Skip to content

A lesson for your classroom or geography club

Why seasons happen

All teacher notes · Open the lab

Start projector

Meteosat view of Earth's day–night boundary on the December solstice, with more of the Southern Hemisphere in daylight.
Loading photograph
Meteosat-9 SEVIRI, 21 December 2010. The tilted day–night boundary gives the Southern Hemisphere longer days. Axial tilt, rather than a change in Earth–Sun distance, controls this seasonal illumination.

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

    Keep Orbit stretch at 0 and set Axial tilt to 0°. Play a year and read the two 12-hour daylight values. Switch to Earth close-up to inspect the terminator and axis.

    Open Observe
  2. 02

    Tinker

    Set tilt to 23.44° and pause at the June direction, then December. Compare London with Sydney and trace the fixed axis direction.

    Open Tinker
  3. 03

    Explain

    Why do the hemispheres experience opposite seasons, even though both are nearly the same distance from the Sun?

    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

Explain how axial tilt changes daylight and solar angle, then predict which hemisphere experiences summer at a chosen point in the year.

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

Keep Orbit stretch at 0 and set Axial tilt to 0°. Play a year and read the two 12-hour daylight values. Switch to Earth close-up to inspect the terminator and axis.

Set tilt to 23.44° and pause at the June direction, then December. Compare London with Sydney and trace the fixed axis direction.

Discuss a common misconception

“Summer happens because Earth is closer to the Sun.” Earth’s axial tilt changes both the angle of sunlight and the length of daylight. The hemisphere tilted towards the Sun has summer while the other has winter. Earth is closest to the Sun in early January, so orbital distance cannot explain their opposite seasons.

Build the explanation

Earth’s tilted axis changes the angle of sunlight and the length of the day as Earth travels around the Sun. When one hemisphere tilts towards the Sun, the other experiences winter.

Set tilt to 23.44° and pause at the June direction, then December. Compare London with Sydney and trace the fixed axis direction.

The adjustable orbit is an experiment for isolating tilt and distance; its calendar alignment is not Earth’s actual orbit.

Teaching notes

Use the model’s position in the year to compare seasonal geometry rather than to identify an exact calendar date.

Distinguish the pattern of incoming sunlight from a prediction of local temperature.

Explain that Earth and its axis are enlarged in the display so students can see the geometry.

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.

Terminator

Meteosat view of Earth's nearly north–south day–night boundary at the March equinox.
Loading photograph
Meteosat-9 SEVIRI, 20 March 2011. The terminator passes close to both poles around the equinox; refraction and the Sun's finite disc mean observed daylight is not exactly twelve hours everywhere.
Read the definition

Perihelion

Hubble observations of Comet ISON's bright coma and tail on 2 November 2013, before perihelion.
Loading photograph
Hubble observed Comet ISON on 2 November 2013, before its closest approach to the Sun. Perihelion names that closest orbital point; the coloured filters show coma and tail structure, not a map of the orbit.
Read the definition

Sources to keep beside the lesson

Watch an explanation

Loading video player

The film stays paused until you play it.

Why we have seasons Khan Academy

Same realm