In simple terms
A friendly intro before the formal notes — no formulas yet.
A Wave Is a Travelling Disturbance, Not Travelling Stuff
A wave carries energy from one place to another without carrying the material along with it. The particles of the medium just wobble on the spot; it is the pattern of that wobble — the disturbance — that moves. Give a wave its speed, its wavelength and its frequency and the single equation links all three.
Picture a 'Mexican wave' running around a stadium. The wave sweeps right around the ground, but no single person leaves their seat — each just stands up and sits down in turn. The people are the medium; their up-and-down motion is the oscillation; the sweeping pattern is the wave. Sound, water ripples and light all work the same way: something oscillates, and the pattern of oscillation travels while the medium stays put.
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Decide the type: if the oscillation is at right angles to the direction the wave travels it is transverse (light, waves on a string); if it is along the direction of travel it is longitudinal (sound).
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Read the size of the wobble: the amplitude is the maximum displacement from the rest position — it sets how much energy the wave carries.
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Read the repeat in space and time: the wavelength () is the length of one full cycle; the period () is the time for one full cycle; the frequency () is how many cycles pass per second.
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Link them with : the wave speed equals frequency times wavelength, so knowing any two gives the third.
Explore the concept
Use the live diagram, PhET or GeoGebra sim, and synced steps — play it, drag controls, or tap a step.
Step 1
Decide the type: if the oscillation is at right angles to the direction the wave travels it is transverse (light, waves on a string); if it is along the direction of travel it is longitudinal (sound).
Key formulas
Tap any symbol to reveal exactly what it means and its units.
Full topic notes
Formal explanation with the rigour you need for the exam.
Two kinds of wave: transverse and longitudinal
Every wave carries energy through a repeating oscillation, but waves split into two families according to the direction of that oscillation. In a transverse wave the particles oscillate at right angles to the direction the wave travels — a wave sent along a rope, ripples on water, and every electromagnetic wave including light. In a longitudinal wave the particles oscillate back and forth along the direction of travel, squeezing the medium into regions of high density (compressions) and low density (rarefactions). Sound in air is the standard longitudinal wave. In both families the medium itself does not travel with the wave: each particle simply oscillates about its own fixed rest position while the disturbance moves on.
Transverse: oscillation perpendicular to energy transfer; shows crests and troughs. Examples: light and all EM waves, waves on a string, water ripples.
Longitudinal: oscillation parallel to energy transfer; shows compressions and rarefactions. Example: sound.
Both transfer energy, not matter: particles oscillate about a fixed point; only the disturbance advances.
A longitudinal wave can still be drawn as a sine curve by plotting displacement (or pressure) against position — the sine shape does not make it transverse.
The language of waves
To describe a wave quantitatively we need five terms. The amplitude () is the maximum displacement of a particle from its rest position, and it sets how much energy the wave carries. The wavelength () is the shortest distance between two points oscillating in phase — crest to crest, or compression to compression — measured in metres. The period () is the time for one complete oscillation, measured in seconds. The frequency () is the number of complete oscillations per second, measured in hertz (Hz). Finally the wave speed () is the distance the disturbance travels each second, in m s⁻¹.
Amplitude (): maximum displacement from equilibrium — NOT crest-to-trough distance, which is .
Wavelength (): length of one full cycle in space, in metres.
Period (): time for one full cycle, in seconds.
Frequency (): cycles per second, in hertz — set by the SOURCE.
Wave speed (): distance advanced per second, in m s⁻¹ — set by the MEDIUM.
The two equations that tie it together
Frequency and period describe the same repetition — one in cycles-per-second, the other in seconds-per-cycle — so they are reciprocals of each other. This gives the first relationship. The second, the wave equation, follows from a simple idea: in one period the wave advances exactly one wavelength, so its speed is one wavelength divided by one period, which rearranges to speed = frequency × wavelength.
