The formulation of linear wave phenomenon in terms of the wave equation, the Helmholtz equation, and its solutions in terms of orthonormal function on the Euclidean plane can be extended readily to three dimensional Euclidean space. For this space the wave equation
can be solved relative to various orthogonal coordinate systems (there are at least eleven of them). The choice of coordinates is invariably dictated by symmetry and boundary conditions. This means that the coordinates are usually chosen so one or more of the coordinate surfaces mold themselves onto boundaries where the boundary conditions are specified. In terms of ubiquity, the three most important coordinate systems are the rectangular, cylindrical, and the spherical coordinates.
We shall now consider the wave equation relative to spherical coordinates is
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A useful observation, rather valuable as we shall see momentarily, is the fact that the first term can be written in the form
Another useful observation is that the second term is easy to remember. Indeed, for small
the familiar two-dimensional Laplacian, Eq.(5.1) on P
, for the Euclidean plane.
This is as it should be: around the north pole of a sphere the spherical
coordinates reduce to the polar coordinates of the Euclidean plane around the
origin.
The physically and mathematically most revealing solutions are the normal modes. They are time translation eigenfunctions and, as we have already learned from Section 5.1.4, they satisfy the equation
A normal mode has the form
Here
or
relative to spherical coordinates. This partial differential equation lends itself to being separated into a system of ordinary differential equations. Letting