tornadoes: how they are formed, predicted and safety

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INTER AMERICAN UNIVERSITY OF PUERTO RICO AGUADILLA CAMPUS EDUCATION AND HUMANISTIC STUDIES DEPARTMENT GEEN 2313 Professor: Dr. Marie J. Agésilas RESEARCH PAPER (Final Exam Part One) TORNADOES: HOW THEY ARE FORMED, PREDICTED AND SAFETY MELVIN SEGARRA PITRE 07DECEMBER2013

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INTER  AMERICAN  UNIVERSITY  OF  PUERTO  RICO  AGUADILLA  CAMPUS  

EDUCATION  AND  HUMANISTIC  STUDIES  DEPARTMENT  GEEN  2313  

Professor:    Dr.  Marie  J.  Agésilas            

     

               

RESEARCH  PAPER  (Final  Exam  Part  One)  

 TORNADOES:  HOW  THEY  ARE  FORMED,  PREDICTED  AND  SAFETY  

                           

     

MELVIN  SEGARRA  PITRE  07-­‐DECEMBER-­‐2013  

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Table of Contents

Introduction………………………………………………………………. 4

Section I. How Tornadoes are formed……………………………………6

A. What is a tornado? ………………………………………………….6

B. How tornadoes are formed……………………………………….....6

1. Thunderstorms and supercell thunderstorms

2. Mesocyclone

C. Geographical locations of tornado formations……………………...7

1. In the United States

a. Florida

b. Tornado Alley

2. Outside of the United States

a. Canada

b. United Kingdom

D. Tornado Classification & Scales……………………………………9

1. How tornadoes are classified.

a. Anemometer

b. Fujita Scale and Enhanced Fujita Scale

i. Creator

ii Table(s)

iii. Criteria for Classification

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Section II. Predicting/Forecasting Tornadoes……………………….14

A. Lead Time……………………………………………………....14

B. Old methods used to predict tornadoes………………………....14

1. Ground Observation/Spotters

2. Weather Balloons

C. New technology on tornado prediction…………………………16

1. Doppler Radar

i. Implementation

ii. Results

D. Effectiveness and Efficiency…………………………………….17

Section III. Safety Measures and Damage Prevention

E. State and Local Emergency Response Warnings/Procedures……….19

1. Severe Weather Watches & Warnings and how to respond to them

i. Severe weather watch and warning

ii. Tornado watch and warning

F. Safety Measures for tornadoes……………………………………23

3. Individual/Family Planning

4. Safe Rooms

a. What is a Safe Room?

b. Above Ground

c. Underground

3. General Safety Guidelines & Tips

Conclusion……………………………………………………………...25

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INTRODUCTION

Today, we observe more often the fury that Nature can bring with meteorological,

geographical and oceanographic phenomenon such as tsunamis (tidal waves),

earthquakes, volcanoes, hurricanes and tornadoes. They occur all over the world. Some

are specific to a geographical area and some can occur anywhere. Many are unpredictable

and several give few minutes or days of notice before the wrath begins. All of these have

the potential to cause mass destruction of property and the loss of life.

Doswell III (2011), states that in case of tornadoes, “people should seek the

sturdiest place of shelter they can find that can reduce the threat of flying debris”. Most

tornado related deaths are from being lifted into the air and thrown or impacted by flying

or falling debris launched through the air by tornadoes’ strong winds. To reduce injuries

and fatalities “safe rooms” are a great idea to incorporate into homes, schools and any

hard structured buildings. Safe rooms above ground work just as good as those

underground, it is only a matter of preference and whether you can afford either one.

Gary England was the first meteorologist to use Doppler radar for tornado warnings in

1981. According to him “you can have the finest radar in the world and yet you really

don’t know for sure, it’s just a piece of electronic equipment. You need to eyes on it, the

person in the field saying “yes I see a tornado; no I don’t see a tornado” (Varley, 2012).

The technology is there; it’s a matter of integrating it with the techniques we have already

used so that they complement each other. Greg Carbon, a meteorologist of 25 years

seems to agree. He says, “The ability to forecast a tornado event prior to an actual

thunderstorm forming is an ability we still don’t have” (Varley, 2012). Currently

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meteorologists are able to give limited information on tornado formation ahead of time.

