/
ocean_ross_drift.in
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ocean_ross_drift.in
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!
! ROMS/TOMS Standard Input parameters.
!
!svn $Id: ocean_soglobec.in 1176 2010-03-02 01:32:31Z kate $
!========================================================= Hernan G. Arango ===
! Copyright (c) 2002-2010 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. !
! !
!==============================================================================
!
! Application title.
TITLE = ROMS/TOMS 3.6 - ROSS - coupled ice-ocean run
! C-preprocessing Flag.
MyAppCPP = ROSS
! Input variable information file name. This file needs to be processed
! first so all information arrays can be initialized properly.
VARNAME = Apps/ROSS/varinfo_ROSS.dat
! Number of nested grids.
Ngrids = 1
! Grid dimension parameters. See notes below in the Glossary for how to set
! these parameters correctly.
Lm == 277 ! Number of I-direction INTERIOR RHO-points
Mm == 368 ! Number of J-direction INTERIOR RHO-points
N == 24 ! Number of vertical levels
Nbed = 0 ! Number of sediment bed layers
NAT = 2 ! Number of active tracers (usually, 2)
NPT = 4 ! 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 == 10 ! I-direction partition
NtileJ == 10 ! 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
!
! Mix Mixed (for ice, see lbc.F & i2d_bc.F)
! 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) == Gra Clo Gra Gra ! free-surface
LBC(isUbar) == RadNud Clo RadNud RadNud ! 2D U-momentum
LBC(isVbar) == RadNud Clo RadNud RadNud ! 2D V-momentum
LBC(isUvel) == Rad Clo Rad Rad ! 3D U-momentum
LBC(isVvel) == Rad Clo Rad Rad ! 3D V-momentum
LBC(isMtke) == Gra Clo Gra Gra ! mixing TKE
LBC(isTvar) == RadNud Clo RadNud RadNud \ ! temperature
RadNud Clo RadNud RadNud \ ! salinity
RadNud Clo RadNud RadNud \ ! dye_01
RadNud Clo RadNud RadNud \ ! dye_02
RadNud Clo RadNud RadNud \ ! dye_03
RadNud Clo RadNud RadNud ! dye_04
! Ice boundary conditions
LBC(isAice) == Mix Clo Mix Mix ! ice concentration
LBC(isHice) == Mix Clo Mix Mix ! ice thickness
LBC(isHsno) == Mix Clo Mix Mix ! snow thickness
LBC(isTice) == Gra Clo Gra Gra ! ice temperature
LBC(isSfwat)== Clo Clo Clo Clo ! surface water
LBC(isSig11)== Gra Clo Gra Gra ! sigma-11
LBC(isSig12)== Gra Clo Gra Gra ! sigma-12
LBC(isSig22)== Gra Clo Gra Gra ! sigma-22
LBC(isUice) == Gra Clo Gra Gra ! ice U-momentum
LBC(isVice) == Gra Clo Gra Gra ! ice V-momentum
! Adjoint-based algorithms can have different lateral boundary
! conditions keywords.
ad_LBC(isFsur) == Gra Clo Gra Gra ! free-surface
ad_LBC(isUbar) == RadNud Clo RadNud RadNud ! 2D U-momentum
ad_LBC(isVbar) == RadNud Clo RadNud RadNud ! 2D U-momentum
ad_LBC(isUvel) == Rad Clo Rad Rad ! 3D U-momentum
ad_LBC(isVvel) == Rad Clo Rad Rad ! 3D V-momentum
ad_LBC(isMtke) == Gra Clo Gra Gra ! mixing TKE
ad_LBC(isTvar) == RadNud Clo RadNud RadNud \ ! temperature
RadNud Clo RadNud RadNud ! 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 enabled. [1:Ngrids].
