GEM/4.6/gem settings.nml

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The gem_settings.nml file is the main GEM configuration file. It must be present in your experiment directory when you launch the GEM model. The gem_settings.nml file is a collection of Fortran namelist blocs.

This page describes only the settings (namelists) located in the gem_settings.nml file that are related to the input, dynamic core and RPN Physics parameterizations of GEM. Other settings are described elsewhere:

You may verify the namelist validity with the checknml tool.

Sample file: see the test cases

Contents

[hide]

1 How to update to the current gem_settings.nml

To update the gem_settings.nml from 4.5 to the current version one can use the python script gem_upcfg that becomes available after establish GEM environment

One can also read the following sections describing the changes to the gem_settings.nml and apply them by hand. In this case, it will be handy to use the script checknml which is part of GEM 4.6 environment.

2 Modifications to the Dynamic namelists

2.1 New Dynamic options

The following table gives the new options (for the complete description, please refer to the documentation below):

Parameter name Namelist Remarks
Hzd_prof_S gem_cfgs See doc below and also
Iau_cutoff gem_cfgs See doc below and also See Variable Recycling in GEM
Iau_interval gem_cfgs See doc below and also See Variable Recycling in GEM
Iau_period gem_cfgs See doc below and also See Variable Recycling in GEM
Iau_tracers_S gem_cfgs See doc below and also See Variable Recycling in GEM
Iau_weight_S gem_cfgs See doc below and also See Variable Recycling in GEM
Schm_bitpattern_L gem_cfgs See doc below
Fcst_start_S step See doc below
Fcst_end_S step See doc below
Var_UU gement See doc below
Var_TT gement See doc below
Var_W gement See doc below
Var_ZD gement See doc below
Var_Q gement See doc below

2.2 Other changes to the Dynamic namelists

The following table gives the other changes that were made the namelists parameters (for the complete description, please refer to the documentation below):

Old parameter name New parameter name Remarks
Step_total Fcst_end_S see complete documentation below Data type is now a character not an integer

3 Modifications to the Physics namelist

3.1 New Physics options

Parameter name Remark
acchr See doc below
fnnmod See doc below
z0hcon See doc below
z0mtype See doc below

3.2 Deleted Physics option

The following keys must be removed from the gem_settings.nml.

Parameter name Remark

4 Complete documentation

*_____________________________________________________________________________
* FILE gem_settings.nml
*_____________________________________________________________________________|

*_____________________________________________________________________________
* |
* PTOPO namelist (obsolete: look in configexp.cfg) |
*_____________________________________________________________________________|

*_____________________________________________________________________________
* |
* GRID namelist |
*_____________________________________________________________________________|
* | | |
* NAME | DESCRIPTION |DEFVAL|
*--------------------|-------------------------------------------------|----- |
* Grd_dx | mesh length (resolution) in x-direction(degrees)| 0. |
* | for the LU grid or the uniform portion of GV grid |
* Grd_dxmax | maximum grid point spacing along x (degrees) | 360. |
* | for the GV grid only | |
* Grd_dy | mesh length (resolution) in y-direction(degrees)| 0. |
* | for the LU grid or the uniform portion of GV grid |
* Grd_dymax | maximum grid point spacing along y (degrees) | 180. |
* | for the GV grid only | |
*--------------------|-------------------------------------------------| |
* Grd_gauss_L | .TRUE. to set for a Gaussian grid |false |
*--------------------|-------------------------------------------------| |
The following 4 parameters apply only for LAM grids | |
* Grd_iref | I reference point (within Grd_ni) | 1 |
* Grd_jref | J reference point (within Grd_nj) | 1 |
* Grd_latr | latitude on rotated grid of reference point | 0. |
* | (Grd_iref,Grd_jref)| |
* Grd_lonr | longitude on rotated grid of reference point | 0. |
* | (Grd_iref,Grd_jref)| |
* | ie: reference point on centre of grid 401x301 | |
* Grd_iref=201,Grd_jref=151,Grd_latr=0.,Grd_lonr=180. | |
* | ie: reference point on centre of grid 400x300 | |
* | where Grd_dx =.14,Grd_dy = .44, | |
* | Grd_iref=201, Grd_jref=151, | |
* | Grd_lonr=180.07, Grd_latr=0.22, | |
*--------------------|-------------------------------------------------| |
* Grd_maxcfl | Determines the # of points for the pilot region | 1 |
* | for current LAM run(Glb_pil=max(1,Grd_maxcfl)+8)| |
* Grd_ni | Total number of points along X | 0 |
* | For LAM, total number of points not incl the | |
* | piloting points along x | |
* Grd_nila | number of points in x of the uniform or higher | 0 |
* | "core" resolution domain (GV grid) | |
* Grd_nj | Total number of points along Y | 0 |
* | For LAM, total number of points not incl the | |
* | piloting points along y | |
* Grd_njla | number of points in y of the uniform or higher | 0 |
* | "core" resolution domain (GV grid) | |
* Grd_typ_S | Computational grid type: first letter is G or L | "GU" |
* | for Global or Lam, second letter is U or V | |
* | for Uniform or Variable mesh | |
*--------------------|-------------------------------------------------| |
* The following four parameters define the rotation of the grid: | |
* Grd_xlat1 | geographic latitude of the center of the | 0.0 |
* | computational domain | |
* Grd_xlat2 | geographic latitude of a point on the equator of| 0.0 |
* | the computational domain | |
* Grd_xlon1 | geographic longitude of a point on the equator |180.0 |
* | of the computational domain | |
* Grd_xlon2 | geographic longitude of a point on the equator |270.0 |
* | of the computational domain | |
*-----------------------------------------------------------------------------

