Concept

Gauss's method

Summary
In orbital mechanics (a subfield of celestial mechanics), Gauss's method is used for preliminary orbit determination from at least three observations (more observations increases the accuracy of the determined orbit) of the orbiting body of interest at three different times. The required information are the times of observations, the position vectors of the observation points (in Equatorial Coordinate System), the direction cosine vector of the orbiting body from the observation points (from Topocentric Equatorial Coordinate System) and general physical data. 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. 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: or where, is the respective observer position vector (in Equatorial Coordinate System) is the equatorial radius of the central body (e.g., 6,378 km for Earth) is the geocentric distance is the oblateness (or flattening) of the central body (e.g., 0.003353 for Earth) is the eccentricity of the central body (e.g., 0.081819 for Earth) is the geodetic latitude (the angle between the normal line of horizontal plane and the equatorial plane) is the geocentric latitude (the angle between the radius and the equatorial plane) is the geodetic altitude is the local sidereal time of observation site The orbiting body direction cosine vector can be determined from the right ascension and declination (from Topocentric Equatorial Coordinate System) of the orbiting body from the observation points via: where, is the respective unit vector in the direction of the position vector (from observation point to orbiting body in Topocentric Equatorial Coordinate System) is the respective declination is the respective right ascension The initial derivation begins with vector addition to determine the orbiting body's position vector.
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