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

被引:3
|
作者
Zingerle, P. [1 ]
Pail, R.
Scheinert, M. [2 ]
Schaller, T. [2 ]
机构
[1] Tech Univ Munich, Inst Astron & Phys Geodesy, Munich, Germany
[2] Tech Univ Dresden, Inst Planetare Geodasie, Dresden, Germany
关键词
Antarctica; combined gravity field modelling; fast synthesis method; global geopotential model; gravity field; SPHERICAL-HARMONICS;
D O I
10.1515/jogs-2019-0004
中图分类号
TP7 [遥感技术];
学科分类号
081102 ; 0816 ; 081602 ; 083002 ; 1404 ;
摘要
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 worstcase 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 effectscan usually be detected, small-scale errors (e.g. of single points) are mostly untraceable due to the uncertainties within the topographic model.
引用
收藏
页码:29 / 40
页数:12
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