Skip to content
Cloud-Scale Model Forecasts: Extreme Sensitivity to Environmental Conditions
NSSL home
Elmore home
The COMMAS Cloud Model
Modified Klemp and Wilhelmson (1978) model
Split mode (vertically propagating sound waves solved implicitly)
Improved numerics for momentum equations
Second-order, upwind scalar advection
Monotonic for water variables
Monotonic potential temperature advection
Small numerical diffusion and phase errors compared to original KW '78
Open boundaries
Horizontally homogenous initialization, 1 km horizontal grid spacing, 70x70 km domain.
Stretched vertical grid - 43 grid levels
Kessler bulk water scheme
Convection initialized with +3.5 K warm bubble
Input soundings adjusted to remove superadiabatic layers
Previous
Next
Back to graphic form