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7.2.2 Parametrization of Reference Motion
Traditionally, an orbital ellipse in a spherically symmetric potential is parametrised
using Kepler parameters
ξ= [
a e I ω Ω M ]T
. (7.2.30)
Numerical tests have shown that this parametrisation for the reference trajectory is not
sufficiently stable when using standard double precision arithmetic. This statement
is supported by the results later presented in section 7.3.2. This instability could
potentially be remedied by computing all parameters relating to the reference trajectory
in quadruple precision arithmetic, and then converting the computed state at each
epoch to double precision for the further steps. It is undesirable to port the complete
orbit integration algorithm to quadruple precision arithmetic, as this is sure to lead to
significant performance penalties, with expected slowdowns on the order of a factor of
5 to 10 (Bailey and Borwein, 2015).
Another solution is to parametrise the reference motion with a more stable set of
orbital elements. Here, the equinoctial elements
ξe= [
a h k p q λ ]T
(7.2.31)
asgiveninBrouckeandCefola (1972)areanattractiveoption. In theseelements, a is the
semi-major axis of the ellipse. The elements h and k define the eccentricity and perigee
of the orbit. The elements p and q encode the inclination of the orbital plane and
the position of the ascending node.λ is the classical mean longitude. The equinoctial
elements are a non-canonical set of orbit elements, with the Poincare´ elements their
canonical counterpart (Vallado and McClain, 2001). Danielson et al. (1995, Section
2.1) gives a concise but comprehensive introduction to their derivation and use. The
transformation from an equinoctial state vector to a Cartesian state vector can mostly
be performed without relying on the evaluation of trigonometric functions, making
this transformation very numerically stable.
In this work all computations relating to the equinoctial elements are performed in
double precision arithmetic, with the exception of the computation ofλ, the mean
longitude. This is the fast-moving variable defining the position of the satellite along
the equinoctial orbit arc.λ is computed and stored in quadruple precision. Asλ is not
used in any expensive operations, the impact on overall performance is negligible. With
this parametrization and implementation, the conversion from equinoctial elements
to Cartesian coordinates shows sufficiently high stability. The results presented in
sections 7.3.3 and 7.3.4 illustrate this statement.
7.2.3 Determination of Best-Fit Orbit
To determine the best-fit Kepler ellipse from eq. (7.2.27), the partial derivatives of
the position and velocity of the satellite in the CRF w.r.t. the equinoctial elements are
Chapter7 Numerical Optimization in Orbit
Integration86
Contributions to GRACE Gravity Field Recovery
Improvements in Dynamic Orbit Integration, Stochastic Modelling of the Antenna Offset Correction, and Co-Estimation of Satellite Orientations
- Titel
- Contributions to GRACE Gravity Field Recovery
- Untertitel
- Improvements in Dynamic Orbit Integration, Stochastic Modelling of the Antenna Offset Correction, and Co-Estimation of Satellite Orientations
- Autor
- Matthias Ellmerr
- Verlag
- Verlag der Technischen Universität Graz
- Ort
- Graz
- Datum
- 2018
- Sprache
- englisch
- Lizenz
- CC BY 4.0
- ISBN
- 978-3-85125-646-8
- Abmessungen
- 21.0 x 29.7 cm
- Seiten
- 185
- Schlagwörter
- Geodäsie, Gravitation, Geodesy, Physics, Physik
- Kategorien
- Naturwissenschaften Physik
- Technik