Light sky under primary rainbowwhy?

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The primary rainbow forms through the dispersion of light by water droplets, with red light emerging at approximately 42 degrees. The area below the rainbow appears bright not because of dispersion, but due to the contrast with the darker rainbow itself, often referred to as Alexander's band. Light from droplets below the rainbow reflects at similar angles, contributing to this brightness when viewed from different locations. The phenomenon is also influenced by constructive interference, which can enhance the brightness of the sky in that area. Understanding these optical effects clarifies why the sky beneath the primary rainbow lacks visible dispersion.
fisico30
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Hello Forum,
I understand how the primary rainbow is formed: dispersion by water droplets suspended in the air. A single internal reflection takes place. Red color (wavelength) emerges at about 42 degrees with respect to the observer...

but why is the sky below the primary rainbow not showing dispersion? There are water droplets also below the rainbow...It is said that the rays emerger rather horizontally for those droplets...
Perceiving white light means that emerging rays of different wavelengths are more or less overlapping each other..

thanks,
fisico30
 
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The drops below the part where you see the rainbow reflect the light with this angle, too. They are visible as part of the rainbow for observers somewhere else.
 
From the title, you seem to be asking about the bright area below the rainbow. To a large extent it's not so much that this area is bright as that the area of the rainbow is dark. See http://en.wikipedia.org/wiki/Alexander's_band
 
fisico30 said:
but why is the sky below the primary rainbow not showing dispersion?

There is- recall that rainbows are an example of a caustic- constructive interference, if you like.

http://www.atoptics.co.uk/fz552.htm
 
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