VolCons(west) == T ! western boundary
VolCons(east) == T ! eastern boundary
VolCons(south) == F ! southern boundary
VolCons(north) == T ! northern boundary
ad_VolCons(west) == T ! western boundary
ad_VolCons(east) == T ! eastern boundary
ad_VolCons(south) == F ! southern boundary
ad_VolCons(north) == T ! northern boundary
! Time-Stepping parameters.
NTIMES == 2733120 !End time = 783360, rst time = 630720
DT == 300.0d0
NDTFAST == 30
! 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 == 2
LcycleRST == T
NRST == 8640
NSTA == 6
NFLT == 12
NINFO == 1
! Output history, average, diagnostic files parameters.
LDEFOUT == T
NHIS == 2880 !1440
NDEFHIS == 8640 !23040
NTSAVG == 1
NAVG == 2880 !1440
NDEFAVG == 8640 !23040
NTSDIA == 1
NDIA == 2880 !1440
NDEFDIA == 8640 !11520
! Output tangent linear and adjoint models parameters.
LcycleTLM == F
NTLM == 72
NDEFTLM == 0
LcycleADJ == F
NADJ == 72
NDEFADJ == 0
NSFF == 72
NOBC == 72
! Output check pointing GST restart parameters.
LmultiGST = F !NEW ! 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 for nonlinear model
! and adjoint-based algorithms: [1:NAT+NPT,Ngrids].
TNU2 == 6*5.0d0 ! m2/s
TNU4 == 2*0.0d0 ! m4/s
ad_TNU2 == 0.0d0 0.0d0 ! m2/s
ad_TNU4 == 0.0d0 0.0d0 ! m4/s
! Harmononic/biharmonic, horizontal viscosity coefficient for nonlinear model
! and adjoint-based algorithms: [Ngrids].
VISC2 == 0.1d0 ! m2/s
VISC4 == 0.0d0 ! m4/s
ad_VISC2 == 0.0d0 ! m2/s
ad_VISC4 == 0.0d0 ! m4/s
! Vertical mixing coefficients for tracers in nonlinear model and
! basic state scale factor in adjoint-based algorithms: [1:NAT+NPT,Ngrids]
AKT_BAK == 1.0d-5 1.0d-5 1.0d-5 ! m2/s
ad_AKT_fac == 1.0d0 1.0d0 ! nondimensional
! Vertical mixing coefficient for momentum for nonlinear model and
! basic state scale factor in adjoint-based algorithms: [Ngrids].
AKV_BAK == 5.0d-5 ! 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 == 3.0d0 ! K-epsilon
GLS_M == 1.5d0
GLS_N == -1.0d0
GLS_Kmin == 7.6d-6
GLS_Pmin == 1.0d-12
GLS_CMU0 == 0.5477d0
GLS_C1 == 1.44d0
GLS_C2 == 1.92d0
GLS_C3M == -0.4d0
GLS_C3P == 1.0d0
GLS_SIGK == 1.0d0
GLS_SIGP == 1.30d0
! Constants used in surface turbulent kinetic energy flux computation.
CHARNOK_ALPHA == 1400.0d0 ! 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 == 0.0d0 ! m/s
RDRG2 == 3.0d-03 ! nondimensional
Zob == 0.02d0 ! m
Zos == 0.02d0 ! m
! Height (m) of atmospheric measurements for Bulk fluxes parameterization.
BLK_ZQ == 10.0d0 ! air humidity
BLK_ZT == 10.0d0 ! air temperature
BLK_ZW == 10.0d0 ! winds
! Minimum depth for wetting and drying.
DCRIT == 0.10d0 ! m
! Various parameters.
WTYPE == 1
LEVSFRC == 22
LEVBFRC == 1
! Set vertical, terrain-following coordinates transformation equation and
! stretching function (see below for details), [1:Ngrids].
Vtransform == 1 ! transformation equation
Vstretching == 1 ! stretching function
! Vertical S-coordinates parameters (see below for details), [1:Ngrids].
