Advanced Trigonometric Functions
| Safle: | Young Education |
| Cwrs: | Advanced Trigonomitry |
| Llyfrau: | Advanced Trigonometric Functions |
| Argraffwyd gan: | Guest user |
| Dyddiad: | Dydd Llun, 9 Tachwedd 2026, 4:37 PM |
1. Review of Trigonometric Functions
Learning outcomes
- I can evaluate all six trigonometric functions for any angle.
- I can interpret trigonometric values using the unit circle.
- I can analyse the domains and ranges of trigonometric functions.
- I can determine exact values using reference angles.
- I can connect graphical, algebraic, and geometric representations.
Review of Trigonometric Functions
Trigonometry describes relationships between angles, coordinates, and ratios. Earlier trigonometry often focuses on the three functions:
sinθ, cosθ, tanθ
However, there are actually six trigonometric functions:
sin, cos, tan, csc, sec, cot
Using the unit circle allows us to extend these functions beyond acute angles in right triangles and evaluate them for angles in all four quadrants.
The Six Trigonometric Functions
For a right triangle, remember:
\( sin \theta = \frac{opposite}{hypotenuse} \)
\( cos \theta = \frac{adjacent}{hypotenuse} \)
\( tan \theta = \frac{opposite}{adjacent} \)
A common memory aid is:
SOH – CAH – TOA
- Sine = Opposite / Hypotenuse
- Cosine = Adjacent / Hypotenuse
- Tangent = Opposite / Adjacent
The Reciprocal Functions
The other three trigonometric functions are the reciprocals of sine, cosine, and tangent.
Cosecant
\( csc \theta = \frac{1}{sin \theta } \)
Secant
\( sec \theta = \frac{1}{cos \theta } \)
Cotangent
\( cot \theta = \frac{1}{tan \theta } \)
Since:
\( tan \theta = \frac{sin \theta }{cos \theta } \)
we can also write:
\( cot \theta = \frac{cos \theta }{sin \theta } \)
The Unit Circle
The unit circle is a circle centred at the origin with radius 1.
It provides one of the most powerful ways to understand trigonometric functions.
For an angle
in standard position, the point where its terminal side intersects the unit circle has coordinates:
(cosθ, sinθ)
Therefore:
- x-coordinate = cosθ
- -coordinate = sinθ

2. Advanced Function Transformations
Learning outcomes
- I can determine amplitude, period, phase shift, and vertical displacement.
- I can write equations from transformed graphs.
- I can sketch transformed trigonometric functions.
- I can analyse the effects of multiple transformations.
- I can interpret transformed functions in context.
Advanced Function Transformations
Trigonometric functions such as sine and cosine can model repeating patterns. Their basic graphs can be transformed to represent many different real-world situations.
A general transformed sine function can be written as:
y = A sin(B(x − C)) + D
A transformed cosine function can be written as:
y = A cos(B(x − C)) + D
The four parameters A, B, C, and D control different features of the graph:
| Parameter | Main Effect |
|---|---|
| A | amplitude and vertical reflection |
| B | period / horizontal stretch or compression |
| C | phase shift |
| D | vertical displacement |
Understanding these four values allows us to move between equations, graphs, and real-world situations.
The Parent Sine and Cosine Functions
Before studying transformations, it is useful to remember the basic functions.
Sine
y = sin(x)
The sine graph:
- oscillates between −1 and 1
- has amplitude 1
- has a midline of y = 0
- has a period of 2π radians or 360°
- begins at the midline and initially rises
Cosine
y = cos(x)
The cosine graph has the same:
- amplitude
- period
- maximum
- minimum
- midline
but it begins at a maximum when x = 0.
These basic graphs are called parent functions.
Amplitude
The amplitude measures the vertical distance from the midline to a maximum or minimum.
For:
y = A sin(x)
or:
y = A cos(x)
the amplitude is:
amplitude = |A|
The absolute value is important because amplitude is a distance and therefore is not negative.
Example
y = 4 sin(x)
Amplitude:
|4| = 4
The graph ranges from:
−4 to 4
instead of:
−1 to 1
This is a vertical stretch.
Finding Amplitude from a Graph
If we know the maximum and minimum values of a sinusoidal graph:
amplitude = (maximum − minimum)/2
Suppose:
maximum = 9
minimum = 1
Then:
amplitude = (9 − 1)/2
= 8/2
= 4
The amplitude is 4.
The Midline
A transformed trigonometric graph oscillates around a horizontal line called the midline.
For:
y = A sin(B(x − C)) + D
the midline is:
y = D
For example:
y = 3 sin(x) + 5
has the midline:
y = 5
The graph oscillates above and below 5.
Finding the Midline from Maximum and Minimum
The midline lies halfway between the maximum and minimum.
Therefore:
midline = (maximum + minimum)/2
Suppose:
maximum = 14
minimum = 6
Then:
midline = (14 + 6)/2
= 20/2
= 10
Therefore:
D = 10
and the midline is:
y = 10
Maximum and Minimum Values
Once we know the amplitude and vertical displacement:
maximum = D + |A|
minimum = D − |A|
For example:
y = 6 sin(x) + 10
Amplitude:
6
Midline:
y = 10
Maximum:
10 + 6 = 16
Minimum:
10 − 6 = 4
These relationships are extremely useful when interpreting graphs.
Vertical Stretch and Compression
The value of |A| determines vertical scaling.
If:
|A| > 1
the graph is vertically stretched.
If:
0 < |A| < 1
the graph is vertically compressed.
For example:
y = 5 sin(x)
is vertically stretched.
y = 0.5 sin(x)
is vertically compressed.
The period does not change when only A changes.
Reflection Across the x-Axis
What happens if A is negative?
Consider:
y = −sin(x)
The negative sign reflects the graph across the x-axis.
Similarly:
y = −3 cos(x)
has:
amplitude = 3
and is reflected vertically.
Remember:
amplitude = |A|
So the amplitude is never −3.
The negative sign tells us about reflection, not amplitude.
Period
The period is the horizontal distance required for a function to complete one full cycle.
For the parent sine and cosine functions:
period = 2π radians
or:
period = 360°
The parameter B changes the period.
For radians:
period = 2π/|B|
For degrees:
period = 360°/|B|
Example: Period
Consider:
y = sin(2x)
Here:
B = 2
Therefore:
period = 2π/2
= π
The function completes one cycle in π radians rather than 2π.
The graph has been horizontally compressed.
Another Period Example
Consider:
y = cos(x/3)
Here:
B = 1/3
Therefore:
period = 2π/(1/3)
= 6π
The graph takes 6π radians to complete one cycle.
It has been horizontally stretched.
Horizontal Stretch and Compression
The effect of B is opposite to what students sometimes expect.
A larger |B| produces a shorter period.
