Q.Under which conditions can a rainbow be observed ? Distinguish between a primary and a secondary rainbow.
You're viewing a preview — the full solution, concept, methods & PYQ mapping are locked.
Start your 14-day free trial to unlock the full solution →Rainbows form when sunlight refracts, reflects internally, and disperses through water droplets while the observer stands between the sun and rain. Primary rainbows (one internal reflection, 42° radius, violet inside) are brighter than secondary rainbows (two reflections, 51° radius, reversed colors).
The Physics Behind Rainbow Formation
A rainbow is not an object in space but an optical phenomenon that depends entirely on the relative positions of three things: the sun, water droplets in the atmosphere, and your eye. Light entering a spherical water droplet undergoes refraction at the entry surface, reflects off the back inner surface, and refracts again on exit. Because different wavelengths bend by different amounts (dispersion), white sunlight separates into its constituent colors.
The key insight is that light emerges from water droplets at specific angles relative to the incoming sunlight direction. Only droplets at particular positions in the sky send their dispersed light toward your eye, creating the circular arc we see.
Conditions for Observing a Rainbow
-
Sunlight and rain must coexist: You need both a source of bright light (typically the sun, though moonbows exist) and water droplets suspended in the air—rain, mist, spray from a waterfall, or even garden hose mist.
-
Sun behind the observer: The sun must be at your back. Rainbows always appear in the part of the sky opposite the sun because the light must travel toward the rain, interact with droplets, and return toward you.
-
Sun at low altitude: The sun should be relatively low in the sky (ideally below 42° elevation). When the sun is too high, the rainbow arc dips below the horizon and becomes invisible from ground level. This is why rainbows are most common in early morning or late afternoon.
-
Clear view of the antisolar point: The center of the rainbow circle is always at the antisolar point (the point directly opposite the sun from your perspective). You need an unobstructed view toward this region with rain or mist present.
Primary Rainbow: One Internal Reflection
When sunlight enters a raindrop, undergoes one internal reflection, and exits, it creates the primary rainbow.
Geometry and angle: The light that reaches your eye after one reflection emerges at approximately from the antisolar direction (more precisely, red light at , violet at ). This defines the angular radius of the primary bow.
Color sequence: Because red light bends less than violet during refraction, red emerges at a steeper angle and appears on the outer edge of the arc, while violet appears on the inner edge. From outside to inside: red, orange, yellow, green, blue, indigo, violet.
Brightness: The primary rainbow is relatively bright because only one internal reflection occurs—less light is lost.
Secondary Rainbow: Two Internal Reflections
When light undergoes two internal reflections inside the droplet before exiting, it produces the secondary rainbow.
Geometry and angle: The extra reflection sends light back at a larger angle, approximately from the antisolar point (red at , violet at ). The secondary bow appears outside and above the primary bow. …
Unlock everything free for 14 days
- Full step-by-step solutions
- Concept-first explanations
- Methods, shortcuts & mistakes
- PYQ mapping + timed mock tests
Full access for 14 days. No credit card required.