Visual walkthrough — Physical meaning of each orbital element
Everything below rests on two arrows measured at one instant:
We also need one fixed piece of scenery, the reference frame, so that words like "tilt" and "swing" have meaning:

The symbol above is the cross product: given two arrows, it returns a new arrow that is perpendicular to both of them, with length equal to the area of the parallelogram they span. Why this tool? Because almost every orbital element is secretly asking "which direction is perpendicular to these two things?" — the plane's up-stick, the intersection line of two planes — and the cross product is exactly the machine that answers that. We lean on it in Angular momentum in orbits.
Step 1 — Read off the size (semi-major axis )
HOW — why energy? The single quantity that stays constant no matter where the satellite is on its orbit and depends only on size is the specific orbital energy (energy per kilogram):
Here is Earth's gravitational strength (its "pull constant"). The Vis-viva equation tells us this same energy equals for any ellipse. Setting the two expressions equal and solving for :
Reading the boxed formula term by term: measure the distance and speed , form the combination , and its reciprocal is . Now is a real, computed number — every later formula that mentions (including the orbit equation in Step 7) is allowed to use it.
All the cases:
- : a bound ellipse.
- : the satellite has exactly escape speed — a parabola.
- : too fast, a hyperbolic flyby (never returns).
PICTURE. The ellipse with its long axis drawn; is half of it. A speed dial shows that faster (for the same ) grows until it snaps to infinity at escape speed.

Step 2 — Fold the two arrows into a plane
HOW. Two arrows that start from the same corner define a flat sheet — like two pencils lying on a table define the tabletop. The up-stick of that sheet is:
Reading the equation term by term: takes the position arrow and the velocity arrow and spits out a new arrow standing straight up out of the orbit plane. Its length is , where is the angle between and .
WHY it matters. Once we own , we own the plane. Every later element is measured against either this plane or the reference plane.
PICTURE. In the figure, the two coral arrows are and ; the mint arrow poking up perpendicular to both is . The transparent disc is the orbital plane it defines.

Step 3 — Measure the tilt (inclination )
HOW — why a dot product? To get the angle between two arrows we use the dot product: . It multiplies the arrows and hands back a single number whose size tells you how aligned they are. Rearranged, it isolates the cosine of the angle — exactly the question "how tilted?"
Term by term: picks out only the vertical part of (call it ). Divide by 's full length and you get the cosine of the lean angle.
All the cases (read them off the picture):
- (flagpole straight up) : equatorial, prograde.
- (flagpole lying in the equator) : polar.
- (flagpole points down) : equatorial, retrograde — orbiting backwards.
PICTURE. The two up-sticks and splay apart by the angle ; three mini-orbits show the , , cases.

Step 4 — Find where the two planes cross (the node line )
HOW. The intersection line is perpendicular to both up-sticks and — so, again, the cross product:
This new arrow lies flat in the equator and points toward the ascending node. (The order , not , is what makes it point at the ascending node rather than the descending one.)
Degenerate case to notice: if , the orbit is the equator, the two planes don't cross in a single line, and . There is no ascending node — so becomes undefined. Keep this in your pocket for Steps 5 and 6.
PICTURE. The equator disc and the tilted orbit disc slice through each other; the slate line where they meet is the node line, and the coral arrow runs along it to the ascending node (green dot).

Step 5 — Swing the plane (RAAN )
HOW. Dot product again, between and :
just reads off 's -component, .
WHY the quadrant fix — the crucial subtlety. Cosine is even: . So can only ever return an angle between and — it literally cannot tell whether points into the front half or the back half of the equator. We break the tie with the sign of (how far leans toward ):
Edge case: if (equatorial orbit from Step 4), there is no node line to measure from, so is undefined. By convention we set , which just means "start counting the in-plane angle from the reference direction itself" — see the equatorial note in Step 6.
PICTURE. Bird's-eye view straight down onto the equator: points right, swings out by , and the shaded left/right halves show which one the sign picks.

