| | 1 | == Available configuration in NEMOTAM == |
| | 2 | This page contains information on current available configuration for NEMOTAM. |
| | 3 | |
| | 4 | To have an overview on available routines, please see the TAM development progress table. We use the following method: The physical choices are set through cpp keys and namelist parameters. We use below a similar table used for NEMO. |
| | 5 | |
| | 6 | === Ocean Components === |
| | 7 | |
| | 8 | |
| | 9 | || '''Used for''' || '''Functionnalities''' || '''cpp keys''' || '''Associated namelist & logical''' || |
| | 10 | ||'''Horizontal Diffusion/Viscosity''' || || || || |
| | 11 | || || Lateral diffusion along isopycnal slopes ||key_ldfslp || || |
| | 12 | ||'''Horizontal Tracer diffusion''' || || ||nam_traldf || |
| | 13 | || || Tracer lateral diffusion eddy induced velocity parameterization ||key_traldf_eiv || || |
| | 14 | || ||Tracer Laplacian operator || ||ln_traldf_lap || |
| | 15 | || || Iso-neutral application direction for the operator || ||ln_traldf_iso || |
| | 16 | || || Tracer lateral diffusion 1d=f°(depth) , 2d=f°(lat,lon) or 3d=f°(lat,lon,depth) ||key_traldf_c2d || || |
| | 17 | ||'''Horizontal Dynamic viscosity''' || || ||nam_dynldf || |
| | 18 | || ||Dynamic Laplacian operator lateral viscosity || ||ln_dynldf_lap || |
| | 19 | || || Geopotential application direction for the operator || ||ln_dynldf_hor || |
| | 20 | || || Dynamic lateral viscosity 1d=f°(depth) , 2d=f°(lat,lon) or 3d=f°(lat,lon,depth) ||key_dynldf_c3d || || |
| | 21 | ||'''Vertical viscosity/Diffusivity''' || || || || |
| | 22 | || ||Vertical diffusion based on the TKE closure scheme ||key_zdftke ||namtke || |
| | 23 | || || Vertical double diffusion mixing for salinity ||key_zdfddm ||namddm || |
| | 24 | ||'''Vertical convective processes''' || || || || |
| | 25 | || || Enhanced vertical diffusion parametrization || || ln_zdfevd|| |
| | 26 | ||'''Surface forcing fields''' || || ||namsbc, key_forced_daily, key_tau_daily || |
| | 27 | ||'''Initial state & damping''' || || || || |
| | 28 | || ||Internal Newtonian tracers (T & S) damping || key_tradmp||namtdp || |
| | 29 | || || Use a 3D monthly salinity data (Levitus) || key_dtasal|| || |
| | 30 | || || Use a monthly temperature data (Levitus) ||key_dtatem || || |
| | 31 | || || ??? ||key_dtasst || || |
| | 32 | || || Sea surface temperature damping || ||namsbc & namsbc_ssr & ln_ssr || |
| | 33 | || || Sea surface salinity damping || ||namsbc & namsbc_ssr & ln_ssr || |
| | 34 | ||'''On-line diagnostics''' || || || || |
| | 35 | || ||Eddy Induced Velocity (Gent & Mc Williams parameterization) || key_diaeiv|| || |
| | 36 | || || Themocline, 20°C & 28°C isotherm depths || key_diahth|| || |
| | 37 | || || ??? ||key_diaobs || || |
| | 38 | ||'''High Performances Computing''' || || || || |
| | 39 | || || Enable MPP computing with MPI ||key_mpp_mpi || || |
| | 40 | || || ??? ||key_mpi_isend || || |
| | 41 | ||'''Vertical coordinates''' || || ||nam_zgr || |
| | 42 | || || Full steps - Z || || ln_zco|| |
| | 43 | || || Partial steps - PS || || ln_zps|| |
| | 44 | ||'''Pressure gradient treatment''' || || || || |
| | 45 | || || Filtered free surface algorithm || key_dynspg_flt || || |
| | 46 | || || Sea surface salinity damping || ||namsbc & namsbc_ssr & ln_ssr || |
| | 47 | ||'''Vorticity schemes''' || || ||nam_dynvor || |
| | 48 | || || enstrophy conserving || ||ln_dynvor_ens || |
| | 49 | ||'''Advection schemes''' || || ||nam_traadv || |
| | 50 | || || 2nd order Centered || ||ln_traadv_cen2 || |
| | 51 | ||'''Configurations''' || || || || |
| | 52 | || || Idealized Double Gyre configuration with a flat bottom || key_gyre || || |
| | 53 | || || Global ORCA configuration at 2° resolution || key_orca_r2 || || |
| | 54 | || '''Others cpp keys''' || || || || |
| | 55 | || || Geothermal boundary condition flux || ||nambbc || |
| | 56 | || || Diffusive Bottom Boundary Layer || key_trabbl_dif ||nambbl || |
