Tornado conditions are caused when different temperatures and humidity meet to form thunderclouds. In the United States, warm, wet winds from the Gulf of Mexico move northward in spring and summer, meeting colder, dry Canadian winds moving southward. The place where these two winds meet is called a dry line. High, dry air coming from the north piles on top of low-moving, moist Gulf air at a height of over 10,000 feet. The warm southern winds try to rise, but the cold northern air blocks them. This clash causes the warm, trapped air to rotate horizontally between the two air masses. At the same time, the sun heats the earth below, warming more air that continues to try and rise. Finally, the rising warm wind become strong enough to force itself up through the colder air layer. - poptart_socks poptart_socks May 16, 2007

When this occurs, the cold air on top begins to sink, sending the rising warm wind spinning upward. The warm winds rotate faster and faster in a high column. When the updraft is strong, the column can rise to heights of 10 miles or more, twisting at speeds of up to 100 miles an hour. The rotating winds produce strong storm clouds about 70,000 feet high, sometimes spreading 10 miles wide. - poptart_socks poptart_socks May 16, 2007

This storm system may stay intact for several hours, at which point its thunderclouds are known as supercells. These storm clouds can send down an inch of rain in a mere ten minutes or shower the ground with baseball-sized hailstones. Supercells can accumulate into huge clusters, forming a line almost 100 miles long, which can then develop into mesocyclones- poptart_socks poptart_socks May 16, 2007.

Tornadoes are formed when hot air and cold air are mixed. The clouds grow larger and larger. Finally, a thunderstorm is brewed up with a strong updraft. The moisture in the warm air rises and condenses into large clouds. Tornadoes often develop from a class of thunderstorms known as supercells. Supercells contain mesocyclones, an area of organized rotation a few miles up in the atmosphere, usually 1–6 miles (2–10 km) across.- Jesse95 Jesse95 May 22, 2007