Light sky under primary rainbowwhy?

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In summary, the primary rainbow is formed by the dispersion of light through water droplets in the air. The red color emerges at an angle of approximately 42 degrees. The drops below the rainbow also reflect light at this angle, which can be seen as part of the rainbow from a different perspective. The bright area below the rainbow is not caused by dispersion, but rather by the dark area of the rainbow. This is due to constructive interference, and is known as a caustic.
  • #1
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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  • #2
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.
 
  • #3
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
 
  • #5


Dear fisico30,
Thank you for your question. The reason why the sky below the primary rainbow does not show dispersion is because the angle of incidence of the sunlight is not favorable for the formation of a rainbow. The rainbow is formed when sunlight enters a water droplet at a specific angle and is refracted, reflected and dispersed inside the droplet before exiting at a specific angle. This process is known as total internal reflection. However, the angle at which sunlight enters the droplets below the primary rainbow is not ideal for this process to occur, resulting in a lack of dispersion and the appearance of white light. Additionally, the droplets below the rainbow may be smaller or less numerous, making it difficult for the same level of dispersion to occur. I hope this helps to clarify your question. Thank you for your interest in understanding the science behind the formation of rainbows.
 

1. What causes the light sky under a primary rainbow?

The light sky under a primary rainbow is caused by the refraction and reflection of sunlight through rain droplets in the atmosphere. The water droplets act as tiny prisms, separating the sunlight into its component colors and creating the rainbow. The light sky under the rainbow is a result of the scattered light that is not reflected back to our eyes.

2. Why is the sky under the primary rainbow lighter than the rest of the sky?

The sky under the primary rainbow appears lighter because the sunlight is being scattered in all directions by the rain droplets, making it appear brighter and less saturated compared to the surrounding sky. Additionally, the light that creates the rainbow is being redirected away from our field of vision, making the sky under the rainbow appear brighter.

3. Is the light sky under the primary rainbow always the same color?

No, the color of the light sky under the primary rainbow can vary depending on the size and shape of the rain droplets, as well as the angle of the sunlight. In some cases, the sky under the rainbow may appear white or even darker than the surrounding sky.

4. Can the light sky under the primary rainbow be seen from all angles?

The light sky under the primary rainbow can only be seen from certain angles. It is best viewed when the sun is behind the observer and the rain droplets are in front, creating a rainbow in the opposite direction. The angle of the sunlight and the position of the observer will determine if the light sky under the rainbow can be seen.

5. Is there a scientific term for the light sky under the primary rainbow?

Yes, the scientific term for the light sky under the primary rainbow is "anti-solar point." This is because the light under the rainbow appears opposite to the direction of the sun. It is also sometimes referred to as the "rainbow cloud," due to its appearance as a bright patch of sky under the rainbow.

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