Step 6 — Point the ellipse and read its shape (eccentricity vector )
HOW. Built purely from our two starting arrows (derived in full in Eccentricity vector):
Term by term:
- is the same gravitational strength we met in Step 1.
- scales the position arrow: when the satellite is moving fast for its height, this term stretches outward.
- subtracts off the part due to climbing/falling, so the leftover arrow settles onto the ellipse's long axis.
- Dividing by makes the length come out to exactly .
WHY the sign-fix, and the general version. We want to know whether periapsis lies on the same side of the node line as the direction of motion (giving ) or the opposite side. The honest test asks which side of the node arrow the arrow falls on, measured in the swing sense of the orbit itself. The cross product points either along (same side of motion) or against it, so the truly general criterion is:
Shape cases from :
- : shrinks to a point — a circle. There is no periapsis, so is genuinely undefined. Convention: set and measure the satellite's position directly from the ascending node instead (this combined angle is called the true longitude).
- : a proper ellipse, points at periapsis.
- Equatorial case (, so undefined): with no node line, measure directly from the reference direction to instead — , with if . This is the " folded into " convention from Step 5 made concrete.
- : parabola (escape); : hyperbola (flyby). See Vis-viva equation for the energy behind these.
PICTURE. Inside the orbit plane: the coral arrow shoots from Earth to periapsis; a short fat arrow (large ) and a tiny arrow (near-circle) sit side by side to show how length encodes squash; the angle opens from to .

Step 7 — Locate the satellite right now (true anomaly )
HOW. Dot with :
WHY the sign? means and point the same way-ish — the satellite is climbing outward toward apoapsis, so . If it is falling inward back toward periapsis, so is in the second half, . This is the same "cosine can't tell halves apart, so use a sign" trick once more.
PICTURE. The orbit with the satellite partway along; the angle opens at Earth's centre from periapsis to ; a small green arrow marks the two travel directions and the sign of .

The one-picture summary
Everything above collapses into one diagram: two starting arrows one energy formula, three cross products and three dot products six numbers. Follow the arrows.

Recall Feynman retelling — the whole walkthrough in plain words
Give me two arrows: one saying where the satellite is, one saying where it's going.
- From just their lengths, energy tells me the orbit's size (fast for your height ⇒ bigger orbit).
- Cross the arrows to get a flagpole sticking straight up out of the orbit. That fixes the flat sheet the whole orbit lives on.
- Compare that flagpole to Earth's North pole stick — the gap between them is the tilt .
- Slice the tilted sheet against the equator floor; they meet in a line. The upward-crossing end of that line is the node, and the arrow along it is .
- Standing on the equator floor, measure how far has swung from the fixed reference direction — that's the swing (and remember to check which half of the floor it's in).
- Build the special arrow from the two starters: it points to the closest approach and its length is the squash ; the angle from to is where the oval points, (check the side with , which works even for backward orbits).
- Finally, the angle from the tip of around to the position arrow tells you where the satellite is this instant, — the only number that keeps ticking. One energy formula, three cross products, three dot products, a few sign-checks. That's the entire machinery — and it reverses too, via State vector to orbital elements conversion. Add real-world drag and bulges and even the "constant" five start to drift; that's Orbital perturbations.
Recall Quick self-test
How do you get the size from the raw arrows, and why is only and needed? ::: From energy: . Energy depends only on the lengths and , not directions, and energy fixes size alone. Which two elements come from the same single arrow? ::: (its length) and (its direction) both come from the eccentricity vector . Why does inclination not need a quadrant sign-fix? ::: Because only ranges , which already covers uniquely; the sign-fixes are only needed for angles that span the full circle. Why is " if " not always safe? ::: It only matches the true test for prograde orbits (); for retrograde orbits () points down and the shortcut flips sign. In a purely equatorial orbit (), which element becomes undefined and how do we then measure ? ::: is undefined (); we set and measure directly from to via (with ). What makes true anomaly special among the six? ::: It is the only element that changes with time in an ideal two-body orbit; the other five stay constant.