Atmospheric Refraction: Temperature, Distance, Object Shape

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Discussion Overview

The discussion revolves around atmospheric refraction, specifically examining the conditions under which it occurs, including temperature, distance, and the shape of objects involved. Participants explore the scientific principles behind atmospheric refraction and share examples and observations related to the phenomenon.

Discussion Character

  • Exploratory
  • Technical explanation
  • Debate/contested

Main Points Raised

  • Some participants inquire whether atmospheric refraction is limited to specific temperatures, distances, and object shapes, particularly questioning if it only applies to spheres.
  • It is noted that cold and warm air are required for atmospheric refraction to occur, prompting questions about the limits of this effect at close distances.
  • One participant suggests that light rays refracting through a change in the index of refraction at an angle can lead to visual displacement, with larger gradients and distances resulting in more pronounced effects.
  • Another participant describes observing shimmering effects due to varying refraction through turbulent air, emphasizing the visibility of these effects through binoculars.
  • There is a discussion about atmospheric density variations due to altitude, indicating that atmospheric refraction can occur without a temperature difference, although the curvature of light rays is influenced by the temperature/density gradient.
  • It is clarified that temperature itself is not directly responsible for refraction; rather, it is the variation in the index of refraction caused by changes in air density that plays a crucial role.

Areas of Agreement / Disagreement

Participants express multiple competing views regarding the conditions necessary for atmospheric refraction, and the discussion remains unresolved as to the specific limits and dependencies of the phenomenon.

Contextual Notes

Participants reference the need for a variation in the index of refraction and discuss the effects of atmospheric density changes with altitude, but there are unresolved aspects regarding the precise conditions and limits of atmospheric refraction.

kmcguir
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Does atmospheric refraction only work at certain temperatures, distances, and shape of the object (i.e. only spheres)?
 
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kmcguir said:
Does atmospheric refraction only work at certain temperatures, distances, and shape of the object (i.e. only spheres)?
Can you post a few links to what you are asking about? That would help us to reply. Thanks.

Like this?

https://c.tadst.com/gfx/750x500/atmospheric-refraction.png?1

atmospheric-refraction.png
 

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Thread closed briefly for Moderation...
 
Thread is re-opened after deleting a questionable reference. We can discuss the science involved in atmospheric refraction in this thread, as long as all references are to mainstream science. Thank you. :smile:
 
kmcguir said:
Does atmospheric refraction only work at certain temperatures, distances, and shape of the object (i.e. only spheres)?
Here's another example of atmospheric refraction from a Google Images search...

https://i.ytimg.com/vi/-sj868IzNrk/maxresdefault.jpg

maxresdefault.jpg
 

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Ok, so cold and warm air are required for this to occur. Can this happen at close distances or is there a limit?
 
kmcguir said:
Ok, so cold and warm air are required for this to occur. Can this happen at close distances or is there a limit?
All it takes is light rays traversing a change in the index of refraction at an angle.

I've seen the same effect from light refracting off the hot hood of a car fairly close by. Since it involves angles, the larger the delta-n and the larger the distance, the larger the apparent visual displacement effect, no?
 
Look over the top of a hot CH radiator at a scene outside. You can often see shimmering due to the varying refraction through the turbulent mix of warm and cooler air. That refraction effect takes place right in front of you and it's more noticeable through binoculars.
 
kmcguir said:
Ok, so cold and warm air are required for this to occur. Can this happen at close distances or is there a limit?
Which "this" are you talking about? Atmospheric refraction can happen with atmospheric density variations due to altitude even without a temperature difference.

As for distance dependence, a particular temperature/density gradient will result in a particular curvature of light rays. At close range and a small gradient, you won't get much total deflection.
 
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kmcguir said:
Ok, so cold and warm air are required for this to occur. Can this happen at close distances or is there a limit?

Temperature isn't directly responsible for the refraction of light through the atmosphere or any other gas. What is needed is a variation in the index of refraction. Hot air is less dense than cooler air, and thus has a lower refractive index. But since density also changes with altitude, the index of refraction of the atmosphere also increases as you get closer to the surface.
 

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