NASA NTRS · 19780048604
The intermediate anomaly
Abstract
Time transformations of the equation dt = cr to the n ds, where s is a variable called the intermediate anomaly, are known to reduce global error in the solution of gravitational systems obtained by numerical integration. Attention is given to the Sundman time transformation, and its relation to equations of Keplerian elliptical motion.
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Nacozy, P.. 1977-11-01. The intermediate anomaly. https://ntrs.nasa.gov/citations/19780048604
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