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Why Does the Wind Blow? - An Interactive Learning Experience, Schemes and Mind Maps of Acting

Explore the physical properties that contribute to the formation of wind through hands-on activities. Learn about the coriolis effect, the sun's rays, and the role of warm and cool air in wind formation. This document also includes extension ideas and related activities for further exploration.

What you will learn

  • How does the Coriolis effect influence wind direction?
  • What physical properties contribute to the formation of wind?
  • What role does the Sun play in wind formation?

Typology: Schemes and Mind Maps

2021/2022

Uploaded on 09/27/2022

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Wind Activity 1
Why Does the Wind
Blow?
Objectives and Standards
- To learn about the physical
properties that contribute to
the formation of the wind
NSTA Standards Addressed
Content Standards
A, B, D, F, G
4-H SET Abilities Addressed
Evaluate
Observe
Communicate
Smmarize/Relate
Background
Our weather and climate are part of a closed system. The Earth is en-
veloped by the atmosphere which protects it from the harshness of the rest of
the Solar System. As such, wind is created from things that already occur in our
atmosphere, like the heating up of air masses by the Sun and the rotation of the
Earth. When the Sun shines down on Earth, it heats the air unevenly. Air tends
to get warmer along the equator and cooler near the poles because of the angle
at which the Sun’s rays hit the Earth. In this activity we look at the different
pieces of the climate puzzle that, when put together, create our winds.
CoCoRaHS Extension Ideas
Print off a copy of the United States map with the associated precipita-
tion measurements from the day from the CoCoRaHS website. Using another
source, like the internet or a television weather forecaster, plot the path of the
Jet Stream on the map of the United States. What direction does the Jet Stream
flow? What physical systems are causing the Jet Stream to flow, and what im-
pact does the Jet Stream have on the weather and climate of the United States?
Supplies Needed
- Ball (to represent globe)
- water
- flashlight
- lazy susan
- piece of cardboard 15 in
square
- scissors
- ruler
- marker
-large, lightweight trash bag
-powerful hair dryer
-cool room with high ceiling
Activity
Part 1.
1. Ask youth if the ball were a globe, where would the North Pole, South Pole and equa-
tor be. Label these on the ball with a washable marker.
2. Turn the ball so that the equator is running parallel to your body and your fingers are
on the North and South poles.
3. Ask youth where water would fall if it was poured on top of the ball. Have them pour
some water on the ball to check their answer. A cupful should be sufficient.
4. Ask what would be different if the ball was rotating when the water was poured. Have
them pour more water on the ball while it is turning to check.
5. Explain that the ball represented the globe and the water represented the air sur-
rounding the globe. When the globe is turning, it deflects air away from the equator and
toward the poles, so when you poured water on the ball, it was deflected, from wherever
it was poured, toward the poles.
6. Rotate the ball so that the North and South Poles are directly vertical, and the equator
is where your hands are grasping the ball.
7. Have someone shine the flashlight directly onto the ball, aimed at the equator, and in
exactly the same plane as the equator.
8. Ask where the sun shines most brightly; turn the ball to explain day and night, sunrise
and sunset.
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Wind Activity 1

Why Does the Wind

Blow?

Objectives and Standards

  • To learn about the physical properties that contribute to the formation of the wind NSTA Standards Addressed Content Standards A, B, D, F, G 4-H SET Abilities Addressed Evaluate Observe Communicate Smmarize/Relate Background Our weather and climate are part of a closed system. The Earth is en- veloped by the atmosphere which protects it from the harshness of the rest of the Solar System. As such, wind is created from things that already occur in our atmosphere, like the heating up of air masses by the Sun and the rotation of the Earth. When the Sun shines down on Earth, it heats the air unevenly. Air tends to get warmer along the equator and cooler near the poles because of the angle at which the Sun’s rays hit the Earth. In this activity we look at the different pieces of the climate puzzle that, when put together, create our winds. CoCoRaHS Extension Ideas Print off a copy of the United States map with the associated precipita- tion measurements from the day from the CoCoRaHS website. Using another source, like the internet or a television weather forecaster, plot the path of the Jet Stream on the map of the United States. What direction does the Jet Stream flow? What physical systems are causing the Jet Stream to flow, and what im- pact does the Jet Stream have on the weather and climate of the United States?

Supplies Needed

  • Ball (to represent globe)
    • water
  • flashlight
  • lazy susan
  • piece of cardboard 15 in square
  • scissors
  • ruler
  • marker -large, lightweight trash bag -powerful hair dryer -cool room with high ceiling

Activity

Part 1.

  1. Ask youth if the ball were a globe, where would the North Pole, South Pole and equa- tor be. Label these on the ball with a washable marker.
  2. Turn the ball so that the equator is running parallel to your body and your fingers are on the North and South poles.
  3. Ask youth where water would fall if it was poured on top of the ball. Have them pour some water on the ball to check their answer. A cupful should be sufficient.
  4. Ask what would be different if the ball was rotating when the water was poured. Have them pour more water on the ball while it is turning to check.
  5. Explain that the ball represented the globe and the water represented the air sur- rounding the globe. When the globe is turning, it deflects air away from the equator and toward the poles, so when you poured water on the ball, it was deflected, from wherever it was poured, toward the poles.
  6. Rotate the ball so that the North and South Poles are directly vertical, and the equator is where your hands are grasping the ball.
  7. Have someone shine the flashlight directly onto the ball, aimed at the equator, and in exactly the same plane as the equator.
  8. Ask where the sun shines most brightly; turn the ball to explain day and night, sunrise and sunset.

Discussion These activities illustrate some of the forces acting on wind; the Coriolis effect and the Sun’s rays. What did you notice about the two activities showing the deflection caused by rotating the Earth? Is there a force that is working on the air that allows some movement? Do you notice this force in your every day life (like spinning in a circle with a bucket full of water, riding on a merry-go-round)? Warm air weighs less, so it floats on top of cool air. When the trash bag moved, it was just acting as a place holder for the air so we could see the air actually move. The warmer the air is relative to the surrounding cool air, the faster and higher it will travel. When the Sun heats the air, it warms and moves upward, and cool air moves down to take its place. We discussed in the introduction that the equator gets more energy from the Sun, so air flows up near the equator. It gets deflected by the rotating Earth, and as it moves upward and away from the equator, it gets cooler. This deflection is the same as the one seen when we poured water on the rotating ball. This creates a big circular path called a convection cell, or Hadley cell when talking about weather.

  1. Ask students if the way you are holding the ball is exactly how the Earth sits in orbit (the answer is no; Earth is tilted about 23 degrees).
  2. Tilt the ball so that the North Pole is about 23 degrees away from vertical and have the flashlight shone on the ball again from the same angle as the first time. Discuss what is different about the areas on the ball/globe that are now lit up. Part 2.
  3. Cut a circle out of the cardboard the size of the lazy susan being used.
  4. Make a dot in the center to represent the North Pole.
  5. Place the cardboard ‘record’ on the lazy susan.
  6. Using a ruler and a marker, draw a straight line from the center of the cardboard to one edge.
  7. Turn the lazy susan counterclockwise. Using the marker, try to draw another straight line from the center to the edge as it is turning.
  8. Examine the second line and discuss what is different from the first. Part 3.
  9. Fill the trash bag with hot air using the hair dryer, then close and seal the opening.
  10. Release bag, watch it rise. Point out that warm air weighs less than cool air.
  11. Ask youth what they think will happen next (air will cool, trash bag will come back down).