## Mathematics 309 - the elementary geometry of wave motion

### Part I - scaling and shifting

One way of obtaining one graph from another is by scaling and shifting either x or y or both, so that the graph y=f(x) becomes the graph y = af(bx + c) + d. The way to see what happens to the graph is to understand what happens in simple steps with just one change at a time.
 y = f(x) y = 2f(x) All y-values on the graph are scaled by 2. In subsituting cf for f, vertical distances are scaled by c. y = f(x) y = f(x)+1 1 is added to all y values. y = f(x) y = f(2x) The height at x on the new graph is equal to the height at 2x on the old one. The new graph is obtained by compressing the old one horizontally by 2. In substituting cx for x, horizontal distances are scaled by 1/c. y = f(x) y = f(x+1) The height at x on the new graph is equal to the height at x+1 on the old one. The new graph is obtained by shifting the old one 1 to the left. y = f(x) y = f(2x-1)+1

Only the last one is tricky, since it involves a sequence of substitutions. In order to see which ones, we unravel the process.

• The function f(2x-1)+1 is obtained from f(2x-1) by adding 1.
• The function f(2x-1) is obtained from f(x-1) by substituting 2x for x.
• The function f(x-1) is obtained from f(x) by substituting x-1 for x.
To get the graph, we go backwards. We start with the graph of f(x).
• Substitute x-1 for x, y = f(x-1):
• Substitute 2x for x, y = f(2x-1):
• Add 1 to y, y = f(2x-1)+1:

### Part II - Wave functions in 1D

This section should be read by high school graduates with the minimum of grade 12 knowledge of math. Some physics from secondary school will also be useful for this page. But the author of this website assumes that the reader carries certain basic knowledge about trigonometry.

GOAL: The main goal of this section is to introduce wave functions in one dimension while using parameters that have been traditional to physics when involving light as a wave. (The other properties of light will not be discussed here as it digresses from the discussion of waves.) In this first section of wave functions of the first dimension we look at the basic building block; the function y = cos (x) and it's relations to waves before discussing changes that can be made to this wave function. Look at the graph below to see what the graph looks like. (In this case we use radians as the x value.)

We first start off by introducing vocabulary that will help us in our discussion about wave equations.

CYCLE: A cycle of a periodic function is a part of its graph from any point to the first point where the graph starts repeating. In the case of the cosine graph a cycle is repeated every horizontal length of 2 . So one cycle consists of 2 , 2 cycles consist of 4 , 3 cycles consist of 6 and so on.

CRESTS: The peak height of of a periodic function. In the case of cos(x) there is a crest at every n x 2.

WAVELENGTH: This is the horizontal length between two consecutive crests. In the 1st graph just above the wavelength is 2 . In the following functions we will denote wavelenth with the Greek letter lambda ().

PERIOD: The time it takes to go through one cycle.

VELOCITY: The speed that an object travels with a specific direction. In this case our object is a wave and will be denoted by the letter C.

FREQUENCY: There are two ways to define frequency they are 1) cycles/second or 2) if dealing with radians we would define it as radians per second. The frequency is denoted by the Greek letter omega ().

AMPLITUDE:This is the vertical distance in which a trough and crest are away from a horizontal line. (Sidenote: A trough is the lowest point in periodic graph.) So for example the Amplitude for a cos(x) graph would be 1, since 1 unit is the distace away from a crest and a trough with the horizontal line being y=0. We denote the amplitude for one dimensional wave graphs with the capital letter A.

Now that we're done all this terminology and Greek letter referencing we can now begin to move onto the more interesting material of wave functions.

Let us suppose that we want the equation of a wave that has not been changed horizontally or vertically at time zero. Then what would it's graph be?
ANSWER: The graph would be y=cos(x) since nothing has changed.

