The paper introduces a multiscale inference scheme that uses contrast minimization to estimate drift parameters from slow-scale observations in systems with fast–slow dynamics.
It employs a stochastic Taylor expansion to approximate the behavior of the slow process and derive effective limits in both homogenization and averaging regimes.
It establishes consistency and asymptotic normality for the estimators while addressing computational challenges with simplified covariance structures.
A multiscale inference scheme for diffusion models provides a principled methodology for inferring unknown parameters or latent processes in systems governed by stochastic dynamics with multiple well-separated time scales. These schemes address the challenges posed by disparate dynamical regimes—often encountered in physical, biological, and engineered systems—where a slow “coarse” process is coupled with rapidly fluctuating “fast” variables. Observational data typically only capture the slow component, necessitating statistically efficient and robust inference strategies that account for the multiscale structure and its homogenization or averaging limits.
where W and B are independent Wiener processes, ϵ>0 is the noise scale, and δ(ϵ) is a small parameter controlling scale separation, with δ→0 as ϵ→0. The target is to estimate unknown drift parameters θ from observations of (Xtε,Ytε)0 alone.
Two asymptotic regimes are central:
Homogenization regime ((Xtε,Ytε)1): The fast process is sufficiently rapid to justify a homogenized effective equation for (Xtε,Ytε)2, under a centering condition on (Xtε,Ytε)3 with respect to the invariant measure (Xtε,Ytε)4 of the frozen fast dynamics.
Averaging regime ((Xtε,Ytε)5): The effective coefficients involve averages over the fast variable with finite memory.
2. Stochastic Taylor Expansion and Effective Limit
The stochastic behavior of (Xtε,Ytε)6 is approximated by an expansion: (Xtε,Ytε)7
where (Xtε,Ytε)8 solves the deterministic averaged ODE
(Xtε,Ytε)9
with dXtε=δϵbθ(Xtε,Ytε)dt+cθ(Xtε,Ytε)dt+ϵσ(Xtε,Ytε)dWtdYtε=δ2ϵf(Xtε,Ytε)dt+δ1g(Xtε,Ytε)dt+δϵτ1(Xtε,Ytε)dWt+δϵτ2(Xtε,Ytε)dBt,0 given by an average of explicit functions of the coefficients over the fast variable (different for homogenization and averaging).
A second-order pathwise stochastic Taylor expansion is derived: dXtε=δϵbθ(Xtε,Ytε)dt+cθ(Xtε,Ytε)dt+ϵσ(Xtε,Ytε)dWtdYtε=δ2ϵf(Xtε,Ytε)dt+δ1g(Xtε,Ytε)dt+δϵτ1(Xtε,Ytε)dWt+δϵτ2(Xtε,Ytε)dBt,1
where dXtε=δϵbθ(Xtε,Ytε)dt+cθ(Xtε,Ytε)dt+ϵσ(Xtε,Ytε)dWtdYtε=δ2ϵf(Xtε,Ytε)dt+δ1g(Xtε,Ytε)dt+δϵτ1(Xtε,Ytε)dWt+δϵτ2(Xtε,Ytε)dBt,2 is the fundamental solution of the linearized system, and dXtε=δϵbθ(Xtε,Ytε)dt+cθ(Xtε,Ytε)dt+ϵσ(Xtε,Ytε)dWtdYtε=δ2ϵf(Xtε,Ytε)dt+δ1g(Xtε,Ytε)dt+δϵτ1(Xtε,Ytε)dWt+δϵτ2(Xtε,Ytε)dBt,3 and dXtε=δϵbθ(Xtε,Ytε)dt+cθ(Xtε,Ytε)dt+ϵσ(Xtε,Ytε)dWtdYtε=δ2ϵf(Xtε,Ytε)dt+δ1g(Xtε,Ytε)dt+δϵτ1(Xtε,Ytε)dWt+δϵτ2(Xtε,Ytε)dBt,4 are solutions of Poisson equations associated with the fast process. This expansion provides the statistical basis for an approximate transition density of dXtε=δϵbθ(Xtε,Ytε)dt+cθ(Xtε,Ytε)dt+ϵσ(Xtε,Ytε)dWtdYtε=δ2ϵf(Xtε,Ytε)dt+δ1g(Xtε,Ytε)dt+δϵτ1(Xtε,Ytε)dWt+δϵτ2(Xtε,Ytε)dBt,5 and motivates the ensuing estimation schemes.
