Chapter 4: WRF Initialization

Table of Contents

• Introduction
• Initialization for Ideal Data Cases
• Initialization for Real Data Cases

Introduction

The WRF model has two large classes of simulations that it is able to generate: those with an ideal initialization and those utilizing real data. The idealized simulations typically manufacture an initial condition file for the WRF model from an existing 1-D or 2-D sounding and assume a simplified orography. The real-data cases usually require pre-processing from the WPS package, which provides atmospheric and static fields with a fidelity appropriate to the chosen grid resolution for the model. The WRF model itself is not altered by choosing one initialization option over another, but the WRF pre-processors, the real.exe and ideal.exe programs, are specifically built based upon a user's selection.

The real.exe and ideal.exe programs are never used together. Both the real.exe and ideal.exe are the programs that are processed just prior to the WRF model run.

The ideal vs real cases are divided as follows:

• Ideal cases – initialization programs named “ideal.exe”
• 3d

_ em_b_wave - baroclinic wave, 100 km

_ em_heldsuarez – global case with polar filtering, 625 km

_ em_les – large eddy simulation, 100 m

_ em_quarter_ss - super cell, 2 km

• 2d

_ em_grav2d_x – gravity current, 100 m

_ em_hill2d_x – flow over a hill, 2 km

_ em_seabreeze – water and land, 2 km, full physics

_ em_squall2d_x – squall line, 250 m

_ em_squall2d_y – transpose of above problem

• Real data cases – initialization program named “real.exe”
• em_real – examples from 4 to 30 km

The selection of the type of forecast is made when issuing the ./compile statement. When selecting a different case to study, the code must be re-compiled to choose the correct initialization model. For example, after configuring the setup for the architecture, if the user issues the command ./compile em_real, then the initialization program is built using module_initialize_real.F as the target module (one of the ./WRFV3/dyn_em/module_initialize_*.F files). Similarly, if the users specifies ./compile em_les, then the Fortran module for the large eddy simulation (module_initialize_les.F) is automatically inserted into the build for ideal.exe. In each of these initialization modules, the same sort of activities goes on:

• compute a base state / reference profile for geopotential and column pressure
• compute the perturbations from the base state for geopotential and column pressure
• initialize meteorological variables: u, v, potential temperature, vapor mixing ratio
• initialize static fields for the projection and the physical surface; for many of the idealized cases, these are simplified initializations such as map factors set to one, and topography elevation set to zero

Both the real.exe program and ideal.exe programs share a large portion of source code, to handle the following duties:

• read data from the namelist
• allocate space
• generate initial condition file

The real-data case does some additional processing:

• read input data from the WRF Preprocessing System (WPS)
• compute dry surface pressure, model levels, and vertically interpolate data
• prepare soil fields for use in model (usually, vertical interpolation to the requested levels)
• check to verify soil categories, land use, land mask, soil temperature, sea surface temperature are all consistent with each other
• multiple input time periods are processed to generate the lateral boundary conditions, which are required unless processing a global forecast
• 3d boundary data (u, v, potential temperature, vapor mixing ratio, total geopotential) are coupled with map factors (on the correct staggering) and total column pressure

The “real.exe” program may be run as either a serial or a distributed memory job. Since the idealized cases only require that the initialization run for a single time period (no lateral boundary file is required) and are therefore quick to process, all of the “ideal.exe” programs should be run on a single processor as a serial job.

Initialization for Ideal Cases

The program "ideal.exe" is the program in the WRF system to run with a controlled scenario. Typically this program requires no input except for the namelist.input and the input_sounding files (except for the b_wave case which uses a 2-D binary sounding file). The program outputs the wrfinput_d01 file that is read by the WRF model executable ("wrf.exe") . Since no external data is required to run the idealized cases, even for researchers interested in real-data cases, the idealized simulations are an easy way to insure that the model is working correctly on a particular architecture and compiler.

