
Stratocumulus volutus
© wetterkurs.ch
The name "volutus" (Latin: rolled) describes the characteristic, elongated, tube-shaped cloud that appears to rotate around a horizontal axis. Stratocumulus volutus is a rare and spectacular cloud formation, also known as a "roll cloud." It appears as a single, elongated cylinder in the sky, completely detached from the surrounding cloud cover. This cloud often forms along gust fronts ahead of thunderstorms or through mesoscale wind phenomena such as sea breeze convergences. A well-known recurring example is the "Morning Glory Cloud" in the Gulf of Carpentaria in northern Australia.
Highlighted: all genera with which volutus occurs.
Stratocumulus volutus typically forms at the boundary between air masses of differing temperature and humidity, particularly along gust fronts ahead of approaching thunderstorm systems. Its appearance can therefore indicate imminent stronger wind gusts and possible convective weather development. In tropical coastal regions, it is often associated with nocturnal inversion and breeze circulations, in which case it carries no immediate severe weather significance. The rolling motion is generated and sustained by wind shear in the lower troposphere. In general, the sighting of a roll cloud is considered a rare meteorological phenomenon, indicative of dynamic processes within the boundary layer.