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.

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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

θ\theta

in standard position, the point where its terminal side intersects the unit circle has coordinates:

(cosθ, sinθ)

Therefore:

  • x-coordinate = cosθ
  • -coordinate = sinθ

This connection allows us to evaluate trigonometric functions for angles much larger than 90o, as well as negative angles.


The Six Functions on the Unit Circle

If a point on the unit circle is: (x, y) then:

sinθ = y

cosθ = x

and:

\( tan \theta = \frac{y}{x} \)

The reciprocal functions become:

\( csc \theta = \frac{1}{y} \)

\( sec \theta = \frac{1}{x} \)

\( cot \theta = \frac{x}{y} \)

So all six trigonometric functions can be determined from the coordinates of a point on the unit circle.


Example Using Coordinates

Suppose a point on the unit circle is:

\( ( \frac{3}{5}, \frac{4}{5}) \)

(35,45)\left(\frac35,\frac45\right)

Then:

\( cos \theta = \frac{3}{5} \)

and:

\( sin \theta = \frac{4}{5} \)

Therefore:

\( tan \theta = \frac{sin \theta }{cos \theta } = \frac{ \frac{4}{5} }{ \frac{3}{5} } = \frac{4}{3} \)

The reciprocal functions are:

csc⁡θ=54\csc\theta=\frac54sec⁡θ=53\sec\theta=\frac53cot⁡θ=34\cot\theta=\frac34

So:

sin⁡θ=45,cos⁡θ=35,tan⁡θ=43\boxed{ \sin\theta=\frac45,\quad \cos\theta=\frac35,\quad \tan\theta=\frac43 }csc⁡θ=54,sec⁡θ=53,cot⁡θ=34\boxed{ \csc\theta=\frac54,\quad \sec\theta=\frac53,\quad \cot\theta=\frac34 }

Important Angles

Several angles appear repeatedly in trigonometry.

The most important are:

0∘,30∘,45∘,60∘,90∘0^\circ,\quad30^\circ,\quad45^\circ,\quad60^\circ,\quad90^\circ

Their radian equivalents are:

0,π6,π4,π3,π20,\quad\frac{\pi}{6},\quad\frac{\pi}{4},\quad\frac{\pi}{3},\quad\frac{\pi}{2}

Students should become familiar with their exact sine and cosine values.

Angle Radians sin⁡θ\sin\theta cos⁡θ\cos\theta tan⁡θ\tan\theta
0∘0^\circ 00 00 11 00
30∘30^\circ π/6\pi/6 1/21/2 3/2\sqrt3/2 3/3\sqrt3/3
45∘45^\circ π/4\pi/4 2/2\sqrt2/2 2/2\sqrt2/2 11
60∘60^\circ π/3\pi/3 3/2\sqrt3/2 1/21/2 3\sqrt3
90∘90^\circ π/2\pi/2 11 00 undefined
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Exact Values

An exact value is written without rounding to a decimal.

For example:

sin⁡60∘=32\sin60^\circ=\frac{\sqrt3}{2}

is exact.

A calculator might give:

sin⁡60∘≈0.866\sin60^\circ\approx0.866

This is an approximation.

When a question asks for an exact value, answers should normally remain as fractions and radicals.


Special Triangles

The exact values on the unit circle come from two important right triangles.

45°–45°–90° Triangle

Its side ratio is:

1:1:21:1:\sqrt2

Therefore:

sin⁡45∘=12=22\sin45^\circ=\frac{1}{\sqrt2} =\frac{\sqrt2}{2}

and:

cos⁡45∘=22\cos45^\circ=\frac{\sqrt2}{2}

30°–60°–90° Triangle

Its side ratio is:

1:3:21:\sqrt3:2

Therefore:

sin⁡30∘=12\sin30^\circ=\frac12cos⁡30∘=32\cos30^\circ=\frac{\sqrt3}{2}sin⁡60∘=32\sin60^\circ=\frac{\sqrt3}{2}cos⁡60∘=12\cos60^\circ=\frac12
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The Four Quadrants

The coordinate plane is divided into four quadrants.

The signs of sine, cosine, and tangent depend on the quadrant containing the terminal side of the angle.

Quadrant I

sin⁡+,cos⁡+,tan⁡+\sin+,\quad\cos+,\quad\tan+

Quadrant II

sin⁡+,cos⁡−,tan⁡−\sin+,\quad\cos-,\quad\tan-

Quadrant III

sin⁡−,cos⁡−,tan⁡+\sin-,\quad\cos-,\quad\tan+

Quadrant IV

sin⁡−,cos⁡+,tan⁡−\sin-,\quad\cos+,\quad\tan-
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A common memory aid is ASTC:

  • Quadrant I – All positive
  • Quadrant II – Sine positive
  • Quadrant III – Tangent positive
  • Quadrant IV – Cosine positive

The reciprocal functions have the same signs as their corresponding functions:

  • cosecant has the same sign as sine
  • secant has the same sign as cosine
  • cotangent has the same sign as tangent

Reference Angles

A reference angle is the positive acute angle formed between the terminal side of an angle and the

xx

-axis.

Reference angles allow us to use familiar exact values for angles in any quadrant.

For example:

150∘150^\circ

is in Quadrant II.

Its reference angle is:

180∘−150∘=30∘180^\circ-150^\circ=30^\circ

We therefore use the values associated with

30∘30^\circ

.


Example: Evaluate

sin⁡150∘\sin150^\circ

Reference angle:

30∘30^\circ

We know:

sin⁡30∘=12\sin30^\circ=\frac12

Sine is positive in Quadrant II.

Therefore:

sin⁡150∘=12\boxed{\sin150^\circ=\frac12}

Example: Evaluate

cos⁡150∘\cos150^\circ

Again, the reference angle is:

30∘30^\circ

We know:

cos⁡30∘=32\cos30^\circ=\frac{\sqrt3}{2}

But cosine is negative in Quadrant II.

Therefore:

cos⁡150∘=−32\boxed{\cos150^\circ=-\frac{\sqrt3}{2}}

Example: Evaluate

tan⁡225∘\tan225^\circ

The angle

225∘225^\circ

lies in Quadrant III.

Its reference angle is:

225∘−180∘=45∘225^\circ-180^\circ=45^\circ

We know:

tan⁡45∘=1\tan45^\circ=1

Tangent is positive in Quadrant III.

Therefore:

tan⁡225∘=1\boxed{\tan225^\circ=1}

Finding Reference Angles

For angles between

0∘0^\circ

and

360∘360^\circ

:

Quadrant I

θR=θ\theta_R=\theta

Quadrant II

θR=180∘−θ\theta_R=180^\circ-\theta

Quadrant III

θR=θ−180∘\theta_R=\theta-180^\circ

Quadrant IV

θR=360∘−θ\theta_R=360^\circ-\theta

where

θR\theta_R

is the reference angle.


Evaluating All Six Functions

Suppose:

θ=120∘\theta=120^\circ

Step 1 – Find the reference angle

180∘−120∘=60∘180^\circ-120^\circ=60^\circ

Step 2 – Identify the quadrant

120∘120^\circ

is in Quadrant II.

Therefore:

  • sine is positive
  • cosine is negative
  • tangent is negative

Step 3 – Find the first three functions

sin⁡120∘=32\sin120^\circ=\frac{\sqrt3}{2}cos⁡120∘=−12\cos120^\circ=-\frac12tan⁡120∘=−3\tan120^\circ=-\sqrt3

Step 4 – Use reciprocals

csc⁡120∘=23=233\csc120^\circ=\frac{2}{\sqrt3} =\frac{2\sqrt3}{3}sec⁡120∘=−2\sec120^\circ=-2cot⁡120∘=−13=−33\cot120^\circ=-\frac{1}{\sqrt3} =-\frac{\sqrt3}{3}

Therefore all six functions can be determined from the reference angle and quadrant.


Domains and Ranges

A function's domain tells us which input values are allowed.

Its range tells us which output values are possible.

The six trigonometric functions have different domains and ranges.


Sine

Because sine represents the

yy

-coordinate on the unit circle:

−1≤sin⁡θ≤1-1\leq\sin\theta\leq1

Domain

All real numbers\boxed{\text{All real numbers}}

Range

[−1,1]\boxed{[-1,1]}
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Cosine

Cosine represents the

xx

-coordinate on the unit circle.

Therefore:

−1≤cos⁡θ≤1-1\leq\cos\theta\leq1

Domain

All real numbers\boxed{\text{All real numbers}}

Range

[−1,1]\boxed{[-1,1]}
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Tangent

Tangent can be written as:

tan⁡θ=sin⁡θcos⁡θ\tan\theta=\frac{\sin\theta}{\cos\theta}

Division by zero is undefined.

