Some planets you do have purple atmospheres. What gases these atmospheres have? Oxigen? These planets are in Baramal and some systems. Also, the planets in Doctor Who Universe have purple and pink atmospheres.

Nice. I think he goes astray a little with the green/yellow/red skies from Rayleigh scattering as the atmosphere thickens, however.Eburacum wrote:My colleague Stephen Inness, at OA, has written this essay on sky colour,, if it is of any help
Odd. Just looking at a distant horizon shows us that blue light is also scattered near the surface of the Earth, between our eyes and distant mountains.Eburacum wrote:One interesting fact that used to be on Les Cowley's excellent Sundog site (but isn't there any more) is that the blue colour in a clear sky is caused by Rayleigh scattering int he thin upper atmosphere; lower down the scattering was negated by destructive interference (speaking from memory)
Just looking at a distant horizon shows us that blue light is also scattered near the surface of the Earth, between our eyes and distant mountains.
Rayleigh scattering is, almost by definition, at the molecular level, since the particles have to be of a size comparable to the wavelength of visible light. Most particulate matter is too big for Rayleigh scattering - it scatters all wavelengths equally, and so introduces a white haze. So it's the blueness of distant objects seen on a clear day that lets us know molecular-level scattering is happening in the intervening space.eburacum45 wrote:I think that might be Rayleigh scattering due to small particles and droplets; the scattering in the upper air occurs between widely spaced air molecules.
Distant mountains look bluish ... This blue veil is called airlight. Airlight is most evident when the sky is clear and is seen against distant objects.
Airlight is simply sunlight that is scattered by air molecules between us and the mountain.
...
Haze can masquerade as airlight. Unlike true airlight which is blue, haze appears grey, white or brown.
I remembered something on your site about
Rayleigh scattering being much more important in the thinner upper
atmosphere and the effects being lessened by destructive interference;
your site no longer mentions this as far as I can see, and it seems to
conflict with the phenomenon of 'airlight'; this is definitely blue and
apparently caused by Rayleigh scattering.
Does any of this have anything to do with the Einstein/Smouluchowski
scattering that you formerly mentioned?
Hoping you can clear this up...
Yes, I recently removed the note about E-S scattering because
it was causing some confusion. When I get more time I want to put in a clearer text.
In the dense lower atmosphere, Rayleigh scattering by air molecules themselves
still takes place and will cause direct sunlight to be reddened. However, there is
not significant sideways scattered blue light from molecules. This is because
molecular scatterers are much closer together than the wave crests of visible light
and there is signifcant destructive interference in the transverse direction. A
quirk of geometry is that destructive interference does not occur in the forward
direction.
Another source of scattering is transient density fluctuations in the air arising from
molecular motions and collisions. These are on a larger scale than the separation
between individual molecules and they _do_ produce a transversely scattered
blue excess in the lower atmosphere. This is E-S scattering.
But to some extent this is pedantry because both types of scattering follow the
same angular and wavelength dependence. Thus to simulate airlight and sky
colours Rayleigh's equations are fully adequate.
Have I just added to the confusion.
Les