[Physics] Do rainbows show spectral lines from the sun

opticsspectroscopysun

I'm aware of a similar question being asked in Do rainbow shows spectral lines?:

The response to this question is that the body producing the light is not the water droplet that merely diffracts it but rather the Sun, which acts as a black body and thus produces a complete spectrum.

However, it is not entirely true that the sun is a black body: like all stars, it has an spectral class with absorption lines.

I am wondering why these lines are not observable in the rainbow or when decompossing sunlight with a prism in otherwise uncontrolled conditions. Are they simply too narrow to be seen without optical instruments? Is it a product of the light source not being coherent? How is this consistent with the possibility of obtaining spectra from distant stars in which the spectral lines are visible?

Best Answer

First you must understand how a (primary) rainbow is formed. Here is a summary with some details that are not in the linked article:

Whenever a beam of light encounters an air-water boundary, it is either reflected or refracted. To form a primary rainbow, we must first have enough small water droplets in the air, as these are close to spherical. Parallel light beams that reach such a water droplet must be refracted once as they enter, reflected off the inner surface of the droplet once, and refracted once more as they exit:

(image from the linked article)

There are 3 important points to note here:

  1. Water droplets in the air are never perfectly spherical. That is one source of fuzziness.

  2. Parallel beams entering the same water droplet can exit at different angles! This is the major reason why rainbows can never give sharp spectra even if you have perfectly spherical water droplets (say in outer space). Why then do we still see the rainbow? There are three reasons, which together result in the rainbow being seen roughly at 42°:

    • Different incident light beams will have different amount reflected/refracted. In particular, the bottommost incident beam (in the diagram) will mostly pass through without being reflected at the back of the droplet, and the topmost incident beam will mostly be reflected rather than enter the droplet.

    • The light beams emerging from the droplet after the above process are 'denser' along the so-called caustic ray, because the emergent angle does not vary monotonically with the distance of the incident beam from the central axis, and it reaches a maximum for the caustic ray, around which the emergent angle varies less.

    • The incident light beams further from the central axis undergo greater refraction, hence resulting in greater separation of different wavelengths. In contrast, the rainbow rays from incident beams close to the central axis largely overlap one another and wash out. (See this webpage for an image illustrating this.)

  3. Light beams may encounter more than one droplet! This is another major reason why we cannot expect a sharp spectrum from a (natural) rainbow.

  4. Even if we assume that the water droplet is a point, the light beams from the sun will not be perfectly parallel. In fact, the sun subtends an angle of about 0.5° to an observer on Earth, so this leads to roughly that same amount of spreading of the rainbow as compared to one generated by a point light source. Still, this is a much less significant effect than point 2.

(jkien's answer is incorrect but inexplicably has lots of upvotes.)