source: lmdz_wrf/trunk/WRFV3/README_test_cases @ 2795

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1WRFV3 (Weather Research and Forecast) model.   
2
3Contents:
4
5A) Directions for running a test case.
6B) List of available test cases
7
8---------------------------------------
9
10(A)  Directions for running a test case
11
12A suite of tests for the WRF model ARW (Advanced Research WRF) core
13can be found in the directory "test".  Each subdirectory in /test
14contains the necessary data (except for the real data case) and
15input files to run the test specific to that directory. 
16To run specific test, builld the WRF model
17and the necessary initialization routine by typing
18
19-> compile "test_name"
20
21in the top directory (the directory containing this README file).
22For example, to build the executables for the 2D (x,z) squall line
23example for Eulerian mass coordinate model, you would type the command
24"compile em_squall2d_x".
25
26after a successful build, go the the specific test directory:
27
28-> cd test/"test_name"
29
30run the initialization code
31
32-> ideal.exe
33
34and then run the simulation
35
36-> wrf.exe
37
38---------------------------------------
39
40(B) Available Test Cases
41
42The available test cases are
43
441) squall2d_x (test/em_squall2d_x)
45
46   2D squall line (x,z) using Kessler microphysics
47   and a fixed 300 m^2/s viscosity.  periodicity
48   condition used in y so that 3D model produces
49   2D simulation.  v velocity  should be zero and there
50   should be no variation in y in the results.
51
522) squall2d_y (test/em_squall2d_y)
53
54   Same as squall2d_x, except with (x) rotated to (y).
55   u velocity  should be zero and there
56   should be no variation in x in the results.
57
583) 3D quarter-circle shear supercell simulation
59   (test/em_quarter_ss).
60
61   Left and right moving supercells are produced.
62   See the README.quarter_ss file in the test directory
63   for more information.
64
654) 2D flow over a bell-shaped hill (x,z) (test/em_hill2d_x)
66
67   10 km half-width, 2 km grid-length, 100 m high hill,
68   10 m/s flow, N=0.01/s, 30 km high domain, 80 levels,
69   open radiative boundaries, absorbing upper boundary.
70   Case is in linear hydrostatic regime, so vertical tilted
71   waves with ~6km vertical wavelength.
72
735) 3D baroclinic waves (test/em_b_wave)
74
75   Baroclinically unstable jet u(y,z) on an
76   f-plane.  Symmetric north and south, periodic east and west
77   boundaries.  100 km grid size 16 km top with 4 km damping layer.
78   41x81 points in (x,y), 64 layers.
79
806) 2D gravity current (test/em_grav2d_x)
81
82   Test case is described in Straka et al,
83   INT J NUMER METH FL 17 (1): 1-22 JUL 15 1993.
84   See the README.grav2d_x file in the test directory.
85
867) 3D large-eddy simulation (test/em_les)
87
88   A large-eddy simulation (LES) of a free convective boundary
89   layer (CBL) with 0 environmental wind at the initial time, and
90   the turbulence of the free CBL driven/maintained by the
91   specified surface heat flux.
92
938) 2D full physics seabreeze (test/em_seabreeze2d_x)
94
95   The case is more set up now to demonstrate how to set all land
96   variables so that full physics options may be used. Tuning is
97   needed to produce real sea-breeze simulation at this point.
98
999) 3D global case (test/em_heldsuarez)
100
101   A coarse-resolution global forecast case that is described in
102   "A proposal for the intercomparison of the dynamical cores of
103   atmospheric general circulation models" by Held and Suarez
104   (Bulletin of the American Meteorological Society; 1994, Vol
105   75, 1825-1830).  This test of the global solver is dry, and
106   produces  midlatitude jets, breaking midlatitude baroclinic
107   waves, etc.
108
10910) Single column model (test/em_scm_xy)
110
11111) 3D tropical cyclone (test/em_tropical_cyclone)
112
113   Idealized tropical cyclone on an f-plane with constant SST in a
114   specified environment.  Uses capped Newtonian relaxation to mimic
115   longwave radiation.  The default setup uses the Jordan (1958) mean
116   hurricane sounding with 28 C SST and no background winds.  The
117   analytic initial vortex is from Rotunno and Emanuel (1987).  This
118   case is useful for testing the effects of new model code (e.g.,
119   new physics options) on tropical cyclones in an idealized framework.
120
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