Axial rotation
Axial rotation refers to the rotation of a body or a particle about an axis. In the context of astronomy, it is often used to describe the rotation of celestial bodies like planets, stars, and galaxies.
Overview[edit | edit source]
Axial rotation is a fundamental concept in physics and astronomy. It is the movement of an object in a circular path around a central point or axis. This is different from orbital rotation, where an object moves in a circular path around another object.
Axial Rotation in Astronomy[edit | edit source]
In astronomy, axial rotation is a key factor in determining the day and night cycle of a planet. For instance, the Earth completes one axial rotation approximately every 24 hours, which results in the cycle of day and night. The speed of this rotation varies depending on the planet. For example, a day on Jupiter lasts only about 9.9 Earth hours due to its rapid axial rotation.
Axial Rotation in Physics[edit | edit source]
In physics, axial rotation is often studied in the context of rotational motion. This type of motion is characterized by the movement of an object around a fixed axis. The speed of axial rotation can be measured in terms of angular velocity, which is the rate of change of an angle per unit of time.
Axial Tilt[edit | edit source]
The angle between an object's rotational axis and its orbital axis is known as its axial tilt. This tilt is responsible for the change in seasons on Earth and other planets. The Earth's axial tilt is approximately 23.5 degrees, which results in the varying intensity of sunlight received at different times of the year.
See Also[edit | edit source]
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