
A small body in space orbits a large one (like a planet around the sun) along an elliptical path, with the large body being located at one of the
ellipse foci.

Two bodies with similar mass orbiting around a common
barycenter with elliptic orbits.
In
astrodynamics or
celestial mechanics an
elliptic orbit is a
Kepler orbit with the
eccentricity greater than 0 and less than 1. In a
gravitational two-body problem with the eccentricity in this range both bodies follow
similar elliptic orbits with the same
orbital period around their common
barycenter. Also the relative position of one body with respect to the other follows an elliptic orbit.
Specific energy of an elliptical orbit is negative.
An orbit with an eccentricity of 0 is a
circular orbit. Examples of elliptic orbits include:
Hohmann transfer orbit,
Molniya orbit and
tundra orbit.
Velocity
Under
standard assumptions the
orbital speed (
) of a body traveling along
elliptic orbit can be computed from the
Vis-viva equation as:
where:
Conclusion:
- Velocity does not depend on eccentricity but is determined by length of semi-major axis (),
- Velocity equation is similar to that for hyperbolic trajectory with the difference that for the latter, is positive.
Orbital period
Under
standard assumptions the
orbital period (
) of a body traveling along an elliptic orbit can be computed as:
where:
Conclusions:
Energy
Under
standard assumptions,
specific orbital energy (
) of elliptic orbit is negative and the orbital energy conservation equation (the
Vis-viva equation) for this orbit can take the form:
where:
Conclusions:
Using the
virial theorem we find:
- the time-average of the specific potential energy is equal to 2ε
- *the time-average of r-1 is a-1
- the time-average of the specific kinetic energy is equal to -ε
Flight path angle
where:
- is the flight path angle
Equation of motion
Orbital parameters
The state of an orbiting body at any given time is defined by the orbiting body's position and velocity with respect to the central body, which can be represented by the three-dimensional
Cartesian coordinates (position of the orbiting body represented by x, y, and z) and the similar Cartesian components of the orbiting body's velocity. This set of six variables, together with time, are called the
orbital state vectors. Given the masses of the two bodies they determine the full orbit. The two most general cases with these 6 degrees of freedom are the elliptic and the hyperbolic orbit. Special cases with less degrees of freedom are the circular and parabolic orbit.
Because at least six variables are absolutely required to completely represent an elliptic orbit with this set of parameters, then six variables are required to represent an orbit with any set of parameters. Another set of six parameters that are commonly used are the
orbital elements.
Solar system
It is commonly thought that in the Solar System,
planets,
asteroids,
comets and
space debris have elliptical orbits around the Sun, relative to the Sun.
See also