CERA-SAT ocean component and further developments · CERA-SAT minus ORA-S5 - Global • CERA-20C...

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ERA-CLIM2 General Assembly, University of Bern 12-15 December 2017 CERA-SAT ocean component and further developments Eric de Boisséson, Dinand Schepers, Patrick Laloyaux, Per Dahlgren, Yuki Kosaka, Giovanna De Chiara, Marcin Chrust, Magdalena Balmaseda, Phil Browne, Patricia de Rosnay, Michael Mayer, Roberto Buizza

Transcript of CERA-SAT ocean component and further developments · CERA-SAT minus ORA-S5 - Global • CERA-20C...

  • ERA-CLIM2GeneralAssembly,UniversityofBern12-15December2017

    CERA-SAToceancomponentandfurtherdevelopments

    EricdeBoisséson,DinandSchepers,PatrickLaloyaux,PerDahlgren,YukiKosaka,GiovannaDeChiara,MarcinChrust,MagdalenaBalmaseda,PhilBrowne,PatriciadeRosnay,MichaelMayer,RobertoBuizza

  • CERA-20C CERA-SAT

    ResoluQon ORCA1_Z42 ORCA025_Z75

    OceanIC 10ensemblemembersfromORA-20C 2x5ensemblemembersfromORAS5

    AssimilaQon EN4.0.2T/Sprofiles EN4.1T/SprofilesAVISOalong-trackSLA(usingORAS5MDT)OSTIAsea-ice

    SSTrelaxaQon HadISST2.1.1¼degreemonthly OSTIA1/20degreedaily

    Period 1901-2010 2008-2016

    IntroducQon

    •  FromCERA-20CoceantoCERA-SATocean:

    •  CERA-SAToceanhasbeenproducedin4separatestreams(6-monthoverlap)thatcover2008-2016:

    CourtesyofD.Schepers

  • •  Thesea-iceissuesinCERA-20Cwere“solved”inCERA-SAT:problemswithsefngsforsea-icealbedoandtemperatureincoupledmode.

    ArcQcicethickness

    March2002icethick.CERA-20C March2014icethick.CERA-SAT March2014icethick.ORA-S5

    •  Driginsea-icethicknessseeninCERA-20Ccontained.Nosignsofsea-iceaccumulaQonintheArcQc.CERA-SATsea-icesimilartoORAS5sea-ice.

    CERA-SAToceanvsORAS5

  • •  CERA-SATstreamsrestartfromORA-S5ICs.LikeinCERA-20C,CERA-SATisdrigingfromitsbaseline.

    CERA-SAToceanvsORAS5

    Temp.CERA-20CminusORA-20C-Global Temp.CERA-SATminusORA-S5-Global

    •  CERA-20CwasgainingheatwrtORA-20Cfromthestartofeachstream.InCERA-SAT,differencesaresmaller,butthingsarelessstraighiorward.DifferencesassociatedwithstraQficaQonbutalsoAMOCadjustment.

    Temp.CERA-SATminusORA-S5-Tropics NextraTropics SextraTropics

  • CERA-SAToceanvsORAS5

    •  OceanheatbudgetanalysisinCERA-SATandORA-S5

    CERA-SATOceanHeatBudget-Global ORA-S5OceanHeatBudget-Global

    •  InCERA-SAT,fluxesandincrementstendstoaddheattotheocean.TheSSTrelaxaQoniscoolingtostayclosetoOSTIASSTanalysis.

    •  HeatfluxeshaveoppositesignsinCERA-SATandORA-S5.ThecontribuQonofthebiascorrecQonschemeinORA-S5isthelargestandcompensatesforthelargenegaQveflux.

    •  Conclusionsunclear.SSTrelaxaQonappropriate?BiascorrecQonneededinCERA?(SeeXiangbo’sreport)

  • CERA-SAToceanvsORAS5

    •  FittoobservaQons:

    RMSTempvsprofiles2011-2014-Global

    RMSSSHvssatellite-Global

    ORAS5CERASAT

    •  CERA-SATdoesnotfitprofilesaswellasORAS5intheupperocean.BiascorrecQonneededinCERA?OceanassimilaQonsefngstoberevisedincoupledmode?

    •  ThefittoalQmeterisalsoslightlyworseinCERA-SAT.DuetotheuseofuncoupledMDTforcoupledrun?Theerrorisnotgrowingthough.

    •  TheoceanassimilaQonincoupledmodeneedsrevisionwhendevelopingthenextreanalysisbasedonCERAifwewanttomatchocean-onlyperformances.

  • Coupledvsuncoupledspread

    •  InanuncoupledatmosphericreanalysissuchasERA5,thespreadattheair-seainterfaceisgeneratedbytheschemedevelopedbyHiraharaetal.(2016)thatappliesperturbaQonstoSSTandsea-iceusinginformaQonfromdifferentreanalysisproducts.ThespreadisstaQc.

    •  InCERA,thespreadattheair-seainterfaceisflow-dependentresulQngfromtheatmosphericEDAandtheperturbaQonsappliedtotheocean.