*_____________________________________________________________________________
* |
* GRDC namelist (definition of cascade grid) |
*_____________________________________________________________________________|
* | | |
* NAME | DESCRIPTION |DEFVAL|
*--------------------|-------------------------------------------------|------|
* Grdc_dx | x horizontal resolution of target cascade grid | -1. |
* Grdc_dy | y horizontal resolution of target cascade grid | -1. |
* Grdc_hblen | number of points for the blending zone (Hblen_x)| 10 |
* Grdc_initphy_L | TRUE to dump out permanent bus for cascade mode |false |
* Grdc_iref | I reference point (within Grdc_ni) | 1 |
* Grdc_jref | J reference point (within Grdc_nj) | 1 |
* Grdc_latr | latitude on rotated grid of reference point | 0. |
* | (Grdc_iref,Grdc_jref)| |
* Grdc_lonr | longitude on rotated grid of reference point | 0. |
* | (Grdc_iref,Grdc_jref)| |
* | ie: reference point on centre of grid 401x301 | |
* Grdc_iref=201,Grdc_jref=151,Grdc_latr=0.,Grdc_lonr=180. | |
* | ie: reference point on centre of grid 400x300 | |
* | where Grdc_dx =.14, | |
* | Grd_iref=201, Grd_jref=151, | |
* | Grd_lonr=180.07, Grd_latr=0.22, | |
* Grdc_maxcfl | Determines the # of points for the pilot region | 1 |
* | for cascade LAM (Glb_pil = max(1,Grdc_maxcfl)+5 | |
* Grdc_nbits | Number of bits for the packing factor | |
* Grdc_nfe | Nesting interval specified with digits ending |'1H' |
* | with one character for the units: | |
* | S-seconds,D-days,M-minutes,H-hours | |
* Grdc_ni | Total number of points along X | 0 |
* Grdc_nj | Total number of points along Y | 0 |
* Grdc_start_S | Time string (units D, H, M or S) from the start | '' |
* | of the run to start producing the cascade files | |
* Grdc_end_S | Time string (units D, H, M or S) from the start | '' |
* | of the run to stop producing the cascade files | |
* Grdc_trnm_S | list of tracers to be written from piloting run |'@#$%'|
*-----------------------------------------------------------------------------

*_____________________________________________________________________________
* |
* GEMENT namelist |
*_____________________________________________________________________________|
* | | |
* NAME | DESCRIPTION |DEFVAL|
*--------------------|-------------------------------------------------|------|
* Anal_cond | ice phase considered in analysis humidity field |false |
* E_schm_adcub | .true. cubic interpolation from phi to UV grid |true |
* | .false. linear interpolation | |
* E_schm_stlag | .true. cubic lagrange interpolation for U,V |true |
* | interpolation coefficients | |
* | .false. not available, error will occur | |
* E_tr3d_list_S | list of tracers to be read from analyse | |
* Var_Q | NOMVAR for q (deviation to the |'QT1' |
* | log-hydrostatic-pressure) | |
* | Choices QT1,'', set it to '' not to read q | |
* | If Var_Q='QT1' and not found, model will | |
* | set q to zero. | |
* Var_TT | NOMVAR for the temperature |'@#$%'|
* | Choices 'TT1','TT','VT' and '@#$%' (default) | |
* | If Var_TT='@#$%', model will look for temp. var | |
* | in the following order TT1, TT and VT | |
* Var_U | NOMVAR for the winds. |'@#$%'|
* | Choices 'UT1','UU' and '@#$%' (default) | |
* | If Var_U='@#$%', model will look for wind var | |
* | in the following order UT1,VT1 and UU,VV | |
* Var_W | NOMVAR for w (true vertical velocity) |'WT1' |
* | Choices 'WT1'(default),'ZZ' and '' | |
* | Set it to '' not to read w | |
* | If Var_W='WT1' the model will look for the | |
* | following varibale in order 'WT1','ZZ', if none | |
* | is found, the model will compute w | |
* | If Var_W='ZZ' and not found the model aborts | |
* Var_ZD | NOMVAR for zd (zeta dot) |'ZDT1'|
* | Choices 'ZDT1'(default),'' | |
* | set it to '' not to read zd | |
* | If choice is not found, model will compute zd | |
* Pil_bmf_L | .true. to have BMF files,.false.to have 3DF |false |
* Pil_dx | resolution of 3DF/BCS data to feed model in rad|Grd_dx|
* Pil_hblen | Number of points for blending (Hblen) | 10 |
* Pil_jobend_S | Ending date for pilot fi(yyyymmdd.hhmmss) |'@#$%'|
* Pil_jobstrt_S | Starting date for pilot fi(yyyymmdd.hhmmss) |'@#$%'|
* Pil_lancemodel | Launches the model job (system call) from the |10000 |
* | GEMNTR after 'Pil_lancemodel" timeframes (LAM) |10000 |
* Topo_clip_oro_L | to clip negative values in topography |true |
*******************************************************************************
* WARNING FOR LAM
* The following keys to filter the topography are not
* effective in LAM configuration. The model will read ME from
* the geophy file and will not apply any filtering. If you
* want the filtered topo, remove ME from the geophy file and
* zap MF to ME. The MF in the geophy file
* (produced with genphysx) is the filtered topography which
* is equivalent, to the machine precision, to what the entrance
* used to do.
*
* Topo_dgfmx_L | .true. -apply digital filter to topography |false |
* Topo_dgfms_L | .true. - consider map scale in digital filtering|true |
* | .false.- ignore map scale in digital filtering | |
* Topo_filmx_L | .true. -filtering 2 delta X topography |true |
* | .false. -no filters to topography | |
*-----------------------------------------------------------------------------

