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Commit a63f7cc6 authored by Aiko Voigt's avatar Aiko Voigt
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Commits git repo for long-term archiving

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&parallel_nml
nproma = 8 ! optimal setting 8 for CRAY; use 16 or 24 for IBM
p_test_run = .false.
l_test_openmp = .false.
l_log_checks = .false.
num_io_procs = 1 ! asynchronous output for values >= 1
itype_comm = 1
iorder_sendrecv = 3 ! best value for CRAY (slightly faster than option 1)
/
&grid_nml
dynamics_grid_filename = "grid_DOM01.nc"
radiation_grid_filename = ""
dynamics_parent_grid_id = 0
lredgrid_phys = .false.
/
&initicon_nml
ifs2icon_filename = "ifs2icon_init.nc"
init_mode = 2 ! operation mode 2: IFS
zpbl1 = 500.
zpbl2 = 1000.
l_sst_in = .true. ! Jennifer
/
&run_nml
num_lev = 90 ! 60
dtime = 180 ! timestep in seconds
ldynamics = .TRUE. ! dynamics
ltransport = .true.
iforcing = 3 ! NWP forcing
ltestcase = .false. ! false: run with real data
msg_level = 7 ! print maximum wind speeds every 5 time steps
ltimer = .false. ! set .TRUE. for timer output
timers_level = 1 ! can be increased up to 10 for detailed timer output
output = "nml"
/
&nwp_phy_nml
inwp_gscp = 1
inwp_convection = 1
inwp_radiation = 1
inwp_cldcover = 1
inwp_turb = 1
inwp_satad = 1
inwp_sso = 1
inwp_gwd = 1
inwp_surface = 1
icapdcycl = 3 ! apply CAPE modification to improve diurnalcycle over tropical land (optimizes NWP scores)
latm_above_top = .false. ! the second entry refers to the nested domain (if present)
efdt_min_raylfric = 7200.
ldetrain_conv_prec = .false. ! ** new for v2.0.15 **; set .true. to activate detrainment of rain and snow; should be used in R3B08 EU-nest only (not for R2B07)!
itype_z0 = 2
icpl_aero_conv = 0
icpl_aero_gscp = 0
! resolution-dependent settings - please choose the appropriate one
dt_rad = 2160.
dt_conv = 720.
dt_sso = 1440.
dt_gwd = 1440.
! lcloudradoff = .true.
! lcloudradonly = .true. !! only heat with cre
ldiag_ddt_temp_dyn2 = .true.
! lradoff = .true. !! uncomment in case of no-radiation simulation
/
&turbdiff_nml
tkhmin = 0.75 ! new default since rev. 16527
tkmmin = 0.75 ! "
pat_len = 100.
c_diff = 0.2
rat_sea = 10. ! ** new since r20191: 8.5 for R3B7, 8.0 for R2B6 in order to get similar temperature biases in the tropics **
ltkesso = .true.
frcsmot = 0.2 ! these 2 switches together apply vertical smoothing of the TKE source terms
imode_frcsmot = 2 ! in the tropics (only), which reduces the moist bias in the tropical lower troposphere
! use horizontal shear production terms with 1/SQRT(Ri) scaling to prevent unwanted side effects:
itype_sher = 3
ltkeshs = .true.
a_hshr = 2.0
/
&lnd_nml
ntiles = 3 !!! 1 for assimilation cycle and forecast
nlev_snow = 3 !!! 1 for assimilation cycle and forecast
lmulti_snow = .true. !!! .false. for assimilation cycle and forecast
itype_heatcond = 2
idiag_snowfrac = 2
lsnowtile = .false. !! later on .true. if GRIB encoding issues are solved
lseaice = .true. !!Sophia Schäfer, 23/03/2017: reads in sea ice (e.g. zero ice), instead of setting by temperature
llake = .false.
itype_lndtbl = 3 ! minimizes moist/cold bias in lower tropical troposphere
itype_root = 2
/
&radiation_nml
irad_o3 = 4 ! APE ozone
irad_aero = 0
irad_cfc11 = 0
irad_cfc12 = 0
albedo_type = 2 ! Modis albedo
vmr_co2 = 348.0e-6
vmr_ch4 = 1650.0e-09
vmr_n2o = 396.0e-09
vmr_o2 = 0.20946
izenith = 3 ! perpetual equinox with diurnal cycle
/
&nonhydrostatic_nml
iadv_rhotheta = 2
ivctype = 2
itime_scheme = 4
exner_expol = 0.333
vwind_offctr = 0.2
damp_height = 50000.