The tornado remains one of the most powerful and unpredictable forces of nature.

Tornadoes have the power to lift objects weighing tons hundreds of feet into the

air and launching them miles away. They are relatively unpredictable and even the

weakest tornadoes can be extremely dangerous. We know something is not right when

the winds are calm, the skies are dark and rotating and if we’re lucky the alarms sounds

to confirm that what can potentially unfold is imminent, a tornado. Tornadoes have

occurred on almost every continent of the world, yet most people don’t know how they

are formed, how they are predicted and what safety measures to take if one occurs. That

is what this investigation is going to bring to light by lo

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SECTION I: HOW TORNADOES ARE FORMED

What is a tornado?

Tornadoes are, according to the American Meteorological Society (AMS 2012)

glossary of meteorology, “a rotating column of air, in contact with the surface, pendant

from a cumuliform cloud, and often visible as a funnel cloud/or circulating debris/dust at

the ground. They are violent windstorms whose wind power ranges anywhere from 67

miles per hour (mph) to 300+ miles per hour. They can travel anywhere between 30 and

70mph and can be as much as two miles wide.

The National Oceanic and Atmospheric and Administration’s (NOAA, 2006)

National Severe Storms Laboratory describes tornadoes as the most violent of all

atmospheric storms. As powerful and destructive as they are, a tornadoes twisting column

of air descending like a dagger from the clouds can be quite a stunning site. It makes us

wonder how these stunningly strong tornadoes are formed.

How tornadoes are formed.

To better understand the formation of a tornado we must learn what a super cell

thunderstorm is and how it leads to the formation of these super storms. A Super cell

thunderstorm is a large, long-lasting, rotating thunderstorm. To become a supercell, a

thunderstorm needs a unique combination of geographical influences. Strong winds

coming from different directions at different altitudes high above the ground, what

meteorologists call “shear”, in addition to warm moist air from the Gulf of Mexico in the

lower atmosphere meeting with colder drier air from the Rocky Mountains and

Southwestern deserts. As the warm moist air rises, called an updraft, it comes into

contact with the much colder air (downdraft), it then condenses into rain or ice crystals,

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this creates a thunderstorm cloud and the beginning of a mesocyclone (a rotating

thunderstorm). The greater the temperature difference the more energy the raising air has.

The condensation into ice crystals releases heat, which also adds to the energy level of

the storm. If the conditions are right the thunderstorm will start to rotate forming vortices

with the high probability of a powerful tornado formation shortly thereafter (Brain &

Lamb, 2000).

Geographical locations of tornado formations.

Tornadoes have occurred on almost every continent except Antarctica. Although

this may seem like a lot, not every country or city on every one of those continents has

had a tornado. There are a few parts of the world where tornadoes thrive and occur more

often than others. In the United States (U.S.) every state (not including U.S. territories)

have had at least one tornado recorded. Three-quarters of the tornadoes that happen on

Earth happen in the North America (Palmer 2013). An average of 1,253 tornadoes occurs

in the U.S. every year (NOAA, 2013). Two spots in particular in the U.S. have the most

disproportionate number of tornado formation: the state of Florida and an area

meteorologists call “Tornado Alley”, which generally runs from Texas up to North

Dakota.

Florida is the state that receives the most tornadoes per square mile (Forbes 2005)

in the United States. This is because in comparison to other tornado-prone states, Florida

is smaller and has the perfect climate for thunderstorms and a very high number of

thunderstorms occur, increasing the probability of tornado formation. Along with its

natural climate for thunderstorms, hurricanes that pass by the area also spawn tornadoes.

Florida’s peak for tornado formation is during the summer and fall months (June thru

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November) (Florida Division of Emergency Management, 2012) and tornadoes here are

usually weak EF-2 or below in force on the Enhanced Fujita scale, with an EF-3 being

the most rare of tornadoes in Florida. Florida averages 66 tornadoes per year according to

the National Oceanographic and Atmospheric Administration’s data, which averages

from 1991 to 2010. (NOAA 2013). Of those 66 tornadoes, there is an average of three (3)

fatalities and 60 injuries yearly that are directly related to tornado activity (SERCC

2007).

