Intuition The one core idea
An orbit is a single fixed ellipse floating in space, and there are two complete ways to name it: six numbers that say "here I am, moving this fast" or six numbers that say "this is the ellipse's size, shape, tilt, and where I sit on it." Converting between them is just re-describing that one ellipse — so before we can convert, we must earn every symbol that either language uses. (The formal names for those two schemes — state vectors and orbital elements — are defined in sections 3 and 8 once their pieces exist.)
This page defines every symbol the parent note Converting between orbital elements and state vectors (r, v) leans on, in an order where each idea rests on the one before it. If a symbol below feels obvious, read it anyway — the conversion recipes break the instant one meaning is fuzzy.
Everything happens around one heavy object (Earth, the Sun). We treat it as a fixed point at the origin, and a tiny body (a satellite) moves around it.
Definition The central body and the orbiting body
The central body sits at the origin — the "pin" the orbit is anchored to.
The orbiting body is the moving dot whose position and velocity we track.
We assume the orbiting body is so light it does not tug the central body — this is the setup of the two-body problem .
Before "position vector" means anything, "vector" must.
a
A vector is an arrow : it has a length (how long) and a direction (which way it points). We write it with a little arrow, a .
We will soon lay down three perpendicular measuring sticks (section 2). Once those exist, a vector can also be written as three numbers ( a x , a y , a z ) — how far the arrow reaches along each stick. Until then, just picture the arrow itself.
Definition Magnitude of a vector — written
∣ a ∣
The magnitude is just the length of the arrow, a single positive number. Once we have the three components (next section) it is computed as
∣ a ∣ = a x 2 + a y 2 + a z 2
The picture: stretch the arrow out straight and measure it with a ruler. Why the topic needs it: r = ∣ r ∣ (how far the satellite is) and v = ∣ v ∣ (how fast) appear in almost every formula.
Common mistake The plain-letter naming convention (and one clash to watch)
By convention we often drop the arrow and bars and write the magnitude as the plain letter : r = ∣ r ∣ , v = ∣ v ∣ , h = ∣ h ∣ , n = ∣ n ∣ , e = ∣ e ∣ . So r is the arrow and r is its length.
One clash to keep straight: the plain letter a is not used for the length of some vector a in this topic — the symbol a is reserved for the semi-major axis (section 9). Whenever you meet a on this page it is just a generic example arrow ; its length we always write in full as ∣ a ∣ , never as bare a .
Definition Reference frame and unit vectors
x ^ , y ^ , z ^
A reference frame is three perpendicular measuring sticks meeting at the origin. The little hats mean unit vectors — arrows of length exactly 1 pointing along each stick. z ^ is special: it points "up" out of the reference plane (for Earth, toward the north pole).
a x , a y , a z
With the frame in place, any arrow a is captured by three numbers : a x is its reach along x ^ , a y along y ^ , a z along z ^ . These are the components . This is exactly why the magnitude formula ∣ a ∣ = a x 2 + a y 2 + a z 2 (section 1) makes sense — it is the 3-D Pythagoras theorem on those three reaches.
Why the topic needs it: the tilt i is measured from the plane spanned by x ^ , y ^ , and the node vector uses z ^ directly (n = z ^ × h ). Without a fixed frame, "tilted" and "swivelled" have no meaning. This particular frame is the ECI frame; a second, orbit-hugging frame (PQW) appears later — see Reference frames — perifocal (PQW) vs ECI .
Definition Position vector
r
The position vector is the arrow from the origin to the satellite right now . Its length r is the current distance to the central body.
Definition Velocity vector
v
The velocity vector is the arrow showing which way the satellite is moving and how fast — it is tangent to the path. Its length v is the speed.
Together, ( r , v ) are the state vectors — this is the first of the two naming schemes the intro promised.
Intuition Why "state" = 6 numbers
r is 3 numbers, v is 3 numbers. Together those six numbers completely pin down the motion: give me where you are and how you move, and Newton's law tells me your entire future orbit. This is the "sensor language" the parent note describes.
