Ignore:
Timestamp:
Jun 30, 2017, 3:29:50 PM (7 years ago)
Author:
musat
Message:

Mise a jour par rapport a la version envoyee par S.Denvil le 16 juin
(les modifis sont comprises entre CMIP6_ps et CMIP6_tauupbl)

File:
1 edited

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  • LMDZ5/trunk/DefLists/CMIP6_ping_atmos.xml

    r2919 r2926  
    202202   <field id="CMIP6_psitem"        field_ref="dummy_lat-P"      /> <!-- P1 (kg s^-1) psitem : Residual mass streamfunction, computed from vstar and integrated from the top of the atmosphere (on the native model grid). Reference: Andrews et al (1987): Middle Atmospheric Dynamics. Accademic Press. -->
    203203   <field id="CMIP6_psl"           field_ref="slp"              /> <!-- P1 (Pa) air_pressure_at_sea_level : Sea Level Pressure -->
    204    <field id="CMIP6_qgwr"          field_ref="dummy_XY"         /> <!-- P1 (kg m-2 s-1) qgwr : Groundwater recharge from soil layer -->
    205204   <field id="CMIP6_rainmxrat27"   field_ref="dummy_XYA"        /> <!-- P2 (1.0) mass_fraction_of_rain_in_air : Rain mixing ratio -->
    206205   <field id="CMIP6_reffcclwtop"   field_ref="dummy_XY"         /> <!-- P1 (m) reffcclwtop : Droplets are liquid only.  This is the effective radius "as seen from space" over convective liquid cloudy portion of grid cell.  This is the value from uppermost model layer with liquid cloud or, if available, or for some models it is the sum over all liquid cloud tops, no matter where they occur, as long as they are seen from the top of the atmosphere. Reported values are weighted by total liquid cloud top fraction of  (as seen from TOA) each time sample when computing monthly mean.daily data, separated to large-scale clouds, convective clouds. If any of the cloud is from more than one process (i.e. shallow convection), please provide them separately.  -->
    207    <field id="CMIP6_reffclic"      field_ref="dummy_site-A"     /> <!-- P2 (m) effective_radius_of_convective_cloud_ice_particle : This is defined as the in-cloud ratio of the third moment over the second moment of the particle size distribution (obtained by considering only the cloudy portion of the grid cell). -->
     206   <field id="CMIP6_reffclic"      field_ref="dummy_XYA"     /> <!-- P2 (m) effective_radius_of_convective_cloud_ice_particle : This is defined as the in-cloud ratio of the third moment over the second moment of the particle size distribution (obtained by considering only the cloudy portion of the grid cell). -->
    208207   <field id="CMIP6_reffclis"      field_ref="ref_ice"          /> <!-- P2 (m) effective_radius_of_stratiform_cloud_ice_particle : This is defined as the in-cloud ratio of the third moment over the second moment of the particle size distribution (obtained by considering only the cloudy portion of the grid cell). -->
    209208   <field id="CMIP6_reffclwc"      field_ref="dummy_XYA"        /> <!-- P2 (m) effective_radius_of_convective_cloud_liquid_water_particle : Droplets are liquid.  The effective radius is defined as the ratio of the third moment over the second moment of the particle size distribution and the time-mean should be calculated, weighting the individual samples by the cloudy fraction of the grid cell. -->
    210209   <field id="CMIP6_reffclws"      field_ref="dummy_XYA"        /> <!-- P2 (m) effective_radius_of_stratiform_cloud_liquid_water_particle : Droplets are liquid.  The effective radius is defined as the ratio of the third moment over the second moment of the particle size distribution and the time-mean should be calculated, weighting the individual samples by the cloudy fraction of the grid cell. -->
