EZFlap wrote:At some point, that cold air falls out of the sky (DOWNward) so much and so fast that it starts to spin like the drain water. That's the tornado.
That would seem an easy explanation based on the life cycle of a thunderstorm and our knowledge of drains, but I don't think it's accurate and/or complete regarding actual tornado formation.
Everything I have read about tornadoes indicates that they are indeed a concentrated vortex of rising air, whether or not the funnel appears to move downward or upward in extension. I concede that downdrafts are most certainly involved, as they are always present in the vicinity of a rising air, but are peripheral to the vortex. The severe shear between downdraft and updraft contributes to the formation of the vortex as well, but the vortex itself, the funnel, is a cyclonic updraft.
I'm not just pulling this from my anus, this thread has forced me to read about tornado formation, and this is what I've learned from several NWS pages. Here's an excerpt:
NWS Flagstaff wrote:A tornado is a vortex of air rising into a cloud. As mentioned, in their early and mature stages, all thunderstorms are characterized by the updraft, which supply the storm with warm, humid air for continued growth. But, in some cases, the column of rising air can give rise to a rapidly spinning vortex, which can become a funnel cloud, or a tornado. Winds in most tornadoes blow at 100 mph or less, but in a few cases, the vortex can become a strong tornado with winds of up to 300 mph.
Often, a tornado forms along the edge of the updraft, next to the downdraft that is formed from falling precipitation and rain cooled air. As mentioned above, in severe thunderstorms the updraft and downdraft remain separate allowing for more optimal tornado generation. To keep the updraft and downdraft separate, wind shear is required. Strong tornadoes tend to form in environments where winds at all levels are not only strong, but also turn in height in a clockwise, or veering, direction. As the downdraft hits the ground, the air is forced to spread outward away from the downdraft. This air acquires spin, which under optimal conditions, can be acted on by the updraft and stretched into the cloud, developing into a funnel cloud. If this funnel cloud reaches the ground, it becomes a tornado. This is one mechanism through which tornadoes can form.
Tornadoes can form in other ways as well. One of the key questions that scientists are trying to answer about tornadoes is why updrafts in some thunderstorms become these twisting whirlwinds, while those in apparently similar thunderstorms do not. Many field studies have occurred which try to increase our knowledge of how tornadoes form.