Therefore tangent is undefined whenever:

cos⁡θ=0\cos\theta=0

This occurs at:

90∘,270∘,450∘,…90^\circ,\quad270^\circ,\quad450^\circ,\ldots

or generally:

θ=90∘+180∘k\theta=90^\circ+180^\circ k

where

kk

is any integer.

Domain

All real numbers except:

θ=π2+kπ\boxed{\theta=\frac{\pi}{2}+k\pi}

Range

(−∞,∞)\boxed{(-\infty,\infty)}
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Cosecant

Since:

csc⁡θ=1sin⁡θ\csc\theta=\frac{1}{\sin\theta}

cosecant is undefined whenever:

sin⁡θ=0\sin\theta=0

Therefore:

Domain

All real numbers except:

θ=kπ\boxed{\theta=k\pi}

Range

Since sine lies between

−1-1

and

11

, cosecant cannot have values strictly between

−1-1

and

11

:

(−∞,−1]∪[1,∞)\boxed{(-\infty,-1]\cup[1,\infty)}

Secant

Since:

sec⁡θ=1cos⁡θ\sec\theta=\frac{1}{\cos\theta}

secant is undefined whenever:

cos⁡θ=0\cos\theta=0

Domain

All real numbers except:

θ=π2+kπ\boxed{\theta=\frac{\pi}{2}+k\pi}

Range

(−∞,−1]∪[1,∞)\boxed{(-\infty,-1]\cup[1,\infty)}

Cotangent

Since:

cot⁡θ=cos⁡θsin⁡θ\cot\theta=\frac{\cos\theta}{\sin\theta}

cotangent is undefined whenever:

sin⁡θ=0\sin\theta=0

Domain

All real numbers except:

θ=kπ\boxed{\theta=k\pi}

Range

(−∞,∞)\boxed{(-\infty,\infty)}

Comparing Domains and Ranges

Function Domain Restrictions Range
sin⁡θ\sin\theta None [−1,1][-1,1]
cos⁡θ\cos\theta None [−1,1][-1,1]
tan⁡θ\tan\theta θ≠π2+kπ\theta\neq\frac{\pi}{2}+k\pi All real numbers
csc⁡θ\csc\theta θ≠kπ\theta\neq k\pi y≤−1y\leq-1ory≥1y\geq1
sec⁡θ\sec\theta θ≠π2+kπ\theta\neq\frac{\pi}{2}+k\pi y≤−1y\leq-1ory≥1y\geq1
cot⁡θ\cot\theta θ≠kπ\theta\neq k\pi All real numbers

Here:

k∈Zk\in\mathbb{Z}

means

kk

can be any integer.


Connecting Geometry and Algebra

Trigonometric functions can be understood in several different ways.

Geometrically

Using right triangles:

sin⁡θ=oppositehypotenuse\sin\theta=\frac{\text{opposite}}{\text{hypotenuse}}

Using the Unit Circle

Using coordinates:

(cos⁡θ,sin⁡θ)(\cos\theta,\sin\theta)

Algebraically

Using identities such as:

tan⁡θ=sin⁡θcos⁡θ\tan\theta=\frac{\sin\theta}{\cos\theta}

and:

sin⁡2θ+cos⁡2θ=1\sin^2\theta+\cos^2\theta=1

Graphically

Using graphs such as:

y=sin⁡xy=\sin x

and:

y=cos⁡xy=\cos x

These are not separate ideas. They are different representations of the same mathematical relationships.


Connecting the Unit Circle to the Sine Graph

Imagine a point moving counterclockwise around the unit circle.

Its vertical coordinate is:

sin⁡θ\sin\theta

As the point travels around the circle, its vertical position changes:

0→1→0→−1→00\rightarrow1\rightarrow0\rightarrow-1\rightarrow0

These values produce the familiar sine wave.

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6

The sine graph is therefore closely connected to circular motion.


Connecting the Unit Circle to the Cosine Graph

Cosine represents the horizontal coordinate of the moving point.

As the point travels around the unit circle:

1→0→−1→0→11\rightarrow0\rightarrow-1\rightarrow0\rightarrow1

These values create the cosine graph.

This explains why sine and cosine have the same general shape but are shifted relative to one another.


Periodic Behaviour

Trigonometric functions repeat their values.

This is called periodicity.

Sine and cosine repeat every:

360∘360^\circ

or:

2π2\pi

Therefore:

sin⁡(θ+360∘)=sin⁡θ\sin(\theta+360^\circ)=\sin\theta

and:

cos⁡(θ+360∘)=cos⁡θ\cos(\theta+360^\circ)=\cos\theta

Tangent and cotangent repeat every:

180∘180^\circ

or:

π\pi

Therefore:

tan⁡(θ+180∘)=tan⁡θ\tan(\theta+180^\circ)=\tan\theta

Example: Angles Greater Than 360°

Evaluate:

cos⁡420∘\cos420^\circ

Subtract one complete rotation:

420∘−360∘=60∘420^\circ-360^\circ=60^\circ

Therefore:

cos⁡420∘=cos⁡60∘\cos420^\circ=\cos60^\circcos⁡420∘=12\boxed{\cos420^\circ=\frac12}

This demonstrates how periodicity allows us to simplify large angles.


Negative Angles

Negative angles are measured clockwise from the positive

xx

-axis.

For example:

−45∘-45^\circ

ends in Quadrant IV.

Therefore:

sin⁡(−45∘)=−22\sin(-45^\circ)=-\frac{\sqrt2}{2}

while:

cos⁡(−45∘)=22\cos(-45^\circ)=\frac{\sqrt2}{2}

This gives the useful relationships:

sin⁡(−θ)=−sin⁡θ\boxed{\sin(-\theta)=-\sin\theta}

and:

cos⁡(−θ)=cos⁡θ\boxed{\cos(-\theta)=\cos\theta}

Sine is an odd function, while cosine is an even function.


A Complete Example

Evaluate exactly:

sec⁡315∘\sec315^\circ

Step 1 – Identify the quadrant

315∘315^\circ

lies in Quadrant IV.

Step 2 – Find the reference angle

360∘−315∘=45∘360^\circ-315^\circ=45^\circ

Step 3 – Determine cosine

Cosine is positive in Quadrant IV:

cos⁡315∘=22\cos315^\circ=\frac{\sqrt2}{2}

Step 4 – Take the reciprocal

sec⁡315∘=122\sec315^\circ= \frac{1}{\frac{\sqrt2}{2}}=22=\frac{2}{\sqrt2}=2=\sqrt2

Therefore:

sec⁡315∘=2\boxed{\sec315^\circ=\sqrt2}

Another Complete Example

Evaluate exactly:

csc⁡240∘\csc240^\circ

Reference angle:

240∘−180∘=60∘240^\circ-180^\circ=60^\circ

The angle lies in Quadrant III, where sine is negative.

Therefore:

sin⁡240∘=−32\sin240^\circ=-\frac{\sqrt3}{2}

Take the reciprocal:

csc⁡240∘=−23\csc240^\circ=-\frac{2}{\sqrt3}

Rationalize:

csc⁡240∘=−233\boxed{\csc240^\circ=-\frac{2\sqrt3}{3}}

A Strategy for Exact Trigonometric Values

When asked to find an exact value:

Step 1: Determine the quadrant.

Step 2: Find the reference angle.

Step 3: Recall the exact value for

30∘30^\circ

,

45∘45^\circ

, or

60∘60^\circ

.

Step 4: Determine whether the answer should be positive or negative.

Step 5: Use a reciprocal if the question asks for

csc⁡\csc

,

sec⁡\sec

, or

cot⁡\cot

.

Step 6: Simplify the answer exactly rather than converting to a decimal.


Common Misconceptions

SOH-CAH-TOA is not limited to the whole study of trigonometry.

It is extremely useful for right triangles, but the unit circle extends trigonometric functions to much broader sets of angles.

Tangent is not always defined.

Since:

tan⁡θ=sin⁡θcos⁡θ\tan\theta=\frac{\sin\theta}{\cos\theta}

it is undefined whenever:

cos⁡θ=0\cos\theta=0

Sine and cosine cannot be larger than 1 or smaller than -1.

Their values are coordinates on a circle of radius 1.

Reference angles are always positive acute angles.

They describe the angle between the terminal side and the

xx

-axis.

Exact values should not automatically be converted to decimals.

For example:

32\frac{\sqrt3}{2}

is usually preferred to:

0.8660.866

when an exact value is requested.


Did You Know?

