Far-Zone Effects for Spherical Integral Transformations II: Formulas for Horizontal Boundary Value Problems and Their Derivatives

IF 4.9 2区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS
Michal Šprlák, Martin Pitoňák
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Abstract

Integral formulas represent a methodological basis for the determination of gravitational fields generated by planetary bodies. In particular, spherical integral transformations are preferred for their symmetrical properties with the integration domain being the entire surface of the sphere. However, global coverage of boundary values is rarely guaranteed. In practical calculations, we therefore split the spherical surface into a near zone and a far zone, for convenience, by a spherical cap. While the gravitational effect in the near zone can be evaluated by numerical integration over available boundary values, the contribution of the far zone has to be precisely quantified by other means. Far-zone effects for the isotropic integral transformations and those depending on the direct azimuth have adequately been discussed. On the other hand, this subject has only marginally been addressed for the spherical integral formulas that are, except for other variables, also functions of the backward azimuth. In this article, we significantly advance the existing geodetic methodology by deriving the far-zone effects for the two classes of spherical integral transformations: (1) the analytical solutions of the horizontal, horizontal–horizontal, and horizontal–horizontal–horizontal BVPs including their generalisations with arbitrary-order vertical derivative of respective boundary conditions and (2) spatial (vertical, horizontal, or mixed) derivatives of these generalised analytical solutions up to the third order. The integral and spectral forms of the far-zone effects are implemented in MATLAB software package, and their consistency is tested in closed-loop simulations. The presented methodology can be employed in upward/downward continuation of potential field observables or for a quantification of error propagation through spherical integral transformations.

Abstract Image

球面积分变换的远区效应 II:水平边界值问题公式及其导数
积分公式是确定行星体产生的引力场的方法论基础。其中,球面积分变换因其对称性而受到青睐,积分域为整个球面。然而,很少能保证边界值的全局覆盖。因此,在实际计算中,为了方便起见,我们用球面帽将球面分为近区和远区。近区的引力效应可以通过对现有边界值进行数值积分来评估,而远区的引力效应则必须通过其他方法精确量化。各向同性积分变换的远区效应以及取决于直接方位角的远区效应已经得到充分讨论。另一方面,对于球面积分公式(除其他变量外,也是后向方位角的函数),这一主题的讨论还很有限。在本文中,我们通过推导以下两类球面积分变换的远区效应,大大推进了现有的大地测量方法:(1) 水平、水平-水平和水平-水平-水平 BVPs 的解析解,包括它们与各自边界条件的任意阶垂直导数的泛函;(2) 这些泛函解析解的空间(垂直、水平或混合)导数,直至三阶。远区效应的积分和频谱形式在 MATLAB 软件包中实现,并在闭环模拟中测试其一致性。提出的方法可用于势场观测值的向上/向下延续,或通过球形积分变换对误差传播进行量化。
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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