3. Minimum Contrast and Simplified Estimators
Utilizing the expansion, the inference strategy is to define an explicit Gaussian “misspecified model” for the increments of dXtε=δϵbθ(Xtε,Ytε)dt+cθ(Xtε,Ytε)dt+ϵσ(Xtε,Ytε)dWtdYtε=δ2ϵf(Xtε,Ytε)dt+δ1g(Xtε,Ytε)dt+δϵτ1(Xtε,Ytε)dWt+δϵτ2(Xtε,Ytε)dBt,6 between discrete observation times dXtε=δϵbθ(Xtε,Ytε)dt+cθ(Xtε,Ytε)dt+ϵσ(Xtε,Ytε)dWtdYtε=δ2ϵf(Xtε,Ytε)dt+δ1g(Xtε,Ytε)dt+δϵτ1(Xtε,Ytε)dWt+δϵτ2(Xtε,Ytε)dBt,7. For any trial parameter dXtε=δϵbθ(Xtε,Ytε)dt+cθ(Xtε,Ytε)dt+ϵσ(Xtε,Ytε)dWtdYtε=δ2ϵf(Xtε,Ytε)dt+δ1g(Xtε,Ytε)dt+δϵτ1(Xtε,Ytε)dWt+δϵτ2(Xtε,Ytε)dBt,8:
For each dXtε=δϵbθ(Xtε,Ytε)dt+cθ(Xtε,Ytε)dt+ϵσ(Xtε,Ytε)dWtdYtε=δ2ϵf(Xtε,Ytε)dt+δ1g(Xtε,Ytε)dt+δϵτ1(Xtε,Ytε)dWt+δϵτ2(Xtε,Ytε)dBt,9, compute
Omits covariance weighting and the W4 drift-correction term. Define
W5
- The SMCE is W6.
Both estimators require solving the deterministic averaged ODE and its linearization. The MCE additionally solves for Poisson correctors and covariance weights.
4. Asymptotic Theory and Efficiency
The main theoretical results are:
Consistency: Both MCE and SMCE are consistent for W7 as W8 at fixed W9:
B0
Asymptotic normality: Under identifiability and regularity assumptions,
B1
with explicit covariance B2 for MCE (achieving efficiency in the limit), and a larger B3 for SMCE reflecting its misspecification.
High-frequency observations: For both estimators, consistency is retained if B4 (SMCE), and B5 (MCE), with B6. The limit covariances match the continuous-time Fisher information.
These properties confirm the statistical optimality (in the Cramér–Rao sense) of MCE for the estimation of drift parameters in the multiscale regime, even though only the slow process is observed.
5. Averaging and Homogenization: Regime Distinctions
The two asymptotic regimes determine the appropriate form of the effective drift, diffusion, and Poisson correctors:
In the homogenization regime, a centering condition for B7 must be enforced, and effective coefficients derive from solutions to associated Poisson equations for the generator of the fast dynamics.
In the averaging regime, effective terms involve averages over the fast variable at finite memory length.
Both regimes lead to the same estimator structure but differ in the computation of these coefficients.
A critical practical point is that neither estimator requires explicit knowledge of B8 or B9: the only inputs are observation times and functional forms of the SDE coefficients. The estimation procedures rely on statistical moment-matching against effective models, sidestepping the need for direct modeling of the fast process.
6. Implementation: Algorithmic Outline and Usage
A canonical workflow for the multiscale inference scheme is:
Preprocessing: Given discrete-time data ϵ>00, set ϵ>01.
For trial parameter ϵ>02:
Solve the deterministic averaged ODE ϵ>03 with initial ϵ>04.
Solve the linearized ODE for ϵ>05.
Solve relevant Poisson equations to obtain ϵ>06 and ϵ>07.
For each ϵ>08, compute ϵ>09 and δ(ϵ)0 (MCE) or δ(ϵ)1 (SMCE).
Contrast minimization: Minimize δ(ϵ)2 (MCE) or δ(ϵ)3 (SMCE) over δ(ϵ)4 to obtain the parameter estimate.
Uncertainty quantification: Estimate asymptotic covariance δ(ϵ)5 or δ(ϵ)6 for confidence intervals.
This scheme is robust to noise levels and sampling rates provided δ(ϵ)7 and δ(ϵ)8 satisfy the separation conditions for the chosen estimator. For large δ(ϵ)9, high-frequency observations may require subsampling unless the strong scaling conditions are met.
7. Broader Applicability and Regime Guidance
The guiding philosophy of these multiscale inference methods is to exploit the analytic homogenization/averaging limit of the slow-fast system, employing locally Gaussian approximations and moment-based contrast minimization. No direct subsampling or explicit estimation of fast-scale parameters is required. Practical recommendations include:
Use MCE for maximal statistical efficiency when computational resources suffice for covariance weight computation.
Use SMCE for greater robustness or in contexts where the full covariance structure is computationally prohibitive.
Ensure regularity and identifiability conditions (e.g., nondegeneracy of Fisher information) for asymptotic guarantees.
This class of multiscale inference schemes provides a rigorous, computationally feasible, and statistically consistent framework for parameter estimation in multiscale diffusion systems observed at the slow scale, accommodating both homogenization and averaging regimes and enabling efficient uncertainty quantification (Gailus et al., 2017).
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