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Global Winds

Global Winds

Assessment

Presentation

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Science

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6th Grade

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Practice Problem

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Medium

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NGSS
MS-ESS2-6, MS-ESS2-5

Standards-aligned

Created by

Barbara White

Used 21+ times

FREE Resource

9 Slides • 9 Questions

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Global Winds

Middle School
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Learning Objectives
  • Understand that global winds are created by the unequal heating of Earth's atmosphere.

  • Describe the three main atmospheric circulation cells: the Hadley, Ferrel, and Polar cells.

  • Explain how the Coriolis effect influences the direction of global winds.

  • Identify the major global wind belts, including the Trade Winds, Westerlies, and Polar Easterlies.

  • Define jet streams and explain how they are formed and affect weather.

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Key Vocabulary

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Global Winds

Planet-wide winds in large belts, caused by the unequal heating of the Earth's atmosphere by the sun.

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Coriolis Effect

The deflection of moving objects, like wind, caused by the Earth's rotation on its own axis.

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Trade Winds

Reliable winds near the equator that blow from east to west, historically used by trade ships.

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Jet Streams

Fast-moving rivers of air high in the troposphere, caused by large temperature differences between air masses.

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Westerlies

Winds in the middle latitudes that blow from west to east, moving from the subtropics toward the poles.

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Unequal Heating Causes Global Winds

  • Global winds are massive, steady streams of air that circle the Earth.

  • They are caused by the unequal heating of Earth’s atmosphere by the sun.

  • Warm air rises at the equator, creating a low-pressure zone.

  • Cooler air sinks elsewhere, creating high-pressure zones that flow to low pressure.

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Multiple Choice

What is the primary cause of large-scale global winds?

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The movement of ocean currents.

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The rotation of the Earth on its axis.

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The gravitational pull of the moon.

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The unequal heating of the Earth's atmosphere.

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The Coriolis Effect

  • Earth's rotation causes the path of winds to curve.

  • This curving phenomenon is known as the Coriolis effect.

  • Winds in the Northern Hemisphere are deflected to the right.

  • In the Southern Hemisphere, winds are deflected to the left.

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Multiple Choice

How does the Coriolis effect alter the path of winds in the Northern Hemisphere?

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It deflects them to the right, causing a curved path.

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It deflects them to the left, causing a curved path.

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It causes them to blow in a straight line from north to south.

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It stops the wind from blowing.

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Global Wind Belts and Circulation Cells

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Trade Winds (Hadley Cell)

  • These winds are found between 0o and 30o latitude.

  • They blow from the northeast to the southwest in the Northern Hemisphere.

  • Historically, sailors used these reliable winds for trade routes across the ocean.

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Westerlies (Ferrel Cell)

  • These prevailing winds are located between 30o and 60o latitude.

  • In the Northern Hemisphere, they blow from the southwest toward the poles.

  • They are responsible for moving air towards the colder polar regions.

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Polar Easterlies

  • These cold, dense winds are found from 60o latitude to the poles.

  • In the Northern Hemisphere, they travel from the northeast toward the west.

  • They are formed as cold air from the poles sinks and moves.

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Multiple Choice

Which wind belt is located between 30° and 60° latitude and is driven by the Ferrel Cell?

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The Westerlies

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The Trade Winds

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The Polar Easterlies

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The Doldrums

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Jet Streams and the Polar Front

Jet Streams

  • Jet streams are fast-moving 'rivers of air' high up in the atmosphere.

  • They are created by big temperature differences between two different air masses.

  • The strongest jet streams, called polar jets, are found near the Earth's poles.

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The Polar Front

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  • The Polar Front is a boundary where cold polar air meets warmer air.

  • This meeting of air masses often leads to cloudy and unpredictable weather conditions.

  • The polar jet stream often forms high above this specific boundary zone.

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Multiple Choice

According to the slide, what creates powerful jet streams?

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The Earth's rotation alone.

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The meeting of two circulation cells of the same temperature.

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Large temperature differences between two air masses.

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The calm winds near the equator.

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Common Misconceptions About Wind

Misconception

Correction

Wind blows in a straight line from north to south.

Earth's rotation causes winds to follow a curved path (the Coriolis effect).

Wind is just a local and short-term weather event.

Global winds are large, long-term systems that circle the planet.

Air sinks at the equator, which causes dry weather.

Warm air rises at the equator, creating a wet, low-pressure zone.

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Multiple Choice

Why are regions at the equator, a low-pressure zone, commonly associated with storms and high rainfall?

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Because high-pressure systems dominate the area.

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Because the Coriolis effect is strongest there.

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Because cool, dense air sinks and releases moisture.

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Because warm, moist air rises, cools, and condenses.

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Multiple Choice

How do the atmospheric circulation cells, like the Hadley and Polar cells, primarily determine a region's climate?

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By creating local winds that only affect coastal areas.

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By controlling whether air is generally rising (wet climate) or sinking (dry climate).

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By changing the length of days throughout the year.

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By influencing the Earth's magnetic field.

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Multiple Choice

If the Earth were to stop rotating, what would be the most significant and immediate impact on the global wind system?

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The winds would blow in straight lines between the equator and the poles.

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The winds would cease to exist entirely.

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The winds would become much stronger and more unpredictable.

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The winds would reverse their primary directions.

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Multiple Choice

Based on the global wind patterns, what would be the most effective strategy for a sailing ship trying to travel from Europe to the Caribbean (located near the equator)?

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Stay in the mid-latitudes to use the Westerlies.

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Sail north to use the Polar Easterlies.

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Sail directly west without changing latitude.

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Sail south to the tropics to use the northeast Trade Winds.

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Summary
  • Unequal heating and Earth’s rotation create large, curved wind patterns.

  • The three main wind belts are the Trade Winds, Westerlies, and Polar Easterlies.

  • Low-pressure systems bring rain, while high-pressure systems bring dry weather.

  • Jet streams are fast air currents where different air masses meet.

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Poll

On a scale of 1-4, how confident are you about the concepts covered in today's review?

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Global Winds

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