homework-and-exercisesreflectionrefractionvisible-light
Why the colors of Secondary rainbow is reverse of that in the color in the Primary rainbow?
What can be the possible reason among the following options
It does follow the same logic. There are some barely seen mini rainbows in the outer layers called supernumeraries. The red on the supernumerary overlaps some of the blue on the original.
The short answer is, of course, that the reflections are not total internal reflections, just normal reflections at an interface. Such reflections have huge losses, and that explains why successive orders are harder to spot, as neils' answer points out.
But let me try to explain why total internal reflection isn't involved. Here's how I understand it: We see a rainbow because (when there are a large number of water droplets in the air), certain '"parts" of the sky are sending us more "red" light, and certain parts more "violet" and so on. Of course, what I mean by this is that the amount of colour in a small unit solid angle is more in that region as opposed to the rest of the sky, and if it is sufficiently strong for our eyes to sense it, it can be "seen" as a band of that colour.
Now why would that be the case? The answer is pretty amazing: it turns out that when parallel rays of light hit a (spherical) drop, some incident rays don't deviate very far from each other, and end up bunching together. This depends on the angle that they strike the back of the drop with (known as the angle of minimum deviation -- something that might be familiar to people who have done simple experiments with prisms). Here's an example:
As you can see, the rays $e$, $f$, and $g$ in the first order rainbow (on the left) and $f$, $g$, and $h$ in the second order rainbow (on the right) pass through the drop and leave very close to each other, while the others get deviated by large angles. This 'minimum deviation' is found to depend rather heavily on the refractive index $\mu$ and the order of the rainbow $K$, and so different colours exit the drop at ever-so-slightly different angles, with each colour tightly bunched together about some angle. A series of simple but painful calculations lets us see that the angle of incidence of the rays that lead to this angle of minimum deviation is given by
$$\cos i = \sqrt{\frac{\mu^2 - 1}{K (K+2)}}.$$
Since we know that the refractive index $\mu$ depends on the wavelength of light, we see that $\mu_\text{red}=1.331$ and $\mu_\text{blue}=1.340$ (in water) cause angles of incidence of roughly $59.52^\circ$ and $59.00^\circ$ respectively.
Now you can calculate what the angle would be at the point of reflection (at the water-air interface), which you should be able to see from the above diagram should be $r$. It's trivial to calculate $r$ given $i$ and $\mu$ and show that it is less than the critical angle required for TIL ($\approx 48.75^\circ$), and so the ray can't undergo total internal reflection!
Most of the light reflecting off the back surface of the drop does get refracted out, but a tiny amount in each of the drops gets reflected, and a smaller amount than that gets reflected at the angle of minimum deviation and all the little drops emitting light at that angle add up to let your eye see (say) the colour red at that angle. The rays of light that reach you from the second order go through this process once more, and much less of them reach you: Frankly, it's pretty amazing that any of it can be seen!
Check out Jearl Walker's amazing article explaining the rainbow.
Best Answer
When a primary rainbow is formed, it is due to one total reflection in water droplets. A secondary rainbow is formed by light that underwent two internal reflections, and that is what changes the ordering of the colours. You can also have a tertiary rainbow formed by three internal reflections that would have the same ordering as primary and so on.