Put and . The plane-layer poloidal-toroidal decomposition supplies the assumed poloidal fields asSince and , potentials proportional to have the required vertical components. Their horizontal components are proportional to , satisfying the stress-free boundary conditions and the horizontal-field boundary conditions. The double-curl representation automatically enforces incompressibility and the solenoidal magnetic-field constraint.
Let be the amplitudes of . The temperature and resistive induction equations immediately giveEliminate the total-pressure perturbation by applying to the vertical momentum equation and subtracting times its divergence. The resulting vertical equation isIn particular, shows explicitly that magnetic tension opposes the displacement.
Taking the determinant of these three amplitude equations gives the horizontal-field magnetoconvection dispersion relation:This cubic polynomial includes all roots of the assumed poloidal coupled system; using its determinant form avoids discarding possible roots by dividing by or . As a check, factors off magnetic diffusion and leaves the standard stress-free Rayleigh-Bénard convection growth equation.
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