Advection of the image point in probabilistically-reconstructed phase spaces

TL;DR

This paper introduces a probabilistic reconstruction method that improves data-driven modeling in fluid dynamics by enhancing hyper-parameterisation, demonstrating increased accuracy and speed in ocean model applications.

Contribution

The paper proposes a novel probabilistic hyper-parameterisation approach for data reconstruction, improving accuracy and computational efficiency in ocean modeling.

Findings

The HP solution outperforms NEMO in accuracy at 1/4-deg resolution.

The HP method is several orders of magnitude faster than NEMO.

Encouraging results suggest potential for operational ocean and atmospheric modeling.

Abstract

Insufficient reference data is ubiquitous in data-driven computational fluid dynamics, as it is usually too expensive to compute or impossible to observe over long enough times needed for data-driven methods. The lack of data can significantly compromise the fidelity of results computed with data-driven methods or render them inapplicable. To challenge this problem, we propose a probabilistic reconstruction method that enhances the hyper-parameterisation (HP) approach with ideas underlying the probabilistic-evolutionary approach. We offer to use the HP method ``Advection of the image point'' on data sampled from the joint probability distribution of the reference dataset. The HP method has been tested regionally on the sea surface temperature and surface relative vorticity computed with the global 1/4-deg and 1/12-deg resolution NEMO model. Our results show that the HP solution (the solution computed with the HP method) in the probabilistically-reconstructed and reduced (in terms of dimensionality) phase space at 1/4-deg resolution is more accurate than the 1/4-deg-solution computed with NEMO. Additionally, the HP solution is several orders of magnitude faster to compute than the 1/4-deg NEMO solution. The proposed method shows encouraging results for the NEMO model and the potential for the use in other operational ocean and ocean-atmospheric models for both deterministic and probabilistic predictions. Furthermore, the method can be used as a fast reanalysis tool allowing the complex dynamics of a comprehensive ocean model to be approximated by the HP solution. It can also function as a dynamic interpolation method to fill gaps in observational data.