JDoolin said:
Well, yes, I do question how significant the changes in CO2 concentrations are... But I think I can make that question more explicit:
From
http://www.skepticalscience.com/saturated-co2-effect-advanced.htm
What does it mean when it says "if we recall that the absorption coefficient is gaussian"? Why is it that the "absorption dip ... becomes wider"
I can comment on the "guassian" part.
First, I would never say an absorption
coefficient is Gaussian. An absorption coefficient is by definition at a specified wavelength. Any absorption of radiated energy is best modeled as a single quanta of energy, that raises an internal system to an allowed/stable excited energy level. The easy ones to understand are the hydrogen atom with it single electron moving up and down between the orbitals. Infrared is energy that corresponds to the molecular bonds between atoms.
If the molecules were perfectly the same in every state, then the absorption would be exactly at a single wavelength. But the reality is that there are always slight differences. Consider two excited CO2 molecules that emit exactly the same photon of energy. But one is traveling toward you, and the photon is slightly blue shifted, and one is traveling away, and the photon is slightly red shifted. The average would then be at the non-moving, but there would be guassian distribution fom velocity around that. Consider that molecules are colliding. There can be a deformation of the energy states of each molecule by that collision. Say that the bond length of one molecule is momentarily shorter and the other is bent to momentarily longer. The absorption energy levels are then changed by that tiny amount. It will again be guassian around the mean. If the molecules are constantly colliding in a gas, and they are constantly vibrating as a result, then there can be quite a bit of spread to what might otherwise be a very perfectly defined energy gap. We just can't measure absorption in perfect isolation, so we end up with every spectroscopic peak being wider than a single wavelength.
Your link kept crashing on me so I can't fully comment on its arguments. But ...
I'm not sure I follow the argument about CO2 saturation. Anytime you work with a spectrometer, you have a beam of light. You can always stick a piece of cardboard in, and block the light. A second piece of cardboard doesn't see any light. Once you've blocked it all, you've blocked it all. There is always a goal in measuring absorption of a chemical to use the lowest possible concentration. The Beer-Lambert law applies. I've followed chemical reactions using spectroscopy, and it is important to know the extinction coefficient for the wavelength you are using, and to not have the particular chemical outside of the concentration window for which that applies. In a spectrometer, you use a defined path length ... for the atmosphere, it could be quite a bit longer.
Simply saying that CO2 shows saturation of absorption is sort of obvious. Everything does. The bottom of the ocean is quite dark, even though a meter of seawater is pretty transmitting of light. Go far enough, and it adds up. The same is surely true with anything. Longer path-lengths and higher concentrations will deviate from Beer's law.
Look at the spectra collected from space shown in post 771. Maybe there is an argument for CO2 absorption already being maximized at the central wavelength. I'm not convinced that the peak broadening is insignificant though.