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Convection-Resolving Forecasting with the WRF Model - cmmap

Convection-Resolving Forecasting with the WRF Model - cmmap

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Advanced Research <strong>WRF</strong> Core<br />

• Nonhydrostatic, compressible flux-form equations<br />

• Terrain-following hydrostatic pressure vertical coordinate<br />

• Arakawa C-grid, two-way interacting moving nested grids<br />

• 3 rd order Runge-Kutta split-explicit time differencing<br />

• Conserves mass, momentum, dry entropy, and scalars<br />

using flux form prognostic equations<br />

• 5 th order upwind or 6 th order centered differencing<br />

for advection<br />

• Multiple physics combinations (many converted from MM5)

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