MRI-CGCM3 MRI-CGCM3 -Regional metrics of the mean state Meridional distribution in zonal-mean shortwave and longwave fluxes at TOA RMSE of geographical distribution of precipitation Meteorological Research Institute MRI Meteorological Research Institute MRI Meteorological Research Institute MRI Meteorological Research Institute MRI 2011 Yukimoto_2011 http://www.mri-jma.go.jp/Publish/Technical/DATA/VOL_64/tec_rep_mri_64.pdf Yukimoto, S., H. Yoshimura, M. Hosaka, T. Sakami, H. Tsujino, M. Hirabara, T.Y. Tanaka, M. Deushi, A. Obata, H. Nakano, Y. Adachi, E. Shindo, S. Yabu, T. Ose and A. Kitoh (2011). "Meteorological Research Institute-Earth System Model v1 (MRI-ESM1) - Model Description -". Technical Report of MRI, No. 64, 83 pp. Yukimoto_2012 https://www.jstage.jst.go.jp/article/jmsj/90A/0/90A_2012-A02/_pdf Yukimoto, S., Y. Adachi, M. Hosaka, T. Sakami, H. Yoshimura, M., Hirabara, T.-Y. Tanaka, E. Shindo, H. Tsujino, M. Deushi, R. Mizuta, S. Yabu, A. Obata, H. Nakano, T. Koshiro, T. Ose, A. Kitoh (2012). "A New Global Climate Model of the Meteorological Research Institute: MRI-CGCM3 —Model Description and Basic Performance— ", J. Meteor. Soc. Japan, 90A, 23-64. Aerosols MASINGAR Aerosol Key Properties Aerosol Key Properties AerosolSchemeScope AerosolSchemeScope stratosphere troposphere BasicApproximations BasicApproximations Ideal gas, primitive equations, external mixture ListOfPrognosticVariables ListOfPrognosticVariables 3D mass/volume mixing ratio for aerosols NumberOfTracers NumberOfTracers ??? kazoeru FamilyApproach FamilyApproach no AerosolTimeStepFramework AerosolTimeStepFramework Method Method specific time stepping (integrated) TimeStep TimeStep 1200sec (???) SchemeType SchemeType semi-implicit Meteorological Research Institute MRI Meteorological Research Institute MRI Meteorological Research Institute MRI Meteorological Research Institute MRI 2012 Aerosol Emission And Conc Aerosol Emission And Conc 2D-Emissions 2D-Emissions Method Method interactive prescribed (climatology) SourceTypes SourceTypes anthropogenic bare ground other sea surface vegetation ClimatologyType ClimatologyType other ClimEmittedSpecies ClimEmittedSpecies terpene (monthly), sulfate, SO2, BC, POM(RCP,monthly, linear interpolation) InteractivEmittedSpecies InteractivEmittedSpecies dust, sea salt, DMS 3D-Emissions 3D-Emissions Method Method other prescribed (climatology) SourceTypes SourceTypes aircraft biomass burning volcanoes ClimatologyType ClimatologyType monthly ClimEmittedSpecies ClimEmittedSpecies aircraft, non-sporadic volcanoes (const) MethodCharacteristics MethodCharacteristics historical volcano database EmittedSpecies EmittedSpecies sporadic volcanoes (SO2) Concentrations Concentrations PrescribedLowerBoundary PrescribedLowerBoundary OCS PrescribedUpperBoundary PrescribedUpperBoundary none Meteorological Research Institute MRI Meteorological Research Institute MRI Meteorological Research Institute MRI Meteorological Research Institute MRI metafor http://proj.badc.rl.ac.uk/svn/metafor/cmip5q/trunk c3eb3f24-5eb5-11e1-9a81-00163e9152a5 1 Metafor Questionnaire 2012-08-06T03:46:34.536358 Aerosol Model Aerosol Model Coupling With: snow albedo on sea ice Gas Phase Precursors: SO3 Processes Processes advection (horizontal) advection (vertical) ageing dry deposition heterogeneous chemistry oxidation (gas phase) oxidation (in cloud) sedimentation wet deposition (impaction scavenging) wet deposition (nucleation scavenging) CouplingWith CouplingWith Clouds HeterogeneousChemistry LandSurface other Radiation GasPhasePrecursors GasPhasePrecursors DMS other SO2 terpene AerosolScheme AerosolScheme SchemeType SchemeType bin bulk BulkSpecies BulkSpecies BC (black carbon / soot) organic POM (particulate organic matter) SOA (secondary organic aerosols) sulphate BinFramework BinFramework single moment BinSpecies BinSpecies dust sea salt Meteorological Research Institute MRI Meteorological Research Institute MRI Meteorological Research Institute MRI Meteorological Research Institute MRI metafor http://proj.badc.rl.ac.uk/svn/metafor/cmip5q/trunk c46b133e-5eb5-11e1-9a81-00163e9152a5 1 Metafor Questionnaire 2012-08-06T03:46:34.619761 Aerosol Transport Aerosol Transport Method Method specific transport scheme SchemeType SchemeType Semi-Lagrangian MassConservation MassConservation concentrations positivity gradients monotony mass adjustment Convection Convection convective fluxes connected to tracers vertical velocities connected to tracers Turbulence Turbulence Method Method use same turbulence scheme as AtmosphericChemistry Meteorological Research Institute MRI Meteorological Research Institute MRI Meteorological Research Institute MRI Meteorological Research Institute MRI metafor http://proj.badc.rl.ac.uk/svn/metafor/cmip5q/trunk c3c69a3e-5eb5-11e1-9a81-00163e9152a5 1 Metafor Questionnaire 2012-08-06T03:46:34.677986 metafor http://proj.badc.rl.ac.uk/svn/metafor/cmip5q/trunk DRS_CMIP5_componentType http://proj.badc.rl.ac.uk/svn/metafor/cmip5q/trunk