| CMIP6 name | CMIP6 description | E3SM variable(s) | conversion formula | CMOR handler complete | conversion formula verified by | Notes | Data checked | |
|---|---|---|---|---|---|---|---|---|
| 1 | tas | Near-Surface Air Temperature | TREFHT | tas = TREFHT | yes | J.Zhang | ||
| 2 | ts | Surface Temperature | TS | ts = TS | yes | J.Zhang | ||
| 3 | psl | Sea Level Pressure | PSL | psl = PSL | yes | J.Zhang | ||
| 4 | ps | Surface Air Pressure | PS | ps = PS | yes | J.Zhang | ||
| 5 | sfcWind | Near-Surface Wind Speed | U10 | sfcWind = U10 | yes | J.Zhang | ||
| 6 | huss | Near-Surface Specific Humidity | QREFHT | huss = QREFHT | yes | J.Zhang | ||
| 7 | pr | Precipitation | PRECC , PRECL | pr = (PRECC + PRECL) * 1000.0 | yes | J.Zhang | ||
| 8 | prc | Convective Precipitation | PRECC | prc = PRECC * 1000.0 | yes | J.Zhang | ||
| 9 | prsn | Snowfall Flux | PRECSC, PRECSL | prsn = (PRECSC + PRECSL) * 1000.0 | yes | J.Zhang | ||
| 10 | evspsbl | Evaporation Including Sublimation and Transpiration | QFLX | evspsbl = QFLX | yes | J.Zhang | ||
| 11 | tauu | Surface Downward Eastward Wind Stress | TAUX | tauu = -TAUX | yes | J.Zhang | Note, 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. | |
| 12 | tauv | Surface Downward Northward Wind Stress | TAUY | tauv =- TAUY | yes | J.Zhang | Same as above | |
| 13 | hfls | Surface Upward Latent Heat Flux | LHFLX | hfls = LHFLX | yes | J.Zhang | ||
| 14 | clt | Total Cloud Cover Percentage | CLDTOT | clt = CLDTOT * 100.0 | yes | Chris Golaz | ||
| 15 | rlds | Surface Downwelling Longwave Radiation | FLDS | rlds = FLDS | yes | J.Zhang | ||
| 16 | rlus | Surface Upwelling Longwave Radiation | FLDS, FLNS | rlus = FLDS + FLNS | yes | J.Zhang | ||
| 17 | rsds | Surface Downwelling Shortwave Radiation | FSDS | rsds = FSDS | yes | J.Zhang | ||
| 18 | rsus | Surface Upwelling Shortwave Radiation | FSDS, FSNS | rsus = FSDS - FSNS | yes | J.Zhang | ||
| 19 | hfss | Surface Upward Sensible Heat Flux | SHFLX | hfss = SHFLX | yes | J.Zhang | ||
| 20 | cl | Percentage Cloud Cover | CLOUD | cl = CLOUD *100.0 | Chris Golaz | on model levels | ||
| 21 | cli | Mass Fraction of Cloud Ice | CLDICE | cli = CLDICE | on model levels For consistency with clivi, don't include snow in cli. | |||
| 22 | clivi | Ice Water Path | TGCLDIWP | clivi = TGCLDIWP | yes | TGCLDIWP doesn't include snow water path. | ||
| 23 | clw | Mass Fraction of Cloud Liquid Water | CLDLIQ | clw = CLDLIQ | on model levels For consistency with clwvi, don't include rain in clw. | |||
| 24 | clwvi | Condensed Water Path | TGCLDCWP | clwvi = TGCLDCWP | yes | TGCLDCWP doesn't include rain and snow water path. | ||
| 25 | hur | Relative Humidity | RELHUM | hur = RELUM | Chris Golaz | interpolated to 19 pressure levels | ||
| 26 | ||||||||
| 27 | hus | Specific Humidity | Q | hus = Q | Chris Golaz | interpolated to 19 pressure levels | ||
| 28 | ||||||||