T = \dfrac{1}{f} \qquad\qquad v = f\lambda
Here is the wave speed in m s⁻¹, is the frequency in Hz, is the wavelength in m, and is the period in s. Because links three quantities, knowing any two immediately gives the third. Keep firmly in mind which quantity is controlled by what: the frequency is fixed by the source, while the speed is fixed by the medium — so when a wave crosses into a new medium it is the wavelength that must change.
Representing waves: wavefronts and rays
There are two complementary ways to draw a wave as it spreads out. A wavefront is a line (or surface) joining points that are all in phase — for instance the line running along the top of one crest. Successive wavefronts are therefore spaced exactly one wavelength apart. A ray is an arrow drawn at right angles to the wavefronts, pointing in the direction the wave travels — that is, the direction of energy transfer. A wave spreading out from a point source has circular wavefronts; a wave far from its source, or a beam, has straight (plane) wavefronts. Rays and wavefronts always cross at 90°, so a diagram with either one implies the other.
Wavefront: joins points in phase; consecutive wavefronts are one wavelength apart.
Ray: an arrow perpendicular to the wavefronts, showing direction of travel / energy transfer.
Point source: circular (or spherical) wavefronts. Distant source / beam: plane (straight) wavefronts.
Rays and wavefronts are always mutually perpendicular.
Reading waves off graphs: distance vs time
The single most tested — and most confused — skill in this topic is reading a wave off a graph, because a displacement–distance graph and a displacement–time graph look identical yet mean different things. A displacement–DISTANCE graph is a snapshot: it freezes the whole wave at one instant and plots the displacement of every particle along the wave. The horizontal length of one full cycle is therefore the WAVELENGTH. A displacement–TIME graph is a movie of a single particle: it plots how that one particle's displacement changes as time passes. The horizontal length of one full cycle is therefore the PERIOD. Both graphs are sine curves and both show the amplitude on the vertical axis — so always read the horizontal axis label first to know whether you are getting a wavelength or a period.
Displacement–distance (horizontal axis = distance): snapshot of the whole wave → one cycle gives the wavelength .
Displacement–time (horizontal axis = time): history of one particle → one cycle gives the period .
Amplitude is the peak height of EITHER graph, read off the vertical axis.
Get from a displacement–time graph via , then combine with from a displacement–distance graph to find .
The electromagnetic spectrum
Visible light is one small band of a much larger family of transverse waves called the electromagnetic (EM) spectrum. In order of increasing frequency (and therefore decreasing wavelength) the regions are: radio waves, microwaves, infrared, visible light, ultraviolet, X-rays and gamma rays. Although they interact with matter in wildly different ways — radio waves pass through walls while gamma rays are ionising — they share one defining property: in a vacuum every one of them travels at the same speed, m s⁻¹. Because is fixed in a vacuum, the higher-frequency regions automatically have the shorter wavelengths.
Order (long , low → short , high ): radio → microwave → infrared → visible → ultraviolet → X-ray → gamma.
All EM waves are transverse and require no medium.
All travel at m s⁻¹ in a vacuum, so links their frequency and wavelength.
Visible light runs from red (longest ) to violet (shortest ) within the spectrum.
Mechanical waves need a medium
A mechanical wave is a disturbance passed from particle to particle through a material, so it cannot exist without that material. Sound, water waves, waves on a string and seismic waves are all mechanical — remove the medium and the wave disappears, which is why a bell ringing inside a jar goes silent as the air is pumped out and why space is soundless. Electromagnetic waves are the exception: they are oscillations of electric and magnetic fields that carry themselves along, needing no particles at all, so light from the Sun crosses the vacuum of space to reach us. This is the fundamental practical divide between the two categories of wave.
Common mistakes examiners penalise
Misusing — dividing when you should multiply, or forgetting to convert nm, cm, kHz or MHz to base SI units before substituting. Rearrange symbolically first, then put numbers in.
Thinking the medium sets the frequency — frequency is fixed by the source. When a wave changes medium the speed and wavelength change together but stays constant, so use with held fixed.
