2Drelief
Case description
The 2Drelief case simulates the interaction between atmospheric flow and a 2D bell-shaped mountain. This is a classic test case for orographic flow dynamics and validates the model ability to reproduce mountain waves and gravity wave drag.
Configuration
Parameter |
Value |
|---|---|
Category |
Idealized cases |
Dynamics |
Non-hydrostatic |
Horizontal grid spacing |
5000 m (256x1 grid) |
Integration length |
10800 s (3 hours) |
Time step |
60 s |
Coriolis effect |
disabled |
Turbulence |
TKEL (3D) |
Cloud scheme |
NONE |
Deep convection |
NONE |
Radiation |
NONE |
Steps
Step |
Script |
|---|---|
001_prep_ideal |
run_prep_ideal_case |
002_mesonh |
run_mesonh |
Specificities
Scientific specificities
2D bell-shaped mountain (Gaussian hill) with height 500m
Horizontal domain: 256 points (10km half-width bell)
48 vertical levels from 0 to 5000m
Open western boundary, cyclic eastern boundary
10m/s westerly flow
Technical specificities
Stretched vertical grid (10m near surface, 500m near model top)
Boussinesq disabled for full compressible dynamics
Damping layer at model top (XALKTOP=0.005)
Horizontal relaxation at boundaries
Validation
Vertical velocity perturbation
Pressure perturbation
Mountain wave visualization
Numerical ressources
Single CPU (1 node, 1 core)
References
Gallus, W.A., and R.A. Ahmadov (2021): Sensitivity of simulated 24-h forecasts to horizontal resolution in the US. Atmosphere, 12, 1686.