From: tkelso@afit.af.mil (TS Kelso) Subject: Two-Line Element Set Questions Keywords: Satellite, Orbital Elements, Keplerian Organization: Air Force Institute of Technology Date: Thu, 9 Dec 1993 07:36:37 GMT Why is it that separate element sets are generated for both STS-61 and the Hubble Space Telescope (HST) when they are docked together? Why aren't these element sets identical? Since these questions have come up several times during the STS-61 mission to service the Hubble Space Telescope and arise from time to time with regard to the Mir space station, I thought I'd take this opportunity to answer them in some detail here. NORAD has responsibility for tracking all man-made objects in earth orbit. In performing this function, NORAD maintains a catalog of each individual it tracks, even if that object is subsequently docked to another object. Such is the case for STS-61 and the HST or the various modules of the Mir space station (Mir, Kvants 1 and 2, Kristall, and various Soyuz and Progress). And they also maintain separate element sets for each object. Of course, these objects are physically locked together and the observations collected for one object could be used for updating the elements for all objects. But that's not necessarily how it works. Since NORAD has to track over 7,000 objects every day, the process is automated. Here's how it works. Observations are collected for an object and used to generate a two-line element set using a process known as differential corrections. The two-line element set is used to predict the observations (using the SGP4 orbital model) and the differences between actual and predicted observations are compared. A correction to the two-line element set is determined which moves to minimize these differences (something like doing a multi-dimensional Newton search). This process is repeated until convergence is reached. The element set generated by this process will be used until subsequent observations show its predictions to be off by more than some preset amount. For the data I make available, that is five kilometers (90 percent confidence interval). Five kilometers may seem like a large distance until you realize that most of the error will be in the in-track direction and that it amounts to less than one second's travel in near-earth orbits. Once the current element set is determined to be out of tolerance, a new element set is generated. Now, since all observations have error, the element sets generated will remain in tolerance for differing periods of time. How long will depend on the site used to collect the observations, the viewing geometry, changes in atmospheric density or spacecraft attitude, maneuvers, and so on. As such, updates to separate components of a docked structure will be updated at different times. Okay, so even if NORAD tracks each object separately and maintains separate element sets, why are the element sets different? To understand the answer to this question requires a basic understanding of satellite orbits. Only ideal orbits describe true ellipses and have constant orbital elements. Real orbits experience both periodic and secular (trending) effects in their elements. Because of this, there are various ways of describing orbital elements. One way is to use osculating (touching) or instantaneous orbital elements, that is, the instantaneous values of each element at the specified epoch (time). The other is to use mean orbital elements. The NORAD two-line element sets use mean orbital elements. In *neither* case will the elements generated be constant over time. In the SGP4 orbital model, the mean is extracted in a particular way to not only allow combination with the various perturbing forces (geopotential, atmospheric drag, solar/lunar gravitational effects, and solar radiation pressure) to generate accurate predictions but to also permit quick calculations (it is an analytical model which means you can plug in a time and get out a position and velocity *without* numerical integration). To develop a better understanding of this concept, try to describe the mean x and y position of an object traveling along a circle. Taken over a long enough period of time, it is the origin of the circle -- not terribly useful. To be more specific, you must specify a time associated with your mean -- change the time and you change the mean. Therefore, if two or more objects are docked together in earth orbit, their orbital elements will not match unless the epoch of the element sets are identical. And even that assumes the elements were generated from identical observations with identical update processes. However, predictions of each object's position and velocity, using the NORAD SGP4 orbital model, should be the same within the error tolerance. Remember, I did not develop this process but am only explaining it. While I can think of ways to improve it, you must also remember that it has evolved slowly over time and is resistant to radical changes (as is any bureaucracy). You may be thinking that it would make more sense to generate only one element set for a group of docked objects, realizing that the error in prediction can be on the order of five kilometers! You might think that a single element set would result in no error. However, the error is still there -- a single element set just seems more consistent. Actually, multiple element sets provide the advantage of redundancy -- protecting you from the occasional bad element set. Before I quit, I'd like to take this opportunity to explain why it is important to use an orbital prediction program based upon the NORAD SGP4 orbital model when using the two-line element sets. As with fitting any kind of data, the coefficients determined depend upon the model used. Imagine a set of points (with noise) that you want to fit a curve to and determine the constant term. If you use a linear fit, you get one value; a quadratic fit yields another; and a cubic fit yet another. If you take the value for the cubic fit and apply a linear projection, you won't get very good results. The same is true for the NORAD two-line element sets. If you take the mean values from these element sets (the constant terms) and put them into a different orbital model (say, a simple two-body model), you won't get very good predictions. Likewise, if you take some other data (for example, the AMSAT data) and "convert" it to the two-line format, that does NOT make it two-line data compatible with the SGP4 model. I *strongly* discourage people from converting other data into the two-line format, particularly if you are reposting it, because the two-line format implies that the data was generated with the NORAD SGP4 orbital model and will produce compatible results. You will cause other users a great disservice by distributing converted two-line element sets since they will *not* produce accurate predictions. I have made, and will continue to make, every effort to make NORAD two-line element sets and the associated orbital models available to the satellite community. I welcome you to take advantage of these materials to produce the most accurate predictions readily available. I hope this answer your questions. - TS -- Dr TS Kelso Assistant Professor of Space Operations tkelso@afit.af.mil Air Force Institute of Technology