Tornado Alley is a tornado-prone area in the Mid-West U.S. that runs from Texas

up to North Dakota, partly covering several others states. Which states specifically

compose tornado alley is debatable, depending on the criteria used, such as intensity,

frequency, etc. The conditions in this area for the development of tornadoes are far more

consistent than in any other parts of the country. Tornadoes in this region typically

happen in late spring, between the months of April and June and occasionally the early

fall (NCDC, NOAA 2013). On average, more than one thousand tornados occur in

Tornado Alley. Texas has the most deaths from tornadoes in this region while Kansas has

the most powerful ones. Tornado fatalities are around 80 per year in tornado alley, with

nearly quadruple that amount in injuries. Of course, ¾ of all tornadoes occur in North

America, that leaves ¼ elsewhere.

The United States isn't the only place in the world where tornadoes occur.

Tornadoes also occur in the United Kingdom, Canada, Argentina, Australia and

Bangladesh. In terms of the amount of tornado occurrences the United States is at the top

of the list with more than 1,000 tornadoes a year (U.S. Tornado Climatology, 2013),

followed by Canada with an average of 100 a year and the United Kingdom with around

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33 per year (Rincon 2003). The United Kingdom has a most per land area but the

tornadoes are relatively weak compared to those in the U.S. (NOAA 2013). Bangladesh

has the most fatalities per year due to the powerful winds of the tornado, poor quality in

building construction and an extremely high population density and almost non-existent

prediction or technology. All of these areas had the same thing in common. Usually flat

land where very cool air from one part of the country encounters very moist warm air

from another part while a thunderstorm mixes these factors to create a tornado.

Tornado Classification & Scales

Experts have developed methods and scales to help accurately estimate and

classify the strength of tornado both in the U.S. and abroad.

Before 1971, tornadoes were not classified at all. It was in this year that Dr.

Tetsuya Theodore Fujita developed methods to estimate the wind speeds. He did this by

observing the destruction left behind by a tornado and developed a scale based on

damage. This became known as the Fujita Scale or F-Scale, which started to be used

worldwide. Before you can make a scale must be able to measure the wind or at least

estimate it.

To measure the speed of wind meteorologists utilize wind-measuring instruments

such as an anemometer. These are hemispherical cups mounted on a vertical shaft at

equal angles to each other and as the wind blows it rotates the cups and based on the

amount of rotations used in a mathematical equation is how the speed of wind is

determined (Oblack, 2013). Since the anemometer is a fragile instrument it was no match

for a tornadoes strong winds and would be destroyed during the pass of a tornado.

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Scientists had to come up with a way to at least estimate the strong wind speeds common

in tornadoes.

Since original F-scale had limitations, such as a lack of damage indicators, no

account for construction quality and variability, and no definitive correlation between

damage and wind speed. Dr. Fujita, in 1991, published his memoirs Mystery of Severe

Storms and which included an estimate of f-scale damage then utilizing the F-scale as a

combination of f-scales and types of structural damage. Scientists later got together with

Fujita and decided, in 2007, to implement this “enhanced” Fujita Scale in place of the

older one (National Weather Service, 2011). Table 1A & 1B show the original Fujita

Scale and the current Enhanced Fujita Scale, respectively.

Table 1A.:

Original F scale

FUJITA SCALE F Number Fastest 1/4-mile (mph) 3 Second Gust (mph)

0 40-72 45-78 1 73-112 79-117 2 113-157 118-161 3 158-207 162-209 4 208-260 210-261

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Source: Storm Prediction Center 2013

Table 1B:

Current Enhanced Fujita Scale

Source: Storm Prediction Center 2013

Along with the new wind ratings on the Enhanced Fujita Scale are the damage

criteria for different types of wind damage to objects. Table 2A lists the 28 different

criteria that are utilized when trying to accurately estimate the strength of a tornado (click

on the number to view damage details.).

