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A lone oak tree on a gentle hill in golden autumn light, with fields stretching to the horizon
AI-generated image, not a photograph of a real person or place.

WHAT THE SCIENCE SAYS

It's the tilt,
not the distance.

Earth is closest to the Sun in January.

That surprises most people. Seasons come from Earth's tilted axis, which leans one hemisphere towards the Sun for half the year and away for the other half, changing both the angle of sunlight and the length of the day.

23.4° the tilt that makes seasons

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THE SHORT ANSWER

One leaning planet,
four seasons.

The axis always points the same way in space.
As Earth orbits, each hemisphere takes its turn.

THE TILT

Leaning at 23.4°

The Royal Observatory says Earth's axis is tilted 23.44°. When the north leans towards the Sun, it gets more direct light and longer days.

How it works

THE SOLSTICES

Longest and shortest days

The solstices are the moments a hemisphere is most tilted towards or away from the Sun. In 2026 the winter solstice falls on 21 December.

See the numbers

TWO CALENDARS

Winter starts twice

Astronomers start seasons at solstices and equinoxes. Meteorologists use whole months: winter is December, January and February.

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A wildflower meadow glowing in late evening sunlight on a long midsummer day
AI-generated image, not a photograph of a real person or place.

FOUR THINGS TO REMEMBER

Reading the
seasons right.

A few ideas clear up most of the confusion about when seasons start and why they feel the way they do.

  1. It is not about distance

    Northern winter happens when Earth is closest to the Sun, NASA points out.

  2. A solstice is a moment

    The solstice is an exact moment in time, when a hemisphere is most tilted towards or away from the Sun.

  3. Warmth lags light

    Oceans and air take time to heat and cool, so the hottest and coldest weather comes after the solstices.

  4. Hemispheres swap

    When it is summer in the north, it is winter in the south, because the South Pole is then tilted away.

TWO NUMBERS WORTH KNOWING

A small lean,
a big difference.

The angle behind every season,
and what it does to a London day.

23.44°

Angle of Earth's axis

The Royal Observatory says Earth's axis of rotation is tilted at 23.44° to its orbit, so each hemisphere spends half the year leaning towards the Sun.

THE TILT · ROYAL OBSERVATORY

8h 49m

Longest minus shortest day, London

London's shortest day lasts 7 hours 49 minutes and 42 seconds, 8 hours 49 minutes shorter than the day of the summer solstice.

DAY LENGTH · ROYAL OBSERVATORY

NASA notes Earth is about 91.4 million miles from the Sun at its closest, in January, and 94.5 million miles at its farthest, in July: too small a change to cause the seasons.

A QUICK DATE CHECK

What happens
on this date?

Pick a date to see what it marks in the astronomical or meteorological year. The bar shows how much daylight the UK gets around then.

Date check

Choose a date
1 DecemberMeteorological winter

Meteorologists start winter on 1 December, so each season is three whole calendar months. That makes seasonal statistics easy to compare.

21 DecemberWinter solstice

The shortest day. In London it lasts 7 hours 49 minutes and 42 seconds, and in 2026 the exact moment falls at 8.50pm GMT.

Around 20 MarchSpring equinox

The Sun lights both hemispheres equally, and day and night are each around 12 hours long. Astronomical spring begins.

Around 21 JuneSummer solstice

The longest day, when the Northern Hemisphere is most tilted towards the Sun. In London it is 8 hours 49 minutes longer than the shortest day.

Around 22 SeptemberAutumn equinox

Day and night are roughly equal again. Meteorological autumn started weeks earlier, on 1 September.

Sources: Royal Observatory Greenwich, summer and winter solstice pages; Royal Meteorological Society, meteorological and astronomical seasons.

Based on the Royal Observatory Greenwich and the Royal Meteorological Society. Solstice and equinox dates can shift by a day or two.

A low winter sun barely above the horizon over a frosty field, casting long shadows from hedgerow trees
AI-generated image, not a photograph of a real person or place.

WHY THE SHORTEST DAY IS NOT THE COLDEST

The light peaks
before the heat.

In summer the Sun climbs higher and stays up longer, so sunlight arrives more directly and for more hours. In winter the glancing angle and short days let the air stay cold.

The Royal Observatory explains that the atmosphere and especially the oceans take time to warm up and cool down. That lag is one reason meteorologists start summer on 1 June and winter on 1 December, rather than at the solstices.

Questions

Questions people ask

Why do we have seasons?

Because Earth's axis is tilted. NASA says that when the North Pole tilts towards the Sun it is summer in the Northern Hemisphere, and when the South Pole tilts towards it, it is winter in the north.

Is Earth closer to the Sun in summer?

No. NASA says Earth is closest to the Sun in January and farthest in July, and the difference in distance does not make much difference to our weather.

When does winter officially start?

It depends who you ask. Astronomical winter begins at the December solstice; meteorological winter begins on 1 December and runs to the end of February.

Why do the solstice dates change?

The Royal Meteorological Society says a full orbit is not exactly 365 days and the orbit is elliptical, so solstice and equinox dates can shift by a day or two.

What does solstice mean?

It comes from the Latin solstitium, meaning 'Sun stands still', because the Sun's path in the sky stops moving north or south before changing direction.

Sources

  1. Royal Observatory Greenwich: What is the summer solstice?
  2. Royal Observatory Greenwich: When is the winter solstice? The shortest day
  3. Royal Meteorological Society: The difference between meteorological and astronomical seasons
  4. NASA Space Place: What causes the seasons?

Updated

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