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A lesson for your classroom or geography club

Ocean currents

All teacher notes · Open the lab

Start projector

False-colour MODIS brightness-temperature image showing the Gulf Stream and warm eddies in the North Atlantic.
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MODIS, 2 May 2001: thermal contrast traces the Gulf Stream and eddies. Brightness temperature includes the sea surface and overlying moist atmosphere.

A suggested lesson sequence

Use these stages at your own pace. Pause for students to sketch, compare observations or lead part of the demonstration.

  1. 01

    Observe

    Select North Atlantic and identify its western and eastern boundaries. Follow the arrows and name Gulf Stream and Canary Current.

    Open Observe
  2. 02

    Tinker

    Compare South Atlantic and explain the reversed sense of rotation. Locate all five subtropical gyres.

    Open Tinker
  3. 03

    Explain

    How do winds, Earth’s rotation and ocean-basin boundaries help organise the major surface gyres?

    Open Explain
  4. 04

    Check

    Choose an answer and explain your reasoning. Each question includes feedback.

    Open Check

Rehearse with the model

The same scene and controls as the lab. Load it when you are ready; use Start projector for the full classroom view.

Before the lesson

Follow the major surface currents and explain how winds and ocean heat transport contribute to regional climate.

Open the model before the lesson and choose a view that makes the important feature easy to see. Drag to rotate, and use the on-screen controls to change one variable at a time. The Controls panel explains the available keyboard shortcuts.

Pause the animation at a useful moment. Ask students what should happen next, then play it to test their explanation.

Guide the demonstration

Select North Atlantic and identify its western and eastern boundaries. Follow the arrows and name Gulf Stream and Canary Current.

Compare South Atlantic and explain the reversed sense of rotation. Locate all five subtropical gyres.

Discuss a common misconception

“Ocean currents are driven only by differences in water temperature.” Winds and pressure gradients drive much upper-ocean circulation, with Earth’s rotation and coastlines shaping the flow. Temperature and salinity affect density and contribute to overturning, while mixing connects different depths. Surface gyres and deep circulation are related but cannot be explained by temperature alone.

Build the explanation

Surface winds and Earth’s rotation help organise subtropical ocean gyres. Warm western boundary currents generally carry water poleward, while cooler eastern boundary currents carry it towards the equator.

Compare South Atlantic and explain the reversed sense of rotation. Locate all five subtropical gyres.

The globe shows the broad routes and directions of currents; their width and tracer speed are enlarged for reading.

Teaching notes

Distinguish wind-driven surface gyres from the deeper overturning circulation.

Explain that the Gulf Stream transports heat as part of a wider ocean–atmosphere system.

Consider atmospheric circulation and maritime exposure as well as ocean currents when discussing the United Kingdom’s climate.

Check understanding

Open Check for 4 questions. Ask students to explain their choice before revealing the answer.

Return to the opening photograph. Ask students to identify one visible feature and explain which part of the model helps account for it.

Look more closely

Use these observations to connect the vocabulary to features students can identify.

Eastern boundary current

Green phytoplankton and sediment-rich water off Mauritania's desert coast, observed by Aqua MODIS.
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Aqua MODIS, 5 May 2020. Upwelling in the Canary Current system supplies nutrients off Mauritania. The visible green water contains phytoplankton and sediment; it is not a temperature map.
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Subtropical high

GOES-East satellite view of the Americas with tropical cloud bands and midlatitude weather systems.
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GOES-East cloud observations over the Americas, 22 April 2014. Tropical cloud bands and midlatitude systems provide evidence of atmospheric circulation. The three-cell pattern is a long-term zonal average, not three fixed cloud rings in this single image.
Read the definition

Sources to keep beside the lesson

Watch an explanation

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The film stays paused until you play it.

How Do Oceans Circulate? Crash Course Geography #9 Crash Course

Same realm