We need to talk about "the angle between two arrows" before the dot product, because the dot product's meaning is built on it.
θ
An angle θ measures how much you turn to go from one direction to another — from 0 (same way) through a right angle (9 0 ∘ ) to a full about-face (18 0 ∘ ) and beyond, up to a whole turn (36 0 ∘ ).
Definition Cosine and sine on a right triangle
On a right triangle with an angle θ : cos θ = hypotenuse adjacent , sin θ = hypotenuse opposite . They convert an angle into a ratio of side lengths — the bridge between "how much turn" and "which numbers." Two facts we will lean on: cos 0 = 1 (no turn), cos 9 0 ∘ = 0 (right angle), cos 18 0 ∘ = − 1 (opposite).
cos − 1
cos − 1 ( x ) asks "which angle has this cosine?" — it undoes cosine. Crucial limit: it only ever answers between 0 and 18 0 ∘ . That limitation is why the conversion recipe attaches a sign check to each angle (spelled out in section 10): cosine alone cannot tell ν = 6 0 ∘ from ν = 30 0 ∘ , so a companion sign rescues the missing half-circle.
The conversions live and die on two ways to combine two arrows. Both use the angle θ we just defined.
a ⋅ b — a number
The dot product multiplies two arrows into a single number :
a ⋅ b = a x b x + a y b y + a z b z = ∣ a ∣ ∣ b ∣ cos θ
where θ is the angle between them (section 4). Why this tool? It answers "how much do these two arrows point the same way?" Because cos θ is positive for angles under 9 0 ∘ , zero at 9 0 ∘ , and negative past 9 0 ∘ , the dot product is positive when the arrows roughly agree, zero when perpendicular, negative when opposing. The parent uses r ⋅ v : its sign tells us whether the satellite is moving away from the central body (positive) or toward it (negative) — the key that unlocks the true-anomaly quadrant.
a × b — a new arrow
The cross product multiplies two arrows into a new arrow perpendicular to both :
a × b = ( a y b z − a z b y , a z b x − a x b z , a x b y − a y b x )
Its length equals the area of the parallelogram the two arrows make. Why this tool? It answers "what direction is perpendicular to this plane?" Point right-hand fingers from a toward b ; the thumb gives a × b .
Why the topic needs it: h = r × v is perpendicular to the orbit plane — so the cross product literally manufactures the axis the orbit spins about . That is how one operation fixes both the tilt i and the swivel Ω .
Definition Specific angular momentum
h
h = r × v . Because it is perpendicular to both position and velocity, it is perpendicular to the entire orbit plane . It is called specific because it is per unit mass (no mass in the formula).
h physically is
Its length h equals twice the rate at which the arrow r sweeps out area . A satellite that sweeps area at a constant rate has constant h — that is Kepler's second law, and the reason h never changes along an orbit. See Angular momentum conservation in orbits .
Why the topic needs it: h is conserved (constant), so it is a rock-solid signpost. Its direction fixes the orbit plane; its magnitude sets the parameter p = h 2 / μ .
μ = GM
G is the universal gravity constant; M is the central body's mass. Their product μ measures how strongly this central body pulls . For Earth μ = 398600 km 3 / s 2 .
Why bundle them? We can measure μ from spacecraft motion far more precisely than G and M separately, and only the product ever appears in orbit formulas.
Definition Specific orbital energy
ε
ε = 2 v 2 − r μ
The first term is kinetic ("energy of motion"), the second is gravitational potential ("energy of position"). Their sum per unit mass is ε , and it is constant along the whole orbit .
Why the topic needs it: energy fixes the size through a = − μ / ( 2 ε ) . A tighter, smaller orbit sits deeper in the well (more negative ε ). This is a cousin of the vis-viva relation.
The sign of ε decides the shape of path entirely: negative = bound ellipse, zero = escape (parabola), positive = flyby (hyperbola).
Now we meet the geometry itself. Follow figure s04 as you read — it labels every quantity below on one drawing.