c354c2f6-5eb5-11e1-9a81-00163e9152a5 1 Metafor Questionnaire 2012-08-06T03:46:34.678080 Yukimoto et al. (2012) MASINGAR Atmosphere MRI-AGCM3.3 Atmos Key Properties atmos key properties Top Of Atmos Insolation Top Of Atmos Insolation ImpactOnOzone ImpactOnOzone yes SolarConstant SolarConstant Type Type transient Characteristics Characteristics Spectral solar insolation provided by SOLARIS is used for historical and future experiments. OrbitalParameters OrbitalParameters Type Type transient ComputationMethod ComputationMethod Berger 1978 TransientMethod TransientMethod obliquity, eccentricity, precession ModelFamily ModelFamily AGCM BasicApproximations BasicApproximations hydrostatic primitive equations VolcanoesImplementation VolcanoesImplementation none Orography Orography OrographyType OrographyType present-day Meteorological Research Institute MRI Meteorological Research Institute MRI Meteorological Research Institute MRI Meteorological Research Institute MRI 2011 Atmos Convect Turbul Cloud AtmosConvectTurbulCloud Microphysics / processes : activation of aerosols ( MEMO in kakushin model Microphysics : cloud droplets, effect of rain drops , effect of snow ) BoundaryLayerTurbulence BoundaryLayerTurbulence SchemeName SchemeName Mellor-Yamada SchemeType SchemeType TKE diagnostic CounterGradient CounterGradient no ClosureOrder ClosureOrder 2 DeepConvection DeepConvection SchemeName SchemeName Yoshimura SchemeType SchemeType mass-flux Processes Processes convective momentum transport (CMT) detrainment entrainment penetrative convection radiative effects of anvils updrafts and downdrafts SchemeMethod SchemeMethod CAPE ShallowConvection ShallowConvection Method Method same as deep (unified) OtherConvection OtherConvection SchemeName SchemeName none LargeScalePrecipitation LargeScalePrecipitation SchemeName SchemeName Tiedtke (1993) PrecipitatingHydrometeors PrecipitatingHydrometeors liquid rain snow Microphysics Microphysics SchemeName SchemeName Sakami (2012) Processes Processes cloud droplets cloud ice effect of raindrops effect of snow ice nucleation mixed phase other water vapour deposition Meteorological Research Institute MRI Meteorological Research Institute MRI Meteorological Research Institute MRI Meteorological Research Institute MRI Atmos Cloud Scheme Atmos Cloud Scheme Cloud Scheme Attributes / Cloud Overlap : other means maximum-random for LW, random for SW. CloudSchemeAttributes CloudSchemeAttributes SeparatedCloudTreatment SeparatedCloudTreatment yes CloudOverlap CloudOverlap other Processes Processes - SubGridScaleWaterDistribution SubGridScaleWaterDistribution Type Type prognostic FunctionName FunctionName uniform FunctionOrder FunctionOrder 2 CouplingWithConvection CouplingWithConvection coupled with deep and shallow Meteorological Research Institute MRI Meteorological Research Institute MRI Meteorological Research Institute MRI Meteorological Research Institute MRI metafor http://proj.badc.rl.ac.uk/svn/metafor/cmip5q/trunk c665c0da-5eb5-11e1-9a81-00163e9152a5 1 Metafor Questionnaire 2012-08-06T03:46:34.975855 Cloud Simulator Cloud Simulator COSPAttributes COSPAttributes COSPRunConfiguration COSPRunConfiguration inline NumberOfGridpoints NumberOfGridpoints 51200 NumberOfColumns NumberOfColumns 120 NumberOfLevels NumberOfLevels 40 InputsRadar InputsRadar RadarFrequency RadarFrequency 94.0 RadarType RadarType spaceborne UseGasAbsorption UseGasAbsorption yes UseEffectiveRadius UseEffectiveRadius yes InputsLidar InputsLidar LidarIceType LidarIceType Ice spheres Overlap Overlap max / random ISSCPAttributes ISSCPAttributes TopHeight TopHeight IR brightness and visible optical depth TopHeightDirection TopHeightDirection highest altitude level Meteorological Research Institute MRI Meteorological Research Institute MRI Meteorological Research Institute MRI Meteorological Research Institute MRI metafor http://proj.badc.rl.ac.uk/svn/metafor/cmip5q/trunk c6e3cb60-5eb5-11e1-9a81-00163e9152a5 1 Metafor Questionnaire 2012-08-06T03:46:35.074918 metafor http://proj.badc.rl.ac.uk/svn/metafor/cmip5q/trunk c663a250-5eb5-11e1-9a81-00163e9152a5 1 Metafor Questionnaire 2012-08-06T03:46:35.075009 Atmos Dynamical Core Atmos Dynamical Core Time Stepping Framework / Scheme Type : semi-implicit semi-Lagrangian Horizontal Diffusion / Scheme Method : bi-harmonic diffusion (MEMO: in kakushin prognostic vapour, cloud water (liquid+solid) ) ListOfPrognosticVariables ListOfPrognosticVariables clouds surface pressure temperature vapour/solid/liquid wind components TopBoundaryCondition TopBoundaryCondition sponge layer HeatTreatmentAtTop HeatTreatmentAtTop 0.01hPa WindTreatmentAtTop WindTreatmentAtTop 0.01hPa LateralBoundaryCondition LateralBoundaryCondition none TimeSteppingFramework TimeSteppingFramework SchemeType SchemeType other TimeStep TimeStep 1800 sec HorizontalDiscretization HorizontalDiscretization SchemeType SchemeType spectral PoleSingularityTreatment PoleSingularityTreatment none SchemeOrder SchemeOrder - HorizontalDiffusion HorizontalDiffusion SchemeName SchemeName bi-harmonic diffusion SchemeMethod SchemeMethod other Meteorological Research Institute MRI Meteorological Research Institute MRI Meteorological Research Institute MRI Meteorological Research Institute MRI Atmos Advection Atmos Advection - Tracers / SchemeName : vertically conservative semi-Lagrangian scheme ( Yoshimura (in preparation) , Yoshimura and Matsumura (2003,2005) and Yukimoto et al. (2011) ) - Momentum / Scheme Name: vertically conservative semi-Lagrangian scheme - Momentum / Scheme Characteristics : 5th order in horizontal, 3rd order in vertical Tracers Tracers SchemeName SchemeName other SchemeCharacteristics SchemeCharacteristics semi-Lagrangian ConservedQuantities ConservedQuantities total mass, water vapour, cloud water and tracers ConservationMethod ConservationMethod conservation fixer Momentum Momentum SchemeName SchemeName other SchemeCharacteristics SchemeCharacteristics other ConservedQuantities ConservedQuantities none Meteorological Research Institute MRI Meteorological Research Institute MRI Meteorological Research Institute MRI Meteorological Research Institute MRI metafor http://proj.badc.rl.ac.uk/svn/metafor/cmip5q/trunk c58539de-5eb5-11e1-9a81-00163e9152a5 1 Metafor Questionnaire 2012-08-06T03:46:35.233694 metafor http://proj.badc.rl.ac.uk/svn/metafor/cmip5q/trunk c580ff5e-5eb5-11e1-9a81-00163e9152a5 1 Metafor Questionnaire 2012-08-06T03:46:35.233763 Atmos Orography And Waves Atmos Orography And Waves SpongeLayer SpongeLayer none Background Background none SubGridScaleOrography SubGridScaleOrography effect on drag OrographicGravityWaves OrographicGravityWaves SourceMechanisms SourceMechanisms linear mountain waves CalculationMethod CalculationMethod non-linear calculation PropagationScheme PropagationScheme linear theory DissipationScheme DissipationScheme total wave Meteorological Research Institute MRI Meteorological Research Institute MRI Meteorological Research Institute MRI Meteorological Research Institute MRI metafor http://proj.badc.rl.ac.uk/svn/metafor/cmip5q/trunk c7cf6714-5eb5-11e1-9a81-00163e9152a5 1 Metafor Questionnaire 2012-08-06T03:46:35.321847 Atmos Radiation Atmos Radiation TimeStep TimeStep 1 hour for SW and 3 hours for LW AerosolTypes AerosolTypes BC (black carbon / soot) dust organic sea salt sulphate GHG-Types GHG-Types CFC CH4 CO2 H2O N2O O3 Longwave Longwave SchemeType SchemeType wide-band model SchemeMethod SchemeMethod layer interaction NumberOfSpectralIntervals NumberOfSpectralIntervals 9 Shortwave Shortwave SchemeType SchemeType wide-band model NumberOfSpectralIntervals NumberOfSpectralIntervals 22 CloudRadiativeProperties CloudRadiativeProperties ice ice Ebert and Curry (1992) liquid liquid Hu and Stamnes(1993) for LW, Slingo (1989) for SW Meteorological Research Institute MRI Meteorological Research Institute MRI Meteorological Research Institute MRI Meteorological Research Institute MRI metafor http://proj.badc.rl.ac.uk/svn/metafor/cmip5q/trunk c6288ad0-5eb5-11e1-9a81-00163e9152a5 1 Metafor Questionnaire 2012-08-06T03:46:35.397961 metafor http://proj.badc.rl.ac.uk/svn/metafor/cmip5q/trunk DRS_CMIP5_componentType http://proj.badc.rl.ac.uk/svn/metafor/cmip5q/trunk c4b2a366-5eb5-11e1-9a81-00163e9152a5 1 Metafor Questionnaire 2012-08-06T03:46:35.398081 Yukimoto et al.(2011) , Yukimoto et al.(2012) Land Ice SMIST SMIST (Simple Model of Ice SheeT) is used as the ice-sheet component of MRI-ESM1. When the SWE is larger than 10 m over the land surface, the excess snow is taken away from the land surface model and treated as an iceberg. The ice mass and its energy are passed to SMIST and transported by SMIST to the ocean through a TRIP channel (Oki and Sud, 1998). Meteorological Research Institute MRI Meteorological Research Institute MRI Meteorological Research Institute MRI Meteorological Research Institute MRI 2011 metafor http://proj.badc.rl.ac.uk/svn/metafor/cmip5q/trunk DRS_CMIP5_componentType http://proj.badc.rl.ac.uk/svn/metafor/cmip5q/trunk ca3f4cb2-5eb5-11e1-9a81-00163e9152a5 1 Metafor Questionnaire 2012-08-06T03:46:35.413326 Yukimoto et al. (2011) Land Surface Land Surface (HAL) Land Surface Key Properties Land Surface Key Properties - ConservationOfProperties / WaterTreatment: River channel used is Oki and Sud(1998). Many rivers bring the water to the ocean, but some of them bring it to inland lakes(storage). BasicApproximations BasicApproximations 2 layer big leaf Genealogy Genealogy SiB CouplingWithAtmosphere CouplingWithAtmosphere implicit LandCoverTypes LandCoverTypes bare soil ice vegetated ListOfPrognosticVariables ListOfPrognosticVariables canopy heat content canopy skin temperature canopy water content other snow albedo snow density snow layer thickness snow mass soil heat content soil moisture surface skin temperature ConservationOfProperties ConservationOfProperties WaterTreatment WaterTreatment other TimeSteppingFramework TimeSteppingFramework Method Method use Atmosphere time step