A smaller |B| produces a longer period.
For example:
| Function | B | Period |
|---|---|---|
| sin(x) | 1 | 2π |
| sin(2x) | 2 | π |
| sin(4x) | 4 | π/2 |
| sin(x/2) | 1/2 | 4π |
Therefore:
larger |B| → more cycles over the same interval
smaller |B| → fewer cycles over the same interval
Frequency and Period
Period and frequency are closely related.
Period tells us how long one cycle takes.
Frequency tells us how many cycles occur per unit.
In many contexts:
frequency = 1/period
For example, if a wave completes one cycle every 0.25 seconds:
frequency = 1/0.25
= 4 Hz
The shorter the period, the greater the frequency.
Phase Shift
The phase shift describes a horizontal movement of the graph.
For:
y = A sin(B(x − C)) + D
the phase shift is:
C
If:
C > 0
the graph shifts right.
If:
C < 0
the graph shifts left.
Example: Shift Right
Consider:
y = sin(x − π/2)
The graph shifts:
π/2 units to the right
because:
C = π/2
Every important point on the parent sine curve moves π/2 units to the right.
Example: Shift Left
Consider:
y = cos(x + π/3)
Rewrite the inside as:
x − (−π/3)
Therefore:
C = −π/3
The graph shifts:
π/3 units to the left
The sign can initially seem backwards because the transformation appears inside the brackets.
Be Careful When B Is Factored
Consider:
y = sin(2x − π)
It would be incorrect to say the phase shift is π.
Factor 2:
y = sin(2(x − π/2))
Now the function is in the form:
sin(B(x − C))
Therefore:
C = π/2
The phase shift is:
π/2 to the right
This is an important advanced skill.
General Rule for Phase Shift
If the function is written as:
y = A sin(Bx − E) + D
factor B:
Bx − E = B(x − E/B)
Therefore:
phase shift = E/B
with the direction determined by the resulting expression.
For example:
y = 2 cos(3x − π) + 4
Factor:
3x − π = 3(x − π/3)
Therefore:
phase shift = π/3 right
Vertical Displacement
The parameter D moves the entire graph vertically.
For:
y = sin(x) + 4
the graph shifts:
4 units upward
Its midline becomes:
y = 4
For:
y = cos(x) − 3
the graph shifts:
3 units downward
Its midline becomes:
y = −3
Vertical displacement does not change the amplitude or period.
Combining Vertical Shift and Amplitude
Consider:
y = 3 sin(x) + 5
Amplitude:
3
Midline:
y = 5
Maximum:
5 + 3 = 8
Minimum:
5 − 3 = 2
The graph therefore oscillates between:
2 and 8
rather than between −1 and 1.
Understanding All Four Parameters
Consider:
y = 4 sin(2(x − π/3)) + 5
Identify each parameter.
A = 4
Amplitude:
4
No vertical reflection because A is positive.
B = 2
Period:
2π/2 = π
C = π/3
Phase shift:
π/3 right
D = 5
Vertical displacement:
5 units upward
Midline:
y = 5
Maximum:
5 + 4 = 9
Minimum:
5 − 4 = 1
So from one equation we can determine a large amount of information about the graph.
A Useful Transformation Table
For:
y = A sin(B(x − C)) + D
or:
y = A cos(B(x − C)) + D
| Feature | How to Find It |
|---|---|
| Amplitude | |
| Period | 2π/ |
| Phase shift | C |
| Vertical displacement | D |
| Midline | y = D |
| Maximum | D + |
| Minimum | D − |
| Reflection | A < 0 reflects across x-axis |
For degree-based functions, use:
period = 360°/|B|
instead.
Sketching a Transformed Sine Function
Suppose we want to sketch:
y = 2 sin(x) + 3
First identify the transformations.
Amplitude:
2
Period:
2π
Phase shift:
0
Midline:
y = 3
Maximum:
5
Minimum:
1
The sine curve begins on the midline.
Over one complete cycle, its five key positions are:
midline → maximum → midline → minimum → midline
So:
| x | y |
|---|---|
| 0 | 3 |
| π/2 | 5 |
| π | 3 |
| 3π/2 | 1 |
| 2π | 3 |
These points provide the structure needed to sketch the curve.
The Five Key Points
One full sine or cosine cycle can often be sketched using five important positions.
Divide the period into four equal sections.
If the period is P:
quarter-period = P/4
For sine, beginning at its standard starting point:
midline → maximum → midline → minimum → midline
For cosine:
maximum → midline → minimum → midline → maximum
This method makes complicated transformations much easier to sketch.
Sketching a More Complex Function
Consider:
y = 3 cos(2x) − 1
Amplitude:
3
Period:
2π/2 = π
Midline:
y = −1
Maximum:
−1 + 3 = 2
Minimum:
−1 − 3 = −4
Quarter-period:
π/4
Cosine begins at a maximum.
Therefore, one cycle follows:
| x | y |
|---|---|
| 0 | 2 |
| π/4 | −1 |
| π/2 | −4 |
| 3π/4 | −1 |
| π | 2 |
The cycle then repeats.
Sketching with a Phase Shift
Consider:
y = 2 sin(x − π/2) + 1
Amplitude:
2
Period:
2π
Phase shift:
π/2 right
Midline:
y = 1
Maximum:
3
Minimum:
−1
Quarter-period:
π/2
The sine pattern begins at:
x = π/2
So the key x-values are:
π/2
π
3π/2
2π
5π/2
and the corresponding y-values are:
1
3
1
−1
1
Writing an Equation from a Graph
We can also work backwards.
Suppose a sinusoidal graph has:
maximum = 10
minimum = 2
First calculate amplitude:
A = (10 − 2)/2
= 4
Find the midline:
D = (10 + 2)/2
= 6
So the function must have:
|A| = 4
and:
D = 6
We then determine the period and phase shift from the horizontal behaviour.
Finding B from the Period
Suppose the graph completes one cycle every:
π radians
Then:
period = 2π/|B|
π = 2π/|B|
Therefore:
|B| = 2
A possible equation might therefore contain:
sin(2x)
or:
cos(2x)
depending on the shape and starting position.
Choosing Sine or Cosine
The same sinusoidal graph can often be represented using several equivalent equations.
A graph that begins at its midline and rises naturally suggests sine.
A graph that begins at a maximum naturally suggests cosine.
Sine is often convenient when the graph starts at:
- the midline and rises
- the midline and falls, using negative sine
Cosine is often convenient when the graph starts at:
- a maximum
- a minimum, using negative cosine
Neither form is automatically more correct.
The goal is usually to choose the simplest equation that matches the graph.
Example: Writing an Equation
Suppose a graph has:
maximum = 7
minimum = −1
period = 4π
and begins at a maximum when x = 0.
