- Timestamp:
- Oct 12, 2017, 11:18:00 AM (7 years ago)
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LMDZ6/branches/IPSLCM6.0.13/DefLists/CMIP6_ping_atmos.xml
r3010 r3021 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. --> 298 298 <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. --> 299 <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. -->299 <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. --> 300 300 <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 --> 301 301 <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 --> 304 304 <field id="CMIP6_tntc" field_ref="tntc" /> <!-- P1 (K s-1) tendency_of_air_temperature_due_to_convection : Tendencies from cumulus convection scheme. --> 305 <field id="CMIP6_tntd" field_ref="d ummy_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. -->305 <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. --> 306 306 <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. --> 307 307 <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. --> 308 308 <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. --> 309 <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. -->309 <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. --> 310 310 <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 --> 311 311 <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 -->
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