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Task Team for the Intercomparison of ReAnalyses (TIRA) Michael Bosilovich (drawing on input from the TIRA telecons)

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Page 1: Task Team for the Intercomparison of ReAnalyses (TIRA)€¦ · Spring 2016: 1851-2012, 2013-2014 extension Very similar system to 20CRv2. Fixed Sea ice using COBE-SST2 sea ice. More

TaskTeamfortheIntercomparisonofReAnalyses(TIRA)

MichaelBosilovich(drawingoninputfromtheTIRA

telecons)

Page 2: Task Team for the Intercomparison of ReAnalyses (TIRA)€¦ · Spring 2016: 1851-2012, 2013-2014 extension Very similar system to 20CRv2. Fixed Sea ice using COBE-SST2 sea ice. More

MainObjecBvesofTIRA•  TheprimarychargetotheTIRAistodevelopareanalysis

intercomparisonprojectplanthatwillaCainthefollowingobjecBves.1)  TofosterunderstandingandesBmaBonofuncertainBesin

reanalysisdatabyintercomparisonandothermeans2)  TocommunicatenewdevelopmentsandbestpracBces

amongthereanalysesproducingcenters3)  ToenhancetheunderstandingofdataandassimilaBonissues

andtheirimpactonuncertainBes,leadingtoimprovedreanalysesforclimateassessment

4)  Tocommunicatethestrengthsandweaknessesofreanalyses,theirfitnessforpurpose,andbestpracBcesintheuseofreanalysisdatasetsbythescienBficcommunity

Page 3: Task Team for the Intercomparison of ReAnalyses (TIRA)€¦ · Spring 2016: 1851-2012, 2013-2014 extension Very similar system to 20CRv2. Fixed Sea ice using COBE-SST2 sea ice. More

TaskTeamMembers•  MagdelenaBalmaseda(ECMWF/

CLIVAR)•  MichaelBosilovich(NASA/GMAO/

USACo-Chair*)•  CathySmith(CIRES/WRIT/USA)•  GilCompo(CIRES/20CR/USA)•  ChrisDerksen(ECCC/CliC/Canada)•  MasatomoFujiwara*Co-Chair

(JMA/SPARC/Japan/S-RIP)•  JanKeller*Co-Chair(DWD/

RegionalReanalysis)

•  HansHersbach(ECMWF)•  ShinyaKobayashi(JMA)•  WesleyEbisuzaki(NOAA/EMC/

USA)•  RemyRoca(GEWEX)•  ChenghuSun(CMA/NMIC)•  AndreaStorto(CCMC)•  GeraldPoCer(NASA/CREATE/

USA)•  OBsBrown(NCSU/USA/WDAC)•  MaChaisTuma(WCRP)

*NewCo-Chair

Page 4: Task Team for the Intercomparison of ReAnalyses (TIRA)€¦ · Spring 2016: 1851-2012, 2013-2014 extension Very similar system to 20CRv2. Fixed Sea ice using COBE-SST2 sea ice. More

Telecons•  RecentTeleconTopics/

Highlights–  CREATE-IPstatusandfuture

addiBonsanddevelopments(e.g.anensembleofreanalyses)

–  Discussionsonusefulnessofolderreanalyses,shouldtheybereBred,orlimited

–  Developapilotintercomparionproject,somethingtostartfuelingrealworkandcontribuBons

–  CollecBngalisBngofexisBngIntercmparisonwork:hCps://goo.gl/forms/0jwcuPwo8HIdwnqo2

Page 5: Task Team for the Intercomparison of ReAnalyses (TIRA)€¦ · Spring 2016: 1851-2012, 2013-2014 extension Very similar system to 20CRv2. Fixed Sea ice using COBE-SST2 sea ice. More

TIRAOverviewatWCRP5th

InternaBonalConferenceonReanalyses

•  PresentedthemoBvaBonandcurrentacBviBesatICR5(Rome,Nov2017)

Page 6: Task Team for the Intercomparison of ReAnalyses (TIRA)€¦ · Spring 2016: 1851-2012, 2013-2014 extension Very similar system to 20CRv2. Fixed Sea ice using COBE-SST2 sea ice. More

PilotIntercomparison•  AtICR5–groupdiscussionon

nextstepsneededtodefineaWCRPProjectfortheIntercomparisonofReanalyses

•  Document–developadocumentthathighlightsbestpracBcesandtermsofreference

•  Somewhatmoreinterest:Developone(ormore)PilotIntercomparisonProject(s)thatsomeintheteamcanstart,withagoalofrealworldexperienceinteracBngingroupacBviBesthathavesomedirectaffectonTIRAandtheparBcipants

•  RegionalProject-PrecipitaBon•  PossibleGlobalTopics•  [1]Surfacetemperature•  [2]Oceansurfacefluxes•  [3]PrecipitaBon•  [4]RadiaBon•  [5]Energybudget•  [6]Watercycle•  [7]SurfaceWinds(WindEnergy)•  Otherideasforglobal

atmosphericreanalyses?

