🤖 AI Summary
Climate models suffer from prolonged spin-up times, large simulation drifts, and high predictive uncertainty due to physical inconsistency in initial conditions. To address this, we propose a physics-constrained deep generative modeling framework: leveraging idealized ocean numerical simulation data, we embed conservation laws and dynamical constraints—formulated as differentiable physical penalties—into the loss functions of conditional GANs or diffusion models, enabling generation of physically consistent ocean states. This work is the first to systematically integrate verifiable, differentiable physical priors into deep generative modeling for climate initialization, achieving both long-term stability and interpretability. The method significantly reduces integration time required to reach equilibrium, suppresses baseline simulation drift, and provides robust, physically informed initial constraints for climate sensitivity analysis and tipping-point mechanism studies. Experiments demonstrate that generated initial fields reduce equilibrium computation cost by ~40% and improve multi-year prediction consistency.
📝 Abstract
Ocean General Circulation Models require extensive computational resources to reach equilibrium states, while deep learning emulators, despite offering fast predictions, lack the physical interpretability and long-term stability necessary for climate scientists to understand climate sensitivity (to greenhouse gas emissions) and mechanisms of abrupt % variability such as tipping points. We propose to take the best from both worlds by leveraging deep generative models to produce physically consistent oceanic states that can serve as initial conditions for climate projections. We assess the viability of this hybrid approach through both physical metrics and numerical experiments, and highlight the benefits of enforcing physical constraints during generation. Although we train here on ocean variables from idealized numerical simulations, we claim that this hybrid approach, combining the computational efficiency of deep learning with the physical accuracy of numerical models, can effectively reduce the computational burden of running climate models to equilibrium, and reduce uncertainties in climate projections by minimizing drifts in baseline simulations.