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Reconstruction of wide spectrum forcing in transport-diffusion and Navier-Stokes equations

Jochen Bröcker, Giulia Carigi, Tobias Kuna, Vincent R. Martinez

TL;DR

The paper tackles the challenge of reconstructing unknown external forcings in infinite-dimensional dissipative systems, specifically transport–diffusion and the 2D Navier–Stokes equations, from incomplete observations. It develops two data-assimilation strategies: (i) the Sieve Algorithm, an iterative scheme that alternates state estimation and forcing reconstruction using low/high-mode projections, and (ii) the Nudging Algorithm, a continuous-time method that synchronizes observed and modeled states while recovering the forcing. A key contribution is allowing forcing terms of quasi-finite rank that can inject energy across all scales, extending prior work limited to band-limited spectra, and providing rigorous convergence analyses under explicit conditions on observational resolution, mode cutoff N, and nudging/relaxation parameters μ. The results demonstrate exponential convergence of both the reconstructed forcing and the state to the true quantities in 2D NSE and transport–diffusion, with the Nudging approach offering a conceptually simpler and more robust framework for time-independent forcings. These findings have potential impact for geophysical data assimilation and environmental monitoring where forcings are uncertain and multi-scale, energy-containing, and only partially observed.

Abstract

This article considers the problem of reconstructing unknown driving forces based on incomplete knowledge of the system and its state. This is studied in both a linear and nonlinear setting that is paradigmatic in geophysical fluid dynamics and various applications. Two algorithms are proposed to address this problem: one that iteratively reconstructs forcing and another that provides a continuous-time reconstruction. Convergence is shown to be guaranteed provided that observational resolution is sufficiently high and algorithmic parameters are properly tuned according to the prior information; these conditions are quantified precisely. The class of reconstructable forces identified here include those which are time-dependent and potentially inject energy at all length scales. This significantly expands upon the class of forces in previous studies, which could only accommodate those with band-limited spectra. The second algorithm moreover provides a conceptually streamlined approach that allows for a more straightforward analysis and simplified practical implementation.

Reconstruction of wide spectrum forcing in transport-diffusion and Navier-Stokes equations

TL;DR

The paper tackles the challenge of reconstructing unknown external forcings in infinite-dimensional dissipative systems, specifically transport–diffusion and the 2D Navier–Stokes equations, from incomplete observations. It develops two data-assimilation strategies: (i) the Sieve Algorithm, an iterative scheme that alternates state estimation and forcing reconstruction using low/high-mode projections, and (ii) the Nudging Algorithm, a continuous-time method that synchronizes observed and modeled states while recovering the forcing. A key contribution is allowing forcing terms of quasi-finite rank that can inject energy across all scales, extending prior work limited to band-limited spectra, and providing rigorous convergence analyses under explicit conditions on observational resolution, mode cutoff N, and nudging/relaxation parameters μ. The results demonstrate exponential convergence of both the reconstructed forcing and the state to the true quantities in 2D NSE and transport–diffusion, with the Nudging approach offering a conceptually simpler and more robust framework for time-independent forcings. These findings have potential impact for geophysical data assimilation and environmental monitoring where forcings are uncertain and multi-scale, energy-containing, and only partially observed.

Abstract

This article considers the problem of reconstructing unknown driving forces based on incomplete knowledge of the system and its state. This is studied in both a linear and nonlinear setting that is paradigmatic in geophysical fluid dynamics and various applications. Two algorithms are proposed to address this problem: one that iteratively reconstructs forcing and another that provides a continuous-time reconstruction. Convergence is shown to be guaranteed provided that observational resolution is sufficiently high and algorithmic parameters are properly tuned according to the prior information; these conditions are quantified precisely. The class of reconstructable forces identified here include those which are time-dependent and potentially inject energy at all length scales. This significantly expands upon the class of forces in previous studies, which could only accommodate those with band-limited spectra. The second algorithm moreover provides a conceptually streamlined approach that allows for a more straightforward analysis and simplified practical implementation.

Paper Structure

This paper contains 35 sections, 26 theorems, 296 equations, 1 table.

Key Result

Theorem 1.1

Let $d = 2$ or $3$. Assume that $f$ is of quasi-finite rank $N_0$. Provided that $N \geq N_0$ is large enough and that $\mu$ is chosen accordingly, depending on $\kappa, N$ and the size of $\mathbf{v}$, there exists a relaxation time $t_* > 0$ such that the sequence of quasi-finite forces $\{f^{(j)} for $t_{j} := j t_*$ for all $j \in \mathbb{N}$.

Theorems & Definitions (55)

  • Theorem 1.1
  • Theorem 1.2
  • Theorem 1.3
  • Theorem 1.4
  • Definition 2.1
  • Theorem 2.2
  • Definition 2.3
  • Theorem 2.4
  • Proposition 2.5: Properties and estimates of the trilinear form
  • Definition 2.6
  • ...and 45 more