Abstract
The forecasting and reconstruction of oceanic dynamics is a crucial challenge. While model driven strategies are still the state-of-the-art approaches in the reconstruction of spatio-temporal dynamics. The ever increasing availability of data collections in oceanography raised the relevance of data-driven approaches as computationally efficient representations of spatio-temporal fields reconstruction. This tools proved to outperform classical state-of-the-art interpolation techniques such as optimal interpolation and DINEOF in the retrievement of fine scale structures while still been computationally efficient comparing to model based data assimilation schemes. However, coupling this data-driven priors to classical filtering schemes limits their potential representativity. From this point of view, the recent advances in machine learning and especially neural networks and deep learning can provide a new infrastructure for dynamical modeling and interpolation within a data-driven framework. In this work we adress this challenge and develop a novel Neural-Network-based (NN-based) Kalman filter for spatio-temporal interpolation of sea surface dynamics. Based on a data-driven probabilistic representation of spatio-temporal fields, our approach can be regarded as an alternative to classical filtering schemes such as the ensemble Kalman filters (EnKF) in data assimilation. Overall, the key features of the proposed approach are two-fold: (i) we propose a novel architecture for the stochastic representation of two dimensional (2D) geophysical dynamics based on a neural networks, (ii) we derive the associated parametric Kalman-like filtering scheme for a computationally-efficient spatio-temporal interpolation of Sea Surface Temperature (SST) fields. We illustrate the relevance of our contribution for an OSSE (Observing System Simulation Experiment) in a case-study region off South Africa. Our numerical experiments report significant improvements in terms of reconstruction performance compared with operational and state-of-the-art schemes (e.g., optimal interpolation, Empirical Orthogonal Function (EOF) based interpolation and analog data assimilation).
Highlights
The spatio-temporal high resolution monitoring of sea surface geophysical parameters is of key interest for a variety of scientific fields [1,2,3].Direct observations of these geophysical tracers are provided by satellite remote sensing observations and in-situ networks
We first evaluate the patch-level interpolation performance of the proposed scheme for four patches corresponding to different dynamical modes as illustrated in Figure 2 located in the area (5° E to 75° E and latitude 25° S to 55° S)
With a view to analyzing the relevance of NN-based parametric covariance model, we apply an ensemble Kalman filter with the trained dynamical model F Ps
Summary
The spatio-temporal high resolution monitoring of sea surface geophysical parameters (e.g., temperature, salinity, ocean colour) is of key interest for a variety of scientific fields [1,2,3]. Direct observations of these geophysical tracers are provided by satellite remote sensing observations and in-situ networks. As a consequence, providing high resolution gape free spatio-temporal fields, in both space and time, based on these observations have long been a crucial challenge that motivated the development of several spatio-temporal interpolation tools. Fine scale components in the other hand may hardly be retrieved with such approaches and a variety of research studies aim to improve the reconstruction of high-resolution components of spatio-temporal fields
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