Trigonometric graphs appear throughout science because many natural processes are periodic.

Sine and cosine functions can model:

  • sound waves
  • light waves
  • alternating electrical current
  • ocean tides
  • vibrations
  • rotating objects
  • seasonal cycles
  • pendulum motion
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6

The unit circle, triangle ratios, and sine-wave graphs may look like different topics at first, but they are all representations of the same underlying trigonometric relationships.


Key Terms

Trigonometric function – A function relating angles to ratios or coordinates.

Unit circle – A circle of radius 1 centred at the origin.

Sine – The

yy

-coordinate of a point on the unit circle.

Cosine – The

xx

-coordinate of a point on the unit circle.

Tangent – The ratio

sin⁡θ/cos⁡θ\sin\theta/\cos\theta

.

Cosecant – The reciprocal of sine.

Secant – The reciprocal of cosine.

Cotangent – The reciprocal of tangent.

Reference angle – The positive acute angle between an angle's terminal side and the

xx

-axis.

Exact value – A value expressed exactly using fractions, integers, or radicals rather than a rounded decimal.

Domain – The possible inputs of a function.

Range – The possible outputs of a function.

Period – The interval after which a function repeats its values.


Key Takeaways

  • There are six trigonometric functions:
sin⁡,cos⁡,tan⁡,csc⁡,sec⁡,cot⁡\boxed{\sin,\cos,\tan,\csc,\sec,\cot}
  • On the unit circle:
(cos⁡θ,sin⁡θ)\boxed{(\cos\theta,\sin\theta)}
  • The reciprocal relationships are:
csc⁡θ=1sin⁡θ\csc\theta=\frac1{\sin\theta}sec⁡θ=1cos⁡θ\sec\theta=\frac1{\cos\theta}cot⁡θ=1tan⁡θ\cot\theta=\frac1{\tan\theta}
  • Exact values for30∘30^\circ,45∘45^\circ, and60∘60^\circcan be determined using special triangles.
  • Reference angles allow exact values to be found in all four quadrants.
  • The signs of trig functions depend on the quadrant.
  • Sine and cosine have range:
[−1,1][-1,1]
  • Tangent and cotangent have all real numbers as their range but have restrictions in their domains.
  • Secant and cosecant have range:
(−∞,−1]∪[1,∞)(-\infty,-1]\cup[1,\infty)
  • Sine, cosine, secant, and cosecant repeat every2π2\pi.
  • Tangent and cotangent repeat everyπ\pi.
  • Trigonometric ideas can be represented geometrically, algebraically, graphically, and through the unit circle.
  • Understanding the connections between these representations provides the foundation for more advanced work with trigonometric identities, equations, functions, and calculus.
 
 
 

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.

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6

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.

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7

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.

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5

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

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5

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.

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6

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.

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4

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.

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4

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:

  1. identify the parent function
  2. determine amplitude and reflection
  3. determine period
  4. determine phase shift
  5. determine vertical displacement
  6. find the midline
  7. determine maximum and minimum
  8. calculate the quarter-period
  9. plot key points
  10. 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.

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5

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.

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5

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.

Composite Trigonometric Functions

Trigonometric functions are often combined to create more complex expressions and models. Instead of working with only:

sin(x)

or:

cos(x)

we might encounter expressions such as:

sin(x) + cos(x)

2sin(x) − cos(x)

sin²(x) + cos²(x)

sin(2x)cos(x)

or even a true composition of functions, such as:

sin(cos(x))

These combinations are called composite or combined trigonometric expressions in many courses. They allow us to describe more complicated patterns than a single basic sine, cosine, or tangent function.

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4

Two Meanings of "Composite"

The word composite needs some care because it can describe two related but different ideas.

Combining Trigonometric Functions

Functions may be added, subtracted, multiplied, or divided:

sin(x) + cos(x)

sin(x)cos(x)

sin(x)/cos(x)

These are combinations of trigonometric functions.

Function Composition

One function can also be placed inside another:

sin(cos(x))

This is a true composite function.

If:

f(x) = sin(x)

and:

g(x) = cos(x)

then:

f(g(x)) = sin(cos(x))

Both ideas are useful, so we will examine both.


Evaluating Combined Trigonometric Functions

Consider:

f(x) = sin(x) + cos(x)

To evaluate f(x), calculate both trigonometric values and then add them.

Suppose:

x = 0

Then:

f(0) = sin(0) + cos(0)

= 0 + 1

= 1

At:

x = π/2

f(π/2) = sin(π/2) + cos(π/2)

= 1 + 0

= 1

At:

x = π

f(π) = sin(π) + cos(π)

= 0 − 1

= −1


Important Exact Trigonometric Values

Composite expressions frequently use familiar angles, so exact values are valuable.

Angle sin cos tan
0 0 1 0
π/6 1/2 √3/2 √3/3
π/4 √2/2 √2/2 1
π/3 √3/2 1/2 √3
π/2 1 0 undefined

Knowing these values allows many expressions to be evaluated without a calculator.


Worked Example: Addition

Evaluate:

2sin(x) + cos(x)

when:

x = π/6

Use:

sin(π/6) = 1/2

cos(π/6) = √3/2

Therefore:

2(1/2) + √3/2

= 1 + √3/2

So the exact answer is:

1 + √3/2


Worked Example: Subtraction

Evaluate:

3cos(x) − 2sin(x)

when:

x = π/3

Use:

cos(π/3) = 1/2

sin(π/3) = √3/2

Substitute:

3(1/2) − 2(√3/2)

= 3/2 − √3

Therefore:

3cos(π/3) − 2sin(π/3) = 3/2 − √3


Multiplying Trigonometric Functions

Functions can also be multiplied.

Consider:

f(x) = sin(x)cos(x)

At:

x = π/4

sin(π/4) = √2/2

cos(π/4) = √2/2

Therefore:

f(π/4) = (√2/2)(√2/2)

= 2/4

= 1/2

Products of trigonometric functions appear frequently in identities, calculus, waves, and physics.


Dividing Trigonometric Functions

Consider:

sin(x)/cos(x)

One of the fundamental trigonometric identities tells us:

sin(x)/cos(x) = tan(x)

as long as:

cos(x) ≠ 0

Therefore:

sin(x)/cos(x)

can often be simplified immediately to:

tan(x)

This also reminds us that the expression is undefined wherever cos(x) = 0.


Fundamental Trigonometric Identities

Identities are extremely useful when simplifying composite expressions.

Three of the most important are:

sin²(x) + cos²(x) = 1

1 + tan²(x) = sec²(x)

1 + cot²(x) = csc²(x)

These are called Pythagorean identities.

They are true for every value of x for which the expressions are defined.

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Simplifying with an Identity

Simplify:

sin²(x) + cos²(x) + sin(x)

Use:

sin²(x) + cos²(x) = 1

Therefore:

sin²(x) + cos²(x) + sin(x)

= 1 + sin(x)

A complicated-looking expression has become much simpler.


Another Simplification

Simplify:

1 − sin²(x)

From:

sin²(x) + cos²(x) = 1

subtract sin²(x):

cos²(x) = 1 − sin²(x)

Therefore:

1 − sin²(x) = cos²(x)

Similarly:

1 − cos²(x) = sin²(x)


Quotient Identities

Two important quotient identities are:

tan(x) = sin(x)/cos(x)

and:

cot(x) = cos(x)/sin(x)

These allow expressions containing fractions to be simplified.

For example:

cos(x)tan(x)

Replace tan(x):

cos(x) × sin(x)/cos(x)

Cancel cos(x), where cos(x) ≠ 0:

= sin(x)


Reciprocal Identities

The reciprocal trigonometric functions are:

sec(x) = 1/cos(x)

csc(x) = 1/sin(x)

cot(x) = 1/tan(x)

These relationships are useful when expressions contain several different trigonometric functions.

For example:

cos(x)sec(x)

= cos(x) × 1/cos(x)

= 1

where cos(x) ≠ 0.


Evaluating True Composite Functions

Now consider actual function composition.

Suppose:

f(x) = sin(x)

and:

g(x) = x²

Then:

f(g(x)) = sin(x²)

The output of g becomes the input of f.

To evaluate at x = 2:

g(2) = 2²

= 4

Then:

f(4) = sin(4)

Therefore:

f(g(2)) = sin(4)

If working in radians, a calculator gives approximately:

−0.757


The Inside Function Comes First

Consider:

sin(cos(x))

To evaluate this expression:

  1. calculate cos(x)
  2. use that answer as the input of sine

Suppose:

x = 0

First:

cos(0) = 1

Then:

sin(1) ≈ 0.841

Therefore:

sin(cos(0)) ≈ 0.841

Notice that the 1 is interpreted as 1 radian.


