Abstract
In this paper, we propose a new reduced-dynamic (RD) method by introducing the second-order time-difference position (STP) as additional pseudo-observations (named the RD_STP method) for the precise orbit determination (POD) of low Earth orbiters (LEOs) from GPS observations. Theoretical and numerical analyses show that the accuracies of integrating the STPs of LEOs at 30 s intervals are better than 0.01 m when the forces (<10−5 ms−2) acting on the LEOs are ignored. Therefore, only using the Earth’s gravity model is good enough for the proposed RD_STP method. All unmodeled dynamic models (e.g., luni-solar gravitation, tide forces) are treated as the error sources of the STP pseudo-observation. In addition, there are no pseudo-stochastic orbit parameters to be estimated in the RD_STP method. Finally, we use the RD_STP method to process 15 days of GPS data from the GOCE mission. The results show that the accuracy of the RD_STP solution is more accurate and smoother than the kinematic solution in nearly polar and equatorial regions, and consistent with the RD solution. The 3D RMS of the differences between the RD_STP and RD solutions is 1.93 cm for 1 s sampling. This indicates that the proposed method has a performance comparable to the RD method, and could be an alternative for the POD of LEOs.
Highlights
The influences of the sampling interval and the a priori dynamic models on the accuracies of integrating the secondorder time-difference position (STP) of satellite will be analyzed according to the accuracy requirement of 0.01 m for the STPs, which is sufficient for the precise orbit determination (POD) of Low Earth orbiters (LEOs), such as gravity field and steady-state ocean circulation explorer (GOCE) [37]
Differing from the traditional dynamic/RD method and the kinematic method, we propose a new reduced-dynamic method for the POD of LEOs using GPS code and carrier phase observations
Given that the STP directly establishes the relationship between the position and acceleration of the LEOs, and can be and precisely computed from known dynamic models, we used it as an additional “pseudo-observation” equation for the dynamic constraint on the kinematic POD observation equation
Summary
Publisher’s Note: MDPI stays neutral with regard to jurisdictional claims in published maps and institutional affiliations. Low Earth orbiters (LEOs) have been widely applied in Earth observation systems, such as remote sensing, ocean altimetry, atmosphere exploration, and Earth gravity field determination. The applications in these fields require high accuracy, reliability, and realtime performance of satellite orbits.
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