Table 2A.:

Damage Indicators (Next Page)

5 261-318 262-317

ENHANCED FUJITA SCALE (EF) EF Number 3 Second Gust (mph)

0 65-85 1 86-110 2 111-135 3 136-165 4 166-200 5 Over 200

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Source: Storm Prediction Center 2013

NUMBER (Details Linked)

DAMAGE INDICATOR

1 Small barns, farm outbuildings 2 One- or two-family residences 3 Single-wide mobile home (MHSW) 4 Double-wide mobile home 5 Apt, condo, townhouse (3 stories or less) 6 Motel 7 Masonry apt. or motel 8 Small retail bldg. (fast food) 9 Small professional (doctor office, branch bank)

10 Strip mall 11 Large shopping mall 12 Large, isolated ("big box") retail bldg. 13 Automobile showroom 14 Automotive service building

15 School - 1-story elementary (interior or exterior halls)

16 School - jr. or sr. high school 17 Low-rise (1-4 story) bldg. 18 Mid-rise (5-20 story) bldg. 19 High-rise (over 20 stories) 20 Institutional bldg. (hospital, govt. or university) 21 Metal building system 22 Service station canopy 23 Warehouse (tilt-up walls or heavy timber) 24 Transmission line tower 25 Free-standing tower 26 Free standing pole (light, flag, luminary) 27 Tree - hardwood 28 Tree - softwood

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Understanding how a tornado forms and how it is classified is just the beginning.

Knowing how to predict or forecast one of these storms and the tools used to do this is

just as important and intriguing. Over the years tornado predictions have improved due to

technological advances and dedicated citizens who are willing to put themselves in harms

way to give the rest of the public advanced notice of one of natures most deadly storms.

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SECTION TWO

Predicting/Forecasting Tornadoes

Most meteorological events can be forecasted and predicted but tornadoes are one

of the few that only has minutes before it strikes. Predictions and forecasts are

occasionally done minutes before a tornado touches down and even as they are forming.

Throughout the years, methods have been devised and technological advances

have been made to give the public warnings on where a tornado might occur or where

one is currently forming so that precautionary measures are taken to avoid losses.

Lead Time

Lead-time is the time given to the public as warning of an impending severe

storm. It is those few minutes that the meteorologist gives so that the public can prepare

for severe weather. Lead-time 23 years ago, 1990, was at an average of 5.4 minutes.

Todays lead times average between 13-14 minutes. On a good day, 15 or 16-minute lead

times are possible and have occurred (Heinselman et al, 2012). With training the

population on how to spot severe weather and the advances of technology the lead times

can be enormous.

Older Traditional methods of Predicting or forecasting a tornado.

Ground Observation/Spotters

Technology 40 years ago was not as sophisticated as it is today. One of the best

methods without all the technology today was obviously ground observation by people,

also known as spotters. This is simply looking outside and observing the area for the tell

tale rotating super cells that usually spawn tornadoes. In fact, the National Weather

Service trains people, who volunteer, how to identify severe weather, specifically

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tornadoes, and report them. One such program is called SKYWARN, created in the

1970’s. A meteorologist of the National Weather Service gives the classes. They are free

and typically 2 hours long and cover various meteorological aspects of severe weather

and how to identify them (NWS SKYWARN, 2013). The National Weather Service

states “These volunteers help keep their local communities safe by providing timely and

accurate reports of severe weather to the National Weather Service” (NWS 2013).

There is no better way to confirm tornado formation than for someone to call it in

and describe the tornado, its location and direction so that it may be corroborated with

radars, weather balloons and meteorologist’s opinion. It is the most basic and reliable

form of prediction and forecasting as long as you can get the information to a person who

can send it out to the public. It does involve some serious risks for those who are

observing and reporting while the storm is forming because these spotters are usually

within the vicinity of the storms’ dangerous path.

Today, Spotters or chasers play an important role in getting the word out on when

and where there is a tornado formation. With technological advances coming in the way

of radars and satellites, combining ground observation can provide a few seconds or even

minutes that can be the difference between life or death, finding a safe spot to take cover

or being sucked into a tornadoes strong vortex and tossed hundreds of yards away.

Weather Balloons

Weather balloons have been used since the late 1930’s (National Weather Service,

2009). They are made of rubber and weigh up to 2.2 pounds (Windows to Universe team,

2008). The NOAA National Weather Service (NWS) and its upper air offices, more than

800 locations worldwide, simultaneously launch weather balloons every 12 hours or

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twice a day and utilize them to take upper air observations with radiosondes.

