At point the surface is less steep than at point , and the surface is steepest at point .
We introduce 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 surface 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.
(In other words, all the points in the level set are assigned the same value, , by the function , and any point in the domain of with output is in that level 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.
In higher dimensions, we 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.
We now confirm our thought process mathematically. The level surface at , where , 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.
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 graph of , i.e., 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 surface from two different perspectives. Having multiple perspectives gives us extra tools to use when considering our surface, as well as allows us to look at the surface in whatever manner we find most convenient. Let’s consider a specific example.
Therefore, the surface can be interpreted as the graph of , where is a function of two variables given by or as a level surface of , where is a function of three variables, given by . To summarize, the following two equations describe the same surface or
- 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.