The Laplace radius is the satellite distance where the small-tilt nodal precession contributions from a planet's axisymmetric quadrupole and the stellar tide have equal magnitudes. In the circular hierarchical limit those rates are and . Equating them proves the displayed fifth-root expression. Inside this radius the planetary quadrupole coefficient controls the preferred plane; outside it the double-averaged circular tidal potential dominates. When equator and planetary orbit are inclined to one another, their balance determines the local Laplace plane.
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