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Review Sheet for Sinusoidal Functions | MTH 112, Study notes of Mathematics

Material Type: Notes; Class: Elementary Functions; Subject: Math; University: Portland Community College; Term: Unknown 1989;

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Pre 2010

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Haberman MTH 112
Section I: Periodic Functions and Trigonometry
Module 5: Sinusoidal Functions
DEFINITION: A sinusoidal function is function f of the form
(
)
sin ( ) , , , , .yA Bth kABhk=−+ R
NOTE 1: Recall from Module 3 that
(
)
2
cos( ) sintt
π
=+
(i.e., since the cosine function is a
transformation of the sine function). Therefore, we can write any function of the form
in the form given in the definition of a sinusoidal function.
Thus, functions of the form
()
cos ( )yA Bth k=−+
(
)
cos ( )yA Bth k
=
−+
are also sinusoidal functions.
NOTE 2: Based what we know about graph transformations (which are studied in the previous
course), we should recognize that sinusoidal functions are transformations of the
function . Below is a summary of what is studied in the previous course
about graph transformations:
sin( )y=t
SUMMARY OF GRAPH TRANSFORMATIONS
Suppose that f and g are functions such that
(
)
() ( )gt A f Bt h k
=
⋅−+
and
. In order to transform the graph of the function f into the graph of g
,,,ABhkR
1st: horizontally stretch/compress the graph of f by a factor of 1
B and, if , reflect
it about the y-axis.
0B<
2nd: shift the graph horizontally h units (shift right if h is positive and left if h is
negative).
3nd: vertically stretch/compress the graph by a factor of
A
and, if 0A
<
, reflect it about
the t-axis.
4th: shift the graph vertically k units (shift up if k is positive and down if k is
negative).
(The order in which these transformations are performed matters.)
Examples 1 – 4 (below) will provide a review of the graph transformations as well as an
investigation of the affect of the constants A, B, h, and k on the period, midline, amplitude,
and horizontal shift of a sinusoidal function. You may want to follow along by graphing the
functions on your graphing calculator. Don’t forget to change the mode of the calculator to
the radian setting under the heading angle.
pf3
pf4
pf5
pf8

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Haberman MTH 112

Section I: Periodic Functions and Trigonometry

Module 5: Sinusoidal Functions

DEFINITION: A sinusoidal function is function f of the form

y = A sin ( B t ( − h ) )+ k , A B h k , , , ∈ R.

NOTE 1: Recall from Module 3 that ( )

2

cos( ) t sin t

π

= + (i.e., since the cosine function is a

transformation of the sine function). Therefore, we can write any function of the form

in the form given in the definition of a sinusoidal function.

Thus, functions of the form

y = A cos ( B t ( − h ) ) + k

y = A cos ( B t ( − h )) + k are also sinusoidal functions.

NOTE 2: Based what we know about graph transformations (which are studied in the previous

course), we should recognize that sinusoidal functions are transformations of the

function. Below is a summary of what is studied in the previous course

about graph transformations:

y = sin( ) t

SUMMARY OF GRAPH TRANSFORMATIONS

Suppose that f and g are functions such that ( )

g t ( ) = Af B t ( − h ) + k and

A B h k , , , ∈ R. In order to transform the graph of the function f into the graph of g

1

st

: horizontally stretch/compress the graph of f by a factor of

1

B

and, if , reflect

it about the y -axis.

B < 0

2

nd

: shift the graph horizontally h units (shift right if h is positive and left if h is

negative).

3

nd:

vertically stretch/compress the graph by a factor of A and, if A < 0 , reflect it about

the t -axis.

4

th

: shift the graph vertically k units (shift up if k is positive and down if k is

negative).

(The order in which these transformations are performed matters .)

Examples 1 – 4 (below) will provide a review of the graph transformations as well as an

investigation of the affect of the constants A , B , h , and k on the period, midline, amplitude,

and horizontal shift of a sinusoidal function. You may want to follow along by graphing the

functions on your graphing calculator. Don’t forget to change the mode of the calculator to

the radian setting under the heading angle.

