Earth Orbit Calculator

Calculate orbital parameters for satellites and spacecraft orbiting Earth.

Determine orbital period, velocity, escape velocity, and gravitational force based on altitude and satellite mass using Kepler's laws and orbital mechanics.

Examples

Click on any example to load it into the calculator.

Low Earth Orbit (LEO)

Low Earth Orbit (LEO)

Typical orbit for Earth observation satellites and the International Space Station.

Altitude: 400 km

Mass: 1000 kg

Eccentricity: 0.001

Medium Earth Orbit (MEO)

Medium Earth Orbit (MEO)

Common orbit for GPS and navigation satellites.

Altitude: 20200 km

Mass: 1500 kg

Eccentricity: 0.002

Geostationary Orbit (GEO)

Geostationary Orbit (GEO)

Communication satellites that stay fixed above one point on Earth.

Altitude: 35786 km

Mass: 2000 kg

Eccentricity: 0.0001

Small Satellite (CubeSat)

Small Satellite (CubeSat)

Modern small satellite in low Earth orbit.

Altitude: 500 km

Mass: 10 kg

Eccentricity: 0.005

Other Titles
Understanding Earth Orbit Calculator: A Comprehensive Guide
Explore the fundamental principles of orbital mechanics and learn how satellites maintain their paths around Earth. This guide covers everything from basic orbital parameters to advanced space science concepts.

What is the Earth Orbit Calculator?

  • Core Concepts
  • Why It Matters
  • Kepler's Laws in Action
The Earth Orbit Calculator is a sophisticated tool that applies the fundamental laws of orbital mechanics to calculate the behavior of satellites and spacecraft orbiting our planet. It uses Kepler's laws of planetary motion, Newton's law of universal gravitation, and the principles of celestial mechanics to determine orbital parameters such as period, velocity, and gravitational forces. This calculator bridges the gap between theoretical physics and practical space applications, making complex orbital calculations accessible to students, engineers, and space enthusiasts.
The Physics Behind Orbital Motion
Orbital motion is governed by the delicate balance between gravitational force and the satellite's inertia. Earth's gravity constantly pulls the satellite toward the planet's center, while the satellite's forward motion creates a centrifugal force that pushes it outward. When these forces are perfectly balanced, the satellite follows a stable orbital path. The calculator uses the universal gravitational constant (G = 6.67430 × 10^-11 m³/kg·s²), Earth's mass (5.972 × 10^24 kg), and Earth's radius (6,371 km) to perform these calculations with high precision.
Kepler's Laws: The Foundation of Orbital Mechanics
Johannes Kepler's three laws of planetary motion, formulated in the early 17th century, form the mathematical foundation of our understanding of orbital motion. The first law states that planets (and satellites) move in elliptical orbits with the central body at one focus. The second law describes how a satellite moves faster when closer to Earth and slower when farther away. The third law establishes the relationship between orbital period and distance from the central body. Our calculator implements these laws to provide accurate orbital predictions.
Real-World Applications
This calculator has numerous practical applications in modern space technology. Satellite engineers use these calculations to design communication satellites, Earth observation systems, and navigation networks. Space agencies rely on orbital mechanics for mission planning, from launching satellites to planning interplanetary missions. Even amateur astronomers and space enthusiasts can use this tool to understand satellite passes and predict when satellites will be visible from their location.

Key Orbital Parameters Explained:

  • Orbital Period: The time it takes for a satellite to complete one full orbit around Earth. Lower orbits have shorter periods.
  • Orbital Velocity: The speed at which the satellite travels along its orbital path. Higher altitudes result in slower velocities.
  • Escape Velocity: The minimum speed required for an object to break free from Earth's gravitational pull at a given altitude.
  • Gravitational Force: The force of attraction between Earth and the satellite, which decreases with the square of the distance.

Step-by-Step Guide to Using the Calculator

  • Understanding Inputs
  • Interpreting Results
  • Practical Applications
Using the Earth Orbit Calculator effectively requires understanding both the input parameters and the physical meaning of the results. This step-by-step guide will help you navigate the calculations and interpret the results correctly.
1. Orbital Altitude: The Foundation Parameter
Orbital altitude is measured from Earth's surface, not from the center of the planet. This is the most critical parameter as it directly affects all other orbital characteristics. Low Earth Orbit (LEO) ranges from 160 to 2,000 km, Medium Earth Orbit (MEO) from 2,000 to 35,786 km, and Geostationary Orbit (GEO) at exactly 35,786 km. The calculator automatically adds Earth's radius to determine the total distance from Earth's center for gravitational calculations.
2. Satellite Mass: Understanding Its Role
While satellite mass affects the gravitational force between Earth and the satellite, it does not influence the orbital period or velocity. This is a counterintuitive but fundamental principle of orbital mechanics. A 1-kg satellite and a 1,000-kg satellite at the same altitude will have identical orbital periods and velocities. The mass only affects the gravitational force and the energy required to change the orbit.
3. Orbital Eccentricity: Shape Matters
Eccentricity describes how circular or elliptical an orbit is. A value of 0 represents a perfect circle, while values approaching 1 represent highly elliptical orbits. Most operational satellites use near-circular orbits (eccentricity < 0.01) for stability and predictable coverage. The calculator uses this parameter to refine the orbital calculations, though for most practical purposes, circular orbit approximations are sufficient.
4. Analyzing the Results
The calculator provides four key results: orbital period (in hours), orbital velocity (in km/s), escape velocity (in km/s), and gravitational force (in Newtons). Compare these values with known satellite parameters to verify accuracy. For example, the International Space Station orbits at about 400 km altitude with a period of approximately 92 minutes, which should match your calculations for similar parameters.

