Changeset 2991 for LMDZ5/trunk/DefLists/CMIP6_ping_atmos.xml
- Timestamp:
- Sep 21, 2017, 11:27:18 AM (7 years ago)
- File:
-
- 1 edited
-
LMDZ5/trunk/DefLists/CMIP6_ping_atmos.xml (modified) (9 diffs)
Legend:
- Unmodified
- Added
- Removed
-
LMDZ5/trunk/DefLists/CMIP6_ping_atmos.xml
r2988 r2991 97 97 <field id="CMIP6_dtauc" field_ref="dummy_XYA" /> <!-- P3 (1.0) atmosphere_optical_thickness_due_to_convective_cloud : This is the in-cloud optical depth obtained by considering only the cloudy portion of the grid cell --> 98 98 <field id="CMIP6_dtaus" field_ref="dummy_XYA" /> <!-- P3 (1.0) atmosphere_optical_thickness_due_to_stratiform_cloud : This is the in-cloud optical depth obtained by considering only the cloudy portion of the grid cell. --> 99 <field id="CMIP6_edt" field_ref=" Kz" /> <!-- P1 (m2 s-1) atmosphere_heat_diffusivity : Vertical diffusion coefficient for temperature due to parametrised eddies -->99 <field id="CMIP6_edt" field_ref="kz" /> <!-- P1 (m2 s-1) atmosphere_heat_diffusivity : Vertical diffusion coefficient for temperature due to parametrised eddies --> 100 100 <field id="CMIP6_epfy" field_ref="dummy_XYA" /> <!-- P1 (m3 s-2) northward_eliassen_palm_flux_in_air : Transformed Eulerian Mean Diagnostics Meridional component Fy of Eliassen-Palm (EP) flux (Fy, Fz) derived from 6hr or higher frequency fields (use daily fields or 12 hr fields if the 6 hr are not available). Please use the definitions given by equation 3.5.3a of Andrews, Holton and Leovy text book, but scaled by density to have units m3 s-2. --> 101 101 <field id="CMIP6_epfz" field_ref="dummy_XYA" /> <!-- P1 (m3 s-2) upward_eliassen_palm_flux_in_air : Transformed Eulerian Mean Diagnostics Meridional component Fz of the Eliassen-Palm (EP) flux (Fy, Fz) derived from 6hr or higher frequency fields (use daily fields or 12 hr fields if the 6 hr are not available). Please use the definitions given by equation 3.5.3b of Andrews, Holton and Leovy text book, but scaled by density to have units m3 s-2. --> … … 116 116 <field id="CMIP6_hfsbl" field_ref="dummy_XY" /> <!-- P1 (W m-2) surface_snow_and_ice_sublimation_heat_flux : Energy consumed or released during vapor/solid phase changes. --> 117 117 <field id="CMIP6_hfss" field_ref="sens" /> <!-- P1 (W m-2) surface_upward_sensible_heat_flux : Surface Upward Sensible Heat Flux --> 118 <field id="CMIP6_hur" field_ref=" hur" /> <!-- P1 (%) relative_humidity : The relative humidity with respect to liquid water for T> 0 C, and with respect to ice for T<0 C. -->118 <field id="CMIP6_hur" field_ref="rhum" /> <!-- P1 (%) relative_humidity : The relative humidity with respect to liquid water for T> 0 C, and with respect to ice for T<0 C. --> 119 119 <field id="CMIP6_hurs" field_ref="rh2m" /> <!-- P1 (%) relative_humidity : The relative humidity with respect to liquid water for T> 0 C, and with respect to ice for T<0 C. --> 120 120 <field id="CMIP6_hursmax" field_ref="CMIP6_hurs" freq_op="1d" operation="maximum"> @this </field> <!-- P1 (%) relative_humidity : Daily Maximum Near-Surface Relative Humidity --> 121 121 <field id="CMIP6_hursmin" field_ref="dummy_XY" /> <!-- P1 (%) relative_humidity : Daily Minimum Near-Surface Relative Humidity --> 122 122 <field id="CMIP6_hursminCrop" field_ref="dummy_XY" /> <!-- P1 (%) relative_humidity : minimum near-surface (usually, 2 meter) relative humidity (add cell_method attribute "time: min") --> 123 <field id="CMIP6_hus" field_ref=" hus"/> <!-- P1 (1.0) specific_humidity : Specific Humidity -->123 <field id="CMIP6_hus" field_ref="ovap" /> <!-- P1 (1.0) specific_humidity : Specific Humidity --> 124 124 <field id="CMIP6_huss" field_ref="q2m" /> <!