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Lesson Plan: Hurricanes
and Tornadoes
Subject: Earth and Space / Meteorology /
Storms
Classtime:Total: 3 class periods (50 minutes
each)
Grade Level: 5-12
Materials/Technology:
- a computer with adequate memory to run an Internet connection
- one computer for each group of two students (recommended)
- a server that allows access to the Internet
- basic computer skill so user can log on to the Internet
Safety, Handling, Disposal:
Close supervision is strongly recommended when students are conducting
searches on the Internet. Inappropriate sites are easy to access either
by mistake or on purpose.
Learner Outcomes:
Students should be able to:
- Explain the difference between a tornado and a hurricane.
- Explain how tornadoes and hurricanes are classified.
Problem/Purpose:
What are the differences between tornadoes and hurricanes; and how are
each of them classified?
Background/Inquiry:
The information below came from this web site:
- University at Buffalo: State University of New York: School of Engineering
and Applied Sciences: http://www.civil.buffalo.edu/wind/windinf2.html
(obsolete)
Tornadoes are spawned by thunderstorms. A variety of mechanisms
give rise to thunderstorms; therefore, storms behave somewhat differently
in the various climatological regions of the nation. All types can occasionally
become severe. A thunderstorm is officially considered severe if it produces
a tornado, winds in excess of 58 mph (26 m/s), or surface hail greater
than 0.75 inch (20 mm) in diameter.
A tornado can produce the highest wind speeds known. This swirling column
of air is usually associated with a severe thunderstorm, though its location
beneath the storm can vary. A worldwide phenomenon, tornadoes occur most
often in the United States. From 1953 through 1989, about 27,000 tornadoes
were documented in the United States. Tornadoes are concentrated in the
central half of the country and are most prevalent in parts of the states
of Texas, Oklahoma, and Kansas (though on a whole-state basis, Indiana
ranks ahead of Kansas).
Tropical cyclones. A few times each year, from early June
through October, low-pressure systems (termed tropical cyclones) form over
warm ocean waters in the tropics. Occasionally, where sea-surface temperatures
are greater than 22o C (72o F.) and when winds high
in the atmosphere are supportive, one of these systems will become more
organized and intensify to become a hurricane (wind speeds exceeding
73 mph (64 knots) or more (Anthes, 1982)).
When fully developed, a hurricane has a calm, central core, or eye,
surrounded by very strong winds concentrated in a doughnut-shaped region
of heavy rain, termed the eyewall. A pattern of rainbands, each consisting
of many thunderstorm cells, spirals inward to merge with the eyewall. These
violent tropical cyclones tend to be self-sustaining until they move either
into a region of sea-surface temperatures less than 26.5o C
(80o F) or over land. In either case, the system is cut off
from its main energy source, the warm sea surface.
The eastern and Gulf coasts of the United States are threatened by tropical
cyclones that form in the tropical Atlantic and in the Gulf of Mexico.
From 1931 through 1987, 551 tropical storms were observed in these areas;
314 of these reached hurricane status. In an average year, about four tropical
storms will make landfall in the continental United States; on average,
two of these will be hurricanes. The actual number of hurricanes per year
in the subtropical northern Atlantic, Caribbean, and Gulf of Mexico has
shown wide variability, ranging from 2 (1931, 1983) to 12 (1969).
Vocabulary List: Here.
Hypothesis:
Example: There are no major differences between tornadoes
and hurricanes.
Procedure:
- Students log onto the Internet and enter the following URL:
- Read the text and answer question #1 in the
Results/Analysissection.
*Note: The following are expected student answers:
- A large amount of warm humid air.
- Low level winds that shift directions and grow stronger just above
the ground.
- Lack of "competition" from nearby storms.
- Enter the following URL:
- After the page has completely downloaded, place the cursor over image
#1. Watch the animation and read the text to the right.
- Place the cursor over image #2. Watch the animation and read the text
to the right.
- Place the cursor over image #3. Watch the animation and read the text
to the right.
- Click on the Fujita wind damage scale rates tornadoes link (used
to classify tornadoes).
- After the page loads, click on F-0 link, then scroll to the
top of the page. This will give a description of the scale and what it
is based on. Read the descriptions of the F-0 through the F-6
classifications.
- Students log onto the Internet and enter the following URL:
- Study the image and read the text below the image.
- Click on the what hurricanes need to grow link.
- Read the text and answer question #2 in the Results/Analysis section.
*Note: The following are expected student answers:
- Ocean water above 80° F in a layer at least 200 feet deep.
- Winds coming together from different directions, which forces air upwards
over the warm water. The air up to 18,000 feet above the ocean surface
needs to be humid to supply adequate moisture.
- Upper atmosphere high pressure above the growing storm. The air in
this high flows outward which encourages more air to rise from the surface.
A hurricane´s winds are caused by the air near the ocean surface
rushing in to replace the rising air.
- Enter the following URL:
- Read the text describing the Saffir-Simpson damage potential scale
(used to classify hurricanes). Note the additional categories of atmospheric
pressure and storm surge that are not on the Fujita Tornado Scale.
- Click on a Category 1 link and read the text.
- Scroll to the top of the page and click on the Storm Surge link.
- After the page has completely downloaded, place the cursor over image
#1. Watch the animation and read the text to the right.
- Place the cursor over image #2. Watch the animation and read the text
to the right.
- Scroll down the page and read the text on storm surge. Answer question
#3 in the Results/Analysis section.
Results/Analysis:
- What three main factors are needed to form a tornado?
- What three main factors are needed to form a hurricane?
- What causes a storm surge?
- What is the Fujita wind damage scale for tornadoes based on?
- What is the Saffir-Simpson damage potential scale for hurricanes based
on?
Conclusions:
Students write a conclusion to answer the question posed in the Problem/Purpose.
Use the answers from Results/Analysis section above as a guide.
Assessments: (if included)
Compare the factors causing tornado formation to those required for a hurricane to form.
What are the major differences between the Fujita scales for tornado
damage and the Saffir-Simpson hurricane damage scale.
Integration: (if included)
Students write a report highlighting the impact of a specific storm on
people living in areas affected by them.
Reflections: Share your thoughts on this lesson with the NTEN team.
Please send an e-mail to Patti Harrison.
Extensions: (if included)
Students go to the USA Today home page and track a current hurricane or
tornado.
References/Resources: (if
included)

Credits
Contributing Teacher: Tim Tharp
NTEN Course: Internet-Based K-14 Earth
Systems Science Instruction
Instructor: Jerry Nelson
Assistant Instructor: Bill Ochs
Developing Team:
T.L. Buck Buchanan, Cathy Hensel, Patti Harrison, John Usher, Don Wilson
HTML Programmers: Christy Cousineau,
John Usher, Ching-Kwong Chia
Copyright © 1998 - 2002, National Teachers
Enhancement Network
Comments: pattih@montana.edu


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