A hyper-parameterization method for comprehensive ocean models: Advection of the image point

TL;DR

This paper introduces a hyper-parameterization method called 'Advection of the image point' applied to a comprehensive ocean model, significantly improving flow structure reproduction and offering flexible, efficient enhancement without modifying the original model.

Contribution

First application of the hyper-parameterization method to a real-world ocean model, improving accuracy and efficiency without model modifications.

Findings

Significant improvement in reproducing Gulf Stream features.

Method is faster and easier to implement than traditional approaches.

Can incorporate real measurement data for enhanced modeling.

Abstract

Idealized and comprehensive ocean models at low resolutions cannot reproduce nominally-resolved flow structures similar to those presented in the high-resolution solution. Although there are various underlying physical reasons for this, from the dynamical system point of view all these reasons manifest themselves as a low-resolution trajectory avoiding the phase space occupied by the reference solution (the high-resolution solution projected onto the coarse grid). In order to solve this problem, a set of hyper-parameterization methods has recently been proposed and successfully tested on idealized ocean models. In this work, for the first time we apply one of hyper-parameterization methods (Advection of the image point) to a comprehensive, rather than idealized, general circulation model of the North Atlantic. The results show that the hyper-parameterization method significantly improves a non-eddy-resolving solution towards the reference eddy-resolving solution by reproducing both the large- and small-scale features of the Gulf Stream flow. The proposed method is much faster than even a single run of the coarse-grid ocean model, requires no modification of the model, and is easy to implement. Moreover, the method can take not only the reference solution as input data but also real measurements from different sources (drifters, weather stations, etc.), or combination of both. All this offers a great flexibility to ocean modellers working with mathematical models and/or measurements.