PhysE-Inv: A Physics-Encoded Inverse Modeling approach for Arctic Snow Depth Prediction
This addresses a critical issue for climate science by improving predictions in data-scarce Arctic environments, though it is an incremental advance combining existing techniques with physics constraints.
The paper tackles the problem of accurately estimating Arctic snow depth, a time-varying inverse problem with sparse data, by introducing PhysE-Inv, a framework that integrates an LSTM Encoder-Decoder with physics-guided inference, resulting in a 20% reduction in error compared to state-of-the-art baselines.
The accurate estimation of Arctic snow depth remains a critical time-varying inverse problem due to the scarcity in associated sea ice parameters. Existing process-based and data-driven models are either highly sensitive to sparse data or lack the physical interpretability required for climate-critical applications. To address this gap, we introduce PhysE-Inv, a novel framework that integrates a sophisticated sequential architecture, namely an LSTM Encoder-Decoder with Multi-head Attention and contrastive learning, with physics-guided inference. Our core innovation lies in a physics-constrained inversion methodology. This methodology first leverages the hydrostatic balance forward model as a target-formulation proxy, enabling effective learning in the absence of direct ground truth; second, it uses reconstruction physics regularization over a latent space to dynamically discover hidden physical parameters from noisy, incomplete time-series input. Evaluated against state-of-the-art baselines, PhysE-Inv significantly improves prediction performance, reducing error by 20% while demonstrating superior physical consistency and resilience to data sparsity compared to empirical methods. Beyond Arctic snow depth, PhysE-Inv can be applied broadly to other noisy, data-scarce problems in Earth and climate science.