Apoapsis and Periapsis Calculator

Apoapsis and Periapsis Calculator

Convert between semi-major axis, eccentricity, apoapsis, periapsis, altitude, period, and apsis speed with JSCalc-Blog.com.

Periapsisnearest point
Apoapsisfarthest point
Shapeeccentricity track
Selected attractorEarthRadius 6,378.137 km
Orbit shapeLow eccentricityNearly circular starter orbit
Apsis spread0 kmApoapsis radius - periapsis radius

🛰Real Orbit Presets

Apsis Solver Deck

Choose the pair of values you already know.
Radius is used to convert center distance to altitude.
Calculations use kilometers internally.
Use more decimals for small body or AU work.
Distance from orbit center to either apsis midpoint.
0 is circular; bound ellipses must be less than 1.
Nearest height above the selected body radius.
Farthest height above the selected body radius.
Formula route: ra = a(1+e), rp = a(1-e), then altitudes subtract the central body radius.

Orbit Apsis Results

Apoapsis distance ra 0 km Altitude 0 km
Periapsis distance rp 0 km Altitude 0 km
Axis and eccentricity a 0 km e = 0
Period and apsis speeds 0 min vₚ 0 km/s, vₚ 0 km/s

📌Selected Body Constants

6,378Radius km
398,600Mu km³/s²
7.91Circular speed at surface km/s
LEOCommon apsis reference

🔢Formula Breakdown

NeedUse this relationInputsMeaning
Apoapsis distancera = a(1 + e)a, eFarthest center distance
Periapsis distancerp = a(1 - e)a, eNearest center distance
Semi-major axisa = (ra + rp) / 2ra, rpAverage of apsis radii
Eccentricitye = (ra - rp) / (ra + rp)ra, rpHow stretched the ellipse is
Altitudeh = r - Rr, body radiusHeight above surface
Speed contextv = sqrt(mu(2/r - 1/a))mu, r, aVis-viva speed at each apsis

🌍Central Body Reference

BodyMean radiusMuTypical orbit use
Earth6,378.137 km398,600.4418 km³/s²LEO, MEO, GEO, lunar transfer
Moon1,737.4 km4,902.800 km³/s²Lunar mapping and landing orbits
Mars3,389.5 km42,828.3 km³/s²Mars relay and science orbiters
Sun695,700 km132,712,440,018 km³/s²Planet, comet, and transfer orbits
Jupiter69,911 km126,686,534 km³/s²High-energy moon tour orbits
Saturn58,232 km37,931,207.8 km³/s²Ring-plane and moon tour orbits
Venus6,051.8 km324,858.592 km³/s²Radar mapping and aerobrake orbits
Mercury2,439.7 km22,032.09 km³/s²Polar science mapping orbits

🛸Real Orbit Preset Data

PresetCentral bodyInput routeReference apsides
ISS low EarthEarthAltitude pairAbout 400 km x 420 km
Starlink shellEarthSemi-major axis and eAbout 550 km circular altitude
GPS navigationEarthAltitude pairAbout 20,180 km x 20,180 km
GeostationaryEarthAltitude pair35,786 km circular altitude
Molniya ellipseEarthAltitude pairAbout 600 km x 39,700 km
Moon around EarthEarthCenter distances363,300 km x 405,500 km
Mars TGO scienceMarsAltitude pairAbout 400 km x 400 km
Mercury around SunSunCenter distances46.0 million km x 69.8 million km
Halley heliocentricSunCenter distances0.586 AU x 35.1 AU from Sun center

📊Orbit Class Comparison

LEOAltitudes usually 160 to 2,000 km, short periods near 90 to 130 minutes.
MEONavigation constellations sit above LEO and below GEO, often near 20,000 km altitude.
GEOCircular equatorial Earth orbit at about 35,786 km altitude with a sidereal-day period.
HEOHighly elliptical paths use a low periapsis and very high apoapsis for long dwell time.
ClassTypical periapsisTypical apoapsisEccentricity cuePeriod cue
Low circular Earth400 km alt400 km altNear 0About 92 minutes
Sun-sync LEO600 km alt900 km altSmallAbout 96 to 103 minutes
GPS-style MEO20,180 km alt20,180 km altNear 0About 12 hours
Geostationary35,786 km alt35,786 km altNear 023 h 56 min
Molniya600 km alt39,700 km altHighAbout 12 hours
Comet-like solarBelow 1 AUTens of AUVery highYears to decades