Typical Orbital Parameters by Altitude:

  • LEO (400 km): Period ~92 min, Velocity ~7.7 km/s, Escape Velocity ~11.1 km/s
  • MEO (20,200 km): Period ~12 hours, Velocity ~3.9 km/s, Escape Velocity ~5.5 km/s
  • GEO (35,786 km): Period ~24 hours, Velocity ~3.1 km/s, Escape Velocity ~4.3 km/s

Real-World Applications and Space Missions

  • Communication Satellites
  • Earth Observation
  • Navigation Systems
The principles calculated by this tool are fundamental to virtually every space mission and satellite operation. Understanding these orbital parameters is crucial for mission planning, satellite design, and space operations.
Communication Satellite Networks
Geostationary satellites at 35,786 km altitude provide continuous coverage over specific regions of Earth. These satellites have a 24-hour orbital period, matching Earth's rotation, so they appear stationary from the ground. The calculator helps engineers determine the exact altitude needed for geostationary orbit and calculate the velocity requirements for station-keeping maneuvers.
Earth Observation and Remote Sensing
Low Earth Orbit satellites provide high-resolution imaging and frequent revisits. The calculator helps determine optimal altitudes for different observation requirements. Lower altitudes provide better resolution but require more frequent orbital corrections due to atmospheric drag. Higher altitudes offer broader coverage but lower resolution.
Global Navigation Satellite Systems (GNSS)
GPS, Galileo, and other navigation systems use Medium Earth Orbits to provide global coverage with reasonable signal strength. The calculator helps determine the optimal altitude for balancing coverage area, signal strength, and orbital stability. These systems require precise orbital knowledge for accurate positioning calculations.

Common Misconceptions and Orbital Myths

  • Weightlessness in Space
  • Orbital Speed Myths
  • Gravity in Space
Space and orbital mechanics are often misunderstood, leading to common misconceptions about how satellites and spacecraft operate.
Myth: There's No Gravity in Space
This is one of the most common misconceptions. Gravity exists everywhere in space, including in Earth orbit. The International Space Station experiences about 90% of Earth's surface gravity. What astronauts experience as 'weightlessness' is actually free-fall - they're falling toward Earth at the same rate as their spacecraft. The calculator shows that gravitational force decreases with distance but never reaches zero.
Myth: Satellites Need Engines to Stay in Orbit
Once in a stable orbit, satellites don't need continuous propulsion to maintain their path. Orbital motion is a natural consequence of the balance between gravity and inertia. However, satellites do need occasional propulsion for station-keeping (maintaining their position), attitude control, and orbital corrections due to perturbations from the Moon, Sun, and Earth's non-uniform gravity field.
Myth: Higher Orbits Mean Faster Satellites
Actually, the opposite is true. Satellites in higher orbits move slower than those in lower orbits. This is a direct consequence of Kepler's laws. The calculator demonstrates this relationship - a satellite at 400 km altitude moves at about 7.7 km/s, while one at 35,786 km moves at only 3.1 km/s. However, higher orbits have longer periods, so satellites take more time to complete one revolution.

Expert Insight:

  • The most efficient way to reach higher orbits is to increase velocity at the lowest point of the orbit, not to apply continuous thrust. This is the principle behind Hohmann transfer orbits.

Mathematical Derivation and Advanced Concepts

  • Kepler's Third Law
  • Escape Velocity Derivation
  • Orbital Energy
The calculations performed by this calculator are based on well-established physical laws and mathematical relationships. Understanding the underlying mathematics helps verify the results and appreciate the elegance of orbital mechanics.
Kepler's Third Law and Orbital Period
Kepler's third law states that the square of the orbital period is proportional to the cube of the semi-major axis. For circular orbits, this becomes T² = (4π²/GM) × r³, where T is the period, G is the gravitational constant, M is Earth's mass, and r is the orbital radius. This law explains why higher orbits have longer periods and why the relationship is not linear.
Orbital Velocity and Centripetal Force
Orbital velocity is determined by balancing the gravitational force with the required centripetal force for circular motion. The equation v = √(GM/r) shows that orbital velocity decreases with the square root of the orbital radius. This is why satellites in higher orbits move slower, despite having more gravitational potential energy.
Escape Velocity and Energy Considerations
Escape velocity is the minimum speed needed for an object to overcome Earth's gravitational pull. It's calculated as v_escape = √(2GM/r), which is √2 times the circular orbital velocity at the same altitude. This relationship shows that escape velocity is always greater than orbital velocity, explaining why spacecraft need significant energy to leave Earth's orbit.

Mathematical Relationships:

  • Orbital Period: T = 2π√(r³/GM) where r = Earth radius + altitude
  • Orbital Velocity: v = √(GM/r) for circular orbits
  • Escape Velocity: v_escape = √(2GM/r) = √2 × orbital velocity
  • Gravitational Force: F = GMm/r² where m is satellite mass