*_____________________________________________________________________________
* |
* ADW_CFGS namelist |
*_____________________________________________________________________________|
* | | |
* NAME | DESCRIPTION |DEFVAL|
*--------------------|-------------------------------------------------|------|
* Adw_gccsa_L | .true. => to improves speed computation of the |false |
* | upwind positions using | |
* | Ritchie-Beaudoin approximations | |
* | ( 1994, Mon.Wea.Rev. 122, 2391–2399).| |
* Adw_ckbd_L | .true. => to check if upstream points from north|false |
* | and south PE's are inside adv. grid | |
* | .true. => to not call the adw_ckbd subroutine | |
* Adw_exdg_L | .true. => to print points of upstream positions |false |
* | outside of advection source grid | |
* | .false.=> to not print | |
* Adw_mono_L | .true. for monotonic advection on tracers |true |
* Adw_nosetint_L | .true. to bypass adw_setint for TRILIN (intern) |false |
* Adw_stats_L | .true. to give advection statistics (glbstat) |false |
* Adw_thermopos_L | .true. to compute thermo upstream positions |false |
* | .false. iterpolated from momentum ones (faster) | |
* Adw_useadx_L | .true. to use "Adx" advection package (not Adw) |true |
*-----------------------------------------------------------------------------
*_____________________________________________________________________________
* |
* STEP namelist |
*_____________________________________________________________________________|
* | | |
* NAME | DESCRIPTION |DEFVAL|s
*--------------------|-------------------------------------------------|------|
* Step_runstrt_S | Analysis date for LAM run (yyyymmdd.hhmmss) |'@#$%'|
* Step_nesdt | Number of seconds between 2 consecutive | 0 |
* | boundary condition(BC) time frames | |
* Step_leapyears_L |  ??? | ??? |
* Step_dt | timestep used by the model | 900. |
* Step_nesdt | Nesting Time Interval in seconds | -1 |
* Step_runstrt_S | Starting date for LAM run (yyyymmdd.hhmmss) |' ' |
* Step_bkup | Number of timesteps to save a restart file for | 9999 |
* | backup if "restart" is not true. | |
* Step_gstat | Number of timesteps for a global stat (glbstat)| 9999 |
* Step_rsti | Number of timesteps to save a restart file | 9999 |
* Step_spinphy | Timestep to save "BUSPER" 9999999|
* Fcst_start_S | A time string (units D, H, M or S) for the |'0H' |
* | forecast start | |
* Fcst_end_S | A time string (units D, H, M or S) for the |'NIL' |
* | forecast end: replaces Step_total as a way to | |
* | define integration length | |
*-----------------------------------------------------------------------------
*_____________________________________________________________________________
* |
* GEM_CFGS namelist |
*_____________________________________________________________________________|
* | | |
* NAME | DESCRIPTION |DEFVAL|
*--------------------|-------------------------------------------------|------|
* Clim_climat_L | .true. for Climate mode |false |
* Clim_inincr_L | .true. to set the surface increments in Climat |false |
* Cstv_bA_8 | value for time off-centering of Semi-lag |0.6 |
* Cstv_ptop_8 | basic state pressure at the top (Pa) |-1.0 |
* Cstv_tstr_8 | T* (basic state temperature) (K) | 240.0|
* Eigv_parity_L | FOR GLOBAL only, (sol_parite_2 instead of mxma) | |
* | .true. to apply the parallel direct solution |false |
* | of high-order diffusion equation with mxma8 | |
* | using reflexion symmetry of C-grid(global) | |
* Eq_sponge | Coefficients that multiply KM to simulate | 0.0 |
* | sponge layer near the top of the model. | |
* | Warning! if this parameter is used, the EPONGE | |
* | in the physics namelist should be removed. | |
* Grd_rcoef | pair of coefficients (min,max) to control the |1.,1. |
* | flattenning of the vertical coordinate | |
*--------------------|-------------------------------------------------|------|
* HYB | array of model levels , 0.0 < HYB < 1.0 |-1.0 |
*--------------------|-------------------------------------------------|------|
* Horizontal diffusion if activated, will be applied to the following | |
* variables  : Horizontal winds, ZDot, W | |
*--------------------|-------------------------------------------------|------|
* Hzd_1d_L | true if 1D diff. (otherw. 2D) for filtering |false |
* Hzd_difva_L | Logical control for latitudinal modulation of |false |
* | the horizontal diffusion coefficient | |
* Hzd_lnr | U and V 2 delta-x removal ratio when using | -1 |
* | HO_IMP range(0.0-1.0) | |
* Hzd_lnr_theta | Theta 2 delta-x removal ratio when using | -1 |
* | HO_IMP range(0.0-1.0). If Hzd_lnr_theta <= 0 | -1 |
* | If Hzd_lnr_theta <= 0 no diffusion on theta | |
* HZD_prof_S | Vertical profile of explicit horizontal |'NIL' |
* | diffusion coefficient. Example : | |
* | Hzd_prof_S= "del2.05@1", "del2.05@.05","del2.6@.02" |
* Hzd_pwr | Hor. diffusion order on U and V when using | -1 |
* | HO_IMP del-n available: 2, 4, 6, 8 | |
* Hzd_pwr_theta | Hor. diffusion order on theta when using | -1 |
* | HO_IMP del-n available: 2, 4, 6, 8 | |
* Hzd_t0_0_L | true if winds T0 filt. in WNDTH (mode NL) |false |
* Hzd_t1_0_L | true if winds T1 filt. in WDPERS (mode NL) |false |
* Hzd_type_S | "HO_IMP" High Order implicit | NIL |
* | "NIL" for no horizontal diffusion | |
* | "HO_EXP" for a 9-point filter diffusion (LAM | |
* | mode only) | |
*--------------------|-------------------------------------------------|------|
* Horizontal diffusion of tracers | |
*--------------------|-------------------------------------------------|------|
* Hzd_pwr_tr | Tracers Hor. diffusion order when using | -1 |
* | HO del-n (n=2,4,6,8) | |
* Hzd_lnr_tr | Tracers 2 delta-x removal ratio when using | -1 |
* | HO_IMP range(0.0-1.0) | |
* Hzd_tr3d_name_S | List of tracers to be diffused | "" |
*--------------------|-------------------------------------------------|------|
* Incremental Analysis Update (IAU) | |
*--------------------|-------------------------------------------------|------|
* Iau_cutoff | The cutoff period for the 'sin' filter (in hours)| 6. |
* Iau_interval | The number of seconds between increment fields. | -1 |
* Iau_period | The number of seconds over which IAU will be | -1 |
* | will be run (typically the length of | |
* | the assimilation window). Default < 0 | |
* | means that no IAUs are applied. | |
* Iau_tracers_S | An optional list of tracers to be incremented. | "" |
* Iau_weight_S | The type of weighting function to be applied to |'constant'|
* | the analysis increments: | |
* | 'constant' (default) uniform increments | |
* | 'sin' DF-style weights (Fillion et al. 1995)| |
*--------------------|-------------------------------------------------|------|
* Init_balgm_L | true -> initialization is performed |false |
* Init_dfnp | number of points for digital filter | 5 |
* | (equals the number of timesteps +1) | |
* Init_dfpl_8 | period limit of digital filter (secs.) |21600.|
* Init_dftr_L | true -> passive tracers digitally filtered |false |
* | false-> passive tracers set to result obtained | |
* | at mid-period during initialization | |
* | period (no filtering) | |
* Init_dfwin_L | true -> windowing is applied |true |
* Lam_0ptend_L | true for Zero physics tendency in blending area |true |