🧭Eccentricity Quick Lookup

EccentricityOrbit shapeApsis behaviorCalculator check
0Circlera equals rpApoapsis and periapsis altitudes match
0.001 to 0.02Very mild ellipseSmall altitude swingCommon for maintained satellites
0.02 to 0.2Moderate ellipseVisible apsis spreadCheck both speeds separately
0.2 to 0.75Stretched ellipseLong dwell near apoapsisPeriod depends on a, not e alone
0.75 to 0.999Extreme ellipseVery fast periapsis passageConfirm periapsis clears the body

Apsis Tips

Distance versus altitude: ra and rp are measured from the center of the central body. Apoapsis altitude and periapsis altitude are found by subtracting the body radius, so a 400 km low Earth orbit has a center distance near 6,778 km.
Speed reading: for a bound ellipse, periapsis speed is higher than apoapsis speed. If the two speeds are almost identical, the eccentricity and apsis spread should also be small.

It is a little geometry and a little energy. Two numbers, the farthest point (apoapsis) and the closest point (periapsis) (form the shape of an ellipse). They determines everything, from fuel budgets to communication windows. And they tell the story of every orbit in two numbers. What is the relationship between these points? This turns the complex ideas of orbital mechanics into a practical engineering problem. The calculator on this page will solve it for you by doing all of the heavy lifting. It turn the values you know into a full orbital picture without you having to remember Kepler’s laws.

Altitude is what most mission parameters specify, and that’s where most people begin. They say they’re launching something to four hundred kilometers, for example, not sixty seven hundred and eighty kilometers from Earth’s center. That makes all the difference in the world, since center-to-center distance is what gravity equation takes as an input. Plugging the surface altitude directly into a formula designed to take radius as input will give you wildly incorrect values.

How Orbit Calculations Work

To avoid this problem, the tool simply converts it to radius automaticaly when you choose the central body. It extracts the appropriate radius from its own database of information. It then keeps track of that value and uses it throughout the rest of the calculation. This prevents the common mistake of forgetting to add or subtract the planet’s radius which can result in a crash instead of a stable orbit.

And then there’s the hidden variable: eccentricity. That’s just a number between zero and one that explains how stretched out the orbit is. Zero mean a perfect circle where the closest and farthest points are the same. Increasing values toward one stretch out the orbit, producing a big contrast between far point and close point. And that shape determines how fast things go. At periapsis, they’re zipping along; at apoapsis, they’re crawling. They do this because angular momentum is conserved. For an orbit highly stretched out, the object may stay for much of its time out at the far end, ideal for communicating with high-latitude areas. The calculator depicts this tradeoff showing how modestley changing the eccentricity can cause a huge shift in velocities at both apsides and hence the period.

It’s also key to select an appropriate reference body. Mu (a.k.a. The gravitational parameter differs greatly throughout the solar system. At any given radius, Mars will pull far less than Jupiter. Because of this it takes much longer to complete an orbit around Jupiter. To visualize how different they are, take a look at the pre-set buttons on the page. They range from the small, close-in loop of the International Space Station to the wide-open and elongated ellipse of a comet such as Halley. Seeing them all together helps put your numbers into context. Perhaps you’ll discover that your proposed lunar transfer orbit needs to have a much larger apoapsis then anticipated, or that you could still maintain a fairly circular science orbit around Mars even though it’s smaller.

Speed calculations shows how much energy is needed to maintain such a shape. The vis-viva equation demonstrates how velocity depends on position and the semi-major axis. It also shows that you pay a premium for high orbits. If you want to raise your apoapsis, you need an exact burn at periapsis. The Oberth effect applies here making fuel more efficient. Aerobraking by lowering your periapsis involves careful timing, too late and you’ll burn up. These is not abstract concepts but constraints that determine spacecraft design and mission length.

With this tool, you can check whether your proposed maneuvers are physically possible based off your available delta-v. You can also get those speeds instently.

Orbital mechanics can be boiled down to constraint management. There’s no setting everything as you please. If you set one thing, something else is locked in. Set the semi-major axis; you’ve pinned down your average distance. Set the period; set the periapsis; and let geometry dictate the apoapsis. Is it restrictive? Sure. But it clears things up. No more guesswork; now there’s design.

You get that concrete feeling that all those unseen forces line up when you see the numbers fall into place. Whether you’re thinking about a hypothetical mission or simply wondering how satellites remain in orbit, it’s about understanding the math behind them. And although it’s cruel, it’s beautiful. When you realize that the periapsis and apoapsis constrains the orbit, suddenly the madness of spaceflight starts to resemble a solved problem.

Apoapsis and Periapsis Calculator