On Sat, 25 May 2013 22:08:33 +0200, Poutnik wrote:
>
>Wally W. posted Sat, 25 May 2013 15:56:38 -0400
>
>> >Not in case of existance downward radiation.
>>
>> On a planetary basis as viewed from space, it doesn't matter whether
>> there is "downward radiation" as observed from the surface.
>
>At surface level, it means surface can afford high temperature,
>wit net flux the same as at -15 or -18 without down radiation.
The energy flows in this link
http://eesc.columbia.edu/courses/ees/climate/lectures/radiation/
may be rewritten:
heat absorbed by (planet + atmosphere) = (1 - a) * pi * R^2 *S_o
heat radiated from (planet + atmosphere) = (4* pi * R^2) * sigma *
T^4
The energy balance is:
(1 - a) * pi * R^2 *S_o = (4* pi * R^2) * sigma * T^4
There is one temperature in this energy balance.
For a planet with no atmosphere, T is measured at the surface of the
planet.
For a planet with an atmosphere (with or without a surface), T is
measured in the atmosphere.
If you disagree with this, please explain why.
>> >> >allowing higher temperatures
>> >> >than theoretized low Te.
>> >>
>> >> What is low about Te when measured at the outer fringe of the
>> >> atmosphere?
>> >
>> >Te means SURFACE radiation.
Only for a planet with no atmosphere.
>>
>> It means effective planetary temperature as viewed from space.
>
>It is kept, and for non absorbing air
>would be mean temperature of surface.
>
>With our air Te,mean is stil those -15 or -18,
>but it is integral parameter of Te = f(lambda)
Needless complication in this discussion.
>> >> What do you think the temperature at the outer fringe of the
>> >> atmosphere should be, if not the -18�C calculated in the link above?
>>
>> You didn't answer this question.
>
>This temperature is unrelated to Te.
No, it is not. If it is, please explain as requested above.
>> >Why do you think it is wavelength independent ?
>> >I am afraid you are rather confused here.
>>
>> Not so much. There is heat flux in and heat flux out. On a planetary
>> basis, as viewed from space, they are equal; regardless of the mix of
>> wavelengths.
>
>Totally yes, Per wavelength it is more complicated.
>Overall, the original Te is kept.
More complicated, but not relevant to this discussion.
>> >and this is your confusion.
>> >Te is for surface without absorbing atmosphere.
>>
>> It is also the effective temperature of a planet with an atmosphere
>> but no surface.
>
>Nonsense.
No it is not. Why do you think *every* planet in the universe must
have a surface?
>> Or do you think Jupiter can't have an effective temperature because it
>> has no surface?
>
>It has surface in sense of solid body radiation.
How much sunlight reaches that "surface"?
>> There is "downward radiation" if there is any object between the
>> source of radiation and the surface.
>
>Explain.
See Figure 3 on page 7 here:
https://www.jstage.jst.go.jp/article/jtst/5/2/5_2_303/_pdf
Any intermediate surface with create/experience "backradiation"
regardless of its size. It need not be an entire atmosphere.
>> >> No, it is not. The "greenhouse effect" singles out particular
>> >> wavelengths of light. The energy balance in the link above allows the
>> >> atmosphere to emit all wavelengths of light.
>> >
>> >Hardly.
There is nothing about wavelengths in the energy balance equation.
>> See above. Either the flux in equals the flux out, or the planet
>> melts.
>
>Unrelated.
No, it is not.
Why do you say it is?
>Some are emitted by surface due atmospheric windows.
It doesn't matter to an observer in space whether the radiation comes
from the surface or the atmosphere.