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WP2.5 – Coupled error covariances and bias
correc7on (1)XiangboFeng,KeithHaines,DavidMulholland
(2)EricdeBoisseson,Pa<rckLaloyaux
(1) DepartmentofMeteorology,UniversityofReading,UK(2) ECMWF,Reading,UK
18/01/17 ERA-CLIM23rdGeneralAssembly
UREAD: Deliverables
• D2.8ReportonstrengthsandweaknessesofweaklycoupledDAmethodsforEarthsystemreanalysis.UREAD18• D2.9Reportontechniquesforcalcula<ngcouplederrorcovariancesfromoutputsofaweaklycoupledDAexperiment.METO+UREAD18
18/01/17 ERA-CLIM23rdGeneralAssembly
• D2.10Reportonassessmentofcoupled-modeldri[andapproachesforobtainingconsistentoceanandatmosphericbiascorrec<ons.
UREAD34+12=46
Outline
1. Calcula<onofcrosserrorcovariancesatvarying<mescalesfromCERA-20C(D2.9)
2. StrengthsofCERA-20CoverERA-20C:SST-Prela<onship(D2.8)
3. TemporalvariabilityofoceanbiasinCERA-20C(D2.10)
18/01/17 ERA-CLIM23rdGeneralAssembly
1. Calcula7ng cross error covariances based on CERA-20C
• Method:CERA-20C=>10memberensembleproductEnsemblemean<>=Bestes<mateEnsemblespread=Uncertaintyes<mate(errors)Ensemblesavailableforboth24hourbackgroundfieldsxbandtheanalysesxaBackgrounderrorcovarianceprovidesbackgrounderrorinforma<onforassimila<onofsubsequentobserva<onsleadingtoanalysis• DataSST,T2m,Mixedlayerdepths,u10,v10andprecipita<onhavebeenstudied3-hourfieldsusedforJanuary2006monthlyfieldsusedfor1900-2010Mostanalysesbasedonanalysisensemblesxa• PaperSubmieedtoQJRMS
18/01/17 ERA-CLIM23rdGeneralAssembly
High-frequency varia7ons
ERA-CLIM23rdGeneralAssembly
3-hourfieldsfor1st-31stJanuary2006
• T2mspread>SSTSpread• T2mspreadlargeinITCZandinareas
withwesternboundarycurrents• SSTspreadislargeinsummerandin
upwellingregions• T2m-SSTerrorcorrela<onsarestronger
insummer(SH)andupwellingregions.• Small-scaledailyanomaliesanddiurnal
cyclesarealsoseen
T2mspread
SSTspread
SST-T2mcorrela1on
1Jananom.
1Jananom.
1Jananom.
DiurnalcyclesofspreadsT2m,SST,SST-T2mCorrel.
1
0E 180E 0W
18/01/17 ERA-CLIM23rdGeneralAssembly
Time mean of monthly 7mescale varia7ons Data:Monthlyaverageofeachensemblemember,2006-2010
• T2mandSSThavesimilarlarge-scalevaria<ons• T2m<SSTspread,exceptinITCZ• Correla<onsmostlysmallerwhereT2mspreadlarger• Note:TAOmooringisposi<oned
T2mspread
SSTspread
T2mspread/SSTspread
T2m-SSTcorrela1on
18/01/17 ERA-CLIM23rdGeneralAssembly
Seasonal cycles
• BothT2mandSSTspreadsexhibitaclearlarge-scaleseasonalcycle,0.02°C(10-20%ofthe<memean),withlargervaluesinsummerhemisphere.
• SSTspreadhas±1-2month<melag.
• AnnualamplitudeofT2m-SSTensemblecorrela<onis>0.1(15%ofthe<memean).
• MLDandatmosphericconvec<onaredis<nguishedtobethecausesforsuchseasonalvariability.
AmplitudeofT2mspread
AmplitudeofSSTspread
AmplitudeofT2m-SSTcorrel.
PhaseofT2mspread
PhaseofSSTspread
PhaseofT2m-SSTcorrel.
Data:Monthlyaverageofeachensemblemember,2006-2010
18/01/17 ERA-CLIM23rdGeneralAssembly
Long-term changes Data:Monthlyaveragesofeachensemblemember,1900-2010
• Spreadsdecreaseasobserva<onsincrease• ChangesaroundWWs,1980and2008correspondingtoabruptdatachanges• T2mspreadregulatedbywinduncertain<esinearlyyears• Correla<onssteadilyincreasethenleveloffa[er1980• Inter-annualvariabilitystronginNino3.4duetothedeepconvec<onmovement
SSTandT2mmean
SST,T2mand10mwindspreads
T2mandSSTensemblespreadra1oandcorrela1on
2. Strengths of weakly coupled DA for CERA-20C
18/01/17 ERA-CLIM23rdGeneralAssembly
SST-precipita<onrela<onship
• AimToevaluatetheimprovementsofCERA-20Cinrepresen<ngatmosphere-oceanfeedbacks• MethodLinearcorrela<onbetweenSSTandPrecipita1onmonthlyvariability• DataCERA-20Cmember0ERA-20CObserva<ons:HadISST2ensemblemean,GPCPobserva<onsMonthlyfieldswithseasonalcycleremovedfor1979-2010
18/01/17 ERA-CLIM23rdGeneralAssembly
SST-P monthly variability correla7ons
ERA-20C CERA-20C
Observa1ons
• ERA-20Chaswiderspreadofposi<vecorrela<ons• CERA-20Cmoreconsistentwithobserva<ons
18/01/17 ERA-CLIM23rdGeneralAssembly
BlackcontourishighPregionsClimatologicalP>12cm/month
SST-P correla7ons: High Precip. P > 12cm/month
ERA-20C CERA-20C
Observa1ons
• CERA-20Cespeciallyimprovestherela<onshipforhighPregions,whereair-seacouplingisstrong
18/01/17 ERA-CLIM23rdGeneralAssembly
ERA-20C CERA-20C
Observa1ons
• CERA-20Calsogreatlyimprovestherela<onshipforthehigh-frequency(sub-seasonal)variability.
