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Accuracy Analysis of Geopotential Coefficients Recovered from In-situ Disturbing Potential by Energy Conservation Method

机译:利用能量守恒方法从原地扰动势中回收地势系数的精度分析

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摘要

The characteristics of the normal equation created in recovering the Earth gravity model (EGM) by least-squares (LS) adjustment from the in-situ disturbing potential is discussed in detail. It can be concluded that the normal equation only depends on the orbit, and the choice of a priori gravity model has no effect on the LS solution. Therefore, the accuracy of the recovered gravity model can be accurately simulated. Starting from this point, four sets of disturbing potential along the orbit with different level of noise were simulated and were used to recover the EGM. The results show that on the current accuracy level of the accelerometer calibration, the accuracy of the EGM is not sufficient to reflect the time variability of the Earth's gravity field, as the dynamic method revealed.
机译:详细讨论了通过从原位扰动电位进行最小二乘(LS)调整来恢复地球重力模型(EGM)时创建的法线方程的特性。可以得出结论,正规方程仅取决于轨道,而先验重力模型的选择对LS解没有影响。因此,可以精确地模拟恢复的重力模型的准确性。从这一点开始,模拟了沿轨道的四组具有不同噪声水平的扰动电位,并将其用于恢复EGM。结果表明,如动态方法所示,在当前加速度计校准的精度水平上,EGM的精度不足以反映地球重力场的时间变化。

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