Voir la source de GEM 5.0 configs

==Complete documentation==

=== adv_cfgs Namelist  ===

{| class="wikitable"
|-
! style="width: 10em;" | Name
! style="width: 40em;" | Description
! style="width: 10em;" | Default Value
! Type


|-
| adv_bc_min_max_l ||
switch:.T.:MONO(CLIPPING) after Bermejo-Conde
(MASS-CONSERVATION for Chemical Tracers)
| .true. || logical

|-
| adv_catmullrom_l ||
switch:.T.:
| .false. || logical

|-
| adv_ilmc_min_max_l ||

|  || 

|-
| adv_ilmc_sweep_max ||

|  || 

|-
| adv_pil_sub_e ||
East boundary in GY for an embedded LAM
(MASS-CONSERVATION for Chemical Tracers)
| -1 || integer

|-
| adv_pil_sub_n ||
North boundary in GY for an embedded LAM
(MASS-CONSERVATION for Chemical Tracers)
| -1 || integer

|-
| adv_pil_sub_s ||
South boundary in GY for an embedded LAM
(MASS-CONSERVATION for Chemical Tracers)
| -1 || integer

|-
| adv_pil_sub_w ||
West boundary in GY for an embedded LAM
(MASS-CONSERVATION for Chemical Tracers)
| -1 || integer

|-
| adv_rhst_mono_l ||
switch:.T.:MONO(CLIPPING) of RHS
| .false. || logical

|-
| adv_scaling ||
Scaling for mass of tracer
* adv_scaling=0 (none)
* adv_scaling=1 (CO2)
* adv_scaling=2 (O3)
| 1 || integer

|-
| adv_slice_rebuild ||
Type of rebuild in SLICE
* SLICE_rebuild=1 (LP)
* SLICE_rebuild=2 (CW)
(MASS-CONSERVATION for Chemical Tracers)
| 2 || integer

|-
| adv_slt_winds ||
Use surface layer winds for advection of lowest thermodynamic level
| .false. || logical

|-
| adv_verbose ||
Activate conservation diagnostics if /=0
(MASS-CONSERVATION for Chemical Tracers)
| 0 || integer
|}
=== bubble_cfgs Namelist  ===

{| class="wikitable"
|-
! style="width: 10em;" | Name
! style="width: 40em;" | Description
! style="width: 10em;" | Default Value
! Type


|-
| bubble_dx ||

| 10. || real

|-
| bubble_dz ||

| 10. || real

|-
| bubble_ictr ||

| -1 || integer

|-
| bubble_kctr ||

| -1 || integer

|-
| bubble_ni ||

| 101 || integer

|-
| bubble_nj ||

| 1 || integer

|-
| bubble_nk ||

| 100 || integer

|-
| bubble_rad ||

| 25 || integer

|-
| bubble_theta ||

| 303.16 || real
|}
=== dyn_kernel Namelist  ===

{| class="wikitable"
|-
! style="width: 10em;" | Name
! style="width: 40em;" | Description
! style="width: 10em;" | Default Value
! Type


|-
| dynamics_kernel_s ||
Main selector for dynamical kernel
* "DYNAMICS_FISL_P" : Fully implicit SL in pressure
* "DYNAMICS_FISL_H" : Fully implicit SL in height
* "DYNAMICS_EXPO_H" : Exponential integrators in height
| 'DYNAMICS_FISL_P' || character(len=32)
|}
=== ensembles Namelist  ===

{| class="wikitable"
|-
! style="width: 10em;" | Name
! style="width: 40em;" | Description
! style="width: 10em;" | Default Value
! Type


|-
| ens_conf ||
Switch to activate generation of Markov chains, use of SKEB
and use of PTP
| .false. || logical

|-
| ens_first_init_mc ||
Switch to activate the first initialisation of Matkov chaines
in PTP & SKEB
| .false. || logical

|-
| ens_iau_mc ||
Switch to activate the
in PTP & SKEB
| .false. || logical

|-
| ens_mc_seed ||
Seed of the random number generator usually we put DAY and member number
(3D MARKOV CHAINES)
| -1 || integer

|-
| ens_ptp_cape ||
CAPE value in Kain-Fritsch scheme to stop perturbing the physical
tendencies
(2D MARKOV CHAINES)
| 0.0 || real

|-
| ens_ptp_conf ||
switch to activate PTP (perturb tendencies of physics)
(2D MARKOV CHAINES)
| .false. || logical

|-
| ens_ptp_crit_w ||
vertical velocity value (m/s) above which we stop perturbing the
physical tendencies
(2D MARKOV CHAINES)
| 100.0 || real

|-
| ens_ptp_env_b ||
bottom value of transition zone of vertical envelope in sigma for PTP
(below that no perturbation)
(2D MARKOV CHAINES)
| 1.0 || real

|-
| ens_ptp_env_u ||
upper value of transition zone of vertical envelope in sigma for PTP
(above that full perturbation)
(2D MARKOV CHAINES)
| 1.0 || real

|-
| ens_ptp_fac_reduc ||
factor of reduction of the perturbation the physical tendencies (in PTP)
when convection occurs
(2D MARKOV CHAINES)
| 0.0 || real

|-
| ens_ptp_l ||
(ignored) Ens_ptp_l = Ens_ptp_trnh-Ens_ptp_trnl+1
(2D MARKOV CHAINES)
| 0 || integer

|-
| ens_ptp_lmax ||
(ignored) Ens_ptp_lmax = maxval(Ens_ptp_l)
(2D MARKOV CHAINES)
| 0 || integer

|-
| ens_ptp_m ||
(ignored) Ens_ptp_m = Ens_ptp_trnh+1
(2D MARKOV CHAINES)
| 0 || integer

|-
| ens_ptp_max ||
maximum value of the 2D Markov chains
(2D MARKOV CHAINES)
| 0.0 || real

|-
| ens_ptp_min ||
minimum value of the 2D Markov chain
(2D MARKOV CHAINES)
| 0.0 || real

|-
| ens_ptp_mmax ||
(ignored) Ens_ptp_mmax = maxval(Ens_ptp_m)
(2D MARKOV CHAINES)
| 0 || integer

|-
| ens_ptp_ncha ||
number of 2d Markov chains
(2D MARKOV CHAINES)
| 1 || integer

|-
| ens_ptp_nlat ||
no. of latitudes for 2D Markov chains
(2D MARKOV CHAINES)
| 8 || integer

|-
| ens_ptp_nlon ||
no. of longitudes for 2D Markov chains
(2D MARKOV CHAINES)
| 16 || integer

|-
| ens_ptp_std ||
standard deviation value for 2D Markov chains
(2D MARKOV CHAINES)
| 0.0 || real

|-
| ens_ptp_str ||
value of stretch for Markov chains
(2D MARKOV CHAINES)
| 0.0 || real

|-
| ens_ptp_tau ||
decorrelation time (seconds) for 2D Markov chains
(2D MARKOV CHAINES)
| 0.0 || real

|-
| ens_ptp_tlc ||
TLC value (convective precipitation) in Kuo (OLDKUO) scheme to stop
perturbing the physical tendencies
(2D MARKOV CHAINES)
| 0.0 || real

|-
| ens_ptp_trnh ||
high wave number horizontal truncation limit for 2D Markov chains
(2D MARKOV CHAINES)
| 8 || integer

|-
| ens_ptp_trnl ||
low wave number horizontal truncation limit for 2D Markov chains
(2D MARKOV CHAINES)
| 1 || integer

|-
| ens_skeb_alph ||
coefficient Alpha for momentum in SKEB
(3D MARKOV CHAINES)
| 0. || real

|-
| ens_skeb_alpt ||
coefficient Alpha for temperature in SKEB
(3D MARKOV CHAINES)
| 0. || real

|-
| ens_skeb_bfc ||
coefficient for Gaussian filter used in SKEB
(3D MARKOV CHAINES)
| 1.0e-01 || real

|-
| ens_skeb_conf ||
Switch to activate SKEB
(3D MARKOV CHAINES)
| .false. || logical

|-
| ens_skeb_dif ||
switch to do SKEB calculation based on diffusion
(3D MARKOV CHAINES)
| .false. || logical

|-
| ens_skeb_div ||
switch to do the calculation of the divergence due to SKEB forcing
(3D MARKOV CHAINES)
| .false. || logical

|-
| ens_skeb_gwd ||
switch to do SKEB calculation based on gravity wave drag
(3D MARKOV CHAINES)
| .false. || logical

|-
| ens_skeb_lam ||
wavelength for Gaussian filter in SKEB
(3D MARKOV CHAINES)
| 2.0e+05 || real

|-
| ens_skeb_max ||
maximum value of the 3D Markov chain (used by SKEB)
(3D MARKOV CHAINES)
| 0. || real

|-
| ens_skeb_min ||
minimum value of the 3D Markov chain (used by SKEB)
(3D MARKOV CHAINES)
| 0. || real

|-
| ens_skeb_ncha ||

(3D MARKOV CHAINES)
| 1 || integer

|-
| ens_skeb_nlat ||
number of latitudes of the gaussian grid used  for the 3D Markov chains
(used in the SKEB calculation)
(3D MARKOV CHAINES)
| 8 || integer

|-
| ens_skeb_nlon ||
number of longitudes of the gaussian grid used for the 3D Markov chains
(in the SKEB calculation)
(3D MARKOV CHAINES)
| 16 || integer

|-
| ens_skeb_std ||
std. dev. value for the 3D Markov chain (used by SKEB)
(3D MARKOV CHAINES)
| 0. || real

|-
| ens_skeb_str ||
value of stretch for 3D Markov chain (used by SKEB)
(3D MARKOV CHAINES)
| 0. || real

|-
| ens_skeb_tau ||
decorrelation time (seconds) for 3D Markov chain (used by SKEB)
(3D MARKOV CHAINES)
| 0. || real

|-
| ens_skeb_trnh ||
high wave number truncation limit used in 3D Markov chain (used by SKEB)
(3D MARKOV CHAINES)
| 8 || integer

|-
| ens_skeb_trnl ||
low wave number truncation limit used in 3D Markov chain (used by SKEB)
(3D MARKOV CHAINES)
| 2 || integer

|-
| ens_stat ||
switch to print global stat related to Markov chains, SKEB and PTP
(3D MARKOV CHAINES)
| .false. || logical
|}
=== gem_cfgs Namelist  ===