rayleigh_coeff = 0.10
lhdiff_rcf = .true.
divdamp_order = 24 ! for data assimilation runs, '2' provides extra-strong filtering of gravity waves
divdamp_type = 32 !!! optional: 2 for assimilation cycle if very strong gravity-wave filtering is desired
divdamp_fac = 0.004
l_open_ubc = .false.
igradp_method = 3
l_zdiffu_t = .true.
thslp_zdiffu = 0.02
thhgtd_zdiffu = 125.
htop_moist_proc= 22500.
hbot_qvsubstep = 22500. ! use 19000. with R3B7
/
&sleve_nml
min_lay_thckn = 20.
max_lay_thckn = 400. ! maximum layer thickness below htop_thcknlimit
htop_thcknlimit = 14000. ! this implies that the upcoming COSMO-EU nest will have 60 levels
top_height = 75000.
stretch_fac = 0.9
decay_scale_1 = 4000.
decay_scale_2 = 2500.
decay_exp = 1.2
flat_height = 16000.
/
&dynamics_nml
iequations = 3
idiv_method = 1
divavg_cntrwgt = 0.50
lcoriolis = .TRUE.
/
&transport_nml
ctracer_list = '12345'
ivadv_tracer = 3,3,3,3,3
itype_hlimit = 3,4,4,4,4
ihadv_tracer = 52,2,2,2,2
iadv_tke = 0
/
&diffusion_nml
hdiff_order = 5
itype_vn_diffu = 1
itype_t_diffu = 2
hdiff_efdt_ratio = 24.0
hdiff_smag_fac = 0.025
lhdiff_vn = .TRUE.
lhdiff_temp = .TRUE.
/
&interpol_nml
nudge_zone_width = 8
lsq_high_ord = 3
l_intp_c2l = .true.
l_mono_c2l = .true.
support_baryctr_intp = .false. !.true.
/
&extpar_nml
extpar_filename = 'extpar_DOM01.nc'
itopo = 1
n_iter_smooth_topo = 1
&io_nml
itype_pres_msl = 4 ! IFS method with bug fix for self-consistency between SLP and geopotential
itype_rh = 1 ! RH w.r.t. water
/
&output_nml
filetype = 5 ! output format: 2=GRIB2, 4=NETCDFv2
dom = -1 ! write all domains
output_bounds = 0., 10000000., 21600. ! start, end, increment
steps_per_file = 4
include_last = .TRUE.
output_filename = 'icon-lc1-i2100-0001-atmfields_ll' ! file name base
ml_varlist = 'temp', 'u', 'v', 'w', 'pres', 'omega', 'pv', 'tot_qv_dia', 'tot_qi_dia', 'tot_qc_dia', 'clc', 'rho', 'z_ifc','pres','qv' ! needed for deriving heating rates on model levels using fluxes
! pl_varlist = 'temp', 'u', 'v', 'w', 'omega', 'pv', 'tot_qv_dia', 'tot_qi_dia', 'tot_qc_dia', 'clc'
remap = 1
! p_levels = 1000, 2000, 3000, 5000, 7000, 10000, 15000, 20000, 25000, 30000, 40000, 50000, 60000, 70000, 85000, 92500, 100000
reg_lon_def = -180.,1,179.5
reg_lat_def = 89.5,-1, -89.5
/
&output_nml
filetype = 5 ! output format: 2=GRIB2, 4=NETCDFv2
dom = -1 ! write all domains
output_bounds = 0., 10000000., 21600. ! start, end, increment
steps_per_file = 4
include_last = .TRUE.
output_filename = 'icon-lc1-i2100-0001-radfields_ll' ! file name base
ml_varlist = 'lwflxall', 'lwflxclr','swflxclr','swflxall'
remap = 1
reg_lon_def = -180.,1,179.5
reg_lat_def = 89.5,-1, -89.5
/
&output_nml
filetype = 5 ! output format: 2=GRIB2, 4=NETCDFv2
dom = -1 ! write all domains
output_bounds = 0., 10000000., 21600. ! start, end, increment
steps_per_file = 4
include_last = .TRUE.
