Intuition What this page is
The parent note proved h = GM p and showed a few clean cases. Here we hunt down every kind of problem this one formula can hand you: circles, ellipses, the special apside points, degenerate limits (radial fall, parabola, straight line), a mid-orbit point where r and v are not perpendicular, a word problem, and an exam trap. Guess each answer before reading the steps — that "Forecast" habit is how the ideas stick.
Before anything, one refresher so no symbol is unearned:
Definition The three players
GM — the central pull strength (gravitational parameter), units m 3 / s 2 . For Earth G M ⊕ = 3.986 × 1 0 14 .
h = ∣ r × v ∣ — specific angular momentum, units m 2 /s . It is r v sin ϕ where ϕ is the angle between the position arrow r and the velocity arrow v (Flight-path angle ).
p = h 2 / GM — semi-latus rectum, the orbit's "half-width at the focus"; and p = a ( 1 − e 2 ) .
Every problem on this topic lives in exactly one of these cells. The examples below tick off each one.
Cell
What makes it special
Which tool you reach for
Example
A Circle, e = 0
p = a = r , speed constant
h = GM r = v c i r c r
Ex 1
B Ellipse at an apside
v ⊥ r , so sin ϕ = 1
h = r p v p = r a v a
Ex 2
C Ellipse at a general point
v ⊥ r
h = r v sin ϕ
Ex 3
D Geometry → h
given a , e only
p = a ( 1 − e 2 ) , then h = GM p
Ex 4
E Degenerate: parabola limit
e → 1 , a → ∞
keep p finite
Ex 5
F Degenerate: radial drop
h = 0 , straight-line fall
sin ϕ = 0
Ex 6
G Real-world word problem
GEO / apogee-kick style
mix B and D
Ex 7
H Exam twist / trap
wrong-quadrant, unit trap
careful sin ϕ , vs /2
Ex 8
Signs & special values covered: e = 0 (A), 0 < e < 1 (B,C,D,G), e = 1 (E), h = 0 (F); angle ϕ = 9 0 ∘ (B), ϕ = 9 0 ∘ (C,H), ϕ = 0 ∘ (F). Constants: G M ⊕ = 3.986 × 1 0 14 m 3 / s 2 throughout.
Worked example Ex 1 — Circular orbit at
r = 7000 km
A satellite circles Earth at radius r = 7 × 1 0 6 m . Find h two ways.
Forecast: in a circle every point is a "peri = apo", so h = r v with v constant. Guess: is h near 5 × 1 0 10 or 5 × 1 0 12 ?
Circle means e = 0 , so p = a = r = 7 × 1 0 6 m .
Why this step? p = a ( 1 − e 2 ) collapses to a when e = 0 , and for a circle a = r .
Plug into the master formula:
h = GM p = 3.986 × 1 0 14 ⋅ 7 × 1 0 6 = 2.79 × 1 0 21 ≈ 5.28 × 1 0 10 m 2 /s .
Why this step? h = GM p is the whole topic; here p is just the radius.
Cross-check via speed: circular speed v = GM / r = 3.986 × 1 0 14 /7 × 1 0 6 = 7546 m/s .
Why this step? In a circle v ⊥ r everywhere, so h = r v directly.
Verify: r v = 7 × 1 0 6 ⋅ 7546 = 5.28 × 1 0 10 m 2 /s ✓ matches step 2. Units: m 3 / s 2 ⋅ m = m 4 / s 2 = m 2 /s ✓.
Worked example Ex 2 — Periapsis data
→ h , p , e
At periapsis a probe has r p = 8000 km = 8 × 1 0 6 m and v p = 9.0 km/s = 9000 m/s . Find h , p , and e .
Forecast: at periapsis v is exactly tangential (see the figure: the velocity arrow is perpendicular to the radius). So h = r p v p with no sin loss. Guess whether e comes out ∼ 0.6 or ∼ 0.06 .
h = r p v p sin 9 0 ∘ = r p v p = 8 × 1 0 6 ⋅ 9000 = 7.2 × 1 0 10 m 2 /s .
Why this step? At an apside the flight-path angle ϕ = 9 0 ∘ , so sin ϕ = 1 — this is cell B's whole trick.
p = GM h 2 = 3.986 × 1 0 14 ( 7.2 × 1 0 10 ) 2 = 1.301 × 1 0 7 m ≈ 13 , 010 km .
Why this step? Invert h = GM p .
From r p = 1 + e p : e = r p p − 1 = 8000 13010 − 1 = 0.626 .
Why this step? Periapsis is θ = 0 in the orbit equation, the cleanest place to read e .
Verify: rebuild r p = p / ( 1 + e ) = 1.301 × 1 0 7 /1.626 = 8.0 × 1 0 6 m ✓. Since 0 < e < 1 the orbit is a genuine ellipse ✓.
h from a mid-orbit snapshot
Somewhere between apsides a spacecraft has r = 1.0 × 1 0 7 m , speed v = 6500 m/s , and the angle between r and v is ϕ = 5 0 ∘ . Find h , then p .
