As we have seen in Exercises listofcurvesfirst - listofcurveslast in Section Relations, Chapter TheConicSections and most recently in Section PolarGraphs, there are scores of interesting curves which, when plotted in the \(xy\)-plane, neither represent \(y\) as a function of \(x\) nor \(x\) as a function of \(y\).

In this section, we present a new concept which allows us to use functions to study these kinds of curves. To motivate the idea, we imagine a bug crawling across a table top starting at the point \(O\) and tracing out a curve \(C\) in the plane, as shown below.

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The curve \(C\) does not represent \(y\) as a function of \(x\) because it fails the Vertical Line Test and it does not represent \(x\) as a function of \(y\) because it fails the Horizontal Line Test.

However, since the bug can be in only one place \(P(x,y)\) at any given time \(t\), we can define the \(x\)-coordinate of \(P\) as a function of \(t\) and the \(y\)-coordinate of \(P\) as a (usually, but not necessarily) different function of \(t\). Traditionally, \(f(t)\) is used for \(x\) and \(g(t)\) is used for \(y\).

The independent variable \(t\) in this case is called a parameter and the system of equations

\[\left \{ \begin{array}{rcl} x & = & f(t) \\ y & = & g(t) \\ \end{array} \right .\]

is called a system of parametric equations or a parametrization of the curve \(C\).

The parametrization of \(C\) endows it with an orientation and the arrows on \(C\) indicate motion in the direction of increasing values of \(t\).

In this case, our bug starts at the point \(O\), travels upwards to the left, then loops back around to cross its path at the point \(Q\) and finally heads off into the first quadrant.

It is important to note that the curve itself is a set of points and as such is devoid of any orientation. The parametrization determines the orientation and as we shall see, different parametrizations can determine different orientations.

If all of this seems hauntingly familiar, it should. By definition, the system of equations \(\left \{ x = \cos (t), \, y = \sin (t) \right .\) parametrizes the Unit Circle, giving it a counter-clockwise orientation.

More generally, the equations of circular motion \(\left \{ x = r\cos (\omega t), \, y = r\sin (\omega t) \right .\) developed on page ?? in Section cosinesinebeyond are parametric equations which trace out a circle of radius \(r\) centered at the origin.

If \(\omega > 0\), the orientation is counter-clockwise; if \(\omega < 0\), the orientation is clockwise. The angular frequency \(\omega \) determines ‘how fast’ the object moves around the circle.

In particular, the equations \(\left \{ x = 2960 \cos \left (\frac {\pi }{12} t\right ), \, y = 2960 \sin \left (\frac {\pi }{12} t\right ) \right .\) that model the motion of Lakeland Community College as the earth rotates (see Example Lakelandrotates in Section cosinesinebeyond) parameterize a circle of radius 2960 with a counter-clockwise rotation which completes one revolution as \(t\) runs through the interval \([0,24)\). It is time for another example.

The curve sketched out in Example parametricparabola certainly looks like a parabola, and the presence of the \(t^2\) term in the equation \(x=t^2-3\) reinforces this hunch.

Since the parametric equations \(\left \{ x = t^2 - 3, \, y = 2t-1 \right .\) given to describe this curve are a system of equations, we can use the technique of substitution as described in Section NonLinearEquations to eliminate the parameter \(t\) and get an equation involving just \(x\) and \(y\).

To do so, we choose to solve the equation \(y = 2t-1\) for \(t\) to get \(t = \frac {y+1}{2}\). Substituting this into the equation \(x = t^2 -3\) yields \(x = \left (\frac {y+1}{2}\right )^2 - 3\) or, after some rearrangement, \((y+1)^2 = 4(x+3)\).

Thinking back to Section Parabolas, we see that the graph of this equation is a parabola with vertex \((-3,-1)\) which opens to the right, as required.

Technically speaking, the equation \((y+1)^2 = 4(x+3)\) describes the entire parabola, while the parametric equations \(\left \{ x = t^2 - 3, \, y = 2t-1 \right .\) for \(t \geq -2\) describe only a portion of the parabola.

In this case, we can remedy this situation by restricting the bounds on \(y\). Since the portion of the parabola we want is exactly the part where \(y \geq -5\), the equation \((y+1)^2 = 4(x+3)\) coupled with the restriction \(y \geq -5\) describes the same curve as the given parametric equations. The one piece of information we can never recover after eliminating the parameter, however, is the orientation of the curve.

Eliminating the parameter and obtaining an equation in terms of \(x\) and \(y\), whenever possible, can be a great help in graphing curves determined by parametric equations.

If the system of parametric equations contains algebraic functions, as was the case in Example parametricparabola, then the usual techniques of substitution and elimination as learned in Section NonLinearEquations can be applied to the system \(\left \{ x = f(t), \, y = g(t) \right .\) to eliminate the parameter.

If, on the other hand, the parametrization involves the trigonometric functions, the strategy changes slightly. In this case, it is often best to solve for the trigonometric functions and relate them using an identity.

