Changeset 3020 for LMDZ6/trunk/DefLists

Timestamp:

Oct 12, 2017, 10:23:49 AM (7 years ago)

Author:

Laurent Fairhead

Message:

Rajout de quelques variables
LF

File:

• LMDZ6/trunk/DefLists/CMIP6_ping_atmos.xml (modified) (2 diffs)

LMDZ6/trunk/DefLists/CMIP6_ping_atmos.xml

@@ -297 +297 @@
    <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. -->
    <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. -->
-   <field id="CMIP6_tnhuspbl"      field_ref="dqvdf"            /> <!-- P1 (s-1) tendency_of_specific_humidity_due_to_boundary_layer_mixing : Includes all boundary layer terms including diffusive terms. -->
+   <field id="CMIP6_tnhuspbl"      field_ref="dqvdf"             > dqvdf+dqthe <!-- P1 (s-1) tendency_of_specific_humidity_due_to_boundary_layer_mixing : Includes all boundary layer terms including diffusive terms. -->
    <field id="CMIP6_tnhusscp"      field_ref="dqlscst"          /> <!-- P1 (s-1) tendency_of_specific_humidity_due_to_stratiform_clouds_and_precipitation : Tendency of Specific Humidity Due to Stratiform Clouds and Precipitation -->
    <field id="CMIP6_tnhusscpbl"    field_ref="tnhusscpbl"       /> <!-- P1 (s-1) tendency_of_specific_humidity_due_to_stratiform_cloud_and_precipitation_and_boundary_layer_mixing : Tendency of Specific Humidity Due to Stratiform Cloud and Precipitation and Boundary Layer Mixing  (to be specified only in  models which do not separate budget terms for stratiform cloud, precipitation and boundary layer schemes.  Includes all bounday layer terms including and diffusive terms.) -->
@@ -303 +303 @@
    <field id="CMIP6_tnta"          field_ref="dtdyn"            /> <!-- P1 (K s-1) tendency_of_air_temperature_due_to_advection : Tendency of Air Temperature due to Advection -->
    <field id="CMIP6_tntc"          field_ref="tntc"             /> <!-- P1 (K s-1) tendency_of_air_temperature_due_to_convection : Tendencies from cumulus convection scheme. -->
-   <field id="CMIP6_tntd"          field_ref="dummy_XYA"     /> <!-- P1 (K s-1) tendency_of_air_temperature_due_to_numerical_diffusion : This includes any horizontal or vertical numerical temperature 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 temperature budget. -->
+   <field id="CMIP6_tntd"          field_ref="dtajs"             > dtajs+dtoro+dtlif+dthin </field> <!-- P1 (K s-1) tendency_of_air_temperature_due_to_numerical_diffusion : This includes any horizontal or vertical numerical temperature 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 temperature budget. -->
    <field id="CMIP6_tntmp"         field_ref="dtphy"            /> <!-- P1 (K s-1) tendency_of_air_temperature_due_to_model_physics : Tendency of air temperature due to model physics. This includes sources and sinks from parametrized physics (e.g. radiation, convection, boundary layer, stratiform condensation/evaporation, etc.). It excludes sources and sinks from resolved dynamics and numerical diffusion not associated with parametrized physics.  For example, any vertical diffusion which is part of the boundary layer mixing scheme should be included, while numerical diffusion applied in addition to physics or resolved dynamics should be excluded.  This term is required to check the closure of the heat budget. -->
    <field id="CMIP6_tntnogw"       field_ref="dummy_XYA"        /> <!-- P2 (K s-1) temperature_tendency_due_to_dissipation_nonorographic_gravity_wave_drag : Temperature tendency due to dissipation of parameterized nonorographic gravity waves. -->
    <field id="CMIP6_tntogw"        field_ref="dtoro"            /> <!-- P2 (K s-1) temperature_tendency_due_to_dissipation_orographic_gravity_wave_drag : Temperature tendency due to dissipation of parameterized orographic gravity waves. -->
-   <field id="CMIP6_tntpbl"        field_ref="dtvdf"            /> <!-- P1 (K s-1) tendency_of_air_temperature_due_to_boundary_layer_mixing : Includes all boundary layer terms including diffusive terms. -->
+   <field id="CMIP6_tntpbl"        field_ref="dtvdf"             > dtvdf + dtthe </field> <!-- P1 (K s-1) tendency_of_air_temperature_due_to_boundary_layer_mixing : Includes all boundary layer terms including diffusive terms. -->
    <field id="CMIP6_tntr"          field_ref="tntr"             /> <!-- P1 (K s-1) tendency_of_air_temperature_due_to_radiative_heating : Tendency of Air Temperature due to Radiative Heating -->
    <field id="CMIP6_tntrlcs"       field_ref="dtlw0"            /> <!-- P1 (K s-1) tendency_of_air_temperature_due_to_longwave_heating_assuming_clear_sky : Tendency of Air Temperature due to Clear Sky Longwave Radiative Heating -->