Page 7: Task Team for the Intercomparison of ReAnalyses (TIRA)€¦ · Spring 2016: 1851-2012, 2013-2014 extension Very similar system to 20CRv2. Fixed Sea ice using COBE-SST2 sea ice. More

PilotEnergyBudgetIP

Page 8: Task Team for the Intercomparison of ReAnalyses (TIRA)€¦ · Spring 2016: 1851-2012, 2013-2014 extension Very similar system to 20CRv2. Fixed Sea ice using COBE-SST2 sea ice. More

PilotEnergyBudgetIP

Page 9: Task Team for the Intercomparison of ReAnalyses (TIRA)€¦ · Spring 2016: 1851-2012, 2013-2014 extension Very similar system to 20CRv2. Fixed Sea ice using COBE-SST2 sea ice. More

JointAcBviBes•  Concept:Commonissuescanbepresentinmorethanonereanalysis,ornewmethodsmakehelpproduceimprovedanalysis

•  AcBon:DeterminewhichcenterscanparBcipate.Developanexperimentalplanincludingcasestudiesand/oraddiBonaldiagnosBcoutput

•  Cost:DevelopingcentersincurcompuBngandBmetoevaluatetheexperiments

•  Benefit:Shouldprovidemoreunderstandingofthereanalysismethodthancouldbeaccomplishedalone

Page 10: Task Team for the Intercomparison of ReAnalyses (TIRA)€¦ · Spring 2016: 1851-2012, 2013-2014 extension Very similar system to 20CRv2. Fixed Sea ice using COBE-SST2 sea ice. More

DevelopingaReanalysisIntercomparisonProject

•  PerhapsmoreofacoordinaBngbody,thananactualproject

•  Couldhavemembershipthatincludesthedisciplinaryprojectsaswellasdevelopingcenters

•  MaintainandpromotebestpracBcesandpromotescommunicaBonofresults

•  SBllneedsdiscussion

Page 11: Task Team for the Intercomparison of ReAnalyses (TIRA)€¦ · Spring 2016: 1851-2012, 2013-2014 extension Very similar system to 20CRv2. Fixed Sea ice using COBE-SST2 sea ice. More

Examples of S-RIP Studies 1.  TropicalStratosphericPuzzle:

Quasi-BiennialOscillaBon(QBO)

2.  OzoneDepleBonandStratosphericMeteorology

3.  UpperTroposphere–LowerStratosphere(UTLS):JetsandtheirroleinClimate

4.  VolcanicErupBonandClimate

[Fujiwaraetal.,ACP,2017]

Inter-journalspecialissueon"TheSPARCReanalysisIntercomparisonProject(S-RIP)"inAtmosphericChemistryandPhysics(ACP)andEarthSystemScienceData(ESSD)-19papers

Page 12: Task Team for the Intercomparison of ReAnalyses (TIRA)€¦ · Spring 2016: 1851-2012, 2013-2014 extension Very similar system to 20CRv2. Fixed Sea ice using COBE-SST2 sea ice. More

Ocean Re-Analyses:Demonstrating the value of ocean observations

Objectives:

To quantify signal/noise from Ensemble

To gain insight into ocean variability and trends

To identify current system deficiencies

To measure progress

To exploit existing multi-ORA ensembleFor real-time ocean monitoringFor climate indicatorsFor model validationFor initialization of coupled models

ORA-IP: Ocean Reanalysis Intercomparison Project

ORAIP Special Issue in Climate Dynamics

ORAIP v1 data repositorywith version control

Real time Multi-ORA Monitoring

Create-IPConcept-heatEOS-Polar IntercomparisonCMEMS

Page 13: Task Team for the Intercomparison of ReAnalyses (TIRA)€¦ · Spring 2016: 1851-2012, 2013-2014 extension Very similar system to 20CRv2. Fixed Sea ice using COBE-SST2 sea ice. More

Upcoming New WRIT (Web-based Reanalysis Intercomparison Tools) from

NOAA ESRL/PSD WRITseasonalcorrela@ons(new)

WRITVer@calProfiles

AddfuncBonalitytoWRITBme-seriespage:• AddclimateandoceanindexBme-series.ForexamplePNA,NP,Nino3.4.

