Kelvin-wave induced equatorial current that get's unstable. 3200x800 grid points, dx=2.5km. Tracer is only injected on the western boundary.
Rossby waves in atmosphere/ocean communicate changes in forcing globally/across an ocean basin. Wave front leaves the adjusted balanced state behind. A linear equatorial adjustment on β-plane with sudden westerly wind.
Temperature in a channel simulation at 10km. Instead of using 64bit floats, only 16bit posits are used here for the entire model.
Turbulence topography in a channel simulation. Sea surface height is indicated with colour, zonal velocity with brightness (hill-shading).