    211210   <field id="CMIP6_reffsclwtop"   field_ref="dummy_XY"         /> <!-- P1 (m) reffsclwtop : Droplets are liquid only.  This is the effective radius "as seen from space" over liquid stratiform cloudy portion of grid cell.  This is the value from uppermost model layer with liquid cloud or, if available, or for some models it is the sum over all liquid cloud tops, no matter where they occur, as long as they are seen from the top of the atmosphere. Reported values are weighted by total liquid cloud top fraction of  (as seen from TOA) each time sample when computing monthly mean.daily data, separated to large-scale clouds, convective clouds. If any of the cloud is from more than one process (i.e. shallow convection), please provide them separately.  -->
    212    <field id="CMIP6_rivi"          field_ref="dummy_XY"         /> <!-- P1 (m3 s-1) rivi : Inflow of River Water into Cell -->
    213    <field id="CMIP6_rivo"          field_ref="dummy_XY"         /> <!-- P1 (m3 s-1) rivo : Outflow of River Water from Cell -->
    214211   <field id="CMIP6_rld"           field_ref="rld"              /> <!-- P1 (W m-2) downwelling_longwave_flux_in_air : Downwelling Longwave Radiation (includes the fluxes at the surface and TOA) -->
    215212   <field id="CMIP6_rld4co2"       field_ref="rld4co2"        /> <!-- P1 (W m-2) downwelling_longwave_flux_in_air : Downwelling longwave radiation calculated using carbon dioxide concentrations increased fourfold (includes the fluxes at the surface and TOA) -->
    … …  
    217214   <field id="CMIP6_rldcs4co2"     field_ref="rldcs4co2"        /> <!-- P1 (W m-2) downwelling_longwave_flux_in_air_assuming_clear_sky : Downwelling clear-sky longwave radiation calculated using carbon dioxide concentrations increased fourfold (includes the fluxes at the surface and TOA) -->
    218215   <field id="CMIP6_rlds"          field_ref="LWdnSFC"          /> <!-- P1 (W m-2) surface_downwelling_longwave_flux_in_air : Surface Downwelling Longwave Radiation -->
    219    <field id="CMIP6_rlds_isf"      field_ref="dummy_??"         /> <!-- P1 (W m-2) surface_downwelling_longwave_flux_in_air : Surface Downwelling Longwave Radiation -->
    220216   <field id="CMIP6_rldscs"        field_ref="LWdnSFCclr"       /> <!-- P1 (W m-2) surface_downwelling_longwave_flux_in_air_assuming_clear_sky : Surface downwelling clear-sky longwave radiation -->
    221217   <field id="CMIP6_rls"           field_ref="soll"         /> <!-- P1 (W m-2) surface_net_downward_longwave_flux : Net longwave surface radiation -->
    … …  
    226222   <field id="CMIP6_rlucs4co2"     field_ref="rlucs4co2"        /> <!-- P1 (W m-2) upwelling_longwave_flux_in_air_assuming_clear_sky : Upwelling clear-sky longwave radiation calculated using carbon dioxide concentrations increased fourfold (includes the fluxes at the surface and TOA) -->
    227223   <field id="CMIP6_rlus"          field_ref="LWupSFC"          /> <!-- P1 (W m-2) surface_upwelling_longwave_flux_in_air : Surface Upwelling Longwave Radiation -->
    228    <field id="CMIP6_rlus_isf"      field_ref="dummy_??"         /> <!-- P1 (W m-2) surface_upwelling_longwave_flux_in_air : Surface Upwelling Longwave Radiation -->
    229224   <field id="CMIP6_rlut"          field_ref="topl"             /> <!-- P1 (W m-2) toa_outgoing_longwave_flux : at the top of the atmosphere (to be compared with satellite measurements) -->
