Who developed a system for predicting planetary positions?

Let’s pick back up with Ptolemy’s Earth-centered model (see Figure 3.4) in about 150 A.D. It was tedious and complicated, but it seemed to work, at least within the accuracy of the naked eye measurements that were possible at the time. As a result, there wasn’t much reason to question it. But that changed over time, for two major reasons.

  • First, errors in the model tended to add up over time, so its predictions gradually got worse.
  • Second and perhaps more importantly, instruments used to measure planetary positions in the sky got much better over time, and this made the errors more noticeable (Figure 3.6).

As a result, by the 1400s and 1500s, it was becoming quite obvious that Ptolemy’s Earth-centered model simply did not work very well. And if the model didn’t work, then it couldn’t be correct. The stage was set for a rethinking of Earth’s place in the universe.

View Figure 3.4

Figure 3.6 - An astrolabe, which could be used to make precise, naked eye measurements of the positions of objects in the sky. Astrolabes were invented in ancient Greece, but their precision was vastly improved by Islamic scholars in the middle ages. As a result, it became much more obvious that Ptolemy’s Earth-centered model was giving incorrect predictions of planetary positions in the night sky. Credit: Museum of the History of Science.

Copernicus

The big change began with a Polish scientist named Nicolaus Copernicus (1473–1543). Copernicus was not the first person to suggest that Earth orbits the Sun; recall that this idea had been proposed by Aristarchus some 1,800 years earlier [Section 3.1.2]. Indeed, in his writings, Copernicus acknowledged that he was aware of Aristarchus’s proposal.

Why did Copernicus decide to try a Sun-centered model? If you think back to what we’ve discussed, you’ll realize that there were almost certainly two main reasons:

  1. Ptolemy’s Earth-centered model wasn’t working well, and therefore needed to be replaced by something.
  2. Copernicus was surely aware that the apparent retrograde motion of the planets in the sky has a much more natural explanation in a Sun-centered model (see Figure 2.34) than in an Earth-centered model (see Figure 3.4). Although his writings do not directly state how this fact influenced him, it is very likely that Copernicus made the decision to try a Sun-centered model because it seemed so much simpler and more natural than an Earth-centered model.

View Figure 2.34

View Figure 3.4

Once he started down the path of using a Sun-centered model, Copernicus spent a lot of time working out its mathematical details so that he could use it to predict planetary positions. In that process, he also discovered that he could use the geometry of his model to calculate how long it took each planet to orbit the Sun and how far (compared to Earth) each planet was from the Sun. The fact that his model led to a mathematically simple layout for the solar system gave him added confidence that he was on the right track in putting the Sun at the center.

Fyi, Copernicus was able to calculate only relative planetary distances; that is, their distances in units of Earth’s orbital distance (the astronomical unit, or AU, discussed in Chapter 1). The same was true for other astronomers of the era, including Kepler and even Newton. Measuring the value of the AU in absolute units, such as miles or kilometers, did not become possible until the 1800s.

Copernicus ultimately wrote a book describing his model in depth (Figure 3.7). The book was titled De Revolutionibus Orbium Coelestium, which translates to “On the Revolutions of the Heavenly Spheres.” It was published in 1543 — the same year in which Copernicus died; in fact, he apparently received the first printed copy of his book on the very day that he died.

Figure 3.7 – This page from Copernicus’s book, published in 1543, shows how his model placed the Sun (Sol) at the center and Earth (Terra) orbiting between Venus and Mars. It also shows the Moon’s orbit around Earth. Credit: Library of Congress.

Copernicus’s book spread quickly among European scholars and scientists, drawing wide interest. It did not immediately convince everyone, for reasons we’ll discuss next. However, the fact that Copernicus began the process with a book title that included the word “revolution” explains why we refer to the dramatic change that overturned the Earth-centered view of the universe as the Copernican revolution.

Why Copernicus’s Idea Was Not Immediately Accepted

To understand why Copernicus’s Sun-centered model was not immediately accepted, you have to remember that scientific models must be able to make predictions that can be tested. In this case, the key predictions were those for planetary positions in the sky.

You might guess that Copernicus’s model would have made much better predictions than Ptolemy’s. After all, Copernicus had the right idea in putting the Sun at the center, while Ptolemy used the wrong idea of Earth at the center. But it didn’t.

What went wrong? The answer is that while Copernicus had been willing to overturn the ancient idea of an Earth-centered universe, he still believed that “heavenly perfection” required that all heavenly motion had to occur in perfect circles. Because planetary orbits are not perfect circles (they are ellipses, as we’ll discuss shortly), his model made inaccurate predictions. He tried to improve the predictions of his model by adding additional complexity to it (including using “circles upon circles” like those in Ptolemy’s model), but it still didn’t work very well.

