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Error analysis of an acceleration corrected diffusion approximation of Langevin dynamics with background flow

Yoichiro Mori, Chanoknun Sintavanuruk, Truong-Son P. Van

TL;DR

The paper analyzes an acceleration-corrected diffusion approximation for Langevin dynamics with a background flow in the averaging regime, proving that the strong error is O(ε) and the weak error O(ε^2) relative to the true dynamics. It develops a Limiting Langevin Calculus framework and uses drift-correction analysis to bound the difference between the true trajectory and the diffusion-approximation, with rigorous strong and weak estimates. The authors also demonstrate, both analytically and numerically, that the corrected diffusion captures long-time, nonuniform stationary distributions that naive diffusion fails to reproduce, and provide comprehensive 1D and 2D numerical validations. The results advance understanding of diffusion-approximations for inertial particles in flows and offer robust tools for predicting population-level transport statistics and stationary states.

Abstract

We consider the problem of approximating the Langevin dynamics of inertial particles being transported by a background flow. In particular, we study an acceleration corrected advection-diffusion approximation to the Langevin dynamics, a popular approximation in the study of turbulent transport. We prove error estimates in the averaging regime in which the dimensionless relaxation timescale $\varepsilon$ is the small parameter. We show that for any finite time interval, the approximation error is of order $\mathcal{O}(\varepsilon)$ in the strong sense and $\mathcal{O}(\varepsilon^2)$ in the weak sense, whose optimality is checked against computational experiment. Furthermore, we present numerical evidence suggesting that this approximation also captures the long-time behavior of the Langevin dynamics.

Error analysis of an acceleration corrected diffusion approximation of Langevin dynamics with background flow

TL;DR

The paper analyzes an acceleration-corrected diffusion approximation for Langevin dynamics with a background flow in the averaging regime, proving that the strong error is O(ε) and the weak error O(ε^2) relative to the true dynamics. It develops a Limiting Langevin Calculus framework and uses drift-correction analysis to bound the difference between the true trajectory and the diffusion-approximation, with rigorous strong and weak estimates. The authors also demonstrate, both analytically and numerically, that the corrected diffusion captures long-time, nonuniform stationary distributions that naive diffusion fails to reproduce, and provide comprehensive 1D and 2D numerical validations. The results advance understanding of diffusion-approximations for inertial particles in flows and offer robust tools for predicting population-level transport statistics and stationary states.

Abstract

We consider the problem of approximating the Langevin dynamics of inertial particles being transported by a background flow. In particular, we study an acceleration corrected advection-diffusion approximation to the Langevin dynamics, a popular approximation in the study of turbulent transport. We prove error estimates in the averaging regime in which the dimensionless relaxation timescale is the small parameter. We show that for any finite time interval, the approximation error is of order in the strong sense and in the weak sense, whose optimality is checked against computational experiment. Furthermore, we present numerical evidence suggesting that this approximation also captures the long-time behavior of the Langevin dynamics.

Paper Structure

This paper contains 28 sections, 19 theorems, 231 equations, 5 figures, 1 table.

Key Result

Theorem 1.1

Let $p\geq 4$, $W_t$ be a standard Brownian motion in $\mathbb{R}^n$, $( X^{\varepsilon } _t, V^\varepsilon_t)$ the solution to the system of SDE eq:Langevin, $Z^\varepsilon_t$ the solution of eq:advection-diffusion, and that they satisfy assumptions. Suppose H1-H3 are true for $p$. Then, for each $ Furthermore, for every $\varphi \in C^\infty(\mathbb{T}^n)$, there exists a constant $C$ such that

Figures (5)

  • Figure 1: The errors $\left| \int (u^\varepsilon(x,t)-g^\varepsilon(x,t)) \cos(kx) \, dx \right|$ of the diffusion approximation \ref{['eq:PDEApprox']} at time $T=1$ in $\log$ scale for Fourier modes $k=1,2,...,6$.
  • Figure 2: The errors $\left| \int (\tilde{u}^\varepsilon(x,t)-g^\varepsilon(x,t)) \cos(kx) \, dx \right|$ of the naive approximation \ref{['eq:naive']} at time $T=1$ in $\log$ scale for Fourier modes $k=1,2,...,6$.
  • Figure 3: Strong and weak errors in $\log$ scale via Monte-Carlo simulations between solution $X^\varepsilon_t$ of \ref{['eq:Langevin']} and $Z^\varepsilon_t$ of \ref{['eq:advection-diffusion']} at time $T=1$. 500,000 trajectories were simulated using SRIW1 method, tested against $\varphi=\cos x$ for the weak error.
  • Figure 4: Long-time behaviors at $T=100$. Row 1 displays the contours of the densities from Monte-Carlo simulation and reconstructed from kernel density estimation: (A) is the density of $X^\varepsilon_T$ satisfying the Langevin equation \ref{['eq:Langevin']}, (B) is the density $Z^\varepsilon_T$ satisfying the approximation \ref{['eq:advection-diffusion']}. Row 2 displays the stationary solution $u^\varepsilon$ of PDE \ref{['eq:PDEApprox']}. (C) is the contour of $u^\varepsilon$. (D) is the heatmap of $u^\varepsilon$, together with the background flow.
  • Figure 5: Long time behavior at $T = 100$ for different methods. (A) describes the density of \ref{['eq:advection-diffusion']}, (B) the density of \ref{['eq:Hasselman-simple']}, (C) the density of \ref{['eq:bakhtin-kifer']}, (D) the density of \ref{['eq:LWX']}.

Theorems & Definitions (40)

  • Theorem 1.1
  • Corollary 1.2
  • Proposition 2.1
  • Lemma 2.2
  • proof
  • proof : Proof of strong estimate in Proposition \ref{['prop:BrownianEst']}
  • proof : Proof of weak estimate in Proposition \ref{['prop:BrownianEst']}
  • Lemma 3.1
  • Remark 3.2
  • Lemma 3.3
  • ...and 30 more