What is it about?

Kelvin-Helmholtz instability (KHI) is a fluid instability that arises from velocity shear within a single continuous fluid or from a velocity difference at the interface between two fluids. This work utilizes the physics-informed neural networks to solve the inverse problems of KHI flows, enabling field reconstruction and parameter inference from sparse, noisy data.

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Why is it important?

(1) Background. Kelvin-Helmholtz instability (KHI) is ubiquitous in nature (cloud formations, surface ripples on lakes, and exhaled breath) and industrial facilities (engines, jet cooling systems). Thus, prediction of KHI is a critical issue across various fields, including astronomy, meteorology, oceanography, life science, environmental science, and engineering. (2) Motivation. The required extensive high-fidelity data underscores the need for field reconstruction and parameter inference from sparse, noisy data, which is one of the capabilities of the physics-informed neural networks (PINNs). (3) Challenge. KHI flows have the spatiotemporal and magnitude multiscale, which challenges the PINNs due to the spectral bias and magnitude preference of neural networks. (4) Solution. The multiscale embedding and small-velocity amplification strategies are adopted to address the spatiotemporal and magnitude multiscale issues, respectively. The results demonstrate the accuracy of PINNs in field reconstruction and parameter inference, and validate the effectiveness of the proposed strategies.

Perspectives

It is exciting to use modern AI methods to solve problems of such a fundamental flow phenomenon. The research is challenging but interesting and meaningful. I hope that our open-source codes and data will help more researchers.

Jiahao Wu
Tsinghua University

Read the Original

This page is a summary of: Physics-informed neural networks for Kelvin–Helmholtz instability with spatiotemporal and magnitude multiscale, Physics of Fluids, March 2025, American Institute of Physics,
DOI: 10.1063/5.0251167.
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