So far we've looked at functions written as **y = f(x) =** (some function of the variable **x**) or **x = f(y) =** (some function of the variable **y**). Often, especially in physical science, it's convenient to look at functions of two or more variables (but we'll stick to two here) in a different way, as **parametric functions**. The easiest way of thinking about parametric functions is to introduce the concept of *time*.

Think about drawing a function like a parabola, from left to right, as time unfolds. Then it's easy to start thinking about both the x-coordinate and the y-coordinate changing as a function of time: **x = f(t), y = g(t)**. In fact, we call time the **parameter** in this sense.

In this section we're going to explore functions for which a point on the graph, **(x, y)** is given by **(f(t), g(t))** – parametric functions.

**Parametric functions** are functions of a number of coordinates (2 for the 2-dimensional plane, 3 for 3-D space, and so on), where each of coordinate **(x, y, z ...)** is expressed as another function of some **parameter**, like time: **x = f(t)**, **y = g(t)**, **z = h(t)**, and so on.

Function: **y = f(x)** Parametric: **x = g(t)**, **y = h(t)**

Let's take a look at this graph by making a table of **(x, y)** coordinates, but we'll match them up with the **t**'s and keep track of those, too.

The x-coordinates of each point on the graph of this function are given by **x = f(t)**, and the y's by **y = g(t)**. The **(x, y)** pairs are plotted in the graph below. Clearly a sideways parabola like this isn't a function when written as **y = f(x)** because there are two y values for all but one of the x's in the domain. But in parametric form, there's one and only one **(x, y)** pair for each **t**. The function would actually have to loop back on itself and intersect to make a duplicate.

In order to express a circle as a function, we'd need to solve for **y** as a function of **x** (in this case, the radius r would be a fixed number). In taking the required square root, we'd actually get two functions with the ± we'd have to attach to the radical, like this:

Now we have a functional form for either the top half of a circle (the "+" function) or the bottom (the "-" function), but not both. If we think about expressing **x** and **y** in terms of another variable, however, we can find a nice parametric form for a circle. The obvious parameter is the angle of the circle, measured, as usual, from the positive side of the x-axis in a counterclockwise direction. Here's the diagram:

So our parameterization is **x = r·cos(θ)**, and **y = r·sin(θ)**, which traces out a circle of radius **r**, from **θ = 0** to **θ = 2π**.

You might recognize these transformations between polar coordinates **(r, θ)** and Cartesian coordinates **(x, y)** if you've worked in polar coordinates before.

If we calculate the first few points of that circle, say for angles of **θ = 0, π/4 **and** π/2**, we can see that the circle is traced in a **counterclockwise** direction as **θ** increases. Here are those values in a table:

and here's how they look on a plot of the circle:

That's a fancy way of saying "converting from parametric to function form." We'll take our first two examples as they were given in parametric form above, and see how we can get them back to functional form.

Take the first example above. We can eliminate the parameter, **t**, by rearranging the expression for y and plugging **y-1** in for t in the expression for **x**.

We get

Now we can complete the square on **y** in a few steps to solve for **y**:

Identify the perfect square on the left and find a common denominator on the right to get:

And finally

We notice that this function comes in two halves, the upper and the lower, as we would expect for a sideways parabola.

Our first example had the parameterization

If we're lucky enough to recognize the possibilities in writing **x ^{2} + y^{2}**, we'll see that

... and this is just the equation of a circle of radius **r**. It turns out that parameterizations of the form **x = a·cos(kx)**, **y = a·sin(kx)** are very common in the physical sciences, so it's worth getting used to manipulating them if that's where you're headed.

First let's make a table to get an idea of the shape and direction of the graph of this curve, then we'll eliminate the parameter to shed some more light on it.

Here's what the graph of that looks like. The direction of the curve is counterclockwise. It's an ellipse with a major axis of 5 units and a minor axis of 2, so that gives us an idea of what the non-parametric form *should* look like.

