Here is the thermal expansion coefficient and is the mass density. Let , , , and , the squared Alfvén frequency. We initially consider a nonzero frequency. The temperature and magnetic equations for a Fourier mode give
In particular, the minus sign in the magnetic relation follows from . Substitution into the magnetohydrodynamic momentum equation, with , gives
For incompressible flow, . Taking the vertical component of the curl eliminates pressure and gives, with ,
Taking another curl and its vertical component uses and . Thus
or, after eliminating temperature,
The two equations for vertical velocity and vertical vorticity have a nontrivial solution only when their determinant vanishes. This proves the stratified magneto-Coriolis wave dispersion relation
No division by was necessary, so a possible is retained. Division by , however, was necessary. Stationary disturbances must be checked directly in the original equations: for example, with , and an appropriate solenoidal magnetic perturbation can balance temperature-induced buoyancy and pressure. Such static balances are separate from the nonzero-frequency wave branches.
For fixed wavevector with , fixed nonzero Alfvén frequency , and , the two roots in of the stratified magneto-Coriolis wave polynomial have and the displayed slow root. This follows from the sum of roots being and their product being . The slow branch is oscillatory for and growing or decaying for the reversed inequality. At equality its frequency vanishes and the original stationary equations must be used.