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The two-layer quasi-geostrophic equations (2QGE) serve as a simplified model for simulating wind-driven, stratified ocean flows. However, their numerical simulation remains computationally expensive due to the need for high-resolution meshes to capture a wide range of turbulent scales. This becomes especially problematic when several simulations need to be run because of, e.g., uncertainty in the parameter settings.
 
             -width. This results in reduced-order models that are both inefficient and inaccurate.
 -width. This results in reduced-order models that are both inefficient and inaccurate.