! ! ROMS/TOMS Standard Input parameters. ! !svn $Id: ocean.in 810 2016-08-05 01:58:16Z arango $ !========================================================= Hernan G. Arango === ! Copyright (c) 2002-2016 The ROMS/TOMS Group ! ! Licensed under a MIT/X style license ! ! See License_ROMS.txt ! !============================================================================== ! ! ! Input parameters can be entered in ANY order, provided that the parameter ! ! KEYWORD (usually, upper case) is typed correctly followed by "=" or "==" ! ! symbols. Any comment lines are allowed and must begin with an exclamation ! ! mark (!) in column one. Comments may appear to the right of a parameter ! ! specification to improve documentation. Comments will be ignored during ! ! reading. Blank lines are also allowed and ignored. Continuation lines in ! ! a parameter specification are allowed and must be preceded by a backslash ! ! (\). In some instances, more than one value is required for a parameter. ! ! If fewer values are provided, the last value is assigned for the entire ! ! parameter array. The multiplication symbol (*), without blank spaces in ! ! between, is allowed for a parameter specification. For example, in a two ! ! grids nested application: ! ! ! ! AKT_BAK == 2*1.0d-6 2*5.0d-6 ! m2/s ! ! ! ! indicates that the first two entries of array AKT_BAK, in fortran column- ! ! major order, will have the same value of "1.0d-6" for grid 1, whereas the ! ! next two entries will have the same value of "5.0d-6" for grid 2. ! ! ! ! In multiple levels of nesting and/or multiple connected domains step-ups, ! ! "Ngrids" entries are expected for some of these parameters. In such case, ! ! the order of the entries for a parameter is extremely important. It must ! ! follow the same order (1:Ngrids) as in the state variable declaration. The ! ! USER may follow the above guidelines for specifying his/her values. These ! ! parameters are marked by "==" plural symbol after the KEYWORD. ! ! ! ! Multiple NetCDF files are allowed for input field(s). This is useful when ! ! splitting input data (climatology, boundary, forcing) time records into ! ! several files (say monthly, annual, etc). In this case, each multiple file ! ! entry line needs to be ended by the vertical bar (|) symbol. For example: ! ! ! ! NFFILES == 7 ! number of forcing files ! ! ! ! FRCNAME == my_tides.nc \ ! ! my_lwrad_year1.nc | ! ! my_lwrad_year2.nc \ ! ! my_swrad_year1.nc | ! ! my_swrad_year2.nc \ ! ! my_winds_year1.nc | ! ! my_winds_year2.nc \ ! ! my_Pair_year1.nc | ! ! my_Pair_year2.nc \ ! ! my_Qair_year1.nc | ! ! my_Qair_year2.nc \ ! ! my_Tair_year1.nc | ! ! my_Tair_year2.nc ! ! ! ! Notice that NFFILES is 7 and not 13. There are 7 uniquely different fields ! ! in the file list, we DO NOT count file entries followed by the vertical ! ! bar symbol. This is because multiple file entries are processed in ROMS ! ! with derived type structures. ! ! ! !============================================================================== ! ! Application title. ! TITLE = ROMS 3.6 - Arctic-4km - Coupled ROMS-CICE ! C-preprocessing Flag. MyAppCPP = ARCTIC4KM ! Input variable information file name. This file needs to be processed ! first so all information arrays can be initialized properly. VARNAME = /cluster/projects/nn9824k/metroms_npi/metroms/apps/common/include/varinfo.dat_ERAatm ! Number of nested grids. Ngrids = 1 ! Number of grid nesting layers. This parameter is used to allow refinement ! and composite grid combinations. NestLayers = 1 ! Number of grids in each nesting layer [1:NestLayers]. GridsInLayer = 1 ! Grid dimension parameters. See notes below in the Glossary for how to set ! these parameters correctly. Lm == 1600 ! Number of I-direction INTERIOR RHO-points Mm == 1200 ! Number of J-direction INTERIOR RHO-points N == 35 ! Number of vertical levels Nbed = 0 ! Number of sediment bed layers NAT = 2 ! Number of active tracers (usually, 2) NPT = 0 ! Number of inactive passive tracers NCS = 0 ! Number of cohesive (mud) sediment tracers NNS = 0 ! Number of non-cohesive (sand) sediment tracers ! Domain decomposition parameters for serial, distributed-memory or ! shared-memory configurations used to determine tile horizontal range ! indices (Istr,Iend) and (Jstr,Jend), [1:Ngrids]. NtileI == 16 ! I-direction partition NtileJ == 24 ! J-direction partition ! Set lateral boundary conditions keyword. Notice that a value is expected ! for each boundary segment per nested grid for each state variable. ! ! Each tracer variable requires [1:4,1:NAT+NPT,Ngrids] values. Otherwise, ! [1:4,1:Ngrids] values are expected for other variables. The boundary ! order is: 1=west, 2=south, 3=east, and 4=north. That is, anticlockwise ! starting at the western boundary. ! ! The keyword is case insensitive and usually has three characters. However, ! it is possible to have compound keywords, if applicable. For example, the ! keyword "RadNud" implies radiation boundary condition with nudging. This ! combination is usually used in active/passive radiation conditions. ! ! Keyword Lateral Boundary Condition Type ! ! Cha Chapman ! Cla Clamped ! Clo Closed ! Fla Flather _____N_____ j=Mm ! Gra Gradient | 4 | ! Nes Nested | | ! Nud Nudging 1 W E 3 ! Per Periodic | | ! Rad Radiation |_____S_____| ! Red Reduced Physics 2 j=1 ! i=1 i=Lm ! W S E N ! e o a o ! s u s r ! t t t t ! h h ! ! 1 2 3 4 LBC(isFsur) == Cha Clo Cha Cha ! free-surface LBC(isUbar) == Fla Clo Fla Fla ! 2D U-momentum LBC(isVbar) == Fla Clo Fla Fla ! 2D V-momentum LBC(isUvel) == RadNud Clo RadNud RadNud ! 3D U-momentum LBC(isVvel) == RadNud Clo RadNud RadNud ! 3D V-momentum LBC(isMtke) == Gra Clo Gra Gra ! mixing TKE LBC(isTvar) == RadNud Clo RadNud RadNud \ ! temperature RadNud Clo RadNud RadNud ! salinity ! Adjoint-based algorithms can have different lateral boundary ! conditions keywords. ad_LBC(isFsur) == Cha Clo Clo Clo ! free-surface ad_LBC(isUbar) == Fla Clo Clo Clo ! 2D U-momentum ad_LBC(isVbar) == Fla Clo Clo Clo ! 2D U-momentum ad_LBC(isUvel) == Cla Clo Clo Clo ! 3D U-momentum ad_LBC(isVvel) == Cla Clo Clo Clo ! 3D V-momentum ad_LBC(isMtke) == Gra Clo Clo Clo ! mixing TKE ad_LBC(isTvar) == Cla Clo Clo Clo \ ! temperature Cla Clo Clo Clo ! salinity ! Set lateral open boundary edge volume conservation switch for ! nonlinear model and adjoint-based algorithms. Usually activated ! with radiation boundary conditions to enforce global mass ! conservation, except if tidal forcing is enabled. [1:Ngrids]. VolCons(west) == F ! western boundary VolCons(east) == F ! eastern boundary VolCons(south) == F ! southern boundary VolCons(north) == F ! northern boundary ad_VolCons(west) == F ! western boundary ad_VolCons(east) == F ! eastern boundary ad_VolCons(south) == F ! southern boundary ad_VolCons(north) == F ! northern boundary ! Time-Stepping parameters. NTIMES == 318240.0 DT == 120 NDTFAST == 60 ! Model iteration loops parameters. ERstr = 1 ERend = 1 Nouter = 1 Ninner = 1 Nintervals = 1 ! Number of eigenvalues (NEV) and eigenvectors (NCV) to compute for the ! Lanczos/Arnoldi problem in the Generalized Stability Theory (GST) ! analysis. NCV must be greater than NEV (see documentation below). NEV = 2 ! Number of eigenvalues NCV = 10 ! Number of eigenvectors ! Input/Output parameters. NRREC == -1 LcycleRST == F NRST == 720 NSTA == 720 NFLT == 299970 NINFO == 360 ! Output history, average, diagnostic files parameters. LDEFOUT == T NHIS == 720 NDEFHIS == 720 NQCK == 720 NDEFQCK == 720 NTSAVG == 1 NAVG == 720 NDEFAVG == 720 NTSDIA == 1 NDIA == 720 NDEFDIA == 0 ! Output tangent linear and adjoint models parameters. LcycleTLM == F NTLM == 72 NDEFTLM == 0 LcycleADJ == F NADJ == 72 NDEFADJ == 0 NSFF == 0 NOBC == 0 ! Output check pointing GST restart parameters. LmultiGST = F ! one eigenvector per file LrstGST = F ! GST restart switch MaxIterGST = 500 ! maximun number of iterations NGST = 10 ! check pointing interval ! Relative accuracy of the Ritz values computed in the GST analysis. Ritz_tol = 1.0d-15 ! Harmonic/biharmonic horizontal diffusion of tracer: [1:NAT+NPT,Ngrids]. TNU2 == 2*1.0d2 ! m2/s TNU4 == 1.6d8 ! m4/s ad_TNU2 == 50.0d0 50.0d0 ! m2/s ad_TNU4 == 0.0d0 0.0d0 ! m4/s ! Harmononic/biharmonic, horizontal viscosity coefficient: [Ngrids]. VISC2 == 1.0d2 ! m2/s VISC4 == 1.6d8 ! m4/s ad_VISC2 == 10.0d0 ! m2/s ad_VISC4 == 0.0d0 ! m4/s ! Logical switches (TRUE/FALSE) to increase/decrease horizontal viscosity ! and/or diffusivity in specific areas of the application domain (like ! sponge areas) for the desired application grid. LuvSponge == F ! horizontal momentum LtracerSponge == F F ! temperature, salinity, inert ! Vertical mixing coefficients for active tracers: [1:NAT+NPT,Ngrids] AKT_BAK == 1.0d-6 1.0d-6 ! m2/s ad_AKT_fac == 1.0d0 1.0d0 ! nondimensional ! Vertical mixing coefficient for momentum: [Ngrids]. AKV_BAK == 5.0d-6 ! m2/s ad_AKV_fac == 1.0d0 ! nondimensional ! Turbulent closure parameters. AKK_BAK == 5.0d-6 ! m2/s AKP_BAK == 5.0d-6 ! m2/s TKENU2 == 0.0d0 ! m2/s TKENU4 == 0.0d0 ! m4/s ! Generic length-scale turbulence closure parameters. GLS_P == 0.0d0 ! Mellor-Yamada 2.5 GLS_M == 1.0d0 GLS_N == 1.0d0 GLS_Kmin == 5.0d-6 GLS_Pmin == 5.0d-6 GLS_CMU0 == 0.5544d0 GLS_C1 == 0.9d0 GLS_C2 == 0.5d0 GLS_C3M == 0.9d0 GLS_C3P == 0.9d0 GLS_SIGK == 1.96d0 GLS_SIGP == 1.96d0 ! Constants used in surface turbulent kinetic energy flux computation. CHARNOK_ALPHA == 1000.0d0 ! Charnok surface roughness ZOS_HSIG_ALPHA == 0.5d0 ! roughness from wave amplitude SZ_ALPHA == 0.25d0 ! roughness from wave dissipation CRGBAN_CW == 100.0d0 ! Craig and Banner wave breaking ! Constants used in momentum stress computation. RDRG == 0.0d-04 ! m/s RDRG2 == 3.0d-03 ! nondimensional Zob == 0.0d0 ! m Zos == 0.02d0 ! m ! Bulk flux measurement heights for atmospheric variables BLK_ZQ == 2.0d0 ! m BLK_ZT == 2.0d0 ! m BLK_ZW == 10.0d0 ! m ! Minimum depth for wetting and drying. DCRIT == 0.10d0 ! m ! Various parameters. WTYPE == 1 LEVSFRC == 15 LEVBFRC == 1 ! Set vertical, terrain-following coordinates transformation equation and ! stretching function (see below for details), [1:Ngrids]. Vtransform == 2 ! transformation equation Vstretching == 2 ! stretching function ! Vertical S-coordinates parameters, [1:Ngrids]. THETA_S == 6.0d0 ! 