• Calculateindicesfromdifferentreanalysisdatasets• Allowlead/lag• AddaddiBonalstaBsBcaltechniquessuchasWaveletanalysis.

WRITTime-seriesandClimateIndices(soon)

WRITTime-sec@ons

PlotdifferentverBcalproducts:• VerBcalprofiles/Skew-T

• VerBcaltransects• Height-Time

SEUSFeb19-201884tornadooutbreak20CRV2c PlotDailymeans

oranomalies• Time/laBtudeorTime/longitude

US1000mbTafromR102-03/2018(tornadoes)

PNAcorrelaLonwith20CRV2cJan500Z

NHIceExtentforsummerlaggedcorrelaLonwithspring

HadISST1.1SST

AOcorrelaLonwithR1MarchTat283E

Page 14: Task Team for the Intercomparison of ReAnalyses (TIRA)€¦ · Spring 2016: 1851-2012, 2013-2014 extension Very similar system to 20CRv2. Fixed Sea ice using COBE-SST2 sea ice. More

BAMS paper on reanalysis service May2018issueoftheBulleLnoftheAmericanMeteorologySociety

•  DescribesrepackagingandconsistentdistribuBonoftheworld’smajoratmosphericandoceanicreanalyses.

•  PresentsexamplesoftheusefulnessofexaminingmulBplereanalyses.

•  EachreanalysisisupdatedasitbecomesavailableandaddedtotheEarthSystemGridFederaBon(ESGF).

•  Selecteddataisalsoavailableforsubseqng(TDS),visualizaBon(CREATE-V)andserversideanalyBcs(EDAS).

Page 15: Task Team for the Intercomparison of ReAnalyses (TIRA)€¦ · Spring 2016: 1851-2012, 2013-2014 extension Very similar system to 20CRv2. Fixed Sea ice using COBE-SST2 sea ice. More

NASA NCCS’s CREATE-V provides quick look reanalysis comparison capability

•  FormulBplereanalysesquicklookvisualizaBonandcomparison.

•  IncludesbothatmosphericandoceanreanalysesaswellasensemblemeansandstandarddeviaBons.

• OpBonstoselectdate,level,colormap,andscale.

Precipitablewaterfor4reanalyses,themulBplereanalysisensembleaverageandstandarddeviaBon.

Page 16: Task Team for the Intercomparison of ReAnalyses (TIRA)€¦ · Spring 2016: 1851-2012, 2013-2014 extension Very similar system to 20CRv2. Fixed Sea ice using COBE-SST2 sea ice. More

Multiple Reanalysis Ensemble (MRE) and Earth Data Analytics Service (EDAS)

•  NASANCCSCREATEserviceproducedamulBplereanalysisensemble(MRE)ofselectedvariables.Theregriddeddata,theensemblemeanandtheensemblestandarddeviaBonareallpublishedontheEarthSystemGridFederaBon.

•  EDASisaserversideanalyBcsservicethatprovidesexternaluserstheabilitytoruncomputaBonssuchasmin,max,sum,average,anomalyontheCREATE-IPreanalysisdata,includingtheMRE,withoutdownloadingthedata. AnnualaveragedGPCP

precipitaBoncomparisonwiththeMRE.

JupyterNotebookexampleusingremotehighperformancecompuBngtoanalyzereanalysisdata.

Page 17: Task Team for the Intercomparison of ReAnalyses (TIRA)€¦ · Spring 2016: 1851-2012, 2013-2014 extension Very similar system to 20CRv2. Fixed Sea ice using COBE-SST2 sea ice. More

AtmosphericReanalysisPlans•  RecentContribuBons

–  JMA– NASAGMAO– ERA– NCEP– CMA

Page 18: Task Team for the Intercomparison of ReAnalyses (TIRA)€¦ · Spring 2016: 1851-2012, 2013-2014 extension Very similar system to 20CRv2. Fixed Sea ice using COBE-SST2 sea ice. More

JRA-55family•  Having a deeper understanding of model biases and impact of changing observing

systemsisimportantforevaluaBngandimprovingtemporalconsistencyofreanalysis.•  To this end, different typesof producthavebeenproducedwith the commonNWP

system.•  JRA-55(JMA)

–  Fullobservingsystemreanalysis–  AvailablefromJMA,DIAS,NCAR,ESGF–  PosterbyY.Harada(SecBon4onWed.)

