At point the surface is less steep than at point , and the surface is steepest at point .

We introduce level sets.

### Level sets

It was Descartes who said “Je pense, donc je suis.” He also developed our rectangular
coordinate system, the -plane. This is also known as the Cartesian coordinate
system. This coordinate system allows us to consider the graph of a function.
First, recall that the graph of a function of a single variable, is a curve in a
two-dimensional plane. In the same sense, the graph of a function of two variables,
is a surface in three-dimensional space. The graph of a function of three
variables, is a surface in *four*-dimensional space. A surfaces in higher than
three dimensions is often called a **hypersurface**. How can we visualize such
functions? For visualizing functions , a graphing utility like Desmos is really
great. For visualizing functions , GeoGebra is very helpful. However, once
we get to functions (or ), visualizing the graph of the function as we do
in two and three dimensions becomes much more difficult. One powerful
technique to help us understand a function visually is known as sketching *level
sets*.

**level set**corresponding to is a set in the domain of the function such that for all points in the set.

When working with functions the level sets are known as **level curves**.

When we are looking at level curves, we can think about choosing a -value, say , in the range of the function and ask “at which points can we evaluate the function to get ?” Those points form our level curve. If we choose a value that was not in the range of , there would be no points in the -plane for which , and hence no level curve associated to .

It may be surprising to find that the concept of level sets is familiar to most people,
but they don’t realize it. Topographical maps, like the one below represent the
surface of Earth by indicating points with the same elevation with **contour lines**.
We also had an example of the contour lines of Meteor Crater as we began this
section.

Another example you may know are **isotherms**, which are curves along which the
temperature does not change. We see these in weather maps.

Below we see a surface with level curves drawn beneath the surface. Remember that the level curves are in the domain of the function, not on the surface itself.

We often mark the function value on the corresponding level set. If we choose function values which have a constant difference, then level curves are close together when the function values are changing rapidly, and far apart when the function values are changing slowly.

Now, let’s see if you can identify some simple surfaces based on their level curves.

Let’s look at another example.

Now let’s find the level curves of for the required values. Each of our level curves will be of the form Now we just need to substitute all of our values for and plot each of the following implicit functions:

To make your sketch, either plot these implicit functions with your favorite graphing device, or recognize that they are crossing lines when and hyperbolas otherwise. As a gesture of friendship, we have included a graph of these level curves. Below, we evaluate on our level curves and plot the resulting curves on the surface .

Let’s see another example.

Now, we find a vector-valued function for the level curve, as well as the curve on the surface. Since the level curve is given by the equation and we can solve for without too much algebra, we set . Then, . The level curve can be described parametrically by: The corresponding curve on the surface can be described parametrically by:

Notice that the -component of the curve on the surface should not require much calculation since we found the curve on the surface by noting . This means that all of the -values on the curve on the surface should be .

So far, the level sets we’ve been working with have been curves in . We can easily
generalize to functions . When working with functions , our level sets are also called
*level surfaces*.

#### Level sets in higher dimensions

In higher dimensions, we want to try to use what we understand about functions of one and two variables to try to better understand functions of three or more variables.

- A function of
**one**variable can be visualized as a**curve**drawn in**two**dimensions. - A function of
**two**variables can be visualized as a**surface**drawn in**three**dimensions. - A function of
**three**variables can be visualized as what we will call a**hypersurface**drawn in**four**dimensions. - A function of variables can be visualized as what we will call a
**hypersurface**drawn in dimensions.

We use the term “hypersurface” to refer to an object which is like a surface, but in more than three dimensions. Hypersurfaces are difficult to imagine, and can even be difficult to picture using modern computer utilities.

For a function of three variables, one technique we can use is to graph the **level
surfaces**, our three-dimensional analogs of level curves in two dimensions. Given ,
the level surface at is the surface in space formed by all points where . It’s time for
an example.

for some constant . Let ; find the level surfaces of .

We now confirm our thought process mathematically. The level surface at is defined by Algebra reveals Given an intensity , the level surface is a sphere of radius , centered at the origin. Every point on each sphere experiences the same intensity of the radiating energy.

We have found that the level surfaces of in the above example are concentric spheres. If we picture several of these concentric spheres at the same time, we can get some intuition about the graph of in four dimensions in the same way that a collection of level curves in two dimensions gave us some intuition about the corresponding surface in three dimensions.

#### From explicit surfaces to level surfaces

We turn our attention to an important concept that will arise again in future sections.

Suppose that is a function of two variables. Then, the surface is a level surface of the function

In fact, if is a function of variables, we can also consider it to be a particular level set for some other function of variables. This idea is very powerful, as it allows us to consider the same function from two different perspectives. Having multiple perspectives gives us extra tools to use when considering our function, as well as allows us to look at the function in whatever manner we find most convenient. Let’s consider a specific example.

Again, it appears that all we did here was some easy algebra. We made a new function of one more variable by simply rearranging the original equation that defined our surface. But having multiple perspectives is always better than having only one. In addition to its other uses, the content of this procedure is vital for

- finding normal vectors for explicitly defined surfaces.
- finding tangent planes for explicitly defined surfaces.

These results will be explored further in later sections. It’s good to become familiar with these ideas now, so that we can make expert use of them later.