- Timestamp:
- 04/01/20 14:55:47 (4 years ago)
- File:
-
- 1 edited
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CONFIG/UNIFORM/v6/IPSLCM5A2CHT/GENERAL/PARAM/ping_nemo.xml
r4930 r5046 194 194 <field id="CMIP6_siareas" field_ref="dummy_XY" /> <!-- P2 (1e6 km2) sea_ice_area : total area of sea ice in the Southern hemisphere --> 195 195 <field id="CMIP6_sicompstren" field_ref="dummy_not_provided" /> <!-- P2 (N m-1) compressive_strength_of_sea_ice : Computed strength of the ice pack, defined as the energy (J m-2) dissipated per unit area removed from the ice pack under compression, and assumed proportional to the change in potential energy caused by ridging. For Hibler-type models, this is P (= P*hexp(-C(1-A))) --> 196 <field id="CMIP6_siconc" field_ref="iiceconc" 196 <field id="CMIP6_siconc" field_ref="iiceconc" > iiceconc*100 <field/> <!-- P1 (%) sea_ice_area_fraction : Area fraction of grid cell covered by sea ice --> 197 197 <field id="CMIP6_siconca" field_ref="dummy_XY" /> <!-- P1 (%) sea_ice_area_fraction : Area fraction of grid cell covered by sea ice --> 198 198 <field id="CMIP6_sidconcdyn" field_ref="dummy_XY" /> <!-- P2 (s-1) tendency_of_sea_ice_area_fraction_due_to_dynamics : Total change in sea-ice area fraction through dynamics-related processes (advection, divergence...) -->
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