Amplitude:
A = (7 − (−1))/2
= 8/2
= 4
Midline:
D = (7 + (−1))/2
= 6/2
= 3
Find B:
4π = 2π/|B|
|B| = 1/2
Since the graph begins at a maximum, cosine is convenient.
Therefore, one possible equation is:
y = 4 cos(x/2) + 3
Multiple Transformations
Advanced functions often involve several transformations at once.
Consider:
y = −2 sin(3(x + π/6)) + 4
Let's analyze it carefully.
Amplitude
2
Reflection
The negative A means reflection across the x-axis.
Period
2π/3
Phase Shift
Because:
x + π/6 = x − (−π/6)
the graph shifts:
π/6 left
Vertical Displacement
4 units upward
Midline
y = 4
Maximum
4 + 2 = 6
Minimum
4 − 2 = 2
A complicated-looking equation becomes much easier when we analyze one transformation at a time.
Order of Transformations
When analysing a transformed function, a useful sequence is:
- identify the parent function
- determine amplitude and reflection
- determine period
- determine phase shift
- determine vertical displacement
- find the midline
- determine maximum and minimum
- calculate the quarter-period
- plot key points
- draw a smooth repeating curve
This systematic approach reduces errors.
Horizontal Transformations Can Be Tricky
Horizontal transformations behave differently from vertical ones.
Consider:
y = sin(2x)
The 2 does not stretch the graph horizontally by 2.
Instead, it makes the period half as long.
Similarly:
y = sin(x/2)
has a period twice as long.
This inverse relationship occurs because the transformation happens inside the function.
Transformations in Context
Trigonometric functions are particularly useful because many real-world phenomena repeat.
Examples include:
- tides
- daylight hours
- seasonal temperatures
- sound waves
- alternating current
- pendulums
- Ferris wheels
- rotating machinery
- ocean waves
- biological rhythms
The parameters A, B, C, and D then have physical meanings.
Example: Ferris Wheel
Imagine a Ferris wheel.
A rider moves repeatedly:
high → middle → low → middle → high
The rider's height can be modelled using a sinusoidal function.
Suppose:
- maximum height = 42 m
- minimum height = 2 m
- one revolution takes 60 seconds
Amplitude:
(42 − 2)/2
= 20 m
Midline:
(42 + 2)/2
= 22 m
The vertical displacement represents the height of the wheel's centre.
The period is:
60 s
If the rider begins at the highest point, cosine is convenient.
Using time t in seconds:
h(t) = 20 cos((2π/60)t) + 22
Simplify:
h(t) = 20 cos((π/30)t) + 22
Interpreting the Ferris Wheel Model
In:
h(t) = 20 cos((π/30)t) + 22
the parameters have physical meanings.
20 represents the wheel's radius.
π/30 determines how quickly it rotates.
The period is 60 seconds.
22 represents the height of the wheel's centre above the ground.
Because cosine begins at its maximum:
h(0) = 42 m
which matches the rider starting at the top.
This demonstrates why transformations are useful: the parameters tell us something about the actual system.
Example: Seasonal Temperature
Suppose a city's average monthly temperature follows a roughly sinusoidal pattern.
A model might be:
T(t) = 12 sin((2π/12)(t − 3)) + 18
where t represents months.
Amplitude:
12°C
This represents the approximate size of seasonal temperature variation from the average.
Period:
12 months
The pattern repeats once per year.
Phase shift:
3 months right
This positions the warm and cool parts of the cycle appropriately.
Vertical displacement:
18°C
This represents the midline or average level of the model.
Example: Tides
Ocean tides often show approximately periodic behaviour, although real tidal systems can be much more complicated than a single sine curve.
A simplified model might be:
h(t) = 1.5 cos((2π/12.4)t) + 2.3
where h is water height in metres and t is time in hours.
Amplitude:
1.5 m
Midline:
2.3 m
Period:
12.4 h
Maximum:
2.3 + 1.5 = 3.8 m
Minimum:
2.3 − 1.5 = 0.8 m
The model provides an approximation of repeating water-level changes.
Phase Shift in Real Situations
Phase shift can represent a delay or a difference in timing.
Suppose two locations experience similar periodic temperature patterns, but one reaches its maximum temperature later.
Their graphs might have similar:
- amplitude
- period
- vertical displacement
but different:
- phase shifts
Similarly, two waves can have the same amplitude and frequency but reach their peaks at different times.
That timing difference is represented by phase.
Transformations and Sound
Sound waves can also be represented using sinusoidal models.
In a simplified wave model:
- amplitude relates to the size of the oscillation
- frequency relates to pitch
- phase describes relative timing
- vertical displacement moves the equilibrium level mathematically
Real sound waves are often combinations of many frequencies rather than perfect sine waves, but sinusoidal functions provide a fundamental model.
Transformations and Physics
Trigonometric transformations are important in physics.
They appear in models of:
- waves
- simple harmonic motion
- alternating current
- circular motion
- pendulums
- springs
- electromagnetic radiation
For example, a simple oscillation may be represented as:
x(t) = A cos(ωt + φ)
where:
A represents amplitude
ω controls the oscillation frequency
φ represents phase
This is closely related to the transformation form used in mathematics.
Domain and Range
Transformations also affect the range of sine and cosine.
The parent functions have:
−1 ≤ y ≤ 1
For:
y = A sin(B(x − C)) + D
or cosine:
the range becomes:
D − |A| ≤ y ≤ D + |A|
For example:
y = 5 sin(2x) − 3
Amplitude:
5
Midline:
−3
Minimum:
−3 − 5 = −8
Maximum:
−3 + 5 = 2
Therefore:
−8 ≤ y ≤ 2
The domain of ordinary sine and cosine transformations remains all real numbers unless the context restricts it.
Transformations and Context Restrictions
A mathematical function may exist for all real x-values, but a real-world model may not.
For example, a Ferris wheel model might mathematically accept:
t = −1000
but if the ride began at t = 0, negative time may have no useful meaning.
Similarly, a model of daylight hours might only be intended for a particular year or location.
Always distinguish between:
the mathematical domain
and:
the meaningful domain of the model
Equivalent Trigonometric Equations
An important advanced idea is that different trigonometric equations can describe the same graph.
For example:
cos(x) = sin(x + π/2)
Therefore, a graph written using cosine can often also be written using sine with an appropriate phase shift.
This means there may be more than one correct equation for a transformed sinusoidal graph.
The goal is usually to find a correct and convenient representation.
Common Mistakes
Treating A as the amplitude without using absolute value
For:
y = −4 sin(x)
the amplitude is:
4
not −4.
Forgetting that negative A causes reflection
The negative sign affects orientation.
Using B directly as the period
For:
y = sin(3x)
the period is not 3.