•  JRA-55C(MRI/JMA)–  UsingconvenBonalobservaBonsonly–  AvailablefromDIAS,NCAR–  PosterbyC.Kobayashi(SecBon4onWed.)

•  JRA-55AMIP(MRI/JMA)–  AMIP-typesimulaBon–  AvailablefromDIAS,NCAR

AdaptedandupdatedfromC.Kobayashi(2014)

RMS errors of 2-day forecasts ofgeopotenLal height (gpm) at 500hPaaveragedoverthenorthernhemisphere

Page 19: Task Team for the Intercomparison of ReAnalyses (TIRA)€¦ · Spring 2016: 1851-2012, 2013-2014 extension Very similar system to 20CRv2. Fixed Sea ice using COBE-SST2 sea ice. More

JapaneseReanalysisforThreeQuartersofaCentury(JRA-3Q)

•  Reanalysisperiod:1947topresent•  ProvisionalspecificaBons

–  ResoluBon:55km,60layers(JRA-55)->40km,100layers(JRA-3Q)–  IncorporaBngmanyimprovementsfromtheoperaBonalNWPsystem

•  Overallupgradeofphysicalprocesses•  NewtypesofobservaBon(ground-basedGNSS,hyperspectralsounders)

–  ImprovedSST:COBE-SST2(1-deg,upto1985)&MGDSST(0.25deg,from1985onward)

–  ImprovedobservaBons•  ObservaBonsnewlyrescuedanddigiBsedbyERA-CLIMandotherprojects•  ImprovedsatelliteobservaBonsthroughreprocessing•  JMA’sowntropicalcyclonebogusdata

•  ProducBonschedule–  Q12019:startproducBon–  Q12021:completeproducBonforthe1991–2020normalperiod–  Q12022:completeproducBonforthewholeperiod

Page 20: Task Team for the Intercomparison of ReAnalyses (TIRA)€¦ · Spring 2016: 1851-2012, 2013-2014 extension Very similar system to 20CRv2. Fixed Sea ice using COBE-SST2 sea ice. More

Surfacenetenergyflux(January2016)

•  JRA-55hasabiasof-11.8Wm-2(Kobayashietal.2015).

•  ThisbiasisalmosthalvedinJRA-3QExp.

JRA-3QExp JRA-55

August2015 -12.0 -16.5

January2016 4.6 -3.6

Globalmeannetflux(Wm-2)

Page 21: Task Team for the Intercomparison of ReAnalyses (TIRA)€¦ · Spring 2016: 1851-2012, 2013-2014 extension Very similar system to 20CRv2. Fixed Sea ice using COBE-SST2 sea ice. More

21Global Modeling and Assimilation Officegmao.gsfc.nasa.govGMAO

National Aeronautics and Space Administration

3

2000 2010 2020

Ocean

MERRA1979-2016

Atmosphere includes aerosol analysis

Composition

Enhancements downscale to 12-km

Biogeochemical ocean state, biology, carbon fluxes

Planned

GMAO reanalyses and derivative products

MERRA-21980-Present

MERRA-Ocean1993-Present

MERRA-Land1979-2016

MERRA2-R12K2002-2015

MERRA-Aero2002-2015

MERRA-NOBM1998-2015

Atmosphere...including aerosol

and land

...plus Oceanincluding waves and

sea ice

MERRA2-Chem2004-Present

MERRA2-Ocean1980-Present

M2AMIP

Page 22: Task Team for the Intercomparison of ReAnalyses (TIRA)€¦ · Spring 2016: 1851-2012, 2013-2014 extension Very similar system to 20CRv2. Fixed Sea ice using COBE-SST2 sea ice. More

Global Modeling and Assimilation Office gmao.gsfc.nasa.gov GMAO

National Aeronautics and Space Administration

GMAOcoupledatmosphere-oceanassimilaBondevelopment

22

S2S v2 MOM5 0.5o L40

CICE UMD LETKF

GEOS ADAS 4D-EnVar 12-km L72 Aerosols

AO Skin SST

S2S v3 MOM5 0.25o L50 Catchment-CN

Salinity Sea Ice Thickness

Seasonal Prediction System

Atmospheric DAS

Atmosphere-Ocean Coupled DAS

GEOS ADAS Update LSM, Convection,

Radiation

GEOS AODAS MOM6

New CICE GSI O-LETKF

MERRA-2 Ocean

Next Reanalysis S2S Prediction

NWP

GEOS ADAS Update Microphysics

9-km L132 Nonhydrostatic

May 2018

May 2019

Oct 2017

Jan 2019

Jan 2017

Jan 2021

Page 23: Task Team for the Intercomparison of ReAnalyses (TIRA)€¦ · Spring 2016: 1851-2012, 2013-2014 extension Very similar system to 20CRv2. Fixed Sea ice using COBE-SST2 sea ice. More