Meteorological Research Institute MRI Meteorological Research Institute MRI Meteorological Research Institute MRI Meteorological Research Institute MRI 2012 Land Surface Albedo Land Surface Albedo Snow Albedo is calculated by using the aerosol mixing ratio. (Aoki et al., 2011) SpecificTiling SpecificTiling no SnowFreeAlbedo SnowFreeAlbedo Type Type prescribed SnowAlbedo SnowAlbedo Type Type prognostic FunctionOf FunctionOf aerosol deposition Snow density Snow grain type vegetation type Meteorological Research Institute MRI Meteorological Research Institute MRI Meteorological Research Institute MRI Meteorological Research Institute MRI metafor http://proj.badc.rl.ac.uk/svn/metafor/cmip5q/trunk ccdc46be-5eb5-11e1-9a81-00163e9152a5 1 Metafor Questionnaire 2012-08-06T03:46:35.534759 Land Surface Energy Balance Land Surface Energy Balance SpecificTiling SpecificTiling no NumberOfSurfaceTemperatures NumberOfSurfaceTemperatures 3 (canopy_temperature, grass_and_bare_ground_temperature and T2m) SchemeMethod SchemeMethod TypeOfEvaporationFormulation TypeOfEvaporationFormulation combined Processes Processes transpiration Meteorological Research Institute MRI Meteorological Research Institute MRI Meteorological Research Institute MRI Meteorological Research Institute MRI metafor http://proj.badc.rl.ac.uk/svn/metafor/cmip5q/trunk ccc3b234-5eb5-11e1-9a81-00163e9152a5 1 Metafor Questionnaire 2012-08-06T03:46:35.572493 Land Surface Lakes Land Surface Lakes CouplingWithRivers CouplingWithRivers yes QuantitiesExchangedWithRivers QuantitiesExchangedWithRivers heat water SchemeMethod SchemeMethod IceTreatment IceTreatment no LakesAlbedo LakesAlbedo diagnostic LakesDynamics LakesDynamics none DynamicLakesExtent DynamicLakesExtent no EndorheicBasins EndorheicBasins yes Meteorological Research Institute MRI Meteorological Research Institute MRI Meteorological Research Institute MRI Meteorological Research Institute MRI metafor http://proj.badc.rl.ac.uk/svn/metafor/cmip5q/trunk cdbf36b8-5eb5-11e1-9a81-00163e9152a5 1 Metafor Questionnaire 2012-08-06T03:46:35.637118 Land Surface Snow Land Surface Snow SpecificTiling SpecificTiling yes NumberOfSnowLayers NumberOfSnowLayers 8 (It depends on the SWE and the history.) SchemeMethod SchemeMethod SnowAlbedo SnowAlbedo prognostic SnowDensity SnowDensity prognostic SnowWaterEquivalent SnowWaterEquivalent prognostic SnowHeatContent SnowHeatContent prognostic SnowTemperature SnowTemperature diagnostic SnowLiquidWaterContent SnowLiquidWaterContent prognostic SnowCoverFractions SnowCoverFractions ground snow fraction vegetation snow fraction Processes Processes snow interception snow melting snow refreezing Meteorological Research Institute MRI Meteorological Research Institute MRI Meteorological Research Institute MRI Meteorological Research Institute MRI metafor http://proj.badc.rl.ac.uk/svn/metafor/cmip5q/trunk cc573104-5eb5-11e1-9a81-00163e9152a5 1 Metafor Questionnaire 2012-08-06T03:46:35.695576 Land Surface Soil Land Surface Soil SoilMap SoilMap Texture Texture It depends on the vegetation type(SiB). Structure Structure It depends on the vegetation type(SiB). Albedo Albedo It depends on the vegetation type(SiB). WaterTable WaterTable It depends on the vegetation type(SiB). Meteorological Research Institute MRI Meteorological Research Institute MRI Meteorological Research Institute MRI Meteorological Research Institute MRI Land Surf Soil Heat Treatment Land Surf Soil Heat Treatment SoilHeatTreatmentAttributes SoilHeatTreatmentAttributes SpecificTiling SpecificTiling no NumberOfGroundHeatLayers NumberOfGroundHeatLayers 14 Method Method HeatStorage HeatStorage Explicit diffusion Processes Processes soil moisture freeze-thaw Meteorological Research Institute MRI Meteorological Research Institute MRI Meteorological Research Institute MRI Meteorological Research Institute MRI metafor http://proj.badc.rl.ac.uk/svn/metafor/cmip5q/trunk cc17852c-5eb5-11e1-9a81-00163e9152a5 1 Metafor Questionnaire 2012-08-06T03:46:35.768972 Land Surf Soil Hydrology Land Surf Soil Hydrology SoilHydrologyAttributes SoilHydrologyAttributes SpecificTiling SpecificTiling no NumberOfGroundWaterLayers NumberOfGroundWaterLayers It depends on the vegetation type(SiB). WaterStorageMethod WaterStorageMethod Explicit diffusion SoilMoistureFreezing SoilMoistureFreezing NumberOfGroundIceLayers NumberOfGroundIceLayers It depends on the vegetation type(SiB). The same as "Ground Water Layers" IceStorageMethod IceStorageMethod If the temperature is lower than the freezing point, the phase change occurs. Permafrost Permafrost specific treatment Runoff-Drainage Runoff-Drainage Method Method differentiated drainage and runoff Processes Processes deep drainage saturated surface runoff Meteorological Research Institute MRI Meteorological Research Institute MRI Meteorological Research Institute MRI Meteorological Research Institute MRI metafor http://proj.badc.rl.ac.uk/svn/metafor/cmip5q/trunk cba9b7e0-5eb5-11e1-9a81-00163e9152a5 1 Metafor