directly back into space. Heat capacity and phase changes matter in the energy flow. The Sun's solar constant matters. Heat energy from the Earth's core matters. Some people choose to regard the changes to the Earth's atmospheric blanket as trivial, when compared to other factors. I think that while the system may be complex, the atmospheric factor is large and important. There are feedback loops that are both positive and negative. In particular the heat capacity if the oceans, ocean currents and temperature mixing, the phase changes of water, and the changes in net albedo ... those all can create a lot of noise in the data.
I am always a bit confused by the use of averages in these systems. If you look at the moon, which has no atmosphere, and is generally (barring eclipses) sunlit on one side and dark on the other, the sunlit side is WAY warmer than the dark side. Is it truly accurate to speak of the AVERAGE temperature as the black body radiation profile of re-emitted radiation? Is it equivalent energy outflo? EG, if right now it is 70-degrees-F at noon for me, and on the other side of the earth, at midnight, it might be 50-degrees-F. Is the energy flow from those two points the same as if they were two points at the AVERAGE temperature of 60-degrees-F?
And I know ... I could do the math myself. But I'm being lazy.