{| class="wikitable"
|-
! style="width: 10em;" | Name
! style="width: 40em;" | Description
! style="width: 10em;" | Default Value
! Type


|-
| cstv_ba_8 ||
SL off-centering parameter for hydrostatic
| 0.6 || real*8

|-
| cstv_ba_m_8 ||
SL off-centering parameter for the momentum equations
| 0.6 || real*8

|-
| cstv_ba_nh_8 ||
SL off-centering parameter for nonhydrostatic
| 0.5 || real*8

|-
| cstv_psadj_8 ||
Fraction of adjustment to be given to the ocean
| 1.d0 || real*8

|-
| cstv_psref_8 ||
another reference pressure
| 1.d5 || real*8

|-
| cstv_re_8 ||
Parameter controlling modified epsilon (Ver_epsi_8) [nonhydrostatic part]
| 1.d0 || real*8

|-
| cstv_tstr_8 ||
T* basic state temperature (K)
| 240.0 || real*8

|-
| eq_ramp_l ||
Latitudinal ramping of equatorial sponge
| .false. || logical

|-
| eq_sponge ||
Coefficients that multiply KM to simulate sponge layer near the top
of the model. Warning! if this parameter is used, the EPONGE in the
physics namelist should be removed.
|  || 

|-
| g_halox ||
number of points for the halo on X
| 4 || integer

|-
| g_haloy ||
number of points for the halo on Y
| 4 || integer

|-
| heap_nk ||
Heap memory will be painted to NaN using an array wrk01(G_ni,G_nj,Heap_nk)
| -1 || integer

|-
| hyb ||
array of model levels ,  0.0 < HYB < 1.0
|  || 

|-
| hyb_rcoef ||
pair of coefficients (min,max) to control the flattenning of the
vertical coordinate
|  || 

|-
| hzd_div_damp ||
Fraction of the maximum divergence damping - range(0.0-1.0)
| -1. || real

|-
| hzd_lnr ||
Background 2 delta-x removal ratio - range(0.0-1.0)
| -1. || real

|-
| hzd_lnr_theta ||
Theta 2 delta-x removal ratio - range(0.0-1.0).
| -1. || real

|-
| hzd_lnr_tr ||
Tracers 2 delta-x removal ratio - range(0.0-1.0)
| -1. || real

|-
| hzd_pwr ||
Order of the background diffusion operator
2, 4, 6, 8
| -1 || integer

|-
| hzd_pwr_theta ||
Order of the background diffusion operator on theta
2, 4, 6, 8
| -1 || integer

|-
| hzd_pwr_tr ||
Order of the background diffusion operator on tracers
| -1 || integer

|-
| hzd_smago_fric_heat ||
Frictional heating is considered when Hzd_smago_fric_heat>0.
| 0. || real

|-
| hzd_smago_lev ||
The levels (bot,top) in the hybrid coordinate where the background diffusion
coefficient varies between the value defined by Hzd_smago_lnr(1) and Hzd_smago_lnr(2).
|  || 

|-
| hzd_smago_lnr ||
Coefficient of background diffusion added to the coefficient computed using the
Smagorinsky approach. The first element of the array determines the constant value
of background diffusion coeff. below Hzd_smago_lev(1). The second element represents
the value at Hzd_smago_lev(2). The third element determines the maximum coefficient
at the model top. Two ramps of COS^2-type are used between Hzd_smago_lev(1) and
Hzd_smago_lev (2), and between Hzd_smago_lev(2) and the model lid.
|  || 

|-
| hzd_smago_param ||
Main Smagorinsky control parameter (usual range 0.1-0.3)
| -1. || real

|-
| hzd_smago_prandtl ||
Apply Smago diffusion on theta using Hzd_smago_param/Hzd_smago_prandtl parameter
| -1. || real

|-
| hzd_smago_prandtl_hu ||
Apply Smago diffusion on HU using Hzd_smago_param/Hzd_smago_prandtl_hu parameter
| -1. || real

|-
| hzd_smago_theta_base_l ||
If TRUE then background diffusion is applied to THETA and HU.
| .true. || logical

|-
| iau_cutoff ||
Filter cutoff period for Iau_weight_S='sin' in hours
| 6. || real

|-
| iau_input_type_s ||
IAU Input TYPE
* 'OLD ' : GEM 4.8 physic's input, MPI blocking based
* 'IO  ' : new input system, RPN_COMM_IO/RPN_COMM_ezshuf_dist based
* 'BLOC' : new input system, RPN_COMM_bloc based
| 'OLD' || character(len=16)

|-
| iau_interval ||
The number of seconds between increment fields
| -1. || real

|-
| iau_ninblocx ||
IAU Input PE blocking along npex
| 1 || integer

|-
| iau_ninblocy ||
IAU Input PE blocking along npey
| 1 || integer

|-
| iau_period ||
The number of seconds over which IAU will be  will be run
(typically the length of the assimilation window).
Default < 0 means that no IAUs are applied.
| -1. || real

|-
| iau_stats_l ||
IAU Input Stats
| .false. || logical

|-
| iau_tracers_s ||
An optional list of tracers to be incremented.
|  || 

|-
| iau_weight_s ||
The type of weighting function to be applied to the analysis increments:
* 'constant' (default) uniform increments
* 'sin' DF-style weights (Fillion et al. 1995)
| 'constant' || character(len=64)

|-
| init_balgm_l ||
true -> Digital filter initialization is performed
| .false. || logical

|-
| init_dflength_s ||
number of points for digital filter (equals the number of timesteps +1)
| '5p' || character(len=16)

|-
| init_dfpl_s ||
period limit of digital filter units D,H,M,S
| '6h' || character(len=16)

|-
| init_dftr_l ||
* true -> passive tracers digitally filtered
* false-> passive tracers set to result obtained at mid-period during initialization period (no filtering)
| .false. || logical

|-
| init_dfwin_l ||
true -> Windowing is applied
| .true. || logical

|-
| inp_blacklist_s ||
List of variables to NOT process during input
|  || 

|-
| inp_npes ||
Number of PEs to use for input
| 1 || integer

|-
| inp_vertintype_tracers_s ||
Type of vertical interpolation scheme
| 'cubic' || character(len=8)

|-
| lam_0ptend_l ||
True-> for blending to zero the physics tendency in blending area
| .true. || logical

|-
| lam_blend_h ||
Number of points for horizontal blending
| 10 || integer

|-
| lam_blend_t ||
Number of levels for top blending
| 0 || integer

|-
| lam_blendoro_l ||
True-> to blend the model topography with the pilot topography
| .true. || logical

|-
| lam_ctebcs_l ||
True-> to force constant (fixed) boundary conditions
| .false. || logical

|-
| lam_gbpil_t ||
Number of levels for top piloting
| -1 || integer

|-
| lam_hint_s ||
Type of horizontal interpolation to model grid
* 'CUB_LAG'
* 'LINEAR'
* 'NEAREST'
| 'CUB_LAG' || character(len=16)

|-
| lam_toptt_l ||
True-> The plane of the top temperature layer is completely
overwritten from the 2D pilot data
| .false. || logical

|-
| lctl_cktimeleft_l ||
True->to check for time left in job
| .false. || logical

|-
| lctl_debug_l ||
True->to print more information to std output
| .false. || logical

|-
| lctl_rxstat_s ||
precision in print glbstats
* 'LCL_4'
* 'GLB_8'
| 'LCL_4' || character(len=6)

|-
| out3_cliph_l ||
True-> to clip humidity variables on output
| .false. || logical

|-
| out3_close_interval_s ||
Interval of output file name change
| ' ' || character(len=16)

|-
| out3_etik_s ||
'etiket' used for output fields
| 'GEMDM' || character(len=12)

|-
| out3_ip3 ||
Default value for IP3 is 0, -1 for IP3 to contain step number,
>0 for given IP3
| 0 || integer

|-
| out3_lieb_conv ||
Precision criteria for the Liebman procedure
| 0.1 || real

|-
| out3_lieb_levels ||
List of levels for underground extrapolation
|  || 

|-
| out3_lieb_maxite ||
Maximum number of iterations for the Liebman procedure
| 100 || integer

|-
| out3_liebxch_iter ||
number of iterations to exchange halo for the Liebman procedure
| 4 || integer

|-
| out3_linbot ||
Number of layers close to the bottom of the model within which a
linear interpolation of GZ will be performed
| 0 || integer

|-
| out3_nbitg ||
Packing factor used for all variables except for those defined in
Out_xnbits_s
| 16 || integer

|-
| out3_ndigits ||
Minimum of digits used to represent output units
| 3 || integer

|-
| out3_npes ||
Total number of PEs for output using MFV collector
| 1 || integer

|-
| out3_npex ||
Total number of PEs along npex for output using MID collector
| -1 || integer

|-
| out3_npey ||
Total number of PEs along npey for output using MID collector
| -1 || integer

|-
| out3_postproc_fact ||
Sortie jobs lauched every Out3_postproc_fact*Out3_close_interval_S
| 0 || integer

|-
| out3_vinterp_type_s ||
Vertical interpolation scheme for output
| 'linear' || character(len=12)

|-
| p_lmvd_high_lat ||
Latitude at which the multiplication factor becomes P_lmvd_weigh_high_lat
| 30.0 || real

|-
| p_lmvd_low_lat ||
latitude at which the multiplication factor becomes P_lmvd_weigh_low_lat
| 5.0 || real

|-
| p_lmvd_weigh_high_lat ||
Multiplication factor of P_pbl_spng at latitude P_lmvd_high_lat
| 1.0 || real

|-
| p_lmvd_weigh_low_lat ||
Multiplication factor of P_pbl_spng at latitude P_lmvd_low_lat
| 1.0 || real

|-
| perturb_nbits ||
Number of bits to perturb on initial conditions
| 0 || integer

|-
| perturb_npts ||
Stride for perturbation on initial conditions
| 10 || integer

|-
| schm_adcub_l ||
* True-> cubic interpolation
* False-> linear interpolation
| .true. || logical

|-
| schm_advec ||
* 0   ->          NO advection
* 1   -> traditional advection
* 2   -> consistent advection with respect to off-centering
* 3   -> reversed advection with respect to off-centering
| 1 || integer

|-
| schm_autobar_l ||
True-> auto barotropic option
| .false. || logical

|-
| schm_bcavg_l ||
True-> averaging B and C in SLEVE scheme
| .true. || logical

|-
| schm_bitpattern_l ||
True-> Modify slightly code behaviour to ensure bitpattern
reproduction in restart mode using FST file
| .false. || logical

|-
| schm_capa_var_l ||
True-> variable cappa in thermodynamic equation
| .false. || logical

|-
| schm_cub_traj_l ||
Use cubic interpolation in trajectory computation
| .true. || logical

|-
| schm_dry_mixing_ratio_l ||
True->
| .false. || logical

|-
| schm_eulmtn_l ||
True-> Eulerian treatment of mountains in the continuity equation
| .false. || logical

|-
| schm_hydro_l ||
* True-> hydrostatic
* False-> non-hydrostatic
| .false. || logical

|-
| schm_hzdadw_l ||
True-> horizontal diffusion of momentum at each CN iteration
| .false. || logical

|-
| schm_itcn ||
Number of iterations for Crank-Nicholson
| 2 || integer

|-
| schm_itnlh ||
Number of iterations to solve non-linear Helmholtz problem
| 2 || integer

|-
| schm_itraj ||
Number of iterations to compute trajectories
| 3 || integer

|-
| schm_nblendyy ||
*  -1: no blending between Yin and Yang
*   0: blending at init only
* > 0: blending at every nblendyy timestep
| -1 || integer

|-
| schm_phycpl_s ||
Physics coupling strategy
| 'split' || character(len=16)

|-
| schm_psadj ||
* 0 -> No conservation of surface pressure
* 1 -> Conservation of Total air mass Pressure
* 2 -> Conservation of Dry air mass Pressure
| 0 || integer

|-
| schm_psadj_lam_l ||
Confirmation to use psadjust with a LAM configuration
| .false. || logical

|-
| schm_psadj_print_l ||
True-> print dry/wet air masses
| .false. || logical

|-
| schm_topo_l ||
True-> to use topography
| .true. || logical

|-
| schm_trapeze_l ||
Use trapezoidal average for advection winds
| .true. || logical

