21 Hipparchus and Ptolemy

Andrew Franknoi; David Morrison; and Sidney C. Wolff

This page is an excerpt from the section Ancient Astronomy in the OpenStax Astronomy textbook.

Hipparchus and Precession

Perhaps the greatest astronomer of antiquity was Hipparchus, born in Nicaea in what is present-day Turkey. He erected an observatory on the island of Rhodes around 150 BCE, when the Roman Republic was expanding its influence throughout the Mediterranean region. There he measured, as accurately as possible, the positions of objects in the sky, compiling a pioneering star catalog with about 850 entries. He designated celestial coordinates for each star, specifying its position in the sky, just as we specify the position of a point on Earth by giving its latitude and longitude.

He also divided the stars into apparent magnitudes according to their apparent brightness. He called the brightest ones “stars of the first magnitude”; the next brightest group, “stars of the second magnitude”; and so forth. This rather arbitrary system, in modified form, still remains in use today (although it is less and less useful for professional astronomers).

By observing the stars and comparing his data with older observations, Hipparchus made one of his most remarkable discoveries: the position in the sky of the north celestial pole had altered over the previous century and a half. Hipparchus deduced correctly that this had happened not only during the period covered by his observations, but was in fact happening all the time: the direction around which the sky appears to rotate changes slowly but continuously. Recall from the section on celestial poles and the celestial equator that the north celestial pole is just the projection of Earth’s North Pole into the sky. If the north celestial pole is wobbling around, then Earth itself must be doing the wobbling. Today, we understand that the direction in which Earth’s axis points does indeed change slowly but regularly—a motion we call precession. If you have ever watched a spinning top wobble, you observed a similar kind of motion. The top’s axis describes a path in the shape of a cone, as Earth’s gravity tries to topple it (Figure 4).

The concept of precession. The left hand panel in this illustration shows a spinning top, with a circular arrow drawn counterclockwise around the axis of spin. Another arrow is shown pointing upward through the axis of spin and makes contact with a blue circular arrow drawn at the top of the figure. The blue circular arrow points clockwise and represents the path the spin axis traces as the top rotates. The right hand panel illustrates this situation as it applies to Earth. An arrow is drawn upward through the spin axis of the Earth emerging from the surface at the north pole, and points to the star Polaris. Polaris lies on a blue circular arrow that points clockwise. Also drawn on the blue circular arrow are the stars Thuban and Vega. The blue circular arrow represents the path the north celestial pole travels over time as Earth spins on its axis.
Figure 4: Precession. Just as the axis of a rapidly spinning top wobbles slowly in a circle, so the axis of Earth wobbles in a 26,000-year cycle. Today the north celestial pole is near the star Polaris, but about 5000 years ago it was close to a star called Thuban, and in 14,000 years it will be closest to the star Vega.

Because our planet is not an exact sphere, but bulges a bit at the equator, the pulls of the Sun and Moon cause it to wobble like a top. It takes about 26,000 years for Earth’s axis to complete one circle of precession. As a result of this motion, the point where our axis points in the sky changes as time goes on. While Polaris is the star closest to the north celestial pole today (it will reach its closest point around the year 2100), the star Vega in the constellation of Lyra will be the North Star in 14,000 years.

Ptolemy’s Model of the Solar System

The last great astronomer of the Roman era was Claudius Ptolemy (or Ptolemaeus), who flourished in Alexandria in about the year 140. He wrote a mammoth compilation of astronomical knowledge, which today is called by its Arabic name, Almagest (meaning “The Greatest”). Almagest does not deal exclusively with Ptolemy’s own work; it includes a discussion of the astronomical achievements of the past, principally those of Hipparchus. Today, it is our main source of information about the work of Hipparchus and other Greek astronomers.

Ptolemy’s most important contribution was a geometric representation of the solar system that predicted the positions of the planets for any desired date and time. Hipparchus, not having enough data on hand to solve the problem himself, had instead amassed observational material for posterity to use. Ptolemy supplemented this material with new observations of his own and produced a cosmological model that endured more than a thousand years, until the time of Copernicus.

The complicating factor in explaining the motions of the planets is that their apparent wandering in the sky results from the combination of their own motions with Earth’s orbital revolution. As we watch the planets from our vantage point on the moving Earth, it is a little like watching a car race while you are competing in it. Sometimes opponents’ cars pass you, but at other times you pass them, making them appear to move backward for a while with respect to you.

Figure 5 shows the motion of Earth and a planet farther from the Sun—in this case, Mars. Earth travels around the Sun in the same direction as the other planet and in nearly the same plane, but its orbital speed is faster. As a result, it overtakes the planet periodically, like a faster race car on the inside track. The Figure shows where we see the planet in the sky at different times. The path of the planet among the stars is illustrated in the star field on the right side of the figure.