THETA_S == 4.0d0 ! surface stretching parameter
THETA_B == 0.98d0 ! bottom stretching parameter
TCLINE == 200.0d0 ! critical depth (m)
! Mean Density and Brunt-Vaisala frequency.
RHO0 = 1025.0d0 ! kg/m3
BVF_BAK = 1.0d-5 ! 1/s2
! Time-stamp assigned for model initialization, reference time
! origin for tidal forcing, and model reference time for output
! NetCDF units attribute.
DSTART = 0.0d0 ! days
TIDE_START = 0.0d0 ! days
TIME_REF = 0.0d0 ! yyyymmdd.dd
! Nudging/relaxation time scales, inverse scales will be computed
! internally, [1:Ngrids].
TNUDG == 6*365.0d0 ! days
ZNUDG == 0.0d0 ! days
M2NUDG == 365.0d0 ! days
M3NUDG == 0.0d0 ! 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 == 30.0d0 ! nondimensional
! Linear equation of State parameters:
R0 == 1027.0d0 ! kg/m3
T0 == 14.0d0 ! 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 specify which variables to consider on
! tracers point Sources/Sinks (like river runoff): [1:NAT+NPT,Ngrids].
! See glossary below for details.
LtracerSrc == T T T T T T ! 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 ! 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 ! NT tracers
Fstate(isUstr) == T ! surface U-stress
Fstate(isVstr) == T ! surface V-stress
Fstate(isTsur) == 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. (Next 6 lines NEW)
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 tracer flux
! Logical switches (TRUE/FALSE) to activate writing of fields into
! HISTORY output file.
Hout(idUvel) == T ! 3D U-velocity
Hout(idVvel) == T ! 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) == T ! 3D W-velocity
Hout(idOvel) == T ! omega vertical velocity
Hout(idUbar) == T ! 2D U-velocity
Hout(idVbar) == T ! 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 ! free-surface
Hout(idBath) == F ! time-dependent bathymetry
Hout(idTvar) == T T ! temperature and salinity
Hout(idPair) == F !Pair ! surface air pressure
Hout(idUair) == F ! surface U-wind
Hour(idVair) == F ! surface V-wind
Hout(idUsms) == F ! surface U-stress
Hout(idVsms) == F ! surface V-stress
Hout(idUbms) == F ! bottom U-stress
Hout(idVbms) == F ! bottom V-stress
Hout(idUairE)== F
Hout(idVairN)== F
Hout(idUbrs) == F ! bottom U-current stress
Hout(idVbrs) == F ! bottom V-current stress
Hout(idUbws) == F ! bottom U-wave stress
Hout(idVbws) == F ! bottom V-wave stress
Hout(idUbcs) == F ! bottom max wave-current U-stress
Hout(idVbcs) == F ! bottom max wave-current V-stress
Hout(idUbot) == F ! bed wave orbital U-velocity
Hout(idVbot) == F ! bed wave orbital V-velocity
Hout(idUbur) == F ! bottom U-velocity above bed
Hout(idVbvr) == F ! bottom V-velocity above bed
Hout(idW2xx) == F ! 2D radiation stress, Sxx component
Hout(idW2xy) == F ! 2D radiation stress, Sxy component
Hout(idW2yy) == F ! 2D radiation stress, Syy component