|-
| schm_wload_l ||
Apply water loading in the calculations
| .false. || logical

|-
| sol2d_precond_s ||
2D preconditioner for iterative solver
| 'JACOBI' || character(len=26)

|-
| sol3d_krylov_s ||
Krylov method for 3d iterative solver (FGMRES or FBICGSTAB)
| 'FGMRES' || character(len=26)

|-
| sol3d_precond_s ||
3D preconditioner for iterative solver
| 'JACOBI' || character(len=26)

|-
| sol_fft_l ||
* True-> use FFT solver if possible
* False-> use MXMA solver (slower,less precise)
| .true. || logical

|-
| sol_fgm_eps ||
Epsilon convergence criteria for none Yin-Yang iterative solver
| 1.d-07 || real*8

|-
| sol_fgm_maxits ||
maximum number of iterations allowed for none Yin-Yang iterative solver
| 200 || integer

|-
| sol_im ||
size of Krylov subspace in iterative solver - should not exceed 100
| 15 || integer

|-
| sol_type_s ||
Type of solver
* 'ITERATIF'
* 'DIRECT'
| 'DIRECT' || character(len=26)

|-
| sol_yyg_eps ||
Epsilon convergence criteria for the Yin-Yang iterative solver
| 1.d-04 || real*8

|-
| sol_yyg_maxits ||
maximum number of iterations allowed for the Yin-Yang iterative solver
| 40 || integer

|-
| spn_cutoff_scale_large ||
The filter will be set zero for smaller scales (in km)
| 300. || real

|-
| spn_cutoff_scale_small ||
The filter will be set 1.0 for larger scales (in km) between
Spn_cutoff_scale_small and Spn_cutoff_scale_large,
the filter will have a COS2 transition.
| 100. || real

|-
| spn_nudging_s ||
Spectral nudging list of variables (eg. 'UVT' or 'UV')
| ' ' || character(len=16)

|-
| spn_relax_hours ||
Nudging relaxation timescale (eg. 10 hours )
| 10. || real

|-
| spn_start_lev ||
Nudging profile lower end in hyb level (eg. 1.0 or 0.8)
If use 0.8, the profile will be set zero when hyb > 0.8
| 1.0 || real

|-
| spn_step ||
Nudging interval in seconds (eg. 1800, means nudging is performed
every every 30 minutes)
| 21600 || integer

|-
| spn_trans_shape_s ||
Nudging profile transition shape('COS2' or 'LINEAR')
Set the shape between Spn_start_lev and Spn_up_const_lev
| 'LINEAR' || character(len=16)

|-
| spn_up_const_lev ||
Nudging profile upper end in hyb level (eg. 0.0 or 0.2)
If use 0.2, the profile wll be set 1.0 when hyb < 0.2
| 0.0 || real

|-
| spn_weight_l ||
Nudging weight in temporal space (.true. or .false.).
If the driving fields are available every 6 hours and Spn_step is
set to 30 minutes then nudging will have more weight every six hours
when the driving fields are available
| .false. || logical

|-
| spn_wt_pwr ||
The weight factor when Spn_weight_L=.true.
(The weigh factor is COS2**(Spn_wt_pwr), Spn_wt_pwr could  be set as
0, 2, 4, 6. If Spn_wt_pwr = 2, weight factor is COS2)
| 2 || integer

|-
| stat_liste ||
list of variables to do blocstat.
Any gmm variable name, or predefine lists :
* 'ALL'
* 'ALL_DYN_T0'
* 'ALL_DYN_T1'
* 'ALL_TR_T0'
* 'ALL_TR_T1'
| ' ' || character(len=32)

|-
| tr3d_anydate_l ||
True-> tracers validity time does not have to match analysis
| .false. || logical

|-
| tr3d_default_s ||
Override for default tracers attributes
| ' ' || character(len=512)

|-
| tr3d_list_s ||
list of tracers to be read from analyse
|  || 

|-
| vspng_coeftop ||
Top coefficient for del-2 diffusion (m2/s)
| -1. || real

|-
| vspng_nk ||
Number of levels from the top of the model
| 0 || integer

|-
| vspng_riley_l ||
True-> Riley diffusion on vertical motion on Vspng_nk levels
| .false. || logical

|-
| vtopo_length_s ||
On which length of time to evolve topography
| '' || character(len=16)

|-
| vtopo_start_s ||
Time at which to start evolving topography toward target
| '' || character(len=16)

|-
| zdot_divhlm_l ||
True-> divergence high level modulation in initial computation of Zdot
| .false. || logical
|}
=== gem_cfgs Namelist  ===

{| class="wikitable"
|-
! style="width: 10em;" | Name
! style="width: 40em;" | Description
! style="width: 10em;" | Default Value
! Type


|-
| cstv_ba_8 ||
SL off-centering parameter for hydrostatic
| 0.6 || real*8

|-
| cstv_ba_m_8 ||
SL off-centering parameter for the momentum equations
| 0.6 || real*8

|-
| cstv_ba_nh_8 ||
SL off-centering parameter for nonhydrostatic
| 0.5 || real*8

|-
| cstv_psadj_8 ||
Fraction of adjustment to be given to the ocean
| 1.d0 || real*8

|-
| cstv_psref_8 ||
another reference pressure
| 1.d5 || real*8

|-
| cstv_re_8 ||
Parameter controlling modified epsilon (Ver_epsi_8) [nonhydrostatic part]
| 1.d0 || real*8

|-
| cstv_tstr_8 ||
T* basic state temperature (K)
| 240.0 || real*8

|-
| eq_ramp_l ||
Latitudinal ramping of equatorial sponge
| .false. || logical

|-
| eq_sponge ||
Coefficients that multiply KM to simulate sponge layer near the top
of the model. Warning! if this parameter is used, the EPONGE in the
physics namelist should be removed.
|  || 

|-
| g_halox ||
number of points for the halo on X
| 4 || integer

|-
| g_haloy ||
number of points for the halo on Y
| 4 || integer

|-
| heap_nk ||
Heap memory will be painted to NaN using an array wrk01(G_ni,G_nj,Heap_nk)
| -1 || integer

|-
| hyb ||
array of model levels ,  0.0 < HYB < 1.0
|  || 

|-
| hyb_rcoef ||
pair of coefficients (min,max) to control the flattenning of the
vertical coordinate
|  || 

|-
| hzd_div_damp ||
Fraction of the maximum divergence damping - range(0.0-1.0)
| -1. || real

|-
| hzd_lnr ||
Background 2 delta-x removal ratio - range(0.0-1.0)
| -1. || real

|-
| hzd_lnr_theta ||
Theta 2 delta-x removal ratio - range(0.0-1.0).
| -1. || real

|-
| hzd_lnr_tr ||
Tracers 2 delta-x removal ratio - range(0.0-1.0)
| -1. || real

|-
| hzd_pwr ||
Order of the background diffusion operator
2, 4, 6, 8
| -1 || integer

|-
| hzd_pwr_theta ||
Order of the background diffusion operator on theta
2, 4, 6, 8
| -1 || integer

|-
| hzd_pwr_tr ||
Order of the background diffusion operator on tracers
| -1 || integer

|-
| hzd_smago_fric_heat ||
Frictional heating is considered when Hzd_smago_fric_heat>0.
| 0. || real

|-
| hzd_smago_lev ||
The levels (bot,top) in the hybrid coordinate where the background diffusion
coefficient varies between the value defined by Hzd_smago_lnr(1) and Hzd_smago_lnr(2).
|  || 

|-
| hzd_smago_lnr ||
Coefficient of background diffusion added to the coefficient computed using the
Smagorinsky approach. The first element of the array determines the constant value
of background diffusion coeff. below Hzd_smago_lev(1). The second element represents
the value at Hzd_smago_lev(2). The third element determines the maximum coefficient
at the model top. Two ramps of COS^2-type are used between Hzd_smago_lev(1) and
Hzd_smago_lev (2), and between Hzd_smago_lev(2) and the model lid.
|  || 

|-
| hzd_smago_param ||
Main Smagorinsky control parameter (usual range 0.1-0.3)
| -1. || real

|-
| hzd_smago_prandtl ||
Apply Smago diffusion on theta using Hzd_smago_param/Hzd_smago_prandtl parameter
| -1. || real

|-
| hzd_smago_prandtl_hu ||
Apply Smago diffusion on HU using Hzd_smago_param/Hzd_smago_prandtl_hu parameter
| -1. || real

|-
| hzd_smago_theta_base_l ||
If TRUE then background diffusion is applied to THETA and HU.
| .true. || logical

|-
| iau_cutoff ||
Filter cutoff period for Iau_weight_S='sin' in hours
| 6. || real

|-
| iau_input_type_s ||
IAU Input TYPE
* 'OLD ' : GEM 4.8 physic's input, MPI blocking based
* 'IO  ' : new input system, RPN_COMM_IO/RPN_COMM_ezshuf_dist based
* 'BLOC' : new input system, RPN_COMM_bloc based
| 'OLD' || character(len=16)

|-
| iau_interval ||
The number of seconds between increment fields
| -1. || real

|-
| iau_ninblocx ||
IAU Input PE blocking along npex
| 1 || integer

|-
| iau_ninblocy ||
IAU Input PE blocking along npey
| 1 || integer

|-
| iau_period ||
The number of seconds over which IAU will be  will be run
(typically the length of the assimilation window).
Default < 0 means that no IAUs are applied.
| -1. || real

|-
| iau_stats_l ||
IAU Input Stats
| .false. || logical

|-
| iau_tracers_s ||
An optional list of tracers to be incremented.
|  || 

|-
| iau_weight_s ||
The type of weighting function to be applied to the analysis increments:
* 'constant' (default) uniform increments
* 'sin' DF-style weights (Fillion et al. 1995)
| 'constant' || character(len=64)

|-
| init_balgm_l ||
true -> Digital filter initialization is performed
| .false. || logical

|-
| init_dflength_s ||
number of points for digital filter (equals the number of timesteps +1)
| '5p' || character(len=16)

|-
| init_dfpl_s ||
period limit of digital filter units D,H,M,S
| '6h' || character(len=16)

|-
| init_dftr_l ||
* true -> passive tracers digitally filtered
* false-> passive tracers set to result obtained at mid-period during initialization period (no filtering)
| .false. || logical

|-
| init_dfwin_l ||
true -> Windowing is applied
| .true. || logical

|-
| inp_blacklist_s ||
List of variables to NOT process during input
|  || 

|-
| inp_npes ||
Number of PEs to use for input
| 1 || integer

|-
| inp_vertintype_tracers_s ||
Type of vertical interpolation scheme
| 'cubic' || character(len=8)

|-
| lam_0ptend_l ||
True-> for blending to zero the physics tendency in blending area
| .true. || logical

|-
| lam_blend_h ||
Number of points for horizontal blending
| 10 || integer

|-
| lam_blend_t ||
Number of levels for top blending
| 0 || integer

|-
| lam_blendoro_l ||
True-> to blend the model topography with the pilot topography
| .true. || logical

|-
| lam_ctebcs_l ||
True-> to force constant (fixed) boundary conditions
| .false. || logical

|-
| lam_gbpil_t ||
Number of levels for top piloting
| -1 || integer

|-
| lam_hint_s ||
Type of horizontal interpolation to model grid
* 'CUB_LAG'
* 'LINEAR'
* 'NEAREST'
| 'CUB_LAG' || character(len=16)

