Diffusion Approximation for Fully Coupled Stochastic Differential Equations 2: The Slow Component Converges Weakly to the Averaged SDE at an Explicit Rate (Regime 1)Research Paper
Motivation
Many stochastic models evolve on two time scales: a fast component that equilibrates quickly and a slow component driven by it. Planetary motion, climate models, geophysical flows and intracellular reaction networks are standard examples, and multiscale numerical methods for them approximate the slow component by a reduced equation. Such approximations are only useful with an error bound, and for the fully coupled case, where the fast and slow equations each depend on both components and the slow equation contains a large fluctuating drift, rates of convergence were missing.
Röckner and Xie (Ann. Probab. 49 (2021) 1205–1236) treat this case with only Hölder continuous coefficients and obtain explicit rates in four regimes. This mission poses the first regime, the classical averaging principle.
Timeline. Papanicolaou, Stroock and Varadhan (1977) proved the diffusion approximation for with a compact fast state space and time-independent coefficients. Pardoux and Veretennikov (2001, 2003, 2005) treated a noncompact homogeneous case with and by martingale problems and the Poisson equation. Rates for the averaging principle when were obtained by several authors, e.g. Givon (2007) and Liu (2010). Röckner and Xie (2021) give rates for the fully coupled system with Hölder coefficients in all four regimes.
Setting
Let (fast) and (slow), . For small parameters tending to , with , the two-scale system (1.4) is
with , and independent Brownian motions .
Freezing gives the frozen equation (1.7), with generator , , and invariant probability measure . A function is centered if its -average vanishes for every . The standing assumptions are: (Aσ), uniform nondegeneracy of ; (Ab), ; (AG), uniform nondegeneracy of ; (AH), is centered; and (2.7), the analogue of (Ab) for , small.
The averaged coefficients of Regime 1 are and , and the averaged equation (2.9) is , .
Regularity is measured in weighted Hölder classes: (index in , in , polynomial growth in ), its bounded version , the time-dependent , the class of measurable functions of polynomial growth, and for test functions.
Formalization targets
Goal: Theorem 2.3(i)
In Regime 1, and , assume , with , and . Then for every and ,
Milestones
- Lemma 4.1: mollification in at scales and costs and gains on and .
- Lemma 4.2: for centered , .
- Lemma 4.4(i): in Regime 1, .
- Lemma 5.1 (): is uniformly nondegenerate and .
Significance
The result. The theorem gives a rate for the weak error of the averaging principle under Hölder regularity only, and the rate depends only on the regularity in the slow variable , not on . It covers the fully coupled case, in which the slow equation contains the singular drift , and it identifies the extra condition under which this drift averages out. For it reduces to the rate (Remark 2.5), optimal for . Error bounds of this kind are what heterogeneous multiscale methods need to be quantitative.
Formalizing it. The result is proved in the paper; nothing in it is machine-checked. A formalization needs an Itô calculus for weak solutions, the elliptic Poisson equation in with parameter (the companion mission's Theorem 2.1), and the parabolic Kolmogorov equation of the averaged SDE. The two fluctuation lemmas are stated for general centered functions and are reusable for other limit theorems.
Difficulty
The obvious argument writes through the Kolmogorov equation of the averaged SDE and Itô's formula, which leaves and . Both integrands are centered but only Hölder continuous in , so the standard corrector argument, which applies Itô's formula to the solution of the Poisson equation along , needs derivatives in and that do not exist. The term with is a central-limit-scale fluctuation, which is why its control needs the regime conditions. Existence and regularity of the averaged coefficients also have to come from the Poisson equation, since is not explicit.
Formalization scope
Spaces are EuclideanSpace ℝ (Fin d). Coefficients are , a matrix, , a matrix. The Itô layer (Brownian motion, Itô integral, Itô processes, SDE solutions) is the published Peng1990.SMP.Stochastic. A solution of (1.4) is a weak solution: any filtered probability space, any Brownian motion for that filtration, any progressive process satisfying the integral equation. The theorem compares every weak solution of (1.4) with every weak solution of (2.9). The paper does not prove existence for (1.4), so the statement is conditional on solutions, as it is used in the paper. A sanity file shows the parameter hypotheses are consistent (, ) and that (2.7) holds for a bounded dissipative drift.
Committed conventions and readings of the page:
- is any family of probability measures that are infinitesimally invariant for with , the generator of (1.7). Under the standing assumptions this is the unique invariant measure.
- (2.7) is read with , the factor that actually multiplies in the fast drift, for all small .
- is any measurable matrix field with , which covers the printed square root.
- The Hölder classes include polynomial growth, constrain all lower -derivatives, and take their constants uniformly in time, including in the time-Hölder clause.
- The constants , , exist after all data are fixed (coefficients, , , , , , the parameter functions) and before or .
- Lemma 4.1 takes on all of in time, since (4.1) evaluates at negative times, and assumes the kernels have the finite moments , that its proof uses; without them (4.2) fails for a Cauchy-type kernel.
- Solutions are Itô processes in the sense of the referenced layer: progressive, with and square-integrable diffusion integrands.
- Lemma 4.4(i) carries the Regime 1 limits of its label.
- Lemmas 4.2 and 4.4(i) are one-sided, as printed, and include integrability of the path integral in their conclusion.
A formalization in which the expectations are junk Bochner integrals, the constant depends on , or a single strong solution is fixed would be a different and weaker statement; the posed statements rule these out.
Not posed: Regimes 2–4 of Theorem 2.3 and Lemma 4.4(ii)–(iv). The printed differs by a factor in the term from the generator used in the proof, so a faithful statement needs a correction that is left to moderation. Regime 2 needs the Poisson solution in the averaged drift. Lemma 5.2 is also not posed: as printed, solves (5.1) only for time-independent coefficients, and its class has time index above , which the paper's notations do not define. Contributions toward Itô's formula for these processes, the Poisson equation (companion mission 1) and parabolic Schauder theory are welcome.
Selected references
- M. Röckner, L. Xie, Diffusion approximation for fully coupled stochastic differential equations, Ann. Probab. 49(3) (2021) 1205–1236. https://doi.org/10.1214/20-AOP1475
- G. Papanicolaou, D. Stroock, S. R. S. Varadhan, Martingale approach to some limit theorems, Duke Turbulence Conference, Duke Univ. Math. Ser. III (1977).
- E. Pardoux, A. Yu. Veretennikov, On the Poisson equation and diffusion approximation. I, Ann. Probab. 29 (2001) 1061–1085. https://doi.org/10.1214/aop/1015345596
- E. Pardoux, A. Yu. Veretennikov, On Poisson equation and diffusion approximation. II, Ann. Probab. 31 (2003) 1166–1192. https://doi.org/10.1214/aop/1055425774
- E. Pardoux, A. Yu. Veretennikov, On the Poisson equation and diffusion approximation. III, Ann. Probab. 33 (2005) 1111–1133. https://doi.org/10.1214/009117905000000062
- D. Givon, Strong convergence rate for two-time-scale jump-diffusion stochastic differential systems, Multiscale Model. Simul. 6 (2007) 577–594. https://doi.org/10.1137/060673345
- D. Liu, Strong convergence of principle of averaging for multiscale stochastic dynamical systems, Commun. Math. Sci. 8 (2010) 999–1020.
- S. Peng, A general stochastic maximum principle for optimal control problems, SIAM J. Control Optim. 28 (1990) 966–979 (source of the Itô layer). https://doi.org/10.1137/0328054