Changeset 3033
- Timestamp:
- Oct 19, 2017, 3:48:54 PM (7 years ago)
- File:
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- 1 edited
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LMDZ6/trunk/DefLists/CMIP6_ping_atmos.xml (modified) (10 diffs)
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LMDZ6/trunk/DefLists/CMIP6_ping_atmos.xml
r3020 r3033 1 1 <!-- $Id$ --> 2 <!-- Ping files generated by dr2xml 0.18 using Data Request 01.00.1 5-->2 <!-- Ping files generated by dr2xml 0.18 using Data Request 01.00.16 --> 3 3 <!-- lrealms= ['atmos'] --> 4 4 <!-- exact= False --> … … 29 29 <field id="CMIP6_O18wv" field_ref="dummy_XYA" /> <!-- P1 () missing : Roche - LSCE --> 30 30 <field id="CMIP6_aerasymbnd" field_ref="dummy_XYA" /> <!-- P1 (1) band_aerosol_asymmetry_parameter : Aerosol level asymmetry parameter for each band --> 31 <field id="CMIP6_aeroptbnd" field_ref="dummy_XYA" /> <!-- P1 (1) atmosphere_absorption_optical_thickness_due_to_ambient_aerosol_particles : Aerosol level extinction optical depthfor each band -->31 <field id="CMIP6_aeroptbnd" field_ref="dummy_XYA" /> <!-- P1 (1) atmosphere_absorption_optical_thickness_due_to_ambient_aerosol_particles : Aerosol level absorption optical thickness for each band --> 32 32 <field id="CMIP6_aerssabnd" field_ref="dummy_XYA" /> <!-- P1 (1) single_scattering_albedo_in_air_due_to_ambient_aerosol_particles : Aerosol level single-scattering albedo for each band --> 33 33 <field id="CMIP6_albdiffbnd" field_ref="dummy_XY" /> <!-- P1 (1.0) band_diffuse_albedo : Diffuse surface albedo for each band --> … … 106 106 <field id="CMIP6_fco2nat" field_ref="dummy_XY" /> <!-- P1 (kg m-2 s-1) surface_upward_mass_flux_of_carbon_dioxide_expressed_as_carbon_due_to_emission_from_natural_sources : This is what the atmosphere sees (on its own grid). This field should be equivalent to the combined natural fluxes of carbon that account for natural exchanges between the atmosphere and land (nep) or ocean (fgco2) reservoirs. --> 107 107 <field id="CMIP6_grpllsprof" field_ref="dummy_XYA" /> <!-- P2 (kg m-2 s-1) large_scale_graupel_flux : unset --> 108 <field id="CMIP6_grplmxrat" field_ref="dummy_XYA" /> <!-- P 2(1.0) mass_fraction_of_graupel_in_air : Graupel mixing ratio -->108 <field id="CMIP6_grplmxrat" field_ref="dummy_XYA" /> <!-- P3 (1.0) mass_fraction_of_graupel_in_air : Graupel mixing ratio --> 109 109 <field id="CMIP6_h2o" field_ref="dummy_XYA" /> <!-- P2 (1.0) mass_fraction_of_water_in_air : includes all phases of water --> 110 110 <field id="CMIP6_hcfc22global" field_ref="dummy_0d" /> <!-- P1 (1e-12) mole_fraction_of_hcfc22_in_air : unset --> … … 157 157 <field id="CMIP6_mcu" field_ref="dummy_XYA" /> <!-- P1 (kg m-2 s-1) atmosphere_updraft_convective_mass_flux : In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. The atmosphere convective mass flux is the vertical transport of mass for a field of cumulus clouds or thermals, given by the product of air density and vertical velocity. For an area-average, cell_methods should specify whether the average is over all the area or the area of updrafts only. --> 158 158 <field id="CMIP6_md" field_ref="dummy_XYA" /> <!-- P1 (kg m-2 s-1) tendency_of_atmosphere_mass_content_of_dust_dry_aerosol_particles_due_to_emission : Balkanski - LSCE --> 159 <field id="CMIP6_mmraerso4" field_ref="concso4"> concso4/(pres/287.04/ta) </field><!-- P1 (kg kg-1) mass_fraction_of_sulfate_dry_aerosol_in_air : Aerosol Sulfate Mass Mixing Ratio -->160 159 <field id="CMIP6_mrroLi" field_ref="dummy_XY" /> <!-- P1 (kg m-2 s-1) land_ice_runoff_flux : Runoff flux over land ice is the difference between any available liquid water in the snowpack less any refreezing. Computed as the sum of rainfall and melt of snow or ice less any refreezing or water retained in the snowpack --> 161 160 <field id="CMIP6_n2o" field_ref="dummy_XYA" /> <!