Back to variables | Category Index
Each Output variable record corresponds to a physical parameter specification.
Link to CMIP7-AFT Data Request - Variable Changes
| Attribute | Value |
|---|---|
| branded_variable_name | zos_tavg-u-hxy-sea |
| cell_measures | area: areacello |
| cell_methods | amns-tmn (Time Mean over Sea) |
| cmip6_compound_name | Omon.zos |
| cmip6_frequency | mon |
| cmip6_tables_identifier | Omon (Monthly ocean data) |
| cmip7_compound_name | ocean.zos.tavg-u-hxy-sea.mon.glb |
| cmip7_frequency | mon |
| description | This is the effective dynamic sea level, so should have zero global area mean. It should not include inverse barometer depressions from sea ice. |
| dimensions | longitude, latitude, time |
| esm-bcv | Omon.zos |
| modelling_realm | Ocean |
| name | ocean.zos.tavg-u-hxy-sea.mon.glb |
| physical_parameter | zos (Sea Surface Height Above Geoid) |
| primary_modelling_realm | Ocean |
| processing_note | See OMDP document for details. Report on native horizontal grid as well as on a spherical latitude/longitude grid. The effective dynamic sea level as if sea ice (and snow) at a grid cell were converted to liquid seawater. The liquid-water equivalent sea surface which the liquid would have if the ice were replaced by an equal mass of sea water of the density of the surface water in its vicinity. Inverse barometer responses from sea-ice (and snow) loading are removed using equation H3 of Griffies et al, 2016 (https://doi.org/10.5194/gmd-9-3231-2016). zos is a dynamic sea level should have zero global area mean. Ocean dynamic sea level is defined by Gregory et al. (2019: [doi.org/10.1007/s10712-019-09525-z](https://airtable.com/appqRFkdpwAitEZNY/tblxLKbWgySWunrpw/doi.org/10.1007/s10712-019-09525-z) ) |
| provenance | Omon ((isd.003)) |
| region | glb |
| spatial_shape | XY-na (Global field (single level)) |
| temporal_shape | time-intv (Temporal Interval) |
| title | Sea Surface Height Above Geoid |
| type | real |
| uid | baa507f2-e5dd-11e5-8482-ac72891c3257 |