    230225   <field id="CMIP6_rlut4co2"      field_ref="rlut4co2"         /> <!-- P1 (W m-2) toa_outgoing_longwave_flux : Top-of-atmosphere outgoing longwave radiation calculated using carbon dioxide concentrations increased fourfold -->
    231226   <field id="CMIP6_rlutcs"        field_ref="topl0"            /> <!-- P1 (W m-2) toa_outgoing_longwave_flux_assuming_clear_sky : TOA Outgoing Clear-sky Longwave Radiation -->
    232227   <field id="CMIP6_rlutcs4co2"    field_ref="rlutcs4co2"         /> <!-- P1 (W m-2) toa_outgoing_longwave_flux_assuming_clear_sky : Top-of-atmosphere outgoing clear-sky longwave radiation calculated using carbon dioxide concentrations increased fourfold -->
    233    <field id="CMIP6_rootdsl"       field_ref="dummy_XY"         /> <!-- P1 (kg m-3) rootdsl : Root Distribution -->
    234228   <field id="CMIP6_rsd"           field_ref="rsd"              /> <!-- P1 (W m-2) downwelling_shortwave_flux_in_air : Downwelling shortwave radiation (includes the fluxes at the surface and top-of-atmosphere) -->
    235229   <field id="CMIP6_rsd4co2"       field_ref="rsd4co2"        /> <!-- P1 (W m-2) downwelling_shortwave_flux_in_air : Downwelling shortwave radiation calculated using carbon dioxide concentrations increased fourfold -->
    236230   <field id="CMIP6_rsdcs"         field_ref="rsdcs"            /> <!-- P1 (W m-2) downwelling_shortwave_flux_in_air_assuming_clear_sky : Downwelling clear-sky shortwave radiation (includes the fluxes at the surface and top-of-atmosphere) -->
    237231   <field id="CMIP6_rsdcs4co2"     field_ref="rsdcs4co2"        /> <!-- P1 (W m-2) downwelling_shortwave_flux_in_air_assuming_clear_sky : Downwelling clear-sky shortwave radiation calculated using carbon dioxide concentrations increased fourfold -->
     232   <field id="CMIP6_rsdcsaf"       field_ref="dummy_XYA"        /> <!-- P1 (W m-2) rsdcsaf : Calculated in the absence of aerosols and clouds (following Ghan). This requires a double-call in the radiation code with precisely the same meteorology. -->
     233   <field id="CMIP6_rsdcsafbnd"    field_ref="dummy_XYA"        /> <!-- P1 (W m-2) rsdcsafbnd : Calculated in the absence of aerosols and clouds (following Ghan). This requires a double-call in the radiation code with precisely the same meteorology. -->
     234   <field id="CMIP6_rsdcsbnd"      field_ref="dummy_XYA"        /> <!-- P1 (W m-2) rsdcsbnd : Calculated with aerosols but without clouds. This is a standard clear-sky calculation -->
    238235   <field id="CMIP6_rsds"          field_ref="SWdnSFC"          /> <!-- P1 (W m-2) surface_downwelling_shortwave_flux_in_air : surface solar irradiance for UV calculations -->
    239    <field id="CMIP6_rsds_isf"      field_ref="dummy_??"         /> <!-- P1 (W m-2) surface_downwelling_shortwave_flux_in_air : surface solar irradiance for UV calculations -->
    240236   <field id="CMIP6_rsdscs"        field_ref="SWdnSFCclr"       /> <!-- P1 (W m-2) surface_downwelling_shortwave_flux_in_air_assuming_clear_sky : surface solar irradiance clear sky for UV calculations -->
     237   <field id="CMIP6_rsdscsaf"      field_ref="dummy_XY"         /> <!-- P1 (W m-2) rsdscsaf : Calculated in the absence of aerosols and clouds. -->
     238   <field id="CMIP6_rsdscsafbnd"   field_ref="dummy_XY"         /> <!-- P1 (W m-2) rsdscsafbnd : Calculated in the absence of aerosols and clouds, following Ghan (2013, ACP). This requires a double-call in the radiation code with precisely the same meteorology. -->
