Evaluation Procedures for the Potential Harmonic Coefficients of a Generally Shaped Polyhedron

IF 4.9 2区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS
Georgia Gavriilidou, Dimitrios Tsoulis
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Abstract

Two computational strategies for the evaluation of the spherical harmonic coefficients of the gravitational potential due to a generally shaped homogeneous polyhedral source are examined in detail. The techniques are implemented numerically for the known asteroid shape models of Eros and Didymos. The aim of the investigation is to quantify specific numerical aspects of the two algorithms, such as the accuracy of the techniques compared to a closed analytical solution for varying distance between source and computation point, the band-limited spectral analysis of the obtained spherical harmonic models and the convergence behavior of the corresponding series expansion in the vicinity of the characteristic Brillouin sphere. From a computational point of view, the line integral approach demands approximately three times the CPU time of Werner’s method. The two sets of spherical harmonic coefficients are 100% correlated up to degree 45 for Eros and up to degree 49 for Didymos. Approaching degree 100, the correlation by degree decreases by 0.0004% for Eros and by 0.004% for Didymos, the corresponding values for the correlation by order being 0.0002% and 0.304%. Inside the Brillouin sphere and approaching its boundary, the numerical agreement of the gravitational potential between the line integral method and the analytical solution is at the 1E-4 level, while with Werner’s approach at the 1E-7 level. At a distance of 33.5 km outside the Brillouin sphere for Eros and 2.2 km for Didymos, both methods are identical, reaching an agreement level with the analytical solution of 1E-11 level for Eros and 1E-14 for Didymos. In terms of spherical harmonic representation, the series defined by the line integral approach converges faster to the analytical value for the gravitational potential by 4 degrees.

Abstract Image

Abstract Image

一般形状多面体势调和系数的评定方法
详细研究了评估一般形状的均质多面体源引起的引力势的球谐波系数的两种计算策略。这些技术是针对已知的厄洛斯和狄迪莫斯小行星形状模型进行数值计算的。研究的目的是对两种算法的具体数值方面进行量化,如在源和计算点之间的距离变化时,与封闭式分析解相比,两种技术的准确性;对所获球谐模型的带限频谱分析;以及在特征布里渊球附近相应序列展开的收敛行为。从计算角度来看,线积分方法所需的 CPU 时间大约是维尔纳方法的三倍。两组球谐波系数在厄洛斯(Eros)的 45 度以内和狄迪莫斯(Didymos)的 49 度以内是 100% 相关的。在接近 100 度时,Eros 和 Didymos 的度相关性分别降低了 0.0004%和 0.004%,阶相关性的相应值分别为 0.0002%和 0.304%。在布里渊球内部和接近其边界的地方,线积分法和解析解之间的引力势数值一致性达到了 1E-4 的水平,而维尔纳方法则达到了 1E-7 的水平。在布里渊球外 33.5 千米的距离(厄洛斯)和 2.2 千米的距离(狄狄莫斯),两种方法完全相同,厄洛斯与分析解的一致性达到了 1E-11 的水平,狄狄莫斯达到了 1E-14 的水平。就球面谐波表示法而言,线积分法定义的数列收敛速度比重力势能分析值快 4 度。
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来源期刊
Surveys in Geophysics
Surveys in Geophysics 地学-地球化学与地球物理
CiteScore
10.00
自引率
10.90%
发文量
64
审稿时长
4.5 months
期刊介绍: Surveys in Geophysics publishes refereed review articles on the physical, chemical and biological processes occurring within the Earth, on its surface, in its atmosphere and in the near-Earth space environment, including relations with other bodies in the solar system. Observations, their interpretation, theory and modelling are covered in papers dealing with any of the Earth and space sciences.
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