This morning someone asked me why it's so cold in January when Earth is actually closest to the sun then. I paused mid-coffee, smiled, and said, "That's exactly the question that breaks the distance myth."
Most people assume seasons happen because Earth moves closer to or farther from the sun in its orbit. It's a reasonable guess—closer should mean warmer, right? But Earth's orbit is nearly circular, and the distance variation is only about 3%. If distance controlled seasons, the entire planet would be warm or cold at the same time. Yet when it's winter in New York, it's summer in Sydney.
Seasons exist because Earth's axis tilts 23.5 degrees. During northern summer, the North Pole leans toward the sun. Sunlight hits the Northern Hemisphere at a steep angle—more direct, more concentrated, like holding a flashlight straight down versus at a slant. The days stretch longer. Six months later, that same hemisphere tilts away. Sunlight arrives at a shallow angle, spreading thin across the surface. Days shrink. Same solar energy, different geometry.