First. A wall cloud is not a cumulonimbus clouds, but is a smaller cloud that extends from the base of a cumulonimbus. Tornadoes often form from wall clouds.
A shelf cloud is produce by thunderstorm outflow, resulting from rain cooled air being force downward and outward in a thunderstorm. A shelf cloud may indicate that strong straight-line winds are coming A wall cloud is found in the mesocyclone, or rotating updraft of a type of thunderstorm called a supercell. This is an indicator that a tornado may soon form.
The footwall
because it forms a layer b/w primary and secondry wall...
Serous membrane (mesothelium) forms the wall of the peritoneal cavity.
a hanging wall is the pieces or rock that that forms the upper half of a fault.
Tornadoes are produces by cumulonimbus clouds. Often a wall cloud and/or funnel cloud are seen before or during a tornado.
Tornadoes often form in a type of cumulonimbus cloud called a wall cloud. Look up what a cumulonimbus cloud looks like on Google images.
Tornadoes are produced by cumulonimbus clouds. Often a wall cloud appears near the base of a cumulonimbus before a tornado forms.
Tornadoes form in thunderstorms, which are composed of cumulonimbus clouds. Usually a tornado will form from a wall cloud that develops are the based of the cumulonimbus cloud, and will develop from a funnel cloud that comes out of the wall cloud.
A tornado usually emerges from a wall cloud, which is at the base of a cumulonimbus cloud.
Yes. Tornadoes are produced by thunderstorms, which from from cumulonimbus cloud. Usually a wall cloud and then a funnel cloud develop at the base of a cumulonimbus cloud before a tornado touches down.
A wall cloud
A wall cloud is suspended from a cumulonimbus cloud (mostly during thunderstorms). Then the wall cloud begins rotating counter-clockwise. Then a funnel cloud will drop from it.
The funnel of a tornado itself is a called a funnel cloud, though this term is usually reserved for when it does not touch the ground. The funnel cloud often emerges from a low-hanging cloud called a wall cloud, which is attatched to the base of a cumulonimbus cloud.
Signs of tornadic activity usually start with a wall cloud, which is attached to the base of a cumulonimbus cloud.
A wall cloud forms when the rotating updraft of a supercell thunderstorm, called a mesocyclone, draws in moist air and causes the moisture to condense. The wall cloud marks the strongest part of the mesocyclone.
Tornadoes develop during thunderstorms, which are associated with cumulonimbus clouds. Many will descned from a wall cloud at the base of a thunderstorm. The tornado itself may be visible as a funnel cloud.