Questionnaire 2012-08-06T03:46:35.835796 metafor http://proj.badc.rl.ac.uk/svn/metafor/cmip5q/trunk cba447b0-5eb5-11e1-9a81-00163e9152a5 1 Metafor Questionnaire 2012-08-06T03:46:35.835868 Land Surface Vegetation Land Surface Vegetation SpecificTiling SpecificTiling no VegetationRepresentation VegetationRepresentation vegetation types VegetationTimeVariation VegetationTimeVariation prescribed (varying from files) Interception Interception yes VegetationTypes VegetationTypes broadleaf tree C3 grass needleleaf tree other SchemeMethod SchemeMethod Phenology Phenology diagnostic (vegetation map) LAI LAI prescribed StomatalResistanceFunctionOf StomatalResistanceFunctionOf CO2 light water availability Meteorological Research Institute MRI Meteorological Research Institute MRI Meteorological Research Institute MRI Meteorological Research Institute MRI metafor http://proj.badc.rl.ac.uk/svn/metafor/cmip5q/trunk cc8c13f6-5eb5-11e1-9a81-00163e9152a5 1 Metafor Questionnaire 2012-08-06T03:46:35.906878 River Routing River Routing SpecificTiling SpecificTiling no Resolution Resolution independent NumberOfReservoirs NumberOfReservoirs many ListOfPrognosticVariables ListOfPrognosticVariables heat water CouplingWithAtmosphere CouplingWithAtmosphere no DrainageMap DrainageMap present-day OceanicDischarge OceanicDischarge Type Type direct (large rivers) QuantitiesTransported QuantitiesTransported heat water Meteorological Research Institute MRI Meteorological Research Institute MRI MRI 1-1, Nagamine, Tsukuba, Ibaraki, 305-0052, Japan http://www.mri-jma.go.jp/Welcome.html MRI Meteorological Research Institute MRI metafor http://proj.badc.rl.ac.uk/svn/metafor/cmip5q/trunk cd8427e4-5eb5-11e1-9a81-00163e9152a5 1 Metafor Questionnaire 2012-08-06T03:46:35.964673 metafor http://proj.badc.rl.ac.uk/svn/metafor/cmip5q/trunk DRS_CMIP5_componentType http://proj.badc.rl.ac.uk/svn/metafor/cmip5q/trunk cb5fea02-5eb5-11e1-9a81-00163e9152a5 1 Metafor Questionnaire 2012-08-06T03:46:35.964816 Yukimoto et al. (2011), Yukimoto et al. (2012) Ocean MRI.COM ver.3 Ocean Key Properties Ocean Key Properties Component Attributes / General Attributes / ListOfPrognosticVariables other = Nitrate, Phosphate, Phytoplankton, Zooplankton, Detritus, Total CO2, Alkalinity, Oxygen SeaWater / EquationState: other based on UNESCO(1981) Horizontal Discretization / PoleSingularityTreatment / other = tripolar If the surface salinity is less than 5 psu, it is nudged to climatological (PHC3) sea surface salinity with a piston velocity of 50 m / 10 day. ModelFamily ModelFamily OGCM BasicApproximations BasicApproximations Boussinesq primitive equations ListOfPrognosticVariables ListOfPrognosticVariables other potential temperature salinity SSH U-velocity V-velocity SeaWater SeaWater EquationOfState EquationOfState other FreezingPoint FreezingPoint varying SpecificHeat SpecificHeat fixed FreezingPointComputation FreezingPointComputation It depends on Salinity. m=-0.0543 S [degreeC/pss] SpecificHeatValue SpecificHeatValue 3.99e3 Non-OceanicWater Non-OceanicWater RiverMouthMixing RiverMouthMixing vertical mixing coefficients (0-30m): 10^(log10(R)+5), where R is the river discharge rate in units of cm/s IsolatedSeasMixing IsolatedSeasMixing no Bathymetry Bathymetry BathymetryType BathymetryType fixed ReferenceDate ReferenceDate present-day HorizontalDiscretization HorizontalDiscretization SchemeMethod SchemeMethod finite differences PoleSingularityTreatment PoleSingularityTreatment other Staggering Staggering Arakawa B-grid TimeSteppingFramework TimeSteppingFramework Tracers Tracers Leap-frog + Periodic Euler backward solver BarotropicSolver BarotropicSolver Forward-backward BaroclinicMomentum BaroclinicMomentum Leap-frog + Periodic Euler backward solver TimeStep TimeStep 1200sec Meteorological Research Institute MRI Meteorological Research Institute MRI Meteorological Research Institute MRI Meteorological Research Institute MRI 2010 Tsujino_2010 http://www.mri-jma.go.jp/Publish/Technical/DATA/VOL_59/59_en.html Tsujino, H., T. Motoi, I. Ishikawa, M. Hirabara, H. Nakano, G. Yamanaka, T. Yasuda, and H. Ishizaki (2010). "Reference Manual for the Meteorological Research Institute Community Ocean Model (MRI.COM) Version 3". Technical Report of the MRI, 59, 1-241. Ocean Advection Ocean Advection Momentum Momentum SchemeName SchemeName Ishizaki and Motoi (1999) SchemeType SchemeType Flux form LateralTracers LateralTracers SchemeType SchemeType Prather 2nd moment (PSOM) MonotonicFluxLimiter MonotonicFluxLimiter yes VerticalTracers VerticalTracers SchemeType SchemeType Prather 2nd moment (PSOM) MonotonicFluxLimiter MonotonicFluxLimiter yes Meteorological Research Institute MRI Meteorological Research Institute MRI Meteorological Research Institute MRI Meteorological Research Institute MRI metafor http://proj.badc.rl.ac.uk/svn/metafor/cmip5q/trunk cfe7020e-5eb5-11e1-9a81-00163e9152a5 1 Metafor Questionnaire 2012-08-06T03:46:36.193677 Ocean Boundary Forcing Ocean Boundary Forcing Momentum