5.2Chapter 5: The Earth in Space
Our planet: seasons — Alhussan Physics - Stage 7 Revision Notes & Topical Questions
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Lesson summary
5.2 Our planet: seasons — Axial Tilt (23.5°) and Solar Hemisphere Heating — Alhussan International Academy — Physics (Stages 7–9) notes: Explain how the tilt of the Earth's axis causes seasons, changes in day length, temperature and the height of the Sun in the sky.Orbit — the Ea…
- Near the poles
- Near the equator
- Changing day length
- Over the year
- Summer in the north
- Winter in the south
Part 1 of 6The year and the seasons
1Orbit
- Orbit the Earth orbits the Sun once every year, or 365 days.
2Seasons
- Seasons the year is divided into spring, summer, autumn and winter.
3Near the poles
- Near the poles countries have a big difference in weather between summer and winter, with longer, warmer days in summer and shorter, colder days in winter.
4Near the equator
- Near the equator countries between the Tropic of Cancer and the Tropic of Capricorn do not notice much change.
5Changing day length
- Changing day length in most places the length of the day changes over the year,
- so the Sun sets earlier each night as winter approaches and later each night as summer approaches.
Part 2 of 6The tilt of the Earth's axis
1Tilt
- Tilt the axis is tilted by an angle of 23.5°, and this angle does not change.
- It always points to the same place in space as the Earth orbits.
2Over the year
- Over the year for 6 months the North Pole is tilted towards the Sun, and for 6 months it is tilted away.
3Summer in the north
- Summer in the north the North Pole is tilted towards the Sun, so the northern hemisphere receives more direct sunlight.
- The Sun stays in the sky for longer each day as the Earth spins, so the day is longer than the night.
4Winter in the south
- Winter in the south at the same time the southern hemisphere is tilted away from the Sun.
- The Sun stays in the sky for less time each day until midwinter.
5Six months later
- Six months later the situation is reversed, so the hemispheres have opposite seasons.
6What the tilt explains
- What the tilt explains different day lengths, different temperatures and the varying height of the Sun in the sky in summer and winter.
Part 3 of 6Changing temperature
Why summer is hotter
- Why summer is hotter the Sun is in the sky for longer, and the rays from the Sun are concentrated over a smaller area.
Rays at 90°
- Rays at 90° if the rays hit the surface at 90°, more energy hits each square metre per second,
- so the surface heats up faster and the air temperature rises more quickly.
Winter
- Winter the Sun's light is spread over a bigger area, such as 2 square metres instead of 1,
- so it is less intense, and the days are shorter,
- so there is less heating.
Part 4 of 6Changing height of the Sun
1Highest at noon
- Highest at noon during the day the Sun is highest in the sky at noon.
2Over the year
- Over the year the height the Sun reaches at noon is higher in summer than in winter, again because of the tilted axis.
3Shadows
- Shadows a fence post makes a shorter shadow at noon in summer than in winter, because the Sun is higher.
Part 5 of 6Midnight Sun and polar night
Midnight Sun
- Midnight Sun in regions in the north inside the Arctic Circle, such as Finland, Norway and Canada, the Sun does not set in summer,
- so they are known as the "Land of the Midnight Sun".
- The same happens in Antarctica during its summer, but no one lives there to see it.
Polar night
- Polar night in winter in these places the Sun does not rise at all.
| Feature | Summer (tilted towards Sun) | Winter (tilted away) |
|---|---|---|
| Sun at noon | High | Low |
| Day length | Longer than night | Shorter than night |
| Heating | More | Less |
Part 6 of 6A common misconception
Distance from the Sun
- Distance from the Sun some people think it is hotter in summer because the Earth is closer to the Sun, which is not true.
Orbit
- Orbit the Earth's orbit is nearly circular, and the Earth is slightly closer to the Sun in January each year.
No tilt
- No tilt if the axis was not tilted, day length would not change over the year and there would be no seasons.
Key terms
| Term | Meaning |
|---|---|
| Axis | the imaginary line through the North and South Poles about which the Earth spins. |
| Tilt | the 23.5° angle of the Earth's axis. |
| Season | one of four periods in the year with typical weather and day length. |
| Hemisphere | half of the Earth, northern or southern. |
| Arctic Circle | the latitude line around the north where the Sun may not set in summer or rise in winter. |
| Polar night | winter in the polar regions when the Sun does not rise at all. |
Avoid these mistakes
1
Thinking seasons are caused by the Earth being nearer the Sun — the tilt of the axis causes them.
2
Thinking the Earth's axis wobbles back and forth during the year — it keeps pointing the same way.
3
Thinking the Sun is hotter in summer — its output is the same, but the energy per square metre changes.
4
Thinking the whole Earth has the same season at once — the hemispheres have opposite seasons.
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