Definition Semi-major axis
a
Half the length of the ellipse's longest diameter — the "size" number, written with the plain letter a (this is the reserved meaning warned about in section 1). In figure s04 it is half of the double-headed cyan arrow labelled 2 a . Big a = big orbit.
e
A single number for how squished the ellipse is. e = 0 is a perfect circle; as e → 1 the ellipse stretches into a long cigar. Always 0 ≤ e < 1 for a closed orbit.
Definition Periapsis, apoapsis, and
p
Periapsis is the point of closest approach to the central body; distance a ( 1 − e ) . It is the white dot nearest the amber focus in figure s04.
Apoapsis is the farthest point; distance a ( 1 + e ) — the white dot on the opposite side.
The semi-latus rectum p = a ( 1 − e 2 ) = h 2 / μ is the orbit's "width" at the central body — the amber up-arrow rising from the focus in figure s04. It packages a and e into the single quantity the orbit equation wants.
ν (defined here, used below)
ν is the angle at the central body, measured from periapsis to the body's current position . At periapsis ν = 0 ; at apoapsis ν = 18 0 ∘ .
Two more arrows must be built before the orientation angles have anything to grab onto.
n and the ascending node
The ascending node is where the orbit crosses the reference plane going upward . The node vector n = z ^ × h is an arrow lying in the reference plane that points from the origin toward that crossing . Its length is n = ∣ n ∣ .
i
The tilt of the orbit plane away from the reference plane, measured between z ^ and h (both "up" arrows). cos i = h z / h . Since i ranges only from 0 to 18 0 ∘ , cos − 1 alone suffices — no sign check needed .
Definition Right ascension of the ascending node
Ω
The swivel angle of the node line around z ^ , measured from x ^ . cos Ω = n x / n .
Quadrant check: if n y < 0 , then Ω = 36 0 ∘ − Ω . (Companion sign: the y -reach of n tells which half of the swivel we are in.)
Definition Argument of periapsis
ω
Inside the orbit plane, the angle from the ascending node (n ) to periapsis (e ) . cos ω = ( n ⋅ e ) / ( n e ) .
Quadrant check — do it right: the correct companion test is the sign of ( n × e ) ⋅ h . If that triple product is negative , then ω = 36 0 ∘ − ω . Why this and not "e z < 0 "? We need to know whether periapsis lies on the upward-swung side of the node within the orbit plane , and h is the axis of that plane; testing against z ^ (i.e. e z ) only works for near-equatorial orbits and fails in general. A common equivalent shortcut for prograde orbits with the reference plane as equator is "if e z < 0 then ω = 36 0 ∘ − ω ," but the triple-product test is the one that is always correct.
Definition True-anomaly quadrant check
For ν (defined in section 9): cos ν = ( e ⋅ r ) / ( e r ) .
Quadrant check: if r ⋅ v < 0 , then ν = 36 0 ∘ − ν — a negative r ⋅ v means the body is falling toward periapsis, so it is on the "return" half.
Definition Orbital elements
The set ( a , e , i , Ω , ω , ν ) is the orbital elements — the second naming scheme the intro promised. Only ν changes with time; the other five stay fixed for an ideal orbit.
The definitions in section 10 quietly assume the arrows n and e are non-zero. When they shrink to zero, some angles become undefined — this is not a bug, it is geometry running out of landmarks.
Common mistake Circular orbit:
e = 0
If the orbit is a perfect circle there is no periapsis — every point is equally close. So e = 0 , its direction is meaningless, and ω and ν are undefined (there is no "start line" to measure from). Fix: replace them with the argument of latitude u = angle from the ascending node to the body, measured in-plane, which stays well-defined.
Common mistake Equatorial orbit:
i = 0 ∘ or i = 18 0 ∘
If the orbit lies flat in the reference plane it never crosses that plane, so there is no ascending node. Then h is parallel to z ^ , giving n = z ^ × h = 0 — and Ω (and ω , which is measured from the node) become undefined . Fix: use the true longitude of periapsis ϖ measured directly from x ^ .
