从全局球面模型到调整局部矩形调和模型的转换

IF 1.4 4区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS
Georgios Panou, Romylos Korakitis
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引用次数: 1

摘要

本文提出了一种将全局球面模型转换为调整后的局部矩形调和模型的方法。首先,给出了全局球谐模型的数学形式。其次,给出了从全局(地心)坐标到局部直角坐标的必要转换。第三,在局部直角坐标系下用分离变量法求解拉普拉斯方程,给出了不同函数形式下的拉普拉斯方程解。然后,以地球重力场扰动势值为数据,用最小二乘平差法对这些数学模型的系数进行估计。在不同的案例研究中描述并验证了为成功的转换选择最佳数学模型的策略。这些是指希腊、中国和德国的地区,包括与其他模型或方法的比较。结果表明了所提出的改造方法的适用性和优越性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Transformation from a global spherical to an adjusted local rectangular harmonic model

Transformation from a global spherical to an adjusted local rectangular harmonic model

This work presents a technique to transform a global spherical to an adjusted local rectangular harmonic model. First, the mathematical form of a global spherical harmonic model is presented. Second, the necessary conversion from global (geocentric) into local rectangular coordinates is given. Third, Laplace’s equation is solved by the method of separation of variables in local rectangular coordinates and its solutions in different functional forms are presented. Then, the estimation of the coefficients of these mathematical models by a least squares’ adjustment process is described, using as data the values of the disturbing potential of the Earth’s gravity field. The strategy for the selection of the best mathematical model for a successful transformation is described and validated in different case studies. These refer to areas in Greece, China and Germany and include comparisons with other models or methods. The results show the applicability of the presented transformation and confirm its advantages.

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来源期刊
Acta Geodaetica et Geophysica
Acta Geodaetica et Geophysica GEOCHEMISTRY & GEOPHYSICS-
CiteScore
3.10
自引率
7.10%
发文量
26
期刊介绍: The journal publishes original research papers in the field of geodesy and geophysics under headings: aeronomy and space physics, electromagnetic studies, geodesy and gravimetry, geodynamics, geomathematics, rock physics, seismology, solid earth physics, history. Papers dealing with problems of the Carpathian region and its surroundings are preferred. Similarly, papers on topics traditionally covered by Hungarian geodesists and geophysicists (e.g. robust estimations, geoid, EM properties of the Earth’s crust, geomagnetic pulsations and seismological risk) are especially welcome.
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