Yesterday, Eli showed that surface warming depends on the average distance that an IR photon will travel before being absorbed by a greenhouse gas molecule. Today, some riffs.
Looking at a high resolution IR spectrum looking down from more than 30 km
and it is clear that there is little overlap and most of the concentration is from CO2. If you add up the absorbance between 620 and 720 cm⁻¹ the total from CO2 would be 30 times that from H2O.
If you asked how much of the IR would be absorbed in a 10 km path (the troposphere) by water vapor in this spectral region the answer would be pretty much all of it. That's what you get from the usual figure that is shown in such discussions elsewhere, or at least that there is a great amount of overlap
But that's the wrong question. The right one is, of the IR emitted from the surface, how much of it is absorbed by CO2 and how much by H2O, and there, the answer is CO2 absorbs essentially all of it in the first few meters so very little is left for water vapor to absorb.
Bunnies can ask, well, what is the distance at which the absorbance is 1 (~2/3 of the IR, or to be more exact 63%, is absorbed). At high resolution this is pretty confusing to look at
but it does look like very little gets more than 30 m or so. By averaging over 1 cm⁻¹ the picture becomes clearer
So, remembering yesterday's lesson, in this region of the spectrum, essentially all of the surface warming is controlled by CO2 back radiation and none of it by water vapor (there is, of course some convection and condensation, but radiative emission and absorption are the primary effect.
By implication this means that a significant part of the urban heat effect is driven by CO2 backradiation.
Perhaps tomorrow the rest of the IR spectrum and the minor greenhouse gases.
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