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Precise local quasigeoid modelling using GNSS/levelling height anomalies and gravity data

机译:使用GNSS /水平高度异常和重力数据进行精确的本地拟胶质建模

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This study compares four approaches of local quasigeoid modelling using GNSS/levelling height anomalies. The first two approaches utilise only a dense network of points with known GNSS/levelling height anomalies and the EGM2008 model. They are based on the interpolation of residual values of height anomalies by applying the least squares collocation (LSC) and the thin plate spline (TPS). The next two approaches use additional data in the form of surface gravity data and the digital elevation model. One of these approaches is based on the classical Molodensky method combined with LSC. The other approach utilises the method of geophysical gravity data inversion (GGI). During the research, the authors used a local network of points with precisely defined GNSS/levelling height anomalies located in South-Western Poland. They obtained comparable results for all tested approaches at the maximum analysed density of GNSS/levelling points (about ). The differences between the modelling results became apparent only with an increase in the distance between the GNSS/levelling data points and the reduced accuracy of the used global geopotential model.
机译:本研究比较了使用GNSS /水平高度异常的局部拟胶质建模的四种方法。前两种方法仅利用具有已知的GNSS /调平高度异常和EGM2008模型的密集点网络。它们通过施加最小二乘搭配(LSC)和薄板样条(TPS)来基于高度异常的剩余值的插值。接下来的两种方法使用表面重力数据和数字高度模型的形式使用附加数据。其中一种方法是基于经典的Molodensky方法与LSC结合。另一种方法利用地球物理重力数据反转(GGI)的方法。在研究期间,作者使用了一个位于波兰西南部的精确定义了GNSS /水平高度异常的当地点。它们在GNSS /调平点(约)的最大分析密度下获得了所有测试方法的可比较结果。建模结果之间的差异仅随着GNSS /划分数据点之间的距离和所使用的全局地球势模型的降低精度的增加而变得显而易见。

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