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In atmospheric thermodynamics, the virtual temperature ( T v {\displaystyle T_{v}} ) of a moist air parcel is the temperature at which a theoretical dry air parcel would have a total pressure and density equal to the moist parcel of air. The virtual temperature of unsaturated moist air is always greater than the absolute air temperature, however, as the…
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temperature virtual displaystyle air density parcel moist pressure vapor dry water potential atmospheric would earth's atmosphere gas partial law equation
| Subject | Predicate | Object | Confidence | Src |
|---|---|---|---|---|
| Virtual temperature | related to Purpose | Rather | 0.60 | section |
| Virtual temperature | related to Purpose | The | 0.60 | section |
| Virtual temperature | related to Purpose | This | 0.60 | section |
| Virtual temperature | related to Purpose | Temperature | 0.60 | section |
| Virtual temperature | related to Purpose | Thus | 0.60 | section |
| Virtual temperature | related to Uses | Virtual | 0.60 | section |
| Virtual temperature | related to Uses | CAPE | 0.60 | section |
| Virtual temperature | related to Uses | The | 0.60 | section |
| Virtual temperature | related to Uses | Thus | 0.60 | section |
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