Hout(idU2rs) == F ! 2D radiation U-stress
Hout(idV2rs) == F ! 2D radiation V-stress
Hout(idU2Sd) == F ! 2D U-Stokes velocity
Hout(idV2Sd) == F ! 2D V-Stokes velocity
Hout(idW3xx) == F ! 3D radiation stress, Sxx component
Hout(idW3xy) == F ! 3D radiation stress, Sxy component
Hout(idW3yy) == F ! 3D radiation stress, Syy component
Hout(idW3zx) == F ! 3D radiation stress, Szx component
Hout(idW3zy) == F ! 3D radiation stress, Szy component
Hout(idU3rs) == F ! 3D U-radiation stress
Hout(idV3rs) == F ! 3D V-radiation stress
Hout(idU3Sd) == F ! 3D U-Stokes velocity
Hout(idV3Sd) == F ! 3D V-Stokes velocity
Hout(idWamp) == F ! wave height
Hout(idWlen) == F ! wave length
Hout(idWdir) == F ! wave direction
Hout(idWptp) == F ! wave surface period
Hout(idWpbt) == F ! wave bottom period
Hout(idWorb) == F ! wave bottom orbital velocity
Hout(idWdis) == F ! wave dissipation
Hout(idTsur) == T T ! surface net heat and salt flux
Hout(idLhea) == F ! latent heat flux
Hout(idShea) == F ! sensible heat flux
Hout(idLrad) == F ! longwave radiation flux
Hout(idSrad) == F ! shortwave radiation flux
Hout(idEmPf) == T ! E-P flux
Hout(idevap) == F ! evaporation rate
Hout(idrain) == F ! precipitation rate
Hout(idDano) == T ! density anomaly
Hout(idSSSf) == F ! surface salinity flux correction
Hout(idVvis) == T ! vertical viscosity
Hout(idTdif) == T ! vertical T-diffusion
Hout(idSdif) == T ! vertical Salinity diffusion
Hout(idHsbl) == F ! depth of surface boundary layer
Hout(idHbbl) == F ! depth of bottom boundary layer
Hout(idMtke) == F ! turbulent kinetic energy
Hout(idMtls) == F ! 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) == T T T T ! inert passive tracers
! Logical switches (TRUE/FALSE) to activate writing of exposed sediment
! layer properties into HISTORY output file. Currently, MBOTP properties
! are expected for the bottom boundary layer and/or sediment models:
!
! Hout(idBott(isd50)), isd50 = 1 ! mean grain diameter
! Hout(idBott(idens)), idens = 2 ! mean grain density
! Hout(idBott(iwsed)), iwsed = 3 ! mean settling velocity
! Hout(idBott(itauc)), itauc = 4 ! critical erosion stress
! Hout(idBott(irlen)), irlen = 5 ! ripple length
! Hout(idBott(irhgt)), irhgt = 6 ! ripple height
! Hout(idBott(ibwav)), ibwav = 7 ! wave excursion amplitude
! Hout(idBott(izdef)), izdef = 8 ! default bottom roughness
! Hout(idBott(izapp)), izapp = 9 ! apparent bottom roughness
! Hout(idBott(izNik)), izNik = 10 ! Nikuradse bottom roughness
! Hout(idBott(izbio)), izbio = 11 ! biological bottom roughness
! Hout(idBott(izbfm)), izbfm = 12 ! bed form bottom roughness
! Hout(idBott(izbld)), izbld = 13 ! bed load bottom roughness
! Hout(idBott(izwbl)), izwbl = 14 ! wave bottom roughness
! Hout(idBott(iactv)), iactv = 15 ! active layer thickness
! Hout(idBott(ishgt)), ishgt = 16 ! saltation height
!
