A Multiscale Nonhydrostatic Atmospheric Model Using Centroidal Voronoi Tesselations and C-Grid Staggering

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A review on regional convection‐permitting climate modeling: Demonstrations, prospects, and challenges (2015, methodology): “The fourth approach uses stretched-grid models [e.g., Schmidt, 1977; Staniforth and Mitchell, 1978] or variable resolution models [e.g., Skamarock et al., 2012; Rauscher et al., 2013; Hagos et al., 2013] to reduce the regional grid spacing over areas of interest, while larger grid spacing is used…”
The Non-hydrostatic Icosahedral Atmospheric Model: description and development (2014, background): “Global non-hydrostatic models using icosahedral grids are also being developed by several international groups including the geodesic grid model at Colorado State University (UZIM; http://www.cmmap.org/ research/models.html), the Icosahedral Non-hydrostatic model (ICON) at the Deutscher Wetterdienst”
A Description of the Advanced Research WRF Model Version 4 (2019, methodology): “Use of Θm as the prognostic thermodynamic variable is also consistent with formulation used in the Model for Prediction Across Scales (MPAS), which utilizes similar split-explicit numerics (Skamarock et al., 2012).”
A multi-resolution approach to global ocean modeling (2013, methodology): “, 2013) and non-hydrostatic (Skamarock et al., 2012) primitive equations.”