-- P1 (1.0) specific_humidity : Near-surface (usually, 2 meter) specific humidity. --> 125 125 <field id="CMIP6_iareafl" field_ref="dummy_0d" /> <!-- P3 (m2) floating_ice_shelf_area : Total area of the floating ice shelves (the component of ice sheet that flows over ocean) --> … … 248 248 <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 --> 249 249 <field id="CMIP6_rsutcs" field_ref="SWupTOAclr" /> <!-- P1 (W m-2) toa_outgoing_shortwave_flux_assuming_clear_sky : Calculated in the absence of clouds. --> 250 <field id="CMIP6_rsutcs4co2" field_ref="rsutcs4co2" 250 <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 --> 251 251 <field id="CMIP6_rsutcsafbnd" field_ref="dummy_XY" /> <!-- P1 (W m-2) band_toa_outgoing_shortwave_flux_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. --> 252 252 <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 --> … … 276 276 <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 --> 277 277 <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 --> 278 <field id="CMIP6_swtoafluxaerocs" field_ref="dummy_XY" 278 <field id="CMIP6_swtoafluxaerocs" field_ref="dummy_XY" /> <!-- P1 (W m-2) shortwave_flux_due_to_volcanic_aerosols_at_TOA_under_clear_sky : downwelling shortwave flux due to volcanic aerosols at TOA under clear sky to be diagnosed through double radiation call --> 279 279 <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 --> 280 280 <field id="CMIP6_t2" field_ref="dummy_XYA" /> <!-- P2 (K2) square_of_air_temperature : Air temperature squared --> 281 <field id="CMIP6_ta" field_ref="t a"/> <!-- P3 (K) air_temperature : Air Temperature -->281 <field id="CMIP6_ta" field_ref="temp" /> <!-- P3 (K) air_temperature : Air Temperature --> 282 282 <field id="CMIP6_tas" field_ref="t2m" /> <!-- P1 (K) air_temperature : near-surface (usually, 2 meter) air temperature --> 283 283 <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") --> … … 296 296 <field id="CMIP6_tnhus" field_ref="tnhus" /> <!-- P1 (s-1) tendency_of_specific_humidity : Tendency of Specific Humidity --> 297 297 <field id="CMIP6_tnhusa" field_ref="dqdyn" /> <!-- P1 (s-1) tendency_of_specific_humidity_due_to_advection : Tendency of Specific Humidity due to Advection --> 298 <field id="CMIP6_tnhusc" field_ref=" rnhusc" /> <!-- P1 (s-1) tendency_of_specific_humidity_due_to_convection : Tendencies from cumulus convection scheme. -->298 <field id="CMIP6_tnhusc" field_ref="tnhusc" /> <!-- P1 (s-1) tendency_of_specific_humidity_due_to_convection : Tendencies from cumulus convection scheme. --> 299 299 <field id="CMIP6_tnhusd" field_ref="dqvdf" /> <!-- P1 (s-1) tendency_of_specific_humidity_due_to_diffusion : Tendency of specific humidity due to numerical diffusion.This includes any horizontal or vertical numerical moisture diffusion not associated with the parametrized moist physics or the resolved dynamics. For example, any vertical diffusion which is part of the boundary layer mixing scheme should be excluded, as should any diffusion which is included in the terms from the resolved dynamics. This term is required to check the closure of the moisture budget. --> 300 300 <field id="CMIP6_tnhusmp" field_ref="dqphy" /> <!-- P1 (s-1) tendency_of_specific_humidity_due_to_model_physics : Tendency of specific humidity due to model physics. This includes sources and sinks from parametrized moist physics (e.g. convection, boundary layer, stratiform condensation/evaporation, etc.) and excludes sources and sinks from resolved dynamics or from horizontal or vertical numerical diffusion not associated with model physicsl. For example any diffusive mixing by the boundary layer scheme would be included. --> … … 320 320 <field id="CMIP6_twap" field_ref="dummy_XYA" /> <!