0 < THETA_S < 20 THETA_B == 0.1d0 ! 0 < THETA_B < 1 TCLINE == 100.0d0 ! m ! Mean Density and Brunt-Vaisala frequency. RHO0 = 1025.0d0 ! kg/m3 BVF_BAK = 1.0d-4 ! 1/s2 ! Time-stamp assigned for model initialization, reference time ! origin for tidal forcing, and model reference time for output ! NetCDF units attribute. DSTART = 14897.0 ! Use start time equal to tidal reference date TIDE_START = 14897.0d0 ! Tides reference TIME_REF = 19700101.00 ! yyyymmdd.dd ! Nudging/relaxation time scales, inverse scales will be computed ! internally, [1:Ngrids]. TNUDG == 05.0d0 05.0d0 ! days ZNUDG == 0.0d0 ! days M2NUDG == 5.0d0 ! days M3NUDG == 15.0d0 ! days ! Factor between passive (outflow) and active (inflow) open boundary ! conditions, [1:Ngrids]. If OBCFAC > 1, nudging on inflow is stronger ! than on outflow (recommended). OBCFAC == 1.0d0 ! nondimensional ! Width of nudgingzone. IWRK == 15 ! no. of gridpoints ! Logical switches (TRUE/FALSE) to specify which variables to process for ! tracers climatology: [1:NAT+NPT,Ngrids]. See glossary below for details. LtracerCLM == T T ! temperature, salinity, inert ! Linear equation of State parameters: R0 == 1027.0d0 ! kg/m3 T0 == 10.0d0 ! Celsius S0 == 35.0d0 ! PSU TCOEF == 1.7d-4 ! 1/Celsius SCOEF == 7.6d-4 ! 1/PSU ! Slipperiness parameter: 1.0 (free slip) or -1.0 (no slip) GAMMA2 == 1.0d0 ! Logical switches (TRUE/FALSE) to activate horizontal momentum transport ! point Sources/Sinks (like river runoff transport) and mass point ! Sources/Sinks (like volume vertical influx), [1:Ngrids]. LuvSrc == T ! horizontal momentum transport LwSrc == F ! volume vertical influx ! Logical switches (TRUE/FALSE) to activate tracers point Sources/Sinks ! (like river runoff) and to specify which tracer variables to consider: ! [1:NAT+NPT,Ngrids]. See glossary below for details. LtracerSrc == F T ! temperature, salinity, inert ! Logical switches (TRUE/FALSE) to read and process climatology fields. ! See glossary below for details. LsshCLM == F ! sea-surface height Lm2CLM == F ! 2D momentum Lm3CLM == F ! 3D momentum LtracerCLM == T T ! temperature, salinity, inert ! Logical switches (TRUE/FALSE) to nudge the desired climatology field(s). ! If not analytical climatology fields, users need to turn ON the logical ! switches above to process the fields from the climatology NetCDF file ! that are needed for nudging. See glossary below for details. LnudgeM2CLM == F ! 2D momentum LnudgeM3CLM == F ! 3D momentum LnudgeTCLM == F F ! temperature, salinity, inert ! Starting (DstrS) and ending (DendS) day for adjoint sensitivity forcing. ! DstrS must be less or equal to DendS. If both values are zero, their ! values are reset internally to the full range of the adjoint integration. DstrS == 0.0d0 ! starting day DendS == 0.0d0 ! ending day ! Starting and ending vertical levels of the 3D adjoint state variables ! whose sensitivity is required. KstrS == 1 ! starting level KendS == 1 ! ending level ! Logical switches (TRUE/FALSE) to specify the adjoint state variables ! whose sensitivity is required. Lstate(isFsur) == F ! free-surface Lstate(isUbar) == F ! 2D U-momentum Lstate(isVbar) == F ! 2D V-momentum Lstate(isUvel) == F ! 3D U-momentum Lstate(isVvel) == F ! 3D V-momentum Lstate(isTvar) == F F F F F F F ! NT tracers ! Logical switches (TRUE/FALSE) to specify the state variables for ! which Forcing Singular Vectors or Stochastic Optimals is required. Fstate(isFsur) == F ! free-surface Fstate(isUbar) == F ! 2D U-momentum Fstate(isVbar) == F ! 2D V-momentum Fstate(isUvel) == F ! 3D U-momentum Fstate(isVvel) == F ! 3D V-momentum Fstate(isTvar) == F F F F F F F ! NT tracers Fstate(isUstr) == T ! surface U-stress Fstate(isVstr) == T ! surface V-stress Fstate(isTsur) == F F F F F F F ! NT surface tracers flux ! Stochastic optimals time decorrelation scale (days) assumed for ! red noise processes. SO_decay == 2.0d0 ! days ! Stochastic Optimals surface forcing standard deviation for ! dimensionalization. SO_sdev(isFsur) == 1.0d0 ! free-surface SO_sdev(isUbar) == 1.0d0 ! 2D U-momentum SO_sdev(isVbar) == 1.0d0 ! 2D V-momentum SO_sdev(isUvel) == 1.0d0 ! 3D U-momentum SO_sdev(isVvel) == 1.0d0 ! 3D V-momentum SO_sdev(isTvar) == 1.0d0 1.0d0 ! NT tracers SO_sdev(isUstr) == 1.0d0 ! surface U-stress SO_sdev(isVstr) == 1.0d0 ! surface V-stress SO_sdev(isTsur) == 1.0d0 1.0d0 ! NT surface tracers flux ! Logical switches (TRUE/FALSE) to activate writing of fields into ! HISTORY output file. Hout(idUvel) == T ! u 3D U-velocity Hout(idVvel) == T ! v 3D V-velocity Hout(idu3dE) == F ! u_eastward 3D U-eastward at RHO-points Hout(idv3dN) == F ! v_northward 3D V-northward at RHO-points Hout(idWvel) == F ! w 3D W-velocity Hout(idOvel) == F ! omega omega vertical velocity Hout(idUbar) == T ! ubar 2D U-velocity Hout(idVbar) == T ! vbar 2D V-velocity Hout(idu2dE) == F ! ubar_eastward 2D U-eastward at RHO-points Hout(idv2dN) == F ! vbar_northward 2D V-northward at RHO-points Hout(idFsur) == T ! zeta free-surface Hout(idBath) == F ! bath time-dependent bathymetry Hout(idTvar) == T T ! temp, salt temperature and salinity Hout(idpthR) == F ! z_rho time-varying depths of RHO-points Hout(idpthU) == F ! z_u time-varying depths of U-points Hout(idpthV) == F ! z_v time-varying depths of V-points Hout(idpthW) == F ! z_w time-varying depths of W-points Hout(idUsms) == F ! sustr surface U-stress Hout(idVsms) == F ! svstr surface V-stress Hout(idUbms) == F ! bustr bottom U-stress Hout(idVbms) == F ! bvstr bottom V-stress Hout(idUbrs) == F ! bustrc bottom U-current stress Hout(idVbrs) == F ! bvstrc bottom V-current stress Hout(idUbws) == F ! bustrw bottom U-wave stress Hout(idVbws) == F ! bvstrw bottom V-wave stress Hout(idUbcs) == F ! bustrcwmax bottom max wave-current U-stress Hout(idVbcs) == F ! bvstrcwmax bottom max wave-current V-stress Hout(idUbot) == F ! Ubot bed wave orbital U-velocity Hout(idVbot) == F ! Vbot bed wave orbital V-velocity Hout(idUbur) == F ! Ur bottom U-velocity above bed Hout(idVbvr) == F ! Vr bottom V-velocity above bed Hout(idW2xx) == F ! Sxx_bar 2D radiation stress, Sxx component Hout(idW2xy) == F ! Sxy_bar 2D radiation stress, Sxy component Hout(idW2yy) == F ! Syy_bar 2D radiation stress, Syy component Hout(idU2rs) == F ! Ubar_Rstress 2D radiation U-stress Hout(idV2rs) == F ! Vbar_Rstress 2D radiation V-stress Hout(idU2Sd) == F ! ubar_stokes 2D U-Stokes velocity Hout(idV2Sd) == F ! vbar_stokes 2D V-Stokes velocity Hout(idW3xx) == F ! Sxx 3D radiation stress, Sxx component Hout(idW3xy) == F ! Sxy 3D radiation stress, Sxy component Hout(idW3yy) == F ! Syy 3D radiation stress, Syy component Hout(idW3zx) == F ! Szx 3D radiation stress, Szx component Hout(idW3zy) == F ! Szy 3D radiation stress, Szy component Hout(idU3rs) == F ! u_Rstress 3D U-radiation stress Hout(idV3rs) == F ! v_Rstress 3D V-radiation stress Hout(idU3Sd) == F ! u_stokes 3D U-Stokes velocity Hout(idV3Sd) == F ! v_stokes 3D V-Stokes velocity Hout(idWamp) == F ! Hwave wave height Hout(idWlen) == F ! Lwave wave length Hout(idWdir) == F ! Dwave wave direction Hout(idWptp) == F ! Pwave_top wave surface period Hout(idWpbt) == F ! Pwave_bot wave bottom period Hout(idWorb) == F ! Ub_swan wave bottom orbital velocity Hout(idWdis) == F ! Wave_dissip wave dissipation Hout(idPair) == F ! Pair surface air pressure Hout(idUair) == F ! Uair surface U-wind component Hout(idVair) == F ! Vair surface V-wind component Hout(idTsur) == F F ! shflux, ssflux surface net heat and salt flux Hout(idLhea) == F ! latent latent heat flux Hout(idShea) == F ! sensible sensible heat flux Hout(idLrad) == F ! lwrad longwave radiation flux Hout(idSrad) == F ! swrad shortwave radiation flux Hout(idEmPf) == F ! EminusP E-P flux Hout(idevap) == F ! evaporation evaporation rate Hout(idrain) == F ! rain precipitation rate Hout(idDano) == F ! rho density anomaly Hout(idVvis) == T ! AKv vertical viscosity Hout(idTdif) == T ! AKt vertical T-diffusion Hout(idSdif) == T ! AKs vertical Salinity diffusion Hout(idHsbl) == T ! Hsbl depth of surface boundary layer Hout(idHbbl) == T ! Hbbl depth of bottom boundary layer Hout(idMtke) == T ! tke turbulent kinetic energy Hout(idMtls) == T ! gls turbulent length scale ! Logical switches (TRUE/FALSE) to activate writing of extra inert passive ! tracers other than biological and sediment tracers. An inert passive tracer ! is one that it is only advected and diffused. Other processes are ignored. ! These tracers include, for example, dyes, pollutants, oil spills, etc. ! NPT values are expected. However, these switches can be activated using ! compact parameter specification. Hout(inert) == F ! inert passive tracers ! Logical switches (TRUE/FALSE) to activate writing of fields into ! QUICKSAVE output file. Qout(idUvel) == F ! u 3D U-velocity Qout(idVvel) == F ! v 3D V-velocity Qout(idu3dE) == F ! u_eastward 3D U-eastward at RHO-points Qout(idv3dN) == F ! v_northward 3D V-northward at RHO-points Qout(idWvel) == F ! w 3D W-velocity Qout(idOvel) == F ! omega omega vertical velocity Qout(idUbar) == F ! ubar 2D U-velocity Qout(idVbar) == F ! vbar 2D V-velocity Qout(idu2dE) == F ! ubar_eastward 2D U-eastward at RHO-points Qout(idv2dN) == F ! vbar_northward 2D V-northward at RHO-points Qout(idFsur) == F ! zeta free-surface Qout(idBath) == F ! bath time-dependent bathymetry Qout(idTvar) == F F ! temp, salt temperature and salinity Qout(idUsur) == F ! u_sur surface U-velocity Qout(idVsur) == F ! v_sur surface V-velocity Qout(idUsuE) == F ! u_sur_eastward surface U-eastward velocity Qout(idVsuN) == F ! v_sur_northward surface V-northward velocity Qout(idsurT) == F F ! temp_sur, salt_sur surface temperature and salinity Qout(idpthR) == F ! z_rho time-varying depths of RHO-points Qout(idpthU) == F ! z_u time-varying depths of U-points Qout(idpthV) == F ! z_v time-varying depths of V-points Qout(idpthW) == F ! z_w time-varying depths of W-points Qout(idUsms) == F ! sustr surface U-stress Qout(idVsms) == F ! svstr surface V-stress Qout(idUbms) == F ! bustr bottom U-stress Qout(idVbms) == F ! bvstr bottom V-stress Qout(idUbrs) == F ! bustrc bottom U-current stress Qout(idVbrs) == F ! bvstrc bottom V-current stress Qout(idUbws) == F ! bustrw bottom U-wave stress Qout(idVbws) == F ! bvstrw bottom V-wave stress Qout(idUbcs) == F ! bustrcwmax bottom max wave-current U-stress Qout(idVbcs) == F ! bvstrcwmax bottom max wave-current V-stress Qout(idUbot) == F ! Ubot bed wave orbital U-velocity Qout(idVbot) == F ! Vbot bed wave orbital V-velocity Qout(idUbur) == F ! Ur bottom U-velocity above bed Qout(idVbvr) == F ! Vr bottom V-velocity above bed Qout(idW2xx) == F ! Sxx_bar 2D radiation stress, Sxx component Qout(idW2xy) == F ! Sxy_bar 2D radiation stress, Sxy component Qout(idW2yy) == F ! Syy_bar 2D radiation stress, Syy component Qout(idU2rs) == F ! Ubar_Rstress 2D radiation U-stress Qout(idV2rs) == F ! Vbar_Rstress 2D radiation V-stress Qout(idU2Sd) == F ! ubar_stokes 2D U-Stokes velocity Qout(idV2Sd) == F ! vbar_stokes 2D V-Stokes velocity Qout(idW3xx) == F ! Sxx 3D radiation stress, Sxx component Qout(idW3xy) == F ! Sxy 3D radiation stress, Sxy component Qout(idW3yy) == F ! Syy 3D radiation stress, Syy component Qout(idW3zx) == F ! Szx 3D radiation stress, Szx component Qout(idW3zy) == F ! Szy 3D radiation stress, Szy component Qout(idU3rs) == F ! u_Rstress 3D U-radiation stress Qout(idV3rs) == F ! v_Rstress 3D V-radiation stress Qout(idU3Sd) == F ! u_stokes 3D U-Stokes velocity Qout(idV3Sd) == F ! v_stokes 3D V-Stokes velocity Qout(idWamp) == F ! Hwave wave height Qout(idWlen) == F ! Lwave wave length Qout(idWdir) == F ! Dwave wave direction Qout(idWptp) == F ! Pwave_top wave surface period Qout(idWpbt) == F ! Pwave_bot wave bottom period Qout(idWorb) == F ! Ub_swan wave bottom orbital velocity Qout(idWdis) == F ! Wave_dissip wave dissipation Qout(idPair) == F ! Pair surface air pressure Qout(idUair) == F ! Uair surface U-wind component Qout(idVair) == F ! Vair surface V-wind component Qout(idTsur) == F F ! shflux, ssflux surface net heat and salt flux Qout(idLhea) == F ! latent latent heat flux Qout(idShea) == F ! sensible sensible heat flux Qout(idLrad) == F ! lwrad longwave radiation flux Qout(idSrad) == F ! swrad shortwave radiation flux Qout(idEmPf) == F ! EminusP E-P flux Qout(idevap) == F ! evaporation evaporation rate Qout(idrain) == F ! rain precipitation rate Qout(idDano) == F ! rho density anomaly Qout(idVvis) == F ! AKv vertical viscosity Qout(idTdif) == F ! AKt vertical T-diffusion Qout(idSdif) == F ! AKs vertical Salinity diffusion Qout(idHsbl) == F ! Hsbl depth of surface boundary layer Qout(idHbbl) == F ! Hbbl depth of bottom boundary layer Qout(idMtke) == F ! tke turbulent kinetic energy Qout(idMtls) == F ! gls turbulent length scale ! Logical switches (TRUE/FALSE) to activate writing of extra inert passive ! tracers other than biological and sediment tracers into the QUICKSAVE ! output file. An inert passive tracer is one that it is only advected and ! diffused. Other processes are ignored. These tracers include, for example, ! dyes, pollutants, oil spills, etc. NPT values are expected. However, these ! switches can be activated using compact parameter specification. Qout(inert) == F ! dye_01, ... inert passive tracers Qout(Snert) == F ! dye_01_sur, .. surface inert passive tracers ! Logical switches (TRUE/FALSE) to activate writing of time-averaged ! fields into AVERAGE output file. Aout(idUvel) == T ! u 3D U-velocity Aout(idVvel) == T ! v 3D V-velocity Aout(idu3dE) == F ! u_eastward 3D U-eastward at RHO-points Aout(idv3dN) == F ! v_northward 3D V-northward at RHO-points Aout(idWvel) == T ! w 3D W-velocity Aout(idOvel) == F ! omega omega vertical velocity Aout(idUbar) == T ! ubar 2D U-velocity Aout(idVbar) == T ! vbar 2D V-velocity Aout(idu2dE) == F ! ubar_eastward 2D U-eastward at RHO-points Aout(idv2dN) == F ! vbar_northward 2D V-northward at RHO-points Aout(idFsur) == T ! zeta free-surface Aout(idTvar) == T T ! temp, salt temperature and salinity Aout(idUsms) == T ! sustr surface U-stress Aout(idVsms) == T ! svstr surface V-stress Aout(idUbms) == F ! bustr bottom U-stress Aout(idVbms) == F ! bvstr bottom V-stress Aout(idW2xx) == F ! Sxx_bar 2D radiation stress, Sxx component Aout(idW2xy) == F ! Sxy_bar 2D radiation stress, Sxy component Aout(idW2yy) == F ! Syy_bar 2D radiation stress, Syy component Aout(idU2rs) == F ! Ubar_Rstress 2D radiation U-stress Aout(idV2rs) == F ! Vbar_Rstress 2D radiation V-stress Aout(idU2Sd) == F ! ubar_stokes 2D U-Stokes velocity Aout(idV2Sd) == F ! vbar_stokes 2D V-Stokes velocity Aout(idW3xx) == F ! Sxx 3D radiation stress, Sxx component Aout(idW3xy) == F ! Sxy 3D radiation stress, Sxy component Aout(idW3yy) == F ! Syy 3D radiation stress, Syy component Aout(idW3zx) == F ! Szx 3D radiation stress, Szx component Aout(idW3zy) == F ! Szy 3D radiation stress, Szy component Aout(idU3rs) == F ! u_Rstress 3D U-radiation stress Aout(idV3rs) == F ! v_Rstress 3D V-radiation stress Aout(idU3Sd) == F ! u_stokes 3D U-Stokes velocity Aout(idV3Sd) == F ! v_stokes 3D V-Stokes velocity Aout(idPair) == F ! Pair surface air pressure Aout(idUair) == F ! Uair surface U-wind component Aout(idVair) == F ! Vair surface V-wind component Aout(idTsur) == T T ! shflux, ssflux surface net heat and salt flux Aout(idLhea) == F ! latent latent heat flux Aout(idShea) == F ! sensible sensible heat flux Aout(idLrad) == F ! lwrad longwave radiation flux Aout(idSrad) == F ! swrad shortwave radiation flux Aout(idevap) == F ! evaporation evaporation rate Aout(idrain) == F ! rain precipitation rate Aout(idDano) == F ! rho density anomaly Aout(idVvis) == T ! AKv vertical viscosity Aout(idTdif) == T ! AKt vertical T-diffusion Aout(idSdif) == T ! AKs vertical Salinity diffusion Aout(idHsbl) == T ! Hsbl depth of surface boundary layer Aout(idHbbl) == T ! Hbbl depth of bottom boundary layer Aout(id2dRV) == F ! pvorticity_bar 2D relative vorticity Aout(id3dRV) == F ! pvorticity 3D relative vorticity Aout(id2dPV) == F ! rvorticity_bar 2D potential vorticity Aout(id3dPV) == F ! rvorticity 3D potential vorticity Aout(idu3dD) == F ! u_detided detided 3D U-velocity Aout(idv3dD) == F ! v_detided detided 3D V-velocity Aout(idu2dD) == F ! ubar_detided detided 2D U-velocity Aout(idv2dD) == F ! vbar_detided detided 2D V-velocity Aout(idFsuD) == F ! zeta_detided detided free-surface Aout(idTrcD) == F F ! temp_detided, ... detided temperature and salinity Aout(idHUav) == F ! Huon u-volume flux, Huon Aout(idHVav) == F ! Hvom v-volume flux, Hvom Aout(idUUav) == T ! uu quadratic term Aout(idUVav) == T ! uv quadratic term Aout(idVVav) == T ! vv quadratic term Aout(idU2av) == T ! ubar2 quadratic term Aout(idV2av) == T ! vbar2 quadratic term Aout(idZZav) == T ! zeta2 quadratic term Aout(idTTav) == T T ! temp_2, ... quadratic tracer terms Aout(idUTav) == T T ! u_temp, ... quadratic tracer terms Aout(idVTav) == T T ! v_temp, ... quadratic tracer terms Aout(iHUTav) == F F ! Huon_temp, ... tracer volume flux, Aout(iHVTav) == F F ! Hvom_temp, ... tracer volume flux, ! Logical switches (TRUE/FALSE) to activate writing of extra inert passive ! tracers other than biological and sediment tracers into the AVERAGE file. Aout(inert) == F F F F F ! dye_01, ... inert passive tracers ! Logical switches (TRUE/FALSE) to activate writing of time-averaged, ! 