核心概念
A novel physics-guided diffusion model framework that efficiently generates high-fidelity PDE solutions from low-fidelity inputs, while maintaining accuracy comparable to traditional fine-scale solvers.
摘要
The paper proposes a novel approach called Physics-Guided Diffusion Model (PGDM) for efficiently downscaling PDE solutions. The key highlights are:
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Formulation of the downscaling problem as a conditional sampling task, where the goal is to sample from the posterior distribution of high-fidelity solutions given low-fidelity inputs.
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A two-step approach:
- Pre-training a conditional diffusion model to generate preliminary high-fidelity samples from low-fidelity inputs in a data-driven manner.
- Refining the generated samples through a physics-informed loss minimization step to ensure adherence to the underlying PDE constraints.
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Extensive numerical experiments on three nonlinear PDE problems (2D/3D Nonlinear Poisson, 2D Allen-Cahn, 2D Navier-Stokes) demonstrate that PGDM consistently outperforms baseline downscaling methods. It achieves comparable accuracy to traditional fine-scale solvers while reducing computational costs by over 10x.
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The proposed framework effectively combines data-driven generative modeling with physics-based refinement, enabling efficient and accurate downscaling of PDE solutions.
统计
Solving PDEs on fine spatio-temporal scales can be prohibitively expensive due to complexities like nonlinearity and multiscale phenomena.
Downscaling techniques generate high-fidelity approximate solutions from low-fidelity counterparts to speed up large-scale computations.
The proposed PGDM framework achieves over 10x computational acceleration compared to traditional fine-scale PDE solvers while maintaining the same level of accuracy.
引用
"Solving partial differential equations (PDEs) on fine spatio-temporal scales for high-fidelity solutions is critical for numerous scientific breakthroughs. Yet, this process can be prohibitively expensive, owing to the inherent complexities of the problems, including nonlinearity and multiscale phenomena."
"Our numerical experiments demonstrate that our model not only outperforms the baselines but also achieves a computational acceleration exceeding tenfold, while maintaining the same level of accuracy as the conventional fine-scale solvers."