! 1 1 1 1 1 1 1
! 1 2 3 4 5 6 7 8 9 0 1 2 3 4 5 6
Hout(idBott) == T T T T T T T T T F F F F F F F
!MARKER TWO - Add in Average/Diag file logical switches
! 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) == T ! 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(idPair) == F
Aout(idUair) == F
Aout(idVair) == F
Aout(idUsms) == F ! sustr surface U-stress
Aout(idVsms) == F ! svstr surface V-stress
Aout(idUbms) == F ! bustr bottom U-stress
Aout(idVbms) == F ! bvstr bottom V-stress
Aout(idUairE)== F
Aout(idVairN)== F
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) == T ! rho density anomaly
Aout(idSSSf) == F
Aout(idVvis) == T ! AKv vertical viscosity
Aout(idTdif) == T ! AKt vertical T-diffusion
Aout(idSdif) == T ! AKs vertical Salinity diffusion
Aout(idHsbl) == F ! Hsbl depth of surface boundary layer
Aout(idHbbl) == F ! 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) == F ! uu quadratic <u*u> term
Aout(idUVav) == F ! uv quadratic <u*v> term
Aout(idVVav) == F ! vv quadratic <v*v> term
Aout(idU2av) == F ! ubar2 quadratic <ubar*ubar> term
Aout(idV2av) == F ! vbar2 quadratic <vbar*vbar> term
Aout(idZZav) == F ! zeta2 quadratic <zeta*zeta> term
Aout(idTTav) == F F ! temp2, salt2 quadratic <t*t> T/S terms
Aout(idUTav) == F F ! utemp, usalt quadratic <u*t> T/S terms
Aout(idVTav) == F F ! vtemp, vsalt quadratic <v*t> T/S terms
Aout(iHUTav) == F F ! Huontemp, ... T/S volume flux, <Huon*t>
Aout(iHVTav) == F F ! Hvomtemp, ... T/S volume flux, <Hvom*t>
! Logical switches (TRUE/FALSE) to activate writing of extra inert passive
! tracers other than biological and sediment tracers into the AVERAGE file.
Aout(inert) == T T T ! 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) == T ! ubar_accel, ... acceleration
Dout(M2pgrd) == T ! ubar_prsgrd, ... pressure gradient
Dout(M2fcor) == T ! ubar_cor, ... Coriolis force
Dout(M2hadv) == T ! ubar_hadv, ... horizontal total advection
Dout(M2xadv) == T ! ubar_xadv, ... horizontal XI-advection
Dout(M2yadv) == T ! ubar_yadv, ... horizontal ETA-advection
Dout(M2hrad) == T ! ubar_hrad, ... horizontal total radiation stress
Dout(M2hvis) == T ! ubar_hvisc, ... horizontal total viscosity
Dout(M2xvis) == T ! ubar_xvisc, ... horizontal XI-viscosity
Dout(M2yvis) == T ! ubar_yvisc, ... horizontal ETA-viscosity
Dout(M2sstr) == T ! ubar_sstr, ... surface stress
Dout(M2bstr) == T ! ubar_bstr, ... bottom stress
! Logical switches (TRUE/FALSE) to activate writing of time-averaged,
! 3D momentum (u,v) diagnostic terms into DIAGNOSTIC output file.
Dout(M3rate) == T ! u_accel, ... acceleration
Dout(M3pgrd) == T ! u_prsgrd, ... pressure gradient
Dout(M3fcor) == T ! u_cor, ... Coriolis force
Dout(M3hadv) == T ! u_hadv, ... horizontal total advection
Dout(M3xadv) == T ! u_xadv, ... horizontal XI-advection
Dout(M3yadv) == T ! u_yadv, ... horizontal ETA-advection
Dout(M3vadv) == T ! u_vadv, ... vertical advection
Dout(M3hrad) == T ! u_hrad, ... horizontal total radiation stress
Dout(M3vrad) == T ! u_vrad, ... vertical radiation stress
Dout(M3hvis) == T ! u_hvisc, ... horizontal total viscosity
Dout(M3xvis) == T ! u_xvisc, ... horizontal XI-viscosity
Dout(M3yvis) == T ! u_yvisc, ... horizontal ETA-viscosity
Dout(M3vvis) == T ! u_vvisc, ... 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) == T T ! temp_rate, ... time rate of change
Dout(iThadv) == T T ! temp_hadv, ... horizontal total advection
Dout(iTxadv) == T T ! temp_xadv, ... horizontal XI-advection
Dout(iTyadv) == T T ! temp_yadv, ... horizontal ETA-advection
Dout(iTvadv) == T T ! temp_vadv, ... vertical advection
Dout(iThdif) == T T ! temp_hdiff, ... horizontal total diffusion
Dout(iTxdif) == T T ! temp_xdiff, ... horizontal XI-diffusion
Dout(iTydif) == T T ! temp_ydiff, ... horizontal ETA-diffusion
Dout(iTsdif) == T T ! temp_sdiff, ... horizontal S-diffusion
Dout(iTvdif) == T T ! temp_vdiff, ... vertical diffusion
!END MARKER TWO
! 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 = 1 ! deflate level [0-9]
! Input NetCDF file names, [1:Ngrids].
