Effects of Horizontal Discretization on Triangular and Hexagonal Grids on Linear Baroclinic and Symmetric Instabilities
Steffen Maa{\ss}, Sergey Danilov

TL;DR
This paper investigates how different grid discretizations, especially triangular and hexagonal, affect the accuracy and stability of simulating baroclinic instabilities in ocean models, revealing numerical subtleties and the importance of parameter calibration.
Contribution
It extends linear instability analysis to complex grids, highlighting issues with spurious modes and their dependence on flow-grid alignment, and offers guidance on parameter calibration.
Findings
Discretizations on triangular and hexagonal grids are less robust against spurious modes.
Spurious modes do not follow Galilean invariance and depend on flow alignment.
Calibrating viscosity and diffusion suppresses spurious modes effectively.
Abstract
As global ocean general circulation models are run at eddy-permitting resolutions, reproducing accurate growth rates of baroclinic instabilities is a major concern when choosing a discretization of the equations of motion. From this viewpoint, we analyze discretizations on triangular and hexagonal grids with different types of variable staggering used in several ocean circulation models. By extending the linear baroclinic instability analysis in the Eady configuration to discretizations on more complex grids, several numerical subtleties are revealed. In comparison to discretizations on quadrilateral grids, the analyzed discretizations are less robust against unstable spurious modes, partly created by the mesh geometry. Some of the subtleties arise because spurious modes on staggered triangular and hexagonal grids do not adhere to Galilean invariance. As a consequence, their growth…
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Taxonomy
TopicsOceanographic and Atmospheric Processes · Meteorological Phenomena and Simulations · Climate variability and models