Order Matters in Function Composition

In general:

f(g(x)) ≠ g(f(x))

For example:

sin(cos(x))

is not generally equal to:

cos(sin(x))

At x = 0:

sin(cos(0)) = sin(1)

≈ 0.841

but:

cos(sin(0)) = cos(0)

= 1

Therefore, the order of composition matters.


Composition Notation

Function composition is often written using the symbol:

∘

If:

f(x) = sin(x)

and:

g(x) = 2x

then:

(f ∘ g)(x) = f(g(x))

Therefore:

(f ∘ g)(x) = sin(2x)

But:

(g ∘ f)(x) = g(f(x))

so:

(g ∘ f)(x) = 2sin(x)

These are different functions.


Combined Functions and Graphs

When two trigonometric functions are combined, their graphs can interact in interesting ways.

Consider:

y = sin(x) + cos(x)

At every x-value, the y-values of the two functions are added.

For example:

x sin(x) cos(x) sin(x) + cos(x)
0 0 1 1
π/2 1 0 1
π 0 −1 −1
3π/2 −1 0 −1
2π 0 1 1

The resulting function is still periodic.

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5

A Surprising Result

The expression:

sin(x) + cos(x)

can actually be rewritten as a single sinusoidal function:

√2 sin(x + π/4)

This means that adding two sinusoidal functions with the same frequency can sometimes produce another sinusoidal function.

Its amplitude is:

√2

rather than 1.

This idea becomes extremely important when studying waves.


Combining a sin(x) + b cos(x)

A more general expression is:

a sin(x) + b cos(x)

This can be rewritten in the form:

R sin(x + φ)

where:

R = √(a² + b²)

The value R becomes the amplitude of the resulting sinusoidal function.

For example:

3sin(x) + 4cos(x)

has:

R = √(3² + 4²)

= √25

= 5

So the combined function has amplitude:

5

The phase angle φ depends on the relative contributions of the sine and cosine terms.


Rewriting a Combination as One Function

Suppose:

3sin(x) + 4cos(x) = R sin(x + φ)

Expand the right side using:

sin(x + φ) = sin(x)cos(φ) + cos(x)sin(φ)

Then:

R sin(x + φ)

= Rcos(φ)sin(x) + Rsin(φ)cos(x)

Compare coefficients:

Rcos(φ) = 3

Rsin(φ) = 4

Since R = 5:

cos(φ) = 3/5

sin(φ) = 4/5

Therefore:

φ ≈ 0.927 radians

or:

φ ≈ 53.1°

So:

3sin(x) + 4cos(x) = 5sin(x + 53.1°)

when working in degrees.

This technique is sometimes called harmonic addition or the auxiliary angle method.


Why This Simplification Is Useful

Suppose we have:

3sin(x) + 4cos(x)

It may not be immediately obvious what its maximum value is.

But once rewritten as:

5sin(x + φ)

we immediately know:

maximum = 5

minimum = −5

amplitude = 5

This makes graphing and solving equations much easier.


Different Frequencies

Not every combination can be simplified into one ordinary sine wave.

Consider:

sin(x) + sin(2x)

The two terms have different frequencies.

The first has period:

2π

The second has period:

π

Their sum produces a more complicated periodic shape.

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6

Finding the Period of a Combined Function

Consider:

f(x) = sin(x) + sin(2x)

sin(x) repeats every:

2π

sin(2x) repeats every:

π

We need a length over which both functions repeat.

The smallest such interval is:

2π

Therefore, the combined function has period:

2π


Another Period Example

Consider:

f(x) = sin(2x) + cos(4x)

Periods:

sin(2x):

π

cos(4x):

π/2

Both functions return to their starting values after π.

Therefore, the combined function has period:

π

This is similar to finding a common multiple.


Graphical Interpretation

To understand:

y = f(x) + g(x)

imagine adding the vertical values of the two graphs at every x-coordinate.

If:

f(x) = 2

and:

g(x) = 3

then:

f(x) + g(x) = 5

If:

f(x) = 2

and:

g(x) = −3

then:

f(x) + g(x) = −1

The resulting graph depends on how the two component functions interact.


Constructive and Destructive Combination

When two waves are combined, their values may reinforce or oppose each other.

If both are positive at the same time, their sum becomes larger.

If both are negative, their combined displacement becomes more negative.

If one is positive and the other negative, they may partly or completely cancel.

This idea is closely connected to wave superposition.

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5

Composite Trigonometric Functions and Waves

One of the most important applications of combined trigonometric functions is wave modelling.

Real waves are often not perfect sine waves.

A complex wave can sometimes be represented as a combination such as:

y = sin(x) + 0.5sin(2x) + 0.25sin(3x)

Each term contributes a different frequency and amplitude.

Together, they produce a more complex waveform.

This idea is fundamental to:

  • sound
  • music
  • acoustics
  • communications
  • electronics
  • signal processing
  • optics
  • vibration analysis

Beats

An interesting pattern occurs when two waves have frequencies that are close but not identical.

For example:

sin(10x) + sin(11x)

The waves repeatedly move into and out of phase.

This creates alternating regions of stronger and weaker amplitude called beats.

Beats can be heard when two musical notes have slightly different frequencies.

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4

Product-to-Sum Identity

Products of trigonometric functions can sometimes be rewritten as sums.

For example:

2sin(A)cos(B) = sin(A + B) + sin(A − B)

If A = B = x:

2sin(x)cos(x) = sin(2x)

Therefore:

sin(x)cos(x) = (1/2)sin(2x)

This identity can make products easier to analyze.


Double-Angle Identities

Some common composite expressions can be simplified using double-angle identities.

Sine

sin(2x) = 2sin(x)cos(x)

Cosine

cos(2x) = cos²(x) − sin²(x)

Other equivalent forms are:

cos(2x) = 2cos²(x) − 1

and:

cos(2x) = 1 − 2sin²(x)

These identities allow us to move between different forms of the same expression.


Example: Simplifying with a Double-Angle Identity

Simplify:

4sin(x)cos(x)

Use:

2sin(x)cos(x) = sin(2x)

Then:

4sin(x)cos(x)

= 2[2sin(x)cos(x)]

= 2sin(2x)

This form may be easier to graph or solve.


Example: Simplifying a Squared Expression

Simplify:

2cos²(x) − 1

Using the double-angle identity:

cos(2x) = 2cos²(x) − 1

Therefore:

2cos²(x) − 1 = cos(2x)

A quadratic-looking trigonometric expression becomes a single cosine function.


Factoring Trigonometric Expressions

Ordinary algebraic techniques also apply.

Consider:

sin²(x) + sin(x)cos(x)

Both terms contain sin(x).

Factor:

sin(x)[sin(x) + cos(x)]

This may be useful when solving equations.


Solving a Combined Trigonometric Equation

Solve:

sin²(x) + sin(x)cos(x) = 0

Factor:

sin(x)[sin(x) + cos(x)] = 0

Therefore either:

sin(x) = 0

or:

sin(x) + cos(x) = 0

The second equation gives:

sin(x) = −cos(x)

Divide by cos(x), where appropriate:

tan(x) = −1

We can then solve each equation over the required domain.


Solving sin(x) + cos(x) = 0

Suppose:

0 ≤ x < 2π

We have:

sin(x) = −cos(x)

Therefore:

tan(x) = −1

Tangent is negative in Quadrants II and IV.

So:

x = 3π/4

and:

x = 7π/4

These are the solutions on the specified interval.


Solving Using a Combined Form

Suppose:

sin(x) + cos(x) = 1

Rewrite:

√2 sin(x + π/4) = 1

Divide:

sin(x + π/4) = 1/√2

= √2/2

This converts the original equation into a familiar trigonometric equation.

The combined form can therefore make equations much easier to solve.


Domain Restrictions

When simplifying composite trigonometric expressions, always check whether a denominator could equal zero.

For example:

sin(x)/cos(x)

can be simplified to:

tan(x)

but the original expression requires:

cos(x) ≠ 0

Therefore:

x ≠ π/2 + kπ

for integer k.

Simplification should not cause us to forget restrictions in the original expression.


Composite Functions and Domain

True function composition also requires us to think carefully about domain.

Consider:

arcsin(2x)

The input to arcsin must satisfy:

−1 ≤ 2x ≤ 1

Therefore:

−1/2 ≤ x ≤ 1/2

The domain of a composite function depends on whether the output of the inside function is allowed as an input to the outside function.


Example with an Inverse Function

Consider:

sin(arcsin(x))

For:

−1 ≤ x ≤ 1

arcsin(x) returns an angle whose sine is x.