|-
| lam_toptt_l ||
True-> The plane of the top temperature layer is completely
overwritten from the 2D pilot data
| .false. || logical

|-
| lctl_cktimeleft_l ||
True->to check for time left in job
| .false. || logical

|-
| lctl_debug_l ||
True->to print more information to std output
| .false. || logical

|-
| lctl_rxstat_s ||
precision in print glbstats
* 'LCL_4'
* 'GLB_8'
| 'LCL_4' || character(len=6)

|-
| out3_cliph_l ||
True-> to clip humidity variables on output
| .false. || logical

|-
| out3_close_interval_s ||
Interval of output file name change
| ' ' || character(len=16)

|-
| out3_etik_s ||
'etiket' used for output fields
| 'GEMDM' || character(len=12)

|-
| out3_ip3 ||
Default value for IP3 is 0, -1 for IP3 to contain step number,
>0 for given IP3
| 0 || integer

|-
| out3_lieb_conv ||
Precision criteria for the Liebman procedure
| 0.1 || real

|-
| out3_lieb_levels ||
List of levels for underground extrapolation
|  || 

|-
| out3_lieb_maxite ||
Maximum number of iterations for the Liebman procedure
| 100 || integer

|-
| out3_liebxch_iter ||
number of iterations to exchange halo for the Liebman procedure
| 4 || integer

|-
| out3_linbot ||
Number of layers close to the bottom of the model within which a
linear interpolation of GZ will be performed
| 0 || integer

|-
| out3_nbitg ||
Packing factor used for all variables except for those defined in
Out_xnbits_s
| 16 || integer

|-
| out3_ndigits ||
Minimum of digits used to represent output units
| 3 || integer

|-
| out3_npes ||
Total number of PEs for output using MFV collector
| 1 || integer

|-
| out3_npex ||
Total number of PEs along npex for output using MID collector
| -1 || integer

|-
| out3_npey ||
Total number of PEs along npey for output using MID collector
| -1 || integer

|-
| out3_postproc_fact ||
Sortie jobs lauched every Out3_postproc_fact*Out3_close_interval_S
| 0 || integer

|-
| out3_vinterp_type_s ||
Vertical interpolation scheme for output
| 'linear' || character(len=12)

|-
| p_lmvd_high_lat ||
Latitude at which the multiplication factor becomes P_lmvd_weigh_high_lat
| 30.0 || real

|-
| p_lmvd_low_lat ||
latitude at which the multiplication factor becomes P_lmvd_weigh_low_lat
| 5.0 || real

|-
| p_lmvd_weigh_high_lat ||
Multiplication factor of P_pbl_spng at latitude P_lmvd_high_lat
| 1.0 || real

|-
| p_lmvd_weigh_low_lat ||
Multiplication factor of P_pbl_spng at latitude P_lmvd_low_lat
| 1.0 || real

|-
| perturb_nbits ||
Number of bits to perturb on initial conditions
| 0 || integer

|-
| perturb_npts ||
Stride for perturbation on initial conditions
| 10 || integer

|-
| schm_adcub_l ||
* True-> cubic interpolation
* False-> linear interpolation
| .true. || logical

|-
| schm_advec ||
* 0   ->          NO advection
* 1   -> traditional advection
* 2   -> consistent advection with respect to off-centering
* 3   -> reversed advection with respect to off-centering
| 1 || integer

|-
| schm_autobar_l ||
True-> auto barotropic option
| .false. || logical

|-
| schm_bcavg_l ||
True-> averaging B and C in SLEVE scheme
| .true. || logical

|-
| schm_bitpattern_l ||
True-> Modify slightly code behaviour to ensure bitpattern
reproduction in restart mode using FST file
| .false. || logical

|-
| schm_capa_var_l ||
True-> variable cappa in thermodynamic equation
| .false. || logical

|-
| schm_cub_traj_l ||
Use cubic interpolation in trajectory computation
| .true. || logical

|-
| schm_dry_mixing_ratio_l ||
True->
| .false. || logical

|-
| schm_eulmtn_l ||
True-> Eulerian treatment of mountains in the continuity equation
| .false. || logical

|-
| schm_hydro_l ||
* True-> hydrostatic
* False-> non-hydrostatic
| .false. || logical

|-
| schm_hzdadw_l ||
True-> horizontal diffusion of momentum at each CN iteration
| .false. || logical

|-
| schm_itcn ||
Number of iterations for Crank-Nicholson
| 2 || integer

|-
| schm_itnlh ||
Number of iterations to solve non-linear Helmholtz problem
| 2 || integer

|-
| schm_itraj ||
Number of iterations to compute trajectories
| 3 || integer

|-
| schm_nblendyy ||
*  -1: no blending between Yin and Yang
*   0: blending at init only
* > 0: blending at every nblendyy timestep
| -1 || integer

|-
| schm_phycpl_s ||
Physics coupling strategy
| 'split' || character(len=16)

|-
| schm_psadj ||
* 0 -> No conservation of surface pressure
* 1 -> Conservation of Total air mass Pressure
* 2 -> Conservation of Dry air mass Pressure
| 0 || integer

|-
| schm_psadj_lam_l ||
Confirmation to use psadjust with a LAM configuration
| .false. || logical

|-
| schm_psadj_print_l ||
True-> print dry/wet air masses
| .false. || logical

|-
| schm_topo_l ||
True-> to use topography
| .true. || logical

|-
| schm_trapeze_l ||
Use trapezoidal average for advection winds
| .true. || logical

|-
| schm_wload_l ||
Apply water loading in the calculations
| .false. || logical

|-
| sol2d_precond_s ||
2D preconditioner for iterative solver
| 'JACOBI' || character(len=26)

|-
| sol3d_krylov_s ||
Krylov method for 3d iterative solver (FGMRES or FBICGSTAB)
| 'FGMRES' || character(len=26)

|-
| sol3d_precond_s ||
3D preconditioner for iterative solver
| 'JACOBI' || character(len=26)

|-
| sol_fft_l ||
* True-> use FFT solver if possible
* False-> use MXMA solver (slower,less precise)
| .true. || logical

|-
| sol_fgm_eps ||
Epsilon convergence criteria for none Yin-Yang iterative solver
| 1.d-07 || real*8

|-
| sol_fgm_maxits ||
maximum number of iterations allowed for none Yin-Yang iterative solver
| 200 || integer

|-
| sol_im ||
size of Krylov subspace in iterative solver - should not exceed 100
| 15 || integer

|-
| sol_type_s ||
Type of solver
* 'ITERATIF'
* 'DIRECT'
| 'DIRECT' || character(len=26)

|-
| sol_yyg_eps ||
Epsilon convergence criteria for the Yin-Yang iterative solver
| 1.d-04 || real*8

|-
| sol_yyg_maxits ||
maximum number of iterations allowed for the Yin-Yang iterative solver
| 40 || integer

|-
| spn_cutoff_scale_large ||
The filter will be set zero for smaller scales (in km)
| 300. || real

|-
| spn_cutoff_scale_small ||
The filter will be set 1.0 for larger scales (in km) between
Spn_cutoff_scale_small and Spn_cutoff_scale_large,
the filter will have a COS2 transition.
| 100. || real

|-
| spn_nudging_s ||
Spectral nudging list of variables (eg. 'UVT' or 'UV')
| ' ' || character(len=16)

|-
| spn_relax_hours ||
Nudging relaxation timescale (eg. 10 hours )
| 10. || real

|-
| spn_start_lev ||
Nudging profile lower end in hyb level (eg. 1.0 or 0.8)
If use 0.8, the profile will be set zero when hyb > 0.8
| 1.0 || real

|-
| spn_step ||
Nudging interval in seconds (eg. 1800, means nudging is performed
every every 30 minutes)
| 21600 || integer

|-
| spn_trans_shape_s ||
Nudging profile transition shape('COS2' or 'LINEAR')
Set the shape between Spn_start_lev and Spn_up_const_lev
| 'LINEAR' || character(len=16)

|-
| spn_up_const_lev ||
Nudging profile upper end in hyb level (eg. 0.0 or 0.2)
If use 0.2, the profile wll be set 1.0 when hyb < 0.2
| 0.0 || real

|-
| spn_weight_l ||
Nudging weight in temporal space (.true. or .false.).
If the driving fields are available every 6 hours and Spn_step is
set to 30 minutes then nudging will have more weight every six hours
when the driving fields are available
| .false. || logical

|-
| spn_wt_pwr ||
The weight factor when Spn_weight_L=.true.
(The weigh factor is COS2**(Spn_wt_pwr), Spn_wt_pwr could  be set as
0, 2, 4, 6. If Spn_wt_pwr = 2, weight factor is COS2)
| 2 || integer

|-
| stat_liste ||
list of variables to do blocstat.
Any gmm variable name, or predefine lists :
* 'ALL'
* 'ALL_DYN_T0'
* 'ALL_DYN_T1'
* 'ALL_TR_T0'
* 'ALL_TR_T1'
| ' ' || character(len=32)

|-
| tr3d_anydate_l ||
True-> tracers validity time does not have to match analysis
| .false. || logical

|-
| tr3d_default_s ||
Override for default tracers attributes
| ' ' || character(len=512)

|-
| tr3d_list_s ||
list of tracers to be read from analyse
|  || 

|-
| vspng_coeftop ||
Top coefficient for del-2 diffusion (m2/s)
| -1. || real

|-
| vspng_nk ||
Number of levels from the top of the model
| 0 || integer

|-
| vspng_riley_l ||
True-> Riley diffusion on vertical motion on Vspng_nk levels
| .false. || logical

|-
| vtopo_length_s ||
On which length of time to evolve topography
| '' || character(len=16)

|-
| vtopo_start_s ||
Time at which to start evolving topography toward target
| '' || character(len=16)

|-
| zdot_divhlm_l ||
True-> divergence high level modulation in initial computation of Zdot
| .false. || logical
|}
=== grdc Namelist  ===

{| class="wikitable"
|-
! style="width: 10em;" | Name
! style="width: 40em;" | Description
! style="width: 10em;" | Default Value
! Type


|-
| grdc_dx ||
x horizontal resolution of target cascade grid (degrees)
| -1. || real

|-
| grdc_dy ||
y horizontal resolution of target cascade grid (degrees)
| -1. || real

|-
| grdc_end_s ||
Time string (units D, H, M or S) from the start of the run to
stop producing the cascade files
| ' ' || character(len=15)

|-
| grdc_hblen ||
Number of points for the blending zone (Hblen_x)
| 10 || integer

|-
| grdc_initphy_l ||
TRUE to dump out permanent bus for cascade mode
| .false. || logical

|-
| grdc_iref ||
Reference Point I on rotated cascade grid, 1 < Grdc_iref < Grdc_ni
| -1 || integer

|-
| grdc_jref ||
Reference Point J on rotated cascade grid, 1 < Grdc_jref < Grdc_nj
| -1 || integer

|-
| grdc_latr ||
Latitude on rotated grid of ref point, Grdc_iref,Grdc_jref (degrees)
| 0. || real

|-
| grdc_lonr ||
Longitude on rotated grid of ref point, Grdc_iref,Grdc_jref (degrees)
| 180. || real

|-
| grdc_maxcfl ||
Max Supported Courrant number;
Pilot area=Grdc_maxcfl +Grdc_bsc_base+Grdc_bsc_ext1
| 1 || integer

|-
| grdc_nbits ||
Number of bits for the packing factor
| 32 || integer

|-
| grdc_nfe ||
Nesting interval specified with digits ending with one character
for the units:
* S : seconds
* D : days
* M : minutes
* H : hours
| ' ' || character(len=15)

|-
| grdc_ni ||
Number of points along X
| 0 || integer

|-
| grdc_nj ||
Number of points along Y
| 0 || integer

|-
| grdc_start_s ||
Time string (units D, H, M or S) from the start of the run to
start producing the cascade files
| ' ' || character(len=15)

|-
| grdc_trnm_s ||
List of tracers to be written from piloting run
| '@#$%' || character(len=4)
|}
=== grid Namelist  ===

