Options: Difference between revisions
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:Option to activate/deactivate 3D model configuration. If activated, ROMS solves 3D (baroclinic) primitive equations. If deactivated, ROMS solves vertically-integrated, shallow water (barotropic) equations. | :Option to activate/deactivate 3D model configuration. If activated, ROMS solves 3D (baroclinic) primitive equations. If deactivated, ROMS solves vertically-integrated, shallow water (barotropic) equations. | ||
:'''routine = ''' [[main2d.F]], [[main3d.F]]<section end=SOLVE3D /> | :'''routine = ''' [[main2d.F]], [[main3d.F]]<section end=SOLVE3D /> | ||
<section begin=SEDIMENT />;<span id="SEDIMENT"></span>'''[[SEDIMENT]]''' | |||
:Option to activate cohesive and non-cohesive sediment model ([[Bibliography#WarnerJC_2006a |Warner et al., 2006]]). | |||
:'''related = ''' [[ANA_BPFLUX]], [[ANA_SEDIMENT]], [[ANA_SPFLUX]], [[BEDLOAD]], [[RIVER_SEDIMENT]], [[SED_DENS]], [[SED_MORPH]], [[SUSPLOAD]] | |||
:'''routine = ''' [[sediment.F]], [[sediment.in]]<section end=SEDIMENT /> | |||
==<span class="alphabet">T</span>== | ==<span class="alphabet">T</span>== |
Revision as of 05:44, 23 November 2006
CPP Options
This wikipage includes all ROMS CPP options in alphabetic order. A single long page is built to facilitate printing. Each option has a unique anchor tag to facilitate linking from any wikipage. The following attributes have been identified to aid in the description of ROMS CPP options:
- conflit: indicates mutually exclusive options.
- parameter: important standard input parameter(s) or state array(s) associtated with the option.
- parent: indicates association to a main option.
- related: indicates other affiliated option(s) that may affect or not its scope.
- required: indicates other dependent option(s) that must be activated.
- routine: main files associated with the option.
Contents | |||||||||||||||||||||||||
A | B | C | D | E | F | G | H | I | J | K | L | M | N | O | P | Q | R | S | T | U | V | W | X | Y | Z |
A
- ANA_BIOLOGY
- Option to initialize any of the biological models with analytical expressions.
- related = BIOLOGY
- routine = analytical.F (ana_biology)
- ANA_BPFLUX
- Option to set passive tracers bottom flux with analytical expressions (usually zero, no flux).
- related = BIOLOGY, SEDIMENT
- routine = analytical.F (ana_bpflux)
- ANA_SPFLUX
- Option to set passive tracers surface flux with analytical expressions (usually zero, no flux).
- related = BIOLOGY, SEDIMENT
- routine = analytical.F (ana_spflux)
B
- BIOLOGY
- Internal option defined when any of the biological models is activated.
- related = BIO_FASHAM, ECOSIM, NPZD_FRANKS, NPZD_POWELL
- routine = biology.F
- BIO_FASHAM
- Option to activate Fasham-type, nitrogen-based biological model (Fasham et al., 1990; Fennel et al., 2006)
- related = ANA_BIOLOGY, ANA_BPFLUX, ANA_SPFLUX, BIO_SEDIMENT, CARBON, DENITRIFICATION, DIAGNOSTICS_BIO, OXYGEN, TALK_PROGNOSTIC
- conflict = ECOSIM, NPZD_FRANKS, NPZD_POWELL
- routine = fasham.h, bioFasham.in
- BIO_SEDIMENT
- Option to restore fallen particulate material to the nutrient pool in Fasham-type model.
- parent = BIO_FASHAM
- routine = fasham.h
C
- CARBON
- Option to include carbon constituents in Fasham-type biological model. Currently, four carbon-based tracer are added to include large detritus (iLDeC), small detritus (iSDeC), total inorganic carbon (iTIC_), and total alkalinity (iTAlk).
- parent = BIO_FASHAM
- required = OXYGEN
- routine = fasham.h
D
- DENITRIFICATION
- Option to include denitrification processes in Fasham-type biological model.
- parent = BIO_FASHAM
- routine = fasham.h
- DIAGNOSTICS
- Internal option to compute and write balance term diagnostics for tracers and momentum.
- related = DIAGNOSTICS_BIO, DIAGNOSTICS_TS, DIAGNOSTICS_UV
- routine = set_diags.F, wrt_diags.F
- DIAGNOSTICS_BIO
- Option to compute and write biological diagnostic terms in Fasham-type model.
- parent = BIO_FASHAM
- related = DIAGNOSTICS_TS, DIAGNOSTICS_UV
- routine = fasham.h, wrt_diags.F
- DIAGNOSTICS_TS
- Option to compute and write diagnostic terms for tracer equations balances.
- related = DIAGNOSTICS_BIO, DIAGNOSTICS_UV
- routine = set_diags.F, step3d_t.F, wrt_diags.F
- DIAGNOSTICS_UV
- Option to compute and write diagnostic terms for momentum equations balances.
- related = DIAGNOSTICS_BIO, DIAGNOSTICS_TS
- routine = set_diags.F, step2d.F, step3d_t.F, wrt_diags.F
E
- ECOSIM
- Option to activate Bio-optical EcoSim (Bissett et al., 1999a, b) model.
- related = ANA_BIOLOGY, ANA_BPFLUX, ANA_SPFLUX
- conflict = BIO_FASHAM, NPZD_FRANKS, NPZD_POWELL
- routine = ecosim.h, ecosim.in
F
G
- GLS_MIXING
- Option to activate Generic Length Scale vertical mixing parameterization (Warner et al., 2005).
