Cylindrical Coordinates#
Cylindrical coordinates are a natural extension of the Polar Coordinates to three dimensions. They identify each point in the Euclidean space \(\mathbb{R}^3\) by its distance from the \(z\)-axis, the angle \(\phi\) its projection in the \(xy\)-plane makes with the \(x\)-axis and its \(z\) component.
Definition: Radial Distance
The number \(\rho\) is known as the radial distance.
Warning
This is not the same as the radial distance used in spherical coordinates.
Definition: Azimuthal Angle (Azimuth)
The number \(\phi\) is known as the azimuthal angle or azimuth.
Definition: Axial Coordinate (Height)
The number \(z\) is known as the axial coordinate or height.
Note
Despite the word "height", the axial coordinate's algebraic sign is crucial.
Theorem: Local Coordinate Basis of Cylindrical Coordinates
Let \(\tau: (0, +\infty) \times (0, 2\uppi) \times \mathbb{R} \to \mathbb{R}^3\) be the transition map from cylindrical coordinates to Cartesian coordinates.
Its normalized local coordinate basis at \((\rho, \varphi, z)\) is the following:
Proof
We have the following by definition:
We see that \(\tau\) is totally differentiable on \((0, +\infty) \times (0, 2\uppi) \times \mathbb{R}\) with the following Jacobian matrix:
For the determinant, we have:
Since \(\rho \ne 0\), we know that the columns of \(J_{\tau}\) form a local coordinate basis:
We just need to normalize them:
Conventions#
Some people prefer to use \(\theta\) or \(\varphi\) for the azimuth.
Additionally, a single point has infinitely many possible values for its azimuth, since adding or subtracting a multiple of \(2\pi\) to an angle has no effect. However, in order to have a coordinate system, coordinates must be unique. This means that the possible values for \(\phi\) must be restricted. Common conventions for the range of \(\phi\) are \([0; 2\pi)\) and \((-\pi, \pi]\).