In the end, Copernicus’s complete model was no more accurate and no less complex than Ptolemy’s model. Given that fact, few people were willing to throw out thousands of years of traditional belief in an Earth-centered universe when the new model worked just as poorly as the old one.

Nevertheless, many scholars and scientists of the time liked Copernicus’s idea. We don’t know for sure what drew these people to the Sun-centered model, but its much simpler explanation for apparent retrograde motion probably played a major role. Copernicus himself had died, but others picked up where he left off.

Imagine that you are students in the year 1560. Your teacher (in the year 1560) has taught you about Ptolemy’s Earth-centered model, explaining that it is the generally accepted model of the universe. But your teacher has also introduced you to this “newfangled” idea from Copernicus, claiming that Earth actually orbits the Sun.

Based on what you have learned so far, hold a class debate about Ptolemy’s model versus the Copernican model. To do this, divide your class into three groups:

  • Group 1 will go first, defending the claim that planets orbit the Sun.
  • Group 2 will go next, defending the claim that planets and the Sun orbit the Earth.
  • Group 3 will then consider the evidence and reasoning presented by each of Groups 1 and 2, and vote on which team presented the strongest case.

Your teacher will serve as the judge, making sure that all groups present and consider only evidence that was available as of the year 1560.

Note: Students in Groups 1 and 2 should take some time to come to agreement within the group on which pieces of evidence support their case most strongly, and in preparing to explain how the evidence supports their argument. Students in Group 3 should discuss the evidence presented before rendering a group verdict on the debate winner.

As described within it, this activity is essentially a mock trial in which you’ll select two groups of students from your class to represent two legal teams, one on each side of the debate (one for Ptolemy’s model and one for Copernicus’s), and the rest of the class will serve as the jury. You will serve as judge to keep the debate on track. Be sure that you steer students to sticking with what was known in the year 1560, as discussed in the text above.

Data and Modeling

In very general terms, doing science always requires two things: data and modeling. The data come from observations and experiments. The models seek to explain why we find that data that we do. We test the models by comparing their predictions to the data.

After Copernicus published his book in 1543, scholars and scientists were faced with a key problem: Neither the old (Ptolemy’s) nor the new (Copernican) models agreed well with the data (observed planetary positions). It was therefore obvious to them that they needed a better model. They also recognized a need for better data against which to test any new model. The problem was that all existing data had been obtained by naked eye using hand-held instruments, and this did not provide enough precision for careful tests of how model predictions compared to actual planetary positions.

Two people ended up playing particularly important roles in developing better data and better models: a man named Tycho Brahe provided the data, and Johannes Kepler provided the models. We’ll talk about them in a moment, but first we need to talk about angle measurement so that you’ll be able to appreciate their work.

Arcminutes and Arcseconds

You are already familiar with angle measurement in degrees, which is defined by the fact that there are 360° in a full circle. Sometimes, however, we need to measure angles that are much smaller than 1°, and for that we divide degrees into smaller units as shown in Figure 3.8:

  • We subdivide each degree into 60 arcminutes (symbolized by ‘ ).
  • Then we further subdivide each arcminute into 60 arcseconds (symbolized by ” ).
Figure 3.8 – To measure very small angles, we subdivide degrees into arcminutes and arcseconds. Credit: The Cosmic Perspective.

In other words, 1 arcminute (1') is 1/60 of 1° and 1 arcsecond (1") is 1/60 of 1', or 1/3600 of 1°. Notice that these are very small angles. Recall that the width of a single finger held at arm’s length is about 1° (see Figure 2.8). This means that one arcminute is less than the thickness of your fingernail at arm’s length, and one arcsecond is considerably less than the thickness of a human hair at that distance.

Tycho’s Data

Tycho Brahe (1546–1601), usually known simply as Tycho (pronounced “tie-koe”), was an eccentric Danish nobleman. When he was 20 years old, he lost much of his nose in a sword fight with another student over who was the better mathematician. He then spent the rest of his life wearing a replacement nose that he made himself out of silver and gold.

Tycho recognized the need for better observations. The telescope still had not yet been invented, so Tycho set out to find a way to make more precise observations by naked eye. He developed numerous new instruments and built an observatory that worked much like a giant protractor (Figure 3.9).

