Transformations of Trigonometric Graphs (SQA National 5 Maths): Revision Note

Exam code: X847 75

Roger B

Written by: Roger B

Reviewed by: Dan Finlay

Updated on

Amplitude, vertical translation, multiple angle & phase angle

What are transformations of trigonometric graphs?

  • You should be familiar with the basic trigonometric graphs for sin, cos and tan

  • There are four ways of transforming these graphs that could appear in an exam question:

    • Changing the amplitude (also known as a vertical stretch)

    • Vertical translation (i.e., shifting the entire graph up or down)

    • Using a multiple angle (also known as a horizontal stretch)

    • Using a phase angle (also known as a horizontal translation, i.e. shifting the entire graph to the left or right)

Examiner Tips and Tricks

On the exam, transformation questions are usually only asked about sine and cosine graphs.

What is a change of amplitude of a trigonometric graph?

  • A change of amplitude of a trigonometric graph is of the form  asinx or  acosx

  • The graph of  asinx is similar to the graph of sinx

    • It has the same 'wave' shape

    • It still has a period of 360° (i.e. it repeats every 360°)

    • However its amplitude changes to a

      • I.e. instead of oscillating between heights of 1 and -1, it oscillates between heights of a and -a

      • It has been stretched vertically

    • It goes through the origin (0, 0)

      • Then every 90° it cycles through the heights a, 0, -a, 0, ...

  • The graph of  acosx is similar to the graph of cosx

    • It has the same 'wave' shape

    • It still has a period of 360° (i.e. it repeats every 360°)

    • However its amplitude changes to a

      • I.e. instead of oscillating between heights of 1 and -1, it oscillates between heights of a and -a

      • It has been stretched vertically

    • It goes through the point (0, a) on the y-axis

      • Then every 90° it cycles through the heights 0, -a, 0, a, ...

What is a vertical translation of a trigonometric graph?

  • A vertical translation of a trigonometric graph is of the form sinx+c or cosx+c

    • Note that the '+c' is outside of the trigonometric function

    • I.e. sinx+c is the same as (sinx)+c; it is not the same as sin(x+c)

      • sin(x+c) is an example of a phase angle, not a vertical translation

    • sinx+c can also be written as c+sinx

  • The graph of sinx+c is similar to the graph of sinx

    • It has the same 'wave' shape

    • It still has a period of 360° (i.e. it repeats every 360°)

    • Its amplitude is still 1

      • I.e. it still oscillates between 1 above and 1 below its 'middle line'

    • However its middle line moves from y=0 (the x-axis) to y=c

      • It oscillates between heights of c+1 and c-1

      • It has been translated (i.e. shifted) by |c| units vertically

        • If c is positive then it is shifted up

        • If c is negative then it is shifted down

    • It goes through the point (0, c) on the y-axis

      • Then every 90° it cycles through the heights c+1, c, c-1, c, ...

  • The graph of cosx+c is similar to the graph of cosx

    • It has the same 'wave' shape

    • It still has a period of 360° (i.e. it repeats every 360°)

    • Its amplitude is still 1

      • I.e. it still oscillates between 1 above and 1 below its 'middle line'

    • However its middle line moves from y=0 (the x-axis) to y=c

      • It oscillates between heights of b+1 and b-1

      • It has been translated (i.e. shifted) by |c| units vertically

        • If c is positive then it is shifted up

        • If c is negative then it is shifted down

    • It goes through the point (0, c+1) on the y-axis

      • Then every 90° it cycles through the heights c, c-1, c, c+1, ...

What is a multiple angle with a trigonometric graph?

  • A multiple angle with a trigonometric graph is of the form sinbx or cosbx

    • These could also be written with brackets as sin(bx) or cos(bx)

    • x is multiplied by b before it is put into sin or cos

  • The graph of sinbx is similar to the graph of sinx

    • It has the same 'wave' shape

    • Its amplitude is still 1 (i.e. it still oscillates between heights of 1 and -1)

    • However its period changes to (360b)° (i.e. it repeats every 360b degrees)

      • It has been stretched horizontally

        • If b>1 then it is 'squished in' (more complete cycles fit into 360°)

        • If 0<b<1 then its is 'stretched out' (it takes more than 360° to complete one full cycle)

    • It goes through the origin (0, 0)

      • Then every (360b)° it cycles through the heights 1, 0, -1, 0, ...

