Season Lab Earth systems · Lesson 02

Field study · 8 min

Observe · The yearly pattern

Why do seasons change?

Earth keeps the same 23.5° tilt as it circles the Sun. That tilt changes the angle of sunlight and the length of each day—not distance from the Sun.

Learning objectiveConnect axial tilt, sunlight angle, and daylight length to the season experienced in either hemisphere.

Lesson progress 02 / 04

02 · Experiment

Move through the year.

Pick a season and hemisphere. Watch Earth move to the matching orbital position, then compare the noon Sun angle and approximate daylight at 40° latitude.

Earth–Sun model

Northern Hemisphere · June solstice

What changed

Light arrives at a new angle.

A hemisphere tilted toward the Sun receives more direct light for more hours. Tilt it away and the same light spreads across a larger surface for fewer hours.

What stayed constant

The axis keeps pointing the same way.

Earth does not wobble back and forth each season. Its axis stays nearly parallel as the planet travels around the Sun, changing which hemisphere leans into the light.

03 · Checkpoint

Test the pattern.

Choose one answer in each card. Feedback appears immediately and stays only in this page—nothing is submitted or saved.

Question 01

What is the main cause of Earth’s seasons?

Pick the factor that changes sunlight angle and day length.

Question 02

When it is summer in the north, what is happening in the south?

Think about which hemisphere is leaning toward the Sun.

Question 03

What happens to daylight as summer approaches?

Use the daylight reading from the experiment as evidence.

04 · Summary

Keep the tilt. Change the view.

March equinox

Spring

Day and night are close to equal. Direct light begins shifting north as days lengthen.

June solstice

Summer

The north tilts toward the Sun, producing its longest days and highest noon Sun.

September equinox

Autumn

Day and night return near balance while direct light shifts south and days shorten.

December solstice

Winter

The north tilts away from the Sun, bringing its shortest days and lowest noon Sun.

01 · Tilt

Earth’s axis is tilted 23.5° relative to its orbit.

02 · Light

Direct, long-lasting sunlight delivers more energy.

03 · Opposites

The hemispheres experience opposite seasons.