Tornado
Classification
Dr. Theodore Fujita, a renowned severe weather researcher at the University of Chicago,
developed a scheme for rating tornadoes based on their intensity. His scale, called the F scale, gives tornadoes a numerical rating from
F0 to F5. F0 and F1 tornadoes are considered "weak" tornadoes, F2 and F3
tornadoes are classified as "strong" tornadoes, and F4 and F5 tornadoes are
categorized as "violent" tornadoes. Table 4 summarizes the
Fujita scale.
FUJITA DAMAGE SCALE
| F0 |
Gale Tornado |
weak |
40-72 mph |
| F1 |
Moderate Tornado |
weak |
73-112 mph |
| F2 |
Significant Tornado |
strong |
113-157 mph |
| F3 |
Severe Tornado |
strong |
158-206 mph |
| F4 |
Devastating Tornado |
violent |
207-260 mph |
| F5 |
Incredible Tornado |
violent |
261-318 mph |
Table 4: The Fujita tornado damage scale.
The F scale is based on tornado damage (primarily to buildings), so there is some
ambiguity in the scale. For example, a tornado which moves over open country will tend to
receive a lower rating than a tornado which strikes a populated area. Since buildings have
a wide variation in age, quality of design, and quality of building materials, more
uncertainties are thrown into the mix. Tornadoes over open country will probably encounter
varying types of vegetation, leading to uncertainties in these cases. Still, the Fujita
scale provides a good baseline for classifying tornadoes according to their intensities.
Tornado/Funnel Cloud Look-Alikes
Experienced spotters are probably aware that a number of features (both natural and
man-made) can bear a resemblance to a tornado or funnel cloud. Some of these natural
features include rain shafts and scud clouds. Some of the man-made features include smoke
from oil flares and factories. If a suspicious-looking cloud formation is observed, watch
it for a minute or two. Look for organized rotation
about a vertical or near-vertical
axis. Figure 34 depicts a number
of tornado look-alikes.

Figure 34(a): Some tornado/wall cloud look-alikes. Scud clouds. |

Figure 34(b): Rain shaft. Photos - NWS, NSSL.
|
Another phenomenon which must be discussed is the gustnado.
Gustnados are small vortices which sometimes form along a gust front (figure
35). Gustnados are generally not associated with the updraft area of the storm and do
not originate in mesocyclones, so in some ways they are not "legitimate"
tornadoes. They can cause damage to lightweight structures and are hazardous to people in
the open, though, so they do pose a threat and should be reported to the
controller/dispatcher.

Figure 35: Gustnados are small vortices which sometimes form along strong
gust fronts. View is to the southwest. Photo - Charles Doswell III. |
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