Why We Have Seasons
Explain that the seasons are caused by the tilt of Earth's axis during its orbit around the Sun, distinguishing this from the common misconception that seasons are caused by changing distance from the Sun
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Earth’s axis is tilted about 23.5° from a line perpendicular to its orbital plane. During one orbit it keeps nearly the same direction in space. A hemisphere tilted towards the Sun gets more direct sunlight and longer days, giving summer. The opposite hemisphere gets winter. Distance alone cannot explain simultaneous opposite seasons. Safety: Paper only; no Sun viewing, heat lamps or exposure experiments. Stop: Stop at two orbit positions and the supplied daylight example. No temperature experiment or year-long observations.
Materials: Paper; Pencil; Ruler 1. Draw a Sun at page centre and equal-size Earth circles 6 cm left and right of it. Label left June and right December. In both Earths draw the axis leaning from lower left to upper right by about 23.5° from page vertical. Mark the upper end N. The page is an orbital-plane schematic, not a distance model. 2. Draw sunlight arrows from the Sun to both Earths. At June, the north end leans towards the Sun; at December it leans away. Add an equator at right angles to each axis. Write north summer/south winter at June and north winter/south summer at December. 3. Create an illustrative daylight card pair for latitude 45°N: June solstice about 15.5 hours daylight; December solstice about 8.5 hours. These rounded practice values are not a forecast for the family’s home. Link the longer day to more daily sunlight. 4. Add a counterexample card: Earth reaches its closest Sun distance around early January, while northern mid-latitudes have winter. Explain why that refutes a whole-Earth closer-means-summer explanation. 5. Write two cause sentences: one about sunlight angle and one about day length. Actual weather varies; summer does not mean every day is hot. Done: Complete both tilted Earths, four hemisphere-season labels, daylight links and the January counterexample. Proof: Keep the diagram and cause sentences. Note adult help keeping the axes parallel or interpreting daylight cards. Stop: Stop at two orbit positions and the supplied daylight example. No temperature experiment or year-long observations.
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NASA Space Place · Practice link — not the full lesson
Sun
Before you open · source notes
Sun supports Why We Have Seasons. An adult previews and guides; this is a learning page, not a scored quiz.
Free educational page, no sign-in required for the tested path.
Before you openAsk the learner one fact they learned and one question they still have.
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Public NASA Space Place page. An anonymous GET on 2026-11-12 returned HTTP 200 with no login or payment prompt for this URL. Opening the link does not save practice or assess mastery. An adult should preview and guide the learner.
NASA Space Place. “Sun.” External page; Gakuva does not copy, host, embed, or redistribute materials.
Unknown — link only
Check understanding
- Explains that Earth's axis is tilted at about 23.5° relative to its orbit
- Describes how the tilted axis causes one hemisphere to receive more direct sunlight in summer and less in winter
- Refutes the misconception that distance from the Sun causes seasons by noting Earth is actually slightly closer to the Sun in January
“If your child was asked why the UK is hot in summer but Australia is cold at the same time, could they explain that it's not about being closer to the Sun but about which half of the Earth is tilted towards the Sun?”
Curriculum record
- Type
- Conceptual
- Subject
- Science
- Domain
- Space Systems & Earth's History
- Age range
- Ages 11–12
Standards