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Intro

MPAS stands for Model for Prediction Across Scales. It is a "collaborative project" for building earth system model components that can be run at multiple scales. MPAS-A is the atmospheric component of MPAS. Often, at least in our circles, "MPAS" means the standalone version of MPAS-A. But it's important to remember that there are other MPAS component models1, and MPAS-A has also been used in larger modeling systems, e.g. as the atmosphere component2 or as the dynamical core only3.

History

https://doi.org/10.1175/MWR-D-10-05056.1 https://doi.org/10.1175/MWR-D-11-00215.1

Meshes

:alt: Global variable-resolution mesh
:width: 300px

What makes MPAS special is its use of unstructured Voronoi meshes on the sphere (SCVT), including C-grid staggering.

Horizontal velocity components are defined normal to the cell edges, and vertical velocity is defined at cell vertices.

There is a primal mesh (usually mostly hexagons, as above) that most variables are defined on, and a dual mesh made up of triangles formed by connecting the primal mesh cell centers. In the model outputs, vorticity is an example of a dual mesh variable.

Links

Footnotes

  1. including ocean and sea-ice, used in E3SM

  2. e.g. MPAS-CMAQ, MPAS-Hydro (in development), NOAA GSL MPAS for smoke and dust, MPAS-GOCART

  3. e.g. in CESM, part of the StormSPEED CSEM/CAM dynamical cores comparison project, and planned for UFS as an alternative to FV3