A 5 year sample of the CMIP6 ocean data has been setup on NERSC under /global/homes/s/sbaldwin/scratch/cmip_sample/CMIP6/CMIP/E3SM-Project/E3SM-1-0/piControl/r1i1p1f1/
on acme1 at /p/user_pub/work/E3SM/cmip6_variables/piControl/CMIP6
the individual variable handlers at https://github.com/E3SM-Project/e3sm_to_cmip/tree/master/e3sm_to_cmip/cmor_handlers/<VARIABLE_NAME>
CMIP6 name | CMIP6 description | CF standard name | E3SM variable(s) | conversion formula | CMOR handler complete | Conversion Formula Verified by Scientist | Notes | Scientist Assigned to Perform Final Quality Control on CMORized files | Date Verified | Data & Metadata Correct (yes/no) | Notes if CMORized files are not correct | check on v20190710 Data correct(yes/no) | |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 1 | tas | Near-Surface Air Temperature | air_temperature | TREFHT | tas = TREFHT | yes | J.Zhang | yes | |||||
| 2 | ts | Surface Temperature | TS | ts = TS | yes | J.Zhang | yes | ||||||
| 3 | psl | Sea Level Pressure | air_pressure_at_sea_level | PSL | psl = PSL | yes | J.Zhang | yes | |||||
| 4 | ps | Surface Air Pressure | PS | ps = PS | yes | J.Zhang | yes | ||||||
| 5 | sfcWind | Near-Surface Wind Speed | U10 | sfcWind = U10 | yes | J.Zhang | yes | ||||||
| 6 | huss | Near-Surface Specific Humidity | specific_humidity | QREFHT | huss = QREFHT | yes | J.Zhang | J.Zhang |
| yes | fixed | yes | |
| 7 | pr | Precipitation | precipitation_flux | PRECC , PRECL | pr = (PRECC + PRECL) * 1000.0 | yes | J.Zhang | J.Zhang |
| yes | fixed | yes | |
| 8 | prc | Convective Precipitation | convective_precipitation_flux | PRECC | prc = PRECC * 1000.0 | yes | J.Zhang | yes | |||||
| 9 | prsn | Snowfall Flux | snowfall_flux | PRECSC, PRECSL | prsn = (PRECSC + PRECSL) * 1000.0 | yes | J.Zhang | yes | |||||
| 10 | evspsbl | Evaporation Including Sublimation and Transpiration | QFLX | evspsbl = QFLX | yes | J.Zhang | yes | ||||||
| 11 | tauu | Surface Downward Eastward Wind Stress | surface_downward_eastward_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. | yes | ||||
| 12 | tauv | Surface Downward Northward Wind Stress | surface_downward_northward_stress | TAUY | tauv =- TAUY | yes | J.Zhang | Same as above | yes | ||||
| 13 | hfls | Surface Upward Latent Heat Flux | LHFLX | hfls = LHFLX | yes | J.Zhang | yes | ||||||
| 14 | clt | Total Cloud Cover Percentage | CLDTOT | clt = CLDTOT * 100.0 | yes | yes | |||||||
| 15 | rlds | Surface Downwelling Longwave Radiation | surface_downwelling_longwave_flux_in_air | FLDS | rlds = FLDS | yes | J.Zhang | yes | |||||
| 16 | rlus | Surface Upwelling Longwave Radiation | surface_upwelling_longwave_flux_in_air | FLDS, FLNS | rlus = FLDS + FLNS | yes | J.Zhang | J.Zhang |
| yes | fixed | yes | |
| 17 | rsds | Surface Downwelling Shortwave Radiation | surface_downwelling_shortwave_flux_in_air | FSDS | rsds = FSDS | yes | J.Zhang | yes (corrected direction ) | |||||
| 18 | rsus | Surface Upwelling Shortwave Radiation | surface_upwelling_shortwave_flux_in_air | FSDS, FSNS | rsus = FSDS - FSNS | yes | J.Zhang | yes | |||||
| 19 | hfss | Surface Upward Sensible Heat Flux | surface_upward_sensible_heat_flux | SHFLX | hfss = SHFLX | yes | J.Zhang | yes | |||||
| 20 | cl | Percentage Cloud Cover | CLOUD | cl = CLOUD *100.0 | on model levels | yes | |||||||
| 21 | cli | Mass Fraction of Cloud Ice | CLDICE | cli = CLDICE | on model levels For consistency with clivi, don't include snow in cli. | yes | |||||||
| 22 | clivi | Ice Water Path | atmosphere_cloud_ice_content | TGCLDIWP | clivi = TGCLDIWP | yes | TGCLDIWP doesn't include snow water path. | yes | |||||