But what if the wave starts to move and in a horizontal direction, what would the new function look like after time t?
ANSWER: It is important to note here that the graph has shifted a certain amount of distance away from the origin. The key word being here is distance. The formula for distance in this case is velocity*time (C*t). So our new graph with just horizontal movement occuring is y=cos(x-Ct) if the wave moves in the positive direction and is y=cos(x+Ct) if the wave moves in the negative direction of the X-axis.

The Following graph shows a horizontal shift of in the positive X-axis direction. The velocity in this case is radians per second and the time for the shift to happen is 1 second.

Now that we know how to shift, is there a way to determine what the cosine function if the wavelength is no longer 2? For example what if we noticed that the the graph has compressed or stretched in the horizontal direction compared to f(x)=cos(x). What would the new wave equation be then?
ANSWER: To determine the new equation we need to know what the new wave length of the graph is. Once we know this information then we can proceed to find the equation of the wave. The equation of the graph that deals with compression and stretching is f(x)= cos[(2/)*x]. If 2 < 1 then the graph is being stretched by a factor of /2 with comparison to the f(x)=cos(x) graph. If it happens that 2 >1 then the opposite occurs and the graph is shrunk by a factor of /2 Let us suppose our new wave function has a wave length of 4, then our function is written as follows. f(x)=cos[(2/4)*x]=cos([1/2]*x). The following graph shows the difference between cos(x) and cos([1/2]*x)

Say that we are given the function instead of the wave length, can we determine the wave length from such a function?
ANSWER: A simple answer is yes. Let cos(Ax) be our graph, with A > 1, then we have a graph that is compressed by a factor of 1/a, then using the following equation we get the wave length of the graph. 2/=(A), then we isolate then =2/A.
The next thing to tackle is the vertical compresion or stretching of the graph. How is this done?

ANSWER: We put the compression or stretching factor in front of the function. There is a direct relationship when we put this number in front of the cosine function. So for example if we wanted a vertical stretch of 2, then the new function would be f(x)=2cos(x). If we wanted to compress the graph vertically by a factor of 1/2 for the cosine graph then our new function would then become f(x)=(1/2)cos(x).

The following graph shows a stretching and compressing of a cosine graph.

Now that we know the basics of waves and the different equations, we can get fancy and combine two or more together to produce a more sophisticated graph. For example the graph below is f(x)=2cos((1/2)(X-)).

To get the above graph we would shift in the right direction by a value of Pi, then expand horizontally by a factor of 2 and then stretch vertically by the factor of 2 when using the cos(x) graph as the comparison. The graph represents at time t=1.

If you've noticed, none of the equations have used frequency directly. It must be noted that = (2C)/
So our equation can be manipulated into the following form
y=Acos ((2)/)(x-Ct))
y=Acos((2/)x-(2C)/)t) So now we replace terms and use frequency directly into the function and Voila we get...

y=Acos((2/)x-t)

It should be noted that if we are given two of the following three, velocity, wave length. For example manipulating the formula /2=C
The period can be found by letter T=period and having T=2/
y=Acos((2)x-(2C)/)t)

### Part III - Affine functions in 2D and 3D

Hmm. Where do we start with this topic? First of all, you need to know what an affine function is. An affine function is any function that can be represented as:

f(x) = ax + b,

where a and b are some arbitrary constants and x is a variable. That was the 1D form. In 2D, we add another variable to the equation, and this changes the function form to:

f(x, y) = ax + by + c,

where c is another arbitrary constant and y is the extra variable that has been added.In 3D, this equation takes the form:

f(x, y, z) = ax + by + cz + d,

where d is another arbitrary constant and z another variable that we need to worry about. Now, let's take a look at how these functions behave in 2D (3D functions behave in the same manner, except that you have to add another dimension to the graph. Since this is hard to convey on graphs, we will be restricting our discussion to 2D graphs).

We will set f(x) = 0. In the grand scheme of things, this is usually done because we can always rewrite this equation as C = ax + by where C is the combination of f(x) and c.

There are many different cases to consider. Let us now take a look at them.

• a = 0

 The equation reduces to by = c. These equations are just horizontal lines.