Therefore:

sin(arcsin(x)) = x

For example:

sin(arcsin(0.6))

= 0.6

This is an example of a function and its inverse undoing each other.


But Order Still Matters

Now consider:

arcsin(sin(x))

It is tempting to say this always equals x.

It does not.

The inverse sine function returns values only within its principal range:

−π/2 ≤ arcsin(x) ≤ π/2

Therefore:

arcsin(sin(x)) = x

only for appropriate x-values within that range.

This is an important distinction in advanced trigonometry.


Graphing Composite Functions

When interpreting a composite or combined graph, ask:

  1. What are the component functions?
  2. What are their amplitudes?
  3. What are their periods?
  4. Are their frequencies the same?
  5. Are they in phase or shifted?
  6. Are they being added, subtracted, multiplied, or composed?
  7. Where do they reinforce one another?
  8. Where do they cancel?
  9. What is the period of the resulting function?
  10. Can the expression be simplified using an identity?

These questions help reveal the structure behind a complicated graph.

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5

Real-World Example: Sound

Suppose a simplified sound signal is:

S(t) = 3sin(200πt) + sin(400πt)

The signal contains two oscillations.

The first term has a larger amplitude.

The second term has a higher frequency.

When combined, the resulting waveform is more complex than either component alone.

This helps explain why musical instruments can produce complicated sounds even when they play a single perceived note.


Real-World Example: Ocean Waves

A water surface may experience several waves simultaneously.

A simplified model might be:

h(t) = 1.2sin(t) + 0.5sin(3t)

The first wave has the larger amplitude.

The second oscillates more rapidly.

At some times the waves reinforce each other.

At other times they partially cancel.

The observed water level is the combined result.


Real-World Example: Alternating Signals

Electrical signals can contain multiple sinusoidal components.

A simplified voltage model might be:

V(t) = 10sin(ωt) + 2sin(3ωt)

The first term is called the fundamental component.

The second has three times its frequency and is an example of a harmonic.

Analyzing these components helps engineers understand complex electrical signals.


Connections to Fourier Analysis

One of the most powerful ideas in advanced mathematics is that many complicated periodic functions can be represented approximately by adding sine and cosine functions.

A representation might look like:

f(x) = a₀ + a₁cos(x) + b₁sin(x) + a₂cos(2x) + b₂sin(2x) + ...

This idea leads to Fourier series.

Fourier methods are fundamental in:

  • audio processing
  • image processing
  • telecommunications
  • medical imaging
  • vibration analysis
  • astronomy
  • engineering
  • physics

A complicated signal can often be understood by examining the simpler sinusoidal components that make it up.


A Strategy for Composite Problems

When faced with a complicated trigonometric expression, do not immediately start calculating.

Instead:

Identify → Simplify → Evaluate → Interpret

Identify

Determine which trigonometric functions are present.

Simplify

Look for:

  • common factors
  • Pythagorean identities
  • quotient identities
  • reciprocal identities
  • double-angle identities
  • sum or difference identities

Evaluate

Substitute values only after simplifying when possible.

Interpret

If the problem involves a graph or real-world situation, explain what the result means.

This approach is usually more efficient and less error-prone.


Common Mistakes

Treating addition like multiplication

sin(x) + cos(x)

cannot simply become:

sin(2x)

Assuming sin(x)cos(x) = sin(x²)

These are completely different expressions.

Forgetting order in composition

sin(cos(x))

is generally not equal to:

cos(sin(x))

Evaluating the outside function first

For:

f(g(x))

evaluate g(x) first.

Forgetting identities

Expressions such as:

sin²(x) + cos²(x)

should immediately suggest:

1

Cancelling terms incorrectly

You may cancel common factors, not terms joined by addition or subtraction.

Ignoring domain restrictions

Expressions containing denominators may be undefined at certain values.

Mixing degrees and radians

Check the expected angle mode before evaluating numerically.

Assuming every sum of waves is a simple sine wave

Functions with different frequencies often produce more complex shapes.

Confusing amplitude with maximum value

A combined function may have a vertical shift, so amplitude and maximum value are not necessarily the same.

Assuming all composite functions are periodic

Composition does not automatically guarantee periodicity.

Ignoring graphical meaning

An expression may be easier to understand by examining how its component functions interact.


Key Terms

Composite function — A function formed by using the output of one function as the input of another.

Function composition — The process of applying one function to the result of another.

Combined function — A function formed by adding, subtracting, multiplying, or dividing functions.

Component function — One of the individual functions making up a combined expression.

Trigonometric identity — An equation involving trigonometric functions that is true wherever both sides are defined.

Pythagorean identity — An identity based on the relationship sin²(x) + cos²(x) = 1.

Quotient identity — An identity expressing tangent or cotangent as a quotient of sine and cosine.

Reciprocal identity — An identity connecting functions such as cosine and secant or sine and cosecant.

Double-angle identity — An identity involving an angle and twice that angle.

Product-to-sum identity — An identity that rewrites products of trigonometric functions as sums.

Exact value — A value expressed precisely rather than as a decimal approximation.

Period — The interval over which a periodic function repeats.

Frequency — The number of cycles completed per unit interval.

Amplitude — The maximum displacement from the midline of a sinusoidal function.

Phase — The position of a periodic function within its cycle.

Superposition — The combination of two or more waves by adding their displacements.

Constructive interference — Reinforcement that occurs when wave displacements combine in the same direction.

Destructive interference — Reduction that occurs when wave displacements oppose one another.

Beat — A repeating variation in amplitude caused by combining waves with similar frequencies.

Harmonic — A frequency that is an integer multiple of a fundamental frequency.

Fundamental frequency — The lowest main frequency in a periodic signal.

Auxiliary angle method — A method for rewriting a sin(x) + b cos(x) as one sinusoidal function.

Domain restriction — A value excluded because an expression or function is undefined there.

Inverse trigonometric function — A function such as arcsin, arccos, or arctan used to determine angles from trigonometric ratios.

Fourier series — A representation of a periodic function using a sum of sine and cosine terms.


Key Takeaways

  • Trigonometric functions can be added, subtracted, multiplied, divided, or composed.
  • A true composite function places one function inside another.
  • In f(g(x)), evaluate the inside function first.
  • Function composition is generally not commutative:

f(g(x)) ≠ g(f(x))

  • Exact trigonometric values can simplify calculations.
  • Identities allow complicated expressions to be rewritten in simpler forms.
  • One of the most important identities is:

sin²(x) + cos²(x) = 1

  • Tangent can be written as:

tan(x) = sin(x)/cos(x)

  • Products such as sin(x)cos(x) can be simplified using double-angle identities.
  • Algebraic techniques such as factoring still apply to trigonometric expressions.
  • Expressions of the form:

a sin(x) + b cos(x)

can be rewritten as a single sinusoidal function.

  • The resulting amplitude is:

√(a² + b²)

  • Functions with different frequencies can create complex periodic patterns.
  • The period of a combined function must allow all component functions to repeat.
  • Combined waves can reinforce or cancel one another.
  • This behaviour is related to constructive and destructive interference.
  • Waves with similar frequencies can produce beats.
  • Composite trigonometric models appear in sound, water waves, electronics, vibrations, and signal processing.
  • Domain restrictions must be preserved when simplifying expressions.
  • Inverse trigonometric compositions require particular care with domains and ranges.
  • Complicated periodic signals can often be understood as combinations of simpler sine and cosine waves.
  • This principle leads to Fourier analysis, one of the most important applications of trigonometric functions in science and engineering.

A useful strategy is:

Identify → Simplify → Evaluate → Interpret


Check Your Understanding

1. Evaluate:

sin(0) + cos(0)

2. Evaluate:

sin(π/2) + cos(π/2)

3. Evaluate:

2sin(π/6) + cos(π/6)

Give an exact answer.

4. Evaluate:

sin(π/4)cos(π/4)

5. Simplify:

sin²(x) + cos²(x)

6. Simplify:

1 − sin²(x)

7. Simplify:

1 − cos²(x)

8. Simplify:

sin(x)/cos(x)

9. Simplify:

cos(x)tan(x)

10. Simplify:

cos(x)sec(x)

11. Simplify:

2sin(x)cos(x)

12. Simplify:

2cos²(x) − 1

13. If:

f(x) = sin(x)

and:

g(x) = 2x

find:

f(g(x))

14. For the same functions, find:

g(f(x))

15. Explain why your answers to Questions 13 and 14 are different.

16. Evaluate:

sin(cos(0))

approximately.

