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Commit aa74f043 authored by dumoda01's avatar dumoda01
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Suppression du repertoire exp

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exp/airsea.nml deleted 100644 → 0
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!$Id: airsea.proto,v 1.1.1.1 2003/03/11 13:38:58 kbk Exp $
!-------------------------------------------------------------------------------
!
!-------------------------------------------------------------------------------
! air-sea interaction (heat, momentum and freshwater fluxes and solar radiation)
!
! calc_fluxes -> surface fluxes calculated by means of bulk formulae
! (.true./.false.). Solar radiation is calculated from
! time, latitude, longitude and clouds. If (.true.),
! meteo_file must be given and wet_mode must be specified.
! If (.false.), surface fluxes and solar radiation are
! prescribed.
!
! meteo_file -> file with meteo data (for calc_fluxes=.true.) with
! - date (yyyy-mm-dd hh:mm:ss)
! - x-comp. of wind (10 m) in m/s
! - y-comp. of wind (10 m) in m/s
! - air pressure ( 2 m) in hectopascal
! - dry air temp. ( 2 m) in Celsius
! - relative humidity in % or wet bulb temperature in C
! or dew point temperature in C (depending on wet_mode)
! - cloud cover in 1/10
!
! wet_mode -> decides what is given in 7. column in meteo_file
! 1: relative humidity
! 2: wet bulb temperature
! 3: dew point temperature
!
! heat_method -> method to provide short wave radiation (swr) and
! surface heat flux (qh)
! (only for calc_fluxes=.false.)
! 0: heat flux not prescribed
! 1: constant "const_swr" and "const_qh" given (see below)
! 2: swr and qh are read from heatflux_file
! const_swr -> constant value of incoming short wave radiation in W/m^2
! (always positive)
!
! const_qh -> constant value of surface heat flux in W/m^2
! (negative for heat loss)
!
! heatflux_file -> file with qin and qout given in W/m^2
! (negative for net outgoing)
!
! momentum_method -> method how momentum fluxes are given
! (only for calc_fluxes=.false.)
! 0: momentum flux not prescribed
! 1: constant surface momentum fluxes given
! 2: surface momentum fluxes given from file momentumflux_file
!
! const_tx -> x-component of surface momentum flux in N/m^2
! const_ty -> y-component of surface momentum flux in N/m^2
!
! momentumflux_file-> file with tx and ty given in N/m^2
!
! p_e_method -> method how fresh water fluxes (P-E) are given
! 0: P-E not used
! 1: constant value for P-E (in m/s) used
! (P-E = precipitation-evaporation)
! 2: values for P-E read from file
!
! const_p_e -> constant value for P-E in m/s (positive for P>E)
!
! p_e_flux_file -> file with value for P-E (positive for P>E)
! used if p_e_method=2
!
! sst_method -> method how sea surface temperature (SST) is given
! 0: no independent SST observation is read from file
! 2: independent SST observation is read from file,
! only for output
!
! sst_file -> file with independent SST observation
!
! sss_method -> method how sea surface salinity (SSS) is given
! 0: no independent SSS observation is read from file
! 2: independent SSS observation is read from file,
! only for output
!-------------------------------------------------------------------------------
&airsea
calc_fluxes= .false.
meteo_file= 'meteo.dat'
wet_mode= 1
heat_method= 2
const_swr= 100.0
const_heat= -100.0
heatflux_file= 'narr_daily_heatflux_ice.dat'
momentum_method= 2
const_tx= 0.1
const_ty= 0.0
momentumflux_file='narr_hourly_momentumflux.dat'
p_e_method= 0
const_p_e= 0.
p_e_flux_file= 'p_e.dat'
sst_method= 0
sst_file= 'sst.dat'
sss_method= 0
sss_file= 'sss.dat'
/
exp/bio.nml deleted 100644 → 0
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!$Id$
!-------------------------------------------------------------------------------
! Basic settings for biogeochemical model
!
! bio_calc -> calculation of the bio model 'bio_model' (.true./.false.)