EXAMPLE 1: Describe how we can transform the graph of f ( ) t = sin( ) t into the graph of

g t ( ) = 2 sin( ) t − 3. State the period, midline, and amplitude of.

y = g x ( )

SOLUTION :

Our goal is to use Examples 1 – 4 to determine how the constants A , B , h , and k

affect the period, midline, amplitude, and horizontal shift of a sinusoidal function so let’s

start by observing what the values of A , B , h , and k are in. It

should be clear that function g is a sinusoidal function of the form

where

g t ( ) = 2 sin( ) t − 3

y = A sin B t ( − h ) k A = 2 , B = 1 , h = 0 , and k = − 3.

After inspecting the rules for the functions f and g , we should notice that we could

construct the function g t ( ) = 2 sin( ) t − 3 by multiplying the outputs of the function

f ( ) t = sin( ) t by 2 and then subtracting 3 from the result. We can express this

algebraically with the equation below:

g t ( ) = 2 f ( ) t − 3

Based on what we know about graph transformations, we can conclude that we can

obtain graph of g by starting with the graph of f and first stretching it vertically by a

factor of 2 and then shifting it down 3 units. Since f ( ) t = sin( ) t has amplitude 1 unit, if

we stretch it vertically by a factor of 2 then we’ll double the amplitude, so we should

expect that the amplitude of g to be 2 units. Also, since f ( ) t = sin( ) t has midline

, when we shift it down 3 units to draw the graph of g , the resulting midline will be

. (Note that since graphing g required no horizontal transformations of

y = 0

y = − 3

f ( ) t = sin( ) t , the graph of g must have the same period as the graph of f ( ) t = sin( ) t :

2 π units.) Let’s summarize what we’ve learned about g t ( ) = 2 sin( ) t − 3 :

period : 2 π units

midline : y = − 3

amplitude : 2 units

horizontal shift : 0 units

The graphs of f ( ) t = sin( ) t and g t ( ) = 2 sin( ) t − 3 are given in Figure 1 below.

Figure 1: The graphs of f ( ) t = sin( ) t and g t ( ) = 2 sin( ) t − 3.

EXAMPLE 3: Describe how we can transform the graph of p t ( ) = cos( ) t into the graph of

and find the period, midline, amplitude, and horizontal shift

of.

q t ( ) = −cos(2 ) t

y = q x ( )

SOLUTION :

Notice that the function q is a sinusoidal function of the form

y = A cos B t ( − h ) + k

where A = − 1 , B = 2 , h = 0 , and k = 0.

After inspecting the rules for the functions p and q , it should be clear that we can write

q in terms of p as follows: q t ( ) = − p (2 ) t. Based on what we know about graph

transformations, we can conclude that we can obtain graph of q by starting with the

graph of p and first stretching it horizontally by a factor of

1

2

(i.e., compressing the

graph by a factor of 2 ) and then reflecting it about the t -axis. Since has

period

p t ( ) =cos( ) t

2 π units, if we compress the graph by a factor of 2 then the period will be shrunk

to π units. Since we aren’t stretching the graph of p vertically, we should expect that

the amplitude of q is the same as the amplitude of p : 1 unit. Also, since we aren’t

shifting the graph of p vertically, we should expect that the midline of q is the same as

the midline of p : y = 0. Let’s summarize what we’ve learned about q t ( ) = −cos(2 ) t :

period : π units

midline : y = 0

amplitude : 1 unit

horizontal shift : 0 units

The graphs of p t ( ) = cos( ) t and q t ( ) = − cos(2 ) t are given in Figure 3.

Figure 3: The graphs of p t ( ) = cos( ) t (blue) and

q t ( ) = −cos(2 ) t (purple).

Notice that the graph of q t ( ) = − cos( 2 t ) completes two periods in the interval [0, 2 π ]. In

general, the number B in a sinusoidal function of the form

y = A sin B ( th ) + k

or

represents the number of periods (or “cycles”) that the function

completes on an interval of length 2

y = A cos B ( th ) k

π. This number B is called the angular frequency

of a sinusoidal function.

When we use sinusoidal functions to represent real-life situations, we often take the input

variable to be a unit of time. Suppose that in the function q t ( ) = − cos(2 ) t , t represents

seconds. Since the input of the cosine function must be radians, the units of must

be “radians per second”. This way,

B = 2

radians

second

t seconds = 2 t radians,

which has the appropriate units for the input of the cosine function. So if t represents

seconds, the angular frequency of q t ( ) = − cos(2 ) t is “ 2 radians per second”.

