Skip to end of metadata
Go to start of metadata

You are viewing an old version of this page. View the current version.

Compare with Current View Page History

« Previous Version 3 Next »



CMIP6 nameCMIP6 descriptionE3SM variable(s)conversion formulaCMOR handler completeconversion formula verified byNotes
1tasNear-Surface Air TemperatureTREFHTtas = TREFHTyesJ.Zhang
2tsSurface TemperatureTSts = TSyesJ.Zhang
3pslSea Level PressurePSLpsl = PSLyesJ.Zhang
4psSurface Air PressurePSps = PSyesJ.Zhang
5sfcWindNear-Surface Wind SpeedU10sfcWind = U10yesJ.Zhang
6hussNear-Surface Specific HumidityQREFHThuss = QREFHTyesJ.Zhang
7prPrecipitationPRECC PRECLpr = (PRECC  + PRECL) * 1000.0yesJ.Zhang
8prcConvective PrecipitationPRECCprc = PRECC * 1000.0
J.Zhang
9prsnSnowfall FluxPRECSC, PRECSLprsn = (PRECSC + PRECSL) * 1000.0yesJ.Zhang
10evspsblEvaporation Including Sublimation and TranspirationQFLXevspsbl = QFLXyesJ.Zhang
11tauuSurface Downward Eastward Wind StressTAUXtauu = -TAUXyesJ.ZhangNote, I was analyzing this variable from e3sm output. It turns out that TAUX(Y) is surface stress, which is in opposite direction to tauu(v) (wind stress). This was not caught in CAM's conversion table.
12tauvSurface Downward Northward Wind StressTAUYtauv =- TAUYyesJ.ZhangSame as above
13hflsSurface Upward Latent Heat FluxLHFLXhfls = LHFLXyesJ.Zhang
14cltTotal Cloud Cover PercentageCLDTOTclt = CLDTOT * 100.0
yesChris Golaz
15rldsSurface Downwelling Longwave RadiationFLDSrlds = FLDSyes

J.Zhang

Chris Golaz


16rlusSurface Upwelling Longwave RadiationFLDS, FLNSrlus = FLDS + FLNSyes

J.Zhang

Chris Golaz


17rsdsSurface Downwelling Shortwave RadiationFSDSrsds = FSDSyes

J.Zhang

Chris Golaz


18rsusSurface Upwelling Shortwave RadiationFSDS, FSNSrsus = FSDS - FSNSyes

J.Zhang

Chris Golaz


19hfssSurface Upward Sensible Heat FluxSHFLXhfss = SHFLXyesJ.Zhang
20clPercentage Cloud CoverCLOUDcl = CLOUD *100.0
Chris Golazon model levels
21cliMass Fraction of Cloud IceCLDICEcli = CLDICE

on model levels


For consistency with clivi, don't include snow in cli.

22cliviIce Water PathTGCLDIWPclivi = TGCLDIWP

Kai Zhang


TGCLDIWP doesn't include snow water path.
23clwMass Fraction of Cloud Liquid WaterCLDLIQclw = CLDLIQ

Kai Zhang

on model levels


For consistency with clwvi, don't include rain in clw. 

24clwviCondensed Water PathTGCLDCWPclwvi = TGCLDCWP

Kai Zhang

TGCLDCWP doesn't include rain and snow water path.
25hurRelative HumidityRELHUMhur = RELUM
Chris Golazinterpolated to 19 pressure levels
26hursNear-Surface Relative HumidityRHREFHThurs = RHREFHT


27husSpecific HumidityQhus = Q
Chris Golazinterpolated to 19 pressure levels
28mcConvective Mass Flux




29o3Mole Fraction of O3O3o3 = O3Need input from Philip Cameron-Smith (Unlicensed)
interpolated to 19 pressure levels
30pfullPressure at Model Full-LevelsP0, PS, hyam, hybmpfull = P0*hyam + PS*hybm
Chris Golaz
31phalfPressure on Model Half-LevelsP0, PS, hyai, hybiphalf = P0*hyai + PS*hybi
Chris Golaz
32prwWater Vapor PathTMQprw = TMQ
Chris Golaz
33rldscsSurface Downwelling Clear-Sky Longwave RadiationFLDS, FLNS, FLNSC
rldscs = FLDS + FLNS - FLNSC
Chris Golaz
34rlutTOA Outgoing Longwave RadiationFSNTOA, FSNT, FLNT

rlut = FSNTOA - FSNT + FLNT


Chris Golaz

Equation originally from NCAR. Using this ensures that individual TOA terms (SW, LW, up/down) are consistent with TOM net flux (rtmt):

rtmt = rsdt - rsut - rlut

35rlutcsTOA Outgoing Clear-Sky Longwave RadiationFLUTCrlutcs = FLUTC

 Chris Golaz

Slight approximation here since we are using TOM, but NCAR does the same.
36rsdscsSurface Downwelling Clear-Sky Shortwave RadiationFSDSCrsdscs = FSDSC
Chris Golaz
37rsdtTOA Incident Shortwave RadiationSOLINrsdt = SOLIN
Chris Golaz
38rsuscsSurface Upwelling Clear-Sky Shortwave RadiationFSDSC, FSNSCrsuscs = FSDSC - FSNSC
Chris Golaz
39rsutTOA Outgoing Shortwave RadiationFSUTOArsut = FSUTOA
Chris Golaz
40rsutcsTOA Outgoing Clear-Sky Shortwave RadiationFSUTOACrsutcs = FSUTOAC
Chris Golaz
41rtmtNet Downward Radiative Flux at Top of ModelFSNT, FLNTrtmt = FSNT - FLNT
Chris Golaz
42taAir TemperatureTta = T
Chris Golazinterpolated to 19 pressure levels
43tasmaxDaily Maximum Near-Surface Air TemperatureTREFHTMX


We cannot use monthly h0 output for this. But the necessary data is in daily h1 files. We would have to create time series of monthly averages from these daily files.
44tasminDaily Minimum Near-Surface Air TemperatureTREFHTMN


Same as above
45uaEastward WindUua = U
Chris Golazinterpolated to 19 pressure levels
46uasEastward Near-Surface Wind




47vaNorthward WindVva = V
Chris Golazinterpolated to 19 pressure levels
48vasNorthward Near-Surface Wind




49wapOmega (=dp/dt)OMEGAwap = OMEGA
Chris Golazinterpolated to 19 pressure levels
50zgGeopotential HeightZ3zg = Z3
Chris Golazinterpolated to 19 pressure levels

AERmon
51abs550aerAmbient Aerosol Absorption Optical Thickness at 550nmAODABSabs550aer = AODABS


52od550aerAmbient Aerosol Optical Thickness at 550nmAODVISod550aer = AODVIS


53reffclwtopCloud-Top Effective Droplet RadiusARELreffclwtop = AREL


  • No labels