Common mistake Both at once:
e = 0 and i = 0
A flat circle has neither a node nor a periapsis, so Ω , ω , and ν are all undefined — only a , e , i survive plus the true longitude ℓ from x ^ to the body. The systematic cure for all these gaps is a re-parameterisation with no singularities: equinoctial elements .
position r and velocity v
sign checks for quadrants
Convert elements and state vectors
Definition A rotation matrix
A rotation matrix is a grid of numbers that, when multiplied onto a vector, spins that arrow by a fixed angle without changing its length. R 3 ( θ ) spins about the z ^ axis; R 1 ( θ ) spins about the x ^ axis. Their explicit forms (with c = cos θ , s = sin θ ) are:
R 3 ( θ ) = c s 0 − s c 0 0 0 1 , R 1 ( θ ) = 1 0 0 0 c s 0 − s c
Why the topic needs it: Direction B first builds r , v in the easy perifocal frame, then applies R 3 ( − Ω ) R 1 ( − i ) R 3 ( − ω ) to swivel–tilt–spin the arrows into the real inertial frame — three simple turns instead of one messy formula. Notice R 3 leaves the z -row untouched (it turns only in the x y -plane) and R 1 leaves the x -row untouched (it turns only in the y z -plane) — exactly the "spin about that axis" behaviour their names promise. To turn the fixed elements into a time you additionally need Kepler's equation and time-of-flight .
Cover each answer and test yourself — if any is shaky, re-read its section before the parent note.
What is the difference between r and r ? r is the arrow (position, 3 numbers);
r = ∣ r ∣ is just its length (distance), one positive number.
Why is the plain letter a not a vector magnitude on this page? Because
a is reserved for the semi-major axis; a generic arrow's length is always written
∣ a ∣ , never bare
a .
What is the dot product formula in terms of θ , and why is cos θ there? a ⋅ b = ∣ a ∣∣ b ∣ cos θ ;
cos θ measures how much the two arrows point the same way (1 aligned, 0 perpendicular, −1 opposite).
What does the sign of r ⋅ v tell you? Positive → moving away from the central body (ν < 18 0 ∘ ); negative → moving toward it (ν > 18 0 ∘ ).
What does the cross product r × v give you geometrically? A new arrow (
h ) perpendicular to the orbit plane; its length is twice the areal sweep rate.
Why is h useful for finding orientation? It is constant and perpendicular to the plane, so it fixes both inclination i and node swivel Ω .
What does the eccentricity vector e encode, and what is its length? It points toward periapsis and its length is exactly the eccentricity,
∣ e ∣ = e ; its formula is
e = μ 1 [( v 2 − μ / r ) r − ( r ⋅ v ) v ] .
What is the correct quadrant test for ω ? The sign of
( n × e ) ⋅ h ; if negative,
ω = 36 0 ∘ − ω (the
e z < 0 shortcut only works for equatorial-referenced prograde orbits).
What does specific energy ε determine, and via what formula? The orbit size: a = − μ / ( 2 ε ) .
What is μ and why use it instead of G and M separately? μ = GM , the pull strength; only the product appears in orbit maths and it is measured more precisely than G or M alone.
Define a , e , and p in one line each. a = half the longest diameter (size); e = squish (0 circle → 1 cigar); p = a ( 1 − e 2 ) = orbit width used in r = p / ( 1 + e cos ν ) .
Why does the orbit equation give smallest r at ν = 0 ? Because cos 0 = 1 makes the denominator 1 + e largest, so r = p / ( 1 + e ) = a ( 1 − e ) (periapsis).
Which companion sign fixes each angle's quadrant? n y for
Ω ,
( n × e ) ⋅ h for
ω ,
r ⋅ v for
ν ;
i needs none.
When do ω and Ω become undefined, and what replaces them? ω , ν undefined when e = 0 (use argument of latitude u ); Ω undefined when i = 0 (use true longitude); equinoctial elements cure both.
Write R 3 ( θ ) and R 1 ( θ ) . R 3 has [ c , − s , 0 ; s , c , 0 ; 0 , 0 , 1 ] (untouched z ); R 1 has [ 1 , 0 , 0 ; 0 , c , − s ; 0 , s , c ] (untouched x ).