For an ordinary function you know how to measure change: the average rate of change on an interval, the slope of the secant line. A parametric function has two coordinates changing at once, so there are three rates worth asking about: how fast changes, how fast changes, and how steep the path is.
Two average rates, one for each coordinate
Take a parametric function and an interval . Each coordinate is a function of , so each has its own average rate of change:
These are the slopes of secant lines on the graphs of and against . If is in meters and in seconds, the rate of is in meters per second. A positive rate of means the point ended up farther right; a negative rate of means it ended up lower.
The slope of the path
To measure how steep the path itself is between the two points, compare the change in with the change in :
This is the average rate of change of with respect to on that piece of the path. Dividing the top and bottom by shows that it is also the rate of divided by the rate of .
Worked example. A skier's horizontal distance and height , in meters, are logged every 2 seconds.
| (seconds) | ||||
|---|---|---|---|---|
| (meters) | ||||
| (meters) |
On : the average rate of change of is meters per second, and of is meters per second.
The slope of the segment from to is
Reading the sign
| Change in | Change in | Slope of the segment |
|---|---|---|
| positive (right) | positive (up) | positive |
| negative (left) | positive (up) | negative |
| nonzero | : a horizontal segment | |
| nonzero | undefined: a vertical segment |
A slope of does not mean the point stood still. On from to , the point goes from to : the segment is horizontal, yet the point moved units right and rose and fell along the way.
How the rates themselves change
Over equal intervals of , compare successive average rates. In the skier's log the rates of on , , are , and meters per second: they increase, so the rate of change of is increasing, and the skier covers more horizontal ground in each 2 seconds. The segment slopes , , decrease, so the path gets steeper downhill from one stretch to the next.
Shorter intervals give a closer picture. The slope of a segment over a small interval of estimates how steep the path is near those points, and the rates of and over a small interval estimate how fast each coordinate is changing there.