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Cumulonimbus (from Latin cumulus 'swell' and nimbus 'cloud') is a dense, towering, vertical cloud, typically forming from water vapor condensing in the lower troposphere that builds upward carried by powerful buoyant air currents. Above the lower portions of the cumulonimbus the water vapor becomes ice crystals, such as snow and graupel, the interaction…
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cumulonimbus cloud clouds top precipitation cumulus form may lightning rain species associated capillatus 000 ft storm thunderstorms hail wind conditions
| Subject | Predicate | Object | Confidence | Src |
|---|---|---|---|---|
| Cumulonimbus cloud | Abbreviation | Cb. | 1.00 | infobox |
| Cumulonimbus cloud | Altitude | 500–16,000 m (2,000–52,000 ft) | 1.00 | infobox |
| Cumulonimbus cloud | Appearance | Dark-based storm cloud capable of impressive vertical growth. | 1.00 | infobox |
| Cumulonimbus cloud | Classification | Family D (Vertically developed) | 1.00 | infobox |
| Cumulonimbus cloud | Genus | Cumulonimbus (heap, rain) | 1.00 | infobox |
| Cumulonimbus cloud | Precipitation | Very common rain, snow, snow pellets, or hail, heavy at times | 1.00 | infobox |
| Cumulonimbus cloud | Species | Calvus | 1.00 | infobox |
| Cumulonimbus cloud | Species | Capillatus | 1.00 | infobox |
| Cumulonimbus cloud | Variety | None | 1.00 | infobox |
| wildfires | instance of | rapidly growing cloud forming from non-atmospheric heat and condensation nuclei sources | 0.80 | text |
| volcanic eruptions.Supplementary featuresAccessory cloudsArcus | instance of | rapidly growing cloud forming from non-atmospheric heat and condensation nuclei sources | 0.80 | text |
| volcanic eruptions | instance of | rapidly growing cloud forming from non-atmospheric heat and condensation nuclei sources | 0.80 | text |
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