It is:
2π/3
Forgetting the inverse effect of B
Larger B means shorter period.
Reading phase shift before factoring B
For:
sin(2x − π)
the shift is not π.
Factor first:
sin(2(x − π/2))
so the shift is:
π/2 right
Reversing the direction of phase shift
x − C → right
x + C → left
Confusing vertical displacement with amplitude
D controls the midline.
|A| controls the amplitude.
Forgetting to shift the midline
For:
y = sin(x) + 7
the midline is y = 7, not y = 0.
Forgetting the quarter-period
When sketching, divide one period into four equal sections.
Drawing sharp corners
Sine and cosine graphs are smooth curves.
Assuming every periodic graph must be sine
Many functions are periodic, and real-world patterns may only be approximately sinusoidal.
Assuming there is only one possible equation
Equivalent sine and cosine forms can represent the same graph.
Mixing degrees and radians
Use:
360°/|B|
for degrees.
Use:
2π/|B|
for radians.
Key Terms
Transformation — A change in the position, orientation, or scale of a graph.
Parent function — The basic function before transformations.
Trigonometric function — A function such as sine, cosine, or tangent associated with angles and periodic behaviour.
Sinusoidal function — A function whose graph has the repeating wave-like form of sine or cosine.
Amplitude — The vertical distance from the midline to a maximum or minimum.
Period — The horizontal length of one complete cycle.
Cycle — One complete repetition of a periodic pattern.
Phase shift — A horizontal translation of a periodic graph.
Vertical displacement — A vertical translation of the graph.
Midline — The horizontal line halfway between the maximum and minimum.
Maximum — The greatest output value in a cycle.
Minimum — The smallest output value in a cycle.
Vertical stretch — A transformation that increases vertical distances from the midline.
Vertical compression — A transformation that decreases vertical distances from the midline.
Horizontal stretch — A transformation that increases the period.
Horizontal compression — A transformation that decreases the period.
Reflection — A transformation that flips a graph across a line such as the x-axis.
Frequency — The number of cycles occurring per unit of the independent variable.
Radians — A standard unit of angular measurement commonly used in advanced mathematics.
Degrees — An angular measurement system in which one complete revolution is 360°.
Quarter-period — One-fourth of the period, useful for locating key points.
Periodic function — A function whose values repeat at regular intervals.
Parameter — A value in an equation that controls a feature of the function.
Domain — The possible input values of a function.
Range — The possible output values of a function.
Phase — The position of a periodic function within its cycle.
Sinusoidal model — A sine or cosine function used to approximate a repeating real-world phenomenon.
Key Takeaways
- Sine and cosine functions can be transformed to model repeating patterns.
- A useful general form is:
y = A sin(B(x − C)) + D
or:
y = A cos(B(x − C)) + D
- The amplitude is:
|A|
- A negative A reflects the graph across the x-axis.
- The period in radians is:
2π/|B|
- The period in degrees is:
360°/|B|
- Larger |B| produces a shorter period.
- Smaller |B| produces a longer period.
- C determines the phase shift.
- In the standard form, positive C shifts the graph right.
- Negative C shifts the graph left.
- Factor B before identifying phase shift when necessary.
- D determines vertical displacement.
- The midline is:
y = D
- The maximum is:
D + |A|
- The minimum is:
D − |A|
- From a graph:
amplitude = (maximum − minimum)/2
- The midline can be found using:
D = (maximum + minimum)/2
- Divide the period by four to locate five important points in one cycle.
- Sine naturally begins at its midline in the parent form.
- Cosine naturally begins at its maximum in the parent form.
- Different sine and cosine equations can sometimes represent the same graph.
- Trigonometric transformations can model tides, seasons, waves, rotating objects, Ferris wheels, sound, and oscillations.
- In real-world models, every parameter should have an interpretation.
- A mathematical model may have a larger domain than is meaningful in the real situation.
- Understanding transformations allows us to move between equations, graphs, and real-world phenomena.
Check Your Understanding
1. What does amplitude describe?
2. Find the amplitude of:
y = 5 sin(x)
3. Find the amplitude of:
y = −7 cos(x)
4. Explain why the answer to Question 3 is not −7.
5. Determine the period of:
y = sin(2x)
6. Determine the period of:
y = cos(4x)
7. Determine the period of:
y = sin(x/3)
8. Describe the phase shift of:
y = sin(x − π/4)
9. Describe the phase shift of:
y = cos(x + π/3)
10. Determine the vertical displacement and midline of:
y = 4 sin(x) + 6
11. Find the maximum and minimum values of the function in Question 10.
12. For:
y = −3 cos(2x) + 5
determine:
a. amplitude
b. period
c. reflection
d. midline
e. maximum
f. minimum
13. Explain why increasing B decreases the period.
14. A sinusoidal graph has a maximum of 14 and minimum of 4. Find its amplitude.
15. Find the midline of the graph in Question 14.
16. A graph has a period of π. Determine |B|.
17. A graph has a period of 6π. Determine |B|.
18. Determine the actual phase shift of:
y = sin(2x − π)
19. Explain why simply reading π as the phase shift in Question 18 would be incorrect.
20. Analyze completely:
y = 4 sin(3(x − π/6)) − 2
Determine:
a. amplitude
b. period
c. phase shift
d. vertical displacement
e. midline
f. maximum
g. minimum
h. quarter-period
21. A sinusoidal graph has:
maximum = 9
minimum = 1
period = 2π
and begins at a maximum when x = 0.
Write a possible equation.
22. Explain why cosine is convenient for Question 21.
23. A Ferris wheel has a maximum rider height of 50 m and minimum height of 4 m. Find the amplitude and midline.
24. If the Ferris wheel in Question 23 completes one revolution every 80 seconds, state the period.
25. Find B for a model of this Ferris wheel using radians and time in seconds.
26. Explain what amplitude represents physically in the Ferris wheel model.
27. Explain what vertical displacement represents physically.
28. Describe how amplitude, period, phase shift, and vertical displacement could each affect a sinusoidal model.
29. Explain why two different trigonometric equations can sometimes represent the same graph.
30. Challenge: A periodic water-level model has:
- maximum height = 5.8 m
- minimum height = 1.2 m
- period = 12 hours
- a maximum occurs at t = 3 hours
Using a cosine model:
a. calculate the amplitude
b. calculate the midline
c. calculate B
d. determine the phase shift
e. write a possible equation for the water height h(t)
f. determine the predicted maximum and minimum from your equation
g. explain the physical meaning of each parameter
h. explain one reason a real tidal pattern might not follow this model perfectly.
3. Composite Trigonometric Functions
Learning outcomes
- I can evaluate composite trigonometric functions.
- I can analyse combinations of trigonometric functions.
- I can simplify composite expressions.
- I can interpret composite functions graphically.
