Back to variables | Category Index
Each Output variable record corresponds to a physical parameter specification.
| Attribute | Value |
|---|---|
| branded_variable_name | rlds_tpt-u-hs-u |
| cell_methods | apt-tpt (Instantaneous Point Values) |
| cmip6_compound_name | CFsubhr.rlds |
| cmip6_frequency | subhrPt |
| cmip6_tables_identifier | CFsubhr (Diagnostics for cloud forcing analysis at specific sites) |
| cmip7_compound_name | atmos.rlds.tpt-u-hs-u.subhr.GLB |
| cmip7_frequency | subhr |
| description | The surface called "surface" means the lower boundary of the atmosphere. "longwave" means longwave radiation. Downwelling radiation is radiation from above. It does not mean "net downward". When thought of as being incident on a surface, a radiative flux is sometimes called "irradiance". In addition, it is identical with the quantity measured by a cosine-collector light-meter and sometimes called "vector irradiance". In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. |
| dimensions | site, time1 |
| modelling_realm | Atmospheric |
| name | atmos.rlds.tpt-u-hs-u.subhr.GLB |
| physical_parameter | rlds (Surface Downwelling Longwave Radiation) |
| positive_direction | down |
| primary_modelling_realm | Atmospheric |
| processing_note | This table includes the 2-D variables listed in the "Amon" spreadsheet, omitting, however, the daily maximum and minimum temperatures. All variables should be reported as synoptic fields, not daily means. |
| provenance | CFsubhr ((isd.003)) |
| region | GLB |
| spatial_shape | S-na (Site (specific locations requested by CFMIP)) |
| temporal_shape | time-point (Instantaneous Value (i.e. Synoptic or Time-Step Value)) |
| title | Surface Downwelling Longwave Radiation |
| type | real |
| uid | atmos.rlds.tpt-u-hs-u.subhr.GLB |