! bio_model -> choice of the bio model:
! 1: NPZD (4 variables)
! 2: IOW-ERGOM (9 variables)
! 3: Suspended matter only (1 variable)
! 4: Fasham et al. 1990 (7 variables)
!
! bio_eulerian -> state variables are Eulerian (.true./.false.)
!
! cnpar -> Cranck-Nicolson parameter for vertical diffusion
!
! w_adv_discr -> advection scheme for vertical motion
! 1: first order upstream
! 2: not coded yet
! 3: third-order polynomial
! 4: TVD with Superbee limiter
! 5: TVD with MUSCL limiter
! 6: TVD with ULTIMATE QUICKEST
!
! ode_method -> ODE scheme for source and sink dynamics
! 1: first-order explicit (not positive)
! 2: second order explicit Runge-Kutta (not positive)
! 3: fourth-order explicit Runge-Kutta (not positive)
! 4: Patankar (first order, not conservative)
! 5: Patankar-RK (second order, not conservative)
! 6: Patankar-RK (does not work, not conservative)
! 7: Modified Patankar (1. order, conservat., posit.)
! 8: Modified Patankar-RK (2. order, conservat., posit.)
! 9: Modified Patankar-RK (does not work, conservat., posit.)
! 10: Ext. Modified Patankar (1. order, conservat., posit.)
! 11: Ext. Modified Patankar-RK (2. order, conservat., posit.)
!
! split_factor -> number of biogeochemical time steps per physical time step
!
! bioshade_feedback -> feedback of bio-turbidity to temp. eq. (.true./.false.)
!
! bio_lagrange_mean -> averaging Lagrangian conc. on output (.true./.false.)
!
! bio_npar -> total number of Lagrangian particles
!-------------------------------------------------------------------------------
&bio_nml
bio_calc= .true.
bio_model= 4
bio_eulerian= .true.
cnpar= 1.0
w_adv_discr= 6
ode_method= 8
split_factor= 1
bioshade_feedback= .true.
bio_lagrange_mean= .false.
bio_npar= 1000
/
exp/bio_fasham.nml deleted 100644 → 0
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#$Id$
!-------------------------------------------------------------------------------
! Fasham et al. biological model with modifications by Kuehn and Radach
!
! numc= number of compartments for geobiochemical model
!
! p_initial= initial phytoplankton concentration [mmol n/m3]
! z_initial= initial zooplakton concentration [mmol n/m3]
! b_initial= initial bacteria concentration [mmol n/m3]
! d_initial= initial detritus concentration [mmol n/m3]
! n_initial= initial nitrate concentration [mmol n/m3]
! a_initial= initial ammonium concentration [mmol n/m3]
! l_initial= initial LDON concentration [mmol n/m3]
! p0 = minimum phytoplankton concentration [mmol n/m3]
! z0 = minimum zooplakton concentration [mmol n/m3]
! b0 = minimum bacteria concentration [mmol n/m3]
! vp = maximum phytoplankton uptake rate [1/day]
! alpha = slope of the PI-curvea [m2/(W day)]
! k1 = half saturation constant nitrate uptake [mmol n/m3]
! k2 = half saturation constant ammonium uptake [mmol n/m3]
! mu1 = phytoplankton mortality rate [1/day]
! k5 = half saturation constant phytoplankton mortality [mmol n/m3]
! gamma = exudation fraction [-]
! w_p = phytoplankton settling velocity [m/day]
! gmax = maximum ingestion rate [1/day]
! k3 = half saturation constant ingestion [mmol n/m3]
! beta = grazing efficiency [-]
! mu2 = maximum zooplankton loss rate [1/day]
! k6 = half saturation zooplankton loss [mmol n/m3]
! delta = fractional zooplankton loss to LDON [-]
! epsi = fractional zooplankton loss to ammonium [-]
! r1 = grazing preference phytoplankton [-]
