air_pseudo_equivalent_temperature
The pseudoequivalent temperature is also known as the adiabatic equivalent temperature. It is the temperature that an air parcel would have after undergoing the following process: dry-adiabatic expansion until saturated; pseudoadiabatic expansion until all moisture is precipitated out; dry-adiabatic compression to the initial pressure. Reference: AMS Glossary http://glossary.ametsoc.org/wiki/Equivalent_temperature. This quantity is distinct from the isobaric equivalent temperature, also known as equivalent temperature, which has the standard name air_equivalent_temperature. It is strongly recommended to include a units_metadata attribute.
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Proposls with this term version:
Proposal: Beate Geyer/Ronny Petrik [New description for pseudo_equivalent_te]
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Proposls with this term version:
Proposal: Beate Geyer / Ronny Petrik [New description for pseudo_equivalent_te]
This term is not aliased.
