
The Physics of a Rainbow
by Courtney Sant
by Courtney Sant

So some of you might be wondering, what exactly is a rainbow? We all enjoy spotting one in the sky on those rare occasions but few of us know why it got there in the first place. A rainbow can be described as a charming chromatic dispersion. It is formed when white sunlight is intercepted by a drop of water in the atmosphere and some of the light refracts into the drop, reflects from the drop's inner surface, and then refracts out of the drop. The first refraction separates the sunlight into its component colors and the second refraction increases the separation ultimately resulting as a rainbow. Colors of a rainbow are caused by the refraction and internal reflection of light rays that enter the raindrops. The concentration of rays near the minimum deviation gives rise to the arc of the rainbow. The incoming ray is unpolarized, and can be represented by two polarized waves whose planes of polarization are perpendicular to each other. There a few things that can happen to the ray when entering atmosphere. Part of the incoming ray is reflected back to the atmosphere; part of the light refracts into the drop and then refracts back to the atmosphere; some reflect from the drop’s inner surface and refract back to the atmosphere. Ultimately this refraction of rays give rise to an ordinary rainbow. In some cases, some rays will reflect twice inside the drop and then refract back to the atmosphere which ultimately gives rise to a secondary rainbow.
Rainbows briefly can be described as an optical and meteorological phenomena which cause a spectrum of light to appear in the sky when the sun shines onto droplets of moisture in the Earth’s atmosphere. As a result one can see a multicolored arc with red on the outside and violet on the inner arc. In most cases the spectrum of colors usually result in a sequence of Newton’s sevenfold red, orange, yellow, green, blue, indigo, violet or also known as Roy G. Biv.A secondary rainbow can be seen on rare occasions outside the primary arc with colors in the opposite order. Though rainbows are usually bow-shaped, there are also phenomena of rainbow-colored strips in the sky: in the shape of stripes, circles or even flames.
The rainbow is actually a disk of scattered light, but it is brightest at the edge; the disk for different wavelengths is a different size, and that is why we see the color effects there. When light refracts, it follows the law of refraction ni sin(ctai)=nr sin( ctar) where n is the index of refraction. There is an angle of incidence and an angle of refraction. Most of the light is refracted out by one ray. When your eyes intercept the separated colors from the raindrops the red color you experience is the product of when drops are angled slightly higher in the sky than when you experience seeing blue. Descartes and Willebrord Snell had determined how a ray of light is bent, or refracted, as it traverses regions of different densities, such as air and water. When the light paths through a raindrop are traced for red and blue light, one finds that the angle of deviation is different for the two colors because blue light is bent or refracted more than is the red light. 
The overall effect is that the incoming light is reflected back over a wide range of angles with the most intense light at an angle of 40-42 degrees. The angle is independent of the size of the drop but does depend on its refractive index. For instance, seawater has a higher refractive index than rain water therefore the radius of a rainbow in the sea spray is smaller than an actual rainbow. It becomes visible to the eye due to a misalignment of these bows.
There are other variances of rainbows as well such as a reflection rainbow and fire rainbow. A reflected rainbow occurs when sunlight reflects off a body of water before reaching the raindrops. This particular rainbow shares the same endpoints as a regular rainbow however it has a far more greater arc when visible. In addition, both primary and secondary reflection rainbows can be seen. The reflected rainbow is not a mirror image of the primary bow but is displaced from it to a degree depending on sun’s altitude. The fire rainbow, also known as the circumhorizontal acr, is produced when sunlight is reflected off clouds. It can sometimes be seen in cirrus clouds with ice crystals and when the sun is at least 58 above the horizon.

So in conclusion, a rainbow is not just freak occurence that presents itself magically when the sun comes out while its raining, nor is it just a book by D.H. Lawrence. A rainbow is caused by dispersion of sunlight as it goes through raindrops and has been mathmetically explained by scientists and astronomers. They include the Persian astromoner, Qutb al-Din al Shirazi (1236–1311) who is thought to have first given a fairly accurate explanation for the rainbow phenomenon and Descartes in 1637 treatise, Discourse on Method, further advanced the Shirazi's explanation. We can ultimately credit these two scientists for their discoveries on the workings of our culture's fascination, the rainbow.
Works Cited
http://www.geocities.com/capecanaveral/hall/6645/Rainbow/rainBow.html
http://eo.ucar.edu/rainbows/
http://www.batesville.k12.in.us/Physics/PhyNet/Optics/Refraction/Rainbows_2.html
http://eo.ucar.edu/rainbows/
http://www.batesville.k12.in.us/Physics/PhyNet/Optics/Refraction/Rainbows_2.html
