source: lmdz_wrf/WRFV3/test/em_scm_xy/README.scm @ 1

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WRF: version v3.3
LMDZ: version v1818

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1This is a single column model test case.
2
3README updated 9 Feb. 2009.
4
5-------------------------------------------------------------------------
6
7Author: Josh Hacker, NCAR
8
9-------------------------------------------------------------------------
10
11Please communicate your changes so that we can all benefit from model
12improvements.
13
14-------------------------------------------------------------------------
15
16Description:  The SCM-WRF runs on a 3x3 stencil with periodic lateral
17boundary conditions in X and Y.  No horizontal gradients are supported
18in this configuration so advection is absent unless explicitly imposed.
19The formulation for advection in the current version, coded in
20module_scm_force.F, is an upstream relaxation following Ghan et al. (1999).
21
22-------------------------------------------------------------------------
23
24Initialization: As with the other test cases, initialization is handled
25with text files input to ideal.exe (via module_initialize_scm_xy.F).
26Here we use both files input_sounding and input_soil.  The format for
27input_sounding is the surface followed by the sounding:
28
29z_terrain u_10 v_10 t_2 q_2 psfc
30z u v theta qv
31. . .   .    .
32. . .   .    .
33. . .   .    .
34
35Here z is in meters, u and v are in m/s, theta is in K, and qv is in
36kg^3/kg^3.  The number of levels does not matter as long as z_top <=
37the top level in input_sounding.  The format for input soil is the skin
38and deep soil temperatures followed by the soil level data:
39
400.0  TSK   TMN
41z    SOILT SOILM
42.    .     .
43.    .     .
44.    .     .
45
46Here z is positive downward, in meters.  TSK, SOILT, and TMN are in K,
47and SOILM is the volumetric soil moisture fraction.  Initialization of
48the soil uses the modules for real-data cases with your specified LSM,
49so use wisely.
50
51-------------------------------------------------------------------------
52
53Forcing:  Solar forcing will follow the dates as specified in the
54namelist.  All other forcing (U_g, V_g, W, and advection) are specified
55in a file that comes in via an auxilliary input.  For example:
56
57&time_control
58auxinput3_inname                    = "force_ideal.nc"
59auxinput3_interval_h                = 59
60
61This file looks very much like wrfbdy_d01 and in fact is used in the
62same way, with values specified at the intervals and tendencies on
63those values valid for the period within the corresponding interval.
64Thus time-dependent forcing on time-dependent height coordinates is
65possible; one simply needs to use multiple intervals.
66
67A script to produce a two-time level (i.e. constant) forcing is
68available, and is called make_scm_forcing.ncl.  See the documentation
69at the beginning of this.  The example that comes with the release is
70documented below.  I have a much more sophisticated script to create
71forcing from a series of met_em files.  Please contact me if you would
72like to work with me on that (hacker at ucar.edu).
73
74-------------------------------------------------------------------------
75
76Namelist: For namelist parameters, see README.namelist.  Non-SCM namelist
77parameters that must be set to get the expected behavior are:
78
79&dynamics
80pert_coriolis                       = .true.,
81
82&bdy_control
83periodic_x                          = .true.,
84periodic_y                          = .true.,
85(all others false)
86
87-------------------------------------------------------------------------
88
89Example:  This example is based on the GABLS II intercomparison case.
90It it not the GABLS II intercomparison case for a number of reasons,
91but the two most important are (1) no advection, and (2) it does not
92specify surface fluxes for forcing.  The advection in GABLES is specified
93differently and this approach was not implemented in this version.
94Also, code to force with surface fluxes still needs to be developed.
95Again, please communicate with me if you would like to do this.
96
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