17. Evaluate:

cos(sin(0))

18. Simplify by factoring:

sin²(x) + sin(x)cos(x)

19. Solve:

sin(x) + cos(x) = 0

for:

0 ≤ x < 2π

20. What is the amplitude of:

3sin(x) + 4cos(x)

after it is rewritten as one sinusoidal function?

21. Rewrite:

sin(x) + cos(x)

as one sinusoidal function.

22. Find the period of:

sin(x) + sin(2x)

23. Find the period of:

sin(2x) + cos(4x)

24. Explain why:

sin(x) + sin(2x)

cannot normally be rewritten as a single basic sine wave with one frequency.

25. Explain what constructive interference means.

26. Explain what destructive interference means.

27. What are beats, and why can they occur when two waves are combined?

28. Explain why domain restrictions must still be considered after simplifying a trigonometric expression.

29. Describe one real-world situation in which several trigonometric functions might be combined.

30. Challenge: Consider:

f(x) = 3sin(x) + 4cos(x)

a. Find the amplitude when the function is rewritten as one sinusoidal function.
b. Find the phase angle φ if the function is written as 5sin(x + φ).
c. Write the resulting single sinusoidal function.
d. State its maximum value.
e. State its minimum value.
f. State its period.
g. Explain why combining the original sine and cosine functions does not change the period in this case.
h. Explain how the graph of the combined function differs from the graph of y = sin(x).
i. Give one real-world situation where combining sinusoidal functions would be useful.
j. Explain how this example connects to the idea of wave superposition.

 
 
 

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.

Inverse Trigonometric Functions

Trigonometric functions allow us to find a ratio or coordinate when we know an angle. Inverse trigonometric functions allow us to work in the opposite direction: they help us find an angle when we know a trigonometric value.

For example:

sin(30°) = 0.5

Therefore:

sin⁻¹(0.5) = 30°

Similarly:

cos(60°) = 0.5

so:

cos⁻¹(0.5) = 60°

Inverse trigonometric functions are especially important in geometry, physics, engineering, navigation, surveying, waves, and mathematical modelling.

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5

What Does "Inverse" Mean?

An inverse function reverses the action of another function.

Consider:

sin(30°) = 0.5

The sine function takes:

angle → ratio

The inverse sine function takes:

ratio → angle

So:

sin⁻¹(0.5) = 30°

This relationship can be thought of as:

30° → sin → 0.5

and:

0.5 → sin⁻¹ → 30°

The same idea applies to cosine and tangent.


The Three Main Inverse Trigonometric Functions

The three most common inverse trigonometric functions are:

Inverse Sine

sin⁻¹(x)

also written:

arcsin(x)

Inverse Cosine

cos⁻¹(x)

also written:

arccos(x)

Inverse Tangent

tan⁻¹(x)

also written:

arctan(x)

The "arc" notation is often useful because it avoids confusion with exponents.


Important: sin⁻¹(x) Does Not Mean 1/sin(x)

This is one of the most important distinctions in this topic.

sin⁻¹(x) means:

inverse sine

It does not mean:

1/sin(x)

The reciprocal of sine is:

csc(x) = 1/sin(x)

Similarly:

cos⁻¹(x) means inverse cosine.

But:

1/cos(x) = sec(x)

And:

tan⁻¹(x) means inverse tangent.

But:

1/tan(x) = cot(x)


Why Do We Need Principal Values?

There is a problem with defining inverse trigonometric functions.

Trigonometric functions repeat.

For example:

sin(30°) = 0.5

but also:

sin(150°) = 0.5

and:

sin(390°) = 0.5

and infinitely many other angles have the same sine value.

So what should:

sin⁻¹(0.5)

equal?

An inverse function must give one output for each input.

Therefore, we restrict the output of inverse trigonometric functions to specific intervals called principal-value ranges.

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5

Principal Values

The principal value is the single angle selected by an inverse trigonometric function.

The standard principal ranges are:

Function Principal Range in Radians Principal Range in Degrees
arcsin(x) −π/2 ≤ y ≤ π/2 −90° ≤ y ≤ 90°
arccos(x) 0 ≤ y ≤ π 0° ≤ y ≤ 180°
arctan(x) −π/2 < y < π/2 −90° < y < 90°

These ranges must be remembered or understood because they determine which answer an inverse function returns.


Principal Range of arcsin

The inverse sine function returns angles in:

−π/2 ≤ y ≤ π/2

or:

−90° ≤ y ≤ 90°

This corresponds primarily to Quadrants I and IV, including the boundary angles.

For example:

arcsin(1/2) = 30°

not 150°.

Even though:

sin(150°) = 1/2

150° is outside the principal range of arcsin.

Therefore:

arcsin(1/2) = 30°


Principal Range of arccos

The inverse cosine function returns angles in:

0 ≤ y ≤ π

or:

0° ≤ y ≤ 180°

This covers Quadrants I and II.

For example:

arccos(−1/2) = 120°

because:

cos(120°) = −1/2

and 120° lies within the principal range.


Principal Range of arctan

The inverse tangent function returns angles in:

−π/2 < y < π/2

or:

−90° < y < 90°

For example:

arctan(1) = 45°

and:

arctan(−1) = −45°

Notice that ±90° are not included because tangent is undefined at these angles.


Exact Principal Values

Some inverse trigonometric expressions can be evaluated exactly.

Inverse Sine

arcsin(0) = 0

arcsin(1/2) = π/6

arcsin(√2/2) = π/4

arcsin(√3/2) = π/3

arcsin(1) = π/2

Inverse Cosine

arccos(1) = 0

arccos(√3/2) = π/6

arccos(√2/2) = π/4

arccos(1/2) = π/3

arccos(0) = π/2

Inverse Tangent

arctan(0) = 0

arctan(√3/3) = π/6

arctan(1) = π/4

arctan(√3) = π/3

These values come directly from familiar trigonometric angles.


Worked Example: Inverse Sine

Evaluate:

arcsin(√3/2)

Ask:

Which angle in the principal range has sine √3/2?

We know:

sin(π/3) = √3/2

Therefore:

arcsin(√3/2) = π/3

or:

60°


Worked Example: Inverse Cosine

Evaluate:

arccos(−√2/2)

We need an angle between:

0 and π

whose cosine is negative.

Cosine is negative in Quadrant II within this range.

The reference angle is:

π/4

Therefore:

arccos(−√2/2) = 3π/4

or:

135°


Worked Example: Inverse Tangent

Evaluate:

arctan(−√3)

We need an angle between:

−π/2 and π/2

with tangent −√3.

The reference angle is:

π/3

Within the principal range, the negative angle is:

−π/3

Therefore:

arctan(−√3) = −π/3


Domain of Inverse Sine

Since ordinary sine produces values only between −1 and 1:

−1 ≤ sin(x) ≤ 1

the input of arcsin must satisfy:

−1 ≤ x ≤ 1

Therefore, the domain of:

y = arcsin(x)

is:

[−1, 1]

For example:

arcsin(0.7)

exists.

But:

arcsin(2)

has no real value.

There is no real angle whose sine is 2.


Domain of Inverse Cosine

Cosine also produces values only between −1 and 1.

Therefore:

−1 ≤ x ≤ 1

is the domain of:

arccos(x)

For example:

arccos(−0.4)

has a real value.

But:

arccos(1.5)

does not have a real value.


Domain of Inverse Tangent

Tangent can produce any real number.

Therefore:

arctan(x)

has domain:

all real numbers

So expressions such as:

arctan(5)

arctan(100)

arctan(−250)

are all defined.

However, the resulting angles always remain between:

−π/2 and π/2

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5

Why Restrictions Are Necessary

The ordinary sine function is not one-to-one over all real numbers.

For example:

sin(30°) = 1/2

sin(150°) = 1/2

Two different inputs produce the same output.

That prevents the unrestricted sine function from having an inverse that is itself a function.

To create arcsin, we restrict sine to:

−90° ≤ x ≤ 90°

Over this interval, sine is one-to-one.

Then we can reflect this restricted graph across:

y = x

to obtain the graph of arcsin.


Inverse Functions as Reflections

A function and its inverse have graphs that are reflections of each other across the line:

y = x

For example, restricted:

y = sin(x)

and:

y = arcsin(x)

are reflections across y = x.

Coordinates switch positions.

If:

sin(a) = b

then:

arcsin(b) = a

So a point:

(a, b)

on the restricted sine graph corresponds to:

(b, a)

on the arcsin graph.

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6

The Graph of arcsin(x)

The graph:

y = arcsin(x)

has:

Domain:

−1 ≤ x ≤ 1

Range:

−π/2 ≤ y ≤ π/2

It is increasing throughout its domain.