     239   <field id="CMIP6_rsdscsbnd"     field_ref="dummy_XY"         /> <!-- P1 (W m-2) surface_downwelling_shortwave_flux_in_air_assuming_clear_sky : Calculated with aerosols but without clouds. This is a standard clear-sky calculation -->
    241240   <field id="CMIP6_rsdscsdiff"    field_ref="dummy_XY"         /> <!-- P1 (W m-2) surface_diffuse_downwelling_shortwave_flux_in_air_assuming_clear_sky : unset -->
    242241   <field id="CMIP6_rsdsdiff"      field_ref="dummy_XY"         /> <!-- P1 (W m-2) surface_diffuse_downwelling_shortwave_flux_in_air : unset -->
    … …  
    248247   <field id="CMIP6_rsucs"         field_ref="rsucs"            /> <!-- P1 (W m-2) upwelling_shortwave_flux_in_air_assuming_clear_sky : Upwelling clear-sky shortwave radiation  (includes the fluxes at the surface and TOA) -->
    249248   <field id="CMIP6_rsucs4co2"     field_ref="rsucs4co2"        /> <!-- P1 (W m-2) upwelling_shortwave_flux_in_air_assuming_clear_sky : Upwelling clear-sky shortwave radiation calculated using carbon dioxide concentrations increased fourfold -->
     249   <field id="CMIP6_rsucsaf"       field_ref="dummy_XYA"        /> <!-- P1 (W m-2) rsucsaf : Calculated in the absence of aerosols and clouds (following Ghan). This requires a double-call in the radiation code with precisely the same meteorology. -->
     250   <field id="CMIP6_rsucsafbnd"    field_ref="dummy_XYA"        /> <!-- P1 (W m-2) rsucsafbnd : Calculated in the absence of aerosols and clouds (following Ghan). This requires a double-call in the radiation code with precisely the same meteorology. -->
     251   <field id="CMIP6_rsucsbnd"      field_ref="dummy_XYA"        /> <!-- P1 (W m-2) rsucsbnd : Calculated with aerosols but without clouds. This is a standard clear-sky calculation -->
    250252   <field id="CMIP6_rsus"          field_ref="SWupSFC"          /> <!-- P1 (W m-2) surface_upwelling_shortwave_flux_in_air : Surface Upwelling Shortwave Radiation -->
    251    <field id="CMIP6_rsus_isf"      field_ref="dummy_??"         /> <!-- P1 (W m-2) surface_upwelling_shortwave_flux_in_air : Surface Upwelling Shortwave Radiation -->
    252    <field id="CMIP6_rsuscs"        field_ref="SWupSFCclr"       /> <!-- P1 (W m-2) surface_upwelling_shortwave_flux_in_air_assuming_clear_sky : Surface upwelling clear-sky shortwave radiation -->
     253   <field id="CMIP6_rsuscs"        field_ref="SWupSFCclr"       /> <!-- P1 (W m-2) surface_upwelling_shortwave_flux_in_air_assuming_clear_sky : Surface Upwelling Clear-sky Shortwave Radiation -->
     254   <field id="CMIP6_rsuscsaf"      field_ref="dummy_XY"         /> <!-- P1 (W m-2) rsuscsaf : Surface Upwelling Clear-sky, Aerosol Free Shortwave Radiation -->
     255   <field id="CMIP6_rsuscsafbnd"   field_ref="dummy_XY"         /> <!-- P1 (W m-2) rsuscsafbnd : Calculated in the absence of aerosols and clouds, following Ghan (ACP, 2013). This requires a double-call in the radiation code with precisely the same meteorology. -->
     256   <field id="CMIP6_rsuscsbnd"     field_ref="dummy_XY"         /> <!-- P1 (W m-2) surface_upwelling_shortwave_flux_in_air_assuming_clear_sky : Calculated with aerosols but without clouds. This is a standard clear-sky calculation -->
    253257   <field id="CMIP6_rsut"          field_ref="SWupTOA"          /> <!-- P1 (W m-2) toa_outgoing_shortwave_flux : at the top of the atmosphere -->
    254258   <field id="CMIP6_rsut4co2"      field_ref="rsut4co2"         /> <!-- P1 (W m-2) toa_outgoing_shortwave_flux : TOA Outgoing Shortwave Radiation calculated using carbon dioxide concentrations increased fourfold -->