output_filename = 'icon-lc1-i2100-0001-phys_tendencies_ll' ! file name base
ml_varlist = 'ddt_temp_dyn2','ddt_temp_radsw','ddt_temp_radlw','ddt_temp_radswcs','ddt_temp_radlwcs','ddt_temp_turb','ddt_temp_pconv','ddt_temp_gscp','ddt_temp_mphy','ddt_temp_totnwpphy','pres' ! for no-radiation or cloud rad only change radlw/radsw to radlwnw/radswnw, for clear-sky delete cs
remap = 1
reg_lon_def = -180.,1,179.5
reg_lat_def = 89.5,-1, -89.5
/
&output_nml
filetype = 5 ! output format: 2=GRIB2, 4=NETCDFv2
dom = -1 ! write all domains
output_bounds = 0., 10000000., 21600. ! start, end, increment
steps_per_file = 4
include_last = .TRUE.
output_filename = 'icon-lc1-i2100-0001-sfcfields_ll' ! file name base
ml_varlist = 'pres_sfc','group:precip_vars','tqv','tqc','tqi','shfl_s','lhfl_s','t_g','t_2m','qv_2m','rh_2m','u_10m','v_10m','clct','clcl','clcm','clch', 'sod_t','sou_t','thb_t','sou_s','sob_s','thu_s','thb_s','lwtoaclr','swtoaclr','lwsfcclr','swsfcclr'
remap = 1
reg_lon_def = -180.,1,179.5
reg_lat_def = 89.5,-1, -89.5
/
&parallel_nml
nproma = 8 ! optimal setting 8 for CRAY; use 16 or 24 for IBM
p_test_run = .false.
l_test_openmp = .false.
l_log_checks = .false.
num_io_procs = 1 ! asynchronous output for values >= 1
itype_comm = 1
iorder_sendrecv = 3 ! best value for CRAY (slightly faster than option 1)
/
&grid_nml
dynamics_grid_filename = "grid_DOM01.nc"
radiation_grid_filename = ""
dynamics_parent_grid_id = 0
lredgrid_phys = .false.
/
&initicon_nml
ifs2icon_filename = "ifs2icon_init.nc"
init_mode = 2 ! operation mode 2: IFS
zpbl1 = 500.
zpbl2 = 1000.
l_sst_in = .true. ! Jennifer
/
&run_nml
num_lev = 90 ! 60
dtime = 180 ! timestep in seconds
ldynamics = .TRUE. ! dynamics
ltransport = .true.
iforcing = 3 ! NWP forcing
ltestcase = .false. ! false: run with real data
msg_level = 7 ! print maximum wind speeds every 5 time steps
ltimer = .false. ! set .TRUE. for timer output
timers_level = 1 ! can be increased up to 10 for detailed timer output
output = "nml"
/
&nwp_phy_nml
inwp_gscp = 1
inwp_convection = 1
inwp_radiation = 1
inwp_cldcover = 1
inwp_turb = 1
inwp_satad = 1
inwp_sso = 1
inwp_gwd = 1
inwp_surface = 1
icapdcycl = 3 ! apply CAPE modification to improve diurnalcycle over tropical land (optimizes NWP scores)
latm_above_top = .false. ! the second entry refers to the nested domain (if present)
efdt_min_raylfric = 7200.
ldetrain_conv_prec = .false. ! ** new for v2.0.15 **; set .true. to activate detrainment of rain and snow; should be used in R3B08 EU-nest only (not for R2B07)!
itype_z0 = 2
icpl_aero_conv = 0
icpl_aero_gscp = 0
! resolution-dependent settings - please choose the appropriate one
dt_rad = 2160.
dt_conv = 720.
dt_sso = 1440.
dt_gwd = 1440.
! lcloudradoff = .true.
! lcloudradonly = .true. !! only heat with cre
ldiag_ddt_temp_dyn2 = .true.
lradoff = .true. !! uncomment in case of no-radiation simulation
/
&turbdiff_nml
tkhmin = 0.75 ! new default since rev. 16527
tkmmin = 0.75 ! "
pat_len = 100.
c_diff = 0.2
rat_sea = 10. ! ** new since r20191: 8.5 for R3B7, 8.0 for R2B6 in order to get similar temperature biases in the tropics **
ltkesso = .true.
frcsmot = 0.2 ! these 2 switches together apply vertical smoothing of the TKE source terms
imode_frcsmot = 2 ! in the tropics (only), which reduces the moist bias in the tropical lower troposphere
! use horizontal shear production terms with 1/SQRT(Ri) scaling to prevent unwanted side effects:
itype_sher = 3
ltkeshs = .true.
