Begrepsinformasjon
Anbefalt term
air_equivalent_temperature
Definisjon
- The equivalent temperature is the temperature that an air parcel would have if all water vapor were condensed at contstant pressure and the enthalpy released from the vapor used to heat the air. Reference: AMS Glossary http://glossary.ametsoc.org/wiki/Equivalent_temperature. It is the isobaric equivalent temperature and not the adiabatic equivalent temperature, also known as pseudoequivalent temperature, which has the standard name air_pseudo_equivalent_temperature.
Note
- Mapping to be determined
URI
https://vocab.met.no/CFSTDN/air_equivalent_temperature
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