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7. Comparison with previous investigations

We attempted to repeat the integrations of the other investigators based on the information provided in their publications but were successful only with Rose's orbit (the measure of success was our ability to closely reproduce the published residual statistics). Failure in the other two cases is most likely due to the inability of our software to duplicate the perturbations included by the other investigators. One problem with the Bec-Borsenberger and Rocher integration is that they did not give the value of Titan's mass used in their Titan perturbation.

We were able to match Rose's orbit because he provided state vectors at both the beginning and end of his integration; we adjusted his initial velocities slightly to ensure that our integration matched his initial and final positions. The integration was performed in the FK4/B1950 system with solar perturbations computed using JPL planetary ephemeris DE102 (Newhall et al. 1995). Rose fit his orbit to 133 observations which he had converted to the FK4/B1950 system. He included the converted observations in his paper but did not provide details of his conversion procedure. He found a standard error of 1tex2html_wrap_inline225152; our reproduction of his orbit gives a standard error of 1tex2html_wrap_inline225146 for those published FK4/B1950 observations. For the pre-1970 observations that we used our work, the respective standard errors for our orbit and Rose's orbit are 1tex2html_wrap_inline225140 and 1tex2html_wrap_inline225178; for the post-1970 observations, they are 0tex2html_wrap_inline225160 and 1tex2html_wrap_inline225132. The root-mean-square of the differences between our orbit and that of Rose over the time period 1966-2001 are 4248 km in the radial direction, 10121 km in the in-orbit direction, and 3405 km in the out-of-plane direction.

Except for the Arequipa data, Bykova and Shikhalev and Bec-Borsenberger and Rocher fit essentially the same observations. Like Rose, each pair of investigators converted the observations to the FK4/B1950 system before processing. Bykova and Shikhalev give a standard error of 1tex2html_wrap_inline22515 (with some unspecified subset of the Arequipa data included), and Bec-Borsenberger and Rocher quote tex2html_wrap_inline3875 and tex2html_wrap_inline2271 errors of 1tex2html_wrap_inline22517 and 1tex2html_wrap_inline22512, respectively. For the pre-1982 observations used our work, our orbit yields respective errors tex2html_wrap_inline3875 and tex2html_wrap_inline2271 of 1tex2html_wrap_inline225156 and 1tex2html_wrap_inline225100.

Bec-Borsenberger and Rocher give sets of polynomial coefficients from which geocentric astrometric positions can be computed for the years 1981-1990 based on their orbit. From those polynomials we constructed positions for the first of January of each of those years and compared them to computed positions from our orbit. In the comparison we assumed that the constructed positions were in the reference frame of DE102, the planetary ephemeris used in the analysis, and transformed them with the published rotation between the J2000 frame and that of DE102. The rms of tex2html_wrap_inline3875 and tex2html_wrap_inline2271 residuals are 0tex2html_wrap_inline225126 and 0tex2html_wrap_inline225130. It appears that our new orbit agrees with that of Bec-Borsenberger and Rocher at a level better than our current orbit accuracy.


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