    255259   <field id="CMIP6_rsutcs"        field_ref="SWupTOAclr"       /> <!-- P1 (W m-2) toa_outgoing_shortwave_flux_assuming_clear_sky : Calculated in the absence of clouds. -->
    256260   <field id="CMIP6_rsutcs4co2"    field_ref="rsutcs4co2"         /> <!-- P1 (W m-2) toa_outgoing_shortwave_flux_assuming_clear_sky : TOA Outgoing Clear-Sky Shortwave Radiation calculated using carbon dioxide concentrations increased fourfold -->
    257    <field id="CMIP6_rsutna"        field_ref="dummy_XY"         /> <!-- P1 (W m-2) rsutna : Based on Ghan (2013, ACP) -->
    258    <field id="CMIP6_rsutnacs"      field_ref="dummy_XY"         /> <!-- P1 (W m-2) rsutnacs : Based on Ghan (2013, ACP) -->
     261   <field id="CMIP6_rsutcsafbnd"   field_ref="dummy_XY"         /> <!-- P1 (W m-2) rsutcsafbnd : Calculated in the absence of aerosols and clouds, following Ghan (2013, ACP). This requires a double-call in the radiation code with precisely the same meteorology. -->
     262   <field id="CMIP6_rsutcsbnd"     field_ref="dummy_XY"         /> <!-- P1 (W m-2) toa_outgoing_shortwave_flux_assuming_clear_sky : Calculated with aerosols but without clouds. This is a standard clear-sky calculation -->
    259263   <field id="CMIP6_rtmt"          field_ref="nettop"           /> <!-- P1 (W m-2) net_downward_radiative_flux_at_top_of_atmosphere_model : Net Downward Radiative Flux at Top of Model : I.e., at the top of that portion of the atmosphere where dynamics are explicitly treated by the model. This is reported only if it differs from the net downward radiative flux at the top of the atmosphere. -->
    260    <field id="CMIP6_rzwc"          field_ref="dummy_XY"         /> <!-- P1 (kg m-2) rzwc : Root zone soil moisture -->
    261    <field id="CMIP6_sandFrac"      field_ref="dummy_XY"         /> <!-- P1 (1.0) sandFrac : Sand Fraction -->
    262    <field id="CMIP6_sbl"           field_ref="dummy_??"         /> <!-- P1 (kg m-2 s-1) surface_snow_and_ice_sublimation_flux : The snow and ice sublimation flux is the loss of snow and ice mass per unit area from the surface resulting from their direct conversion to water vapor that enters the atmosphere. -->
     264   <field field_ref="CMIP6_rv" grid_ref="CMIP6_p850" id="CMIP6_rv850" />   <!-- P1 (s-1) atmosphere_relative_vorticity : Relative Vorticity at 850 hPa -->
     265   <field id="CMIP6_sandfrac"      field_ref="dummy_XY"         /> <!-- P1 (1.0) sandFrac : Sand Fraction -->
    263266   <field id="CMIP6_sci"           field_ref="ftime_th"         /> <!-- P1 (1.0) shallow_convection_time_fraction : Fraction of time that shallow convection occurs in the grid cell. -->
    264267   <field id="CMIP6_scldncl"       field_ref="dummy_XY"         /> <!-- P1 (m-3) scldncl : Droplets are liquid only.  Report concentration "as seen from space" over stratiform liquid cloudy portion of grid cell.  This is the value from uppermost model layer with liquid cloud or, if available, it is better to sum over all liquid cloud tops, no matter where they occur, as long as they are seen from the top of the atmosphere. Weight by total liquid cloud top fraction of  (as seen from TOA) each time sample when computing monthly mean. -->
    … …  
    266269   <field id="CMIP6_sconcso4"      field_ref="sconcso4"         /> <!-- P1 (kg m-3) mass_concentration_of_sulfate_dry_aerosol_in_air : mass concentration of sulfate dry aerosol in air in model lowest layer. -->
