Horseshoe cloud

rdf:langString Horseshoe cloud

rdf:langString A horseshoe cloud is a relatively uncommon meteorological phenomenon which manifests as a cloud in the shape of a horseshoe or inverted letter "U". They occur when a horseshoe vortex deforms a cumulus cloud. The clouds are relatively short-lived. Horseshoe vortex clouds are a form of "fair-weather" funnel cloud and are similar to the shear funnel type of funnel cloud. A March 2018 instance was explained by the United States' National Weather Service: As the updraft pushes flattish cumulus clouds up & a horizontal vortex develops from differential updraft speeds... As the vortex climbs, it's caught in the faster horizontal winds aloft, & the middle part of the vortex catches the faster speeds with the ends being slower. These clouds don't occur often because the conditions that must be met almost never occur at once.