For an exterior mean-motion resonance, use mean longitude in , , and . Given and , the leading Keplerian detuning gives . Differentiating and using proves the displayed equation. It retains resonant forcing and eccentricity damping without the coordinate singularity at . True longitude adds a fast orbital ripple and does not yield this autonomous averaged equation directly.
For positive locally constant , supplement damped first-order resonant complex eccentricity by . Balancing the two dissipative rates gives , and . Two fixed points exist when . The negative-cosine branch has and is stable in this leading model: a phase increase raises the positive resonant torque, raises semi-major axis, lowers mean motion, and reverses the phase drift. The positive-cosine branch has the opposite feedback.
For a coupled verification put . The characteristic polynomial at either fixed point is . For its positive coefficients satisfy the cubic Routh-Hurwitz stability criterion, since the remaining inequality reduces to . For its negative constant term forces a positive real root. At the equality threshold the equilibria merge and an eigenvalue is zero. This is local stability for the frozen smooth-coefficient approximation, not a conclusion for arbitrary rapidly varying dissipation laws.

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