Radiosondes are small instrument packages that are suspended about 80 feet from a

weather balloon that is usually filled with hydrogen or helium gas. These balloons rise at

about 1000 feet per minute (300 meters/min). As the balloon rises, sensors on the

radiosonde measures atmospheric pressure, temperature, relative humidity, wind speed

and wind direction. The sensors are connected to a battery powered, 300 milliwatt or less,

radio transmitter that sends the sensor measurements to a sensitive ground-tracking

antenna. The measurements are then converted and translated into meteorological values

that meteorologists then use to forecast the weather. (National Weather Service 2009).

Weather balloons are one of the oldest methods that help to predict and forecast

weather. Over the years, the weather balloon method has proven useful and dependable.

So much that they are still in use today by scientists and meteorologists all over the

world.

New technology on tornado prediction

Doppler Radar

One of the more modern methods on tornado forecasting and prediction is the

Doppler radar. In 1973, NSSL scientists were able to identify the tornado vortex

signature pattern in Doppler radar data for the first time (National Severe Storms

Laboratory). It wasn’t until between 1988 and 1992 that the Doppler radar was fully

implemented into weather forecasting and prediction with the National Weather Service

putting up about one hundred Weather Surveillance Radars 1988 Doppler (WSR-88D) as

part of the Next Generation Radar Technology (NEXRAD) (Glahn, 2005). Doppler radar

works by sending electromagnetic pulses at raindrops, which bounce back to the radar

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and from there the radar can tell whether the raindrops are moving toward or away from

the radar and since the raindrops follow the wind it can also tell the wind direction and

speed. Doppler radars do not necessarily show you when a tornado touches down, but it

shows what is happening in the clouds, which in turn can translate to a tornado warning

by meteorologists. These radars give updates every minute, whereas older systems gave

updates every 5 minutes (University of Michigan College of Engineering, 2012).

In a video, Using Doppler Radar to Detect Tornadoes, on the University of

Michigan College of Engineering website, Frank Marsik states that Doppler radar

technology has allowed us to warn people between a whopping 5-7 minutes before a

tornado actually touches down. That’s 5-7 minutes lead-time, not including assistance

from trained spotters that observe from the ground or weather balloons that are launched

twice a day. In combination, the weather balloons daily atmospheric measurements,

Doppler radar’s 5-7 minute severe weather models and the public’s observations before a

tornado even touches down to even the moment it does gives us that 13-14 minute

preparation time for a tornado’s feared appearance (University of Michigan College of

Engineering, 2012).

The effectiveness or efficiency of the combination of these techniques and

technologies are great. From a zero minute lead time, which meant there was no warning

when a tornado struck, to a now 13-minute lead time which is enough time to gather the

family and find a place to bunker down on is a huge step in terms of effectiveness and

efficiency. It is up to the public to take these few precious minutes and use them wisely

and effectively.

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Tornadoes are an unpredictable and destructive force of nature. The public must

have a plan for when and if a tornado touches down, measures that are taken before,

during and after a tornado strikes.

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SECTION III

Safety Measures and Damage Prevention

Tornadoes can cause catastrophic destruction wherever they touch down. Sometimes

tornado warnings come too late to prepare. A lot of the injuries and deaths from

tornadoes occur because of bad decisions and having no choice in the moment the

tornado appears from the clouds. The public must have a plan and prepare before a

tornado before tornado season approaches. There are various precautions and family

plans that can serve as safety measures and prevent the loss of life and property.

Severe Weather Watches & Warnings

Television stations, radio stations, and Internet news and weather sites can all

provide information on weather in your local area. If you are in a tornado prone area

(Tornado Alley or Florida), there will most likely always be some kind of tornado status

or update from the National Weather Service during the seasons where tornadoes usually

form. These updates come in the form of severe thunderstorm watch, severe thunderstorm

warning, tornado watch and tornado warning. They might sound similar and you might

think they pretty much mean the same but specific criterion separate each of them into

their own category.

A severe thunderstorm watch means that the potential exists for the development

of thunderstorms, which may produce large hail or damaging winds (NOAA 2010). This

would mean there’s nothing to be worried about it’s just a heads up but stay vigilant for

any changes in the clouds or surroundings by observing the area and listening or

watching for updates from the NOAA’s National Weather Service. Severe thunderstorm

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warning on the other hand signifies that a severe thunderstorm is occurring or is

imminent based on Doppler radar and ground observation. When you have one of these

warnings it is time to start taking precautions.