a_hshr = 2.0
/
&lnd_nml
ntiles = 3 !!! 1 for assimilation cycle and forecast
nlev_snow = 3 !!! 1 for assimilation cycle and forecast
lmulti_snow = .true. !!! .false. for assimilation cycle and forecast
itype_heatcond = 2
idiag_snowfrac = 2
lsnowtile = .false. !! later on .true. if GRIB encoding issues are solved
lseaice = .true. !!Sophia Schäfer, 23/03/2017: reads in sea ice (e.g. zero ice), instead of setting by temperature
llake = .false.
itype_lndtbl = 3 ! minimizes moist/cold bias in lower tropical troposphere
itype_root = 2
/
&radiation_nml
irad_o3 = 4 ! APE ozone
irad_aero = 0
irad_cfc11 = 0
irad_cfc12 = 0
albedo_type = 2 ! Modis albedo
vmr_co2 = 348.0e-6
vmr_ch4 = 1650.0e-09
vmr_n2o = 396.0e-09
vmr_o2 = 0.20946
izenith = 3 ! perpetual equinox with diurnal cycle
/
&nonhydrostatic_nml
iadv_rhotheta = 2
ivctype = 2
itime_scheme = 4
exner_expol = 0.333
vwind_offctr = 0.2
damp_height = 50000.
rayleigh_coeff = 0.10
lhdiff_rcf = .true.
divdamp_order = 24 ! for data assimilation runs, '2' provides extra-strong filtering of gravity waves
divdamp_type = 32 !!! optional: 2 for assimilation cycle if very strong gravity-wave filtering is desired
divdamp_fac = 0.004
l_open_ubc = .false.
igradp_method = 3
l_zdiffu_t = .true.
thslp_zdiffu = 0.02
thhgtd_zdiffu = 125.
htop_moist_proc= 22500.
hbot_qvsubstep = 22500. ! use 19000. with R3B7
/
&sleve_nml
min_lay_thckn = 20.
max_lay_thckn = 400. ! maximum layer thickness below htop_thcknlimit
htop_thcknlimit = 14000. ! this implies that the upcoming COSMO-EU nest will have 60 levels
top_height = 75000.
stretch_fac = 0.9
decay_scale_1 = 4000.
decay_scale_2 = 2500.
decay_exp = 1.2
flat_height = 16000.
/
&dynamics_nml
iequations = 3
idiv_method = 1
divavg_cntrwgt = 0.50
lcoriolis = .TRUE.
/
&transport_nml
ctracer_list = '12345'
ivadv_tracer = 3,3,3,3,3
itype_hlimit = 3,4,4,4,4
ihadv_tracer = 52,2,2,2,2
iadv_tke = 0
/
&diffusion_nml
hdiff_order = 5
itype_vn_diffu = 1
itype_t_diffu = 2
hdiff_efdt_ratio = 24.0
hdiff_smag_fac = 0.025
lhdiff_vn = .TRUE.
lhdiff_temp = .TRUE.
/
&interpol_nml
nudge_zone_width = 8
lsq_high_ord = 3
l_intp_c2l = .true.
l_mono_c2l = .true.
support_baryctr_intp = .false. !.true.
/
&extpar_nml
extpar_filename = 'extpar_DOM01.nc'
itopo = 1
n_iter_smooth_topo = 1
&io_nml
itype_pres_msl = 4 ! IFS method with bug fix for self-consistency between SLP and geopotential
itype_rh = 1 ! RH w.r.t. water
/
&output_nml
filetype = 5 ! output format: 2=GRIB2, 4=NETCDFv2
dom = -1 ! write all domains
output_bounds = 0., 10000000., 21600. ! start, end, increment
steps_per_file = 4
include_last = .TRUE.
output_filename = 'icon-lc1-i2100-0002-atmfields_ll' ! file name base
ml_varlist = 'temp', 'u', 'v', 'w', 'pres', 'omega', 'pv', 'tot_qv_dia', 'tot_qi_dia', 'tot_qc_dia', 'clc', 'rho', 'z_ifc','pres','qv' ! needed for deriving heating rates on model levels using fluxes
! pl_varlist = 'temp', 'u', 'v', 'w', 'omega', 'pv', 'tot_qv_dia', 'tot_qi_dia', 'tot_qc_dia', 'clc'
remap = 1
! p_levels = 1000, 2000, 3000, 5000, 7000, 10000, 15000, 20000, 25000, 30000, 40000, 50000, 60000, 70000, 85000, 92500, 100000
reg_lon_def = -180.,1,179.5
reg_lat_def = 89.5,-1, -89.5
/
&output_nml
filetype = 5 ! output format: 2=GRIB2, 4=NETCDFv2
dom = -1 ! write all domains
output_bounds = 0., 10000000., 21600. ! start, end, increment
steps_per_file = 4
include_last = .TRUE.
