Analytical Solutions for Gravitational Potential up to Its Third-order Derivatives of a Tesseroid, Spherical Zonal Band, and Spherical Shell

IF 4.9 2区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS
Xiao-Le Deng, Nico Sneeuw
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引用次数: 0

Abstract

The spherical shell and spherical zonal band are two elemental geometries that are often used as benchmarks for gravity field modeling. When applying the spherical shell and spherical zonal band discretized into tesseroids, the errors may be reduced or cancelled for the superposition of the tesseroids due to the spherical symmetry of the spherical shell and spherical zonal band. In previous studies, this superposition error elimination effect (SEEE) of the spherical shell and spherical zonal band has not been taken seriously, and it needs to be investigated carefully. In this contribution, the analytical formulas of the signal of derivatives of the gravitational potential up to third order (e.g., V, \(V_{z}\), \(V_{zz}\), \(V_{xx}\), \(V_{yy}\), \(V_{zzz}\), \(V_{xxz}\), and \(V_{yyz}\)) of a tesseroid are derived when the computation point is situated on the polar axis. In comparison with prior research, simpler analytical expressions of the gravitational effects of a spherical zonal band are derived from these novel expressions of a tesseroid. In the numerical experiments, the relative errors of the gravitational effects of the individual tesseroid are compared to those of the spherical zonal band and spherical shell not only with different 3D Gauss–Legendre quadrature orders ranging from (1,1,1) to (7,7,7) but also with different grid sizes (i.e., \(5^{\circ }\times 5^{\circ }\), \(2^{\circ }\times 2^{\circ }\), \(1^{\circ }\times 1^{\circ }\), \(30^{\prime }\times 30^{\prime }\), and \(15^{\prime }\times 15^{\prime }\)) at a satellite altitude of 260 km. Numerical results reveal that the SEEE does not occur for the gravitational components V, \(V_{z}\), \(V_{zz}\), and \(V_{zzz}\) of a spherical zonal band discretized into tesseroids. The SEEE can be found for the \(V_{xx}\) and \(V_{yy}\), whereas the superposition error effect exists for the \(V_{xxz}\) and \(V_{yyz}\) of a spherical zonal band discretized into tesseroids on the overall average. In most instances, the SEEE occurs for a spherical shell discretized into tesseroids. In summary, numerical experiments demonstrate the existence of the SEEE of a spherical zonal band and a spherical shell, and the analytical solutions for a tesseroid can benefit the investigation of the SEEE. The single tesseroid benchmark can be proposed in comparison to the spherical shell and spherical zonal band benchmarks in gravity field modeling based on these new analytical formulas of a tesseroid.

Abstract Image

曲面、球带和球壳三阶导数的重力势解析解
球壳和球带状是重力场建模中常用的两种基本几何形状。将球壳和球带状带离散成曲面时,由于球壳和球带状带的球对称性,可以减小或消除曲面叠加的误差。在以往的研究中,对球壳和球带状带的叠加误差消除效应(SEEE)没有重视,需要认真研究。在这篇文章中,当计算点位于极轴上时,推导了曲面三阶(例如V, \(V_{z}\), \(V_{zz}\), \(V_{xx}\), \(V_{yy}\), \(V_{zzz}\), \(V_{xxz}\)和\(V_{yyz}\))重力势导数信号的解析公式。与先前的研究相比,这些新的曲面表达式推导出了球形带引力效应的更简单解析表达式。数值实验中,在卫星高度为260 km的不同三维高斯-勒让德正交阶(1,1,1)到(7,7,7)以及不同网格尺寸(\(5^{\circ }\times 5^{\circ }\)、\(2^{\circ }\times 2^{\circ }\)、\(1^{\circ }\times 1^{\circ }\)、\(30^{\prime }\times 30^{\prime }\)和\(15^{\prime }\times 15^{\prime }\))下,比较了单个曲面与球带带和球壳的引力效应的相对误差。数值结果表明,对于离散成曲面的球形带状带的重力分量V、\(V_{z}\)、\(V_{zz}\)和\(V_{zzz}\), SEEE不发生。在总体平均值上,对球面带状带离散成曲面的\(V_{xxz}\)和\(V_{yyz}\)存在叠加误差效应,而对\(V_{xx}\)和\(V_{yy}\)存在叠加误差效应。在大多数情况下,SEEE发生在离散成曲面的球壳上。综上所述,数值实验证明了球带状带和球壳的SEEE存在,而曲面的解析解有利于SEEE的研究。基于这些新的曲面解析公式,可以在重力场建模中与球壳基准和球带基准进行比较,提出单曲面基准。
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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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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