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Gauss's method

Way to determine a preliminary orbit from initial observations in astronomy

  • 5 min read
  • 3 chapters

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Through Orbital mechanics, Direction cosine and Earth

Working in 1801, Carl Friedrich Gauss developed important mathematical techniques (summed up in Gauss's methods) which were specifically used to determine the orbit of Ceres. The method shown following is the orbit determination of an orbiting body about the focal body where the observations were taken from, whereas the method for determining Ceres' orbit requires a bit more effort because the observations were taken from Earth while Ceres orbits the Sun.

Observer position vector

The observer position vector (in Equatorial coordinate system) of the observation points can be determined from the latitude and local sidereal time (from Topocentric coordinate system) at the surface of the focal body of the orbiting body (for example, the Earth) via either:

Rn=[Re1−(2f−f2)sin2⁡ϕn+Hn]cos⁡ϕn(cos⁡θnI^+sin⁡θnJ^)+[Re(1−f)21−(2f−f2)sin2⁡ϕn+Hn]sin⁡ϕnK^=[Re1−e2sin2⁡ϕn+Hn]cos⁡ϕn(cos⁡θnI^+sin⁡θnJ^)+[Re(1−e2)1−e2sin2⁡ϕn+Hn]sin⁡ϕnK^ or Rn=recos⁡ϕn′cos⁡θnI^+recos⁡ϕn′sin⁡θnJ^+resin⁡ϕn′K^ where,

  • Rn is the respective observer position vector (in Equatorial Coordinate System)
  • Re is the equatorial radius of the central body (e.g., 6,378 km for Earth)
  • re is the geocentric distance
  • f is the oblateness (or flattening) of the central body (e.g., 0.003353 for Earth)
  • e is the eccentricity of the central body (e.g., 0.081819 for Earth)
  • ϕn is the geodetic latitude (the angle between the normal line of horizontal plane and the equatorial plane)
  • ϕn′ is the geocentric latitude (the angle between the radius and the equatorial plane)
  • Hn is the geodetic altitude
  • θn is the local sidereal time of observation site

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