Figure 3.
Oscillation of the angle θ in two models: with the entire Earth potential and with pure two-body model. Here the time-span is about three months and the inclination and semimajor-axis difference are correspondingly $i=30^{\circ }$, δa0 = 1 km.

Oscillation of the angle θ in two models: with the entire Earth potential and with pure two-body model. Here the time-span is about three months and the inclination and semimajor-axis difference are correspondingly |$i=30^{\circ }$|⁠, δa0 = 1 km.

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