IB Physics SL Topic C.3 — How Waves Behave Paper 1 & 2 Wavefronts ⟂ rays ~6 min read

Wavefronts & Rays

Before we can talk about waves bending, bouncing and overlapping, we need two simple ways of drawing them. Wavefronts capture the shape of a wave; rays capture the direction it’s heading. Get these straight and every later diagram falls into place.

📘 What you need to know

Waves in Two and Three Dimensions

Drop a stone in a pond and the ripples spread out as growing circles — that’s a surface wave, travelling in two dimensions with circular wavefronts. Sound and light instead spread out in every direction through space as growing spheres — spherical wavefronts in three dimensions. (A spherical wavefront of radius r spreads its energy over a sphere’s surface area, A = 4πr², which matters later when we look at intensity.)

λpoint source wavefront ray
A surface wave from a point source: circular wavefronts (teal = crest, dashed = trough) spread outward, with rays (grey) pointing radially outward at 90° to them. Successive wavefronts are one wavelength apart.

Wavefronts

A wavefront is a line joining all the points of a wave that are oscillating in phase — all at a crest together, say, or all at a trough together. Because those points move in step, the wavefront marks the “leading edge” of one part of the wave. Each wavefront is one wavelength behind the last.

Rays

A ray is simply an arrow showing the direction the wave is travelling (and carrying its energy). The key rule to remember: a ray is always drawn perpendicular — at 90° — to the wavefronts. Viewed from above, a flat wave’s wavefronts look like a series of parallel straight lines, and the ray cuts straight across them.

ray 90° λ wavefronts (crest = solid, trough = dashed)
Viewed from above, wavefronts are parallel lines and the ray runs perpendicular to them. The wavelength λ is the gap between two successive crest wavefronts.

Reading Wavefront Diagrams

In exam diagrams, crest wavefronts are usually drawn as darker solid lines and troughs as fainter or dashed lines — though some diagrams show only the crests. Whichever is used, the rule for measuring is the same: the distance between two successive crest wavefronts (or two successive trough wavefronts) is exactly one wavelength.

🧭 Sketching and reading wavefronts

  1. Draw wavefronts as straight, evenly spaced lines with a ruler — sloppy sketches lose marks
  2. Keep the spacing equal to one wavelength between successive crests
  3. Add the ray as an arrow at exactly 90° to the wavefronts
  4. To find λ from a diagram, measure between two successive crest (or trough) wavefronts
  5. Circular wavefronts ⇒ 2D surface wave; spherical wavefronts ⇒ 3D wave like sound or light
Quick recap: wavefronts join points in phase and sit one wavelength apart; rays point the way the wave travels, always at 90° to the wavefronts.
WE 1

On a wavefront diagram, six successive crest wavefronts are spread evenly over a distance of 10 cm. The wave travels at 3.0 m s⁻¹.

(a) Determine the wavelength. (b) Hence find the frequency.

Part (a) Six wavefronts make five equal gaps, so λ = 10 cm ÷ 5 λ = 2.0 cm = 0.020 m λ = 0.020 m Part (b) Using v = fλ, so f = v/λ f = 3.0 ÷ 0.020 f = 150 Hz Careful: six wavefronts means five gaps, not six — a classic counting slip.
WE 2

A small loudspeaker emits sound equally in all directions.

(a) State the shape of its wavefronts. (b) State how a ray is drawn relative to these wavefronts.

Part (a) Sound spreads in three dimensions, so the wavefronts are spherical Part (b) A ray points radially outward from the speaker, perpendicular (90°) to each wavefront Circular wavefronts would be for a 2D surface wave; sound in open air is 3D, hence spherical.

💡 Top tips

⚠ Common mistakes

Up next: now that we can draw waves, we watch what happens when they hit a boundary — Reflection, Refraction & Transmission.

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