Now let's convert to standard form by eliminating the parameter. Suspecting that this is an ellipse, which will involve the squares of **x** and **y**, we'll begin by squaring the parameterization:

Now divide by 25 on the left and 4 on the right:

Now we can add these two equations, using the Pythagorean identity to get one on the right side ...

So the formula of our ellipse is

which indeed has a long axis along **x** of length 10 (= 2 × 5) and a short axis along **y** of 4 units (2 × 2). See the conic sections section if you need a refresher on ellipses.

It's not necessarily worth memorizing, but we've also got the idea that the parameterization **x = a·cos(t)**, **y = b·sin(t)** is an ellipse centered at the origin with axes of * 2a* and

As in the previous examples, plot a few points to get an idea of the shape and direction of each parameterization, then convert each to non-parameterized form.

Parametric functions allow us to calculate (using integration) both the **length of a curve** and the amount of **surface area** on a given 3-dimensional curve. As you study

multi-variable calculus, you'll see that the idea of "surface area" can be extended to figures in higher dimensions, too. It's a tricky thing to wrap your head around, the surface area of a 5-dimensional object, but it's mathematically sound.

Finding the slope of a parametric curve at a point is just finding the derivative at that point. The trouble is that we want **dy/dx** when what we have to work with is **x = f(t)** and **y = g(t)**. But as long as we're working with the Leibniz form of derivative notation, the solution is pretty obvious:

So to find the slope of a parametric function at a point, we take the derivative with respect to **y** and divide by the derivative with respect to **x**. This method can be generalized for higher dimensions, too.

__Solution__: First we find the derivatives of **x** and **y** with respect to t:

Then take the ratio D_{x} / D_{y}:

That's the general derivative of the function. Noticed that it's undefined at t = 0. The specific slope at t = 3 is

(Remember that we do calculus in radians.)

Now to determine the concavity, we need to calculate the second derivatives. The second derivative is a bit tricky. It looks like this:

Now we can take the second derivative of dy/dx and plug in the rest:

The we just evaluate that at x = 3:

Here is a plot of that parametric function. The graph may not look concave up at t = 3, but there is an inflection point at about t = 2.7, and it is.

x = 3 cos(t), y = 3 sin(t)

A tangent is horizontal to this parametric curve if **dy/dt = 0** and **dx/dt ≠ 0**, and it is vertical if **dx/dt = 0** and **dy/dt ≠ 0**. First we'll calculate the derivatives:

Now it's just a matter of plugging **t = 0, π, π/2 and 3π/2** into our parametric equations to get vertical tangents at (3, 0) and (-3, 0), and horizontal tangents at (0, 3) and (0, -3).

The graph of this parametric function is a circle:

Let's go back to a circle to calculate arc length. It's handy because we already know that the length of a circle is its circumference, **c = 2πr**, so we should get that answer. If we take a chord, **s** , of the circle, we can calculate its length as shown below:

Now we can blow the circle up a bit and take an infinitesimally small chord, ds, and show that its length is just (ds)^{2} = (dx)^{2} + (dy)^{2}.

So we have an equation for the length of the infinitesimal arc,ds:

Here is how we incorporate the parameter, t, into that expression:

Now we can use the parameterization, **x = r cos(t)** and **y = r sin(t)** *(I'm switching from θ to t here because t is more commonly used to denote a parameter)* to find

We solve for ds by taking the square root of **r ^{2}** to get

Finally, we can integrate those infinitesimal segments of arc around the circle, from **0** to **2π** to find the formula for the circumference of a circle, **c = 2πr** – pretty cool.

In general, we can state the length of a smooth curve in the box below.

If a smooth curve is defined parametrically by

then its length is given by

My students often have the mistaken impression that **time** is the "**fourth dimension**." It's not. In fact, any real problem in physics can have many *true* dimensions. For example, the position of an airplane in the sky is only fully specified by a set of *x, y* and *z* coordinates and three angles, *pitch*, *roll* and *yaw*, to describe the orientation of the plane with respect to the ground. It's a six-dimensional problem. Time, on the other hand, is *never* a dimension. Dimensions can have negative and positive values. Time is never negative. **Time is always a parameter, not a dimension**.

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