[2759] | 1 | WRFV2 (Weather Research and Forecast) model. |
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| 2 | |
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| 3 | Contents: |
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| 4 | |
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| 5 | A) Directions for running a test case. |
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| 6 | B) List of available test cases |
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| 7 | |
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| 8 | --------------------------------------- |
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| 9 | |
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| 10 | (A) Directions for running a test case |
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| 11 | |
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| 12 | A suite of tests for the WRF model ARW (Advanced Research WRF) core |
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| 13 | can be found in the directory "test". Each subdirectory in /test |
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| 14 | contains the necessary data (except for the real data case) and |
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| 15 | input files to run the test specific to that directory. |
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| 16 | To run specific test, builld the WRF model |
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| 17 | and the necessary initialization routine by typing |
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| 18 | |
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| 19 | -> compile "test_name" |
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| 20 | |
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| 21 | in the top directory (the directory containing this README file). |
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| 22 | For example, to build the executables for the 2D (x,z) squall line |
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| 23 | example for Eulerian mass coordinate model, you would type the command |
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| 24 | "compile em_squall2d_x". |
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| 25 | |
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| 26 | after a successful build, go the the specific test directory: |
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| 27 | |
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| 28 | -> cd test/"test_name" |
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| 29 | |
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| 30 | run the initialization code |
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| 31 | |
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| 32 | -> ideal.exe |
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| 33 | |
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| 34 | and then run the simulation |
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| 35 | |
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| 36 | -> wrf.exe |
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| 37 | |
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| 38 | --------------------------------------- |
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| 39 | |
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| 40 | (B) Available Test Cases |
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| 41 | |
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| 42 | The available test cases are |
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| 43 | |
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| 44 | 1) squall2d_x (test/em_squall2d_x) |
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| 45 | |
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| 46 | 2D squall line (x,z) using Kessler microphysics |
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| 47 | and a fixed 300 m^2/s viscosity. periodicity |
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| 48 | condition used in y so that 3D model produces |
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| 49 | 2D simulation. v velocity should be zero and there |
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| 50 | should be no variation in y in the results. |
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| 51 | |
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| 52 | 2) squall2d_y (test/em_squall2d_y) |
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| 53 | |
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| 54 | Same as squall2d_x, except with (x) rotated to (y). |
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| 55 | u velocity should be zero and there |
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| 56 | should be no variation in x in the results. |
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| 57 | |
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| 58 | 3) 3D quarter-circle shear supercell simulation |
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| 59 | (test/em_quarter_ss). |
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| 60 | |
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| 61 | Left and right moving supercells are produced. |
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| 62 | See the README.quarter_ss file in the test directory |
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| 63 | for more information. |
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| 64 | |
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| 65 | 4) 2D flow over a bell-shaped hill (x,z) (test/em_hill2d_x) |
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| 66 | |
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| 67 | 10 km half-width, 2 km grid-length, 100 m high hill, |
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| 68 | 10 m/s flow, N=0.01/s, 30 km high domain, 80 levels, |
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| 69 | open radiative boundaries, absorbing upper boundary. |
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| 70 | Case is in linear hydrostatic regime, so vertical tilted |
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| 71 | waves with ~6km vertical wavelength. |
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| 72 | |
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| 73 | 5) 3D baroclinic waves (test/em_b_wave) |
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| 74 | |
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| 75 | Baroclinically unstable jet u(y,z) on an |
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| 76 | f-plane. Symmetric north and south, periodic east and west |
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| 77 | boundaries. 100 km grid size 16 km top with 4 km damping layer. |
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| 78 | 41x81 points in (x,y), 64 layers. |
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| 79 | |
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| 80 | 6) 2D gravity current (test/em_grav2d_x) |
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| 81 | |
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| 82 | Test case is described in Straka et al, |
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| 83 | INT J NUMER METH FL 17 (1): 1-22 JUL 15 1993. |
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| 84 | See the README.grav2d_x file in the test directory. |
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| 85 | |
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| 86 | 7) 3D large-eddy simulation (test/em_les) |
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| 87 | |
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| 88 | A large-eddy simulation (LES) of a free convective boundary |
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| 89 | layer (CBL) with 0 environmental wind at the initial time, and |
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| 90 | the turbulence of the free CBL driven/maintained by the |
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| 91 | specified surface heat flux. |
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| 92 | |
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| 93 | 8) 2D full physics seabreeze (test/em_seabreeze2d_x) |
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| 94 | |
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| 95 | The case is more set up now to demonstrate how to set all land |
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| 96 | variables so that full physics options may be used. Tuning is |
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| 97 | needed to produce real sea-breeze simulation at this point. |
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| 98 | |
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| 99 | 9) 3D global case (test/em_heldsuarez) |
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| 100 | |
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| 101 | A coarse-resolution global forecast case that is described in |
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| 102 | "A proposal for the intercomparison of the dynamical cores of |
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| 103 | atmospheric general circulation models" by Held and Suarez |
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| 104 | (Bulletin of the American Meteorological Society; 1994, Vol |
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| 105 | 75, 1825-1830). This test of the global solver is dry, and |
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| 106 | produces midlatitude jets, breaking midlatitude baroclinic |
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| 107 | waves, etc. |
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