Momentum BottomFriction BottomFriction non-linear LateralFriction LateralFriction no-slip SurfaceFluxCorrection SurfaceFluxCorrection no Meteorological Research Institute MRI Meteorological Research Institute MRI Meteorological Research Institute MRI Meteorological Research Institute MRI Ocean Bound Forcing Tracers Ocean Bound Forcing Tracers General Attributes / Geothermal heating : no General Attributes / SurfaceFluxCorrections : no SurfaceSalinity / FromSeaice : Sea ice has salinity, 4psu. SunlightPenetration SunlightPenetration SchemeType SchemeType 2 extinction depths OceanColorDependent OceanColorDependent no SurfaceSalinity SurfaceSalinity FromAtmosphere FromAtmosphere freshwater flux FromSeaIce FromSeaIce other FromRiver FromRiver freshwater flux Meteorological Research Institute MRI Meteorological Research Institute MRI Meteorological Research Institute MRI Meteorological Research Institute MRI metafor http://proj.badc.rl.ac.uk/svn/metafor/cmip5q/trunk d182b662-5eb5-11e1-9a81-00163e9152a5 1 Metafor Questionnaire 2012-08-06T03:46:36.269221 metafor http://proj.badc.rl.ac.uk/svn/metafor/cmip5q/trunk d18072b2-5eb5-11e1-9a81-00163e9152a5 1 Metafor Questionnaire 2012-08-06T03:46:36.269287 Ocean Lateral Physics Ocean Lateral Physics Meteorological Research Institute MRI Meteorological Research Institute MRI Meteorological Research Institute MRI Meteorological Research Institute MRI Ocean Lateral Phys Momentum Ocean Lateral Phys Momentum Operator Operator Direction Direction horizontal Order Order harmonic (second order) Discretization Discretization second order EddyViscosityCoefficient EddyViscosityCoefficient CoefficientType CoefficientType time + space varying (Smagorinski) MinimalBackgroundValue MinimalBackgroundValue 0 Meteorological Research Institute MRI Meteorological Research Institute MRI Meteorological Research Institute MRI Meteorological Research Institute MRI metafor http://proj.badc.rl.ac.uk/svn/metafor/cmip5q/trunk d031d04a-5eb5-11e1-9a81-00163e9152a5 1 Metafor Questionnaire 2012-08-06T03:46:36.329345 Ocean Lateral Phys Tracers Ocean Lateral Phys Tracers MesoscaleClosure MesoscaleClosure no Operator Operator Direction Direction isoneutral Order Order harmonic (second order) Discretization Discretization second order EddyViscosityCoefficient EddyViscosityCoefficient CoefficientType CoefficientType constant BackgroundValue BackgroundValue 0 CoefficientValue CoefficientValue 1000 m^2/s^2 Eddy-inducedVelocity Eddy-inducedVelocity SchemeType SchemeType GM scheme FluxType FluxType skew flux AddedDiffusivity AddedDiffusivity none CoefficientType CoefficientType diagnostic Meteorological Research Institute MRI Meteorological Research Institute MRI Meteorological Research Institute MRI Meteorological Research Institute MRI metafor http://proj.badc.rl.ac.uk/svn/metafor/cmip5q/trunk d055f84e-5eb5-11e1-9a81-00163e9152a5 1 Metafor Questionnaire 2012-08-06T03:46:36.439912 metafor http://proj.badc.rl.ac.uk/svn/metafor/cmip5q/trunk d00804ae-5eb5-11e1-9a81-00163e9152a5 1 Metafor Questionnaire 2012-08-06T03:46:36.439991 Ocean Up And Low Boundaries Ocean Up And Low Boundaries FreeSurface FreeSurface Type Type non-linear split-explicit BottomBoundaryLayer BottomBoundaryLayer Type Type advective SillOverflow SillOverflow no specific treatment Meteorological Research Institute MRI Meteorological Research Institute MRI Meteorological Research Institute MRI Meteorological Research Institute MRI metafor http://proj.badc.rl.ac.uk/svn/metafor/cmip5q/trunk d1681ece-5eb5-11e1-9a81-00163e9152a5 1 Metafor Questionnaire 2012-08-06T03:46:36.491437 Ocean Vertical Physics Ocean Vertical Physics General Attributes / Tide-induced Mixing : The tidally driven mixing is applied around the Kuril Islands and the Sea of Okhotsk. Convection Convection non-penetrative convective adjustment Tide-inducedMixing Tide-inducedMixing other Meteorological Research Institute MRI Meteorological Research Institute MRI Meteorological Research Institute MRI Meteorological Research Institute MRI Ocean Interior Mixing Ocean Interior Mixing Tracers / Background value : Basically vertical profile. The diffusivity is large around the Kuril Islands and the Sea of Okhotsk. Tracers Tracers SchemeType SchemeType constant values BackgroundType BackgroundType other MixingCoefficient MixingCoefficient It depends on the depth. About 0.1e^(-4) (top) to 2.7e^(-4) (bottom). Momentum Momentum SchemeType SchemeType constant values BackgroundType BackgroundType other MixingCoefficient MixingCoefficient 1e(-5) m^2/s^2 Meteorological Research Institute MRI Meteorological Research Institute MRI Meteorological Research Institute MRI Meteorological Research Institute MRI metafor http://proj.badc.rl.ac.uk/svn/metafor/cmip5q/trunk d11073c2-5eb5-11e1-9a81-00163e9152a5 1 Metafor Questionnaire 2012-08-06T03:46:36.569551 Ocean Mixed Layer Ocean Mixed Layer Tracers / Scheme Type : modified Noh and Kim (1999) Momentum / Scheme Type : modified Noh and Kim (1999) Tracers Tracers