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Next: 2.13.5 Lateral dissipation
Up: 2.13 Flux-form momentum equations
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For the non-hydrostatic equations, dropping the thin-atmosphere
approximation re-introduces metric terms involving and are
required to conserve angular momentum:
Because we are always consistent, even if consistently wrong, we have,
in the past, used a different discretization in the model which is:
Next: 2.13.5 Lateral dissipation
Up: 2.13 Flux-form momentum equations
Previous: 2.13.3 Curvature metric terms
Contents
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