! r2 = grazing preference bacteria [-]
! r3 = grazing preference detritus [-]
! vb = maximum bacterial uptake rate [1/day]
! k4 = half saturation bacterial uptake [mmol n/m3]
! mu3 = bacteria excretion rate [1/day]
! eta = uptake ratio ammonium:LDON [-]
! mu4 = detritus breakdown rate [1/day]
! w_d = detritus settling velocity [m/day]
! kc = attenuation constant for the self shading effect [m**2/mmol N]
! I_min = minimum photosynthetically active radiation (PAR) [W/m**2]
! I_opt = optimal photosynthetically active radiation (PAR) [W/m**2] !CHG1
! inib = inhibition slope of the PI-curve (positive) [m2/(W day)] !CHG1
! theta = phytoplancton buoyancy parameter [m3 day/(mmol N)] !CHG2
!-------------------------------------------------------------------------------
&bio_fasham_nml
numc= 7
p_initial= 0.012
z_initial= 0.012
b_initial= 0.001
d_initial= 0.01
n_initial= 12.0
a_initial= 0.1
l_initial= 0.1
p0= 0.0001
z0= 0.0001
b0= 0.0001
vp= 0.3
alpha= 0.04
inib= 0.06
I_opt= 20.0
k1= 1.0
k2= 0.8
mu1= 0.05
k5= 0.2
gamma= 0.05
w_p= -0.38
theta= 0.0
w_pmin= -0.06
w_pmax= -0.38
gmax= 1.0
k3= 1.0
beta= 0.625
mu2= 0.3
k6= 0.2
delta= 0.1
epsi= 0.70
r1= 0.55
r2= 0.4
r3= 0.05
vb= 0.24
k4= 0.5
mu3= 0.03
eta= 0.0
mu4= 0.02
w_d= -5.0
kc= 0.03
aa= 0.70
g2= 14.0
/
exp/gotmmean.nml deleted 100644 → 0
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!$Id: gotmmean.proto,v 1.1.1.1 2003/03/11 13:38:58 kbk Exp $
!-------------------------------------------------------------------------------
! The namelists 'meanflow' is read in meanflow.F90.
!-------------------------------------------------------------------------------
!-------------------------------------------------------------------------------
! Specify variables related to the 1D meanflow model.
!
! h0b= bottom roughness - Note: z0b=0.03*h0b+0.1*nu/ustar [m]
! z0s_min= minimum value of z0s, default value if charnock=.false. [m]
! charnock= .true.: adaptation of Charnok 1955 formula used
! .false.: constant surface roughness length z0s_min used
! charnock_val= emp. constant in Charnok 1955 formula (default = 1400.)
! ddu= grid zooming (surface), 0: no zooming; > 3 strong zooming
! ddl= grid zooming (bottom), 0: no zooming; > 3 strong zooming
! grid_method= 0: zooming of grid with ddl, ddu >= 0
! 1: sigma grid (relative depth fractions) read from file
! 2: cartesian grid (fixed layer height in m) read from file
!
! grid_file= file for sigma or cartesian grid. the first line gives the
! number of layers, the following lines give fractions or
! layer heights in m from the surface down to the bottom.
! gravity= gravitational acceleration [m/s^2]
! rho_0= Reference density [kg/m^3].
! cp= Specific heat of sea water [J/kg/K].
! avmolu= molecular viscosity for momentum [m^2/s].
! avmolt= molecular diffusity for temperature [m^2/s].
! avmols= molecular diffusity for salinity [m^2/s].
! MaxItz0b= max # of iterations for z0b as function of u_taub.
! no_shear= .true.: shear production term P is set to zero
! avmoln= molecular diffusivity for nitrate [m^2/s]. !DD
!-------------------------------------------------------------------------------
&meanflow
h0b= 0.05
z0s_min= 0.02
charnock= .false.
charnock_val= 1400.
ddu= 1.
ddl= 0.
grid_method= 0
grid_file= 'grid.dat'
gravity= 9.81
rho_0= 1027.
cp= 3985.
avmolu= 1.3e-6
avmolt= 1.4e-7
avmols= 1.1e-9
MaxItz0b= 1
no_shear= .false.