    267270   <field id="CMIP6_sconcss"       field_ref="sconcss"         /> <!-- P1 (kg m-3) mass_concentration_of_seasalt_dry_aerosol_in_air : mass concentration of seasalt dry aerosol in air in model lowest layer -->
     271   <field id="CMIP6_sedustCI"      field_ref="dummy_XY"         /> <!-- P1 (kg m-2 s-1) sedustCI : Balkanski - LSCE -->
    268272   <field id="CMIP6_sfcWind"       field_ref="wind10m"          /> <!-- P1 (m s-1) wind_speed : near-surface (usually, 10 meters) wind speed. -->
    269273   <field id="CMIP6_sfcWindmax"    field_ref="wind10max"         /> <!-- P1 (m s-1) wind_speed : Daily maximum near-surface (usually, 10 meters) wind speed. -->
    270274   <field id="CMIP6_sftlf"         field_ref="fract_ter"         /> <!-- P1 (1) land_area_fraction : Please express "X_area_fraction" as the fraction of horizontal area occupied by X. -->
    271    <field id="CMIP6_sic"           field_ref="fract_sic"         /> <!-- P1 (1.0) sea_ice_area_fraction : fraction of grid cell covered by sea ice. -->
    272275   <field id="CMIP6_siltFrac"      field_ref="dummy_XY"         /> <!-- P1 (1.0) siltFrac : Silt Fraction -->
    273276   <field id="CMIP6_slbnosn"       field_ref="dummy_XY"         /> <!-- P1 (kg m-2 s-1) slbnosn : Sublimation of the snow free area -->
    274    <field id="CMIP6_sltbasin"      field_ref="dummy_basin_zonal_mean"/> <!-- P2 (kg s-1) northward_ocean_salt_transport : function of latitude, basin -->
    275    <field id="CMIP6_slthick"       field_ref="dummy_XY"         /> <!-- P1 (m) slthick : Thickness of Soil Layers -->
    276    <field id="CMIP6_sltnorth"      field_ref="dummy_basin_zonal_mean"/> <!-- P2 (kg s-1) northward_ocean_salt_transport : unset -->
    277    <field id="CMIP6_sltnortha"     field_ref="dummy_basin_zonal_mean"/> <!-- P1 (kg s-1) northward_ocean_salt_transport : unset -->
    278277   <field id="CMIP6_smc"           field_ref="f_th"        /> <!-- P2 (kg m-2 s-1) atmosphere_net_upward_shallow_convective_mass_flux : The net mass flux represents the difference between the updraft and downdraft components.  For models with a distinct shallow convection scheme, this is calculated as convective mass flux divided by the area of the whole grid cell (not just the area of the cloud). -->
    279278   <field id="CMIP6_snmsl"         field_ref="dummy_XY"         /> <!-- P1 (kg m-2 s-1) snmsl : Water flowing out of snowpack -->
    280    <field id="CMIP6_snowmxrat27"   field_ref="dummy_XYA"        /> <!-- P2 (1.0) mass_fraction_of_snow_in_air : Snow mixing ratio -->
     279   <field id="CMIP6_snowmxrat27"   field_ref="dummy_XYA"        /> <!-- P3 (1.0) mass_fraction_of_snow_in_air : Snow mixing ratio -->
    281280   <field id="CMIP6_snrefr"        field_ref="dummy_XY"         /> <!-- P1 (kg m-2 s-1) surface_snow_and_ice_refreezing_flux : Re-freezing of water in the snow -->
    282281   <field id="CMIP6_snwc"          field_ref="dummy_XY"         /> <!-- P1 (kg m-2) snwc : Total water mass of the snowpack (liquid or frozen), averaged over a grid cell and interecepted by the canopy. -->
    283    <field id="CMIP6_sw"            field_ref="dummy_XY"         /> <!-- P1 (kg m-2) sw : Total liquid water storage, other than soil, snow or interception storage (i.e. lakes, river channel or depression storage). -->
    284    <field id="CMIP6_swsffluxaero"  field_ref="dummy_XY"         /> <!-- P2 (W m-2 ) swsffluxaero : shortwave heating rate due to volcanic aerosols to be diagnosed through double radiation call, zonal average values required -->
