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Equivalent potential temperature, commonly referred to as theta-e ( θ e ) {\displaystyle \left(\theta _{e}\right)} , is a quantity that is conserved during changes to an air parcel's pressure (that is, during vertical motions in the atmosphere), even if water vapor condenses during that pressure change. It is therefore more conserved than the ordinary…
Applications, Use in estimating atmospheric stability & Usage
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temperature air potential pressure parcel equivalent water height heat displaystyle motions even would vertical vapor saturated constant stability fluid atmosphere
| Subject | Predicate | Object | Confidence | Src |
|---|---|---|---|---|
| Equivalent potential temperature | has effect | Clausius | 0.60 | section |
| Equivalent potential temperature | has effect | Clapeyron | 0.60 | section |
| Equivalent potential temperature | has effect | If | 0.60 | section |
| Equivalent potential temperature | has effect | Such | 0.60 | section |
| Equivalent potential temperature | has effect | The | 0.60 | section |
| Equivalent potential temperature | related to Formula | The | 0.60 | section |
| Equivalent potential temperature | related to Formula | Where | 0.60 | section |
| Equivalent potential temperature | related to Usage | This | 0.60 | section |
| Equivalent potential temperature | related to Usage | For | 0.60 | section |
| Equivalent potential temperature | related to Usage | North American Ice Storm | 0.60 | section |
| Equivalent potential temperature | related to Usage | Gyakum | 0.60 | section |
| Equivalent potential temperature | related to Usage | McGill University | 0.60 | section |
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