arXiv:2608.06011v1
Abstract
In this paper, we study the strong averaging principle for multiscale time-inhomogeneous stochastic systems driven by multiplicative -stable processes with . Based on Khasminskii's discretization approach, we first establish that the fast component processes with a frozen slow variable admits a periodic measure. We then prove the strong convergence of the slow subsystem to an averaged system that depends on the time scale . For any fixed , if the reciprocals of the two periods and are rationally linearly independent, an important consequence is that the averaged system has random quasi-periodicity. Furthermore, by applying the ergodic theorem, we prove the strong convergence of the slow subsystem to another averaged system, a time-inhomogeneous SDEs independent of the time scale . Our result is also novel even in the time-homogeneous case for a fully coupled multiscale system with multiplicative -stable noises. Finally, we apply the result to a climate-weather system.
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Detailed mathematical audit
01Statements3 reported findingsContains unsupported statements
The two strong averaging theorems and the all-moment clause of the periodic-measure theorem are not verified for every under the printed assumptions. Assumption (A4) gives the required dissipation inequality for only one unspecified exponent, while the proof needs it at the exponent selected in each conclusion. The results are verified for each that separately satisfies .
Strong averaging to the time-dependent averaged equation
Pages 6 and 21–25 · Assumption (A4), Theorem 2.2, and its proof · arXiv:2608.06011v1
The theorem claims the rate for every . Assumption (A4), however, requires only for some , where contains and therefore tends to infinity as . A finite can satisfy (A4) at one exponent while failing at another. Lemmas 3.5, 3.7, 3.8, and 3.10 and the block estimate (3.29) use positive exponential contraction at the same exponent as the theorem. Hence the printed assumptions do not establish the full all- conclusion. The statement is verified after restricting it to each for which ; no counterexample to the broader conclusion is supplied.
Full paper, version 1 ↗Strong averaging to the epsilon-free averaged equation
Pages 7 and 25–28 · Theorem 2.5 and its proof · arXiv:2608.06011v1
This theorem makes the same assertion for every with rate . Its proof uses the -moment estimates and the averaged coefficients derived from Theorem 3.9, which in turn depend on contraction at that same . Assumption (A4) supplies this only at an existentially chosen exponent. The Khasminskii argument does establish the displayed conclusion for each satisfying , but the paper does not provide a separate argument covering exponents for which that inequality fails.
Full paper, version 1 ↗Periodic measure and its moment bounds
Pages 17–20 · Theorem 3.9 · arXiv:2608.06011v1
The pullback contraction at an exponent admitted by (A4), followed by Jensen's inequality, correctly gives the stated convergence, existence, uniqueness, periodicity, and continuity. The additional claim that for every is not established under the existential exponent in (A4): Lemma 3.7 derives its uniform -moment bound using . Thus the periodic-measure conclusion is verified, while its full all- moment clause is not.
02Proofs5 reported findingsContains incorrect or incomplete proofs
The main proof chain is correct for each exponent satisfying , but the paper applies that contraction to every although (A4) assumes it for only one exponent. The periodic-measure proof also equates unbounded moments after only convergence; lower semicontinuity gives a verified repair. One domain mismatch and one omitted constant are harmless local corrections.
A contraction hypothesis at one exponent is applied at every exponent
Pages 6, 13–17, and 21–28 · (A4), Lemmas 3.5, 3.7–3.10, and proofs of Theorems 2.2 and 2.5 · arXiv:2608.06011v1
Writing the dependence explicitly, Assumption (A4) states for some , whereas the cited lemmas and both main proofs substitute an arbitrary selected and use as a decaying factor. Because as , the required sign does not follow for all selected exponents. Downstream dependency: the periodic-measure -moment estimates, the averaged-drift estimates, (3.29), and both main rates. Repair classification: Verified repair. State (A4) for the exponent used in a conclusion and replace 'for any ' by 'for every such that .' Every contraction and balancing estimate in the paper then has the needed sign and yields the stated rate.
First-Wasserstein convergence does not imply convergence of higher moments
Page 20 · first display in Step 4 of Theorem 3.9 · arXiv:2608.06011v1
The proof writes after establishing only convergence. For , the integrand is unbounded and this equality does not follow from convergence plus a uniform -moment bound. Repair classification: Verified repair. Weak convergence and the nonnegative lower-semicontinuous function give the Portmanteau inequality with in the needed direction; combining it with Lemma 3.7 yields the displayed upper bound (3.13). No equality of moments is required.
Full paper, version 1 ↗Khasminskii discretization and rate optimization
Pages 21–28 · Sections 3.4–3.5 · arXiv:2608.06011v1
For a fixed exponent with , the auxiliary frozen process has the required moment and contraction estimates. The proof controls the discretization, frozen-fast-variable, and averaging-block terms by and , then chooses . The analogous periodic averaging estimate for the second system has the same balance. After the exponent restriction stated above, these steps yield both displayed strong rates.
The fast process requires the terminal time to follow the initial time
Pages 14 and 20 · definition of and statement of Lemma 3.10 · arXiv:2608.06011v1
The lemma quantifies over arbitrary , but and the two-parameter transition operator were defined only for . Add the restriction . Every application in the averaging proofs satisfies this order, and the proof then applies without change.
The time-Holder estimate omits its coefficient
Page 25 · Equation (3.34) · arXiv:2608.06011v1
Printed: . Assumption (A1) has an arbitrary Holder constant, so the mechanically determined correction is . All later estimates already absorb such coefficients into generic constants, so no argument or rate changes.
03Novelty0 reported findingsNo non-novelty findings
No non-novelty findings.