- I can solve problems involving multiple trigonometric functions.
4. Inverse Trigonometric Functions
Learning outcomes
- I can determine principal values of inverse trigonometric functions.
- I can evaluate inverse trigonometric expressions.
- I can solve equations involving inverse functions.
- I can interpret inverse functions graphically.
- I can apply inverse functions in modelling problems.
5. Trigonometric Modelling
Learning outcomes
- I can model periodic phenomena using trigonometric functions.
- I can determine model parameters from data.
- I can interpret amplitude, period, and phase shift.
- I can evaluate the suitability of trigonometric models.
- I can solve real-world modelling problems.
Trigonometric Modelling
Many real-world quantities change in patterns that repeat over time. Daylight hours increase and decrease each year, tides rise and fall, a Ferris wheel repeatedly carries passengers up and down, and vibrating objects move back and forth around an equilibrium position.
These are examples of periodic phenomena.
Sine and cosine functions are especially useful for modelling smooth repeating patterns because they naturally describe periodic motion.
A general sinusoidal model can be written as:
y = A sin(B(x − C)) + D
or:
y = A cos(B(x − C)) + D
The parameters A, B, C, and D describe important features of the real system.
Recognising Periodic Behaviour
A phenomenon is periodic when it repeats after a regular interval.
Examples include:
- rotation of a wheel
- motion of a pendulum
- seasonal daylight patterns
- approximately seasonal temperature patterns
- tides
- alternating electrical current
- some biological rhythms
- vibrating springs
- sound waves
If the pattern is smooth and oscillates around a central value, a sine or cosine model may be appropriate.
A repeating pattern does not have to start at zero.
It might begin at:
- a maximum
- a minimum
- the midline while increasing
- the midline while decreasing
The starting position helps us choose the most convenient equation.
The General Sinusoidal Model
Consider:
y = A sin(B(x − C)) + D
The parameters have different roles.
| Parameter | Meaning |
|---|---|
| A | controls amplitude |
| B | controls period |
| C | controls phase shift |
| D | controls vertical displacement or midline |
For sine and cosine:
amplitude = |A|
period = 2π/|B|
phase shift = C
midline = y = D
These mathematical features often have direct physical meanings.
Amplitude in a Model
The amplitude measures the maximum distance between the midline and the highest or lowest point.
If the maximum and minimum are known:
amplitude = (maximum − minimum)/2
Suppose a periodic quantity varies between:
maximum = 18
minimum = 6
Then:
amplitude = (18 − 6)/2
= 12/2
= 6
The amplitude tells us the size of the oscillation around the central value.
Finding the Midline
The midline is halfway between the maximum and minimum.
Calculate:
D = (maximum + minimum)/2
Using:
maximum = 18
minimum = 6
we get:
D = (18 + 6)/2
= 24/2
= 12
Therefore, the model oscillates around:
y = 12
Its maximum is:
12 + 6 = 18
and its minimum is:
12 − 6 = 6
Maximum and Minimum
For:
y = A sin(B(x − C)) + D
or the equivalent cosine model:
maximum = D + |A|
minimum = D − |A|
This means that amplitude and midline completely determine the vertical range of a sinusoidal model.
For example:
y = 7cos(Bx) + 20
has:
amplitude = 7
midline = 20
maximum = 27
minimum = 13
Period
The period is the amount of input required for one complete cycle.
For example:
- Earth's seasonal cycle is approximately 1 year
- a Ferris wheel might complete a revolution every 60 seconds
- a pendulum might repeat its motion every 2 seconds
- a periodic signal might repeat every 0.01 seconds
For:
y = A sin(B(x − C)) + D
the period is:
P = 2π/|B|
Therefore, if the period is known:
|B| = 2π/P
This equation is extremely useful when building models from data.
Finding B from the Period
Suppose a periodic phenomenon repeats every:
12 hours
Then:
P = 12
Use:
B = 2π/P
B = 2π/12
= π/6
So the model could contain:
sin((π/6)t)
or:
cos((π/6)t)
depending on its starting position.
Frequency
Frequency describes how often a cycle occurs.
A useful relationship is:
frequency = 1/period
or:
f = 1/P
If a machine completes 5 cycles every second:
f = 5 Hz
Its period is:
P = 1/5
= 0.2 s
Frequency is especially important when modelling waves, vibrations, sound, and electrical signals.
Phase Shift
The phase shift determines the horizontal position of the periodic pattern.
In:
y = A sin(B(x − C)) + D
C represents the phase shift.
For example:
y = 4sin((π/6)(t − 3)) + 10
has a phase shift of:
3 units to the right
In a real-world model, phase shift often tells us when a particular stage of the cycle occurs.
For example, it might describe:
- when high tide occurs
- when maximum temperature occurs
- when a Ferris wheel rider reaches the midline
- when daylight begins increasing from its average
- when a seasonal population reaches its peak
Choosing Sine or Cosine
Sine and cosine can model the same type of periodic behaviour.
The choice often depends on where the data begin.
Cosine is convenient when the cycle begins at:
- a maximum
- a minimum
Sine is convenient when the cycle begins at:
- the midline while increasing
- the midline while decreasing
For example, if a Ferris wheel rider starts at the top, cosine is usually convenient.
If the rider begins at the wheel's centre height while travelling upward, sine is usually convenient.
Different correct equations can sometimes describe the same sinusoidal pattern.
Building a Model from Maximum and Minimum Data
Suppose a quantity varies between:
maximum = 34
minimum = 10
Amplitude:
A = (34 − 10)/2
= 12
Midline:
D = (34 + 10)/2
= 22
We already know that a possible model has the form:
y = 12sin(B(x − C)) + 22
or:
y = 12cos(B(x − C)) + 22
We still need the period and phase information to determine B and C.
A Step-by-Step Modelling Strategy
When constructing a sinusoidal model from data, use this process:
Identify maximum and minimum → Find amplitude → Find midline → Find period → Calculate B → Determine phase shift → Choose sine or cosine → Check the model
This systematic method works for many problems.
Worked Example: Ferris Wheel
A Ferris wheel has:
maximum rider height = 46 m
minimum rider height = 6 m
one revolution = 80 seconds
A rider begins at the highest point.
Find the Amplitude
A = (46 − 6)/2
= 40/2
= 20 m
Find the Midline
D = (46 + 6)/2
= 52/2
= 26 m
This also represents the height of the wheel's centre.
Find B
P = 80
B = 2π/80
= π/40
Since the rider begins at a maximum, cosine is convenient.
Therefore:
h(t) = 20cos((π/40)t) + 26
Interpreting the Ferris Wheel Equation
Consider:
h(t) = 20cos((π/40)t) + 26
Each part has meaning.
