WRF EMS MODEL RUN SUMMARY FOR ch_nest Scheduled Processors WRF REAL program WRF NMM core -------------------------------------------------------------------------------- Machine wrfpc : 04 04 Total Processors : 04 04 Domain Decomposition : Internal Internal Active Domains Domain 01 Domain 02 Domain 03 -------------------------------------------------------------------------------------------------------- Domain & Run Information Primary Time Step : 28.08 Seconds 9.36 Seconds 3.11 Seconds Grid dimentions (NX x NY) : 36 x 62 64 x 82 55 x 94 Vertical Layers (NZ) : 45 45 45 Grid Spacing : 13.89km 4.63 km 1.54 km Top of Model Atmosphere : 50mb 50mb 50mb Parent Domain : NA Domain 01 Domain 02 Nesting Feedback : Feedback Off Feedback Off Feedback Off Timing Information Start Date : 2012 Feb 22 18:00 UTC 2012 Feb 22 18:00 UTC 2012 Feb 23 00:00 UTC End Date : 2012 Feb 26 18:00 UTC 2012 Feb 26 18:00 UTC 2012 Feb 25 00:00 UTC Simulation Length : 96 Hours 96 Hours 48 Hours Boundry Update Freq : 03 Hours Restart File Interval : 06 Hours 06 Hours 06 Hours File Output Information File Output Freq : 01 Hour 30 Minutes 30 Minutes Output File Format : netCDF netCDF netCDF Adjust Ouput Times : Yes Yes Yes Model Physics Dynamics : Non-Hydrostatic Non-Hydrostatic Non-Hydrostatic Cumulus Scheme : Betts-Miller-Janjic None None Microphysics Scheme : Thompson Double-Moment 6-Class Thompson Double-Moment 6-Class Thompson Double-Moment 6-Class PBL Scheme : Mellor-Yamada-Janjic Mellor-Yamada-Janjic Mellor-Yamada-Janjic Land Surface Scheme : Noah 4-Layer LSM Noah 4-Layer LSM Noah 4-Layer LSM Number Soil Layers : 4 4 4 Surface Layer Physics : Monin-Obukhov (Janjic) Monin-Obukhov (Janjic) Monin-Obukhov (Janjic) Long Wave Radiation : RRTM RRTM RRTM Short Wave Radiation : GFDL Short Wave Radiation GFDL Short Wave Radiation GFDL Short Wave Radiation NMM Core Model Dynamics Dynamics : Non-Hydrostatic Non-Hydrostatic Non-Hydrostatic Gravity Wave Drag : Off Off Off Time-Integration : Horizontally propagating fast-waves - Forward-backward scheme : Vertically propagating sound waves - Implicit scheme Horizontal : Adams-Bashforth Vertical : Crank-Nicholson Advection of T, U, and V Horizontal : Energy and enstrophy conserving, quadratic conservative, 2nd order Vertical : Quadratic conservative, 2nd Order TKE and Moisture Adv : Explicit, Upstream, Flux-Corrected, Positive Definite, Conservative Vertical Diffusion : Handled by PBL and Surface Layer Schemes Lateral Diffusion : Smagorinsky Non-linear Approach Divergence Damping : Horizontal component of divergence is damped