Changeset 3117 for LMDZ6/trunk/DefLists/CMIP6_ping_atmos.xml
- Timestamp:
- Dec 8, 2017, 2:04:01 PM (6 years ago)
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LMDZ6/trunk/DefLists/CMIP6_ping_atmos.xml
r3116 r3117 58 58 <field id="CMIP6_clcalipsoice" field_ref="clcalipsoice" /> <!-- P1 (%) ice_cloud_area_fraction_in_atmosphere_layer : CALIPSO ice cloud Fraction --> 59 59 <field id="CMIP6_clcalipsoliq" field_ref="clcalipsoice" /> <!-- P1 (%) liquid_cloud_area_fraction_in_atmosphere_layer : CALIPSO liquid cloud Fraction --> 60 <field id="CMIP6_cldicemxrat" field_ref=" cldicemxrat" /> <!-- P3 (1.0) cloud_ice_mixing_ratio : Cloud ice mixing ratio -->60 <field id="CMIP6_cldicemxrat" field_ref="dummy_XYA" /> <!-- P3 (1.0) cloud_ice_mixing_ratio : Cloud ice mixing ratio --> 61 61 <field id="CMIP6_cldnci" field_ref="dummy_XY" /> <!-- P1 (m-3) number_concentration_of_ice_crystals_in_air_at_ice_cloud_top : Concentration 'as seen from space' over ice-cloud portion of grid cell. This is the value from uppermost model layer with ice cloud or, if available, it is the sum over all ice cloud tops, no matter where they occur, as long as they are seen from the top of the atmosphere. Weight by total ice cloud top fraction (as seen from TOA) of each time sample when computing monthly mean. --> 62 62 <field id="CMIP6_cldncl" field_ref="cldncl" /> <!-- P1 (m-3) number_concentration_of_cloud_liquid_water_particles_in_air_at_liquid_water_cloud_top : Droplets are liquid only. Report concentration 'as seen from space' over 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. --> 63 63 <field id="CMIP6_cldnvi" field_ref="cldnvi" /> <!-- P1 (m-2) atmosphere_number_content_of_cloud_droplets : Droplets are liquid only. Values are weighted by liquid cloud fraction in each layer when vertically integrating, and for monthly means the samples are weighted by total liquid cloud fraction (as seen from TOA). --> 64 <field id="CMIP6_cldwatmxrat" field_ref=" cldwatmxrat" /> <!-- P2 (1.0) cloud_liquid_water_mixing_ratio : Cloud water mixing ratio -->64 <field id="CMIP6_cldwatmxrat" field_ref="dummy_XYA" /> <!-- P2 (1.0) cloud_liquid_water_mixing_ratio : Cloud water mixing ratio --> 65 65 <field id="CMIP6_clhcalipso" field_ref="pclhcalipso" /> <!-- P1 (%) cloud_area_fraction_in_atmosphere_layer : Percentage cloud cover in layer centred on 220hPa --> 66 66 <field id="CMIP6_cli" field_ref="iwcon" /> <!-- P1 (kg kg-1) mass_fraction_of_cloud_ice_in_air : Includes both large-scale and convective cloud. This is calculated as the mass of cloud ice in the grid cell divided by the mass of air (including the water in all phases) in the grid cell. It includes precipitating hydrometeors ONLY if the precipitating hydrometeors affect the calculation of radiative transfer in model. --> 67 <field id="CMIP6_clic" field_ref=" icc3dcon" /> <!-- P2 (1.0) mass_fraction_of_convective_cloud_ice_in_air : Calculated as the mass of convective cloud ice in the grid cell divided by the mass of air (including the water in all phases) in the grid cell. This includes precipitating hydrometeors ONLY if the precipitating hydrometeors affect the calculation of radiative transfer in model. -->67 <field id="CMIP6_clic" field_ref="dummy_XYA" /> <!-- P2 (1.0) mass_fraction_of_convective_cloud_ice_in_air : Calculated as the mass of convective cloud ice in the grid cell divided by the mass of air (including the water in all phases) in the grid cell. This includes precipitating hydrometeors ONLY if the precipitating hydrometeors affect the calculation of radiative transfer in model. --> 68 68 <field id="CMIP6_climodis" field_ref="climodis" /> <!