20 = radius of the Ferris wheel
π/40 = controls the rotational period
80 s = time for one revolution
26 = height of the centre of the wheel
At:
t = 0
cos(0) = 1
so:
h(0) = 20 + 26
= 46 m
This confirms that the rider begins at the highest point.
Predicting with the Ferris Wheel Model
What is the rider's height after 20 seconds?
Use:
h(t) = 20cos((π/40)t) + 26
Substitute:
t = 20
h(20) = 20cos((π/40)(20)) + 26
= 20cos(π/2) + 26
= 20(0) + 26
= 26 m
After one-quarter of the 80-second cycle, the rider is at the wheel's midline.
Understanding Quarter-Periods
One complete sinusoidal cycle can be divided into four equal sections.
If:
period = P
then:
quarter-period = P/4
For the Ferris wheel:
P = 80 s
quarter-period = 80/4
= 20 s
Starting at the maximum:
| Time | Position |
|---|---|
| 0 s | maximum |
| 20 s | midline |
| 40 s | minimum |
| 60 s | midline |
| 80 s | maximum |
This pattern makes many modelling problems easier to solve without extensive calculation.
Worked Example: Daylight Hours
Suppose a simplified model of daylight has:
maximum daylight = 15 hours
minimum daylight = 9 hours
period = 12 months
Amplitude:
A = (15 − 9)/2
= 3
Midline:
D = (15 + 9)/2
= 12
Period:
P = 12
Therefore:
B = 2π/12
= π/6
If maximum daylight occurs at:
t = 6 months
a convenient cosine model is:
D(t) = 3cos((π/6)(t − 6)) + 12
Interpreting the Daylight Model
In:
D(t) = 3cos((π/6)(t − 6)) + 12
the amplitude 3 means daylight varies approximately:
3 hours above and below the midline
The midline 12 represents:
12 hours of daylight
The period is:
12 months
The phase shift places the maximum at:
t = 6
This demonstrates how the parameters connect mathematical features to real-world meaning.
Worked Example: Tides
Suppose water depth at a harbour varies approximately between:
1.5 m and 5.5 m
and the simplified period between successive high tides is:
12 hours
Suppose high tide occurs at:
t = 2 hours
Amplitude:
A = (5.5 − 1.5)/2
= 2 m
Midline:
D = (5.5 + 1.5)/2
= 3.5 m
Period:
P = 12
B = 2π/12
= π/6
Since high tide represents a maximum, cosine is convenient:
h(t) = 2cos((π/6)(t − 2)) + 3.5
Using the Tide Model
Find the predicted water depth at:
t = 5 hours
Use:
h(t) = 2cos((π/6)(t − 2)) + 3.5
Substitute:
h(5) = 2cos((π/6)(3)) + 3.5
= 2cos(π/2) + 3.5
= 3.5 m
Three hours after the high tide, the model predicts that the water level has reached its midline.
Models from Tables
Sometimes we are given data rather than a description.
Consider:
| Time |
Height (m) |
|---|---|
| 0 | 8 |
| 2 | 12 |
| 4 | 8 |
| 6 | 4 |
| 8 | 8 |
| 10 | 12 |
The maximum is:
12
The minimum is:
4
Amplitude:
A = (12 − 4)/2
= 4
Midline:
D = (12 + 4)/2
= 8
Maximum values occur at:
t = 2 and t = 10
Therefore:
period = 8 hours
So:
B = 2π/8
= π/4
A convenient cosine model with a maximum at t = 2 is:
h(t) = 4cos((π/4)(t − 2)) + 8
Models from Graphs
When determining a trigonometric model from a graph, identify:
- maximum
- minimum
- midline
- amplitude
- distance between consecutive peaks
- distance between consecutive troughs
- direction of movement at useful points
- location of a maximum, minimum, or midline crossing
The distance between consecutive peaks or consecutive troughs gives the period.
Once the period is known:
B = 2π/P
Modelling Seasonal Temperature
Seasonal temperatures often show an approximately periodic annual pattern.
Suppose a simplified temperature model is:
T(t) = 11cos((π/6)(t − 7)) + 18
where t is measured in months.
Amplitude:
11°C
Period:
2π/(π/6)
= 12 months
Phase shift:
7 months
Midline:
18°C
Maximum:
18 + 11 = 29°C
Minimum:
18 − 11 = 7°C
The model predicts a maximum at approximately:
t = 7
Interpreting Parameters in Context
A good modelling answer should not merely calculate parameters. It should explain what they mean.
Suppose:
T(t) = 11cos((π/6)(t − 7)) + 18
Then:
Amplitude = 11°C
The temperature varies approximately 11°C above and below its central level.
Period = 12 months
The pattern repeats annually.
Phase shift = 7 months
The model is positioned so that its maximum occurs around month 7.
Vertical displacement = 18°C
The sinusoidal pattern oscillates around 18°C.
Mathematical parameters should always be interpreted using the appropriate units.
Modelling Oscillations
Consider a mass attached to a spring.
Its displacement from equilibrium might be modelled by:
x(t) = 0.12cos(4πt)
where:
x = displacement in metres
t = time in seconds
Amplitude:
0.12 m
Angular parameter:
B = 4π
Period:
P = 2π/(4π)
= 0.5 s
Frequency:
f = 1/0.5
= 2 Hz
The mass completes two oscillations each second.
Modelling Sound and Waves
A simple sound wave can be modelled using:
y(t) = A sin(2πft + φ)
where:
A = amplitude
f = frequency
φ = phase constant
t = time
For example:
y(t) = 0.02sin(880πt)
Since:
880π = 2πf
divide by 2π:
f = 440 Hz
This corresponds to 440 oscillations per second.
The period is:
P = 1/440
≈ 0.00227 s
Comparing Models
Suppose we have:
Model A: y = 4sin(x) + 10
and:
Model B: y = 7sin(x) + 10
Both have the same:
- period
- phase
- midline
But Model B has a larger amplitude.
Therefore, Model B represents greater variation around the average level.
Now consider:
Model C: y = 4sin(2x) + 10
Compared with Model A, Model C has the same:
- amplitude
- midline
but a shorter period.
It oscillates more rapidly.
Determining Parameters from Real Data
Real data rarely fit a perfect sine or cosine curve.
Suppose measurements show:
maximum ≈ 24.3
minimum ≈ 9.7
Rather than expecting exact values, we might estimate:
Amplitude:
A ≈ (24.3 − 9.7)/2
= 7.3
Midline:
D ≈ (24.3 + 9.7)/2
= 17.0
The use of ≈ is important because the model is an approximation.
Mathematical modelling often involves estimates rather than exact values.
What Makes a Good Trigonometric Model?
A good sinusoidal model usually requires:
- a repeating pattern
- an approximately constant period
- reasonably stable maximum and minimum values
- a central value around which the data oscillate
- smooth changes rather than sudden jumps
If these conditions are approximately satisfied, a sine or cosine model may be useful.
