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Navigator · Module 4

Orbital speed: the vis-viva equation

One short equation gives the speed of anything in orbit at any point, if you know how far it is and the size of its orbit.

12 min

NASA/JPL/Space Science Institute

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Orbit Sandbox

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What is an orbit? Throw a ball sideways and it curves down to the ground. Throw it faster and it lands farther away. Throw it fast enough and the ground curves away beneath it as quickly as it falls, so it never lands: it keeps falling around the planet and always misses. That is an orbit. Nothing holds a satellite up; it is falling all the time.

What happens:

Speed now
Height now
One lap takes
Lowest height
Highest height

Try this

Falls back Orbits Escapes

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Fine-tune the orbit (orbital elements and Kepler's laws)

Astronomers describe an orbit with five numbers called orbital elements. Change them here; the height and speed above follow.

Fastest (periapsis)
Slowest (apoapsis)
Kepler's 3rd law check: T² / a³
How to use it
Sideways speed
This one control decides what happens. Too slow and it falls back. Fast enough and it goes round in a circle. Faster and it swings out into an ellipse. Faster than escape speed and it leaves for ever. The coloured bar under the slider shows where each begins at the chosen height.
Height
Where it starts. Higher up, gravity is weaker, so a slower speed is enough to stay in orbit.
Time speed
Real orbits take hours, days or years, so time runs faster here. Time ×1,000 means each second on screen is 1,000 seconds (about 17 minutes) in space. The planet's turning is sped up by the same amount. The numbers shown are always the real ones.
Ground track
The gold trail on the ground is the path directly beneath the satellite. Earth turns underneath the orbit, so each lap passes over different places.
Gold arrow
Which way it is moving and how fast: the longer the arrow, the faster.
Looking around
Drag to turn the view, scroll or pinch to zoom. The faint grid is the plane of Earth's equator (or, around the Sun, the plane of Earth's orbit).
Data table (text alternative)
Distance and speed at twelve equal time steps around the orbit
Time stepDistance from the Sun nowSpeed now

How fast is a spacecraft moving? Tell me how far it is from the planet and how big its orbit is, and one short equation answers the question anywhere along its path. Mission planners use it every day.

Earth seen through the seven windows of the International Space Station's Cupola.
Earth through the Cupola of the International Space Station, which circles the planet about every 90 minutes. Credit: NASA

One short equation gives the speed anywhere along an orbit.

Look

Anything in orbit is always trading height for speed, like a skateboarder on a half-pipe.

  • Falling closer to the central body, it speeds up.
  • Climbing away, it slows down.

In the sandbox the yellow arrow shows the speed: long arrow, fast; short arrow, slow. Watch it grow as the body swings in, and shrink as it climbs out.

Earth does the same thing, just gently because its orbit is almost circular: it moves about 30.3 km/s in early January and about 29.3 km/s in early July.

Understand

The vis-viva equation (“living force”, an old word for energy) gives the speed at any point:

v = √( μ · (2/r − 1/a) )

  • v: speed
  • μ: the central body’s gravitational parameter (GM)
  • r: current distance from the centre of the central body
  • a: semi-major axis of the orbit

Check it:

  • Circle (r = a): v = √(μ/a). That is the circular speed from the Newton lesson.
  • At periapsis, r is smallest, so 2/r is largest and v is fastest.
  • Very far away on an escape path (a → ∞): v = √(2μ/r). That is the escape speed, covered in the next lesson.

Worked example: Earth around the Sun, μ = 1.327 × 10¹¹ km³/s², a = 149.6 million km. At aphelion r = 152.1 million km:

v = √(1.327 × 10¹¹ × (2/1.521 × 10⁸ − 1/1.496 × 10⁸)) ≈ 29.3 km/s.

Master

Vis-viva is energy conservation in disguise. The specific orbital energy (energy per kilogram) is

ε = v²/2 − μ/r = −μ / (2a)

Kinetic plus potential energy is constant along the orbit and depends only on a. Solve for v and you get vis-viva. Consequences:

  • The sign of ε classifies the orbit: negative for ellipses, zero for a parabola, positive for a hyperbola.
  • At any given distance, the speed alone determines a. This is why a single engine burn at one point changes the size of the whole orbit, and why the next lessons can talk about delta-v budgets.

Apsis speeds follow from vis-viva with r = a(1 ± e):

v_p = √(μ/a · (1+e)/(1−e)),   v_a = √(μ/a · (1−e)/(1+e))

Their product is v_p · v_a = μ/a = v_circ², so the circular speed is the geometric mean of the two, not the arithmetic mean. That answers the Try it question.

Try it

With the Sun as central body, set a = 1 au and e = 0. Note the speed. Now raise e to 0.6 and compare the fastest and slowest speeds with that number. Is the average of the two equal to the circular speed?

Quick quiz

3 quick questions. Pick an answer to see if you are right.

  1. In the vis-viva equation, what happens to the speed as the body moves closer to the central body?

    1. A It increases
    2. B It decreases
    3. C It stays constant
    4. D It becomes zero
    Show the answer

    A. It increases

  2. For a circular orbit (r = a), vis-viva gives:

    1. A v = √(2μ/r)
    2. B v = √(μ/r)
    3. C v = μ/r
    4. D v = 0
    Show the answer

    B. v = √(μ/r)

  3. Earth moves about 29.8 km/s around the Sun on average. Roughly how fast at perihelion?

    1. A 29.3 km/s
    2. B 30.3 km/s
    3. C 35 km/s
    4. D 42 km/s
    Show the answer

    B. 30.3 km/s v_p = √(μ/a · (1+e)/(1−e)) with e = 0.0167 gives about 30.3 km/s.

Finish line

  • Played with the interactive
  • Read the lesson
  • Did the challenge
  • Took the quiz

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This lesson is licensed CC BY-SA 4.0.

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