FESOM-C v.2: coastal dynamics on hybrid unstructured meshes
We describe FESOM-C, the coastal branch of the Finite-volumE Sea ice – Ocean Model (FESOM2), which shares with FESOM2 many numerical aspects, in particular its finite-volume cell-vertex discretization. Its dynamical core differs in the implementation of time stepping, the use of a terrain-following...
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Veröffentlicht in: | Geoscientific Model Development 2019-03, Vol.12 (3), p.1009-1028 |
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Format: | Artikel |
Sprache: | eng |
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Zusammenfassung: | We describe FESOM-C, the
coastal branch of the Finite-volumE Sea ice – Ocean Model (FESOM2), which
shares with FESOM2 many numerical aspects, in particular its finite-volume
cell-vertex discretization. Its dynamical core differs in the implementation
of time stepping, the use of a terrain-following vertical coordinate, and the
formulation for hybrid meshes composed of triangles and quads. The first two
distinctions were critical for coding FESOM-C as an independent branch. The
hybrid mesh capability improves numerical efficiency, since quadrilateral
cells have fewer edges than triangular cells. They do not suffer from
spurious inertial modes of the triangular cell-vertex discretization and need
less dissipation. The hybrid mesh capability allows one to use
quasi-quadrilateral unstructured meshes, with triangular cells included only
to join quadrilateral patches of different resolution or instead of strongly
deformed quadrilateral cells. The description of the model numerical part is
complemented by test cases illustrating the model performance. |
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ISSN: | 1991-9603 1991-959X 1991-962X 1991-9603 1991-962X |
DOI: | 10.5194/gmd-12-1009-2019 |