2D momentum (ubar,vbar) diagnostic terms into DIAGNOSTIC output file. Dout(M2rate) == F ! acceleration Dout(M2pgrd) == F ! pressure gradient Dout(M2fcor) == F ! Coriolis force Dout(M2hadv) == F ! horizontal total advection Dout(M2xadv) == F ! horizontal XI-advection Dout(M2yadv) == F ! horizontal ETA-advection Dout(M2hrad) == F ! horizontal total radiation stress Dout(M2hvis) == F ! horizontal total viscosity Dout(M2xvis) == F ! horizontal XI-viscosity Dout(M2yvis) == F ! horizontal ETA-viscosity Dout(M2sstr) == F ! surface stress Dout(M2bstr) == F ! bottom stress ! Logical switches (TRUE/FALSE) to activate writing of time-averaged, ! 3D momentum (u,v) diagnostic terms into DIAGNOSTIC output file. Dout(M3rate) == F ! acceleration Dout(M3pgrd) == F ! pressure gradient Dout(M3fcor) == F ! Coriolis force Dout(M3hadv) == F ! horizontal total advection Dout(M3xadv) == F ! horizontal XI-advection Dout(M3yadv) == F ! horizontal ETA-advection Dout(M3vadv) == F ! vertical advection Dout(M3hrad) == F ! horizontal total radiation stress Dout(M3vrad) == F ! vertical radiation stress Dout(M3hvis) == F ! horizontal total viscosity Dout(M3xvis) == F ! horizontal XI-viscosity Dout(M3yvis) == F ! horizontal ETA-viscosity Dout(M3vvis) == F ! vertical viscosity ! Logical switches (TRUE/FALSE) to activate writing of time-averaged, ! active (temperature and salinity) and passive (inert) tracer diagnostic ! terms into DIAGNOSTIC output file: [1:NAT+NPT,Ngrids]. Dout(iTrate) == F T ! time rate of change Dout(iThadv) == F F ! horizontal total advection Dout(iTxadv) == F F ! horizontal XI-advection Dout(iTyadv) == F F ! horizontal ETA-advection Dout(iTvadv) == F F ! vertical advection Dout(iThdif) == F F ! horizontal total diffusion Dout(iTxdif) == F F ! horizontal XI-diffusion Dout(iTydif) == F F ! horizontal ETA-diffusion Dout(iTsdif) == F F ! horizontal S-diffusion Dout(iTvdif) == F F ! vertical diffusion ! Generic User parameters, [1:NUSER]. NUSER = 0 USER = 0.d0 ! NetCDF-4/HDF5 compression parameters for output files. NC_SHUFFLE = 1 ! if non-zero, turn on shuffle filter NC_DEFLATE = 1 ! if non-zero, turn on deflate filter NC_DLEVEL = 3 ! deflate level [0-9] ! Input NetCDF file names, [1:Ngrids]. GRDNAME == /cluster/work/users/andriani/metroms_run/arctic-4km/a4_input/input_files_NS9081/grid/arctic4km_grd.nc ININAME == /cluster/work/users/andriani/metroms_run/arctic-4km/ocean_ini.nc ! ININAME == /cluster/work/users/andriani/metroms_run/arctic-4km/ocean_rst.nc ITLNAME == ocean_itl.nc IRPNAME == ocean_irp.nc IADNAME == ocean_iad.nc FWDNAME == ocean_fwd.nc ADSNAME == ocean_ads.nc ! Nesting grids connectivity data: contact points information. This ! NetCDF file is special and complex. It is currently generated using ! the script "matlab/grid/contact.m" from the Matlab repository. NGCNAME = ocean_ngc.nc ! Input lateral boundary conditions and climatology file names. The ! USER has the option to split input data time records into several ! NetCDF files (see prologue instructions above). If so, use a single ! line per entry with a vertical bar (|) symbol after each entry, ! except the last one. CLMNAME == /cluster/work/users/andriani/metroms_run/arctic-4km/a4_input/input_files_NS9081/ocean_clm_KLAR.nc_v2 BRYNAME == /cluster/work/users/andriani/metroms_run/arctic-4km/a4_input/input_files_NS9081/ocean_bry_KLAR.nc ! Input climatology nudging coefficients file name. NUDNAME == ocean_nud.nc ! Input Sources/Sinks forcing (like river runoff) file name. SSFNAME == /cluster/projects/nn9824k/metroms_npi/metroms/apps/common/rivers/newA4_rivers_mitya.nc ! Input forcing NetCDF file name(s). The USER has the option to enter ! several files names per each nested grid. For example, the USER may ! have a different files for wind products, heat fluxes, rivers, tides, ! etc. The model will scan the file list and will read the needed data ! from the first file in the list containing the forcing field. Therefore, ! the order of the file names is very important. If multiple forcing ! files per grid, enter first all the file names for grid 1, then grid 2, ! and so on. Use a single line per entry with a continuation (\) symbol ! at the each entry, except the last one. NFFILES == 2 ! number of forcing files FRCNAME == /cluster/work/users/andriani/metroms_run/arctic-4km/a4_input/div_fra_vilje/tide.nc \ /cluster/work/users/andriani/metroms_run/arctic-4km/era5_A4_intrp/era5_2010_intrp.nc | /cluster/work/users/andriani/metroms_run/arctic-4km/era5_A4_intrp/era5_2011_intrp.nc ! Output NetCDF file names, [1:Ngrids]. DAINAME == ocean_dai.nc QCKNAME == ocean_qck.nc GSTNAME == ocean_gst.nc RSTNAME == ocean_rst.nc HISNAME == /cluster/work/users/andriani/metroms_run/arctic-4km/A4_long_run/2011/ocean_his.nc TLMNAME == ocean_tlm.nc TLFNAME == ocean_tlf.nc ADJNAME == ocean_adj.nc AVGNAME == /cluster/work/users/andriani/metroms_run/arctic-4km/A4_long_run/2011/ocean_avg.nc STANAME == /cluster/work/users/andriani/metroms_run/arctic-4km/A4_long_run/2011/ocean_sta.nc ! DIANAME == /ocean_dia.nc FLTNAME == ocean_flt.nc ! Input ASCII parameter filenames. APARNAM = s4dvar.in SPOSNAM = stations.in FPOSNAM = ../External/floats.in BPARNAM = ../External/bio_Fennel.in SPARNAM = ../External/sediment.in USRNAME = ../External/MyFile.dat IPARNAM = /cluster/work/users/andriani/metroms_run/arctic-4km/ice.in ! ! GLOSSARY: ! ========= ! !------------------------------------------------------------------------------ ! Application title (string with a maximum of eighty characters) and ! C-preprocessing flag. !------------------------------------------------------------------------------ ! ! TITLE Application title. ! ! MyAppCPP Application C-preprocession option. ! !------------------------------------------------------------------------------ ! Variable information file name (string with a maximum of eighty characters). !------------------------------------------------------------------------------ ! ! VARNAME Input/Output variable information file name. This file need to ! be processed first so all information arrays and indices can be ! initialized properly in "mod_ncparam.F". ! !------------------------------------------------------------------------------ ! Grid dimension parameters. !------------------------------------------------------------------------------+! ! These parameters are very important since it determine the grid of the ! application to solve. They need to be read first in order to dynamically ! allocate all model variables. ! ! WARNING: It is trivial and posible to change these dimension parameters in ! ------- idealized applications via analytical expressions. However, in ! realistic applications any change to these parameters requires redoing all ! input NetCDF files. ! ! Lm Number of INTERIOR grid RHO-points in the XI-direction for ! each nested grid, [1:Ngrids]. If using NetCDF files as ! input, Lm=xi_rho-2 where "xi_rho" is the NetCDF file ! dimension of RHO-points. Recall that all RHO-point ! variables have a computational I-range of [0:Lm+1]. ! ! Mm Number of INTERIOR grid RHO-points in the ETA-direction for ! each nested grid, [1:Ngrids]. If using NetCDF files as ! input, Mm=eta_rho-2 where "eta_rho" is the NetCDF file ! dimension of RHO-points. Recall that all RHO-point ! variables have a computational J-range of [0:Mm+1]. ! ! N Number of vertical terrain-following levels at RHO-points, ! [1:Ngrids]. ! ! Nbed Number of sediment bed layers, [1:Ngrids]. This parameter ! is only relevant if CPP option SEDIMENT is activated. ! ! Mm+1 ___________________ _______ Kw = N ! | | | | ! Mm | _____________ | | | Kr = N ! | | | | |_______| ! | | | | | | ! Jr | | | | | | ! | | | | |_______| ! | | | | | | ! 1 | |_____________| | | | ! | | |_______| ! 0 |___________________| | | ! Ir | | 1 ! 0 1 Lm Lm+1 h(i,j) |_______| ! ::::::::: 0 ! ::::::::: ! ::::::::: Nbed-1 ! ::::::::: Nbed ! ! NAT Number of active tracer type variables. Usually, NAT=2 for ! potential temperature and salinity. ! ! NPT Number of inert (dyes, age, etc) passive tracer type variables ! to advect and diffuse only. This parameter is only relevant ! if CPP option T_PASSIVE is activated. ! ! NCS Number of cohesive (mud) sediment tracer type variables. This ! parameter is only relevant if CPP option SEDIMENT is ! activated. ! ! NNS Number of non-cohesive (sand) sediment tracer type variables. ! This parameter is only relevant if CPP option SEDIMENT is ! activated. ! ! The total of sediment tracers is NST=NCS+NNS. Notice that ! NST must be greater than zero (NST>0). ! !------------------------------------------------------------------------------ ! Domain tile partition parameters. !