• b = 0

 The equation reduces to ax = c. These equations are just vertical lines.

• b not equal to 0 and a not equal to 0

 The equation ax + by = C represents level lines that are neither horizontal nor vertical lines. See below for graphs.

• b = 0 and a = 0

 This is a rather trivial case and we will not bother to graph this.

Ok, so now we want to express all the above cases in a simpler model. Let's look at level lines (a level line is a curve where a function has a single value) of the function ax + by = C

If you look at the equation ax + by = C and set C to 0, then we see that this is [ a b ].[x y]' = 0, from linear algebra. This means that [x y] is perpendicular to the vector [a b]'.

In fact, if we put C back into the equation, we see that all level lines are perpendicular to [a b]'. In the graph below, [a b] was chosen to be [1 1] as an example.

One thing that is useful and handy to know concerning affine functions - that would be the distance between level lines in a set (C varies, but [a b] is chosen and stays constant within the set).

To figure this out, think of the vector [a b] as the distance between level lines. Calculating the length of the vector would be equivalent to calculating the distance between level lines! Since the distance from the line ax + by = 0 would be c1 / sqrt( a^2 + b^2 ) (using our knowledge of vector algebra), the general formula for this would be:

distance = (c2-c1) / sqrt( a^2 + b^2 )

This effectively calculates the distance between level lines. This distance is also signed (positive or negative), indicating the direction in which the level line lies.

### Part IV - Waves in 2D and 3D and the Wave Equation

In order to understand waves in multidimensions, namely in 2 and 3 dimensions, we must have a good grasp of the wave equation in 1 dimension. Please refer to the second section of this page titled "Wave Functions in 1 Dimension".

In the one dimensional case, we have:

1) f(x)=Acos[(2/)*(x-ct)]

A = amplitude, or height of the wave
= 3.14159265358979323846264338327950288419716939937510....
= the wavelength

Whereas in the 2 and 3 Dimensional case respectively, consider

2) f(x,y)=Acos(ax+by-ct)+g
3) f(x,y,z)=Acos(ax+by+cz-dt)+g

In the 2 dimensional case, a and b are the stretching/compressing factors on the axises x and y respectively. (This equation is actually the wave equation as a function of space x,y and time t.) Similarly, in the 3 dimensional case, a, b, and c are the stretching/compressing factors on the axises x, y, and z axises accordingly. (Here, the wave equation as a function of x,y,z and t. This would make it impossible to graph since it would require using four axises.)

What does it mean by stretching and compressing factors? Let's take a look at the the wave equation in 2D.

Here are some graphs of the 2D equation (in 3D). Remembering what you already know from the section on "Wave Functions in 1D", apply this knowledge to the 2D case. We have the amplitude A which is going to stretch all values of f(x,y) by a factor of A. If A<1, then the waves will appear shallow, whereas when A>1, the waves will appear to be taller in comparison to the case when A=1.

For a and b >1, points on the x and y axises are compressed by a factor of 1/a and 1/b respectively. However, if a and b <1, then points on the x and y axises are stretched out because of the factor 1/a and 1/b.

At time t=0, f(x,y)=Acos(ax+by) where [a,b] is the vector perpendicular to the waves (level lines) and is a multiple of [a,b]. The signed distance from level 0 to level 2 is 2/[(a^2+b^2)^0.5], also the length of . However, as time increases, the wave moves in the positive xy plane given c is the velocity in the equation

f(x,y)=Acos(ax+by-ct)

However, it would move in the opposite direction in the negative xy plane if c were negative, changing the wave equation to

f(x,y)=Acos(ax+by+ct).

Finally, in the equation f(x,y)=Acos(ax+by-ct)+g, the graph is shifted by a factor of g on the f(x,y) axis.

We would apply similar shifting and scaling techniques for graphs of 3 dimensions if it were at all possible to conceive.

And now, a couple of final animations to leave you with (which mimicks wave-like motion)