For the second-harmonic feedback in a long-wave convection amplitude equation, at the linear steady operator is . Its eigenvalue on is , so the critical Fourier modes are . More generally the linear dispersion relation is , giving first onset at .
At order , the weakly nonlinear expansion givesWith ,The constant part disappears under differentiation. Inverting on the second harmonic, whose eigenvalue is , givesup to a critical-harmonic correction absorbed into the definition of . At order ,The coefficient of in the last three terms is respectivelyThe Fredholm solvability condition requires their sum to vanish, because annihilates the critical Fourier mode. For a nonzero amplitude,This requires . The cubic amplitude coefficient is positive for , yielding a small-amplitude branch in a supercritical bifurcation; it is negative for , yielding a subcritical bifurcation branch in this leading approximation. At , the cubic coefficient vanishes and the quoted relation is singular: higher-order nonlinear terms and a different detuning balance are needed. One must not assert a finite there.
If a term were included in , order would also contain . The quadratic nonlinearity produces only the zeroth and second harmonics, with the zeroth differentiated away, so it cannot balance a first-harmonic contribution at that order. Solvability would give . Hence a nontrivial critical-mode expansion forces and first balances detuning against cubic amplitude effects at order .
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