Skip to content

A lesson for your classroom or geography club

Climate types

All teacher notes · Open the lab

Start projector

Grassland with scattered acacia trees in Serengeti National Park, Tanzania.
Loading photograph
Serengeti savanna: seasonal rainfall helps explain the balance between grasses and scattered trees.

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

    Read the A–E legend and identify the highlighted family on the globe.

    Open Observe
  2. 02

    Tinker

    Choose Tropical, then Dry. Compare their distribution and explain why temperature alone cannot separate them.

    Open Tinker
  3. 03

    Explain

    Why must rainfall be considered alongside temperature when comparing tropical and dry climates?

    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

Explore the five major climate families and explain how long-term temperature and rainfall patterns shape their global distribution.

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.

Ask students to predict the result before you change a setting. Compare the new view with the starting state.

Guide the demonstration

Choose Tropical and ask students to describe where it occurs. Then choose Dry and discuss why rainfall matters as well as temperature.

Locate London as a temperate example, then compare Helsinki and Nuuk. Ask students why a city’s classification should not be assigned to its whole country.

Finish by distinguishing climate from today’s weather. Discuss why vegetation also depends on soil, land use and disturbance, then use Check to test the explanation.

Discuss a common misconception

“One unusual day of weather can change a place’s climate classification.” Climate classifications use long-term patterns, such as monthly temperature and precipitation statistics. A heatwave or wet day is an event within that distribution. Classifying a place therefore requires a representative record, while a longer-lasting shift in the statistics may eventually change its classification.

Build the explanation

Köppen–Geiger groups climates using long-term monthly temperature and rainfall. Tropical, dry, temperate, continental and polar families describe different combinations of warmth, seasonality and moisture.

Select a family below the globe, then rotate Earth to compare where it occurs. The marked city gives one local example; nearby coasts and highlands may have a different class.

The colours summarise the 1991–2020 reference period; a location’s climate class does not determine its current weather or exact vegetation.

Teaching notes

Use long-term temperature and rainfall patterns to explain climate classes rather than treating them as today’s weather.

Keep a reference point’s climate separate from the range of climates found across a whole country.

Explain that a climate family can support several vegetation types and does not determine one unique biome.

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.

Köppen

Green fields and wooded valleys on Exmoor in North Devon.
Loading photograph
Exmoor, North Devon: a landscape within the Cfb oceanic climate region. Köppen classes use long-term monthly temperature and precipitation, not the weather on the day of the photograph.
Read the definition

BWh

Tall orange sand dunes under a clear sky at Sossusvlei, Namibia.
Loading photograph
Sossusvlei dunes, Namib Desert. Wind transports loose sand by surface creep and saltation; the dunes record accumulated transport rather than individual grain paths.
Read the definition

Sources to keep beside the lesson

Same realm