------------------------------------------------------------------------------ ! ! Model tile decomposition parameters for serial and parallel configurations ! which are used to determine tile horizontal range indices (Istr,Iend) and ! (Jstr,Jend). In some computers, it is advantageous to have tile partitions ! in serial applications. ! ! NtileI Number of domain partitions in the I-direction (XI-coordinate). ! It must be equal or greater than one. ! ! NtileJ Number of domain partitions in the J-direction (ETA-coordinate). ! It must be equal or greater than one. ! ! WARNING: In shared-memory (OpenMP), the product of NtileI and NtileJ must ! be a MULTIPLE of the number of parallel threads specified with ! the OpenMP environmental variable OMP_NUM_THREADS. ! ! In distributed-memory (MPI), the product of NtileI and NtileJ ! must be EQUAL to the number of parallel nodes specified during ! execution with the "mprun" or "mpirun" command. ! !------------------------------------------------------------------------------ ! Time-Stepping parameters. !------------------------------------------------------------------------------ ! ! NTIMES Total number time-steps in current run. If 3D configuration, ! NTIMES is the total of baroclinic time-steps. If only 2D ! configuration, NTIMES is the total of barotropic time-steps. ! ! DT Time-Step size in seconds. If 3D configuration, DT is the ! size of baroclinic time-step. If only 2D configuration, DT ! is the size of the barotropic time-step. ! ! NDTFAST Number of barotropic time-steps between each baroclinic time ! step. If only 2D configuration, NDTFAST should be unity since ! there is not need to splitting time-stepping. ! !------------------------------------------------------------------------------ ! Model iteration loops parameters. !------------------------------------------------------------------------------ ! ! ERstr Starting ensemble run (perturbation or iteration) number. ! ! ERend Ending ensemble run (perturbation or iteration) number. ! ! Nouter Maximum number of 4DVAR outer loop iterations. ! ! Ninner Maximum number of 4DVAR inner loop iterations. ! ! Nintervals Number of time interval divisions for stochastic optimals ! computations. It must be a multiple of NTIMES. The tangent ! linear model (TLM) and the adjoint model (ADM) are integrated ! forward and backward in different intervals. For example, ! if Nintervals=3, ! ! 1 NTIMES/3 2*NTIMES/3 NTIMES ! +..................+..................+..................+ ! <========================================================> (1) ! <=====================================> (2) ! <==================> (3) ! ! In the first iteration (1), the TLM is integrated forward from ! 1 to NTIMES and the ADM is integrated backward from NTIMES to 1. ! In the second iteration (2), the TLM is integrated forward from ! NTIMES/3 to NTIMES and the ADM is integrated backward from ! NTIMES to NTIMES/3. And so on. ! !------------------------------------------------------------------------------ ! Eigenproblem parameters. !------------------------------------------------------------------------------ ! ! NEV Number of eigenvalues to compute for the Lanczos/Arnoldi ! problem. Notice that the model memory requirement increases ! substantially as NEV increases. The GST requires NEV+1 ! copies of the model state vector. The memory requirements ! are decreased in distributed-memory applications. ! ! NCV Number of eigenvectors to compute for the Lanczos/Arnoldi ! problem. NCV must be greater than NEV. ! ! At present, there is no a-priori analysis to guide the selection of NCV ! relative to NEV. The only formal requirement is that NCV > NEV. However ! in optimal perturbations, it is recommended to have NCV greater than or ! equal to 2*NEV. In Finite Time Eigenmodes (FTE) and Adjoint Finite Time ! Eigenmodes (AFTE) the requirement is to have NCV greater than or equal to ! 2*NEV+1. ! ! The efficiency of calculations depends critically on the combination of ! NEV and NCV. If NEV is large (greater than 10 say), you can use NCV=2*NEV+1 ! but for NEV small (less than 6) it will be inefficient to use NCV=2*NEV+1. ! In complicated applications, you can start with NEV=2 and NCV=10. Otherwise, ! it will iterate for very long time. ! !------------------------------------------------------------------------------ ! Input/Output parameters. !------------------------------------------------------------------------------ ! ! NRREC Switch to indicate re-start from a previous solution. Use ! NRREC=0 for new solutions. In a re-start solution, NRREC ! is the time index of the re-start NetCDF file assigned for ! initialization. If NRREC is negative (said NRREC=-1), the ! model will re-start from the most recent time record. That ! is, the initialization record is assigned internally. ! Notice that it is also possible to re-start from a history ! or time-averaged NetCDF files. If a history file is used ! for re-start, it must contains all the necessary primitive ! variables at all levels. ! ! LcycleRST Logical switch (T/F) used to recycle time records in output ! re-start file. If TRUE, only the latest two re-start time ! records are maintained. If FALSE, all re-start fields are ! saved every NRST time-steps without recycling. The re-start ! fields are written at all levels in double precision. ! ! NRST Number of time-steps between writing of re-start fields. ! ! NSTA Number of time-steps between writing data into stations file. ! Station data is written at all levels. ! ! NFLT Number of time-steps between writing data into floats file. ! ! NINFO Number of time-steps between print of single line information ! to standard output. If also determines the interval between ! computation of global energy diagnostics. ! !------------------------------------------------------------------------------ ! Output history and average files parameters. !------------------------------------------------------------------------------ ! ! LDEFOUT Logical switch (T/F) used to create new output files when ! initializing from a re-start file, abs(NRREC) > 0. If TRUE ! and applicable, a new history, average, diagnostic and ! station files are created during the initialization stage. ! If FALSE and applicable, data is appended to an existing ! history, average, diagnostic and station files. See also ! parameters NDEFHIS, NDEFAVG and NDEFDIA below. ! ! NHIS Number of time-steps between writing fields into history file. ! ! NDEFHIS Number of time-steps between the creation of new history file. ! If NDEFHIS=0, the model will only process one history file. ! This feature is useful for long simulations when history files ! get too large; it creates a new file every NDEFHIS time-steps. ! ! NTSAVG Starting time-step for the accumulation of output time-averaged ! data. ! ! NAVG Number of time-steps between writing time-averaged data ! into averages file. Averaged date is written for all fields. ! ! NDEFAVG Number of time-steps between the creation of new average ! file. If NDEFAVG=0, the model will only process one average ! file. This feature is useful for long simulations when ! average files get too large; it creates a new file every ! NDEFAVG time-steps. ! ! NTSDIA Starting time-step for the accumulation of output time-averaged ! diagnostics data. ! ! NDIA Number of time-steps between writing time-averaged diagnostics ! data into diagnostics file. Averaged date is written for all ! fields. ! ! NDEFDIA Number of time-steps between the creation of new time-averaged ! diagnostics file. If NDEFDIA=0, the model will only process one ! diagnostics file. This feature is useful for long simulations ! when diagnostics files get too large; it creates a new file ! every NDEFDIA time-steps. ! !------------------------------------------------------------------------------ ! Output tangent linear and adjoint model parameters. !------------------------------------------------------------------------------ ! ! LcycleTLM Logical switch (T/F) used to recycle time records in output ! tangent linear file. If TRUE, only the latest two time ! records are maintained. If FALSE, all tangent linear fields ! are saved every NTLM time-steps without recycling. ! ! NTLM Number of time-steps between writing fields into tangent linear ! model file. ! ! NDEFTLM Number of time-steps between the creation of new tangent linear ! file. If NDEFTLM=0, the model will only process one tangent ! linear file. This feature is useful for long simulations when ! output NetCDF files get too large; it creates a new file every ! NDEFTLM time-steps. ! ! LcycleADJ Logical switch (T/F) used to recycle time records in output ! adjoint file. If TRUE, only the latest two time records are ! maintained. If FALSE, all tangent linear fields re saved ! every NADJ time-steps without recycling. ! ! NADJ Number of time-steps between writing fields into adjoint model ! file. ! ! NDEFADJ Number of time-steps between the creation of new adjoint file. ! If NDEFADJ=0, the model will only process one adjoint file. ! This feature is useful for long simulations when output NetCDF ! files get too large; it creates a new file every NDEFADJ ! time-steps. ! !------------------------------------------------------------------------------ ! Generalized Stability Theory (GST) analysis parameters. !