Long-term integrations, conventionally performed with globally uniform 1˚ grids coupled to an ocean model, but may also leverage variable-resolution grids down to convection permitting scales.
Configurations for climate, weather and air-quality using increased complexity for describing chemical processes, and deeper vertical grids to resolve middle atmosphere dynamics and related chemical reactions.
Simulations using very deep vertical grids resolving the thermosphere and ionosphere, requiring the deep atmosphere equations set and magnetohydrodynamic solvers.
