(June 7, 2017 at 6:17 pm)Alex K Wrote: I think I'm addressing the right crowd here: I am trying to quantitatively understand the greenhouse effect on a back-of-envelope level. I've worked out the equilibrium temperature w/o greenhouse gases. Does anyone know a not too difficult explanation how to take into account the co2 blanketing effect in that radiation balance as a function of the %?
I know an atmospheric scientist (retired). If I see him tomorrow at my carving class, I'll try to remember to ask.
If you get to thinking you’re a person of some influence, try ordering somebody else’s dog around.