SchemeType SchemeType other BackgroundCoefficient BackgroundCoefficient 1x10^(-5) (0m) - 2.7x10^(-4) (6300m) Momentum Momentum SchemeType SchemeType other BackgroundValue BackgroundValue 1x10^(-5) uniform Meteorological Research Institute MRI Meteorological Research Institute MRI Meteorological Research Institute MRI Meteorological Research Institute MRI metafor http://proj.badc.rl.ac.uk/svn/metafor/cmip5q/trunk d0994e32-5eb5-11e1-9a81-00163e9152a5 1 Metafor Questionnaire 2012-08-06T03:46:36.613150 metafor http://proj.badc.rl.ac.uk/svn/metafor/cmip5q/trunk d0971de2-5eb5-11e1-9a81-00163e9152a5 1 Metafor Questionnaire 2012-08-06T03:46:36.613219 metafor http://proj.badc.rl.ac.uk/svn/metafor/cmip5q/trunk DRS_CMIP5_componentType http://proj.badc.rl.ac.uk/svn/metafor/cmip5q/trunk cf41c2b2-5eb5-11e1-9a81-00163e9152a5 1 Metafor Questionnaire 2012-08-06T03:46:36.613345 Tsujino et al. (2010), Yukimoto et al.(2011), Yukimoto et al.(2012) Tsujino, H., T. Motoi, I. Ishikawa, M. Hirabara, H. Nakano, G. Yamanaka, T. Yasuda, and H. Ishizaki (2010). "Reference Manual for the Meteorological Research Institute Community Ocean Model (MRI.COM) Version 3". Technical Report of the MRI, 59, 241pp. Sea Ice Sea Ice Sea Ice Key Properties Sea Ice Key Properties BasicApproximations BasicApproximations 1 layer multi category ListOfPrognosticVariables ListOfPrognosticVariables concentration, ice thickness, snow thickness, ice temperature, horizontal velocity SeaIceRepresentation SeaIceRepresentation SchemeType SchemeType multi-levels Multi-LevelsScheme Multi-LevelsScheme 5 TimeSteppingFramework TimeSteppingFramework Method Method use Ocean time step Meteorological Research Institute MRI Meteorological Research Institute MRI Meteorological Research Institute MRI Meteorological Research Institute MRI 2010 Sea Ice Dynamics Sea Ice Dynamics General Attributes / advection : MPDATA Rheology Rheology EVP Advection Advection other HorizontalDiscretizationGrid HorizontalDiscretizationGrid Ocean grid Redistribution Redistribution Type Type ridging IceStrengthFormulation IceStrengthFormulation Hibler(1979) type Meteorological Research Institute MRI Meteorological Research Institute MRI Meteorological Research Institute MRI Meteorological Research Institute MRI metafor http://proj.badc.rl.ac.uk/svn/metafor/cmip5q/trunk d233b8c2-5eb5-11e1-9a81-00163e9152a5 1 Metafor Questionnaire 2012-08-06T03:46:36.713540 Sea Ice Thermodynamics Sea Ice Thermodynamics General attributes / surface albedo: The formulation of sea-ice surface albedo is fundamentally similar to that in the Los Alamos sea ice model CICE (Hunke and Lipscomb, 2001). Both the ice albedo and the snow albedo are estimated. The sea-ice surface albedo is determined as an average weighted by the snow cover percentage, which depends on the snow amount. However, the parameterization of Aoki and Tanaka (2008), who account for the albedo decline due to pollution by aerosol deposition, is applied to the estimation of snow albedo. Moreover, the effect of permeation on albedo is taken into account for both ice and snow for visible and near-infrared wavelengths, respectively. WaterPonds WaterPonds no SurfaceAlbedo SurfaceAlbedo It depends on amounts (depths) of ice or snow, temperature, and pollution due to aerosol deposition. See also additional information. This is calculated on Atmospheric grid. NewIceFormation NewIceFormation Sea ice is formed when sea surface temperature is below the freezing point. Snow Snow HeatDiffusion HeatDiffusion one layer SchemeType SchemeType snow-ice Ice Ice VerticalHeatDiffusion VerticalHeatDiffusion one layer OceanToIceBasalHeatFlux OceanToIceBasalHeatFlux parametrized (calculated in SeaIce) BrineInclusions BrineInclusions thermal properties depending on S-T (fixed salinity) Processes Processes Solar radiation transmission Surface sublimation TransportInThicknessSpace TransportInThicknessSpace linear remapping Meteorological Research Institute MRI Meteorological Research Institute MRI Meteorological Research Institute MRI Meteorological Research Institute MRI metafor http://proj.badc.rl.ac.uk/svn/metafor/cmip5q/trunk d20645a4-5eb5-11e1-9a81-00163e9152a5 1 Metafor Questionnaire 2012-08-06T03:46:36.778413 metafor http://proj.badc.rl.ac.uk/svn/metafor/cmip5q/trunk DRS_CMIP5_componentType http://proj.badc.rl.ac.uk/svn/metafor/cmip5q/trunk d1c114fc-5eb5-11e1-9a81-00163e9152a5 1 Metafor Questionnaire 2012-08-06T03:46:36.778503 Tsujino, H., T. Motoi, I. Ishikawa, M. Hirabara, H. Nakano, G. Yamanaka, T. Yasuda, and H. Ishizaki (2010). "Reference Manual for the Meteorological Research Institute Community Ocean Model (MRI.COM) Version 3". Technical Report of the MRI, 59, 241pp. metafor http://proj.badc.rl.ac.uk/svn/metafor/cmip5q/trunk c34e4fac-5eb5-11e1-9a81-00163e9152a5 2 Metafor Questionnaire 2012-08-06T03:46:36.778649 Yukimoto et al.(2011), Yukimoto et al.