WRF - Developmental Testbed Center

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:BOTTOM-TOP_PATCH_END_STAG = 28 ;:DX = 0.289143f ;:DY = 0.287764f ;:DT = 90.f ;:CEN_LAT = 32.f ;:CEN_LON = -83.f ;:TRUELAT1 = 1.e+20f ;:TRUELAT2 = 1.e+20f ;:MOAD_CEN_LAT = 0.f ;:STAND_LON = 1.e+20f ;:GMT = 0.f ;:JULYR = 2008 ;:JULDAY = 11 ;:MAP_PROJ = 203 ;:MMINLU = "USGS" ;:NUM_LAND_CAT = 24 ;:ISWATER = 16 ;:ISLAKE = -1 ;:ISICE = 24 ;:ISURBAN = 1 ;:ISOILWATER = 14 ;:I_PARENT_START = 1 ;:J_PARENT_START = 1 ;}Extended Reference List for WRF-NMM Dynamics and PhysicsArakawa, A., and W. H. Schubert, 1974: Interaction of a cumulus cloud ensemble withthe large scale environment. Part I. J. Atmos. Sci., 31, 674-701.Chen, F., Z. Janjic and K. Mitchell, 1997: Impact of atmospheric surface-layerparameterization in the new land-surface scheme of the NCEP mesoscale Eta model.Boundary-Layer Meteorology, 48Chen, S.-H., and W.-Y. Sun, 2002: A one-dimensional time dependent cloud model. J.Meteor. Soc. Japan, 80, 99–118.Chen, F., and J. Dudhia, 2001: Coupling an advanced land-surface/ hydrology modelwith the Penn State/ NCAR MM5 modeling system. Part I: Model description andimplementation. Mon. Wea. Rev., 129, 569–585.Chou M.-D., and M. J. Suarez, 1994: An efficient thermal infrared radiationparameterization for use in general circulation models. NASA Tech. Memo. 104606, 3,85pp.Dudhia, J., 1989: Numerical study of convection observed during the winter monsoonexperiment using a mesoscale two-dimensional model, J. Atmos. Sci., 46, 3077–3107.Ek, M. B., K. E. Mitchell, Y. Lin, E. Rogers, P. Grunmann, V. Koren, G. Gayno, and J.D. Tarpley, 2003: Implementation of NOAH land surface model advances in the NCEPWRF-NMM V3: User’s Guide 5-33
operational mesoscale Eta model. J. Geophys. Res., 108, No. D22, 8851,do1:10.1029/2002JD003296.Fels, S. B., and M. D. Schwarzkopf, 1975: The simplified exchange approximation: Anew method for radiative transfer calculations. J. Atmos. Sci., 32, 1475-1488.Ferrier, B. S., Y. Lin, T. Black, E. Rogers, and G. DiMego, 2002: Implementation of anew grid-scale cloud and precipitation scheme in the NCEP Eta model. Preprints, 15thConference on Numerical Weather Prediction, San Antonio, TX, Amer. Meteor. Soc.,280-283.Gopalakrishnan, S. G., N. Surgi, R. Tuleya and Z. Janjic, 2006. NCEP’s Two-way-Interactive-Moving-Nest NMM-WRF modeling system for Hurricane Forecasting. 27 thConf. On Hurric. Trop. Meteor. Available online athttp://ams.confex.com/ams/27Hurricanes/techprogram/paper_107899.htm.Grell, G. A., 1993: Prognostic Evaluation of Assumptions Used by CumulusParameterizations. Mon. Wea. Rev., 121, 764-787.Grell, G. A., and D. Devenyi, 2002: A generalized approach to parameterizing convectioncombining ensemble and data assimilation techniques. Geophys. Res. Lett., 29(14),Article 1693.Hong, S.-Y., J. Dudhia, and S.-H. Chen, 2004: A Revised Approach to Ice MicrophysicalProcesses for the Bulk Parameterization of Clouds and Precipitation, Mon. Wea. Rev.,132, 103–120.Hong, S.-Y., H.-M. H. Juang, and Q. Zhao, 1998: Implementation of prognostic cloudscheme for a regional spectral model, Mon. Wea. Rev., 126, 2621–2639.Hong, S.-Y., and H.-L. Pan, 1996: Nonlocal boundary layer vertical diffusion in amedium-range forecast model, Mon. Wea. Rev., 124, 2322–2339.Janjic, Z. I., 1979: Forward-backward scheme modified to prevent two-grid-intervalnoise and its application in sigma coordinate models. Contributions to AtmosphericPhysics, 52, 69-84.Janjic, Z. I., 1984: Non–linear advection schemes and energy cascade on semi–staggeredgrids. Mon. Wea. Rev, 112, 1234–1245.Janjic, Z. I., 1990: The step–mountain coordinates: physical package. Mon. Wea. Rev,118, 1429–1443.Janjic, Z. I., 1994: The step–mountain eta coordinate model: further developments of theconvection, viscous sublayer and turbulence closure schemes. Mon. Wea. Rev, 122,927–945.Janjic, Z. I., 1996a: The Mellor-Yamada level 2.5 scheme in the NCEP Eta Model. 11thConference on Numerical Weather Prediction, Norfolk, VA, 19-23 August 1996;American Meteorological Society, Boston, MA, 333-334.Janjic, Z. I., 1996b: The Surface Layer in the NCEP Eta Model. 11th Conf. on NWP,Norfolk, VA, American Meteorological Society, 354–355.Janjic, Z. I., 1997: Advection Scheme for Passive Substances in the NCEP Eta Model.Research Activities in Atmospheric and Oceanic Modeling, WMO, Geneva, CAS/JSCWGNE, 3.14.WRF-NMM V3: User’s Guide 5-34
Page 1 and 2: ForewordUser's Guide for the NMM Co
Page 3 and 4: • WPP Directory Structure 7-3•
Page 5 and 6: The WRF modeling system software is
Page 7 and 8: WRF-NMM FLOW CHARTTerrestrialDataMo
Page 9 and 10: Vendor Hardware OS CompilerCray X1
Page 11 and 12: If all of these executables are def
Page 13 and 14: Once the tar file is obtained, gunz
Page 15 and 16: HWRF is set, then (3) will be autom
