We have learned from our early school time that the Earth has two motions: revolution around the Sun that is 365 days 5 hour and 48 minutes (tropical year) and the Earth’s rotation around its own axis that takes 23 hours 56 minutes and 4 seconds (sidereal day), 24 hours (solar day).
However, the Earth has other motions that are not well known to the public. In this article, we intend to have a glimpse on some of these motions of the planet that we live on.
The motions of the Earth
Some of the main additional motions of the Earth that have been discovered until now are the following:
- Precessional or wobbling motion of the Earth’s axis
- Ellipticity change of the Earth’s orbit around the Sun (change of eccentricity)
- Tilt change of the Earth’s rotation axis
- Perihelion change of the Earth’s orbit around the Sun
- Change in orbital inclination of the Earth
In this article, we are going to take a closer look at them in more details.
1. Precessional motion of the Earth’s axis
This motion is very similar to that of a spinning top in the Earth’s gravitational field. Besides its rotation around its own axis, the top’s axis also has a rotation around the vertical axis with a fixed frequency. This is called precessional or wobbling motion of the top.
The same rule applies to the Earth. The Earth is not precisely a sphere and owing to its rotation and the fact that it is not a completely rigid, its shape has become more an oblate ellipsoid instead of a complete sphere. Indeed, the equatorial diameter of the Earth is 42 kilometers larger than the polar diameter. As a result, due to the combined tidal forces of the Sun and the moon on the Earth’s equatorial bulge, and its inclined axis of rotation relative to its orbital plane, there is a periodic motion of the Earth’s axis with a period of about 23,000 years. This has an interesting observable consequence. Although this motion is too slow to be discovered during our lifetime, yet it is observable over long periods of time. Some 5,000 years ago, the pole star was another star called Thuban (α Draconis) and not the present pole star (Polaris) that we see at nights.
2. Tilt change of the Earth’s rotation axis
Although the present angle of inclination of the Earth’s axis of rotation relative to its plane of orbit around the Sun is 23.5⁰, careful observations by astronomers have made it clear that this angle is changing periodically with a period of 41,000 years from about 24.5⁰ to 22.5⁰. This motion is primarily due to the gravitational attraction of the Earth by the Sun and deviances of the Earth’s shape from a sphere. Interestingly it has been found that this movement combined with the precessional movement of the Earth’s axis of rotation has been the major cause of the Earth’s periodic ice ages.
3. Ellipticity (eccentricity) change of the Earth’s orbit around the Sun (change of eccentricity or stretch)
The Earth revolves around the Sun with a period of about 365 days. The shape of the Earth’s orbit around the Sun is an ellipse with the Sun at its center. This shape indeed is not static and the ellipticity of this orbit changes over time from a complete circle to an ellipse and back. The period of this motion is not constant and it ranges from 100,000 to 120,000 years.
4. Perihelion change of the Earth’s orbit around the Sun
This motion is mainly due to gravitational forces of other planets on the Earth and leads to the regular change of the direction that the elliptical orbit of the Earth points to.
5. Change in the orbital inclination of the Earth
It has been discovered that the Earth’s plane of the orbit is not constant in time; rather, its inclination changes relative to the orbit or other planets. The average period of this motion is about 100,000 years. During this period the angle of inclination changes from 2.5⁰ to -2.5⁰.
Although the above-mentioned motions of the Earth seem to be slight as compared to its two major motions; nevertheless, investigations have proven that these periodic motions indeed have significant long-term impacts of which we can mention the periodic climate changes on the Earth.
In 1941, a Serbian astronomer named Milutin Milankovitch managed to prove that the tilt change of the Earth’s axis of rotation combined with its precessional movement has led to many ice ages on the Earth. Later investigations confirmed his findings and now it is believed that from three to one million years ago, the period of ice ages was 40,000 years with an abrupt change from 20,000 years prior to that.
We do not feel the motions of the Earth because we move with it or their effect cannot be sensed in our normal life, but they are real, but still not fully understood.
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