We demonstrate these techniques in the following example.

Now that we have had some good practice sketching the graphs of parametric equations, we turn to the problem of finding parametric representations of curves. We start with the following.

Parametrizations of Common Curves
  • The graph of \(y=f(x)\) as \(x\) runs through some interval \(I\) is parametrized by:

    \(\left \{ x = t, \, y = f(t) \right .\) as \(t\) runs through \(I\).

  • The graph of \(x=g(y)\) as \(y\) runs through some interval \(I\) is parametrized by:

    \(\left \{ x = g(t), \, y = t \right .\) as \(t\) runs through \(I\).

  • The graph of a directed line segment from \((x_{\text {\tiny $0$}}, y_{\text {\tiny $0$}})\) to \((x_{\text {\tiny $1$}}, y_{\text {\tiny $1$}})\) is parametrized by:

    \(\left \{ x = x_{\text {\tiny $0$}} + (x_{\text {\tiny $1$}} - x_{\text {\tiny $0$}}) t, \, y = y_{\text {\tiny $0$}} + (y_{\text {\tiny $1$}} - y_{\text {\tiny $0$}}) t \right .\) for \(0 \leq t \leq 1\).

  • The graph of a circle or ellipse \(\dfrac {(x-h)^2}{a^2} + \dfrac {(y-k)^2}{b^2} = 1\) where \(a,b > 0\) is parametrized by:

    \(\left \{ x = h+a\cos (t), \, y = k+b\sin (t) \right .\) for \(0 \leq t < 2\pi \).

    NOTE: This will impart a counter-clockwise orientation.

The reader is encouraged to verify the above formulas by eliminating the parameter and, when indicated, checking the orientation. We put these formulas to good use in the following example.

We note that the formulas given on page 7 offer only one of literally infinitely many ways to parametrize the common curves listed there. At times, the formulas offered there need to be altered to suit the situation.

Adjusting Parametric Equations
  • Reversing Orientation: \(~\)

    Replacing every occurrence of \(t\) with \(-t\) in a parametric description for a curve (including any inequalities which describe the bounds on \(t\)) reverses the orientation of the curve.

  • Shift of Parameter: \(~\)

    Replacing every occurrence of \(t\) with \((t-c)\) in a parametric description for a curve (including any inequalities which describe the bounds on \(t\)) shifts the start of the parameter \(t\) ahead by \(c\) units.

We demonstrate these techniques in the following example.

We put our answer to Example adjustparametricex number adjustcircleex to good use to derive the equation of a cycloid.

Suppose a circle of radius \(r\) rolls along the positive \(x\)-axis at a constant velocity \(v\) as pictured below. Let \(\theta \) be the angle in radians which measures the amount of clockwise rotation experienced by the radius highlighted in the figure.

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Our goal is to find parametric equations for the coordinates of the point \(P(x,y)\) in terms of \(\theta \). From our work in Example adjustparametricex number adjustcircleex, we know that clockwise motion along the Unit Circle starting at the point \((0,-1)\) can be modeled by the equations \(\left \{ x = -\sin (\theta ), \, y = -\cos (\theta ) \right .\) for \(0 \leq \theta < 2\pi \). (We have renamed the parameter ‘\(\theta \)’ to match the context of this problem.)

To model this motion on a circle of radius \(r\), all we need to do is multiply both \(x\) and \(y\) by the factor \(r\) which yields \(\left \{ x = -r\sin (\theta ), \, y = -r\cos (\theta ) \right .\).

Next, we adjust for the fact that the circle isn’t stationary with center \((0,0)\), but rather, is rolling along the positive \(x\)-axis. Since the velocity \(v\) is constant, we know that at time \(t\), the center of the circle has traveled a distance \(vt\) down the positive \(x\)-axis. Furthermore, since the radius of the circle is \(r\) and the circle isn’t moving vertically, we know that the center of the circle is always \(r\) units above the \(x\)-axis. Putting these two facts together, we have that at time \(t\), the center of the circle is at the point \((vt,r)\).

From Section circularmotion, we know \(v = \frac {r \theta }{t}\), or \(vt = r\theta \). Hence, the center of the circle, in terms of the parameter \(\theta \), is \((r\theta ,r)\). As a result, we need to modify the equations \(\left \{ x = -r\sin (\theta ), \, y = -r\cos (\theta ) \right .\) by shifting the \(x\)-coordinate to the right \(r\theta \) units (by adding \(r\theta \) to the expression for \(x\)) and the \(y\)-coordinate up \(r\) units (by adding \(r\) to the expression for \(y\)).

We get \(\left \{ x = -r\sin (\theta )+ r\theta , \, y = -r\cos (\theta ) + r \right .\), which can be written as \(\left \{ x = r(\theta -\sin (\theta )), \, y = r(1-\cos (\theta )) \right .\). Since the motion starts at \(\theta = 0\) and proceeds indefinitely, we set \(\theta \geq 0\).

We end the section by using technology to graph a cycloid.