{| class="wikitable"
|-
! style="width: 10em;" | Name
! style="width: 40em;" | Description
! style="width: 10em;" | Default Value
! Type


|-
| grd_dx ||
(LU only) Mesh length (resolution) in x-direction (degrees)
| 0. || real

|-
| grd_dy ||
(LU only) Mesh length (resolution) in y-direction (degrees)
| 0. || real

|-
| grd_iref ||
Reference Point I on rotated grid, 1 < Grd_iref < Grd_ni
| -1 || integer

|-
| grd_jref ||
Reference Point J on rotated grid, 1 < Grd_jref < Grd_nj
| -1 || integer

|-
| grd_latr ||
Latitude on rotated grid of reference point, Grd_iref,Grd_jref (degrees)
| 0. || real

|-
| grd_lonr ||
Longitude on rotated grid of reference point, Grd_iref,Grd_jref (degrees)
| 180. || real

|-
| grd_maxcfl ||
Max Supported Courrant number;
Pilot area=Grd_maxcfl +Grd_bsc_base+Grd_bsc_ext1
| 1 || integer

|-
| grd_ni ||
Number of points along NI
| 0 || integer

|-
| grd_nj ||
Number of points along NJ
| 0 || integer

|-
| grd_overlap ||
(GY only) Overlap extent along latitude axis for GY grid (degrees)
| 0. || real

|-
| grd_typ_s ||
Type of grid described using 2 characters:
* "GY" : Global Yin-Yang
* "LU" : LAM    Uniform
| 'GY' || character(len=2)

|-
| grd_xlat1 ||
Geographic longitude of the center of the computational domain (degrees)
| 0. || real

|-
| grd_xlat2 ||
Geographic latitude of a point on the equator of the computational domain
east of  Grd_xlon1,Grd_xlat1  (degrees)
| 0. || real

|-
| grd_xlon1 ||
Geographic latitude of the center of the computational domain (degrees)
| 180. || real

|-
| grd_xlon2 ||
Geographic longitude of a point on the equator of the computational domain
east of Grd_xlon1,Grd_xlat1  (degrees)
| 270. || real
|}
=== mtn_cfgs Namelist  ===

{| class="wikitable"
|-
! style="width: 10em;" | Name
! style="width: 40em;" | Description
! style="width: 10em;" | Default Value
! Type


|-
| mtn_dx ||

| 500. || real

|-
| mtn_dz ||

| 300. || real

|-
| mtn_flo ||

| 10. || real

|-
| mtn_hght ||

| 250. || real

|-
| mtn_hwx ||

| 10. || real

|-
| mtn_hwx1 ||

| 8. || real

|-
| mtn_ni ||

| 401 || integer

|-
| mtn_nj ||

| 1 || integer

|-
| mtn_nk ||

| 65 || integer

|-
| mtn_nstar ||

| 0.01 || real

|-
| mtn_tzero ||

| 303.16 || real

|-
| mtn_zblen_thk ||

| 0. || real
|}
=== resources Namelist  ===

{| class="wikitable"
|-
! style="width: 10em;" | Name
! style="width: 40em;" | Description
! style="width: 10em;" | Default Value
! Type


|-
| ptopo_npex ||

|  || 

|-
| ptopo_nthreads_dyn, ||

|  || 
|}
=== step Namelist  ===

{| class="wikitable"
|-
! style="width: 10em;" | Name
! style="width: 40em;" | Description
! style="width: 10em;" | Default Value
! Type


|-
| fcst_bkup_additional_s ||
Save a restart file + continue at that time
| 'NIL' || character(len=16)

|-
| fcst_bkup_s ||
Save a restart file + continue every Fcst_bkup_S
| 'NIL' || character(len=16)

|-
| fcst_end_s ||
End date for model run slice (yyyymmdd.hhmmss)
| ' ' || character(len=16)

|-
| fcst_gstat_s ||
Output global stat (glbstat) every Fcst_gstat_S
| ' ' || character(len=16)

|-
| fcst_nesdt_s ||
Read nesting data every Fcst_nesdt_S
| ' ' || character(len=16)

|-
| fcst_rstrt_s ||
Save a restart file + stop every Fcst_rstrt_S
| ' ' || character(len=16)

|-
| fcst_spinphy_s ||

| ' ' || character(len=16)

|-
| fcst_start_s ||
Starting date for model run slice (yyyymmdd.hhmmss)
| ' ' || character(len=16)

|-
| step_alarm ||
Setting for Fortran alarm time
| 600 || integer

|-
| step_dt ||
Length of model timestep (sec)
| -1. || real*8

|-
| step_leapyears_l ||
Account for leap years
| .true. || logical

|-
| step_runstrt_s ||
Starting date for model run  (yyyymmdd.hhmmss)
| 'NIL' || character(len=16)
|}
=== theo_cfgs Namelist  ===

{| class="wikitable"
|-
! style="width: 10em;" | Name
! style="width: 40em;" | Description
! style="width: 10em;" | Default Value
! Type


|-
| theo_case_s ||

| 'NONE' || character(len=15)
|}
=== dcmip Namelist  ===

{| class="wikitable"
|-
! style="width: 10em;" | Name
! style="width: 40em;" | Description
! style="width: 10em;" | Default Value
! Type


|-
| dcmip_case ||
Dcmip case selector
* Dcmip_case=0 (none)
* Dcmip_case=11 (3D deformational flow)
* Dcmip_case=12 (3D Hadley-like meridional circulation)
* Dcmip_case=13 (2D solid-body rotation of thin cloud-like tracer in the presence of orography)
* Dcmip_case=20 (Steady-state at rest in presence of oro.)
* Dcmip_case=21 (Mountain waves over a Schaer-type mountain)
* Dcmip_case=22 (As 21 but with wind shear)
* Dcmip_case=31 (Gravity wave along the equator)
* Dcmip_case=41 (Dry Baroclinic Instability Small Planet)
* Dcmip_case=43 (Moist Baroclinic Instability Simple physics)
* Dcmip_case=161 (Baroclinic wave with Toy Terminal Chemistry)
* Dcmip_case=162 (Tropical cyclone)
* Dcmip_case=163 (Supercell -Small Planet-)
| 0 || integer

|-
| dcmip_lower_value ||
Set lower value of Tracer in Terminator
* Dcmip_lower_value=0 (free)
* Dcmip_lower_value=1 (0)
* Dcmip_lower_value=2 (1.0e-15)
| 0 || integer

|-
| dcmip_moist ||
Account for moisture
* Dcmip_moist=0 (dry)
* Dcmip_moist=1 (moist)
| 1 || integer

|-
| dcmip_nuz_th ||
Vertical Diffusion Theta (if <0,we remove REF)
| 0. || real

|-
| dcmip_nuz_tr ||
Vertical Diffusion Tracers (if <0,we remove REF)
| 0. || real

|-
| dcmip_nuz_wd ||
Vertical Diffusion Winds (if <0,we remove REF)
| 0. || real

|-
| dcmip_pbl_type ||
Type of planetary boundary layer
* Dcmip_pbl_type=-1 (none)
* Dcmip_pbl_type=0 (Reed-Jablonowski Boundary layer)
* Dcmip_pbl_type=1 (Georges Bryan Planetary Boundary Layer)
| -1 || integer

|-
| dcmip_prec_type ||
Type of precipitation/microphysics
* Dcmip_prec_type=-1 (none)
* Dcmip_prec_type=0 (Large-scale precipitation -Kessler-)
* Dcmip_prec_type=1 (Large-scale precipitation -Reed-Jablonowski-)
| -1 || integer

|-
| dcmip_rayleigh_friction_l ||
Do Rayleigh friction if T
| .false. || logical

|-
| dcmip_terminator_l ||
Do Terminator chemistry if T
| .false. || logical

|-
| dcmip_x ||
Earth's radius reduction factor
| 1.d0 || real*8
|}
=== williamson Namelist  ===

{| class="wikitable"
|-
! style="width: 10em;" | Name
! style="width: 40em;" | Description
! style="width: 10em;" | Default Value
! Type


|-
| williamson_alpha ||
Rotation angle  in DEGREE - W_NAIR=0)
| 0. || real

|-
| williamson_case ||
Williamson case selector
* Williamson_case=0 (none)
* Williamson_case=1 (Advection 2D - Williamson_NAIR/Terminator_L)
* Williamson_case=2 (Steady-state nonlinear zonal geostrophic flow - Williamson et al.,1992,JCP,102,211-224)
* Williamson_case=5 (Zonal flow over an isolated mountain - Williamson et al.,1992,JCP,102,211-224)
* Williamson_case=6 (Rossby-Haurwitz wave - Williamson et al.,1992,JCP,102,211-224)
* Williamson_case=7 (The 21 December 1978 case - Williamson et al.,1992,JCP,102,211-224)
* Williamson_case=8 (Galewsky's barotropic wave - Galewsky et al.,2004,Tellus,56A,429-440)
| 0 || integer

|-
| williamson_clat0 ||
LAT cosine Bell  in DEGREE - W_NAIR=0)
| 0. || real

|-
| williamson_clon0 ||
LON cosine Bell  in DEGREE - W_NAIR=0)
| 270. ! 3*pi/2 rad in the paper || real

|-
| williamson_lower_value ||
Set lower value of Tracer in Terminator
* Williamson_lower_value=0 (free)
* Williamson_lower_value=1 (0)
* Williamson_lower_value=2 (1.0e-15)
| 0 || integer

|-
| williamson_nair ||
Used when Williamson_case=1
* Williamson_NAIR=0 (Solid body rotation of a cosine bell - Williamson et al.,1992,JCP,102,211-224)
* Williamson_NAIR=1 (Deformational Non-divergent winds - Lauritzen et al.,2012,GMD,5,887-901)
* Williamson_NAIR=2 (Deformational divergent winds - Lauritzen et al.,2012,GMD,5,887-901)
* Williamson_NAIR=3 (Deformational Flow for Circular vortex - Nair and Machenhauer,2002,MWR,130,649-667)
| 0 || integer

|-
| williamson_period ||
rotation period in SECS - W_NAIR=0)
| 12.*24.*3600. || real

|-
| williamson_rlat0 ||
LAT rot.POLE  in DEGREE - W_NAIR=3)
| 0. || real

|-
| williamson_rlon0 ||
LON rot.POLE  in DEGREE - W_NAIR=0/3)
| 0. || real

|-
| williamson_terminator_l ||
Do Terminator chemistry if T
| .false. || logical
|}