Forecast: here v is tilted relative to r (figure). If you forget the sin ϕ you'll overshoot. Guess: is h bigger or smaller than r v ?
Use the general relation h = r v sin ϕ .
Why this step? h = ∣ r × v ∣ and a cross product's magnitude is r v sin ( angle between them ) . Only the component of v perpendicular to r contributes to sweeping area.
sin 5 0 ∘ = 0.766 , so h = 1.0 × 1 0 7 ⋅ 6500 ⋅ 0.766 = 4.98 × 1 0 10 m 2 /s .
Why this step? Plug numbers; note it is less than r v = 6.5 × 1 0 10 — the tilt "wastes" some speed radially.
p = h 2 / GM = ( 4.98 × 1 0 10 ) 2 /3.986 × 1 0 14 = 6.22 × 1 0 6 m .
Why this step? Same inversion as always.
Verify: h / ( r v ) = 4.98 × 1 0 10 /6.5 × 1 0 10 = 0.766 = sin 5 0 ∘ ✓. And h < r v as forecast because ϕ = 9 0 ∘ ✓.
Worked example Ex 4 — Given the ellipse's shape only
A Molniya-like orbit has semi-major axis a = 2.66 × 1 0 7 m and eccentricity e = 0.74 . Find h .
Forecast: never use p = a here (that's only for circles!). We must shrink a by ( 1 − e 2 ) . Guess whether h is above or below the circular value GM a .
p = a ( 1 − e 2 ) = 2.66 × 1 0 7 ( 1 − 0.7 4 2 ) = 2.66 × 1 0 7 ⋅ 0.4524 = 1.203 × 1 0 7 m .
Why this step? p = a ( 1 − e 2 ) is the bridge between "size" a and the h -carrying half-width p .
h = GM p = 3.986 × 1 0 14 ⋅ 1.203 × 1 0 7 = 4.795 × 1 0 21 = 6.93 × 1 0 10 m 2 /s .
Why this step? The master formula, now that p is known.
Verify: the "if it were a circle of the same a " value is GM a = 3.986 × 1 0 14 ⋅ 2.66 × 1 0 7 = 1.03 × 1 0 11 , and indeed 6.93 × 1 0 10 < 1.03 × 1 0 11 ✓ — eccentric orbits carry less h for the same a (they're skinnier at the focus). Units ✓.
Worked example Ex 5 — Escape (parabolic) trajectory
A comet grazes periapsis at r p = 5.0 × 1 0 10 m on a parabolic (e = 1 ) escape path. Find h . What happens to a ?
Forecast: parabola means "just barely unbound". The semi-major axis blows up (a → ∞ ), yet p stays finite. Can we still get a finite h ?
For e = 1 : r p = 1 + e p = 2 p , so p = 2 r p = 1.0 × 1 0 11 m .
Why this step? The periapsis form still holds for any e ; set e = 1 .
a = 1 − e 2 p = 0 p → ∞ — undefined/infinite.
Why this step? 1 − e 2 = 0 at e = 1 ; the ellipse formula degenerates. This is why we work with p , not a , in the limit.
h = GM p = 3.986 × 1 0 14 ⋅ 1.0 × 1 0 11 = 3.986 × 1 0 25 = 6.31 × 1 0 12 m 2 /s .
Why this step? p is finite, so h is perfectly finite even though a isn't.
Verify: parabolic periapsis speed should be escape speed v esc = 2 GM / r p . Check h = r p v esc = r p 2 GM / r p = 2 GM r p = 2 ⋅ 3.986 × 1 0 14 ⋅ 5 × 1 0 10 = 6.31 × 1 0 12 ✓ — matches, and equals GM ⋅ 2 r p = GM p ✓.
Worked example Ex 6 — Straight drop toward the centre
A stone is released from rest above the Earth and falls straight down. At one instant r = 1.0 × 1 0 7 m , v = 3000 m/s , but v points directly toward the centre (ϕ = 0 ∘ ). Find h and p .
Forecast: if the velocity is aimed straight at the focus, is any area being swept? Guess h = 0 — but prove it.
h = r v sin ϕ = 1.0 × 1 0 7 ⋅ 3000 ⋅ sin 0 ∘ = 0 .
Why this step? r and v are parallel (or anti-parallel), so their cross product vanishes — no perpendicular velocity component, no sweeping.
p = h 2 / GM = 0 .
Why this step? A "line" orbit has zero half-width: the conic has collapsed to a radial segment (e = 1 and p = 0 , a degenerate straight line).
Verify: Kepler's Second Law says d A / d t = h /2 = 0 — the radius sweeps no area, consistent with motion straight along the radius ✓. Units: m 2 /s , value 0 ✓.
