Handling Four Systematic Effects in Three Gravimetric Geoid Determination Methods from a Viewpoint of the Centimetre-Precise Geoid

IF 7.1 2区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS
R. Goyal, S. J. Claessens
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引用次数: 0

Abstract

Over the past few decades, calculating a cm-precise geoid has been a major pursuit of geodesists. Numerous geoid modelling methods exist because geoid modelling theory was necessarily developed with some assumptions, which are handled differently by respective research groups. In the literature, numerous papers discuss in detail the theory of (aspects of) any one computational method. There are also numerous papers with empirical comparisons between different geoid modelling methods, where differences in excess of 1 cm are typically found. Almost all previous studies simply provide numerical comparisons of final geoid models, but more work is required to find out what causes the discrepancies. This study reviews the similarities and dissimilarities among three different geoid modelling methods: the approach followed at Curtin University of Technology, the Stokes-Helmert method, and the method of Least Squares Modification of Stokes formula with additive corrections. These methods may provide varying solutions due to, including but not limited to, choices of parameters and freely available data (Global Geopotential Models, Digital Elevation Models), kernel modifications, handling of the dataset (gridding, merging, interpolation etc.), etc. However, only the four following aspects are covered in this paper, i.e. the handling of 1) topographic masses, 2) atmospheric masses, 3) the ellipsoidal shape of the Earth, and 4) downward continuation. The major motivation behind this study is that with the pursuit of the cm-precise geoid, different geoid modelling methods should agree with one another within a given threshold because methods differ primarily in handling the discussed four aspects. Therefore, this study reviews these four aspects and compares them to identify the possible causes of discrepancies between the geoid modelling methods. Further, since no numerical comparisons are available on handling these corrections individually in different methods, this paper compares the mathematical formulations and suggests strategies as a roadmap to quantify the identified discrepancies among the methods.

Abstract Image

从厘米级大地水准面角度处理三种重力大地水准面确定方法中的四种系统效应
在过去的几十年里,计算一个厘米精度的大地水准面一直是测地线学家的主要追求。由于大地水准面建模理论必须在一些假设的基础上发展,因此存在许多大地水准面建模方法,而各个研究小组对这些假设的处理方式不同。在文献中,许多论文详细讨论了任何一种计算方法的理论(方面)。还有许多论文对不同的大地水准面建模方法进行了经验比较,其中通常发现差异超过1厘米。几乎所有以前的研究都只是简单地提供最终大地水准面模型的数值比较,但需要做更多的工作来找出导致差异的原因。本文综述了三种不同的大地面线建模方法的异同点:科廷理工大学采用的方法、Stokes- helmert方法和Stokes公式的最小二乘加性修正方法。这些方法可能会提供不同的解决方案,包括但不限于,参数的选择和免费提供的数据(全球地势模型,数字高程模型),核修改,数据集处理(网格化,合并,插值等)等。但本文只涉及以下四个方面,即1)地形质量的处理,2)大气质量的处理,3)地球椭球形状的处理,4)向下延拓的处理。本研究的主要动机是,随着对厘米精度大地水准面的追求,不同的大地水准面建模方法应该在给定的阈值内彼此一致,因为方法的差异主要体现在处理所讨论的四个方面。因此,本研究综述了这四个方面,并对它们进行了比较,以确定大地水准面模拟方法之间差异的可能原因。此外,由于在不同方法中单独处理这些修正时没有数字比较,因此本文比较了数学公式,并建议作为路线图的策略来量化方法之间已确定的差异。
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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