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A wall cloud (murus or pedestal cloud) is a large, localized, persistent, and often abrupt lowering of cloud that develops beneath the surrounding base of a cumulonimbus cloud and from which tornadoes sometimes form. It is typically beneath the rain-free base (RFB) portion of a thunderstorm, and indicates the area of the strongest updraft within a storm.…
Supercell and tornado significance, Genesis & Structure
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wall cloud clouds tornadoes often storm form supercell tornado thunderstorm inflow base also precipitation may shelf typically rotating feature tornadogenesis
| Subject | Predicate | Object | Confidence | Src |
|---|---|---|---|---|
| Wall cloud | Abbreviation | Cb mur. | 1.00 | infobox |
| Wall cloud | Altitude | 500-16,000 m (2,000-52,000 ft) | 1.00 | infobox |
| Wall cloud | Appearance | A dark cloud feature that protrudes from the base of a cumulonimbus more popularly known as a wall cloud. | 1.00 | infobox |
| Wall cloud | Classification | Family C (Low-level) | 1.00 | infobox |
| Wall cloud | Genus | Cumulonimbus (heap, rain) | 1.00 | infobox |
| Wall cloud | Precipitation | Very common nearby, but not under : Rain, Snow, Snow pellets or Hail, heavy at times | 1.00 | infobox |
| Wall cloud | Species | Calvus | 1.00 | infobox |
| Wall cloud | Species | Capillatus | 1.00 | infobox |
| Wall cloud | Variety | None | 1.00 | infobox |
| Wall cloud | is a | area of the thunderstorm that is most likely to produce tornadoes | 0.90 | text |
| the QLCS above | instance of | but also occasionally with intense multicellular thunderstorms | 0.80 | text |
| the wall cloud will often be seen to be rotating | instance of | but also occasionally with intense multicellular thunderstorms | 0.80 | text |
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