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Rainbow is a phenomenon observed mostly in the Earth's atmosphere when the [[light|visible light]] from the [[Sun]] [[reflection|reflects]] and [[refraction|refracts]] inside the raindrops that are opposite to the Sun. The phenomenon can be observed as an arc if an observer looks at these raindrops from an angle of 42°. The formation of the arc is the result of [[dispersion]] of the visible light into its individual components — Red, Orange, Yellow, Green, Blue, Indigo, and Violet (ROY G BIV).
 
Rainbow is a phenomenon observed mostly in the Earth's atmosphere when the [[light|visible light]] from the [[Sun]] [[reflection|reflects]] and [[refraction|refracts]] inside the raindrops that are opposite to the Sun. The phenomenon can be observed as an arc if an observer looks at these raindrops from an angle of 42°. The formation of the arc is the result of [[dispersion]] of the visible light into its individual components — Red, Orange, Yellow, Green, Blue, Indigo, and Violet (ROY G BIV).
  
Here is how it works! When the visible light enters a rain droplet, some of it refracts through the drop, which means that the individual components of the light slows down when entering the water medium and thereby bend at different angles due to dispersion. Some of this refracted light then reflects from the inner walls of the droplet like a mirror at an angle. When this light refracts again through the opposite wall of the droplet, the individual components of the light that are at different [[wavelength]]s leave the water medium and enter the air medium at different angles as a [[spectrum]]. When viewed from a 42° angle, we see the individual components of each raindrop. The result is a beautiful arc of all the different colours spanned out across the droplets in the sky that are exactly at 42°. When the observer is looking at the rainbow from a certain height, say from an airplane, they would be observing a complete circle of a rainbow.
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Here is how it works! When the visible light enters a rain droplet, some of it refracts through the drop, which means that the individual components of the light slows down when entering the water medium and thereby bend at different angles due to dispersion. Some of this refracted light then reflects from the inner walls of the droplet like a mirror at an angle. When this light refracts again through the opposite wall of the droplet, the individual components of the light that are at different [[wavelength]]s leave the water medium and enter the air medium at different angles as a [[spectrum]]. When viewed from a 42° angle, we see the individual components of each raindrop. The result it is an arc of all the different colours spanned out across the droplets in the sky that are exactly at 42°.
  
 
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== Frequently Asked Questions ==
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