  • The graph of cosbx is similar to the graph of sinx

    • It has the same 'wave' shape

    • Its amplitude is still 1 (i.e. it still oscillates between heights of 1 and -1)

    • However its period changes to (360b)° (i.e. it repeats every 360b degrees)

      • It has been stretched horizontally

        • If b>1 then it is 'squished in' (more complete cycles fit into 360°)

        • If 0<b<1 then its is 'stretched out' (it takes more than 360° to complete one full cycle)

    • It goes through the point (0, 1) on the y-axis

      • Then every (360b)° it cycles through the heights 0, -1, 0, 1, ...

What is a phase angle with a trigonometric graph?

  • A phase angle with a trigonometric graph is of the form sin(x+d) or cos(x+d)

    • d is added to x before it is put into sin or cos

  • The graph of sin(x+d) is similar to the graph of sinx

    • It has the same 'wave' shape

    • It still has a period of 360° (i.e. it repeats every 360°)

    • Its amplitude is still 1 ((i.e. it still oscillates between heights of 1 and -1)

    • However its 'starting point' moves from the origin (0, 0) to (-d, 0)

      • Note the negative sign in front of the d

      • It has been translated (i.e. shifted) by |d| units horizontally

        • If d is positive then it is shifted left

        • If d is negative then it is shifted right

    • It 'starts' at the point (-d, 0) on the x-axis

      • Then every 90° it cycles through the heights 1, 0, -1, 0, ...

        • I.e. through the points (-d+90, 1), (-d+180, 0), (-d+270, -1), (-d+360, 0), ...

  • The graph of cos(x+d) is similar to the graph of cosx

    • It has the same 'wave' shape

    • It still has a period of 360° (i.e. it repeats every 360°)

    • Its amplitude is still 1 ((i.e. it still oscillates between heights of 1 and -1)

    • However its 'starting point' moves from the origin (0, 0) to (-d, 0)

      • Note the negative sign in front of the d

      • It has been translated (i.e. shifted) by |d| units horizontally

        • If d is positive then it is shifted left

        • If d is negative then it is shifted right

    • It 'starts' at the point (-a, 1) on the x-axis

      • Then every 90° it cycles through the heights 0, -1, 0, 1, ...

        • I.e. through the points (-d+90, 0), (-d+180, -1), (-d+270, 0), (-d+360, 1), ...

Summary of single transformations

Function

Type

Period

Amplitude

Roots

1st turning points

 asinx

change of amplitude

360°

a

0°, 180°, 360°, ...

(90°, a) maximum
(270°, -a) minimum

 acosx

change of amplitude

360°

a

90°, 270°, 450°, ...

(0°, a) maximum
(180°, -a) minimum

sinx+c

vertical translation

360°

1

(depends on value of c; there may be none)

(90°, c+1) maximum
(270°, c-1) minimum

cosx+c

vertical translation

360°

1

(depends on value of c; there may be none)

(0°, c+1) maximum
(180°, c-1) minimum

sin(bx)

multiple angle

(360b)°

1

0°, (180b)°, (360b)°, ...

((90b)°, 1) maximum
((270b)°, 1) minimum

cos(bx)

multiple angle

(360b)°

1

(90b)°, (270b)°, (450b)°, ...

(0°, 1) maximum

((180b)°, 1) minimum

sin(x+d)

phase angle

360°

1

-d°, (180-d)°, (360-d)°, ...

((90-d)°, 1) maximum
((270-d)°, -1) minimum

cos(x+d)

phase angle

360°

1

(90-d)°, (270-d)°, (450-d)°, ...

(-d°, 1) maximum
((180-d)°, -1) minimum

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Roger B

Author: Roger B

Expertise: Development Editor

Roger's teaching experience stretches all the way back to 1992, and in that time he has taught students at all levels between Year 7 and university undergraduate. Having conducted and published postgraduate research into the mathematical theory behind quantum computing, he is more than confident in dealing with mathematics at any level the exam boards might throw at you.

Dan Finlay

Reviewer: Dan Finlay

Expertise: Portfolio Lead

Dan graduated from the University of Oxford with a First class degree in mathematics. As well as teaching maths for over 8 years, Dan has marked a range of exams for Edexcel, tutored students and taught A Level Accounting. Dan has a keen interest in statistics and probability and their real-life applications.