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Earth is closest to the Sun in January, so distance does not cause the seasons
Many people believe seasons happen because Earth swings closer to the Sun in summer and farther away in winter. In fact the cause is Earth's axial tilt of about 23.4 degrees. Because the axis is tilted, each hemisphere leans toward the Sun for part of the year, which brings longer days and sunlight that hits the ground more directly. When the Northern Hemisphere leans toward the Sun it has summer, and when it leans away it has winter. Earth actually reaches the point of its orbit closest to the Sun in early January and the farthest point in July, so the small effect of orbital distance works against the Northern Hemisphere's seasons rather than causing them.
This explains why the Northern and Southern hemispheres have opposite seasons at the same time, something a distance-based explanation cannot account for. It is a clear example of a commonly held belief that sounds plausible but fails when checked against the facts.
Earth is at its closest point to the Sun in early January, during Northern Hemisphere winter.
background
In astronomy, axial tilt, also known as obliquity, is the angle between an object's rotational axis and its orbital axis, which is the line perpendicular to its orbital plane; equivalently, it is the angle between its equatorial plane and orbital plane. It differs from orbital inclination.
At an obliquity of 0 degrees, the two axes point in the same direction; that is, the rotational axis is perpendicular to the orbital plane.
The rotational axis of Earth, for example, is the imaginary line that passes through both the North Pole and South Pole, whereas the Earth's orbital axis is the line perpendicular to the imaginary plane through which the Earth moves as it revolves around the Sun; the Earth's obliquity or axial tilt is the angle between these two lines.
From Wikipedia: Axial tilt (CC BY-SA 4.0) ↗From Wikipedia, the free encyclopedia · text CC BY-SA 4.0
Illustrative photo · Dna-webmaster, CC BY 3.0, via Wikimedia Commons
