PeterDonis said:
suppose we try to model the planetary motions in order to try to understand what determines the apparent size of the retrograde loop in the sky
I've tried constructing an approximate model by using small segments of circles to approximate the elliptical planetary orbits near perihelion and aphelion. Unfortunately that model isn't working out well--even for small segments, the error using circles instead of the actual ellipses is too large. However, working through that process showed me that "geometry" in and of itself can't be the entire answer. Sure, you can draw geometric pictures of the two oppositions and see how the angles compare, but in order to draw those pictures, you have to already know the dynamics--where the Earth and Mars actually are in their orbits at the start and end of Mars's retrograde loop. And that is a problem of dynamics, not just geometry.
As a try at describing the relevant dynamics, let's consider two approximations, which don't exactly capture the true conditions of the 2003 and 2012 oppositions, but will at least illustrate a key difference between them. The shortest possible Earth-Mars distance at opposition would occur if Earth were exactly at aphelion and Mars were exactly at perihelion (the 2003 opposition was fairly close to this). The longest possible Earth-Mars distance at opposition would occur if Earth were exactly at perihelion and Mars were exactly at aphelion (the 2012 opposition was not quite as close to this).
Under those conditions, the problem should be time symmetric about the time of opposition: i.e., Mars's apparent retrograde motion should start some time ##\Delta t## before the time of opposition, and should end exactly the same time ##\Delta t## after the time of opposition. So we only need to consider one half of the problem, and then just reflect it in mirror image to get the other half. We'll focus on the first half.
Of course we're not actually interested in ##\Delta t##, we're interested in ##\Delta \theta##, the angle between the Earth-Mars line at the start of Mars's apparent retrograde motion, and the Earth-Mars line at opposition (which for both of the cases described above is just the major axis of both the Earth and Mars orbit ellipses, i.e., the line passing through the Sun, Earth, and Mars). What determines that angle is where on their respective orbits Earth and Mars are when Mars starts its apparent retrograde motion. But time is also a factor in when that is.
A comment about the shapes of the orbits: the segments of each planet's orbit that we are considering
have the same shape. In other words, the curvatures of both orbits along segments centered on the major axis, at perihelion and aphelion, are the same. So in both cases described above, we are looking at the same two curves; the only things that vary are how far apart they are, and how fast each planet is moving along its curve.
Also, because Mars's orbit is more eccentric than Earth's, the curvature of its orbit at perihelion and aphelion is greater. That means that more of its motion between the start of its apparent retrograde motion and opposition is parallel to the major axis, and less is perpendicular to the major axis.
Now, a key point: since the shapes of the curves are the same in both cases, and since what we're interested in is the Earth-Mars line, we can actually plot
both cases on a single diagram. We take one Earth curve, and two Mars curves, at the two different distances (smallest and largest). We mark the two points on the Earth curve where the apparent retrograde motion of Mars starts for the two cases, and the corresponding two points on the Mars curve. Then we just look at the respective angles that the Earth-Mars lines make with the corresponding lines through Earth and parallel to the major axis of the orbits.
If we also draw lines through the two Mars positions parallel to the major axis of the orbits, we can call the Earth lines ##E_S## and ##E_L## (for Earth lines at smallest and largest Earth-Mars distances at opposition), and the corresponding Mars lines ##M_S## and ##M_L##. If we then call the perpendicular distances between the Earth and Mars lines ##D_S## and ##D_L##, and the Earth-Mars distances at opposition ##O_S## and ##O_L##, then the tangents of the two angles we want to compare are (approximately) the ratios ##D_S / O_S## and ##D_L / O_L##. So the question is, which of these two ratios is larger? Or, if we want to combine everything into a single formula, is the quantity ##D_S O_L / D_L O_S## greater than or less than ##1##?
Let's look at how the distances compare. We know ##O_L > O_S##, indeed ##O_L## is larger by about a factor of two. Call the actual factor ##f_O##, i.e., ##O_L = f_O O_S##. We also know that ##D_L > D_S## by a significant factor, because the Earth is moving faster in its orbit in the ##L## case while Mars is moving slower. Indeed, to a first approximation, if we call the times from the start of retrograde motion to opposition ##t_S## and ##t_L##, and the orbital speeds of Earth and Mars in the two cases ##v_{ES}##, ##v_{EL}##, ##v_{MS}##, and ##v_{ML}##, then we expect that ##D_S = \left( v_{ES} - v_{MS} \right) t_S## and ##D_L = \left( v_{EL} - v_{ML} \right) t_L##. Or, adopting obvious notation, ##D_S = \Delta v_S t_S## and ##D_L = \Delta v_L t_L##. And we can define the velocity factor ##f_v## by ##\Delta v_L = f_v \Delta v_S##, and the time factor ##f_t## by ##t_L = f_t t_S##, so ##D_L = f_V \Delta v_S f_t t_S##.
Putting all of the above together, we have
$$
\frac{D_S O_L}{D_L O_S} = \frac{f_O}{f_v f_t}
$$
From the numbers already given in this thread, we have
$$
f_O = 1.81
$$
$$
f_t = 1.33
$$
I couldn't find where the orbital speeds had been posted in this thread, so I got them from Wikipedia: for Earth, ##30.3## km/s at perihelion and ##29.3## at aphelion; for Mars, ##26.5## at perihelion and ##22.0## at aphelion. That gives
$$
f_v = \frac{30.3 - 22.0}{29.3 - 26.5} = 2.96
$$
So we have
$$
\frac{D_S O_L}{D_L O_S} = \frac{f_O}{f_v f_t} = \frac{1.81}{2.96 \cdot 1.33} = 0.46
$$
This is less than ##1##, so it is telling us that the ##L## angle is larger than the ##S## angle by a factor of a little more than ##2##. Of course this is only an approximate number even for the idealized cases described above, which are not quite the same as the actual oppositions we've discussed in this thread; but it serves to illustrate what the angle depends on and why we should not be surprised to find the ##L## angle being significantly larger than the ##S## angle: because the "shrinking" effect of the greater distance (which is what ##f_O## is capturing) is more than outweighed by the greater speed difference (##f_v##) and the longer time (##f_t##), both of which act to increase the angle.