* Lam_acidtest_L | true for LAM acid test |false |
* Lam_blendoro_L | true to blend the topography with the pilot |true |
* Lam_blend_H | number of points for horizontal blending |10 |
* Lam_blend_T | number of levels for top blending |0 |
* Lam_gbpil_T | number of levels for top piloting |-1 |
* Lam_ctebcs_L | true-> to force constant (fixed) boundary condit|false |
* Lam_hint_S | Types of horizontal interpolation from 3DF/BCS | |
* | files onto model grid in GEMDM: CUB_LAG|
* | 'CUB_LAG'/'LINEAR'/'NEAREST' | |
* Lam_toptt_L | true -> The plane of the top temperature layer |false |
* | is completely overwritten from the 2D pilot data| |
* Lctl_debug_L | .true. to print more information to std output |false |
* Lctl_rxstat_S | precistion in print glbstats |'LCL_4'|
* Out3_cliph_L | .true. to clip humidity variables on output |false |
* Out3_closestep | period (in timesteps) to accumulate records in | -1 |
* | one output file. -1 to have one timestep/file | -1 |
* The following are 7 switches used in the context of vertical | |
* interpolation toward pressure levels: | |
* Out3_cubdd_L | .true. for cubic interpolation for DD |true |
* Out3_cubds_L | .true. for cubic interpolation for DS |true |
* Out3_cubqq_L | .true. for cubic interpolation for QQ and QR |true |
* Out3_cubqs_L | .true. for cubic interpolation for QS and Q3 |true |
* Out3_cubuv_L | .true. for cubic interpolation for UU,VV and UV |true |
* Out3_cubww_L | .true. for cubic interpolation for WW |true |
* Out3_cubzt_L | .true. for cubic interpolation for GZ,VT and HU |true |
* Out3_debug_L | .true. to have verbose during output calls |false |
* Out3_etik_S | 'etiket' used in output fields. | ' ' |
* Out3_flipit_L | .true. to flip output from ni*nj*nk to ni*nk*nj |false |
* Out3_fullplane_L | true to trigger new output system by full planes|false |
* | This replaces the # files | |
* Out3_ip3 | default value for IP3 is 0 | 0 |
* | -1 for IP3 to contain step number, >0,given IP3 | |
* Out3_linbot | number of layers close to the bottom of the | 0 |
* | model within which a linear interpolation of GZ | |
* Out3_nbitg | Packing factor used for all variables except for| 16 |
* | those defined in Out_xnbits_s | |
* Out3_ndigits | minimum of digits used to represent output units| 3 |
* Out3_newout_L | true to get new physics output system |false |
* Out3_satues_L | .true. for humidity variables to consider |flase |
* | water/ice phase for saturation | |
* Out3_uencode_L | true to trigger direct encoding of the 'U' grid |false |
* | for yin-yang configurations | |
* Out3_unit_S | 'H' or '' for output in hours, 'P' for in steps,| '' |
* | 'S'(seconds),'M'(minutes),'D'(days) | |
* Out3_zund | list of levels for underground extrapolation | 0 |
* | and VT is done even if flcubic is .true. | |
* Out3_postfreq | Frequency in minutes at which the outputs will | 0 |
* | be done during the integration. The default | |
* | behavior is to launch a single job at the end | |
* | of the integration. | |
*--------------------|-------------------------------------------------|------|
* The following variables are to help compute latitudinal modulation of| |
* vertical diffusion coefficient on momentum by fitting a cubic btwn | |
* values P_lmvd_weigh_low_lat and P_lmvd_weigh_high_lat | |
* at latitudes P_lmvd_low_lat and P_lmvd_high_lat | |
* | |
* P_lmvd_high_lat | latitude at which the multiplication | 5.0 |
* | factor becomes P_lmvd_weigh_high_lat | |
* P_lmvd_low_lat | latitude at which the multiplication factor | 30.0 |
* | becomes P_lmvd_weigh_low_lat | |
* P_lmvd_weigh_high_lat| multiplication factor of P_pbl_spng at | 1.0 |
* | latitude P_lmvd_high_lat | |
* P_lmvd_weigh_low_lat| multiplication factor of P_pbl_spng at | 1.0 |
* | latitude P_lmvd_low_lat | |
*--------------------|-------------------------------------------------|------|
* P_pbd_dumpbus | Row statistics on physics buses content on every| 0 |
* | 'P_pbd_dumpbus' timesteps | |
* P_runlgt | Running length: width (number of points) of the | l_ni |
* | physics slice | |
*--------------------|-------------------------------------------------| |
* P_zong_nbin | number of geographical latitude bands | G_nj |
* P_zong_znli | zonal diagnostic interval in timesteps | 0 |
* P_zong_znmod | extraction mode: | 1 |
* | 1 => save variables | |
* | 2 => save the square of the variables | |
* | 3 => save both | |
* P_zong_znprf_S | list of zonal diag for profile variables | |
* P_zong_znsrf_S | list of zonal diag for surface variables | |
* P_zong_znsus_L | .true. for zonal diagnostics requested |false |
*--------------------|-------------------------------------------------| |
* perturb_nbits | Number of bits to perturb on initial conditions | 0 |
* perturb_npts | Stride for perturbation on initial conditions | 10 |
*--------------------|-------------------------------------------------| |
* Rstri_glbcol_L | .true. to write one global binary restart file |false |
* Schm_adcub_L | .true. => cubic interpolation |true |
* | .false.=> linear interpolation | |
* Schm_Adw_extrap_L | .false.=> Semi-Lag. traj. cannot go above first |false |
* | momentum level or below last momentum level | |
* | .true. => Semi-Lag. traj. can go up top model | |
* | top or to model surface. | |
* Schm_autobar_L | .true. => auto barotropic option |false |
* Schm_bitpattern_L | .true. => Modify slightly code behaviour to |false |
* | ensure bitpattern reproduction in restart mode | |
* | using FST file | |
* Schm_hydro_L | true -> hydrostatic run |false |
* | false-> non-hydrostatic run | |
* Schm_hzdadw_L | true to trigger horizontal diffusion of momentum|false |
* | at each CN iteration (default=.F.) | |
* Schm_itcn | number of iterations for Crank-Nicholson | 2 |
* Schm_itnlh | number of iterations to solve non-linear | 2 |
* | Helmholtz problem | |
* Schm_itraj | number of iterations to compute trajectories | 2 |
* Schm_modcn | frequency of Crank-Nicholson procedure | 1 |
* Schm_pcsty_L | compute physics tend. for tpt1,tplt1,tdt1,psdt1 |true |
* Schm_pheat_L | compute physics tendencies for fit1 and fipt1 |true |
* Schm_psadj_L | true -> ps adjust is activated (at every time |false |
* | step, the integral of ps over the domain| |
* | is restored to the value of the previous| |
* | time step; afterward, q and s are re- | |
* | computed;this can be done in | |
* | hydrostatic mode only)| |
* Schm_Tlift | =1 Last thermo level at momentum level | 0 |
* | =0 Last thermo level is staggered | |
* Schm_topo_L | true to have topography | true |
* Schm_wload_L | Apply water loading in the calculations |false |
* Schm_xwvt3 | type of extrapolation for wind calculation | 0 |
* | at time t-dt/2 (th): | |
* | =0 => two time levels (t1, t2) | |
* | =1 => two time levels (t1, t2) for u,v | |
* | three time levels for vertical wind | |
* | =2 => three time levels (t1, t2, t3) | |
* Sol_fgm_eps | Epsilon value for non Yin-Yang iterative solver |1.d-07|
* Sol_fgm_maxits | maximum number of iterations allowed for the |200 |
* | non Yin-Yang iterative solver | |
* Sol_fft_L | .true. to use FFT solver if possible | true |
* | .false. to use MXMA solver (slower,less precise)| |
* Sol_im | size of Krylov subspace in iterative solver |15 |
* | - should not exceed 100 | |

