Droctagonopus said:
Thank you all for your replies.
Can you explain or link a resource explaining what measurements are made and how they are made and what calculations are then performed to determine the orbital parameters? Thanks in advance.
Time, elevation, azimuth, and range for each observation.
Convert your spherical coordinates to Cartesian.
Then transform your Cartesian to geocentric coordinates.
From the geocentric coordinates of each observation, you can determine the velocity vector for the middle vector using the Gibbs method - provided each observation is at least 5 degrees apart. It's essentially solving simultaneous equations to find a velocity that would result in all three observations, but it's done using vectors.
Converting from spherical to Cartesian is simple.
Coordinate transformations are more involved and require knowing how to do matrix multiplication.
The Gibbs method is very involved to use and even harder to follow how it was developed. The essence of the Gibbs method is comparing the area encompassed by a chord and the secant line joining the ends of the chord to the difference in the three radii. This solves for the eccentricity of the orbit (which is what the procedure was originally designed for). The remainder of the procedure is to determine the velocity vector (a process easier to understand if you've looked at orbital velocity hodographs) and numerous algebra steps (except with vectors) to isolate what you're solving for. It helps to understand vector algebra (cross products, dot products, etc).
All three processes are detailed in
Vallado's Fundamentals of Astrodynamics and Applications. There's probably a slew of other books that include the process. Vallado also details just about all of the other methods, including angles only, how to handle situations where separation is less than 5 degrees (initial observations of a newly discovered comet, for example), etc.
About the only ones I'd try to include in a short reply would be the spherical to Cartesian conversion, but why bother when you need a real book to do the rest.