    SSTspread5S-5N–UncoupledCERA-SAT SSTspread5S-5N–CERA-SAT

    •  Thespreadislargerintheuncoupledreanalysis.ButtheCERA-SATspreadisabletocapturefinephysicalfeaturesassociatedtoENSOvariabilityandTIWs

  • Coupledvsuncoupledspread

    •  TheSSTspreaddirectlyimpactstheatmosphericvariablethatarecloselyassociatedSKTspread5S-5N

    Uncoupled CERA-SAT2Tspread5S-5N

    Uncoupled CERA-SAT

    Uncoupled CERA-SATEvaporaQonspread5S-5N

    •  TheextenttowhichthisimpactshigheratmosphericlevelsandwindsremainstobeinvesQgatedasnodirectimpactisasobviousasfortheparametersshownhere...

  • Impactofscaqerometerdataontheocean

    •  CasestudyontheimpactofassimilaQngscaqerometerdatainCERA-SAT:

    •  Directimpactonthemomentumforcingovertheocean.Oceancurrentsresponse.

    CourtesyofG.DeChiara

    Impactonsurfacewinds

    Impactonsurfacecurrents

  • Impactofscaqerometerdataontheocean

    •  CasestudyontheimpactofassimilaQngscaqerometerdatainCERA-SAT:NWPacific

    SCATNoSCAT

    NWAtlanQc

    Nino3.4

    SCATNoSCAT

    NWPacific

    Impactonoceantemperature

    Impactonoceansalinity

    CourtesyofG.DeChiara

    SSS

    E-P

  • Impactofscaqerometerdataontheocean

    •  CasestudyontheimpactofassimilaQngscaqerometerdatainCERA-SAT:

    SCATNoSCAT

    ImpactonsealevelFittoalQmeter–50S-50N

    •  AssimilaQngornotscaqerometerimpactsoceanparametersandtheabilityofthesystemtofitobservaQons.ScaqerometerdatahelpswiththeassimilaQonofT/SprofilesandalQmeterSLA

    •  On-goingstudythatwillfurtherinvesQgatetheimpactofscaqerometerobservaQonsinthe

    coupledsystem.

    CourtesyofG.DeChiara

  • Futuredevelopments:SSTassimilaQon

    •  ImplementaQonofdevelopmentsfromprojectpartnersintothereanalysissystem

    •  AssimilaQonofSST:usingUKMOframeworktoreplacethecurrentSSTrelaxaQonscheme

    •  TestdatasetprovidedbyUKMO:oneyearofbias-correctedSSTin-situandsatelliteobservaQons

    •  DatafromAMSRE,NOAA-AVHRR,AATSR,METOP-AVHRR,AMSR2,ships,drigersandmooredbuoys~8e5obs/day(3e4fortheprofiles)

  • Futuredevelopments:SSTassimilaQon

    •  TesQngoftheMLDparameterisaQonfortheverQcalcorrelaQonlengthscaletopropagatetheincrementduetoSSTobservaQonsdowntothethermocline

    •  SensiQvitytestswithSSTobservaQonerrorsdvandthinning

    SSTrelaxaQon-stdvert.lengthscales SSTassim-stdvert.lengthscales

    SSTrelaxaQon–MLDparam SSTassim–MLDparam

    SSTassim–thinning SSTassim–thin+OEincrease

    •  MLDparamallowsthepropagaQonoftheTincr.downtothethermocline

    •  FurtherthinningandincreasedSSTOEreducetheweightgiventoSSTobs.wrttoprofiles

  • FittoprofileobservaQonsJan-May2010–50S-50N

    SSTrelaxaQon-stdvert.lengthscalesvsMLDparamBKGRMSE(solid),ANRMSE(dashed)

    SSTassim–MLDparamBKGRMSE(solid),ANRMSE(dashed)

    •  SSTrelaxaQon:fittoprofilesgreatlyimprovedwithMLDparam.Butmuchmoreexpensive.

    •  SSTassimwithMLDparam:assimilaQngallthedataimprovesthebkginthefirstlevelsbutdegradesthefitinthethermoclineandatdepth.ThinningandincreasingtheOEsdvforSSThelpreducingthedegradaQonatdepthbutfirstlevelssQllworse.

    Futuredevelopments:SSTassimilaQon

    •  Firstresultsencouraging.WorksQllongoingtofindthebestconfiguraQon:convergence,MLDparam,OE,biascorrecQon…

  • Conclusion

    •  CERA-SATprovidesa¼degree10-memberensembleofoceanreanalysisproducedbyacoupledsystemover2008-2016

    •  CERA-SATisbeingrouQnelycomparedtotheORA-S5ocean-onlyreanalysisintermsofoceanparametersandfittoobservaQons.

    •  InsightsonpotenQalimprovements,impactofcoupled/forcedapproaches

    •  TheCERA-SATframeworkisbeingusedatECMWFforobservaQonstudiesinacoupledanalysissystem:exampleofscaqerometerdata

    •  CERA-SATisonlyamilestoneinthedevelopmentofanEarthsystemapproachtoNWPandreanalysis:coupledsystemadaptedforhigh-resoluQonNWP,baselineforERA6…

    •  CrucialdevelopmentssuchastheassimilaQonofSSTdataarebeingtestedforfutureimplementaQon