* Sol_precond_S | name of preconditioner for iterative solver | |
* | 'JACOBI','MULTICOL','DIAGO' |JACOBI|
* Sol_type_S | type of solver:'ITERATIF','DIRECT' |DIRECT|
* Sol_yyg_eps | Epsilon value for the Yin-Yang iterative solver |1.d-07|
* Sol_yyg_maxits | maximum number of iterations allowed for the |40 |
* | Yin-Yang iterative solver | |
* Stat_liste | list of variables to do blocstat |'ALL_DYN_T1'|
* | Any gmm variable name, or predefine lists : |'TR/HU:P' |
* | 'ALL', 'ALL_DYN_T0', 'ALL_DYN_T1', 'ALL_TR_T0', | |
* | 'ALL_TR_T1' | |
*--------------------|-------------------------------------------------|------|
* Vertical sponge if activated, will be applied to the following variables  : |
* Horizontal Wind, Temperature (Top level), Zdot, W | |
*--------------------|-------------------------------------------------|------|
* Vspng_coeftop | Top coefficient for del-2 diffusion (m2/s) | -1 |
* Vspng_njpole | (non-LAM) Number of points along j on which to | 3 |
* | apply modulation to 0. of the diff. coefficient | |
* Vspng_nk | # of levels from the top of the model (thickness| |
* | of the vertical sponge layer) | 0 |
* Vspng_vec_L | .true. to use vectorial diffusion of winds |false |
* Vspng_zmean_L | .true. will subtract the zonal mean of U |false |
* | component before diffusion and then added back | |
* Vtopo_ndt | Number of timesteps for topography to evolve | 0 |
* Vtopo_start | Timestep to start topography which varies in time -1 |
*-----------------------------------------------------------------------------
* Zblen parameters are active in theoretical cases only |
* Zblen_L | .true. to apply vertical sponge | false|
* Zblen_spngthick | thickness (in meters) of vertical sponge |7.e+03|
* Zblen_spngtt_L | if .T. and Zblen_L=.T., apply sponge also to | false|
* | temperature field | |
*-----------------------------------------------------------------------------
* Zdot_divhlm_L | true for divergence high level modulation |false |
* | in initial computation of Zdot | |
*-----------------------------------------------------------------------------