Page 17 and 18: In addition to these three links, a
Page 19 and 20: • Real-data simulations• Non-hy
Page 21 and 22: k. Morrison double-moment scheme (1
Page 23 and 24: g. GFDL surface layer (88): (This s
Page 25 and 26: Other physics optionsa. gwd_opt: Gr
Page 27 and 28: to the convergence of meridians app
Page 29 and 30: Variable NamesValue(Example)Descrip
Page 39 and 40: mpirun.lsf wrf.exeand for interacti
Page 41 and 42: The boundary conditions for the nes
Page 43 and 44: Examples:1. One nest and one level
Page 45 and 46: ottom_top_stag = 28 ;soil_layers_st
Page 47 and 48: float HLENSW(Time, south_north, wes
Page 49: float HBOTS(Time, south_north, west
Page 53 and 54: Mlawer, E. J., S. J. Taubman, P. D.
Page 55 and 56: NCEP WRF Postprocessor (WPP)WPP Int
Page 57 and 58: ./configureYou will be given a list
Page 59 and 60: equested output field. If the pre-r
Page 61 and 62: RAINCV SNOW HBOTRAINNCVSNOWCNote: F
Page 63 and 64: Running WPPFour scripts for running
Page 65 and 66: i. As the grid id of a pre-defined
Page 67 and 68: The GrADS package is available from
Page 69 and 70: Height on pressure surface HEIGHT O
Page 71 and 72: MELTPrecipitation type (4 types) -
Page 73 and 74: Press at tropopause PRESS AT TROPOP
Page 75 and 76: RIP4RIP IntroductionRIP (which stan
Page 77 and 78: A successful compilation will resul
Page 79 and 80: iinterp = 0v v v v vH V H V h h h h
Page 81 and 82: espectively, of the centered domain
Page 83 and 84: This can be either 'h' (for hours),
Page 85: eal variable expect values that are
Page 88 and 89: of all the requested trajectories a
Page 90 and 91: Creating Vis5D Dataset with RIPVis5
Page 92 and 93: User’s Guide for the NMM Core of
Page 94 and 95: Configuration: The configure script
Page 96 and 97: This program reads the contents of
Page 98 and 99: Period - Describes communications f
Page 100 and 101:
fine grid), f (forcing, how the lat
Page 102 and 103:
# halo HALO_NMM_K dyn_nmm8:q2;24:t
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(http://www.mmm.ucar.edu/wrf/WG2/Ti
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User's Guide for the NMM Core of th
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2. Make sure the files listed below
Page 110 and 111:
User's Guide for the NMM Core of th
Page 112 and 113:
Program geogridThe purpose of geogr
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1. Define a model coarse domain and
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to GEOGRID.TBL in the geogrid direc
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the GRIB data were downloaded to th
Page 120 and 121:
By this point, there is generally n
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two nests are defined to have the s
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Note: For the WRF-NMM the variables
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simulations may use a constant SST
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entire simulation domain, and data
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that lists the variables and attrib
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http://www.ecmwf.int/products/data/
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intermediate formats (metgrid/src/r
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GRIB1| Level| From | To |Param| Typ
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corresponding source grid point. Gi
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tile_x = 1200tile_y = 1200tile_z =
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1. PARENT_ID : A list of MAX_DOM in
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V -DX- H| / |DY dx DY| / |H - DX- V
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intermediate files if ungrib is to
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the index and data tiles for the da
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1. PROJECTION : A character string
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25. SCALE_FACTOR : A real value tha
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10. INTERP_MASK : The name of the f
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1. four_pt : Four-point bi-linear i
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8. search : Breadth-first search in
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19 Mixed Tundra20 Barren TundraTabl
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LU_INDEX:units = "category" ;LU_IND
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netcdf met_em.d01.2009-01-05_12:00:
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}:ISOILWATER = 14 ;:grid_id = 1 ;:p
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WRF - Developmental Testbed Center

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