In simple terms
A friendly intro before the formal notes — no formulas yet.
Riding the Waves of Data
Lots of things in the real world go up and down and then repeat: the tide, the temperature, the seat on a Ferris wheel. A sinusoidal function — a stretched, shifted sine or cosine curve — captures that rhythm in one equation. Pin down three numbers, the height of the swing (amplitude), how long one cycle lasts (period) and the height of the middle line (vertical shift), and you can predict the value at any moment.
Picture yourself on a Ferris wheel. Your height above the ground never settles — it climbs to a top, sinks to a bottom, and repeats every turn. The centre of the wheel is the principal axis, the line that the curve wobbles around. The radius is the amplitude , how far above and below that line you swing. The time for one full turn is the period. Once you know those three numbers you know your height at every instant, without ever getting back on the wheel.
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Find the middle line, . Average the maximum and minimum values: . This is the principal axis, the horizontal line the curve oscillates about.
- 2
Find the amplitude, . Take half the gap between the maximum and minimum: . It is the height of the swing above (and below) the middle line.
- 3
Find from the period. Measure the length of one complete cycle, then use , so when working in degrees.
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Use the model. Substitute a value to predict an output, or set the model equal to a target value and let the GDC find the input — reading the answer that fits the interval the question asks for.
Explore the concept
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Step 1
Find the middle line, . Average the maximum and minimum values: . This is the principal axis, the horizontal line the curve oscillates about.
Key formulas
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Full topic notes
Formal explanation with the rigour you need for the exam.
The anatomy of a sinusoidal model
Almost every periodic quantity in this course can be written in one of two closely related forms. The parameters , and do all the work: sets the size of the swing, sets how quickly the cycle repeats, and sets the height of the line the curve oscillates about. Read those three numbers correctly and the whole model is under your control.
A sign warning: if the coefficient in front of the sine or cosine is negative — say — the curve is reflected in the principal axis, so it begins at a minimum instead of a maximum. The amplitude is still . The sign changes the starting shape, never the size of the swing.
Amplitude : the distance from the principal axis up to a maximum (or down to a minimum). From data, . It is always positive — it measures the size of the swing, not its direction.
Period and : the period is the length of one full cycle. In degrees, , so ; in radians replace with .
Vertical shift / principal axis : the curve oscillates about the horizontal line , where . This is the 'middle' of the wave.
Maximum and minimum: with the model reaches a maximum of and a minimum of . Knowing and hands you the top and bottom instantly.
Reading the parameters: from a graph, from max/min, or from a context
Whichever way a question presents the oscillation, the same three questions unlock it. Where is the middle line? That is . How big is the swing? That is . How long is one cycle? That gives . From a graph, read the highest and lowest values for and , and the distance between consecutive peaks for the period. From a worded context — a tide with a stated high and low, a temperature that ranges between two values, a Ferris wheel of known diameter — translate the words into a maximum, a minimum and a cycle length, then do exactly the same arithmetic.
Using the model: predicting and solving with the GDC
Once the parameters are known, the model earns its keep. To predict a value, substitute the input and evaluate on the GDC — checking first that the calculator mode matches the model. To find WHEN a quantity reaches a target, set the model equal to that target and solve: graph the model together with the horizontal target line and read the intersections, or use the equation solver, then choose the solution that lies in the interval the question asks about. A sinusoidal equation repeats every cycle, so there are always several answers — reading the right one is part of the skill.
Common mistakes examiners penalise
Calling the amplitude — the amplitude is the coefficient that multiplies the sine or cosine, not the vertical shift . In the amplitude is , not .
Getting the period the wrong way up — the period is (degrees) or (radians), not and not simply . For the period is , not .
Working in the wrong calculator mode — a model written with or an angle like is in degrees, so the GDC must be in degree mode. Radian mode gives a plausible-looking but wrong answer.
Forgetting the maximum is , not — with the maximum is principal axis plus amplitude, , and the minimum is . Quoting the amplitude as the maximum loses the mark.
Putting the principal axis at — the curve oscillates about , not the -axis. State the principal axis as using the vertical-shift value.
Taking amplitude as negative when the graph dips below the axis — amplitude is the positive distance . A negative coefficient only reflects the curve; the amplitude is still .
Reporting every solution instead of the first — a sinusoidal equation repeats each cycle, so pick the solution inside the interval the question specifies (often the smallest ), not just any intersection the GDC shows.
Model answer — marked the way our engine marks it
On Paper 2 the marks are analytic: each is tied to a specific line of working — a method mark (M) or an accuracy mark (A) — and an accuracy mark depends on the method mark it follows. Follow-through (FT) means an earlier slip need not cost you the marks that depend on it, provided the later step is done correctly on your own figure, and a GDC answer is expected rather than hand-computed values. Study how each mark below is earned by a specific line.
Where this leads
Sinusoidal modelling is where the trigonometry of angles meets the language of functions. The amplitude, period and vertical shift you read here are the same transformations of graphs you met earlier, now attached to a repeating curve; the GDC solving you practise is exactly the technique you will reuse whenever a model has to be set equal to a target. Every context that repeats — tides, temperatures, daylight, rotating wheels, alternating signals — reduces to the same three questions: how big is the swing, how long is the cycle, and where is the middle line. Answer those and read the model with a calculator in the right mode, and periodic phenomena stop being mysterious and become just another function you can predict from.
Worked examples
See the formulas applied — reveal one step at a time, like the exam.
