Ways of showing waves

Throughout this website we will mainly use three ways of representing the propagation of waves. Examples are given below that illustrate the different representations.

We have already seen how waves travel through air by showing the motion of small air ‘particles’. It can be easier to look at the pressure variations that move with the wave. During compression the particles are closer together, and the pressure will be higher than normal. During rarefaction they will be further apart and the pressure will be lower than normal.

Remember the black and red dots represented in the below animation are not molecules. They are just markers enabling us to visualize the local displacement of air particles and so, the rise and fall of pressure within the wave medium. In a typical sound wave the particles would only move by a very small amount from their original positions, far too small to be seen. For the sake of clarity, the particle displacement has been exaggerated a lot.


In the following image a colour pattern moves with the wave.


The ‘hot’ colours occur wherever particles are close together and the ‘cold’ colours occur wherever they are far apart. The colours therefore represent the density of air, which changes as the wave passes through, or (more usually) the pressure which is proportional to density for small variations like these. In many pictures from now on we will just use the colours instead of the dots to show the variations of density and pressure in a wave. Unless otherwise stated, the scale of colour is proportional to the variations of density and pressure.


In many (but not all) of the acoustic waves in nature, the variations in pressure are much smaller than atmospheric pressure. Rather than talking about ‘high’ and ‘not so high’ pressure regions, it is easier to define acoustic pressure as the difference between the usual atmospheric pressure and the pressure at a point in the wave. This acoustic pressure can be positive or negative.

Transverse waves are readily visualized by means of line graphs. As illustrated by the animation below, the local oscillations generated at the left end are always up and down while waves travel from left to right. We can, however, use a simple line to indicate the pressure in a longitudinal wave where this is convenient.


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