output_filename = 'icon-lc1-i2100-0002-radfields_ll' ! file name base
ml_varlist = 'lwflxall', 'lwflxclr','swflxclr','swflxall'
remap = 1
reg_lon_def = -180.,1,179.5
reg_lat_def = 89.5,-1, -89.5
/
&output_nml
filetype = 5 ! output format: 2=GRIB2, 4=NETCDFv2
dom = -1 ! write all domains
output_bounds = 0., 10000000., 21600. ! start, end, increment
steps_per_file = 4
include_last = .TRUE.
output_filename = 'icon-lc1-i2100-0002-phys_tendencies_ll' ! file name base
ml_varlist = 'ddt_temp_dyn2','ddt_temp_radswnw','ddt_temp_radlwnw','ddt_temp_radswcs','ddt_temp_radlwcs','ddt_temp_turb','ddt_temp_pconv','ddt_temp_gscp','ddt_temp_mphy','ddt_temp_totnwpphy','pres' ! for no-radiation or cloud rad only change radlw/radsw to radlwnw/radswnw, for claer-sky delete cs
remap = 1
reg_lon_def = -180.,1,179.5
reg_lat_def = 89.5,-1, -89.5
/
&output_nml
filetype = 5 ! output format: 2=GRIB2, 4=NETCDFv2
dom = -1 ! write all domains
output_bounds = 0., 10000000., 21600. ! start, end, increment
steps_per_file = 4
include_last = .TRUE.
output_filename = 'icon-lc1-i2100-0002-sfcfields_ll' ! file name base
ml_varlist = 'pres_sfc','group:precip_vars','tqv','tqc','tqi','shfl_s','lhfl_s','t_g','t_2m','qv_2m','rh_2m','u_10m','v_10m','clct','clcl','clcm','clch', 'sod_t','sou_t','thb_t','sou_s','sob_s','thu_s','thb_s','lwtoaclr','swtoaclr','lwsfcclr','swsfcclr'
remap = 1
reg_lon_def = -180.,1,179.5
reg_lat_def = 89.5,-1, -89.5
/
&parallel_nml
nproma = 8 ! optimal setting 8 for CRAY; use 16 or 24 for IBM
p_test_run = .false.
l_test_openmp = .false.
l_log_checks = .false.
num_io_procs = 1 ! asynchronous output for values >= 1
itype_comm = 1
iorder_sendrecv = 3 ! best value for CRAY (slightly faster than option 1)
/
&grid_nml
dynamics_grid_filename = "grid_DOM01.nc"
radiation_grid_filename = ""
dynamics_parent_grid_id = 0
lredgrid_phys = .false.
/
&initicon_nml
ifs2icon_filename = "ifs2icon_init.nc"
init_mode = 2 ! operation mode 2: IFS
zpbl1 = 500.
zpbl2 = 1000.
l_sst_in = .true. ! Jennifer
/
&run_nml
num_lev = 90 ! 60
dtime = 180 ! timestep in seconds
ldynamics = .TRUE. ! dynamics
ltransport = .true.
iforcing = 3 ! NWP forcing
ltestcase = .false. ! false: run with real data
msg_level = 7 ! print maximum wind speeds every 5 time steps
ltimer = .false. ! set .TRUE. for timer output
timers_level = 1 ! can be increased up to 10 for detailed timer output
output = "nml"
/
&nwp_phy_nml
inwp_gscp = 1
inwp_convection = 1
inwp_radiation = 1
inwp_cldcover = 1
inwp_turb = 1
inwp_satad = 1
inwp_sso = 1
inwp_gwd = 1
inwp_surface = 1
icapdcycl = 3 ! apply CAPE modification to improve diurnalcycle over tropical land (optimizes NWP scores)
latm_above_top = .false. ! the second entry refers to the nested domain (if present)
efdt_min_raylfric = 7200.
ldetrain_conv_prec = .false. ! ** new for v2.0.15 **; set .true. to activate detrainment of rain and snow; should be used in R3B08 EU-nest only (not for R2B07)!
itype_z0 = 2
icpl_aero_conv = 0
icpl_aero_gscp = 0
! resolution-dependent settings - please choose the appropriate one
dt_rad = 2160.
dt_conv = 720.
dt_sso = 1440.
dt_gwd = 1440.
lcloudradoff = .true.