*_____________________________________________________________________________
* |
* SERIES namelist (for timeseries data) |
*_____________________________________________________________________________|
* | | |
* NAME | DESCRIPTION |DEFVAL|
*--------------------|-------------------------------------------------|----- |
* P_serg_serstp | times series package stops at this timestep | 99999|
* P_serg_srprf_S | list of time series for profile variables | |
* P_serg_srsrf_S | list of time series for surface variables | |
* P_serg_srsus_L | .true. for time-series requested |false |
* P_serg_srwri | number of timesteps between time-series writeout| 1 |
* Xst_stn_ij | Stations chosen in gridpoints i,j for time-serie|-9999.|
* | For LAM, i,j values refer the core grid | |
* | Format: "STN_NAME",i,j, | |
* | ^ ^ ^ | |
* | string 2 integers | |
* Xst_stn_latlon | Stations chosen in lat,lon for time-series |-9999.|
* | Format: "STN_NAME",ilat,lon, | |
* | ^ ^ ^ | |
* | string 2 reals | |
*-----------------------------------------------------------------------------

*_____________________________________________________________________________
* |
* ENSEMBLES namelist (for ensemble forecasting) |
*_____________________________________________________________________________|
* | | |
* NAME | DESCRIPTION |DEFVAL|
*--------------------|-------------------------------------------------|----- |
* Ens_conf | switch to activate generation of Markov chains, |false |
* | use of SKEB and use of PTP | |
* Ens_mc_seed | seed of the random number generator usually we | -1 |
* | put DAY and member number | |
* Ens_skeb_conf | switch to activate SKEB |false |
* Ens_skeb_dif | switch to do SKEB calculation based on diffusion|false |
* Ens_skeb_gwd | switch to do SKEB calculation based on gravity |false |
* | wave drag | |
* Ens_stat | switch to print global stat related to Markov |false |
* | chains, SKEB and PTP | |
* Ens_skeb_div | switch to do the calculation of the divergence |false |
* | due to SKEB forcing | |
* Ens_mc3d_nlon | number of longitudes of the gaussian grid used | 16 |
* | for the 3D Markov chains (in the SKEB | |
* | calculation) | |
* Ens_mc3d_nlat | number of latitudes of the gaussian grid used | 8 |
* | for the 3D Markov chains (used in the SKEB | |
* | calculation) | |
* Ens_mc3d_trnz | vertical truncation for 3D Markov chain (used | 3 |
* | by SKEB) | |
* Ens_mc3d_trnl | low wave number truncation limit used in | 8 |
* | 3D Markov chain (used by SKEB) | |
* Ens_mc3d_trnh | high wave number truncation limit used in | 8 |
* | 3D Markov chain (used by SKEB) | |
* Ens_mc3d_max | maximum value of the 3D Markov chain (used by | 0.0 |
* | SKEB) | |
* Ens_mc3d_min | minimum value of the 3D Markov chain (used by | 0.0 |
* | SKEB) | |
* Ens_mc3d_std | std. dev. value for the 3D Markov chain (used by| 0.0 |
* | SKEB) | |
* Ens_mc3d_tau | decorrelation time (seconds) for 3D Markov chain| 0.0 |
* | (used by SKEB) | |
* Ens_mc3d_str | value of stretch for 3D Markov chain (used by | 0.0 |
* | SKEB) | |
* Ens_skeb_alph | coefficient Alpha for momentum in SKEB | 0.0 |
* Ens_skeb_alpt | coefficient Alpha for temperature in SKEB | 0.0 |
* Ens_skeb_bfc | coefficient for Gaussian filter used in SKEB |1.e-01|
* Ens_skeb_lam | wavelength for Gaussian filter in SKEB |2.e+05|
* Ens_ptp_conf | switch to activate PTP (perturb tendencies of |false |
* | physics) | |
* Ens_mc2d_nlon | no. of longitudes for 2D Markov chains (used in | 16 |
* | PTP) | |
* Ens_mc2d_nlat | no. of latitudes for 2D Markov chains (used in | 8 |
* | PTP) | |
* Ens_mc2d_ncha | number of 2d Markov chains | 1 |
* Ens_mc2d_trnl | low wave number horizontal truncation limit for | 8 |
* | 2D Markov chains (used in PTP) | |
* Ens_mc2d_trnh | high wave number horizontal truncation limit for| 8 |
* | 2D Markov chains (used in PTP) | |
* Ens_mc2d_min | minimum value of the 2D Markov chains (used by | 0.0 |
* | PTP) | |
* Ens_mc2d_max | maximum value of the 2D Markov chains (used by | 0.0 |
* | PTP) | |
* Ens_mc2d_std | standard deviation value for 2D Markov chains | 0.0 |
* | (used by PTP) | |
* Ens_mc2d_tau | decorrelation time (seconds) for 2D Markov | 0.0 |
* | chains (used by PTP) | |
* Ens_mc2d_str | value of stretch for Markov chains (used by PTP)| 0.0 |
* Ens_ptp_cape | CAPE value in Kain-Fritsch scheme to stop | 0.0 |
* | perturbing the physical tendencies (in PTP) | |
* Ens_ptp_critw | vertical velocity value (m/s) above which we | 100.0|
* | stop perturbing the physical tendencies (in PTP)| |
* Ens_ptp_env_u | upper value of transition zone of vertical | 1.0 |
* | envelope in sigma for PTP (above that full | |
* | perturbation) | |
* Ens_ptp_env_b | bottom value of transition zone of vertical | 1.0 |
* | envelope in sigma for PTP (below that no | |
* | perturbation) | |
* Ens_ptp_fac_reduc | factor of reduction of the perturbation the | 0.0 |
* | physical tendencies (in PTP) when convection | |
* | occurs | |
* Ens_ptp_tlc | TLC value (convective precipitation) in Kuo | 0.0 |
* | (OLDKUO) scheme to stop perturbing the physical | |
* | tendencies (in PTP) | |
*-----------------------------------------------------------------------------
*_________________________________________________________________________________
* |
* PHYSICS_CFGS namelist (phy_namelist.cdk) |
* initialized in phy_opt.ftn ( BLOCK DATA PHY_OPTIONS_DATA) |
* |
* Please! Keep list in strict alphabetical order |
* |
* New options in red, deleted options in gray |
*_________________________________________________________________________________|