-- P1 (%) ice_cloud_area_fraction : MODIS Ice Cloud Area Percentage --> 69 <field id="CMIP6_clis" field_ref=" icc3dstra" /> <!-- P2 (1.0) mass_fraction_of_stratiform_cloud_ice_in_air : Calculated as the mass of stratiform cloud ice in the grid cell divided by the mass of air (including the water in all phases) in the grid cell. This includes precipitating hydrometeors ONLY if the precipitating hydrometeors affect the calculation of radiative transfer in model. -->69 <field id="CMIP6_clis" field_ref="dummy_XYA" /> <!-- P2 (1.0) mass_fraction_of_stratiform_cloud_ice_in_air : Calculated as the mass of stratiform cloud ice in the grid cell divided by the mass of air (including the water in all phases) in the grid cell. This includes precipitating hydrometeors ONLY if the precipitating hydrometeors affect the calculation of radiative transfer in model. --> 70 70 <field id="CMIP6_clisccp" field_ref="clisccp2" /> <!-- P1 (%) cloud_area_fraction_in_atmosphere_layer : Percentage cloud cover in optical depth categories. --> 71 71 <field id="CMIP6_clivi" field_ref="iwp" /> <!-- P1 (kg m-2) atmosphere_cloud_ice_content : mass of ice water in the column divided by the area of the column (not just the area of the cloudy portion of the column). Includes precipitating frozen hydrometeors ONLY if the precipitating hydrometeor affects the calculation of radiative transfer in model. --> … … 168 168 <field id="CMIP6_od550so4so" field_ref="dummy_not_provided" /> <!-- P1 (1.0) missing : Balkanski - LSCE --> 169 169 <field id="CMIP6_od865dust" field_ref="dummy_not_provided" /> <!-- P1 (1.0) atmosphere_optical_thickness_due_to_dust_ambient_aerosol_particles : Balkanski - LSCE --> 170 <field id="CMIP6_parasolRefl_sea" field_ref="parasol_refl"> parasol_refl*fract_oce </field> <!-- 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). --> 171 <field id="HomeCMIP6_parasolCRefl" field_ref="parasol_crefl" /> <!-- P4 (1.0) toa_bidirectional_reflectance (integral) : Simulated reflectance from PARASOL as seen at the top of the atmosphere integrated over all 5 solar zenith angles. --> 170 <field id="CMIP6_parasolRefl_sea" field_ref="parasolRefl"> parasolRefl*fract_oce </field> <!-- 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). --> 172 171 <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 --> 173 172 <field id="CMIP6_pfull" field_ref="pres" /> <!-- P1 (Pa) air_pressure : Air pressure on model levels --> … … 231 230 <field id="CMIP6_rsdscsafbnd" field_ref="dummy_not_provided" /> <!-- P1 (W m-2) surface_downwelling_shortwave_flux_in_air_assuming_clean_clear_sky : 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. --> 232 231 <field id="CMIP6_rsdscsbnd" field_ref="dummy_not_provided" /> <!-- 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 --> 233 <field id="CMIP6_rsdscsdiff" field_ref=" rsdscsdiff" /> <!-- P1 (W m-2) surface_diffuse_downwelling_shortwave_flux_in_air_assuming_clear_sky : unset -->234 <field id="CMIP6_rsdsdiff" field_ref=" rsdsdiff" /> <!-- P1 (W m-2) surface_diffuse_downwelling_shortwave_flux_in_air : unset -->232 <field id="CMIP6_rsdscsdiff" field_ref="dummy_XY" /> <!-- P1 (W m-2) surface_diffuse_downwelling_shortwave_flux_in_air_assuming_clear_sky : unset --> 233 <field id="CMIP6_rsdsdiff" field_ref="dummy_XY" /> <!-- P1 (W m-2) surface_diffuse_downwelling_shortwave_flux_in_air : unset --> 235 234 <field id="CMIP6_rsdt" field_ref="SWdnTOA" /> <!-- P1 (W m-2) toa_incoming_shortwave_flux : Shortwave radiation incident at the top of the atmosphere --> 236 235 <field id="CMIP6_rss" field_ref="sols" /> <!-- P1 (W m-2) surface_net_downward_shortwave_flux : Net downward shortwave radiation at the surface -->
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