Well, it's going to take some effort to respond to you last post ...
When I stated the following:
SammyS said:
No sidereal information is needed. All that is needed is observing what is the maximum angle between the line of sight to the Sun and the line of sight to the inferior planet.
I meant only what I said, not what you assumed that I meant.
You see, the observations are made from earth. The observations of an inferior planet are totally independent (not simultaneous with) the observations of a superior planet.
In the following quote (also from post #2) I merely pointed out how to use figure S1.1 to understand the relative positions of the earth, the sun, an an inferior planet for the case of greatest elongation.
At greatest elongation, Earth would be at position P2 in figure S1.1 and the inferior planet would be at position E2, assuming that angle P2E2S is 90°. (The labels in the figure were chosen for the case of observing a superior planet.)
From your original post, I gathered that
' observable angles between the planets and the Sun, orbital configurations, and synodic periods ' were assumed to be available, as they would have been available to Copernicus.
For the case of an inferior planet, such as Venus, you could consult a table with a daily listing of the angle between the line of sight to the Sun and the line of sight to Venus. When this angle is at a maximum, on that day, Venus is at greatest elongation. This does require that you understand what is mean by "greatest elongation", or for that matter, what is mean by "elongation", of an inferior planet.
From the standpoint of more casual observation, the greatest elongation of Venus occurs either when the time between Venus rising and sunrise is greatest, or when the time between Venus setting and sunset is greatest.
All the above is in regards to finding the distance of an inferior planet from the Sun, relative to Earth's distance from the sun. All that is needed for this calculation is the angle observed between Venus and the Sun at the time of greatest elongation.
The following quote from Post #2 is in regards to the case of a superior planet. It states the condition for quadrature of a superior planet from the point of view of an observer on Earth.
The superior planet is at quadrature when the line of sight to the planet makes an angle of 90° with respect to the line of sight to the Sun.
All the rest of the quoted material is from you in Post #3. (Some deletions ... not all of Post #3 is quoted here.)
s3a said:
So, the availability of the synodic/sidereal periods are computationally useless in solving this problem, right? In other words, they serve only for qualitatively stating that we can obtain ∠P_1 S P_2, right?
The availability of sidereal periods is only important for the case of superior planets, in which case it is crucial. In this case it's not only important in obtaining ∠P
1 S P
2, it's also important in finding ∠E
1 S E
2. Both of these are needed for finding ∠P
2 S E
2.
...
Also, to confirm, in the attached Position_astronomy.jpg image, the circle labeled with “Greatest western elongation” is at quadrature, right? Furthermore, why is it called the greatest WESTERN elongation if it's on the right of the image? Is it because the superior planet is to the left (=west) of the inferior planet?
I do not see this figure.
Another thing I'd like to know is if points E_1 and E_2 in Figure S1.1 are at greatest elongation with the superior planet as a reference point. Are they?
Hopefully, after reading the above, you will see that this question makes no sense.
Yet another thing I'd like to know is, in real life, how is one supposed to know that P_2 is at quadrature? Put differently, how is the astronomer (or whatever person) supposed to know when to stop calculating how much time it took for P_1 to go from opposition to quadrature?
This question has also been answered above, but to repeat:
The superior planet is at quadrature when the line of sight to the planet makes an angle of 90° with respect to the line of sight to the Sun.
This information should have been available to Copernicus. It occurs when the planet rises or sets at Solar midnight (midway between sunset and sunrise).
Of course, all of this assumes circular orbits, and in the case of superior planets, assumes that the orbits are in the same plane.