* | | |
* NAME | DESCRIPTION | DEFAULT |
* | | VALUE |
*--------------------|-------------------------------------------------|----------|
* ADVECTKE | .TRUE.: turbulent kinetic energy advect. is done| .FALSE. |
* AGREGAT | .TRUE.: aggregation of surface fields is done | .FALSE. |
* AS2 | parameter for stability function | 12.0 |
* BETA2 | parameter for stability function | 1.0 |
* BKGALB | .TRUE.: to use background albedo (no snow) | .TRUE. |
* | .FALSE.: to compute albedo considering snow,ice,| |
* | and vegetation | |
* CHAUF | .TRUE.: surface heat flux from oceans (PHYSIMP) | .TRUE. |
* CONVEC | convection scheme name | 'NIL' |
* | 'SEC','MANABE','OLDKUO','FCP','KFC','KUOSTD', | |
* | 'KUOSYM','KUOSUN','RAS','FCPKUO','KFCKUO2', | |
* | 'BECHTOLD' | |
* DBGMEM | .TRUE.: activate debug physics memory management| .FALSE. |
* | system | |
* DIAG_TWIND | .TRUE. to obtain estimate of surface wind gusts | .FALSE. |
* DIFFUW | .TRUE.: diffuse vertical motion | .FALSE. |
* DRAG | .TRUE.: surface friction is on (PHYSIMP) | .TRUE. |
* DRYLAPS | .TRUE. : uses dry adiabat | .TRUE. |
* | .FALSE.: uses Schuman-Newell lapse rate | |
* DZSEDI | thickness of the lowest model layer near the | 60. |
* | surface (used to calc. sedimentation timestep | |
* | in 'EXCRIG' condensation scheme). | |
* EPONGE | coefficients that multiply KM to simulate | 0.0 |
* | sponge layer near the top of the model | |
* ETRMIN2 | minimal value for TKE in stable case | 1.E-4 |
* | (for 'CLEF') | |
* EVAP | .TRUE.: surface evaporation is on | .TRUE. |
* | (valid for full and simplified physics) | |
* FACDIFV | factor (usually 1 or 2) that multiplies the | 1. |
* | the timestep to enhance the effect of the | |
* | vertical diffusion | |
* FACTDT | =1 for 2-time level integration scheme | 1. |
* | =2 for 3-time level (leapfrog) int. scheme | |
* FLUVERT | boundary layer processes | 'NIL' |
* | 'CLEF': non-cloudy boundary layer formulation | |
* | 'MOISTKE': cloudy boundary layer formulation | |
* | 'NIL': no vertical diffusion | |
* FNNMOD | Non-dimensional parameter that modulates the | 2 |
* | cloud fraction enchancement factor (fnn) used | |
* | in the PBL scheme 'clef' | |
* | (note: fnnmod must be >= 2) | |
* FOMIC | .TRUE.: Fomichev radiation code | .FALSE. |
* GWDRAG | gravity wave drag formulation | 'NIL' |
* | 'GWD86': gravity wave drag + low-level blocking | |
* | 'GWD95': gravity wave drag (1995 version) | |
* HC2 | 0.0 -> 1.0; threshold relative humidity for | 0.6 |
* | onset of moist convective adjustment| |
* HF2 | 0.0 -> 1.0; threshold relative humidity for | 1.0 |
* | upward moisture flux during | |
* | convective adjustment | |
* HINES_FLUX_FILTER | Number of iteration of the vertical smoothing | 0 |
* | of the wind fluxes due to non-orographic gravity| |
* | wave drag | |
* HM2 | 0.0 -> 1.0; an input in the calculation of the | 1.0 |
* | saturation relative humidity for the| |
* | first iteration (conv. adjustment) | |
* ICELAC | .TRUE. water temperature of ice-covered likes | .FALSE. |
* | is 0C only if point is north of ice line, needs | |
* | an initialization file otherwise the model stops| |
* ICEMELT | .TRUE.: sea ice melting | .FALSE. |
* IHEATCAL | 1: consider heating from non-orog. drag | 0 |
* | 0: no " " " " | |
* IMPFLX | .TRUE. : implicit surface fluxes | .FALSE. |
* | .FALSE.: explicit surface fluxes | |
* INILWC | .TRUE.: to initialize water content and cloud | .FALSE. |
* | fraction at time 0 for Sundqvist schemes| |
* KFCDEPTH | minimum depth of conv. updraft in KFC scheme | 4000. |
* KFCDET | total forced detrainment in KFC scheme | 0.0 |
* KFCDLEV | init. level of forced detrainment in KFC scheme | 0.5 |
* KFCMOM | .TRUE.: to generate wind tendencies in KFC | .FALSE. |
* KFCPCP | 'ORI': KFC orig. scheme (not conserv. for HU) | 'ORI' |
* | 'CONSPCPN': conservation of water in KFCP | |
* KFCRAD | initial convective updraft radius in KFC scheme | 1500. |
* KFCTIMEA | convect. time adjustment in Kain-Fritsch scheme | 3600. |
* KFCTIMEC | convective time scale in Kain-Fritsch | 3600. |
* KFCTRIG4 | 4 values to control trigger parameter of | |
* | Kain-Fritsch convection scheme (WKLCL): 0.,0.,0.05,0.05 |
* | Trigger parameter will increase from | |
* | kfctrig4(3) | 0.05 |
* | to kfctrig4(4) | 0.05 |
* | between timestep kfctrig4(1) | 0.0 |
* | to timestep kfctrig4(2) | 0.0 |
* KFCTRIGA | nominal resolution for which KFCTRIG4 is set. | -1.0 |
* | This is inactive if value <= 0. | |
* KFCTRIGL | over land and lakes | 0.05 |
* | we keep the value set by the "ramp" above | |
* | over sea water: | |
* | for |lat| >= TRIGLAT(2) we keep value set | |
* | by the "ramp" KFCTRIG4 | |
* | for |lat| <= TRIGLAT(1) we use the new value | |
* | KFCTRIGL | |
* | and linear interpolation in between TRIGLAT(1) | |
* | and TRIGLAT(2) | |
* KFCTRIGLAT | logical key for variation of the trigger | .FALSE. |
* | function depending on latitude and land-sea-lake| |
* | mask | |
* KKL2 | sedimentation threshold for mixphase | 0.1 |
* KNTRAD | number of timesteps between full radiation | 0 |
* | calculations | |
* KTICEFRAC | .TRUE.: calculate ice fraction in KTRSNT_MG | .TRUE. |
* LIMSNODP | .TRUE.: to limit snow depth to 10 cm over | .FALSE. |
* | seaice and glacier | |
* LMETOX | .TRUE.: add methane oxydation as source of | .FALSE. |
* | humidity in the stratosphere | |
* LONGMEL | 'BLAC62': mixing length calc. using Blackadar | 'BLAC62' |
* | 'BOUJO': mixing length calc. using Bougeault | |
* MOYHR | time length (hours) for special time average | 0 |
* | physics variables | |
* MY_CCNTYPE | switch for airmass type | 1 |
* | 1 = maritime, 2 = continental 1 | |
* MY_DBLMOM_C | double-moment for cloud (for 'my_dm' only) | .TRUE. |
* MY_DBLMOM_G | double-moment for graupel (for 'my_dm' only) | .TRUE. |
* MY_DBLMOM_H | double-moment for hail (for 'my_dm' only) | .TRUE. |
* MY_DBLMOM_I | double-moment for ice (for 'my_dm' only) | .TRUE. |
* MY_DBLMOM_R | double-moment for rain (for 'my_dm' only) | .TRUE. |
* MY_DBLMOM_S | double-moment for snow (for 'my_dm' only) | .TRUE. |
* MY_DIAGON | diagnostic fields get calculated | .TRUE. |
* MY_DZSEDI | thickness of the lowest model layer near the | 50. |
* | surface (used to calc. sedimentation timestep) | |
* MY_FULL_VERSION | specific sub-version for 'my_full' | 4 |
* | 1=single-moment | |
* | 2=double-moment_fixed_dispersion | |
* | 3=double-moment_diagnostic_dispersion | |
* | 4=triple-moment | |
* MY_ICEON | ice-phase switched on | .TRUE. |
* MY_RAINON | autoconversion (cloud to rain) switched on | .TRUE. |
* MY_SEDION | sedimentation switched on | .TRUE. |
* MY_SNOWON | snow initiation switched on | .TRUE. |
* MY_WARMON | warm-phase switched on | .TRUE. |
* NON_ORO | .TRUE.: Hines non-orographic GWD scheme is on | .FALSE. |
* NSLOFLUX | number of timesteps for which surface | 0 |
* | fluxes "FC" and "FV" are gradually set from 0 | |
* | to their full value in a "slow start fashion" | |
* | at the beginning of a time integration | |
* OWFLUX | .TRUE.: in coupling mode, fluxes over ocean are | .FALSE. |
* | taken from ocean model | |
* PARSOL | thermal parameters for ground (force-restore) | |
* | (1) heat capacity of soil | 2.3E+6 |
* | (2) heat capacity of snow | 1.0E+6 |
* | (3) heat capacity of ice | 2.0E+6 |
* | (4) heat diffusivity of soil | 0.5E-6 |
* | (5) heat diffusivity of snow | 0.6E-6 |
* | (6) heat diffusivity of ice | 1.1E-6 |
* PBL_COUPLED | Run with a coupled high vertical resolution | .FALSE. |
* | boundary layer (PBL). | |
* PBL_KTOP | | 1 |
* PBL_RICRIT | Richardson num. critical values for hysteresis | 1.,1. |
* PBL_TSPLIT | | 1 |
* PBL_ZSPLIT | | 1 |
* PCPTYPE | 'BOURGE': use Bourgouin algorithm (bourge1) | 'NIL' |
* | to determine precip. types. Cannot use with | |
* | 'EXC' and 'EXCRIG' condensation schemes | |
* | 'NIL': no call to bourge1 | |
* QCFC11 | CFC11 bckgrnd atmospheric concentration (PPMV) | 0.280 |
* QCFC12 | CFC12 " " " | 0.530 |
* QCH4 | CH4 " " " " | 1.783 |
* QCO2 | CO2 " " " " | 380. |
* QN2O | N2O " " " " | 0.3186 |
* RADFILES | format of radiation files to be read | 'STD' |
* | 'STD': RPN standard file | |
* | 'UNF': unformatted | |
* RADFIX | .TRUE.: radiation fixes near the model top | .TRUE. |
* RADFLTR | .TRUE.: vertical smoothing on radiative fluxes | .TRUE. |
* RADIA | radiation scheme | 'NIL' |
* | 'OLDRAD': simple radiation scheme | |
* | 'NEWRAD': complete radiation scheme | |
* | 'CCCMARAD': most advanced radiation scheme | |
* RADNIVL | list of levels on which IR and VIS radiation | 0 |
* | calculations are performed (to save on CPU time)| |
* RADSLOPE | key for activation of the radiation along slopes| .FALSE. |
* REFRACT | Additional output for low level refraction | .FALSE. |
* RMSCON | launching level value of GW rms wind (m/s) from | 1.0 |
* | non-orographic origin | |
* SALTY_QSAT | TRUE: takes into account effect of ocean | .FALSE. |
* | salinity on saturation specific humidity at | |
* | ocean surface (boundary condition for LH flux | |
* | calculation) | |
* SATUCO | .TRUE. : water/ice phase for saturation calc. | .TRUE. |
* | .FALSE.: water phase only for saturation calc. | |
* SCHMSOL | land surface processes | 'FCREST' |
* | 'FCREST': force-restore (simple) | |
* | 'ISBA': ISBA surface scheme (complex) | |
* | 'CLASS': CLASS surface scheme (most complex) | |
* SCHMURB | urban surface processes | 'NIL' |
* SGO_STABFAC | Turns on/off the amplification factor | .TRUE. |
* | (due to stability) of the drag coefficient in | |
* | the orographic blocking scheme | |
* SGO_NLDIRFAC | Turns on/off the non-linear amplification factor| .TRUE. |
* | (depending on wind direction) of the drag | |
* | coefficient in the orographic blocking scheme | |
* SGO_CDMIN | Sets the minimum value of the drag coefficient | 1.0 |
* | in the orographic blocking scheme. | |
* SHLCVT | shallow convection schemes | 2 * 'NIL'|
* | (two schemes can be used concurrently) | |
* | (1) 'GELEYN','CONRES','SHALOW','SHALODQC','NIL' | |
* | (2) 'KTRSNT','NIL' | |
* SIMISCCP | .TRUE.: run ISCCP cloud simulator | .FALSE. |
* SNOALB_ANL | .TRUE. : use snow albedo "I6" directly | .TRUE. |
* | .FALSE.: to use snow age "XA" to calculate | |
* | snow albedo | |
* SNOWMELT | .TRUE.: snow melting in force-restore | .FALSE. |
* STCOND | condensation scheme name | 'NIL' |
* | 'CONDS','NEWSUND','CONSUN','EXC','EXCRIG', | |
* | 'MY_SM','MY_DM','MY_FULL','MY_EXP1' | |
* STOMATE | .TRUE.: stomatal resistance taken into account | .FALSE. |
* | in force-restore | |
* STRATOS | .TRUE.: special treatment of stratosphere | .FALSE. |
* TAUFAC | factor used in the gwd formulation | 8.E-6 |
* | = 1/(LENGTH SCALE) | |
* TDIAGLIM | .TRUE.: to limit temperature inversions | .FALSE. |
* | at the surface | |
* TRIGLAT | real dimension(2), over land and lakes | 2*0.0 |
* | we keep the value set by the "ramp" above | |
* | over sea water: | |
* | for |lat| >= TRIGLAT(2) we keep value set | |
* | by the "ramp" KFCTRIG4 | |
* | for |lat| <= TRIGLAT(1) we use the new value | |
* | KFCTRIGL | |
* | and linear interpolation in between TRIGLAT(1) | |
* | and TRIGLAT(2) | |
* TSCONFC | .TRUE.: TS constant (force-restore only) | .FALSE. |
* TS_FLXIR | .TRUE.: to use TT(12000) instead of skin temp | .FALSE. |
* | in downward IR flux calculation | |
* TYPSOL | .TRUE.: take into account soil types | .FALSE. |
* | in force-restore | |
* Z0DIR | .TRUE. directional roughness length | .FALSE. |
* Z0HCON | Value of the constant heat/moisture roughness | 4E-5 |
* | length (in m) to be used over water, within the | |
* | latitudinal band defined by z0tlat | |
* Z0MIN2 | minimum value of roughness length over oceans | 1.5E-5 |
* Z0MTYPE | Sets the formulation ("charnock" or "beljaars") |'CHARNOCK'|
* | to be used in the calculation of the momentum | |
* | roughness length over water | |
* Z0TLAT | latitude (2 elements, in degrees) used to | 2 * 0.0 |
* | specify Z0T over water | |
* | If |lat| <= Z0TLAT(1) constant Z0T. | |
* | If |lat| >= Z0TLAT(2) Charnock's relation. | |
* | In between, linear interpolation is used. | |
* ZTA | height (m) of T and Q input for sfc fluxes calc.| -1. |
* ZUA | height (m) of wind input for sfc fluxes calc.| -1. |
*_________________________________________________________________________________|


