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[Regional Climate Modeling] [Teaching] [Publications]
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Three-dimensional hydrostatic primitive equation model that utilizes the terrain-following normalized pressure (sigma-p) coordinate in the vertical. Arakawa staggered C grid is used in both horizontal and vertical directions. The model has prognostic equation for momentum, heat, surface pressure, turbulent kinetic energy (TKE), and all phases of water. Forward-backward scheme (Sun 1984) is used for terms involved in the inertial gravity waves. Horizontal advection is computed using a combination of Crowley fourth-order and Gadd scheme (Sun 1993). The pressure gradient force terms are computed by the introduction of a local reference (Sun 1995). Time-splitting technique is used in time integrations. |
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