Abstract

Due to complex natural and anthropogenic interconnected forcings, the dynamics of suspended sediments within the ocean water column remains difficult to understand and monitor. Numerical models still lack capabilities to account for the variabilities depicted by in situ and satellite-derived datasets. Besides, the irregular space-time sampling associated with satellite sensors make crucial the development of efficient interpolation methods. Optimal Interpolation (OI) remains the state-of-the-art approach for most operational products. Due to the large increase of both in situ and satellite measurements more and more available information is coming from in situ and satellite measurements, as well as from simulation models. The emergence of data-driven schemes as possibly relevant alternatives with increased capabilities to recover finer-scale processes. In this study, we investigate and benchmark three state-of-the-art data-driven schemes, namely an EOF-based technique, an analog data assimilation scheme, and a neural network approach, with an OI scheme. We rely on an Observing System Simulation Experiment based on high-resolution numerical simulations and simulated satellite observations using real satellite sampling patterns. The neural network approach, which relies on variational data assimilation formulation for the interpolation problem, clearly outperforms both the OI and the other data-driven schemes, both in terms of reconstruction performance and of a greater ability to recover high-frequency events. We further discuss how these results could transfer to real data, as well as to other problems beyond interpolation issues, especially short-term forecasting problems from partial satellite observations.

Highlights

  • Marine Sediment fluxes result from a combination of natural and anthropogenic forcing factors [1,2]

  • Besides Optimal Interpolation (OI), we investigate state-of-the-art data-driven techniques, namely EOF-based interpolation (DinEOF), analog data assimilation (AnDA), and neuralnetwork interpolation schemes based on a variational formulation (4DVarNet)

  • The different interpolation methods are evaluated according to two standard metrics: the global root mean square error (RMSE) and a global reconstruction score (R-score), in terms of rate of variance of the true data captured by the interpolation

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Summary

Introduction

Marine Sediment fluxes result from a combination of natural and anthropogenic forcing factors [1,2]. The main source of sediment load comes from land, and the resuspension of sediments occurs under the effect of tidal currents and waves and from fish trawling and maritime development, such as harbor sediment dredging and dumping, aggregate extraction, submarine cable installation, offshore wind farm exploitation, oil and gas activities, etc. Due to to those complex natural and anthropogenic interconnected forcings, sediment process characterization has to be improved [3,4,5].

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