------------------------------------------------------------------------------ ! ! LrstGST Logical switch (TRUE/FALSE) to restart GST analysis. If TRUE, ! the check pointing data is read in from the GST restart NetCDF ! file. If FALSE and applicable, the check pointing GST data is ! saved and overwritten every NGST iterations of the algorithm. ! ! MaxIterGST Maximum number of GST algorithm iterations. ! ! NGST Number of GST iterations between storing of check pointing ! data into NetCDF file. The restart data is always saved if ! MaxIterGST is reached without convergence. It is also saved ! when convergence is achieved. It is always a good idea to ! save the check pointing data at regular intervals so there ! is a mechanism to recover from an unexpected interruption ! in this very expensive computation. The check pointing data ! can be used also to recompute the Ritz vectors by changing ! some of the parameters, like convergence criteria (Ritz_tol) ! and number of Arnoldi iterations (iparam(3)). ! ! Ritz_tol Relative accuracy of the Ritz values computed in the GST ! analysis. ! !------------------------------------------------------------------------------ ! Harmonic/Biharmonic horizontal diffusion for active tracers. !------------------------------------------------------------------------------ ! ! TNU2 Lateral, harmonic, constant, mixing coefficient (m2/s) for ! active (NAT) and inert (NPT) tracer variables. If variable ! horizontal diffusion is activated, TNU2 is the mixing ! coefficient for the largest grid-cell in the domain. ! ! TNU4 Lateral, biharmonic, constant, mixing coefficient (m4/s) for ! active (NAT) and inert (NPT) tracer variables. If variable ! horizontal diffusion is activated, TNU4 is the mixing ! coefficient for the largest grid-cell in the domain. ! !------------------------------------------------------------------------------ ! Harmonic/biharmonic horizontal viscosity coefficients. !------------------------------------------------------------------------------ ! ! VISC2 Lateral, harmonic, constant, mixing coefficient (m2/s) for ! momentum. If variable horizontal viscosity is activated, UVNU2 ! is the mixing coefficient for the largest grid-cell in the ! domain. ! ! VISC4 Lateral, biharmonic, constant mixing coefficient (m4/s) for ! momentum. If variable horizontal viscosity is activated, UVNU4 ! is the mixing coefficient for the largest grid-cell in the ! domain. ! !------------------------------------------------------------------------------ ! Vertical mixing coefficients for active tracers. !------------------------------------------------------------------------------ ! ! AKT_BAK Background vertical mixing coefficient (m2/s) for active ! (NAT) and inert (NPT) tracer variables. ! !------------------------------------------------------------------------------ ! Vertical mixing coefficient for momentum. !------------------------------------------------------------------------------ ! ! AKV_BAK Background vertical mixing coefficient (m2/s) for momentum. ! !------------------------------------------------------------------------------ ! Turbulent closure parameters. !------------------------------------------------------------------------------ ! ! AKK_BAK Background vertical mixing coefficient (m2/s) for turbulent ! kinetic energy. ! ! AKP_BAK Background vertical mixing coefficient (m2/s) for turbulent ! generic statistical field, "psi". ! ! TKENU2 Lateral, harmonic, constant, mixing coefficient (m2/s) for ! turbulent closure variables. ! ! TKENU4 Lateral, biharmonic, constant mixing coefficient (m4/s) for ! turbulent closure variables. ! !------------------------------------------------------------------------------ ! Generic length-scale turbulence closure parameters. !------------------------------------------------------------------------------ ! ! GLS_P Stability exponent (non-dimensional). ! ! GLS_M Turbulent kinetic energy exponent (non-dimensional). ! ! GLS_N Turbulent length scale exponent (non-dimensional). ! ! GLS_Kmin Minimum value of specific turbulent kinetic energy ! ! GLS_Pmin Minimum Value of dissipation. ! ! Closure independent constraint parameters (non-dimensional): ! ! GLS_CMU0 Stability coefficient. ! ! GLS_C1 Shear production coefficient. ! ! GLS_C2 Dissipation coefficient. ! ! GLS_C3M Buoyancy production coefficient (minus). ! ! GLS_C3P Buoyancy production coefficient (plus). ! ! GLS_SIGK Constant Schmidt number (non-dimensional) for turbulent ! kinetic energy diffusivity. ! ! GLS_SIGP Constant Schmidt number (non-dimensional) for turbulent ! generic statistical field, "psi". ! ! Suggested values for various parameterizations: ! ! MY2.5 K-epsilon K-omega K-omega K-tao ! ! GLS_P = 0.d0 3.0d0 -1.0d0 -1.0d0 -3.0d0 ! GLS_M = 1.d0 1.5d0 0.5d0 0.5d0 0.5d0 ! GLS_N = 1.d0 -1.0d0 -1.0d0 -1.0d0 1.0d0 ! GLS_Kmin = 5.0d-6 7.6d-6 7.6d-6 7.6d-6 7.6d-6 ! GLS_Pmin = 5.0d-6 1.0d-12 1.0d-12 1.0d-12 1.0d-12 ! ! GLS_CMU0 = 0.5544d0 0.5477d0 0.5477d0 0.5477d0 0.5477d0 ! GLS_C1 = 0.9d0 1.44d0 0.555d0 0.52d0 0.173d0 ! GLS_C2 = 0.5d0 1.92d0 0.833d0 0.8d0 0.225d0 ! GLS_C3M = 0.9d0 -0.4d0 -0.6d0 -0.6d0 0.0d0 ! GLS_C3P = 0.9d0 1.0d0 1.0d0 1.0d0 0.0d0 ! GLS_SIGK = 1.96d0 1.0d0 2.0d0 2.0d0 1.46d0 ! GLS_SIGP = 1.96d0 1.30d0 2.0d0 2.0d0 10.8d0 ! !------------------------------------------------------------------------------ ! Constants used in the computation of momentum stress. !------------------------------------------------------------------------------ ! ! RDRG Linear bottom drag coefficient (m/s). ! ! RDRG2 Quadratic bottom drag coefficient. ! ! Zob Bottom roughness (m). ! ! Zos Surface roughness (m). ! !------------------------------------------------------------------------------ ! Jerlow Water type. !------------------------------------------------------------------------------ ! ! WTYPE Jerlov water type: an integer value from 1 to 5. ! !------------------------------------------------------------------------------ ! Body-force parameters. Used when CPP option BODYFORCE is activated. !------------------------------------------------------------------------------ ! ! LEVSFRC Deepest level to apply surface momentum stress as a body-force. ! ! LEVBFRC Shallowest level to apply bottom momentum stress as a body-force. ! !------------------------------------------------------------------------------ ! Vertical S-coordinates parameters. !------------------------------------------------------------------------------ ! ! THETA_S S-coordinate surface control parameter, [0 < theta_s < 20]. ! ! THETA_B S-coordinate bottom control parameter, [0 < theta_b < 1]. ! ! TCLINE Width (m) of surface or bottom boundary layer in which ! higher vertical resolution is required during stretching. ! ! WARNING: Users need to experiment with these parameters. We ! have found out that the model goes unstable with ! high values of THETA_S. In steep and very tall ! topography, it is recommended to use THETA_S < 3.0. ! !------------------------------------------------------------------------------ ! Mean Density and background Brunt-Vaisala frequency. !------------------------------------------------------------------------------ ! ! RHO0 Mean density (Kg/m3) used when the Boussinesq approximation ! is inferred. ! ! BVF_BAK Background Brunt-Vaisala frequency squared (1/s2). Typical ! values for the ocean range (as a function of depth) from ! 1.0E-4 to 1.0E-6. ! !------------------------------------------------------------------------------ ! Time Stamps. !------------------------------------------------------------------------------ ! ! DSTART Time stamp assigned to model initialization (days). Usually ! a Calendar linear coordinate, like modified Julian Day. For ! Example: ! ! Julian Day = 1 for Nov 25, 0:0:0 4713 BCE ! modified Julian Day = 1 for May 24, 0:0:0 1968 CE GMT ! ! It is called truncated or modified Julian day because an offset ! of 2440000 needs to be added. ! ! TIDE_START Reference time origin for tidal forcing (days). This is the ! time used when processing input tidal model data. It is needed ! in routine "set_tides" to compute the correct phase lag with ! respect ROMS/TOMS initialization time. ! ! TIME_REF Reference time (yyyymmdd.f) used to compute relative time: ! elapsed time interval since reference-time. The "units" ! attribute takes the form "time-unit since reference-time". ! This parameter also provides information about the calendar ! used: ! ! If TIME_REF = -2, model time and DSTART are in modified Julian ! days units. The "units" attribute is: ! ! 'time-units since 1968-05-23 00:00:00 GMT' ! ! If TIME_REF = -1, model time and DSTART are in a calendar ! with 360 days in every year (30 days each month). The "units" ! attribute is: ! ! 'time-units since 0000-01-01 00:00:00' ! ! If TIME_REF = 0, model time and DSTART are in a common year ! calendar with 365.25 days. The "units" attribute is: ! ! 'time-units since 0000-01-01 00:00:00' ! ! If TIME_REF > 0, model time and DSTART are the elapsed time ! units since specified reference time. For example, ! TIME_REF=20020115.5 will yield the following attribute: ! ! 'time-units since 2002-01-15 12:00:00' ! !