On Rayleigh Scattering and UV Light Absorption

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Discussion Overview

The discussion revolves around the effects of Rayleigh scattering on UV light absorption in the atmosphere, particularly during winter. Participants explore the implications of scattering on the intensity of UV light reaching the Earth's surface and the visibility of blue light in the sky. The conversation includes hypotheses about the relationship between scattering, absorption, and the need for direct sunlight for vitamin D synthesis.

Discussion Character

  • Exploratory
  • Debate/contested
  • Technical explanation

Main Points Raised

  • One participant hypothesizes that Rayleigh scattering causes UV light to be reflected into space, leading to reduced UV light reaching the surface during winter, but questions the validity of this due to the visibility of blue light.
  • Another participant argues that the reasoning presented is oversimplified, emphasizing the complexity of light paths and scattering angles.
  • A third participant expresses frustration with the discussion format, suggesting that the initial hypothesis should not precede questions.
  • It is noted that absorption by oxygen and ozone also plays a significant role in UV radiation effects, alongside scattering.
  • One participant asserts that while UV light scatters more than blue light, the unscattered UV light is primarily responsible for sunburn and vitamin D production.
  • There is a correction regarding the appearance of the Sun, stating that it appears white during most of the day, contrary to the claim that it appears orange throughout the day.

Areas of Agreement / Disagreement

Participants express differing views on the effects of scattering and absorption on UV light, with no consensus reached on the initial hypothesis or the implications of scattering for vitamin D synthesis.

Contextual Notes

Participants mention various factors affecting UV light, including scattering, absorption by atmospheric gases, and the angle of sunlight, but do not resolve the complexities involved in these interactions.

mk9898
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  1. I've read that UV light cannot "penetrate" the atmosphere as easily during winter. But what does this exactly mean? My hypothesis is that due to rayleigh scattering, since light with smaller wave lengths scatter more, the UV light doesn't end up reaching the surface of the Earth (i.e. gets reflected into space). But, this hypothesis isn't water tight, because blue light is still visible in winter. Yes, UV light has a much smaller wavelength than blue or violet light and therefore could scatter much more in winter, but since the sky is still blue in winter, I am not convinced that just due to the angle of the sun in winter, there is less UV light.
  2. Another thing, even if the UV light is more scattered, wouldn't that just mean, that there is a higher chance the scattering points eventually go back into space i.e. we are still getting UV light but at a less intensity as say in summer?
  3. With this logic, the amount of blue light that we see in the sky would also have a less intensity in the winter, right?
  4. In general, UV light scatters more than say blue light. Since the sky is in general always blue during the day, why would we need direct sunlight to obtain UV light i.e. vitamin D when UV scatters so much? Since we see blue sky, we should also, if our eyes were able to see UV light, see a lot of UV light in the sky. Since also the Sun appears orange throughout the day, "most" blue light is not hitting us directly from the sun but rather via rayleigh scaterring. So that should be valid for UV light as well, right?
 
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I think you're getting hung up on more/less, all/none, direct and oblique.

Blue light reaching our eyes may have entered the atmosphere in a direct line to your eye, or at an angle tangent to the atmosphere, or other angles. It may have multiple scatterings, and multiple chances of absorbsion, before reaching your eye. Light that doesn't scatter, moves on a more-or-less straight line from the source to your eye.

That makes your reasoning oversimplified.

How about just asking questions without giving your hypothesis first?
 
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anorlunda said:
How about just asking questions without giving your hypothesis first?

Jeez are you guys never happy? First you want people to give their opinion of what is right and now someone like you doesn't want us to do so?

But what you said before your question is pretty obvious and doesn't help.
 
Scattering is not the only effect present. There is also absorption by oxygen in the Hertzberg continuum and Schumann Runge bands, and ozone down to about 300 nm. These are the dominant effects for UV (and near UV) radiation. All this is related to why ozone depletion is such a big issue. See the reference:

Miller, C., Meakin, P., Franks, R.G.E., and Jesson, J.P., The Fluorocarbon-Ozone Theory – V. One Dimensional Modeling of the Atmosphere: The Base Case, Atmospheric Environment, 12, 2481-2500 (1978)
 
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mk9898 said:
In general, UV light scatters more than say blue light. Since the sky is in general always blue during the day, why would we need direct sunlight to obtain UV light i.e. vitamin D when UV scatters so much?

However much UV may be scattered, there is still far more that isn't, and it is predominantly this unscattered UV light that gives you a sunburn and that your body uses to make vitamin D.

mk9898 said:
Since also the Sun appears orange throughout the day, "most" blue light is not hitting us directly from the sun but rather via rayleigh scaterring.

The Sun does not appear orange throughout the day. Except in the early morning and late evening, the Sun appears white, regardless of the time of year.
 
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