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2101.04300

EMERGENT BEHAVIORS OF HIGH-DIMENSIONAL KURAMOTO MODELS ON STIEFEL MANIFOLDS

Seung-Yeal Ha, Myeongju Kang, Dohyun Kim

wrongmedium confidenceCounterexample detected
Category
math.DS
Journal tier
Strong Field
Processed
Sep 28, 2025, 12:55 AM

Audit review

The paper’s Theorem 1.3 asserts that for the homogeneous second-order Stiefel model (Ξi ≡ 0, m,γ,κ>0), every global solution satisfies limt→∞ ||Ṡi(t)||F = 0 and, moreover, limt→∞ G(t) = 0 (complete consensus) without further restrictions on initial data. The energy dissipation part is correct (via Proposition 4.1, yielding dE/dt = -(2γ/N)∑||Ṡi||^2 when Ξ≡0), hence velocities indeed vanish . However, the universal consensus claim contradicts explicit stationary “balanced” equilibria: for N=2, take S2(0) = -S1(0) and Ṡ1(0)=Ṡ2(0)=0. Then the right-hand side of (1.4) vanishes identically and Si(t) ≡ Si(0), hence G(t) stays constant and strictly positive (here G = 2p) rather than approaching 0, contradicting Theorem 1.3’s second conclusion . The paper’s key inequality mG̈ + γĠ + 2κξG ≤ … (Lemma 4.2) would force G→0 when the forcing tends to 0, but for the stationary non-consensus state one has G̈=Ġ=0 and thus 2κξG ≤ 0, which is false for G>0, revealing a gap in Lemma 4.2 or in its applicability . The candidate solution correctly proves velocities go to zero and supplies the balanced counterexample, so the universal consensus claim is false as stated, absent an additional non-degeneracy assumption (e.g., M(0)≠0).

Referee report (LaTeX)

\textbf{Recommendation:} major revisions

\textbf{Journal Tier:} strong field

\textbf{Justification:}

While the first-order analysis and the second-order velocity decay are well-supported, the key homogeneous second-order consensus claim is not correct as stated. Balanced stationary configurations provide a simple counterexample, and the differential inequality used to deduce consensus appears to need additional hypotheses. The manuscript can likely be salvaged with corrected statements and assumptions clarifying the role of such equilibria.