Earth's tilt and rotation are key factors that influence how solar radiation reaches different parts of our planet. Earth's axis is tilted at approximately 23.5 degrees relative to its orbital plane around the sun. This tilt is responsible for the changing seasons.
Over one year, Earth completes one full rotation around the sun while it rotates on its axis every 24 hours.
- Because of this rotation, different parts of the Earth experience daytime and nighttime.
- The tilt creates varying angles of sunlight at any given location throughout the year, impacting the intensity and distribution of solar radiation.
During different times of the year, the Earth's tilt causes certain regions to be closer to the sun, influencing seasonal variations in solar radiation. This tilt, combined with Earth's constant rotation, explains why some areas receive more sunlight than others.