Physics/Lessons/Waves & the Particle Nature of Light/Longitudinal & Transverse Waves
Physics · Waves & the Particle Nature of Light · AS Level

Longitudinal & Transverse Waves

Every wave belongs to one of two families, sorted purely by the direction its oscillation points relative to the direction the wave is travelling. That single geometric distinction turns out to explain why light can be polarised and sound can't — and why that fact is one of the clearest pieces of evidence physicists have for how light actually behaves.

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Two families of wave

In a transverse wave, the particles of the medium (or the oscillating field) oscillate perpendicular to the direction the wave travels. A wave sent along a rope by shaking one end up and down is transverse. All electromagnetic waves — radio, microwaves, infrared, visible light, ultraviolet, X-rays and gamma rays — are transverse, with the oscillating electric and magnetic fields perpendicular to the direction of travel (and to each other).

In a longitudinal wave, the particles oscillate parallel to the direction of travel. Sound is the standard example: air molecules are pushed back and forth along the same line the sound travels, creating alternating regions of compression (bunched closer, higher pressure) and rarefaction (spread further, lower pressure).

Two stacked diagrams sharing the same horizontal direction-of-travel arrow, one above the other, for direct comparison. The top diagram illustrates a transverse wave: a horizontal line with a smooth continuous sine-wave curve drawn along it, with small vertical double-headed arrows at several points along the curve showing the up-and-down oscillation direction of particles, and one larger horizontal arrow beneath labelled direction of wave travel, clearly perpendicular to the vertical oscillation arrows. The bottom diagram illustrates a longitudinal wave: a horizontal row of evenly spaced small dots representing particles, but grouped so that some regions show the dots bunched closely together labelled compression and other regions show the dots spread further apart labelled rarefaction, alternating periodically along the row, with small horizontal double-headed arrows above a few particles showing their back-and-forth oscillation direction, and one larger horizontal arrow beneath labelled direction of wave travel, parallel to the small oscillation arrows above the particles.
Transverse waves oscillate perpendicular to the direction of travel; longitudinal waves oscillate parallel to it, producing alternating compressions and rarefactions.
All EM waves, one speed

In a vacuum, every electromagnetic wave — regardless of frequency or wavelength — travels at the same speed, $c \approx 3.00\times10^{8}\,\text{m}\,\text{s}^{-1}$. Radio waves and gamma rays differ enormously in frequency and wavelength, but not in vacuum speed; the wave equation $c=f\lambda$ still has to balance, so a higher frequency simply means a proportionally shorter wavelength.

The electromagnetic spectrum

All electromagnetic waves are the same kind of thing — an oscillating electric and magnetic field, travelling at $c$ in a vacuum — differing only in frequency and wavelength, related by $c=f\lambda$. The continuous range of frequencies is divided by convention into seven named regions, from lowest frequency (longest wavelength) to highest (shortest):

RegionApprox. wavelength rangeTypical use
Radio> 1 mm (up to km)Broadcasting (radio, TV signals)
Microwave1 mm – 30 cmSatellite communications, cooking
Infrared700 nm – 1 mmThermal imaging, remote controls
Visible400 nm – 700 nmHuman vision
Ultraviolet10 nm – 400 nmSterilisation
X-ray10 pm – 10 nmMedical imaging
Gamma< 10 pmCancer treatment, sterilisation

Because $c$ is fixed, ordering by increasing frequency is the same as ordering by decreasing wavelength — radio waves have the longest wavelengths and lowest frequencies, gamma rays the shortest wavelengths and highest frequencies. The boundaries between neighbouring regions aren't sharp physical cutoffs, just conventional dividing lines that vary slightly between sources.

Polarisation: evidence for transverse waves

An unpolarised transverse wave, like light from an ordinary bulb, oscillates in every direction perpendicular to its direction of travel simultaneously. Polarisation restricts the oscillation to a single plane containing the direction of travel, filtering out every direction except one.

A polarising filter only allows through oscillations aligned with its own transmission axis. For a transverse wave, that's coherent, since the oscillation direction is perpendicular to the direction of travel, leaving an entire plane of directions to restrict.

For a longitudinal wave, this doesn't work: its oscillation is locked onto the single line along which the wave travels — there's no perpendicular plane of directions to restrict, since particles only move backward and forward along that one line. A polarising filter placed in a sound wave's path has nothing to act on.

That's why the ability to be polarised is evidence that a wave is transverse: only a transverse wave has more than one possible oscillation direction to restrict. That light can be polarised — readily demonstrated by looking through two polarising filters and rotating one — confirms directly that light is a transverse wave.