! lcloudradonly = .true. !! only heat with cre
ldiag_ddt_temp_dyn2 = .true.
! lradoff = .true. !! uncomment in case of no-radiation simulation
/
&turbdiff_nml
tkhmin = 0.75 ! new default since rev. 16527
tkmmin = 0.75 ! "
pat_len = 100.
c_diff = 0.2
rat_sea = 10. ! ** new since r20191: 8.5 for R3B7, 8.0 for R2B6 in order to get similar temperature biases in the tropics **
ltkesso = .true.
frcsmot = 0.2 ! these 2 switches together apply vertical smoothing of the TKE source terms
imode_frcsmot = 2 ! in the tropics (only), which reduces the moist bias in the tropical lower troposphere
! use horizontal shear production terms with 1/SQRT(Ri) scaling to prevent unwanted side effects:
itype_sher = 3
ltkeshs = .true.
a_hshr = 2.0
/
&lnd_nml
ntiles = 3 !!! 1 for assimilation cycle and forecast
nlev_snow = 3 !!! 1 for assimilation cycle and forecast
lmulti_snow = .true. !!! .false. for assimilation cycle and forecast
itype_heatcond = 2
idiag_snowfrac = 2
lsnowtile = .false. !! later on .true. if GRIB encoding issues are solved
lseaice = .true. !!Sophia Schäfer, 23/03/2017: reads in sea ice (e.g. zero ice), instead of setting by temperature
llake = .false.
itype_lndtbl = 3 ! minimizes moist/cold bias in lower tropical troposphere
itype_root = 2
/
&radiation_nml
irad_o3 = 4 ! APE ozone
irad_aero = 0
irad_cfc11 = 0
irad_cfc12 = 0
albedo_type = 2 ! Modis albedo
vmr_co2 = 348.0e-6
vmr_ch4 = 1650.0e-09
vmr_n2o = 396.0e-09
vmr_o2 = 0.20946
izenith = 3 ! perpetual equinox with diurnal cycle
/
&nonhydrostatic_nml
iadv_rhotheta = 2
ivctype = 2
itime_scheme = 4
exner_expol = 0.333
vwind_offctr = 0.2
damp_height = 50000.
rayleigh_coeff = 0.10
lhdiff_rcf = .true.
divdamp_order = 24 ! for data assimilation runs, '2' provides extra-strong filtering of gravity waves
divdamp_type = 32 !!! optional: 2 for assimilation cycle if very strong gravity-wave filtering is desired
divdamp_fac = 0.004
l_open_ubc = .false.
igradp_method = 3
l_zdiffu_t = .true.
thslp_zdiffu = 0.02
thhgtd_zdiffu = 125.
htop_moist_proc= 22500.
hbot_qvsubstep = 22500. ! use 19000. with R3B7
/
&sleve_nml
min_lay_thckn = 20.
max_lay_thckn = 400. ! maximum layer thickness below htop_thcknlimit
htop_thcknlimit = 14000. ! this implies that the upcoming COSMO-EU nest will have 60 levels
top_height = 75000.
stretch_fac = 0.9
decay_scale_1 = 4000.
decay_scale_2 = 2500.
decay_exp = 1.2
flat_height = 16000.
/
&dynamics_nml
iequations = 3
idiv_method = 1
divavg_cntrwgt = 0.50
lcoriolis = .TRUE.
/
&transport_nml
ctracer_list = '12345'
ivadv_tracer = 3,3,3,3,3
itype_hlimit = 3,4,4,4,4
ihadv_tracer = 52,2,2,2,2
iadv_tke = 0
/
&diffusion_nml
hdiff_order = 5
itype_vn_diffu = 1
itype_t_diffu = 2
hdiff_efdt_ratio = 24.0
hdiff_smag_fac = 0.025
lhdiff_vn = .TRUE.
lhdiff_temp = .TRUE.
