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Mathematical predictions must account for these orbital disturbances to provide space systems engineers with accurate spacecraft trajectory models.


Perturbations

Atmospheric drag is most prevalent in Low Earth Orbit (LEO) up to about 800 km. It is difficult to model, since atmospheric density changes drastically from activity in the magnetosphere and global temperatures that vary with day-night and seasonal tilt.

Earth's oblate shape skews gravitational force from that of a perfect sphere. This affects the right ascension of the ascending node and argument of perigee from the orbital elements.

Solar radiation pressure over a long period of time may result in uncommanded spacecraft rotation, which onboard attitude control systems must then dampen.

The Moon, Sun and planets cause third-body gravitational effects most evident on interplanetary transfers and orbits above LEO.

 

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