Having determined the position of Mercury about its epicycle in Ptolemy’s time, he now sets out to do the same for an ancient observation so that the can determine the rate Mercury moves about the epicycle.
Here’s the observation:
[I]n the
year of Dionysius’ calendar (which was in the year from Nabonassar), Scorpion , [which is Thoth [I] in the Egyptian calendar [ BCE, Nov. ], at dawn, Stilbon [i.e., Mercury] was moon to the rear of the straight line through the northern [star in the] forehead of Scorpius and the middle [star in the forehead], and was moons to the north of the northern [star in the] forehead. Now, according to our coordinates at that time, the midmost of the stars in the forehead of Scorpius had a longitude for into Scorpio, and is the same amount [ ] south of the ecliptic, while the northernmost star had a longitude of into Scorpio and is north of the ecliptic. So, the planet Mercury had a longitude of about into Scorpio. Furthermore, it is clear that it had not yet reached its greatest elongation as morning-star, since,
days later, on Scorpion , it is recorded that its distance from the same straight line towards the rear was moons; for [by that time] the elongation had become greater, the sun having moved about degrees, but the planet [only] half a moon. And on Thoth at dawn, the longitude of the mean sun, according to our tables, was into Scorpio., while the longitude of the apogee of the planet was about into Libra, since the or so years between the observations produce a displacement of the apogee of about .
Here’s the diagram we’ll use this time:
By and large, this one is the same as the previous one. The points are all even given the same lettering, so I won’t repeat all of them except to note that, when we dropped the perpendicular from
To begin, we’ll first determine the angle of the eccentres relative to the line of apsides. In other words,
This is slightly more complicated than in the last post. There, we were simply able to use Ptolemy’s determination of the solar position to determine where
However, we must be careful to recall that Ptolemy determined that Mercury’s line of apsides precesses at the same rate as the sun. This is what Ptolemy is telling us when he reminds us of the “
Specifically, at that time, the line of apsides did not point to a position of
We can then state that
If we now turn our attention to
I solved this triangle by bisecting it and then using some trig, coming up with
Next, we’ll want to turn our attention to
Now we can create the demi-degrees circle about this triangle. This allows us to state that
We can also determine the remaining angle in this triangle
We just determined
Ptolemy comes up with
We can now determine
Recalling that,
Next, we can add,
Now, we’ll focus on
In it, we know
As a quick side note, we can determine the remaining angle in this triangle,
We can then use the Pythagorean theorem to determine
Again, we’ll translate these to the context in which the eccentricities are
And similarly, we can determine,
Now we’ll add
We now know two of the sides in
We’ll now create a demi-degrees circle about this triangle and enter into that context, first converting all the sides to a context in which the hypotenuse,
While we could determine the remaining side,
Instead, we’ll look up the arc corresponding to
This means that the angle it subtends,
We can then determine the other non-right angle in this triangle,
Next, we can determine
As a quick note, Ptolemy specifies that we’ll find
In contrast, Toomer suggests it’s
Resuming the calculation:
We’ll now turn back to the observation in which Mercury was observed, at
Thus, we can subtract:
We’ll now construct a demi-degrees circle about
Then,
We’ll now convert back to our overarching context:
Ptolemy comes up with
We’ll now focus on
Ptolemy inexplicably rounds this off to an even
Ptolemy then calculates the corresponding arc,
When I calculated it, I came up with
This means that
Let’s zoom out a bit and consider
We can then use this to determine that
If we then subtract
We can then subtract from this,
Here,
This is then compared with the position we explored in the previous post from Ptolemy’s time at which point Mercury was
Ptolemy states the interval between these observations as
This interval contains
complete returns of the planet in anomaly (for Egyptian years produce very nearly returns, so years produce , and the remaining years, plus the additional days, another complete returns).
We can get the first of these (
which we can round down to
For the
Then, we’ll repeat for the additional
Again, we only want the complete returns, so that rounds down to
Thus, we have shown that in
Egyptian years, days, and hours, the planet Mercury moved in anomaly, beyond complete revolutions, , which is the amount by which the position at our observation is beyond the previous one.
In this post, we determined the historic position of Mercury to be
So, if we incorporate the full revolutions, the total motion in anomaly is:
This motion was done in a period of
Taking the ratio of these to find the degrees per day, I come up with a value of
Ptolemy then directs us to compare this value to what we get out of the mean motion table.
And just about the same increment [in anomaly] results from the tables we set out before: for it was on the basis of these very same calculations that we made our correction to the periodic motions of Mercury, by reducing the above interval to days, and the above revolutions in anomaly plus the increment to degrees. For when the total of degrees is divided by the total of days, there results the mean daily motion in anomaly which we set out for Mercury in our previous discussion.
As Ptolemy states, this value is very similar to the one that is laid out in his table of mean motion, matching up to the third sexagesimal place exactly. Toomer notes this discrepancy and explores in in Appendix C of his translation.
There, he suggests that Ptolemy is falsely claiming that these calculations were used to derive the mean motion table. Rather, he suggests, Ptolemy took these mean motions from another source which he likely trusted, and simply performed these calculations as a check on it finding that three sexagesimal places of agreement is enough to affirm it.
Alternatively, he suggests that Ptolemy did indeed use the above equations as the basis for his calculations, but then applied some small correction which he did not explain. If that was the case, then the actual methodology would likely be unrecoverable.
Regardless, that ends this chapter and we only have one more, very short chapter left to go in Book IX.
- As demonstrated in this post.
- I did this by using the chord table and, starting at an arc of
(as this was the one closest to a chord of , successively added the sixtieths until I was as close to as possible. - If we were more careful with the math, we could do the following:
Again, we would need to remove the fractional interval and only keep the complete rotations of
returns. However, this does make it seem that there is some fractional component with which Ptolemy doesn’t grapple. However, including this makes the final result further from the values given in the Mean Motion tables than the one we’ll be ending up with shortly. - It does strike me that we’ve left
and returns on the table here, so I feel like there should be one more return. Ptolemy does not explain why he does not include it.