Important points include:

(−1, −π/2)

(0, 0)

(1, π/2)


The Graph of arccos(x)

The graph:

y = arccos(x)

has:

Domain:

−1 ≤ x ≤ 1

Range:

0 ≤ y ≤ π

Unlike arcsin, arccos is decreasing.

Important points include:

(−1, π)

(0, π/2)

(1, 0)


The Graph of arctan(x)

The graph:

y = arctan(x)

has:

Domain:

all real numbers

Range:

−π/2 < y < π/2

The graph approaches:

y = π/2

and:

y = −π/2

but never reaches them.

These are horizontal asymptotes.


Calculator Mode Matters

When evaluating inverse trigonometric functions with a calculator, check whether the calculator is in:

  • degree mode
  • radian mode

For example:

arcsin(0.5)

in degree mode gives:

30°

In radian mode it gives approximately:

0.524

These are the same angle because:

π/6 ≈ 0.524 radians

A correct calculation in the wrong mode may appear to give the wrong answer.


Using Inverse Trigonometry to Solve Equations

Suppose:

sin(x) = 0.7

We can apply inverse sine:

x = arcsin(0.7)

Using a calculator:

x ≈ 44.4°

But this is only the principal value.

If we are solving a trigonometric equation over a larger interval, there may be additional solutions.

This distinction is extremely important.


Principal Value vs All Solutions

Suppose:

sin(x) = 0.5

Then:

arcsin(0.5) = 30°

This gives the principal value.

But if the problem asks for all solutions between:

0° ≤ x < 360°

then sine is positive in Quadrants I and II.

Therefore:

x = 30°

or:

x = 150°

The inverse function gives a starting angle, not necessarily every solution to a periodic trigonometric equation.

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5

Solving a Cosine Equation

Solve:

cos(x) = −0.6

for:

0° ≤ x < 360°

First find the principal angle:

x = arccos(−0.6)

≈ 126.9°

Cosine is negative in Quadrants II and III.

The second solution is:

360° − 126.9°

= 233.1°

Therefore:

x ≈ 126.9°, 233.1°


Solving a Tangent Equation

Solve:

tan(x) = 2

for:

0° ≤ x < 360°

Find the principal value:

x = arctan(2)

≈ 63.4°

Tangent is positive in Quadrants I and III.

Therefore, the second solution is:

63.4° + 180°

= 243.4°

Solutions:

x ≈ 63.4°, 243.4°


General Solutions

Because trigonometric functions are periodic, equations can have infinitely many solutions.

For:

sin(x) = a

if:

α = arcsin(a)

then solutions can be represented using:

x = α + 2πn

or:

x = π − α + 2πn

where n is any integer.

For cosine:

cos(x) = a

if:

α = arccos(a)

then:

x = ±α + 2πn

For tangent:

tan(x) = a

if:

α = arctan(a)

then:

x = α + πn

These forms describe infinitely many repeating solutions.


Solving Equations with Coefficients

Consider:

2sin(x) = 1

First isolate the trigonometric function:

sin(x) = 1/2

Now apply inverse sine:

arcsin(1/2) = 30°

The principal angle is:

30°

If:

0° ≤ x < 360°

then the second solution is:

150°

Therefore:

x = 30°, 150°


Solving an Equation with a Shift

Consider:

cos(x − 20°) = 0.5

Let:

u = x − 20°

Then:

cos(u) = 0.5

Over one full cycle:

u = 60°

or:

u = 300°

Now substitute back.

x − 20° = 60°

x = 80°

or:

x − 20° = 300°

x = 320°

Always check the requested interval when solving transformed trigonometric equations.


Inverse Trigonometry and Right Triangles

One of the most common real-world uses of inverse trigonometric functions is finding an unknown angle in a right triangle.

Recall:

sin(θ) = opposite/hypotenuse

cos(θ) = adjacent/hypotenuse

tan(θ) = opposite/adjacent

If the side lengths are known, inverse functions allow us to determine θ.

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6

Worked Example: Finding an Angle

A right triangle has:

opposite = 6 cm

adjacent = 8 cm

Use tangent:

tan(θ) = 6/8

= 0.75

Apply inverse tangent:

θ = arctan(0.75)

θ ≈ 36.9°

So the angle is approximately:

36.9°


Choosing the Correct Inverse Function

The side information determines which function to use.

Opposite and Hypotenuse

Use:

θ = arcsin(opposite/hypotenuse)

Adjacent and Hypotenuse

Use:

θ = arccos(adjacent/hypotenuse)

Opposite and Adjacent

Use:

θ = arctan(opposite/adjacent)

A useful strategy is:

  1. label the sides relative to the unknown angle
  2. choose the appropriate ratio
  3. calculate the ratio
  4. apply the corresponding inverse function

Real-World Example: Angle of Elevation

Suppose you stand 40 m from the base of a building.

The building is 30 m high.

Ignoring eye height, let θ be the angle of elevation to the top.

Then:

tan(θ) = 30/40

= 0.75

Therefore:

θ = arctan(0.75)

≈ 36.9°

Inverse tangent converts the measured ratio into an angle.


Real-World Example: Ramp Angle

A ramp rises 1.2 m over a horizontal distance of 8 m.

Then:

tan(θ) = 1.2/8

= 0.15

Therefore:

θ = arctan(0.15)

≈ 8.5°

This kind of calculation is useful in construction and engineering.


Real-World Example: Direction of Motion

Suppose an object moves:

12 m east

and:

5 m north.

Its direction relative to east can be found using:

tan(θ) = 5/12

Therefore:

θ = arctan(5/12)

≈ 22.6°

So the displacement direction is approximately:

22.6° north of east

Inverse trigonometry is extremely useful when working with vectors.

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5

Inverse Trigonometry and Vectors

Suppose a vector has components:

Vₓ = 8

Vᵧ = 6

Its magnitude is:

V = √(8² + 6²)

= √100

= 10

Its direction can be found using:

tan(θ) = Vᵧ/Vₓ

= 6/8

Therefore:

θ = arctan(6/8)

≈ 36.9°

The inverse tangent converts component information into directional information.


Quadrants Matter with Vectors

There is an important complication.

Suppose:

Vₓ = −8

Vᵧ = 6

If we simply calculate:

arctan(6/−8)

we obtain a negative principal angle.

But the vector actually lies in Quadrant II.

Therefore, when finding vector directions, we must examine the signs of the components and determine the correct quadrant.

Many programming languages and calculators provide a function often called atan2(y, x) that uses both component signs to determine the appropriate direction.


Inverse Functions in Modelling

Inverse trigonometric functions appear whenever a model gives us a ratio and we need to recover an angle.

Applications include:

  • surveying
  • navigation
  • astronomy
  • robotics
  • engineering
  • computer graphics
  • architecture
  • physics
  • satellite positioning
  • slope measurement

In many cases, sensors measure distances or components first, and inverse trigonometry converts those measurements into angles.


Example: Surveying

A surveyor measures:

horizontal distance = 120 m

vertical rise = 18 m

The angle of elevation is:

tan(θ) = 18/120

= 0.15

Therefore:

θ = arctan(0.15)

≈ 8.5°

This allows geometric measurements to be converted into useful directional information.


Inverse Trigonometry and Slopes

Recall that:

slope = rise/run

For an inclined line:

tan(θ) = rise/run

Therefore:

tan(θ) = slope

and:

θ = arctan(slope)

This creates an important connection between algebra and trigonometry.

For example, if:

slope = 0.5

then:

θ = arctan(0.5)

≈ 26.6°

So the line forms an angle of approximately 26.6° with the positive horizontal axis, subject to the line's direction and quadrant.


Example: Road Grade

Suppose a road has a grade of:

10%

This means approximately:

rise/run = 0.10

Therefore:

tan(θ) = 0.10

θ = arctan(0.10)

≈ 5.7°

A 10% grade does not mean the road is inclined at 10°.

This is an important real-world distinction.


Compositions with Inverse Functions

Consider:

sin(arcsin(x))

For:

−1 ≤ x ≤ 1

the inverse sine produces an angle whose sine is x.

Therefore:

sin(arcsin(x)) = x

Similarly:

cos(arccos(x)) = x

for:

−1 ≤ x ≤ 1

And:

tan(arctan(x)) = x

for every real x.


Reversing the Order Is More Complicated

It may seem that:

arcsin(sin(x)) = x

for every x.

But this is not true.

Remember that arcsin can only return values in:

−π/2 ≤ y ≤ π/2

For example:

sin(5π/6) = 1/2

Then:

arcsin(sin(5π/6))

= arcsin(1/2)

= π/6

not:

5π/6

The inverse function returns the principal value.


