Seasons come from Earth's tilt

Years 3–8Stage 2 to Stage 4Run it

Earth's tilted axis always points one way in space. Watch a place's noon Sun and day length over the year.

Demonstration: a simplified modelNot to scale1 · December

Earth goes around the Sun on a path seen here at a slant. Its axis is tilted 23.4 degrees and points the same way in space all year; dashed outlines show Earth at the March, June, September and December marks. Month: December. Season in Sydney: Summer. The noon Sun in Sydney is 80 degrees above the horizon. Direction of the noon Sun: North. A beam of noon sunlight spreads over a patch of level ground. Daylight: Fourteen hours and fifteen minutes. Earth is 147.2 million kilometres from the Sun.

The south end of Earth's axis leans towards the Sun. Sydney's noon Sun is high, though never overhead, and the day is long.

  1. Sun
  2. Noon sunlight
  3. Lit patch

Key Dashed: Earth's path, seen at a slant, and Earth at the March, June, September and December marks. Arrowheads on the path: the way Earth goes around the Sun. Line through Earth: its axis. The arrowhead marks the north end. Dark: night, on Earth's side away from the Sun and on the day bar. Yellow on the bar: the hours of daylight, centred on noon. Arrows in a pale band: the noon sunlight, one beam width in every month. Thick line on the ground: the patch the beam lights. Arc at the ground: the noon Sun's height above the horizon. Dashed lines on the bar: where a twelve-hour day would begin and end.

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The idea, step by step

Not to scale

  1. Earth goes around the Sun on a path seen here at a slant. Its axis is tilted 23.4 degrees and points the same way in space all year; dashed outlines show Earth at the March, June, September and December marks. Month: March. Season in Sydney: Autumn. The noon Sun in Sydney is 56 degrees above the horizon. Direction of the noon Sun: North. A beam of noon sunlight spreads over a patch of level ground. Daylight: Twelve hours. Earth is 149.1 million kilometres from the Sun.
    2 · MarchEach dashed Earth's axis points the same way in space. Now it leans neither towards nor away from the Sun, so day equals night.1 Sun · 2 Noon sunlight · 3 Lit patch
  2. Earth goes around the Sun on a path seen here at a slant. Its axis is tilted 23.4 degrees and points the same way in space all year; dashed outlines show Earth at the March, June, September and December marks. Month: June. Season in Sydney: Winter. The noon Sun in Sydney is 33 degrees above the horizon. Direction of the noon Sun: North. A beam of noon sunlight spreads over a patch of level ground. Daylight: Nine hours and forty-five minutes. Earth is 152.0 million kilometres from the Sun.
    3 · JuneThe south leans away. Sydney's noon Sun is low, the same sunlight spreads over more ground, and the day is short: winter.1 Sun · 2 Noon sunlight · 3 Lit patch
  3. Earth goes around the Sun on a path seen here at a slant. Its axis is tilted 23.4 degrees and points the same way in space all year; dashed outlines show Earth at the March, June, September and December marks. Month: December. Season in London: Winter. The noon Sun in London is 15 degrees above the horizon. Direction of the noon Sun: South. A beam of noon sunlight spreads over a patch of level ground. Daylight: Seven hours and thirty-five minutes. Earth is 147.2 million kilometres from the Sun.
    4 · LondonIn December the north end leans away from the Sun, so London has winter, though Earth is nearly at its closest to the Sun.1 Sun · 2 Noon sunlight · 3 Lit patch
  4. Earth goes around the Sun on a path seen here at a slant. Its axis is tilted 0.0 degrees and points the same way in space all year; dashed outlines show Earth at the March, June, September and December marks. Month: June. Season in Sydney: Almost none, with no tilt. The noon Sun in Sydney is 56 degrees above the horizon. Direction of the noon Sun: North. A beam of noon sunlight spreads over a patch of level ground. Daylight: Twelve hours. Earth is 152.0 million kilometres from the Sun.
    5 · No tiltSydney's day lasts 12 hours and the noon Sun is as high in June as in December. The seasons almost vanish.1 Sun · 2 Noon sunlight · 3 Lit patch

Each month mark at the place chosen, with the tilt set, and the month on the model

MonthSeasonNoon Sun's height (°)DaylightDistance from the Sun (million km)In the first figure
DecemberSummer80Fourteen hours and fifteen minutes147.2Shown
JanuarySummer76Thirteen hours and fifty-five minutes147.2
FebruarySummer68Thirteen hours and five minutes147.9
MarchAutumn56Twelve hours149.1
AprilAutumn45Ten hours and fifty-five minutes150.3
MayAutumn36Ten hours and five minutes151.4
JuneWinter33Nine hours and forty-five minutes152.0
JulyWinter36Ten hours and five minutes152.0
AugustWinter45Ten hours and fifty-five minutes151.3
SeptemberSpring56Twelve hours150.1
OctoberSpring68Thirteen hours and five minutes148.8
NovemberSpring76Thirteen hours and fifty-five minutes147.8
With a learner

Three questions to ask

  1. Which end of Earth's axis leans towards the Sun in December?
  2. Why does a square metre of ground in Sydney get more sunlight at noon in December than in June?
  3. When it is summer in Sydney, what season is it in London?

What to expect

Many learners say summer comes when Earth is closest to the Sun.

What to try next

Open a practical in Try it in the Lab, above, to carry a tilted globe around a lamp or tip a torch beam over grid paper.

About this model

What is simplified

  • Earth's path is drawn as a circle seen at a slant. The real path is so nearly round that, drawn true, it would look the same; Earth's distance from the Sun still changes a little, and the distance readout uses the real path.
  • The Sun and Earth are drawn far larger than to scale, and far closer together.
  • Each month mark stands for about the twenty-first of its month, when the solstices fall. The real equinoxes and solstices fall between the twentieth and the twenty-third.
  • The day is counted from when the middle of the Sun crosses a flat horizon, with no air. Sunrise and sunset tables count from the Sun's top edge and allow for the air bending sunlight, so their days are about eight to fourteen minutes longer at these places. Day lengths are rounded to five minutes.
  • The seasons are the Bureau of Meteorology's four: summer is December, January and February. Australia's tropical north counts a wet and a dry season, and Aboriginal and Torres Strait Islander seasonal calendars count others, so no tropical place is offered here.
  • The noon sunlight is drawn as a beam of one width arriving at the noon Sun's height, so the patch it lights shows how the same sunlight spreads. Clouds, the air and sloping ground are left out.
  • Run to December moves Earth on a month each second, from the month shown to the December mark.

Numbers and their sources

Review

Demonstration: a simplified model. Checked against its written sources, 26 September 2026. Not reviewed by a qualified teacher.

Curriculum references

SC4-OTU-01ST2-10ES-SAC9S6U02AC9S7U03

Reference, not a verified alignment.

All demonstrations Practicals in the Lab