-- P1 (mol mol-1) mole_fraction_of_nitrous_oxide_in_air : N2O volume mixing ratio --> … … 166 165 <field id="CMIP6_od550so4so" field_ref="dummy_XY" /> <!-- P1 (1.0) missing : Balkanski - LSCE --> 167 166 <field id="CMIP6_od865dust" field_ref="dummy_XY" /> <!-- P1 (1.0) atmosphere_optical_thickness_due_to_dust_ambient_aerosol_particles : Balkanski - LSCE --> 168 <field id="CMIP6_orog" field_ref="dummy_XY" /> <!-- P1 (m) surface_altitude : The surface called "surface" means the lower boundary of the atmosphere. Altitude is the (geometric) height above the geoid, which is the reference geopotential surface. The geoid is similar to mean sea level. -->169 167 <field id="CMIP6_parasolRefl_sea" field_ref="dummy_XY" /> <!-- P1 (1.0) toa_bidirectional_reflectance : Simulated reflectance from PARASOL as seen at the top of the atmosphere for 5 solar zenith angles. Valid only over ocean and for one viewing direction (viewing zenith angle of 30 degrees and relative azimuth angle 320 degrees). --> 170 168 <field id="CMIP6_pctisccp" field_ref="ctpisccp" /> <!-- P1 (Pa) air_pressure_at_cloud_top : ISCCP Mean Cloud Top Pressure. Time-means are weighted by the ISCCP Total Cloud Fraction {:cltisccp} - see http://cfmip.metoffice.com/COSP.html --> … … 187 185 <field id="CMIP6_prw" field_ref="prw" /> <!-- P1 (kg m-2) atmosphere_water_vapor_content : vertically integrated through the atmospheric column --> 188 186 <field id="CMIP6_ps" field_ref="psol" /> <!-- P1 (Pa) surface_air_pressure : surface pressure (not mean sea-level pressure), 2-D field to calculate the 3-D pressure field from hybrid coordinates --> 189 <field id="CMIP6_psitem" field_ref="dummy_ lat-P" /> <!-- P1 (kg s^-1) meridional_streamfunction_transformed_eulerian_mean : 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. -->187 <field id="CMIP6_psitem" field_ref="dummy_XYA" /> <!-- P1 (kg s^-1) meridional_streamfunction_transformed_eulerian_mean : 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. Academic Press. --> 190 188 <field id="CMIP6_psl" field_ref="slp" /> <!-- P1 (Pa) air_pressure_at_sea_level : Sea Level Pressure --> 191 189 <field id="CMIP6_rainmxrat" field_ref="dummy_XYA" /> <!-- P2 (1.0) mass_fraction_of_rain_in_air : Rain mixing ratio --> … … 215 213 <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) --> 216 214 <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 --> 217 <field id="CMIP6_rlutcs" field_ref="topl0" /> <!-- P1 (W m-2) toa_outgoing_longwave_flux_assuming_clear_sky : TOA Outgoing Clear-sky Longwave Radiation-->215 <field id="CMIP6_rlutcs" field_ref="topl0" /> <!-- P1 (W m-2) toa_outgoing_longwave_flux_assuming_clear_sky : Upwelling clear-sky longwave radiation at top of atmosphere --> 218 216 <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 --> 219 217 <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) --> … … 253 251 <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. --> 254 252 <field id="CMIP6_rv" field_ref="dummy_XY" /> <!-- P1 (s-1) atmosphere_relative_vorticity : Relative Vorticity at 850 hPa --> 253 <field id="CMIP6_sblnosn" field_ref="dummy_XY" /> <!-- P1 (kg m-2 s-1) sublimation_amount_assuming_no_snow : Sublimation of the snow free area --> 255 254 <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. --> 256 255 <field id="CMIP6_scldncl" field_ref="dummy_XY" /> <!-- P1 (m-3) number_concentration_of_stratiform_cloud_liquid_water_particles_in_air_at_liquid_water_cloud_top : 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. --> … … 261 260 <field id="CMIP6_sfcWind" field_ref="wind10m" /> <!-- P1 (m s-1) wind_speed : near-surface (usually, 10 meters) wind speed. --> 262 261 <field id="CMIP6_sfcWindmax" field_ref="CMIP6_sfcWind" freq_op="1d" operation="maximum"> @this </field> <!-- P1 (m s-1) wind_speed : Daily maximum near-surface (usually, 10 meters) wind speed. --> 263 <field id="CMIP6_sftgif" field_ref="pourc_lic" /> <!-- P1 (%) land_ice_area_fraction : Fraction of grid cell covered by land ice (ice sheet, ice shelf, ice cap, glacier) -->264 262 <field id="CMIP6_sftlf" field_ref="pourc_ter" /> <!