Summer is tilt, not distance
Grades 7–8 · 45 minutes · Explain the mechanism. The driving question: Why is it summer here and winter in Sydney — on the same day? Every step below is a link that opens the exact view — one link puts the projector and every student screen on the same sky. Part of the lesson plans by topic and grade.
Teach this tomorrow
Before the lesson — what this assumes
- Assumes: day length varies with latitude and season — the data, if not the graph. Anchorage in December vs Singapore the same day restores it in two clicks.
- Assumes: the Earth orbits the sun once a year and spins on a tilted axis (names, not mechanisms — the mechanism is today).
- Pre-work: ask three adults why summer is warmer than winter. Bring their answers. (Most will say “closer to the sun”, and that's the lesson's raw material.)
The plan — every step carries its minutes
The minutes are there for the teacher's pacing — and so that any single step can be handed to a student as their own five-minute lesson. See students teach the class.
What they should find — the teacher's key
- Perihelion: early January, ≈ 147.1 million km; aphelion early July, ≈ 152.1 — closest in northern winter.
- Sydney vs a northern town on the December solstice: hours of day-length difference, same date.
- The lesson's shape IS the science: a hypothesis, two tests, one survivor.
Standards: MS-ESS1-1 (the tilt model, argued from evidence).
What the picture fakes: Every sunrise is computed in the browser from the date and the place, never looked up, so any date works. The solver assumes a flat horizon — a mountain to the east makes the real sunrise later than the page says, and the methodology pages state the accuracy bounds.
Three pathways through the same hour
Access
- ELL: the vocabulary row above is six terms; pre-teach them with the simulator picture rather than definitions — every one of them is visible.
- Reading: nothing in the lesson requires reading beyond the sheet; every fact arrives as a picture or a number read aloud.
- Visual: the day lengths are the numbers, not the picture — read Sydney's and your town's aloud from the page; the flashlight patch can be traced by touch.
- Motor: no student manipulation is required in the core path; the simulator is driven from the projector.
- Hearing: every step's content is on screen or on the sheet; the vote works by hands.
- Screen reader: the sun pages carry their figures as text (the day-length tables and readouts are HTML, not canvas), so a student on a reader gets the same two facts from the same pages.
What each student walks out with
Every student leaves with a written claim-evidence-reasoning paragraph — claim: tilt, not distance; evidence: perihelion falls in early January, and Sydney and their own town have opposite seasons on the same date; reasoning: one sentence on why only the tilt survives both facts — plus the before/after vote counts copied off the board. That paragraph is the assessment, the record, and the thing to show a parent who still believes the distance story.
Assessment
Success looks like:
- Can state the two facts that rule out distance — without notes.
- Can say what the axis does through a full year (nothing — it keeps pointing the same way) and what changes (which hemisphere leans toward the sun).
- Can explain why a LOW sun is a WEAK sun in one sentence.
Checks along the way:
- After Task 2: thumbs — same planet, same day, opposite seasons: can distance explain that? (All thumbs down before moving on; anyone unsure re-reads the two day lengths aloud.)
- During Task 3: cold-call “what just changed?” on each pass of the orbit until “only which end leans toward the light” comes back unprompted.
Exit ticket — the same three questions are on the student view, without the answers:
- Earth is closest to the sun in January. What does that single fact do to the “closer = summer” idea?
- It is December 21. Sydney has a long day and you have a short one. What one word explains how both can be true at once?
- Your friend says the tilt makes us closer to the sun in summer. Fix the sentence.
Answer key
- Earth is closest to the sun in January. What does that single fact do to the “closer = summer” idea?
It kills it: if distance ran the seasons, January would be northern summer — it is the middle of northern winter. - It is December 21. Sydney has a long day and you have a short one. What one word explains how both can be true at once?
Tilt (accept: the hemispheres lean differently — south toward the sun, north away). - Your friend says the tilt makes us closer to the sun in summer. Fix the sentence.
The tilt doesn't change the distance — it changes the ANGLE: the leaning hemisphere gets higher sun (more direct light) and longer days. Distance barely changes, and the whole planet shares it.
Questions to chase on your own
For the student who wants more — each answerable with the tools, no teacher required:
- If Earth's tilt were 0°, what happens to seasons? If it were 90°? One paragraph each, using what the simulator showed.
- Uranus really is tilted ~98°. Read its page: what are its seasons like?
Questions the curious actually ask
Real questions, mostly from real kids — the kind that sound simple and open trapdoors. Worth raising in class before someone raises them for you:
Why isn't the hottest day the longest day?
The longest day is around June 21 — check yours — but the hottest weeks come in July and August. Why the lag? Because the land and the oceans are still filling up with heat, like an oven that keeps warming after you turn the dial. As long as each day brings in more heat than the night lets out, temperatures keep climbing — even as the days start shrinking. The sea does the same thing harder: beach water is warmest in September, months after the sun's peak.
Do people at the equator have seasons?
Not ours. Day length barely moves — check Singapore on any date, it's near 12 hours year-round — and there's no warm-and-cold cycle to hang "summer" on. Instead the year is carved into wet and dry seasons as the planet's rain belt migrates north and south, chasing the overhead sun. And there's a bonus strangeness: at the equator the sun passes straight overhead twice a year, and on those days at noon, you have almost no shadow.
If we're closer to the sun in January, shouldn't January be warmer?
It is — in Australia: look at Sydney's daylight today against your own town's. That's the tell that unravels the whole "closer = summer" idea: Earth really is 3 million miles closer to the sun in early January, and the southern hemisphere really is in summer then. The distance change is real but small (about 3%); the tilt's effect on sun-angle and day length is enormous. The 7–8 lesson turns this exact trap into a full period of hypothesis-testing.
Go further — beyond this site
- NASA Space Place: Seasons — the model, cleanly drawn.
- NOAA Solar Calculator — declination and sun position for any date — the data behind task 4.
Same question, other grades
Each grade band re-asks this topic's question one level deeper — observe it, describe the pattern, measure it, explain the mechanism, quantify it and question the model. This page is the explain the mechanism rung.
Teachers: make this lesson better
You are the one standing in front of the class, so you will see what we cannot: a task that runs long, a question that lands better another way, a grade level pitched wrong, a topic we should build next. Tell us — improvements go into the page, and if we use yours, your class gets the credit on it, the same promise the classroom request form makes.
Have a lesson of your own? Send us the one you already run and we will build it into a page like this one, with your name on it. That is the ask we would most like you to take.