Figure 3.9– This engraving shows Tycho in his naked-eye observatory (located on the island of Ven, now part of Sweden). The observatory worked much like a giant protractor. Notice the small rectangular hole in the wall at the upper left. The observer (in this case, Tycho) would observe a planet as its light came through the hole, using a slider marker (moved by the assistant at lower right) to measure the planet’s precise position. Credit: Royal Danish Library.

Tycho’s instruments and observatory allowed him to make naked-eye measurements of the positions of planets and stars in the sky that were accurate to within about 1 arcminute — far better than anyone had ever before achieved. Tycho and his assistants made observations for more than two decades, thereby acquiring the data that would finally prove the Earth-centered model to be wrong.

Tycho was convinced that his data held the key to coming up with a correct model for the heavens, but he himself struggled to come up with one. He therefore sought help. In the year 1600, he hired a man named Johannes Kepler (1571-1630) for this purpose. As Tycho lay dying just over a year later, he handed over all his data to Kepler. Kepler later wrote that while Tycho lay on his death bed, he kept repeating over and over the words “Let me not seem to have lived in vain.”

Kepler’s Model

When Kepler began work on creating a new model, he shared Copernicus’s beliefs that the model should be Sun-centered and that it should use only perfect circles for planetary orbits. After years of effort, he succeeded in creating a model with perfect circles that matched most of Tycho’s observations quite well. The match was not perfect, but even in the worst cases (which were for the planet Mars), this model with circular orbits predicted planetary positions that were within 8 arcminutes of Tycho’s observed positions. This is quite close, since 8 arcminutes is barely one-fourth the angular diameter of the full moon.

Kepler surely was tempted to attribute such small discrepancies to errors by Tycho. But he was convinced that Tycho’s observations had been made and recorded very carefully. He therefore concluded that it must be the circular orbits of his model, not Tycho’s data, that were wrong. About this fact, Kepler wrote:

If I had believed that we could ignore these eight arcminutes, I would have patched up my hypothesis accordingly. But, since it was not permissible to ignore, those eight arcminutes pointed the road to a complete reformation in astronomy.

With his decision to abandon perfect circles, Kepler began to try other shapes for orbits, and ultimately found the correct answer: Earth and other planets do indeed orbit the Sun, but their orbits take the shapes of the special ovals known as ellipses . Moreover, Kepler found that planets move faster in the portions of their elliptical orbits in which they are close to the Sun and slower when they are farther away (Figure 3.10).

Figure 3.10 – This diagram illustrates Kepler’s key discoveries about planetary orbits: (1) Each planet’s orbit takes the shape of an ellipse, with the Sun slightly off-center (at a point called a focus); (2) the planet moves faster in the portion of its orbit where it is closer to the Sun and slower where it is farther away. (The two triangles illustrate the mathematical description of varying orbital speed, which is that if you trace a planet’s motion back to the Sun, the planet always sweeps out equal areas in equal amounts of time.)

Kepler summarized his discoveries with three precisely stated mathematical laws that we now call Kepler’s laws of planetary motion . He published the first two of these laws, which were the ones needed to match Tycho’s data, in the year 1609. (The third law, which he published a decade later, describes how the time it takes each planet to orbit the Sun — called the orbital period — depends on its distance from the Sun.)

Kepler’s laws represent a model of planetary motion that can be used to predict the locations of planets in our sky at any time. Just as with the earlier models of Ptolemy and Copernicus, the process works basically like this:

  • Start by observing the current positions of planets in the sky.
  • Then use the mathematics of the model to predict future (or past) locations for the planets.

The critical difference is that while the models of both Ptolemy and Copernicus made noticeably inaccurate predictions, Kepler’s model gave essentially perfect predictions. Kepler’s model also had a second important advantage over the earlier ones: It was much simpler. Recall that calculations with Ptolemy’s model were extremely tedious and complex, and the same was true for Copernicus’s model with the complexity he was forced to add in his attempt to keep circular orbits.

In contrast, Kepler’s model is so simple that it is possible to build clockwork-like mechanisms that can reproduce planetary motion. Figure 3.11 shows one such device, in which each planet moves along an elliptical track, driven by clockwork built to follow Kepler’s laws. Of course, today it is much easier to program Kepler’s laws into a computer than to build a mechanical device. This is essentially how modern software can make perfect predictions of past and future planetary positions.

Figure 3.11 – This mechanical model uses pendulum clocks to move the first six planets of our solar system (Mercury, Venus, Earth, Mars, Jupiter, Saturn) along tracks in accord with Kepler’s laws. The model shows the planets in their correct positions in real time, and it has been doing so almost continuously since it was completed in 1781. You can see the current positions by clicking “show current position” on this web site. Credit: Eise Eisinga Planetarium.

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