Rainbow — Explained

Detailed Explanation

The phenomenon of a rainbow is a spectacular display of light's interaction with water droplets, involving the principles of dispersion, refraction, and total internal reflection. Understanding its formation requires a detailed look into the path of light through spherical raindrops.

1. Conceptual Foundation: The Role of Water Droplets

Sunlight, which we perceive as white, is actually a composite of various colors, each with a different wavelength. When this sunlight encounters a spherical water droplet suspended in the atmosphere, several optical processes occur sequentially to produce the rainbow effect. The key is that each raindrop acts like a tiny prism, dispersing the light, and a mirror, reflecting it.

2. Key Principles and Laws Involved:

Dispersion: — This is the phenomenon where white light splits into its constituent colors (VIBGYOR) when passing through a medium. It occurs because the refractive index of water is slightly different for different wavelengths (colors) of light. Violet light has a shorter wavelength and thus experiences a higher refractive index, bending more significantly than red light, which has a longer wavelength and a lower refractive index.
Refraction: — The bending of light as it passes from one medium to another (e.g., from air to water, or water to air). Snell's Law governs this: $n_1 sin \theta_1 = n_2 sin \theta_2$, where $n_1$ and $n_2$ are the refractive indices of the two media, and $heta_1$ and $heta_2$ are the angles of incidence and refraction, respectively.
Total Internal Reflection (TIR): — When light travels from a denser medium (water) to a rarer medium (air) and the angle of incidence in the denser medium exceeds a certain critical angle ($heta_c$), the light is entirely reflected back into the denser medium. The critical angle is given by $sin \theta_c = \frac{n_{\text{rarer}}}{n_{\text{denser}}}$. For water-air interface, $heta_c approx 48^circ$.

3. Formation of the Primary Rainbow:

The primary rainbow is the most common and brightest type. Its formation involves the following steps within each raindrop:

First Refraction and Dispersion: — A ray of sunlight enters a spherical raindrop. As it passes from air ($n approx 1$) into water ($n approx 1.33$ for visible light), it refracts and disperses. Violet light bends more than red light. The angle of incidence is $i_1$, and the angle of refraction is $r_1$.
Total Internal Reflection: — The dispersed light rays travel to the back inner surface of the raindrop. Here, they strike the interface between water and air. For angles of incidence greater than the critical angle, total internal reflection occurs, and the light is reflected back into the water droplet. This is a single internal reflection.
Second Refraction and Further Dispersion: — The reflected light rays then travel to the front surface of the raindrop, where they exit the water and re-enter the air. As they do so, they undergo a second refraction, further separating the colors and directing them towards the observer's eye.

Angular Position of the Primary Rainbow:

Due to the specific geometry of these refractions and one reflection, the light emerges from the raindrops at specific angles relative to the incident sunlight. For the primary rainbow, the maximum angular deviation for red light is approximately $42^circ$ and for violet light is approximately $40^circ$.

This means that red light is seen at a slightly larger angle from the anti-solar point (the point directly opposite the sun in the sky) than violet light. Consequently, in a primary rainbow, red appears on the outer (top) edge, and violet appears on the inner (bottom) edge.

4. Formation of the Secondary Rainbow:

The secondary rainbow is fainter and appears outside the primary rainbow. Its formation is similar but involves an additional internal reflection:

First Refraction and Dispersion: — Similar to the primary rainbow, sunlight enters the raindrop, refracts, and disperses.
First Total Internal Reflection: — The light undergoes one total internal reflection at the back surface.
Second Total Internal Reflection: — Instead of exiting, the light travels to another point on the inner surface and undergoes a *second* total internal reflection.
Second Refraction and Further Dispersion: — Finally, the light exits the raindrop after the second reflection, undergoing a second refraction.

Angular Position of the Secondary Rainbow:

Because of the two internal reflections, the light undergoes a greater total angular deviation. For the secondary rainbow, the maximum angular deviation for red light is approximately $51^circ$ and for violet light is approximately $54^circ$.

This results in an inverted color sequence compared to the primary rainbow: violet appears on the outer (top) edge, and red appears on the inner (bottom) edge. The increased number of reflections also leads to a significant loss of intensity, making the secondary rainbow much fainter.

5. Geometry of Observation:

For an observer to see a rainbow, two conditions must be met:

Sun behind the observer: — The sun must be positioned behind the observer. The center of the rainbow arc is always at the anti-solar point, which lies on the line connecting the sun through the observer's eye and extending into the sky.
Water droplets in front: — There must be water droplets (rain or mist) in the portion of the sky opposite the sun.

Each observer sees a rainbow formed by different raindrops. The rainbow is not a physical object located at a specific distance but an optical phenomenon whose apparent position depends on the observer's location and the angle at which light reaches their eyes from the raindrops.

6. Supernumerary Rainbows:

Occasionally, fainter, narrower bands of color can be seen inside the primary rainbow or outside the secondary rainbow. These are called supernumerary rainbows. They are not explained by geometric optics alone but require the wave nature of light (interference and diffraction) for a complete explanation. They arise from the interference of light rays that follow slightly different paths within the raindrop and emerge at nearly the same angle.

7. Common Misconceptions:

Rainbows are located at a specific distance: — Rainbows are optical illusions; they don't exist at a fixed point in space. Their appearance is relative to the observer's position.
All colors are equally bright: — Due to varying dispersion and reflection efficiencies, colors are not uniformly bright. The intensity varies across the spectrum.
Rainbows are always perfect arcs: — While often seen as arcs, a full circle rainbow can be observed from an elevated position (like an airplane), as the ground usually obstructs the lower part of the arc.
Only one rainbow can be seen: — While the primary is most common, the secondary rainbow is also frequently observed, and under ideal conditions, even fainter tertiary or quaternary rainbows (involving three or four reflections) are theoretically possible, though rarely seen due to extreme faintness.

8. NEET-Specific Angle:

For NEET aspirants, the focus should be on:

The sequence of phenomena: Refraction $ightarrow$ TIR $ightarrow$ Refraction (Primary); Refraction $ightarrow$ TIR $ightarrow$ TIR $ightarrow$ Refraction (Secondary).
The angular radii: Primary $approx 40^circ - 42^circ$, Secondary $approx 51^circ - 54^circ$.
The order of colors: Primary (Red outside, Violet inside), Secondary (Violet outside, Red inside).
Relative intensities: Primary is brighter than secondary.
Conditions for observation: Sun behind observer, rain in front.
The underlying principles: Dispersion, Refraction, TIR. Numerical problems often involve calculating critical angles or applying Snell's law in simplified scenarios, or conceptual questions about the properties of primary and secondary rainbows.