    285    <field id="CMIP6_swtoafluxaerocs" field_ref="dummy_XY"         /> <!-- P1 (W m-2 ) swtoafluxaerocs : downwelling shortwave flux due to volcanic aerosols at TOA under clear sky to be diagnosed through double radiation call -->
     282   <field id="CMIP6_solbnd"        field_ref="dummy_XY"         /> <!-- P1 (W m-2) solbnd : Top-of-Atmosphere Solar Insolation for each band -->
     283   <field id="CMIP6_swsffluxaero"  field_ref="dummy_XY"         /> <!-- P2 (W m-2) swsffluxaero : shortwave heating rate due to volcanic aerosols to be diagnosed through double radiation call, zonal average values required -->
     284   <field id="CMIP6_swsrfasdust"   field_ref="dummy_XY"         /> <!-- P1 (W m-2) swsrfasdust : Balkanski - LSCE -->
     285   <field id="CMIP6_swsrfcsdust"   field_ref="dummy_XY"         /> <!-- P1 (W m-2) swsrfcsdust : Balkanski - LSCE -->
     286   <field id="CMIP6_swtoaasdust"   field_ref="dummy_XY"         /> <!-- P1 (W m-2) toa_instantaneous_shortwave_forcing : proposed name: toa_instantaneous_shortwave_forcing_due_to_dust_ambient_aerosol -->
     287   <field id="CMIP6_swtoacsdust"   field_ref="dummy_XY"         /> <!-- P1 (W m-2) toa_instantaneous_shortwave_forcing : proposed name: toa_instantaneous_shortwave_forcing_due_to_dust_ambient_aerosol_assuming_clear_sky -->
     288   <field id="CMIP6_swtoafluxaerocs" field_ref="dummy_XY"         /> <!-- P1 (W m-2) swtoafluxaerocs : downwelling shortwave flux due to volcanic aerosols at TOA under clear sky to be diagnosed through double radiation call -->
     289   <field id="CMIP6_sza"           field_ref="dummy_XY"         /> <!-- P1 (degree) solar_zenith_angle : The angle between the line of sight to the sun and the local vertical -->
    286290   <field id="CMIP6_t2"            field_ref="dummy_XYA"        /> <!-- P2 (K2) square_of_air_temperature : Air temperature squared -->
    287    <field id="CMIP6_t20d"          field_ref="dummy_XY"         /> <!-- P2 (m) depth_of_isosurface_of_sea_water_potential_temperature : unset -->
    288    <field id="CMIP6_ta"            field_ref="ta"               /> <!-- P1 (K) air_temperature : Air Temperature -->
     291   <field id="CMIP6_ta"            field_ref="ta"               /> <!-- P3 (K) air_temperature : Air Temperature -->
    289292   <field id="CMIP6_ta27"          field_ref="dummy_XYA"        /> <!-- P3 (K) air_temperature : Air Temperature -->
    290293   <field id="CMIP6_ta500"         field_ref="t500"             /> <!-- P1 (K) air_temperature : Temperature on the 500 hPa surface -->
    … …  
    293296   <field id="CMIP6_ta850"         field_ref="t850"             /> <!-- P1 (K) air_temperature : Air temperature at 850hPa -->
    294297   <field id="CMIP6_tas"           field_ref="t2m"              /> <!-- P1 (K) air_temperature : near-surface (usually, 2 meter) air temperature -->
    295    <field id="CMIP6_tas_isf"       field_ref="dummy_XY"         /> <!-- P1 (K) air_temperature : near-surface (usually, 2 meter) air temperature -->
    296298   <field id="CMIP6_tasmax"        field_ref="t2m_max"          /> <!-- P1 (K) air_temperature : maximum near-surface (usually, 2 meter) air temperature (add cell_method attribute "time: max") -->
    297299   <field id="CMIP6_tasmin"        field_ref="t2m_min"          /> <!-- P1 (K) air_temperature : minimum near-surface (usually, 2 meter) air temperature (add cell_method attribute "time: min") -->
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