Earth's Tilt and Seasons
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Earth's Tilt and Seasons
Read the science-fair evidence
Harper shines a flashlight at a tilted globe. When the Northern Hemisphere tilts toward the light, its sunlight arrives more directly and daylight lasts longer. The same hemisphere receives more solar energy each day, so temperatures tend to rise: this is summer. At the same time, the Southern Hemisphere tilts away, gets less direct sunlight and shorter days, and experiences winter. Six months later, Earth is on the other side of its orbit, but its axis still points in the same direction. The hemispheres’ seasons have switched. At the June solstice, the Northern Hemisphere is tilted toward the Sun, so it has longer days and more direct sunlight. During the March and September equinoxes, neither hemisphere tilts strongly toward the Sun; day and night are close to equal in length around the world. Earth’s orbit is slightly elliptical, but the distance change is not what causes the seasons. The equator receives fairly direct sunlight throughout the year, so its seasonal temperature changes are usually smaller than those at higher latitudes.
Investigate and explain
- Earth’s axis is tilted, changing sunlight angle and daylight length during the year.
- The Sun becomes hotter during summer.
- Earth spins faster in summer.
- Earth’s axis points toward the Sun only in summer.
- Earth’s axis keeps pointing in nearly the same direction in space.
- Earth’s axis flips direction every six months.
- Earth’s tilt disappears at the equinoxes.
- Earth’s axis points directly at the Sun at every point in orbit.
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