=== convection_cfgs Namelist  ===

{| class="wikitable"
|-
! style="width: 10em;" | Name
! style="width: 40em;" | Description
! style="width: 10em;" | Default Value
! Type


|-
| bkf_closures ||
Select closures for shallow convection
* 'CAPE'
* 'EQUILIBRIUM'
| 'CAPE' || character(len=16)

|-
| bkf_detrains ||
Select formulation of fractional detrainment rate for shallow convection
* 'BECHTOLD01'
* 'CUIJPERS95'
* 'DEROOY10'
| 'BECHTOLD01' || character(len=16)

|-
| bkf_entrains ||
Select formulation of fractional entrainment rate for shallow convection
* 'BECHTOLD01'
* 'BECHTOLD08'
* 'DEROOY11'
* 'SIEBESMA03'
| 'BECHTOLD01' || character(len=16)

|-
| bkf_evaps ||
Evaporate detrained condensate in shallow convection
| .false. || logical

|-
| bkf_kch ||
Number of species for convective transport (never tested)
| 0 || integer

|-
| bkf_kens ||
Number of additional ensemble members (max 3) for deep bkf convection
| 0 || integer

|-
| bkf_kice ||
Take ice phase into account in deep bkf (yes=1)
| 1 || integer

|-
| bkf_ktdia ||
Limit vertical computation by ktdia-1 levels
| 1 || integer

|-
| bkf_lch1conv ||
Activate convective transport of species for deep and shallow bkf
| .false. || logical

|-
| bkf_ldown ||
Allow downdrafts in deep bkf
| .true. || logical

|-
| bkf_lshalm ||
Activate shallow convective momentum transport
| .false. || logical

|-
| bkf_rads ||
Cloud radii at LCL for bkf_shallow
from bkf_rads(1) to bkf_rads(2)
with increment bkf_rads(3)
| (/50., 50., 0./) || real

|-
| bkf_tperts ||
Temperature perturbations at LCL for triggering bkf_shallow
An ensemble of shall. cumuli will be generated using perturbations
starting from  bkf_tperts(1) to bkf_tperts(2)
with increment bkf_tperts(3)
| (/0.2, 0.2, 0./) || real

|-
| deep ||
Deep convection scheme name
* 'NIL     ' :
* 'SEC     ' :
* 'OLDKUO  ' :
* 'KUOSTD  ' :
* 'KFC     ' :
* 'KFC2    ' :
* 'KFC3    ' :
* 'BECHTOLD' :
| 'nil' || character(len=16)

|-
| deep_cloudobj ||
Treat convective clouds as cloud objects
| .false. || logical

|-
| deep_codecay ||
Decay timescale for convective cloud objects (seconds)
| 600. || real

|-
| deep_conserve ||
Conservation corrections for deep convective scheme
* 'NIL   ' : No conservation correction applied
* 'TEND  ' : Temperature and moisture tendencies corrected
* 'PRECIP' : Surface precipitation rate corrected
| 'PRECIP' || character(len=16)

|-
| deep_timeconv ||

| -1. || real

|-
| deep_timeent ||

| -1. || real

|-
| deep_timerefresh ||

| -1. || real

|-
| kfcdepth ||
Minimum depth of conv. updraft for KFC  trigger (m)
| 4000. || real

|-
| kfcdpdd ||
Maximum depth of the downdraft detrainment layer (Pa) for 'kfc2' and 'kfc3'
| 10000. || real

|-
| kfcmom ||
generate wind tendencies in KFC or deep BKF if .true.
| .false. || logical

|-
| kfcprod ||
Compute production terms for Kain-Fritsch scheme
| .false. || logical

|-
| kfcrad ||
Initial convective updraft radius in KFC scheme(m)
| 1500. || real

|-
| kfcradw ||
Convective updraft radius over water in KFC scheme(m)
| -1. || real

|-
| kfctaucape ||
Varies convective timescale as a function of CAPE for Kain-Fritsch scheme
KFCTAUCAPE = time1, time2, cmean, dcape
* time1 (s): max kfctimec
* time2 (s): min kfctimec
* cmean (J/Kg): cape value at which kfctimec will be mean of time1 and time2
* dcape (J/Kg): decrease in kfctimec from time1 to time2 will occur over range cmean-dcape to cmean+dcape
| (/-1., -1., -1., -1./) || real

|-
| kfctrig4 ||
Trigger parameter of Kain-Fritsch convection scheme (WKLCL).
Trigger parameter will increase from kfctrig4(3) to kfctrig4(4) [m/s]
between timestep kfctrig4(1) and timestep kfctrig4(2)
| (/0., 0., 0.05, 0.05/) || real

|-
| kfctriga ||
Nominal resolution for which KFCTRIG4 is set.
This is inactive if value <= 0.
| -1.0 || real

|-
| kfctrigl ||
Over land and lakes 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 [m/s]
* and linear interpolation in between TRIGLAT(1) and TRIGLAT(2)
| 0.05 || real

|-
| kfctriglat ||
Logical key for variation of the trigger function depending on latitude and land-sea-lake mask
| .false. || logical

|-
| kfctrigtau ||
Relaxation timescale for trigger velocity
| -1. || real

|-
| kfctrigw ||
Trigger parameter of Kain-Fritsch convection scheme (WKLCL).
Trigger parameter will increase from kfctrigw(3) to kfctrigw(4) [m/s]
between wstar values kfctrigw(1) and kfctrigw(2)
| (/0., 0., 0., 0./) || real

|-
| mid ||
Switch for mid-level convection
* 'NIL' : No mid-level convective scheme
* 'KF ' : Kain-Fritsch-based mid-level convective scheme
| 'nil' || character(len=16)

|-
| mid_conserve ||
Conservation corrections for mid-level convective scheme
* 'NIL   ' : No conservation correction applied
* 'TEND  ' : Temperature and moisture tendencies corrected
* 'PRECIP' : Surface precipitation rate corrected
| 'PRECIP' || character(len=16)

|-
| mid_depth ||
Minimum cloud depth for mid-level convection (m)
| 2000. || real

|-
| mid_dpdd ||
Downdraft detrainment depth for mid-level convection (Pa)
| 6000. || real

|-
| mid_emffrac ||
Fraction of environmental mass flux that enters updrafts
| 'all' || character(len=16)

|-
| mid_emfmod ||
Modulation of the minimum environmental mass flux for mid-level convection
| 'nil' || character(len=16)

|-
| mid_maxcape ||
Maximum deep CAPE (J/kg/m2) for mid-level convective triggering
| -1 || real

|-
| mid_minbase ||
Minimum parcel departure level for mid-level convection (m)
| 500. || real

|-
| mid_minemf ||
Minimum environmental mass flux for mid-level convection (kg/s)
| 1e7 || real

|-
| mid_peff ||

| -1. || real

|-
| shal ||
Switch for shallow convection
* 'NIL'
* 'KTRSNT'
* 'KTRSNT_MG'
* 'BECHTOLD'
| 'nil' || character(len=16)

|-
| shal_conserve ||
Conservation corrections for shallow convective scheme
* 'NIL ' : No conservation correction applied
* 'TEND' : Temperature and moisture tendencies corrected
| 'NIL' || character(len=16)

|-
| shal_timeconv ||

| -1. || real

|-
| triglat ||
Over land and lakes 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)
| 0.0 || real
|}
=== physics_cfgs Namelist  ===

{| class="wikitable"
|-
! style="width: 10em;" | Name
! style="width: 40em;" | Description
! style="width: 10em;" | Default Value
! Type


|-
| acchr ||
Time length (hours) for special time accumulated physics variables
| 0 || integer

|-
| advectke ||
Turbulent kinetic energy advect. is active if .true.
| .false. || logical

|-
| chauf ||
Surface heat flux from oceans is active if .true.
| .true. || logical

|-
| clip_tr_l ||
Clip tracers negative values
| .true. || logical

|-
| cond_conserve ||
Conservation corrections for gridscale condensation
* 'NIL ' : No conservation correction applied
* 'TEND' : Temperature and moisture tendencies corrected
| 'NIL' || character(len=16)

|-
| cond_evap ||
Evaporation parameter for Sunqvist gridscale condensation
| 2.e-4 || real

|-
| cond_hmrst ||
Minimum cloud mixing ratio (kg/kg) for autoconversion in
Sunqvist gridscale condensation
| 3.e-4 || real

|-
| cond_hu0max ||
Max allowed values of modified hu00 (threshold relative humidity
for stratiform condensation, Sunqvist gridscale condensation)
| 0.975 || real

|-
| cond_hu0min ||
Min allowed values of modified hu00 (threshold relative humidity
for stratiform condensation, Sunqvist gridscale condensation)
| 0.85 || real

|-
| cond_infilter ||
Standard deviation length scale (gridpoints) of Gaussian smoother
applied to temperature and humidity inputs for Sunqvist gridscale
condensation)
| -1. || real

|-
| debug_mem_l ||
Activate Debug memory mode
| .false. || logical

|-
| debug_trace_l ||
Print a trace of the phy functions (MSG verbosity = debug)
| .false. || logical

|-
| diag_twind ||
Obtain estimate of surface wind gusts if .true.
| .false. || logical

|-
| diffuw ||
Diffuse vertical motion if .true.
| .false. || logical

|-
| drag ||
Surface friction is active if .true.
Uses Schuman-Newell lapse rate if .false.
| .true. || logical

|-
| etrmin2 ||
Minimal value for TKE in stable case (for 'CLEF')
| 1.E-4 || real

|-
| evap ||
Surface evaporation is active if .true.
| .true. || logical

|-
| fluvert ||
Boundary layer processes
* 'NIL    ': no vertical diffusion
* 'CLEF   ': non-cloudy boundary layer formulation
* 'MOISTKE': cloudy boundary layer formulation
* 'SURFACE': TODO
* 'SIMPLE ': a very simple mixing scheme for neutral PBLs
| 'NIL' || character(len=16)

|-
| fnn_mask ||
(MOISTKE only) Apply factor fnn_reduc
* .false.: everywhere
* .true.: over water only
| .false. || logical

|-
| fnn_reduc ||
(MOISTKE only) Reduction factor (between 0. and 1.) to be applied to the
parameter FNN (turbulent flux enhancement due to boundary layer clouds)
| 1. || real

|-
| fnnmod ||
(CLEF+CONRES only) Non-dimensional parameter (must be >= 1.) that controls
the value of the flux enhancement factor in CONRES
| 2. || real

|-
| fomic ||
Use Fomichev radiation code if .true.
| .false. || logical

|-
| gwdrag ||
Gravity wave drag formulation
* 'NIL  ': no Gravity wave drag
* 'GWD86': gravity wave drag + low-level blocking
* 'SGO16': new formulation (2016) of GWD86
| 'NIL' || character(len=16)

|-
| hines_flux_filter ||
Number of times the 3-point filter will be applied to smooth the GW flux profiles
| 0 || integer

|-
| iheatcal ||
Consider heating from non-orog. drag if = 1
| 0 || integer

|-
| indiag_list_s ||
Comma-separated list of diagnostic level inputs to read.
Default: indiag_list_s(1) = 'DEFAULT LIST',
expanded to: UU, VV, TT, HU + all dynamic Tracers
| ' ' || character(len=32)

|-
| inilwc ||
Initialize water content and cloud fraction seen by radiation for time 0 if .true.
| .false. || logical

