Evaluation of terrestrial and airborne gravity data over Antarctica – a generic approach

IF 0.9 Q4 REMOTE SENSING Journal of Geodetic Science Pub Date : 2019-01-01 DOI:10.1515/jogs-2019-0004
P. Zingerle, R. Pail, M. Scheinert, T. Schaller
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引用次数: 3

Abstract

Abstract The AntGrav project, funded by the German Research Foundation (DFG) has the main objective to homogenize and optimize Antarctic gravity field information. Within this project an evaluation procedure is needed to inspect all different kind of gravity field surveys available in Antarctica. In this paper a suitable methodology is proposed. We present an approach for fast 3D gravity point data reduction in different spectral bands. This is achieved through pre-calculating a fine 3D mesh of synthesized gravity functionals over the entirety of the Antarctic continent, for which two different global models are used: the combined satellite model GOCO05s for the long-wavelength part, and the topographic model Earth2014 for the shorter wavelengths. To maximize the applicability separate meshes are calculated for different spectral bands in order to specifically reduce a certain band or a selected combination. All meshes are calculated for gravity anomalies as well as gravity disturbances. Utilizing these meshes, synthesized gravity data at arbitrary positions is computed by conventional 3D interpolation methods (e.g. linear, cubic or spline). It is shown that the applied approach can reach a worst-case interpolation error of less than 1 mGal. Evaluation results are presented for the AntGG grid and exemplary for the in-situ measurements of the AGAP and BAS-LAND campaigns. While general properties, large-scale errors and systematic effects can usually be detected, small-scale errors (e.g. of single points) are mostly untraceable due to the uncertainties within the topographic model.
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评估南极洲地面和空中重力数据。一种通用方法
由德国研究基金会(DFG)资助的antgravity项目的主要目标是对南极重力场信息进行均匀化和优化。在这个项目中,需要一个评价程序来检查南极洲现有的所有不同种类的重力场调查。本文提出了一种合适的方法。提出了一种不同光谱波段的三维重力点数据快速约简方法。这是通过预先计算整个南极大陆合成重力函数的精细三维网格来实现的,其中使用了两种不同的全球模型:长波部分使用组合卫星模型GOCO05s,短波部分使用地形模型Earth2014。为了最大限度地提高适用性,对不同的光谱波段分别计算网格,以便有针对性地减少某一波段或选定的组合。所有网格都是根据重力异常和重力扰动计算的。利用这些网格,通过传统的三维插值方法(如线性、三次或样条)计算任意位置的合成重力数据。结果表明,该方法的最坏情况插补误差小于1 mGal。给出了AntGG网格的评估结果,并举例说明了AGAP和BAS-LAND运动的现场测量结果。虽然一般性质、大尺度误差和系统效应通常可以检测到,但由于地形模型的不确定性,小尺度误差(例如单点误差)大多无法追踪。
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来源期刊
Journal of Geodetic Science
Journal of Geodetic Science REMOTE SENSING-
CiteScore
1.90
自引率
7.70%
发文量
3
审稿时长
14 weeks
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