Idealized runs can use any of the boundary conditions except "specified", and are not, by default, set up to run with sophisticated physics (other than from microphysics). Most have are no radiation, surface fluxes or frictional effects (other than the sea breeze case, LES, and the global Held-Suarez). The idealized cases are mostly useful for dynamical studies, reproducing converged or otherwise known solutions, and idealized cloud modeling.

There are 2d and 3d examples of idealized cases, with and without topography, and with and without an initial thermal perturbation. The namelist can control the size of domain, number of vertical levels, model top height, grid size, time step, diffusion and damping properties, boundary conditions, and physics options. A large number of existing namelist settings are already found within each of the directories associated with a particular case.

The input_sounding (also already in appropriate case directories) can be any set of levels that goes at least up to the model top height (ztop) in the namelist. The first line is the surface pressure (hPa), potential temperature (K) and moisture mixing ratio (g/kg). Each subsequent line has five input values: height (meters above sea-level), potential temperature (K), vapor mixing ratio (g/kg), x-direction wind component (m/s), y-direction wind component (m/s). The “ideal.exe” program interpolates the data from the input_sounding file, and will extrapolate if not enough data is provided.

The base state sounding for idealized cases is the initial sounding minus the moisture, and so does not have to be defined separately. Note for the baroclinic wave case: a 1-D input sounding is not used because the initial 3d arrays are read in from the file input_jet. This means for the baroclinic wave case the namelist.input file cannot be used to change the horizontal or vertical dimensions.

Making modifications apart from namelist-controlled options or soundings has to be done by editing the Fortran code. Such modifications would include changing the topography, the distribution of vertical levels, the properties of an initialization bubble, or preparing a case to use more physics, such as a land-surface model. The Fortran code to edit is contained in ./WRFV3/dyn_em/module_initialize_[case].F, where [case] is the case chosen in compilation, e.g. module_initialize_squall2d_x.F. The subroutine to modify is init_domain_rk. To change the vertical levels, only the 1d array znw must be defined, containing the full levels starting from 1 at k=1 and ending with 0 at k=kde. To change the topography, only the 2d array ht(i,j) must be defined, making sure it is periodic if those boundary conditions are used. To change the bubble, search for the string "bubble" to locate the code to change.

Each of the cases provide an excellent set of examples to the user. The method to specify a thermal bubble is given in the super cell case. In the hill2d case, the topography is accounted for properly in setting up the initial 3d arrays, so that example should be followed for any topography cases. A symmetry example in the squall line cases tests that your indexing modifications are correct.

Available Ideal Test Cases

The available test cases are

1. squall2d_x (test/em_squall2d_x)
• 2D squall line (x,z) using Kessler microphysics and a fixed 300 m^2/s viscosity.
• periodicity condition used in y so that 3D model produces 2D simulation.
• v velocity should be zero and there should be no variation in y in the results.
2. squall2d_y (test/em_squall2d_y)
• Same as squall2d_x, except with (x) rotated to (y).
• u velocity should be zero and there should be no variation in x in the results.
3. 3D quarter-circle shear supercell simulation (test/em_quarter_ss).
• Left and right moving supercells are produced.
• See the README.quarter_ss file in the test directory for more information.
4. 2D flow over a bell-shaped hill (x,z) (test/em_hill2d_x)
• 10 km half-width, 2 km grid-length, 100 m high hill, 10 m/s flow, N=0.01/s, 30 km high domain, 80 levels, open radiative boundaries, absorbing upper boundary.
• Case is in linear hydrostatic regime, so vertical tilted waves with ~6km vertical wavelength.
5. 3D baroclinic waves (test/em_b_wave)
• Baroclinically unstable jet u(y,z) on an f-plane.
• Symmetric north and south, periodic east and west boundaries.
• 100 km grid size 16 km top with 4 km damping layer.
• 41x81 points in (x,y), 64 layers.
6. 2D gravity current (test/em_grav2d_x)
• Test case is described in Straka et al, INT J NUMER METH FL 17 (1): 1-22 JUL 15 1993.
• See the README.grav2d_x file in the test directory.
7. 2D sea breeze (test/em_seabreeze_x)
• 2 km grid size, 20 km top, land/ water.
• Can be run with full physics, radiation, surface, boundary layer, land options.
8. 3D large eddy simulation (test/em_les)
• 100 m grid size, 2 km top.
• Surface layer physics with fluxes.
• Doubly periodic
9. 3D Held-Suarez (test/em_heldsuarez)
• global domain, 625 km in x-direction, 556 km in y-direction, 120 km top.
• Radiation, polar filter above 45^o.
• Period in x-direction, polar boundary conditions in y-direction