Another way to obtain the unit of the angular frequency is to use what we noticed above:

the number 2 in represents the number of cycles that the function

completes on an interval of length 2

q t ( ) = − cos( 2 t )

π. Since a cycle is equivalent to a complete rotation

around a circle, or 2 π radians, two cycles is equivalent to 4 π radians. If the input

variable t represents seconds, then the angular frequency is

4

2

radians

seconds

rad/sec

π

π

EXAMPLE 4: Describe how we can transform the graph of p t ( ) = cos( ) t into the graph

( ) ( )

1

2 3

w t ( ) 3 p t 5

π

= − +. State the period, midline, amplitude, and

horizontal shift of y = w x ( ).

SOLUTION :

Notice that the function w is a sinusoidal function of the form

y = A cos B t ( − h ) + k

where A = 3 ,

1

2

B = ,

3

h

π

= , and k = 5.

After inspecting the rules for the functions p and w , it should be clear that we can write

w in terms of p as follows: ( ) ( )

1

2 3

w t ( ) 3 p t 5

π

= − +. Based on what we know about

graph transformations, we can conclude that we can obtain graph of q by starting with

the graph of p and first stretching it horizontally by a factor of 2 , then shifting it right

3

π

units, then stretching it vertically by a factor 3 , and finally shifting it up 5 units. Since

p t ( ) = cos( ) t has period 2 π units, if we stretch the graph by a factor of 2 then the period

will be stretched to 4 π units. Similarly, if we stretch the graph of vertically

by a factor of 3 then we’ll triple the amplitude, so we should expect the amplitude of w to

be 3 units. Also, since has midline

p t ( ) =cos( ) t

p t ( ) = cos( ) t y = 0 , when we shift it up 5 units to

draw the graph of w , the resulting midline will be y = 5. Since we are shifting the graph

Based on what we learned in the examples above, we can summarize the affect of the

constants A , B , h , and k on the period, midline, amplitude, and horizontal shift of functions

of the form and

y = A sin B t ( − h ) k

y = A cos B t ( − h ) + k.

SUMMARY: Graphs of Sinusoidal Functions

The graphs of the sinusoidal functions

y = A sin B t ( − h ) + k and

y = A cos B t ( − h ) + k

(where A B h k , , , ∈ R ) have the following properties:

period:

2

B

π

units

midline: y = k

amplitude: A units

horizontal shift: h units

angular frequency: B radians per unit of t

EXAMPLE 5: Sketch a graph of

4

f t ( ) 2sin t 3

π

SOLUTION :

In order to use what we’ve just studied about functions of the form

, we need to write the given function in this form, i.e., we need to

factor

y = A sin B t ( − h ) + k

π (which is playing the role of “ B ”) out of the input expression “

4

t

π

π − ”:

4

1

4

( ) 2sin 3

2sin 3

f t t

t

π

It should be clear that

1

4

f t ( ) 2sin π t 3

is a sinusoidal function of the form

where

y = A sin B t ( − h ) k A = 2 , B = π,

1

4

h = , and k = − 3. Using what we

found above, we can find the period, midline, amplitude, and horizontal shift of y = f t ( ):

period :

2 2

2

B

π π

π

= = units

midline : y = − 3

amplitude : 2 = 2 unit

horizontal shift:

1

4

of a unit

We can use this information to sketch a graph of

1

4

f t ( ) 2sin π t 3

; see Figure

5 below. (Note that the horizontal shift tells us where to “start” our usual sine wave.)

Figure 5: The graph of

1

4

f t ( ) 2sin π t 3

. The

blue point represents where we “start” our sine

wave since the horizontal shift is

1

4

of a unit.

Note that, according to what we discussed in Examples 3 and 4, if we let t represent

seconds then we could state that the angular frequency of

1

4

f t ( ) 2sin π t 3

is π radians per second. Since π radians represents one-half of a rotation around a

circle, the angular frequency “ π radians per second t ,” is equivalent to one-half of a cycle

per second. Notice that our graph in Figure 5 shows a function that completes one-half of

a period in one unit of t!