On Thu, 17 May 2007, [EMAIL PROTECTED] wrote:
> I am trying to understand the greenhouse effect in more detail and
> stumbled upon this page:
> http://www.applet-magic.com/atmostemp.htm (beware your eyes, and
> decrease the font size)
> It has a derivation using radiation laws for an equation to calculate
> the temperature profile of the atmosphere:
> T(x) = [(S/σ)((xmax−x) +1)]1/4
> where S is the net energy per unit area received from the Sun, and x
> the optical path length. Can someone confirm if this is correct?
>
> Now, if I would increase the absorption, so multiplying xmax and x by
> a factor  > 1, the temperature would rise for all x, so this would not
> lead to a cooling in the upper layers as predicted by the greenhouse
> effect. Of course, this model does not include the ozone layer (where,
> as I understand it, the conditions are somewhat reversed). Would it be
> correct to say that the stratosphere would not cool because of the
> greenhouse effect if it were not heated in the first place by the UV
> radiation? I understand that it cools because CO2 (and other
> greenhouse gases) cool the stratosphere because they increase the
> emissivity. Is that correct?

See 
http://mustelid.blogspot.com/2005/03/why-does-stratosphere-cool-under-gw.html

-W.


> Oliver
> (the guy behind http://fermiparadox.wordpress.com/)
>
>
> >
>

William M Connolley | [EMAIL PROTECTED] | http://www.antarctica.ac.uk/met/wmc/
Climate Modeller, British Antarctic Survey | 07985 935400
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