|-
| input_type ||

|  || 

|-
| intozot ||
Update ozone climatology during the run
| .false. || logical

|-
| kntrad_s ||
Time between full radiation calculation (units D,H,M,S,P)
| '' || character(len=16)

|-
| kticefrac ||
Compute ice fraction in KTRSNT_MG if .true.
| .true. || logical

|-
| lightning_diag ||
Compute lightning diagnostics if .true.
(currently for Milbrandt-Yau microphysics only)
| .false. || logical

|-
| lmetox ||
Add methane oxydation as source of humidity in the stratosphere if .true.
| .false. || logical

|-
| longmel ||
Mixing length calc. scheme
* 'BLAC62  ': mixing length calc. using Blackadar
* 'BOUJO   ': mixing length calc. using Bougeault
* 'TURBOUJO': mixing length calc. using Bougeault in turbulent regimes (otherwise Blackadar)
* 'LH      ': mixing length calc. using Lenderink and Holtslag
| 'BLAC62' || character(len=16)

|-
| moyhr ||
Time length (hours) for special time averaged physics variables
| 0 || integer

|-
| mp_aeroact ||
Switch for aerosol activation scheme (1 = default, 2 = ARG + Aerosol climatology)
| 1 || integer

|-
| my_ccntype ||
Switch for airmass type (1 = maritime, 2 = continental)
| 1 || integer

|-
| my_dblmom_c ||
Double-moment for cloud (for 'mp_my' only)
| .true. || logical

|-
| my_dblmom_g ||
Double-moment for graupel (for 'mp_my' only)
| .true. || logical

|-
| my_dblmom_h ||
Double-moment for hail (for 'mp_my' only)
| .true. || logical

|-
| my_dblmom_i ||
Double-moment for ice (for 'mp_my' only)
| .true. || logical

|-
| my_dblmom_r ||
Double-moment for rain (for 'mp_my' only)
| .true. || logical

|-
| my_dblmom_s ||
Double-moment for snow (for 'mp_my' only)
| .true. || logical

|-
| my_diagon ||
Compute MY Diagnostic fields if .true.
| .true. || logical

|-
| my_iceon ||
Ice-phase switched on if .true.
| .true. || logical

|-
| my_initn ||
Initialize the number concentration for each category
| .true. || logical

|-
| my_rainon ||
Autoconversion (cloud to rain) switched on
| .true. || logical

|-
| my_sedion ||
Sedimentation switched on
| .true. || logical

|-
| my_snowon ||
Snow initiation switched on
| .true. || logical

|-
| my_tc3comp ||
Parameters for three-component freezing term
| (/-5.,-5.,-5./) || real

|-
| my_warmon ||
Warm-phase switched on
| .true. || logical

|-
| ninblocx ||
Physic input blocking along X
| 1 || integer

|-
| ninblocy ||
Physic input blocking along Y
| 1 || integer

|-
| non_oro ||
Hines non-orographic GWD scheme is active if .true.
| .false. || logical

|-
| non_oro_pbot ||
Pressure (in Pa) that defines the bottom emission level for gravity waves
| 61000.0 || real

|-
| nsloflux ||
Number of timesteps for which surface 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
| 0 || integer

|-
| p3_debug ||
switch for real-time debugging in microphysics (P3)
| .false. || logical

|-
| p3_depfact ||
calibration factor for ice deposition in microphysics (P3)
| 1.0 || real

|-
| p3_dtmax ||
Maximum time step (s) to be taken by the microphysics (P3) scheme, with time-splitting
used to reduce step to below this value if necessary
| 60. || real

|-
| p3_ncat ||
Number of ice-phase hydrometeor categories to use in the P3 microphysics
scheme (currently limited to <5)
| 1 || integer

|-
| p3_pfrac ||
precipitation fraction factor used by SCPF in microphysics (P3)
| 1.0 || real

|-
| p3_resfact ||
model resolution factor used by SCPF in microphysics (P3)
| 1.0 || real

|-
| p3_scpf_on ||
switch for subgrid cloud/precipitation fraction scheme (SCPF) in microphysics (P3)
| .false. || logical

|-
| p3_subfact ||
calibration factor for ice sublimation in microphysics (P3)
| 1.0 || real

|-
| p_runlgt ||
Vectoc lenght physics memory space folding for openMP
| -1 || integer

|-
| pbl_cmu_timeavg ||
Time-averaging of transfer coefficient for momentum to reduce 2-dt
oscillations in fluxes
| .false. || logical

|-
| pbl_conserve ||
Conservation corrections for PBL scheme
* 'NIL ' : No conservation correction applied
* 'TEND' : Temperature and moisture tendencies corrected
| 'NIL' || character(len=16)

|-
| pbl_cucloud ||
Include the turbulent effects of trade wind cumulus clouds
| .true. || logical

|-
| pbl_diff_condens ||
Diffuse condensate fields
| .false. || logical

|-
| pbl_diss ||
Run with a modified closure for the dissipation length scale
* 'NIL  ' : No modified closure for the dissipation length scale
* 'LIM50' : A maximum value of 50m is imposed on dissipation length
| 'NIL' || character(len=16)

|-
| pbl_dissheat ||
Dissipative heating tendencies are computed for the PBL scheme such
that total energy (kinetic + internal) is conserved
* 'NIL       ' : No dissipative heating is computed
* 'LOCAL_K   ' : Local total energy conservation based on diffusion coefficients
* 'LOCAL_TEND' : Local total energy conservation based on wind tendencies
| 'NIL' || character(len=16)

|-
| pbl_flux_consistency ||
Call surface scheme immediately before the PBL
| .false. || logical

|-
| pbl_func_stab ||
Class of stability functions (stable case) to use in the PBL
* 'DELAGE97  ' : Use functions described by Delage (1997; BLM)
* 'LOUIS79   ' : Use functions described by Louis (1979; BLM)
* 'DERBY97   ' : Use functions described by Derbyshire (1997; Cardignton Tech Note)
* 'BELJAARS99' : Use functions described by Beljaars and Viterbo (1999; Clear and Cloudy Boundary Layers)
* 'BELJAARS91' : Use functions described by Beljaars and Holtslag (1991; JAM)
* 'LOCK07    ' : Use functions described by Lock (2007; Tech Report) employed at UKMO
| 'DELAGE97' || character(len=16)

|-
| pbl_func_unstab ||
Class of stability functions (unstable case) to use in the PBL
* 'DELAGE92' : Use functions described by Delage and Girard (1992; BLM)
* 'DYER74  ' : Use functions described by Dyer (1974; BLM)
| 'DELAGE92' || character(len=16)

|-
| pbl_mlblac_max ||
Choose form of asymptotic mixing length for Blacadar-type estimates
* 'BLAC62' : Asymptotic 200 m proposed by Blackadar (1962; JGR) with clipping
* 'LOCK07' : Diagnosed asymptotic scale of Lock (2007; Tech Report) used at UKMO
| 'BLAC62' || character(len=16)

|-
| pbl_mlturb_diss ||
Apply "turboujo" turbulence conditions to dissipation length scale
| .false. || logical

|-
| pbl_moistke_legacy_cloud ||
Run with legacy moistke clouds (no limits on cloud effects)
| .false. || logical

|-
| pbl_nonloc ||
Use the non-local PBL cloud formulation
* 'NIL   ' : no non-local PBL cloud formulation
* 'LOCK06' : Non-local cloud scheme of Lock and Mailhot (2006)
| 'NIL' || character(len=16)

|-
| pbl_ribkg ||
Use the mixing length to average the Richardson number profile of (potentially)
many layers to derive a "background" Ri estimate
| .false. || logical

|-
| pbl_ricrit ||
Richardson num. critical values for hysteresis
| 1. || real

|-
| pbl_shal ||
PBL representation of boundary layer clouds
* 'NIL     ': No Shallow convection
* 'CONRES  ': Bulk Richardson number-based turbulent enhancement
* 'SHALOW  ': Deprecated (see 1998 RPN physics doc)
* 'SHALODQC': Deprecated (see 1998 RPN physics doc)
* 'GELEYN  ': Deprecated (see 1998 RPN physics doc)
| 'NIL' || character(len=16)

|-
| pbl_slblend_layer ||
Layer over which to adjust from SL to PBL stability functions [(bot,top) in m]
|  || 

|-
| pbl_tkediff ||
Adjustment to coefficient for TKE diffusion
| 1. || real

|-
| pbl_tkediff2dt ||
Control of time scale for TKE diffusion
| .false. || logical

|-
| pbl_turbsl_depth ||
Depth (Pa) of the always-turbulent near-surface layer in the PBL
| 3000. || real

|-
| pbl_zerobc ||
Use true (motionless) surface boundary conditions for TKE diffusion
| .false. || logical

|-
| pbl_zntau ||
Relaxation timescale (s) for mixing length smoothing
| 7200. || real

|-
| pcptype ||
Scheme to determine precipitation type
* 'NIL     ': no call to bourge
* 'BOURGE  ': use Bourgouin algorithm (bourge1) to determine precip. types.
* 'BOURGE3D':
| 'NIL' || character(len=16)

|-
| phystat_2d_l ||
Physic statistics output for 3d varables:
* .false. : mean, var, min and max for the whole 3d fiels
* .true.  : mean, var, min and max are done for each levels independently
| .false. || logical

|-
| phystat_dble_l ||
Use double presision for physic statistics output
| .false. || logical

|-
| phystat_freq_s ||
Physic statistics output Frequency
| '0h' || character(len=16)

|-
| phystat_input_l ||
Print stats for phy_input read var
| .false. || logical

|-
| phystat_list_s ||
Physic statistics output: bus variable list that should be included in physics
"block" stats. Possible values:
* Long varnames
* Short varnames
* 'ALLVARS=EDPV': all variables from E, D, P, V buses (any combination of the 4 letters);
| ' ' || character(len=32)

|-
| qcfc11 ||
CFC11 bckgrnd atmospheric concentration (PPMV)
| -1. || real

|-
| qcfc12 ||
CFC12 bckgrnd atmospheric concentration (PPMV)
| -1 || real

|-
| qch4 ||
CH4 bckgrnd atmospheric concentration (PPMV)
| -1. || real

|-
| qco2 ||
CO2 bckgrnd atmospheric concentration (PPMV)
| -1. || real

|-
| qn2o ||
N2O bckgrnd atmospheric concentration (PPMV)
| -1. || real

|-
| rad_atmpath ||
Atmospheric path length for solar radiation
* 'RODGERS67' : Formulation used by Li and Barker (2005)
* 'LI06' : Estimate of  Li and Shibata (2006)
| 'RODGERS67' || character(len=16)

|-
| rad_cond_rei ||

| 15. || real

|-
| rad_cond_rew ||

| -1. || real

|-
| rad_conserve ||
Conservation corrections for radiation scheme
* 'NIL ' : No conservation correction applied
* 'TEND' : Temperature and moisture tendencies corrected
| 'NIL' || character(len=16)

|-
| rad_esfc ||
Use emissivity computed by the surface schemes
| .false. || logical

|-
| radfiles ||
format of radiation files to be read
* 'STD': RPN standard file
* 'UNF': unformatted
| 'STD' || character(len=16)

|-
| radfix ||
Radiation fixes near the model top(for newrad only) if .true.
| .true. || logical

|-
| radfltr ||
Vertical smoothing on radiative fluxes(for newrad only) if .true.
| .true. || logical