Initialization for Real Data Cases

The real-data WRF cases are those that have the input data to the “real.exe” program provided by the WRF Preprocessing System (WPS). This data from the WPS was originally generated from a previously run external analysis or forecast model. The original data was probably in GriB format and was probably ingested into the WPS by first ftp'ing the raw GriB data from one of the national weather agencies’ anonymous ftp sites.

For example, suppose a WRF forecast is desired with the following criteria:

• 2000 January 24 1200 UTC through January 25 1200 UTC
• the original GriB data is available at 6 h increments

The following files will be generated by the WPS:

• met_em.d01.2000-01-24_12:00:00
• met_em.d01.2000-01-24_18:00:00
• met_em.d01.2000-01-25_00:00:00
• met_em.d01.2000-01-25_06:00:00
• met_em.d01.2000-01-25_12:00:00

The convention is to use "met" to signify data that is output from the WPS “metgrid.exe” program and input into the “real.exe” program. The "d01" portion of the name identifies to which domain this data refers, which permits nesting. The trailing characters are the date, where each WPS output file has only a single time-slice of processed data. For regional forecasts, multiple time periods must be processed by “real.exe” so that a lateral boundary file is available to the model. The global option for WRF requires only an initial condition.

The WPS package delivers data that is ready to be used in the WRF system by the “real.exe” program.

• The data adheres to the WRF IO API. Unless you are developing special tools, stick with the netCDF option to communicate between the WPS package and “real.exe”.
• The data has already been horizontally interpolated to the correct grid-point staggering for each variable, and the winds are correctly rotated to the WRF model projection.
• 3D meteorological data from the WPS: pressure, u, v, potential temperature, vapor mixing ratio, geopotential height
• 3D surface data from the WPS: soil temperature, soil moisture, soil liquid
• 2D meteorological data from the WPS: land sea mask, sea level pressure, sea surface temperature, sea ice, snow depth, water equivalent snow depth, canopy water
• 2D static data for the physical surface: terrain elevation, land use categories, soil texture categories, temporally interpolated monthly data, elevation of the input model’s topography
• 2D static data for the projection: map factors, Coriolis, projection rotation
• 1D array of the vertical coordinate
• constants: domain size, date

Real Data Test Case: 2000 January 24/12 through 25/12

• A test data set is accessible from the WRF download page. Under the "WRF Model Test Data" list, select the January data. This is a 74x61, 30-km domain centered over the eastern US.
• make sure you have successfully built the code (fine-grid nested initial data is available in the download, so the code may be built with the basic nest option), ./WRFV3/main/real.exe and ./WRFV3/main/wrf.exe both exist
• in the ./WRFV3/test/em_real directory, copy the namelist for the January case to the default name (cp namelist.input.jan00 namelist.input)
• link the WPS files (the “met_em*” files from the download) into the ./WRFV3/test/em_real directory
• for a single processor, to execute the real program, type real.exe (this should take less than a minute for this small case with five time periods)
• after running the real.exe program, the files “wrfinput_d01” and “wrfbdy_d01” should be in the directory, these will be directly used by the WRF model
• the “wrf.exe” program is executed next (type wrf.exe), this should take a few minutes (only a 12 h forecast is requested in the namelist file)
• the output file wrfout_d01:2000-01-24_12:00:00 should contain a 12-h forecast at 3-h intervals