*_________________________________________________________________________________
* |
* "PHYSICS_2" namelist is a subset of "PHYSICS_CFGS" namelist used to |
* define a second physics configuration in the variable resolution region |
* of the grid, in climate mode. Refer to the definitions and default values |
* above. |
* |
* Allowed: |
* |
* AGREGAT,CHAUF,CONVEC,DRAG,EVAP,FLUVERT,ICEMELT,INILWC,KFCDEPTH,KFCDET, |
* KFCDLEV,KFCMOM,KFCRAD,KFCTIMEA,KFCTIMEC,KFCTRIG4,KFCTRIGA,KTICEFRAC, |
* LONGMEL,SATUCO,SCHMSOL,SHLCVT,SNOWMELT,STCOND,STOMATE,TYPSOL |
* |
*_________________________________________________________________________________|



*_________________________________________________________________________________
* |
* PHYSICS_SIMPLIFIED namelist |
*_________________________________________________________________________________|

* | | |
* NAME | DESCRIPTION |DEFVAL |
*--------------------|-------------------------------------------------|----------|
* LIN_KPH | Kind of physics (full=0) (simplified=1) | 0 |
*--------------------|-------------------------------------------------|----------|
* LIN_LSC | Option number of moist processes | 0 |
* | option LS CONDENSATION MOIST CONVECTION | |
* | 0 false false | |
* | 100 true false | |
* | 200 false true | |
* | 300 true true | |
*--------------------|-------------------------------------------------|----------|
* LIN_PBL | Option number of planetary boundary layer | 0 |
* | 0 = no parameterization | |
* | 1 = linear diffusion coefficients | |
* | 2 = linear diffusion coefficients | |
* | (coefficients from the nonlinear | |
* | low-resolution run) | |
*--------------------|-------------------------------------------------|----------|
* LIN_SGO | sub-grid scale orography schemes avail | 0 |
* | in V4d adjoint and tangent linear model | |
* | The option indicates the settings of | |
* | the parameters. | |
* |-------------------------------------------------| |
* | option GWD BLOCKING AA1 AA2 APPLYTEND | |
* | 0 No parameterization | |
* | 100 true true 1 1 false | |
* | 110 true true 0 1 false | |
* | 120 true true 1 0 false | |
* | 130 true true 0 0 false | |
* | 101 true true 1 1 true | |
* | 111 true true 0 1 true | |
* | 121 true true 1 0 true | |
* | 131 true true 0 0 true | |
* | 210 false true 0 1 false | |
* | 220 false true 1 0 false | |
* | 230 false true 0 0 false | |
* | 201 false true 1 1 true | |
* | 211 false true 0 1 true | |
* | 221 false true 1 0 true | |
* | 231 false true 0 0 true | |
* | 300 true false 0 0 false | |
* | 301 true false 0 0 true | |
* where : |
* |
* GWD : true to compute gravity-wave drag tendency |
* BLOCKING : true to compute orographic-blocking tendency |
* APPLYTEND : true to apply total tendency to winds inside this LIN_SGO scheme |
* AA1 : '1' for the directional factor in blocking term to be linearized |
* AA2 : '1' for the vertical factor in blocking term to be linearized |
*_________________________________________________________________________________|