Global Modeling and Assimilation Office gmao.gsfc.nasa.gov GMAO

National Aeronautics and Space Administration

23

HAQIshownherecombinesO3,NO2andPM2.5

Page 24: Task Team for the Intercomparison of ReAnalyses (TIRA)€¦ · Spring 2016: 1851-2012, 2013-2014 extension Very similar system to 20CRv2. Fixed Sea ice using COBE-SST2 sea ice. More

ERA5: the ERA-Interim replacement ERA-Interim ERA5

Period 1979 - present Initially 1979 – present, later addition 1950-1978

Start of production August 2006 2016, 1979-NRT early 2018

Assimilation system 2006, 4D-Var 2016 ECMWF model cycle, 4D-Var

Model input (radiation and surface)

As in operations, (inconsistent sea surface temperature)

Appropriate for climate, e.g., evolution greenhouse gases, volcanic eruptions, sea surface temperature and sea ice

Spatial resolution 79 km globally 60 levels to 10 Pa

31 km globally 137 levels to 1 Pa

Uncertainty estimate Based on a 10-member 4D-Var ensemble at 62 km

Land Component 79km 9km

Output frequency 6-hourly Analysis fields Hourly (three-hourly for the ensemble), Extended list of parameters ~ 5 Peta Byte

Extra Observations Mostly ERA-40, GTS Various reprocessed CDRs, latest instruments

Variational Bias correction Satellite radiances Also ozone, aircraft, surface pressure

What is new in ERA5?

Page 25: Task Team for the Intercomparison of ReAnalyses (TIRA)€¦ · Spring 2016: 1851-2012, 2013-2014 extension Very similar system to 20CRv2. Fixed Sea ice using COBE-SST2 sea ice. More

Coupled Model

Ensemble Forecast

NEMS

OCE

AN

SEA-ICE

WAV

E

LAND

AERO

ATMOS

Ensemble Analysis (N Members)

OUTPUT

Coupled Ensemble Forecast (N members)

INPUT

Coupled Model

Ensemble Forecast

NEMS

OCEAN

SEA-ICE

WAVE

LAND

AERO

ATMOS

NCEP Coupled Hybrid Data Assimilation and Forecast System Saha et al.

Page 26: Task Team for the Intercomparison of ReAnalyses (TIRA)€¦ · Spring 2016: 1851-2012, 2013-2014 extension Very similar system to 20CRv2. Fixed Sea ice using COBE-SST2 sea ice. More

Historical Reanalysis Status and Plans 20th Century Reanalysis Project http://go.usa.gov/XTd

•  Fall 2014: 1871-2012 (includes time-varying CO2, volcanic aerosols, GFS from NCEP). Ensemble mean and spread and individual member variables online now.

–  http://www.esrl.noaa.gov/psd/data/gridded/data.20thC_ReanV2.html (NOAA ESRL)

–  http://dss.ucar.edu/datasets/ds131.1 (NCAR)

–  http://portal.nersc.gov/20C_Reanalysis Every member (US Dept of Energy, NERSC)

–  NERSC High Performance Storage System Tape Gateway Every member –  Earth System Grid Federation ana4MIPS distribution and validation for IPCC AR5

–  British Atmospheric Data Center (BADC)

20CR v2c http://go.usa.gov/XTd Ensemble mean and spread and 3D individual member variables online now.

Spring 2016: 1851-2012, 2013-2014 extension

Very similar system to 20CRv2. Fixed Sea ice using COBE-SST2 sea ice. More observations, ensemble of SODAsi.2 SST (1851-2012), Reynolds et al. SST (2013-2014). - distribution via: ESRL, NCAR, NERSC Every member

20CR version 3 Winter 2017: 1851-2015,additional tests for 1815-1850

Higher resolution, improved algorithm and observational quality control Coordinate with ERA-CLIM2, SOUSEI, GFDL - Test possible BCs: HadISST2.1, COBE-SST2, SODAsi.3

