FreeLesson 1 of 36 min read
Why the Earth has seasons: tilt, not distance
Learn how the tilt of Earth's axis changes the angle of sunlight and the length of days, and why distance from the Sun is not the cause of seasons.
Seasons shape when crops are planted, when animals migrate and what you wear to school. Many people think summer happens because Earth gets closer to the Sun. It is a sensible guess, but it is wrong. Seeing why is a good lesson in testing an idea against evidence.
Why distance is not the answer
Earth's orbit is very nearly a circle, so our distance from the Sun changes only slightly during the year. In fact, Earth is closest to the Sun in early January, which is winter in the Northern Hemisphere.
There is a second clue. If distance caused seasons, the whole planet would have summer at the same time. It does not. When it is summer in Canada, it is winter in Australia. Any good explanation must account for this.
The real cause: a tilted axis
Earth spins on an imaginary line called its axis. This axis is tilted about 23.5 degrees compared with a line standing straight up from the plane of Earth's orbit. The key detail is that the axis keeps pointing in the same direction in space all year. So as Earth travels around the Sun, the Northern Hemisphere leans towards the Sun for part of the year, and six months later it leans away.
Leaning towards the Sun changes two things for a hemisphere:
- Sunlight arrives at a steeper angle, so the energy is more concentrated.
- Days are longer and nights are shorter, so the ground has more hours to warm up.
- In the opposite hemisphere, both effects are reversed, giving winter.
Why the angle of sunlight matters
Example: the torch test
Shine a torch straight down onto a sheet of paper. You get a small, bright circle.
Now tilt the torch so the beam hits the paper at a low angle. The same light spreads into a larger, dimmer oval.
Cause: same amount of light, bigger area.
Effect: each square centimetre receives less energy, so it warms less.
This is what happens in winter, when the Sun stays low in the sky.
In summer the Sun climbs high at midday, so its light is concentrated like the straight-down torch. In winter the Sun stays low, so its light is spread out like the tilted torch. Sunlight also passes through more atmosphere at a low angle, which weakens it a little more.
Why day length matters
Longer days mean more hours of heating and fewer hours of cooling at night. In summer, the land and sea gain more energy than they lose each day, so temperatures climb. Near the poles the effect is extreme: in midsummer the Sun may not set at all, and in midwinter it may not rise.
Four key points in the year (exact dates shift by a day or so):
- Around 21 June: June solstice. Northern Hemisphere tilted most towards the Sun; longest day there.
- Around 21 December: December solstice. Southern Hemisphere tilted most towards the Sun.
- Around 20 March and 22 September: equinoxes. Neither hemisphere leans towards the Sun; day and night are roughly equal everywhere.
Facts versus models
It is an established fact that axial tilt causes the seasons. Textbook diagrams, however, are simplified models. They often draw the Sun far too small, the orbit as an obvious oval and Earth far too close to the Sun. Use them to see the tilt, not to judge sizes or distances.
Next time you explain seasons, name both causes, angle of sunlight and length of day, and give the evidence against the distance idea: opposite seasons in the two hemispheres, and Earth being closest to the Sun in January.
Key takeaways
- Seasons happen because Earth's axis is tilted and keeps pointing the same way as Earth orbits.
- The hemisphere tilted towards the Sun gets steeper sunlight and longer days, so it has summer.
- Distance from the Sun is not the cause, because the two hemispheres have opposite seasons.
Check your understanding
Written with AI help. Spotted a mistake? Tell us.