THE EFFECT OF TOPOGRAPHY ON AIR MOVEMENT (WIND FUNNEL)

KEY CONCEPTS

  1. The shape of land can cause specific wind characteristics.
  2. Coastal area winds are produced by the warming and cooling of land and water.
  3. Air moves from areas of high-pressure to areas of low-pressure.
 

MATERIALS

  • masking tape
  • tissue paper
  • wooden stick
  • fan
  • meter stick
  • railroad board
  • bricks
  • field journal
  • (optional) QuickTime animation viewer installed on your computer.
 
 

PROCEDURE

 
 
 

Activity

  1. Discuss how winds are formed in nature and how friction can cause winds to slow down near the ground.
  2. Use the tissue paper to create a wind strip that will show the movement of wind.
  3. To do this, carefully cut the tissue paper into strips 1 cm wide and 30 cm long.
  4. Tape the strips to the edge of a wooden stick.
  5. Set the fan at the end of your table and switch it on low to simulate a light breeze.
  6. Raise the wind strip one meter from the fan and make note of the height of the windstrip.
  7. Record how high the wind elevates the strips.
  8. Use the railroad board and bricks to form a "valley."
  9. Stand the bricks in pairs and lean the railroad board against the bricks.
  10. Place the fan at the large end of the funnel.
  11. Hold the wind strip at the small opening of the "valley" at the same height as in step 5.
  12. Turn on the fan (low setting).
  13. Measure the movement of the strips. How high do they rise? Do the strips show that the valley's shape has changed the character of the winds?
  14. Record you observations.
  15. Read the description of anabastic winds (below). How does this process relate to your experiment?
  16. Increase the setting and observe the change in the wind.
  17. Record your observations.
 
 

Assessment Ideas

  • Have the students construct models of both anabastic and katabastic wind flow. Use a large sheet of butcher paper to design a model of each of the wind types. Label the wind direction using arrows.
  • Use your observations to construct a graph that illustrates the data collected at each fan setting.
  • Use a computer graphing program to make final charts.
  • Devise a plan to illustrate the difference in wind flow as the settings are increased and decreased.
 
 
 

CROSS-CURRICULAR IDEAS

  • English/Language Arts: Have the students keep a journal. Write a poem about anabastic and katabastic winds.
  • Mathematics: Calculate the atmospheric pressure range for the local area.
  • Fine Art: Make drawings to illustrate the effects of katabastic and anabastic wind on various land forms.
 
 

VOCABULARY

  • anabastic winds: are caused when the ground warms during the day and the air warms as it comes in contact with the ground. Air rises up the hillsides and thereby causes winds to blow.
  • friction: force that is caused by rubbing two surfaces against each other. This action can cause "wind" to slow down near the ground.
  • katabastic winds: are formed when the ground cools at night and the air cools as it comes in contact with the ground. This causes air to sink down the hillsides and into valleys.
  • wind: results from the movement of air from areas of high and low pressure.
 
 

SOURCE

  • Adapted from "Winds of Change" educational CD-ROM, Copyright Caltech and NASA/Jet Propulsion Laboratory