inclination
Quick Summary
The inclination of Earth's equator to its orbit, known as the obliquity of the ecliptic, is approximately 23.44°. This tilt is not constant and varies between 22.1° and 24.5° over tens of thousands of years. The gravitational pull of the Moon helps stabilize this tilt.12
This axial tilt is the primary reason for the seasons. As Earth orbits the Sun, each hemisphere receives varying amounts of direct sunlight. When a hemisphere leans towards the Sun, it experiences summer due to longer days and increased solar energy absorption. Conversely, the hemisphere tilted away from the Sun experiences winter with less direct sunlight. The equator experiences less pronounced seasonal changes because sunlight strikes it more consistently year-round.3
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