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The tropopause is the atmospheric boundary that demarcates the lowest two layers of the atmosphere of Earth – the troposphere and stratosphere – which occurs approximately 17 kilometres (11 mi) above the equatorial regions, and approximately 9 kilometres (5.6 mi) above the polar regions.
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stratosphere troposphere temperature layer atmosphere height equator cold trap potential boundary vorticity water average vertical earth tropical air vapor lapse
| Subject | Predicate | Object | Confidence | Src |
|---|---|---|---|---|
| Tropopause | is a | atmospheric boundary that demarcates the lowest two layers of the atmosphere of Earth | 0.90 | text |
| Tropopause | is a | atmospheric level where the air ceases to become cool with increased altitude and becomes dry | 0.90 | text |
| Tropopause | is a | boundary that demarcates the troposphere below from the stratosphere above | 0.90 | text |
| Tropopause | is a | first-order discontinuity surface | 0.90 | text |
| a constant potential temperature surface | instance of | the two surfaces arising from the positive and negative thresholds need to be matched near the equator using another type of surface | 0.80 | text |
| Tropopause | related to Alternative definitions | Given | 0.60 | section |
| Tropopause | related to Alternative definitions | It | 0.60 | section |
| Tropopause | related to Alternative definitions | Instead | 0.60 | section |
| Tropopause | related to Alternative definitions | PVU | 0.60 | section |
| Tropopause | related to Alternative definitions | Northern Hemisphere | 0.60 | section |
| Tropopause | related to Alternative definitions | Southern Hemisphere | 0.60 | section |
| Tropopause | related to Alternative definitions | Equator | 0.60 | section |
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