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The intent here is to direct you to the best tornado info available, regardless of domain. There is also a partial list of technical scientific references related to tornadoes for those with some meteorological education and training. However,...
Meteorologists also can disagree on precisely defining large, intense, messy multivortex circulations, such as the El Reno tornado of , compared to the parent mesocyclone and surrounding winds of damaging intensity. It is well-known that a tornado...
Recent theories and results from the VORTEX programs suggest that once a mesocyclone is underway, tornado development is related to temperature changes across the edge of downdraft air wrapping around the mesocyclone the occlusion downdraft. Mathematical modeling studies of tornado formation also indicate that it can happen without such temperature patterns; and in fact, very little temperature variation was observed near some of the most destructive tornadoes in history on 3 May The details behind these theories are given in several of the Scientific References accompanying this FAQ.
Does the region of the US play a role in path direction? Tornadoes can appear from any direction. Most move from southwest to northeast, or west to east. Some tornadoes have changed direction amid path, or even backtracked. This is because of an increased frequency of certain tornado-producing weather patterns say, hurricanes in south Texas, or northwest-flow weather systems in the upper Midwest. Utter silence? Not necessarily, for any of those. Rain, wind, lightning , and hail characteristics vary from storm to storm, from one hour to the next, and even with the direction the storm is moving with respect to the observer.
While large hail can indicate the presence of an unusually dangerous thunderstorm, and can happen before a tornado, don't depend on it. Hail , or any particular pattern of rain, lightning or calmness, is not a reliable predictor of tornado threat. The details are still debated by tornado scientists. We do know tornadoes need a source of instability heat, moisture, etc. There are a lot of processes around a thunderstorm which can possibly rob the area around a tornado of either instability or vorticity. One is relatively cold outflow --the flow of wind out of the precipitation area of a shower or thunderstorm. Many tornadoes have been observed to go away soon after being hit by outflow. For decades, storm observers have documented the death of numerous tornadoes when their parent circulations mesocyclones weaken after they become wrapped in outflow air--either from the same thunderstorm or a different one.
The irony is that some kinds of thunderstorm outflow may help to cause tornadoes, while other forms of outflow may kill tornadoes. Not in a literal sense, despite what you may have read in many older references, news stories, or even damage survey reports. By definition above , a tornado must be in contact with the ground. There is disagreement in meteorology over whether or not multiple ground contacts of the same vortex or funnel cloud mean different tornadoes a strict interpretation. In either event, stories of skipping tornadoes usually mean There was continuous contact between vortex and ground in the path, but it was too weak to do damage; Multiple tornadoes happened, but there was no survey done to precisely separate their paths very common before the s ; or There were multiple tornadoes with only short separation, but the survey erroneously classified them as one tornado.
That is more unusual than it seems, because most video that seems to show tornadoes merging actually involves either one tornado, or one among multiple subvortices , going behind another. On those very rare occasions when tornadoes do merge, it usually involves a larger and stronger tornado that simply draws in and absorbs the lesser circulation, then keeps on going. On 24 May , the author of this FAQ witnessed and photographed a merger of a long-lived, violent tornado with a satellite tornado that had grown about as large and strong, based on mobile Doppler-radar data. That rare and maybe unique event is documented in this formal journal paper. Tornadoes can last from several seconds to more than an hour. The longest-lived tornado in history is really unknown, because so many of the long-lived tornadoes reported from the early-mid s and before are believed to be tornado series instead.
Most tornadoes last less than 10 minutes. To oversimplify this a bit, a tornado or any other atmospheric vortex is the most efficient way to move air from one part of the atmosphere to another on its size and time scale. In fluid flow whether gas or liquid , a vortex often forms when some kind of instability exists between one part of the fluid and another, and that difference is strong enough that the fluid needs to relocate mass quickly to restore more stable conditions again. This happens on many scales, from huge midlatitude cyclones to hurricanes, supercells, tornadsoes and backyard whirlwinds--even the vortex that forms above a bathtub drain. Most thunderstorms apparently do not need a vortex as intense and efficient at moving air as a tornado, to fulfill their own function of transporting a plume of initially unstable air from the lower atmosphere to higher levels.
Why some thunderstorms go far enough to require a tornado's assistance is a matter of great speculation and debate in meteorology. For those with a strong scientific background, Chuck Doswell offers some in-depth insights on possibilities for the role of tornadoes. And how far does it drop? It varies. A barometer can start dropping many hours or even days in advance of a tornado if there is low pressure on a broad scale moving into the area.
Strong pressure falls will often happen as the mesocyclone parent circulation in the thunderstorm moves overhead or nearby. The biggest drop will be in the tornado itself, of course. It is very hard to measure pressure in tornadoes since most weather instruments can't survive. A few low-lying, armored probes called " turtles " have been placed successfully in tornadoes. This includes one deployment on 15 May by the late Tim Samaras, who recorded pressure fall of over 40 millibars through an unusually large tornado.
On 24 June , another of Tim's probes recorded a millibar pressure plunge in a violent tornado near Manchester, SD National Geographic report. On 21 April , a private storm-chase vehicle--outfitted with fully functional, scientific-grade instruments-- measured the current record pressure drop of millibars in Tulia, TX. Despite those spectacular results, and a few fortuitous passes over barometers through history, we still do not have a large database of tornado pressures to say much about averages or other barometric characteristics.
That has to be left to the world of computer simulations, using known physical characteristics of intense vortices of air. A waterspout is a tornado over water --usually of non-supercell origin. Waterspouts are common along the southeast U. Although waterspouts are always tornadoes by definition; they don't officially count in U. They are smaller and weaker than the most intense Great Plains tornadoes, but still can be quite dangerous. Waterspouts can overturn boats , damage larger ships, do significant damage when hitting land, and kill people.
The National Weather Service will often issue special marine warnings when waterspouts are likely or have been sighted over coastal waters, or tornado warnings when waterspouts can move onshore. The sense of rotation is usually the opposite. Most tornadoes but not all! Anticyclonic tornadoes clockwise-spinning in the northern hemisphere have been observed, however--usually in the form of waterspouts, non-supercell land tornadoes, or anticyclonic whirls around the rim of a supercell's mesocyclone. There have been several documented cases of cyclonic and anticyclonic tornadoes under the same thunderstorm at the same time. Anticyclonically rotating supercells with tornadoes are extremely rare; but one struck near Sunnyvale, CA , in Two clockwise tornadoes from another anticyclonic storm struck south-central Oklahoma on 10 May Remember, "cyclonic" tornadoes spin counter-clockwise in the northern hemisphere, and clockwise in the southern.
Multivortex a. When a tornado doesn't contain too much dust and debris, they can sometimes be spectacularly visible. These vortices may form and die within a few seconds, sometimes appearing to train through the same part of the tornado one after another. They can happen in all sorts of tornado sizes, from huge " wedge " tornadoes to narrow " rope " tornadoes. Subvortices are the cause of most of the narrow, short, extreme swaths of damage that sometimes arc through broader tornado tracks. From the air, they can mow down crops preferentially and stack the stubble, leaving cycloidal marks in fields. Multivortex tornadoes are the source of most of the old stories from newspapers and other media before the late 20th century that told of several tornadoes seen together at once.
Theodore Fujita developed a damage scale Fujita , Fujita and Pearson for winds, including tornadoes, which was supposed to relate the degree of damage to the intensity of the wind. This scale was the result. The original F scale should not be used anymore, because it has been replaced by an enhanced version. Tornado wind speeds are still largely inferred, or estimated; and the wind speeds on the original F scale have never been scientifically tested and proven.
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