
Why Do We Have Seasons? The Science of Earth's Tilt
Earth's 23.5-degree axial tilt, not its elliptical orbit, is why we have seasons. The tilt means each hemisphere receives more direct sunlight and longer daylight hours for part of the year (summer), then less direct light and shorter days for another part (winter). The two hemispheres always experience opposite seasons simultaneously. Solstices and equinoxes mark the extremes and midpoints of this tilt cycle.