Evaluating Model Suitability
A mathematical equation can always produce numbers, but that does not mean it is a good model.
Ask:
Does the phenomenon actually repeat?
Is the period approximately constant?
Are the peaks and troughs reasonably consistent?
Does the model follow the observed data?
Are there important factors the model ignores?
Are predictions being made inside or outside the observed data range?
A model should be judged by how well it represents reality, not simply by how convenient its equation is.
Residuals
One way to evaluate a model is to compare predicted and observed values.
A residual can be calculated as:
residual = observed value − predicted value
Suppose:
observed temperature = 25.4°C
predicted temperature = 24.8°C
Then:
residual = 25.4 − 24.8
= 0.6°C
A small residual means the prediction is close to the observation.
A large residual suggests a poorer fit at that point.
Residual Patterns
Residuals are especially useful when viewed across many data points.
If residuals are:
- relatively small
- scattered above and below zero
- without an obvious pattern
then the model may be reasonable.
If residuals show a strong pattern, the model may be missing something important.
For example, if residuals repeatedly become positive near each peak and negative near each trough, the model may have the wrong amplitude.
Interpolation
Interpolation means using a model to estimate values within the range of the data used to construct it.
Suppose temperature measurements were collected from January through December.
Using the model to estimate the temperature in June is interpolation.
Interpolation is often relatively reliable if the model fits the data well.
Extrapolation
Extrapolation means using a model to predict beyond the range of observed data.
Suppose we use one year of measurements to predict conditions 50 years later.
That is extrapolation.
Extrapolation is generally less reliable because the underlying system may change.
For example:
- climate conditions may change
- machinery may wear
- biological populations may shift
- human behaviour may change
- environmental conditions may change
Models should therefore be used cautiously outside the data range.
Real Phenomena Are Often More Complicated
A simple sine curve may approximate tides, but real tides are influenced by:
- the Moon
- the Sun
- coastline shape
- water depth
- weather
- atmospheric pressure
- local geography
Similarly, temperature depends on more than seasonal position.
A simple sinusoidal model captures the main periodic pattern, not every detail.
This is an important principle:
A model is a useful simplification of reality, not reality itself.
Sinusoidal Regression
When many real data points are available, technology can be used to find a sinusoidal regression model.
Instead of estimating every parameter manually, software can find values for A, B, C, and D that provide a good fit.
A regression equation might look like:
y = 7.42sin(0.53(x − 2.18)) + 16.37
The decimals reflect the fact that real data do not usually fit perfectly.
Even when technology creates the equation, we still need to interpret:
- amplitude
- period
- phase shift
- midline
- predictions
- limitations
Technology does not replace mathematical interpretation.
Choosing the Correct Domain
Suppose a Ferris wheel ride lasts only:
0 ≤ t ≤ 240 seconds
The trigonometric equation itself continues forever mathematically.
But the real-world model should only be used during the relevant time interval.
This is called a domain restriction.
Likewise, a seasonal model may be mathematically defined for any value of t but only be supported by the years for which data were collected.
Solving a Modelling Problem
Suppose:
h(t) = 6cos((π/10)t) + 8
models the height of an object in metres.
When does:
h = 11 m?
Set:
11 = 6cos((π/10)t) + 8
Subtract 8:
3 = 6cos((π/10)t)
Divide by 6:
1/2 = cos((π/10)t)
We know:
cos(π/3) = 1/2
So one solution is:
(π/10)t = π/3
Multiply by 10/π:
t = 10/3 s
≈ 3.33 s
However, because cosine is periodic, there may be another time during the same cycle when the object has the same height.
Finding the Second Solution
The cosine function has the same value at two points in most cycles.
For:
cos(θ) = 1/2
within:
0 ≤ θ < 2π
the solutions are:
θ = π/3
and:
θ = 5π/3
Therefore:
(π/10)t = 5π/3
t = 50/3 s
≈ 16.67 s
So during one 20-second cycle, the object reaches 11 m at approximately:
3.33 s and 16.67 s
This demonstrates why real-world trigonometric problems can have multiple valid answers.
Checking Whether an Answer Makes Sense
After solving a modelling problem, ask:
- Is the answer inside the allowed domain?
- Are the units correct?
- Is the value between the model's maximum and minimum?
- Does the timing make sense within the cycle?
- Should there be more than one answer?
- Does the graph support the calculation?
For example, if a Ferris wheel has maximum height 40 m, a calculated rider height of 65 m indicates an error.
Model Parameters Tell a Story
Suppose:
P(t) = 250sin((π/6)(t − 2)) + 1200
models a seasonal population.
We can interpret:
250 — the population varies by about 250 above and below its central level.
π/6 — gives a period of 12 time units.
2 — shifts the timing of the cycle.
1200 — the population oscillates around approximately 1200.
The equation is therefore not merely a collection of numbers. Each parameter describes part of the system.
Comparing Two Periodic Models
Suppose:
A(t) = 5sin((π/6)t) + 20
and:
B(t) = 5sin((π/6)(t − 2)) + 20
Both have:
amplitude = 5
period = 12
midline = 20
The only difference is the phase shift.
Model B occurs:
2 time units later
than Model A.
This could represent two locations experiencing similar seasonal patterns at different times.
Multiple Periodic Effects
Some real systems contain more than one periodic pattern.
For example, a temperature model might contain:
- a yearly cycle
- a daily cycle
A simple model could involve multiple trigonometric terms:
T(t) = 20 + 8sin(2πt/365) + 2sin(2πt)
where the time units are chosen appropriately.
The first sine term represents a longer cycle.
The second represents a shorter cycle.
More advanced modelling often combines several periodic functions.
Trigonometric Models in Science and Engineering
Sinusoidal models appear throughout science.
Physics
They describe:
- waves
- oscillations
- circular motion
- alternating current
- simple harmonic motion
Biology
They can approximate:
- circadian rhythms
- seasonal populations
- some heart and respiratory patterns
Earth Science
They can model:
- tides
- seasonal temperatures
- daylight cycles
Engineering
They are used for:
- vibration analysis
- rotating machinery
- electrical signals
- communications
- structural oscillations
Astronomy
Periodic functions can help describe:
- rotating objects
- repeating brightness patterns
- orbital phenomena
Common Mistakes
Using maximum − minimum as the amplitude
Correct:
amplitude = (maximum − minimum)/2
Using the maximum as the midline
Correct:
midline = (maximum + minimum)/2
Assuming B is the period
B controls the period, but:
P = 2π/|B|
Forgetting units
A period might be measured in:
seconds, hours, days, months, or years.
Ignoring phase shift
A model may have the correct amplitude and period but still be badly positioned horizontally.