/
exp/gotmrun.nml deleted 100644 → 0
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!$Id: gotmrun.proto,v 1.1.1.1 2003/03/11 13:38:58 kbk Exp $
!-------------------------------------------------------------------------------
!
!-------------------------------------------------------------------------------
! general model setup
!
! title -> title of simulation
! nlev -> number of levels
! dt -> time step in seconds
! cnpar -> parameter for "explicitness" of numerical scheme
! (between 0.0 and 1.0)
! buoy_method -> method to compute mean buoyancy
! 1: from equation of state
! (i.e. from potential temperature and salinity)
! 2: from prognostic equation
!
!-------------------------------------------------------------------------------
&model_setup
title= "Arctic SCM"
nlev= 80
dt= 300.
cnpar= 1.0
buoy_method= 2
/
!-------------------------------------------------------------------------------
! geographic location
!
! name -> name of the station
! latitude -> latitude in degree (north is positive)
! longitude -> longitude in degree (east is positive)
! depth -> water depth in meters
!
!-------------------------------------------------------------------------------
&station
name= "Amundsen Gulf"
latitude= 71.5
longitude= -127.0
depth= 200.0
/
!-------------------------------------------------------------------------------
! duration of run
!
! timefmt -> method to specify start and duration of model run
! 1: duration computed from number of time steps, MaxN
! (bogus start date used)
! 2: duration computed from given start and stop dates
! (number of time steps MaxN computed)
! 3: duration computed from number of time steps, MaxN
! (start date as specified, stop date computed)
!
! MaxN -> nominal number of time steps (see "timefmt")
! start -> nominal start date: YYYY/MM/DD HH:MM:SS (see "timefmt")
! stop -> nominal stop date: YYYY/MM/DD HH:MM:SS (see "timefmt")
!
!-------------------------------------------------------------------------------
&time
timefmt= 2
MaxN= 1200
start= '2004-01-01 00:00:00'
stop= '2004-12-31 00:00:00'
/
!-------------------------------------------------------------------------------
! format for output and filename(s).
!
! out_fmt -> format for GOTM output
! 1: ASCII
! 2: NetCDF
! 3: GrADS
!
! out_dir -> path to output directory (set permissions)
! out_fn -> output string used to generate output file names
! nsave -> save results every 'nsave' timesteps
! diagnostics -> diagnostics are written to output (if .true.)
!
! mld_method -> how to diagnose mixed layer depth
! 1: mixed layer depth computed from TKE threshold
! 2: mixed layer depth from Ri threshold
! diff_k -> TKE threshold [m^2/s^2] for mixed layer depth
! ri_crit -> Ri threshold for mixed layer depth
!
! rad_corr -> correct surface buoyancy flux for solar radiation
! for output (if true)
!
!-------------------------------------------------------------------------------
&output
out_fmt= 2
out_dir= "."
out_fn= "amdgulf"
nsave= 36
diagnostics= .false.
mld_method= 2
diff_k= 1.e-5
Ri_crit= 0.5
rad_corr= .true.
/
!-------------------------------------------------------------------------------
! Specify variables related to the equation of state.
!
! eq_state_mode -> choice for empirical formula for equation of state
! 1: UNESCO equation of state by Fofonoff and Millard (1983)
! 2: equation of state according Jackett et al. (2005)
!
! eq_state_method -> method to compute density and buoyancy from salinity,
! potential temperature and pressure
! 1: full equation of state (i.e. with the LOCAL
! pressure). This implies that T is NOT treated as
! the potential temperature but rather as the in-situ
! temperature!
! 2: equation of state with pressure evaluated at the surface.
! This implies that T is treated as the potential
! temperature and thus rho as the potential density.
! 3: linearized equation of state at T0,S0,p0
! (again, use p0=p_surf to work with potential
! temperature and density.)
! 4: linear equation of state with T0,S0,dtr0,dsr0
!
! For the precise definition of the following quantities, see
! GOTM documentation:
!