| 23 | clw | Mass Fraction of Cloud Liquid Water | CLDLIQ | clw = CLDLIQ | on model levels For consistency with clwvi, don't include rain in clw. | yes | |||||||
| 24 | clwvi | Condensed Water Path | atmosphere_cloud_condensed_water_content | clwvi = TGCLDCWP | yes | TGCLDCWP doesn't include rain and snow water path. | yes | ||||||
| 25 | hur | Relative Humidity | RELHUM | hur = RELHUM | interpolated to 19 pressure levels | J.Zhang |
| yes | fixed | yes | |||
| 26 | hus | Specific Humidity | Q | hus = Q | interpolated to 19 pressure levels | yes | |||||||
| 27 |
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| 28 | 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." | yes | |||||||
| 29 | pfull | Pressure at Model Full-Levels | P0, PS, hyam, hybm | pfull = P0*hyam + PS*hybm | J.Zhang |
| yes | fixed | yes(pfull is monthly data instead of climotology according to our formula. cmor asks for climatology but it is not clear years to average over. It is safer to have monthly data and consistent with other Amon variables ) | ||||
| 30 | phalf | Pressure on Model Half-Levels | P0, PS, hyai, hybi | phalf = P0*hyai + PS*hybi | J.Zhang |
| yes | fixed | yes(same as above) | ||||
| 31 | prw | Water Vapor Path | TMQ | prw = TMQ | yes | ||||||||
| 32 | rldscs | Surface Downwelling Clear-Sky Longwave Radiation | surface_downwelling_longwave_flux_in_ air_assuming_clear_sky | FLDS, FLNS, FLNSC | rldscs = FLDS + FLNS - FLNSC | yes | J.Zhang |
| yes | fixed | yes | ||
| 33 | rlut | TOA Outgoing Longwave Radiation | toa_outgoing_longwave_flux | 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 | J.Zhang |
| yes | fixed | yes | |
| 34 | rlutcs | TOA Outgoing Clear-Sky Longwave Radiation | toa_outgoing_longwave_flux_assuming_ clear_sky | FLUTC | rlutcs = FLUTC | yes | Slight approximation here since we are using TOM, but NCAR does the same. | J.Zhang | yes | fixed | yes | ||
| 35 | rsdscs | Surface Downwelling Clear-Sky Shortwave Radiation | surface_downwelling_shortwave_flux_in_ air_assuming_clear_sky | FSDSC | rsdscs = FSDSC | yes | J.Zhang |
| yes | fixed | yes | ||
| 36 | rsdt | TOA Incident Shortwave Radiation | SOLIN | rsdt = SOLIN | yes | J.Zhang |
| yes | fixed | yes | |||
| 37 | rsuscs | Surface Upwelling Clear-Sky Shortwave Radiation | surface_upwelling_shortwave_flux_in_ air_assuming_clear_sky | FSDSC, FSNSC | rsuscs = FSDSC - FSNSC | yes | yes | ||||||
| 38 | rsut | TOA Outgoing Shortwave Radiation | toa_outgoing_shortwave_flux | FSUTOA | rsut = FSUTOA (v2) rsut =SOLIN - FSNTOA (v3) For v3 output, both FSUTOA and FSUTOAC are removed. This PR is to update formula to use available variables, i.e., rsut = SOLIN - FSNTOA, and rsutcs = SOLIN - FSNTOAC | yes | yes | ||||||
| 39 | rsutcs | TOA Outgoing Clear-Sky Shortwave Radiation | toa_outgoing_shortwave_flux_assuming_ clear_sky | FSUTOAC | rsutcs = FSUTOAC (v2) rsutcs = SOLIN - FSNTOAC (v3) | yes | yes | ||||||
| 40 | rtmt | Net Downward Radiative Flux at Top of Model | net_downward_radiative_flux_at_top_of_ atmosphere_model | FSNT, FLNT | rtmt = FSNT - FLNT | yes | yes | ||||||
| 41 | ta | Air Temperature | T | ta = T | interpolated to 19 pressure levels | yes | |||||||
| 42 |
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TREFMXAV (available on h0 starting v2) | J. Zhang | Update The monthly averaged daily mean max/min surface temperature are now standard output on h0 starting v2. 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 | ||||||||
| 43 |
