
Facts
About Tornadoes
A tornado is
defined as a violently rotating column of air extending from a
thunderstorm to the ground.
The most violent tornadoes
are capable of tremendous destruction with wind speeds of 250 mph or
more. Damage paths can
be in excess of one mile wide and 50 miles long.
Once a tornado in Broken Bow,
The
The Atlantic seaboard states -
Tornado reports have only been officially collated since
1950. Prior to then, the
Weather Bureau could not mention tornadoes in forecasts for fear of
causing panic! Reports of
tornadoes since 1950 have been gathered by the National Climatic
Data Center (NCDC), based in
The most active tornado region of all is the southern part
of The Great Plains. According
to figures from the NCDC,
1.
Glazier-Higgins-Woodward
Tornadoes in April, 1947
2.
Goliad Tornado in
May, 1902
3.
4.
5.
Jarrell Tornado of
May, 1997.
The Oklahoma Tornado Outbreak of May, 1999, was the most
costly in
The Midwest and the states around the
The entire region is vulnerable - from western
The New Richmond Tornado of May, 1899 and the
The
Some areas are particular Tornado “blackspots”, such as
the
Some people mistakenly believe that tornadoes only occur
out in the countryside. This is hardly the case.
While it is true that the
plains states are the most tornado-prone places in the nation, it
should be noted that tornadoes have been reported in every
One likely reason why tornadoes are so common in the
central
or the F-2 twister in parts of
Tornadoes can occur west of the continental divide but
they are infrequent and usually relatively weak with a short
duration. Recently tornadoes
have struck the Pacific coast town of
The California Central Valley is an area of some frequency
for tornadoes, albeit of weak intensity.
More tornadoes occur in
The state with the highest number of strong tornadoes per
unit area is
Tornadoes occasionally accompany tropical storms and
hurricanes that move over land. Tornadoes are most commonly and
frequently to the right and ahead of the path of the storm center as
they come onshore.
Thunderstorms develop in warm, moist air in advance of
eastward-moving cold fronts. These
thunderstorms often produce large hail, strong winds, and tornadoes.
Tornadoes in the winter and
early spring are often associated with strong, frontal systems that
form in the Central States and move east.
Occasionally, large outbreaks of tornadoes occur with strong and
eastwardly moving weather patterns. Several
states may be affected by numerous severe thunderstorms and
tornadoes.
During the spring in the Central Plains, thunderstorms frequently
develop along a "dryline," which separates very warm, moist air to
the east from hot, dry air to the west.
Tornado-producing
thunderstorms may form as the “dryline” moves east during the
afternoon hours.
Along the front range of the Rocky Mountains, in the
·
Some tornadoes may form during the early stages of
rapidly developing
thunderstorms. This type of
tornado is most common along the front range of
the Rocky Mountains, the Plains, and the
·
Tornadoes may appear nearly transparent until dust
and debris are picked up.
·
Occasionally, two or more tornadoes may occur at the
same time.
·
Waterspouts are weak tornadoes that form over warm
water.
·
Waterspouts are most common along the
In the western
during a time when you least expect tornado development.
·
Waterspouts occasionally move inland becoming
tornadoes causing damage and injuries.
Tornado Measurement and Intensity Rating
Over time,
several scales have been developed and utilized to measure tornado
intensity and damage.
The TORRO Scale, the Beaufort Scale and the Fujita Tornado Intensity
Scale are the most widely known tornado “scoring or rating” scales
of recent times.
The most
frequently used scale is The Fujita Tornado Intensity Scale and
subsequently, the Enhanced Fujita (eFS) Scale.
While the Fujita Scale may not be a perfect system or tool
for linking damage to wind speed, it does have distinct advantages
over its predecessors and tornado intensity ratings before its
inception. The
Fujita Scale is used to rate the intensity of a tornado by examining
the damage caused by the tornado after it has passed over a man-made
structure (and/or landscape).
The scale has six (6) categories and groups tornadoes in four
(4) “families” as described below:
Gale -
Moderate Tornadoes (F-0 and F-1 Categories)
1.
Represent 69% of all tornadoes.
2.
Result in less than 5% of all tornado related deaths.
3.
Typically last from 1 – 10+ minutes.
4.
Gale category tornadoes have winds of 40 – 72 mph.
5.
Moderate tornadoes have winds reaching 73 - 112 mph.
Significant – Severe Tornadoes (F-2 and F-3 Categories)
1.
Represents 29% of all tornadoes.
2.
Result in approximately 30% of all tornado related deaths.
3.
Typically last up to 20 minutes or longer.
4.
Significant tornadoes have winds reaching 113 – 157 mph.
5.
Severe tornadoes have winds reaching 158 - 206 mph.
Devastating - Incredible Tornadoes (F-4 and F-5 Categories)
1.
Represent only 2% of all tornadoes.
2.
Result in approximately 70% of all tornado deaths.
3.
Can last up to 20 minutes or longer.
4.
Typically span miles of geography and have very unpredictable
movement patterns.
5.
Devastating tornadoes have winds reaching 207 – 260 mph.
6.
