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Tornadoes can take many shapes. Storm spotters recognize three common shapes: wedges, ropes, and stove pipes. Wedges are the largest and most powerful, and therefore usually the most dangerous. These are almost always associated with supercell thunderstorms. Ropes are smaller and usually less violent; they are easily recognized by their rope-like appearance. Stove pipes have similar width from top to bottom, usually with the entire column centered over a point on the ground. Because of their destructive power, scientific observation of tornadoes has been difficult, and they are still not fully understood. Today, tornadoes are often classified according to wind speed on the Enhanced Fujita Scale. Since it is not always possible to measure wind speed exactly in such dangerous storms, levels of destruction can be used to estimate speed. Where do tornadoes occur? In North America, most tornadoes occur in an area known as "Tornado Alley", which is the central Great Plains region of the United States. However, every state east of the Rocky Mountains is at moderate to high risk of tornado activity. This is due to the clash of contrasting air masses (cool, dry continental air meeting warm, moist maritime air) that frequently occurs over the eastern two-thirds of the United States. The states of Oklahoma and Kansas usually experience the most tornadoes per 10,000 square miles, followed by Iowa and Illinois (Florida may also experience a high number of tornadoes, but problems with reporting make this unclear). Most importantly, the greatest number of significant tornadoes (EF2 - EF5) per ten thousand miles occurs in Oklahoma, Iowa, and Indiana, respectively. States west of the Rocky Mountains are generally considered to be in a low-risk region. In April of 1974, the worst tornado outbreak in history occurred when 148 twisters touched down in 13 U.S. states and parts of Canada, killing 316 people. When do tornadoes occur? How do we cope with
tornadoes? In the United States, the National Weather Service issues tornado watches when atmospheric conditions are favorable for the formation of tornadoes and tornado warnings when a tornado appears to have formed. Doppler radar has proved to be an essential tool for detecting and studying tornadoes. A network of Severe Weather Spotters, who are citizen volunteers trained by the National Weather Service, provide critical local field observations. Currently, watches and warnings are communicated to citizens by the media (radio and television), the Internet, NOAA weather radios, and outdoor alert sirens. Improving tornado warning times through better weather forecasting continues to be one of the highest priorities of the National Weather Service. |
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