The height above the ground, metres, of a seat on a Ferris wheel is modelled by , where is the time in seconds and the angle is in degrees. State the amplitude and the principal axis, find the period, and hence write down the maximum and minimum heights of the seat. [5]
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Read the parameters straight from the model .\n\nAmplitude. The coefficient of the sine term is , so the amplitude is m. [A1]\n\nPrincipal axis. The vertical shift is , so the seat oscillates about the line m. [A1]\n\nPeriod. Working in degrees, seconds. [M1 for ] [A1]\n\nMaximum and minimum heights. With , maximum m and minimum m. [A1]\n\nSo the wheel carries the seat between m and m above the ground, completing a full turn every seconds.
The depth of water in a harbour is modelled by , where is the depth in metres, is the time in hours after midnight, and the angle is measured in degrees. State the amplitude and the period, and find the maximum depth and the first time it occurs. [5]
- 1
Amplitude. The coefficient of the sine term is , so the amplitude is m. [A1]\n\nPeriod. In degrees, hours. [M1 for ] [A1]\n\nMaximum depth. The principal axis is and the amplitude is , so the greatest depth is m. [A1]\n\nFirst time it occurs. A sine model that starts on its principal axis and rises reaches its first maximum a quarter of a period after . Here a quarter period is hours, so the depth first reaches m at (i.e. 03:00). A GDC graph of confirms the first peak at . [A1]\n\nAnswers: amplitude m, period h, maximum depth m first reached at h.
The number of hours of daylight in a northern town is modelled by , where is measured in hours, is the number of months after the longest day, and the angle is in degrees. \n (a) State the maximum and minimum hours of daylight the model predicts. \n (b) Use your GDC to find the first value of (for ) at which the town has exactly hours of daylight. [5]
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(a) Maximum and minimum. The amplitude is and the principal axis is , so maximum hours and minimum hours. [A1 max] [A1 min]\n\n**(b) When is ?** Set the model equal to : , so . [M1 setting model target]\nGraph and on the GDC (degree mode) and read the first intersection for . [M1 GDC method]\nThe first intersection is at months. [A1]\n\n(The cosine model starts at its maximum of hours at , the longest day, and first crosses the principal axis of hours a quarter of a cycle later — a quarter of the -month period, i.e. .)
The depth of water is modelled by (metres, hours, degrees). State the amplitude and period, and find the maximum depth and the first time it occurs. [5]
- 1
Model answer — full working.\n\nThe model is , with the angle in degrees, so set the GDC to degree mode.\n\nAmplitude. The coefficient of is , so the amplitude is m.\n\nPeriod. Using with : hours.\n\nMaximum depth. The principal axis is and the amplitude is , so the maximum depth is m.\n\nFirst time it occurs. The sine model starts on the principal axis at and rises, so its first maximum is a quarter of a period later: hours. A GDC graph of confirms the first peak at .\n\nAnswers: amplitude m, period h, maximum depth m, first reached at h.\n\n---\nHow our marking engine awards the 5 marks:\n\n- A1 — amplitude. Awarded for stating the amplitude is , read as the coefficient of the sine term. This accuracy mark stands on correctly identifying , not .\n- M1 — period method. A method mark for using with , i.e. forming . It is the approach that is rewarded, so it survives an arithmetic slip in the division.\n- A1 — period. Awarded for hours. This A-mark depends on the M1 above: it is earned once is set up and evaluated correctly. FT applies — a candidate who mis-copied but divided correctly still earns it on their own figure.\n- A1 — maximum depth. Awarded for maximum m, combining the principal axis and amplitude. FT on the candidate's own and .\n- A1 — first time. Awarded for h, identified as a quarter of the period (or read from the GDC graph). This is FT on the candidate's own period: a student whose period differed but who correctly took a quarter of THEIR period keeps this mark.\n\n**'Accept equivalent forms and correct rounding.'** The engine accepts the period written as or or , the maximum as or , and the time as or '03:00'. Once a correct value appears, subsequent restatements do not lose marks (ISW).\n\nBottom line: of the 5 marks, the period method mark survives an arithmetic slip and three accuracy marks are shielded by follow-through. A student who writes only 'max , ' with no amplitude, no and no reasoning risks losing 3 marks; a student who shows the amplitude, the period formula, the sum and the quarter-period keeps the method regardless of a slip in one number.
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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What is a sinusoidal model?
A model of a repeating (periodic) quantity built from a sine or cosine curve, usually written or . The three numbers , and fix the size, speed and height of the oscillation.
Key takeaways
Review these before you close the topic — retrieval beats re-reading.
- ✓
Amplitude : the distance from the principal axis up to a maximum (or down to a minimum). From data, . It is always positive — it measures the size of the swing, not its direction.
- ✓
Period and : the period is the length of one full cycle. In degrees, , so ; in radians replace with .
- ✓
Vertical shift / principal axis : the curve oscillates about the horizontal line , where . This is the 'middle' of the wave.
- ✓
Maximum and minimum: with the model reaches a maximum of and a minimum of . Knowing and hands you the top and bottom instantly.
Practice — then mark it
The whole point: a real Cambridge question, marked mark-by-mark.
Get a Paper 2 sinusoidal model marked: state the amplitude and period, then predict and solve with full working
Get a Paper 2 sinusoidal model marked: state the amplitude and period, then predict and solve with full working
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Frequently asked
Checkpoint
One marked question is worth ten re-reads — close the loop before you move on.
Reading it isn’t knowing it — prove it.
Before you move on: do Get a Paper 2 sinusoidal model marked: state the amplitude and period, then predict and solve with full working on paper, snap a photo, and get examiner-style feedback on exactly where you win and lose marks.