Magnetoconvection is thermal convection coupled to the evolution and forces of a magnetic field. Conserved magnetic flux can supply a slow field that must be retained along with the convective complex amplitude, rather than being eliminated into a single local amplitude equation.
A representative scaled amplitude model has complex and real with
Periodic boundary conditions conserve , because the right-hand side is a total second derivative. The slow field can change long-wave convection roll stability and permit localized pulses. For zero mean , the uniform convection rolls are , , .
For a real steady amplitude and zero-mean field, twice integrating the field equation yields , . The amplitude equation becomes . Using gives and , requiring . Its finite-window mean is . For , consistency gives . The leading roots coalesce at ; for the leading upper parameter limit is , while retaining the finite-window factor makes the necessary inequality strict. The isolated sech profile has an exponentially small derivative mismatch on a periodic interval, so exact periodic tails need correction. For the algebra supplies no finite upper bound of this form.
Linearize around and write . For sideband wavenumber , the sum and difference of the two amplitude sidebands, together with the field amplitude , evolve under
Expanding gives
At , the eigenvalues are ; the field's constant mode must be removed if its mean is prescribed. Nonzero long-wave field modes are still dynamically active.
Putting into the sideband cubic and retaining gives
For , makes the constant coefficient negative. There is a positive real , so sufficiently small nonzero grows. On a finite period , however, only are allowed. For , , , , every nonzero allowed mode has negative growth rates despite this long-wave inequality. Thus an arbitrarily-small-wave-number conclusion cannot be asserted without the domain-size qualification.

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