-- P1 (%) land_area_fraction : Please express "X_area_fraction" as the percentage of horizontal area occupied by X. --> 265 263 <field id="CMIP6_siltfrac" field_ref="dummy_XYSo" /> <!-- P1 (1.0) missing : Silt Fraction --> 266 <field id="CMIP6_slbnosn" field_ref="dummy_XY" /> <!-- P1 (kg m-2 s-1) sublimation_amount_assuming_no_snow : Sublimation of the snow free area -->267 264 <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). --> 268 265 <field id="CMIP6_snmsl" field_ref="dummy_XY" /> <!-- P1 (kg m-2 s-1) surface_snow_melt_flux_into_soil_layer : Water flowing out of snowpack --> … … 282 279 <field id="CMIP6_tas" field_ref="t2m" /> <!-- P1 (K) air_temperature : near-surface (usually, 2 meter) air temperature --> 283 280 <field id="CMIP6_tasmax" field_ref="CMIP6_tas" freq_op="1d" operation="maximum"> @this </field> <!-- P1 (K) air_temperature : maximum near-surface (usually, 2 meter) air temperature (add cell_method attribute "time: max") --> 281 <field id="CMIP6_tasmaxCrop" field_ref="dummy_XY" /> <!-- P1 (K) air_temperature : maximum near-surface (usually, 2 meter) air temperature (add cell_method attribute "time: max") --> 284 282 <field id="CMIP6_tasmin" field_ref="CMIP6_tas" freq_op="1d" operation="minimum"> @this </field> <!-- P1 (K) air_temperature : minimum near-surface (usually, 2 meter) air temperature (add cell_method attribute "time: min") --> 283 <field id="CMIP6_tasminCrop" field_ref="dummy_XY" /> <!-- P1 (K) air_temperature : minimum near-surface (usually, 2 meter) air temperature (add cell_method attribute "time: min") --> 285 284 <field id="CMIP6_tau" field_ref="taux" > sqrt( taux^2 + tauy^2) </field> <!-- P1 (N m-2) surface_downward_stress : module of the momentum lost by the atmosphere to the surface. --> 286 285 <field id="CMIP6_tauu" field_ref="taux" /> <!-- P1 (Pa) surface_downward_eastward_stress : Downward eastward wind stress at the surface --> 287 <field id="CMIP6_tauupbl" field_ref="dummy_XY" /> <!-- P1 (Pa) surface_downward_eastward_stress_due_to_planetary_boundary_layer : The downward eastward stress associated with the models parameterization of the plan tary boundary layer. (This request is related to a WGNE effort to understand how models parameterize the surface stresses.) -->286 <field id="CMIP6_tauupbl" field_ref="dummy_XY" /> <!-- P1 (Pa) surface_downward_eastward_stress_due_to_planetary_boundary_layer : The downward eastward stress associated with the models parameterization of the planetary boundary layer. (This request is related to a WGNE effort to understand how models parameterize the surface stresses.) --> 288 287 <field id="CMIP6_tauv" field_ref="tauy" /> <!-- P1 (Pa) surface_downward_northward_stress : Downward northward wind stress at the surface --> 289 <field id="CMIP6_tauvpbl" field_ref="dummy_XY" /> <!-- P1 (Pa) surface_downward_northward_stress_due_to_planetary_boundary_layer : The downward northward stress associated with the models parameterization of the plan tary boundary layer. (This request is related to a WGNE effort to understand how models parameterize the surface stresses.) -->288 <field id="CMIP6_tauvpbl" field_ref="dummy_XY" /> <!-- P1 (Pa) surface_downward_northward_stress_due_to_planetary_boundary_layer : The downward northward stress associated with the models parameterization of the planetary boundary layer. (This request is related to a WGNE effort to understand how models parameterize the surface stresses.) --> 290 289 <field id="CMIP6_tdps" field_ref="dummy_XY" /> <!-- P2 (K) dew_point_temperature : unset --> 291 290 <field id="CMIP6_tendacabf" field_ref="dummy_0d" /> <!-- P3 (kg s-1) tendency_of_land_ice_mass_due_to_surface_mass_balance : The total surface mass balance flux over land ice is a spatial integration of the surface mass balance flux -->
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