A Tornado watch steps it up a notch indicating that a few severe thunderstorms

may have the capability of producing a tornado and conditions are likely. Again, it’s an

advisory of sorts and hints to be watchful for more inclement weather. A tornado warning

is the mother of all severe warnings meaning that a tornado has been sighted or is

imminent based on Doppler radar. At this point, sirens may be wailing nearby and you

should start putting your family plans into action immediately, take cover and brace for

impact. Tornado warnings can come anywhere from 13-14 minutes before the touchdown

of a tornado and even during or after one already forms. The only thing that will get you

through with the best results is the planning and preparation you or your family set up

prior to a tornadic event.

Individual/Family Planning

The best way to come out of any event successfully is by way of preparation prior

to it and having a backup plan in the case the initial one fails. Individual or family plans

put in place for any specific event is crucial. The Federal Emergency Management

Agency has a website (www.ready.gov) that sums up the steps for preparation. These

steps are to prepare, plan and stay informed. Preparation and planning go hand-in-hand.

These plans should include preparing a disaster supplies kit, which is simply a collection

of basic items your household may need in the event of an emergency (FEMA, 2013). It

consists of enough materials to last you for at least the next 72 hours after the emergency

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or tornado passes. Water, food, fist aid, flashlights, clothing and communication plans are

a few items of the ideal kit. The kit is only one part of the plan. You must have a

communication plan. This plan would include how you will get to safety, how the family

will communicate during and after the emergency, pre-arranged meeting areas in the case

of separation and how they will react with each different situation. The plan also can

include what precautions you will take in places the family can possibly spend time

together such as sporting events, schools, daycare, work etc. (FEMA, 2013). Once you

have prepared a plan prior to a tornado all you need to do now is keep yourself and your

family informed on the current weather or emergency situation. Listen to NOAA Weather

Radio, local news weather forecasts or the watches of warnings issued by the National

Weather Service for any changes in the weather and any advice they may give for the

imminent inclement weather that will be arriving.

Safe Rooms

Another part of the preparation that plays an important role is the construction of

some kind of room or shelter within the home that can withstand the winds and debris

that strong tornadoes unleash.

According to FEMA (2013), a safe room is “a hardened structure specifically

designed to meet the Federal Emergency Management Agency (FEMA) criteria and

provide "near-absolute protection" in extreme weather events, including tornadoes and

hurricanes”. Edwards (2013) of the Storm Prediction Center of the National

Oceanographic and Atmospheric Administration defines safe rooms as “reinforced small

rooms built in the interior of a home, which are fortified by concrete and/or steel to offer

extra protection against tornadoes, hurricanes and other severe windstorms” Safe rooms

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can be built above ground or underground. They must be built to withstand high winds

and flying debris, even if the rest of the residence is severely damaged or destroyed.

Above ground/in-house safe rooms include the basement, existing rooms within

the home such as closets and bathrooms or a room separate from the rest of the house.

One of the advantages of the indoor safe rooms is its accessibility from within the home.

It eliminated the possibility of traveling to another spot utilizing the valuable time you

have and possible getting struck by flying debris. The safe rooms in homes can double up

to be a walk-in closet or even a master bathroom. These rooms are usually built with

reinforced concrete or reinforced masonry on a concrete slab, which is stable enough to

withstand what a tornado has to offer (Baxter, 2009). If it has any openings they must be

able to withstand strong winds and debris flying at a high rate of speed, the test that the

FEMA utilizes is a 15-pound 2x4 piece of wood launched horizontally at 100 miles per

hour. The one most important factor that people have when considering a safe room is the

cost. One must be willing to pay a hefty sum since the materials that are used are the

most solid and stable that comes. The cost of constructing a safe room with the

dimensions of 8’ x 8’ x 8’ in a residential home or small business is approximately

$6,600 to $8,700 (FEMA, 2013). For a larger size that would be appropriate for a school

or large business, 16’ x 16’ x 8’ would coast an approximate $12,000-$16,000.

