ConceptDEPRECATED
upward_air_velocity_expressed_as_tendency_of_sigma
| URI | http://vocab.nerc.ac.uk/collection/P07/current/CFSNA010/1/ | ||
|---|---|---|---|
| Within Vocab | Climate and Forecast Standard Names | ||
| Alternative Labels | |||
| Definition | 'tendency_of_X' means derivative of X with respect to time. The Lagrangian tendency of a quantity is its rate of change following the motion of the fluid, also called the 'material derivative' or 'convective derivative'. The Lagrangian tendency of sigma plays the role of the upward component of air velocity when the atmosphere sigma coordinate (a dimensionless atmosphere vertical coordinate) is being used as the vertical coordinate. If the vertical air velocity is upwards, it is negative when expressed as a tendency of sigma; downwards is positive. See Appendix D of the CF convention for information about dimensionless vertical coordinates. | ||
| Date | 2006-09-26T18:12:43 | ||
| Identifier | SDN:P07::CFSNA010 | ||
| Note | deprecated | ||
| Is Version Of | CFSNA010 | ||
| isReplacedBy | lagrangian_tendency_of_atmosphere_sigma_coordinate | ||
| version | 1 | ||
| Same As | |||
| P07 Climate and Forecast Standard Names - (2) | |||
| MMI | http://mmisw.org/ont/cf/parameter/upward_air_velocity_expressed_as_tendency_of_sigma | ||
| CF | http://vocab.nerc.ac.uk/standard_name/upward_air_velocity_expressed_as_tendency_of_sigma/ | ||
| Broader | P04:G253 |
EARTH SCIENCE > Atmosphere > Atmospheric Winds > Vertical Wind Motion | |
P64:G253 |
EARTH SCIENCE > Atmosphere > Atmospheric Winds > Vertical Wind Motion | ||
| Related | P04:G984 |
EARTH SCIENCE > Oceans > Ocean Winds > Vertical Wind Motion | |
P64:G984 |
EARTH SCIENCE > Oceans > Ocean Winds > Vertical Wind Motion | ||
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