GRDNAME == /scratch/scumb002/Forcing/ross_grd.ishelf.davey.r36.5km.nc
ININAME == /scratch/scumb002/Forcing/ross_rst.088.cdw.yr6.4dye.5km.nc
ITLNAME == ocean_itl.nc
IRPNAME == ocean_irp.nc
IADNAME == ocean_iad.nc
FWDNAME == ocean_fwd.nc
ADSNAME == ocean_ads.nc
! Input lateral boundary and climatology file names. The USER has the
! option to enter several files names per each nested grid. For example,
! the USER may have a different files for velocity, ice, etc.
! The model will scan the file list and will read the needed data
! from the first file in the list containing the boundary field. Therefore,
! the order of the file names is very important. If multiple boundary
! 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.
! 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.
NCLMFILES == 1 ! number of climate files
CLMNAME == /scratch/scumb002/Forcing/ross_clm.ishelf.davey.3dye.r36.5km.nc
NBCFILES == 1 ! number of boundary files
BRYNAME == /scratch/scumb002/Forcing/ross_boundary.davey.4dye.r36.1012.5km.drift.nc
! Input forcing NetCDF file name(s). The USER has the option to enter
! several file names for each nested grid. For example, the USER may
! have 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 using multiple forcing
! files per grid, first enter 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 == 1 ! number of forcing files
FRCNAME == /scratch/scumb002/Forcing/ross_forcing.ishelf.eraint.ice.1012.5km.drift.nc
! Output NetCDF file names, [1:Ngrids].
GSTNAME == ross_gst.nc
RSTNAME == /scratch/scumb002/Output/054/ross_rst.nc
HISNAME == /scratch/scumb002/Output/054/ross_his.nc
TLMNAME == ross_tlm.nc
TLFNAME == ross_tlf.nc
ADJNAME == ross_adj.nc
AVGNAME == /scratch/scumb002/Output/054/ross_avg.nc
DIANAME == /scratch/scumb002/Output/054/ross_dia.nc
STANAME == /scratch/scumb002/Output/054/ross_sta_054.nc
FLTNAME == ross_flt.nc
! Input ASCII parameter filenames.
APARNAM = ROMS/External/s4dvar.in
SPOSNAM = Apps/ROSS/stations.ROSS.in
FPOSNAM = ROMS/External/floats.in
IPARNAM = Apps/ROSS/ice.in
BPARNAM = ROMS/External/bio_Fennel.in
SPARNAM = ROMS/External/sediment.in
USRNAME = ROMS/External/MyFile.dat
!
! GLOSSARY:
! =========
!
!------------------------------------------------------------------------------
! Application tile (string with a maximum of eighty characters) and
! C-preprocessing flag.
!------------------------------------------------------------------------------
!
! TITLE Application title.
!
! MyAppCPP Application C-preprocessing option.
!
!------------------------------------------------------------------------------
! Variable information file name (string with a maximum of eighty characters).
!------------------------------------------------------------------------------
!
! VARNAME Input/Output variable information file name. This file needs 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 they 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 possible 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 number 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 to or greater than one.
!
! NtileJ Number of domain partitions in the J-direction (ETA-coordinate).
! It must be equal to 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 the 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 no need to split 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 at 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 a 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 (say 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 file. 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. It also determines the interval between
! computation of global energy diagnostics.
!
!------------------------------------------------------------------------------
! Output history and average files parameters.
!------------------------------------------------------------------------------
!