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TREFMNAV (available on h0 starting v2) | J. Zhang | Same as above | ||||||||
| 44 | ua | Eastward Wind | U | ua = U | interpolated to 19 pressure levels | yes | |||||||
| 45 | va | Northward Wind | V | va = V | interpolated to 19 pressure levels | yes | |||||||
| 46 | wap | Omega (=dp/dt) | OMEGA | wap = OMEGA | interpolated to 19 pressure levels | J.Zhang | yes | fixed | yes | ||||
| 47 | zg | Geopotential Height | Z3 | zg = Z3 | interpolated to 19 pressure levels | yes | |||||||
| 48 | AERmon | ||||||||||||
| 49 | abs550aer | Ambient Aerosol Absorption Optical Thickness at 550nm | AODABS | abs550aer = AODABS | J. Zhang | yes | |||||||
| 50 | od550aer | Ambient Aerosol Optical Thickness at 550nm | AODVIS | od550aer = AODVIS | J. Zhang | yes | |||||||
| 51 | airmass | Vertically Integrated Mass Content of Air in Layer | atmosphere_mass_of_air_per_unit_area | ||||||||||
| 52 | ptp | Tropopause Air Pressure | TROP_P | ptp = TROP_P | |||||||||
| 53 | so2 | SO2 Volume Mixing Ratio | mole_fraction_of_sulfur_dioxide_in_air | SO2 | so2 = SO2 | ||||||||
| 54 | mmrbc | Elemental Carbon Mass Mixing Ratio | Mass_bc or bc_a1, bc_a3, bc_a4, bc_c1, bc_c3, bc_c4 | mmrbc=Mass_bc or bc_a1 + bc_a3 +bc_a4 + bc_c1 + bc_c3 + bc_c4 | |||||||||
| 55 | mmrdust | Dust Aerosol Mass Mixing Ratio | Mass_dust or dst_a1, dst_a3, dst_c1, dst_c3 | mmrdust=Mass_dust or dst_a1 + dst_a3 + dst_c1 + dst_c3 | |||||||||
| 56 | mmroa | Total Organic Aerosol Mass Mixing Ratio | Mass_pom + Mass_soa or pom_a1, pom_a3, pom_a4, soa_a1, soa_a2, soa_a3, pom_c1, pom_c3, pom_c4, soa_c1, soa_c2, soa_c3 | mmroa = Mass_pom + Mass_soa or pom_a1 + pom_a3 + pom_a4 + soa_a1 + soa_a2 + soa_a3 + pom_c1 + pom_c3 + pom_c4 + soa_c1 + soa_c2 + soa_c3 | |||||||||
| 57 | mmrsoa | Secondary Organic Aerosol Mass Mixing Ratio | Mass_soa or soa_a1, soa_a2, soa_a3, soa_c1, soa_c2, soa_c3 | mmrsoa = Mass_soa or soa_a1 + soa_a2 + soa_a3 + soa_c1 + soa_c2 + soa_c3 | |||||||||
| 58 | mmrss | Sea-Salt Aerosol Mass Mixing Ratio | Mass_ncl or ncl_a1, ncl_a2, ncl_a3, ncl_c1, ncl_c2, ncl_c3 | mmrss = Mass_ncl or ncl_a1 + ncl_a2 + ncl_a3 + ncl_c1 + ncl_c2 + ncl_c3 | |||||||||
| 59 | mmrso4 | Aerosol Sulfate Mass Mixing Ratio | Mass_so4 or so4_a1, so4_a2, so4_a3, so4_a5, so4_c1, so4_c2, so4_c3, so4_c5 | mmrso4 = Mass_so4*96/115 or (so4_a1 + so4_a2 + so4_a3 + so4_a5 + so4_c1 + so4_c2 + so4_c3 + so4_c5)*96/115 | v1/v2 use MAM4 which don’t have so4_a5/c5 should multiply by 96/100 since sulfate is NH4HSO4 in default MAM5/MAM4 | ||||||||
| 60 | emibc | Total Emission Rate of Black Carbon Aerosol Mass | SFbc_a4, bc_a4_CLXF | emibc = SFbc_a4 + bc_a4_CLXF*12/6.022e+22 | |||||||||
| 61 | emidust | Total Emission Rate of Dust | SFdst_a1, SFdst_a3 | emidust = SFdst_a1 + SFdst_a3 | |||||||||
| 62 | emiss | Total Emission Rate of Sea Salt | SFncl_a1, SF_a2, SFncl_a3 | emiss = SFncl_a1 + SFncl_a2 + SFncl_a3 | |||||||||
| 63 | emioa | Primary Emission and Chemical Production of Dry Aerosol Organic Matter | SFpom_a4, pom_a4_CLXF, soa_a1_sfgaex1, soa_a2_sfgaex1, soa_a3_sfgaex1 | emioa = SFpom_a4 + pom_a4_CLXF*12/6.022e+22 + soa_a1_sfgaex1 + soa_a2_sfgaex1 + soa_a3_sfgaex1 | |||||||||
| 64 | emiso4 | Total Direct Emission Rate of SO4 | SFso4_a1, SFso4_a2, SFso4_a3, so4_a1_CLXF, so4_a2_CLXF | emiso4 = (SFso4_a1 + SFso4_a2 + SFso4_a3)*96/115 + (so4_a1_CLXF + so4_a2_CLXF)*96/6.022e+22 | |||||||||
| 65 | emiso2 | Total Emission Rate of SO2 | SFSO2 | emiso2 = SFSO2 | |||||||||
| 66 |
* 51-65 rows: Not yet verified or added to e3sm_to_cmip workflow.