Abstract

AbstractA method has been implemented and tested for estimating bias and scale factor parameters for all six individual accelerometers that will fly on-board of GOCE and together form the so-called gradiometer. The method is based on inclusion of the individual accelerometer observations in precise orbit determinations, opposed to the baseline method where so-called common-mode accelerometer observations are used. The method was tested using simulated data from a detailed GOCE system simulator. It was found that the observations taken by individual accelerometers need to be corrected for (1) local satellite gravity gradient (SGG), and (2) rotational terms caused by centrifugal and angular accelerations, due to the fact that they are not located in the satellite’s center of mass. For these corrections, use is made of a reference gravity field model. In addition, the rotational terms are derived from on-board star tracker observations. With a perfect a priori gravity field model and with the estimation of not only accelerometer biases but also accelerometer drifts, scale factors can be determined with an accuracy and stability better than 0.01 for two of the three axes of each accelerometer, the exception being the axis pointing along the long axis of the satellite (more or less coinciding with the flight direction) for which the scale factor estimates are unreliable. This axis coincides with the axis of drag-free control, which results in a small variance of the signal to be calibrated and thus an inaccurate determination of its scale factor in the presence of relatively large (colored) accelerometer observation errors. In the presence of gravity field model errors, it was found that still an accuracy and stability of about 0.015 can be obtained for the accelerometer scale factors by simultaneously estimating empirical accelerations.

Highlights

  • The gravity field and steady-state ocean circulation explorer (GOCE) will be the first European Space Agency (ESA) core earth explorer mission

  • Each accelerometer experiences different accelerations due Use has been made of simulated GOCE observations to the local satellite gravity gradient and due to rotational (April 2008) from a comprehensive End-to-End simulator

  • A separate orbit determination is carried out during which biases, drifts and scale factors can be estimated for all three axes

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Summary

Introduction

The gravity field and steady-state ocean circulation explorer (GOCE) will be the first European Space Agency (ESA) core earth explorer mission. The X axis is aligned with the long axis of the satellite, the Z axis is perpendicular to the X axis and is aligned with the wings of the GOCE satellite, and the Y axis completes an orthonormal frame. The orientation of these axes is derived from star tracker observations The gradiometer will observe local satellite gravity gradients with high precision in a measurement bandwidth (MB) of 0.005–0.1 Hz. In addition, GOCE will be equipped with a dual-frequency Lagrange GPS receiver (Banfi et al 2000) for precise orbit determination and for providing information of the longer wavelengths of the earth’s gravity field.

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