| 29 | o3 | Mole Fraction of O3 | O3 | o3 = O3 | interpolated to 19 pressure levels. Philip Cameron-Smith (Unlicensed): Yes, the E3SM variable O3 is what is wanted here. However, it would be good to note somehow that "Stratospheric ozone is prognostic, and tropospheric ozone follows the input4mips prescribed concentrations." | |||
| 30 | pfull | Pressure at Model Full-Levels | P0, PS, hyam, hybm | pfull = P0*hyam + PS*hybm | Chris Golaz | |||
| 31 | phalf | Pressure on Model Half-Levels | P0, PS, hyai, hybi | phalf = P0*hyai + PS*hybi | Chris Golaz | |||
| 32 | prw | Water Vapor Path | TMQ | prw = TMQ | Chris Golaz | |||
| 33 | rldscs | Surface Downwelling Clear-Sky Longwave Radiation | FLDS, FLNS, FLNSC | rldscs = FLDS + FLNS - FLNSC | yes | Chris Golaz | ||
| 34 | rlut | TOA Outgoing Longwave Radiation | FSNTOA, FSNT, FLNT | rlut = FSNTOA - FSNT + FLNT | yes | 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 | ||
| 35 | rlutcs | TOA Outgoing Clear-Sky Longwave Radiation | FLUTC | rlutcs = FLUTC | yes | Slight approximation here since we are using TOM, but NCAR does the same. | ||
| 36 | rsdscs | Surface Downwelling Clear-Sky Shortwave Radiation | FSDSC | rsdscs = FSDSC | yes | Chris Golaz | ||
| 37 | rsdt | TOA Incident Shortwave Radiation | SOLIN | rsdt = SOLIN | yes | Chris Golaz | ||
| 38 | rsuscs | Surface Upwelling Clear-Sky Shortwave Radiation | FSDSC, FSNSC | rsuscs = FSDSC - FSNSC | yes | Chris Golaz | ||
| 39 | rsut | TOA Outgoing Shortwave Radiation | FSUTOA | rsut = FSUTOA | yes | Chris Golaz | ||
| 40 | rsutcs | TOA Outgoing Clear-Sky Shortwave Radiation | FSUTOAC | rsutcs = FSUTOAC | yes | Chris Golaz | ||
| 41 | rtmt | Net Downward Radiative Flux at Top of Model | FSNT, FLNT | rtmt = FSNT - FLNT | yes | Chris Golaz | ||
| 42 | ta | Air Temperature | T | ta = T | Chris Golaz | interpolated to 19 pressure levels | ||
| 43 | J. Zhang | 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. double checked that TREFHTMX and TREFHTMN saved to h1 have the same values as TREFHT. Checked code in cam_diagnostics.F90, TREFMNAV and TREFMXAV should be the correct field to output. Unfortunately, those high frequency data saved are not useful | ||||||
| 44 | J. Zhang | Same as above | ||||||
| 45 | ua | Eastward Wind | U | ua = U | Chris Golaz | interpolated to 19 pressure levels | ||
| 46 | ||||||||
| 47 | va | Northward Wind | V | va = V | Chris Golaz | interpolated to 19 pressure levels | ||
| 48 | ||||||||
| 49 | wap | Omega (=dp/dt) | OMEGA | wap = OMEGA | Chris Golaz | interpolated to 19 pressure levels | ||
| 50 | zg | Geopotential Height | Z3 | zg = Z3 | Chris Golaz | interpolated to 19 pressure levels | ||
| AERmon | ||||||||
| 51 | abs550aer | Ambient Aerosol Absorption Optical Thickness at 550nm | AODABS | abs550aer = AODABS | J. Zhang | |||
| 52 | od550aer | Ambient Aerosol Optical Thickness at 550nm | AODVIS | od550aer = AODVIS | J. Zhang | |||
| 53 | reffclwtop | Cloud-Top Effective Droplet Radius | AREL | reffclwtop = AREL | J. Zhang |
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