Automatically choosing sine
Cosine may produce a much simpler model if the data begin at a maximum or minimum.
Assuming sine and cosine models must look different
A sine model and appropriately shifted cosine model can describe the same curve.
Treating a model as exact
Real-world data contain variation, uncertainty, and measurement error.
Ignoring residuals
Differences between predictions and observations help reveal how well a model fits.
Extrapolating too far
A model fitted to current data may not remain accurate indefinitely.
Ignoring domain restrictions
A model should only be used where it makes physical and contextual sense.
Forgetting multiple solutions
A periodic system may reach the same value more than once during a cycle.
Rounding parameters too early
Early rounding can noticeably change later predictions.
Key Terms
Mathematical model — A mathematical representation of a real system or phenomenon.
Trigonometric model — A model using trigonometric functions such as sine or cosine.
Periodic phenomenon — A phenomenon that repeats after a regular interval.
Sinusoidal model — A model having the wave-like form of sine or cosine.
Parameter — A value in a model controlling one of its features.
Amplitude — The maximum distance from the midline.
Period — The input interval required for one complete cycle.
Frequency — The number of cycles occurring per unit of input.
Phase shift — A horizontal displacement of a periodic model.
Vertical displacement — A vertical shift of a graph.
Midline — The central value around which a sinusoidal model oscillates.
Maximum — The greatest predicted value during a cycle.
Minimum — The smallest predicted value during a cycle.
Cycle — One complete repetition of a periodic pattern.
Quarter-period — One-fourth of a complete period.
Oscillation — Repeated movement or variation around an equilibrium or central value.
Regression — A statistical method for fitting a mathematical model to data.
Sinusoidal regression — A method for fitting a sine or cosine model to periodic data.
Observed value — A value actually measured or recorded.
Predicted value — A value produced by a mathematical model.
Residual — The difference between an observed and predicted value.
Interpolation — Prediction within the range of observed data.
Extrapolation — Prediction outside the range of observed data.
Domain restriction — A limitation placed on input values so that a model matches its real-world context.
Model suitability — How appropriately and accurately a model represents the phenomenon being studied.
Approximation — A value or model that is close to, but not exactly equal to, reality.
Equilibrium — A central or resting position around which an oscillating system moves.
Angular frequency — A measure of the rate of oscillation commonly represented in radians per unit time.
Key Takeaways
- Trigonometric functions are useful for modelling repeating phenomena.
- Sine and cosine are particularly useful for smooth periodic patterns.
- A general model is:
y = A sin(B(x − C)) + D
or:
y = A cos(B(x − C)) + D
- The amplitude is:
|A|
- From maximum and minimum:
amplitude = (maximum − minimum)/2
- The midline is:
D = (maximum + minimum)/2
- Maximum:
D + |A|
- Minimum:
D − |A|
- Period is the length of one complete cycle.
- The relationship between B and period is:
P = 2π/|B|
- Therefore:
|B| = 2π/P
- Frequency and period are related by:
f = 1/P
- Phase shift determines the timing of the cycle.
- Cosine is often convenient when the model begins at a maximum or minimum.
- Sine is often convenient when the model begins at its midline.
- Different sine and cosine equations can represent the same periodic pattern.
- Parameters should always be interpreted in context and with units.
- Models can be constructed from descriptions, tables, graphs, or measured data.
- Real-world data rarely follow perfect sinusoidal curves.
- Residuals measure the differences between observed and predicted values.
- Small, randomly distributed residuals generally support the suitability of a model.
- Interpolation uses a model within the observed data range.
- Extrapolation predicts beyond the observed data and is generally less reliable.
- Real systems often contain influences that a simple sinusoidal model ignores.
- A model's mathematical domain may be larger than its meaningful real-world domain.
- Periodic equations can produce multiple solutions to real-world problems.
- Trigonometric modelling is widely used in physics, engineering, biology, Earth science, astronomy, and signal analysis.
- A mathematical model is a simplification of reality, not a perfect copy of it.
A useful modelling process is:
Data → Pattern → Parameters → Equation → Prediction → Evaluation
Check Your Understanding
1. What makes a phenomenon periodic?
2. Give three real-world examples of periodic phenomena.
3. For:
y = 6sin(2x) + 10
identify the amplitude and midline.
4. Find the maximum and minimum of the function in Question 3.
5. Find the period of:
y = 4cos(3x)
6. A periodic phenomenon has a period of 10 seconds. Find B.
7. A quantity varies between 8 and 24. Find its amplitude.
8. Find its midline.
9. A periodic pattern repeats every 12 months. Find B.
10. Explain what phase shift means in a real-world model.
11. When might cosine be more convenient than sine?
12. A Ferris wheel has maximum height 54 m and minimum height 6 m. Find its amplitude.
13. Find the height of the Ferris wheel's centre.
14. The wheel completes one revolution every 72 seconds. Find B.
15. If a rider begins at the maximum height, write a cosine model for the rider's height.
16. Where will the rider be after one-quarter of the period?
17. A temperature model is:
T(t) = 8cos((π/6)(t − 7)) + 21
Determine:
a. amplitude
b. period
c. phase shift
d. midline
e. maximum temperature
f. minimum temperature
18. Explain the meaning of the period in Question 17.
19. Explain the meaning of the amplitude in Question 17.
20. A tide model is:
h(t) = 1.8cos((π/6)(t − 3)) + 3.2
Determine its maximum and minimum predicted water levels.
21. At what time does the model first predict maximum water level?
22. Explain why a simple sinusoidal tide model may not perfectly predict real tides.
23. Define residual.
24. A model predicts 18.7°C but the measured value is 20.1°C. Calculate the residual using:
observed − predicted
25. Explain the difference between interpolation and extrapolation.
26. Why is long-range extrapolation often unreliable?
27. Explain why a mathematically valid input might not make sense in a real-world model.
28. Describe two characteristics of data that would suggest a sinusoidal model might be appropriate.
29. Explain why a periodic equation may give more than one time when a particular value occurs.
30. Challenge: The depth of water at a harbour varies approximately between 1.4 m and 6.2 m. Successive high tides occur approximately 12.4 hours apart, and one high tide occurs at t = 2.5 hours.
a. Calculate the amplitude.
b. Calculate the midline.
c. Determine the period.
d. Calculate B.
e. Choose an appropriate sine or cosine function and explain your choice.
f. Write a possible model for the water depth h(t).
g. Use the model to predict the water depth 3.1 hours after the high tide.
h. Determine approximately when the first low tide occurs after t = 2.5 hours.
i. Explain what each parameter in your model represents physically.
j. Give at least three reasons why actual harbour measurements might differ from the model's predictions.
k. Explain how residuals could be used to evaluate the model.
l. Explain why predictions several years into the future should be treated cautiously.