🤖 AI Summary
This work addresses the challenges of high computational cost, rapid error accumulation, and energy drift in long-term ocean state prediction by proposing a novel approach based on continuous-time Koopman autoencoders. The method embeds the nonlinear ocean dynamical system into a latent space governed by linear ordinary differential equations, enabling time-resolution-independent inference through matrix exponential evolution. Evaluated over a 2083-day rolling forecast, the model maintains bounded prediction errors and stable large-scale statistical properties, achieving inference speeds several orders of magnitude faster than conventional numerical solvers and significantly outperforming autoregressive Transformer baselines.
📝 Abstract
We investigate the Continuous-Time Koopman Autoencoder (CT-KAE) as a lightweight surrogate model for long-horizon ocean state forecasting in a two-layer quasi-geostrophic (QG) system. By projecting nonlinear dynamics into a latent space governed by a linear ordinary differential equation, the model enforces structured and interpretable temporal evolution while enabling temporally resolution-invariant forecasting via a matrix exponential formulation. Across 2083-day rollouts, CT-KAE exhibits bounded error growth and stable large-scale statistics, in contrast to autoregressive Transformer baselines which exhibit gradual error amplification and energy drift over long rollouts. While fine-scale turbulent structures are partially dissipated, bulk energy spectra, enstrophy evolution, and autocorrelation structure remain consistent over long horizons. The model achieves orders-of-magnitude faster inference compared to the numerical solver, suggesting that continuous-time Koopman surrogates offer a promising backbone for efficient and stable hybrid physical-machine learning climate models.