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Each Output variable record corresponds to a physical parameter specification.
| Attribute | Value |
|---|---|
| branded_variable_name | msftmz_tavg-rho-hys-sea |
| cell_methods | bzzsum-tmn (Basin Zig-Zag Zonal Sum) |
| cmip6_frequency | mon |
| cmip6_tables_identifier | Omon (Monthly ocean data) |
| cmip7_compound_name | ocean.mon.msftmz_tavg-rho-hys-sea |
| cmip7_frequency | mon |
| description | CMIP5 called this "due to Bolus Advection". Name change respects the more general physics of the mesoscale parameterizations. |
| dimensions | latitude, rho, basin, time |
| flag_-_variable_change_since_cmip6 | True |
| modelling_realm | Ocean |
| name | Omon.msftmrhompa |
| physical_parameter | msftmrhompa (Ocean Meridional Overturning Mass Streamfunction Due to Parameterized Mesoscale Advection) |
| processing_note | Function of latitude, rho, basin. For a model with a cartesian latxlon grid, this is the same as the "Ocean Y Overturning Mass Streamfunction" (msftyrhompa), which should in this case be omitted. For other models, this transport should be approximated as the transport across zig-zag paths corresponding to latitudes with spacing between latitudes appropriate to the model's resolution. CHANGE SINCE CMIP6 in Cell Methods - CMIP6:longitude: sum (comment: basin sum [along zig-zag grid path]) depth: sum time: mean CMIP7:longitude: sum (basin sum [along zig-zag grid path]) depth: sum time: mean, |
| provenance | Omon ((isd.003)) |
| spatial_shape | YB-R (Ocean basin meridional section (on density surfaces)) |
| temporal_shape | time-intv (Temporal Interval) |
| title | Ocean Meridional Overturning Mass Streamfunction Due to Parameterized Mesoscale Advection |
| type | real |
| uid | baa5b364-e5dd-11e5-8482-ac72891c3257 |