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Now, let’s consider what this means from a scientific perspective. The Earth's tilt, about 23.5 degrees, causes the varying amounts of sunlight each hemisphere receives throughout the year. The Winter Solstice is when the North Pole is tilted farthest from the sun, giving the Northern Hemisphere the least amount of direct sunlight and the Southern Hemisphere the most. The angle of the sun's rays also affects the intensity of the sunlight. The more directly the sun's rays hit the Earth, the warmer it gets. During the Winter Solstice, the sunlight hits at a more oblique angle, spreading the same amount of solar energy over a larger area, reducing the intensity of sunlight.