- related = CANUTO_A, CANUTO_B
- conflict = MY25_MIXING, LMD_MIXING
- routine = gls_corstep.F, gls_prestep.F, ocean.in
H
I
J
K
L
M
N
- NPZD_FRANKS
- Option to activate Franks et al. (1986) NPZD biological model.
- related = ANA_BIOLOGY, ANA_BPFLUX, ANA_SPFLUX
- conflict = BIO_FASHAM, ECOSIM, NPZD_POWELL
- routine = npzd_Franks.h, npzd_Franks.in
- NPZD_POWELL
- Option to activate Powell et al. (1986) NPZD biological model.
- related = ANA_BIOLOGY, ANA_BPFLUX, ANA_SPFLUX
- conflict = BIO_FASHAM, ECOSIM, NPZD_FRANKS
- routine = npzd_Powell.h, npzd_Powell.in
O
- OCMIP_OXYGEN_SC
- Option to use the Keeling et al. (1998) formulae for the Schmit number to model O2 gas exchange. If deactivated, the formulation of Wanninkhof (1992) is used instead.
- parent = BIO_FASHAM
- required = OXYGEN
- routine = fasham.h
- OXYGEN
- Option to include oxygen dynamics in Fasham-type biological model. Currently, an additional tracer is added for dissolved oxygen concentration (iOxyg).
- parent = BIO_FASHAM
- routine = fasham.h
P
Q
R
S
- SOLVE3D
- Option to activate/deactivate 3D model configuration. If activated, ROMS solves 3D (baroclinic) primitive equations. If deactivated, ROMS solves vertically-integrated, shallow water (barotropic) equations.
- routine = main2d.F, main3d.F
- SEDIMENT
- Option to activate cohesive and non-cohesive sediment model (Warner et al., 2006).
- related = ANA_BPFLUX, ANA_SEDIMENT, ANA_SPFLUX, BEDLOAD, RIVER_SEDIMENT, SED_DENS, SED_MORPH, SUSPLOAD
- routine = sediment.F, sediment.in
T
- TALK_PROGNOSTIC
- Option to activate prognostic computation of alkalinity.
- parent = BIO_FASHAM
- required = CARBON
- routine = fasham.h
U
- UV_ADV
- Option to activate/deactivate horizontal and vertical advection of momentum. If no additional options are specified, the default is to discretize the horizontal momentum with a third-order upstream bias advection scheme with velocity dependent hyper-viscosity and the vertical momentum with a fourth-order, centered differences scheme. Since there is some implicit viscosity associated with the default discretization, the user may avoid adding an explicity vicosity to the solution to suppress excisive smoothing.
- routine = step2d.F, rhs3d.F
- UV_COR
- Option to activate/deactivate Coriolis acceleration term in momentum equations.
- routine = step2d.F, rhs3d.F
- UV_C2ADVECTION
- Option to use second-order, centered, finite differences in advection of momentum.
- parent = UV_ADV
- conflit = UV_C4ADVECTION
- UV_C4ADVECTION
- Option to use fourth-order, centered, finite differences in advection of momentum.
- parent = UV_ADV
- conflit = UV_C2ADVECTION
- UV_SADVECTION
- Option to use conservative, parabolic splines discretization of momentum vertical advection. This scheme requires high vertical resolution so it is recommended to use this option in shallow, coastal applications.
- parent = UV_ADV
- conflit = UV_C2ADVECTION, UV_C4ADVECTION
- UV_VIS2
- Option to activate/deactivate horizontal, harmonic viscosity of momentum. The hamonic mixing of momentum can be applied along terrain-following or geopotential levels. In ROMS, the viscosity is derived from the horizontal divergence of the deviatory stress tensor (Wajsowicz, 1993).
- parameter = visc2(ng), visc2_p(:,:), visc2_r(:,:)
- required = MIX_S_UV, MIX_GEO_UV
- related = VISC_GRID
- routine = uv3dmix2_s.h, uv3dmix2_geo.h, uv3dmix.F
- UV_VIS4
- Option to activate/deactivate horizontal, biharmonic viscosity of momentum. The bihamonic mixing of momentum can be applied along terrain-following or geopotential levels. In ROMS, the viscosity is derived from the horizontal divergence of the deviatory stress tensor (Wajsowicz, 1993).
- parameter = visc4(ng), visc4_p(:,:), visc4_r(:,:)
- required = MIX_S_UV, MIX_GEO_UV
- related = VISC_GRID
- routine = uv3dmix4_s.h, uv3dmix4_geo.h, uv3dmix.F
- UV_LOGDRAG
- Option to activate/deactivate logarithmic bottom friction of momentum.
- parameter = Zob(ng)
- required = SOLVE3D
- confict = BBL_MODEL, UV_LDRAG, UV_QDRAG
- routine = set_vbc.F
- UV_LDRAG
- Option to activate/deactivate linear bottom friction of momentum.
- parameter = rdrg(ng)
- confict = BBL_MODEL, UV_LOGDRAG, UV_QDRAG
- routine = set_vbc.F
- UV_PSOURCE
- Option to activate/deactivate point sources/sinks of momentum. This option is used to specify the mass transport in river runoff.
- parameter = Dsrc(1:Nsrc), Qsrc(1:Nsrc,k)
- related = ANA_PSOURCE, TS_PSOURCE
- confict = BBL_MODEL, UV_LOGDRAG, UV_QDRAG
- routine = step2d.F, step3d_uv.F
- UV_QDRAG
- Option to activate/deactivate quadratic bottom friction of momentum.
- parameter = rdrg2(ng)
- confict = BBL_MODEL, UV_LDRAG, UV_LOGDRAG
- routine = set_vbc.F