Another Composition Example

Consider:

arccos(cos(4π/3))

First:

cos(4π/3) = −1/2

Then:

arccos(−1/2) = 2π/3

not 4π/3.

Why?

Because the principal range of arccos is:

0 ≤ y ≤ π

and 4π/3 lies outside this range.


Graphical Interpretation of Principal Values

The restricted domains used to define inverse functions explain principal values.

For sine, we retain the section from:

−π/2 to π/2

For cosine:

0 to π

For tangent:

−π/2 to π/2

These restricted sections are one-to-one.

Their inverses therefore pass the vertical line test and behave as proper functions.

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5

Checking an Inverse-Trig Answer

When evaluating an inverse trigonometric expression, use this process:

Check the Input

Is the input in the domain?

For arcsin and arccos:

−1 ≤ input ≤ 1

Determine the Reference Angle

Use known exact values or a calculator.

Check the Sign

Is the trigonometric value positive or negative?

Check the Principal Range

Does your angle lie in the correct output range?

Check the Calculator Mode

Should the answer be in degrees or radians?

This method prevents many common errors.


Solving vs Evaluating

It is important to distinguish these two tasks.

Evaluate

arcsin(1/2)

asks for one principal value:

π/6

Solve

sin(x) = 1/2

may ask for multiple values of x.

For:

0 ≤ x < 2π

the solutions are:

x = π/6, 5π/6

So:

inverse function → one principal value

while:

trigonometric equation → potentially many solutions


Common Mistakes

Thinking sin⁻¹(x) means 1/sin(x)

It means inverse sine.

The reciprocal is csc(x).

Giving every possible angle when evaluating an inverse function

An inverse function returns a principal value.

Giving only the principal value when solving an equation

A trigonometric equation may have additional solutions.

Forgetting principal ranges

arcsin, arccos, and arctan return angles from different intervals.

Using arcsin with an input greater than 1

For real numbers:

arcsin(1.5)

is undefined.

Using arccos with an input below −1

For real numbers:

arccos(−2)

is undefined.

Forgetting calculator mode

30° and approximately 0.524 radians represent the same angle.

Assuming arcsin(sin(x)) always equals x

This is only guaranteed when x lies within the appropriate principal range.

Ignoring quadrants when solving equations

The principal angle may not be the only solution.

Ignoring quadrants when finding vector directions

The signs of the vector components determine the actual quadrant.

Confusing grade with angle

A 10% slope does not mean a 10° angle.

Rounding too early

Keep several decimal places during calculations and round only at the end.


Key Terms

Inverse function — A function that reverses the action of another function.

Inverse trigonometric function — A function used to determine an angle from a trigonometric value.

Inverse sine — The function arcsin(x) or sin⁻¹(x).

Inverse cosine — The function arccos(x) or cos⁻¹(x).

Inverse tangent — The function arctan(x) or tan⁻¹(x).

Principal value — The single output angle selected by an inverse trigonometric function.

Principal range — The restricted range from which an inverse trigonometric function returns its principal value.

arcsin — Alternative notation for inverse sine.

arccos — Alternative notation for inverse cosine.

arctan — Alternative notation for inverse tangent.

One-to-one function — A function in which different inputs produce different outputs.

Restricted domain — A limited part of a function's domain selected so that an inverse can be defined.

Domain — The set of permitted input values.

Range — The set of possible output values.

Reference angle — The positive acute angle associated with a trigonometric value.

Periodic function — A function whose values repeat at regular intervals.

General solution — An expression representing all solutions of an equation.

Angle of elevation — The angle measured upward from a horizontal line of sight.

Angle of depression — The angle measured downward from a horizontal line of sight.

Vector component — The part of a vector acting along a particular direction or axis.

Slope — Vertical change divided by horizontal change.

Road grade — Slope expressed as a percentage.

Radian — An angle unit based on the radius of a circle.

Degree — An angle unit in which a complete revolution contains 360°.

atan2 — A computational form of inverse tangent that uses two coordinates or components to identify the correct quadrant.

Horizontal asymptote — A horizontal line that a graph approaches without necessarily reaching.


Key Takeaways

  • Trigonometric functions convert angles into ratios or coordinates.
  • Inverse trigonometric functions convert trigonometric values back into angles.
  • The three main inverse functions are arcsin, arccos, and arctan.
  • sin⁻¹(x) means inverse sine, not 1/sin(x).
  • The reciprocal of sine is cosecant.
  • Trigonometric functions repeat, so they must be restricted before inverse functions can be defined.
  • Inverse functions return principal values.
  • arcsin returns values from −π/2 to π/2.
  • arccos returns values from 0 to π.
  • arctan returns values between −π/2 and π/2.
  • arcsin and arccos accept real inputs only between −1 and 1.
  • arctan accepts every real number.
  • A function and its inverse are reflections across y = x.
  • Calculator mode must match the required angle unit.
  • Evaluating an inverse function gives one principal value.
  • Solving a trigonometric equation may produce multiple solutions.
  • Periodicity explains why trigonometric equations can have infinitely many solutions.
  • Inverse trigonometry is especially useful for finding unknown angles.
  • Right-triangle ratios can be reversed using inverse functions.
  • Inverse tangent can convert slope into an angle of inclination.
  • Vector components can be used with inverse tangent to determine direction.
  • Quadrant information must be considered when interpreting inverse tangent.
  • sin(arcsin(x)) = x for −1 ≤ x ≤ 1.
  • arcsin(sin(x)) does not necessarily equal x because arcsin must return a principal value.
  • Inverse trigonometric functions are widely used in physics, engineering, surveying, navigation, robotics, and modelling.

A useful way to remember the basic purpose is:

Trig: angle → ratio

Inverse trig: ratio → angle


Check Your Understanding

1. What does an inverse trigonometric function determine?

2. Explain why sin⁻¹(x) does not mean 1/sin(x).

3. Evaluate:

arcsin(1/2)

4. Evaluate:

arccos(1/2)

5. Evaluate:

arctan(1)

6. Evaluate:

arcsin(−1)

7. Evaluate:

arccos(−1)

8. Evaluate:

arctan(−√3)

9. State the principal range of arcsin in radians.

10. State the principal range of arccos in radians.

11. State the principal range of arctan in radians.

12. Explain why:

arcsin(1/2) = π/6

rather than 5π/6.

13. Does:

arcsin(1.4)

have a real value? Explain.

14. Does:

arctan(20)

have a real value? Explain.

15. Solve:

sin(x) = 1/2

for:

0° ≤ x < 360°

16. Solve:

cos(x) = −1/2

for:

0° ≤ x < 360°

17. Solve:

tan(x) = 1

for:

0° ≤ x < 360°

18. Explain the difference between evaluating:

arcsin(1/2)

and solving:

sin(x) = 1/2

19. A right triangle has opposite side 8 cm and adjacent side 15 cm. Calculate the angle between the adjacent side and hypotenuse.

20. A ladder reaches 6 m up a wall and its base is 2.5 m from the wall. Calculate its angle with the ground.

21. A hill rises 35 m over a horizontal distance of 200 m. Calculate its angle of inclination.

22. A vector has components:

Vₓ = 12

Vᵧ = 5

Calculate its direction relative to the positive x-axis.

23. Explain why vector components must be checked for their signs when using inverse tangent.

24. A road has a 15% grade. Estimate its angle of inclination.

25. Simplify:

sin(arcsin(x))

and state the appropriate domain.

26. Evaluate:

arcsin(sin(5π/6))

27. Explain why the answer to Question 26 is not 5π/6.

28. Evaluate:

arccos(cos(4π/3))

29. Explain graphically why trigonometric functions require restricted domains before inverse functions can be defined.

30. Challenge: A drone is located 240 m horizontally from an observer and 180 m above the observer's level.

a. Draw or imagine the right triangle representing the situation.
b. Identify the opposite and adjacent sides relative to the angle of elevation.
c. Write a tangent equation for the angle θ.
d. Use inverse tangent to calculate θ.
e. Calculate the straight-line distance from the observer to the drone.
f. Explain why arctan is appropriate for determining the angle.
g. Explain what would happen to θ if the drone maintained the same height but moved farther horizontally away.
h. Explain what would happen to θ if the drone moved vertically upward while remaining at the same horizontal distance.
i. Describe how inverse trigonometry could be used by a tracking or navigation system.
j. Explain the difference between the principal value returned by arctan and the need to consider quadrants in a more general two-dimensional vector problem.

 
 
 

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.

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5

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.

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5

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
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5

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

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5

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.

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5

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 calon 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

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5

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.

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5

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.

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6

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.