|-
| radghg_l ||
Use climatological values of GHG in radiation (CCCMARAD2 only)
| .false. || logical

|-
| radia ||
Radiation scheme
* 'NIL      ': no radiation scheme
* 'NEWRAD   ': complete radiation scheme
* 'CCCMARAD ': most advanced radiation scheme
* 'CCCMARAD2': most advanced radiation scheme v2
| 'NIL' || character(len=16)

|-
| radnivl ||
List of levels on which IR and VIS radiation calculations are
performed (to save on CPU time) (for newrad only)
| 0 || integer

|-
| radslope ||
Key for activation of the radiation along slopes
| .false. || logical

|-
| refract ||
Additional output for low level refraction
| .false. || logical

|-
| rmscon ||
Launching level value of GW RMS wind (m/s) from non-orographic origin
| 1.0 || real

|-
| satuco ||
water/ice phase for saturation calc. if .true.;
water phase only for saturation calc. if .false.
| .true. || logical

|-
| sgo_bhfac ||
Tuning factor for blocking height
| 1.5 || real

|-
| sgo_cdmin ||
Sets the minimum value of the drag coefficient in the orographic
blocking scheme.
| 1.0 || real

|-
| sgo_nldirfac ||
Turns on/off the non-linear amplification factor (depending on wind
direction) of the drag coefficient in the orographic blocking scheme
| .true. || logical

|-
| sgo_phic ||
Critical phase for blocking height
| 0.2 || real

|-
| sgo_stabfac ||
Turns on/off the amplification factor (due to stability) of the drag
coefficient in the orographic blocking scheme
| .true. || logical

|-
| sgo_tdfilter ||
Standard deviation length scale (gridpoints) of Gaussian smoother
applied to wind GWD tendencies
| 1. || real

|-
| sgo_windfac ||
Description of threshold for mean wind speed for blocking
|  || 

|-
| simisccp ||
Run ISCCP cloud simulator (cccmarad only) if .true.
| .false. || logical

|-
| stcond ||
Condensation scheme name
* 'NIL       ' : No explicit condensation scheme used
* 'CONSUN    ' : Sunqvist type condensation scheme
* 'NEWSUND   ' : Sunqvist type condensation scheme
* 'MP_MY2_OLD' : Milbrandtl and Yau microphysics scheme (old formulation)
* 'MP_MY2    ' : Milbrandtl and Yau microphysics scheme
* 'MP_P3     ' : P3 microphysics scheme
| 'NIL' || character(len=16)

|-
| stratos ||
Special treatment of stratosphere;
if .true. ignore convection/condensation tendencies where pressure is lower
than topc or specific humidity is lower than minq as specified in nocld.cdk
| .false. || logical

|-
| taufac ||
Factor used in the gwd formulation = 1/(LENGTH SCALE)
| 8.E-6 || real

|-
| test_phy ||
Run the physics in test harness mode
| .false. || logical

|-
| timings_l ||
Print runtime timings
| .false. || logical

|-
| tofd ||
Select a turbulent orographic form drag scheme
* 'NIL'        : No turbulent orographic form drag scheme
* 'BELJAARS04' : Form drag scheme described by Beljaars et al. (2006; QJRMS)
| 'NIL' || character(len=16)

|-
| ts_flxir ||
(newrad only) Use TT(12000) instead of skin temp in downward IR
flux calculation if .true.
| .false. || logical
|}

=== series Namelist  ===

{| class="wikitable"
|-
! style="width: 10em;" | Name
! style="width: 40em;" | Description
! style="width: 10em;" | Default Value
! Type


|-
| p_serg_serstp ||
Times series package stops at this timestep
| huge(1) || integer

|-
| p_serg_srprf_s ||
List of time series for profile variables
| ' ' || character(len=SER_STRLEN_VAR)

|-
| p_serg_srsrf_s ||
List of time series for surface variables
| ' ' || character(len=SER_STRLEN_VAR)

|-
| p_serg_srwri ||
Number of timesteps between time-series writeout
| 1 || integer

|-
| xst_stn_latlon ||
Stations chosen in lat,lon for time-series
Format: "STN1_NAME",lat1,lon1, "STN2_NAME",lat2,lon2, ...
|  || 
|}
=== surface_cfgs Namelist  ===

{| class="wikitable"
|-
! style="width: 10em;" | Name
! style="width: 40em;" | Description
! style="width: 10em;" | Default Value
! Type


|-
| adj_i0_snow ||
Adjust surface temperature over snow after reading (coherency check)
| .true. || logical

|-
| beta ||
Prandtl number for neutral stability (initialized by SL module)
| 0. || real

|-
| diusst ||
Diurnal SST scheme
* 'NIL    ' : No Diurnal SST scheme
* 'FAIRALL' : #TODO: define
| 'NIL' || character(len=16)

|-
| diusst_coolskin ||
Diurnal SST scheme active coolskin if .true.
| .true. || logical

|-
| diusst_coolskin_lakes ||
Diurnal SST scheme active coolskin over freshwater lakes if .true.
| .true. || logical

|-
| diusst_warmlayer ||
Diurnal SST scheme active warmlayer if .true.
| .true. || logical

|-
| diusst_warmlayer_lakes ||
Diurnal SST scheme active warmlayer over freshwater lakes if .true.
| .true. || logical

|-
| dp_svs ||
Depth of soil layers in [METERS] in SVS land surface scheme (schmsol=SVS)
| -1.0 || real

|-
| ice_emiss ||

| -1. || real

|-
| icelac ||
Set water temperature of ice-covered lakes to 0C for points north of
ice line if .true.
needs an initialization file otherwise the model stops
| .false. || logical

|-
| icemelt ||
Sea ice melting
| .false. || logical

|-
| impflx ||
Implicit surface fluxes if .true.; explicit fluxes if .false.
| .false. || logical

|-
| isba_melting_fix ||
If .true. apply temporary fix to ISBA
* timestep dependent KCOEF
* No PSN factor for meting and freezing
| .false. || logical

|-
| isba_snow_z0veg ||
Use the vegetation-only roughness length to compute vegetation snow fraction
| .false. || logical

|-
| isba_soil_emiss ||

| -1. || real

|-
| isba_zr_freeze ||
If .true., freeze precipitation reaching the ground in sub-zero conditions
| .false. || logical

|-
| kdp ||
Deepest active (permeable) soil layer in SVS land surface scheme (schmsol=SVS)
| -1 || integer

|-
| kntveg_s ||
Vegetation field update frequency (units D,H,M,S,P)
| '' || character(len=16)

|-
| leadfrac ||
Minimum fraction of leads in sea ice.&nbsp; Multiply ice fraction by (1.-leadfrac)
| 0.03 || real

|-
| limsnodp ||
Limit snow depth to 10 cm for calculation of heat conductivity of snow
over sea-ice and glacier if .true.
| .false. || logical

|-
| owflux ||
(coupling) fluxes over ocean are taken from ocean model if .true.
| .false. || logical

|-
| read_emis ||
read-in land surface emissivity if .true.
| .false. || logical

|-
| salty_qsat ||
Takes into account effect of ocean salinity on saturation specific
humidity at ocean surface (boundary condition for LH flux calculation)
| .false. || logical

|-
| schmsol ||
Land surface processes
* 'NIL ' : No Land surface processes
* 'ISBA' : Interaction Soil Biosphere Atmosphere (ISBA) land sfc scheme
* 'SVS ' : Soil, Vegetation, and Snow (SVS) (Multibudget) land sfc scheme
| 'ISBA' || character(len=16)

|-
| schmurb ||
Urban surface processes
* 'NIL' : No Urban surface processes
* 'TEB' : Town Energy Balance (TEB) urban scheme
| 'NIL' || character(len=16)

|-
| sl_func_stab ||
Class of stability functions (stable case) to use in the surface layer
* 'DELAGE97  ' : Use functions described by Delage (1997; BLM)
* 'BELJAARS91' : Use functions described by Beljaars and Holtslag (1991; JAM)
* 'LOCK07    ' : Use functions described by Lock (2007; Tech Report) employed at UKMO
| 'DELAGE97' || character(len=16)

|-
| sl_func_unstab ||
Class of stability functions (unstable case) to use in the surface layer
* 'DELAGE92' : Use functions described by Delage and Girard (1992; BLM)
* 'DYER74  ' : Use functions described by Dyer (1974; BLM)
| 'DELAGE92' || character(len=16)

|-
| sl_lmin_soil ||
Mimimum Obukhov length (L) for soil surfaces
| -1. || real

|-
| sl_rineutral ||
Define bulk Ri values for near-neutral regime in the surface layer
| 0. || real

|-
| sl_z0ref ||
Use a reference roughness for surface layer calculations
| .false. || logical

|-
| snoalb_anl ||
Use snow albedo "I6" directly if .true.;
Use snow age "XA" to calculate snow albedo if .false.
| .true. || logical

|-
| snow_emiss ||

| -1. || real

|-
| soiltext ||
Soil texture database/calculations for SVS land surface scheme
* 'GSDE   '   : 8 layers of sand & clay info from Global Soil Dataset for ESMs (GSDE)
* 'SLC    '   : 5 layers of sand & clay info from Soil Landscape of Canada (SLC)
* 'SOILGRIDS' : 7 layers of sand & clay info from ISRIC — World Soil Information
| 'GSDE' || character(len=16)

|-
| tdiaglim ||
Limit temperature inversions to 8K/40m in surface layer if .true.
| .false. || logical

|-
| use_eff_surf_tq ||

| .false. || logical

|-
| use_photo ||
OPTION TO USE PHOTOSYNTHESIS CODE FOR STOMATAL RESISTANCE in SVS
| .true. || logical

|-
| veg_rs_mult ||
Factor multiplying stomatal resistance in ISBA
| 1. || real

|-
| water_emiss ||

| -1. || real

|-
| z0dir ||
Use directional roughness length if .true.
| .false. || logical

|-
| z0hcon ||
Constant value of thermal roughness length (m) applied over water within
latitudinal band defined by z0tlat
| 4.0e-5 || real

|-
| z0min ||
Minimum value of momentum roughness length (m)
| 1.5e-5 || real

|-
| z0mtype ||
Momentum roughness length formulation over water
* 'CHARNOCK' : #TODO: define
* 'BELJAARS' : #TODO: define
| 'CHARNOCK' || character(len=16)

|-
| z0tevol ||
Thermal roughness length formulation over vegetation
* 'FIXED' : Uses z0h = z0m
* 'ZILI95': evolves with u*
| 'FIXED' || character(len=16)

|-
| z0tlat ||
Latitude (2 elements, in degrees) used to specify Z0T over water
* If :lat: <= Z0TLAT(1) constant Z0T.
* If :lat: >= Z0TLAT(2) Charnock's relation.
* In between, linear interpolation is used.
| 0. || real

|-
| z0ttype ||
Thermal roughness length formulation over water
* 'MOMENTUM' : Uses z0h = z0m (replaces key z0trdps300=.false.)
* 'DEACU12'  : #TODO: define  (replaces key z0trdps300=.true.)
* 'ECMWF'    : #TODO: define  (New formulation used by ECMWF)
| 'MOMENTUM' || character(len=16)

|-
| zt ||
Height at which to compute screen-level temperature (m)
| 1.5 || real

|-
| zu ||
Height at which to compute anemomenter-level winds (m)
| 10. || real
|}