Retrograde Motion of an Outer Planet. This diagram has two parts. The portion at right illustrates the apparent motion of Mars projected against the fixed background stars. The portion at left shows the Sun surrounded by two blue circles. The innermost circle represents the orbit of the Earth, the outermost the orbit of Mars. The Earth is shown as a blue dot in 5 positions, labeled A through E, along its orbit. Likewise, Mars is shown as a yellow dot in 5 positions, labeled A through E, along its orbit. Since the Earth travels faster than Mars, the 5 points for Earth are spread evenly around the circle of its orbit. As Mars moves more slowly, its 5 dots are all plotted close together on the right-hand side of its orbit. Beginning with Earth at point A on the lower left side of Earth’s orbit, an arrow connects with Mars at its point A at the lower right side of its orbit. This arrow continues and connects with Mars at point A near the bottom of its projected path of motion in the illustration at right. As Earth moves counter-clockwise along its orbit, it travels to point B at lower right, and Mars moves slightly upward on its orbit to its point B. An arrow points from Earth through Mars and continues on to connect with Mars at the third point B, which is above center on the projected path of motion. Thus, Mars has moved upward as seen from Earth in this figure. Earth then moves to point C at center-right on its orbit as does Mars. An arrow connects Earth through Mars to point C at the center of the projected path of motion. Mars has moved slightly downward as seen from Earth. Earth moves to point D at the upper right of its orbit and Mars moves upward to its point D. An arrow connects Earth through Mars and on to point D, which is below center on the projected path of motion. Mars has moved downward as seen from Earth. Finally, Earth moves to point E at the upper left of its orbit and Mars moves upward to its point E. An arrow connects Earth through Mars and on to point E near the top of its projected path of motion. Mars has moved upward as seen from Earth. In total, Mars has made a sideways
Figure 5: Retrograde Motion of a Planet beyond Earth’s Orbit. The letters on the diagram show where Earth and Mars are at different times. By following the lines from each Earth position through each corresponding Mars position, you can see how the retrograde path of Mars looks against the background stars.
This retrograde simulation of Mars illustrates the motion of Mars as seen from Earth as well as Earth’s retrograde motion as seen from Mars. There is also an animation of the movement of the two planets relative to each other that creates the appearance of this motion.

Normally, planets move eastward in the sky over the weeks and months as they orbit the Sun, but from positions B to D in Figure 5, as Earth passes the planets in our example, it appears to drift backward, moving west in the sky. Even though it is actually moving to the east, the faster-moving Earth has overtaken it and seems, from our perspective, to be leaving it behind. As Earth rounds its orbit toward position E, the planet again takes up its apparent eastward motion in the sky. The temporary apparent westward motion of a planet as Earth swings between it and the Sun is called retrograde motion. Such backward motion is much easier for us to understand today, now that we know Earth is one of the moving planets and not the unmoving center of all creation. But Ptolemy was faced with the far more complex problem of explaining such motion while assuming a stationary Earth.

Furthermore, because the Greeks believed that celestial motions had to be circles, Ptolemy had to construct his model using circles alone. To do it, he needed dozens of circles, some moving around other circles, in a complex structure that makes a modern viewer dizzy. But we must not let our modern judgment cloud our admiration for Ptolemy’s achievement. In his day, a complex universe centered on Earth was perfectly reasonable and, in its own way, quite beautiful. However, as Alfonso X, the King of Castile, was reported to have said after having the Ptolemaic system of planet motions explained to him, “If the Lord Almighty had consulted me before embarking upon Creation, I should have recommended something simpler.”

Ptolemy’s epicycles. A yellow dot labeled
Figure 6: Ptolemy’s Complicated Cosmological System. Each planet orbits around a small circle called an epicycle. Each epicycle orbits on a larger circle called the deferent. This system is not centered exactly on Earth but on an offset point called the equant. The Greeks needed all this complexity to explain the actual motions in the sky because they believed that Earth was stationary and that all sky motions had to be circular.

Ptolemy solved the problem of explaining the observed motions of planets by having each planet revolve in a small orbit called an epicycle. The center of the epicycle then revolved about Earth on a circle called a deferent (Figure 6). When the planet is at position x in Figure 6 on the epicycle orbit, it is moving in the same direction as the center of the epicycle; from Earth, the planet appears to be moving eastward. When the planet is at y, however, its motion is in the direction opposite to the motion of the epicycle’s center around Earth. By choosing the right combination of speeds and distances, Ptolemy succeeded in having the planet moving westward at the correct speed and for the correct interval of time, thus replicating retrograde motion with his model.

However, we shall see in Orbits and Gravity that the planets, like Earth, travel about the Sun in orbits that are ellipses, not circles. Their actual behavior cannot be represented accurately by a scheme of uniform circular motions. In order to match the observed motions of the planets, Ptolemy had to center the deferent circles, not on Earth, but at points some distance from Earth. In addition, he introduced uniform circular motion around yet another axis, called the equant point. All of these considerably complicated his scheme.

It is a tribute to the genius of Ptolemy as a mathematician that he was able to develop such a complex system to account successfully for the observations of planets. It may be that Ptolemy did not intend for his cosmological model to describe reality, but merely to serve as a mathematical representation that allowed him to predict the positions of the planets at any time. Whatever his thinking, his model, with some modifications, was eventually accepted as authoritative in the Muslim world and (later) in Christian Europe.

Ancient Greeks such as Aristotle recognized that Earth and the Moon are spheres, and understood the phases of the Moon, but because of their inability to detect stellar parallax, they rejected the idea that Earth moves. Eratosthenes measured the size of Earth with surprising precision. Hipparchus carried out many astronomical observations, making a star catalog, defining the system of stellar magnitudes, and discovering precession from the apparent shift in the position of the north celestial pole. Ptolemy of Alexandria summarized classic astronomy in his Almagest; he explained planetary motions, including retrograde motion, with remarkably good accuracy using a model centered on Earth. This geocentric model, based on combinations of uniform circular motion using epicycles, was accepted as authority for more than a thousand years.

Glossary

apparent magnitude: a measure of how bright a star looks in the sky; the larger the number, the dimmer the star appears to us

cosmology: the study of the organization and evolution of the universe

epicycle: the circular orbit of a body in the Ptolemaic system, the center of which revolves about another circle (the deferent)

parallax: the apparent displacement of a nearby star that results from the motion of Earth around the Sun

precession (of Earth): the slow, conical motion of Earth’s axis of rotation caused principally by the gravitational pull of the Moon and Sun on Earth’s equatorial bulge

retrograde motion: the apparent westward motion of a planet on the celestial sphere or with respect to the stars

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