------------------------------------------------------------------------------ ! Nudging/relaxation time scales, inverse scales will be computed internally. !------------------------------------------------------------------------------ ! ! When passive/active open boundary conditions are activated, these nudging ! values correspond to the passive (outflow) nudging time scales. ! ! TNUDG Nudging time scale (days) for active tracer variables. ! (1:NAT+NPT,1:Ngrids) values are expected. ! ! ZNUDG Nudging time scale (days) for free-surface. ! ! M2NUDG Nudging time scale (days) for 2D momentum. ! ! M3NUDG Nudging time scale (days) for 3D momentum. ! ! OBCFAC Factor between passive (outflow) and active (inflow) open ! boundary conditions. The nudging time scales for the ! active (inflow) conditions are obtained by multiplying ! the passive values by OBCFAC. If OBCFAC > 1, nudging on ! inflow is stronger than on outflow (recommended). ! !------------------------------------------------------------------------------ ! Linear equation of State parameters. !------------------------------------------------------------------------------ ! ! Ignoring pressure, the linear equation of state is: ! ! rho(:,:,:) = R0 - R0 * TCOEF * (t(:,:,:,:,itemp) - T0) ! + R0 * SCOEF * (t(:,:,:,:,isalt) - S0) ! ! Typical values: R0 = 1027.0 kg/m3 ! T0 = 10.0 Celsius ! S0 = 35.0 PSU ! TCOEF = 1.7d-4 1/Celsius ! SCOEF = 7.6d-4 1/PSU ! ! R0 Background density value (Kg/m3) used in Linear Equation of ! State. ! ! T0 Background potential temperature (Celsius) constant. ! ! S0 Background salinity (PSU) constant. ! ! TCOEF Thermal expansion coefficient in Linear Equation of State. ! ! SCOEF Saline contraction coefficient in Linear Equation of State. ! !------------------------------------------------------------------------------ ! Slipperiness parameter. !------------------------------------------------------------------------------ ! ! GAMMA2 Slipperiness variable, either 1.0 (free slip) or -1.0 (no slip). ! !------------------------------------------------------------------------------ ! Adjoint sensitivity parameters. !------------------------------------------------------------------------------ ! ! DstrS Starting day for adjoint sensitivity forcing. ! ! DendS Ending day for adjoint sensitivity forcing. ! ! The adjoint forcing is applied at every time step according to ! desired state functional stored in the adjoint sensitivity ! NetCDF file. DstrS must be less or equal to DendS. If both ! values are zero, their values are reset internally to the full ! range of the adjoint integration. ! ! KstrS Starting vertical level of the 3D adjoint state variables whose ! sensitivity is required. ! KendS Ending vertical level of the 3D adjoint state variables whose ! sensitivity is required. ! ! Lstate Logical switches (TRUE/FALSE) to specify the adjoint state ! variables whose sensitivity is required. ! ! Lstate(isFsur): Free-surface ! Lstate(isUbar): 2D U-momentum ! Lstate(isVbar): 2D V-momentum ! Lstate(isUvel): 3D U-momentum ! Lstate(isVvel): 3D V-momentum ! Lstate(isTvar): Traces (NT values expected) ! !------------------------------------------------------------------------------ ! Stochastic optimals parameters. !------------------------------------------------------------------------------ ! ! SO_decay Stochastic optimals time decorrelation scale (days) assumed ! for red noise processes. ! ! SOstate Logical switches (TRUE/FALSE) to specify the state surface ! forcing variable whose stochastic optimals is required. ! ! SOstate(isustr): surface u-stress ! SOstate(isvstr): surface v-stress ! SOstate(isTsur): surface tracer flux (NT values expected) ! ! SO_sdev Stochastic optimals surface forcing standard deviation for ! dimensionalization. ! ! SO_sdev(isustr): surface u-stress ! SO_sdev(isvstr): surface v-stress ! SO_sdev(isTsur): surface tracer flux (NT values expected) ! !------------------------------------------------------------------------------ ! Logical switches (T/F) to activate writing of fields into HISTORY file. !------------------------------------------------------------------------------ ! ! Hout(idUvel) Write out 3D U-velocity component. ! Hout(idVvel) Write out 3D V-velocity component. ! Hout(idWvel) Write out 3D W-velocity component. ! Hout(idOvel) Write out 3D omega vertical velocity. ! Hout(idUbar) Write out 2D U-velocity component. ! Hout(idVbar) Write out 2D V-velocity component. ! Hout(idFsur) Write out free-surface. ! ! Hout(idTvar) Write out active (NAT) tracers: temperature and salinity. ! ! Hout(idUsms) Write out surface U-momentum stress. ! Hout(idVsms) Write out surface V-momentum stress. ! Hout(idUbms) Write out bottom U-momentum stress. ! Hout(idVbms) Write out bottom V-momentum stress. ! ! Hout(idUbrs) Write out current-induced, U-momentum stress. ! Hout(idVbrs) Write out current-induced, V-momentum stress. ! Hout(idUbws) Write out wind-induced, bottom U-wave stress. ! Hout(idVbws) Write out wind-induced, bottom V-wave stress. ! Hout(idUbcs) Write out bottom maximum wave and current U-stress. ! Hout(idVbcs) Write out bottom maximum wave and current V-stress. ! ! Hout(idUbot) Write out wind-induced, bed wave orbital U-velocity. ! Hout(idVbot) Write out wind-induced, bed wave orbital V-velocity. ! Hout(idUbur) Write out bottom U-velocity above bed. ! Hout(idVbvr) Write out bottom V-velocity above bed. ! ! Hout(idTsur) Write out surface net heat and salt flux ! Hout(idLhea) Write out latent heat flux. ! Hout(idShea) Write out sensible heat flux. ! Hout(idLrad) Write out long-wave radiation flux. ! Hout(idSrad) Write out short-wave radiation flux. ! Hout(idevap) Write out evaporation rate. ! Hout(idrain) Write out precipitation rate. ! ! Hout(idDano) Write out density anomaly. ! Hout(idVvis) Write out vertical viscosity coefficient. ! Hout(idTdif) Write out vertical diffusion coefficient of temperature. ! Hout(idSdif) Write out vertical diffusion coefficient of salinity. ! Hout(idHsbl) Write out depth of oceanic surface boundary layer. ! Hout(idHbbl) Write out depth of oceanic bottom boundary layer. ! Hout(idMtke) Write out turbulent kinetic energy. ! Hout(idMtls) Write out turbulent kinetic energy times length scale. ! ! Hout(inert) Write out extra inert passive tracers. ! ! Hout(idBott) Write out exposed sediment layer properties, 1:MBOTP. ! !------------------------------------------------------------------------------ ! Generic User parameters. !------------------------------------------------------------------------------ ! ! NUSER Number of User parameters to consider (integer). ! USER Vector containing user parameters (real array). This array ! is used with the SANITY_CHECK to test the correctness of ! the tangent linear adjoint models. It contains information ! of the model variable and grid point to perturb: ! ! INT(user(1)): tangent state variable to perturb ! INT(user(2)): adjoint state variable to perturb ! [isFsur=1] free-surface ! [isUbar=2] 2D U-momentum ! [isVbar=3] 2D V-momentum ! [isUvel=4] 3D U-momentum ! [isVvel=5] 3D V-momentum ! [isTvar=6] Firt tracer (temperature) ! [ ... ] ! [isTvar=?] Last tracer ! ! INT(user(3)): I-index of tangent variable to perturb ! INT(user(4)): I-index of adjoint variable to perturb ! INT(user(5)): J-index of tangent variable to perturb ! INT(user(6)): J-index of adjoint variable to perturb ! INT(user(7)): K-index of tangent variable to perturb, if 3D ! INT(user(8)): K-index of adjoint variable to perturb, if 3D ! ! Set tangent and adjoint parameters to the same values ! if perturbing and reporting the same variable. ! !------------------------------------------------------------------------------ ! Input/output NetCDF file names (string with a maximum of eighty characters). !------------------------------------------------------------------------------ ! ! GRDNAME Input grid file name. ! ININAME Input nonlinear initial conditions file name. It can be a ! re-start file. ! IRPNAME Input representer model initial conditions file name. ! ITLNAME Input tangent linear model initial conditions file name. ! IADNAME Input adjoint model initial conditions file name. ! FRCNAME Input forcing fields file name. ! CLMNAME Input climatology fields file name. ! BRYNAME Input open boundary data file name. ! FWDNAME Input forward solution fields file name. ! ADSNAME Input adjoint sensitivity functional file name. ! ! GSTNAME Output GST analysis re-start file name. ! RSTNAME Output re-start file name. ! HISNAME Output history file name. ! TLFNAME Output impulse forcing for tangent linear (TLM and RPM) models. ! TLMNAME Output tangent linear file name. ! ADJNAME Output adjoint file name. ! AVGNAME Output averages file name. ! DIANAME Output diagnostics file name. ! STANAME Output stations file name. ! FLTNAME Output floats file name. ! !------------------------------------------------------------------------------ ! Input ASCII parameters file names. !