• Obs.andCERA-20C:nega<vecorrela<on=>Precip.iscoolingSSTs.
SST-P correla7ons: Sub-seasonal variability (3-month running mean removed)
18/01/17 ERA-CLIM23rdGeneralAssembly
Monthly precipita7on differences for 7me mean GPCP-ERA-20C GPCP-CERA-20C
Errorreduc1oninCERA-20CcomparedtoERA-20C(posi1veforimprovement)
• CERA-20Cprovidesabeeeres<mateofPrateoveroceansthanERA-20C,presumablyasaresultofthebeeersimulatedSST-Prela<onship.
RedcontourishighPregionsClimatologicalP>12cm/month
18/01/17 14
GlobalP.average,60°N-60°S
ERA-20CCERA-20CGPCP
Oceans Lands
Monthly varia7ons
UREAD: Deliverables • D2.8ReportonstrengthsandweaknessesofweaklycoupledDAmethodsforEarthsystemreanalysis.UREAD18• D2.9Reportontechniquesforcalcula<ngcouplederrorcovariancesfromoutputsofaweaklycoupledDAexperiment.METO+UREAD18• D2.10Reportonassessmentofcoupled-modeldri[andapproachesforobtainingconsistentoceanandatmosphericbiascorrec<ons.
UREAD34+12=46
18/01/17 ERA-CLIM23rdGeneralAssembly
18/01/17 ERA-CLIM23rdGeneralAssembly
3.1 Bias in Seasonal Forecas7ng system 4
• ReportedatlastERACLIM2mee<ng• Publ.Mulhollandetal2016
• OceanAssimila<onBiascorrec<ons(T,S)maintainedintocoupledforecastruns
• Correc<onsDampedover20days• Equatorialwavenoisereduced• Manyhindcastini<alcondi<onstested1980’sonwards
• Nino3.4SSTforecastskillincreasedin4-7months
• Availablefortes<ngatECMWF(alsoMetO)
Mulholland,HainesandBalmaseda2016QJRMS
18/01/17 ERA-CLIM23rdGeneralAssembly
3.2 Ocean bias in CERA-20C
SSTincrement
• SSTinCERA-20Chasregionalbiasesw.r.tHadISST2by±0.5°C,andis~0.05°Cwarmeronglobalaverage
• SSTincrementisusuallynega<ve,andisoneorderofmagnitudesmallerthan∆SST• SSTbiasisconsiderablyconstantwith<me
∆SST
∆SST = CERA_an - HadISST2, and CERA_an- CERA_fc, 1900-2010
18/01/17 ERA-CLIM23rdGeneralAssembly
Mean subsurface T increment along tropics (5°N-5°S), 1990-2010
• Modelzonalheatredistribu<oninerrorneardateline• Errorsclearlyan<-correlated• Nobiascorrec<onscurrentlybeingappliedwhichcouldreducethesemean
incrementscf.Mulholland
Time mean
Temporal variability
18/01/17 ERA-CLIM23rdGeneralAssembly
Associa7on with ver7cal thermocline advec7on
• Monthlytemporalvaria<onsareassociatedwithlocalver<calvelocity,by~66.6deg.C/daypercm/s.
• NoteTAOmooringsites
Correla<onbetweenTincrementandWvelocityvariability,1990-2010
Further bias correc7on work • Oceanbiascorrec<onmethodshave(a)Climatologicalcorrec<on(needinglongpriorrun)+(b)Onlinecorrec<on• TestwhetherOnlinecorrec<onscancompensatefor“approximate”climatologicalcorrec<one.g.useORAS4pre-processedclimatologicalcorrec<onsinCERA-20C?• Inves<gateapplyingbiascorrec<oninCERA-20C(shortrunstotestimpact)• Inves<gatebiascorrec<onsinCERA-SAT?Shortrunse.g.usingCERA-20CorORAP/S5climatologicalcorrec<ons• Inves<gateotherapproachesforcorrec<ngoceanbiasinthetropicalthermocline,e.g.parametrizedwithver<calvelocity.
18/01/17 ERA-CLIM23rdGeneralAssembly
18/01/17 ERA-CLIM23rdGeneralAssembly
Thanks!