Set and . Distinguish the scalar magnetic field strength perturbation from the vector perturbation . To first order,
where the last identity is the solenoidal magnetic-field constraint. For a Fourier mode with the stated time convention, put
The linear momentum conservation equation, after division by , is
Use the solenoidal magnetic-field constraint in its component. The coefficient of reduces to . Thus
Both scalar pressure perturbations act within the plane. The component therefore decouples, independently of their closure. The ideal magnetohydrodynamic equations give
Eliminating the amplitudes gives the Alfvén wave dispersion relation
For this Shear Alfvén wave, the velocity and fluid displacement are along , perpendicular to both and the equilibrium magnetic field. Let ; then
A real snapshot bends the magnetic field lines sideways, with . There is no first-order compression or change of magnetic field strength: , and . Scalar pressure perturbations are unnecessary in this transverse subsystem. For a traveling stable branch, , so the velocity and transverse magnetic field perturbations are in phase or opposite phase according to the branch. At the bending force and this angular frequency vanish.
Figure 1.
Transverse displacement and the sign of the effective tension
. Original schematic for a Fourier displacement varying along the equilibrium magnetic field. With positive effective tension the force opposes the displacement; with negative effective tension it reinforces it. Details.

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