The axial tilt of a planet significantly influences its seasons by determining the angle and intensity of sunlight received at different latitudes throughout its orbit. For example, Earth’s axial tilt of approximately 23.5 degrees causes variations in solar radiation, leading to distinct seasonal changes as different parts of the planet receive varying amounts of sunlight over the course of the year. In contrast, a planet with little to no axial tilt experiences minimal seasonal variation, maintaining relatively consistent climate conditions year-round. Thus, the degree of axial tilt is crucial in shaping a planet's seasonal patterns.
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