source: lmdz_wrf/WRFV3/test/em_quarter_ss/README.quarter_ss @ 1

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WRF: version v3.3
LMDZ: version v1818

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1em_quarter_ss test case:
2
3This test case produces a simulation of a supercell
4thunderstorm.  The environmental wind makes a
5"quarter circle" when plotted on a hodograph, and
6is commonly referred to as "quarter circle shear".
7"ss" refers to "super-cell".
8
9The default version of this test case uses a constant
10eddy viscosity for turbulent mixing ->
11diff_opt=1 and km_opt = 1 in namelist.input.
12The Coriolis terms in the model are off (f = 0)
13
14The prognostic TKE can be activated by setting
15diff_opt=2 and km_opt = 2 (see README.namelist).
16
17In idealized cloud model simulations, it is common practice
18to use Coriolis forcing calculated from wind fields defined
19as perturbations from the initial sounding.  This option
20can be activated by setting the "dynamics" namelist option
21"pert_coriolis = .true."  (the default is false).
22Additionally, the value of the Coriolis parameter "f"
23will need to be reset (from zero to the desired value)
24in WRFV1/dyn_em/module_initialize_quarter_ss.F, and
25the initial state recomputed.
26
27Also, a constant surface drag and heat flux can be specified
28in the TKE formulation by setting the "dynamics" namelist option
29"tke_drag_coefficient = Cd",
30"tke_heat_flux = S".
31The default values are zero.  Please note that these are
32specified constants; the formulations do not make use of
33similarity theory.  These momentum and heat fluxes will
34not be active if surface and boundary layer formulations are
35activated in the model physics.
36
37The sounding used in this case is from Weisman and Klemp, MWR 1982, 504-520,
38with subtle different in mixing ratio above troposphere.
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