What Type of Clouds Make Tornadoes?

Tornadoes form at the base of cumulonimbus clouds, especially when these clouds turn into supercell thunderstorms.

Cumulus Clouds

Tornadoes are fascinating, although frightening, weather phenomena.Tornadoes are fascinating, although frightening, weather phenomena.
The updraft of the cumulonimbus cloud causes a funnel-shaped cloud to form at the base of the cumulonimbus cloud. When this funnel touches the ground, it becomes a tornado.

The first stage of cloud formation leading to a tornado is the cumulus cloud. Cumulus clouds are the puffy, white clouds that appear often even in calm weather. They occur when warm, moist air rises and meets colder air, at which point the moisture condenses into clouds. There are several types of cumulus clouds, and cumulus congestus, or tower-like cumulus clouds, are the most likely to become cumulonimbus clouds.

Cumulonimbus Clouds

Cumulonimbus clouds form from cumulus clouds, frequently along a cold front. They are low- to middle-level clouds, tall and dense, and they are often associated with thunderstorms and lightning. Cumulonimbus clouds have a characteristic anvil shape, with a flat top due to wind shear. They can look like a huge mushroom. Lightning can descend from the flat top; this is called anvil lightning. These anvil-shaped clouds are the largest clouds in the atmosphere.

Mesocyclones

The wind shear at the top of an anvil-shaped cumulonimbus cloud can cause a convective loop of air to start spinning within the cloud. Then the updraft causes the spinning air to tilt upwards, vertically. This vertical updraft then rotates within the cloud and a mesocyclone forms. At this point, the cloud is part of a supercell thunderstorm, with high winds and frequently a lot of rain and hail.

Tornado

This cloud, with a mesocyclone within it, can become a tornado because of a phenomenon called the rear flank downdraft, or RFD. This downdraft occurs because the rain from the cloud drags the mesocyclone within the cloud down toward the ground. At this point, you can see a funnel cloud descending from the cumulonimbus cloud. When the funnel cloud touches the ground, it becomes a tornado within a few minutes. The tornado can last from a few minutes to over an hour. Eventually, the RFD cools off the warm air powering the tornado, and it diminishes in power and speed.

About the Author

Shannon Stoney holds a B.A. in English and comparative literature from Princeton University, as well as an M.F.A. in visual art from the Maine College of Art. She has been a fiber artist since 1985 and a fine artist since 1998. Stoney is also a writer and editor, with work published in magazines such as "Cite," "Spin-Off" and "Permaculture Activist."