Changeset 3159

Timestamp:

Jan 22, 2018, 3:54:23 PM (6 years ago)

Author:

Laurent Fairhead

Message:

Update to ping file
OB

Location:

LMDZ6/trunk/DefLists

Files:

• CMIP6_ping_aerosol.xml (modified) (1 diff)
• CMIP6_ping_atmos.xml (modified) (1 diff)

LMDZ6/trunk/DefLists/CMIP6_ping_aerosol.xml

@@ -35 +35 @@
    <field id="CMIP6_c3h8"          field_ref="dummy_XYA"        /> <!-- P1 (mol mol-1) mole_fraction_of_propane_in_air : C3H8  volume mixing ratio -->
    <field id="CMIP6_ccn"           field_ref="dummy_XY"         /> <!-- P1 (m-3) number_concentration_of_cloud_condensation_nuclei_at_stp_in_air : proposed name: number_concentration_of_ambient_aerosol_in_air_at_liquid_water_cloud_top -->
-   <field id="CMIP6_cdnc"          field_ref="scdnc"        /> <!-- P1 (m-3) number_concentration_of_cloud_liquid_water_particles_in_air : Cloud Droplet Number Concentration in liquid water clouds. -->
+   <field id="CMIP6_cdnc"          field_ref="scdnc"> @scdnc / @lcc3d        </field> <!-- P1 (m-3) number_concentration_of_cloud_liquid_water_particles_in_air : Cloud Droplet Number Concentration in liquid water clouds. -->
    <field id="CMIP6_ch3coch3"      field_ref="dummy_XYA"        /> <!-- P1 (mol mol-1) mole_fraction_of_acetone_in_air : CH3COCH3  volume mixing ratio -->
    <field id="CMIP6_ch4"           field_ref="dummy_XYA"        /> <!-- P1 (mol mol-1) mole_fraction_of_methane_in_air : CH4 volume mixing ratio -->

LMDZ6/trunk/DefLists/CMIP6_ping_atmos.xml

@@ -191 +191 @@
    <field id="CMIP6_psl"           field_ref="slp"              /> <!-- P1 (Pa) air_pressure_at_sea_level : Sea Level Pressure -->
    <field id="CMIP6_rainmxrat"     field_ref="dummy_not_provided"        /> <!-- P2 (1.0) mass_fraction_of_rain_in_air : Rain mixing ratio -->
-   <field id="CMIP6_reffcclwtop"   field_ref="dummy_XY"         /> <!-- P1 (m) effective_radius_of_convective_cloud_liquid_water_particle_at_liquid_water_cloud_top : 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. -->
-   <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). -->
+   <field id="CMIP6_reffcclwtop"   field_ref="dummy_not_provided"         /> <!-- P1 (m) effective_radius_of_convective_cloud_liquid_water_particle_at_liquid_water_cloud_top : 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. -->
+   <field id="CMIP6_reffclic"      field_ref="dummy_not_provided"  /> <!-- 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). -->
    <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). -->
-   <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. -->
-   <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. -->
+   <field id="CMIP6_reffclwc"      field_ref="dummy_not_provided"  /> <!-- 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. -->
+   <field id="CMIP6_reffclws"      field_ref="reffclws">@reffclws / @lcc3dstra </field> <!-- 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. -->
    <field id="CMIP6_reffgrpls"     field_ref="dummy_XYA"        /> <!-- P2 (m) effective_radius_of_stratiform_cloud_graupel_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). -->
    <field id="CMIP6_reffrainc"     field_ref="dummy_XYA"        /> <!-- P2 (m) effective_radius_of_convective_cloud_rain_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). -->
    <field id="CMIP6_reffrains"     field_ref="dummy_XYA"        /> <!-- P2 (m) effective_radius_of_stratiform_cloud_rain_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). -->
-   <field id="CMIP6_reffsclwtop"   field_ref="dummy_XY"         /> <!-- P1 (m) effective_radius_of_stratiform_cloud_liquid_water_particle_at_liquid_water_cloud_top : 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. -->
+   <field id="CMIP6_reffsclwtop"   field_ref="reffclwtop"> @reffclwtop / @lcc </field> <!-- P1 (m) effective_radius_of_stratiform_cloud_liquid_water_particle_at_liquid_water_cloud_top : 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. -->
    <field id="CMIP6_reffsnowc"     field_ref="dummy_XYA"        /> <!-- P2 (m) effective_radius_of_convective_cloud_snow_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). -->
    <field id="CMIP6_reffsnows"     field_ref="dummy_XYA"        /> <!-- P2 (m) effective_radius_of_stratiform_cloud_snow_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). -->