Physics-Consistent Diffusion for Efficient Fluid Super-Resolution via Multiscale Residual Correction
On the map: Diffusion models → Flow matching, time series and science
Abstract (arXiv)
Existing image SR and generic diffusion models transfer poorly to fluid SR: they are sampling-intensive, ignore physical constraints, and often yield spectral mismatch and spurious divergence. We address fluid super-resolution (SR) with ReMD (underlineResidual-underlineMultigrid underlineDiffusion), a physics-consistent diffusion framework. At each reverse step, ReMD performs a multigrid residual correction: the update direction is obtained by coupling data consistency with lightweight physics cues and then correcting the residual across scales; the multiscale hierarchy is instantiated with a multi-wavelet basis to capture both large structures and fine vortical details. This coarse-to-fine design accelerates convergence and preserves fine structures while remaining equation-free. Across atmospheric and oceanic benchmarks, ReMD improves accuracy and spectral fidelity, reduces divergence, and reaches comparable quality with markedly fewer sampling steps than diffusion baselines. Our results show that enforcing physics consistency inside the diffusion process via multigrid residual correction and multi-wavelet multiscale modeling is an effective route to efficient fluid SR. Our code are available on https://github.com/lizhihao2022/ReMD.
Key facts. No citing papers in the map yet (data through 7 Oct 2026). Placed in Flow matching, time series and science, one of 14 directions in Diffusion models. Builds on 17 of its 26 references that are in the map. First posted on arXiv 25 Feb 2026.
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17 of 26 references.
References · 17
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5 more
- 2021Multiwavelet-based Operator Learning for Differential Equationscited by 229
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- 2026Bridging Restoration and Generation in One-step Diffusion for Real-World Image Super-Resolution
- 2026Multiphase-Diff: Diffusion-Based Generative Modeling for High-Contrast Multiphase Physical Systems with Sharp Interfaces
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