! T0 -> reference temperature (deg C) for linear equation of state
! S0 -> reference salinity (psu) for linear equation of state
! p0 -> reference pressure (bar) for linear equation of state
! dtr0 -> thermal expansion coefficient for linear equation of state
! dsr0 -> saline expansion coefficient for linear equation of state
!-------------------------------------------------------------------------------
&eqstate
eq_state_mode = 2
eq_state_method= 2
T0= 10.
S0= 35.
p0= 0.
dtr0= -0.17
dsr0= 0.78
/
exp/gotmturb.nml deleted 100644 → 0
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!$Id: gotmturb.proto,v 1.1.1.1 2003/03/11 13:38:58 kbk Exp $
!-------------------------------------------------------------------------------
!-------------------------------------------------------------------------------
! What type of equations are solved in the turbulence model?
!
! turb_method -> type of turbulence closure
!
! 0: convective adjustment
! 1: analytical eddy visc. and diff. profiles, not coded yet
! 2: turbulence Model calculating TKE and length scale
! (specify stability function below)
! 3: second-order model (see "scnd" namelist below)
! 99: KPP model (requires "kpp.inp" with specifications)
!
!
! tke_method -> type of equation for TKE
!
! 1: algebraic equation
! 2: dynamic equation (k-epsilon style)
! 3: dynamic equation (Mellor-Yamada style)
!
!
! len_scale_method -> type of model for dissipative length scale
!
! 1: parabolic shape
! 2: triangle shape
! 3: Xing and Davies [1995]
! 4: Robert and Ouellet [1987]
! 5: Blackadar (two boundaries) [1962]
! 6: Bougeault and Andre [1986]
! 7: Eifler and Schrimpf (ISPRAMIX) [1992]
! 8: dynamic dissipation rate equation
! 9: dynamic Mellor-Yamada q^2l-equation
! 10: generic length scale (GLS)
!
!
! stab_method -> type of stability function
!
! 1: constant stability functions
! 2: Munk and Anderson [1954]
! 3: Schumann and Gerz [1995]
! 4: Eifler and Schrimpf [1992]
!
!-------------------------------------------------------------------------------
&turbulence
turb_method= 99
tke_method= 2
len_scale_method=8
stab_method= 3
/
!-------------------------------------------------------------------------------
! What boundary conditions are used?
!
! k_ubc, k_lbc -> upper and lower boundary conditions
! for k-equation
! 0: prescribed BC
! 1: flux BC
!
! psi_ubc, psi_lbc -> upper and lower boundary conditions
! for the length-scale equation (e.g.
! epsilon, kl, omega, GLS)
! 0: prescribed BC
! 1: flux BC
!
!
! ubc_type -> type of upper boundary layer
! 0: viscous sublayer (not yet impl.)
! 1: logarithmic law of the wall
! 2: tke-injection (breaking waves)
!
! lbc_type -> type of lower boundary layer
! 0: viscous sublayer (not yet impl.)
! 1: logarithmic law of the wall
!
!-------------------------------------------------------------------------------
&bc
k_ubc= 1
k_lbc= 1
psi_ubc= 1
psi_lbc= 1
ubc_type= 1
lbc_type= 1
/
!-------------------------------------------------------------------------------
!What turbulence parameters have been described?
!
! cm0_fix -> value of cm0 for turb_method=2
! Prandtl0_fix -> value of the turbulent Prandtl-number for stab_method=1-4
! cw -> constant of the wave-breaking model
! (Craig & Banner (1994) use cw=100)
! compute_kappa -> compute von Karman constant from model parameters
! kappa -> the desired von Karman constant (if compute_kappa=.true.)
! compute_c3 -> compute c3 (E3 for Mellor-Yamada) for given Ri_st
! Ri_st -> the desired steady-state Richardson number (if compute_c3=.true.)
! length_lim -> apply length scale limitation (see Galperin et al. 1988)
! galp -> coef. for length scale limitation
! const_num -> minimum eddy diffusivity (only with turb_method=0)
! const_nuh -> minimum heat diffusivity (only with turb_method=0)
! k_min -> minimun TKE
! eps_min -> minimum dissipation rate
! kb_min -> minimun buoyancy variance
! epsb_min -> minimum buoyancy variance destruction rate
!
