;colony/science  / Space & Astronomy  / Why do we have seasons?
Space & Astronomy

Why do we have seasons?

Earth is actually closest to the sun in January, mid winter up north. What makes the seasons is the lean of its axis.

Plate 20 — Tilt, not distance δ = 23.5°·cos(orbit) · cos H = −tanφ·tanδ
Slide Earth around its year and watch your daylight stretch and shrink.
Predict firstBefore you change the tilt: will a bigger axial tilt make summers more extreme or milder?
Nyou · 45°Nside view · sunlight always arrives from the leftJune · lean 23.5°
PLATE 20 · TILT, NOT DISTANCE
Where in the orbit June · summer (north)
One full slide = one year. The axis never changes direction.
Your latitude 45°N
Daylight
15.4hours
Noon sun height
69°
Look at the bright part of your latitude line — that's your daytime. In June the north leans toward the sun, so your line is mostly in the light: long days, high sun, summer. Slide to December: same distance from the sun, but now you lean away — short days, low sun, winter.
Try with the plate
  • Set the tilt to zero and watch the seasons disappear.
  • Find a latitude that gets a midnight sun in summer.

Seasons come from Earth's 23.5° axial tilt, not its distance from the sun. As Earth orbits, each hemisphere leans toward the sun for half the year (giving long days and steep, concentrated sunlight) and away for the other half. Earth is actually closest to the sun in January.

The short answer

Earth is tilted like a spinning top that never straightens up. For half the year your half of the world leans toward the sun, for long, warm days. For the other half it leans away, for short, cold ones.

The common mix-up

Most people think summer happens because Earth is closer to the sun. In fact Earth is closest in early January, and seasons come entirely from the 23.5° tilt swinging each hemisphere's sun angle and day length.

What's actually happening

The most popular wrong answer in science: "summer is when we're closer to the sun." Earth's orbit is nearly circular, and the small difference there is runs backwards: we're closest in early January, the depths of northern winter. Distance is innocent.

The culprit is the tilt. Earth's spin axis leans 23.5° and, like a gyroscope, keeps pointing at the same patch of sky (near Polaris) all year. So as we travel around the sun, there's a month where your hemisphere leans sunward: the sun climbs high, days run long, and sunlight hits the ground steeply, concentrated like a torch aimed straight on. Six months later the same hemisphere leans away: the sun stays low, days shrink, and the same sunlight smears across more ground at a shallow angle. Summer and winter are a lighting-angle story.

The tilt also draws the calendar's strangest lines. Above 66.5° latitude, there are summer days when your latitude line never crosses into the night side at all (the midnight sun), and winter days when it never leaves it. And while the north roasts, the south freezes: the two hemispheres always run opposite seasons off the same single lean.

Remember this

Seasons are a lighting-angle story, not a distance story: the tilt sets how steeply and how long the sun shines on you.

Try it at home Seasons with a torch
  1. 1In a dark room, shine a torch straight down at a sheet of graph paper and trace the bright patch.
  2. 2Now tilt the torch to hit the paper at a shallow angle from the same distance and trace again: the same light now smears over a far bigger patch, so each square gets less.
  3. 3That's winter: not less sunlight, but the same sunlight spread thin.

Common questions

Why are the seasons reversed in the southern hemisphere?

The two hemispheres always lean opposite ways off the same single tilt, so when the north leans sunward into summer, the south leans away into winter. December is high summer in Australia.

What is the midnight sun?

Above about 66.5° latitude, the tilt is steep enough that in summer your latitude line never crosses into the night side at all, so the sun never sets for weeks. In winter it never rises.

Why does winter sunlight feel weaker?

In winter the noon sun sits up to 47° lower in the sky, so the same sunlight strikes the ground at a shallow angle and smears over more area. It is spread thin, not reduced.

Built & checked by Nilesh Singh · how this is made · last updated June 2026