CMIP6 name | CMIP6 description | E3SM variable(s) | conversion formula | CMOR handler complete | conversion formula verified by | Notes | ||
---|---|---|---|---|---|---|---|---|
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 | 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 | ||
12 | tauv | Surface Downward Northward Wind Stress | TAUY | tauv = TAUY | yes | J.Zhang | ||
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 | Kai ZhangNote: for | on model levels For consistency with clivi, don't include snow in cli. | on model levels | |
22 | clivi | Ice Water Path | TGCLDIWP | clivi = TGCLDIWP | Kai ZhangNote: TGCLDIWP | TGCLDIWP doesn't include snow water path. | ||
23 | clw | Mass Fraction of Cloud Liquid Water | CLDLIQ | clw = CLDLIQ | Kai ZhangNote: for | on model levels For consistency with clwvi, don't include rain in clw. | on model levels | |
24 | clwvi | Condensed Water Path | TGCLDCWP | clwvi = TGCLDCWP | Kai ZhangNote: TGCLDCWP | 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 | Need input from Philip Cameron-Smith (Unlicensed) | interpolated to 19 pressure levels | ||
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 | Chris Golaz | |||
34 | rlut | TOA Outgoing Longwave Radiation | FSNTOA, FSNT, FLNT | rlut = FSNTOA - FSNT + FLNT | 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 | Slight approximation here since we are using TOM, but NCAR does the same. | |||
36 | rsdscs | Surface Downwelling Clear-Sky Shortwave Radiation | FSDSC | rsdscs = FSDSC | Chris Golaz | |||
37 | rsdt | TOA Incident Shortwave Radiation | SOLIN | rsdt = SOLIN | Chris Golaz | |||
38 | rsuscs | Surface Upwelling Clear-Sky Shortwave Radiation | FSDSC, FSNSC | rsuscs = FSDSC - FSNSC | Chris Golaz | |||
39 | rsut | TOA Outgoing Shortwave Radiation | FSUTOA | rsut = FSUTOA | Chris Golaz | |||
40 | rsutcs | TOA Outgoing Clear-Sky Shortwave Radiation | FSUTOAC | rsutcs = FSUTOAC | Chris Golaz | |||
41 | rtmt | Net Downward Radiative Flux at Top of Model | FSNT, FLNT | rtmt = FSNT - FLNT | Chris Golaz | |||
42 | ta | Air Temperature | T | ta = T | Chris Golaz | interpolated to 19 pressure levels | ||
43 | tasmax | Daily Maximum Near-Surface Air Temperature | TREFHTMX | 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. | ||||
44 | tasmin | Daily Minimum Near-Surface Air Temperature | TREFHTMN | 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 | ||||
52 | od550aer | Ambient Aerosol Optical Thickness at 550nm | AODVIS | od550aer = AODVIS | ||||
53 | reffclwtop | Cloud-Top Effective Droplet Radius | AREL | reffclwtop = AREL |
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