🤖 AI Summary
Ocean salinity observations from drifting buoys are extremely sparse, spatiotemporally irregular, and highly noisy. Conventional interpolation methods suffer from restrictive linear or stationarity assumptions and remote-sensing limitations (e.g., cloud contamination, low revisit frequency), while existing deep learning models exhibit poor generalization under extreme sparsity and lack physically interpretable mechanisms for integrating auxiliary covariates. Method: We propose the Ocean Salinity Imputation System (OASIS), the first framework coupling diffusion modeling with adversarial training, incorporating spatiotemporal embeddings and multi-task learning to jointly leverage physical covariates—such as temperature and geographic position—without requiring dedicated sensors. A physics-informed consistency constraint is further introduced to enhance interpretability and robustness. Contribution/Results: Evaluated on real-world buoy data, OASIS significantly outperforms classical interpolation and state-of-the-art deep learning baselines, enabling high-fidelity, physically consistent global salinity field reconstruction.
📝 Abstract
Ocean salinity plays a vital role in circulation, climate, and marine ecosystems, yet its measurement is often sparse, irregular, and noisy, especially in drifter-based datasets. Traditional approaches, such as remote sensing and optimal interpolation, rely on linearity and stationarity, and are limited by cloud cover, sensor drift, and low satellite revisit rates. While machine learning models offer flexibility, they often fail under severe sparsity and lack principled ways to incorporate physical covariates without specialized sensors. In this paper, we introduce the OceAn Salinity Imputation System (OASIS), a novel diffusion adversarial framework designed to address these challenges.