!-------------------------------------------------------------------------------
&turb_param
cm0_fix= 0.5477
Prandtl0_fix= 0.74
cw= 100.
compute_kappa= .true.
kappa= 0.4
compute_c3= .true.
ri_st= 0.25
length_lim= .false.
galp= 0.53
const_num= 5.e-4
const_nuh= 5.e-4
k_min= 1.e-10
eps_min= 1.e-12
kb_min= 1.e-10
epsb_min= 1.e-14
/
!-------------------------------------------------------------------------------
! The generic model (Umlauf & Burchard, J. Mar. Res., 2003)
!
! This part is active only, when len_scale_method=10 has been set.
!
! compute_param -> compute the model parameters:
! if this is .false., you have to set all
! model parameters (m,n,cpsi1,...) explicitly
! if this is .true., all model parameters
! set by you (except m) will be ignored and
! re-computed from kappa, d, alpha, etc.
! (see Umlauf&Burchard 2002)
!
! m: -> exponent for k
! n: -> exponent for l
! p: -> exponent for cm0
!
! Examples:
!
! k-epsilon (Rodi 1987) : m=3/2, n=-1, p=3
! k-omega (Umlauf et al. 2003) : m=1/2, n=-1, p=-1
!
! cpsi1 -> emp. coef. in psi equation
! cpsi2 -> emp. coef. in psi equation
! cpsi3minus -> cpsi3 for stable stratification
! cpsi3plus -> cpsi3 for unstable stratification
! sig_kpsi -> Schmidt number for TKE diffusivity
! sig_psi -> Schmidt number for psi diffusivity
!
!-------------------------------------------------------------------------------
&generic
compute_param= .false.
gen_m= 1.0
gen_n= -0.67
gen_p= 3.0
cpsi1= 1.
cpsi2= 1.22
cpsi3minus= 0.05
cpsi3plus = 1.0
sig_kpsi= 0.8
sig_psi= 1.07
gen_d= -1.2
gen_alpha= -2.0
gen_l= 0.2
/
!-------------------------------------------------------------------------------
! The k-epsilon model (Rodi 1987)
!
! This part is active only, when len_scale_method=8 has been set.
!
! ce1 -> emp. coef. in diss. eq.
! ce2 -> emp. coef. in diss. eq.
! ce3minus -> ce3 for stable stratification, overwritten if compute_c3=.true.
! ce3plus -> ce3 for unstable stratification (Rodi 1987: ce3plus=1.0)
! sig_k -> Schmidt number for TKE diffusivity
! sig_e -> Schmidt number for diss. diffusivity
! sig_peps -> if .true. -> the wave breaking parameterisation suggested
! by Burchard (JPO 31, 2001, 3133-3145) will be used.
!-------------------------------------------------------------------------------
&keps
ce1= 1.44
ce2= 1.92
ce3minus= -0.4
ce3plus= 1.0
sig_k= 1.
sig_e= 1.3
sig_peps= .false.
/
!-------------------------------------------------------------------------------
! The Mellor-Yamada model (Mellor & Yamada 1982)
!
! This part is active only, when len_scale_method=9 has been set!
!
! e1 -> coef. in MY q**2 l equation
! e2 -> coef. in MY q**2 l equation
! e3 -> coef. in MY q**2 l equation, overwritten if compute_c3=.true.
! sq -> turbulent diffusivities of q**2 (= 2k)
! sl -> turbulent diffusivities of q**2 l
! my_length -> prescribed barotropic lengthscale in q**2 l equation of MY
! 1: parabolic
! 2: triangular
! 3: lin. from surface
! new_constr -> stabilisation of Mellor-Yamada stability functions
! according to Burchard & Deleersnijder (2001)
! (if .true.)
!
!-------------------------------------------------------------------------------
&my
e1= 1.8
e2= 1.33
e3= 1.8
sq= 0.2
sl= 0.2
my_length= 3
new_constr= .false.