The 'orbital speed' of a body, generally a
planet, a
natural satellite, an
artificial satellite, or a
multiple star, is the speed at which it
orbits around the
barycenter of a system, usually around a more
massive body. It can be used to refer to either the mean orbital speed, the average speed as it completes an orbit, or instantaneous orbital speed, the speed at a particular point in its orbit.
The orbital speed at any position in the orbit can be computed from the distance to the central body at that position, and the
specific orbital energy, which is independent of position: the
kinetic energy is the total energy minus the
potential energy.
Thus, under
standard assumptions the orbital speed (
) is:
★ in general:
★
★
elliptic orbit:
★
★
parabolic trajectory:
★
★
hyperbolic trajectory:
where:
★
is the
standard gravitational parameter
★
is the distance between the
orbiting body and the
central body
★
is the
specific orbital energy
★
is the
semi-major axis
Note:
★ Velocity does not explicitly depend on
eccentricity but is determined by length of
semi-major axis (
),
Radial trajectories
In the case of radial motion:
★ if the energy is non-negative: the motion is either for the whole trajectory away from the central body, or for the whole trajectory towards it. For the zero-energy case, see
escape orbit and
capture orbit.
★ if the energy is negative: the motion can be first away from the central body, up to r=μ/|ε|, then falling back. This is the limit case of an orbit which is part of an ellipse with eccentricity tending to 1, and the other end of the ellipse tending to the center of the central body. See also
free-fall time.
Transverse orbital speed
The transverse orbital speed is inversely proportional to the distance to the central body because of the law of conservation of
angular momentum, or equivalently,
Kepler's
second law. This states that as a body moves around its orbit during a fixed amount of time, the line from the barycenter to the body sweeps a constant area of the orbital plane, regardless of which part of its orbit the body traces during that period of time. This means that the body moves faster near its
periapsis than near its
apoapsis, because at the smaller distance it needs to trace a greater arc to cover the same area. This law is usually stated as "equal areas in equal time."
Mean orbital speed
For 'orbits with small
eccentricity', the length of the orbit
is close to that of a circular one, and the mean orbital speed can be approximated either from observations of the
orbital period and the
semimajor axis of its orbit, or from knowledge of the
masses of the two bodies and the semimajor axis.
:
:
where
is the orbital velocity,
is the
length of the
semimajor axis,
is the orbital period, and
is the
standard gravitational parameter. Note that this is only an approximation that holds true when the orbiting body is of considerably lesser mass than the central one, and eccentricity is close to zero.
'Taking into account the mass of the orbiting body',
:
where
is now the mass of the body under consideration,
is the mass of the body being orbited, and
is specifically the distance between the two bodies (which is the sum of the distances from each to the center of mass). This is still a simplified version; it doesn't allow for
elliptical orbits, but it does at least allow for bodies of similar masses.
For an 'object in an eccentric orbit' orbiting a much larger body, the length of the orbit decreases with eccentricity
, and is given at
ellipse.
This can be used to obtain a more accurate estimate of the average orbital speed:
:
[1]
The mean orbital speed decreases with eccentricity.
See also
★
examples
References
1. Handbook of Mathematics and Computational Science, H. St̀eocker, J. Harris, , , Springer, 1998, ISBN 0387947469