(2012) Meteorological Research Institute MRI Meteorological Research Institute MRI Meteorological Research Institute MRI Meteorological Research Institute MRI project http://proj.badc.rl.ac.uk/svn/metafor/cmip5q/trunk C_piCntrol_02 C_piCntrol_02 bcee1404-d3a5-11df-837f-00163e9152a5 piControl experiment 1 Reference to an Experiment called piControl with experimentNumber 3.1 MRI The resources(deployment) on which this simulation ran 282acc04-5eb4-11e1-8dd9-00163e9152a5 MRI Super Computer System platform 1 Reference to a platform called MRI Super Computer System 2351-12-30T23:59:59Z 1851-01-01T00:00:00Z c34e4fac-5eb5-11e1-9a81-00163e9152a5 MRI-CGCM3 modelComponent 2 Reference to a modelComponent called MRI-CGCM3 f17d36a0-cc9b-11e1-9eda-00163e9152a5 1 QN_DRS The QN_DRS value allows mapping from data files to metadata being exported from the metadata questionnaire, and contains the institution name, the model name on which the simulation was run, the experiment name to which the simulation conforms, the simulation level base rip value, and finally the given start year for the simulation. The format of the string will thus be: institute_model_experiment_rip_startyear. Also note, that in particular cases, i.e. decadal and noVolc exps, the start date and expdate may differ - this will occur in those cases where the simulation start date is 1st january but still refers to an experiment for the year before. - (see cmip5 experiment design document) DRS_CMIP5_ensembleType Metafor Questionnaire 2012-08-06T03:46:36.813193 Pre-Industrial Control. Control experiment against which perturbations are compared. piControl Pre-Industrial Control Pre-Industrial coupled atmosphere/ocean control run. Imposes non-evolving pre-industrial conditions. 3.1 ic.001 3.1.ic A description of initial condition for the control run. bc.001 3.1.bc.wmg_conc Prescribed atmospheric concentrations of pre-industrial well mixed gases: excluding CO2 bc.002 3.1.bc.CO2_conc Prescribed atmospheric concentrations of pre-industrial well mixed gas: Carbon Dioxide bc.003 3.1.bc.sls_conc Prescribed atmospheric concentration of pre-industrial short lived (reactive) gas species 3.1.bc.nat_aer Prescribed concentrations or emissions of pre-industrial natural aerosols bc.004 3.1.bc.nat_aer_conc Concentrations bc.007 3.1.bc.nat_aer_em Emissions 3.1.bc.nat_aer_precur Prescribed concentrations or emissions of pre-industrial natural aerosol precursors bc.005 3.1.bc.nat_aer_pre_conc Concentrations bc.008 3.1.bc.nat_aer_pre_em Emissions 3.1.bc.sl_aer Prescribed concentrations or emissions of pre-industrial short lived (reactive) aerosol species bc.006 3.1.bc.sl_aer_conc Concentrations bc.009 3.1.bc.sl_aer_em Emissions bc.010 3.1.bc.LU Unperturbed Pre-Industrial Land Use stc.024 3.1.stc.1850_500yr P500Y 1850-12-30T23:59:59Z 1850-01-01T00:00:00Z bcee1404-d3a5-11df-837f-00163e9152a5 1 Metafor Questionnaire 2012-08-06T03:46:36.834210 MRI Super Computer System_Other Machine MRI Super Computer System and compiler Other Power6 121nodes 4MCMs in each node 4 chips and 8 Cores in each MCM Hitachi Fortran Meteorological Research Institute MRI MRI Super Computer System Parallel machineOperatingSystem http://proj.badc.rl.ac.uk/svn/metafor/cmip5q/trunk machineVendor http://proj.badc.rl.ac.uk/svn/metafor/cmip5q/trunk 121 32 machineProcessorType http://proj.badc.rl.ac.uk/svn/metafor/cmip5q/trunk Other I do not know 282acc04-5eb4-11e1-8dd9-00163e9152a5 1 Metafor Questionnaire 2012-08-06T03:46:36.834414 TL95L48_aero TL95L48 192x96 -90 90 0 360 95 SpectralTruncatureNumber p = A(k)+B(k)*Psfc (A=0 below 930hPa, B=0 above 50hPa) Hybridization TL95 6c7792a6-c599-11e1-b203-00163e9152a5 1 Metafor Questionnaire 2012-08-06T03:46:37.044232 TL159L48 TL159L48 Gaussian Grid (320x160) -90 90 0 360 159 SpectralTruncatureNumber p = A(k)+B(k)*Psfc (A=0 below 930hPa, B=0 above 50hPa) Hybridization TL159 0d56a186-5eb5-11e1-9a81-00163e9152a5 1 Metafor Questionnaire 2012-08-06T03:46:37.151194 1x1_TRIP 1x1_TRIP 1x1 -90 90 0 360 180 NumberOfLatitudinalGridCells 360 NumberOfLongitudinalGridCells 8378d242-cbbd-11e1-aabb-00163e9152a5 1 Metafor Questionnaire 2012-08-06T03:46:37.254598 Ocean_tripolar Ocean_tripolar [Lon]360 x [Lat] 368x [Lev]50 Yukimoto_2012 https://www.jstage.jst.go.jp/article/jmsj/90A/0/90A_2012-A02/_pdf Yukimoto, S., Y. Adachi, M. Hosaka, T. Sakami, H. Yoshimura, M., Hirabara, T.-Y. Tanaka, E. Shindo, H. Tsujino, M. Deushi, R. Mizuta, S. Yabu, A. Obata, H. Nakano, T. Koshiro, T. Ose, A. Kitoh (2012). "A New Global Climate Model of the Meteorological Research Institute: MRI-CGCM3 —Model Description and Basic Performance— ", J. Meteor. Soc. Japan, 90A, 23-64. 78S 90N 0 360 90S ThirdPoleLat 0E ThirdPoleLon 64N FirstPoleLat 64N SecondPoleLat 364 (including 4 margin grids) NumberOfCellsInFirstGridDimension 368 NumberOfCellsInSecondGridDimension 100W SecondPoleLon 80E FirstPoleLon 10 NumberOfLevelsInUpper100m 0m UpperLevel 6300m + 50m BBL LowerLevel 50 + 1 Bottom Boundary Layer NumberOfLevels sigma: upper 5 layers (-32m) Hybridization N/A f96881d0-5eb4-11e1-9a81-00163e9152a5 1 Metafor Questionnaire 2012-08-06T03:46:37.359148