kmcguir
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Does atmospheric refraction only work at certain temperatures, distances, and shape of the object (i.e. only spheres)?
Atmospheric refraction occurs due to variations in the index of refraction, primarily influenced by temperature and density gradients in the atmosphere. Cold and warm air layers create conditions for light rays to bend, resulting in visual displacement effects. This phenomenon is not limited to spherical objects; it can occur with any shape as long as there is a change in the index of refraction. The degree of deflection is dependent on the distance and the magnitude of the temperature or density gradient.
PREREQUISITESPhysicists, meteorologists, optical engineers, and anyone interested in the effects of atmospheric conditions on light behavior.
Can you post a few links to what you are asking about? That would help us to reply. Thanks.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...kmcguir said:Does atmospheric refraction only work at certain temperatures, distances, and shape of the object (i.e. only spheres)?
All it takes is light rays traversing a change in the index of refraction at an angle.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.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?
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?