A torsional Alfvén wave couples azimuthal velocity to a toroidal magnetic field around a fixed poloidal magnetic field. Axisymmetric induction gives and magnetic tension gives . Their combination is the displayed wave equation. Its local dispersion relation is .
For uniform-density incompressible flow with , and , the azimuthal magnetohydrodynamic momentum equation and ideal magnetohydrodynamic induction equation hold automatically. Let . The remaining equations require and , so is necessary and locally sufficient. A single traveling profile is unrestricted; two nonzero profiles on an unrestricted axial domain must be opposite exponentials or independent of their traveling arguments. Bounded profiles of both signs therefore reduce to steady solutions.
For a rotating conducting sphere, a geostrophic azimuthal velocity couples to the cylinder-integrated magnetic stress . Put and let be the cylinder height. With an insulating boundary and no flow through it, cylindrical averaging removes the Coriolis force and gives , . The local squared wave speed is , the cylinder average of .
For a cylinder-averaged torsional Alfvén wave with time-independent , differentiating this quadratic form gives . Regularity at the axis and vanishing magnetic torque at the outer endpoint therefore imply conservation. By Cauchy-Schwarz inequality, ; equality holds for the torsional-wave magnetic component proportional to along each cylinder. A stationary magnetic component orthogonal to is invisible to .
The magnetic tension stress transports axial angular momentum along a poloidal magnetic field. In purely azimuthal ideal flow the poloidal energy flux is . This proportionality is valid even at vanishing flux, where an ordinary ratio is undefined. The coupled fluxes explain how a torsional Alfvén wave redistributes rotation.

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