Confusing transverse and longitudinal — the test is the direction of oscillation relative to travel: perpendicular = transverse, parallel = longitudinal. Sound is longitudinal even though it is often drawn as a sine curve.
Reading wavelength off a displacement–time graph (or period off a displacement–distance graph) — check the horizontal axis: distance gives wavelength, time gives period. They are not interchangeable.
Calling the crest-to-trough height the amplitude — the amplitude is measured from the rest position to a crest; crest-to-trough is twice the amplitude.
Claiming some EM waves are faster than others in a vacuum — every part of the EM spectrum travels at exactly in a vacuum; they differ only in frequency and wavelength.
Saying sound can travel through space — sound is mechanical and needs a medium; only electromagnetic waves cross a vacuum.
Model answer — marked the way our engine marks it
In Paper 2 the marks are analytic: each is tied to a specific line of working — a method mark (M) or an answer mark (A) — and error-carried-forward (ECF) means a wrong number early on does not have to cost you the marks that follow. But that protection only exists if your method is written down. The question below deliberately mixes a calculation with a 'state and explain' part, because the explaining marks are earned by distinct physics statements, not by the number.
Where this leads
The wave model you have built here is the foundation for everything in wave behaviour that follows. The wave equation reappears whenever a wave changes medium — the physics of refraction is simply with the frequency held constant. Wavefronts and rays become the tools for describing reflection, refraction and diffraction, and the amplitude you learned to read off a graph is what determines intensity when waves superpose and interfere. Master the habit — identify the wave type, read the right graph for the right quantity, rearrange before you substitute, and keep frequency and medium in their proper roles — and the rest of the topic becomes variations on a model you already own.
Worked examples
See the formulas applied — reveal one step at a time, like the exam.
A wave travels along a stretched string at 12 m s⁻¹ with a wavelength of 0.40 m. Calculate (a) its frequency and (b) its period. [3]
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List what you know. m s⁻¹, m, ,
A single wave is described by two graphs. Its displacement–distance graph shows one complete cycle spanning 0.80 m, with a peak displacement of 3.0 cm. Its displacement–time graph shows one complete cycle spanning 0.20 s. Determine (a) the amplitude, (b) the wavelength, (c) the period and frequency, and (d) the wave speed. [4]
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Read each graph for what it uniquely gives.
Green light has a wavelength of m in a vacuum. Taking m s⁻¹, calculate (a) its frequency and (b) its period. [3]
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List what you know. m, m s⁻¹.
A sound wave has a frequency of 512 Hz and travels at 340 m s⁻¹ in air. Calculate its wavelength, then state and explain what happens to the wavelength if the wave passes into water, where it travels faster. [4]
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Model answer — full working.
How it all connects
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Tap a linked idea to see how it connects back to the main topic — that connection is what examiners reward.
Glossary
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Quick check
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Revision flashcards
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Transverse wave
A wave in which the oscillations are perpendicular (at right angles) to the direction of energy transfer. Examples: light and all electromagnetic waves, waves on a string, water surface ripples.
Key takeaways
Review these before you close the topic — retrieval beats re-reading.
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Transverse: oscillation perpendicular to energy transfer; shows crests and troughs. Examples: light and all EM waves, waves on a string, water ripples.
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Longitudinal: oscillation parallel to energy transfer; shows compressions and rarefactions. Example: sound.
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Both transfer energy, not matter: particles oscillate about a fixed point; only the disturbance advances.
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A longitudinal wave can still be drawn as a sine curve by plotting displacement (or pressure) against position — the sine shape does not make it transverse.
Practice — then mark it
The whole point: a real Cambridge question, marked mark-by-mark.
Get a Paper 2 calculation marked: solve a wave-equation problem with full working
Get a Paper 2 calculation marked: solve a wave-equation problem with full working
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Frequently asked
Checkpoint
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Reading it isn’t knowing it — prove it.
Before you move on: do Get a Paper 2 calculation marked: solve a wave-equation problem with full working on paper, snap a photo, and get examiner-style feedback on exactly where you win and lose marks.