Vertical scaling means multiplying every output of a function by a scale factor: g(x)=af(x), mapping each point (x,y) to (x,ay). For a>1, the graph stretches away from the x-axis; for 0<a<1, it compresses toward it, while x-values and zeros remain unchanged. Negative scale factors and their accompanying reflections are outside this scope.
Detailed Explanation: Identify vertical stretches and compressions
A vertical scaling changes only the y-values of a function.
If
g(x)=af(x),
then each point (x,y) on f becomes
(x,ay)
on g.
If a>1, the graph has a vertical stretch: points move farther from the x-axis.
If 0<a<1, the graph has a vertical compression: points move closer to the x-axis.
The x-values stay the same, so the zeros of the function do not change.
Example: Let
f(x)=x2−4
and
g(x)=21​f(x).
Step 1: Identify the scale factor.
Compare g(x)=21​f(x) with g(x)=af(x). The scale factor is
a=21​.
Step 2: Classify the transformation.
Since
0<21​<1,
the graph is vertically compressed by a factor of 21​.
Step 3: Apply the scale factor to points.
For f(x)=x2−4:
When x=0, f(0)=−4, so (0,−4) becomes
(0,21​(−4))=(0,−2).
When x=3, f(3)=5, so (3,5) becomes
(3,21​(5))=(3,25​).
The x-intercepts remain the same. Since f(x)=0 at x=−2 and x=2, g(x) also has zeros at x=−2 and x=2.
Therefore, g(x)=21​f(x) is a vertical compression toward the x-axis by a factor of 21​.
Learn by doing: Identify vertical stretches and compressions
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Function Transformations (Definition) - Double Definition (Values) to Transformation