------------------------------------------------------------------------------ ! ! APARNAM Input assimilation parameters file name. ! SPOSNAM Input stations positions file name. ! FPOSNAM Input initial drifters positions file name. ! BPARNAM Input biological parameters file name. ! SPARNAM Input sediment transport parameters file name. ! USRNAME USER's input generic file name. ! ! ! *************** COUPLING ************ ! ! ! Logical switch to report verbose information about import/export field ! ranges. Lreport = T ! Number of models to couple. Nmodels = 2 ! Coupled models order label used to process information arrays, [1:Nmodels] ! string values are expected. The order is arbitrary, the indices below are ! ordered from bottom to top grids. ! ! OrderLabel = ocean \ ! waves \ ! atmos \ ! cice OrderLabel = ocean \ cice ! Number of parallel threads assigned to each model in the coupled system, ! [1:Nmodels] KEYWORD entries are expected with the order label (OrderLabel) ! in parenthesis. The sum of all entries must be equal to the total number ! of processors. Nthreads(ocean) = 384 Nthreads(cice) = 128 ! Time interval (seconds) between coupling of models, [1:Nmodels] real ! values are expected corresponding to the entries of a lower triangular ! matrix Aij for i>j. For example, for three model components ordered ! as ocean, waves, and atmos, the time interval is read as: ! ! Aij 1 2 3 ! i\j ocean waves atmos ! 1 ocean - - - v(1): ocean-waves coupling interval ! 2 waves v(1) - - v(2): ocean-atmos coupling interval ! 3 atmos v(2) v(3) - v(3): waves-atmos coupling interval ! ! TimeInterval = v(1) v(2) v(3) ! TimeInterval = 60.0d0 10.0d0 10.0d0 TimeInterval = 360 ! Coupled model standard input file name, [1:Nmodels] KEYWORD entries are ! expected with the label code in parenthesis. INPname(ocean) = /cluster/work/users/andriani/metroms_run/arctic-4km/roms.in INPname(cice) = /cluster/work/users/andriani/metroms_run/arctic-4km/ice_in ! Coupled models variables information file name. ! This file gets copied to the bin dir by the build script CPLname = coupling.dat ! Export/Import fields: Use the following string codes to set the fields ! to export/import for each coupled model. ! ! Field Export Import ! ! NONE - - No field to import or export ! Pair atmos ocean surface air pressure ! Tair atmos ocean surface air temperature ! Hair atmos ocean surface air relative humidity ! cloud atmos ocean cloud fraction ! SWrad atmos ocean shortwave radiation flux ! LWrad atmos ocean longwave radiation flux ! rain atmos ocean rain fall rate ! Uwind atmos ocean, waves surface U-wind component ! Vwind atmos ocean, waves surface V-wind component ! heat atmos ocean surface net heat flux ! Ustr atmos ocean surface U-momentum stress ! Vstr atmos ocean surface V-momentum stress ! SST ocean atmos sea surface temperature ! bath ocean waves bathymetry ! SSH ocean waves free-surface ! Ubar ocean waves vertically integrated U-momentum ! Vbar ocean waves vertically integrated V-momentum ! ZO ocean waves bottom roughness ! Wdir waves ocean wave direction ! Wamp waves ocean significant wave height ! Wlen waves ocean average wave length ! Wptop waves ocean surface wave relative peak period ! Wpbot waves ocean bottom wave period ! Wdiss waves ocean wave energy dissipation ! Wbrk waves ocean percent wave breaking ! Wubot waves ocean wave bottom orbital velocity ! ! Export fields per model, [1:Nexport(...)] string values are expected per ! coupled model. The string inside parenthesis must be the same as the one ! given in "OrderLabel". If there is no field to export, set ! ! Nexport(...) = 0 ! Export(...) = NONE Nexport(ocean) = 6 Nexport(cice) = 7 Export(ocean) = SST \ SSS \ FRZMLT \ u \ v \ SSH ! Export(ocean) = SST \ ! bath \ ! SSH \ ! Ubar \ ! Vbar ! Export(waves) = Wdir \ ! Wamp \ ! Wlen \ ! Wptop \ ! Wpbot ! ! Export(atmos) = Pair \ ! Tair \ ! Hair \ ! cloud \ ! SWrad \ ! LWrad \ ! rain \ ! Uwind \ ! Vwind Export(cice) = AICE \ freshAI \ fsaltAI fhocnAI \ fswthruAI \ strocnx \ strocny ! Import fields per model, [1:Nimport(...)] string values are expected per ! coupled model. If there is no field to import, set ! ! Nimport(...) = 0 ! Import(...) = NONE Nimport(ocean) = 7 Nimport(cice) = 6 Import(ocean) = AICE \ freshAI \ fsaltAI fhocnAI \ fswthruAI \ strocnx \ strocny ! Import(waves) = Uwind \ ! Vwind \ ! bath \ ! SSH \ ! Ubar \ ! Vbar ! ! Import(atmos) = SST Import(cice) = SST \ SSS \ FRZMLT \ u \ v \ SSH ! ! GLOSSARY: ! ========= ! !------------------------------------------------------------------------------ ! Coupled model parameters. !------------------------------------------------------------------------------ ! ! Lreport Logical switch (T/F) to report verbose information about ! import/export field ranges. ! ! Nmodels Number of models to couple. ! ! OrderLabel Coupled models label code, [1:Nmodels] string values are ! expected. Enter one string per line and use the continuation ! backlash for each entry, except last. The order of the ! strings determines how information arrays are processed ! and DO loops executed. Currently, the following labels ! and associated indices are used: ! ! ocean => Iocean Ocean model label ! waves => Iwaves Wave model label ! atmos => Iatmos Atmosphere model label ! ! These labels and indices are defined in "mod_coupler.F" ! and processed in "inp_par.F" (routine read_CouplePar). ! ! Use the same label code in other KEYWORD entries set ! in this input file. It is highly recommended to use ! "ocean" first since all coupled models use ROMS framework ! to build the program driver. This allows ROMS to own ! the master thread (node 0 in MPI). ! ! Nthreads(...) Number of parallel threads assigned to each model in the ! coupled system, [1:Nmodels] KEYWORD entries are expected ! with label code in parenthesis: ! ! Nthreads(ocean) = ? Ocean model ! Nthreads(waves) = ? Wave model ! Nthreads(atmos) = ? Atmosphere model ! ... ! ! The sum of all entries must be equal to the total number ! of processors. ! ! TimeInterval Time interval (seconds) between coupling of models, ! [1:Nmodels] real values are expected corresponding to ! the entries of a lower triangular matrix Aij for i>j. ! For example, for three model components ordered ! as ocean, waves, and atmos, the time interval is ! assigned as follows: ! ! Aij 1 2 3 ! i\j ocean waves atmos ... ! 1 ocean - - - ! 2 waves v(1) - - ! 3 atmos v(2) v(3) - ! ... ! ! where: ! ! v(1): ocean-waves coupling interval ! v(2): ocean-atmos coupling interval ! v(3): waves-atmos coupling interval ! ... ! ! This matrix is read in "inp_par.F" using the following ! statements: ! ! ic=0 ! DO j=1,Nmodels ! DO i=1,Nmodels ! IF (i.gt.j) THEN ! ic=ic+1 ! TimeInterval(i,j)=v(ic) ! TimeInterval(j,i)=v(ic) ! END IF ! END DO ! END DO ! !------------------------------------------------------------------------------ ! Coupled models standard input file names. !------------------------------------------------------------------------------ ! ! INPname(...) Coupled model standard input file names, [1:Nmodels] KEYWORD ! entries are expected with the label code in parenthesis: ! ! INPname(ocean) = ? Ocean model ! INPname(waves) = ? Wave model ! INPname(atmos) = ? Atmosphere model ! ! CPL_name Coupled models variables information file name. ! !------------------------------------------------------------------------------ ! Export/Import fields to process. !------------------------------------------------------------------------------ ! ! Export/Import fields names (abbreviated string codes). Currently, the ! following fields below are processed. However, the list can be expanded ! easly. ! ! NONE No import or export field ! Pair surface air pressure ! Tair surface air temperature ! Hair surface air relative humidity ! cloud cloud fraction ! SWrad shortwave radiation flux ! LWrad longwave radiation flux ! rain rain fall rate ! Uwind surface U-wind component ! Vwind surface V-wind component ! heat surface net heat flux ! Ustr surface U-momentum stress ! Vstr surface V-momentum stress ! SST sea surface temperature ! bath bathymetry ! SSH free-surface ! Ubar vertically integrated U-momentum ! Vbar vertically integrated V-momentum ! ZO bottom roughness ! Wdir wave direction ! Wamp significant wave height ! Wlen average wave length ! Wptop surface wave relative peak period ! Wpbot bottom wave period ! Wdiss wave energy dissipation ! Wbrk percent wave breaking ! Wubot wave bottom orbital velocity ! ! Nexport(...) Number of export fields per model, [1:Nmodels] KEYWORD ! entries are expected with the label code in parenthesis. ! Set to zero if no fields to export by a particular model. ! ! Nexport(ocean) = ? Ocean model ! Nexport(waves) = ? Wave model ! Nexport(atmos) = ? Atmosphere model ! ! Export(...) Export fields codes per model, Nexport(...) string codes ! are expected. If Nexport(...) = 0, set Export = NONE. ! ! Nimport(...) Number of import fields per model, [1:Nmodels] KEYWORD ! entries are expected with the label code in parenthesis. ! Set to zero if no fields to import by a particular model. ! ! Nimport(ocean) = ? Ocean model ! Nimport(waves) = ? Wave model ! Nimport(atmos) = ? Atmosphere model ! ! Import(...) Import fields codes per model, Nimport(...) string codes ! are expected. If Nimport(...) = 0, set Import = NONE. !