Weller, H.
ORCID: https://orcid.org/0000-0003-4553-7082
(2013)
Non-orthogonal version of the arbitrary polygonal C-grid and a new diamond grid.
Geoscientific Model Development, 7.
pp. 779-797.
ISSN 1991-959X
doi: 10.5194/gmd-7-779-2014
Abstract/Summary
Quasi-uniform grids of the sphere have become popular recently since they avoid parallel scaling bottle- necks associated with the poles of latitude–longitude grids. However quasi-uniform grids of the sphere are often non- orthogonal. A version of the C-grid for arbitrary non- orthogonal grids is presented which gives some of the mimetic properties of the orthogonal C-grid. Exact energy conservation is sacrificed for improved accuracy and the re- sulting scheme numerically conserves energy and potential enstrophy well. The non-orthogonal nature means that the scheme can be used on a cubed sphere. The advantage of the cubed sphere is that it does not admit the computa- tional modes of the hexagonal or triangular C-grids. On var- ious shallow-water test cases, the non-orthogonal scheme on a cubed sphere has accuracy less than or equal to the orthog- onal scheme on an orthogonal hexagonal icosahedron. A new diamond grid is presented consisting of quasi- uniform quadrilaterals which is more nearly orthogonal than the equal-angle cubed sphere but with otherwise similar properties. It performs better than the cubed sphere in ev- ery way and should be used instead in codes which allow a flexible grid structure.
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| Item Type | Article |
| URI | https://reading-clone.eprints-hosting.org/id/eprint/35337 |
| Identification Number/DOI | 10.5194/gmd-7-779-2014 |
| Refereed | Yes |
| Divisions | Science > School of Mathematical, Physical and Computational Sciences > Department of Meteorology |
| Publisher | Copernicus |
| Download/View statistics | View download statistics for this item |
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