During the summer months, the tilt of the Earth's axis causes the sun to take a higher and more direct path across the sky. In the Northern Hemisphere, for example, the North Pole is tilted toward the sun, resulting in longer days and a higher solar angle at noon. This increased angle means the sun rises higher in the sky, leading to more intense sunlight and warmer temperatures. Conversely, during winter, the sun follows a lower path, resulting in shorter days and less direct sunlight.
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