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TORNADO DAMAGE The most widely used
method worldwide, for over three decades, was the F-scale
developed by Dr. T. Theodore Fujita. In the U.S., and probably elsewhere within
a few years, the new Enhanced F-scale
is becoming the standard for assessing tornado damage. Enhanced F-scale winds
are derived from engineering guidelines but still are only judgmental
estimates. Because: Nobody knows the "true" wind speeds at ground
level in most tornadoes, and the amount of wind needed to do similar-looking
damage can vary greatly, even from block to block or building to building,
damage rating is (at best) an exercise in educated guessing. Even experienced
damage-survey meteorologists and wind engineers can and often do disagree among
themselves on a tornado's strength. This varies from place to place; and there
are no rigid criteria. The responsibility for damage survey decisions at each NWS office usually falls on the
Warning-Coordination Meteorologist (WCM) and/or the Meteorologist in Charge
(MIC). Budget constraints keep every tornado path from having a direct ground
survey by NWS personnel; so spotter,
chaser and news accounts may be used to rate relatively weak, remote or
brief tornadoes. Killer tornadoes, those striking densely populated areas, or
those generating reports of exceptional damage are given highest priority for
ground surveys. Most ground surveys involve the WCM and/or forecasters not
having shift responsibility the day of the survey. For outbreaks and unusually
destructive events - usually only a few times a year - the NWS may support
involvement by highly experienced damage survey experts and wind engineers from
elsewhere in the country. Aerial
surveys are expensive and usually reserved for tornado events with multiple
casualties and/or massive degrees of damage. Sometimes, local NWS offices may
have a cooperative agreement with local media or police to use their
helicopters during surveys. Most of the time, this happens either with multiple-vortex tornadoes or very small,
intense single-vortex tornadoes. The winds in most of a multivortex tornado may only be strong enough to do minor damage
to a particular house. But one of the smaller embedded subvortices, perhaps
only a few dozen feet across, may strike the house next door with winds over
200 mph, causing complete destruction. Also, there can be great differences in
construction from one building to the next, so that even in the same wind
speed, one may be flattened while the other is barely nicked. For example, a
flimsy, unanchored mobile home may be obliterated
while all surrounding objects suffer little or no damage. The differences are in scale. Even though winds from the
strongest tornadoes far exceed that from the strongest hurricanes, hurricanes
typically cause much more damage individually and over a season, and over far
bigger areas. Economically, tornadoes cause about a tenth as much damage per
year, on average, as hurricanes. Hurricanes tend to cause much more overall
destruction than tornadoes because of their much larger size, longer duration
and their greater variety of ways to damage property. The destructive core in
hurricanes can be tens of miles across, last many hours and damage structures
through storm surge and rainfall-caused flooding, as well as from wind.
Tornadoes, in contrast, tend to be a few hundred yards in diameter, last for
minutes and primarily cause damage from their extreme winds. |