/
&interpol_nml
nudge_zone_width = 8
lsq_high_ord = 3
l_intp_c2l = .true.
l_mono_c2l = .true.
support_baryctr_intp = .false. !.true.
/
&extpar_nml
extpar_filename = 'extpar_DOM01.nc'
itopo = 1
n_iter_smooth_topo = 1
&io_nml
itype_pres_msl = 4 ! IFS method with bug fix for self-consistency between SLP and geopotential
itype_rh = 1 ! RH w.r.t. water
/
&output_nml
filetype = 5 ! output format: 2=GRIB2, 4=NETCDFv2
dom = -1 ! write all domains
output_bounds = 0., 10000000., 21600. ! start, end, increment
steps_per_file = 4
include_last = .TRUE.
output_filename = 'icon-lc1-i2100-0003-atmfields_ll' ! file name base
ml_varlist = 'temp', 'u', 'v', 'w', 'pres', 'omega', 'pv', 'tot_qv_dia', 'tot_qi_dia', 'tot_qc_dia', 'clc', 'rho', 'z_ifc','pres','qv' ! needed for deriving heating rates on model levels using fluxes
! pl_varlist = 'temp', 'u', 'v', 'w', 'omega', 'pv', 'tot_qv_dia', 'tot_qi_dia', 'tot_qc_dia', 'clc'
remap = 1
! p_levels = 1000, 2000, 3000, 5000, 7000, 10000, 15000, 20000, 25000, 30000, 40000, 50000, 60000, 70000, 85000, 92500, 100000
reg_lon_def = -180.,1,179.5
reg_lat_def = 89.5,-1, -89.5
/
&output_nml
filetype = 5 ! output format: 2=GRIB2, 4=NETCDFv2
dom = -1 ! write all domains
output_bounds = 0., 10000000., 21600. ! start, end, increment
steps_per_file = 4
include_last = .TRUE.
output_filename = 'icon-lc1-i2100-0003-radfields_ll' ! file name base
ml_varlist = 'lwflxall', 'lwflxclr','swflxclr','swflxall'
remap = 1
reg_lon_def = -180.,1,179.5
reg_lat_def = 89.5,-1, -89.5
/
&output_nml
filetype = 5 ! output format: 2=GRIB2, 4=NETCDFv2
dom = -1 ! write all domains
output_bounds = 0., 10000000., 21600. ! start, end, increment
steps_per_file = 4
include_last = .TRUE.
output_filename = 'icon-lc1-i2100-0003-phys_tendencies_ll' ! file name base
ml_varlist = 'ddt_temp_dyn2','ddt_temp_radsw','ddt_temp_radlw','ddt_temp_turb','ddt_temp_pconv','ddt_temp_gscp','ddt_temp_mphy','ddt_temp_totnwpphy','pres' ! for no-radiation or cloud rad only change radlw/radsw to radlwnw/radswnw, for clear-sky delete cs
remap = 1
reg_lon_def = -180.,1,179.5
reg_lat_def = 89.5,-1, -89.5
/
&output_nml
filetype = 5 ! output format: 2=GRIB2, 4=NETCDFv2
dom = -1 ! write all domains
output_bounds = 0., 10000000., 21600. ! start, end, increment
steps_per_file = 4
include_last = .TRUE.
output_filename = 'icon-lc1-i2100-0003-sfcfields_ll' ! file name base
ml_varlist = 'pres_sfc','group:precip_vars','tqv','tqc','tqi','shfl_s','lhfl_s','t_g','t_2m','qv_2m','rh_2m','u_10m','v_10m','clct','clcl','clcm','clch', 'sod_t','sou_t','thb_t','sou_s','sob_s','thu_s','thb_s','lwtoaclr','swtoaclr','lwsfcclr','swsfcclr'
remap = 1
reg_lon_def = -180.,1,179.5
reg_lat_def = 89.5,-1, -89.5
/
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&master_nml
lrestart = .false.
/
&master_time_control_nml
calendar = "proleptic gregorian"
checkpointTimeIntval = "P6M"
restartTimeIntval = "P1Y"
experimentStartDate = "1001-01-01T00:00:00Z"
experimentStopDate = "1001-01-15T00:00:00Z"
/
&time_nml
is_relative_time = .false.
/
&master_model_nml
model_name="atmo"
model_namelist_filename="NAMELIST_lc1-i2100-0001"
model_type=1
model_min_rank=0
model_max_rank=65535
model_inc_rank=1
/
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