Worked example Ex 7 — Geostationary transfer orbit (GTO)
A satellite sits on a transfer ellipse with perigee radius r p = 6.578 × 1 0 6 m (200 km altitude) and apogee radius r a = 4.216 × 1 0 7 m (GEO). Find h , p , e , and the perigee speed v p .
Forecast: two apside radii fix the whole ellipse. Guess whether v p is above or below LEO circular speed (≈ 7.9 km/s ).
Semi-major axis a = 2 r p + r a = 2 6.578 × 1 0 6 + 4.216 × 1 0 7 = 2.437 × 1 0 7 m .
Why this step? Peri and apo are the two ends of the major axis; their average is a .
Eccentricity e = r a + r p r a − r p = 4.874 × 1 0 7 3.558 × 1 0 7 = 0.730 .
Why this step? r a = a ( 1 + e ) , r p = a ( 1 − e ) ; subtract & divide.
p = a ( 1 − e 2 ) = 2.437 × 1 0 7 ( 1 − 0.73 0 2 ) = 2.437 × 1 0 7 ⋅ 0.4671 = 1.138 × 1 0 7 m .
Why this step? Cell D bridge, now with the derived a , e .
h = GM p = 3.986 × 1 0 14 ⋅ 1.138 × 1 0 7 = 6.735 × 1 0 10 m 2 /s .
Perigee speed: at an apside h = r p v p ⇒ v p = h / r p = 6.735 × 1 0 10 /6.578 × 1 0 6 = 10238 m/s ≈ 10.2 km/s .
Why this step? Cell B: at perigee v ⊥ r .
Verify: harmonic-mean check p 2 = r p 1 + r a 1 : RHS = 1/6.578 × 1 0 6 + 1/4.216 × 1 0 7 = 1.7576 × 1 0 − 7 , and 2/ p = 2/1.138 × 1 0 7 = 1.758 × 1 0 − 7 ✓. And v p = 10.2 > 7.9 km/s ✓ (you burn extra to raise apogee to GEO). Cross-check with Vis-viva equation v p = GM ( 2/ r p − 1/ a ) (see verify block).
Worked example Ex 8 — The two-trap question
"At a point on an orbit, r = 1.2 × 1 0 7 m , v = 5000 m/s , and the angle between velocity and the local horizontal (perpendicular to r ) is γ = 3 0 ∘ . A student writes h = GM ⋅ r v . Fix the two errors and find h and p ."
Forecast: two traps hide here — (i) GM ⋅ r v is nonsense (h = GM p , and r v isn't p ); (ii) the given angle is measured from the horizontal , not from r . Guess which angle goes into sin .
The angle between r and v is ϕ = 9 0 ∘ − γ = 6 0 ∘ , because γ (the Flight-path angle ) is measured off the local horizontal, while ϕ is measured off the radial line.
Why this step? sin ϕ needs the angle between the two vectors themselves; horizontal and radial differ by 9 0 ∘ .
h = r v sin ϕ = 1.2 × 1 0 7 ⋅ 5000 ⋅ sin 6 0 ∘ = 1.2 × 1 0 7 ⋅ 5000 ⋅ 0.8660 = 5.196 × 1 0 10 m 2 /s .
Why this step? The correct general formula, with the correct angle. (Equivalently h = r v cos γ .)
p = h 2 / GM = ( 5.196 × 1 0 10 ) 2 /3.986 × 1 0 14 = 6.774 × 1 0 6 m .
Why this step? Invert the master formula. The student's GM ⋅ r v = 3.986 × 1 0 14 ⋅ 6 × 1 0 10 = 1.55 × 1 0 13 would be off by ~300×, and dimensionally wrong (r v has units m 2 /s , not length).
Verify: h = r v cos γ = 6 × 1 0 10 ⋅ cos 3 0 ∘ = 6 × 1 0 10 ⋅ 0.8660 = 5.196 × 1 0 10 ✓ (matches step 2 since sin 6 0 ∘ = cos 3 0 ∘ ). Units of p : ( m 2 /s ) 2 / ( m 3 / s 2 ) = m ✓.
Common mistake The four traps this page kills
Using p = a for an ellipse (Ex 4/5) — use p = a ( 1 − e 2 ) .
Dropping sin ϕ off an apside (Ex 3/8) — h = r v only when v ⊥ r .
Confusing flight-path angle γ (from horizontal) with ϕ (from radial): ϕ = 9 0 ∘ − γ (Ex 8).
h = GM p — square root , never GM p /2 (parent mistake), never GM ⋅ r v .
Recall Scenario self-test
Which cell is "given a and e , find h "? ::: Cell D — compute p = a ( 1 − e 2 ) first.
Which cell gives h = 0 and why? ::: Cell F — radial fall, v ∥ r so sin ϕ = 0 .
In the parabolic limit what stays finite, a or p ? ::: p stays finite; a → ∞ (Cell E).
Given angle γ from the horizontal, what enters sin ? ::: ϕ = 9 0 ∘ − γ , i.e. h = r v cos γ (Cell H).