Changeset 3681 for CONFIG/UNIFORM

Timestamp:

03/22/18 18:46:39 (6 years ago)

Author:

cetlod

Message:

Removing duplicated variables in ping_nemo

File:

• CONFIG/UNIFORM/v6/IPSLCM6/GENERAL/PARAM/ping_nemo.xml (modified) (2 diffs)

CONFIG/UNIFORM/v6/IPSLCM6/GENERAL/PARAM/ping_nemo.xml

@@ -206 +206 @@
    <field id="CMIP6_zostoga"       field_ref="scsshtst" />       <!-- P1 (m) global_average_thermosteric_sea_level_change : There is no CMIP6 request for zosga nor zossga. -->
 <!-- for variables which realm equals one of _seaIce-->
-   <field id="CMIP6_fsitherm"      field_ref="dummy_XY"         /> <!-- P1 (kg m-2 s-1) water_flux_into_sea_water_due_to_sea_ice_thermodynamics : computed as the sea ice thermodynamic water flux into the ocean divided by the area of the ocean portion of the grid cell. -->
-   <field id="CMIP6_hfsifrazil"    field_ref="dummy_XYO"        /> <!-- P1 (W m-2) heat_flux_into_sea_water_due_to_freezing_of_frazil_ice : Heat Flux into Sea Water due to Frazil Ice Formation -->
-   <field id="CMIP6_hfsifrazil2d"  field_ref="dummy_XYO"        /> <!-- P1 (W m-2) heat_flux_into_sea_water_due_to_freezing_of_frazil_ice : Heat Flux into Sea Water due to Frazil Ice Formation -->
-   <field id="CMIP6_sfdsi"         field_ref="dummy_XY"         /> <!-- P1 (kg m-2 s-1) downward_sea_ice_basal_salt_flux : This field is physical, and it arises since sea ice has a nonzero salt content, so it exchanges salt with the liquid ocean upon melting and freezing. -->
    <field id="CMIP6_siage"         field_ref="iceage"            /> <!-- P1 (s) age_of_sea_ice : Age of sea ice -->
    <field id="CMIP6_siareaacrossline" field_ref="transport_siarea_transect"        /> <!-- P2 (m2 s-1) siareaacrossline : net (sum of transport in all directions) sea ice area transport through the following four passages, positive into the Arctic Ocean 1. Fram Strait = (11.5W,81.3N to (10.5E,79.6N) 2. Canadian Archipelego = (128.2W,70.6N) to (59.3W,82.1N) 3. Barents opening = (16.8E,76.5N) to (19.2E,70.2N) 4. Bering Strait = (171W,66.2N) to (166W,65N) -->
@@ -299 +295 @@
    <field id="CMIP6_sndmasswindrif" field_ref="dummy_XY"         /> <!-- P2 (kg m-2 s-1) sndmasswindrif : the rate of change of snow mass through wind drift of snow (from sea-ice into the sea) divided by grid-cell area -->
    <field id="CMIP6_snmassacrossline" field_ref="transport_snmasse_transect"        /> <!-- P2 (kg s-1) snmassacrossline : net (sum of transport in all directions) snow mass transport through the following four passages, positive into the Arctic Ocean 1. Fram Strait = (11.5W,81.3N to (10.5E,79.6N) 2. Canadian Archipelego = (128.2W,70.6N) to (59.3W,82.1N) 3. Barents opening = (16.8E,76.5N) to (19.2E,70.2N) 4. Bering Strait = (171W,66.2N) to (166W,65N) -->
-   <field id="CMIP6_vsfsit"        field_ref="dummy_XY"         /> <!-- P1 (kg m-2 s-1) virtual_salt_flux_into_sea_water_due_to_sea_ice_thermodynamics : This variable measures the virtual salt flux into sea water due to the melting of sea ice. It is set to zero in models which receive a real water flux. -->
 <!-- for variables which realm equals one of _ocean_seaIce_ocnBgchem-->
    <field id="CMIP6_arag"          field_ref="dummy_XYO"        /> <!-- P2 (mol m-3) mole_concentration_of_aragonite_expressed_as_carbon_in_sea_water : Sum of particulate aragonite components (e.g. Phytoplankton, Detrital, etc.) -->