A Multiscale Nonhydrostatic Atmospheric Model Using Centroidal Voronoi Tesselations and C-Grid Staggering
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- William C. Skamarock
- National Center for Atmospheric Research,* Boulder, Colorado
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- Joseph B. Klemp
- National Center for Atmospheric Research,* Boulder, Colorado
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- Michael G. Duda
- National Center for Atmospheric Research,* Boulder, Colorado
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- Laura D. Fowler
- National Center for Atmospheric Research,* Boulder, Colorado
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- Sang-Hun Park
- National Center for Atmospheric Research,* Boulder, Colorado
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- Todd D. Ringler
- Los Alamos National Laboratory, Los Alamos, New Mexico
書誌事項
- 公開日
- 2012-09-01
- DOI
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- 10.1175/mwr-d-11-00215.1
- 公開者
- American Meteorological Society
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説明
<jats:title>Abstract</jats:title> <jats:p>The formulation of a fully compressible nonhydrostatic atmospheric model called the Model for Prediction Across Scales–Atmosphere (MPAS-A) is described. The solver is discretized using centroidal Voronoi meshes and a C-grid staggering of the prognostic variables, and it incorporates a split-explicit time-integration technique used in many existing nonhydrostatic meso- and cloud-scale models. MPAS can be applied to the globe, over limited areas of the globe, and on Cartesian planes. The Voronoi meshes are unstructured grids that permit variable horizontal resolution. These meshes allow for applications beyond uniform-resolution NWP and climate prediction, in particular allowing embedded high-resolution regions to be used for regional NWP and regional climate applications. The rationales for aspects of this formulation are discussed, and results from tests for nonhydrostatic flows on Cartesian planes and for large-scale flow on the sphere are presented. The results indicate that the solver is as accurate as existing nonhydrostatic solvers for nonhydrostatic-scale flows, and has accuracy comparable to existing global models using icosahedral (hexagonal) meshes for large-scale flows in idealized tests. Preliminary full-physics forecast results indicate that the solver formulation is robust and that the variable-resolution-mesh solutions are well resolved and exhibit no obvious problems in the mesh-transition zones.</jats:p>
収録刊行物
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- Monthly Weather Review
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Monthly Weather Review 140 (9), 3090-3105, 2012-09-01
American Meteorological Society