Incredible tornadoes have winds reaching 261 - 318 mph.
Inconceivable Tornadoes (F-6 Category)
1.
Generally surrounded by F-4 and F-5 gales; generally not
identifiable as a single “swirl” pattern or tornado.
2.
No known and individually recorded F-6 category tornadoes to
date.
3. Wind speed could reach 319 – 379 mph.
Understanding and Using the Fujita Scale (F-Scale)
Tornadic activity or storms may be accompanied by complex
combinations of strong downbursts and other straight line winds.
Therefore, separating tornado damage from other wind damage
makes for a daunting and difficult task for even the most
experienced surveyor or climatologist in “rating or scoring”
tornadic intensity and damage.
Tornadoes are VERY, VERY dangerous events that can be VERY,
VERY destructive dependent upon what is in their path!!
Therefore, it is important to understand thattornadoes
basically have three (3) factors that influence the Fujita Scale
rating
[1]:
1.
Loss of life.
2.
Property
damage/destruction
3.
Wind speed and
size.
The
The
The
The
There have been about 45 tornadoes since 1950 that have killed 18 or more people. In the 1950s, there were 18 tornadoes that killed 18 or more people. In the 1960s, there were 12 tornadoes that killed 18 or more people. In the 1970s, there were 11 tornadoes that killed 18 or more people. And in the 1980s, there were only 2 tornadoes that killed more than 18 people. In spite of an ever-burgeoning population, death figures continue to go down as improved forecasting, detection, communications, and public awareness increase.
|
Rank |
Affected States |
Date |
Time |
Deaths |
Injured |
F-Scale Category[1] |
Affected Towns |
Damages
(Millions) |
|
1 |
MO, IL, IN |
March 18, 1925 |
1:01 pm |
695 |
2,027 |
F-5 |
Murphysboro, Gorham & DeSoto
|
$16MM |
|
2 |
LA, MS |
May 7, 1840 |
1:45 pm |
317 |
109 |
Not Rated
|
Nachez |
$1.3MM |
|
3 |
MO, IL |
May 27, 1896 |
6:30 pm |
255 |
1,000 |
F-4 |
|
$2MM |
|
4 |
MS |
April 5, 1936 |
8:55 pm |
216 |
700 |
F-5 |
|
$3MM |
|
5 |
GA |
April 6, 1936 |
8:27 am |
203 |
1,600 |
F-4 |
|
$13MM |
|
6 |
TX, OK, KS |
April 9, 1947 |
6:05 pm |
181 |
970 |
F-5 |
Glazier, Higgins & Woodward
|
$9MM |
|
7 |
LA, MS |
April 24, 1908 |
11:45 am |
143 |
770 |
F-4 |
Amite, Pine & Purvis
|
$.5MM |
|
8 |
WI |
June 12, 1899 |
5:40 pm |
117 |
200 |
F-5 |
New
|
$.3MM |
|
9 |
MI |
June 8, 1953 |
8:30 pm |
115 |
844 |
F-5 |
|
$19MM
|
|
10 |
TX |
May 11, 1953 |
4:10 pm |
114 |
597 |
F-5 |
|
$41MM
|
Frequency Of Tornadoes
1.
In the southern states, peak tornado occurrence (season) is
March through May, while peak tornado occurrence in the northern
states are during the summer months.
2.
In some states, a secondary tornado maximum occurrence peak
occurs in the fall.
3.
Tornadoes are most likely to occur between 3 p.m. and 9 p.m. but
have been known to occur at all hours of the day or night.
4.
The average tornado moves from southwest to northeast, but
tornadoes have been known to move in any direction.
The average forward speed
is 30 mph but may vary from nearly stationary to 70 mph.
5.
The total number of tornadoes is probably higher than indicated
in the western states. This
is due primarily to sparse population resulting in reduction in
the number of actual tornadoes spotted and reported.
|
Location |
Date |
Time of Day |
# of
Tornadoes |
Deaths |
Injuries |
Damages
(in millions) |
||
|
|
|
|
|
Homes |
Other |
Total |
|
|
|
Costal |
3/28/84 |
Afternoon - evening |
22 |
21 –
mobile homes |
36 |
67 |
1,248 |
$200MM |
|
|
5/31/85 |
Late
Afternoon - evening |
27
in PA and
OH
(41 total region) |
78
in PA and
OH |
|
90
(total
region) |
1,025 |
$450MM |
|
Plains States Region |
4/26
-27/91 |
Early
morning - Afternoon
|
54 |
13 –
mobile homes |
10
-
2 in vehicles |
23
|
308 |
$277MM + |
Those
Most at Risk
·
People in automobiles
·
The elderly, very young, and the physically or mentally impaired
·
People in mobile homes
·
People who may not understand the warning due to a language
barrier
[1]
F-Scale ratings were not developed and used until 1971 with the
introduction and standardized use of the Fujita Tornado
Intensity Scale.
The table below lists the Top Ten U.S. Killer Tornadoes.
[1]
The basic Tornado Intensity factors are listed in the order of their
relative importance and use in the Fujita Scale.
The data comparing the