Underground safe rooms are another alternative to the above ground/in-house

option. It can either be in an in-house reinforced basement, which is already underground

or a pre-fabricated container/room or constructed completely from scratch apart from the

house and have the area dug up to fit the room. Construction of these would be the same

as an above ground safe room. Underground safe rooms must be able to undergo pressure

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limits from being underground and the saturation that comes with rains from these

windstorms. Underground spots also can’t be constructed in any areas prone to flooding

or soft soil. Engineer studies indicate that the safety potential of shelters depend on

features such as the quality of materials used and the quality of the construction work

(Merrell et al, 2002).

With or without a safe house you still need to know how to protect yourself and

what to do when a tornado touches down. Safety is paramount and needs to be practiced

at all times during an emergency such as a tornado.

General Safety Guidelines and Tips

As with any emergency or storm, general safety measures are recommended to

reduce injuries and fatalities. The safest place to be is an underground shelter, basement

or safe room (American Red Cross, n.d.). Stay low and always protect your head. Wear a

helmet, with your hands, hiding under something strong and sturdy and by any means. In

the  Birmingham/ Tuscaloosa tornado of April 27, 2011 twenty two percent of the

approximate 340 killed, died of a traumatic brain injury (Metcalfe, 2013).

One safety tip that almost always should be taken is to stay away from windows

or glass. These tend to break with the wind pressure from the outside and the difference

on the inside. Flying debris can easily knock them out sending glass and more debris into

you. Do not stay in a mobile home or inside of a vehicle. Tornadoes can toss them like

salad in a salad bowl since they are not anchored permanently and you can end up being

projected out of your vehicle even if you’re properly secured. Go to your nearest shelter.

If shelter is nowhere in sight, find the lowest part of the land, away from trees and lay

face down covering your head with your hands until the tornado passes. Taking shelter

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under bridges is not a good shelter spot since the tornadoes winds can act like a vacuum

or debris can still get pushed under trapping you. If you are in any building, get to the

lowest floor possible. In the event of a collapse or in the case you have to evacuate it is a

lot easier than jumping or falling from a 5th floor.

There are countless other tips and guidelines for safety. Choose what is best for

your situation under the circumstances. Most important of all, don’t panic. Have a plan,

practice it and be prepared to execute it.

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Conclusion

Tornadoes are indeed one of the world’s most dangerous and feared storms. It is

one of the most unpredictable forces of nature. Warm moist air collide with the cool and

dry air from Canada and create a rotation, that given the perfect circumstances, can create

a monster of a wind storm that appears out of the sky almost magically. Scientists and

meteorologists have studied tornadoes and how they form. Although some aspects of its

formation still remains a mystery, a lot has been discovered and used as an advantage.

From the very first tornado ground observations to the first Doppler radar used for

tornado forecasting to the weather balloons and satellites. We have come a long way in

predicting & forecasting tornadoes. From a minus 2 minute warning to a whopping

thirteen minute notice prior to a tornado touching down we have seen that technology and

bravery have played an important role as radars and satellites paired with daring storm

spotters/chasers give us those few valuable minutes to prepare or move away from the

tornado’s imminent arrival.

For anyone in a tornado prone area such as Tornado Alley and Florida, safety

measures are highly important. Safety and survival steps taken prior to the tornado season

are just as important as those steps taken during one. Family plans or individual plans can

be the difference between panic and disorder and an organized, calm family. It can also

be the difference between life and death.

Understanding how a tornado is formed, how they are detected or forecasted and

what safety measures to take is the best combination to you could follow. Whether it is

safe rooms, a survival kit or a family plan, knowledge or information, preparation and

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vigilance is the key to surviving a tornado strike anytime, anywhere with minimum

damage to property and lives.

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American Meteorological Society. (2012) Glossary of Meteorology. Retrieved from http://glossary.ametsoc.org/wiki/Tornado.