-- P2 (K Pa s-1) product_of_omega_and_air_temperature : Product of air temperature and pressure tendency --> 321 321 <field id="CMIP6_u2" field_ref="dummy_XYA" /> <!-- P2 (m2 s-2) square_of_eastward_wind : u*u --> 322 <field id="CMIP6_ua" field_ref=" ua"/> <!-- P1 (m s-1) eastward_wind : Eastward Wind -->322 <field id="CMIP6_ua" field_ref="vitu" /> <!-- P1 (m s-1) eastward_wind : Eastward Wind --> 323 323 <field id="CMIP6_uas" field_ref="u10m" /> <!-- P1 (m s-1) eastward_wind : Eastward component of the near-surface (usually, 10 meters) wind --> 324 324 <field id="CMIP6_uqint" field_ref="dummy_XY" /> <!-- P1 (m2 s-1) integral_of_product_of_eastward_wind_and_specific_humidity_wrt_height : Column integrated eastward wind times specific humidity --> … … 332 332 <field id="CMIP6_uwap" field_ref="dummy_XYA" /> <!-- P2 (Pa m s-2) product_of_eastward_wind_and_omega : u*omega --> 333 333 <field id="CMIP6_v2" field_ref="dummy_XYA" /> <!-- P2 (m2 s-2) square_of_northward_wind : v*v --> 334 <field id="CMIP6_va" field_ref="v a"/> <!-- P1 (m s-1) northward_wind : Northward component of the wind at 850hPa -->334 <field id="CMIP6_va" field_ref="vitv" /> <!-- P1 (m s-1) northward_wind : Northward component of the wind at 850hPa --> 335 335 <field id="CMIP6_vas" field_ref="v10m" /> <!-- P1 (m s-1) northward_wind : Northward component of the near surface wind --> 336 336 <field id="CMIP6_vortmean" field_ref="dummy_XY" /> <!-- P1 (s-1) atmosphere_relative_vorticity : Mean vorticity over 850,700,600 hPa --> … … 341 341 <field id="CMIP6_vtendogw" field_ref="dummy_XYA" /> <!-- P2 (m s-2) tendency_of_northward_wind_due_to_orographic_gravity_wave_drag : Tendency of the northward wind by parameterized orographic gravity waves. (Note that CF name tables only have a general northward tendency for all gravity waves, and we need it separated by type.) --> 342 342 <field id="CMIP6_vwap" field_ref="dummy_XYA" /> <!-- P2 (Pa m s-2) product_of_northward_wind_and_omega : v*omega --> 343 <field id="CMIP6_wap" field_ref=" wap"/> <!-- P1 (Pa s-1) lagrangian_tendency_of_air_pressure : Omega (vertical velocity in pressure coordinates, positive downwards) -->343 <field id="CMIP6_wap" field_ref="vitw" /> <!-- P1 (Pa s-1) lagrangian_tendency_of_air_pressure : Omega (vertical velocity in pressure coordinates, positive downwards) --> 344 344 <field id="CMIP6_wap2" field_ref="dummy_XYA" /> <!-- P2 (Pa2 s-2) square_of_lagrangian_tendency_of_air_pressure : omega*omega --> 345 345 <field id="CMIP6_wbptemp" field_ref="dummy_XYA" /> <!-- P1 (K) wet_bulb_potential_temperature : Wet bulb potential temperature --> … … 348 348 <field id="CMIP6_ygwdparam" field_ref="dummy_XYA" /> <!-- P2 (Pa) atmosphere_northward_stress_due_to_gravity_wave_drag : Parameterised y- component of gravity wave drag --> 349 349 <field id="CMIP6_zfull" field_ref="dummy_XYA" /> <!-- P2 (m) height_above_reference_ellipsoid : Altitude of Model Full-Levels --> 350 <field id="CMIP6_zg" field_ref=" zg"/> <!-- P1 (m) geopotential_height : Geopotential height on the 1000 hPa surface -->350 <field id="CMIP6_zg" field_ref="geop" /> <!-- P1 (m) geopotential_height : Geopotential height on the 1000 hPa surface --> 351 351 <field id="CMIP6_zhalf" field_ref="dummy_XYA" /> <!-- P2 (m) height_above_reference_ellipsoid : Altitude of Model Half-Levels --> 352 352 <field id="CMIP6_zmla" field_ref="dummy_XY" /> <!-- P1 (m) atmosphere_boundary_layer_thickness : Height of Boundary Layer -->
Note: See TracChangeset
for help on using the changeset viewer.
