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We study an autonomous three-dimensional system defined by x˙=αx(1−x2)ẋ=α x(1-x^2)x˙=αx(1−x2), y˙=−y(β+κx2+ηy2)ẏ=-y(β+κ x^2+η y^2)y˙=−y(β+κx2+ηy2), z˙=−δz+ϵy2ż=-δ z+ε y^2z˙=−δz+ϵy2. We prove that this system admits closed-form solutions for all coordinates: x(t)x(t)x(t) is given explicitly, y(t)y(t)y(t) via a Bernoulli linearization, and z(t)z(t)z(t) via variation of constants. Consequently, we establish global convergence to one of three equilibria: a hyperbolic saddle at the origin and two sinks at (±1,0,0)(± 1, 0, 0)(±1,0,0). The stable manifold of the saddle is exactly the plane {x=0}\{x=0\}{x=0}, which acts as a separatrix between the basins of attraction. The parameters ααα and βββ are chosen to match the logarithmic rates of the Jonah triangle multipliers (λu=451/343λ_u=451/343λu=451/343, λs=−143/343λ_s=-143/343λs=−143/343), though this correspondence is a parameter convention rather than a dynamical derivation; notably, the negative sign of the discrete multiplier is lost in the continuous flow. This model serves as a rigorous, analytically solvable benchmark for testing edge-tracking algorithms in dynamical systems, without claiming physical relevance to Navier-Stokes or fluid turbulence.
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Schloss Jonah (2026) studied this question.
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