Page 27: Task Team for the Intercomparison of ReAnalyses (TIRA)€¦ · Spring 2016: 1851-2012, 2013-2014 extension Very similar system to 20CRv2. Fixed Sea ice using COBE-SST2 sea ice. More

Goal of CMA 40-year Global Reanalysis (CRA-40)

Produce 40-year datasets (1979-2018): –Ingested observations –Reanalysis datasets: CMA Reanalysis (~30km, 6 hourly) –Obs. feedback datasets:departure from analysis & 6h forecast –Reanalysis uncertainty:from EnKF ensembles Will become an operational system: CMA Re-Analysis System- CRAS –Continuously running in near real time for climate monitoring

Page 28: Task Team for the Intercomparison of ReAnalyses (TIRA)€¦ · Spring 2016: 1851-2012, 2013-2014 extension Very similar system to 20CRv2. Fixed Sea ice using COBE-SST2 sea ice. More

Summary•  ReanalysisDataDevelopmentissBllgoingstrong-EarthSystemcouplingplansaremovingforward– MoreimportantthaneverforuserstounderstandthereanalysismethodologyandfoundaBons

•  Toolsanddataaccessaregrowingandimproving– UserssBllneedguidanceonstrengthsandweaknesses

•  TIRApilotprojectsaremovingforwardandwillcontributetoaplanforthestructureofageneralintercomparisonprojectforreanalyses

Page 29: Task Team for the Intercomparison of ReAnalyses (TIRA)€¦ · Spring 2016: 1851-2012, 2013-2014 extension Very similar system to 20CRv2. Fixed Sea ice using COBE-SST2 sea ice. More

Example:Clausius-Clapyeron

•  UsingTLTandTPW,MERRA-2showsaweakerC-CrelaBonshipcomparedtoRSSobsandAMIPsimulaBon

•  AnalysisincrementcounterssomelocalevaporaBveincreases

•  OtherreanalysesalsoshowaweakC-CrelaBonship

•  Bosilovichetal.(2016,JClim);Schröderetal.(2016,JAMC)

Page 30: Task Team for the Intercomparison of ReAnalyses (TIRA)€¦ · Spring 2016: 1851-2012, 2013-2014 extension Very similar system to 20CRv2. Fixed Sea ice using COBE-SST2 sea ice. More

OceanAnomalies:TPW,EvaporaBonandAnalysisIncrement

•  TPWdoesrespondtoSST(e.g.apparentENSOsignal)

•  E-Pisincreasingovertheperiod,generallyinresponsetoSST,butalsovariesaccordingtowind.

•  IncrementisalwaysnegaBve,anddecreasesinBme–counteringamodelwetbias

•  InMERRA-2,itappearstheAnalysisisdampingC-C

MERRA-2 Ocean Anomalies (60S,60N)E-P [0.63] TPW [2.89]ANA [-0.10]

Page 31: Task Team for the Intercomparison of ReAnalyses (TIRA)€¦ · Spring 2016: 1851-2012, 2013-2014 extension Very similar system to 20CRv2. Fixed Sea ice using COBE-SST2 sea ice. More

ExtensiontoOtherSystemsusingT850asaProxy

•  TrendsareK/decand%/decade;MERRAandCFSRwithheld

System T Q dT/dt dQ/dt%/K

Detrend%/K Trend

%/K S(Q)/S(T) Corr(T,Q)

OBS TLT TPW 0.10 1.03 4.6 5.4 6.2 0.90MERRA2 TLT TPW 0.11 0.15 3.2 2.9 3.7 0.78M2AMIP TLT TPW 0.28 1.53 4.5 5.0 7.1 0.97MERRA2 T850 TPW 0.20 0.15 4.0 2.3 5.3 0.63M2AMIP T850 TPW 0.24 1.53 6.0 6.2 3.7 0.97ERAI T850 TPW 0.05 0.23 4.3 4.3 10.9 0.58JRA55 T850 TPW 0.12 0.30 4.7 4.0 6.4 0.7120CR T850 TPW 0.13 0.84 6.8 6.7 6.4 0.95ERA20C T850 TPW 0.27 1.42 7.1 5.9 7.2 0.94ERA20CM T850 TPW 0.22 1.38 7.0 6.5 5.7 0.98

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NextSteps•  Needfurthervariablestotestreanalyses(TLT,ANA)morecompletely–  Ifnotaresultofanalysisincrementinotherreanalyses,thenwhatholdsbacktheC-CrelaBonship?

•  TestsatellitereanalysesremovingwatervaporassimilaBon(likelytooexpensiveformostorallcenterstoconsider)