American Red Cross. (n.d.). Tornado Safety. American Red Cross. Retrieved

from http://www.redcross.org/prepare/disaster/tornado Baxter, K. (2009). FEMA Extreme Wind Safe Room Guidelines. Federal Emergency

Management Agency. Retrieved from http://www.norman.noaa.gov/nsww/talks/004_thu_baxter.pdf

Brain, M., & Lamb, R. (2000). HowStuffWorks "How Tornadoes Work". HowStuffWorks

"Science". Retrieved September 2, 2013, from http://science.howstuffworks.com/nature/climate-weather/storms/tornado.htm

Edwards, R. (2013). The online tornado FAQ. Storm Prediction Center of the National

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Edwards, R. (n.d.). Tornado Safety (Online Tornado FAQ). NOAA/NWS Storm

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Prediction Center. Retrieved from http://www.spc.noaa.gov/faq/tornado/safety.html

FEMA. (2011). Frequently Asked Questions: Tornado/Hurricane Safe Rooms. Federal

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FEMA. (2013). Make a plan. Ready.gov. Retrieved from http://www.ready.gov/make-a-

plan FEMA. (2013). Make a kit. Ready.gov. Retrieved from http://www.ready.gov/build-a-kit Baird, S. L., & Ritz, J. M. (2001). Weathering Storms--Designing Safe Rooms.

Technology Teacher, 60(6), 22. Florida Division of Emergency Management. (2012). Tornadoes. Florida Disaster.org.

Retreived from http://www.floridadisaster.org/EMTOOLS/Severe/tornadoes.htm. Glahn, Bob. (2005). Tornado Warning performance in the past and future- Another

Persepective. Bulletin of Meteorological Society. 86(8). P 1135-1141. Doi: http://dx.doi.org/10.1175/BAMS-86-8-1135

Heinselman, P. L., LaDue, D. S., & Lazrus, H. (2012). Exploring impacts of rapid-scan

radar data on NWS warning decisions. Weather amd Forecasting, 27(4), 1031-1044.

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radar data on NWS warning decisions. Weather forecasting, 27(4), 1031-1044. doi: http://dx.doi.org/10.1175/WAF-D-11-00145.1.

Merrell, D., Simmons, K.M., Sutter, D. (2002). Taking shelter: Estimating the safety

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Metcalfe, J. (2013). Doctors Now Advise Wearing Helmets During Tornado Warnings.

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The Atlantic Cities. Retrieved from http://www.theatlanticcities.com/arts-and-lifestyle/2013/04/looking-injuries-caused-massive-tornado/5383/

National Weather Service/ (2011). What is a supercell? National Weather Service

Weather Forecast Office. Retrieved from http://www.srh.noaa.gov/ama/?n=supercell

National Weather Service. (2011). The enhanced Fujita scale (EF scale). National

Oceanic and Atmospheric Administration. Retrieved from http://www.spc.noaa.gov/efscale/

NOAA. (2010). Severe weather watches vs. warnings. Eastern Regional Headquarters.

Retrieved from http://www.erh.noaa.gov/box/watchvswarn.html NOAA 200th: Foundations: Severe Weather Watches and Warnings: Tornado

Classification System. (2006). NOAA Celebrates 200 Years of Science, Service and Stewardship. Retrieved August 26, 2013, from http://celebrating200years.noaa.gov/foundations/severe_weather/side_tornado.html

NSSL: Severe Weather 101: Tornadoes. (n.d.). NOAA's National Severe Storms

Laboratory. Retrieved August 26, 2013, from http://www.nssl.noaa.gov/education/svrwx101/tornadoes/

NWS SKYWARN. (2013). NWS SKYWARN. Retrieved from

http://www.nws.noaa.gov/skywarn/ Oblack, M. (2013). Anemometer - A Weather Guide Definition. About.com. Retrieved

from http://weather.about.com/od/a/g/anemometer.htm Simmons, K. M., & Sutter, D. (2005). WSR-88D Radar, Tornado Warnings, And

Tornado Casualties. Weather and Forecasting, 20(3), 301-310. doi: http://dx.doi.org/10.1175/WAF857.1

Storm Prediction Center. (2013). Enhanced F scale for tornado damage. National

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Supercell Thunderstorms: thunderstorms with deep rotating updrafts. (n.d.). WW2010 (the weather world 2010 project):. Retrieved September 2, 2013, from http://ww2010.atmos.uiuc.edu/(Gh)/guides/mtr/svr/type/spr/home.rxml

Tornadoes | Ready.gov. (n.d.). Home | Ready.gov. Retrieved September 2, 2013, from

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University of Michigan College of Engineering. (2012). Using Doppler Radar to detect

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U.S. Tornado Climatology. (2013). Tornado Climatology. Retrieved from

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