Earth Science Grade 9-12

Earth Science: The Coriolis Effect and Global Wind Patterns

How Earth's rotation shapes winds and circulation cells

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How Earth's rotation shapes winds and circulation cells

Earth Science - Grade 9-12

Instructions: Read each problem carefully. Use complete sentences when explaining your reasoning. Show any sketches or labels in the space provided.
  1. 1
    Earth rotating with an air parcel path shown curving due to rotation.

    Explain why the Coriolis effect occurs on Earth. Include the role of Earth's rotation in your answer.

  2. 2
    Globe showing opposite Coriolis deflection in the two hemispheres.

    State the direction that moving air is deflected by the Coriolis effect in the Northern Hemisphere and in the Southern Hemisphere.

  3. 3
    Air moving north from the equator curves to the right in the Northern Hemisphere.

    A wind begins moving directly north from the equator into the Northern Hemisphere. Describe how its path will appear to curve and explain why.

  4. 4
    Global wind belts shown as colored latitude bands with directional arrows.

    Name the three main global wind belts in each hemisphere and give the approximate latitude range for each one.

  5. 5
    Northern Hemisphere trade winds curving from subtropics toward the equator.

    The trade winds in the Northern Hemisphere generally blow from the northeast toward the southwest. Explain how pressure belts and the Coriolis effect combine to create this wind direction.

  6. 6
    Surface winds spiral inward counterclockwise around a low-pressure center.

    Complete this comparison: A low-pressure system in the Northern Hemisphere has surface winds that spiral in which direction, and why?

  7. 7
    Coriolis deflection appears weaker near the equator and stronger near the poles.

    Why is the Coriolis effect weakest at the equator and strongest near the poles?

  8. 8
    Hadley cell with rising equatorial air, sinking subtropical air, and surface trade winds.

    Describe the Hadley cell. Include where air rises, where it sinks, and how it helps form the trade winds.

  9. 9
    Dry sinking air in the subtropics creates clear conditions over desert regions.

    At about 30 degrees latitude, many deserts are found, such as the Sahara and Australian deserts. Explain how global circulation contributes to dry conditions there.

  10. 10
    Prevailing westerly winds shown moving from west toward east across a midlatitude band.

    Explain the difference between a wind's direction of movement and the name of the wind. Use the prevailing westerlies as an example.

  11. 11
    Weather balloon carried eastward by prevailing westerlies in the Northern Hemisphere.

    A weather balloon is released at 45 degrees north latitude and moves with the prevailing westerlies. In what general direction will it likely travel, and what global wind belt is affecting it?

  12. 12
    Unlabeled model of Northern Hemisphere atmospheric circulation cells and surface wind belts.

    Draw or describe a labeled model of global atmospheric circulation from the equator to the North Pole. Include the Hadley, Ferrel, and Polar cells, plus the major surface wind belts.

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