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A complete-graph second-order landscape application
Statement
Let be a finite set of vertices. The unweighted complete graph has one edge between each pair of distinct vertices. A phase configuration is ; write also for an angular representative. Its cosine-difference energy is . An equilibrium means a configuration at which the gradient of in angular coordinates vanishes. Its Hessian is the matrix of second angular partial derivatives; it is positive semidefinite if for every . Fully synchronized means that all phases coincide modulo .
Every equilibrium of this energy whose Hessian is positive semidefinite is fully synchronized. Common rotation means adding the same phase to every coordinate; the conclusion is invariant under this rotation. No general converse from a positive semidefinite Hessian to local minimality is asserted.
Statement references
Facts & Assumptions
Angular representatives differ by integer multiples of , and angular chart transitions are translations. Thus the displayed gradient and Hessian conditions are independent of the chosen angular chart (Finite phase tori, local lifts and the flat metric).
For real , has modulus one, , and these expressions are unchanged by adding integer multiples of to angles. The derivatives of sine and cosine are cosine and minus sine, respectively (Phasors, trigonometric identities and periodic derivatives).
For a symmetric array of real weights and an even twice continuously differentiable periodic pair potential, the gradient is the sum of its first derivatives over neighbors and the Hessian quadratic form is one half the ordered sum of the second derivative times the squared coordinate difference (Differentiation of symmetric periodic pair potentials).
For a real symmetric matrix, positive semidefiniteness on real vectors implies nonnegativity of its complex quadratic form. For a real symmetric array , the complex form of equals (Real symmetric quadratic forms tested on phasors).
A nonzero average of unit phasors can be rotated to its positive modulus by multiplying all phasors by a common unit phasor (Rigidity and rotation of a unit-phasor average).
Proof
Given: A configuration on the complete graph with vanishing angular gradient and positive semidefinite Hessian .
Goal: Show that all its phases coincide modulo .
Set and . Apply [F3] with for , , and . By [F2], the gradient component is , and the real Hessian is the weighted Laplacian with entries for and . Adding the harmless diagonal coefficients leaves this Laplacian unchanged. Since , finite-sum expansion gives . Expanding the complex quadratic form from [F4] therefore gives, for every , .
If , choose . By [F2], and . Step 1.1 gives , contradicting [F4] and the assumed positive semidefiniteness. Hence .
Put . By [F5], a common rotation makes ; it leaves phase differences, the gradient equations and unchanged. At equilibrium, step 1.1 then gives for every . Since , each is either or . If some , choose the real coordinate vector that is at and zero elsewhere. Step 1.1 gives , contradicting positive semidefiniteness. Thus every rotated phasor equals .
Therefore the original phasors are all equal. The phase-torus identification with the unit circle in [F1], together with [F2], implies that their phases agree modulo . This is full synchronization. The proof used only the stated equilibrium and Hessian hypotheses and makes no sufficiency claim for general semidefinite Hessians.
Depends on
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