Two stacked panels. The top panel shows unpolarised light, drawn as a bundle of red double-headed arrows at many different angles around the beam axis, travelling left to right toward a vertical polarising filter marked with its transmission axis. After passing through the filter, the beam continues as a single blue double-headed arrow oscillating only in the vertical transmission-axis direction, labelled polarised light. The bottom panel shows this same polarised blue beam travelling on to a second polarising filter, the analyser, whose transmission axis is tilted at an angle theta to the vertical. The beam that emerges beyond the analyser is drawn as a shorter, fainter blue double-headed arrow along the analyser's tilted transmission axis, showing reduced amplitude.
Passing light through one polarising filter selects a single oscillation plane; passing that polarised light through a second, rotated filter reduces the transmitted amplitude further, down to zero when the two transmission axes are at 90°.

Malus's law: the transmitted intensity through a rotated polariser

Once light has passed through one polarising filter, it's polarised in a single, definite plane. If that polarised light then meets a second polarising filter — usually called the analyser — set with its transmission axis at some angle $\theta$ to the light's plane of polarisation, only part of the light gets through, and exactly how much depends on $\theta$. This relationship is called Malus's law.

DerivationI = I₀cos²θ
1
Model the polarised light arriving at the analyser as having amplitude $A_0$, oscillating along a fixed plane, with intensity $I_0 \propto A_0^2$.
2
The analyser only transmits the component of the oscillation that lies along its own transmission axis. Resolving the incoming oscillation onto that axis, at angle $\theta$ to it, gives a transmitted amplitude $A = A_0\cos\theta$.
This is the same resolving-into-components idea used everywhere else in mechanics — only the component along the relevant direction survives.
3
Since intensity is proportional to amplitude squared, the transmitted intensity is $I \propto A^2 = A_0^2\cos^2\theta = I_0\cos^2\theta$.
4
So $I = I_0\cos^2\theta$, where $I_0$ is the intensity of the light arriving at the analyser and $\theta$ is the angle between the analyser's transmission axis and the light's existing plane of polarisation.
At $\theta = 0°$ (axes aligned), $I = I_0$ — full transmission. At $\theta = 90°$ ("crossed polarisers"), $I = 0$ — no light gets through at all.
▪ derived
A further, quantitative step

The core requirement is the qualitative argument above — that polarisation is possible for transverse waves and impossible for longitudinal ones. Malus's law, derived below, extends this to a precise, quantitative relationship: know $I=I_0\cos^2\theta$, and be able to use it to find a transmitted intensity or required rotation angle.

Applications of polarisers

Polaroid material is a widely used polarising filter, made from long-chain molecules aligned in one direction that absorb light oscillating parallel to the chains while transmitting light oscillating perpendicular to them. It's used in sunglasses to cut glare — light reflected off water or a road becomes partially polarised in the horizontal plane, so Polaroid sunglasses with a vertical transmission axis block much of that glare. It's also used in LCD screens and photography filters.

Polarisation also matters for radio and television signal transmission. A transmitting aerial launches radio waves polarised in the same plane as the aerial itself. A receiving aerial only picks up the component aligned with its own length, so the aerials have to be aligned for efficient signal transfer — one mounted at right angles to the transmitter would pick up almost nothing. That's why domestic TV aerials are mounted with a specific, deliberate orientation relative to the local transmitter.

Key takeaways

  • Transverse waves oscillate perpendicular to the direction of energy transfer (e.g. electromagnetic waves, waves on a string); longitudinal waves oscillate parallel to it (e.g. sound), producing compressions and rarefactions.
  • All electromagnetic waves travel at the same speed in a vacuum, $c \approx 3.00\times10^8\,\text{m}\,\text{s}^{-1}$, regardless of frequency or wavelength.
  • The electromagnetic spectrum, in order of increasing frequency (decreasing wavelength): radio, microwave, infrared, visible, ultraviolet, X-ray, gamma — each with distinct practical uses, from broadcasting to medical imaging.
  • Polarisation restricts oscillation to a single plane — possible for transverse waves because they have a perpendicular plane of oscillation directions to restrict, impossible for longitudinal waves because their oscillation is locked to a single line.
  • The fact that light can be polarised is direct evidence that light is a transverse wave.
  • Malus's law, $I = I_0\cos^2\theta$, gives the intensity transmitted through an analyser set at angle $\theta$ to the light's plane of polarisation — full transmission at $\theta=0°$, zero at $\theta=90°$ (crossed polarisers).
  • Polaroid material polarises light by absorbing one oscillation direction; it's used to cut glare in sunglasses and manage reflections in photography and displays.
  • Transmitting and receiving aerials must be aligned in the same plane of polarisation for efficient signal reception — misaligned aerials receive very little signal.