DOI: 10.1063/5.0351033 ISSN: 1070-6631

A multiscale deep learning framework for predicting stratified shear flow instabilities

Sangeetha Sankar, Vallabh Deogaonkar, Arjun Jagannathan, Abhilash Somayajula

Kelvin–Helmholtz (KH) instability in stratified shear flows exhibits strong multiscale dynamics, in which large-scale vortical structures evolve into smaller-scale motions through nonlinear interactions. Accurate prediction of KH dynamics is important for understanding mixing and transport in geophysical and environmental flows. Although high-fidelity simulations such as direct numerical simulation and large eddy simulation (LES) can resolve these dynamics, their computational cost limits their use across a wide range of flow conditions. Data-driven reduced-order models based on convolutional neural network autoencoders (CNN-AEs) and long short-term memory (LSTM) networks offer a promising alternative but often underrepresent dynamically important fine-scale structures. This study presents a parameter-conditioned multiscale deep learning framework for reduced-order prediction of stratified KH instability. The framework employs a state CNN-AE to capture dominant large-scale flow structures, a difference CNN-AE to learn finer-scale motions, and a parameter-conditioned LSTM to jointly evolve both latent representations using the gradient Richardson number (J) and the shear-to-stratification thickness ratio (R). The model is trained using vorticity and buoyancy fields from two-dimensional LES-like simulations spanning multiple flow configurations and is evaluated on both training and previously unseen test cases. The framework accurately reproduces the evolution of KH billows and preserves fine-scale structures throughout the nonlinear stages of instability development, as assessed through comparisons with the conventional CNN-AE–LSTM framework and LES using statistical metrics and physics-based diagnostics, including perturbation enstrophy, instability growth rates, and kinetic energy spectra. The proposed model also enables long-horizon forecasting from a single early-stage flow snapshot and generalizes successfully to previously unseen (J,R) combinations.

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