利用移位球面谐波在布里渊球面以下绕行

David Cunningham, Ryan P. Russell, Martin W. Lo
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摘要

恩克拉多斯南极附近的航天器轨迹违反了与球谐波模型收敛半径相关的布里渊球。在这项研究中,我们展示了一个移动坐标框架,以确保在运行感兴趣的区域提供收敛模型。在一个模拟天体周围进行了假设实验,该天体的真实外部重力场是完全已知的。证实了未偏移模型的布里渊球以下谐波发散,而偏移谐波模型收敛。接下来,我们将该方法应用于卡西尼得出的土卫二重力场,包括不确定性。使用这些低度和低阶参考模型(预计用于运行环境),结果表明,在地表或地表以上的所有评估中,移位谐波模型和以身体为中心的谐波模型都接近机器精度,没有发现任何偏差。这些结果表明,任务设计人员和导航工程师可以放心地在恩克拉多斯使用传统的球面谐波场,即使在布里渊球面以下的区域也是如此。对于前往除 "恩克拉多斯 "之外的其他天体的低空飞行任务,可以重复本研究中进行的实验。对于越来越多的非球形天体和布里渊球内更深的轨道,更需要传统球面谐波的替代方法,如提出的移动模型。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

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Orbiting below the Brillouin sphere using shifted spherical harmonics

Spacecraft trajectories near the south pole of Enceladus violate the Brillouin sphere associated with the convergence radius of spherical harmonics models. In this study, a shifted coordinate frame is demonstrated to ensure a convergent model is available in regions of operational interest. Hypothetical experiments are performed around a simulated celestial body where the truth exterior gravity fields are known exactly. The divergence of the harmonics below the Brillouin sphere of the unshifted models is confirmed, while the shifted harmonics model converges. The method is next applied to the Cassini-derived gravity field for Enceladus, including uncertainties. Using these low-degree and low-order reference models, expected for use in an operational setting, the results show that the shifted and body-centered harmonics models agree to near machine precision for all evaluations at or above the surface, and no divergence is noticed. The results imply that mission designers and navigation engineers can safely use a traditional spherical harmonics field for Enceladus, even in regions that dip below the Brillouin sphere. For low-flying missions to celestial bodies besides Enceladus, the experiments conducted in this study can be repeated. The need for an alternative to the traditional spherical harmonics, such as the presented shifted model, increases for bodies that are increasingly non-spherical and orbits that are deeper inside the Brillouin sphere.

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